W.G. SMITHERINGALE & ASSOCIATES LTD.

1379 EXPLORATIdN PROGRAM

CASMO PRCPERTY, CASSIAR, B.C.

prepared fcr

SHELL CANADA RESOURCES LTD.

W.G. SMITHERINGALE & ASSOCIATES L T D .

4. D D l I 73-4 7 . DDll 79-7 10. DDlI 79-10 1. DI)ll 79-1

2 ” I)UII 79-2 5. DDlI 79-5 8 . DDl1 79-8 A . New Jersey Z i n c Cdrnp

3 . U1)Il 79--3 6 . D U I I 79-6 9 . D D l l 79-9 B. Crone Faul t GuIIey

m-1 Base Line ?-toutline of N . ] . Z , P i t .

?

TABLE OF CONTENTS

. Page -

S U M M A R Y LOCATlON A N D ACCESS

PROPERTY S I Z E , TOPOGRAPHY CLIMATE, VEGETATlON A N D SURFICIAL DEPOSITS

PREVIOUS EXPLORATION

1979 PROGRAM

C0i~fl:vl.ENTS ON DRlLL PROGRAM

REGlONAL GEOLOGY

PROPERTY GEOLOGY

L i t h o l o g y

Alteration

h i i n e r a l i za t ion

F rac tu res

F a u l t s a n d Brecc ia t ion

CONTROLS O F Ml NERALl ZATI ON

lNDUCED POLARlZATlON A N D MAGNETOMETER TEST SURVEY

ASSAY RESULTS

ORE RESERVES

RECOMMENDED EXPLORATlON

Drilling

Core L o g g i n g

14 a pp i n g

M Z o n e

C e o p h y si cs

G e o c h e m i s t r y

S t a k i n g

CERTI F l C A T ION

B 1 BL 1 OGRAP HY

1 Folio 1

3 11

II 3 6 6 7 8 9 9

1 2

1 3 1 4

20

21

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II

II

11

11

II

II

11

I,

11

II

II 23 23 26

2 7

2 7

2 8

2 8

2 9 30 30

30 31 3 2

I t

II

II

II

11

11

11

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II

II

II

II

FIGURES

P a g e

V 1. VIEW OF CASMO MoS2 PROPERTY

2. LOCATION

3. GEOLOGY

4. 5. SECTION 450-885, GEOLOGY.

6. SECTION 450-762, GEOLOGY

7. SECTION 450-643, GEOLOGY 8. SECTION 450-508, GEOLOGY



SECTION 451 -01 1 , GEOLOGY

11. VARIATION AMONG D R I L L HOLES OF ANGLES BETWEEN MoS2 FRACTURES AND CORE AXIS

12. DOWN HOLE HISTOGRAM OF NUMBER OF MoS2 FRACTURES AND % MoS2

1 7

19 13. SECTION 451-011 D R I L L HOLE ASSAYS

14. SECTION 452-885 D R I L L HOLE ASSAYS



1 7 . SECTION 451 -01 1 ORE RESERVE CALCULATIONS

18. SECTION 450-885 ORE RESERVES CALCULATIONS

19. SECTION 450-732 ORE RESERVES CALCULATIONS

20. SECTION 450-643 ORE RESERVE CALCULATIONS

w

21. APPARENT R E S I S T I V I T Y CONTOURS n = 1

22. APPARENT R E S I S T I V I T Y CONTOURS n = 2 23. APPARENT R E S I S T I V I T Y CONTOURS n = 3

'

Front isp iece , F o l i o 1

" 2

4 II

11

I 1

I 1

I1

I 1

I 1

11

1

2 11

II

I t

II

APPENDICES

I

I1 1979 ASSAY CERTIFICATES

111 L I S T OF PROPOSED 1980 D R I L L HOLES I V

1979 DIAMOND D R I L L HOLE LOGS SUMMARY OF L979 D R I L L HOLE DATA

L I S T OF WORKING DRAWINGS SUBMITTED UNDER SEPARATE COVER

V STATEMENT OF CASMO PROJECT: 1979 EXPENDITURES

- 3

33 'I 1 34 1 35 1

36 1

37 1

38 1 V I GEOPHYSICAL TEST RESULTS

SUMMARY

- 1. The Cass i a r h!oS2 proper ty l i e s i n mountainous t e r r a i n about

6 km. by d i r t road from the mining town of C a s s i a r , in

the Liard Mining Division of Northern B.C. C a s s i a r i s

connected b y ail-weather roads to the Alaska Highway

and to the seaport of Stewart , B.C., 3 0 km. to the southwest .

2. The deposi t is located in the C a s s i a r Stock, a ycung phase

( d a t e d a t 72 2 2.5 Ma) of the C a s s i a r i la thol i th . This stock

i s zoned a n d h a s a core of qua r t z - f e ldspa r po rphyry . Besides

the Casmo p rope r ty , the stock con ta ins two o ther po rphyry

type MoS2 showings a n d around i t s marg ins the re a r e s e v e r a l

s k a r n deposi ts conta in ing i ron a n d b a s e metal su lph ides ,

n a g n e t i t e , a n d in p laces c a r r y i n g Sn a n d W . Within the

thermal aureole in the the ad jacen t limestone t h e r e a r e

s e v e r a l Pb-Zn-Ag ve ins .

3. In the Casmo deposit bios2, the oniy s ign i f i can t o re mine ra l ,

occurs mainly in th in q u a r t z s t r i n g e r s with or without p y r i t e .

The s t r i n g e r s occupy s e v e r a l s e t s of f r a c t u r e s , bu t the main

mineral ized set s t r i k e s e a s t e r l y a n d d i p s nor thward . The

minera l iza t ion occurs in ser ic i t ized a n d poss ib ly fe ldspa th ized

qua r t z - f e ldspa r porphyry i the core rock 1 a n d ove r ly ing

K-feldspar po rphyr i t i c , biot i te q u a r t z monzonite, i n p a r t

assoc ia ted with a no r the r ly d ipp ing contact zone between

the two host rocks , i n p a r t with the Crone Fau l t , which

cu t s both rock types , a n d in p a r t with s h e a r e d , brecc ia ted

and/or in tense ly ser ic i t ized zones i n the q u a r t z monzonite.

Specific p r imary ore controls h a v e not been recagnized.

4 . The 15.179 explora t ion program inc luded geological mapping ,

r ehab i l i t a t ion a n d re logging of about 5000 m. of old diamond

d r i l l core a n d 2154 m. of NQ d i a m m d dr i l l i r?g . A l l 1379 d r i l l core was sp l i t i n 10 f t . sec t icns a n d a s s a y e d for to t a l

Mo a s h f 0 3 , a n d s9me samples were a s s a y e d for oxide Lfo,

Ag, Au a n d W .

- L -

5. Drill indicated reserves r e c o v ~ r a i , ) ~ ~ b y open plt n;in!ilg

a r e Pstimated a s 50.7 million tonnes of C.I375;1 McS, L w1:h a

waste: ore r a t i o of 1.1:l.

6. The dril l program recommended for 1980 comprises of 5415 m .

of h'Q d r i l l i n g within the a r e a of known mineral izat ion :o

f u r t h e r d e t a i l g r a d e and tonnage , a n d 3190 m . of NQ d r i l l i n g

to explore for extensions of mineral izat ion.

- 3 -

1979 EXPLOD.TlON PROGRAM

CASMO PROPERTY - CASSIAR, BRlT.1SH COLUMBlA

LOCATION AND ACCESS

The Casmo molybdenite proper ty is located a t 59'14 ' 3 O " N L a l . ,

and 129°51'2L"W Long., about 6 km. from C a s s i a r i n the L ia rd

idining Division, B.C. ( F i g . 2 ) . Access is b y four wheel d r i v e

vehicle on a d i r t road from Cass i a r . C a s s i a r i s a n asbesros

mining town of about 2000 conzected b y al l -weather roads

to Watson Lake, Y . T . (160 km., 1OC m i . ) on the Alaska Highway

and to S tewar t , B.C. (540 km., 335 m i . ) . Stewart i s a seapor t

through wnich the asbes tos f ib re from Cass i a r Mine is sh ipped .

PROPERTY SIZE, TOPOGRAPHY, CLIMATE, VEGETATION A N D SURFlClAL DEPOSITS

The Casmo proper ty optioned from New Je r sey Zinc Ltd. b y

Shell Canada Resources Ltd. i n the s p r i n g of 1979 consis ted

of the SQE, KON a n d West claim g roups ( F i g . 2 ) . During the

summer cf 1979 the Alta 6 a n d 8 claims were s t aked a n d l a t e

i n the f a l l of 1979 the Storie 1, 2 , 3, 4 a n d 5 c la ims were

purchased from Placer Development Ltd. The SQE, KON a n d

West g r o u p s were s t a k e d on the old two post system a n d the

other c la ims were s t a k e d on the modified g r i d system. The

to ta l a r e a of the present Casmo proper ty is approximate ly 2822

hectares (6975 a c r e s ) . The main showings, where most of the

explora t ion work to d a t e h a s been done, a r e on the SQE 13, 14 , 15, 15, 17 a n d 18 claims a n d cn the KON 3 , 4 a n d 5 claims.

The proper ry l i e s i n r cgged rnoun!ainous t e r r a i n with a maximum

re l ie f , from Lang Creek to the 649.3 foat peak on t h e West c la im

g r c u p $ G f L23 rn. (2700 r t . j .

Tree l i n e i s about 1300 m. ( 4 2 6 5 f t . 1 a n d the forest cover below

t h i s e leva t ion is mainly coniferous.

- 4 -

I I

I' *T-

59'15'

Spring. summer and f a l l ex tend from e a r l y June to i a t e October.

Average r a i n f a l l du r ing t h i s per iod i s LO cm. (16 i n c h e s ) ,

most of which f a l l s d u r i n g August, September a n d October.

June arid Ju ly a r e often sunny witn tempera tures in the r a n g e

of 23°C. Winter ex tends from l a t e October to May, d c r i n g which

ave rage temperatures a t the town of Cass i a r a r e in the r a n g e

-10 to -15OC. The ave rage ove ra l l snowfall a t Cass i a r is approx-

imately 295 cm. (116 i n . ) . The Cass i a r open p i t , which is at

a n elevat ion of 1830 m . (6000 f t . ) ope ra t e s throughout the win te r .

The main a r e a of i n t e re s t on the Casmo proper ty l i e s above

t imberl ine between 1400 m. a n d 1750 m. (4600 f t . a n d 5750 f t . ) .

The old New Jersey explora t ion camp is a t a n e leva t ion 01 1550 m . (5085 f t . ) . Most of t h i s a r e a is a gent le nor th f a c i n g

s lcpe , bu t i t s southern p a r t is a s teep south fac ing s lope

- a v e r a g i n g 33' (F ig . 1 ) . A network of rough roads provides access

to a l l of t h i s a r e a except the southwestern co rne r , W h l C I - i con-

s i s t s of rock cl i f fs . Strong winter winds prevent the accumula-

tion of much snow except i n the gu l l eys . However, the access

road from Cass i a r is normally blocked b y snowdrif ts u n t i l about

mid-June. I t could, however, e a s i l y be bulldozed c l e a r much

e a r l i e r a n d would be p a s s a b l e a s long a s d r a i n a g e d i tches

a r e well main ta ined .

The region h a s been g l a c i a t e d , bu t l i t t l e i f a n y t i l l remains

in the main a r e a of i n t e re s t . Most of i t is covered b y t a l u s

slopes or a mixture of t a l u s a n d soil on which a l p i n e g r a s s

a n d sca t te red s c r u b b r u s h grow. Soil prof i les a r e poorly deve-

loped. A n a l l u v i a l f a n , emanat ing from the gu l l ey through

which the eas t e rn extensioii of t he Crone Faul t p a s s e s , covers

p a r t of the eas t e rn s ide of the dr3w i n which the old New

Jersey Zinc camp is s i t u a t e d .

PREVIOUS EXPLORAT 10N

The first s ign i f i can t explora t ion on the Casno p rope r ty G a s

done in 1964 b y Casmo k i n i n g Ltd . , a s u b s i d i a r y of New Je r sey

Zinc Cn., a n d involved LLO f t . of t r ench ing , 50 p i t s a n d 11

d r i l l holes. Explorat ion b y Casmo hiining Ltd. cont inued in

1965 with d r i l l holes 12 to 18, i n 1966 with d r i l l holes 18A to

30 and in 1968 with d r i l l holes 31 to L8. The t o t a l footage

d r i l l ed to the end of the 1968 season was 22,307 f t . Ten r o t a r y

d r i l l holes to t a l l i ng 330 f t . were a l s o d r i l l e d , bu t the d r i l l i n g

a n d sampl ing techniques were found t o be unsa t i s f ac to ry . The

1964-1968 holes were BX o r BQ core a n d were d r i l l ed without

d r i l l i ng mud. Recoi.rery i n mineral ized i n t e r v a l s was a s l o w

a s 30%, a n d in m a n y cases w a s between LO a n d 85%.

In 1971 the Levana Explorat ion Co. , a s u b s i d i a r y of Cy2rus

iqines Ltd . , dr i l led four N Q holes to t a l l i ng 3163 f t . ( t h e C-71 s e r i e s ) . The f i r s t 100 f t . of Hole #1 was d r i l l e d without mud

a n d recovery was poor. The remainder of the holes were d r i l l e d

with mud a n d recovery a v e r a g e d 98-100%. Comparison of the

1971 holes with n e a r b y o lder holes ind ica t ed a n inc rease in

g r a d e with improved recovery. At the end of the 1971 program

the ore r e se rves mineable b y open p i t were est imated a s 50.6

million tons of d r i l l i nd ica t ed a n d p robab le ore with a n a v e r a g e

g r a d e of O . l Z 3 % MoS2 a n d a waste to ore r a t i o of 1.53:l. The

proper ty l a y id i e between 1571 a n d 1979.

THE 1979 PROGRAM

The 1970 program in the a r e a of the main showing r a n f r o m .

J u l y 20th to November 7 t h , a n a consis ted cf :

1. geologicai mapping ,

2. t es t I . P . a n d magnetometer s u r v e y s ,

3. a topographic s u r v e y loca t ing old a n d new d r i l l holes a n d ty ing the p rope r ty i n t o the na? iona l topographic g r i d ,

L . renabi i i ta i ic r i of about i5,OXl f t . of old , d i a m o n d d r i l l c a r e ,

5. construct ion of r a c k s for s to rage of c ld a n d nes; d r i l l core on the proper ty of B i l l S tor ie , where tne core will be access- ib le year-round,

6. 2154 m . (7066 f t . ) of N Q diamond d r i l l i n g ,

7. colour photographing cf a l l old and new core ,

8. logging old a n d new core ,

9. sampling of a i l 1979 core i n 10 f t . i n t e r v a l s .

A l l samples were a s sayed for t o t a l hlo. Severa l holes were

a s sayed for oxide Mo and Ag a n d one hole was a s sayed for

tungs ten and gold.

COMMENTS ON DRILL PROGRAM

The d r i l l crew a r r i v e d on August 28th a n d depa r t ed on October

18th. -Exc lud ing the time r equ i r ed to move t h e i r equipment on

a n d off the p rope r ty , they ave raged about 1000 f t . a week

runn ing two - twelve hour sh i f t s . Few hold-ups were encountered.

Dri l l ing mud was used throughout a n d was undoubtedly p a r t l y

respons ib le for good core reovery in most p l aces , even in incom-

pe ten t , f r a c t u r e d a n d shea red rock. The a v e r a g e core recovery

was about 97%, however, i t v a r i e d from about 50% to 100%.

Poor recovery occurred i n p laces i n both mineral ized a n d

unmineral ized rock over i n t e r v a l s up to 10 to 15 m . i n some

p 1 a c e s f r a c t u re s

were p a r t i a l l y ground, a:id a t times a b lack scum of molybdenite

was c l e a r l y v is ib le i n the mud t a n k s . Nevertheless, the core

recovered from most mineral ized zones is considered to be qui te

r ep resen ta t ive . Sludge samples were collected . from about ha l f

the holes , bu t these a r e not completely r ep resen ta t ive because

p rcpe r sample bags were not a v a i l a b l e . They ha.ve rlot been

a n a l y z e d . Cas ing was left i n a l l the holes . ?i summary of d r i l l

hole d a t a is g iven in Appendix I .

of a 1 mo s t 100% r e c ove r y m ol y b d en i t e- be a r i n g

REGIONAL GECLOGY. -

The Casmo p rope r ty is located i n the C a s s i a r Stock, which

l i e s a long the e a s t e r n edge af the Ea r ly to Middle Cretaceous

Cass i a r Bathcl i th i n the Omineca tectcnic be l t .

The Cass i a r Stock is a 32 x 13 km. (20 x 8 miles) ova l shaped

body t r end ing nor thward . I t is f lanked on the west b y the

Cass i a r Batholith a n d on the e a s t b y a Proterozoic a n d Lower

Palaeozoic shelf sequence of ca rbona te a n d c l a s t i c rocks t h a t

i t i n t rudes . I t is cons idered to be younger phase of t he C a s s i a r

Batholith a n d h a s been da ted a t about 72 2 2.5 hIa ( p e r s .

cornm. A. Panteleyev 1.

The stock is dominant ly q u a r t z monzonite. I t i s zoned a n d

the zones a p p e a r io g r a d e in to each o ther . The outermost zone

is megacrys t ic , K-feldspar po rphyr i t i c q u a r t z monzonite, the - middle zone is medium to coarse-gra ined , K-feldspar pc rphyr i t i c

q u a r t z monzonite c h a r a c t e r i s e d b y p lag ioc lase mantled K-feldspar

phenocrys ts a n d the core of the stock is p ink qua r t z - f e ldspa r

po rphyry with a f ine-gra ined groundmass ( p e r s . comrn. A.Panteleyevj .

The C a s s i a r Stock con ta ins th ree cen t r e s of 1.40 (W) minera l iza t ion ,

the Casmo p rope r ty , the C a s s i a r molybdenum prope r ty 5.3 krn.

( 3 . 3 miles) south of Casmo a n d s e v e r a l W-Mo showings north

of C a s s i a r or about 10 km. ( 6 miles) north of Casmo. The Casrno

a n d C a s s i a r molybdenum depos i t s occur in the p ink qua r t z -

f e ldspa r po rphyry core a n d the ad jacen t K-feldspar q u a r t z

monzonite. North of C a s s i a r most of the W-Mo minera l iza t ion

is s k a r n hosted, a l thoagn q s a r t z monzonite away from the contact

conta ins disseminated MoS2. Severa l small sulphide-magnet i te

s k a r n s occur a round the margin of the C a s s i a r Stock, i nc lud ing

two e a s t cf the Cclsrno prope r ty , cne of which c a r r i e s t ungs t en .

A.?ong :he e a s t margin of the siock in the g e n e r a l v i c in i ry

of the Casmo p rope r ty the re a r e s e v e r a l ga lena-sphaler i te -pyr i te

ve ins a n d s e v e r a l smal l galena-sphaler i te-magnet i te-pyri te

replacement depos i t s , t h a t conta in Sn or W va lues in

- 9 -

'CII places. The veins and replacement deposits occur in limestone

within the thermal aureole of the Cassiar Stock. The Cassiar

asbestos deposit lies in a fault bounded ultramafic body near

the east border o f the Cassiar Stock.

Dates on sericite and biotite associated with Mo mineralization

on the Casmo and Cassiar molybdenum properties are essentially

the same as dates on the stock itself, indicating that emplace-

ment and mineralization were part o f the same event (pers.

comm. A . Panteleyev).

Faults and shear zones in the vicinity o f the Cassiar asbestos

deposit fall into two groups, one striking easterly the other

striking northerly. Both sets dip steeply. The movement on

the east striking faults is north side down and west relative

to the south side. In the vicinity o f the Casmo property faults

trend east to slightly north of east and northerly. In the

Cassiar molybdenum and Rex areas faults trend east-northeast

and northerly.

PROPERTY GEOLOGY

Detailed mapping during the 1979 program was restricted to the area of the main showing, i.e. the SQE 1 3 , 14, 15, 16, 17 and 18 claims and the KON 4 and 5 claims. The following

description of the property geology refers only to that area.

Lithology

The property is underlain by four mappable intrusive rock

units (see accompanying geological map, Figure 3 , and geological

sections, Figures 5-10). Each unit comprises several different

- 13 -

phases , s x n e of i,-hick represen; s e p a r a t e in t rus ive pu l ses ,

some c rys t a i i za t i cn a n d flow d i f fe ren t ia t ion a n d scme,

p a r t i c u l a r l y in uni t 3. poss ib ly represent potassium metasomatism.

Unit 1 is a l ign t p inkish g r e y , dominant ly coarse-gra ined ,

K-feldspar po rphyr i t i c , b io t i te q u a r t z monzonite. I t gene ra l ly

conta ins l a r g e (to L cm.) K-feldspar phenocrys ts and q u a r t z

g r a i n s over 1 cm. in diameter ( a c t u a l l y aggrega te s of smal le r

q u a r t z g r a i n s ) , however, where these a r e absent or s p a r s e

the rock may be medium g r a i n e d a n d ind i s t ingu i shab le from

Unit 3. Pods of g r a n i t e pegmati te a r e a minor but common

component ( e . g . DH 79-10, 4-50 m . ) .

Unit 1 occurs a s a f a u l t bounded wedge s t r u c t u r a l l y above

uni t 2. An a l t e r ed or nonfaul ted contact between u n i t s 1 a n d

2 w a s observed i n only one outcrop , where un i t 1 seemed (wi th

some ques t ion) to be ch i l l ed a g a i n s t un i t 2. In the nor theas t

pa r r of the map-area un i t 1 con ta ins one ore more zones of

medium-grained q u a r t z monzonite t h a t h a s been mapped a n d

logged a s uni t 3. This zone is l i ke ly a phase of un i t 1 r a t h e r

t h a n a n in t rus ion of 3.

Unit 2 i s a l i gh t to medium g r e y , fine-to medium-grained, q u a r t z

and K-feldspar po rphyr i t i c q u a r t z monzonite cha rac t e r i zed b y

ve ry f ine-gra ined 'Tepper - l ike ' b io t i te i n addi t ion to the normal

fine-to-medium g r a i n e d b io t i te . The K-feldspar phenocrys ts a r e

1 to 2 cm. long a n d a r e g e n e r a l l y mantled with a r i m of white

sodic p lag ioc lase . Var ia t ions , which approach un i t 3 i n a p p e a r - ance , are s p a r s e l y po rphyr i t i c a n d e n t i r e l y medium-grained

or phases with ve ry l i t t l e , pepper b io t i te . These v a r i a t i o n s

a r e best seen in core f r o m DH's 24 a n d 2 9 , where phases h a v e

both g r a d a t i o n a l a n d s h a r p contac ts . Unit 2 a p p e a r s to be

a t a b u l a r body tha r l i e s s t r u c t u r a l l y above u n i t 3 a n d d i p s

gent ly sou?hward , except for the southernmost f a c l t s l i ce , which

d ips nor thward .

- I! -

un i t s L a n d

In p laces ,

1, unit 3 groundmass

numerous f

Unit 3 I s the mcsr commcn rock type in the map-area. 1 1 is

l igh t p inkish-grey , v a r i a t i y tex tured Du: domipant iy medium-

g r a i n e d , K-feldspar porphyr i t ic . biot i te q u a r t z monzonite. Grain

s ize v a r i e s from dox inan t ly f ine to dominant ly coa r se , a n d

tex ture f r c m nonporphyri t ic to s t rongly q u a r t z ( t o 1 cm. 1 a n d

K-feldspar ( t o 3 cm.1 pa rphyr i t i c . A common v a r i e t y i s mediun-

g r a i n e d a n d s p a r s e l y porphyr i t ic . Some K-feldspar phenocrys ts a r e

mantled. In p l aces , most noteably nea r i t s contact with un i t

2 , i t con ta ins some ve ry f ine-grained b io t i te a n d s t rong ly

resembles uni t 2. In d r i l l core different phases d i s p l a y g r a d a -

t ional , a b r u p t l y g r a d a t i o n a l or s h a r p contac ts . Biotite sch l ie ren

and a p l i t i c to q u a r t z - f e ldspa r po rphyry p h a s e s a r e p re sen t ,

espec ia l ly n e a r a b r u p t or s h a r p contacts . The contact with

uni t 2 is often marked b y a n a p l i t i c phase ( e . g . DH's 23, 32, 29, 30 a n d 79-21, which i s in te rpre ted a s a bo rde r phase

forriled b y f low different ia t ion. Unit 3 s t r u c t u r a l l y l i e s above

a n d north of uni t - 4 a n d the region occupied b y a mixture of

3.5 *

espec ia l ly ad jacent to or within reg ions of un i t

s d i s l inc t ly pink a n d h a s a fine-to medium-grained

conta in ing more pink K-feldspar t h a n u s u a l a n d

ne-grained, euhedra l q u a r t z g r a i n s . In p l aces i t

h a s the compisition of g r a n i t e . Fine-grained v a r i e t i e s a r e tex-

t u r a l l y g r a d a t i o n a l with type 4 , a n d in some d r i l l core t h i s

rock a p p e a r s to g r a d e in to uni t 4 . T h i s v a r i a n t h a s been

des igna ted e i the r uni t 3a or g r a n i t e , depending on compcsition.

I t is not known i f i t is a product of potassium a n d s i l i c a

metasomatism or of normal igneous d i f fe ren t ia t ion .

Unit 4 comprises pink quar tz - fe ldspar po rphyry , with a fine-

g r a i n e d groundmass and v a r i a b l y developed K-feldspar : ( u s u a l l y less t h a n 1 crn.), q u a r t z and p lag ioc lase phenocrys ts . Unit L conta ins lenses seve ra l m?tres ?hick of rock types 3s a n d 2 a n d sca t t e red pods of K-feldspar-quartz-biotite-muscovite pegEa-

t i t e . Unit 4 under l ies the south-central p a r t of t he map-area

and p robab ly much of the s lcpe south of i t . Drill core ind ica t e s

- 12 -

a zone of intermixed 5 m. to 3 C m . th ick b a n d s cf 2 , 3a dnd

3 under ly ing uni t 3 t h a t d i p s nor thward . Only a few of the

deeper holes a p p e a r to pene l r a t e rock t h a t i s dominant ly uni t 4 .

Thin, nor tner ly t rending a p l i t e dykes cu t u n i t s 1 , 2 a n d 3. However, m u c h of the a p l i t e encountered in d r i l l cere a ? p s a r s

to the wr i t e r to be border phase ma te r i a l or in t r a - in t rus ive

lenses formed by flow d i f fe ren t i&t ion .

Sketchy evidence f r o a the d r i l l core a n d reg iona l cons idera t ions

sugges t t h a t un i t 2 (peppe r b io t i te q c a r t z monzonite) i s the

oldest un i t a n d uni t L (qua r t z - f e ldspa r p o r p h y r y ) t he youngest

un i t .

P, 1 t e r a t i on

Alteration comprises wide-spread s l igh t to moderate se r ic i t iza t ion

of p l ag ioc la se , more local in tense se r i c i t i za t ion a n d kaol in iza t ion

of p lag ioc lase a n d K-feldspar accompanied b y des t ruc t ion of

b io t i te , widespread py r i t i za t ion both d isseminated a n d in f rac-

t u r e s , t he development of q u a r t z ve ins from a f rac t ion of a

mm. to 10 cms. th ick a n d the development of zoned, p ink potassium fe ldspar -green muscovite-quartz - p y r i t e b a n d s ad jacen t

gen t ly nor thward d ipp ing f r ac tu res . As nientioned above , t he re

is evidence to sugges t t h a t wholesale potassium msrasomatism

w a s rzspons ib le for some of the phases of qua r t z - f e ldspa r

porpnyry .

Pe rvas ive s i l i c i f ica t ion is no! common, a l though -0.5 to 2 m .

th ick zcnes were in te rsec ted by dr i l l i r ,g i n s evz ra l p l zces . Small pods up to 0.5 m . th ick of metasomatic pegmati:e coatair ,-

ing potassium f e l d s p a r , quGrtz, g reen muscovite and /o r Lioti te

a r e developed loca i iy , p r c b a b l y by the same process t h a t

developed the more widespread a l t e r a t ion b a n d s of s imi l a r

mineralogy.

' ? - 1,: -

Serici t izea p lag iocIas2 i s va r ious s h a d e s of green and h a s

v a r i a b l e h a r d n e s s . In g e n e r a l the d a r k e r green g r a i n s a r e

sof ter , a n d presumably such g r a i n s represent a more intense

degree of a l t e r a t ion . i r o n , ident i f ied a s a component of the

ser ic i te by electron microprobe a n a l y s i s ( 8 ) *, i s undoubtedly

respons ib le for the green colour. In p l aces p lag ioc lase is a l te red

opaque white with v a r y i n g degrees of sof tness . This type of

a l t e r a t ion h a s not yet been ident i f ied . K-feldspar a l t e r s to

se r ic i te a n d a c l a y mineral s imi la r to i n composition to kaol in i te

(81, a l s o conta in ing minor i ron. K-feldspar phenocrysts , w h i s h

a r e commonly l i gh t pink i n una l t e red rock , a r e g rey i sh p i n k ,

g rey a n d f i n a l l y green in inc reas ing ly a l t e r ed rocks.

Alterat ion was plotted on d r i l l sections, b u t no h o l e - t o - h o l e cc r r e l a t ion of a l t e r a t ion p a t t e r n s was d iscern ib le . Nor was zoning

recognized, o ther t h a n the presence of l e s s in-tense a l t e r a t ion

in the nor thern row of New Jersey Zinc d r i l l holes (e .g . , DH's 30, 35, 36, 4 3 , 47 a n d the upper por t ions of 38 a n d 39). This

less in tense a l t e r a t ion comprises p lag ioc lase a i t e r ed pa le green

a n d opaque white b u t remain ing h a r d , occass iona l i n t e r v a l s of una l t e red p l ag ioc la se a n d the absence of zones with both

f e ldspa r s in tense ly a l t e r ed a n d b io t i te destroyed. The re la t ion-

s h i p of minera l iza t ion to a l t e r a t ion i s d i scussed below.

Miner a 1 i za t ion

In a g e n e r a l sense minera l iza t ion occurs i n a nor thward clipping

zone t h a t outcrops along the top of the scclthern slope (e .g .

i n the v i c in i t i e s of d r i l l holes 79-1 a n d 79-4). I t h a s been

t r aced b y d r i l l i n g for about 500 m . i n a n E-W direct ion a n d for about 450 m . down d i p to the nor th . Miner5:ization

does not occur uniformly throughout bu; i n a number of s u b

zones t h a t a p p e a r to be t a b u l a r , s t r i k e e a s t e r l y a n d d i p ,iorth-

ward ( s e e r e se rve est imat ion sec t ions , Figs . 17 to 20).

"Refers to ( 3 ) in Bib l icgraphy.

- li -

Me5t rnc?!ybdenlie 15 fine g r a i n e d and occurs in 5 u a r t z s t r i n g e r s

or ve in l e t s C.1 t c 2 mn. th ick -6’ith or h,iti:ou? . p y r i t e . I t a l s o

occurs a s tn in smears on s l i p s , mechanically d i s b u r s e d i n f a u l t

gouge ( b l a c k c l a y s e a m s ) , in the q u a r t z cores of some K-feldspar

a l t e r a t ion b a n d s a n d to a minor extent a s small pockets of

disseminated molybdenite in quartz-feldspar porphyry a n d

r e l a t ed phases . Some coa r se rosette molybdenite occurs i n eas t e r ly

t rending q u a r t z veins south of t he g u l l e y through which the

Crone Fau l t pas ses .

To d a t e s ign i f i can t mineral izat ion h a s been found only within

the region containing i n t e r v a l s of soft green a n d opaque white

a l t e r e d plagioclase. However, within t h i s region good g r a d e

mineral izat ion may occur in rock containing sericiTized b u t s t i l l h a r d plagioclase. In sections 150-6L3E a n d C51-011E the

best mineral izat ion occurs i n the region of mixed u n i t s 3a a n d

L , bu t i n sections 450-762E a n d ~50-88jE the best mineral izat ion

occurs i n the s t r u c t u r a l l y h i g h e r un i t 3, where, i n a g e n e r a l

sense , it is close to or o v e r l a p s i n t e r v a l s i n which both feld-

s p a r s h a v e been intensely a l t e r e d a n d biot i te destroyed.

Frac tures

Considerable effort w a s pu t i n to the s t u d y of f r a c t u r e o r i en ta -

t ions a n d mineralogy. lnc luded in t h i s s t u d y were jo in t s ,

ve in l e t s (which formed b y f r a c t u r e f i l l i ng r a t h e r t h a n replace-

men t ) , s l ickensided s u r f a c e s , f a u l t gouge (b l ack c l a y ) seams

a n d I(-feldspar a l t e r a t ion b a n d s . Frac ture or vein le t f i l l i n g s

include q u a r t z , p y r i t e , molybdenite, green muscovite, gypsum

or a n h y d r i t e , ch lo r i t e , p ink K-feldspar a l t e r a t i o n ad jacent

to some f r a c t u r e s , s p a r s e f luz r i t e a n d b e r y l , a n d i n weathered f r a c t u r e s , l i non i t e a n d a secorrdary. car ia ry yel?cw nolybdenzm

mineral ( ferrimolybdcnite? ) . h!o!ybder.ite occurs iri f r a c t u r 2 s

aloile, with py r i t e and/or q u a r t z ar,d/or ad jacent p ink K-feldspa r

a l t e ra t ion a n d i n gouge seams, so only these s t r u c t u r e s a r e

discussed nere.

- 15 -

Three joint ( f r a c t u r e j se t s 6r-k developed rhrouzhout the map

a r e a , a n d in p laces a v a r i e t y of jo in ts , some p robab ly r e l a t ed

to f a u l t s , a r e loca l ly developed. The g e n e r a l a t t i t b d e s of the

dominant s e t s a r e : s t r i k e e a s t e r l y - d i p moderate no r thward ,

s t r ike e a s t e r l y - d i p s teep southward a n d s t r i k e no r the r ly - d i p ve r t i ca l . A l l se t s contain py r i t e , bu t the nor thward d ipp ing

set is the most in tense ly pyr i t ized .

Frac tures were mapped in de t a i l between d r i l l holes 79-4 a n d

C71-1 a n d the r e su l t s were compared with d a t a from d r i l l hole

23, one of the nea res t v e r t i c a l d r i l l holes with core in t ac t .

Of 61 jo in ts conta in ing e i the r p y r i t e , l imonite, q u a r t z or MoS2,Ly f a r the most h a d a n eas t -nor theas te r ly s t r i k e a n d a northwest-

ward d i p of between 4 5 O The other two dominant joint

se t s r e fe r r ed to above a r e preserlt, o u t only weakiy developed

in t h i s a r e a . In d r i l l hale 23, a v e r t i c a l hole 150 metres north

of the s t u d y a r e a , most of the MoS2 or pyr i t e b e a r i n g f r a c t u r e s

d i p 55' t o 80' . The s t rong predominance of eas t -nor theas te r ly

s t r i k i n g f r a c t u r e s i n the s t u d y a r e a a n d the good cor re la t ion

of d i p s between outcrops a n d core sugges t s t h a t mcst of the

mineral ized f r a c t u r e s in d r i l l hole 23 a l s o s t r i k e e a s t e r l y .

a n d B O o .

Before the 1979 d r i l l i n g program began i t w a s found t h a t old

v e r t i c a l l y d r i l l e d holes inc luded a number of mineral ized f rac-

t u re s t h a t in te rsec ted the core a x i s a t l e s s t h a n 15 , whereas

the 1971 hc le s , which were d r i l l e d a t a n inc l ina t ion of -60' in a d i rec t ion !70°, conta in few mineral ized f r a c t u r e to core

a x i s in te rsec t ions of l e s s t h a n 25 . Not only i s core conta in ing

f r ac tu res with l o w f r a c t u r e to core a x i s in te rsec t ions d i f f icu l t

to sample f a i r l y , bu t v e r t i c a l holes do not t a k e a s r ep resen ta t ive

a sample cf s teeply d ipp ing f r a c t u r e s a s do inc l ined holes,

provided the l a t t e r a r e d r i l l e d in the a p p r o p r i a t e direct ion.

I t was consequent ly dec ided , on the b a s i s of f r a c t u r e d a t a

from obtcrops a n d the C71 d r i l l ho les , t h a t the most a p p r o p r i a t e

or ien ta t ion f x the 1979 d r i l l holes would be -70° in a d i rec t ion 170°.

0

0

- 16 -

Frac ture d a t a f ron ;he 1979 holes show t n a t t h i s x i e n t a t i o n 1s

appropr i a t e i n t ha t r e l a t ive ly few mineral ized f r a c t u r e s in te rsec t

:he core a x i s a t l e s s t h a n 15 . 0

Frequency d is t r ibu t ion d i ag rams of mineral ized f r a c t u r e to care

a x i s in te rsec t ions for the 1979 holes show s e v e r a l consis tent

p a t t e r n s ( F i g u r e 11). MoSi b e a r i n g f r a c t u r e s in d r i l l holes

79-2, 3 a n d 5 s h o w a s t rong concentrat ion of in te rsec t ions in the

35O-50' r a n g e wi:h a mean of about 42'. I n d r i l l holes 79-1 a n d L ,

which l i e south of the previous. t h ree holes , :here a p p e a r s T O b e - two populat ions of MoS2 b e a r i n g f r a c t u r e s , one the same as

in d r i l l holes 79-2, 3 and 5 a n d the o ther between 50"-65Owith a

mean of about 57'. In d r i l l hoies 79-6 a n d 10, which l i e e a s t

of the prev ious f ive hc les , most of t he hloS b e a r i n g f r a c t u r e s

in te rsec t the core a x i s a t 6Oo-75O with a mean 01 about 67' a n d

the -35' -50' populat ion is r e l a t i v e l y small . These d a t a sugges t

t h a t t he re a r e seve ra l s e t s of MoS b e a r i n g f r a c t u r e s a n d t h a t

i n the th ree a r e a s s h o x n cn Figure 11 these se t s a r e develaped

to different degrees . The r a n g e of inc l ina t ion a n d azimuth

among the 1979 holes is only about 10' a n d is too smal l to

account for the p a t t e r n s shown i n F igure 11. The 35O-5Oo. set

of MoS2 bea r ing f r ac tu res p robab ly co r re l a t e s with the eas t -

nor theas t s t r i k i n g , 4.5' -80' nor thward d ipp ing , set of mineral-

ized f r a c t u r e s recognized on su r face . The p robab le or ien ta t ion

of the 5Oo-6j0 set a n d the 60°-750 set a r e unknown, however,

de ta i led f r ac tu re mapping in the th ree a r e a s shown i n F igure 11 may throw l igh t on t h i s subjec t . . Although the s igni f ica2ce

of the p a t t e r n s shown in F igure 11 a r e a t p re sen t unknown, the

wr i te r be l ieves t h a t i t migh? prove worthwhile to continlle

col lect ing :his type of d a t a .

2

2

c. l n e most coirimon assoc ia te of molybdenite is p y r i t e , as i n quartz-pyrite-hloS ve in le t s . Less common, b u t s t i l l important

occurrences, a r e in K-feldspar a l t e r a t i o n b a n d s a n d f au l t gouge

seams. Data from d r i l l hole 23 p a r t l y i l l u s t r a t e t h i s . Of the

2

- 1 7 -

-

r

CASMO MoS2 PROPERTY CASSIAR, B.C.; LIARD MINING DIVISION

- 1 - VARIATION AMONG DRILL HOLES OF

ANGLES BETWEEN MoSz FRACTURES

- l l - l - - /35-50- 50-65-

- ,T ,T !

DDH 79-3 (160’ at -7OO)

8

IO 20 30 40 SO SO 70 EO 90

Angle between fracture and core axis

To Y) W 0 = 60 t g so

t 240 El i;

5 x IO E

L =I 0

0

c 30

20 f L

z ’ o AND CORE AXIS Date: Fcb. 8 , I980

W. G. Smitheringale EI Associates Ltd.

1 do

2 DDH79-9 i (156Oat - 7 6 O ) r4(

z

z

Angle between f ra

nsufficient Data FIGURE I I

S H E L L C A N A D A R E S O U R C E S L I M I T E D

EXPLORATION - MiNERALS

- 16 -

:38 K ~ S ~ t lear ing f r a c t u r e s ( 8 3 ~ ~ c.f ;**~-iich h a v e dip-. cf - 5 j G - ~ ~ = ' ' ~ ~ - J

96SS conta in py r i t e . About P976 of thes? a r e simple MoS2-pyrite

- q u a r t z ve in le t s without 1;-feldspar a l t e r a t ion a n d 1Lb have

ad jacent K-feldspar a l t e r a t ion aureoles . There a r e two 7opula t ion s

of p y r i t e bea r ing f r ac tu res in d r i l l hole 23, one or ien ted 20 -

50@ to the core a x i s and the other 60@-80° to the core a x i s .

However, 78% of the py r i t e f r ac tu res conta in ing koS, f a l l withir,

the 2Oo-5O0 populat ion. There a r e a l s o two g roups of pyr i te -

MoS2 ve in l e t s with K-feldspar a l t e r a t ion au reo le s , one g roup

or iented 2j0-3j0, a n d a smaller g roup or ien ted €35' to the core

a x i s . The l a t t e r group p robab ly co r re l a t e s with the e a s t e r l y

s t r i k i n g , gen t ly nor thward d ipping K-feldspar a l t e r a t ion ve in le t s

commonly observed on sur face . Pe rhaps useful . information about

mineral pa ragenes i s a n d mineral izat ion h i s to ry could be ob ta ined

i f s imi l a r a n a l y s e s were made of f r a c t u r e d a t a a l r e a d y collected

for the 1979 d r i l l holes a n d some o lder ve r t i ca l holes.

i

0

-

- A comparison of the down-hole h is tograms of Moq f r a c t u r e dens i ty

and MoS a s s a y v a l u e s for DH79-3 ( F i g u r e 12) shows a cor re la t ion

between the two plots that supports the conclusion t h a t the most

important mode of occurrence of MoS2 i s i n f r ac tu res . For example, below 160 m . where MoS f r a c t u r e s a r e more a b u n d a n t ,

a s s a y v a l u e s in g e n e r a l a r e h igher . Spec i f ica l ly , some i n t e r v a l s .

of d i s t inc t ly h ighe r f r a c t u r e dens i ty h a v e cor respondingly h igh

a s s a y v a l u e s , e .g . at 245-250 m . , 285-295 a n d 330- 335 m . On the o ther h a n d , some i n t e r v a l s ha-.?€ a h igh a s s a y b u t low

f r ac tu re dens i ty . This is due to the presence of abnormal ly

thick MoS2 ve in le t s , e . g . , the i n t e r v a l 315-320 171. con ta ins

1 t3 10 cm. thick q u a r t z ve ins c a r r y i n g coarse rose t tes of )nos2.

-2

2

2

Frac ture logging should be cont inued in step-out d r i l l holes

tc e n s u r e t h a t a su i t ab le d r i l l hole inc l ina t ion is main ta ined .

An ex tens ive f r ac tu re s tudy of a l l new d r i l l holes might r e v e a l

zoning with respect to or ien ta t ion cf hIo5 f r a c t u r e s or wi?h

respect ta the mineralogy of the f r ac tu res . L

- 20 -

Faul t s a n d Brecciation

The map-area is cut by

070' and h a s a s t rong

a nor thward d ipp ing f au l t t h a t s t r i k e s

topographic express ion i n the gu l l ey

runn ing between DH's 22 a n d 79-L. Where t h i s f a u l t cu t the

intrusive-sediment contact e a s t of the p rope r ty i t s movement

is normal a n d i ts dip-s l ip component is about 100 m . This s t ruc-

t u re h a s been ca l l ed the Crone Faul t in prev ious repor t s . Another

eas t e r ly t r e n d i n g , nor thward d ipp ing f a u l t t h s t r u n s j u s t south

of the base l ine between 1W a n d LW is ind ica t ed b y su r face

mapping and b y consis tent offsets of the Unit 2 - Unit 3 contac t

in the geological sect icns .

Numerous gouge seams ( t h i n b l ack or d a r k g r e e n , c lay- l ike

seams) a n d s l ickens ided f r a c t u r e s a r e present i n d r i l l core

a n d a r e shown on the geological sect ions. They a r e so numerous

t h a t they a r e impossible t o co r re l a t e p rec i se ly from one hole

to another . However, i n p l aces in the sect ions where contac ts

bet-**een rock uriits a r e discont inuous i t is assumed t h a t f a u l t i n g

r a t h e r t h a n p r imary contact i r r e g u l a r i t i e s a r e respons ib le ,

a n d f a u l t s a r e d rawn i n to se rve a s a diagramma-

t i s r e sp resen ta t ion of probable f a u l t p a t t e r n s . This approacn

is jus t i f ied b y the fac t t h a t i n many p laces d r i l l hole in te r -

sect ions ind ica t e f a i r l y continiious a n d regular15 d ipp ing con-

t ac t s . Few of the f a u l t s shown d iagrammar ica l ly in the geologi-

c a l sect ions h a v e been ident i f ied on the su r face , however ,

where they h a v e they t r end e a s t e r i y a n d no r the r ly , i n g e n e r a l

agreement with the r eg iona l f au l t p a t t e r n .

Assuming the contact i r r e g u l a r i t i e s ind ica ted in geological sections a r e i a u l t r e l a t e d , the displacements on e a s t e r l y t rend-

ing f a u l t s is nor ths ide down r e l a t i v e t o sou ths ide , which is

the same a s for the Crape Faul t a n d for f a u l t s a t the C a s s i a r

asbes tos deposit . The a p p a r e n t displacement ac ross no r the r ly

t r end ing f a u l t s ind ica ted b y su r face mapping is r i g h t - l a t e r a l

for nor thward d ipp ing contac ts a n d l e f t - l a t e ra l for southward

- 21 -

dipping contac ts . This implies movement across ti:ese f a u l t s

of e a s t s ide down re l a t ive to west s ide . The movement on tne

e a s t e r l y t r end ing f au l t t h a t l i e s jus t south of t he base l ine

a p p e a r s to be ro ta t iona l i n t h a t south of it the contact between

un i t s 2 a n d 3 consis tent ly d ips northward a n d north of i t the

same contac t cons is ten t ly d i p s southward.

Breccia zones ad jacent to gouge seams and s l ickens ided f r a c t u r e s

a r e common in d r i l l core. Sone conta in obvious brecc ia f ragments

(macrobreccia in 1979 logs) a n d o thers consis t of a stockwork l i ke p a t t e r n of close spaced h a i r l i n e f r a c t u r e s t h a t d i sp l ace

g r a i n boundar i e s by only 1 or 2 m m . (microbreccia of 1979 l o g s ) . I n mineral ized i n t e r v a l s the randomly or ien ted f r a c t u r e s

in these brecc ia zones may conta in smears of MoS2 powder.

These in t ra -brecc ia zone f r ac tu res were not counted i n the

f r a c t u r e s tud ie s descr ibed above.

The presence of MoS2 powder mechanical ly d i spe r sed i n gouge

seams, of s l ickens ided MoS2 f r a c t u r e s a n d of MoS2 smears i n

brecc ia z m e s ind ica t e s t h a t s ign i f i can t f a u l t i n g occurred a f t e r

the inain per iod of mineral izat ion.

CONTROLS OF MINERALIZATlON

Clear cu t p r imary ore controls a r e not a p p a r e n t , o ther t h a n

the i n t e n s i t y of f r ac tu re development (especial ly e a s t e r l y t r end ing

nor thward d ipp ing f r ac tu res ) which must h a v e inf luenced the

d i s t r ibu t ion of mineral izat ion to some exten t .

Sornc s p a t i a l r e l a t ionsh ips of s ignif icar , t minera l iza t ion a r e :

i. Confinement to region of mixed soft a n d h a r d s e r i c i z a r i m

of p lag ioc lase (d iscussed under ' a l t e r a t i o n ' 1.

2 . Proximity a t depth to the Crone Faul t .

U 3 . hssociati<ln i:; some a r e a s w i y h tk,e .zone cf mixed L , 3 3 ,

a n d j rock types (d i scussed unde r 'minera l iza t ion ' ) . -

L . A tendency for mineral izat ion to b e in t he p r c x i z i t y of ,

b u t not necessar i ly coinciding wi th , zones of in tense f e ldsphr

ser ic i r iza t ion and des t ruc t ion of b io t i te (d i sccs sed unde r

' a l t e r a t i o n ' 1 .

5. Since zones of in tense a l t e r a t ion a r e u s u a l l y bounded by and /o r conta in gouge seams the re is a l s o a s p a t i a l re la i ion-

s h i p to f au l t i ng . However, t h i s is secondary because fo r

the m o s t p a r t mineral izat ion preceded f a u l t i n g . I t seems

t h a t zones suscept ib le to minera l iza t ion were a l s o , a t a

l a t e r s t a g e , suscept ib le to f a u l t i n g .

6. Although mineral izat ion is not excluded from rock un i t s

1 a n d 2 , r e l a t ive ly l i t t l e s ign i f i can t minera l iza t ion occurs

i n them.

- 23 -

- lNDUCED POLARlZATlON AND MAGNETOMETER TEST SURVEY

An I P a n d magnetometer su rvey were conducted over th ree l i nes

runn ing north for 700 metres a n d south for 500 metres from

base l ine s t a t ions O+OO, l+OOZ a n d 2+00E. The r e su l t s have been

reported b y Saydam ( 9 ) . He reported t h a t :

1. Chargeab i l i t y v a l u e s over the a r e a of minera l iza t ion a r e

uniforn;, i nd ica t ing a more or l e s s uniform su lph ide d i s t r i -

bu t ion .

2. Apparent r e s i s t i v i t y va lues a r e about 5 to 10 times l e s s

over the zone of mineral izat ion t h a n beyond i t , a n d t h a t

a s t h e electrode sepa ra t ion is increased the lowest point

' on tne r e s i s t i v i ty prof i les sh i f t s nor thward ind ica t ing a

nor thward d i p for the lower r e s i s t i v i ty zone. -

3. The magnetic f ie ld is h igh ly v a r i a b l e over t he zone of

minera l iza t ion re f lec t ing a n e r r a t i c d i s t r ibu t ion of magnet i te , poss ib ly due e i the r to the non-uniform des t ruc t ion of magnet-

i t e between zones v a r y i n s i n in t ens i ty of hydro thermal

a l t e r a t ion or to the non-uniform introduct ion of magnet i te

i n ve in le t s d u r i n g a l a t e s t a g e of minera l iza t ion . Saydam

conc 1 u des t h a t r e s i s t i v i ty a n d magnetometer s u r v e y s would

be useful i n the f u r t h e r explora t ion of the proper ty .

ASSAY RESULTS

A l l the 1979 core was sp l i t a n d sampled i n 10 foot i n t e r v a l s .

A l l the sdmples were a s sayed for t o t a l 140 a n d some were

a s sayed for oxide Mo, Ag9 Au, a n d W . For ssmples t h a t h a v e

both to t a l Mo a n d oxide Mo a n a l y s e s , MoS2 was ca l cu la t ed b y

s u b t r a c t i n g the oxide Mo from the to t a l Mo a n d mul t ip ly ing

the remainder b y 1.668. For sainples without oxide Mo a n a l y s e s

MoSf was ca l cu la t ed assuming the to t a l h i0 was present on ly

in the form of MoS2. The a s s a y r e su l t s a r e reported in terms

b

- 2L -

of Mc% i n the dril: logs a n d on the accompanyin'g a s s a y sect ions

(F igs . 13 to 16) . Assay cer t i f ica tes a r e submit ted in Appendix 11.

The fcllowing t a b l e summarizes the a n a l y t i c a l work.

Samples Analyzed b v Cnemex for : Hole - 79-1 79-2 79-3 79-4 79-5 79-6 79-7 79-8 79-9 79-10

Total Mo Oxide Mo

1-122

1-89 1-120f

1-58 1-73 1-39 1-2 j 1-29 1-49 1-89

1-122

1-89 1-120

1-53

1-45 -

- - - -

2 A i 1-121 -

10-5-120

4i-58 62-73 1-39 1-25 - -

- 79-x 1-61 ( r e m a i n i n g sp l i t of samples 29-89

* P u l p s submit ted to Min-En Labora tor ies Ltd. for check a n a l y s i s .

In s ign i f i can t amounts of oxide Mo were found in holes 1 to

5 except i n the top 20 m . of s e v e r a l holes where the

proport ion of oxide 140 t o t o t a l Mo v a r i e d e r r a t i c a l l y from

a few percent to 50%. Below 20 m. about 80% of the samples

c a r r i e d l e s s t h a n . O O l % oxide Mo, a n d the remainder c a r r i e d

.001%or .002% cxide Mo with only a few samples r u n n i n g 8 s

high a s .005% oxide Mo. I t was therefore decided t h a t a n a l y s e s

for oxide Mo were unnecessary .

P,g a n d A u a n a l y s e s were r u n cn some samples :.o determine

whether t he h igh Ag a n d Au a s s a y s reported from the t rench

Rear the DH 1 (R.C.hlacdonald, i n covering l e t t e r to Crones

1964 r e p o r t ) ex tend down dip . The r e su l t s w r r e nega t ive , a n d

the h igh a s s a y s repor ted in 1964 remain unexpla ined . .

.

The W ana lvses for D H 3 chow notk, i r ,q s ign i f i can? . However,

t r a c e element a n a l y s e s frcm one hole a i e Insuff ic ien? tc detect

zcr?:ng Q a t t e r n s .

The precis ion of the s p l i t t i n g a n d sampling procedure was checked

b y submit t ing the remain ing sp l i t of samples 29 to 89 of DH79-2

for a n a l y s i s . These samples were labe l led Di-iigX, samples 1 - 61. Samples 29 - 89 of D H 2 uniformly cover a r a n g e of va lues from

.012% to .5LO% MoS2. The two se t s of a s s a y s compare well. Differ-

ences a r e g r e a t e r for h ighe r v a l u e s , bu t the differences a r e

not cons is ten t ly h ighe r o r lower. For the 61 samples a n a l y s e d

those des igna ted DH79-2 a v e r a g e .086% MoS2 with a s t a n d a r d

deviat ion of .093, whereas those des igna ted DH79-X a v e r a g e

.087% MoS with a s t a n d a r d devia t ion of .085. 2

Analy t ica l accu racy w a s checked b y submit t ing a l l of the pu lps

p repa red by Chemex fo r DH79-3 to Min-En Laborator ies Ltd.

of North Vanccuver, B.C. for a n a l y s e s of t o t a l Mo a s MoS2. The r e s u l t s a r e g iven i n the following tab le .

% Difference 2 Min-En %MoS 2 Samples Chemex %MoS

1-120 0.117 (1170', 357m. ) 28-114 0.147 (870 ' , 265m. 1

61 samples a s s a y i n g l e s s t h a n

0.136 +16%

0.170 +16%

-07% MoS2 b y Chemex . . . . .+13%

The Min-En a s s a y s a r e cons s t en t ly h i g h e r , the difference n

ave rage MoS2 for the e n t i r e hole be ing +16%. The experience

of another Vancouver explora t ion office runn ing a major MoS2

program was s imi la r . They submit ted four p u l p s t o four different

l abora to r i e s (Chemex Labs Ltd . , General Test ing Labora tor ies ,

Rossbacher Labora tory a n d Min-En Labora tor ies Ltd. , a l l of

the Greater Vancouver a r e a ) . The r e s u l t s from Chemex were

lowest, from General Test ing in te rmedia te a n d from Rossbacher

and Min-En about e q u a l a n d h ighes t . Both Chemex a n d Min-

En use a type of hot perchlor ic ac id d iges t ion , bu t Chemex

uses a 2-gram sample a n d Min-En a 5-gram sample. The above

- 26 -

exercise did not check sample p r e p a r a t i c n , s ince the Chemex

pu lps were submit ted to hlin-En. The g rea t e s t . e r r o r s i n MoS2

a n a l y s i s a r e most l i ke ly to be due to f au l ty sample p r e p a r a t i o n .

l t is recommended t h a t f ive samples from DH79-3 cover ing tne

r a n g e of .@5% to .5% hloS2 be selected as s t a n d a r d s . About

1000 g m . of each s t a n d a r d should be pulver ized to provide

s t a n d a r d pu lps for per iodic submission to whatever l a b is

a n a l y s i n g Casmo samples in the fu ture . These p u l p s a n d the

s t a n d a r d sample re jec ts should be submit ted a n d resubmit ted

severa l times to four or f ive l abora to r i e s before the 1980 program

in order to select a l a b t h a t h a s both good sample p r e p a r a t i o n

and a n a l y t i c a l precis ion. The p repa ra t ion of s t a n d a r d s w i l l

be espec ia l ly useful i f d i f ferent l abora to r i e s a r e used d u r i n g

fu tu re explora t ion .

ORE RESERVES

Assay d a t a p r io r to 1979 was plot ted on a s s a y sec t ions d i r ec t ly

from a s s a y ce r t i f i ca t e s i n terms of MoS2 wherever possible .

In cases for which s e v e r a l a s s a y v a l u e s were a v a i l a b l e , a n d

in the few cases for which there w a s incomplete d a t a , a con-

se rva t ive approach w a s t aken . These d a t a a n d the 1979 a s s a y s

were then used to ca l cu la t e dri l l ind ica ted r e se rves b y the

s t a n d a r d weighted a v e r a g e method a n d b y assuming a r e a s a n d

volumes of inf luence ex tend ha l fway to the next sample sec t ion ,

with the exception of s e v e r a l small blocks t h a t were a s s i g n e d

smaller volumes of in f luence . The ca l cu la t ions a r e shown on

the accompanying ore r e se rve sect ions ( F i g s . 17-213).

The boundar ies of ore blocks i n each section were drawn assum-

ing a 0.07% MoS2 cut off, t h a t a s s a y hounds-ries a n d t r e n d s

gene ra l ly d i p moderately nor thward a n d t h a t i n t e r v a l s down

to 30 feet c a n be mined se lec t ive ly . An exac t matching of ore

block boundar i e s t o geological can tac t s a n d s t r u c t u r e s was

not a t tempted. A tonnage fac tor of 2.79 tonnes per C U . m . w a s

- 27 -

u s e d 19 the ca l cd la t i cns . Tkie r e s u l t s far the pit proposed b:j

Nex j e r sey Zine and fsr a 1979 modified p i t deepened a t t he

west end b y 85 m . (280 f t . ) t o e levat ion 1315 m . a r e shown

in following t ab le .

Total Vel. Tonnes Ore Grade h’aste: @re Ratio (cu.metres) )

NJZ Pit 35,262,000 LO, 874,000 C!. 130 1 . L : l

1979 P i t 39,62L, LOO 50.76 j,OOO* 0.137 1.1:l

*Using a tonnage fac tor of 2-85 tonnes/cu.m. g i v e s 53,585,000 tonnes.

RECOMMENDED EXPLORATION

The proper ty w a r r a n t s f u r t h e r d r i l l i n g both to more a c c u r a t e l y

determine the g r a d e a n d tonnage within the present ly known

body of mineral izat ion a n a tc explore for - f u r t h e r mineral izat ion

a t depth a n d to the eas t a n d west.

Drilling

1. Most of the drilling to further detail reserves within the

known area of mineralization should be done on sections

midways between, and parallel to, the present drill sections.

However, it would be worthwhile drilling several more holes

on existing sections and deepening several 1979 and C-71

holes if possible. The proposed holes, nos. 8 0 - 4 to 19, and

the holes to be deepened are shown on the geological plan

(Fig. 3 ) . They total 5 4 1 5 m. (17,761 ft.). They should be

drilled on an azimuth of 170 and an inclination of - 7 0 ° , the 0

c

sawe a s ior the !979 holes.

2 . The d r i l l holes recommended to explore the extension of

mineral izat ion to the e a s t a n d west a n d to depth a r e a l s o

shown on Figure 3 (holes 80-1 to 3 and 20 t o 2 5 ) . Tney

to ta l 3190 m . (10,463 f t . ) and should be d r i l l ed 170" a n d

-70°, a l though c a r e should be t aken to detect changes i n

a t t i t u d e of MoS2 f r a c t u r e s t h a t would r equ i r e chang ing the

the or ien ta t ion of the holes.

The to t a l 1930 d r i l l program recornmended is 25 new holes a n d

7 deepened holes for a t o t a l of 8605 m . (28 ,224 f t . ) . The longest

hole i s 500 m . (1640 f t . 1. Core s ize should be N Q a n d d r i l l i n g

muds should be used a t a l l times. A list of hole l eng ths is

given in Appendix 111.

- Core Logging

1. I t is recommended t h a t the core be colour photographed

a n d t h a t a l t e r a t ion a n d f r a c t u r e composition a n d o r i en ta t ion

d a t a be logged a s in 1979.. Gouge seams a n d brecc ia zones

should a l so be logged , however, i t is not necessa ry t o record

a i l the s l ickens ided slips. Even though the 1979 photos

a re a useful record , they lack consis tency in exposure ,

colour tone a n d focus, a n d t h e i r va lue would be g r e a t e r

i f the camera h a d been mounted closer t o the core. Con-

s i d e r a b e pre-field e f for t is jus t i f ied to improve the photo-

g r a p h y for 1980.

Mapping

1. Detailed mapping on a sca le of 1:IOOO snould be re f ined

s n d extended i n a n d beyond the south bo rde r of the 1379

map-area. F rac tu re or ien ta t ion mapping i n spot l oca l i t i e s

within the 1979 map-area would he a usefu l a i d t o in te r -

p re t ing d r i l l hole f r a c t u r e d a t a .

- 2 9 -

2. An attempt should be made to determine the displacement

across the eastern most northerly trending fault shown

in Fig. 3 .

3 . The entire property should be mapped on a scale of 1 : 5 0 0 0 ,

with local 1 :2000 scale mapping where required. Particular

attention should be given to tracing the contacts o f unit

4 and to identifying possible cupola areas in the roof of

unit 4 .

Ge op h y s i c s

Resis t ivi ty and magnetometer su rveys should be conducted over

1he 1.5 km. x 2 km. a r e a recammended by Saydam (91. Displace-

ment of the low points on the r e s i s t i v i t y prof i les i n the n o r t h e a s t

p a r t of the 1979 map-area may provide a c lue t o the displacement

across the nor ther ly t r end ing f au l t in t h a t v i c in i ty .

Geochern i s t r v

1. h stream s i l t su rvey should be conducted throughout the

expanded propert) ' , p a r t i c u l a r a t ten t ion be ing g iven to the

s t reams d ra in ing the north a n d south s ides of Lang Valley.

2. An or ien ta t ion soi l su rvey should be conducted over the

zone of known minera l iza t ion , a n d i f i t is successful a

soi l su rvey should be c a r r i e d cu t a long the nor thern slope

cf Lang Valley eas t a n d west of the known minera l iza t ion . - 3. A tes t program is recommended to determine i f t r a c e q u a n t i t i e s

of molybdenum in oxidized f r a c t u r e s out l ine the a r e a of

known mineral izat ion. If such a r e l a t ionsh ip ex i s t s i t would

be a n extremely usefu l geochemical explora t ion tool i n

regions outs ide the 1979 map-area.

- 31 -

CERTIFICATION ' -

1.

2.

3.

4 .

5.

I , William G. Smither ingale , ce r t i fy t h a t :

I a m a p r a c t i s i n g Professional Geological Engineer , res ident a t 219 - 1L5 West Keith Road, North Vancouver, B.C.

1 am a g r a d u a t e of the Universi ty of Bri t ish Colunbia . . with a degree in Geological Engineer ing (B.Ap.Sc., 1955) a n d of the Massachusset ts In s t i t u t e of Technology with the degree of Doctor of Philosophy in Geology (Ph.D. , 1962).

I h a v e p rac t i s ed my profession cont inuously for e ighteen y e a r s a s geologist with the Geological Survey of C a n a d a , a s Assis tant a n d Associate Professor , Department of Geology, Memorial Universi ty of Newfoundland, a n d s ince 197.L. a s a Consul t ing Geologist.

I a m a member. i n good s t a n d i n g of t he Association of Professional Engineers of the Province of Bri t ish Colnmbia. .

1328 - 510 West Hast ings Street Vancouver, B . C .

Feb rua ry 8, 1980

V

- 32 -

BIBLIOGRAPHY .

1. Ariz, J . F . , 1971: Storie Mo Prope r ty , p r i v a t e r epor t , Levana Expiorat ion Company.

2. Gabr ie l se , H . , 1958: McDame Map Area, Cass i a r Distr ic t , B.C., G.S.C. Memoir 319.

New Je r sey Zinc Explorat ion Company ( C a n a d a ) Ltd. Exploration 2eports on Cosmo Proper ty .

3. 196L Peter Crone 4 . 1965 Peter Crone 5. 1966 R.C. hlacdonald 6. 1959 J .F . Ariz

7. Pewsey, Brian G . , 1978: The Cassiar Story - In t roduct ion , Canad ian Min. a n d Met. Bul l . , April .

Shell Canada Resources Ltd. Reports.

8. G a s p a r r i n i , C . , 1979: Mineralogical s tudy of ten samples, t he molybdenite deposi t of C a s s i a r i n Bri t ish Columbia.

9. Saydam, S. , 1979: Geophysical t es t r e s u l t s over t he Storie MoS. p rope r ty , C a s s i a r , B.C. 2

10. Van Ingen , R., 1979: Report on the megascopic descr ip t ions of d r i l l core and su r face rock samples from the Storie molybdenum prospect and v i c in i ry , C a s s i a r , B.C.

- 33 -

APPENDIX 1

1979 D I A M O N D D R l L L HOLE LOGS

see Folio 3

DH

79-1 79-2 79-3 79-4 79-5 79-6 79-7 79-8 79-9 79-10

- Average

D I P

76'20' 72 " 70" 68" 72 " 70" 76 " 75" 75"30' 68"

Average Azimuth

170" 171" 160" 169" 157" 160" 170" 165" 156" 155"

-- Length

jme t r e s )

367.3 277.4 368.2 182.9 227.7 124.7 78.3 91.8 160.9 275.2

SUMMARY OF 1979 DRILL HOLE DATA

E l e v a t i o n Nor th ings Eas t i n g s (metres )

6 567 675.06 450 692.33 1691.3 6 567 840.84 450 669.65 1659.5

450 781.82 1633.1 6 567 863.50 6 567 625.59 450 827.49 1640.8 6 567 847.69 450 9ii.6a lGOl.7 6 567 588.88 450 958.96 1584.2 6 567 467.94 450 976.12 1563.9 6 567 620.18 451 079.30 1552.7 6 567 754 451 055 1561 6 568 050 451 017 1570

4

Thickness o f overburden

1.2 7 . 3 3.7 G. 7 6.4 6.4 3.4 4 .O 13.1 4.3

(metres- Length o f

Casing L e f t -7;11et r E]--

1.2 7.3 3.7 12.8 6.1 6. I 6. I 5.5 18.9

3 . 7

I' (

SHELL CANADA LlMl TED - MINERALS OEPARTMENT DIIILL HOLE OH SECTION DATA RECOHO

ADOITIONAL INFO

- OR8 JNl l -

1

1

2

-

__ REC WER

T

90%

..--.

95 de . .-

82 r ' s r e

-

98

98

. ..-.

98 .. .. -

97 t h

92

1150 . ._

95

( s o -

- INT N F -

8. P

._

I O Y O

10 i r PO

__

__ 10

._

10

l o __

10 S

~-

l o IO' : ... .

10

9(

#AMPLE No.

FROM TO F t .

Stwcturd Angle VMBOL C.AJD(p 4 REEes

- 3.6 I

3.60 - 5.66

5 . 7 - 6 . 7

6.7 - 20.0

20 - 49.7

L I T I I O C W V . Tei tw* , Structurs. Mimdlz.tkm ILMholct#l

-77

Overburden

of r k ) . Py - 0.1% Mag - 0.5%.

-- K-spar PorpJyrr: _- 85% I:-phenos same as 3.6 - 5.7, 10% qtiz, 5% plag, - 1% bio. Top contact abrupt. but missing, bottom contact sharp but not c h i l l e d and marked by 3 cm b l o schl ieren.

Looks l i k e a product o f f i l t e r pressing o r flow d i f f e r e n t i a t i o n o f normal quartz monroni t e maqma.

mag - 0.1 McjS - 0.05% as coatings along wa l l o f I id py-qtz vn.

gM: pk-grn-gry, med-gr ( s o w q t t and p lag cse-gr) pk k-spar phenos up t o 1x3 cm - 30%. p lagmos t l y I t grn, l o c a l l y dk grn. b io f-nmd-gr. 5 - 7%. 1 m'serp 'a l tn 11.5 - 12.5 py .022, dissem and vn mag .O1 d i s s m and vn MoS -0.011, some dissem, most along fr. usci<Ily w i t h py and/or q t t .

pk, cse-gr.

py - 0.1

Qiza

85 j991T 18-1-1

- 19-1-2

19-1-3

11.8' - 20.0'

. ~ .

c .003 .02

. - - -. .- . - . - .. -

.003 .01

. -- .

.003 .04

~. .- - ----

< .003 .02

- -. __ . . - . .- . .. c .003 .01 . - ~ . . _ ~ . ... .

< .003 .01

. ~ _. .~

0 .003 .01

r ingers - . .. .. .

c .003 .OJ

20 - 30 (black so( __. .

30 - 40 w i t h p y r i i n t e r v a l I

__ ___ I _-

40 - 50

30

35

._

20

. . . -- --

50

...

35 -

I2

-

4 0

-

5

__

__

. -.~

wery

19-1-4

19-1-5 50 - 60

79-1-6 __ .. - .- __ 79-1-7

79- 1-8

- - __ 79-1 -9

60 - 70

70 - 80 hai r l i ne - - - ._

80 - 90

as f o r 70

90 - 100

as f o r no Qy: scattered plag IC k-spar. phenos mantled. CHI. some k-spar.

grey, f i n e (some components tned) - gr., Phenos tip t o 1X1.5

-2.A.l-

:o 0.1% ($001)

SYMBOlS AND ARRRFVIATIONS 79-1 samples analysed fnr oxide (Ox) Mo

I N 1 nEc , E s t . .

SAMPLE No s, TO F t I N F T DVERV ~ 1 9

79 - 1 - 1 C 100 - 110 10 85 0.05% as f o r 80 - 90' ~ _ _ I _. . - -.

9 - 1 - 11 110 - 120 10 97 0.05 - as f o r 80 . 90' 0.1%

-. .

9 - 1 - 12 120 - 130 10 92 0.1 -

_I

'ota l Mo

0.054

-- i S A V

M O S L Ox tb

.090 ( n i l )

Strvcturml An@# ;VMROL C.AJD(p( Au

C, .003 Green a l t ' n of plag. Upper contact missing bu t marked b b i o L k-phcno r i c h zone 20 cm wide I n Qd. 21m: @i-dike 15O t o C.A.

35.8m: becomes s l i g h t l y coarser gr. with less very f -g r . blo; marginal t o med-f-gr QMl; continues t o 49.7.

38.8 - 49.7: p o s i t i v e I.D. o f r k type.

py: ~0 .1%. mostly vn, some dlssetn. mag: ~0.01%. less than previous In te rva l ;

y: pink ish grey, medium grained; pink, p e r t h i t i c k-phenos av. 0.5 - 1 cm across comprise 25% k-phenos not c o m n l y mantled. Blo 5 - 7%. f i n e medium grained. not 'pepper textures. Some f i n e grained 'sugary' quartz feldspar i n groundmass. py. ~0.15; dissem. and i n py-musc-kspar vns mag <0.1%, r k weakly mag.; dissem.

10 o r 20 cm th i ck pk. almost aphani t ic

Intense a l t ' n prevents __-___-

. n i

-

.01 0.029 < .003

0.180

1 t Y 1y;

.299 (.001:

< .003 .02

I--- t-- 0.009 .015

( n i l ) < .003

. _~.

.003

< .003

...

< .003

5 .

.03

.- ..

.02

- - - . . ..

.01

.01

9 - 1 - 13 130 - 140 1C I i n frac. I 95 0.01 -

0.05 ..- . .- - _ _ -

92 0.15

- - _._.I

90 0.5% rema nder 1 and seams . __ ~_.

80 0.15% fr. & d iss

eams recoiery, i

. -. - .- .. .

97 0.01

...

-

99.7 - 168.6

-__-

0.060 as 120-130 ----+---- I---

0.136 ilack

. 55.3 - __-- 58.0: F r . cleav 15' t o C.A. -t------t--- 0.074

udes I

--. 54: k-phenos become less abundant (10%).

- - -- i 0.om

.003 . . -. -. -.

0.01 __ - .. . .

- SVMROLS AND AORREVIAlIONS ~~ ~ Sl4FET I N T l R V A L . I r n m I"

SHELL CANADA LIMITED - MINERALS DEPARTMENT DRILL HOLE OR SECTION DATA RECORD

LLLd ADDITIONAL INFO

r-

FORN UNIT -

L

Pplnn

1

15

MWLE FROM. INT. No. INf1 TO F t .

79 - 1 - 34 180 - 190 I C several quart2 -.--I__

79 - 1 - 35 190 - 200 1c no veins

._____ ______ .-

79 - 1 - 36 zoo - ~ I O i o one py - q:z P .__I__ - -

79 - 1 - 37 210 - 220 i o qtz-py-MoS ve

Structu*d Anqle iVMBOL C . A l D l o C ""7

93 0.05 loS2 veins --_ -. . _ _ - -

92 co.01

.

90 0.02 v e i f l .

_ .- - - - - -. 96 0.02

_I

100 0.05 os2 veins

0.015

0.012 35

.-

7 0.010

-

0.032

------I I--

20

I---------I--- 0.032 IS

. 83.5 - 87.5: abundant and mantled-l ike quartz monzonite ; 10 cm b i o schl leren a t 87.0.

_- 90.5: k-phenos become la rge r 1x2 cm conmn: some mantled, comprise 25% o f rk .

K-phenos are smaller, more 79 - 1 - 3 230 - 240 10 1 qt2-MoS2 vbl"s 8 _ _

10 I-----I-----

0.013 s on b

~ _ _ .

0.009

_ _

0.02 marg5n

10 79 - 1 - 41 250 - 260 10 qtz-py-MoS, ve

79 - 1 - 42 260 - 270 10 qtz-py-MoS, ve

_-. . - .- __ - ..- - -

79 - 1 - 4 3 270 - 280 10 qtz-py-MoS, ve

- _ f. + .

35

( n i l )

0.043 20

I . . . . ,

_. SYMBOLS AND ABBflEVIATIONS I" S H F E I I N I F R V A C horn

H V r l m l V

WORK DONE N s m

DnlLLlNG ..

LOGGING.

AODl l lONAL INFO ASSAYING:

- INT N r i

10

-

-_

10

-_ 10

__ 10 ant

lo

.-

__ 10 a nc -_ 10

-

IO

- __ 10 rti

l o z z

__

.s t . 105, 0.05

- __

0.08

.003 0.01 9 - 1 - 44 200 - 290 as above

< .003 0.02 0.064 ( n i l ) .

9 - 1 - 45 290 - 300 as above

9 - 1 - 46 300 - 310 as above

0.038

0.042 0.05 i .003 0.02

0.1 eins

0.021 0.01

__ ._

0.05

9 - 1 - 47 310 - 320 qtz-py-Mo!

I--- 0.1

.-

0.1 eins

0.040

0.029

9 - 1 - 48 320 - 330 as above I I----------

.ffl3 ( n i l )

0.05

._

0.02

_-- 102n: quartz MoS veins 2 n thick cu t by barren quartz v e i t 2 cm th ick.

9 - 1 - 49 330 - 340 q tr -py-Mo!

I--- 0.05 0.037 i .003 9 - 1 - 50 340 - 350 I as above

I-------- 0.01 0.015 i .003

~-

< .003

0.05 9 - 1 - 51 350 - 360 MoSZ vein I ___---- 117.5 - 119.2:

groundmass i s f i ne grained quartz and whlte c lay w i t h i n a general ly a l t e red i n te rva l .

p a r t i a l replacement o f

I- 0.05 wrf

3.020 veins

0.05 9 - 1 - 52 360 - 370 MoS2 and c I I---

0.1 y r i t e

1.060 ins

0.02 9 - 1 - 53 370 - 380 MoS2 f qua I , . . . . I

SYMBOLS AND ABBllEVlAllflNS

SHELL CANADA LIMITED - MINERALS DEPARTMENT PAGF _ OF 13 PROJECT NAMF

PIIOJECT N O

HOLElSEC N O _ _ 5%;; ~ -

OHILL HOLE OR SECTION DATA RECORD

79 - 1 -- - -- _ _ - - WORK DONE N ~ W aim nemrts

______ _.___

D R I L L I N 0 _ _ _ _ ~ -

COGGING __ ___ __ _ _ _____.__

_____ ___ - ___-- ASSAVING ____.________

SAMPLE No.

I

Slrwturd Anqh VMBOL C.A.lDlp

79 - 1 - 541 380 - 39\21“80 4 0.02 quartz Mo )lac c lay vc 1 cm b lac se ns n t countc

,p.01 I

0.01

0.02 i lack I Hos2 __ __

88 :0.01 .013 .021 (?!!I .072

seams -(!!!!I

-hi I) .095

.OY3 5 o f b l

.003 .02 ~

MoS2 i n a id a1 99

mg n 0.1

3rglns (

.043 ’ black

.003

.

. on _ ..- -.

.003 ck seam!

.u1

._ .. . . -

.03 __ _ _

.05

l l e l C . I

7

10

10

98 0.01 .057

___I - --------i- 98 vei I

i e f r

0.1 j and a1 IC. W i t t

.056 mg r a l

I I------ I

98 to.01

:0.01

._

___ __ , , O . O l

45 - _ _

. .- ..- -. . - .. -

i n grey c ay s

99

98 ?oms - --

Q

20

- -. . _ _

SVMBOLS AND ABRREVIArlONS - .. I O S I l F F l I N l E R V A L liom

MVNWZV

OHILL HOLE OR SECTION DATA RECORD

POLITICAL U N I T

L A l l T U DE F I E L O LOCATION SURVEY

- A Y g

30

_ _ R E S U L T S O?

Au Ay

.003 .07

--

.. - - . . . . .- . . . .

.003 .06

. -.-

.003 .os

.-.. -. .- __ .. . .003 .U2

.003 .U1

.- - .. .. . . ..~. -.

.uo3 .03 .. - - . . -. . -. .-

.003 .05 k seam%. lib-para1 le1 C.

Slruclurel Anglw iYM0OL C.AJDia#

INT. REC- IN F T . 3VER

10 80

10 88 ack :lay _-

10 95 's a l m g I ; one s l -__ _.

10 88 ~

10 99 Id a l m g I . . -__ ..

10 98 ~.

10 98 a r t z ve i l i r l i le f r - - - - . .-

10 98 .- .- . _.

10 99 ... _- . -

10 98 ay s !am5

- .

-

0.01 ns 0.02 c lay v count

79 - 1 - 51 380 - 39( quartz MI 1 cm blac

1-- -- 0.01 earns

0.05 11s o f kensid, __.__

0.01

0.01 33 79 - 1 - 55 several 390 - 40( I I 0.02

lack MOs2 _ _

.013

25 79 - 1 - 56 400 - 41( Hos smet c l a j Sean

5

2

-. . .

10

79 - 1 - 57 410 - 42( I I----.--

0.1 rg ins I

.043 black

79 - 1 - 58 420 - 43[ NOSz i n z I --I--------

0.01 .057 79 - 1 - 59 430 - 44t I 1 0.1 and a'

:. w i t ) .

.056 ig w a l , c a t te

10

4 5

19 - 1 - 60 440 - 45C MoS i n t i S e d r a l I

0.01 .001 79 - 1 - 61 450 - 46C I ----I---------

0.01 .013 8

20

79 - 1 - 621 460 - 47C {

D.O1 I n grey c

.. - -

SYMBOLS AND A0OREVlATlONS S I I E F l I N l E n V A L lrnm $0

M V N W l V

i 13

PAGE 6 or - .

P n o K c i NAME . Casnw,


ADDITfONAL INFO ASSAYING

PROJECl N O 3991T. HOLEKEC NO 79 - 1 . - -

- -

168.6 - 169.6

169.6 - 177.3

Aplj_te: porphyr i t ic . ~ 5 % bio. Top contact marked by b io schileren 5 cm thick (hio not or iented) .

Strongly a l te red (sof t green a l t ' n ) . R e l i c t textures suggest t h i s In terva l was interbanded quartz monzonite 1 and Apl i te .

pink grey, f i n e grained, non-

SYMBOLS AND ABBREVlAllONS

Slruoerd Angh YMBOL C.A./Mp

I .05

. c2

- . . . . ..

.Ol

__.

.Ol

~. __ .Ol

.02

.05

.04

.01

G 4 3

55

20

18

33

S t l F E l I N l F R V A L lrnm 1"

- 3AM N I T - 1

-

n) !.la!

20

J E 177.3 - 226.4

-

LITHOLOGY. T a i l u s . Structwe. H l n r d i r e l w n ILllholnJI

-?--TI ~. . . I

Quartz &nLmlLe---l.: 160.6.

186.3 - 193.1: about 202 o f rock i s quartz j%sc.)-par a l t ' n veins w i th much plnk metasomatic k-spar between veins.

221.3 - 226.4: azcr-ore mask contact. Parts o f t h i s i n t e r v a l are f lt bx.

s i m i l a r t o 49.7 -

Pervastve green a l t e r a t i o n

eg. 224.5.

Total A S S A Y n E r u L i (oj A I

.01

-

. l o

.04

-_ - .

.02

.. _ _

.05

- -

. O l

.-

.02

.05

.05

.

. O l

Strueturd Angle YMBOL C . A J M p C Au

c .003

_ _ c . 003 100 0.07

ne d sseinlna __ ___ - -

98 0.03 y r i t veins. __ . ! - - __

13 as 590 above - 6oo a c d lo s(

7 9 - 1 - 7

224.5: bx .

) .

F t . 7 9 - 1 - 7 ,026 < .003 60

t--- .015

--

.w1

<. 003 1 95 0.1

_- 100 0.03

.

99 0.01

610 - 620 10 as above.

620 - 630 10 as above.

7 9 - 1 - 7

7 9 - 1 - 7

7 9 - 1 - 7

c.003

. .

r.003

35

30 .031 630 - 640 10 I as above.

t 7 9 - I - e .042

iins

.070 ( n i l )

<. 003 R

-.

3

195.6 - 197.1.: pervasive s l l i c l f l c a t l o n p F o m n g f i ne gralned matr ix of quartz and feldspar.

ZW-5--T5 200.7 - 205.2: c- Fracture clegv 20' to C.A. . . m a p l t t e d i ke 40 t o C.A.

216.2: 10 cm a p l i t e d l ke 30' t o C.A. 212.2 - 213.7: 213.3: A l tered a p l i t e d ike 30 to C.A. 203.5: Quartz MoS2 vetn cuts k-spar-nnisc.

a1 t e r a t i o n band. 201.3: Q i ra r t z HOS vein forms core of

k-spar a1 t 8 r a t l o n band.

lntense a l tera$ton ( so f t grel

640 - 650 10 quartz MoS, f I not counti 19 S I

,---- --

650 - 660 10 quartz HOS, f I

- . - --

660 - 670 10 as above.

.050 <. 003

7 9 - 1 - 8

--

7 9 - 1 - 8

.065 c.003 6

I . w 5 c.003 I t 670 - 680 10 I as above.

I r . . . l

SYMBOLS AND ABBREVIATIONS SIiFET INTFRVAL hnm I O

MVtJOOZV

i

L A - - AODITIONAL INFO

1 3 . O F - - 8 PAGE. ~

SHELL CANADA LIMITED - MINERALS DEPARTMENT

DRILL HOLE OR SECTION DATA RECORD Pnoxci NAMF CSZF r R o t E c - T NO 39911 - - _ _

- _. 79 - i I IOlCISEC N O ~

7- 1 -T ---I------- L A l l l U D E OEPARTIJRE ELEVATION IDAlUM) BEAAING

- _____ N E

FIELI) LOCATION

GRID

- A Z

s u n w y

!26.4 - 219.3

216.3 - 221.7: quartz and feldspar. (metasomatic?) I n ground mass gives rock a f i n e grained appearance.

f i n e grained intergrowth of

gljart_zJzAcPor~ r : Plnk, very ne gra ne t o $anfdc, phenocrysts of

plagioclase and quartz up t o 0.5 cm 15 - 2% of rock. Occaslonal k-s a r pheno. dominantly f ine grained E l o t52.

233.5 - 235.6: green.

fnterisely a l t e red t o s o f t

Strvccurd And. SYMBOL C.AJMp a

as above

7 9 - 1 - 1

79- 1-107 -- 79-1-108

--T-

7 9- I - 109

I-

79-1-1 10

79-1 -1 11

19-1-112

-_ 19-1-113

I I

690 - 700 as above

700 - 710 -

710 - 720 quartz Ho

720 - 730 as above. fragmenta -._I___

730 - 740 as above. Half o f s, -___ 740 - 750

l l a l f of S i quartz Mo!

_- 750 - 760 quartz Mol

760 - 770 as above. probably (

INT. REC E s t . Total A S S A Y

hkJ< IN F l . UVERY Fb FbS

ox IO 100 0.01 .015 (.025

( n i l , -- - ~ --- - . ___

10 98 0.01 .031 .052 ( n i l 1

10 .022 __ -(?_i.U

10 100 0.03 .o50 .083 ( n i l 1 * Cyrite veins

___

98 (0.01 .(I13

--..- I....-__._-_____ ~-

10 88 Cko5 .062 . lo3 ( n i l ] Half o f sample i r t e r v a l i s

niud d t h 752 recovery. - ~- ~

10 95 0.02 .011 .068 8 m b l a c r seams and 6 cn brown p i e i s fragnentec mud w i t h 75% r

<.003 01

c.003 .01

- - - - - -

<.003 .01 ay not Loiintcc overy . - __ - - - - <.003 .01

20

__ . -. .. 14

25

60

33

.-

6

- ~- ~- SYMEOLS AND AOBREVIAllONS I" SIIEFT I N l E R V A L lrom

YVNWYV

AOOITIONAL INFO

FOnM UNIT -

1

3

I b

-

Dfiq"

49.3 - 249.8

!49.8 - 279.8

'79.8 - 280.7

'80.7 - 284.9

LITI4OLOGV. lerlvra. Slrwwrs. MtnrJir.ilm IClihOlogl

_7 . . . I

248: s t a r t s t o become coarser g r . ( s t l l l f i n e grained) w i t h a few more k-phenos. places i t looks l i k e quartz monzonite 1 by v i r t u e o f numerous plagloclase phenos and scattered k-phenos, but the groundmass remains ftne gralned.

I n

252.5 - 254 and 257 - 260.5 and several smaller i n te rva l s : t o a l t e r a t i o n of feldspar I n groundnqss t o white c lay ( k a o l i n i t e ? ) .

Gradational contact.

crumbly and f r i a b l e due

quartz M o j z ~ ~ ~ : p lnk l sh grey, medtwn gr'd7neK scattered K-phenos up t o 1 X 2 cm (5% o f rock.

249.8 - 261: Sections w t th a f i n e grained su ary component i n the m a t r i x - l i k e quartz fevdspar porphyry s i m i l a r t o 79-3, 163.5 - 211.2 and 214.6+.

271.7 - 278: Frocture cleav mainly 15' t o C.A., l o c a l l y 40 t o C.A.

9_uarrrd~~~e_ar_~~r~h~-~ d l ke. Upper contac! co inc i es with musc. - k-spar a l t e r a t i o n band, lower contact masked by broken core.

Qu5rt-t-Monzoni te: medium t o f lne gralned k-phenos up t o 0.5 X 1 cm 5% o f rock.

Siructurd Awl* YHBOL C.A.IDIp

I2

20

12

40

6

- 5

8

25

12 -- W E € T INTFRVAC lrnm I"

...... -...

S

10 13 e:mm PAGE-. . ~ _ _ -

m o m 1 NAMS. - jgyrf PROJECT NO - _-

IIOLEISEC NO . ~ ''-1 '.:-~:: -I.-:---

SHELL CANADA LIMITED - MINERALS DEPARTMENT DRILL HOLE OR SECTION DATA RECORD ~ - . ..

_I____. - Datu Renurtr

.-___ .- LATITUOE DEPARTURE - __I-. FIELD

~ - LOCATION

N E A 2 SUHVEV ~ _ _ _ _ _ _ _ _ _

WORK W N E Name

DRILLING:-p.

L O C C I N G ~

ASSAYINO: l - . - - . - - L U ADOITIONAL INFO - .-

-- L-;141m

60

30

_ _ 18

7

18

!5

. - . . ..

14

.

15

-.

FROM

To Ft

870 - 880 As above

__- - 880 - 890 As above

€ S U I .

YlnrL

.003

-

.01!3

.003

-_ .003

-003 .~

,003

_ _ - <.003

.. -

<.003

SAUCLE No.

79-1-87

79-1 -88

79-1-89

-- Bind.

.03

.07

.07

--

.05

.03

. O l

- ..

.03

-

.01

..

-_

10 100 0.1

~ -_ 10 100 0.05

-- --- .__

10 100 0.02

10 100 0.06

- FoSz tn.

10 100 0.03

I s 0 me

--- --

10 100 0.1 !OS t p j r i te VF I d s c qt artr k - - _ - --

10 99 0.05

- -

10 90 0.2 lned disspmfnat lark grey c lay ! l v i s l b l e i b S 2 __ . - -_

.035

890 - 900 As above

.066 283.5: Musc. i n a k-spar a l t e r a t i o n band has been a l te red t o ta lc , perhaps dur lng development o f a coincident quartz-MoS2 vein.

(Questionable i f t h i s In te rva l 1s s i g n i f i c a n t l y d i f f e r e n t from 249.8 - 279.8 no, I don' t th ink i t i s ; y e t i t 1s s i m i l a r to 79-2. One so lu t i on i s t ha t 249.8 - 279.8 i s u n i t 3 - i t i s gradational w l t h Q . F . P . )

TJfl: pink grey, medium f i n e grqtned scattered k-phenos (0.5 t o 1 cm, pink, p e r t h i t i c ? not mmt led ) = 52, b i o 5%. fine-medtum grained but no t pepper, plagioclase a l te red t o green hard and s o f t and some white s o f t p y r i t e .

900 - 910 As above q tz - musa

. lo6 .177 ( n i l )

79-1 -90

79-1-91 -- 79-1 -92

-_._

19-1 -93

__ 79-1 -17

910 - 920 .074

.068 5 . !ir ban( .. ___ .. .

.028

0.110 i n fra ms a t 4

-- -.

920 - 920 MoS 6 q t i Sod MoS2

930 - 940 As above

940 - 950 As f i n e g

t o C.A.)U (plus 1 CI

--I___

- Granite: plagioclase and quartz po rphy r i t i c . Borders on quartz monzonlte. k-phenos pfnk, p e r t o h i t i c ? 0.5 - 1 cm 102; plagioclase phenos 0.5 cm 52; quartz phenos 0.5 - 0.7 cm 15% p y r i t e < 0.05 dissem. Mag. 0.1% dissent. mod. magnetic.

pink. f i n e grained. k-spar, 284.9 - 326.0

1 I

SVMROLS AND ABBnEVlATlONS SIIEET INTERVAL lrnm I"

0.04j - MoS2 - .

0.086 HoSz

0.03F

- - - -

0.16C nm th.ck

.078 veins A!!! !

.143 veins.

(nl! .060 ( n i l . . -

.264 and

( .002


WORK OONF N o m

DRILLING

Owa Remarks

I L A T I T U M O€PARTUR€ ELEVATION I D A l U M ) REARING I__t_-- F I E I D LOCATION sunwv

LOGGING: __

ASSAVING' -____ .- --Ad

ADOITIONAL INFO. F

AOM

0 F t SAMPLE

No. L I 1HOLOGV. Texture. Slruclwe. Mlnndlrellar ILitholngl

I ' ' ' . l SWA

.34 79-1-18 c . 003 and

tcd) ns .

79-1 -1 9 <. 003

mne ed). core 1 -

'.003

.07

40 1:I;

.01

17

l o

0.16 .277 long m glns (

MoS v ins an( seEms o t cot MoS2 r a l l e l

.002

0.15 .250 veins. i ( n i l )

_ . _ _ I

286 - 293.5: @d€fTveiyldenti fy rock type.

s t rongly altered, can ' t

79-1 -20 970 - 9 8 i l$ 9 i 0.2 As MoS2 v Ins nd quar t

79-1 -21 1-

980 - 9 9 j li 9\ 0.1 As MoS v ins nd n quart (0.6 c81 b ack lay o t cou

.01

. O l

8

35

veins. ( n i l ed) .

____._

79-1 -22 -- t --

79-1 -23 c.003 .01 2 A l i t e : pink, f i n e ralned; equfgranular. $E, k-spar and ~ 3 % bio. D i f f e rs from above i n t e r v a l by absence o f plagioclase phenos and less b io .

326.0 332.6

1000- lo lo

79-1 -24 :.003 .01 5

'.003 Mos2

.@4 quart;

5 eins.

79-1 -25 Has micro-breccia s t ructure healed in gypsum and white c lay min. p y r i t e 0.1% I n t h f n veins, pods and disseminations. No mag. . . . . . I

SYMBOLS AND AREAEVIATIONS SHFFT INTERVAL Irern I"

MVELWIV


WORK OONE Nema

DRILLING ___ LOGGING

ASSAYING. ~.

I---------- AOOITIONAL IPIFO ~

- N T U FT -

10 -- -

10 5 ( __

10 _- 10

cn -

10

a i t

5 7

-

10 i r

9 4

10 Not

._-

10 ns. .- -

10 PY r

10 se

. _

- -

--L--/sg[ 79 - 1 - 26 1030-1040

LITHOLOGY. TeI Iwo. Slruccurs. Minrmllr*t lar ILltholnp)

?"I

MoS occurs along f ractures i n h a i r l i n e and i d g u l a r veins and as threads and d i sseml na t ions between breccla fragments. Upper contact abrupt, masked by a1 terat ion.

Lower contact appears t o be sharp but masked by a l te ra t i ons .

ElLazu c.00:

c.00:

. -

c.003 -

.003

. _._

.003

. __ .003

d snieai eccia 1

<. 003 5 ) .

~

.003

- . . .

.003

-. .- - .-

< .003

__

lgcarLi .01

Ilpm 5 08 I 0.03

I--- --- .01

- _. - .

.01

8

4

79 - 1 - 27 1040-1050 Excludl ng I :lay se P m H n l l I

79 - 1 - 28 1050-1060 I I

10

5

___ 8

79 - 1 - 29 1060-1070 I (excluding ( n i l 1

79 - 1 - 30 1070-1080 As MoS ve f i l l i n & i

0.076 .I27 i i r l i n e fractui

( n i l 1 - --I.-.-..- -- -- t----

1000 - 1100: Grey areas adJacent and between black seams. very f i n e grained mineral causing grey colour.

Granite: pink, medium rained ( f f n e grained

P y r i t e ~ 0 . 1 disseminations. Mag =0.1 = very weakly magnetic.

Can't i d e n t i f y the

components) non-porphyr 3 t i c . S imi lar t o 284.9 - 326.0.

79 - 1 - 31 1000-1090 V ls fb le ma (Not count

t . ~ . _ .

.01 5

. ..

4

l 9 - 1 - 32 1090-1100 As above. I 332.6 -

367.3

.02 79 - 1 - 94 1100-111O dlsseminat I

I

90 0.01 te v i n . _- I - -. --1--------- - _- _I.__ .I

10 79 - 1 - 95 1110-1120 As smear 1 I .020 .033

( n t l ) __ - - . ty .016 seam; ( n i l ) .026 10 100 0.03

? r a l black I 79 - 1 - 96 1120-1130 Not counti I

I . . . . ,

SYMBOLS AND ABBIIE V I A 1 IONS ~. - Sl lFEr I N l E R V A L l r ~ m I"

MVNrMlV

.. . r . (

17 PAGE l 3 _ _ O F


DRILL HOLE OR SECTION DATA RECORD PROJECT NAME cBsnw, - - 3991T

79 1 1- -- ---- PROJECT N O - _

t1OLEISEC NO - _ _ - - - _ _ _ WORK DONE Name Dele Ilemsrks

DRILLING ______

LOGGING LOCATION

LATITUDE DEPARTURE ELEVATION lDATUMl BEARlNt i

N E

______ __ r i ~ ~ o - ~ _ _ _ _____ .

SURVEV GRID A 2 _ _ _ _ _ _ _ - - ~

______ ASSAVINO

I A I AI>UITIONAL INFO

SAMPLE No. 3(ozll

.06

I " ' ' I

' 9 - 1 - 9

< .003 .16

.02

- ..

.04

'9 - 1 - 9' __I--

' 9 - 1 - 9

.023 (nil

.030 (nil

_..I_

.018 (nil

.003

< .003 '9 - 1 -101

_.__ 353 m - gradually becomes coarser grained over 2 - 3 m. S t i l l medium grained. (Occasional plnk k-spar pheno). Only a few seen.

0.5 X 1 cm. '9 - 1 -10 .023

(nil < .003 .02

'9 - 1 -10 .025 (nil

< .003 .06

.014 (.001

.033 seam

< .003 '9 - 1 -10

c .003 '9 - 1 -10

-- SYMBOLS A14D ABBREVIATIONS SHEET I N r E n V A L horn I"

M V N M Y V

WELL CANADA LIMITED - MINERALS DEPARTMENT DRILL HOLE OR SECTION DATA RECORD

LATITUDE OEPAIlTUHE ELEVATION

I I

i32.L 0 - 7.

1.2 - 33.0

33.0 - 33.3

- !NT. N F T

a1 A S S A Y n C s u L i 'ROW 10 Feet

24 - 30

Struccud An@ YMBOL C.A./Db #

SAMICE No. LITl4OLOGY. Trrlure. Slruclwa. Minadlzrlia I L I l h o ~

Casing 9 - 2 - 1 6

.- _.-

10

.006 .004 .ow1

- f)uartz -._.. Wnzonite: grey, fine-medlum- grainea, feldsirr porphyrl t i c , 'pepper' hlo (some b l o i s very fine-gralned, l i k e pepper f lakes) .

K-phenos pink, mostly less than 1 cm long but some 1 X 2 cm, some mantled with plagioclase.

P r i t e - . d F e l . i t e : ... _I__- .= 0.01. rock moderately magnetic.

- - - - - 7.2 - 11: broken, weathered core. 8.ZzZlJ!_1.: several short i n te rva l s o f s o f t crumbly a l t e ra t i on . . 7.2 - - .- ._ 15: -. plagioclase a l te red t o l i g h t green, hard, w i t h several shor t i n te rva l s plagioclase a l te red t o soapy s o f t and 1 30 cm In te rva l ; pervasive green w i t h bio. gone; 5 k-spar-muscovl te-quartz f p y r l t e veins i n t h i s i n te rva l . 15 - 32.7: plagioclase a l te red to white hard, w i t h several patches mixed white hard and white s o f t .

4 1% mainly i n veins.

29 - 29.3: pervasive green, no hio.

Aeljditg: pink. f ine-grained, no phegos, 3% blo. Upper contact sharp, a t 40 t o C.A. lower contact gradational with f ine-medium- grained quartz monzonl t e 1.

- -

.013 - . 001

010$ ( n i l ,

.052, ( n i l ,

- _ _

029! _._ (n i l , _ _

.051 .e recc In ve i l

.om -

.097

.012 ._._ .

.034

.001 - _-

_._I__

30 - 40 9 - 2 - 2 . Do9 .

.006 . .- _-_ .

.031

S .

.- - -

.017

9 - 2 - 3

9 - 2 - 4

40 - 50 10

10

{ri t ihyd

0.07

i r t z ve

0.05 1 - 2 - 5 GO - 70 10

3 - 2 - 6 70 - 80 s above. .8 . Two un r t ~-Mol

10

! C t i ve l

0.05

. t i moly k-spar

F_ .

0.05

82 sect

0.03

.-.

- _ __ - _-

.035

eins (

l t e r a l

3 - 2 - 7 80 - 90 10

1st

.070

ns .

10 .021

-_ - - . - __ - SYMBOLS AND ABRAEVIATIONS

-... OEPlb

.metre

33.0 - 155.5

79 - 2 - 13

79 - 2 - 14

- -_

'9 - 2 - 15

-- - -- -- - .

9 - 2 - 16

Not c lea r whether a p l i t e i s a d ike o r a border phase o f quartz monzonite 1. i t was probably emplaced whi le quartz monzonite 1 s t i l l hot or mushy - perhaps squeezed out of quartz monzonite 1. emplaced a f t e r quartz monzoni t e 2.

I t h i r

I t was

140 - 150 I C

Same veln 2 s a f o r 112 o f Mos

--

150 - 160 10 Quartz-MoS. f 1

160 - 170 10 A s above.

--. __ - - .

170 - 180 10

@WW Monzonite: medium-f ine-gra 1 ned. k-spar po rphy r i t i c . K-phenos general ly (1 cm across, pink, p e r t h i t i c , general ly not mantled. Bio fine-medium grained but no 'pepper' bio.

l i g h t grey n f t h pink t i n

.077

.010 :ounts

Pyr i te : ~0.1%. - _ Ra$elite: .____ strongly magnetic . 0.01 t o 0.1%. rock moderately t(

32.7 - 35.1: plagioclase a l te red t o l i g h t green hard.- - 35.1 _.--____ - 47.8: most plagioclase opaque white hard, i n places very s l i g h t l y green. some so white next t o c e r t a i n fractures, except 39.5 - 41.2 where plagioclase a l te red t o 1 i q h t green. 17.8 - - 58.1: l i g h t green hard, although some s t i l l opaque white o r very f a i n t l y green except:

most plagioclase a l te red t o

48.6 - 49.7: plagioclase a l te red t o sof t soapy green, tio. gone; several quartz MoS veins. 52.8: s o f t soapy green w i th b i o gone and quartz MoS2 vein i n center.

5 8 . 1 - 59.9: ;oapy medSum t o dark green, b f o gone ?xcept f o r 10 cm a t each margin, 7 quartz f bS veins i n i n te rva l .

20 2m plagioclase a l te red to

plagioclase a l te red t o s o f t

I

.lo] 0.1 .056

ve r ns 15 c and a

. -- ~-

x 1 0 0 0.01 .022 ? l t e veins. --

83 0.03 .032

- .. - . - - ._ - . . . .

88 0.01 .022 -

POLITICAL UNIT

:- ADDITIONAL INFO

PAGE - 3 __ or- 13-

PROJECT NO - 3Y91T


DRILL HOLE OR StCTlON DATA RECORD PROJECT NAME _ _ Caste - _ _

IIOLE/SEC NO - - 2 9 -_zII--_ _ _ ___ W R K DONE N a m Dnn Rswurki

DRILLING

- - _ _ ~ -I__

-- LOGGING

-_ _. -_ ASSAYIHG _____

59.9 - 65,5: most plagioclase i n c i p i e n t l y a i G s very pa le green, although some d i s t i n c t l y green bu t hard and other grafns not a l t e red except:

62.0 - 62.5: so f t soapy green, b f o gone several quartz - p y r f t e veins. 62.7: p lag ioc lase a l te red to Soft soapq green adjacent quartz and s u l f i d e vetn. 63.1: plagioc lase a l te red to s o f t soap: green adjacent quartz and s u l f i d e veln.

-.I_-_- 65.5 - 85.7: white, hard.

plagioclase a l te red t o opaque

74.0: E z a r only.

10 cm pegmatite lens, quartz and

- 85.7 -. .-.- - 89.4: ._ - l i y h t green hard, some s t i l l whlte, some a1 tered t o s o f t soapy green.


_-_-- 89.4 - 98.0.: plagioclase a l te red t o soft soapy green.

91.0: 5 cm crumbly core adjacent sl ickensided s l i p . Ground mass consists o f f ine-grained quartz set t n aphanftfc opaque whi te matr ix . Probably a p a r t l y a l t e red f ine-grained f a u l t breccia o r 'crush zone'. 92-92.3: same type 'crush zone' texture as a t 91.0 bounded by black sllckensfded c lay seams. 93.6: 5 cm crumbly crush zone next t o sl ickensided black c lay seam w i t h HoS2 smears. 94.8 - 95.4: adjacent s l ickenslded black c lay seam w i t h MoS2 smear.

crumbly 'crush zone'

, . . . . I

Slructurd An@s YMBOL C.A.IDip I

19 - 2 - 24IG50 - 260 uartz-MoS

19 - 2 - 25 260 - 270

~

As above a a 3 cm p i n ~

- _._ - - SYMBOLS A N 0 AeBRCVlATIONS

LITHOLOGY. TewIwe. Structure, Mirrrollmllon (Lltholagl

l . ' . - l

97.5 - 97.8: crumbly 'crush zone' next t o s l i p .

-_ 98.0 -.- - 110.7: plagioclase mostly l i g h t gree h a d , but % a l l y plagioclase a l te red t o sof soapy green eq.

99.1 - 99.3 99.8 - 100.0

103.0 - 103.8 105.9 - 106.1 108.0 - 108.2

. 103.1 - -_. - 103.4: containing several s l i ps .

NLB..: From 98 on the core surface seems s l q h t l y f i n e r grained and k phenos less d i s t i n c t than before 98, although there I s nt d i f ference v i s i b l e on f reshly broken surface except f o r s l i g h t l y more pervasive a l t e r a t i o i o f plagfoclase a l te red to green a f t e r 98 m. A f te r 98 m i s d e f i n i t e l y quartz monzonite 1B and therefore before 98 m must a lso be ca l l ed quartz monzonite 10, even though I n other holes i t does not appear d i s t i n c t from normal quartz monzonite 1. The d l s t i n c t l o n between quartz monzonite 1 and quartz monzonite 10 must include the s i ze and abundance o f k-phenos. Descrlpt ion o f quartz monzonite 1B fol lows.

Quartz Monzonl t e : weakly po rphy r i t i c ; k-phenos pink, p e r t h i t i c . general ly ~ 0 . 5 X 1 cm, < lo2 o f rock; ground mass contains some f ine-grained quartz and feldspar but i t i s not l i k e type 3; some f ine-grained b io , but no 'pepper' b io .

crumbly 'crush zone'

medi um-f i ne-gra I ned.

I . . . . ,

r9 - 2 - 26 270 - 280 quartz -Mol

.- _- I_ .- .._ -

'9 - 2 - 27 280 - 290 As above.

- __ - _ _ -___ - .- -- __ _.

'9 - 2 - 28 290 - 300 As above.

_I______ ___I___

'9 - 2 - 29 300 - 310 As above.

quartz-)lo! __

As above. __

As above.

__

-- INT REC N F T OVEII -

10 9 i * p.rr i tt

10 -101

-_

-__ l o =lo(

-I_

10 91

- -_ 10 9s f p: r i t e

10 99

---. - - -

_ _ 10 =loa

- - .__

10 97

.-.

10 70

--- .-

Est. 1 %

0.0; veins.

0.0:

~ -_ ____

0.0;

0.0':

0.06 veins.

0.01

0.02

__ .

(0 .01

-- .-

<0.01 .008

I E S U L l S

.

SYMBOLS AND ABBRf VlATlONS


PAGE ... PROJECT PROJECT N O ~ 311 .lYY ._ I I .~~ - IiOLEISEC. NO: ~ ~. . _ _ . -..

5 NAME -

WORK OONE Nam Datu Remarks

DRILLING. -______

LOGGING

_.

INT. IN FT -

10 and

10 2

M W L E No. ";i" uartz f p y r i t e

i S S A Y 7-

1%

'OX Mo .155

reins. - - .no1 . . - - .

.035 (n i 1 )

R E S V L l S FROM . TO Feet

360 - 370 MoS2 vein!

79 - 2 - 35 . 360ftAOOft:pyrl te .- __ .. - .0.1%, mostly i n quartz veins. 20 o r lgss t o C.A., although a few are about 45 .

Most MoS2 360 - 340 I s i n veins about

370 - 380 Several Mr

.____ 110.7 - 111.5: most feldspar a l tered. A l l plagioclase a l te red t o s o f t soapy dark green, most K-spar a l t e red t o green.

SLIPS: (not logged before 114111)

1 14.5 : 30OtoCA Mi o f bx zone

115:20°to C.A 121.5:45°to "

125.2: 1O"to "

125.7:35""

127.6:3O0" 5 0 0 ~ ~ " I(

128: 35'" " 128.2:35°" "

broken core 129: 40'" I31.7:45On "

134: 35O" " 134.2: 35'" "

134.8 : 50' "

135.4 :45O" "

136.1:40°" "

45Ou II

111.5 - 114.5: plagioclase a l te red t o l i g h t green h a r d . 0.05 .033

e quart . - _-- _- I _ - 114.5 - - 115.3:

soapy green.

--._-_I-- 114.5 - 115:

115.3 - I____ - 119.8: ~

green. h a x -

119.8 - 122.5: zoned a l t e r a t l o n - on marglns P13?j3=<:1 tered t o so f t soapy dark green; passes inwards t o l i g h t grey zone I n whlch plagioclase a l te red to pale green and l l g h t grey very s o f t and k-spar. grey-pink, b i o gone; center zone of a l l feldspar a l t e red green, plagioclase a1 tered t o s o f t dark green but g r i t t y no t soapy and k spar a l t e red t o grey green so f t . b i o gone. bearing s l i p .

plagioclase a l te red t o s o r t

Micro breccta zone.

plagioclase a l te red t o l i g h t

Bleached pale

The center zone contalns a MoS2

.029

0.04 te ve ln ,. less

0.01 .030 _ _ - - . . - - I .

10.011 ,042

. 122.5 - - - 124.5: - plagioclase e l t h e r opaque whlte hard o r a l t e red t o l i g h t green hard.

SHECT I N I F A V A L lrnm I*

_ _ - L W G I N O :

--

LATITUDC: OEPARTURE ELEVATION (OATUM)( BEARING INCLlNATION

N E

FIELD LOCATION SURVEY GRID A 2

ASSAYING: I_---

!

POLITICAL UNIT: ...... ........... ;... ....... ..

WORU OONE Name

I A I ADDITIONAL INFO.: ___

-- -__-___ _. LANDMARKS.

-_ -_- I__ LOGGED BY: OTHER FEATURES. C L A W V E R M I T NO.:

_I_--_

- -

Est. Ros, T

Structural Anple SYMBOL C.A.IDIp

SLIPS:

137.5: 359 ToC

145.8:30'" "

ROM . D Feet

L I T H O L W Y . Tczluo. Slvmlun. Mir*)rdlzation fLiiholqlt

t ' . . , l

-. 124.5 - 126.9: no b -xoc lase a l te red t o so f t soapy dark green, k-spar grey green. Zoned a t margins th ru l i g h t grey t o p lag ioc lase a l te red t o so f t soapy dark green wlth bio.

mostly a l l feldspar altered,

SAMPLE wa.

R e l i c t texture suggest8 20 cm a p l i t e d fke a t 126.2 w i th contacts 20 t o C.A.

148.3:55'" " 155.2:20"" "

50"" " 1 56.3 : 50'. " ''

157-8 :60" 'I " 158.2:50" " I'

161.3:50"" Hw TO 6X

162.2:60"" " 40"" "

162.5:blk sei

162.6:45"" " 162.8:45"" " 163.7:50"" " 165 b l k seam

60" ToC HW t o Bx

zone 165.1 :45"ToC. 165.3:blk sed

70' ToC . 65.7:blk sea

606 ToC . 66.5-1 71

?umerous s l i l 15" !OW ToC bst35 ' t o 5!

55. roc

_--- 126.9 - 128: green hard.

p lag ioc lase a l te red t o l t g h t

128 - 129.7: a p l l t e atG.

l i k e 124.5 - 126.9. zone but n -- I

129.7 - 131.5: p lag ioc lase a l te red t o l i g h t green hard.

I 131,5 -136.7: l i k e 124.5 - 126.9. No dike n d t m e zoning about several s l i p s and quartz veins.

136.7 - 154.8-: plagioclase a l te red t o l l g h t g r e e m h a r d ; n places plagloctase s t f l l opaque white hard, l o c a l l y p lag ioc lase a l te red t o s o f t soapy green.

9 - 2 - 4 4 50 - 460 u a r t t MoS --- 60 - 470 s above.

.010

.010

-- .OO6

.OM --- .012

.017 ( n i l :

.017

. - .-

( n i l I

0.02 elns. --I

0.01

--- co.01

(0.01

-----

0.01

l__l

9 - 2 - 4 5 150 m: s t i l l same rock type. Most i f i m n g u f s h i n g feature i s sparci ty o f k-spar! over 0.5 cm. Rock I s non-porphyrit ic.

--- 9 - 2 - 4 6 70 - 480

---- BO - 490

90 - 500

- 153 --I_ - 155.5: gradual increase I n number of pTnk k-phenos.

_.

9 - 2 - 4 7 Quartz MonzonlJ$: p i nk-grey , medi um-gra 1 ned pink p e r t h t t i c k-phenos. some mantled, up to 1 X 3 cm, 53 o f rock.

55.5 - 186.6

3 - 2 - 4 8

SYUIOLS A N 0 ABBREVIATION-._- ~ . ..._ ..

-. SHEET INTCAVAL horn I"

LA- ADOlTlONAL INFO

PAGE 7 nr '3

rnoKcT NO

S H E L L CANADA LIMITED - MINERALS DEPARTMENT DRILL H O L E OR SECTION DATA RECORD PRVIECT NAME Ca sin0

3WTT -- -- - - -

7 9 x 7 - - - - _ . - _- HOLEISEC N O _.

154.8 - 157.5: white, medium hard to soft.

plagioclase altered to opaquc

157.5 - 1.60.3: - green hard.

plagioclase altered to light

_- -_ 160.3 - 161.5: plagioclase opaque white hard to soft.

161.5 - 1 6 c : plagioclase light green hard, l a soft soapy green in k-spar alteratior envelopes.

155 - 158.7: Broken and partly crumbly core Tu< to anhydrite fractures sub parallel core and local micro breccia adjacent s l i p s .

- 161.3 - - - 163_: - Micro breccia zone.

- 165 - 189: - Breccia zone wlth many black seams. Mostly micro breccia, some macro breccia. Some intervals falrly competent core wlth weakly developed micro breccia.

. 165.4 - 172: - s o f t soapy dark green, some plagloclase liyht green medium hard and locally all feldspar altered green wlth blo gone.

172 - _182,5: %Smy plagioclase a1 tered to light green medium hard to soft. soapy and locally dark green soft soapy.

164: becoming coarser grained. Numerous coarse quartz grains.

mainly plagioclase altered to

variable alteratlon plagloclasf

Some light green soft

Structurd An* VMBOC C.AJMp 4

in SYMBOIS AND AIBREVIATIONS _._Eg._.MoS2; .-MoSZ-equi.va!ent to Tota! Mo, calculated assuming no oxide Mo i s present, Oxide leach s w t I N t F h V A l hot performed on these samples.

i

13 .or ___-__ 8 PAGF- SHELL CANADA LIMITED - MINERALS DEPARTMENT

DRILL HOLE OR SECTION DATA RECORD PROJECT NAME - C a S F __ ~ _ _ - P A O X C T N O _ _ -jig!'2 klOLE/SEr NO . -

~ _ _ _ _.___

WOnK OONE N u n Dates Aenurks

DRILLING ____

LOGGING LOCATION

LA711UUE OEPARTURE ELEVATION IDATIJMI BEARING ~ _ _ ~ FIELD

SUAVEV GRID

._ N A 2 € -__-__

ASSAYING - -. - AOOITIONAL INFO

--

&E&

186.6 191.4

- INT. Y F l -

10 f l

ick -. -

10

r l 10'

l o

' I i i n i -

10

ome

-

- 9cc VE I -

Z l C

" i t !an __

9

? V fr

__

4

' i t on I

91

os

-

Total A S S A Y - 'ROM . ro. Feet

SAMPLE No.

LIPS:

85.5:50" ToC . HW o f intense mic bx

several b seam 50" t o 80" To C.A.

85.5- 186 :

B6.5:Two set a t 55' 140

87-200 numerous f rac turns; s 1 ips :2se 45" -60' t t C.A. one i 30" and an0 the r 70' - 85".

9 - 2 - 5 ! io0 - 610 luartz Mol lumerous I

i10 - 620

leformed I 'erhaps 2!

0.0 veins not co

173.5 - 179: Mainly coarse-medim grained WTS-f i rzk phenos l o c a l l y 90%. Some i nterva 1 s medt um-coarse grained.

- 182.5 - 186.5: m a % F m o c l a s e a1 tered t o s o f t soapy darl green.

185.5 - 186: w j j h p s along black seams and a l l feldspar altered, b i o gone.

179 - 186.6: quartz monzonite.

186.6: h 6 n s e l y brecciated zone.

quartz Feldspar Porphyry-: ptnk, q u i t e f fne- g ra jnea quartz monzonite, quartz phenos 10%. s m a l l plagtoclase phenos less than 53. less than 3% b io .

106.6 - 202;!5: plagioclase a l te red t o s o f t ;name= s o f t l i g h t green t o s o f t soapy dark green; i n many places i n quartz feldspar porphyry. Plagtoclase a1 tered t o dark green soapy cores w i t h l i g h t green s o f t rims. Some plagioclase medium hard.

E x w p t 196.8 - 197.8 k-spar also a l te red t o pa le grey-pink o r grey green.

Contact a t 191.4 I s s l i p a t 85' t o C.A. w i th adjacent micro breccia developed b e t t e r i n quartz monzoni t e than quartz feldspar

Variable green a l te ra t i on ,

extreme micro breccia (gouge)

medium grained po rphy r i t i c

contact a s l i p SO0 t o C.A. I n

Porphyry *

, . . . . I

S .

.-

ars.

ited. -..___

.OM

j as 5 v corf

.065

ing s l

.070

-

9 - 2 - 6 ( 0.0 to 0.1 IS i n broke

. O l to .05 reins,

.023

ecc 1 a 1 crum --I-

.039

os2 fi

9 - 2 - 6 : i20 - 630

f r a c t luartz-Mo! i lnor diss

) - 2 - 6 2 30 - 640

s above.

.042 0.01 o .05


POLITICAL UNIT

L - A - A ADDITIONAL INFO. ___

._ CLAlMlPFRMlT N O ' ___

SAMPLE (lo.

FROM Feet

540 - 650

l a i n l y qua

FORh UNIT __

S@rwiur.( A,n#I. SYMBOL C.AJD(e 4

SLIPS:

200.5: 50" ToC . 200.7:55"" "

209: 50"" "

HW o f bx LO 209.5 : 50" ToC . 210: 25"' "

21 0.3 : 70' 'I " 210.7:35"" "

50"" I'

211: 50"" 'I

21 1 . 1 : 25" " " 211.2:70"" "

211 .5:70'" "

212.3:50"" "

FW t o bx zo 215.1 : 30' ToC ., 219: 30"" "

50"" I'

21 9.4 : 40" 'I It

221 . 1 : 30" " 222.3:45"" "

225.4:20"" "

226.5 :40" I' " T29.1: 50" " " T30.3: 30" " "

23). 1 : 30" " "

two sets a t

20a.7:750" H

"

T32.3-232.5

10-15"To C.A

LITHOLOGY, Tsrlws. Structurs. M~mmllrotlon (Lllholcql

--I

Quartz Monzonite: same as 179 - 186.6. Contact a t 1q.q marked by concentrat ion of a1 t w e d plagioclase and hence i s probably i n t rus i ve . P a r t l y masked by s l i p 35 t o C.A

f$muaz-Felds a r Porphyry-: s im i l a r t o 186.6 - im%-a uartz phenos 1 cm 10%. plagioclase phenos t o 0.7 cm 5 - 10%. occasional k-pheno t o 1.5 cm. Very weak t o non-magnetic.

-- 202.5 - 207.5: gre-5 medium hard. s o f t soapy.

Contact a t 206.7 8s a s l i p with adjacent breccia. S l l p 50 t o C.A.

Q u a r e Monzonite: pink-grey, medium- graTnea t o 1 X 2 cm 5 - lo%, an occasional mantled k-pheno.

S imi lar t o quartz monzonite before 186.6 m.

.- f'yrite: disseminations. _ _ f laynetite: s t rongly magnetic.

207.6 - 21-2.7: Variable plagioclase aTTerxon.--'Most i s plagioclase a1 tered t o s o f t g r i t t y t o soapy l i g h t t o dark green. Between these In te rva l s plagioclase a l te red t o l i g h t green hard.

2p!12-_206,7-: contact .

plagioclase a l te red t o l l g h t A few a l te red t o

mostly less than 1 cm, some

~ 0 . 1 % mostly i n vefns. some

0.05 t o 0.1%; rock moderately t o

Micro breccia zone i n H.W. 01

191.4 192.4

192.4 206.7

206.7 219.4

9 - 2 - 6 i y r i t e to.:511 eins, . M 6 1 s me .110 i n :

9 - 2 - 6 ' 550 - 660 In veins a

9 - 2 - 6 '

9 - 2 - 6 1

i60 - 670 l a i n l y i n

i70 - 680 \s above.

.045

9 - 2 - 6

__

i80 - 690 \s above.

.067

__ - -

n . . . . 1

I O S t I E F t I N l F R V A L lrom

POLITICAL UNIT

L-- ADDITIONAL INFO

SHELL CANADA LIMITED - MINERALS DEPARTMENT 10 13 c--- ~

PAGE. _ ~ _ . . _ _ O F

DRILL HOLE OR SECTION DATA RECORD PROJECT NAME ~. $$Yr PAOECT N O - ~,9 17, HOLEISFC NO -~ _ _ _ ~ --- ---r---

WORK DONE N m Dalo R*marki

DAILLINO.-.-

- LOGGING. . ___~ -

~ _ _ - ~ _____ ASSAVINO,

LATITUDE DEPARTURE ELEVATION I O A I U M I 6EAl l lNG INCLINATION

N E

F IELD LOCATION SURVEV GRID AZ.

~ --

DCPl H

219.4 - 219.9

219.9 - 221.1

221.1 - 221.9

221.9 - 222.3

222.3 - 223.2

223.2 - 226

209 - 212.5: Breccia zone with several s l i ps . Some crumbly core.

209 - 211: Micro breccia. 211 - 212.5: Macro breccla.

___ 212.7 .---_ - 218: green hard.

Contact a t 219.4 i s a s l i p 40' t o C.A.


uar tz F e l d g a r PorphyD: l i k e previous f--- n t e r v q c La&r contact I s abrupt, but I t could be gradational.

gErtz Monzonite: S l m i l a r t o 206 - 219. Contact a t m.7 s l i p 30 t o C . A .

uar tz Feldlpar Pwhyly_: Contact a t 221.9 ?-- s S h > F b u t 5 e q u a r t z mnzon l te on each

'f- o r some f ine-grained quartz i n quartz

side i s i den t i ca l .

uar tz Monzonite.: S imi lar t o 206 - 219 but

monzonl te .

Contact a t 222.3 I s a s l l p a t 45' t o C.A. w i t h adjacent f a u l t breccia.

Qu_arLz Felds ar-P>T)yg-: I s g r a m & over 2 - 3 cm. 10 cm below contact o f quartz monzonite contains patches o f very f ine-grained quartz monzonite.

~u~r~t.b_n~ontte: but appears gradat ional over 1 cm. could be tex tu ra l e q u i l i b r a t i o n across an i n t r u s l v e contact.

Contact a t 223.2

Contact a t 226 i s abrupt This

, . . . . I

SYMBOLS AND ABBREVIATIONS ._ - _

SiruccurJ An@# SYMBOL C.AJD@C

SAMPLE No.

S S A V E S U L l --

I" il4FET INTFRVAL from

L I I ADDITIONAL INFO ~

11 13 PAGE _ _ ~ r ) F

SHELL CANADA LIMITED - MINERALS DEPARTMENT DRILL HOLE OR SECTION DATA RECORD PROJECl NAME casna -- - _

-_-.3991T PnOJECT N O '

HOLElSEC N@ ~ - ~ ~ _ _ _ - ~79 .~ ~ - - ---. .

- FIELD ___ N E

_____

- WORK DONE N s m Dalm Renurka

DRILLING.- LATITUUE OEPARlUnE EI.EVATION __

LOGGING. LOCATION

A 2 SURVEY GRlV

ASSAYING:

SER'4

226 - 229.1

223.1 231.1

231.1 277.4

LITHOLOGY. Tenlure. Slwctwe. Mlnrsllrsllon ILilhologl

-7 . . . . ,

gEartz F e l d s p t t Pocphyr? Contact a t 229.1 Is -6y brecc a an a s l l p a t 50' t o C.A

@art2 Monzonite: by Z T r E G zone and s l l p a t 30 t o C.A.

218 --- - 222.3.: white. s F t soapy l i g h t green and s o f t soapy dark green.

Contact a t 231.1 glasked


-- 222.3 - 225.5: opaqu- t e ha rd .

plagioclase a l te red t o

__._- 224.5 - 230: plagloclase a l te red t o s o f t soapy 773i- green.

-- 230 - 233.1: Feldspar a l t e r a t i o n varlable. Z o n e s o f a g i o c l a s e a1 tered t o s o f t soapy dark green and o f pa le grey zones w i t h plagioclase a l te red t o s o f t soapy l i g h t yel low green, k-spar pale grey-plnk and b io gone.

229.8 - 233.6: 30 cm very Intense micro breccia and macro breccia a t 231.

micro breccla developed about

uar tz Feldspar Porphjrx: S lmi lar t o previou 7- n tFiGIS, -

__ 233.1 -- - 233.6: a l l feldspar altered, b i o gone. dark green, k-spar a1 tered t o dark grey-green s o f t but g r i t t y .

233.6 - - - - - 234.7: - _. soapy l i g h t and dark green.

f%$oclase a l te red t o s o f t soapy


, . . . . I

SYMBOLS A N D AEEflEVlAllONS . 10

12 13 PAGE OF

SHELL CANADA LIMITED - MINERALS DEPARTMENT DRILL HOLE OR SECTION DATA RECORD P n o x c i NAME - --39~,T casmii-- ~- ~-

2- . - .. _. . .. .. . . _ PROJECT NO. - ~ - ~ ~ ~ WORK DONE Name OMsr Remarks IIOCEISEC N O - --I. ~

DRILLING:p-p-

LOGGING~ _____ ASSAYINO.

~. .

LITHOLOGY. Tenlure. Slrwtur*. Mimdlmtlm ILllhologI

r s s ? . - r . v

234.7 - 235: soapy yJT& green and k spar a l t e r e d t o grey p ink t o grey green, b i o gone.

235 - 236.2.: s o a p y I v h t and dark green.

236.5 - 237.5: same as 234.7 - 235.

237.5 - 244.4: l i g h t green hard t o medium hard.

p lagioclase a l te red t o s o f t

p lagioclase a l t e r e d t o s o f t

.____I___

mostly plagioclase a l t e r e d t c Loc8 l l y

a l t e r e d t o s o f t soapy dark green.

244.4 - 245.1: same as 234.7 - 235.

245.6 - 246.2: same as 234.7 - 235.

___ 246.2 - 2485.: green x u m s o f t o f t e n w i t h s o f t soapy green cores.

248.5 __ - -- 250.9:

. -_ _ _ __ __ . - .- plagioclase a l t e r e d t o

same 3s 234.7 - 235.

i g h t dark

250.9 - 255.4: m < G - L i Z J f o very s o f t . ..- 255.4 __ - 263,6-: a l l feldspar a l tered, b i o gone; f ig loc lase a1 tered t o s o f t soapy ye1 low green t o dark green, k-spar pa le grey pink t o grey green medium s o f t .

_ _ 256.9 - 263.6: numerous black seams and s l i p s .

263.6 - 273.3.: mainly so f t soapy dark green. some medium so f t white, some cores green and r ims o f whi te .

p lagioclase a l t e r e d t o whl te ,

Breccia. micro and macro,

p lagioclase a l t e r e d t o

1 . . . . I

Strwtur.1 A+. SYMBOL C.AJDIp

SLIPS:

232.7: 25' toC .P ?33: 50"" " Z33.6: 70" " " !36.5 : 70" " " t45.7 : 50" " I'

!48.4:60" " " !48.8:60"" 'I

!49.5:20" " 'I

!49.6:50"" ' !57.2:40"" "

37 .8 : 40' " HWof bx zone

?60.8: 50' toC .A ?61: 50"toC.A !61.3:55"" I'

45"" "

!61.4:25"" "

!61.5:45'" " !62.2:40"" "

!63.5:45"" " FM o f bx Lon

!67.7:60" toC .A w i t h 10 cm m i crobx

!72.2:?0" toC .A w i t h 10 cm rnicrobox

!4a.9:70"" 18

TO Feet

79 - 2 - 77 780 - 790 t Quart z-Mo!

79 - 2 - 78 790 - 800 As above.

t---- ..._____

79 - 2 - 79 800 - 810 As above. some l o s t .

-

19 - 2 - 80 810 - 820 As above a I +---

79 - 2 - 81 820 - 830 Veins and Much broke

I------ '9 - 2 - 82 830 - 840

Mainly as -

'9 - 2 - 83 840 - 850 Mainly ve l

- __ I____ - '9 - 2 - 84 850 - 860

As veins a

'9 - 2 - 85 860 - 870 As veins a

I

- INT. N FT -

10 + I

IO

-_

._

10 jevc

-_ 10

f M c _ _ _ 10

I nor cor - _ _ 10

i a r t __ - 10

i . 5 __ 10

I sn -

10 I sn

-

99 0.01 r i t e veins.

.loo 0.0

-- - -_ ____ -

- - -- ____ - 3100 o.o< a1 c ~ a r s e b

97 0.0' sm!ars. I

-- - -

75 0.0: l t s s !minatic

- - - _ - - - 70 0.1

MoS, f pyri - - - . - - -

80 0.Of ne d ssemini -_ - . - -_ - .

94 O.O! t o 0.1 n brecc i r s '

- -. -_ _ _ - 87 O.OE

i r s . Sone 1

SYMBOLS AND ARAREVlArlONS . _ - -

L A T l r U M DErARTUnE ELEVATION IDATUM) ------ ~~ FIELO

N E

.~ LOCATION - SURVEY G R I D L __. ----

BCAnlNG

AZ

t

___-- T o t a l A S S A Y n E s u L T s

- NT. I FT -

10

-_ IO

- 10

10

__

SAMPLE No.

ROW Feet

170 - 880 is veins. - 180 - 890 1s above.

Strvctud Awl* iYMBDL C.AJDlt,e

LITHOLOGY. Textus, Structun, Mirrr.lir.ltm IL l lholq)

- - -v ‘” ’ I

.048 .080 - - 273.3 - En!,: wh1-m hard, some s o f t soapy, some hard. Local ly s o f t soapy l i g h t green.

. 266.5 - End: many t h i n quartz-MoS f p y r t t e veins 0.05 - 3 cm t h i c k n l t h scattzred HoS2 - almost a stockwork I n places.

N.B. : m a s p a r porphyry f r o m near end.

END.

plagioclase a l te red t o mainly

Take Tlifn Sectionof t yp tca l quartz

____

‘9 - 2 - 86 0.02

0.0;

- -

0.Oi

O.O!

-_I

19 - 2 - a7 ,054

-

.148 )90 - goo i s above.

’9 - 2 - 88

______-

‘9 - 2 - 89 .054 .090 !77.4 (910‘) IO0 - 910

Is above.

SMEET INTERVAL. Itom ” UVNOBlV

33- 0 - 4

4.0 - 64.6

Cas1 ng (Overburden).

()yarJz_Monro_ni tg: grey, f ine-wdium-grained pink k-spar pFenos 52 - 10% o f rock (conmon- l y O . 5 t.0 1 cm long, p e r t h i t i c , some ninntled), plagioclase phenos 0.5 cm o r less

long 10 - 152 o f rock, bio. 7 - 102, some very f ine-grained looks l i k e pepper f lakes.

Ppirie.: veins. __ Ilagneti te: . . - 0.01'. rock without plagioclase a l te red t o green i s moderately t o almost s t rongly magnetic; rock w i th plagioclase a l te red t o green i s moderate t o weak o r non inagnetic depending on i n t e n s i t y of a l t e r a t i o i

4 - 7.5: plagioclase opaque white but hard.

7.5 - 13.3: --. plagioclase a l te red to l i g h t green, hard; a few spots with some plagioclase a1 tered t o so f t soapy green.

- 13.3 . - - - - 14.3: green hard and p a r t i a l a l t e r a t i o n o f feldspar i n m a t r i x t o white c lay min, producing c r m b l y core.

- 14.3 - 24.5.: green hard.

. W ~ ~ 24.5 le -.-_ - 26.7.: - t o C.A . green hard. imposed on l i g h t green).

4 . 1 2 some disseminations, mostly i i



plagioclase a l te red t o soft,

Some plagioclase a l te red to l i g h t (Appears that s o f t whl t e super-

Adjacent t o several fractures -20

Slruclurd An#* YMEOL C.A./Dip

SAMPLE No.

9 - 3 - 1

- -.

9 - 3 - 2

9 - 3 - 3

9 - 3 - 4

_-___.

9 - 3 - 5

9 - 3 - 6

9 - 3 - 7

9 - 3 - 0

12 - 20 8 P y r i t e be r i m

I--- Mainly i n t h f i One such e i n

30 - lo

50 - 60 I U Some core losj I . - -. - -

70 - 80 10 MoS2 as alove

80 - 90 10

. - - ._ . - _- .

As above. I.

90 - 100 10 As above, but

(Anhydrite cou

I

rac ures wc "1 < O * O 1 I -- 1 -

05 0.02 r t z f p y r i l

s i c ks i r I -- 85 0.06

_ _ 90 0.06

t rn, i n quar . - . - - . . - - 100 0.03 r i t ! veins ve ns los!

. - - . - - - - - -

100 0.05

- - . . __ __ - 100 0.03

- - - -

100 0.03 so .everal he a te r t t

1 A S S A Y R E S U L T S

'f- .011 .018

(nil) . . . -

- . .-

.-

lost.. . . .

__

- ... - - - ~

SYMBOLS AND ABBREVlArlONS . . - . - __ SMFEI I N I E R V A L horn I"

MVEIOWV


-- ADDITIONAL INFO ASSAYING.

FIELD LOCATION SURVEY

64.6 - 74.2

74.2 - 109.0

LITHOLOGY. Tixiwe. Slrwlure. Mlnraliralion !Lllhalql

l . . . . l

k-spar f quartz muscovite and p y r i t e a l t e r a t i o n veins: 4 - 1Om: 10 veins 10 - 15m: 1 vein 15 - 1Em: 19.3 - 19.8: 4 veins 20 - 37 * about 1 per met re ~ o s t few are about 45 .

13 veins (about 5% o f rock)

vein8 are SO' - 90' t o C.A . a

26.7 - 63.4: -- plagioclase mainly opaque wh tl

hard, although adjacent t o c e r t a i n f ractures i t i s s o f t white except: plagioclase a l te red t o l i g h t green hard.

63.4 - 69.6: fCghtGg hard, except:

44.8 - 47.4 some


plagioclase a l te red t o 64.9 - 66.0: s o f t soapy green; i n places b io . gone and rock crumbly or even sof t c lay due t o c lay a l t e r e t i o n o f matr ix feldspar.

Ap l i t e : p ink i sh grey, f ine-grained matr ix o G u x and feldspar, b io 5X, plagioclase and small pink k-spar phenos (mostly <0.5 cm) 10% o f rock. No quartz phenos.

P r l t e : <0.012 as t h i n velns. & x - i t e : <O.O l% rock weakly magnetlc.

Between 73 and 75 m i t grades into f i ne grained quartz monzonite o f next i n t e r v a l .

Quartz Monzonite: -.-- -- pink-grey, fine-medium-

9 plagioclase mostly 0.5 cm l o n k-spar mostly 0.5 to 1 cm long!: [ lo . f ine- medium grained. 5 - 7%. t o 0.5 cy diameter.

r a i n e K l 0 - 15% phenos o f feldspar Ink

Occasional quartz u

Sl~uclural An#* iYMROL C.AJ0i.C

SAMPLE No.

79 - 3 - 10

.I__I_.

79 - 3 - 11

-__-

79 - 3 - 12

. ___

79 - 3 - 13

79 - 3 - 14

79 - 3 - 15

~-___

79 - 3 - 16

--__-_ ___ 79 - 3 - 17

__ ____ .

79 - 3 - 18

___I__

79 - 3 - 19

FROM . TO Feet.

100 - i i a Quar tz-Ma

110 - 120 As above.

-__

-_--

120 - 130 As above.

130 - 140 As above.

140 - 150 As above. -____ 150 - 160 As above. __I

160 - 170 As above.

170 - 180 As above.

180 - 190 As above.

190 - 200 As above.

-

-____

-- E S U L l

I" SIIEET INlEFlVAL lrom

MVNWYV

POLlTlCP

L+L2 ADDITIONAL INFO


LITHOLOGV. Tsiturs. Slwctwe. Monrallratim N.ithol~1

-,,..., This phase resembles both quartz feldspar porphyry unit 3 (but it has few quartz phenos, more bio and is coarser grained) and quartz monzonite 1 (but Is finer grained Important that it is gradatlonal with aplite which is probably a border phase.

69.6 - 75.7: opaque white hard although a few altered to light green and 72.3 - 73 altered t o light green hard.

75.7 - 83.0: plagioclase altered to llght green hard, except 76.9 - 78.8 plagioclase a1 tered to soft soapy green with several intervals o f matrix feldspar altered to clay making crumbly core.

83.0 - 86.0: except white soft adjacent certain fractures parallel core axis.

86,o - 86.3: green.

86.3 :.94:2: pervasive green alteration; alternating sections still with bio und without bio, the latter also with strong alteration o f matrix feldspar to white clay producing crumbly or soft core.

94.3 - 1052.: plagioclase altered to lfght greenhard. local patches plagioclase altered to soft soapy green.

-- 93: grained quartz monzonite lb.

most plagioclase altered to

plagioclase opaque nhlte hard

plagioclase altered to llght

Texture strongly resembles fine-medlum-

# . . . . I

Structural Aylm YMBOL C.A.IMp a

- - E S U L T S

MVNWZV

I

A . - LOGGINO:

_ _ _ ~

LATITUDE DEPARTURE ELEVATION IflATUM) BEARING

N E A 2

FIELD LOCATION SURVEY GRID :--

1 --

109.0

109.0 132.3

132.3 133.9

ROM Feet

290 - 300 Quartz No!.2

300 - 310 As above.

310 - 320 As above.

320 - 330 As above.

330 - 340 In quartz.MoS2 __ - ___

105.7 - 112.5: crunibly t o s o f t clayey core l@-oundniass feldspar a l t e r ed t o white c lay) except: 108 - 110.3: several zones compose mainly of bands, s t r i nge r s and whisps of black, grey and purple clayey material . Ahout 50% of t h i s in te rva l composed of t h i s

INT REC Est. Total A S S A Y INFT x E n Y ~ 0 s Mo Mos7

ox I40 10 90 0.06 ,041 .OG9 f J y r i t ? veins. - - -- -~ ..-(!!L! 1

10 e100 0.13 .078 .130 Abolit 2UL of vef IS l o s t n cor1

~ _ ____I - - . - ( n i l ) - - -.

__ (nil-) ._

_ _ . _- ( n i l 1

__ - - . - -. - - __ __ - (nil L

10 e100 0.02 a020 .033

10 96 0.06 .046 .076 Somi qua*tz-MoS2 l o s t in coring

10 93 0.03 .011 .Ole vein : , a l so , s M0S2 . , l t p s H

material . A h u l t zone3 Yes. most surfaces s l ickensided. (Simflar t o zones i n 79 - 1) .

340 - 350 As above - Sone MoS2

350 - 360 Quartz-Mo' Probably

S t r ingers to

70 C . 8 . f 45O t o

10 98 0.15 .114 .190 vei s an1 s l i p s .

l o s t in citrlng (a iproxima ;ely 20 ~ _ _ (n i l 1

10 95 0.05 -031 .04R f y r i t 1 veins. Crwnbl:, core

rbme S2 "ost in I.oring. I ~ .002

Footwall of zone of black s t r inge r s and seam , 1.e. F.W. of f a u l t zone.

Quar t z Monzonite: pink-grey, medium-gralned k-spar porphyrit ic. Differs from 74.2 -+lo9 by having k-spar phenos la rger (1 X 2 cn-) and nnre abundant (10 - 152 of rock).

112.5 - 117.1: l i g h t green hard, some a l t e red t o s o f t soapy green. 10 cm crumbly clayey core a t 116.4 m

117.1 - 132.3: plagioclase a l t e r ed to s o f t soapy green except:

f most plagioclase a l t e r ed t o __--__--

I I__---

121.7-122.5: plagioclase s l t e r e d t o l i g h t green hard. 124.7-125.6: plagioclase a l t e r ed t o l i g h t green hard.

and 118-121: pervasive green, bio gone. 122.8-123.1: pervasive green, bio gone 124-124.4: pervasive green, bio gone. 125.8-131.8: pervaslge green, bio gone 131.8: S l ip plane 45 to C . A . . slickensided MoS2.

s t r i nge r .

. Aplite: Upper contact 5' to C . A . . abrupt bu d i f fuse ; lower contact s l i p along black clay

Probably a dike sub-parallel t o C A . 1 360 - 370 As above;

370 - 380 As ahove; _____I__

M U L E b.

10 95 0.01 .027 .045 cruiil ly c w e .

( n i l ) _ _ _ _ . _ _ ...

10 98 0.04 .024 -040 ayprtxinia e ly 102 of MoS2 ve lns

(n i l 1 .- ..

'9 - 3 - 25

_I_-

'9 - 3 - 3c

'9 - 3 - 31

i__l

9 - 3 - 3 2

9 - 3 - 3 :

I_-___

9 - 3 - 3 4

9 - 3 - 3 5

_____ 7 9 - 3 - 3

7 9 - 3 - 3

E s u c r

~_ ~ _ _ - SYMBOLS AND ABBREVIATIONS _ _ _ . ~ I O . SHEET INTERVAL I,nm _..

MVNOOIV


I I I I 7--l-----1 ___ LATITUDE OEPARTURE ELEVATION I D A l U M l R E A R I N G ~ N C I INArlON: LENGTH I

FIELO LOCATION SURVEY GRID N E A 2

DEPTIf M ~ --

133.9 - 163.5

LITHOLOGV. Tarlure. Struclura. Minrdi r r t ion ILIlhalag~

I ' ' . ' l

quartz Monzonite: pink-grey, medium-grained k-spar p o r p h y r n i c . k phenos c o i m n l y up t o 1 X 2 cm o r la rger and 15 - 25% o f rock.

Pyr i te : (0.01 mostly i n velns i n mineral ize sections, on ly traces elsewhere. Magnetite: <0.01 disseminatlons, rock mad t weakly magnetic.

132.3 - 150.9: most plagioclase a l t e r e d t o l i g h t green hard, although several shor t i n t e r v a l s plagioclase a1 tered t o s o f t soapy green.

In te rva ls o f crumbly, clayey or s l l g h t l y critmbly core due t o varying degrees o f a l t e r a t i o n m a t r i x feldspar a l t e r e d t o whi te c lay mineral a t :

123.9 - 124.4, 125.8 - 126.5. 127 - 127.7, 123.5 - 129.2, 133.9 - 134.4. 135.2 - 136. 139.9 - 135.5.

~ ~ ~ ~ ~ ~ ~ % . % : Fau l t gouge and c lay a 1 teration.--

--- 150.9: sl ickensided MoSZ s l l p 45' t o C.A.. minor f a u l t .

150.9 - 163.5: pervaslve reen a l te ra t lon , 6 f i i e x Z p t : 152.4 - 754.0: plagioclas a1 tered t o soapy green, b i o present.

_- N.B. 154-154.4: almost complete s i l i c i f i c a t i o n , inc lud ing r e l i c t phenocrysts. before s i l i c i f i c a t i o n .

This was a f a u l t breccia

Structural Anqla VMBOL C.AIDip

: l i p 50' t o C . A .

SAYICE No.

'9 - 3 - 3f

9 - 3 - 3 9

9 - 3 - 4 0

9 - 3 - 4 1

9 - 3 - 4 2

9 - 3 - 4 3

9 - 3 - 4 4

9 - 3 - 4 5

9 - 3 - 4 6

9 - 3 - 4 7

IO s w p r INIERVAL ilnm

MVNOdZV


GRID

14 PAGF or. . r n u J E c T NAME C a w ._ -~ r n o E c T NO IIOLFISFC NO 79 - 3

_ - 3991T- _ _ - -.

163.5 211.2

''.V''..1

157.2 - 160.3: b i o present.

Note: 152.4 - 154 and 157.2 - 160.3 are alsc h z r v a l s o f s l f g h t t o d i s t i n c t l y crumbly core due t o i nc ip ien t t o d i s t i n c t a l t e r a t i o n o f matr ix feldspar t o clay.

s o f t clayey core due to

crumbly core due t o

160.9 - 161.7: a l t e r a t i o n feldspar t o clay.

162.3 - 163.6: p a r t i a l a1 t e r a t i o n matr ix feldspar t o white clay.

Quartz Monzonie,: pink-grey . nedlun-grained I k-spar po rphy r l t l c . k-phenos m s t l y (1 cm, but some t o 1 X 2 cm; bio flne-medium-grainec 5%; considerable f ine-grained pink k-spar i n groiindmass gives rock a pink t i n t . IS t h i s k- spar nie ta soma t i c ?

rock moderately magnetic. t h i s I s l b o r simply a f l ne -

grained 1. and 79.3, 214.6+. be p a r t o f 3).

163.5 - 169.7: - green hard except 167.7 - 168.2 plagioclase a l te red t o s o f t nh l te .

. 169.7 _ _ - - 176.1: pervasive green a l t e r a t l o n w i t h nii-6To; several I n te rva l s o f j u s t plagioclase a l te red t o so f t soapy green.

176.1 --- - 194.2: - most plagioclase opaque whitc hard, a1 though some has i nc ip ien t green a1 terat ion.

Same as 79-1. 249.8 -'279.8 By r e d e f i n l t l o n these may


l . . r r l

SYMBOLS AND AOOREVIATIONS . - _.._

SAMPLE No.

7 9 - 3 -

7 9 - 3 -

7 9 - 3 -

7 9 - 3 -

7 9 - 3 -

7 9 - 3 -

7 9 - 3 -

7 9 - 3 -

$ 9 - 3 -

7 9 - 3 -

mow .. INT. REC Est. TO. F e e t . ._.... IN '1. 'VERY - i j

48 480 - 490 10 ~ 1 0 0 0.15 Quartz MoS. f p s V r l t e veins. some %s2 ' os t n co 'ing.

~ ~_.. -. ._.

49 490 - 500 10 98 0.03 As above. Some MoS2 l o s t i

~ -- .- .

50 500 - 510 10 85 0.05 As above. 25% o r mo*e o f M

_I____

51 510 - 520 10 95 0.1 As above. 25% u r mo-e MoS2 _ _ _ _ _ .- . .-____

52 520 - 530 10 80 0.05 9s above. 25% r M 'e MoS2 One vein pirallcml co1.e f o r . __ - __ . . . _ _ . __ .-

53 530 - 540 10 75 0.15 4s above. Probi b l y 10% ( a t

. . __ _ _ -. __ 54 540 - 550 10 90 0.02

As above. Son@ MoS2 l o s t f . __ - _ _ _ .. _- - -. . .

55 550 - 560 10 95 <0.01 . __ _ _ .--

56 560 - 570 10 ~ 1 0 0 0.15 MoS velns and uart.-MoS ParPs of s2 v ins ' o s t I n ._.__ 1 98 0.1

57 570 - 580 Quartz-MoS vel s ? p y r i t e .

Total Mo

.064 Also s(

.013 cor 1 ng

.OG2

-

N 2 l o s t ___..

.054 o s t frc

.118 o s t frc " I .

.284 east 2!

.032 lin brokc .

.038

. 082 p y r i t e or ing.

.029 some MI

, S S A Y R F S U L I S pi le ( n i l ) disse i i na t i o i

. - __ - _ _ - __ -

.090 I f r t a b l core. (?!!I. -. _ _ _ _ __

.195 I bi-okeii core. .001

-474 ; /!I!!.-/! o f Ho l o s t

.137 Ieins. ( n i 1)

- . _ _ . . . . -. - .

i1 l o s t . I ( n i l 1

_ _ ~ - SHEET I N I E R V A L lrom I"

MV?J(I(IYV


7 14 PAGE- - -OF - _ _ _ _ PROJECl NAME ~ c!?sE___ _ _ PROJECT N O - _ _ _ 3991T- - _ _ I IOIF ISFC NO - 79:3 - __.___ ~ _ _ ___ __ WORK DONE Nema Detn Rcrruvks

DRILLING __ - L A T l l U M DEPARTURE ELEVATION IDATUM) RFARlNG 1141 L l N A l l O N L F N G l I i ~~~ - __ ~ _ _ _ _ ~ - FIELD ~ ~ _ _ - LOCATION SURVEY

LOGGING

N E A2 ~ _ _ - - GRID -- -- ASSAYING - ~~

ADDITIONAL INFO -_

TO Feet . 7 Slruclud An#. SYMBOL C.A./DIp I oePr7M LITHOLOGY. Texture. Siructun. M l n a r d l r e i l a n (Lllhnla(ll

rn . ( . , . .

I F S U L

176: =e f ine-grained quartz i n matrix and less Plagioclase. I t borders on grani te .

169.1: 10 cm a p l i t e d ike 40' t o C.A.

170.9: 15 cm a p l i t e dtke 40' to C.A.

. Exceptions _..._ t o plagioclase a l te red whlte hard w0-l 180.7: plagioclase a l te red l i g h t green hard. 183 - 183.8: plagioclase a l te red l i g h t green hard. 184.6: soapy green adjacent t o a MoS vein. 188.3 - 193.6: t o s o f t white i n fractured i n te rva l s . 194.2 - 194.9: 1 i g h t green hard. 194.9 - 195.3: pervasive green a l te ra t i on , b i o gone. 195.3 - 195.8: plagioclase a l te red t o l i g h t green hard. 195.8 - 205.0: plagioclase a l te red t o white opaque hard. 205.0 - 206.7: plagioclase a l te red t o l i g h t green hard. 206.7 - 207.2: plagioclase a l te red t o sof t soapy green w i t h 25 cm b i o gone and a quartz-tbS2-pyri te ve in i n the middle o f the no bio. i n te rva l .

Rock i s a l i t t l e f i n e r grained. w i th

10 cm plagioclase a l te red sof t

Some plagiocl%se a l t e r e

plagioclqse a l te red t o

207.2 - 210,0,: opaque white hard.


rg - 3 - 58 580 - 590 quartz -Mo

-1oc O.OL IS f i y r i t e .

? loo 0.0:

- . . __ _._

~

=loo 0.02

-100 0.01 _-_ ____ = l o 0 0.05 s .t i y r i t e .

-100 0.01

- .- - _ _ - ._ __

_____ .- 2100 0.15

--to0 0.05

.. - -. - .- -.- - ..

e100 0.02

.- . .. . ._ _- ___ =IO0 0.02

--

' 9 - 3 - 59 .032

__ .037

.053

( n i l

.061

( n i l

.055

__

-. -__

-W!. . oao

( n i l

.060

( n i l

. I33

.012

__ - .. -.

_ _ - .

590 - 600 As above.

600 - 610 As above.

610 - 620

620 - 630

' 630 - 640

,quartz b' __

As above. - ___.I___

640 - 650 As above.

' 9 - 3 - 6

' 9 - 3 - 6

' 9 - 3 - 6

9 - 3 - 6 .

9 - 3 - 6 d

9 - 3 - 6 !

9 - 3 - 6 f

9 - 3 - 6 ;

.033 - -. -

.048

.036

.068

. lo2

._ - -

.024

650 - 660 As above.

.I70

( n i l :

.040

( n i l J

.053

.002

- - - -. . -

-. - .- - -

660 - 670 As above. ___ - -

670 - 680 .034 210.0 - .-. .. - .

SYMBOLS AND ARBREVlATlWS -~ ~ _ _ _ _ 1" SIIFET INTERVAL lrnnl

MVNIM?V


L A T I T U M FIELD LOCATION sunvw

L O G G I N O ~

ADDITIONAL INFO. __ __ ASSAYINO:

- FOAU UNIT -

1

-

~~ ~

SlrucIu.( A d @ YMBOL C.A JOip 4

Faul t 60' t o C.A.

-- E S U L T S SAMPLE

No. FROM

10 Feet

As quartz 680 - 690

LITHOLOGY. rsrcur.. Slruciur.. Minr~llr.Oon ILithalopr - , . , . . . . - N.O.: -- Questionable whether 163.5 - 211.3 i s u n i t 1 o r l b . The l a s t 15 m s t rongly resembles u n i t 1. Yes, same as 79-1, 249.8 - 279.8 and 79-3, 214.6. (By r e d e f i n i t i o n these may be p a r t o f 3).

211.2: slickensided. moly-smeared black c l a seam w i th adjacent 5 cm F.W. breccia zone. A f a u l t contact.

Quartz T e l d ~ P o ~ p J y ~ : Top 6 bottom contacts are aufts.

. 212.2: __. smeared, 10 cm adjacent breccia zone chat-acterized by crumbly core.

N.B.: Some of the granulw. f ine-grained quartz r i ch , crumbly i n te rva l s rev ious ly logged i n 79-1 and 79-3 may be 8reccla zones

211.5 - 220.2: plagioclase a l te red t o l i g h t g r e m s o f t - g d - soapy; some plagloclase a1 t e r e d - t o s 7 i f t whTte:

__-- 214.6: sl lckensided c lay zone wlth adjacent granular textured, semi-crumbly core w l t h In tergranular aphanl t l c n h l t e mater ia l t ha t i s robably f l n e l y ground quartz and feldspai

logged previously i n 79-1 L 79-3. or-. posslb such crush zones are p a r t l y a1 tered.

QUartw-&n-~o~itt.: pink-grey, medium grained sparcely po rphy r i t i c w i t h pink p e r t h i t i c k-phenos up t o 1 cm long.

----I__ 214.6 - 219.0: clear. i n tyc. dfrect ions contr ibutes t o

Black c lay seam, sl ickensided 6 M o S p

r a t R er than feldspar a l t e red t o whlte c lay (I'

weakly developed fractures

unblv s t ructure.

7 9 - 3 - 6

7 9 - 3 - 6

7 9 - 3 - 7

0.04 t p y r i '

0.03 690 - 700 As above.

700 - 710 0.01

0.02

.074 .- -.

.066

- -

-060 lost fl

211.3 - 214.6

Faul t 45' t o C.A.

710 - 720 As above.

7 9 - 3 - 7

7 9 - 3 - 7

7 9 - 3 - 7

7 9 - 3 - 7

720 - 730 As above. __ ___-_ - 730 - 740 As above. .

740 - 750 As above.

0.03 02 MoS, ,

0.02 ox Mos;

0.03 l o s t .

.132 lost fl

___-_ - .050

?14.6 - 231.1

SYMBOLS AND ABBREVIATIONS - -. - - - - SliFFT I N I F R V A L from I"

MVNWfV

POLITICAL UNIT

I . 1 I ADDITIONAL INFO __

231.1 - 319.0

DRILL HOLE OR SECTION DATA RECORO

WORK DONE N a m Dales Rnrurka

DRILLING ____ LATI IUDE FIELD LOCATION SURVEV

- .~ - - ----___ LOGGINO

_ _ _ ~ ~ ASSAYING.

- LITtlOLOGV. Tsxlurs. Slruclurs. M i n r d l r a i l m I L i i h o I ~

- . - 7 . . ' . I

220.2 - 225.9: wh&ilTbTattered local patches o f soft soapy light to dark green alteration.

plagioclase altered to soft

- 225.9 - - - 227.2: most plagioclase grains a l t e r e d m i g h t green hard, some white hard.

- - 227.2 - 228.9: to soft soapy green, bio gone.

Complete alteration feldspar

228.2 - 229.0: local breccia bands.

Crumbly core with

228.9 - - - .- 230.4: plagioclase altered to soft soapy green. blo still present, some of k-spar has a brownish to deep salmon colour.

- 230.4 I---- - 238.8: aTtered to soft soapy green.

complete alteratton feldspar Relict textures

230.4 - 231.1 : medium-coarse-grained. 231.1 - 232.7: fine-grained. 232.7 - 238.8: dominantly fine-grained, some medium-grained components. Includes several short Intervals o r plnk fine-grained quartz monzonite or granite with small plagioclase and quartz phenos.

!'!!artL.jzoli te: pink, fine-grained to medium-grained; 'sugary' textured groundmass plagioclase porphyritic. a few quartz phenos.

- Pyrite --- ~0.1% - Magnetite: -. - _-. inodera tely magnetic.

0.01 to 0.1. non-magnetlc to

Contact at 231.1 is based on change of texture in altered rock marked by a slip.

L. I . I . . . . I

Slrwlural An* YMBOC C.AJDlp(

m.R:sLiP 60 to C . A .

31 .O black lay slip 45' D C.A.

3 to C.A. 3a.4: slip

y.1: s l i p i to C.A.

I" SIIEET INTERVAL l r w m

MV)IOOYV

I

SHELL CANADA LIMITED - MINERALS DEPARTMENT PAGE _ l o - - O F - _ _ _ 14

DRILL HOLE OR SECTION DATA RECORD P n o K c T NAMF - C a g ~ q - - -

PROJECl N O -. _ _ 399! HULEISEC NO __ -7_9, ._

T- -

____ FIELD

N

____I__

WORK W N E N w Oatan A ~ n u i h s

DRILLING __I ________ LATITUDE DEPARTUPE ELEVATION IDAIUMI BEARING _ _ ~ _ _

-- - LOCAI ION SURVEY GRID

LOGGING

E A 2 -____ - ASSAYING I__ ___-_ ______ .__

- E S W L T

--____- blruclvrd And.

iVMBOL C.AJDIp

--__ 242.3 - 243.3: f i n e l y dlsseminated hematit ic a l t e r a t K 3 feldspar, gives rock a browntst colour.

238.8 - 245.2: g r e e n m - a z d s o f t soapy green.

245.2 - 247.7: ~. a l t e r i n g t o s o f t soapy green, b i o gone.


complete a l t e r a t i o n feldspar

core crumbled, probable

plagioclase mostly a l t e red t o

247 - 247.3: s l i p .

241.7 - 248.9: T G h T g r e e n a r d except a1 tered t o wht t e sof t adjacent f ractures p a r a l l e l t o core.

248.9 - 250.0: plagioclase a l te red t o s o f t soapy green.

250.0 - 256.0: m s t plagioclase a l te red t o l i g h t green hard, although some grajns a l te red t o soapy green.

-. 256.0 __ - 258.3: -.

soapy green and b i o gone. a l l feldspar a l t e red t o s o f t

IO 99 0.01

--

10 97 0.02

10 95 0 .06

_- - - - 10 98 0.08

~

10 99 0 . 0 3

- . -. _- ____ 10 -100 0.06

- - - .- - - _.__I .

10 = loo 0.12

-_ _. MoS2

10 = loo 0.08 Moi2 ve n sub-l:

10 99 0 .02 s w o l l a usual t z Tveins up t o 1

ome quar:z

. ~...

~

.082 ' .137 ( n i l )

.076

.128

.om

.114

As above.

I----

As above.

As above. .294

tins 2 .488

n t h i c l .001

.

79 - 3 - 91 910 - 920 As above.

257 - 258.3: 3- t o 257.3.

crush zone w i th f a u l t gouge .237

i r e act (n!! 1- .070 tz veir .(ni l 1

. l42 a l l e l

_ _ _ . ..

.042 I n qua m th i c

- 258.3 -- - 260.3: a T t e r e a - s T T g h t green hard and p l aglocl asp a1 tered to s o f t soapy green.

260.3 - 262.5: plagioclase a l te red t o so f t white I n zone w i th f ractures suh-paral lel t o core.

a l t e rna t i ng plagioclase I As above. bearing qu

, . . . . I

_ - __ ~

SYMBOLS AND AEBREVIAllONS 1" S I tEEl I N I C R V A L I e o w

MVNbCYV

-- POLITICAL UNIT

I A I __ AUDITIONAL INFO.

LOGGINO:

ASSAYING: ..

PAGE.-/^- OF 14 ____ SHELL CANADA LIMITED - MINERALS DEPARTMENT

DRILL HOLE OR SECTION DATA RECORD PROJECT N A M E . cc?? . _ PROJECT NO.'-. . 3gq1 ~

HOlElSEC NO 7g-IIj-I ~

Dats, A e w r k s

- LATITUDE DFPARlURE ELEVATION IDATUMI BEAnlNG _____ FIELD

LOCATION SURVEY GRID

-__-___ N E AZ.

.- .

- ann JNIT -

-

"'"0 N.B. : n o n i n t h i s and 79-1 and 79-2 i s phenocryst not groundmass plagioclase (except f o r a l l feldspar a1 tered t o green). Groundmass plagioclase usual ly remains white whi le plagioclase phenocrysts a l t e red t o l i g h t o r soapy green.

262.5 - 267.3: plagioclase phenos a l te red t o nq%t green hard i n r i m s and sof t soapy green cores.

267.3 - 271.6: ___ plagioclase white opaque hard except T o c a l l y a1 tered t o l i g h t green.

271.6 - 272.5: plagioclase phenos a l te red t o 71ght green hard rims, s o f t soapy green cores

-I 272.5 - 273.5: - - a l l feldspar a l t e red t o s o f t soapy green, b i o gone.

273.5 - 274.8: Plagloclase phenos a l te red t o li7jm green rims, s o f t soapy green cores.

2]4.8_=-277-.7.: a l l feldspar a l t e red t o sof t soapy green, b i o gone.

277.7 - 282.5: mainly plagioclase a l te red t o 7mt green hard rims and s o f t soapy green core.

. 282.5 __ .__ - 286.2: soapy green, b io gone.

286.ZL292.8_: a l l plagioclase a l te red t o sm soapy green, b to gone, remaining k-spar has deep salmon colour. Thls i s a new type o f a l t e r a t i o n .

the plagioclase used t o define a1 te r -

a l l feldspar a l t e red t o s o f t

- . I . . . . I

MMPLL No.

7 9 - 3 - 9

7 9 - 3 - 9

1 9 - 3 - 9

1 9 - 3 - 9

1 9 - 3 - 9

rg - 3 - 91

r9 - 3 - 9'

'9 - 3 -101

FAOM

TO Feet ..

930 - 940 Mainly i n th i ck quar One seam 5

__I__

940 - 950 Quartz Mo! s l l p s w i t t --I__

950 - 960 Quartz Mo: not count€

960 - 970 Quartz MoS a t l eas t 2

910 - 980 Quartz MoS

980 - 990 As above.

990 - 1000 As above. .- __

1000- 101 0 As above. Some MoS2

202.

: seams tha t 1( 1-

ent to x Mos

i n c6

era1 1

t r i nge

- 2 c

w.

ck c ls

i s

re -

__

SYMBOLS A N 0 AflEREVlArlONS - _ _ S t I F E l I N I E A V A L Itom I"

MVNWYV

i

14 PACF ~ 12 _ _ o r - _ -

PROJECT N O 3991T


DRILL HOLE OR SECTION DATA RECORD PROJECT NAME &e?!!!- - _ _ ~-

-. - ._ . ___ ---7!i - 3 - - tIOLEISEC N O .

--_. Dales Remerki

LATITUDE OEPARIURE ELEVATION (OATUM) BEARING INCLINA r lON L E N C l H - ___-- FIELO

-- LOCATION SURVEY

~~

N E A2 _____ _

WORK DONE Nan*

D R I L L I N G ' ~ .

LOGGING. .

__ ASSAVING:

L A - AOOITIONAL INFO

- NT. I r i

1

r t

-

+

-

11

-

s t . Total A S S A Y R E S U L I SAMPLE No.

nOM o Feet

010-102( luartz Mi n thick

Struourd Ando SYMBOL C AJMp

!85.5: 30 cm ni cro brec6i a ; ? s l i p s 60 t o :.A.

?91.2 - 316.0 'crush zone' vi t h micro- weccia s t ruc . ; l ips at: !91:40 $0 CA !91.6:45, t o C !94.1:400 t o C !97.0:45 t o C !97.2:45' t o C !98.2:40° to C !9a.9:30° to c 301.2:45' to C 302.0:45' to C 302.6:35' to C 309.9: 30' to C 310:30° t o C.I

s l i p s , 30 toCI

312.3:55' to C

312.7:80° to C

312.8:45' to C

314.8:75' to C

310-311.566

~~

led ro it.

os3 0. oa

reins. Most

79 - 3 -10

79 - 3 -10

291.2 - 316.0: crumbly L , in places, clayey Core Z u s h z o n e . -. 292.8s0.5_: plagioclase phenos a l t e r ed to sofi-soapy aark green, bio present. places rims a r e l i g h t green and semi-hard. Except: 302.5 - 303: a l l feldspar a l t e r ed t

._ 299:

308.5 - 309:9: quartz vein. 30' t o C.A. I t i s veineaby muscovite and contains r o s e t k s of MoS2.

- Breccia - Zone: Not a l l rock i n breccia zone i? crumbly, but a l l has a d i s t i n c t micro breccia s t ruc tu re consisting of a f i ne ly ground intergranular matrix and in many places numerous shor t ha i r l i ne f rac tures .

The brecciation a f f ec t s the a p l i t e dfke , the quartz vein but not the MoS vein. Some MoS2 has grown $long the ha i r l i ne f rac tures . HOS i s post brecciation, ye t i t i s smeared alon8 s l i p s in breccia zone, there fore shearing i s post brecciation. anhydrite veins a r e a l so post brecciation.

- 316.2: _ _ _

In

green. bio gone.

15 cm a p l i t e dike 40' to C . A .

in the quartz

Thln

15 cm a p l i t e dike, contacts broken.

~-~ 317.6 - 318.0: a p l l t e dike, contacts 45' to . .

316-316.2: 7C to C.A.

317:30° t o CA

317.5:60° to C

Gradational change from f ine t o medium- grained groundmass t o fine-grained groundmass and fewer quartz phenos.

319.0 - 320.0

020- 103( s above.

0.04

- . -- - __ - .. - . . SVMBOLS AND ABBREVIATIONS StlEET I N I E R V A L hum I O

SHELL CANADA LIMITED - MINERALS DEPARTMENT ORILL HOLE OR SECTION DATA RECORD

LATITUDE

FIELD LOCATION SURVEY GRID N

POLITICAL UNIT

DEPARTURE ELEVATION I O A l U M l

F A 2 ___ I- I A I AOOITIONAL INFO

___- .. .~ LANDMARUS: ~ ~ _ _ _ _ . _ _

CLAIMIPERMIT NO: LOGGED BY: OTHER FEATURES.p--.- _. . -. -. -. -. . . . . _- .-

oE7w 320 -

342.8

342.8 - 368.2

LITHO1 OCY. T a x t u c . Structure. Mlnrdlmtlon ILlthdapl

Zone o f quartz veins 1 t o 15 cm th i ck continues t o 323 m.

316.0 - 322.3: b r e c c i x s s intense, a1 though s t i l l present, however 2 0.5 m In te rva l s o f crumbly brecciated core.

322.3 - 331: b e v m f i i c r o breccia s t ructure - broken 6 crirmbly core.

320.5 - 350.2: soapy s o f t and l i g h t green t o opaque white. However, from 336 - plagioclase phenos tojudge by.

331 - 351.5: breccia zone. A t 331 the i j c r o b r e c c i a grades i n t o a macro breccla. w i t h fragments comnonly up t o 1 cm across. Several 1 m i n t e r v a l s o f non-brecclated rock.

Granite: pink, medium-fine-grained, non- po rphy r i t i c . Colour due t o abundant salmon k-spar; 5% bfo. porphyry above i s masked by brecc iat lon bu t appears to be abrupt although w i th no tex tu ra l dif ferences i n e i t h e r phase.

350.2 - 350.7: A l l feldspar a l t e red t o s o f t soapy green, no bio.

. 350.7 ___ - 352: plagioclase phenos a l te red t o so f t soapy dark green cores, l i g h t green r i m s

Core more competent, micro

crush zone w i t h var iab ly

plagioclase phenos a l te red to

there are very l e

Contact w i t h quartz feldspar

- 3 -104

- 3 -105

- 3 -106

- 3 -107

more thae 45 . 339.3:85 t o C

1030- 1040 co.01

Quartz 1040-1 050 MoS 1 ~ 1 ~ ~ 1 0 ~ ~ ~ t p r i t e veins.

quartz vei s . i g n i i can t F

1050-1060 I 101 991 0.02 Rs above. Seve a1 b ack clz

s2 los l

.027 seams

.018

-- .082

5 not c

I--

. I60 t counl

. loo and i r

.088 l os t . __ - _ _

.029

.013 . somc

... ._ . StIECT INTERVAL lrom ID

h lVNM1V '

I . I ADDITIONAL INFO

WORK DONE N a m

DRILLING

LOGGING ____ ___ ASSAYING

14 PAGE . ! 4 .. - .. or ~

SHELL. CANADA LIMITED - MINERALS DEPARTMENT DRILL HOLE OR SECTION DATA RECORD PROJECT NAME ~~. ~ c??? . ~. ~~. .~

PROJECT NO. ~ ~. ~~~~ .?Y9!T- I l01ElSEC N O .. - 7 9 .- 3 . - ~- -

.

OM.) Remarks - .~__- .____ LATITUDE OEPARTUflE ELEVATION {DATUM1 IlEARlNG I N C L l t J ~ N LFNGTH

-~

r

~ ~ _ _ _ FIELD LOCATION - SURVEY GRID

-- __ N E AZ. ~- ~ _.__ -

Ezh

368.2

352 - 353.5: o p z u e w m e so f t .

plagioclase phenos a l te red t o

__ 353.5 - 351.1: soapy green, no b io .

351.1 - 368.2: s o f t soapy green. dark green cores, l i g h t green r i m s .

Except: 367.6 - 368.0: A l l feldspar a1 tered t o s o f t soapy green.

351.5 - 363.5,: but i t i s r ' iadled w i t h microfractures, some w i t h displacements of several mn.

363.5 - 368.2: Variably crumbly core; micro b r e z t o macro breccia.

366.5:

A l l feldspar a l t e red t o s o f t

Plagioclase phenos a l te red t

Core not crumbly brecciated,

20 cm clayey core adjacent t o s l i p .

END. --

Slruclwd Angle SYMBOL C AJDip a

343:10° &o CA 346.5:700 to 349.8: 70 t o 350.1 : 30' t o 350.4:60° t o 350.5 : 60; t o 350.9 : 65 t o 351 .5:60° t o 353.9:25: t o 354 .O: 30 t o 354.1:ljwo a t

40 60 CA 354.8: ZOO t o 355.3: 38 t o 355.8:O t o C 356.4: 30' t o 358.3: 30' t o 359.7: 40' t o 362.1 : 40' t o 362.7: 35' t o 364.3: loo t o 366.5. severa

367.9:05 t o 60-70' t8 CA

IN1 UMPLE FAOM IN r i No TO Fppt

9 - 3 -113 1130-1140 1[ __ __ __ _-

9 - 3 -114 1140-1150 I ( D i ssemi na t ons _ _ - - __ __

9 - 3 -115 1150-1160 1( As quartz f,oS2 - ___ - - - __

9 - 3 -116 1160-1170 II As above. Not

-

9 - 3 -117 1170-1180 1( Dlssemina t ons

- -_- __

9 - 3 -118 1180-1190 1t As above.

9 - 3 -119 1190-1200

__ ___ ~-

1t I n quartz FoS2 - - . ___

1 - 3 -120 1200-1208 e As above. Sonic _- -I - __ -- -

- REC IVF R -

9'

-101 hroi -

2101 PYI

= lo( oun

_-

_. -

-101 nd

9

I

9 ? i n __

9! losl __

-

Total A S S A Y LSL a b ,-

- ~ ... -~ -.(nil-).

ox Ho 4 . 0 1 .015 .025

0.25 .234 .388 hout a .8 m se t t i on . -~ ___ -. . ..>OOl-- t e 0.02 vein: and .013 pu1.e .019 MoS2

0.02 .032 .053

.- _ _ _ _ .002.

ng 2 cnt and sevcbral sm

~ ...- _ _ .-

.. . . - .- . . .. .(.!!Ll-I

0.02 .050 .083 small ! i t c o n t i i uous SI

-. . -.l-n!JJ 0.02 .024 .040

... . --(.nlll nd 0.01 as SI a l l .008 disi:ontinuc .013

. - _-Cni!l

0.04 .030 .059 from c r tinbly co1.e.

. - ..oos. -

___

me 1 .- ..-.

?ins.

l e r t

a r s i

.

; sine

. - S H E E l INTERVAL Itom IO

LWNW?V


""h

o - 7.0

7.0 - 50.7

LITI4OLOGY. Tartwe. Slrucluic. Mwwvallza~lm lLithalql

. . Casing 7

Overburden

Quartz Honzoni te: p f n k - rey, medium-grainec p f n k p m t T z phenos !mostly less than 1Xl.5 cm; a sca t te red few 2x3 cn) some mantled 5 - 202 (normally 102) of rock; snal plagioclase phenos 0.5 X 0 .8 cm. 10 - 15% of rock; bio fine-medim-grained 7%.

Pyrite: approximately 0.1%. some disseminations, nas t ly in veins I patches.

&lr!e_t&: approximately 0.1%, rock moderate to aTmost strongly magnetic.

Scattered patches, f ine ly dissemlnated MoS2 - accoiiipanied by disseminated pyr i te .

. 7 _ .. - __ 15.5: .. -- -

.- 7.0 - 15.6-: white anbgenera l ly hard. Several spots very Paint green a l t e r a t ion .

15.6 - 35.5: groundmass-. Plagioclase a1 tered from 1 ight green to dark green, hard to s o f t and soapy; many places dark green s o f t soapy core and l i g h t green harder rim.

Except: 20 - 20.4: a l l plagioclase dFerFd to-SbTcs%Tpy dark green bio s t i l l present.

a l t e r ed to s o f t soapy green, bio gone.

broken, weathered core.

plagioclase phenos. opaque

plagioclase phenos and

21.6 - 22.0: a l l plagioclase

..I.I..I -- . I

Slructwal Awl. WMBOL

SLIPS:

( f l t.6gouge) 18.9:350to CB (clayey core) 21.6:H.W.of6n zone 45Oto C A

numerous s l i p

C.A.;comprise severa 1 s e t s .

18.5:200to cn

21.6-?9.5:

20" to 450 to

.005

.012

.012 te. S( ached (

.004

.017

.003 ed

.036 lo s t I

.036

(ni If

(n i l 1

.045

.002

SVMBDLS AND A8BnEVlATION.S . ~ . ... - I O swrE r INTFRVAL I..,,~

t

POLITICAL UNIT

8 PAGF ~ OF

SHELL CANADA LIMITED - MINERALS DEPARTMENT DRILL HOLE OR SECTION DATA RECORD PROJFCI NAMF Lasir% -

3991T ._ PROJECT NO

I IOLl /SEC N O 79 - 4 ~.

WORK DONE N a m Dsln Remarks

DRILLING

LOGGING _ _ _ _

ASSAYING _________ _______.

50.7 - 58.5

LITHOLOGY. Tcilura. Strtocturs. MIner.llzaItar (Lltholop)

- , . . . . , 31.8 - 32: a l l plagioclase

a l te red t o s o f t soapy green, b i o present.

21.6 - 34.0; Micro breccia zone. 1/3 core crumbly. snme clayey gouge adjacent some s l i p s . Competent core has some h a i r l i n e f ractures, crumbly core has many micro fractures.

35.5 -.__--I- - 50.7: Breccia zone. Variably micro brecciated and macro brecciated. I n places accompanied by a l t e r a t i o n of matr ix t o whitc c lay mineral. 41.8 - 49.2 intense macro b r c c i a g i t h nuvierous black c lay seams 30 - 90 t o C.A.

. ~ - 35.5 - 50.7: plagioclase t o l i g h t and dark green sof t , soapy.

Most k-spar a l t e r i n g to l i g h t green and g r i t t y and i n places i t i s s i l i c i f i e d . producing a dark green (plagioclase white (quartz and s l l i c l f i e d k-spar mott led rock. k-spar remains pale salmon. nlos t places.

41.8: 49.2: a l t e r e d - w h i t e clay, producing incompeten clayey core.

G r a d te : p i nk-grey , med tun-f {ne-grained, sparcely po rphy r i t i c (pink k-phenos up t o 0.5 X 1 cm). L ike quartz monzonite 16 I n OH-3. Sugary matr ix i n places. pyrite: about 0.1 dissemination. Magnetjc.: ~ 0 . 1 , rock weakly magnetic.

More intense a l t e r a t i o n

1 and In places p a r t l y a l t e red

Bio gone i n

matr ix o f breccia p a r t l y

I

SYMBOLS AND ARBRCVIATIONS ~ . - -

Slructerd Angle YMROL C.A.ID!+

;L IPS: I5.7:7O0 to CI 15.9:3S0 to C I

iumerous b l k : lay seams prc iably s l i p s 3(

11.8-49.2:

' 900 to C . A .

19.1:25' to C I

some Mo ) quart

.080 ns i n b ed. So

.044 ccia.

.035

- -_

_ _ .014

veins.

. o n

.025

__ - - .025

-. _ _ _

lost. 'veins lave beell 1 ot'

( n i l ) ~

.130 eccia. Numerou; black e MoS ost . . ooz -. . . - - . - . __ .__ . . -

.073 bout 50; MoSz l ~ t . . - ( n i l ) . . . . . - _ -

.057

.001

. _-

_. __ - -. . .- . .- _- - ..

.024 No more quartz reins 1 . ( n i l ) _ _ - . .. . -. -. .

.045 ( n i l )

~ .- ~

.040

.001 ._ _ _ _ __ .-

.042 ( n i l 1

_._ _ -

- SHEET I N I E R V A L l i ~ m

..

0

MVNWYV

. CLAIMPERMIT NO.

ORILLING. ~ - __ - . ~ - _ _ _ _ _

~____ ____ _ _ _ _ ~ -.

58.5 - 139.8

LATITWOE DEPARrURE ELEVATION I O A I U M ) BEAfllNG INCLINATION LENGll4

- N :a .- -

FIELD LOCATION . SURVEY GfllO

.

E A 2

- monzonite elsewhere. Here there appears t o be very l i t t l e plagioclase i n m a t r i x .

__ 50.7 - 58.5: plagioclase phenos a l te red t o so f t . soapy, dark green cores, l i g h t green rims.

57.0 - 58.5: Gradational change t o next rock type by increase i n propor t ion and s i ze o f plagioclase and k-spar phenos. Several bands w i t h gradational boundaries o f 50.7 - 58.5 type w i t h i n gradational zone.

quay_tr Monzonite: gra ined matr ix w i t h med=cse g ra in plagioclase and k-phenos, k-phenos mostly less than 1 X 2 cm, although sane larger , comprise 5 - 10% o f rock.

D i f f e r s from previous i n t e r v a l by appeartng coarter grained due to l a rge r more abundant plimos and by greater propor t ion plagioclase.

5c.5 - 6 5 2 : plagioclase a l tered t o opaque white o r f a i n t l y green, medium hard to hard, except f o r several bands a l te red t o soft. soapy green adjacent quar tz-pyr i te veins.

pink-grey. f f n e - medium

SLIPS:

60.2: 300toCA 60+3:400 toCA 60,5:several 20" t o C.A .

~ 65.3 -_ - 65.6: .- _- zone.

crumbly core, micro brecciated

. 65.3 ._.-. - __-. 69.4: white and s o f t soapy l i g h t green.

plagioclase a l te red t o soft.

SYMBOLS A N 0 ARBREVIATIONS .. . - . -

SAMPLE Na.

'ROW

ro

IO SMEFT INTEflVAL lrnm

MVNW'lV

I I I AOOITIONAL INFO

r n c E - _ - P - ~ - or._.-8 ~

rrioxcr NAME _--Cn?!!J ~ ~ ~ .

PAOJECl N O -. ?!?!?.- -

I IOLflSEC NO _._ !9.:..4 . . ~ _ ~ ~

SHELL CANADA L lMl rED - MINERALS DEPARTMENT DRILL HOLE OR SECTION DATA RECORD

~~~~ -. . .--

____ -. - - WORK DONE Nam D a m Ammarks

DRILLING. - FIELD LOCATION

GRID

____ LOGGING.

AZ. s u n v E v - _ _ ~

_- ASSAYING:

LITHOLOGY. Tsrltrw. Slrwturs. Mimrdiml im ILilhologl

-, 1 . . ' , - 65.6 - 69.4: core, nuprous anhydrite f i l l e d f ractures about 20 t o C.A.

- 69.4 L-- - 71.2: l $h t green hard.

--- 71.2 ---. - 80.9: and hard. Occasional l i g h t green.

- 00.9 - 109.7: l j g h t green hard, w i t h scattered patches, soapy green next t o veins.

- Ex -. cepL:

82.4 - 83:

Varlably crumbly and competent


plagioclase phenos opaque whit1


plagioclase opaque white hard. 88.5 - 89: 96.2 - 96.9: 38.6 - 101.2: 105.9 - 106.3:

I " t I,

,I n I, I,

I, I, ,I I,

I " ,I "

77: k-phenos being to comprise 15 - 20% o f rock.

90.5: Medium grained. L i t t l e f ine-grained quartz i n matr ix .

90.8 - 9 1 . 4 ~ 30 cm t h i c k a p l i t e d ike contacts 15 t o C.A.

Dike cu t by MoS2 - quartz velns.

95111: medium t o almost cse-grained. grained quartz grains i n m a t r i x . man t 1 ed k-pheno .

Begins t o look coarser grained.

Rock has become coarser-grained, now A few f i ne -

Occasional

, . . . . I

SYMBOLS AND ABBREVIATION!j

Swuclurd Angle SYMBOL C.AlOtp

S t W f T INTERVAL ham

UVNWlV

I

LATITUDE FIELD LOCATION SURVEY Grit0 N


OEPARIURE ELEVATION IDATUMI

-

E

WORK DONE N s m Dan R e w h

DRILLING ____

- AOOlTlONAL INFO ASSAYING

---I-__ 109.4 - 112.4: hard.

plagloclase opaque white,

112.4 - 116: plagioclase l i g h t green, hard; m y y z t and soapy adjacent s l i p s o r quartz veins.

-. 116 - - - 116.9: plagloclase opaque white, hard

__.-- 116.5: medium grained w i t h s o w f ine-grained quartz i n matrix.

116.9 - 122.9: - - green. plagloclase a l te red t o sof t , soapy p is tachio green and dark green, k-spar a1 tered t o moderately hard and g r i t t y and s o f t soapy dark green Bio gone.

117.3 - 122.5: Breccla zone 0.5 t o 1 m macro breccia a t each end, micro breccia between. Many s l i p s have h S 2 .

-- 122.9 - 125: soapy l i g h t and dark green. k-spar bleached pale pink.

125: medium grained quartz monzonite, same ar-before 1 16.9.

-. 125 - 134.3: - Except 130 - 131.8 plagioclase altehed t o s o f t white i n zone w i t h f rac tu re 15

134.3 ~ - 139.2: a l tered to l i g h t green hard, o f ten only bare ly a l tered. plagioclase opaque white.

Quartz monzonlte I s d i s t i n c t l y

a l l feldspar a l t e red t o

_._----


plagioclase opaque white, hard

t o C.A.

I n most places plagioclase

One 50 cm i n t e r v a l

u * . t * * . . l

Slruccurd An#@ iYM0OC C.A./Ob

L I P S :

miner. bx. 07.5:45O toCP

14.5: 5 cm f l t bx, s l i p 35' t o C.A.

17-117.2: 3, 450-60°to C . P 17.3:50°to CP H.W. o f bx zone 18.4: 60°toC! 18.8: 35OtoCP 20.8: 45°toC!

SAMPLE FROM.. . I N T . REC No. TOFeet ... ....... IN FT. DVER'

1 - 4 - 30 310 - 320 10 ~ 1 0 0 As above.

___I ._

9 - 4 - 31 320 - 330 10 -100 As above.

9 - 4 - 32 330 - 340 10 95 80% i s i n i qua-tz-11 some Mos2 os t .

___I -

9 - 4 - 33 340 - 350 10 -100 quartz MOS., vel I S .

-~ .- -

9 - 4 - 34 350 - 360 10 =IO0 As quartz-fbS2 f py

9 - 4 - 35 360 - 370 10 98 As above.

._I_.- ____.__~

9 - 4 - 36 370 - 380 IO 9 As above.

_I__.. ~_____-- __ __ 9 - 4 - 37 380 - 390 i o =loo

As above. Seve-a1 1 not countec. Sbme P

0.15 1 .130 1 ;:::I S2 vein subpara l e l l n g

___ __ - - .-

.110 ( n i l )

.056 ! l o s t .

( n i l )

.244 (n l1 )

0.06 1 .070 1 ;:::I - 2 mn lack s t ingers s2 l o s t

- E S U L r

-

i r e fo

_____

I quar

-

ted.

1

SYMBOLS AND A00REVIATlONS - -~~ . -~ - S H E E l INTFRVAL horn I O

MVNW2V


L A T I T U M FIELD LOCATION SURVEY GRID N

DEPARlUnE ELEVATION IDATUMI REAnlNG I N C L l N A l l O N L E N f i I H

E AZ.

DEPTH --

139.8 - 147.3

147.3 - 148.5

Slruclural An* iVMBOL C.A./Dip

$LIPS:

139.4:80°to CA 139.6:80°to CA ?ach w l t h b l k : lay seams 139.8:50°to Cr 140.6:30°to CA 140.8:30°to CA 142-1 42.3 : two ;ets a t 30° to ioo t o C.A. 143.2:300to CA 145.9:45°to CA 147.3:65'to CA W to bx zone

ieveral se ts it 30° to 60° to C.A. 148.4:60°to CA 'w o f bx zone 148.6:50°to CR

147.4-147.9:

LITHOLOGY. T8xlur*. Strwtuta, MinrJIzaliar ILitholopl

"-'r""l-r--

__ 139.3 _- - - -__ 139.8: s l i p s marks contact.

_- Quartz Felds a r Por h f l : grained matryx o f q:a:tz and k-spar; plagioclase phenos 5 - 10%. quartz phenos 1%, b l o less than 5%.

_py*e.: Mgne t l c : Stro@iF magnetic.

Disseminated MoS2 <0.01%.

Contact a t 145.3 masked by breccia zone.

Breccla zone w i t h numerous black s t r l nae rs anfl seams, some w i t h MoS2 smears a t 30 - 45 t o C.A. Robk breaks on conjugate s l i p planes, each 30 t o C.A.

139.2 - 140.8: most feldspar a l t e red t o dark green, medium hard and g r l t t y , some w i t h sof t , soapy cores. Several patches w i t h k-spar not altered. These are composed o f f ine-grained k-spar, quartz and muscovite suggestive o f strong k-metasomatism. Bio gone.

-- 140.8 - 157.9: t o T ight green cores w i t h white rims, both sof t soapy.

Breccia zone with several

pink, very f lne-

about 0.196, mostly I n veins. 0.1 t o 0.5%, moderate t o

__---

plagioclase phenos a l te red

________ 141.2 - 143.4:

. ~ - - 144.9 - 146.2:

Micro breccia zone.

Micro breccia zone.

---t---- .098 ' .163 I ( n i l )

-----t----

----+---

t---- __-.

.042 .070 ( n i 1)

. i ~ o .3on

- . otdi;lf!i .. - - __ uartz-1

. lo4 .173 lack s l r ngc s

--

In1 1 r -

.IO4 ,170 ay haw been 1

-,Q_92-

f f i c i i l t t o sac .on8 .143

._ .002

.049 .078 lack c .ay seam

.002 -

~~ ~- - SYMBOLS AND ABBnEVIAl lONS -

,(

P n o J E c i PAGE- ~. 7- NAME -~ ~ ~ C a s w OF 8- ~ ~~ ~ . .~

SHELL CANADA LIMITED - MINERALS OEPARTMENT DRILL HOLE OR SECTION DATA RECORD

PnO.tEci NO ~. . .?991T-- - MOLEISEC. NO ~. 79~ - -4.. ~-~ ~~ ~- .-

___ WORK W N C N a m Oat.( Remarks

DRILLING: ____ ...____ L A T l l U M OEPARTUIW ELFVArlON IOATUMI

N F

___- FIELD LOCATION SURVEY GRID

1-OGGINO: - _ _ _ ~ ~ _ _ _ _ _ _ _ _ _ _ ~ . AZ __ -~ _____--___--

ASSAY ING;

__._

O E M

147.3 157.5

157.5 169.5

LITHOLOGY T r x ~ u a . Stvuc~urc. Mtnardirallm ILNholog) -, . . . , , Qugru t@nzoni te : pink-grey, medium- gra?nea, 3 l < p r - a n d plagioclase po rphy r i t i c . K-phenos less than 1.5 X 0.7 cm about 5% o f rock. Plagtoclase pbenos up t o 0.5 cm 5-10% of rock are most d i s t i ngu ish ing feature. I den t i ca l t o rock a t 75 m.

147.3 - 149.3: Breccia zone, micro and mahro. 35 to C.A.

_--__- 150.4 - 154 : Breccia zone, micro and macro breccia; numerous s l i ps , many w i t h black c lay seams.

157.5: Contact marked by s l i p w i t h black clay.

Quu_artz P l g ~ o c 1 a s e - P o r p t h ~ : pink, Plne- gra- grou-ss of quartz and k-spar. quartz phenos 5%. Same as quartz Peldspar porphyry but w i t h few plagioclase and no k-spar phenos. plagioclase phenos present. The abundance o f salmon coloured k-spar suggests t h i s rock inany have formed by k metasomatism.

157.9 - 159.5 k-spar var iab ly a l t e red t o green, medium hard and g r i t t y . places a l l k-spar altered, elsewhere only p a r t i a l l y altered.

161.9 - 162.9: - -

162.9 - 169.5: grren cores and white rims, both s o f t and soapy.

Numerous ha i r1 i ne macro f ractures

From 162 - 166.6 about 3%

_-- I n m s t

Macro breccia zone.

plagioclase a l te red t o l l g h t

, . . . . I

Slruclvrd Anpla YMBOL C.A.IDip

LIPS: 51 .3:50-20°ta A 51.6:85°to CP 51 .9:40°to CA 52.3:30°to CP 52.8:30°to CP 52.9:20°to CA

45'to CP 60°to CP

53.9:55'to CP 55.4:30°to CP 55.8:30°to C A 57.5:60°to CA 57.8:60°to CA 57.9:35Oto CA 58.2:30°to CP

45'to CA 58.5:15'to CA

40°to CA 60.6:60°to CA 60.9:55'to CA W o f bx zone 63.8:9g0to C A 65: 30 &o CA 65.4:80 t o CA

60°to CA

4U0t0 CA

As above a

'9 - 4 - 50 510 - 520 A s above a veins. Nu

'9 - 4 - 51 520 - 530 As above. I

'9 - 4 - 52 530 - 540 As above. I

------ --

'9 - 4 - 56 570 - 580 As quartz- dlsseminat

I------ ____ .-

r9 - 4 - 57 580 - 590 As veins a

-. E S I J L 1 s

froin h *oken c( - .- .- ._ . __.

ng quar :z-MoS2

~

- - -. - __ -

. __ __ -.

issemin t ions. -.

Black c lay sea1

- -.

- -. . .

ccia a n j minor

.

SYMBOLS AND ABBREVIATIONS .. - SHEET INTERVAL- horn 10

MVNORYV

SHELL CANADA LIMITED - MINERALS DEPARTMENT DRILL HOLE OR SECTION DATA RECORO

L-Ld AODlTlONAL INFO

- Est. q 0.03

,eccia

A S S A Y - - __ NT. I F T -

1c ear -

~-

Strueturd Angle 5VMBOL C.A./Ob

E S U L l ROM

0 SAMPLE

Ne.

160.4 - 170.4: Macro breccia zone. ;L 1 PS

166.2:55'to CA 166.5:45'to CA 166.6:45'to CA 167.5:45'to CA 167.8:45'to CA 168.3:45'to CA 168.4:60°to CA 168.7:45'to CA 169: 35'to CA 169.7:60°to CA 169.8:60°to CA

9 - 4 - 5 0 90 - 600 s veins, la t ion!

169.9 - 170.5: moderately hard and g r i t t y .

__ Granite: __- pink. medium grained. About 40% quartz, 402 k-spar, minor plagioclase and 2% b io. Scattered small k-spar pheno. S imi lar t o types o f coarser grained quartz feldspar porphyry's except f o r abundance o f quartz. Metasomatic?

About 173 quartz grains become la rge r than k-spar. - 178 - 178.8: Gradational I n t o quartz feldspar porphyry by groundmass becming f i n e r gralned and quartz becoming d i s t i n c t phenos . 170.5- 182.9: i 7 t e r s t d 7 1 g h t green o r white, s o f t soapy.

A l l feldspar a l t e red to greer

_---

Where plagioclase present i t

169.5 - 178.8

_- Quartz - Felds a r Porphyry.: very f i ne - o r a l i d - 6 6 ~ ~ p a r c e small k-phenos

178.8 - 182.9

i ca t te red plagioclase phenos, prominent (10%) quartz phenos.

182.9 END

SHEET I N l E R V A L ham I O

9

39911

PAGE 1 ~~ OF _ _ - SHELL CANADA LIMITED - MINERALS DEPARTMENT

C_as!no_ _ - DRILL HOLE OR SECTION DATA RECORD PROJECl NAhlE ~ -

PROJECT N O _ _ _ HOLEISEC N O _. 7 3 - 5 - - -~ - - - - -

_ _ _ - __- WORK W N L N a m Oalo Remarks

ORILLIN(; ~ - LATITUDE DEPARTURE

FlELn _ _ __--_______ ____ LOGGING LOCATION

ASSAYING __ ________

__ ~ . N A 7 Z 7 . 4 ni E 1601.74 m SURVEY

GRID __ - __

__ REC

DVER' __

90 PYI'

- ORM JNlT -

-

r M W L E

No.

7 9 - 5 - 1

.-

7 9 - 5 - 2

7 9 - 5 - 3

____.

7 9 - 5 - 4

7 9 - 5 - 5 __-__i__

7 9 - 5 - 6

7 9 - 5 - 7

.

7 9 - 5 - 8 _I_-.

7 9 - 5 - 9

-I__I_

79 - 5 - 10 .- ----_ L_

--I---- - A S S A Y R F S U L 1

e res

0 - 6.4

6.4 - 13.3

13.3 - 17.4

17.4 - 56.2

Slructud Angle YMnOL C.A.IOm a LITHOLOGY. lcxlurs. Slruclurs. MmralIr.llm I L ~ t l ~ o l q ~

-- ---- Casing 0 - 20' .

Overburden.

quartz Monzonite: Pfnk-grey, mediuni-coarse- grained. k-spar po rphy r i t i c . Large k-phenos over 1 X 2 cm comnon, some mantled. Bio. medium-grained, 5%.

Py r i t e : as veins. Magnet i c: (0.052. d i ssemf nat Ions. Rock weakly to almost non-magne t I c . 6.4 - 13.3: l i g h t to aark green. hard t o Soft.

.__-- 13.3 - 17.4: s o f t soapy, k-spar var iab ly a l t e red pink- grey t o green, medium hard.

- 10.3 - 17.4: Breccia zone, macro and micro. V e n e - g r a i n e d clayey gouge w i th over 50% black and dark grey s t r i nge rs and seam (mylonite) a t 14.3 t o 14.6 and 15.6 - 16.4.

Primary features o f rock destroyed by brecci a t ion. Contact a1 so destroyed . e r t z Monzonite.: pink-grey, medium- grafned. k-spar phenos mostly less than 1.5 cm. 5 - 10%. plagioclase phenos about 0.5 cm 10 - 20%.

Py r i t e : 0.1 t o 0.52: disseminated and i n veins. Magnetic: 0.1% disseminations. Rock moderately magnetic.

about 0.1% some dissemination. most

Plagioclase var fab ly a l t e red t o

Plagioclase a l te red t o green

SLIPS: J.8:60°to C . l

t- 90

smea As 30 above - 40 a i d I as 10 .015 l o s t 1.3-14.6 I

5.6-16.4:blk D ms 6 s l i p s 3 to 80°toCP 1.7:2 d i f f e r - n t s l i p s 30° J C.A.

8 1 ____

83 a1 c rom

. l40 t o c .

t-- ._____..

85 .055 50 - 60 I 10

--I- I __-I_

99 60 - 70 I 10 ~ 0 . 0 1 .026 - __ -

0.03 .028 t e vein! .

__ _-

0.02 . lo9

. -- .- -- (0.01 .008

t-- 99

py r 70 - 80 10

In quartz-f os2 I 80 .031 80 - 90 10

&s above.

I- L I P S : 3.0:45'to C.P -loa .013

-

.065 a slng

_ _ . ._ -

.015 .-. _ -

90 - 100 I l o

1100 r i t e veins. 90% frc

0*12 I *039 t- __ __ 90

. -

I- L _ L d . . . . L -

SYMBOLS AND AOIIREVIATIONS *Eg.FbS?: ks2 epuivelent t o t o t a l Mo; calcu lated assuming no oxide Mo i s present. Oxide leach not w--s,,,,T formed on 79 - 5 samples.

1(

uvfl6(11v

POLITICAL UNIT

ADDITIONAL INFO

PACE .OF I)

vno.mcT NO .- -K!9J! . . ~ ~ .

SHELL CANADA LIMITED - MINERALS DEPAHlMENT

DRILL HOLE OR SECTION DATA RECORD PROJECT N A M E carm ~ ~~ ~.

MOLEISEC NO ~~ 7?. -- 5.. -. - ~ - WOAK DONE N s m 0aIm Remarks

DRILLING .._______~_____

LOtiGING. . -__-____-.

ASSAYING:-- ___~__________ '

LATITUUE OEYARTURE E L E V A l I O N IOATUMI

N E

-~ __-.______ FIELD

____ LOCATION SURVEY G n l o AZ. __ __-_ ___

LITHOLOGY. Texture. Slruoute. Minrdlt.lim ILllholnJl

1 " " l

17.4 - 22.5.: s a w spe&n. some white and so f t g r i t t y , some very pa le green and s o f t soapy.

__-_- 22.5 - 34.8: hard t o s o f t g r i t t y .

34.8 - 44.8: whltihar7.-

plagioclase var iab ly a l t e red i i Some opaque white and hard,

plagioclase white, moderately

plagioclase mostly opaque

20.1: 7--:-22 bio.

20 cm w i t h 502 large k-phenos and onl:

--c___.- 20.3 - 21.3: Several 5 cm c l o t s o f 602 bio. Not schl ieren and don ' t look l i k e inclusions

38.4: 20 CR th i ck band of k-feldspathizatlol Orb icu lar k-spar overgrowths on k- henos has replaced groundmass, leaving agout 15% quartz, minor muscovite and about 0.05% disseminated MoS2.

-- 45 - 45.8: prominent than usual.

44.8 - 48.7: green, hara. . _ _ _ ~ 48.7 - 49.8:

%9&- 51.5: g r c e n , T r d .

50.9.: green, s o f t soapy.

Large k-phenos 1 X 2 cm more

plagloclase a l te red t o l i g h t

plagioclase opaque whlte hard.


20 cm plagioclase a1 tered t o dark

L Y L L l L . 1 1

S~ructurd A+ YMOOL C.A.IDb

SLIPS:

51.0:45'to CA 56.3 : 20' t o CA

'9 - 5 - 11 120 - 130 I n veins a __--_

'9 - 5 - 12 130 - 140 I n quartz-

-_ -

'9 - 5 - 13 140 - 150

'9 - 5 - 14 150 - 160 .-

'9 - 5 - 15 160 - 170 -_I_

'9 - 5 - 16 170 - 180

I---- '9 - 5 - 17 180 - 190

952 I n one conta ln l ng Some proba

'9 - 5 - 181190 - 200

.025

.042

.013

.008

.067 snt t o ample.

-

.033

R E S U L T S

SYMBOLS AND ABBREVIATIONS *Eg. ~ 0 ~ 2 : M ~ S equivalent t o t o t a l Mo calcu lated assunh! no. oxide Mo i s present. Oxide leach no t SHEEr l N I E R V A L I O

performed on $9 - 5 samples.

- ADOlrlONAL INFO -

9 PAGE- 3 _ O F

FROJECT N O - - 3991J- ~ -

HOLEISEC N O --79 - 5 - . - -~ _ _


PROJECT NAME Casnn, - - DRILL HOLE OR SECTION DATA RECORD

WORK W N E Nma Osln Remarks

DRILLING ____ ___ . __ _-__ L A T I T U M OEPARTURF. ELEVATION I D A T I M I

__ ---____-_____ FIELD I___-_~__ -I____ - ~ I _ _ _ .

LOCATION SURVEY GRID

LOGOING -

N E 6 7 _ _ ~ _ _ .___.___._l_l- -----. ASSAYING -

-

56.2 58.:

50.3 192.

LITHOLOGY. Texture. Ssruaurs. MI-mlIzmtlm (Lllholog)

u . - . ' v 51.5 - 58.8: hard. Several 10 - 30 cm i n t e r v a l s plagioclase a l t e r i n g t o dark, s o f t soapy green.

Granite,: grey, fine-medium grained, sparcely po rphy r i t i c . Gradatlonal top contact from medi um-grained porphyri t l c quartz monroni t e through medlum-grained ( w i t h some f ine-grained quartz mnzon l te ) . Granite w i t h no plagioclase phenos t o f ine- grained. Granite w i t h scattered small k-phenos. Bottom contact 1s sharp a t 25' t o C . A . and i s pa ra l l e led by f a i n t 2 cm b f o schl ieren. Another 15 cm band fine-gralned g ran i te a t 59.9.

most plagioclase opaque white

Structural A n ~ h mYMBOL C.A.lDip

- quartz Monzonite: pink-grey. medium- ' L ps: l. l :30°to C . A 30 cm bx

10 - 20%.

g G T % d - ~ ~ f i n e - g r a i ned quartz ) ; k-phenos pink, p e r t h l t i c . up to 1 X 2 cm 5 - 15%; plagioclase phenos t o 0.5 cn)

of rock. Local ly large k-phenos over 25%

. . ~

l i g h t green and s o f t soapy dark green.

75.3 - 80.2; plagioclase a l t e r i n g t o m g h t green hard.

4.5:30°to C.A I 1 . . . . I 1

--

---_I-

r9 - 5 - 24 250 - 260

SYMBOLS AND ABBREVIATIONS *Eg.MP&i Fb$z_equivalent t o - t o t a l Mo. calcu lated assumlru.ao oxide i s present. Oxide leach no t performed on 79-5 samples.

.055

.063

.051

.013

.056

.I23 over !

.020 -- - -. . .

.033

.040

W E E 1 I N T C R V A I Itam in

ADDITIONAL INFO

SHELL CANADA LIMITED - MINERALS DEPAflTMENT DRILL HOLE OR SECTION DATA RECORD

WORK WNE Na=

DAlCLlNG .

LOGGING.

-- ASSAYING,

. 73.5111: - quartz monzonite; some f ine-grained quartz i n gm; plagioclase phenos about 0.5 cm 10 - 20%. k-phenos 0.5 t o 1 cm 5 - 10% o f t e n not eas f l y d is t inguishable from k-spar i n gm. occasional k-pheno 2 cm long, fen are mantled

80.2 - 87.0: %dTiwT t o hard.

+E .5: 20 to C.A. - broken.

t yp i ca l p i nk-grey medl wn-grained

plagioclase opaque white

Several quartz MoS2 veins less than 4- 80 - 87: SLIPS: numerous, 20%. No s ign l f i can t difference 91.8:35't0 C.A from quartz monzonite - 1. medium - coarse 92-0:4o0t0 C . A grained. 92.3:35'to C . A

94.1 :25Oto C .A

Larger k-phenos, 1 X 2 cn), m r e

87.0 - 91.1-: plagioclase a l t e r i n g t o l i g h t 94.5:40°to C.A green harb, except l o c a l l y plagloclase 50°to C.A a 1 t e r i ng t o s o f t soapy dark green.

3845 t o C . A 91.1 - 94.2: a11 feldspar altered; b l o gone. 96.6:55Oto C.A n G m e a l t e r i n g t o sof t soapy dark 97.1:20°to C . A green, k-spar a l t e r i n g t o l l g h t green medium 97.6:40°to c . A hard. 97.7:50°to C . A

60°to C.A 94.2 - 95.8: a l l feldspar a l t e red b l o gone; 99-1:3O0to C - A f ; T a c c l a s e a l te red t o s o f t soapy dark and 99-3-101.1: p fs tnchio green, k-spar replaced by some type nuprous S l i grey feldspar ( a quartz?). 25 - 60'

93.5-2104: Breccia zone, several s l i p s w i t h black c s y seams.

93.5 - 95.8: macro breccia 95.8 - 96.6: micro breccia 96.6 - 99.8: mostly mlcro breccia 99.8 - 104 : mostly micro breccia.

94.7-98 :

, . . . . I I SYMBOLS AND ABBAEVlAIlONS

FAOM TO F t .

A S S A Y -- E S U L '

tn EllEFl INTERVAL Iron,

--_I- ADDITIONAL INFO

95.8 - 97.5: a l l feldspar a l tered, b i o gone TKemr 94.2.

--.-- 97.5 - 104: green mostly hard, some so f t and g r i t t y .

I- 104 - 132.8: plagioclase opaque white, hard t o 3 G f G X a r d . l o c a l l y a l t e r i n g t o whlte s o f t adjacent c e r t a i n f rac tu re sub a r a l l e l core.

plagioclase a l t e r i n g t o l l g h t

116.2 - 118.7: macro breccia and micro breccta.

Breccia zone w i t h 3

- 1 1 2 - ~ - - 115.4: 35 t o C.A.

A p l i t e dikes, 3 cm 1

ips;

5 cm,

116.5:

132.8 - 141: most plagioclase a l te red t o ltght- hard l o c a l l y plagioclase opaque white or s o f t soapy green i n k-spar a l t e r a t i c aureoles.

134.7 - 135.8: 'Porphyrite' : 75% k-phenog, p l - r i k F t h l t f c . 2 X 3 cm; 15% medium-coarse gralned quartz; 10% plagioclase phenog 0.5 X 1 cm.

137.5 - 138:

141 - 142.4: Plagioclase a l te red t o so f t soapy K r F g r e e n .

142.4 __ - .--. 142.7: a l l feldspar altered, b i o gone. dark green. k-spar a l t e red t o grey green, medium hard g r i t t y .

A p l i t e dike, 15 cm. 40' t o C.A.

Breccia zone with several s l i p s __

Plagioclase a l te red t o s o f t soapy

Structural An#. SYMBOL C.A.Imp 4

SLIPS: 109.5:40°to C! 111.4:45°to CF 111.6:40°to CF

112.7:65'to CP 116.3:50°to CF

3O0tO CP 116.9:10°to CP 117.0:30°to CF 117.5:50°to CP llR.5:2 sets

each 4a0toCA 121.5:55 to.CB 127.4:35'to CA ihroughout t h i tole f rac.wl tg

:o 20 t o C.A. 20-1 23 : f rac . ri t h anhydri t e 1-15' t o C.A.

112.2:4O0to Cb

IO slhps @ 35

SVMBOLS AND AORREVlATlONS *Eg.MSZ MgS equivalent to t o t a l Mo, calcu lated assuming no oxide hio i s prespnt. Oxide leach not performed on 3~ - 5 iawlcs. SIIEET I N T F n u a ~ *

L- AODl l lONAL INFO

L

SHELL CANADA LIMITED - MINERA

dark green i n k-spar a l t e r a t i o n envelopes or breccia zones and i n places plagioclase i s opaque white but medium hard.

156.5 - 159.5: Micro breccia zone, some crumb-

163.2 - 165: Breccia zone with several s l l p s m a m y T r o breccia).

170.6 - 176.2: Breccia zone. Mainly micro breccia. Some crurnbly core.

170.6 - 174.3: Mainly lag loc lase a l te red t o sof t s o a p y x r k green, u t several i n te rva l s o f p laq ioc lase a l te red t o l l g h t green mdlum

--

E __-

S DEP

SLIPS:

163.8:35Oto CA 164*3:400to ''

3O0to CA 164.4:40°to CA 164.5:50°to CA 164.6:45Oto CA 171 .3:50°to CA 71*8:350to CA

75.3:45Oto CA j14.6:350t0 'A

R l

79 e 5 - 42 430 - 440 10 =lo0 0.02 Thin quart;-MoS., t p ' r i t e v

_-_I ___ - 79 - 5 - 43 440 - 450 10 =lo0 0.04

4s quartz-foS2 - pyr t e vei ~

79 - 5 - 44 450 - 460 10 ~ 1 0 0 0.02 AS above. Unkniwn m l t a l l i c Colour and l u s t g 11 :e bism 1 good c l e i r -61 t o perfec

___. -- __-

79 - 5 - 45 460 - 470 10 -100 0.03 As above.

-__ -____ ___ 79 - 5 - 46 470 - 480 10 99 0.02

As above. . _-_

79 - 5 - 47 480 - 490 10 95 0.20 Quartz-MoS. f p:,rite veins. Some l o s t ' rom crumb y core

__ _ _ .

79 - 5 - 48 490 - 500 10 ~ 1 0 0 0.05 As above.

__-c_ __--- __ -_

79 - 5 - 49 500 - 510 10 ~ 1 0 0 0.02 As above. Some l o s t (10%).

1E DRILL HOLE OR SECTION DATA RECORD

_ _ _ _ .om

w i t h k - .

.044

__--.

.090 -k-spar It 2 - 4 , o r perp.

. loo -_ - - .

-- .090

- - . - . .752

i n b1a:k

-. - __ - .

.083

.092

9 FAOF ._ 6- OF

PROJECT NAME _ _ - _ - - _ _

IT

rnoxci NO ~ -79 - ~ - . ~

-- IIOIEISEC N O _ _ -____ -__

LAl lTUOE OEPARlURC ELEVATION I D A l U M ) EEAfllNG INCLINAl ION I E N G l I l FIELD LOCATION SURVEY GR!D

.____-.

N E A2 __I- -_-

__.

,par a1

-_-

muscov 1 per to ot l -

___

__- __ -

5eam

- __ .. __ .

___I

"%!be

hard OF mixed plagioclase a1 terat ion.

174.3 - 175.3: gone; plagtoclase a l te red t o so f t soapy dark green, k-spar a l t e red t o l i g h t grey green, medium so f t .

a l l feldspar a l tered, bio

175.3 - 177.0: TTsiit greenTard.


---- 177 - 188.3: hard, l o c a l l y plagioclase a l te red to l i g h t green hard o r s o f t white.

most plagioclase opaque White

I .029

Ins, on1

.026

L-- _-

1 .

-.

.054 n guar h i n l t e and 1 I

.060

-___

.054

.451 One ve.

.050

__ - - .055

SYMBOLS AND ABBREV(Allom *Eg. M$2: _MoS equivalent t o t o t a l Mo, calcu lated assuming no oxide Mo i s present. Oxide leach no t perrormea on 3s - 5 ~ i i i o l i s .

m

._

r a t i on -.

e-pyr i c t p l a r two.

_ _ _ _

-

- . - .

--

R p p m

- - - - . .

nvelop

vein. c lea r

.___

__-

-

--


L------ AODllIONAC INFO ..

S R K DONE Name

DRILLING’-.--

~

LOGGING,

ASSAYING

192.5 203.5

-_.___ 188.3 - 190: green hard, some w i t h s o f t soapy dark green cores.

190 - 200.3: plagioclase a l te red t o opaque f i i i a i k r w h i t e medium soft. l o c a l l y a l l feldspar a l t e red t o green.

-_-_ 190 - 2 1 7 L . : Breccia zone. Mostly micro breccia, some macro breccfa. 30% o f core i s crumbly o r f i n e l y broken.

Contact a& 192.5 i s sharp and about 45’ t o C.A. t 20 . Texture of quartz monzonite above not d i f f e ren t , but pink g ran i te below i s f i n e r grsincfd and contatns less b i o . a t the contact.

thnfi_e,: Plnk. f ine-grained, quartz phenos 5 mn. 10% plagioclase phenos 2 X 4 nm 5 - 10% b i o 3%. q u i t e f ine-grained gm. Borders on quartz monzonite.

20 cm from contact g ran i te grades i n t o f i n e - medtmn grained quartz monzonfte with plagioclase phenos 10% k-phenos 1 X 2 cm. Between 191.2 and 195 (broken core) t h i s grades back t o f ine-gratned grani te .

193 - 195: i Z & ~ e n o s , some i n gm.

__ 200.4 . - 201.1: Most k-spar a l t e r i n g t o grey green so f t , some remains pale plnk. No plagloclase v l s i b l e .

._ 201.1 ._ .. - - 202.5: -. plagioclase a l t e r i n g t o s o f t s o a E g r e e n cores w i t h 1 l g h t green s o f t rina.


Nucnerous s l i p s .

Much salmon plnk k-spar, same as

-Lu . . I

I“ SYMBOLS AND ABB~EVIATIONS *E9. b s z : 4 s ~ equJvalent t o t o t a l Ho. calcu lated assuming-no oxide Mo Is-present. Oxide leach not

I,am prepared on 79 - 5 samples.

I

POLITICAL UNIT

-__ ADDITIONAL INFO -

WORK DON€ N a m

DRILLING ____

LOGGING

__ ASSAYING:

PACF * OF - SHELL CANADA LlMlTEO - MINERALS OEPARTMENT

P R w E c r NAMF Casna - -. - - __ PROJtCT N O _ _ 3991T- - -~ -

DRILL HOLE OR SECTION DATA RECORD

HOLE/SFC N O 79 - _ 5 ~ - _ _ - - Dais, Memarks

C A l l T U M OEPAflrURE E L E V A I I O N IDATUMI

~ _ _ _ _ _ _ _ _ _ N

-_______ - _ _ _ _ _ _ ~ ~ FIELU

LOCATION SunVEv GfllD

- -I_-___

€ - -

203.5 - 218

218 - End

202.5 - 206.5: a l t e r a t i o n same as 200.4 - SLIPS: 201.1 but w i t h i n te rva l s of most k-spar remalning pale p ink. Mlnor v i s l b l e plagioclase a l l a l t e r i n g t o so f t soapy green. (b lk seam)

Ih-ecciated and in tensely altered. Or lg lna l (b l k seam) rock type not p o s i t i v e l y i d e n t i f i a b l e .

205.1:60°to CP 205.4:60°to CP

205.6:60 t o CP

206.2:60°to CP

I - - - ~ - -

206.7:60°to CP 207 - 216.5: Probably medium-fine-grained, 207.1:35~to cn sparcely po rphy r i t i c quartz monzoni te, but I 208.1 :60°to CP intense b recc ia t i on and a l t e r a t i o n makes (b lk segms) I.D. uncertain. 1.0. based on what appear t o 208.3:40 t o c p be scattered k-phenos and more granular, 208.5:35'to C A coarser grained texture. kt no plqgioclase 20g.8:45~to C A phenos v f s ib le . 210.1:45'to CA

(b l k s e p ) _- 217.3 - 218.: Probably was quartz Peldspar 211: 35 t o CA porphyry, 6nsed on r e l i c t texture. H.W. (b l k seams) i s s l i p and macro breccia. 211.6:blk~seam

45O - 60' 201 - 216.5: Contains much salmon ink 213-blk ijeams

Quariz Feldspar Porphyry: pink, very f l ne - gra ne gm, quartz. Phenos t o 0.5 cm 216.blk s6am 5 - 10;. plagioclase phenos t o 0.5 cn, 5% o r less, scattered k-pheno, b i o 3%. 217: 45 t o CA

217.1:55'to CA _- 218 - 220: plagioclase phenos a l te red t o 60°to CA s o m y dark green. some w i t h l i g h t green b l k seams 1 rims. macro bx mark

main FW o f bx _-- 220 - 227.3: in most places plagioclase so f t zone. white and/or s o f t pa le green. m d l m hard or s o f t soapy green.

215 5:blk seam =(except where feldspar a l l a ! tered). 60* I 5

45* 6 5O

45' - 80

Local ly whl te

. . . . . 1

ore. -_

-_

t ( 5 - .. __ -

,e blac ' there It!

.-- hlppm.

.

-

_ _ _ _

O X ) .

seamr Ire, nc

I O

SYMBOLS AND ABBRFVIATIONS *Eg. _MoSp: MoS equivalent t o t o t a l Fb, calculated assuming no oxide Mo i s present. Oxide leach n o t . l N r F n V I L

performed on 33 - 3 samples.

9 FAG€ 9 0 6 -

n o L E m c NO 79 - 5 ~


DRILL HOLE OR SECTION OATA RECORD PROJFCT NAME casmo . - - . 3991T- ~ - - PnOJECT NO

Dmn R r n w k s I I I -r---- -----7--1

POLITICAL UNIT

LONCIIUDE I 1 WORK DONE N=

DRILLING _I_ -

-- LOGGING ___

ASS A V 1 NG

LENGTH

L - L L - L ADDITIONAL INFO -

s2i

!27.7

___--_ s t . Total A S S A Y R E S U L T S ROM 1NT. REC

qg.R)S, Av(oz/t Ay[oz/t W pp "' 0 Ft. . 5 Mo

90 - 700 10 98 0.1, .058 .097

I N r r -vEn

ome veins. man:' blal:k h a i r 1 ne seam. wi th M)S2 mea-s. Sani. l o s t . --___- __ ---I -

.0371 .062 00 - 710 10 98 0.1

SIructwn.l A+ iVMROL C.A./Olp

SAMPLE No.

-___ 227.3 - E: as weTfas plagioclase phenos 81 tered t o s o f t l i g h t green.

about h a l f o f feldspar i n gm. 9 - 5 - 6 8

9 - 5 - 6 9 END. ack s e h . Some l o s t . h i n l y as p a r s i n

--____ 9 - 5 - 7 0

- 1c

!n d ick ___

10 -.

10 Mo S I

7 sev -.

10 - 720 a i n l y bro unrerous b

0.1+ nuous lot COl

9 - 5 - 7 1

9 - 5 - 7 2

20 - 730 co.01

30 - 740 s quartz

0.01 i t e ve

9 - 5 - 7 3 90 - 750 n t i r e l y a

0.10 artz-tJ

, . . . . I

SYMBOLS AND A B ~ n t V I A r l O N S *E_g.MoS2: MoSz e g u j s l e n t t o t o t a l Mo, calcu lated assuming ~ ._ no oxide Mo i s present formed on 79 - 5 samples.

Oxide leach not p.er-SIIEEI INTERVAL tram

I

WORK W N E N e m

ORIt L ING ___ LOGOING:

ASSAYING,

~- OF ' 1 PAGE

PROJECI NCME - 'aSmo P R O J E r l NO

IIOLEISEC N O -

SHELL CANADA CIMITEO - MINERALS DEPARTMENT DRILL HOLE OR SECTION DATA RECORD

35alT -- 79 - 6- -- --- _ _ . -- ____ - OOWI Remarks

LATITUOE DEPARTURE ELEVATION IVATUMI

N

LOCATION

sunvEY E 1584.24 m A 7

- __.___-----

- _______ FIELV

-__I _ _ _ _ _ _ _ ~

- ___--__

3 - 7

7 - 20

Slructurd Angh SYMBOL C.AJOlp

LIltlOLOGY. Texture. Structure, M l n n . l i z m l l a ILlIhnlngl

I . . ' * l I Casing t o 12.2 m. SJiJ2:

Overburden. 7.5:sgveral a t 30 t o C.A

Quartz Monzonite: pink-grey, med-cse grained: k-spar po rphy r t t i c . Pink pe r th i t i c 8.2:20° t o CA t o 3 cm 25 - 502. Occasionally mantled. B io - 52. 8.3:30° t o CA

Py r i t e : 0.1 t o 0.5% mostly i n veins. 9.2:60° t o CA Mag: 0.1% disseminated. Moderately magnetic.

- 7 -- - 20,5: Breccia zone. Mostly micro b recxa . some macro breccia. Local ly due I n 12,,3: two sets pa r t t o f rac tu re c l e w . sub p a r a l l e l core 40 t o C.A. axis, but also numerous s l i p s and some black clayey seams. 12.5:70° to CA

12.1:20° to Cil

7 - lo: &vum so f t , opaque white.

10 - 12: 6 d f i b a r d . --- 12 - 15: b i o gone. about black c lay s l i p s with -q@ge (Intense microbrecciat ion) - 0.5 m i n te rva l l i k e 10 - 12 m between.

Plagioclase a l t e r i n g t o s o f t t o

Plagioclase a l t e r i n g t o l i g h t grec

mostly a l l feldspar a l t e red and Two such i n t e r v a l s each zoned

13.4:20° t o CA

13.5 - 14.2: mblack seams &

s l i p s 80 - 60'' t o C . A .

14.8:30° t o CA

15.2:60° t o CA

15-18:numerous From s l i p outwards zoning i s :

1. plagioclase a1 te r i ng t o s o f t soapy to C.A.

fractures I s l ips. 45O-60'

17.2:30° t o CA dark ween and k-spar a l t e r i n g t o grey greer , medium s o f t .

2. narroM zone plagioclase a l t e r i n g to 18.2:40° to CA soft soapy yel low green and k-spar as i n 1

18.2-20.4: crumbled core

u.1

SAMPLE No.

3 - 6 - 1

3 - 6 - 2

5 - 6 - 3

9 - 6 - 4

9 - 6 - 5

_____-

9 - 6 - 6

9 - 6 - 7

~- CROW . ro FT

tluch coul Also frac

21 - 30

30 - 40 As quartz

__-___ 40 - 50 As above:

50 - 60 As above.

60 - 70 As above.

BO - EO As above --__

80 - 90 As above.

- NT. I F T -

9 ha b re5 __

10 os; -_ 10 10

10 Son _- l o Mo:

I O d : _ - l o Son

.os0

.103 BS no t

.123 -

.

.120 en.

.160 quartz

. loo n quar'

.__ -_

SYMeOLs AND ABBRFVlArlONS y l g , MoS2; MoSZ-equivalent t o t o t a l Mo, calcu latedass_ming no oxide Mo t s present. Oxide leach not SHEEl ,NTCRVAL ,>erformed on 79 - 6 samples. 1

MVNOOYV


LAI ITUOE DEPARTURE ELEVATION IDATUMI

N E

FIELD LOCATION SURVEY GRID A 2

- AEC IVER -

99 ous

99 SI1w!

80 t

_.

99

so1 SIN?

- _ _

-

SAUTLE No. ' O T t 0 I r Z T

90 - 100 10 \ s above. Numc I____ __

too - 110 10 \s above a id as

___ 110 - 120 10 [ n quartz . Mo:

__ 120 - 130 10 \s above a id as Iisseminat ons.

_- -

' . . I . . . . !

3. plagioclase a l t e r i n g t o s o f t soapy dark green and k-spar greyish pink o r unaltered. a l i t t l e b i o may remain.

15 - 20: mainly plagioclase a l te red t o opaque white, medium so f t , except a l t e red t o l i g h t green nedium hard 17 - 18 m w i t h centra l zone a l te red t o so f t soapy dark green adjacent t o a s l l p a t 17.5.

Contact a t 20 masked by breccia zone and crumbled core.

__ Quartz Felds a r Por h r : g r m , a f P _ - e w p a g + oc ase phenos 2 - 3 mn (3%; fine-medium grained b i o 3%. or k-spar phenos w i t h i n 5 m of contact. Moderately magnetic. Spec S - l C , although S-1C I s more potassic.

_ _ 20 - 30.8: plagioclase a l te red to medfun, s o n - m t e , some w i t h s o f t soapy l i g h t green cores.

30.8 - 31.3: Plagioclase a l te red t o s o f t white, k-spar a1 tered t o medium hard grey green adjacent s l i p and micro breccia.

.- 31.3 - 33.2: s o f t opaque white.

25 m..o)"t small quartz phenos 1 - 2 mn. 2 - 32 of rock.

32:

pink, q u i t e f ine-

No quartz

Texture i s s i m f l a r t o

a l l feldspar a l t e r e d .

plagtoclase s o f t t o medium

30 cm breccia zone adjacent s l l p 40' C.A

sllps:

25.8: 60' t o C.Q. 70 t o C.A. I

Many f ractures i n quartz feldspar porphyry same angles as quartz nmnzoni t e but few are s l ickensi ded.

28.3:60° to CA

29.3:60° to CA

30.7:30° to CA

30.9:60° to CA & 10 cm brecci I

31 :50° t o C.! 32.6:10-20° .!I 20 cm brecc i

33.2:90° to CA

34.1:80° to CA

34.4:40° to CA

black s l i p s 75 t o C.A. 60: t o C.A. 45 t o C.A.

36.4-36.5:

.116 t z ve i l

7 9 - 6 - 8 .193 . Som

0.05 h in qu l o s t .

7 9 - 6 - 9 0.05 s i n b

.078 ccia.

.130

79 - 6 - 11 0.03 r i t e v

0.15 s i n b l o s t

-

.092 ns. B:

.153 ck sea no t CI

.180 ccia, : om hrol

.300 lme loc n core

7 9 - 6 - 1

1 . . . . 1

SYYOOLS ANV ABBAEVIATIONS In W E E T INTERVAL (,om

MVf(W7V

ZEXi

'7 - 48

48 - 66.3

34.4 - 35.8.: macro breccia 50% broken core Sllp~: l o s t . Fracture c l . 5 - 10 t o C.A.

37:70° to CA 36.3 - 58.5: 37.5:60° t o CA macrobreccla, numerous s l i ps , some along t h i n black seams. 37.7:20° t o CA 37: contact masked by breccia. 37.8:30° t o CA

@wrtz Monzoni t e Por h pink-grey, f l ne - 50' t o CA grained .sugary matr!xy quartz phenos t o 0.8 20' t o CA cm 20%. plagioclase phenos t o 0.5 cm 10%. pink p e r t h i t i c k-phenos t o 1 cm 5% o r less. 38.5:500 to

38.7:45' t o CA

38.8:40° t o CA Moderately magnetic.

S imi lar t o Spec S-1B i n texture, although 39: 45' t o CA S-1-8 i s more potassic. 39.2:70: to CA Spec 79-2-147.2, although the l a t t e r doesn't 39.3:40 to CA

30' t o CA have qtz . phenos. 40.2:90° t o CA

45' t o CA 3 3 . 2 5 0 . 1 : plagioclase l i g h t green t o a%st w m e , medium so f t , some w i t h soft, 40.4:50~ to CA

41.1 :several soapy cores. black seaas I Contact a t about 48 masked by brecc lat lon. slips 6o to

Breccia zone, microbreccia and

38 - 38.4:

Same g ra in s ize as

C.A. 41.8:300 to CA 42.5:700 to 42.7:50° to CA 42.9:30° to CA 47:65 t o C.A.

quartz Monzonite: pink. grey, medium-fine- g r m , - * F l a s e phenos to 0.5 cm 10%. k-phenos to 1 cm <5X, some mantled. s i m i l a r t o Spec 79-5-73.5 except tha t plagioclase phenos are more d i s t i n c t .

Texture

.. .

50,l - 51.8: a l l feldspar a l t e red b i o gone p l a f i d a s e a l te red t o so f t soapy yel low green, k-spar a l t e red t o grey green so f t . Hi-grade in te rsec t i on w i t h many black seams i s i n center of t h i s zone.

3*2 :450- to 44-1:400 to 44.2:650 to 44*5:580 to 44.7:5 t o CA I 20' t o CA

, . . . . I I

SAMPLE No.

9 - 6 -

9 - 6 -

_- -

9 - 6 - 1 4

-__-

9 - 6 - 1 5

9 - 6 - 1 6

- -

9 - 6 - 1 7

~- INT. n E c E s t , Total FROM

TO F t , I N F T DVEAV L L

130 - 140 10 95 0.05 to *076 0.1

Veins and riany mear; i n b r e x i a . Black seam not counked. Sow l o s t . --__.__.I-..______ ____

140 - 150 10 95 0.02 -049 quartz - MtrS2 ? pyri :e veins. Blacl Crumbly t o 'e.

__

150 - 160 10 97 0.02 .064 As above ai d as sinea -s i n b r v c i a . Some l o s t rom 1:rumb y core.

160 - 170 10 93 0.3, -441 Most I n shtsared and irayrnent?d quarl contalning much b lac : clayey seams. seams. Sol e qu r t z - S + p r i t e v( outs i de h I -'grad:! 1 n t !vi 1 'kobabl j

__ - . . - _- _ _ -. .- - - - -

. - - . -. - -- --- -

170 - 180 10 97 0.01 .027 Crumbly coi'e. __-__ - __ _._ __ --- - - --

180 - 190 10 83 0.2 .09O quartz-MoS. i p l - r i t e veins. CrunblJ

t

_ - _ _ _ _ _ _ ~ --

I

I

SYMBOLS AND ABBRFVlATlONS quartz Monzonlte~Porphyry - Intermediate-between quar t z fe ldspar porphyry and f i ne-medium grained quartz monzonl e.

S S A V R E S U L l

~~~~

.127

--__ -

.082 seanis n i t counl

-

.736

. ___

d.

_ _

m

-. -

m i n te i i n cla: brecc

- _-

-

l o s t . __

E

a1

c.

,

--

S I E E ~ INTERVAL ilnm IO

MVNOlllV


' R W

ro f e e t .

I90 - 200 )uartz - M

!OO - 210

E s t . Total A S S A Y

Mo I EQ. MoS; SAMPLE

No.

79 - 6 - I I

79 - 6 - l !

79 - 6 - 2(

_ _ 79 - 6 - 2'

~ - -

79 - 6 - 2;

L

Slruclurd Angle SYMBOL C.AIDip 4

LITHOLOGY. Taxlure. Slruclurr. MinerdIration Kithnlop)

-T- ' . 1 I I M Y

56.3 - 69.2

59.2 - 76.0

m .

E a

.

I .133 0.03

e vein! -I-

<0.01

51.8 - 58.5: bnxTe66; s o f t soapy t o medium hard.

58.3: X a f rac tu re c leav .50~ t o C.A.

58.5 - 62: opaque white, s o f t t o medium hard, l o c a l l y pa le green.

62 - 66.3: s o f t soapy t o medium hard.

62.5:

._ 63.4:

E: 63.5 - 65: -- Microbreccla.

plagioclase a l te red l i g h t t o

Becomes less o f a microbreccia, more

plagioclase a l te red t o malnly

plagioclase mainly l i g h t green,

A p l i t e dike 20 ctn 40' t o C . A .

A p l i t e dike, 3 cm 50' t o C . A .

A p l i t e dike, 3 cm 50' t o C . A .

SJks-:

45.5:20° t o C I 46.5:20° t o C I 48.3:50° t o CI

70' t o CI 48.5:40° t o C I 50:50 bo CA 50.1:60 t o C I 50.2:20° t o CI 50.5-51.3:manj black seams w i t h B l i p s 45' t o 90 to C.A .

54.5:70° t o C I 55: 65' t o CC 62.4:8o0 t o cr 62.5:80° t o CC 63.4:250 t o CC

-;5-1-; -

.041

-__I_

.007

.076

!10 - 220 luar tz - M

0.02 e vein!

.068

.012 0.01

__ 0.05

!20 - 230 Is above.

!30 - 240 is above.

. I27

qtgrtz Felds a r Por h r : pink, f ine-graine smaw quartzPpm$6di phenos t o 0.5 cm. Simi lar t o Spec S - l D only deeper salmon pink. K metasomatism? Contacts gradatlonal 64.1:lo"to CI over 10 cm. 68: 50' t o CC

Q u a r e Monzonite: plnk rey, Redim-f ine- 75.1: black

2 cin) 5 - 10% plagioclase phenos t o 0.5 Cm

3 - 5%. 75.2:75 t o C I

74.5: 5O t o C!

seam & s l i p grsnea, k-phenos 0.5 - s cm (occasional ly 80 t o &A

I 66,3 - 67.6: t o inedium hard.

plagloclase opaque white s o f t

67.6 - 91.5: green, so f t soapy t o medium hard. green next breccia zone a t 75 m.

plagioclase a l te red t o l i g h t Dark

, . . . . I I 5HFF7 I N l F R V A L lrnm In

- INT. r( F 1 -

10

no +

10

-

10 fei 1

10 ?rot . __ -

- E S U L

(v(oz/

c ia .

t.

-

- AEC VCR' -

90 r i tc COUl

97

75 L r __ 94 smf

_ _ -

ist . bS:,

0.01 veins ed .

'o ta l A S S A V

T 'AOY

ro F t . Slruclursl Angle M W L E

No.

75.4:45' t o CA

75.8:25' t o CA 76: 30' t o Cfl

76.1:20° t o CA

76.5:45' t o CA 76.6:70° t o CA 76.8: 70' t o CA

80.5:50° t o CA 81.7:75' t o CA

40' t o CA 70' t o CA

82.4:40° t o CA 82.6:50° t o CA 82.9:60° t o CA 83: 80; t o CA 83.4:70 t o CA

40' t o CA 83.6:70° t o CA 83.7:20° t o CA 84.1:75' t o CA 84.2: black segms IC s l ips 70 t o &.A. 84.8:15 t o CA - 60' to CA

80' t o CA 85: 50' t o CA (black seam) 85.3: black segm s l i p : 60

Contact a t about 76 obscured by breccia.

75 - 76: Breccia, micro and macro.

Quartz Felds a r Por h r : very f ine-grained pink, small w l a g i o c l a s e and quart; phenos. S imi lar t o Spec S-1E. Much salmon pink k-spar i n gm - K metasomatism?

Since 60 m (o r before) salmon pink k-spar has been prominent.

Contact a t 79.7 obscured by breccla but I t appears abrupt.

76 - 79.7

79.7 - 81

Quartz MonzoKte:

79 - 81.4: Breccia. Crumbly core.

l i k e 69.2 - 76.

81 - 95.5

Q i E r t z Feldspar Porphyry: pink. q u i t e f l ne - g r a i n m r m phenos. Very weakly magnet i c . __ 81 - 83.5: and-plagioclase phenos t o 0.3 cm 5%.

83.5 - 90.7: gm. as wel l as very few phenos.

Quartz phenos t o 0.5 cm 10 - 20%

r e l i c t texture suggests f i n e r

.016 d smeai

.027 i n bi

.- - __ .053

? 9 - 6 - 2 ?40 - 250 )ua r t z -Mo' 3lack seal

l 9 - 6 - 2 ?50 - 260 \s above.

0.02 -032 - 82.8 -30.7: Breccia zone, mostly micro- bras, some macro-breccia.

90.7 - 94.5: very f ine-grained gm. Quar phenosm%; plagioclase phenos 1 - 21, scattered k phenos.

7 9 - 6 - 2 !60 - 270 Is above

0.01 ears.

.008 5me lo !

.013

.I10 Sone 1

Z

1 9 - 6 - 2 ?70 - 280 feins I ni

0.03 rs i n

.066 ecci a.

91.5-93-: Gdqum h a r l t o grey green so f t .

. pl.ayp!ofl,a,se.

k spar a1 tered t o grey pink No v i s i b l e

SYMBOLS AND AABIIEVIArlONS -~ 1.3 StIEFT I N l E R V A L lronr

M V N W l V

- FORL UNIT

L

- NT. 4 FT -

10 ne a _I

10 nea

10 I S S I

-

- 10

_ _ _ 10

l l a i

10 m i I

10 leal . _-

-

- IEC VE fl -

85

-

83

-_ 90 i na __ IO0

_ _ I 00 se --_

80 :ed -

97 on - .-

-

- E S U L I iqiE7-f

t coun - --___

t coun

Some 1

_ _

SAMPLE No.

FROM

TO Feet .

280 - 290 Veins and

Slructural Angle SYMROL C.A./OIp

86.2:blajik segms 90 to 45 t o C.A. 86.7 : black seam and s l i p 50 t o C.A. 85.5 - 90: crumbled o r broken core

90.2: black seam and s l i p 70

90.5: s l i p w i th gouge 60' 92.3: black seam 50° t o C.A. i s HW o f breccia zone.

92.6: Black seam 55 FW 01 breccia.

93: black seam 75 t o CI 97.2:20° t o CI 98.1:50° t o CI

40' t o CI oo t o CI

98.2: bback seams 40

101:20° t o CA 104.2: 30'

70'

1 0" 1 so

DEPTH rptrec

35.5 - 114

92.3 - 93: Micro breccia zone w i t h several black seams.

93 - - 104: opaque nhi te.

-- 94.5 - 95.5: gra i n i n i t e . Granite: pink, medium-fine-grained, non po rphy r i t i c . Texture s i m i l a r t o medium- f ine-grained quartz monzonite 69.2 - 76 except no phenos and more k-spar.

Py r i t e : 0.5% mainly as veins. Mag: <0.01%. almost non magnetic.

NE: k-spar. Above and below t h i s i s also abnormally h igh i n salmon pink k-spar. t h i s i s K-nietasomatism.

__ 100: scattered k-phenos appear.

104: but only less than 1%.

Plagioclase a l te red t o s o f t

Gradation t o medium - Pine-

90.7 - 95.5 contains 75% salmon p ink

Sure

plagioclase phenos t o 0.3 cm appear,

7 9 - 6 - 2

7 9 - 6 - 2

7 9 - 6 - 2

7 9 - 6 - 3

290 - 300 Veins and .._I_ ._

300 - 310 Veins and

!d. . . . - .

310 - 320 As above.

7 9 - 6 - 3

7 9 - 6 - 3

320 - 330 Rs above. -- -

330 - 340 Wainly d i !

101.4 - 102: massive grey-green muscovite mx3i ssemina ted MoS2.

__ 104: around a s l l p and breccla zone.

104 - 112.3: Plagioclase a l te red t o s o f t s-ght green, many w i th white r i m , except 30 cm zones a t 109 and 109.5 o f a l l feldspathic a l t e red green adjacent s l i p s .

~ - _ _ 106 - 107: Breccia zone - n l c r o brecclq.

30 cm both feldspar altered, no bio, t .

7 9 - 6 - 3 340 - 350 Mainly i n

SVMBOLS A N 0 ABBnEVlATlONS - __ I" SHEET INTFnVAL lrnm

MVNOWZV

I


______ LATITUDE DEPAnTUnE ELEVATION IDATUfrO

N E

FIELO LOCATION SURVEY GRID

-

-___

14 - 110.4

112.3 - 114: Zoned a l t e r a t ton :

112.3 S l t p 75' 10 cm plagioclase a l t e r ed to soapy dark green, k spar a l t e r ed t o grey pink.

30 cm macro breccla, k spar a1 tered to dark grey green, remainder replacement quartz.

15 cm banded muscovite. quartz. py r t t e , minor gissemtnated HoS2 and s l i p a t 60 . black s l i p a t 50'; 10 cm plagio- c l a se a l t e r ed to soapy yellow gree k spar a l t e r ed t o grey green.

30 cm mtxed a l l feldspar a l t e r ed to green and plagfoclase a l t e r ed t green, k spar grey pink.

black s l t p 70'

40 cm plagioclase a l t e r ed to soapy green and k-spar a l t e r ed to grey plnk.

114 Contact: s l i p a t 70'.

Aplite: pink, very fine-gratned, 99.5% quartz and k-spar, non magnetic.

Lower contact sharp a t 30' t o C . A .

Slruclur.1 Angle SYMBOL C A I D b 4

slfps:

104.5: 40'

104.6: bl acb s l t p 70

105.2: 25' 40'

105.8: 20' 1 oo

106: 45' 106.9: black seam 70' 100.5: 70' 109.1: 50' with 30 cm zoned a1 terat ion. 109.6 : black seam 55' 110: 40'

110.3: 45' 110.4: 50' 110.5: 70'

25O black seam & quartz vein 4( 110.6: 5'

111.8: 35O 5O

112.6: 40'

A S S 4 V I I-

-

E S U L l

SYYBOLS LND ABBREVIATIONS ~.

MVNW'IV

DEPTH lmtrQs-

118.4 - End

'24.7111 109 f t )

-_I Granite: pink-grey, medium-fine-grained, non porphyrt t i c (except f o r scattered plagioclase phenos to 0.5 cn). 95.5 - 114 only f i ne r grained. non-magnetic.

Same as Weak t o

114 - 118.4: no v i s i b l e plagioclase l o c a l l J t o grey green.

118.4 - 122_: soapy dark green, same w i t h s o f t whtte r l m s .

plagioclase a l te red t o sof t

122 - 124.2: soapy l i g h t green, some medium s o f t whlte.

plagioclase a l te red t o so f t -.

124.2 - End: Plagioclase a l te red t o s o f t n h t t e or sof t soapy l i g h t green. grey pink.

a l l feldspar a l tered.

K-spar a l t e red t o

END

14.8: 65' 15.4: b l act earn 55'

17.4: black eam 60'


DRILL HOLE OR SECTION DATA RECORD PAr,€--- -8 o[ain;~ PnOtECf NAhW -. 3991T ~. .~

PROJECT N!J ~- 79. ~~ ~ . ~ - ~

fKNElSEC N O . . - .~ ~

-

-.

~- - - WORK DONE N a m D a m Retrurks

OnlLLlNG L A T I T U M DEPARTUnE ELEVATION IDATUMI HEAnlNG INCLINATION LENGTl l

_ _ _ _ -EfZfZl - FIELD . _----- __ __ __ .

-_ --.__ LOCATION

GRID

-- -- LOGGING.

~ ---- - - - ~ ~ ASSAY INO

N E I Z , SURVEY

---- LANDMARKS. __ --- ~ .. -. .-

LOGGED BV.-- OTHER FEATURES. .- - -- __- ~ ~ ~

P --- M M P L E FROM.. . INT. REC.

INF'. JvEn tal A S S A Y

79 - 6 - 34 350 - 360 10 97 <O.O1 .005 .008

Eg .?bS?+A 0 2 , TO. . F t . ..... . v (o r / t As(

Black seal s no COUI Led. ---

~

_ _ - ~ .---__ -_ ~.

79 - 6 - 3. 360 - 370 10 93 0.02 -027 -045 Quartz-Ho:2 ?r l y r i t , veins. smears n brecc a, some dlssen

-- --__ ---.__- - _- - 370 - 300 10 97 0.02 .011 .018 As above.

~- - ______- __ - _ 380 - 390 10 -100 0.01 .010 .017 Veins and sneai's i n f rac tu r s. Blatk seams not cou~ ted .

-__. _ _ - - ~ ---__ - -

390 - 400 10 98 dj.01 -014 .023 _- ---- __---

400 - 409 9 -100 <0.01 -018 .030 ._ __.

I" SHEET INrFRVAL from

POLITICAL UNIT

:YrE

D -

- 47.6

---___ L I rH0LOC.Y. T e ~ t w s . S t r u c t ~ s . Mirarmllratlm ILithalqI

---r--r,

Casing t o

0verl)urden

-. Ovartz _ _ _- Feldspar _I - __ fom-r-: g r a i n e d sirgary quartz mnzoni te, quartz phenos t o 0.7 cm lox, p lag ioc lase phenos to 0.7 cm 1 - 52. scattered k-phenos to 1.5 cm. Variable s lze and propor t ion o f phenos. Bio less than 32.

Py r i t e : 0.1% mostly i n veins. Mag: <0.01%, general ly mi-negnet lc , l o c a l l , weakly magnetic.

. 8.7 _.__-- - 9.3: Ap l i t e . No phenos, contacts inwked by breccia.

. 10.1 - .- - 10.7: Ap l i t e . 1 - 22 small quartz phenos. Contacts masked by breccia.

___- 10.9 - 12.3: Ap l l t e . Top contact masked by breccx.-Bottotn contact gradational over 0.7 m i n t o quartz feldspar porphyry.

- 10: Mostly brecciated, micro and macro breccia.

14.5: Several 3 cm pods medium grained, pegmatit ic intergrowth o f quartz and b io .

- 27.5: soapy white t o very pa le green and white medium s o f t t o so f t .

pink, very f'ine-

plagioclase a l t e r a t i o n varlable. so

19.0: 20 cm k-spar a l t e r i n g grey pink t o grey -and b l o a l t e r i n g m u s c . . d p lag ioc lase a l t e r i n g soFt soapy yel low - green, some micro breccla.

Strur.turd Awls VMBOL C.AJDlo

U S - :

2.5: 60' t o

6.0: 45' t o

6.5: cbay seam 55 t o

C.A.

6.8: s l i p i n musc. ve in 60

C.A.

C.A.

7.9: 35O

8.7: aoo 4 0'

9.9: 30'

13.6: 30'

14.3: 50' w i t h 10 cm brecc fa.

19: nwJy seam 70 t o C.A. w i th 20 cm a1 tera t ion - breccia zon

SAMPLE No.

r 9 - 7 - 1

1 9 - 7 - 2

"OM ro F t ,

11- 20 Too broken

?O - 30

- UT. I F 1 -

9 nd

10

-

- IEC- IER' -

50 a t t

80

-

iota1 A S S A Y =r E S U L T

v(oz7l

.01

.01

--

E m :

__

.-

SYMOOLS AND ABBnFVlAllONS *Eg.MoSZ: _ ~ o ~ 2 _ e q u i y a l e n t t o t o t a l Mo, calculated assuming no oxide Mo i s present. Oxide leach not INIcnVAL I" performed on 79 - 7 samples.

MV@lJRZV

ADDITIONAL INTO -.

WORK DONE Name

OAlLLlNG ___ LOGGING

- ASSAYING


L A riTuoE FIELD LOCATION SURVEY

- FORY UNIT -

-

L l 1 HOLOGY. T e x ~ w s . Slriocwvc. M i n r m l h l l a ILitholq)

-.--.-7). . . . , 19.4 - 25,g: b a d l y r a c t u r e d and broken core between. Too broken t o l og s l tps.

--- 27.5 - 32: - Both feldspar a l tered, plagioclase a l te red t o s o f t soapy opaque white t o l i g h t yel low green and k-spar pink grey medium hard. Bio general ly present but l o c a l l y gone.

20 cm k-spar a l t e red t o s o f t grey-

Numberous breccia zones w i t h

27.7: green around a quartz-musc MoS2 vein.

32.7 - 50.3: Mainly both feldspar a l t e red l i k e 27.5 - 32, w i t h i n te rva l s o f only plagioclase a1 tered t o so f t soapy l i g h t green between k-spar varies from l i g h t grey pink th ru l i g h t grey t o dark grey green.

8 i o gone i n some a l t e r a t i o n zones. o f plagioclase only a l t e red are:

I n te rva l s

33.5 - 34.4, 34.9 - 35.0, 35.4 - 35.8, 36 .T - 36.6. 39.5 - 39.6. 41.4 - 43.5. and 47 - 49.4.

Some o f these a l t e r a t i o n zones are a lso mlcro brecciated, notably 36.6 - 41.5, 43.5 - 44, and 45.2 - 46.4.

37.8 - 40.8: Grain s ize of ground mass coarser { f i n e to l o c a l l y medium grained) and phenos not as prominent. 40 - 41 rock Is fine-medium grained pink quartz monzonite. These changes are gradational.

44 - 45.3: Granite, pink, medium-fine- grained, quartz 'pseudo-phenoa' 152. Top contact f a u l t wi&h breccia 30 t o C . A . , bottom contact f a u l t 70 t o C . A .

Siruciurd Anglm l Y M B M C.A.l(hp

19.4: 50' t c C . A . Hw breccia zone.

20.3: 40'

20.4: 60' FW breccia zone.

21 .l: 30' 10 cm micro breccia.

25.2: 35'

27.4: 50'

27.5: 30'

28.1: 50' t o C . A .

28.8: 30' t o

32.7: 70' t o C.A.

34.5: 50' t o C . A .

36: 20' t o C . A .

36.6: 30' t o C . A .

376 MoS2 s l i 55 to c . . A

C . A .

SAMPLE No.

7 9 - 7 - 3

I__ __

7 9 - 7 - 4

' 9 - 7 - 5

' 9 - 7 - 6

' 9 - 7 - 7

---- ' 9 - 7 - 8

' 9 - 7 - 9

79 - 7 - 1c

-__-

79 - 7 - 11

$Liz

:.01

< .01

c.01

c.01

-

< -01 :rutnbl!

c .01

SYMROLS AND AOBREVIArlOllS

0

DRII.LING.- ___ - LATITUDE OEPARIURE

_ _ ~ FIELO - LOCATION

SURVEY LOOGING: ___ .___ ..

Gnlo , N. E __ ______

POLITICAL UNIT

ELEVATION IDATUMI BEAnlNG INCLINAI ION I C N G I I I

- b Z _____________-- ADDITIONAL INFO

- __-.._____.

CLAIMIPERMIT NO '

SAMPLE No.

79 - 7 - 12

___-

79'- J-- 13

____-.

o mn etres

17.6 - 69.8

Grant&(?) and uar tz Monzonite: pink-grey, mcJ7wn - f i ne gra 5 K 3 q u a r t z ranges t o ccc grant te and gives pseudo impresston of

__ 37.1:35' t o CA

37.3:45' t o CA

Contact a t 47.6 i s sharp, bu t no c h i l l e d margins. 1 ~ :

- 52.3 _. - 52.7: texture approaches f i ne - g r a m q u a r t z porphyry. Can't t e l l i f gradational o r f a u l t contacts.

39.5:25' t o CA

39.7:20° t o CA

37.4:40° t o CA

absent o r not recognizable i n m to 49.4

contains white opaque plagtoclase. Does

compositional change o r i s plagioclase simp1

Plagioclase quartz phenos. Scattered k-phenos t o 1.5 cm.

but w i t h i n a l t e r a t i o n zone begqnnlng 49.4 gw

a l t e r a t i o n correspond t o a gradational

not v i s i b l e before 49.41

54 - 59: Quartz feldspar porphyry w t th

which texture l s medium-flne grained and gm plagioclase i s much more abundant ( t h i s plagioclase a l t e r i n g t o sof t soapy opaque white); s o f t soapy opaque whlte mater ia l also occurs i n fractures.

. NU: -. changes due t o soda (plagioclase) metasoma- t i s m before a l te ra t i on , was the s o f t soapy opaque white (c lay) mineral formed as a 'pr imary' a l t e r a t i o n mineral ra ther than by a l t e r a t i o n o f plagioclase. d i d micro breccia prepare these zones for metasomatism and/or a l t e ra t i on , o r were there primary compositional and tex tu ra l dt fferences? Take spec. --_- fo r T.S. arc s t r i c t l y due t o rnetasomatlsa during a1 terat ion.

patches o f "two-feldspar a l t e ra t i on " i n

are these tex tu ra l and composlttonal

1 th ink differences

40.2:35' t o CA

' 1: tp a t 40

:nd 45

41.3:30° a t CA

41.9:300 at CA

42.1:400 at CA

42.4:200 at CA

43.7: black seam 70

43.9: ps2 s l i p 60

O.J:JO~ t o CA

I I

'nOM

10 Feet

4s above. 120 - 130

-

130 - 140 4s above.

SYMBOLS AND ABBREVIATIONS -~ _ _ _ . - S H E E I IN IERVAI . horn I"

LITHOLOGY. Ttxturn. Structure. Minsrdir,tim ILlthn1n)l Slructurd Angle SYMBOL C.A.tDIp4

--I . . . . I ----- 53 - 55.5: abundant a l t e r a t i o n plagioclase SHE: a l t e r i n g t o so f t (some s o a p ) opaque white adjacent f ractures 0 t o 20 t o core and development o f same opaque white mineral (earthy s e r i c i t e ? ) along fractures.

A t 54 rock i s a macro breccia, quartz feldspar porphyry, fragments 3 - 10 an; m a t r i x between i s a fine-medi-m-grqined micro breccia w i t h g s o f s o f t opaque white mineral also several pure vetns 5 m wide o f s o f t opaque white mtneral. Here brecc iat ion preceeded i ntroduc t i o n o f s o f t opaque white mineral.

55 - 55.5 and 57 - 59:

Two feldspar a1 terat lons; plagtoclase phenos s o f t soapy l i g h t green, k-spar

45.3: black seam 70 - /IN brecc 1 a

45.7: 30'

46: black seam 50

46.6: pS2 ~ ~ ~ ~ ~ ' t t v o 6.t!:mly 5116 30

a l t e r i n g grey ptnk t o dark grey green (banded) and small yrclins so f t o aque M t t e 51.5: 0'

a1 te ra t i on of plagiohlase). The boundaries 54.9: 20' banding are 0' t o 30 t o C . h . I can ' t t e l l i f 2-feldspar a l t e r a t i o n was superimposed 56.2: 30' on opaque white or visa-versa.

59 - 70.: composition of quartz monzonite o r grant te 56.8: writ&. bordering on quartz mnzonl te.

- - . - ~ 59.8 - 61: 2-feldspar a l t e ra t i on , p lag io- 57: 45' clase phenos a l t e r i n g t o s o f t soapy l i g h t green, k-spar pale grey pink and many sof t 57.2: 15' white grains. - NB: I thfnk these sof t opaque n h l t e grains 58.4: Bp1Y are not a l t e red plagioclase but s e r i c i t e o r s l f p 10

59.2: 50' kao l i n formed from a l t e r a t i o n of k-spar.

a l t e r a t i o n (formerly assumed t o E e

56.5: 5'

moly s l f p 70

Unaltered i n te rva l s have

Quartz - n _____

4s above a Black sear

-I----- '9 - 7 - 16 160 - 170

uar tz - m (9 s above a

I 1 - --

elns and _I I --

s above ai orphyry 0'

- I N I . N F l -

10 lY '

10 I a1 wi t

-

-__ 10 Y t

10 I as 'om

10 ear

10 as

r 61 -- -

-

Total A S S A Y

M o v .loo 0.02 Pyrl :e vein1

!loo 0.02 J smi!ars on )ut obvious

-- - . __

___

99 0.01 l y r i .e vetn:

f100 0.02 meal's on s l .okei and cr

-

___ _

95 0.01 on c l i ps .

100 0.12 1.5% dissenl cm .

-

- ._ - - - -

__- .036 1 .013 .022

l i p s . 01y not countec - -- - - __ - __

.021 .035

I

.024 .040 1 s .

Rbly cote. _ _

.011 .01R

--_ -

.067 .112 i t ions n quart

-- -__ . - - -

SYMDOLS AND AARREVIATIONS I" S I IFET INTERVAL lrnm

MVNMYV


SURVEY

TO Feet F - NT. il FT -

10 Y ! - 10

-

10

-

10

10 as

.-

7 .-

-

- IEC wni -

,100 iyri

100

-

100

100

100 mea ___

100

- o t a l A S S A Y

b (€9 . Mos7 s t . E

0.05 ? vein! I.__.

0.01

0 PTH nefres

69.8 - End

78.3 257')

m . 01 . 63.8 .. ___ - - 6 4 2 :

centerex around a quartz-mol3 vein.

65 - 68: opaque white mineral i n otherwise normal medium-fine grained pink grey sparcely po rphy r i t i c quar$z monzonite. fractures 0 - 15 to C.A. conta in the opaque white mineral.

68 - 69.8: wTh-m&eral. Plagioclase phenos a1 te r l ng t o s o f t soapy l i g h t green cores w i th whlte r l m

__ 69.8: .- Gradational contact.

g u ~ r t z _ f e l d l p ~ p O r p ~ y ~ : pink. very f i ne - grained ground mass, quartz phenos t o 0 .7 cm 102, k-phenos t o 1.5 cm 52 and var iab le scattered and var iab le plagioclase phenos.

68,8--- 72: a1 t e r e d t o musc.

7_2_:-7(i l : in tensely a1 tered, plagioclase phenos a l te red t o s o f t soapy l i g h t green, k-spar a1 te r i ng t o pink grey, abundant sof t opaque white mineral both i n t e r s t l t l a l and as d iscrete grains, b io var iab ly a l t e r i n g t o musc. i n places completely.

76.1 --En$: more pink than a t 69.8. only p%g%clase phenos a1 tered t o s o f t soapy l i g h t green some w i t h whlte rims.

2-feldspar a l t e r a t i o n as above

patchy and i r r e g u l a r content of soft

A numher of

sparce development o f sof t opaque

greyish pink, b i o var iab ly

.044 .073 9 - 7 - 20 200 - 210 Quartz - m

-____ .____.

9 - 7 - 21 210 - 220 As above.

--I__-

9 - 7 - 22 220 - 230 As above.

9 - 7 - 23 230 - 240 As above.

.O1

0.01 .O1

~.

.01 0.01

0.01 , on sl

<0.01

t <.01

s above ai

. 0 1 9 - 7 - 25 250 - 257 I

END

.-

SYMBOLS A N D AROftFVlAllONS

DRILL HOLE OR SECllON DATA RECORD

POLITICAL U N I T

AOOlllONAL INFO .

- INT. Y F? -

7

ire! m

__

10 Ve' . _.

10

- __ 10 Son ' l y -

l o Son

--

__ 10

__ 10 -_ 10

.. .

-

- HEC WE A -

70 Y + and

86 s ai -

92

100 ve

usc - 90 ve

100

-.

_-

97 _.

95

__-

-

__--- FROM

TO f t . .

13 - 20 AS quart2 Mos t frac

SAMPLE No. "k""

0 - 4

4 - 53

7 9 - 8 - 1 0.06 t r i t e !ins h

Casing t o 18 ft. 7.8:

8.5:

9.4:

9.6:

30' t o C.A.

15' t o C.A.

5O

50'

Overburden

uar tz MonzonBe: pink grey, w d t m - It- ne g X e 7 , sparcely t o moderately k- porphy r i t i c . P e r t h i t i c k-phenos 1 t o 2 cm long.

p y r i t e : disyeminations.

mag: 0.1 t o 0.53 dlsseminations. moderate t o l o c a l l y s t rongly magnetic.

about 0.1% as veins. almost n i l

.030 es o x i

.05( zed.

2 20 - 30 As above.

0.03 f r a c t

3 30 - 40 As above.

.014 .02: ;o. 01

4 40 - 50 As above. 1 quartz- .____

50 - 60 As above.

0.12 i and rein.

0.02 ; and

.111 acture

--I

.041 acture

.10! oxid iz i

_ _ _ .OM

oxid iz i 5 4 - 32:

medium hard to medium so f t , l o c a l l y sof t white near fractures; s o w in te rva l s plagioclase a l te red to very f a i n t green.

4 - 24:

. 24 ._- - : Ground mss maln1Y medium- grains w i th some f i n e grained quartz, k-phenos 5 - 10%. plagloclase phenos t o 0.7 cm increase t o 32.

-___- 32 - 34.5: a l t e red to very pale green, medium sof t .

plagioclase phenos a l te red t o white

Very few k-phenos.

plagioclase phenos dominantly

6 60 - 70 As above.

0.01

.-

0.01

.035 .05F

7 70 - 80 .032 ,019

,028 8 00 - 90 0.05 .047

-

1

Oxide leach not SVMBOIS AND A#,HREVlATlONS *Eg.@S2: MoS2 equivalent t o t o t a l Mo, - calcu lated assuming no oxide Mo i s present. - - _ _ _ _ performed 66 79 E Caiiipli3. W E E T INTFAVAL lrnm I,,


L - - _ L _ I _ I ____ ~- ASSAYING, .- ADOITIONAL INFO

LOCATION

GRID

- FOR UNI -

-

L ITHOLOCY, Te.lwc. Slruclum, Mlnardlrallon Il~llhologl Slrwiurml Awls SYMBOL C.A.IDlp

m?_-. 1

34.5 -46.: plagioclase phenos a l te red t o S , : I - i G K g r e e n sof t , some w i t h white r i m s . Local ly s o f t soapy dark green. 32: 30' t o C.

38.7: 30 cm 2 feldspar a l t e ra t i on , 8.7: s l i p , p lag ioc lase a1 tered t o s o f t soapy green,ilack seamsd k-spar a l t e red t o s o f t grey-green. b l o zone. breccia. 60 Zoned around quartz ve in and s l i p w i t h grey-pi nk k-spar on outs Ide. 40: 40'

-- 41.6: IO cm 2 feldspar a l t e r a t i o n (as a t 40.2: 30' 38.7) on H.W. of quartz=moly vein. F.W. o f ve in i s 3 cm black c lay seams (gouge:q0.5: 30'

50' underlain by breccia zone.

____ 41.7 - 43.5: Micro and macrobreccia zone.

---- 43.5 - 53.9: k and plagioclase phenos s l i g h t l y l a rge r and more abundant (10% 6 5%) 41.5: and s i ze range o f quartz grains tocoarse- g r a i n e d j n places they appear as phenos. 41.6: s l i p t,

40.7 - $1.5: 4 a t 30

50'

black seams __ 46 - 48: plagioclase a1 tered to medlum along qMartz s o f t a q u e white. ve in 60 - 70'

HW o f breccia 48 - 54: plagioclase a l te red to l l g h t green zone. s T t i y m w i t h white rims. Some almost white. 43.5: 45O.

- 43.5 - 48: semi-breccieted 06 f r i a b l e due FW o f breccia to f rac tu re cleavage 40 - 50 t o C.A.

44 - 44.3: 48 - 49.3: Macrobrecciated, u i t h s l i p Segeral at P a Y Z - a n d f ractures about 45 t o C.A. 40 - 45 . Sl ips and fractures contain so f t opaque white a l t e r a t i o n mn. 45: 40'

45.5: loo - ) . . . . I

I" SHEET INTERVAL lrovn - _ _ _ SYMBOLS AND ABBREVIATIONS


- _ _ I _ ~

L A - ADDITIONAL INFO .

- B A W L € No.

- INT. N F1

11

no r +

11 Id I

'OUI

10 lo11 . _ _ _

FROM ro F t .

E S U L

!miiii

n hrec

-- -_ ~

t i n n

46.3: 45' 46.7: black seam 70 , s l i p 50'

.017 smears

.080 r a l t e

,010 nd nolj

..___

.048 i n k-si

53.2 - 54: Macro breccia. 17 170 - 181 Qua r t z -nn Black sei

0.01 veins d . Contact a t 53.9 I s a s l i p about 60' t o C.A. 46.9: 40'

47.6: 60'

48: 50 quartz Feldspar Por hyn: pink, q u i t e f l ne - 48.1: Black y r a i n e d s u g a r y gm.: quartz phenos t o 0.5 seam 80 cm 52, plagioclase phenos t o 0.5 cm 23, few 48.2: I f any k-phenos.

Po

60'

18 180 - 191 As above envelope

0.01 a t i on z vel

i3.9 - 61.3

48.5: Black seam 60 49.3: 30'

50.4: b l ack seams agd s l i p 80

51.5: 40'

53.2: 70'

53.3: biack seams 50 - 70

53.8: s l i p 58 black seam 70

54: 30'

57.5: 0-loo

54 - 67.5: opaque whlte, l o c a l l y l i g h t green.

-. 54.5 ~I - 55.5: by fractures 0 - 20 t o C.A. Fractures F i l l e d w i t h so f t opaque whlte a l t e ra t i on . ( i s t h i s amorphous gypsum?).

58.4 - 60L4-: Micro and macro breccia. Some f r a c t u r e s f i l l e d w l th anhydrite o r gypsum? Passes i n t o a 0.5 m i n t e r v a l o f f racture cleavage 35' t o C.A.

Contact a t 61.3 a s l i p a t 70' t o C.A.

Quartz Monzonite & Quartz Feldspar Porphyry-:

plagioclase phenos s o f t soapy

Coarsg macro breccia produced

-i

ailfe=ng.

.030 5 and I

.050 pars o

9 - 8 - 1 9 190 - 20( As quar t i

0.02 te ve

11.3 - 64.4

SYMBOLS AND ABBREVIAl10NS ~. _ _ _ S l W E l I N t F R V A L horn 1"

POLITICAL UNIT

L O N G I T U M

ADDITIONAL l N r O

PAGE OF - 5 _ _

PROJECT N O . - .~ .. . 391T- . ....


PROJECT NAME..-_._ ..Castno ~ .

HOLCKEC NO _. 79 -. 8-

DRILL HOLE OR SECTION OATA RECORD

WORK DONE N s m Oatn Remarks

N

DAN LING,.-_---- __ l_l____l_ _____- FlECO

SURVEY GRID

COGGING, LOCATION

az --__- - -___ ASSAYING:

@Vi

64.4

LITHOLOGY. Texlvra. Sirucrors. Mtn~nl irmlm lt.itholog) -- 61.3 - 62: Quartz Monzonite: pink grey, medTi%--fine gr;FfKX('iT%Eugh quartz range up t o cse g r . ) , k-phenos to 1 o r 2 cm 10%. plagioclase phenos to 0.8 cm 5 - 10%.

Contact a t 62 sharp, no textural o r conipos i t i onal e f f ec t s .

--___ 62 - 63.5: Quartz- Felds a Por h ry: Contact a t 63:TTs s l i p ;OK to E.:. 63.5 - 6_44,4.: g r a m , sparce k-phenos.. Much salmon pink k-spar (metasoma t ic7 1. (Texture l ikg quartz monzonite). Contact at 64.4 s l i p 70 to C.A.

Granite; pink, medium - f ine -

.._.___I__ 63.5 - 65.6: Micro breccia.

Qu2rtrdFel;lspar Porphyry: very f ine- graine , p nk-grey. quartz phenos to 0 . 5 cm 5 - 102 (var iab le) , plagioclase phenos t o 0.7 cm 3 - 5% (var iab le) few & scat tered k-phenos, bio 3%. medlum-grained and sub hedral - suggests metasomatic or ig in .

Bio malnly

Pyri te : (0.1% mainly in veins. Mag: 0.1 - 0.52 dissemination, mod. magneti

67.5 - 76.7: Plagioclase white, medium medium s o f t .

-- 76.7 - 77.3: Plagioclase a l te red to medium soJ,t.to spft white.

SYMBOLS AND ABBREVIATIONS ~.

SlrwlurJ Anple YMBOC C.A./Mp 1

i1.4: ,jOo i6: 30 'ractures but w s l i p s 66 m ;o end.

SAMPLE Me.

9 - 8 - 2 c

3 - 8 - 2 1

1 - 0 - 2 2

9 - 8 - 2 :

9 - 8 - 2 4

P - 8 - 2 5

1 - 8 - 2 6

'ROM I N T REC ro Feat I N F T OVER'

200 - 210 i o 98 Several b- ack I elms

210 - 220 10 97 Several b-ack e eanis

----__I_____ I

- - ~ - - 220 - 230 10 94 As quartz-moly f pj II__ __ 230 - 240 10 99 As above. I~

240 - 250 IO 100 As quartz-noly ? py l_l_- -_- -

250 - 260 10 100 As above.

___ - -

260 - 270 10 100 9s above.

_. _ _

k co.01 o t cou I____

co.01 o t cou

0.01 te vel

0.01

0.01 te vel

0.01

.. - -_ -.

0.03

_-

A S S A Y R E S U L l

1-j

I_ J .041 ed .

.016 _I_

__

.005

.020

.007

_I .-

.015

-_

.06R

-- .027

I-

* om

.033

- -_ .012

.025

I" S f I E E l I N I E R V A L liom


r--- r------a -____ I BEAfllNE l lNCLlNAllDNl ILENGTH 1 ELEVATION IOATUMI

I FIELD LOCATION

___ LOGGING. __

I A Z I I I

_- OP H meT ,-e

91.75 301 f t

s t . E (0.01

<O.D1

FROM

TO Feet .

270 - 28(

St~ucturd A- XMBOL C.A./D*, 4

M W L E No.

9 - 8 - 2

LITHOLOGY. Tantwa. Structure. Minsr.llr~tlon Klthalql

--v' 1 . I

77.3 - 79: Plagioclase a l te red t o s o f t h d - t x - s o f t l i g h t green and s o f t soapy green.

- . 79 - End: plagtoclase only s l l g h t l y a l tere l translucent hard rims and opaque whlte medium and hard and medim s o f t cores. Most gra ins are dominantly o r completely opaque whi te . Local sof t soapy white o r l i g h t green as a t 91 m and 80 .3 - 81.3 m.

Some va r ia t i on i n shade of pink due t o va r ia t i on i n k-spar content.

82.7 - 83.7: Several dif fuse bands 1 - 2 CI o f very fine-grained. grey s i l i c i f i c a t i o n .

--- 88.3 - 89.3: greyer and f iner-gra ined due t o very fif le-grained quartz f looding. Bandtng 30 t o C.A.

____-

9 - 6 - 2 1 280 - 29C

9 - 8 - 2 ' 290 - 301 - -

<O.O l . - .-

s but

.008 .013 _ _

wren. '50 - END: !any t h i n kt are

END --

SYMBOLS A N 0 ABBREVIATIONS SHEET INTERVAL Iran, I"

MUNIIWV

r

FORl UNll I-

-

--

"%TS

0 - 13.

13.1 - 52.6

- LITHOLOGY. Tartwe. Strvc~un. Minerdizatlm ILltholql

. 1 . . , Caslng t o 43'.

Overburden.

QuarJz Monzoni te: pink-grey. medium-coarse g r g n & J - s p a r porphyri t i c . Quartz 40%. h i o 5 - 102, plag. 25% k-spar 252. Plnk p e r t h i t l c k-phenos t o 3 cm 5 - 20%. some mantled. Composi t i o n variable, esp. k-pheno

PiJg: < O . l mafnly I n veins. a s e t f t e : 0.1 to 0.5 dissemtnatlons. rock

Gdera te t o weakly magnetic.

13.1 - 17.2: plagioclase a l te red t o opaque WmfeGdih hard.

17.2 - 19.8: green medTm hard, some with s o f t soapy dark green cores.

plagioclase a l te red to l t g h t

17.2 - 18: micro breccia, crumbly core and iTnX.---- _- 19.8 - 24-99: plagioclase a l te red t o almost t r z c e n t hard t o opaque white medium hard

22.6 - 24 .9 : medium-fine-grained, fewer and s m m - p h e n o s , more b to (10 - 15%) inc lud ing some very f ine-grained b io . contact masked by broken core. but appears abrupt ly gradational over several Bottom contact breccia and s l t p a t 50 t o C.A.

24.9 - 30: both feldspar a l t e ra t i on , b i o gone, numernus quartz-moly vetns. several s l i p s w i t h micro breccia.

Top

-LLJ . . . . I SYMBOLS A N 0 ABBAFVIATIONS ~ _ _ - _ _

Slruclud An#* EYMBOL C.A./Dip a

SL I P s i 18:65 t o C.A

F.U. o f bx 20.2: 350 24.9: 5 0 0

25: 45O 25.3: 70' 25.6: 45O 28.8: 50' 29.3: 50° 29.5: 45' 29.8: approx

MI o f bx

500 Fn o f bx

POLITICAL UNIT

LONGITUDE I 1

I A 1 ADDITIONAL INFO.:

2 10 " E - - - ~

PAGE--_ ~

PROJECT N A M E ~ . -~

PROJECT NO :_ - -__JwlT 79-.- _- I4OLEISEC NO .. . ._ ___ ~. _ _


m K DONE N a m Datn Reinaka

DRILLING. -_ I I CATl lUDE I DEPAATUAE TELEVATION l D A T U M l l R C A n L L I L t a

FIELD LOCATION SURVEY

A 2

-______ L W G I N G

_______ - ASSAY INO,

Structvrl A+ LITHOLOGY. T r w m . Structurr. M l ~ d I ~ . t I m ILlthoW s w e m c.Aiotv

I " . ' , I

Plagioclase a l te red t o dark green s o f t t o soapy s o f t . k-spar a1 tered t o 1 i gh te r grey-green, medium so f t . Several zones plagioclase yellow, green and k-spar grey o r pink-grey. inc lud ing margins o f main dark green zone.

--I_- 25.2 - 26: black seams 70 t o C.A.

mij iro breccia around s l i p and

_ _ 28 _-- - 29.8: micro and macro breccia.

plagioclase mainly a l t e red t o

I 30 -=: jlght green hard, some more grey than green, l o c a l l y s o f t dark green.

SLIPS: ___- 35 - 41: 40.6: 60' t o C

41.3: 70° 412: 30 cm both feldspar a l t e red green. 41.4: 700 b l o oone. 41.5: 600

k-phenos t o 2.5 cm 25 t o 40%.

47: 2.6: 30'

41.4 - 49.2: plagioclase mainly a l t e red t o 2.7: 45'

5.2: 55' ______ 41.8 - 46.4: micro breccia and Inc ip ien t 5.8: 50' HW t micro breccia. some broken and crumbly core. 20 cm bx

6.9: b l k seam 46.4 - 47.1: gouge and micro breccia around i n f l t gouge Ua-searns 40 t o C.A. & bx 50

7.1: b l k seam 47.1 - 58.3: Micro breccia and i n c i p i e n t i n f l t bx 45 Gjcro breccia. Most core competent. 8.4: 35'

8.5: 40' 49.2 - 50.6: Plagioclase a l te red t o opaque 8.7: 45' white moderately s o f t t o very s o f t . 48.0: 60"

30 cm s a w as 41.2

n g h t x a a r k green, moderately so f t t o 4.3: 35O s o f t soapy green. 44.5: 5O

49.7: moly s l i I . . . . I 550

50.3: 15O

3 SHELL CANADA LIMITED - MINERALS DEPARTMENT PAGE OF lo PROJECT NAME' ~113gg,T11~1.. t a r T 5 ~ - DRILL HOLE OR SECTION DATA RECORD

POLITICAL UNIT. .. .. . . . . . .L . . ............ .... PROJ€CT NO.

HOLEISEC NO ~

- - 79 . = ~ -_ LONGITUDE W R K W N E Nmm D a m flmwrhs -

L A T I T U M DFPAnTURF ELEVATION I D A T U M I BEARING INCLINATION CENGlH DRILLING:

- F I E I D LOCAllON

GRID

w

~ _ _ _ N E A 2 sunvw

AOOITIONAL INFO.:.- ASSAVING:.

~ ;- LANDMARKS.

__ LOGOED BY: OTHER FEATURES. CLAlMlPERMlT NO: ~

__-_I

-

52.6 - 68

-___- 50.6 - 52.3: qreen moderately so f t .

52.3 - 53.2: both feldspar m & i o c l a s e a l te red t o so f t soapy yel low green.

K-spar a l t e red t o dark grey green with plnk grey a t margins o f zone.

Contact a t 52.6 i s an a l te red breccia zone.

Quartz Feldspar Porphyry-: pink; f ine- r a m q u a r t z phenos t o 0.5 cm 10% 7- l o c a l l y 20%); plagioclase phenos t o 0.5 cm

5%; very few scattered k-phenos. (Local ly quartz monzonite) composition.

P r i t e : di i i~~~ te: disseminated; rock moderate t o s t rongly magnetic.

53.2 - 69: T ight green s o f t soapy, some w i t h dark green s o f t soapy cores, sow opaque whlte medium so f t , l o c a l l y opaque white so f t except f o r zones o f both feldspar a l t e ra t l on , b l o gone, plagioclase a l te red t o sof t soapy yel low green and k-spar medium s o f t grey- green t o plnk-grey a t margin o f zones a t :

Plagioclase a l t e r i n g t o l i g h t

Granite


56.6 - 57.6, 57.9 - 58.2. 60.6 - 61.4. 63.3 - 63.6, 64.9 - 65.1, 67.6 - 68, 70.0 - 72.3.

Contact a t 68 gradational ( i n t e r v a l masked by breccia) by coarsening o f ground mass.

# . . . . I

Structurat SYMBOL C.AJDIp

SLIPS: 51.7: 40' 52.5:2 a t 40'1 50° i n a l t ' d bx

52.7: 70' i n gouge

53.7: 350 55.4: zoo 56.8:moly s l i l i n bx 45'

57.3: 60 &40° i n a1 t ' d bx

to 10 cm f l t 57.4: 450 Fw

!Pug@ 57.8:moly s l i r 25O

58.1: 45' 50.6:moly s l i p 70° HH t o bx zone il .d:moly s l i p 65 FW t o bx zone

i7.3:50°in bx zone

i7.6:blk seams L moly s l i p i n 2 f l dsp a i t ' n 6one75' i7.8:70 w i t h 10 cm fat bx. i7.9: 50 io.a:moiy s i i p 65 19.0: 00

SAMPLE No.

'ROM ro

A S S A V

T

I" . SHEET IN tERVAL Itom

MVNUI1V

POLITICAL UNIT

L-1 AODITIONAL INFO -

10 PAGE--4 _ _ OF

SHELL CANADA LIMITED - MINERALS DEPARTMENT DRILL HOLE OR SECTION DATA RECORD r n o J F c i NAME ---Cas%

FnOJECT N O - 7g 3v911 -- 9- - - - ____ --- - HOCEISEC NO _ _ ~

WORK DONE Nanm Dalsr Remmka

DI I ILLINC ___

N E

_______ FIELD LOCATION LOGGING ___

A 2 SURVEV ______

___________ ASSAYING

n&w 68 - 84.3

84.3 - 96.5

LITHOLOGV. T.xrwa. Siraclwr. Miwrdiratim ILilhnh*l

- - - T v

Quartz Monzonite ( pink-grey , meaGm1 -

porphy r i t i c ; plagioclase phenos t o 0.5 cm 1-31. quartz phenos t o 0.7 cm i n sone places, scattered k-pheno. Co o s i t i o n boarders. Grad t e i n places. T r a i n s i ze o f ground mass varies so rock changes from medium-fine-grained quartz monzonl t e margina t o quartz feldspar porphyry t o quartz feldspar porphyry with f lne-grained gm.

69 - 86: opaque white moderately s o f t t o soft, l o c a l l y hard white and l o c a l l y so f t soapy and f a i n t l y green.

genera l ly plagloclase a l te red t o

83.5 - 84.1: mlcro and macro breccia.

Contact a t 84.3 masked by breccia but I t i s gradational. t4.L. As a whole thls i n t e r v a l 60 - 84.3 more c losely resembles quartz feldspar porphyry than quartz monzonite. No s ign i f i can t d i f ference between above and below 84.3 - only s l l g h t d i f ference i n g ra in size.

Quartz Feldspar Porph-ry: pink-grey, f i ne - g r y z i g a r y t e x t i r e d ground mass quartz phenos t o 0.7 cm 5 - lo%, plagioclase phenos t o 0.5 cm 3 - 5%. few k-phenos concentrated l o c a l l y .

86 - 87.5: 87.5 - 88.5: 88.5 - 90.5: soapy l i g h t green. opaque white rims.

plagioclase opaque whlte hard. plagioclase opaque white so f t . plagioclase a l te red to s o f t

Cores w i t h s o f t

, . . . . I

Slrw1"r.l An!$. SYMBOL C . A . / W 4

SLIPS: 70.9:blk sean

i n HN a1 t 'n zone 70' 5 c bx

83.8:moly s l i i n bx zone 6

84.1: 70' FU t o bx zone

87.8:molv s l i 550

"

89.5: 55O 91.1: 40' 93.3: 30°in b

zone

SAMPLE No.

5

19 - 9 - 2c

1 9 - 9 -

19 - 9 - 21

_____ ?9 - 9 - 22

_i___

19 - 9 - 2:

FROM I N T IN F1 TO Ft,

230 - 240

As above.

250 - 260 1 As above. Bla I 260 - 270 1 As above. 75%

- iEC VER -

1 O( PYI :ouI -_ -

101 PYI __

1 O(

__ 1 O( Sei

9! I 01

-

0.01 t e vel ed. ~ __

0.05 t e vel

0.05

0.03 s not __I

0.15 vein.

33- b

.oa4 and SI

.248 , Blac __..

.07Q

____ .040

mted.

-066

.073 ars on

_. - .- .__

.414 scams

.116

E S U L - -

lips.

-

)t cou

- - SYMBOLS ANU ABBnCVlATlONS ~ SIIEET INTERVAL t r a m 10

POLI l ICAL UNIT. . . ... . ... j . . . ...... ..... ...... ....._.........

96.5 - 135.8

I- 90.5 - - 9G: t o s o n soapy. opaque white. 98.5 - 100.7: to hard. 100.7 - 110.2: plagioclase a l te red t o iii5-y s o f t t o sof t . opaque white. Short i n t e r v a l s medium hard t o hard; l o c a l l y s o r t soapy l i g h t green i n a l t e r a t i o n aureole 88.L: 20 cm micro breccfa. - 89.7 - 91.6: micro breccia. 9 3 - 9 3 . 9 3 micro breccia and macro breccia. some broken and crumbled core. 101.2: 20 cm micro breccia.

Contact a t 96.5 gradational over 1 m.

uar tz Monzoni te(margina1 t o quartz 9- e m p o r p h y r y ) : pink-grey , f fne- medium-grafned, sparcely porohyr l t tc ; pl3gioclase phenos to 0.5 cn) var iab le 1-5%; quartz g ra in s i ze grades f i ne t o coarse. no t rue phenos; a few scattered k-phenos t o 1.5 cm. some mantled. grained 3 - 5%.

Py r i t e : Mainetite-: 0.1 t o 0.5, disseminated, rock IW erate t o s t rongly magnetic.

107: s tT i1 only 1% o r less.

113: k-phenos 25% for 20 cm. From here &%in k-phenos 1 - 5%. usual ly only 1 - 2%. _.___--- 110.5 - 113: plagioclase medium hard t o hard, white t o semi-translucent.

plagioclase a l te red to so f t

plagfoclase white medium hard

___

Bto fine-medtum

about (0.1 mainly i n veins.

k-phenos become more abundant but .-

. . . . . I

I SLIPS: 13.9:30°FW o f bx zone

97.2:moly s l i p

101.2:75°in 20 cm bx zone

104:mly s l i p 25'with 10 cm

400

I bx

s l i D 85' ni th 105.8:m0ly-p~

10 cm b8

s l i p 60° 106.2:40 &moly

108.1 :blk seam &moly s l i p

108.9:moly s l i 55O HU t o bx zone

109.5 : severa 1 b l k seama& s l i p s 45 over 20 cm

I1 0.3 : 30' 110.4 : 30'

50O O0

110.7 :moJy-py

i io.9:mljy

s l i p 80 FH to bx

s l l p 45

_ _ SVMBOLS AND ABBREVIATIONS _ _ - .

.332 70% i n

.120 Black

__I_

.043 e.

. lo2

moly v

.

--

.a10

~ _-- .028 Some b ___

.047

.062 reads .._--

I" SHEET INTERVAL horn

M V H 1 V

SHELL CANADA LIMITED - MlNEflALS DEPARTMENT 6 10 PAGE-_-_ OF

DRILL HOLE OR SECTION DATA RECORD P I l O X C l NAME -

7v- ~~~ PROJECT NO

HOI ElSEC NO __ . ~. . . POLITICAL UNIT . .... ... .. .!. . .. ......._...... ... .__....._.... .

LONGITUDE WORK DONE N e m Omln Remarks

- A A

___ FIELD

SURVEY ORID

LOGGINO LOCATION

ASSAVING:- -~ E -

AOOITIONAC INFO. - - _ _ _ ~ _ _ _ _ L A N W A R K S : ____ ~

CLAlMlPERMlT NO.: LOGGEO BY:- - OTHER FEATURES:---

_ _ _ _ ~ - ~ ~ ~ ~ _ _ _ _ _________

SlruclurJ Am#* SYMBOL C A J O i p 4

LITHOLOGY. Tentwe. Strvcwre. Minsr.lltacim (Lllholql -- !lL-J-ZJ2J: s o f t soapy, opaque white. Local ly l i g h t greer.with a l i p s

108.9 - 110.7: Micro and macro breccia 14.9: 70' ; & n y w T t h e r a l black seams and s l i p s . ;15.6: 85'

116: 50 HU 01 116 - 117.8: micro and macro breccia zone. bx zone

116.4: 50' 123.2 - 125.5: plagioclase s o f t l i g h t green 117. moly s l i r t o s o f t soapy l i g h t and dark green.

117.2: 35' 125.5 - 128.2: plagioclase a l te red t o s o f t 117.4: 50' t o s o f t soapy, opaque white. Local ly l i g h t 117.5: 30' green. 117.6: moly

128.2 - 130.3: plagioclase a l te red t o s o f t 117.8:blk Sean

plagioclase a l te red to s o f t t o 113.5-113.8 b,

30-45

65d

s l i p 60'

60 .Fblof bx. and s o f t soapy very l i g h t green. & p l y s l i p

130.3 - 135.8: 129.2. 118.5: 15

plagloclase same as 125.5 to 118:'0° t8 50

119-119.1:flt NAB,: The more tntensely brecciated zones gouye ,sldps i n t h i s fine-medium gralned quartz about 45 on monzonite are l i g h t e r i n colour. a r t l y due H W 8 FW

and, i n some breccia zones, due t o the salmorll9.5:blk k-spar being s l i g h t l y a l t e red t o pa le salmon tht;eada 45;. o r greyish pink. (Could be microscoplc 85 ,10 .35 i r kaol 1 niza t ion) . macro bx

119.6: 40' 119 - 124: Intense macro breccia except 119.8: 50' =ebrecciation 119.7 - 120.4. 120:bl k tareac

i n bx 50 125.5 - 126.5: macro breccia. Some micro 120.5: 30'

121 :blk threac breccia from 124 - 125.5. i s a p l y s l i

128.8 - 129.8: Macro breccia. a t 35 121.1 :d i f f e re r

131 - 131.6: Micro breccia. sets b l k

t o the k-spar being more salmon t P, an p ink 119.2: 20'

----

-

I . ... I thl;eadsLs 1 ips 30"

SAMPLE Ho.

9 - 9 - 3 2

9 - 9 - 3 4

9 - 9 - 3 5

9 - 9 - 3 6

-

9 - 9 - 3 7

-_i-

9 - 9 - 3 8

9 - 9 - 3 9

____ 9 - 9 - 4 0

FROM INT REC Est Total A S S A Y R E S U L T S TO p t . I N F T OVERY&I

360 - 370 10 97 0.1 As above.

___ 370 - 380 10 98 0.01 As above. B lac: thr iads i n

380 - 390 I 101

1001 0.02 As above. Wac t h r ads an

t--I-- I---- --__

390 - 400 1 101 9810.05-0 Mainly as l i p s I n b ack se Black seam and t h r e ds con

I---t--t--- .-__-

400 - 410 Rs above. contal n.

410 - 420

4s above.

420 - 430 4s above. _____ . _-- .- - -

4s Y:!::lj-:: above. Oepe dent on mol:

SYMBOLS AND ABBREVIATIONS __ - __ - ._

.016 .027 seams i 1 brecc i I not comted. __-- . __ - __ -

.040 .067 IS. Depl?ndetit 0 1 how mu:h inoly i n . S o w l o s t 'rom cru.tbled c(

__ - . - _ _ - - - __ -030 .05U

iuch mol.( black ;earns a n l threat

--- --__ __ .027 .045

content black s?ams and threadq _ _ _ _

.007 .012

-~ ___ .011 .018

content, black ieanis an1 threac -- __ . _ - _ _ -

I" W E F T INTERVAL tram

POLITICAL IJNIT

ADDITIONAL INFO __

7 10 PAGE-- _ _ or--- P n o x c r NAME - Casnlo 399,T __- - - _ _ _ _ -

79 --v---- - -- --


PROJECT NO __ HOLFREC N O _ - _ _ _ _ -

WORK DONE Nmm Dam Rmwrks- _- DnlLLlNG __ - LATITUDE DEPAflTUnE ELEVATION IDATUMI BFAnlNG INCLINATION LENGTH

LOGGING ___ LOCATION FIELD

SURVEY -.

N E A 2 - ~ _ _ ASSAYING

__-- LANDMARKS _ _ _ _ ~ _- LOGGED BY OTIIER FEATURES __--.___-____ CLAIWPERMIT N O :

133.5 - 142.3: Macro breccia, l o c a l l y In tense, and micro breccia.

134 - 134.4.: E o v c . ?0 , bottom contact I s a 3 cm b i o schlieren.

D i s t i n c t l y f lner gralned, non TOP contact i s moly s l i p a t

28 : sexerah se 0 ,10 ,20 29. 3:40° 29 4:moly s l l 506 31 .3:0° 32.7 :45O

135: 30' 1 35.5 :ma 1 v

FROM INT. I N F T ro

REC. A S S A Y VERY


POLITICAL UNIT

LOGGING:

AOOlrlONAL INFO - ASSAYING. -

I I I I OEPARTUnE ELEVATION I D A T U I BEAOING INCLlNAl lON LENGlH

I E k - t

1

kw!!

135.8 142.3

2.3 4 7 . 3

147.3 158.1

1 . . , Contact i n v i c i n i t y of 135.8 obscur6ed by breccia. Contact taken as s l i p , 80 t o C . A . True contact possibly gradational.

uar tz Felds a r Por h r : pink-grey. f ine- w v & d t i c . Quartz phenos t o 0.5 cm 5%. plagioclase phenos to 0.5 cm 1 - 3%. Bio fine-medium grained 2 - 3% ( d i s t i n c t l y less than i n quartz monzonite above).

___-- 135.8 - 142,3: t o v e r y m g h t green, s o f t soapy.

Contact a t 142.3 a moly s l l p a t 75'.

Quartz Feldspar PorphLry-: grained,-arcely porphyrl t l c . Quartz phenos t o 0.5 cm 5%. plagioclase phenos t o 0.3 cm 1% o r less. l e s s than 1%.

plagioclase mainly a l te red

pink, q u i t e f lne-

Bio fine-medium grained

- Pyri te : <0.12. Rock weak t o moderately magnetic.

Contact a t 147.3 gradational over 10 cm. Dis t inc t increase i n grain s i z e and b i o content.

quartz Monzonite: pink-grey, medium-fine- grBilledlLToFpFphyr 1 t l c . Some f n terval s grade in to and out of quartz fe ldspar porphyry.

143.2 - 147.2: Macro breccia. , . . . . I

Slrwlwd A M 0 iYMnoL c.n.mg,

'LIPS: 36.2 :moly s l i p s

4 8 . ~ 0 1 ~ s l i p 50' 48.1: 20' 48.9: 75O

35O 49 4:mol sl 79' & 408

Y:moly s 1

35:m1y s1 53 : 55Oqly

56: 40

s l i p 75 55.2: aso

2'' s1

57.2: 70'

160.5: 50" ~

MWLC Ne.

FROM ro

A S S A Y

_ _ . ~ SIIEFT I N l E n V A L lvom I O

SI

_.---___ 147.2 - 151.5: i n te rva l s ofmacro breccia, micro breccia and non-breccta.

A l ternat ing 0.3 t o 1 m

Mtcro o r macro breccia a t :

152.5: 753:

rsL6: 156: s n p s 70' and 90 157.2 - 157.6.: a l t e red micro and macro 6recc i a __ 135.8 - 157.2: plagioclase a l te red t o mainl; soft soapy, very l i g h t green cores and opaque white r i m s . l o c a l l y opaque white soft, dark green i n a l t e r a t l o n envelopes. No 2 feldspar green a l t e r a t i o n zone) betweer 72 and 149 m. i n te rva l s :

10 cm, s l t p 75' t o C.Ad

10 cm a l te red gouge w i th s l i p 75'

IO cm. w i t h moly s l i p 75

20 cm alteged micro breccla with

T n . 8 - 154.5:

They occur a t the Pollowing

143: --- 749.4: 154.5: S F 20 cm between two s l tps - ~ - - - 157.2 - 159.7: plagloclase a l te red t o s o f t soapy yel low green. s o f t dark grey green, medium hard t o hard. L i g h t greyrgrean and hard gre p i n i n zonal arrangement. Most Intense a l r e r a t l o n i s adjacent t o s l i ps .

5 cm around a s l i p . 10 cm around a s l ip . 10 cm around a s l i p

k-spar a l t e red t o medium

Contact a t 158.1 masked by a l te ra t i on , but r e l i c t textures show i t i s sharp. although no c h i l l e d features I d e n t i f i a b l e .

I . . . . , I

I A I ADOITIONAL INFO


WOAK DONE Nnnr D a m Rcmsrks

DRILLING

____ LOCATION LOGGING - SURVEY

~~~- _ ~ _ _ _ _ _ _ _ _ ASSAYING

m@€tw -__

158.1 159.1

159.4 End

160.9 (528' 1

LITHOLOGY. Tcriurc. Structure. Mhmditetlon K i t h o l q l

A p l i t e dike. Contact a t 159.4 sharp. quartz monzonite a t contact.

Quartz Monzonite: same as 147.3 - 158.1.

-. 159.4 - End: green.

END

I d e n t i f i e d from r e l l c t texture No c h i l l i n g o f

plagioclase s o f t soapy l l g h t

. _-

, . . . . I

SYMBOLS AND ABBREVIATIONS .- . -. --

SAMPLE No.

9 - g - 4 9

;qt.

520 - 52E Quartz -ma Some blac

0.03

counte l l y f l l !d f rac ures a

.035 1 .05

E S U L T

s l i p s

SHEEr INTFRVAL horn I O

",


POLITICAL UNIT --___

s t Fkls7

SAMPLE No.

ROM

o Feet . S t r w t t d Angle

YMBOL C.A.IOb

Casing t o 12'.

Overburden

u a r t r MonroEi te: pink-grey, coarse-grained 9 &dTu%grane& quartz & plagioclase) k-spar po rphy r i t i c . but many not p e r t h i t i c t o hand lens many zorled j t bu t few i f any arc mantled,l - 23 cm, 20% l o c a l l y 50%. L i t t l e k-spar Inground

mass. quartz 50%. plagioclase 25%. b i o a boir t 7%.

Scattered 10 - 20 cm in te rva l s k-pheno r i ch . b i o poor, some seml-pegmatitic texture. sharp contacts. Probably l o c a l d l f f e r e n t i a t i o n pods rather than dikes. Spec. normal rock taken 4.3 p~. 14.5: 15 cm a p l i t e dike, 10 t o C.A. 16: 15 cm a p l i t e dike, 15 t o C.A.

Py r i t e : (0.12 malnly i n velns. Magnetite: moderately maqnetic.

_____- - 3.7 - 7: - hard.

7 - 14: O p q ~ e white hard t o s o f t i n a l t e r a t t o n enwlopes.

14 - 72: plagioclase same as 3.7 - 7.

K phenos pink, some p e r t h i t i c

l i g h t grey,

0.1% dlsseminated rock weak t o

plaqioclase white semi-translucent

plagioclase l i g h t green hard except

_ _ _

l i p s I fau l t s

: 10 cm brecc

.5: 10 cm reccig, s l i p

0.5: 20 cm reccla.

50

79-10- 1 12 - 20 IS quartz

(0.01 te vein -. _. - -__

0.03 teather

(0.01

.002 , Frac

. 0 3 :ures WI

I - 3.7

3.7 - 44.8

- J..

79-10- 2 20 - 30 #s above.

.021 I .

-

.003

. - - -

79-10- 3

79-10- 4

30 - 40

2 . 5 : 4 0' 40 - 50 <0.01

10.01

(0.01

co.01

-

.- - - .- .

-.

79-10- 5 50 - 60

79-10- 6 -

79-10- 7

60 - 70

70 - ao

22 - 24.5: plagioclase l i g h t green l i k e 7 - 14.

. 24.5 - _ _ - - __ 30.2: - - - - plagioclase l i t t l e a l tered, -.-I. . . . I l i k e 3.7 - 7.

SYMBOLS AND ABBREVlAlIONS . I" SHEET INTTRVAL from

PAGE '.- O F - 16. PROJECI NAME .- - .cf!sl!?.- PROJECT N O '-.~.. ~ .--.!99! HOlFlSEC N O __ _79 -. .


~. DRILL HOLE OR SECTION DATA F7ECORD

1~ ~- ~~.

0m.1 R8kmatks

~ _ _ _ _ _. . _ _ ____--_

POLITICAL UNIT

p R K DONE Nema

ORILLING:

LOGGING. ___

AS3AVING' ____ -- I I J

ADDITIONAL INFO

- NT. I F1 -

10 -_-

l o -

10 . _-

l o -_ 10 __ 10

b l i

-

DEPTH - Est. MQSL

(0.01

(0.01

otal 0

S S A V

t z p s p Struclur.( And8

iYMBOL C.A.IOb SAMPLE

No.

, 79-10- 8 ___-- 79-10- 9

. __ - __ 79-1 0-10

~ __- - - -_ 79-10-11

. - - - _ - - -_ 79- 10-1 2 .-

79-1 0-1 3

27.5 - 29: quartz monzonite w i t h very f ine-grained 'pepper' b i o (not quartz monzonite 2). a p l t t e and medium grained b i o r i c h k-spar po rp l t y r i t i qvartz monzonite; bounded top and bottom by 20 cm quartz-k-spar pegmatite. I n te rna l contacts are sharp and sgme are marked by b io schl ieren. Schl ieren 20 t o C.A. These are l a t e stage d i f f e r e n t i a t i o n phenomenon, perhaps abetted by l oca l flow, ra ther than s i g n i f i c a n t i n t r u s i v e contacts.

Between 24 and 30 m are several other 3 t o 10 cm rounded pods o f b i o r i c h non po rphy r i t i c quartz d i o r i te. some f ine-grained, others medium-gra ined. Or ig in unknown.

medium grained, non-porphyrit ic

80 - 90 .022 30.2 - 37.6: plagioclase a l te red t o l i g h t green hard. lo sl ickensidt

12: s l i g h t l y ;1 Ickensbded, ; l i p s 70 160

; l i p s 12.5-42. 90 - 100 .005 jlL6---4l.5: plagioclase l i t t l e a l t e red l i k e

3.7 - 7 m except 38.6 - 40 some opaque white hard i n zone w i t h f ractures sub p a r a l l e l core L l g h t grey b i o poor 20 cm zones a t top 6 bottom o f t h i s i n t e r v a l .

. 41 .5 - 42.8: - - plagioclase l i g h t green hard.

100 - 110 (0.01 .003 - . . ..

.002

.003 -

.002

110 - 120 .- .-

120 - 130

<0.01

co.01 ~- (0.01

42.13 - 44.9: 3.7 -77-

plagioclase l i t t l e a l t e red l i k e

130 - 140 4 4 , 8 - 47.7.: Zone o f s l l i c i f l c a t i o n s u r r o i i x g a 0.5 m quartz-k-spar pegmatite (w i th mlnor plagioclase, b i o and muscovi te) . Zone contains pure f ine-grained quartz bands, p a r t l y quartz-replaced po rphy r i t l c quartz monzonite, and f i n e t o mediimm grained b i b r i c h "quartz diorite". a l l wlth sharply

No moly v' 140'.

--

SYMBOLS AND ABRIEVIATIONS ~ .- -- .. . - S l 4 t E T INTERVAL horn I"

,: c i SHELL CANADA LIMITED - MINERALS DEPARTMENT PAGE 3 OF 16

PnoJFcT NO 79 ..--,77 DRILL HOLE OR SECTION DATA RECORD P n o m T NAME .ggx;"r:T ~ -

HOLEBEC. N O ' - Ootn Renurks -

. .~ __- I LATITUDE I DEPAflTUflE

WORK DONE Name

DRILLING,.--

LOGGINC:

ASSAVING: __. AOOITIONAL INFO

1

-- E S U L I LITHOLOGV. T e ~ t w e . Structure. Mlmellzetlon ILlthnlogl

l . . . , l

gradational boundaries. Several blebs o f coarse-grained moly in pegmatite. Contact a t 47.7 gradational.

0 PTH &res

47.7 - 50

50 - 52.3

52.3 - 217.6

.039 I .065 t i t e .

n.

-01 1

uartz Monzonite: Same as 3.7 - 44.8. cro brecciated.

100 <0.01 lebs in peg

100 (0.01 ly-p.rri t e vm

93 0.02 r i t e veins.

v f s ble mo core

-- - -

- _I_

- __ - 99 0.01

and s smeai couited. !

89 0.02 l i p s Many y CO-e in bi -- .. __I

96 0.02 noly lost .

97 <0.01 - .- -

90 (0.01 - . . . . -

98 0.01 yr i to vein.

Fault gouge and breccia. seams, threads an# s l i p s 30 to 60 to C.A. Main H . W . s l i p 50 , Main F.W. s l l p 50'.

@ a r t z Monzonite: pink grey, mediiwn-grained k spar p o r p x y a i c . Pink, c lear ly pe r th l t i c (perhaps due to a1 te ra t ion of plagioclase) k phenos 0.5 - 2 cm 10% ( loca l ly more); flne-medfum-grained blo 5 - 10% uartz

ahout 25%.

- Pyri te : _. Mtiy$I&: 0.1 t o 0.516 disseminitted rock, med um mag.

44.9 - 60: g?>Gi-diun, hard t o dark green so f t soapy; local ly some plagioclase opaque white medium so f t .

- 52.3 - 59: adjacent s l i p s a t 55 - 55.5. 57 - 57.3,

Nlprousoblack clay

nmrizonite k spar, plagioclase an 1 quartz each

about 0.1%, mainly in velns.

plagioclase a l te red to l i gh t

nilcrobreccia with macrobreccia

57.9 - 58.4.

____

ile i s ia t e r i i

13.2: 40' 13.4: 80' 15.7: 40' 18.3: 40°,

minor n j ly . 18.5: 45

- micro breccl i n H.W. of f aul t zone,,

19.4: 5O, 40 IO - 52.3: man l i p s 18 f au l t one 30 to 60

18.5 - 50:

12.5: nOly S l l 70'

3.1: molv

79-10-16 160 - 170 10 Quartz-mol:' f I material v t h I l o s t in cri nhlj

-I-__ .-

79-10-17 170 - 180 10 I n quartz yein! clayey searts nc

79-10-18 180 - 190 10 Mainly a s ly counted. rum1

79-10-19 190 - 200 1:; --_-_ __-_ ~

As above. .029 I -048

-__

J I

79-10-21 (210 - 220 I 10 zones between.

79-10-22 I220 - 230 4 10 As quar t z - oly- , . . . . I I

S W E T I N l E R V A l born I"

U V N M Z V

L - d . - L ADOITIONAL INFO

WORK DONE Nms

OR11 LING,

- LOQGINQ..

-- ASSAYINQ.

-- DEPTH letres

65: k-phenos over 1 cm become rare. Some 55.1: 70' jntervals below 65 are sparcely porphyritic. 56: 40°, mol8

sltps 25'860 . - 71: gratn size decreases slightly, malnly due 56.1: 50 to decrease In number of 0.5 cm quartz gralns.57.3:

sltp 40 . Breccia zones at: 57.5 : bJac k

slips 58 . . 63.5 . - 63.9: broken missing core, 58: 50

- 64.1) -. - _-- - 66.7: some anhydrite filled fractures sllp 30 . sub-parallel core broken and crumbly core, 58.6: 15:

59: 300,55 67,_0: 18 cm fault breccia adjacent sllp 59.8:60 ,,2O0. about 45 to C.A. 60.3: 85 .

67: 45 , 10 c - 70.R: fault bre6cia.

70.8: 30 . 2

p l y

58.3: p l y

some lost. 58.7: 80

2 cm fault breccia, s l l p about 30'.

71 - 71.8: Fault breccla and gouge, black s l i p s 70 .

cm faulh brecc 171: 70 H.W.

- o f gouge

f gouge. 72.6: ",ao.

86.4: 50-

.I---.- 62 - 64.5: plagtoclase translucent whtte to 71.5: 60' F.W very p a E green, hard.

64.5 - 67.1: opaque wmte, some medlum hard.

most plagioclase altered to soft 76.5: oo: ..__-

Zone of anhydrite fractures. 0".

67.1 - 70.5: plagioclase mafnly whlte medium 86.5: 30", hard- to hard. 1F.H. sltp fir - _L-

70.5 -_L2.7: plagioclase malnly light green

72.7 - 91.5: plagioclase translucent white h a d to opaque white medium hard and, locally soft. Locally soft light-dark green In k-spar

medlwnsox to soft.

alteration envelopes.

__

MWLE FROM TO Feet

79-10-23 230 - 240 Dlack seal

---__ -

79-10-24 240 - 250 --I__ _ _ _ - 79-10-25 250 - 260

__ 79-10-26 260 - 270

As quartz -_1-- __I__- -

79-10-27 270 - 280 ______ - 79-10-28 280 - 290

~-

79-10-29 290 - 300 4s quartz- _I__

SYMBOLS AND ABBREVIATIONS - ~ - - . I" W E F T INTERVAL Itom

HVNW'JV

PAGE.-- 5 _.__OF 16 SHELL CANADA LlMlTED - MINERALS DEPARTMENT DRILL HOLE OR SECTION DATA RECORD PROECT NAME -._ clsmo -

39917 -- -~ PROECT N O _- 79.: ,u -_ _- -- HOLElSEC N O __

~~ N E

- 0.1- flcnurks

___ LATITUDE DEPARTURE ELEVATION I O A I U M ) BEARING FIELD LOCATION

QUI0

_ _

A2 sunwv

WOflK DONE Nom

D A I L L I N G ~ ___

LOGCINO~

ASSAYING. L------ AODlTlONAL INFO

- REC IVE I -

9 te -_

7 sa

8 -.

7 r r i -

9' - 101 ir i

-

-I

E S U L l -- Est. Total A S S A Y T3OM INT. ro Feet . . INFT

00 - 310 10 uartz-mol: -pyr ____ 10 - 320 10 ore crumb' ed t

__ 20 - 330 10

SAMPLE No.

78 -82.3,: W i t h a n G d r i t e f i l l e d f ractures 0 - 10 t.0 C.A.

opaque white sof t I n sectign

I 91.5 - 95.4: green.

opaque white soft, some l i g h t

06.5 - 86.9: fault macrobreccia, F.W. s l i p 85 . P ____

79-10-30

92.5 - g-: mgcrobreccia and microbreccia with1 - 20 t o C.A. 50% o f core i s crumbled o r badly broken. t h i s f a u l t zone on ly about lm.

95.4 - 99.3.: plagioclase mainly a l t e red t o s o f t l i g h t green t o s o f t soapy dark green.

_-_ 99.3 - - 105.8: plagioclase a l te red t o l i g h t green, h-to medium so f t .

True thickness o f

.024 ! l o s t

.013

__

1 m. -- - -

.016 __.__

.014

.mu -

.019

-

.040 0.01 n. Sc

O0 15'

8.2: 30' 103.9: 30'

If breccla zor 04.1: 30'

80' 04.2: 50'

80' 03.3: cogjugat 5 6 5 5 04.5: 55'

104: 55 , 1 l . W ~ P 104 - 104.5: faul t zone macrobreccla. ~ u ~ - ~ 5 5 ° t o C.A. 79-10-31 10.01

96 t o

qo.01

.022

.027

105.8 - 110.9: translucent; l o c a l l y opaque white medlwn hard.

110.9 - _-_-- 111.5: plagioclase a l te red t o l i g h t green, medlum hard - so f t .

-- 111.5 - 119: 2-feldspar a l t e ra t i on , b i o gone except mym a t 115 and 30 cm a t 116.5 m. Several adjacent i n te rva l s of zoned a1 te ra t i o r comprising k-spar a1 tered progressively from hard grey pink t o s o f t l i g h t grey t o so f t grey-green. Corresponding plagioclase a l t e r a t i o n i s s o f t soapy throughout but changing colour from dark green t o l i g h t grey

d m u i v a l e n t t o yel low green i n other hol

plagioclase ma1nly hard

79- 10- 32

-_I--- 79-10-33 0.01

vein.

10.01

0.02 vel ns .

.W. of brecci

5 )

79-10-34

I---

79-10-35 .032

I - S W F T INTERVAL lvom I" -. .

M V P W l V

6 16 WELL CANADA LIMITED - MINERALS DEPARTMENT

DRILL HOLE OR SECTION DATA RECORD PAGE ~- .- ~

PROJECT NAME ---($$; .- __ - ._ _ ~ _

IIOLEISEC. N O . . - ~. ..

OF ___ ._

r R o K c T NO:.- 7~~~--Tu- -

Oacu Remmhc

LATITUDE DEPARTURE ELEVATION IDAlUMt .~ ---_I_____

N E

FIELO LOCA r l O N SURVEY GRID

~ _ _ _ _ _ _ _ _ _ 1 _ _ - ~

AZ.

WORK W N E Name

DRILLING: .

LOGGING.

-_I_ -_ ASSAYING.

I I I AOOlTlONAL INFO ~-

- PEC. VER -

10 vi no

lo(

__ 1 O( os 1 --

I OI PJ

9t

I_

'ROM

ro Feet 1.ITHOLOGY. Tsitar., Slruclure. M l n s r o l l ~ ~ t l m I L l i ho l~~ l S l r u c l ~ ~ a l A 4 6

SYMBOL C.A./MI, V I . , . , . ,

t o dark green again I n inner zone.

This a l t e r a t i o n superimposed on numerous quartz-muscovt te-k spar a l t e r a t i o n bands.

Much o f t h l s I n t e r v a l i s also a f a u l t breccia 111.7: quart, and microbreccia. The brecc lat lon occurred vefn L p l y --I_ before the a l t e r a t l o n (because s o f t gralns s l i 70 - H.1 would not f racture) . Several undisturbed of [reccla. quartz-moly-pyri te veins I n breccia, p a r a l l e l s l i ps , but also some s l i p s w i t h moly smears. 117*8: quart' Implied sequence i s n ine ra l t za t ton - veJn L moly s1

brecc i a. brecctat ion-a l terat ion. 50 - F.W. O f

W C C wo.

.084 nd mol

79- 10-36 r60 - 370 \s quartz iome b l ac -_I__

170 - 380 is above. --l__

180 - 390 IS above. -- .

90 - 400 n quartz. -___ 00 - 410 v above. ~ _ _

0.01 veins

:ounte - ___

0.02

.140 mea r s

- _ _ -_

,120 79-10-37

79- IO- 38

79- IO- 39

.072

.018

--

.032 L .

.021

0.1 .030 117.7 - 118.2: replacement quartz, 20% coarse p y r i t e , 20% p a r t l y replaced a l te red host. Moly i n quartz.

60% quartz as veins and 112.5: 40' I H.W. of breccl 113.8: 40' 113.9: 50' 115.2: 60' 115.3: SO0 115.8: black seam 45

0.01 t e ve ---

0.01

.053 119 - 134.5-: p l a ioclase a l te red t o l i g h t g - m t o medym green medium hard, except sof t dark green I n k spar a l t e r a t l o n bands. 19-10-40 .035

116.8: doo o f breccia.

111.7 - 111.8: f a u l t breccia H.W. s l l p 70' 117: 70 H.w. F . W . m 50 . I -.--

112.5 - 114.7: macrobreccla and mlcrobreccla. 117*5: 6oo 117.6: 80' 118.7: 70' 118.8: 85' . 115.3 - 116.1: mlcrobreccta.

117 - 117.7: macrobreccla and mfcrobreccla. 122*9: noly sldp L brecclz 122.9: 10 cm f a u l t breccla. s l i p 40'. 40 .

124.5: 70' 134.5 - 137.5: plagioclase a l te red t o opaque 125.6: 50' w h i G K r X - 127.7: 70'

128.R: 70'

___ _ _

-- -_ .

I . . . . 1 2 cm b r P c c L g

SYMBOLS AND ARRREVIATIONS . __ - - -

WORK DONE Nan*

ORILLING.

--- LOGGING.

--- __ ASSAYING:

7 SHELL CANADA LIMITED - MINERALS DEPARTMENT

DRILL HOLE OR SECTION DATA RECORD PAfiF- -~ - OF 1 6 - PROJECT NAME ___ <!?F PROJFCT NO - 3991 T HOLEISEC NO .-_ - _- -

__ __ ._ ,~ ,~ - _ - - _- _ _ _

I____-___

N E

0.10 RctwrCs

L A I I T U D E DEPARfUAE ELEVATION I D A l V H l BEARING - FIELD

-- - LOCATION SUnVEY GRID A 2

-_I

F.W. o f brecc i i

_- 139.6 - 142,; plagioclase a l te red t o l i g h t 130.5: 5' gre-um hard. 130.6: 50'

I i x . 2 : so0 1 142.3 - 150:

137.5 - 138.4:

w h T s w t o medium sof t .

150 - 152: plagioclase a l te red t o l i g h t green medium hard t o s o f t .

f i f te%Xum hard to sof t .

plagioclase a l te red t o opaque

breccia zone w i t h several s l ip

1 5 _ 2 ~ 155.2: Plagioclase a l te red t o opaque

-

I 138: 60' 138.4: 50'

1311.7: 45'

-I--.- 155.2 - 156.2: l i g h t - dark green medium hard t o s o f t i n several adjacent k-spar a1 t e r a t i o n bands.

plagioclase a l te red t o of brecci

__ 156.2 - ._ 166.4: .. - - plagioclase translucent, hard 146: 35" t o opaque wh7te hard, l o c a l l y so f t . 151.3: 55'

159,3 - 153.7: breccia zone w i t h several s1ip,51.5:

166.4 - 167: .?-feldspar a l t e r a t i o n zoned abou151.7: 40' a - g G b m i c r o b r e c c l a zone. From center out 151 -8:

70' plagioclase a l te red t o sof t soapy yel low green, k-spar grey green, b f o gone; plagioclase black segm 4 5 ~ a l te red t o s o f t soapy pale green, k-spar grey 152. 15 , 4 5 ~ pink, b i o gone; plagioclase a l te red t o so f t 153; 400 soapy dark green, k-spar and b i o unaffected.

153.2: 20' 167 - 170.6: plagioclase a l te red to l i g h t 153.7: so^ =-to l o c a l l y s o f t soapy dark green inrF.". of brecc, k-spar a l t e r a t l o n bands.

I1.W. o f brecci;

> . . I . . . . 1

SAMPLE No.

79-10-41

--I___

79- 10-42

I_____.

79-10-43

79-10-44

_I__

79-10-45

79- 10-46

--- 79- 10-47

79-10-48

79-1 0-49

410 - 420

As quartz- o l y I 10 1 1 0 1

0.06

pyr t e vet 0 0.1

-II__ -- -- -- ----_ _ _ 420 - 430 10 100 0.01 As above.

-- _-I___

430 - 440 10 1OC 0.01 As above.

-- -- 440 - 450 10 100 0.01 As above. NumePous luartz-1

I___

450 - 460 10 1OC 0.03 As above a id as smears i n bl black c lay - qu r r t z ieams nc

- -

460 - 470 10 90 0.35 952 t n one quar :z vein. ----- -- -- -_- - -I _ _ _ 470 - 480 10 100 0.2 ?uartr-mol ve i i s . 30% as c nuscovi te- :-spa - a1 t v a t i o n - __I-- -_- __ __ 480 - 490 10 1OC 0.01 Quartr-mol:r _t p t r i t e veins. Numerous q ra r t r - p y r i :e vein! _I--- -. -- -- - -

490 - 500 10 92 0.02 AS above. Nume-ous i a r ren c Black seam; i n w-eccla zone

- 1

.013 .022

---_-- ~

.011 .018

._ __ .007 .017 ' l t e velns but not w i

.046 .077 :k seam;. 1 - 2 cm counte $.

- - - - _ -

-I_ -

.232 .387

.089 .148 rse blzbs i n a 30 cm d. Sone l o s t .

.013 .022

,ut w i t $ l i t t l e moly.

-

-_-__ - .- .- -- . - ____ -

.020 .033 i r t z - p y r i t e veins. 1 t coup !ed.

- - - -_ - . - -- - SYMBOLS AND ABBREVIATIONS - - - I" . SHFET IN lERVAC

LLU AODITIONAL INFO,

WORK OONE Name

DRILLING.---

LOGGING:

__I_.__

ASSAYING;

170.6 - 171.9: both feldspar a l t e r a t i o n zone a 6 3 u F G w a n d breccia as 166.4 - 167.

_- 171.9 - 173.3,: green hard. l o c a l l y s o f t I n k-spar a l t e r a t i o n bands and i n breccia.

173.3 - 174,A: p lag ioc lase a l te red t o opaque vh7t~wi&fhm hard.

174.5 - 176.5: plagioclase a l te red t o s o f t 169.7: 70'

soapy a t h green cores and white rims. 171.3: 10 cm w i t h several

- 176.5 - 177.2: plagioclase a l te red t o l i g h t black seams 6C 172.4: 75' green h a r r

f s d s o a r aTterat ion around a Quartz ve in and 30


-I- --L

177.2 - 178.4: 3 adjacent zones of both 17d: mO1y S l i F - -c

Nd 153.9: 50' 166.6: 10 cm f a u l t breccia, H.W. 1 F,,W. s l i p s 60 . 168.9: p l y s l i p 50 , 20 cm breccia.

2 s l i p s w i t h breccia.

__ -. 175: 400, tw 171 - 171.8: macrobreccia and microbreccia zone w n f i e v e r a l black seams.

177.3 - 178.3: micro and macrobreccia. A 185-b76: sever qi iartz-moly-pyri te ve in c l e a r l y broken by 0 -5 wlth brecc iat ion. However, adjacent s o f t a1 tered breccia.

177.6: 50' plagioclase i s not defonned, suggesting a1 te ra t i on occurred a f t e r brecc iat ion. other hand a l te red plagioclase 1s sl ickenslded 178.2: 55'

cn s l l p s . 179: 25' 178.4 - 186: plaqioclase a l te red t o mainly 180.5: 25' I l g h w e F n medium hard t o medium soft, some greyer very pale green hard, some s o f t dark green i n k-spar a l t e r a t i o n bands.

186:

174.8: 45'

a t 70'.

__..I---

On

181 3 " 8 l Y slil; 4o . 181.6: 60' or

k-spar a l t e r a t 5 cm b f o r i c h rock i n H.W. o f a l t e r a t i o n molY-qUartZ- ---

zone. I . . . . l Ivein.

POLl l lCAL UNIT. . ... . . ... .. .. .. ....... ......... _.......__...

ADDITIONAL INFO :-

WOnK OONE Nm*

DRILLING:----

-.

LOGGING.

______ ASSAYING:

9 16 FAGF-- _ --or--- SHELL CANADA LIMITED - MINERALS DEPARTMENT

DRILL HOLE OR SECTION DATA RECORD PROJECT NAME - <a?-- __ __ 3991 r PROJECT NO

- 7~ - I~ HOLF/!XC NO __ - -

__- - Dam Remarks

-____- l__l

__- ______

LATITUDE DEPARTURE ELEVATION I O A l U M )

N E

ClELO LOCATION SURVEY OR10

- A2

I

FOAL UNIT _.

-- 186 - 186.8: z o n & J K d s l i p w i t h black seam and b recc ia - l i ke 166.4 - 167.

186.8 - l8S,q: green rnedium s o f t t o s o f t .

_ _ 188.6 - 189.6-: g o n e . T a r o u n d s l Ip a t 188.9.

.---- 189.6 - 193: green medium hard t o s o f t soapy dark green i n nunierous k-spar a1 t e r a t l o n bands.

123 - 197.5: plagtoclase hard translucent n h j t e t o opaque white except l f g h t green hard i n k-spar a l t e r a t i o n bands.

both feldspar altered, b l o gone,

plagfoclase a l te red t o l i g h t

both feldspar a1 terat lon, b i o

plagioclase a l te red t o l l g h t

185.5: 70' 185.7: 85' 186.2: H.W. SI i p onoblack seam 60 , 10 (

breccia,, F.W. s l i p 60 . 186.7: 50'. 10 cm breccia.

187.5: 70'

188.9: b lack seams 40 , H.L 10 cm breccia 65'.

189: 50'. F . k 197.5 --. - 206.5.: plagioclase a l t e r e d t o l f g h t o f breccia. green h a r d o s o f t soapy dark green i n k-spar 189.6: blach

seam s l i p 80 . a1 t e r a t i o n bands.

206.5 - 217.6: plagioclase a l te red t o medium 190.2: 55' ?nmt green t o s o f t soapy dark green I n 190.8: sl Ip o~

quartz p l y k-spar a1 te ra t i on bands. ve in 45 . 189 - 218: average about 202 o f rock af fected

Fy-k'+r f muscovite and quartz a l t e r a t i o n 192.5: s l i p 06 bands. Some o f these quartz velns ca r ry black seam 60

molybdenum and/or p y r i t e . 197.7: moly

breccia 60 . Breccia zones w i t h s l i p s :

198: moly s l i p

s l i p & Il.W* of

197 - 198, with both feldspar altered, b i o gone. & F.W. o f 198.5: 10 cm, wlth both feldspar breccia 55'. altered. b i o gone. 200.8:

uuL-

10 cm. w i t h both feldspar

M W L t No.

79-10-58

I-

79-10-59

79-10-60

- - 79-10-61

79-10-62

79-10-63

--_._I

79-10-64

79-10-65

79-10-66

IN FT. FROM.. . . . I N ~ . R E ~ . E s t .

"VERY Total A S S A Y - - n E s u L

TO. F t ~ t ... Mb7 7

580 - 590 10 97 0.05 - -032 .053

As quartz-noly t py. l black seam! and thre,id --I- _. .- -_ -

590 - 600 10 100 0.02 .014 .023 quartz-molj f p y i t e veins.

__ -- I_ __ __ .--I_. I__

600 - 610 10 100 0.05 .015 .025 Most I n on qua t z - d l y vein -.I_ _-___..-__-_-_--_-I.

610 - 620 10 86 0.01 t I .023 .038 0.1 deiending iln moly

620 - 630 10 100 0.05+ .012 .020 quartz-mol) _t p : r i t e velns. Several black !

. .- __ - - -_ . -.I_-.. - - - - - . -

_-_I__ _____ ._I__-_ 630 - 640 10 100 q0.01 -004 .007 Black seam not ountcpd.

- ___ ___ _ _

640 - 650 10 97 0.15 -068 . l l 3 I n quartz-noly f py 4 t e vei s.

__ . __I-_. ._.

650 - 660 10 95 0.02 -017 .028 4s above.

~ ~ . . ..

660 - 670 10 100 0.02 .022 .037 I n qua r t z - r y r i t c vetiis and a', smears on sllF threads i n breccia nv t countlld.

n blac ips i n

--

-

n blac __

ams no I -..

_-

_ - - -.

. B l a

SIRET I N l € I I V A L Itam I"

POLITICAL UNIT

L A I I ADDITIONAL INFO

CLAlM/l'ERMIT N O

10 r m - _ - _ _ O F 16 SHELL CANADA LIMITED - MINERALS DEPARTMENT

PAOJECT NAME _.-_Gsmo-- PROJECT N O _- - - ~ ~ -7(T 8IOLEISEC N O ___ - -_

J991T _ _ - _ ..


- _ _

-__- . WORK OONE N o m O a t n Ramarks

LATITUDE FIELO LOCATION SURVEY

-~ DRILLING ___ -

LOGGING~ ~_.__

_ _ _ _ ASSAY ING

OEPARlUnE ELEVATION IOATUMI BEARING INCLlNArlON LENGTH 4 Slrututr l Ample

SYMBOL C.A./W 4 LITHOLOGY. Taxturs. Struturs. Mlnr.lirmtlon ILitholnel

I , . . . ,

201-202: macrobreccla bounded by 198.5: with 11 nicrobrecci a. cm breccia 80 207 - 219.4: microbreccia with sllps moly 202.5 - 202.7: gouge and nicrobreccla.

cm breccia 60' macrobreccia at 207.7, 207.9. 208.6,

(10 cm both feldspar altered and blo g0neLt.W. o f brecci 215.1, 215.3. 215.6. 216. 216.3.

andsli; ifth 210.2 - 210.7, 210.9, 211.3, 211.9, 212.7, 213.1 to 213.3. 213.9, 214.5 201.2: 75O.

202.3: 30'. 201.6: black s e p (gouge) 60 . 202.5: 40' 6 ! congruent.

202.6: 80'

203.1: 70' 203.3: 70'

204: q l y s l l p 70 . 204.6: 20' 205: slip on quartz-ply vein 70 . 205.7: slip c quartz -moly- pyrite vein 7( 207: slip on quartz-gyri te efn 70 .

;07.2: SO0 207.7: 45' 207.9: 55' 208.4: 50'

217 - 217.5.

202.8: 80'

M W r L E No.

79-10-67

ROY

o Feet

70 - 680 5 above,

- - _ _ _ SYMBOLS AND ABBREVIATIONS . _ _ _

- REC- VE R' -

98 ve i I

Total A S S A Y

T 0.02

,. .029 .OM

E S U L l

... SIIEET INTERVAL horn I"

UVNIMSV

L- ADOI I IONAL INFO.

11 SHELL CANADA LIMITED - MINERALS DEPARTMENT PAGE - - OF._1_6_

DRILL HOLE OR SECTION DATA RECORD PROJECr NAME. -..~:;$f . ~

PIIOJECT N O ' ---, ~ I..,u _.. - __-_

14OLEISEC. NO: __ - - ._

- WORK DONE Nime Oslo Remarks

DRILLING: L A T I T U M DEPARTUIIE E L E V A l l O N I D A I U M I BEARING

N E

FIELD LOCATION SURVEY GRID

. -_ LOGGING:

ASSAYING: A2 __-.

-

8m!!

217.6 . 2 28

--

SYMBOL C.A./OIp

Contact a t 217.6 masked by 10 cm both feldspar a l t e r a t i o n , cm 50 .

208.66 3 i n 1

208.7: moly s l Quartz Monzonl te.: pink-grey, var iab le texture near contact as follows: - grained p lag ioc lase (to 3 m 4%) porphyry; s im i l a r t o quartz feldspar porphyry but f o r lack of phenos.

Within 20 cm o f contact q u i t e f i ne -

I 210.3: H . I . o breccia 50 . 210.4: -black

- Grades through 50 cm quartz (302) - seam 7sU. plagioclase (20%) - k spar (20%) 210.5: F.1 . porphy r i t i c quartz monzonite with fine-medium breccia 70 grained matr ix , a l l phenos under 1 cm to: 210*7:

gouge L brecc i - pink grey, medium-coarse-grained 60".

w i t h some f i n e grained quartz and k-spar I n 22;;::; $* sparsely k spar po rphy r i t l c quartz monzonite

ma tr I x . 220: k phenos t o 2 cm become abundant. 213.1: 40°, 2

w l t h breccba. 212.9: 60

cm gouge. - __ 21 3 I 2 : 45"

:~3c~.brf9ia' 213:7; 6oo 213.8: 45' 214.3: 60'

220 - 228: l o c a l l y 502 and up t o 3 cm as a t 225 f o r 20 cm. Grain s ize varies between medium-coarse and medium, general ly w i t h a small component o f quartz 0.7 t o 2.0 nnn i n m a t r i x .

k phenos range from 10 - 252,

214.5: 60' 215.1: 55' 215.4: 35'

217.6 - 219.4: opaque w W t t e ,


215.5: 80' 216: 50 , I 5 cm breccia.

- 219.4 .---___-I - 220.4: - translucent.

plagioclase mainly hard

220.4 - 225.3: -_ plagioclase a l te red t o l l g h t 21&.3: 35" a green hard exce t f o r zone both feldspar In bre6cia a l te red and no E i o next t o s l i p and breccia 216.7: 30 221.6 - 221.9.

IN1 SAMPLE FROM

No 10 Feet

79-10-68 680 - 690 10 As above.

. - - .- 79-10-69 690 - 700 10

___ --_-

79-10-70 700 - 710 10 l u a r t z mol^ _+ p

~ -_ -____ 79-10-71 710 - 720 10

Rs above. ---- -_ 79-10-72 720 - 730 10

As above. .---I___ --

79-10-73 730 - 740 10 As above. Seve

----I_ . __ - 79-10-74 740 - 750 10

As above. -

0.03

0.01

0.04 'eins.

-

0.04

0.03

-I--.

0.02 ick sea

0.07

.036

-033 h e b l

.038

.037

--

-020 ).

.040

SYMBOLS AND ABBRFVIATIONS

POLITICAL UNIT --- AOOITIONAL INFO

SHELL CANADA LIMITED - MINERALS DEPARTMENT 12 16 PAGE-- _ _ _ F- PROJECT NAME -

PROJECT NO _ _ - HOLE/SfC NO . _- _ _

DRILL HOLE OR SECTION DATA RECORD 3wir-- - - - - -

~~ ~,~ - __ WORK DONE N a m 0.1- A m u r l l i

DRILLING ___ -

~ _ _

- FIELO LOCATION SURVEY GRlO

LOGOING _____ -

ASSAYING N __ - -

_ _ _ ~

228 - 233

233 - 255.2

225.3 - 226.1: gone.

- 226.1 - 230.7: green hard.

Contact a t 228 masked by k-spar a l t e r a t i o n band but appears gradat ional .

t u a r t z Monzonite: pink-grey, medium-fine- grained,k-sF-porphyrlt ic . No k-phenos within 1 m of contact. Normally k phenos to 2 cm 152.

229.8:

Coetact ( a t 2337) appears to be a s l i p a t 40 t o C.A. . but i s masked by breccia and a1 tc ra t ion .

Original character obscurred by brecciation and a l te ra t ion . Appears to be gEar&-Monzonite.: l i g h t pink white due t o low b ioGome l o s t by a l t e r a t i o n ) and abundant salmon k-spar; medium-grained but bordering on fine-grained i n places and contalning smaller rounded (euhedral) quartz grains; sparsely t o moderately quartz and k-spar porphyrit ic. quartz phenos t o 0.8 cm yenerally less than 10% but loca l ly 25%. K-phenos t o 1.5 cm 1% to 10%; bio Redim- grained 3%.

230.8 - 256: microbreccia; moderately t o 1 Y t . y - a e v e l o p e d w i t h s l l p s , gouge and macrobreccia. Both feldspar comnonly al tered. k-spar salmon pink - k fe l dspa t h i za t ion?

both feldspar a l te red , bio


10 cm w i t h k-phenos t o 3 cm 50%.

216.9: 45'865' 218.8: 30 219.4: p l y s l i p 60 . 221..5: moly s l i p & H.W. 0 1 20 cm by 70'. 221.7: F . U . (

breccia 50 . 224: 60 224.1: 70' 224.8: 60' 225.6: 80" 225.8: 50°, 20 cm breccia 230.8: s l i p 01 black seam 60 230.9: moly s l i p onoblack seam 80 . 231: q l y s l i p 40 . 231.2: p l y s l i p 40 . 231.8: moly s l i p i n black seam 60'. 232.1: moly s l i p I n black seam 40'. 232.7: several black seams, some moly 60'. 233.5: p l y o s l l p s 20 &85 I

233.9: moly

234.5: moly s l i p 40'.

s l i p 55O.

M W L C No.

FROM

ro Feet ---a - -Y s t . I I E S U L T

- - . - -__ .____ SYMBOLS AND ABBREVIATIONS .. SIIFET INTERVAL Irnm I O

MVHWlV

~ ~~

ADDITIONAL INFO

Slrwtur.) Angle SVMIIOL C.AlDlp1

234.6: p l y s l i p 70 . 234.9: p l y s l i p 70 . 235.1: p l y s l i p 50 . s l i p 60 . many black seam 50 -70 , scnne w i t h

235.4: p l y

235.5-237,

moly s l ips6 237.7: 38 237.9: 50 ,30 23$.1: 60' 6 30 congruent 238.2: p l y s l i p 65 . 238.5: 40'.

239.1: 35'.

240.1: p l y s l i p 40 . 240.3: p l y s l i p 25 . 240.4: p l y s l i p 50 . 240.5: p l y

239: oo. 239.8: p l y s l i p 4 5 .

s l i p 50 . 242: q y s l l p 35 . 242.5: p l y s l i p 50 . 243: 25'. 243.5: &lack s e a m 5 0 .

13 16 PAGE _____ OF __ - PROJECT NO n o L E m c NO ~lijl--16 ______I


DRILL HOLE OR SECTION DATA RECORD PROJECT NAME -c??E 3991 I

WORK W N E Nrme 011s , flcnurks

ORICLINO

LOCATION FIELO

SURVEY LOGGING

ASSAVINO GRID A 2

LANDMARKS --___

OTHER FEATURES, - ~ _ _ _ I _ - _ - ~ -

__ LOGGED IIV. CLAlMlPERMlT N O . -

_-__-___I__

I_-_

Z301_7 - 231.3: gone, zoned about s l i p and gouge.

---_- 231.3 - 235.5: t o sof t soapy, l i g h t t o dark green; k-spar general ly medium hard t o medlum s o f t and som i s greyish pink.

Short i n te rva l s o f both feldspar a l t e red and b i o one a t : 232.9 (20 cm). 234 (20 cm). 235 740 cn).

23S15 - 236.9: bfi gone. contorted lenses and pods, i . e . i f black c l a j i s gouge there have been 2 o r more periods of movenen t . 236.9 - 248.6: same a l t e r a t i o n as 231.3 t o 235.5. a l t e red and b i o gone a t 240 (20 cm), 214 (50 cm), 245.2 (60 cm k spar a l t e red t o pink grey) 247.2 (30 cm).

- 248.6 -__ - 252: both feldspar altered, blo gone 248.6 - 250: k spar a l t e red t o mediun s o f t grey green. 250-252: pink grey.

252 - 253: &%--green k-spar a1 tered medium hard grey pink bio present.

~ 253 - _ _ __ - _I_ 259.4: gone. 253 - 256.8: k-spar a l t e r e d t o grey green. 256.8 - 259.4: k-spar a l t e red to pink grey.

both feldspar altered, bio


both feldspar a l t e red green, I fherous black c lay seams and

_--__-I_

Short i n t e r v a l s of both feldspar

k spar a l t e red t o medium s o f t

plagfoclase q l te red t o s o f t soapj

both feldspar a l tered, bio

I . . . . ,

SAWLE

s quartz- nastamosi ome black

79-10-76 P O - 770 s above.

not counte

s above.

s above.

79-10-80 800 - 810 As above. I

- INT. N Fl

10 1Y ha

lay

lo 1 ac

1

-

IO 3 C __ I O

__ 10 bla

I

10 ssa -

- REC VE A

1 oc PYr l f r ean

1 oc cla the

I

1 oa b l a -.

90

--_

9! SC

__ U(

del -

-_ - - - -_ - 0.074 .055 I .092

seains nd many h a i r l i n are l y s l i p this i

0.05+ on mo .073

0.02+ dependi g on ma IS. I .035 f .058

0.03tb .039 I .065 ids on I l y con ent o f

Ips an

-- -- -.

black a h igh

i n b l

i n ha

I i n ha

lack se

as

ireads irade 1

k c l a j

-

- - __. -

l f n e t

SVMBOLS AND A R R ~ E V I A T I M J S ~. __

POLITICAL UNIT: ...... ...... ... 1 . . ............................ ...._..,. . LONGITUDE

i :- ADDITIONAL INFO.:-

(

PAGE -...14-~....-OC --16-- SHELL CANADA LIMITED - MINERALS DEPARTMENT

PROJECT NAME.--.C~~SOK)--_

PROJECT N O -399.1 HOLEKEC. NO: --..;%:-LO ___


W R K DONE Nula Oain Remrks

DRILLIN0.- LATITUDE DEPARTURE ELEVATION (DATUM1 BEARING INCLINATION LENGTI I _ _ _ _ ~ FIELD LOCATION SURVFY ORlD

~- LOGOING: __ N E A l . ~-

ASSAYING : --

43.7: 40'. a T t e r m n t B i o present, plagioclase a l t e r e d t o sof t soapy l i g h t green, k-spar a l t e r e d t o

- - 259.4 - 259.6:

grqy pink.

marglnal zone t o above

m macrobreccii

I . . . . I

seam 3OU. 247.2: 30'

247.6: 50 247.7: loo

247.4: 10;

248.8: &lack seam 50 249.6: 50' I

- SYMDOLS AND ABIRFVIATIONJ -~ ~ . ~ . ~

~~

A S S A Y I 7-

E S U L T S -

IO - SHEEl INTERVAL from

MvlrmYV

L- AOOITIONAL INFO

15 16 PAGE - _ O F

PROJECT NAME ._ -ca%v- PROJECT NO . ___ 2 9 c __ H O L E M C NO - -79 1 lo-- ____


___- __ WORK DONE Nmm Oatn RSmuLs

ORILLING

- FIELD ~ _ _ _ _ I _

LOCATION SURVEY

LOGGING ~

ASSAYING GRID

EVA!

255.2 End

Contact a t 255.2 based on r e l i c t texture i n a1 tered zone.

guartz-felds a r Por h x: pink, f ine-grainel sparsely quaFtz <d$ fag ioc lase po rphy r l t l c . Plagioclase phenos t o 0.5 cm 1 - 3%. quartz phenos t o 0.8 cm 3 - 5%. 610 medlum gralned 3%. Not very f ine-grained type.

. 259.6 -- - 260.1: plagloclase a l te red to so f t s o a p y m r e e n .

260.1 - 260.5.: & d i m hard grey pink.

260.5 _-___- - 261.4: -..-

b i o gone.

__.__ 261.4 - 26_1-8-: soapy Tf$it green.

261.8 - 262.6: Mott led a l l green wlth b i o gone and grey pin1

- 262.6 - - 264.3: plagioclase a l tered to s o f t soapy l i g h t green.

-- 264.3 - - 2 6 5 . 3 : gone. Zonediaround s l i p a t 264.8. 70 t o C.A. yel low green w i t h narrow marglns of dark green; k spar a l t e red t o medium s o f t plnk-

265.3 - 265.5: s o a p y 7 t h t green, some w i t h dark green core' except f o r both feldspar a1 tered and b i o goni a t :

plagioclase as qbove, k-spar

both feldspar a l t e red green,

plagloclase a l te red t o s o f t

both feldspar a l tered.

both feldspar alteredd b l o

Plagioclase a l te red t o sof t soapy

grey.


266.7 (20 cm) and 269 (20 cm). , . . . . I

SIIuclurd An#*

250.4: 40' 251.4: 50' 251.5: &lack seam 15 . 253.1: 30' 253.4: doo 254: 30

SYMBOL C.AJMp4

254.4: 45O 254-255.2:

many blac segms 8 s l i p s

about 60'. 255.2: F.W. s l i p of gauge 256.8: 55 259.6: 30' 260.5: p l y s l l p 70 . 264.4: 60' 264.6: g l y s l i p s 60 . 264.8: p l y s l i p 60 , 5 cm breccia. 265 : blgck gem 60 , 5 cm breccda. 266.2: 35 . 266.7: p l y s l l p 30 . 269.9: 50'. 270: biack s l l p 45 .

45 -70 , mst

MMPLE no.

79-1 0-81

79-10-82

79-10-83

tr,e,

3--̂ ----

jg-10-84

l_l.l

79-1 0-85

79-10-86

79-10-87

79-10-88

870 - 880 I n k-spar -_-I_

880 - 890 I n quartz,

890 - 900 As above. -. - - .-

' 9 a t l o -- -_

9 * PY

9

-

I---- -- ..-_I .--

0.051 .Om

1 SVMIIOLS AND AOBnEVlATlONS - ~ . ~ .... .

I" . . S W E I INTERVAL bum - .- -

I----- ADDITIONAL INTO '

-__--_--- CLAIM/PERMIT NO : ____

16 16 -

3 9 9 , ~

SHELL CANADA LIMITED - MINERALS DEPARTMENT PACE ~- .. - - - .or

-- DRILL HOLE OR SECTION DATA RECORD PAOJECT PROJCCT NAMF NO -.--C!??mo HOLEISKC. N O ' .- - ~ . -. ~- -

~ - - 7 v T.,n.- WORK DONE Nmm Dmlm f l e w u r h

-- __ FIELD COCA= --___- - LOOGtNG~ ____ - GRID

ASSAYINO'

N E A 2 s u n v E v _____

_ _ LANDMARKS: LDGGCD BV: OTHER FEATURES'p-- - __ __ __ __-_p.-___p -

269.6 - 270.3: Both feldspar altered green, I m-jiG.-- 270.3 - End: plagioclase altered to soft I s=py7r?fii; green, l oca l ly dark green.

B A W L € No.

L

A S S A Y

--/-

SHEET INTEflVAL lwm 1"

- 3L -

W

1979 ASSAY CERTIFICATES

Chemex Labs Ltd.

50529 66654 50612 693 50691 770 50768 771 50927 540 66261 8.41 ( 2 p a g e s )

328 88L ( 2 p a g e s ) 381 913 4 50 946 526 947 534 9.48 582 949 6L5 968 646 969 653

Min-En Labora tor ies Ltd.

File 0-7, J a n . 9/80 - 6 pages 0-7-R, Feb. 7 / 8 0 - 1 page

CHEMEX LABS LTD. -

ANALYTICAL CHEMISTS GEOCHEMISTS REGISTERED ASSAYERS

CERTIFICATE OF ANALYSIS TO: S h e l l Cazada R233urces L t d .

If: .,n-c?rals Zep t .

P.O. 52x 100

212 BROOKSBANK AVE NORTH VANCOUVER. B C CANADA V7J2C1 TELEPHONE 984-0221 4REA CODE 604 TELEX 04-3525a7

50529 CERTIFICATE NO.

32556 INVOICE NO.

RECEIVED Sept. 11/79

I SAMPLE NO. : w J l s o on Cert.f60261 - 19-1- 1 85 2 30 3 35 4 20 5 50 6 3> 7 12 8 40 9 5 10 2 11 12 12 15 13 14 -

-

14 15

10 12

17 15 18 12 19 17 20 10 21 8 22 35 23 2 24 5 25 5 Z b 2 27 8 28 4 29 10 30 5 31 U

5

I I

1 W

I -

C I U I D I A U TESTING

A S S O t l A l l O M

212 BROOKSBANK AVE NORTH VANCOUVER. B C CANADA V7J2C1 TELEPHONE 8844221

504 LTD. . :ER:;~~~~~ G4-352597 CHEMEX LABS -

ANALYTICAL CHEMISTS GEOCHEMlSrS REGISTERED ASSAYERS

CERTIFICATE OF ANALYSIS CERTIFICATE NO. 50612

TO: S h e l l Ctnz-Js ?.oso-rces L t Z . INVOICE NO. 32744

1 S A M P L E NO. : L i L .

v 73 - 1 - 3 4 1

35 1 5 36 35 37 7 3a 20 39 8 40

73 - i - 41 7 9 - 1 - 4 4

10 10 2

- 45 2 46 14 47 20 4 s 30

I zr 49 20 i 50 10

7 9 - 1 - 51 15 79 - 1 - 57 5

58 2 59 10

7 9 - 1 - 60 IO

Y L Y D E I

O N A D I 4 U TECTINO

ALSOCUTION

212 BROOKSBANK AVE NORTH VANCOUVER. B C CANADA V7J2C1 TELEPHONE 9843221

604 CHEMEX LABS LTD. @4-352587

I


Z?H v M s o cn Cert.d 66381

SAMPLE NO

7 9 - 1 - 3 3 40 L2 35 4 3 20 52 30 53 35 5 4 30 55 3 3 5 6 35 61 45 6 2 8 6 3 20 64 4 3

CERTIFICATE OF ANALYSIS CERTIFICATE NO. 53691

32258 INVOICE NO.

RECEIVED szpt . 15/79

I A

Y E Y B C R

CANADI&N TESTIN0

ASSOCIITIOY

C E R T l F l E t B Y : .. 1

Y E Y B C R

CANADI&N TESTIN0

ASSOCIITIOY

. ..

212 BROOKSBANK AVE NORTH VANCOUVER, 0 C CANADA V7J2C1 TE LEP Hv" N E 884 4 22 1

604 CHEMEX LABS LTD. ;:::xCoDE 04-352597

- ANALYTICAL CHEMISTS GEOCHEMISTS REGISTERED ASSAYERS

CERTIFICATE OF ANALYSIS CERTIFICATE NO. 50788 TO: S h e l l Cznadz ;.?sources Ltd.,

!:Facials 52Pt. T.0 . 3QX 100 c . c. S z l t b e r i q e l e

33061

RECEIVED S e p t G b e r 20 , 1579

ANALYSED 0c:cber 5, 1479

INV9ICE NO.

i r'H W

i Y - 1 - 1 3 13 76 60 77 1 78 35 79 30

SAMPLE NO. .

6 U (I

81 3 32 6 83 16 84 20 b> 14 S6 12 87 60 86 30 89 18 Y U I

92 125. 93 14 94 4 113 6 I14 32 115 12 116 20 117 12 115 4 0 119 6 120 5 121 8

91 ia

73-1-122 25

MEMBER C I N A D I A N TLLTIUG

bLSOClATlON

‘I

CHEMEX LABS LTD.

212 BROOKSBANK AVE NORTH VANCOUVER. 0 C CANADA V7J2C1 TELEPHONE 934-022: AREA CODE 604

04-352597 TELEX. -


50927 CERTIFICATE OF ANALYSfS CERTIFICATE NO.

INVOICE NO 33259

S e p t . 2 6 / 7 9

Ocr. 17/79

Also on . ~ S E Y f66534 FiJK w

79-1-95 10 96 10 97 20 98 13 99 9 100 11 101 8 102 8

7 9 1.- 1- 9 4 9

SAMPLE NO

10 3 a

-

I

2 1 2 BROOKSBANK K V E

NORTH VANC0UVER.B C CANADA V7J 2C1

K R E A CODE 604 T E L E X 0 4 3 52597

T E L E P H 3 N E 995-054 8


TO.

ATTN

C E R T I F I C A T E O F A S S A Y C i ~ ~ l l C;~.zla F e s o m c e s Ltd.

~ Iz?r; .LS 27: * r.C. 50?: 193 c z l g a r p , P l t a 7 2 P 2H5 CC: S d t h e r i c g a l e PZOJBCT: 3991-T Kr . J. Brander P.O.859454

- - . * .

-

€€261 CERTIFICATE NO.

32759 INVOICE NO.

RECEIVED S e ? t . i l l 7 9

Se;. t . 21/79 ANALYSED

SAMPLE NO. :

.. ; c i 0.007 0.02 < 0.003 0.005 0.01 ~0.003 0.010 . .

.- .’ 0.038

- 0.240 0.34 ~0.003 0.144 - . - n.277 0.02 ~0.003 0.168 f 0.250 0.01 ~0.003 0.150

0.078 0.01 ~0.003 0.047 -’ 0.143 0.01 ~0.003 0.056

79 - 1 -32 0.027‘ 0.01

i

I

..

4 6 0.042 0.070 0 .02 <O. GO3 i

CHEhiEX L A B S LTD. -


C E R T I F I C A T E OF A S S A Y CERTIFICATE NO. 6c326

INVOICE NO. 32147

RECEIVED Se;te=‘,er l E , 1 9 7 9

FZOJZCT - 3291-T ANA LYSED c. c . W.G. S i c i t h e r i n g a l e

x I oz/ton o=/ton Y ! K3S, Ag Au

I S A M P L E NO.

! 79-1-34 0.022 0.037 0 . 0 3 <O. 003

35 0.015 0.025 0. c5 4 . 0 0 3 36 0.012 0.030 0.01 < O . 003 37 0.010 0.016 0.04 <0.003 7 c1.032 0 . c54 0.05 4.003 39 0.032 0.052 0.02 ~ 0 . 0 0 3 40 0.013 0.013 0.01 ~ 0 . 8 0 3

0.089 0.014 0.05 <0. 033 ! 7 2 - 1 - 4 4 0.013 0.021 0.01 ~0.003

-.

I 75-1-41

47 0.021 0.034 0.01 - <O. 003 0.040 0.066 0.05 ~0.003

w 49 0. C29 0.0L8 0.05 ~0.003

79-1-51 0.015 0.025 0.05 <O.OO3 75-1-57 0.013 0.021 0.02 <O. 003

58 0.043 0.072 0.01 <O. 003 5 9 0.057 0.035 0.03 <O. 003

70-1 -60 0.056 0.093 0.05 <O. 003

i

I qn 0.037 0.061 0.02 <o. 003

4 6

I

/ ’ / / - I I

v C A N A D I L h TESTING

ASSOZIATION R f C ’ S T L 6 i D A 5 5 i V E R . P R 3 V l h C E C F B R I T l j d C ? Z ? V , l A

CHEh4EX LL4RS LTD. ANALYTICAL CHEMISTS GEOCHEMISTS REGISTERED ASSAYERS

C E R T I F I C A T E O F A S S A Y TO Shell Cards Resources L t d . ,

! : h e r d s Cept. P.O. Lox 100 PROJECT - 3991-T C z l ~ z r y , k l t a . T2P 2H5 ATTN C . C . W.G. k i t h e r i n g a l e

CERTIFICATE NO. 66381

INVOICE NO. 33147

RECEIVED Sep tezAer 15, 1479

ANA LYSED O c t o b e r 11, 1979

x x oz / ton oz/ton 1 )lo tcs S & Au

iY-1-33 u.uut5 0.013 0.01 <O. 003 I 42 0.025 0.042 0.02 <O. 003

4 3 0.043 0.071 0.01 <O. 003 52 0.020 0.033 0.05 ~0.003 53 0.060 0.100 0.02 ~0.003

I 54 0.010 0.016 0.07 ~0.003 I 55 0.010 0.016 0.06 <O. 003

56 0.024 0.040 0.05 <0.@03 61 0.004 0.006 0.06 <O. 003 62 0.013 0.022 0.06 ~0.033

64 0.050 0.063 0.05 <O. 003 65 0,009 0 .014 0.05 <O. 003 66 0.015 0.025 0.02 <O. 003 67 0.011 0.018 0.01 ~0.003 68 0.008 0.013 0.01 <O. 003 69 0.019 0.032 0.01 ~ 0 . 0 0 3 70 0.020 0.033 0.02 <O. 003 71 0.042 0.070 0.05 <O. 003 72 0.007 0.011 0.04 ~0.003 73 0.058 0.097 0.01 ~0.003 74 0.019 0.031 0.01 <O. 003 107 0.013 0.022 0.01 <O. 003 108 0.053 0.083 0.01 <O. 003 109 0.062 0.103 0.01 <O. 003

1 S A M P L E N O

I

i i i

63 0.008 0.013 0.06 <O. 003

-7

110 0.041 0.058 0.01 4. G33

7 9 - 1 4 12 0.026 0.043 0.01 4.003 1 1 1 0,114 0.190 0.01 <c). 003

I

212 B R O O K S t A h t ' 4 \ E

NORTH V4rVCOL'VEF t L

C A N A D A v;d 2c :

w

CHEMEX

73-2-10 0.014 0.024

L A B S LTE. TELEPHONE -: 8&cM2, A R E 4 CODE O'.W

G3-52557 - - I ~ L E T .

A N A L Y T I C A L CHEM:STS - GEOCHEMISTS REGISTERED ASSAYERS

C E R T I F I C A T E O F A S S A Y CERTIFICATE NO €6153

TO S h e l l C L Y Z ~ E Lesources Ltd., INVOICE NO. 33147

CalGEry , M t a . T2P 2-25 kTTN

Se3texber 29, 157f

October 11, RECEIVED

F X O E C T - 3ggl-T C . C . W.G. S z i i E e r i c g s l e ANALYSED

1 4 7 9

- I x h C Z I :on O Z / t on - Yki x 3 S , -Q3 xu 1 S A M P L E N:., I ,:-, - _ - e

I 76 0.026 0.044 0.OL 4 . 0 0 3 77 G.015 0.025 0.32 <O. 003 75 0.041 0.067 0.05 <O. 003 79 0.031 0.051 0.01 <O. 003 30 u. u4z u . u / u u. UL <U. mJ s1 0.1559 G . OS3 0.05 <O. 003 82 0.005 0.109 0.05 <O. 003 s3 0.045 0.075 0.01 <O. 003 &4 0.015 0.025 0.01 <O. 003 8> 0.u31 U.U>L U.U/ <u. uuj

I 56 0.066 0.110 0.01 <O. 003 87 0.056 0.110 0.03 <O. 003

0

1 I

I -

I

88 0.035 0.058 0.07 <O. 093 39 0.056 0.110 0.07 <0.003 90 0.106 0.177 0.05 <o. 003 91 0.074 0.123 0.03 <O. 003 92 0.068 0.113 0 . a1 <O. 003 93 0.025 0.047 0.03 <O. 003 84 0.015 0.025 0.02 <O. 003

114 0.048 0.078 0.04 <O. 003 115 0.116 0.193 0.04 <O. 003 116 0.298 0.438 0.01 <O. 003 117 0.108 0.180 0.03 <O. 003 - 7 1s U. U L i j U . U / l u.uz <u.uI)j 119 0.138 0.230 0.10 <0.003 120 0.032 0.137 0.01 <0.003 121 0.200 0.330 0.02 <O. 003

1 1 3 U.UbU u. 1vu 0 . u 3 <u. uu3

79-1- 122 0.042 0.070 79-3-1 0.004 0. c32

2 0.011 0.G18 3 0.022 0.036 4 0.037 0.062

0.028 0.046 6 5

L' 'J '4 U.U.rU 7 0.0'16 0.C75 a 0.026 0.043

‘CI CHEMEX L A R S LTD.

-

2 1 2 BROOKSEANK L\’E NORTt ! VANCOIJ\’ER, E: C C A b; & DA v:? 2c1 T E L E P H O N E 9-1 A E E A C O 3 E 604 T E L E X 043 52557

11 0.339 0.014 1 2 0.068 13.113 1 5 0.032 0.053 13 0.334 0.056 19 0.014 0.024 23 0.019 0.032 21 3.043 0.071 22 3.056 0.092 23 0.047 0.078 94 0.019 0.032 25 0.932 0.054

GE0CHEM:STS REGISTERED ASSAYERS ANALYTICAL CHEMISTS

TO

C E R T I F I C A T E O F A S S A Y CERTIFICATE NO. 6 6 j 2 3

INVOICE N O

RECEIVED

3 3 3 3 9

Se3t . 27!73

O c t . 19/79

i S A M P L E NO. 1. ;c

1 !O ? 3 S 2

39 0.3$5 0.090 3 1 0.033 0.055 32 3.035 0.058 33 0.003 0.005

79 =2- 34 0.008 0.013 7P-2-12 0.330 0.050

1 4 0.023 0.038 15 0.030 0.050 25 0.013 0.022

7?-3-28 0.100 0.167 7 9 - 4 - 1 0.011 0.005

3 0.U15 0.095 5 6 7

0.013 0.017 0.022 0.036 0.022 0.036

9. 0.023 0 . 0 3 3 10 0.018 0.030 11 0.014 0.024 12 0.072 0.120

0.044 0.073 0.027 0.045 0.025 0.040

-

19 20

I 21

I 0.025 0.042 0.020 0.033 0.038 0.063

LTD. ANALYTICAL CHEMISTS GEOCHEMISTS REGISTERED ASSAYERS

C E R T I F I C A T E OF A S S A Y

?l? B R O O K S b A N E A V E NORTH V 4 N C O U V i R . b C CANAG.4 V7J 2C1 T E L E P H O N E f i R E A CODE 634 T E L E X iM4j-5755;

9Rco221

CERTiFlCATE NO. 6 6 5 3 4 3325'6 INVOICE NO.

Se;rt. 2 6 / 7 9 RECEIVED

ANA LYSED Oct. S / ? 9

c c I. J. oz / ton oz/ton 1 S A M P L E NO. '

I ! Ja Y 3 s 2 AF SU '1

- I r z - - - 9 5 0.uZO 2.533 0.04 < 0.003 i 96 0.016 0.026 0.02 c 0.003 I 97 0.035 0.142 0.36 e 0.003 1 I 98 0.014 0.923 0.16 c 0.003

39 0.@18 0.030 0.02 c 0.003 100 0.011 0.318 0.04 c 0.033 I 1 0 1 102 103

0.014 0.023 0.02 c 0.033 0.015 0.025 0.06 c 0.033 0.039 0.014 0.06 < 0.033

79-1-104 0,020 3.033 0.01 c 0.003 79-2-1 0.0C6 0.034

2 4

1 9r 5

0.009 0.013 0.031 0.052 0.017 0.029

6 @. 035 0.057 7 0.070 0.097

i

8 9.021 0.034 9 0.012 0.020 10 0.039 0.314 13 0.056 0.077 1 4 0.022 0.035 16 17 27

0.022 0.037 0.011 0.019 0.010 0. Dl7

7?-2-28 3.023 0.038 72-3-11 0.018 0.G30

13 16 17

0.013 0.021 0.015 0.025 0.041 0.058

t 18 0.020 0 .033 1 9 0.a12 0.020 20 0.056 0.093 21 0.009 0.014 22 0.098 0.013 2 3 0.639 0.014

1 1

I 24 0.010 0.917 -7 25 27 i 29

W

)r

212 EROOKSBANK A V E NORTH V A N C O U V E R e c C 4 h A D A V7J 2C1

A R E A CODE 604 CHEMEX L A B S LTD T E L E X 043 52597

TE L E P H O t i E 985-064-18


C E R T I F I C A T E O F A S S A Y 10. S i z i l C>:zda Resources L t d . ,

! 2 7 : e r 2 l S I k p t . 0.0, 59x 1c)o

A';TN, C31,r;l iy, Alta.

65552

33339

O t r . 2 / 7 3

O c t . 1 9 / 7 9

CERTIFICATE NO.

INVOICE NO.

RECEIVED

ANALYSED

SAMPLE NO. :

7 3 4 - 2 0.014 @.035 4 0.011 0,012 8 0.029 0.045 13 0.030 0.133 15 0.035 0.057 16 0.014 0.024 22 0.068 0.113 24 0 . 2 7 2 0.454 25 0.318 0.517 26 0.072 0.119 27 0.044 0.074

- 28 29 30

0.064 0.107 0.045 0.075 0.029 0.04s

31 0.019 0.032 32 0.130 0.217 33 0.066 0.110 34 0.034 0.056 35 0.146 0.244 36 0.108 0.130 37 O.LI70 0.117 ;a 0.106 0.177 39 O.iI37 O.OG1 4 0 0.398 0.163 L 1 0.390 0.150 L 2 0.349 0.032 L 3 0.042 0.070 14 0,180 0.3:30 4 5 0.104 0.173

-

4 6 0.104 0.170 4 7 0.088 0.143

7 ? - 4 - L 3 0.049 0.078

- A N A L Y T I C A L CHEMISTS GEOCHEMISTS REGISTERED ASSAYERS

C E R T I F I C A T E O F A S S A Y TO Shell Ctnade Yeso-rces L t d . ,

! ! h e r d s k p t . P.C. sox 100 C ~ l ~ z r y , A-lta.

krrNY,? 255 3591-T

C . C . C s s i e r . E.C.

CERTIF ICATE N O . 65645

3 350 1 INVOICE NO.

RECEIVED O c t o t e r 4 , 1979

ANALYSED Octcye r 29, 1 9 7 9

. A x

:,os S E V P L E Pi3 *:o 1 iY -3 -31 ii. 320 0.033 I 32 0 . 3 4 6 0.076

33 2.911 O.C)18 I I 34 0.114 0. I Y O

j 35 0.031 0.048 I 35 @.a27 0.945

37 0.024 0.040 38 0.962 0.103 39 0 .036 0.ch0 40 0.048 0. O W 4 1 a. 094 0.155 42 0.140 0.231 4 3 0.106 0.177

I 44 0.01s 0.030 45 0.03s 0.064 46 0 .007 0.012 47 0.018 0.030 46 0.264 0.197 44 0.013 0 . ii22 so 0 .362 0.103 51 9.054 u. m 0 52 0.118 0.195 53 0 .284 0.474 54 9.332 0.054 55 0.i;;9 0. d 6 4

13.137 57 u . 929 0.948 53 0. u76 0.127 59 0.032 0.053 59 0.037 0.061 61 0.033 0.055 6 2 0.048 0 .030 6 3 0.036 9.060

7 2 - 3 - 6 4 0.26s 0.133

C L .I T.27 2 U u. \,"&

_.___ _- 7 9 - 4 - 4 9 0.070 0.115 50 G.024 17.937 51 0.026 0 . 0 4 4 52 0. c45 0.1J75 53 9 . 0 3 2 0 .354

212 E R O O K S B 4 N K 4 V E lJORTH VANCOUVER. E C C f i N f i D A V7J 2C1 7 E L E P H G h t 9E5-0SE A R E A CODE 6134 TELEY c J 3 52597


C E R T I F I C A T E O F A S S A Y

399 1-T C . C . Cassier, E.C.


INVOICE NO. 33501

RECEIVED O c t o 5 e r 4, 1473

ANALYSED @:tot;er 2 9 , 1 5 7 9

c .-9

h /.

S A M P L E NO. l.b ?:o S TP i r c n I r - J > U. -0,J

56 0.04 1 0.069 57 3.G33 0.055

79-4-53 0.019 0 . 0 3 2

n n r r

i -

W CHEMEX L A B S LTD. ANALYTICAL CHEMISTS GEOCHEMISTS REGISTERED ASSAYERS

TO.


Sneli Cmada Kesources Ltd., ? i i x e r d s !kipartmefit, P.C,. 30:; lU0.

CERTIFICATE NO. 6 6 6 5 3

A ~ N . M g a r y , Alberta. T2P 2 s cc; Cesslar

I x ! :o ?iOSZ

S A M P L E NO. -

75-2-65 C. 102 0.170 66 0 . 0 2 4 67 0.034 68 0.036

C. 040 (5.053 0.060

64 0.106 0.177 70 0.074 0.123 7 1 O.i)66 0,110

0.060 0.100 0.132 0.220

0.093 0.127

1 0.050 75 0.076

-i 6 0.064 0.107 7 7 0.116 0.193 78 0.094 0.157 73 0.1137 0.170 63 0.126 0.210 6 1 0.490 0.660 62 0.357 0.592 83 0.070 0.117 64 0.062 0.103 65 0.082 0.137 86 0.076 0.127 a7 0.128 0.213 68 0.088 0.147 89 0.114 0.190 YO 0.294 0.488 41 92 9 3

0.142 0.237 0.042 0.070 0.076 0.125

94 0.126 0.210 95 0.116 0.191 96 0.228 0.380 97 0.044 0.073 98 0.058 0.097 9 9 0.025 0.042

133 0. I26 0.207 191 0.228 0.380 1172 0.136 9.227

-

0.096 0.009 0.490 0.816

I . ,

? l ? BRDOKSBANK A V E NOFiTH L'AYCOUVEP.. E C

V7J 2c1 C A N A C C

TELCPHONE 0- . A R E S CODE

I CHEh4EX L A B S L.TD. TELEX 043 52557

- ANALYTICAL CHEMISTS GEOCHEMISTS REGISTERED ASSkYERS

C E R T I F I C A T E O F ASSAY CERTIFICATE NO. 6 6 6 5 4

INVOICE NO. 33395 TO Cr.ell C ~ z z c a Sksoxrces L t t . ,

!,r.erLls ;eF;rrs2r=:, F.C. L C X l i i C , C E l G a i y , Albert&. T2P 2H5 cc: Cassiar ATTN

i, a

110 XOS2 S I M P L E NO. '

73-3-105 0.027 0 .045 106 L'. 01E E. 030 10 7 0.382 0.137

7 4 - 3 - 10 8 0.160 0.258

W

w

I

CHEMEX L A B S

48 0.912 0 . 0 2 0 49 0.039 0.050 50 0 . 0 3 u. 060 51 0.236 0 . 3 9 4 52 0.929 0 . r)4& 53 0.017 0.028

79-2-54 0.020 0. u33 I Y - 3 - L : . I'

110 0.1228 0.146 111 0. IJ2Y 0 .048 112 O . : j 1 3 0 . 0 2 1 113 U.dl5 3,025

115 u . 01 3 0.019 116 0.032 0 . (153 117 O.ir50 0.033 118 0 . 3 2 4 1). 043 119 0.038 0.013

79-3- 120 f1.030 0.059

A i 4 '!. - 3 4 u. 3ad

LTC. ANALYTICAL CHEMISTS GEOCHEMISTS REGISTERED ASSAYERS

C E R T I F I C A T E OF A S S A Y S h e l l Cznada Rcsot i rc2s L t Z . , .-lr,erels Pep:. F.G. 3cs 100

TO ,,.

CERTIF ICATE NO 66693

INVOICE NO. 33505

OctcLer 15. 157'9 RE C E I \'ED

ANALYSED C c t o L e i 23, 1 9 7 5 C . C . C z q s i a r , 13.C.

I

212 EROOKSBANK A V E NORTH VANCOUVER, e C C A N A D A V7J 2C1

AREA CODE 604 CHEMEX L A B S L T D . . T E L E X 043 52537

TELEPHONE 985-0648

r z .€c- ,, //; 5; Ib(Tota1) : -. , . f * > 3 > ?.Ir

SAMPLE NO. :

- - u.u93 . G:-f ./

56 0.060 - / 3 3

57 0.031 * - : -

58 0.013 . - - - 59 0.049 . ’. 6 1 0.039 . LJc,c 62 0.042 . ; 7 3 6 3 0.066 - , ‘3

0 5 0.018 . c i ,3 66 0.027 , S q J - -

- - - . - -

.- - - 60 0.023 . ; I f

64 0.043 & 7,i

e ANALYTICAL CHEMISTS GEOCHEMISTS REGISTERED ASSAYERS

C E R T I F I C A T E O F A S S A Y TO: S h e l l C m d a Resources L t d . ,

F!!nerals k p t . P.O. zox 100 Calgary, -Uta.

A r ’ k P 2Ii5 C . C . Czsoier, B.C.

CERTlF ICATE NO. 66770

INVOICE NO. 33595

RECEIVED October 16, 1979

ANALYSED Koves3er 2, 1979

69 0,086 . I l l

70 0.045 , 5 7:- 71 0.048 . : , d o 72 0.032 - 95-2 73 0.052 . !23 74 0.019 332 15 0.338 - 5 1 - 76 0.056 h 522 77 0.144 * 2 4 78 0.062 * ‘Cj 79 0.162 9 2 70 60 0.104 I < C . :

6 9 7 --i

81 0.056 82 0.104 I *

83 0.054 , 1 5 7 s4 0.062 . /j 7 85 0.074 . I22 s5 0.048 . oeo 87 9.054 , 2 3 3 88 0.148 .: q7

79-2-59 0.054 -040 /L:->-Ul 0,009 . c /f

03 0.084 . I do 04 0.033 .2<:’

02 0.009 . E I ~

79-5-05 0.026 . - 1 7 ?

/x A ? ! - M E Y S E R ;/,-A% 3

R E G I S T L R E D Z S S i V C R . P R 3 V I X C E OF B R I T I S H C O L - * ’ B I ~ CAN4DlAN TESTING

ASSOCI4TION

2 i 7 B R O O K S B A N K A V E N O R T r VANCOUVER, E.C C A N A D A V7J ? C 1

7 E 1 E P P 0 N E 9 d E-OME F R E F , CODE 604 CHEMEX LL4BS LTD. -. , r E L E X w3- 57597

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CERTIFICATE NO 66771 C E R T I F I C A T E O F ASSAY TO INVOICE NO 33595

S h e l l Cz-Tzda & s o u r c e s Ltd . , t5it,erals ZS?t. RECEIVED GctoSer 1 8 , 1979

SDv,zSer 2 , 1979 P.O. 33x 100 ANALYSED

A m T a l p r y , A l t ~ . C . C . Cassiar, B.C. - q q 7 - c J.L. i - A

SAMPLE NO. I x I f - V.'-C

79-5-06 OY028 bTG27 07 0.109 0.031 09 0.038 0.013 c9 0.039 0.065 *U .-' .e 4 7 u. 3 S d

11 0.027 0.045 12 0.023 0.038 13 0.015 0.025 14 0.025 0.042 I2 U . V U 0 V. 3 L J

16 0.005 0.038 17 '0.040 0.067 18 0.020 0.033 19 0.017 0.028 LV LJ. LL4 U.202 2 1 0.034 0.055 22 0.038 0.063 23 0.031 0.051 2 4 0.098 0.013

h h n . r

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LI

26 0.074 0.123 27 0.012 0.020 28 0.030 0.033 29 0.024 0.040

w CHEh4EX L A B S LTD. -


C E R T I F I C A T E O F A S S A Y T O . S h e l l C a x d s Res3urces L t d .

YLnerals C ? p t . ?.O. 5oxl03 C e l g z ~ , Alta.

ATTN: 3?31-T CC. Czssiar, B . C .

7 1 ? CIGOOKSBANK AVE Pi ; ) i iT? iVANCOUVEG E C c F rd A D A V7J ZC1 TELEPr iGNE 9350648 A G E A CODE 604 T E L E X 043 52597


INVOICE NO. 33710

RECEIVED O c t . 30/79

ANA LYSED Sov. 8 / 7 9

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V CHEh4EX L A B S LTD. ANALYTICAL CHEMISTS GEOCHEMISTS REGISTERED ASSAYERS

C E R T I F I C A T E OF A S S A Y Shell Cansda ko-sources Ltd. ?Xgers l s ?-.pt. P . 0 , 39ox 100 C a l ~ ~ r y , Xice.

TO.

ATTN T2P A i T . 3991-T C . C . l . Cassiar

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6 6 5 4 1 CERTIFICATE NO.

INVOICE NO

RECEIVED

ANA LYSED

33756

Occober 33, 1479 Xovenber 9 , 1 9 7 9

35 36

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2 1 ? BRGOKSBANK AL'E N O S T F VANCOLJVER. E C C A N A D G V7J 2C1

A R E A COGE 604 TELEPHONE 985-9648

r E L E X 043-52597


33882

O c t . 30/79

Kov. 16/79

TO ??icIi Cz;-,a?a Pcsources Ltd. INVOICE NO. * I : - . ' . A A . E r 2 1 s Z'ept .

L,,: I f 3rp , C t a. P.0. P2x 100 RECEIVED r -

AnN. TI? 2F5 A t t . 39?1-T C.C.l. Cessiar ANA L Y SE D

Oz/T S A M P L E NO. '

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?:? ERGGKS6CNK A V E Q O Z T H V4NCO'JVER E C C A N A D A V7J 2c1 TELEPUONE 935OM8 & R E A COGE 604 T E L E X 0 4 3 52597


CERTIFICATE NO. 66E94 C E R T I F I C A T E O F A S S A Y INVOICE NO. 33350

RECEIVED O c t . 31/79

C e l g 3 r y , . r l tz . , T2P 2F5 ANA L Y SE D ?;m.16/79 P3C)JZCT: 3991-T CC. CEssiar, B.C. ATTN.

Oz . /T 1 S A M P L E NO. ' l

0

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I.r CHEMEX LABS LTD.

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21? GFiOOKSf?$NI: A V E NORTH vAr;couvEs. e c C 4 h A D A \ 'JJ 2 C l TE LEPYOfJE 985-3648 A K E A CODE 604 T E L E X w3-515s:

CERTIFICATE NO. 4 t S E 4

INVOICE NO. 337G7

RECEIVED C r t . 31/79

ANA LYSED '::\*. lj/i9

: !4 . f ;;.- .'. x 1 S A M P L E NO. ' '.- . , , .- i . . , 1 , - ?;O .. 7 9 - 7 - 2 3.028 * - - -7

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21? GROOKSBANK A V E NGRTH V A N C 0 U V E R . e C C A N A D A V7J 2 C 1 TELEPHCNE 985-0642 A e E A CaDE 604 T E L E X c3 3 - 52 59 7

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C E R T I F I C A T E O F A S S A Y CERTIF ICATE NO. 65513

INVOICE NO. 33s23

RECEIVED ? ; 3 v . 5 / 7 9

ANA LY SE D cc: Cesslar

x I . - - S A M P L E NO. '

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A N A L Y T I C A L CHEMISTS GEOCHEMISTS

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A S S A Y

CC. Casslar

2 1 2 B H D O K S b A N K A V E N O R T H V A N C 0 U V E G . E C C A FJ A D A v71 ?C1 TELEPHONE 985064E A R E F CODE 604 T E L E X 043-5?537

CERTIFICATE

INVOICE NO.

RECEIVED

ANA LY SE D

NO 659L6

33918

I k v . 1 2 / 7 9

?ic\*. 19/79

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2 i 2 SROOKSBANK A V E IwORTH VANCOUVER i? C CANADA V i J 2C1 TELEPHONE 985 @ME A R E A CODE 604

w CHEMEX L A B S LTTD.. T E ~ E Y 043 52597

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- A N A L Y T I C A L CHEMISTS GEOCHEMISTS REGISTERED ASSAYERS

-, I I 0.237 ,3u-- , 3 J ? 0.032

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33891 C E R T I F I C A T E O F A S S A Y

S I i e l l Ca2sda 2esources INVOICE NO.

P.O. sox 100 RECEIVED

TO. V'rlcrzls k p t . ?<ov. 12/79

c d ~ a r y , .2lta. !;ov. 19/79 ANALYSED A T f N . CC. Cassiar, BC

? 1 2 EROOKSBGNV L V E NORTH VANCOUVEF E C C 4 N G D 4 v7J zc1 TELEPHOPJE 335-0645 AFIEA CODE 604 CHEMEX L A B S LTD. , T C L E Y c s 3 5?557


C E R T I F I C A T E O F A S S A Y To. S F , e l l Csnada RePources L t d . ,

?!:nerds Dept., ?.@. sox 109

66949

INVOICE NO. 33351

RECEIVED A.uwc-Ser 12, 13;

CERTIFICATE NO.

.-_____

n

?J2 D-/d 7.j - z S A M P L E NO.

7 9-::-47 . - 0.022 4 8 - - c.041

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0 . C57 56 -- - O.C?8 57 - - 7

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A N A L Y T I C A L CHEMISTS GEOCHEMISTS REGISTERED ASSAYERS

C E R T I F I C A T E O F ASSAY

212 BROOKSBANK A V E NORTH V A N C O U V E R . E C C A N A D A V7J 2C1 T E L EF H ON € 985-064E A R E A CODE 604 T E L E X 093- E: 259 7

66959 CERTIFICATE NO.

INVOICE NO. 33969

RECEIVED Xovecb2r 1 4 , 157

!:ove=lber 2 2 , 147 ANALYSED

7-

SAMPLE N O 1. z ?.b L'. u1)z 1s-10-1 I d

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CHEMEX LABS LTD.

2;: BROOKSBANK A V E NOPTH VANCOUVEf i , E C C A N A D A v 7 1 2c1

A R E 4 CODE 604 TE LEPhCJl\iE 985G64E

T E L E X 043-52597


C E R T I F I C A T E O F A S S A Y S h e l l Canada Resources Ltd . , ?2n;_re ls Eep:. , P.O. Lox 100

TO:

C ~ I g z r ) . , Alta., ATTN T2P 2%

P?OECT f3931-T --_

66963

33969

?:ovPJSer 1 4 , 1979

CERTIFICATE NO.

INVOICE NO.

RECEIVED

ANALY SE D !;over,3er 22, 1979

5 Y I :: - r , - . , ' J - - - - 78-X-61 0.038

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DATE Jan.9/80.

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N O R T H V A N C O U V E R , 9 . c . P h o n r 980-5814

I

I

A g I I ~ o z / t o n I

.01 i I i ~ 1 0 6 ! . 0 2 I

S M P L E No. 1

I I

1 . 7 9 - 3 - 1 0 5 !

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I 1 0 7

1 3 2 8 - 5 1 0 W . Hastings St..

V a n c o u v e r . B . C .

i ~ 1 I I I

! 002

S h e l l PROJECT No.

DATE F e b . 7 / 8 0 .

0-7-R File NO .._.._ ,... ___.. . ___.__.._ __. ._.......

109

110

111

112

113

3 14

.03

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I

. 0 2 I I

. 0 2

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117 .01

.01

119 .01

11 b

I

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79-3-12)D

I

I .01 i

I I

/--,

- 35 -

A P P E N D l X 111

Hole No.

LIST OF PROPOSED 1980 D I A M O N D DRTLL HOLES

Depth (me t re s 1 Hole No.

1 2 3 4 5 6 7 8 9

10 11 12 13

C71-3 C71-4

79-2 79-4 79-5 79-6 79-10

100 150 250 400 250 250 150 100 150 200 250 475 LOO -

j eepen 100 m . 100 m .

90 m . 50 m.

200 m. 100 m . 150 m .

I I

1 1

I 1

I 1

1 1

' ,I

14 15 16 17 18 19 20 2i 22 23 24 25

Depth ( m e t r e s )

220 220 280 400 330 500 390 460 470 450 500 420

I t is impor t an t t h a t d r i l l i n g i n e a c h sec t ion s t a r t a t t h e s c u t h ,

where holes a r e sho r t e s t , a n d progress no r thward . Th i s w i l l

p rov ide t h e bes t information on which to dec ide how deep t o

d r i l l t h e longe r no r the rn holes .

A l l holes should be d r i l l e d on a n az imuth of 170° a n d a t a n

i n c l i n a t i o n of -70°,

out holes i n d i c a t e s o therwise .

un le s s new hloS2 f r a c t u r e d a t a f rom. s tep-

- 36 -

APPENDIX I V

To be forwarded l a t e r

APPENDIX V

CASMO PROJECT: 1979 EXPENDITURES

c General Company Labour General Non-Company Labour General Materials Fuels and lub r i can t s Camp Supplies and Materials Photos, Maps and Reports Chemicals General Contract Services Catering Contract Servi ces Location Clean Up Analysis and Laboratory Services Dr i l l ing - Core - Contract Services Geophysics - Contract Services Geochemistry - Contract Services Consultants - Geological Contract Services Mobilization and Demobilization - Coates Auto and Truck - Contract Transportation Ai rc ra f t - Contract Transportation Helicopter - Contract Transportation Communi cat ion - Telephone Postage, Express , Communi cations L i g h t , Heat, Power, U t i l i t i e s Off ice , Contract Rentals Tool and Equipment Rentals - Contract Dwell i ngs - Contract Rental s Employee Travel Survey, Drafting A1 locat ions Ai rc ra f t Allocations E & P

L

$11,311.80 5,887.41 6,997.79 1,883.49 2,155.21 4,087.00

142.63 4,729.59 5,845.90 5,204.18 7,608.23

148,696.31 2,679.19

100.80 28,524.00 12,990.30 1,493.65

581.25 5 , 100.00

751.11 2,950.41 1,500.00

300.00 6,566.13 7,043.82 4,902.50 5 , 625.00 6,112.25

TOTAL : $291 , 769.95

*Does n o t include Overhead o r Permanent Sa la r i e s

w

SYNOPSIS OF EXPENDITURE BREAKDOWN

The expenditures made a t our Casmo Pro jec t d u r i n g 1979 have been broken down in to two ca t egor i e s . Spec i f ic Expenditures a re those cos t s w h i c h per ta in t o s p e c i f i c c la ims, i . e . D r i l l i n g , Analysis and Laboratory Services , Geophysical Surveying and Geological Contract Services. General c o s t s a r e those cos t s pe r t a in ing t o the e n t i r e Casmo Project . w Specif ic Costs

In the case of s p e c i f i c c o s t , a l lotments of expenditures have been made on the basis of the proport ionate amount of work t h a t has been performed on individual claims.

General Costs

The general c o s t s have been a l loca ted t o the individual s p e c i f i c cos ts . The breakdown of the a l lo tment i s based on the proport ionate amount each s p e c i f i c cost makes u p o f t he t o t a l s p e c i f i c costs.

Drill i n g , Analysis and Laboratory expenditures = $1 56,304.54 Geological Contract Serv ices = $ 28,524.00 Geophysical Contract Serv ices = $ 2,679.19

Drilling and Analysis = 83.36% of t o t a l Spec i f i c Costs Geol ogi cal Work = 15.21% of t o t a l Spec i f ic Costs Geophysical Work = 1.43% of t o t a l Spec i f ic Costs

Total General Expend i tu re s = $104,262.22

D r i l l i n g Expend i tu re s , etc.= $156,304.54 = 86,912.99 - 243921 i . 5 3 - 83.36% x $1 04,262.22

Total w

Geological Expenditures = $ 28,524.00 15.21% x $104,262.22 = 15,858.28 Total - - , -

Geophysical Expenditures = 8 2,679.19 - 1.43% x $104,262.22 = 1,490.95 - Total - 491 /0-1

General Expenditures by C1 aim % of Total General Spec i f i c Expendi tures

Claim Dr i l l i ng Geological Geophysical Analysis Total Expendi tures (%x104,262.22) - _ S t o r i e 3 SQE 15 110,175.22 7,245.09 893.06 5,630.09 123,943.47 66.1 68,917.37 West 1-14 Kon 1-3 f r a c t i o n 7 -

Kon 3&4 7,558.86 7,558.86 4.03 4,201.77

Y.

S t o r i e 4&5 Kon 1&2 SQE 9-14 16,259.12 5,276.94 893.90 836.90 23,266.02 12.41 12,938.94

SQE 16-18 22,261.96 6,902.81 893.06 1,141.23 31,199.06 16.64 17,349.23 Kon 5-15 1,540.30 1,540.30 0.82 854.95

187,507.73 104,262.22

Speci f i c Expendi t u r e s

D r i l l i n g Expendi tures = $148,696.31

V Hole No.

DH 79- 1 DH 79- 2 DH 79- 3 DH 79- 4 DH 79- 5 DH 79- 6 DH 79- 7 DH 79- 8 DH 79- 9 DH 79-10

C 1 aim

SQE-15 SQE-15 SQE-15 SQE-15 SQE-15 SQE-15 . SQE-15 & 17 SQE-16 SQE-16 SQE-13 & 15

Hole DeDth (m)

367.3 277.4 368.2 182.9 227.7 124.7

78.3 91.8

160.9 275.2

2,154.4

$148,696*31 = $69.02/m Amount spent p e r metre = 2,154.4

* Breakdown by c l a i m f o r Grouping Purposes

Hole No. C1 aim % o f Hole/Claim

DH 79-7 SQE-15 10.8 SQE-17 89.2

DH 79-10 SQE-13 85.6 SQE-15 14.4

V D r i 11 nu ExDendi t u r e s

$/Hole

148,696.31

Met r e s $/Hole By C l a i m

Kon 3 & 4 26.5 SQE-15 25.4 SQE-13 & 14 18.5 SQE-16, 17 & 18 24.2 Kon 5 5.4

25,351.05 1 9,146.1 5 25,413.1 6 12,623.76 15,715.85

8,606.79 5,404.27 * 6,336.04

11,105.32 17.751.94 *

8.4564 583.66 69.8436 4,820.60

235.5712 1 6,254.12 39.6288 2,735.1 8

Group No. 1 = $110,175.23 Group No. 2 = $ 16,259.12 Group No. 3 = $ 22,261.96

Geological Survey Cost Breakdown z

To ta l Expendi t u r e s = $28,524 .OO

C 1 a i m % o f Survey (By Area) c o s t

Ana lys is and Labora tory Serv ices Breakdown

Group No. 1 = 74% o f t o t a l d r i l l i n g Group No. 2 = 11% o f t o t a l d r i l l i n g Group No. 3 = 15% o f t o t a l d r i l l i n g

c To ta l Expendi ture = $7,608.23

$7,558.86 7,245.09 5,276.94 6,902.81 1,540.30

Group Expenditures: 1 = $5,630.09 f o r SQE-15 2 = $ 836.90 f o r SQE-13

. 3 = $1,141.23 f o r SQE-16 & 17

Geophysical Cost Breakdown by C1 aim

Geophysical work carried o u t i n the 1979 program was spread over Claims SQE 13, 15 and 17. Therefore, the $2,679.19 spent will be equally d i v i d e d over these 3 claims.

” C1 aims

SQE 13 SQE 15 SQE 17 Total

Geophysical Expenditure

893.063 893.063 893.063

2,679.1 9

W

L

C1 aims

w SQE 1 5 S t o r i e 3 West 1-14 Kon 1-3 f r a c t i o n Kon 3&4

S t o r i e 485 Kon 1&2 SQE 9-14

SQE 16-18 Kon 5-15 S t o r i e 1&2

Expendi tures

Dri 11 i ng Geol ogi c a l Geophysical Assay, etc. General Tota l

11 0,175.23 7,245.09 893.06 5,630.09 68,917.37 192,860.84

7,558.86 4,201.77 11,760.63

16,259.12 5,276.94 893.06 836.90 12,938.94 36,204.96

22,261.96 6,902.81 893.06 1,141.23 17,349.23 48,548.29 1,540.30 854.95 2,395.25

148,696.31 28,524.00 2,679.19 7,608.23 104,262.22 291,769.95

.

L

WORK REQUIREMENT BREAKDOWN

w Work Requirements (Years) Claim Name # o f Un i ts 3 5 6 10 Work Conducted

SQE 15 1 600 - - - Stor ie 3 20 - - - 34,000 West 1-14 14 - 14,000 - -

1,800 - - - Kon 1-3 f rac t ion 3 , Kon 3 & 4 2 1,200 - - -

51,600,OO 204,621.47

Stor ie 4 20 - - 18,000 - Storoe 5 6 - - - 10,200 Kon 1 & 2 2 - 2,000 - - SQE 9 & 10 2 - 2 , 000 - SQE 11-14 4 2,400 - - -

34,600.00 36 , 204 96 SQE 16-18 3 1,800 - - Kon 5-15 11 6,600 - - - Stor ie 1 & 2 25 - - 42,500

50,900 .OO 50,922- 69

Recording Fee - $5.00/$100.00 work Total Work Requirement- $1 37,100.00 Recording Fee - $6,855

38

APPENDIX V I

GEOPHYSICAL TEST RESULTS

OVER THE STORIE MoS2

PROPERTY, CASSIAR, B.C.

DECEMBER, 1979

L

L

Table o f Contents

Summary, Concl usions and Recommendations

1 n troducti on

Test Results

Chargeabi 1 i t y

Resis t ivi ty

Magnetic

Conclusions & Recommendations

Figures 1 t o 7

Page

1

2

3

3

3

3

4

( I n Pocket)

.

V

1.

Summary, Conclusions and Recommendations

Induced Polarization and magnetometer t e s t surveys have been carried o u t along three l ines over the Stor ie MoS2 Property. ab i l i t y response was uniform over the zone o f i n t e re s t and i s n o t expected t o be helpful in fur ther exploration e f fo r t s . be useful in delineating the zones of a l te ra t ion a n d f ractur ing, and indicated good correlat ion with the extent of outlined mineralization. Magnetometer t e s t resu l t s were inconclusive, b u t a more extensive survey i s expected t o be helpful in delineating the geology in more d e t a i l .

Charge-

Resistivity d a t a proved t o

A r e s i s t i v i t y and a magnetometer survey i s recommended t o cover an approximately 2 km by 1 . 5 km area as indicated on the enclosed plan maps.

2.

I ntroducti on

I n September, 1979, a b o u t 4 . 2 l i n e kilometers of Induced Polarization and magnetometer t e s t surveys have been carr'ied out over the S tor ie MoS Property for the purpose of evaluating the effectiveness of these methgds i n exploring the type of deposit under consideration. survey was conducted along three l ines which were 100 meters a p a r t and were oriented in North-South direction. The l ines were centered across a n area over which most o f the previous exploration ac t iv i ty has taken place. The angle between the Shel l ' s 1979 DDH Sections a n d the survey l i nes i s a b o u t 15 degrees.

The

Chargeability and r e s i s t i v i ty d a t a were gathered u s i n g a Huntec 7 . 5 K W time domain I P transmitter and a Huntec Mark-3 receiver. dipole array with a potential electrode separation ( a ) of 100 metres and potential to current electrode separations of 100, 200 and 300 meters were used ( n = 1 to 3 ) . Creek Valley a b o u t 1 krn Northwest of the closest s t a t ion surveyed. Measurements were taken normally a t 100 meter in te rva ls and the interval was reduced t o 50 meters over the anomalous areas.

A pole

Inf ini ty current pole was grounded in the Granite

Magnetic survey was carried o u t using a Scintrex MP-2 proton magnetometer which has an accuracy o f +1 Gammas. 25 meter intervals . About 400 meter s t re tch a t the Sou th end of the l ines could not be surveyed due t o disappearance of s t a t ions under snow l a t e r in the f a l l .

Readings were taken a t

3 .

Test Results - Chargeabi 1 i ty

Chargeability values .ove'r the area o f interest are qui te uniform indicating a more or less uniform su l f ide dis t r ibut ion within the in t rus ive . There are no chargeability anomalies which can be correlated with the zones which contain the molybdenum mineralization. increase t o a b o u t twice the background value close t o the S o u t h East end o f t he g r i d indicating an increase in the sulf ide content of the underlying rocks or a change in the rock types. the main intrusive a t the Sou th end of the l ines has been pointed out by W . Smitheringale, which i s in agreement with the survey r e su l t s .

Chargeabilities

Existance of a d i f fe ren t phase of

Resistivity

Apparent r e s i s t i v i ty values obtained over the extent o f the zones which contain the MoS mineralization are a b o u t 5 to 10 times l e s s t h a n those values obtained $lose t o North and S o u t h end of the l ines outside the mineralization. Apparent r e s i s t i v i ty lows a t a l l three separations indicate a good correlation with the intensely al tered and fractured zones which are claimed to be controlling the MoS Lowest point o n the r e s i s t i v i ty prof i les gradually s h i f t s &ward North as the electrode separation i s increased from 100 meters t o 300 meters, indicating a d i p for the low r e s i s t i v i t y zone in the Northerly direct ion.

mineralization.

Unaltered grani t ic rocks have r e s i s t i v i t i e s usually in the order of several thousand Ohm-meters. among the a l te ra t ion products of an intrusive, have an average r e s i s t i v i t y o f a b o u t 30 Ohm-meters. a resul t o f a l te ra t ion would tend t o decrease the r e s i s t i v i ty d ra s t i ca l ly .

Kaolin and other clay minerals which a re

A n increase in clay content o f an intrusive as

I t i s believed t h a t the increased conductivity as a r e su l t of increase in clay content and presence of e lec t ro ly t ic conduction as a resu l t o f intense fracturing within the mineralized zones, are responsible for the apparent r e s i s t i v i ty lows obtained over the intrusive.

- Magnetic

Magnetometer survey resu l t s a re noisy in character ref lect ing a n e r r a t i c dis t r ibut ion of magnetic minerals within the intrusive. Magnetic variations in the order of a few hundred gammas within a distance of 50 meters are common a s can be seen on the enclosed prof i les . This high degree of variation i n the response i s believed t o be due to intermit tent destruction o f original magnetite as a resul t of intense a l t e r a t ion , and possibly introduction of younger magnetite along veinlets a t a l a t e r stage. Lack o f overburden and surface weathering are believed t o fur ther enhance the var iabi l i ty of the mag response.

C

4.

There i s a weak indicat ion of a magnetic trend marked by a low on the magnetic p r o f i l e s over the zone of i n t e r e s t , b u t th i s p o i n t can not be emphasized due t o short length of l i n e s a n d lack of information on the magnetic background 1 eve1 . Conclusions a n d Recommendations

The r e s i s t i v i t y d a t a obtained over the S t o r i e MoS2 Property ind ica tes a c l e a r l y defined r e s i s t i v i t y low which c o r r e l a t e s well with the zone of i n t e r e s t . I t i s believed t h a t the r e s i s t i v i t y method will be useful i n del ineat ing the areal and depth extent of the zones o f a l t e r a t i o n and intense fractur ing.

Chargeabili ty data d i d not contain any anomaly which could be r e l a t e d t o molybdenum mineralization.

Magnetometer t e s t r e s u l t s should be considered inconclusive, s i n c e the survey extent was ra ther l imited and covered only about half o f t h e area which was or ig ina l ly planned f o r coverage. ground magnetometer survey i s expected t o give useful information related t o s t r u c t u r a l fea tures , l i t h o l o g i c units and the degree of a l t e r a t i o n .

A more extensive

I t i s recommended t h a t an approximately 2 km X 1.5 km area as indicated on the enclosed maps should be surveyed u s i n g the r e s i s t i v i t y method. a t a l i n e separat ion of 100 meters.

Total length of the l i n e s t o be surveyed would be about 32 km

The same area should a l so be surveyed by a magnetometer i f f u r t h e r geologic invest igat ions i n the general area warrant such a survey.

5.

Y Estimated c o s t s for a 32 l i n e ki lometers of survey i s a s follows:

I tern

Line cu t t i ng

Unit Cost

$ZOO/ k m

R e s i s t i v i t y equipment $600/day and people

Total Cost

$6 , 400

25 days (3 $600/day $15,000

Accomodation for $40/day/person 25 days 8 $160/day four people 94,000

T o t a l : $25,400

Contingency 10% $2 , 540

Grand To ta l : $28,000

A n add i t iona l $3,000 would be required t o do t he mag survey.

Res

A.

z

W

13.2

13.5

e

13.5

13 .*9

e

11.2 e

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~-

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12 -2

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8 . 8

e

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13.5

0

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2 9. 6 e

15.0

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la.?

13.6 e

0

1 1 . 8 e -

*

12.1

- B. L.

f5 .5 3.8 12. I 0 0 e

16.6 e e

1 2 . 5 13.5 0 .o 0 e

e 0

18. 6 18.4 17.9 e

21. I

9 . 9 15.9 35.4 0 e e

28.7 e

26.8 27.1

N

POLE DIPOLE ARRAY

a = 100rn

CASSIAR B.C. STORIE MoS2 PROPERTY

APPARENT CHARGEABILITY VALUES (IN MILLISECONDS)

n = 1 SCALE 1:5000

21. I 19.7 0 DEC. '79 S. SAYDAM

F i g 1

--

--

-_

-. 14.4

-. 15.5

15.9

J6.

--/6.2

14.6

lo. 3-

17.5

20.1

16.Y

14.9

26.6

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.Is. 0

- 1 7 . 2

I62

15.4

N

15.0

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5.9

77

1 7.t

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B. L

POLE D I P O L E A R R A Y

PI na

a = 100 rn

CASSIAR B.C. STORIE MoS2 PROPERTY

APPARENT C H A R G EABl L l T Y V A L U E S ( I N MILL ISECONDS)

n = 2 SCALE 1:5000

DEC. '79 S. SAYDAM

Fig 2

T

--

--

s -

- - 15.0

-- 16.9

-

-- 13. I

--20.5

17.3

--2/.4

--

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--

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8

IS. 7

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N

POLE DIPOLE A R R A Y

a = 100m

CASSIAR B.C. STORIE MoSz PROPERTY

APPARENT C H A R G E A B I L I T Y VALUES (IN MILL ISECONDS)

n = 3 SCALE 1:5000

DEC. 79 S M Y D A M -

Fig 3

U

w z

r

- N

D0+9

- N

OW

S

. N

OO

+t

NO

O+&

NO

WZ

NO

W1

DtO

sow 1

soO+z

SOW

E

SDo+P

< C > < (I

(I

a c C P

U

d c

.- U

- 19 -

loo-

120-:

DDH 79-3

~

I I

I

I

I 1

1 1 I

1 I

Number of MoS2 Fractures 0 IO 20 0 335 .IO .I3 20 23 30 .33 .40 -45 .so 33 bo .63 -70 .IS .eo .e3

MoS2 Assay Values (%I I I

260

220E I

1 I

I

I ' I

260 240e 200

I I

I

300

320 I I

I 340

360

EOH I

280

300

20

40

60

80

I - 1 I

I I

I ' 1 - 1

340-

I40

- c

E

s

Y

I00 f n

200

220

I ' 1

1 1

I I

240 3

197

EOH 3mi

FIGURE 12

S H E L L C A N A D A R E S O U R C E S L I M I T E D

EXPLORATION - MINERALS

CASMO MoS2 PROPERTY I CASSIAR, B.C.; LIARD MINING DIVISION

DOWN HOLE.HlSTOGRAM OF I NUMBER OF MoS2 FRACTURES I

81 % MoS2 W. 0. Smithrrlngalr 8 Aimciator Ltd. lDa'o: FOR 8, 1980

W.G. SMITHERINGALE & ASSOCIATES LTD.

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