Township OF ASHMORE Work performed by: HOLLINGER MINES LTD ... · Work performed by: HOLLINGER MINES LTD. (WILSON s KALSON OPTIONS) Claim NQ TB 229617 TB 229616 TB 10971 TB 139353

42EieNWei45 16 ASHMORE 010

Diamond Drilling

Township OF ASHMORE Report NQ: 16

Work performed by: HOLLINGER MINES LTD. (WILSON s KALSON OPTIONS)

Claim NQ

TB 229617

TB 229616

TB 10971

TB 139353

Hole NO Footage Date

A-14-73- 790' June 11 3

NoteA-l-70 'A-2-70 -A-3-72 :A-4-72 -A-5-72 -A-8-72 :A-10-73 -A-12-73 '

A-6-72- 'A-7-72 '.

A-9-73A-ll-73 -

642'323.3'443'494'448'301'402'491'

492'302'

302'301'

Aug/70Nov/70Jan/72Jan/72Jan/72Feb/7219731973

Jan/72Jan/72

19731973

(D(D(D(D(D(D(D(D

(D(D

(D(D

(2)(3)(4)(4)(5)(5)(6)(6)

(5)(5)

(6)(6)

(l) (6) (7)

Notes:

( . .. ) date placed on file(1) (May/74)(2) 145/70(3) 228/70

(4) 6/72(5) 22/72(6) MEAP GB #33 (cross-sections only)(7) 102/73

AWL.004(r-69Jrev.9-7-2

iyxii'iiiit

. A 3 /S rt Q&jZ

Location of

A"

t

c PA,W2? from w,*p * on West Side of Claim TB 22961? ,^LO t,o. M^——.f ̂ ?'D|AIVIOND DRILL REpORTEAST. -*.ELEV. —— AZIM. DIP -

HOLE NO. COMMENCED.

/ -l

. ,. -, .100 'C' PURPOSE OF-

HOLE ———-—-.

Claim TB 22951?'

FROM

0

A3

1U

137

\*^

kX*

TO

Ae

115

-137

331

DESCRIPTION

CaoinK

Clroy r,ro(in n^iiuivo non na^nntic

Amiocito uniforn app. to coro

i'cldspar Tor. ('roy to ^-Toen

v.ith incr. in chlorito riuriorous plwnocrytv

of feldspar 2/10 of mi inch in ciia.

throughout aoBtioa.

Cwtfjcto (-round 23' C'ol of I'orphry.

Harvlod chloritic "uff or !"od. brov;nioh

b-rJ!icio rica? nml ^.roon chloritic b'lndn

ioc-'.Ily rdn \-'ith Pyrr Ty -*- chalco

bnruiin..- ' ' rtOO to 60 to i". A.

2 f l^icitic band at 157.

162* sn. blebs 1'yr. oba.

170 am blobs of pyrr. oba.

190 - 261 nottled

Lt. col. D-icitic Tui'f?

it 264' chorty section ninor pyrr. and

c lin le o

FROM

f '

3

170

192

2A2

261

ccTO

170.5

193

2AA-5

26A

)RE SAMPI

RECOV.

.5

1.0

2.5

3.

-ES

WIDTH

B

1.0

2.5

3.

ASSAY

50'

9(1 '

157*

215'

315

DESCRIPTION OF SAMPLE

l* f r.r'd Amesite

n-,)!j r. ij'netic

rattled fins fr'a nd ;;.-,i;.e

non n 'f n otic

I acite It. col. bracci ted

I'oitlftci ^nd or d-ic.tte?

! 1, cherty section '~yrr.

-

c: hi b -md :'yrr -*- c ha le o.

Vr?ry n.-ii -K-tic

/i" r.ass Tyrr * Py minor :'nalc

, ; tz. ;;trs. 30 to .A

bleached section yollow

" ^ricitic

Chl. band I'yrr * chalco

11

FORM S22

NORTH ——. EAST. —-. ELEV. —— AZIM. -—— DIP ____-

DIAMOND DRILL REPORTPROPERTY __ i.IL. : /; orVIO'I - I'iOh

HOLE NO. COMMENCED. FINISHED--— PURPOSE OK- HOLE-

r.Vp.

FROM

Wfn1970

ilL^iiilii.

367

402,

TO

W

404.5

442

DESCRIPTION

rosaivo speckled AncJeaito fine (;r'do

c intict ?it 70 to RA

Dk. fra..'Roritfil Andesite nun niifnotio

iiO niu.

I'aoo. elk. t', f* Anclnnite opockled app.

t.j core n-jn ni'i 4 notic.

.FROM

264.5

269.5

?79.5

2;!4.5

2^7.5

2?t9

315

323

!,64

ccTO

269.5

274.5

279.5

2^4.5

2^7.5

2*59

293.5

urt

32fl

465

)RE SAMPl

RECOV.

5.0

5.0 '

5.0

5.0

3.0

1.5

4.5

1.0

5.0

1.0

.ES

WIDTH

5.0

5.0

5.0

5.0

3.0

1.5

4.5

3.0

5.0

1.0

ASSAY

i

f DESCRIPTION OF SAMPLE

r.liwrty chl. ection

1 inar pyrr. V.L. chaico

''inor pyrr. V,.,. c.v'dc^

rinor i*yrr. C. L. c::ilc3

Very little riner.il

band of Pyrr ririor ch-ilco

1" nearly mss Pyrr. * i y

r.iinor chaico

vftry little nin.

ciil. section

f T ir .uruunt o!' Fyrr ch'ilco

in cectijn Udert y

l,ao:.'l streaks of lyrr rinar

chalco.

fdss. ryrr * r^alco

/l.

NORTH.— EAST. —— E LEV. -—— AZIM. —— DIP ____

DIAMOND DRILL REPORT*'I'--'-OH U''TI )H - /isl-j-i

HOLE NO. COMMENCED.————..FINISHED---—^——. PURPOSE OF—————. HOLE___________

-

THUNDER BAY"" ni.'iirjo ,-Jivir.iOfi

iJflhCHf fc TTSEP 10 1970

WA PM

7j8!9|10|l!jl2| 1^3^5,6

i

FROM

U2

Ufl.5

t "-7.5

501. J

607

TO

.M. 5

4*7.5

501.5

6;;?

620.5

DESCRIPTION

6.5* Cherty Tuff

Dk. sp. ftndcnito

Fine f,r'd reta-Tuff-.".ed

bnr.ilinr -? 60O to C. A.

f-' ne, a highly Alt. Ant'i-site

r'in with pyrr ninor

chalet)

572' cherty bands tf 500 to C. A.

Bluish c bort: fractured

and brecciated minor min.

01';. 5 - 619.9 Breccia

"radation to amygdaloidal

,'iii. Andesite wall rein

highly nartifttic pyrr.

arid chalet) ffttn

FROM

497

502

517

522

5*7

532

537

572

575

577

579

587

592

597602

607

612

617

619

622

ccTO

502

507

522

527

532

537

5L2

575

577

579

582

592

597

602

607

612

617619

622

624

)RE SAMPL

RECOV.

5

5

5

5."

5.0

5.0

5.0

3.0

2.0

2.0

3.0

5.0

5.0

5.05.0

5.0

5.02.0

3.02.0

-ES

WIDTH

5

5

5. c

5. c

5. f

5. t

5. C

3.'

2.(

2.(

3.t

5.t

5.1

5.'

5.'

5. C

5. t2.(

3

2

ASSAY

0

0

DESCRIPTION OF SAMPLE

V.L. vin.

Highly Alt. dies r-yrr.

: ;ias. ! yrr. Mt. .lection

2 en qtz. strs. r yrr in

section

3 arc qtz. stra. n.n

sections

Hin. .net. cherty V.L. min

fair ar-.^unt of i yrr. in Ut.

.'flction ninor chnlc'J

2 1 chort bines

Disa. Vyrr. fin. chart b.mus

."in. with ! yrr * c.Tilco

i^iss. 1'yrr minor ciialco

iyrr. tain., vdth chalco

i;iss. I'yrr. minor ci.alco

r " qta. i;tr. win sect.

i'iss, iyrr in 'ect.

Thirty b^ncJa V.L. min.

.1 ii ' ,. ft

Very little nin.

V.ell nin action i yrr -tchslco

Tin. diss Tyrr some chalco

FORM S22

EAST. DIAMOND DRILL REPORT* ELEV. -^

AZIM. — DIP ——— PROPERTY-

,.;-j;i OPTI r; - ,\.;-.v. s

HOLE NO.COMMENCED-FINISHEDPURPOSE OF— HOLE_______

FROM

620.5

TO

Gl,2

DESCRIPTION

U-k f;roon silicified amygdaloidalotuiosito well ciin with

!'yrr. -m. clmlc;) pyrite

6jJ**6it2 micaceous section rum rricnotic

.-6^2 r!il) OP IDLE

x' '^'^ yna^fo^+jf^

HOlUNfiER-M!NES-i!MHfl ———————————Tiiiiiitip nuTADin.TIMMINS, DNIARIU

-

CORE SAMPLES

FROM

)2n

\?.7

•29>32

^4

TO

627

629632

632

RECOV.

'1.0

2.03.0

2.0

WIDTH

3.0

2.0

3.02.0

ASSAYDESCRIPTION OF SAMPLE

i pll f)i!! T VlflRt ?:-fCt-i^1

spjts pyrr * chslcov^ry n .. rv- tic

i-.all nin not so rmch chi.icoViri. vith pyrr * ch.-iicoVery li'.tl^ n-.in.

THUMDER'bAY" .

iEeeiifiHpSEP 10 1970

7|8|9|10;1!|12|I|2|3|4|5|S|

i

*^SiSK

^:i ̂

^^.feiiA

l^rf^fcf^asM

ate

s- WA ^

•,', f. t//''M'? v Q i t.'/,,,-. - *j i -- ' a- tt Y -' - i ' i -'

f/'-^l'' //6\'//;1U^ ' V-i—,-

7

r

9 P Z Z

MjUwWM

DDH f Al, A2, 1^3 ft. M -Wave previously

DDH # A5 coaaenqed Jan. 22/72 Finished " 24/7^

A6 Commencd Jan Pinishe

DDH ^ A7 Comcaenc Finis]

nee* Feb. 2/72 Ishedl " 3/72

- Bradley Bros. Ltd. Timmins, Ontario.

Dia. of Core :- 3/16*

-a--74

VS.-'

yz-t;

NORTH EAST. —— E LEV. —— AZIM.. DIP

00 -i- HOLE NO.i "j *n " '

IAMOND DRILL REPORTPURPOSE OF

loo*; PROPERTY-

TS- 2. Z tt'7 !. t."facle'v~!Trj'3.

FROM

0

20

30.5

49.7

TO

20

30.5

49.7

71.6

DESCRIPTION

(!ua ing

nilicifted andesite fra/oaentul . The

fragments are very snull-lesn than J"

and cenorally obscure the franmonts are

siliceous. The andesite is dork preen

to. grey,.. siliceous, chloritic cut by quart

carbonate stringers* No ninornlisfition.

Amygdaloidal andesite - amygdalos are

locally well defined - rounded to elliptic

in shape and either siliceous or filled

with chalcopyrite and pyrrhotite.

There are also strin^ero of pyrrhotite

and chalcopyrite in this section.

The andesite is weoniah to ere y withchlorite and silica and cut by

quarta-CO.j stringers.

Aniieaite i'rafTaontal-probably a tuff

ainco the f rapnonts are very snail i"

in size. It is separated fron the

ipiypdaloidal andenite wainly on the

basis that the framents ere very

anr.ular and siliceous in nature* Also

them does not appear to be any roplnccner

or fillinr of the frafjient structure by

pyrrhotite and

chalcopyrite. Instead the mineral

CORE SAMPLES

FROM

i

al

45

i. j

70

TO

50

72

RECOV. WIDTH

5

2

ASSAYDESCRIPTION OF SAMPLE

-

Anyfdaloidal andesite Cp t Po

for Cu, Hi, Au,Ag

l,^K^.^y-,M^^L[/^^'

\,H r'?r:i4'MQ ^iUlOjSiJ;:,/!.!-;, i., ."^-Jii-JiL?l''J'*i5j5/

A

Lower part of fragmental Vv.

Po-Cp section

FORM E22 NORTH——. EAST, -—— ELEV. —— A2IM. —— DIP ____

DIAMOND DRILL REPORT

PROPERTY- lv TO'.:HSHIP

HOLE NO. COMMENCED. FINISHED——. PURPOSE OF- HOLE————.

FROM

71.6

79.4

90.7

TO

79.4

90.7

L05.4

DESCRIPTION

j ci sinply oissoninated and localized

o stringers. From 49. 7 to 55

.radational contact uith the frumontal.

71-71.5 near maoaive (section of

jyrrhotite and chalcopyrito-noatly

pyrrhotite.

'ono of nixed chort und amygdaloidal

"aterial. The amygdaloidal sections

aliow abundant po and aono cp completely

filling; tho amygdales.

such are: 75-76.3 77.3-79.2

Tho chort is vory d-irk and hard

j.t is brownish in colour, no mineral or

very ninor py along shears. Of ton

fractured and filled with chlorite.

Andesite fra^nontsl - tho fra^raonto

iro Ip.rncr hore |" size and only

Locally were defined. Thoy nay be either

:hftrty or chloritic. The andenito is

rreen in colour, fine frained with

ibund'int chlorite - cut by snail quartzcarbonate stringers.

Another aone of brownish chort-

fractured with chlorite, epidote and

quart z -c arb onate .

FROM

75

ccTO

77

1

IRE SAMPl

RECOV.

-ES

WIDTH

'

2

ASSAYDESCRIPTION OF SAMPLE

Some chert and amyfdaloidal

rnterial Cp To in anygdalticlal

.

j'^J.-v'^i-S^Tfj i/ij' ' f^ if, li W [c ii j)( "f r t si- / '•i/ci1 A\l ' '-J l - I"'U

^ii^^i^ipffj—————————— t ——————————

FORM SC2 NORTH —— EAST. —— ELEV. —— AZIM. . DIP ————.

DIAMOND DRILL REPORTPROPERTY- ASHMORE

HOLE NO.COMMENCED,FINISHED-—.PURPOSE OF- HOI F

A-2-70 3.

FROM

105. t

U9.t

23S./,

TO

UQ.i,

233.1

r

248.7

DESCRIPTION

Ant! e site fra&tvmtal - fra/jRanta are

around ^" size and vory numerous.

'i'hcro are chorty, chloritic, epidote and

sillc80U3 typos* Vho clvirty snf* sillcooustypes of frafmanto may bo separated

uinco tho corty typos ixro i^ttyioli ^^ fcrownand nearly clear while the siliceousfrnrrionto are a bleached white colour

and noticeably different. Thore are

numerous small chert bands cutting thecore as v/ell (i rt acrosa) 113-125 asilicified zone where t hore are not asnany fra/unents aa surrounding. Theandesite is Kreenioh (dark) in colour.:!o nin.

Zone of weakly anyjTdaloidal andesito119.4 152.3 eradutional contact with

above. Generally the andesite looks

ascive to a medium grained variety with

occasional anyfidaloa filled with po and

py. i'he andesite is {'roon, contains chloi

cut by qunrtz-COj otrinKcra.197.6 - 200 - anall chnrt breccia

Zone of chert as before - brownish incolour.

FROM

'

LtA, ——

GC

TO

)RE SAMP1

RECOV.

-ES

WIDTH ASSAY DESCRIPTION OF SAMPLE

1 i ' -' r T:;-;-' 'pXv"

iW^^v'i^L n;:r H HO ".

•httfii-W^wij^firfli

FORM S22

NORTH— EAST. —— ELEV. —— AZIM. ——— DIP ————

DIAMOND DRILL REPORT

PROPERTY- ASiiMOltE TOWilSHIP

HOLE NO. COMMENCED- FINISHED- PURPOSE; OF—HOLE————-

A-2-70

FROM

?;rt 7

2i'0

2fl2.

300.4

30^.1

TO

?ftn

2*2.9

9 300.4

304.1

323.3

DESCRIPTION

y.ono o.'" coarae {'.rained andesitehornoblendo -carbonute-chlorito Schist.

Schistosity at 55 to Core Axis

^roen in colour, cut by quartz carbonate

chlorite stringers.I'one of brownish chort a&ain.

Andefjito fr-ncnontal-fragmnts aro

J" in s J ae and often obscure, occurring

'j s siliceous or chloritic p^tehnsrinned by chalcopyrite nnd pyrrhotite*Chero io uune Cp and To dissjeninntcd

throughout and some ciineraliaation in

the quartz-carbonate etrin^ora. There isabundant chlorite und oome epidote.

('one of chert - crean coloured and locally

;)rocciated-gradea into lowor eone- no

lino ra li nation.

Anyfdaloidal anriesite-very

ainilar to tho pievioua horiaon witht

C p and Po in tho anygdalna and ala o in

lenses and disseminated throughout.

/Vr.yrdales locally woll defined-anall 1/fJ"

sise aone pyrite may be found in strinfiors:ir. well.

AT/, /C5 attMHtLusHOlll^OER KiJiS LIMITED

FROM

2^5

315

ccTO

2<X)

320.

)RE SAMP1

RECOV.

-ES

WIDTH

5

5

ASSAY DESCRIPTION OF SAMPLE

Andesite fr-ipaental cp, Po

Anygdaloidil andes, Cp, Po

!

L Jp^'-vK^'lIfiJ''.- 1.!.'' 1 '™ .-.J

————— i ——— ,,^.,.,,, , ,,.... .,..r/MM/NS, ONTARIO

N\

-v.

LEGEND

ALGOMAN

Ng — Feldspar (Albite ) Porphyry

Ki r- Gabbro ( Hornblende)

KEEWATIN

A2 SP Andesite

bx -breccia

Shearing

Topographic Feature

TR. - Trench

JTS. - Joints

; \ Esker

, JTS

HAS ELI AZi DIP

xl 2K LHAIVIUNUv ?yrfac*M ..80"

CO Tar © 4" PBOPFBTV VJTTi3)*300 — L.5 o "Aij

FROM

0

60

-

TO

60

342.:

.DESCRIPTION

Casing

Andesite - dark green - fairly haichloritic and siliceous - locally carlsections which are slightly more browr

in colour. Locally there are small

quartz-carbonate stringers. @ 62 and@ 67.5 there are a few chlorite blebs

in the core, which is somewhat leachecin these two sections. Mineralization

at the first is practically negligibl*only rare splashes of py.

186.1-204 Much more siliceous bamIt is not a chert band though - fairly

hard, black. Sulphides are very minorbut there is some cp.

190-200 apparently there is some

lost core - it is broken up here butno evidence of a fault is indicated.

At 204 the rock is less siliceousand mor* andesitic in appearance. Aft 1

a short zone of carbonatization, the

mineral consent increases, around208.2. The reck here is identical to

the rock @ 2 50 in DDH A-4-72, except

that the mineralization here is mainl

disseminated, flhal ropyrit* pnnt-.*nt. i n

UK ILL MtKUKI FINISPUR! HOU

SON — OPTION #1 ———— ——Ashmore Twp.

•M™ TanuarJ ZG/^STftsr. F-yr.ftnsion of

rnnn^r 7.on(* and ma?.

Drilled by: Bradley BrothersCORE SAMPLES

FROM

donatizish

-

r

208210

TO

ed

210213

RECOV. WIDTH

2

3

ASSAYDESCRIPTION OF SAMPLE

A2C03 - 10^ sulph. Tr.cp" - 7fi sulph. Tr.cp

FORM B22 NORTH —- EAST. -— ELEV. —— AZIM, -—— DIP ____

DIAMOND DRILL REPORTPBQPFPTV WILSON OPTION #1 ———————————

Ashmore TWP.

HOLE NO. A-3-72COMMENCED——-——-———— FINISHED——————.-——————PURPOSE OF- HOLE______

FROM TO DESCRIPTION

very minor - The main mineral is

pyrrohotite and some pyrite. Totalmineral - 7-10# Even with 5-7# po

the rock is only slightly magnetic.

This above rock gradually gradesback to a carbonatized andesite. fh~e

pyrrohotite also becomes more magnet^

around 230. The mineralization graduitends to change to a more throughgoirstringer type of mineralization, Thei

is also a gradual increase in copper

content, although pyrrohotite andpyrite are the major minerals present

Where there is a larger amount ofsulphides, the pyrrohotite is genera!

much more strongly magnetic.The rock changes gradually from

silicified to carbonatized zones

throughout this entire section.Around 283 the mineralization

is in the form of both stringers anddisseminations, and increases to

approximately 7# sulphides overall.

The sulphide content remains highuntil around 321, where the mineral

content decreases rapidly. As previo

CORE SAMPLES

FROM

215

220

225

234240

c 249

ryS 255e

4

ly285290

295300

305

310

315

*,

TO

220

225

230

235

245

250

260

290

295

300

305

310

315

320

,

RECOV. WIDTH

555

.151

5

55555

5

5

ASSAYDESCRIPTION OF SAMPLE

Cu,Zn,AgA2C03 - 7J6 Sulph. minor c p

n .556" it cp

" - 5# " " cp" - 756 " " cpn . 5*j H n Cp

" - 5jJ " some cp

n - minor Sulph. vis cp

.

" -105S Sulph 1^ cpn - 3jJ Sulph. smell cp

" - 5j5 " minor cpn . 5^ " " cp

11 - minor Sulph. no

visible cp" - 7-10J& po py very

minor cp" - 7-lOjJ po py neg. c p

FORM 122 NORTH EAST. — ELEV. —— AZIM. —— DIP ____

DIAMOND DRILL REPORT

PROPERTY- WIESON OPTJ.QN j lAshmore Twn-

HOLE NO. A-3-72 ...3COMMENCED-—————————————————FINISHED——————————.————————.PURPOSE OF————..^-——.———.—.——— HCil F -——-—-.———.-...-—....————

FROM

3.42.2

TO

443

DESCRIPTION

most of the mineralization is pyrite

and pyrrohotite, with only local splaof chalcopyrite. This zone is the mos

strongly magnetic. There is also some

biotization developed.Around 321, the rock grades to a

dark green, unmineraliaed andesite -it is chloritized and carbonatized.

Diorite - grey in colour, with

numerous feldspar phenocrysts (ormetacrysts) developed - often feldspa

shows minor epidote alteration. Silic

Weakly magnetic in the presence of sp

- being po and py After 360^ theredoes not appear to be any pyrrohotite- only very minor pyrite. Here the.

rock gradually becomes more massive awell.

387-394 strongly carbonatized zor

only vestiges of feldspar crystalsremain.

394-405 massive as 360-3^7

@ 405 the diorite becomes more hi

altered with a much higher epidote coSome of the feldspar crystals are sta

reddish by iron, while others ara

CORE SAMPLES

FROM

she s•'

n

Lfied

irse s

j

! -

'

Shly

itent.Lned

TO

alphid

RECOV.

es

WIDTH ASSAYDESCRIPTION OF SAMPLE

FORM SSl

NORTH EAST. —— ELEV. ——- AZIM. -—DIP ____

DIAMOND DRILL REPORT

PROPERTY WILSON OPTION

HOLE NO. COMMENCED. FINISHED—-- PURPOSE OF- HOLE-—————

A-3-72 * . .4

Tvm.

FROM TO

443

DESCRIPTION

completely altered to epidote. The

rock now is a limey grey-green asopposed to the original grey colourof the earlier intersection. As befo:

some sparse pyrite.

End of Hole

HGIHTa ft&S LiDEi)JIMKINS ONTARIO

-

*

CORE SAMPLES

FROM

e

TO RECOV. WIDTH ASSAY DESCRIPTION OF SAMPLE

FORM M2 NORTH EAST. —— ELEV. —— A2IM. —— DIP ————

DIAMOND DRILL REPORT

WILSON OPTION #11———— Ashmore

HOLE NO. A-3-72 ...5COMMENCED-——.^—...—-—™—.————. FINISHED^-—————.^.-————.-——.— PURPOSE OF__________________.——— HOLE___________________________

FROM TO

62

100

150200

250

300350

393438

DESCRIPTION

SAMPLES FOR THIN SECTION

Andesite - a few chlorite blebs in a

zone which is cut by a short quartz-carbonate stringer with wall rock lea

Andesite - dark, chloritic, siliceoue

Silicified and carbonatized andesitezone of dark silicified andesite

Carbonatized andesite with po and py

Carbonatized andesite, po, magneticGrey silicified diorite

Carbonatized dioriteAltered diorite - some epidote

* .

CORE SAMPLES

FROM

:hing

TO RECOV. WIDTH ASSAY DESCRIPTION OP SAMPLE

O/yts. P.Ct/t^tf/itk^pii?!RFR r;:;^ OED

NllUKIHS, ONTARIO

f--T3 t3 fD

FORM O2

AZIM. .

. '.r

1 0,-.-i /T

— 5-rr-t-rc-f: di la r

r ~ /, i *

3'i?'f -ice." IrV"

Lt-L-Li, 0

DIAMOND DRILL REPORT

PROPERTY- /JOlJ GFTIiJ!- ..''l

HOLE NO. COMMENCED- FINISHED___ PURPOSE OF- HOLE————

_____ , A s h" o r r: Tovnphi

FROM

r,l'l

TO

-V337

DESCRIPTION

C n ^ i n c*The rock is best described as or

andrsitic flow, although there are a

vide variety of charges in the rockitself. For thn r.ost pr.rt the ar.d^sitf

io dark groen end fairley "*ssivf;. It

is chloritic tind ^enorally highly

C 9rborinti aecl. Thor-'; a re a few s." -fell

qxiartz-carbonnte Gtrin^ors v.'hich

locally show loachin^ and silicifcr-t

into tho surrotu.dinr rock. Locallythe andesite ^rc'.dcs into n member

vhich is corrpo.sr.d of nunr-ronr. blebs

of chlorite. Ac theso bleb? brcon'O

larger thoy appear to bc altered fr.^

Th?ro is n S':."'ll a: ount of epidot.f;

"iRsocifted with thir unit P. s veil.

This rrprrbf-r ir- pro^ir^nt fror^ ICO-l?

"."isll ci..- t of pyrite : 137

A zone of strong c.-rbonitiaetion sta

'•:' 14^, rock is d i rk 2r0(?n in colourand prfdop to a much li^htrr 2rr""in

'vith increased, car'ionate ccntfnt.Around 15? start to 2 Qt a ruinor airou

of dir-sernirct^l riyr.it o witli about 3;'- disseriinated pyrite -: Ifi/,-]/)?. Here

CORE SAMPLES

FROM

i. on

y - ftiits

-t p

\t

TO RECOV, WIDTH ASSAYDESCRIPTION OF SAMPLE

'

FORM (22 NORTH EAST. —- ELEV. —— AZIM. —— DIP ————

DIAMOND DRILL REPORTHOLE NO. * COMMENCED—— FINlSHFO PURPOSE OF— HOLE—————.

PROPERTY-Ashi or'H T.-: r -,

FROM TO DESCRIPTION

there are occasional splash??, of cp

with the py, hut or.ly a ve rv minor an164-173 Short chert band - con

are diffuse pince th^ andesite is silat the contacts. F.inor py in first

chert bc,nd(or flow top) at the contacotherwise barren. Colour is nark grey

black.After the chert band the andesi

again highly carbonatized; the firstoccurrence, of po is noted h(-;re - only

weakly ra^netic though.

Around 200 the alteration is qu

strong and lc.t"r around ? 25 thn rockcrudely ba-'d^d in layers of alterati

at 6C 0 to the core axis.- nairlybrownish carbonate a::d chlorite.

After 175 there is j'-rerplly ssulphide tninfirali nation throughout.

ov fi r,?ll py-3/^ - in Isr^e clots,

in stringer fillir^s, disseminations

and alon^; s hoar planes,po - ninor - usually associated

with small clots or blobs of py.

cp-ninor may bo disseminated in srnal

splasher, - m rely alonr ;-ir, a 1 z.r?cr

CORE SAMPLES

FROM

Mint.•-acts

cifie

' ito

.e is

164

.tee

)n

llliS

TO

16?

'

RECOV. WIDTH

.

3 '

ASSAYDESCRIPTION OF SAMPLE

3^ dipi-CBiin.-trd r-, :-.ir.rcp in cc-r'horati W'-T! A?

NORTH EAST. — ELEV. —— AIIM. ——DIP ———

DIAMOND DRILL REPORTOPTIC,;; '

HOLE NO. COMMENCED FINISHED-— PURPOSE OF HOLE——

FROM TO DESCRIPTION

bleb, since usually found with py

either vith or without po.213. 5-214. 5 ~ sreill white chert '

Around 230 the cp content begins to

increase - still in the. cfrbonati^odandesite .

cp is the ne in mineral here - upto approximately 254.

- 239-23/4. isolated stringers andblobs of cp. I ~2fo o verall

- 234-~49 very rinor cp

- 249-25C chert, white250-254 numerous small stringers

of cp w/w'out po approximately 5;a cp

254-265 brownish, carbonatised,andesite - blobs calcite, numerous

blebs cp, po, some py locally along

shoars especially pfter ?57*5

some biotite? small xls. tfiay be Zn.

265-271 mainly stringers of cpa^sin, FOP. e po - rock grades back to

more ^rey green cftrbonatized andesite

2?l-274 srey green carbonati?,edandesite. Only one small stringer of

275-276 sorne brownish carbonate' 4^ cp

CORE SAMPLES

FROM

2200and

230

250

252254

258

25926C

265

270

275

cp.

TO

235252

. 25425?

259

260265

27C

275

276

RECOV. WIDTH

52

24

1

15551

ASSAYDESCRIPTION OF SAMPLE

s:r:?ll c]ot of vty ir.calcite - Groche*1". f. au

Cu,"n,AsA2-C03 -2;'- cp

" -5?5 cp 3^ TO

" -2-3JJ cp 2,1 po" -minor cp, po, py

" -4; J cp, 4;^ T O py" -].5/' cp rilnor po pyI! -2-3;1 c p 4;' py po" -l-2;4 cp 5;: po py

" -;::' nor c p

" -4!?. CP

rORM Ut NORTH—™ EAST. —- ELEV. —— AZIM. ——. DIP ————

DIAMOND DRILL REPORT

PROPERTY- OPTION

HOLE NO. A-4-72 COMMENCED—————————.FINISHED——————————PURPOSE OF————————HOLE——^—-—————-———

...A

FROM TO

1

DESCRIPTION

276-291 mostly grey green carbonatize

andesite, local blotches of cp with pysome brown carbonate with cp @ 278.5-

280 and 290-291.5

291-294 3 short bands of chert, breccwith minor py po

294-302 some stringers of py, a few s

of cp, very minor po302-303 small chert band

303-314 strongly silicified zone,brecciated with substantial blobs of

dark grey - local patches of chloritevery massive

314-320.5 more of a transition zone t

an actual change in rock type. Locall

silicified and local patches ofcarbonate alteration, minor cp locall

320.5-337 a short unit .of tuff -

would appear to be more of a dacite tandesite. - paler green - fragments

are generally small and leached whiti

Mineralization - negligible - onlyoccasional py. Both contacts are

gradational into 5 feet of heavilycarbonatized rock.

CORE SAMPLES

FROM

afc PO

Lated

iringe

2?6280285

:p 29C295

300

lan 303,305307

r 316

lan an

ih in

TO

'S

280285

290

295300

303

305307310318

:olour

RECOV. WIDTH

4

55

55

322

32

ASSAYDESCRIPTION OF SAMPLE

A2-C03 - IJf cp # 3# py po" -1 small blob cp" - very minor cp

11 - minor cp" - minor cp

" - minor cp

w - 456 cp blobs" - minor cp" - 1J& cp very minor" - minor cp po

FORM S22

NORTH ———

EAST. —— EUEV. —— AZIM. —— DIP —~—

DIAMOND DRILL REPORT

OptionAshmore Twp.

HOLE NO. A-4-72 COMMENCED-—————— FINISHED___________ PURPOSE OF—^————— HOLE—————.——————

...5

FROM

337

357.7

456

TO

357.7

458

494

494

DESCRIPTION

Diorite? - this zone is siliceous, gr

in colour, with a general developemerof feldspar phenocrysts throughout.

fairly massive unit, unmineralized -

some epidote near contacts. Sugarytexture - strongly carbonatized.

Andesite - darker green and more chic

contacts, while the central portion itlighter in colour and more siliceous.

There are a few splashes of cp in thefirst 20 feet but afterwards the

mineralization is negligible. Some smj

quartz carbonate stringers with local

iron stainings. Minor epidote.

Diorite - Pale grey to dark grey i)

colour. Darker than previous intersecNumerous small blotches of epidote

alteration, rock is silicified and ea:Feldspar phenocrysts (or metacrysts) ,,

common as before. No mineralization

non-magnetic.End of hole.

CASING LEFT IN HOLE.

miumm m^ LI?MED

CORE SAMPLES

FROM

3y'f

ritic

11

ion.

bonatire

TO

at the

zed.

*

RECOV. WIDTH

*

'

ASSAYDESCRIPTION OF SAMPLE

TJMMIHS, UNTARIU

FOHM (22 NORTH EAST. —- ELEV. -—— AZIM. ___ DIP ————

DIAMOND DRILL REPORTWILSON OPTION #1

Ashmore Twn.

HOLE NO. COMMENCED FINISHED—— PURPOSE OF HOLE.-——

* * * ^J

FROM TO

117.;150

200249.

300

350

400

450479

DESCRIPTION

SAMPLES FOR THIN SECTION

Andesite (tuff?) with chloritic frag)Carbonatized andesite with minor

disseminated pyCarbonatized andesite minor py, cp

i Just previous to the copper zone ~Carbonatized andesitePale grey green Carbonatized andesiti

(dacite?) py fc cpCarbonatized diorite

Silicified andesite

Altered andesiteCarbonatized diorite with epidote

Check collar @ 42 0 Azimuth @ 1800

CORE SAMPLES

FROM

ents

TO RECOV. WIDTH

*

ASSAYDESCRIPTION OF SAMPLE

DtHU- K. UC6'sYtfsvtt4f "

I'.-X J"|-:-p II'*'fN ["'JTCJl- hUl.Ui- u .ii L;rt:i Lii.uitJ

OHTARiO

A^i-7241 6*1-005

00

OV b 53'

,

scale i*-ioo'

FORM S22

NORTHEAST

I-H____ ______1S-•. —— xI-J DIAMOND DRILL REPORTHOLE NO. A-5-72 COMMENCED

AZI DIP

M IgC' 0

— Collar @ 4-5-? — ©JOO-^-5— PROPERTY __ WU,uiaira Ttf **ye

FROM

0

76

TO

76235.6

DESCRIPTION

CasingAndesite - massive with tuffaceous

sections. The andesite is generally da

green in colour but is often lighter ituffaceous sections.

The first part is unmineralized,non-magnetic , and chloritic

The tuffs have a very fine fragmesize - usually less than 1/1)6". In sonsections there is a predominance of

chlorite blebs throughout the rock :Tuff : 95-97, 103-106, 108-112. Q 117.and 122-122.5.

@ 112 a crude chicken track structureis developed with numerous blebs ofchlorite and some lath-like crystals

which appear to be altered to chloriteThere are also some quartz-carbon

stringers with hematite staining in thzone.

Some contacts between different

units are readily visible and areconsistently @ 60" to the core axis.Some other contacts are either irregulor gradational.

OAV nomTrtxt Jl*oUft UriiUfi ffi17* Aflhmora— SWD On.

HOLI

t. r-

CORE SAMPLES

FROM

•k

1

It

1

J

it e.6

ir

TO RECOV. WIDTH

t

ASSAY

: —— Te 8 t~*xt* rtsi en-of ——— copper-zone ————————H*illftri W i Rririlf-x- Rrjvn

DESCRIPTION OF SAMPLE

FORM B2e

NORTH EAST. ELEV. AZIM. - DIP -

DIAMOND DRILL REPORT

PROPERTY WILSON—&PHON

HOLE NO. COMMENCED. FINISHED—— PURPOSE OF- HOLE——————

A-5-72 ...2

FROM

'

TO DESCRIPTION

around 162, as pyrite in a short sill(

band 160.9-162

Small amount of tuff ? G 165 withchlorite blebs.

169.8-171.5 , Short zone of chert

bands (or flow tops). Same as materia]in holes A-l &A-2. A short stringer oipyrite @170.9. The rock is grey in coland leached whitish.

171. 5-177. L - Grey green andesitewith minor disseminated pyrite.

177.4-181 very dark chloritic andes- tiny white flecks of leucoxene - ma)be a diorite since there are vestigesof feldspar.

The rock now becomes strongly

carbonatized - brownish carbonate wit Jsome minor pyrite.

200.6-205 small chert bands also fe214.1-215.4, 217-218.8

Around these chert bands, the andesJappears to be tuffaceous, only occasi(

fragments though.

@ 2 21.5 start of a zone of carbonat

- brownish colour. Extends to 233 wher

it jrrfidofi into a V^T*V siiicflovifl DOHA

CORE SAMPLES

FROM

eous

our

ite

tenal

Lzatio

S

TO

n

RECOV. j WIDTH ASSAYDESCRIPTION OF SAMPLE

'

rOSM (22 NORTH EAST. —— ELEV. —— AZIM. —— DIP ————

DIAMOND DRILL REPORTPROPERTY———WfilS&N

HOLE NO. ^. COMMENCED FINISHED— PURPOSE OF HOLE——————

-.3

FROM

235.6

254.9

264.2

26?270.1

TO

254.9

264.;

26?

270.1279.5

DESCRIPTION

up to 235.6. First minor cp in thiszone - 2 small splashes - one @ 221.5and one @ 230. Minor py

Short dyke of hornblende gabbro -very dark green with numerous smallblocky crystals of hornblende 1/16 "size, carbonatized

Contacts with the andesite are ir;upper @ 90" to C, A. lower 3 45 0 t.n C.

@ 240.2 a large bibob of cp alonga quartz-carbonate stringer. No miner;

^ ft f*or^ t/h&tj- but afterwards there sorntcp and py all through the dyke. It isusually associated with small quartz-carbonate stringers but this is notalways the case.

' Silicified and carbonatized ancle;- very minor py po

Diorite (or albite porphyry) - gn

with numerous feldspar phenocrysts

(or metacrysts) . There is some epidoti

alteration - mrit.artjR irregular. Minoidisseminated pyrite throughout.

Andesite, Krey-green, unmineraliz*Diorite (or albite porphyry), as

previous SPCfclnn py^y folHfirtny* AP|t(

CORE SAMPLES

FROM

egulaiA,

1240

241

245250

ite

302

y

d.

OfjA

TO

241

245250255

303

RECOV. WIDTH

.

'

1

45

5

1

ASSAY

;'

DESCRIPTION OF SAMPLE

Cu, Zn, Ag

Kl - 23, Cu?

" - neg. sulphides

" - I fi sulph, 1-5^ cp11 - minor sulph. vis. cp

A2 - ty aulph. 2* ftp

FORM SZ2 NORTH__ EAST. ___ ELEV. —— AZIM. ——. DIP ————

DIAMOND DRILL REPORTHOLE NO. COMMENCED. FINISHED——— PURPOSE OF- HOLE______

A-5-7?

PROPERTY

FROM

279.5

306.5

326

330.9

336.8

TO

306.5

326

330.9

336.8

437

DESCRIPTION

and disseminated pyrite.

Andesite - grey-green, locallycarbonatized or silicified, minor ser

in streaks. Mineralization is minor,disseminated pyrite, very minor cp.

There are two blots of cp between 302with some po,- just cutting the core.

Diorite (or albite porphyry),contact 3 SO0 to the core axis. Spars'

mineralized with py cp -only one tin;

splash of cp seen, carbonatized.The rock is similar to before ex

that from 317-322 it becomes more mas

and finer grained.

Carbonatized andesite - unminera:

Diorite (or albite porphyry), ve:dark here, with feldspar as before, t!is a lot of epidote alteration in thijOnly one small splash of cp seen @ 33;

Andesite - grey-green to the var:that is carbonatized and brownish, Verj

sparsely mineralized - cp is very mintMineralization is usually with quartz*

carbonate stringers. Around 402 the

andesite becomes darker in colour and

weakly amygdaloidal in pla^As, ^^w*

CORE SAMPLES

FROM

cite

3.03

ly

e pt

ive

ized

yerezone.

ety

r.

is

TO RECOV. WIDTH

*

ASSAYDESCRIPTION OF SAMPLE

.

FOKM XI NORTH EAST. —— ELEV. —— AZIM. ——— DIP ————

DIAMOND DRILL REPORT

WILSON -OPTION

HOLE NO. A -5-72 ...JCOMMENCED———^——.^———-..^.-^.^ FINISHED————-.———————————PURPOSE OF——^————————-———.^ HOLE_________________,_______

FROM

437

TO

448

448

DESCRIPTION

iron staining in the quartz-carbonatestringers. Minor epidote and/or seric

Diorite (or albite porphyry), asbefore - a bit coarser grained, minordisseminated pyrite, epidote alteraticarbonatized.

End Of Hole

CORE SAMPLES

FROM

Lte.

m,

TO RECOV. WIDTH

*

ASSAYDESCRIPTION OF SAMPLE

FORM *22 NORTH— EAST. —- ELEV. —— AZIM. ——— DIP ————

DIAMOND DRILL REPORTHOLE NO. A-5-72COMMENCED——————————FINISHED————-———————. PURPOSE OF—-—-—-———. HOLE————.————————

.. .6

FROM TO

76112

150200

250300350

400440

DESCRIPTION

SAKPLES FOR THIN SECTION

Grey green andesite - chloriticChicken track structure in tuff 7 -

chloriticGrey green andesiteCarbonatized andesite

Hornblende gabbroAndesite - grey greenAndesite - dark green - weakly carbona

Andesite - few quartz-carbonate stringDiorite (or albite porphyry) - pyrite

CORE SAMPLES

FROM

tized

srs

TO

1

RECOV. WIDTH

,

ASSAYDESCRIPTION OF SAMPLE

HOLLINGER KiKS IWITED4 IKHiS, ONTARIODdU. /f. QjtMO*ebA

A .

A/

scole '"-100

NORTH EAST. . ELEV. . AZIM. —--

S7-5-N-

DIP —^heok—

-xi-l-2-E———- Surface————-OSO*———-——

DIAMOND DRILL REPORT

jSON OPTION

HOLE NO. A-6-72COMMENCED

PURPOSE OF-HOLE—check— E,V-a no ir,aly-

a ,w-.**. . Claim TB 229616 Ashmore Twp. Ont. Rr

FROM

0

4

37.4

TO

437.4

40.8

DESCRIPTION

Casing(AX)

Hornblende Gabbro - medium to dark

green in colour with numerous blockycrystals of hornblende. The rock ie

quite highly altered with carbonate a

talc, local specks of leucoxene.Some shearing with talc and chlori

13.5 - 14 @ 45 0 to Core axis and @ 18.

20 also® 45 0 to core axis There aresome very fine hairline stringers of

quartz-carbonate which usually carry asmell of po and cp.

23.5-23.9 blob of chert very irreg

in shajpeThe lower contact of the hornblend

gabbro is finer grained @ 45* to theCore Axis along a quartz-carbonatestringer with po, cp

Chert - grey to whitish in colourrather milky. The first inch is filled

with numerous laths of amphibole - verblack. The remainder of the zone is

weakly banded in darker and lighter

patches, massive. There are some blobs

of po with some cp. The po is quitestrongly magnetic, locally, very fine

CORE SAMPLES

FROM

id

e -

.

ilar

r

37

TO

41

'

RECOV. WIDTH

.

4

ASSAY

JLX&d by * Brsdl^v Bros

DESCRIPTION OF SAMPLE

Chert - 5# po minor cp

NORTH EAST. — ELEV. — AZIM. — DIP ———

DIAMOND DRILL REPORTPROPERTY—WJiSQiJ—OPTION

Ashmore Twp.

HOLE NO. ^..fc..72COMMENCED—————,—— FINISHED^-———^—^-— PURPOSE OF————————HOLE——————————-—.

...2

FROM

40.8

46.3

4 7.9

TO

46.3

47.9

63.2

DESCRIPTION

disseminated mineral.Zone of carbonatized andesite -?-

Kost of the rock is carbonate and therare local patches of dark grey chert -gradational - and irregular in shape.

It is also gradational from the moremassive cherty material. There is a lo

of blue-grey chert as interstitial witthe carbonate. Mineralization is mostl

po - very minor cp. (5# po)Short zone of cherty material, ban

blue-grey and darker grey @ 45 C to theCore Axis. Numerous quart z- carbonatestringers. The upper contact is more oless gradational - lower @ 45 C to the iSome shearing and some biotite along

single planes of shearing @ 45" Thereare some small stringers of po usually

with quartz-carbonate often minor cp.@ 47.8 small bit od cp with a po

bearing stringer.

Andesite - and carbonatized andes:The first 2 feet is massive andesite w:numerous quartz-carbonate stringers © ito the Core Axis, bearing some po and

Mineralization is erratic though.

CORE SAMPLES

FROM

41

47

ed

ore A:

teth5"y.

TO

4649

is

RECOV, WIDTH

52

ASSAY

,j"

DESCRIPTION OF SAMPLE

A2? - minor po,py,cp

" - 5# po cp

FORM ta

NORTHEAST. -EUEV. _ AZIM. - DIP -

DIAMOND DRILL REPORT

PROPERTY —— WILSON OPTION #1 ——— —Ashmore Twp.

HOLE NO, . A-6-72 COMMENCED———.^———. FINISHED—-^-™.——-—-. PURPOSE OF———.—^-.^—. HOLE________________

...3

FROM

63.2

76.4

84.8

TO

76.4

84.8

128.4

'

DESCRIPTION

After that the andesite is generallymassive with carbonatized sections.Very minor disseminated py,cp onlylocally. Lower contact slightly irreg

d 60" to the Core Axis.

Albite porphyry (logged in previholes as diorite), There are numerousfeldspar phenocrysts or metacrysts,some epidote alteration, and some biotMineralization is minor with some very

finely disseminated po,py4 The lowercontact of the dyke is nearly normal t

the Core Axis.Andesite - brownish, carbonatiz

with very minor mineral (some py visib!Contact with dyke @ 84.fi is at 450

Albite porphyry with numerousfeldspars as before, locally finer

grained. There is some biotite developthroughout. Epidote alteration is comnxThere is approximately 3# pyrite dissei

throughout. A quartz-carbonate stringe@ 103.5 has the only po cp seen in thizone - only a minor amount -

The pyrite commonly shows a cubic habilLower contact @ A.5 0 .

CORE SAMPLES

K ROM

lar

us

te.

d ,

e)

dn.inatec

*

TO RECOV. WIDTH ASSAYDESCRIPTION OF SAMPLE

FOAM .22

NORTH EAST. —— ELEV. —— AZIM. __ DIP ————

DIAMOND DRILL REPORT

WILSON OPTION #1———— Ashmore Twp.

HOLE NO. COMMENCED- FINISHED-.— PURPOSE OF- HOLE——————

A-6-72 ...

FROM

128.4

187.2

195.6

TO

187.2

195.6

492

DESCRIPTION

Andesite - the first few feet are

massive and chloritic but it grades ina darker carbonatized lava. Mineralizeis very minor - usually pyrite but a fspecks of cp are seen (rare). Around 1

you start to get some epidote alteratiin the andesite, some talc ? in thesections that are strongly chloritic.

Around 183 the andesite becomesbrecciated with infillings of calciteand numerous bands of alteration. Theebands show no consistent strike. Q 185the andesite becomes quite siliceous

and hard with a few of the brecciafractures filled with py,po,and cp. Itappears to grade into a chert horizon

A short blue-grey chert band,

locally layering @ 80 to 85 0 to theCore Axis. The chert is brecciated asthe surrounding andesite with mainlypo filling stringers - very minor cp.

The EM-17 conductor plots here. Thepo is magnetic but not strongly so.

Andesite - banded @ 90" to the

Core Axis in alteration layers of

FROM

0

ionw0

n

round

185

190

ccTO

187.2

190

195

)RE SAMPL

RECOV.

.ES

WIDTH

55

ASSAY DESCRIPTION OF SAMPLE

5# po minor cp5/6 po minor cp

'

FORM S22 NORTH EAST. .,— ELCV. - AZIM. — DIP ————

DIAMOND DRILL REPORT

PROPERTY—WILSON—OPWON—#4-

HOLE NO. A.Q.. 72 COMMENCED-————... FINISHED———————— PURPOSE OF———————HOLE^—————————.

...5

Ashmore Twp.

FROM TO DESCRIPTION

There is some biotite developed. Therock grades to a more uniform carbonat

andesite around 202.- it is nore greerthan the ordinary brownish carbonatize

andesite. Generally unmineralized but

there is a small stringer @ 212.7 witlsome po,cp and py.

- 253-255 blue-Grey chert band wittsome py and minor cp in stringers*

Contacts normal to the Core Axis,After 255 we return to a carbonatiz

andesite with a speckled type ofcarbonate alteration.

@ 286 and @ 299.8 quartz stringer

with some tourmaline.328-329 short black siliceous band

with strong alteration at both contactContacts are gradational - 7/6 dissemir

After that there is. minor dissemirpo,py and cp in a zone that has patchy

alteration - mainly local zones ofof silicification and carbonatization.

@ 346.5-348.5 gradational contactson a paler green tuff unit. The fragmeare small - leached white - locally

feldspar metacrysts T After t.h* *.iiff

CORE SAMPLES

FROM

.zedishd

254

3d

328j fited p

ited335340

its

TO

255

329

r

340

345

RECOV. WIDTH

1

1

5

5

ASSAY DESCRIPTION OF SAMPLE

Chert - minor py cp

10# di BS. py

minor diss. sulph, py po c p

w " " py po cp

-

TORM S22

NORTH EAST. —— EUEV. ..— A1IM. ——— DIP —————

DIAMOND DRILL REPORTHOLE NO. COMMENCED. FINISHED- PURPOSE OF. HOLE______

A-6-72 ...6

PROPERTY #1Ashrcore TWP.

FROM TO DESCRIPTION

there are a few bands of the brownish

carbonatized andesite.

Around 350 there is some silicificand another tuff unit. -(352. 3-353)

353-360 zone of strong leaching,chloritization and carbonatizationno mineral.

After 360 a return to the dark grecarbonatized andesite - only rare spec

of mineralization - some biotite devel389.2-369.6 Short altered band

containing 15# po 3# cp (EK-16 ?)Around 415, the rock starts to bee

strongly silicified and greyer in colo

It is not a chert unit., unroineralizedaround 424 this zone ends in a shortaltered, breccia zone.

After 424 - brownish carbonatized

andesite, leaching around quartz-carbostringers. @435 and @438 chert.

440.8-444 short tuff band as befo444-463.8 andesite carbonatized463.8-465 a highly contorted zone

of mixed andesite and blue-grey chert.465-467 silicified andesite

The remainder of the hole is

CORE SAMPLES

FROM

tion

ncs

389imeir.

late

•e

TO

390

RECOV. WIDTH

V

1

ASSAYDESCRIPTION OF SAMPLE

A2 alt. - 10# po 2# cp

FORM 6 22 NORTH EAST. —— EUEV. —— AZIM. ——— DIP ————

DIAMOND DRILL REPORT

WILSON OPTION #1———— Ashmore Twp.

HOUC NO. A-6-72 COMMENCED———————- FINISHED___________

...7

PURPOSE OF- HOLE—____

FROM

-

TO

492

551100

15020025C

254300350356399450492

DESCRIPTION

andesite with short zones ofcarbonatization.

END OF HOLE

SAMPLES FOR THIN SECTION

Hornblende Gabbro

Massive andesiteAlbite porphyry - with epidoteChloritic and carbonatized andesite miDark green strongly chloritized andesiVery dark silicified andesiteChert bandCarbonatized andesite - unmineralizedCarbonatized band in the andesiteStrongly altered zone - chlorite carboDark groen andesite with biotiteAltered andesite with carbonate chlorimassive andesite.

CORE SAMPLES

FROM

ior py;e

late

:e

TO RECOV. WIDTH ASSAYDESCRIPTION OF SAMPLE

flCUra HIKES LIFTED\IIMMIKS. OMIQ

^W- X? (Zfara^jb^

A-6-72

txl.

Az 1800

l 1.' . 3 Ve U t. , .Cd* i -S

scale 1*100'

NORTH EAST. -EUEV. ___D^-Tr-T——i0P

-@-300—U*—-

DIAMOND DRILL REPORT

PROPERTY——WJiSQN——OPTION——#1———

JLEtiniore Iwoj

A-7-72—January-29/72-- FINISHED——ja nua rv—31/72

PURPOSE OF— HOLE

Pytl 1 ort hvf Brfldlpy'

FROM

010

.

53

TO

10

53

76.3

DESCRIPTION

CasingHornblende Gabbro - after 39 the ga

is similar to the previous hole. -numerous blocky crystals of hornblende- some altered to chlorite, occasionalhairline stringers of quartz-carbonatenonmagnetic, unmineralized, carbonatiz

Previous to 39, the gabbro is muchmore highly altered - almost all of thhornblende crystals are altered to chlwith the pseudomorphic shapes best seeon the fresh surface. There are somelarge greenish feldspars developed andoccasionally you can see some amphiboland biotite. Kuch more carbonate in thzone - unmineralized.

The gabbro becomes finer grainednear the contact. Contact broken.

The first 2 feet here is massiveandesite, while after that there is a

whole zone of interbedded chert andandesite. Units are too small to be

logged individually.3 main types - grey-green carbona

andesite, blue-grey chert-, and a darkto black siliceous member, the latter

CORE SAMPLES

FROM

bro

d.

rite,

s

izedrey

TO RECOV. WIDTH ASSAYDESCRIPTION OF SAMPLE

FORM B22

ELEV. .AZIM. - DIP _

DIAMOND DRILL REPORTPROPERTY———WILSON—— OPTWN——#i~

HOLENO. COMMENCED FINISHED —— PURPOSE OF HOLE —

...2

Ashmore Twp.

FROM

-

76.3

131.1

150.6

TO

131.1

150.6

302

DESCRIPTION

is very massive. Banding is generallynormal to the Core Axis. There is somefinely disseminated py po locally, whimost of the mineralization i e in largeblobs and stringers as po fi cp.69.5-69.9 iron? very fine grained,black, strongly magnetic, with cp po.

Andesite - the first foot is thebrownish carbonatized variety, whileafter that there is approximately 10*of massive andesite. The rest of the ^is carbonatized andesite but it is daigreen in colour. Strong alteration @ Swith some epidote. There is usually sovery fine specks of cp throughout thethe zone although there is not much c;overall. Some tremolite ? locally.

Around 121 some silicification -core changes to a dark grey to black@ 123 After 128, brownish carbonatizat

Albite porphyry - asin previous hwith feldspar, minor epidote, somebiotite, and unmineralized. Upper cont@ 90 0 lower @ 45 0 .

Massive grey-green andesite, 2small pyritic bands S 187.5. The rock

CORE SAMPLES

FROM

ler 63

7073

mek

)

ne

Lon.)les

tct

TO

707375

RECOV. WIDTH

2' 3

2

ASSAYDESCRIPTION OF SAMPLE

minor cp ponegligible sulphidesminor sulphides

..

FORM 922

NORTH EAST. —— ELEV. —.. AZIM. ___ DIP ————

DIAMOND DRILL REPORTPROPERTY WILSON OPTION-

HOLE NO. A-7. 72COMMENCED——..————- FINISHED—————-^—— PURPOSE OF———-——HOLE——-—————————

Ashmore Twp.

FROM

-

TO

302

DESCRIPTION

becomes highly carbonatized and brown!around 194, then the rock grades intoone of the dark silicified zones arour

208-210.2 - Silicified but pale gr*andesite.

210.2-216.5 - Darker andesite grade

darker grey with cherty and carbonatissections. 5/5 py po cp

216.5-218 - banded altered andesite218-219.8 - silicified band - grey219.8-240.2 - banded altered andesi

- banding @ 90 0 , numerous stringers ofquartz-carbonate; Some bands are chloxsome carbonatized andesite with talc?le. biotite. @ 225,5 3 tiny bands carrjArsenopyrite ^" of core along quartz-carbonate stringers. Very minor minerssome core broken P 230.

240.2-250 - grey silicified andesitvery minor mineralization - isolated lof po cp. 250-302 - Massive andesite (

local splashes of mineralization.264-265 Quart z-c&rbonate stringer

along the core axis with minor po py c

END OP HOLS

CORE SAMPLES

FROM

sh

i 203.an

2108 2129d 215

217

be

i. t i zed

Ing225,

Lizati

9 -

Lebsnly

264P*

TO

212215217220

i

5on

'

265

RECOV. WIDTH

2

323

1

ASSAY DESCRIPTION OF SAMPLE

A2 silic - minor po py cp" - 5-7# po py cp" - 5-7/S po py cp

A2 alt. - neg. sulph.

*

grab sample - Aspy forGeochemistry de Au

mass, ando s. - minor po py

'

'

FORM S22 NORTH—-- EAST. —— ELEV. .AZIM. — — DIP ____

DIAMOND DRILL REPORTHOLE NO. ^.0^COMMENCED—— FINISHED-———— PURPOSE OF———HOLE

Ashrrore Twp.

FROM

-

TO

1050

ICO200250300235

'

DESCRIPTION

SAMPLES FOR THIN SECTION1

Hornblende Gabbro - alteredHornblende GabbroCarbonatized andesite - tremolite?Carbonatized andesite -brownish baneDark green silicified andesite.Massive andesiteBanded altered andesite with talc?

-

*

CORE SAMPLES

FROM TO

' f

RECOV. WIDTH ASSAY

'

DESCRIPTION OF SAMPLE

*

MllfJRW f"?'w invTtnTJF""i'l1 rv-sn-r,———— 11.0, tl.^, U i^nfliJ ——————

Zk/Jl fc. UJjtlaHC/f.'L^

A -7- 7 2

Az 180e

scale 1-100'

DIAMOND DRILL REPORT

PROPERTY- WILSOM OPTION ffi

HOLE NO. A-3-72

COMMENCED————FINISHED—PURPOSE OF .^——————HOLE____^T^st copper

Claim TB 229617,Ashnore Townahipj Qnt. —DriHed"'byT"Trradlgy~^rgg,'-

FROM

0

60

TO

69

160. L

DESCRIPTION

Casino.

The fire, t 1C f oat IB cnrbonatijsecl andesiti

brownish - minor biotite. Then the endesi

becop.p,c nore massive tmd frey ffrcon in

colour. First bit of riiroralizfition seen

around S2 . minor pyrite,,

Around 100 there aro u couple of elliptic)

lensoo of po py - nagnetio.

After that the andesite becorjoo wenkly

brecciated vdth chlorite and minor pyrite

along these fracturoo.

Locally the rock is carbonatized brownish

There are a few qta-C03 otringora cutting

the core - aopifl are stained brovmish.

Around 119 there is some dark green

silicified andesite which grades to the

brownish cnrhonatisted andesite around 12k

The intermediary (121-124) io a putty

colour* Only minor mineralization - a feit

specks cp seen.

129-133 grey ^reen nilicified andesite.

133-H3 brownish carbonatized andesite.

143-144. 2 intermediary.

144*2-145.3 dark p.roen oilicified andesit

Short band of py (i 145*1

FROM

.

te

1

.

ccTO

)RE SAMPL

RECOV.

-ES

WIDTH ASSAYDESCRIPTION OF SAMPLE

rORM 522

NORTH—- EAST. —— ELEV. ——- AZIM. —— DIP ———

DIAMOND DRILL REPORTPPOPP..TV W ILSON OPTION A_______,

Ashmore Tovmship

HOLE NO. COMMENCED- FINISHED-—— PURPOSE OF- HOLE______

FROM

160 A

183.8

TO

183.8

212

DESCRIPTION

145.3-H8 grey preen silicified andesite

grades to a tore chorty member Q 147

with 155* py.

148 dark prosn cnrbonntizod andoaito

grades to a trey #reen naasive andesite

around 150.

153*2 dark proen and carbonatized ondesiti

apain v;ith minor pyrite, grades to a

brownish carbonatizod rock a round 154.5

and then to a massive frey green andesite

with local carbonatized patches around 157

Albite porphyry - lipht grey to dark Krey

with numerous feldspar phenocryst!! (or

metacrystal. This dyke is a bit finer

grained than that usually encountered.

Minor biotite developed, epidote alterati

common. Upper contact broken. Lower ®

600 to the Cure Axis.

Up to 185 - short sone of highly cur-

bonatiaed andoaito, some very fine

disseminated Mineralization; 05 184.7 Rome

py cp.185-193 a whole Bone of nixed blue-r,rey

chert und andesite. A few quartz strirrer

and some cp, po.jpy throughout*193-200.9 weakly banded oarbonatized

FROM

5.

184

186

n

188

19?

196

ccTO

166

183

193

196

201

)RE SAMP1

RECOV.

-ES

WIDTH

t

2

2

5

3

5

ASSAYDESCRIPTION OF SAMPLE

-

Ag * chert minor sulph.

Cherty .6Cu.

Cherty neg. oulph.

Neg. sulph*

A? - minor py, po, c p.

rORM 922 NORTH—— EAST. —— ELEV, -— AZIM, —— DIP ————

DIAMOND DRILL REPORT

PROPERTY. WILSON OPTION /

HOLE NO. COMMENCED,FINISHED.-— PURPOSE OF HOLE——^^—

As'more Township

FROM

212

213.6

TO

213.6

301

,-i

301

DESCRIPTION

andnaitft, somft biotite - nilieoous zona

(clnrk) 19'v. 5-195 some dinnominatvad py po

cp. 200.9-212 zona of mostly blue-grey

chart fractured with cp nnd po. Mnor pySomft ondsfiite?

Albite porphyry - an previous with

foldopar, Clino? epidota, BOGIO biotite.

Andoaito - niXfld groyinh silicfjous ZOHflS

and frey graen maaaiva andeaitq zona s, in

general crud^ contacts *it ^5O *- n 1'-hft

Core Axis. .Only minor -.cp s e an in ntz-CQ*f . . t \ } strincers. ** 21*1* 2?6, 290 the rockitself is generally unmineralized. Somebiotite.

.EH!) OP HOLE.

-

CORE SAMPLES

FROM

201

202

201.

210

242

TO

202

204

23,0212

244

RECOV. WIDTH

1

2

6.2

2

ASSAYDESCRIPTION OF SAMPLE

Cherty - minor sulph*

Chorty - l^S Cu.

w - minor nulph.

A^ * chert - .5 Cu.

*2 - with qtz-CO^ atr.

Minor cp, py, po.

:., : .

. '^i '

.•- :

FORM 922

NORTH——

EAST. —— ELEV. ——- AZIM. ——— DIP ————

DIAMOND DRILL REPORTPROPERTY. WILSON OTTIOM if l

HOLE NO. COMMENCED FINISHED—— PURPOSE OF-HOLE——^-.

Ashmore Tovmship

FROM TO

69100

150

200

250

300

DESCRIPTION

3AMPW.S FOR THIN SECTION

Brownish cerbonatizsd andesite.Mannive andesite.

Park prenn carhonati^ed and-nita vith py

Massive andesite.

Silicified andesite . biotite.

Mafloive AndftnitOf

-

FROM

CC

TO

)RE SAMP1

RECOV.

-ES

WIDTH

t

ASSAYDESCRIPTION OF SAMPLE

bOJU Z. QJiiX(M-dL^Howra BSSS flwnto"" upSS. OIUWIO

(fi o

DDH A-3-72

Appendix III Sheet

SUMMARY OF ASSAY RESULTS

Average Values

Cu(ppn) Zn(pptn) Nl(ppra) AE(OZ) Pb(ppm) Au(oe)

203-213

215-230

234-235

240-245

249-250255-260235-320

1174

7791330

2940

3330

700

1026

64

7567

261

6100

126

67

165

254

326

133

222

,070

.059

.093

.128

.231

.073

.072

id209

2060

4321

Nil

Nil

Nil

Nil

Nil

.02

Nil

Best intersoctions: 240-245 .294^ Cu, .123 oz Ag,

249-250 .33#i Cu, ,61# Zn, .231 oz Ag.

DDH A-4-72

164-16?

@ 200 - py

230.235

250-307

307-310

316-313

34

173

4990

4700

1630

1370

60

1050

132

182

199

92

121

1410

119

139

51

171

.029

.032

.131

.14

.070

.073

12

35

10

13

10

13

Nil

Nil

.02

.006

Nil

Nil

best intersections: 250-252 1.56?; Cu, .43 OB Ag.

275-276 ,69?i Cu, ,23 oa Ag.303-305 2.36# Cu, .15 OB Ag,

III Sheet flbf

Cu(ppm) Zn(ppn) Ni(ppm) AE(OZ)

DDH A- 5 -72

240-255

302-303

Best

DDH A-6-72

37-46

47-49

1*5-195

254-255

328-329

335-345389-390

Best

DDH A-7-72

53-83

207-232

5987

15200

intersections

176

720

393

1550

282

145

3010

intersection:

151

95

ft 225,5 Aspy 8

264-265 454

80

134

: 240-241

302-303

56

38

33108

137

56

71

389-390

55

75

3790

90

299

6.9^ Cu,

1.52# Cu,

106

78

9756

105

139

156

.3* Cu, .

82

193

264

93

176

789

1.578

.789

035

038

028

064

053

034

088

088 oz

024

046

096

094

Pb(ppm)

18

34

oz Ag.

oz Ag.

27

10

8.5

17

39

913

Aft.

12

14

27

10

Au(oa

Nil

.01

.005

.005

Nil

Nil

.005

.01?

Nil

.15

.05

- 56-75 .025 oa Au,

lv : -A

*

4

AppendJ^III Sheet Wbt 3

Cu(pDm) Zn(ppm) Ni(ppm) AK(OB) Pb(ppm) Avi(paJDDH A-g-72

184-212 1540 74 8^ .086 14 Nil

242-244 5490 60 110 .266 15 .005

Bent intersections: 201-204 .fl5# Cu, .199 oe Ag.

242-244 .55^ Cu, .266 OB Ag,

42E18NW0MS 16 ASHMORE020

HOUXNOER MINES LIMITED

REPORT

GOVERNMENT EXPLORATION ASSISTANCE PROORAMKB

WILSON and KALSON OPTIONS

ASHMORK TOWNSHIP

taE10NW0M5 16 ASHMORE

TABLE OF CONTENTS

020C

X - SUMMARY (F EXPLORATION

A - LOCATION

B * WORK DONE

II - OPTION TERMS

III - GENERAL OROLOGY

XV - RESULTS

A * DRILLINO

B - ASSAYING

V - CONCLUSIONS UtA RECOMMENDATIONS

l

JL

1

2

6

6

APPKNDIX I

APPKriDIX II

APPT.NDZX III

Al'Pt^UIX IV

APPENDICES

PLANS OF DRILLING

DRILL SECTICXiS

SUMMARY GP ASSAYS

MAP OF PROPERTY

OF EXPLORATION

A* Location

Ashmore Township ia located in the Thunder Bay Mining Division and comprises part of the Little Long Lac gold mining area*The property consists of 25 unpatented and two patented claims under option, and ia located approximately four miles east of Geraldton along Highway H*The unpatented claims included are t

TO 139350.353 inel.i TB 229616-61* inel| incl*l TB 23*726-72* inol*t 325351*359 incl.t and

)1*

The two patented claims under option are i TB 10164 and TB 10971*

B* Work DoneThe original 14 claim group waa acquired in March, 1970. and Hollinger Mines United performed geophysical (magnetic and electromagnetic) surveys over most of this group* On tha basis of tha geophysical data, two holes were drilled in 1970. with a total length of 1117 feet* Later in mid-1971 a geological survey was performed over thia original group* Both the drilling results and the geological eurvey were filed for assessment*

In the last quarter of 1971* Hollinger Mines United applied and received a subsidy to do further work on the property through the provisions of the Ontario Government's Exploration Assistance Programme* Under thia programme, geophyeloal (magnetic and electromagnetic) surveys were performed on nine claims that had been added in 1971* These claim (numbered TB 325351*359 inol.) were adjacent to the original group on the eastern boundary*

The assistance programme continued into the first quarter of 19721 when-a drilling programme waa initiated* Six holea, with a total footage of 24*3 feet, were drilled to check anomalous copper values obtained in the 1970 drilling and to teat a one of ground conductivity*

- 2 -

Since that programme expired on March 31. 1972, two patented claims, adjacent to ths west boundary of the original group, have boon added* In May 1972, a geological survey was completed over the nine claims to the east (TB 325351*359 inel*)i and in November 1972, Magnetic, electro* Magnetic and geological surveys were completed over the two patented claims*

In April 1973, a second Exploration Assistance Agreement was signed to cover a drilling programme designed to teett

(a) a coincident magnatic*slsetromagnstic anomaly on patented claim 1097l|

(b) the best interssctlon obtained in the 1972 drilling at depth) and

(c) a Magnetic anomaly assumed to be on or near ths contact between the Tsmiskaming ssdimsnts and Keewatin volcanics*

XI* OPTION TERMS

An option agreement, dated March 23, 1970i between Donald Wileon of P* O* Box 730, Geraldton, Ontario, of the first part and Hollinger Mines Limited of the second part, gave Hollinger the riant to explore the original 14 claims and any subsequent contiguous elaias staked by Wilson or Hollinger,

The payments, under which Hollinger may acquire the property, aret

A sum of 6 l j 500.00 upon signing the Option1 . upon gnng pon, ljooo.00 on or before March 23* l 1,000*00 on or before March 231 1 lJOOO.00 on or before March 23! 1

T 1^000.00 on or before March 23l 1 and a further sum of 9100,000*00 on or before March 23, 1

* #

Thua, total payaents of ^105, 500*00 are needed to acquire the property*

Also, for any ore mined and Billed from eaid mining lands in excess of the first million tons, Wilson shall receive a 25*eent**per~ton royalty*

A total of ^4,500*00 hae been paid to date ae set out by the above agreement*

-l *, t

By a similar agreement dated Oetobar 30, 1972. tha two patented claims (TB 10164 and TB 10971) were optioned to Hollinger by Mr* Herbert Kalson of Geraldton, Ontario*The payments by whioh Hollinger nay acquire this property aret

A sun of 6 1.000*00 on signing the Option. -i ljooo.00 on or before October 30* 197 f liOOO.OO on or before October 30J l"

and a further sura of 9135*000*00 on or before October 30, lf *

A total of ^1,000*00 has been paid to date, ae outlined in the above agreement.

Ill, GKNKRAL GEOLOGY l

The property ie largely underlain by a sequence of Keewatin lavas Intruded by younger hornblende gabbro*, hornblende** * . * * * * ̂ J A M. A t* A f̂ A. W m—. .diorites and albite (or just feldspar! porphyry* The southern portion of the property is underlain by Tewiekaraing sediments. The Teolskaraing sediments encountered were congloneratea and arkose which are similarly intruded by the gabbro, diorite and albite porphyry*The Keewatin lavas consist of andeeitic to daeitio flowe and tuffs whioh are highly metanorphosed. Biotite and chlorite are often found in these volcanics, with accessory carbonate and silica* Tho tuffe are characterised by nunxtrous, mall, subangular fragment e in a chloritic matrix. The tuff horisons generally have a gradational contact with the massive flowe*The nasslve flowe often contain narrow chert horisons. Initially these cherty B nee were thought to represent flow tope, but there are at least three different types of occurrencesil* Chert band*gradation*! with the andesite

(How top*?)2* Chert banda with abrupt contact**3* 2one s of nixed blue grey chert and andesite

(silicification?)Although intersections of chert were quite cosnon in the 1972 drilling, very few chert horlsons were encountered in the present program** Hence, no additional inter* pretatlons can be made about the** unit**

The hornblende gabbroa are easily distinguished by the numerous blocky crystals of hornblende in a dark green chloritic natrix* Often these blocky crystals ara altered to chlorite) however, the crystal habit usually remains* The gabbro*, as with ths diorite*, are presumed to be Early Algoman in age*

The only hornblende diorite encountered waa in hole A~14*73| on claim TB 139352* No surfaes exposure* of thie unit are noted on the property* Although the blocky crystal* of hornblende still persist, as in the

fabbro, they ore only locally developed and calcic eldspar is the predominant mineral. Unlike the gabbro, the diorite was weakly magnetic. although there is no expression of an anomaly from the geomagnetic survey performed in the area*

The albite porphyry dykes are presumed to be Late Algonan in age, since in a couple of surfac* exposures ths porpnyrie* are seen to intrude the hornblende gabbro* The high sodic feldspar content is diagnostic of all dykes encountered* This rook is usually pale grey in colour and quite hard, with the main alteration noted * ' alight amounts of epidote after feldspar*

taming sediments are encountered in surface exposures on the Kalson claim* and in drill hole A-14-73, on claim TB 139352* Moat of the Teadekaming aerie* her* is represented by conglomerates, with only a few sonss of arkosic material noted in the drill hole*

Tha conglomerate contain* a variety of pabbla typos that show a wide range of alse and snaps* 'Many of tha smaller pebble* (usually lass than i inch), tend to bs - quits angulari while the larger one* (l inch or greater), ara distinctly nora rounded in nature* Tha matrix of tha conglomerate is brownieh and moderately biotitio with small quarts 'eye*' scattered throughout* Local increase* in alteration create a much softer, mor* chloritic natrix*

Tha arkosic bands saan in tha drill hols ara relatively narrow and ara characterised by numerous Miall grains of quarts and feldspar, in a grayish to grey-green matrix, Contact* ara usually gradation*! with the conglomerate units*

f ~IV* RESULTS

A. Prilling

Fivo holes were drilled encountering tho rook types previously described under general geology, beingi Chert, Andesite. Hornblende Diorite, Hornblende Oabbro, Albite Porphyry, and Toniokaming sediments including arfcose and conglomerate,

AU of t ho drill logs will bo filed for assessment, hence only a plan of tho drilling plus a copy of tho drill sections accompany thio report. A total of 2)91 feat wore driilodj 1005 foot to test tho magnetic-electromagnetic anomaly on tho Kaloon clalmsi 996 foot to check tho wide ooppor bearing ono found in tho 1972 drilling, and 790 foot to tost tho magnetic anomaly in the Tomtofcaming oodimonto*

Tho n*gn*tic*cloctromagnotio anomaly on tho Kaloon elaino Mao attributed to a narrow (up to ono foot) band of aaooiva pyrrhotite carrying adnor pyrite and chalcopyrite, Tho excellent profile! obtained fron the geophysical eunreya fron ouoh a narrow tone oro probably related to tho rather shallow overburden depth* in tho area*

t

During tho 1972 drilling, an intersection of 17 foot assaying .47? ooppor. *X4 ounces/ton silver v was obtained in holo A**~7** Hole A-12-7J was set out to cross thio sons approximately 100 foot vertically below tho original intersection. Although a substantial -width of rook anomalous in ooppor was encountered, assays show tho sons to bo Manor at thio depth.

Drill hole A*H-7J was designed to cross section a magnetic anonaly prosunod to bo in tho Keewatin volcanics -~ tho additional footage allowing tho hole to out the voleanio^sediaentary contact, Unexpectedly, after 196 foot of overburdoni tho hole ooUarod in Tomiskaning conglomerate which extended to a dyke of hornblende diorite at 610*) foot, Tho magnetic anomaly was attributed to approximately 45 foot of conglomerate containing numerous dioaorn* inated blobs of pyrrhotite.

Previous to tho drilling of hole A-14-7J, two olaims wore added along our south boundary to protect any possible results obtained in that hole. Thus, tho

present number of claims Mentioned at the first of this report it two creator than the number indicated upon signing tho Exploration Assistance Agreement* No work was carried out on those two now claim (TB 37279s and TB 372799), to that nono of tht provisions of tht Agreement woro violated*

Bt AssayingAssaying of oora camples waa completed at Hollinger Mine* limited. Assay Department, by tho atomic absorption method* Samples woro asaayad for ' various elements, inducing i copper, sine, nickel, silver, lead and gold*Each smplo is nroparod by crushing and grinding the rock to a -100 nosh fraction than dacoamoslng tht product by tho addition of hot nitric and hydrochloric acids*A list of tho assay rosults acccajpanlta this report in suvsiary fora*

V, COHCUI3IOH3 and RECOMMENDATIONS

Exploration to data has rtvtalad two rtlativtljr strong tlactroraagnttic anonaUos with associated high nagnttlos, to bs related to narrow bands of massiyt or ntar smssivs pyrrhotite with minor acstssory pyritt and ohaloopyrlto* One of these anomalios waa outlinod and drilled in 1972, the seoond anomaly lying within tho Kalson claims and boing drilled during tha course of the present programs*

t

Further, a sons of dissoainatod sulphides haying economic implications WAS previously outlined by drilling, to the east of the geophysical anomalies more recently located on tho Kalson claims* Thus, the Kelson anomalies appeared to be ideal targets for drilling as suggested from the nearby pyrrhotlte-chalcopyrite sone* Unfortunately, the data now available indicate that this entire section is not viable for mineral exploitation*

r

However, due to the intimate relationship between pyrrhotite and chalcopyrite noted in this area, magnetic horisons would appear to be favourable drill targets, either with or without a coincident electromagnetic anomaly* Several untested magnetic anomalies, which do not appear to bo indicative of a change in rook type, remain on tho Wilton elaias* The most probable interpretation to be applied to this is that the anomalies suggest the presence of pyrrhotite - hopefully continuing its association with chalcopyrite*

.7 -

The presence of Timiskaming sediments on ths property may indicate an additional exploration opportunity, in anarch of gold* Although most of the Tinlskaning bslt here has boon extensively drilled, very little work has boon dona in ths Rides Lake area* Unfortunately, the results received to date in the sedlnsnts hairs been very poor and no major structural features, which ars often closely associated with gold ores, appear to be indicated* In ths absence of known stringer aonss, or structural controls, a couple of oross*sootional hoist nay bs warranted to test ths Keewatin-Timiskaming contact*

August l, 1973*

WHINGER MINES LIMITED MHHINS, ONTARIO

APPENDIX I

Sheet

l of 2

(j^j^^SBassgssgfcaSf

(t W

^

-s?

V

^

* .^ 5

APPENDIX I Sheet 2 of 2

^ C'O '

APPEN

DIX

II

Sheet

l of 5

5o,VV,

(Vi

APPENDIX II

Sheet

2 of

5

xvj

APPEN

DIX

II

Sheet

4 of

5

\

H

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t*

3I: e

* **w\

55 3*1m

m I^f

o o

*"t

. .

Mb

d 3 ii^

* *

I*; ^*fi

tt tt

N

N *

N

N

*~O

O

O

~

"o

e

eaMaeW*

s fe•3m

o

a ^

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** o o

ott

tt g

tt tt

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-S R

li.a* *A

9399

00

00

*3|J^* **

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^A

C*

XiA ^*

-^ nR 5*4 ia ^

i* ^ ;J

is*

iH

^1 O

M

M

^O

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O

ae g

- 0 0

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tt tt

lsaS

w *rv

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t*- IB

^

\*4

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JS f-l

-PCoe e

4*

*o to *• 4*

B.O

^

5•S

^^S

*ft i-4 O

fi.h

a

o

5fci

O7

e

*4 vt

*4 *4

NO

*^ IA

i.P.^ s^sss ssS

H

loll

K\

O

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CM O

S

O\ to

a••^ *^

*53S

J5 O w

** O

rf rf

APPENDIX Stott 2

A*10*73 (continued)

242*245 .19* Cu, .11 OB Ag 245*247 .10* Cu .05 OB Ag370*375 .34* Cu, .13 OB Ag 375*3*0 .135* Ctt, . OB Ag

All grab aamploB ahowod background valuta, All assays for gold woro Nil.

DDK A*U*73 Cu(pptj) Zn(ppn) Ni(ppei) Ag(os) Pb(pjpft) Au (on)

40*50 190 45 *7 .03 12 Nil 30-130 264, 02 64 .03 17 Nil

Highest aeeayai 100*105 .10* Ou, .05 OB Ag123*125 .W Cu, .09 OB Ag * l foot of

pyrrhotite.All assay* and grab aamplta in thia holo war* mie h pooror. AU asaaya for gold Vftra Nil.

DDK A*12*73 Cu(pjw) Zn(ppa) Ni(pjw) Ag(os) Pb(ppw) AU(OB)160*195(172*177)250*2652d5*360(350*360)

3341608201372510

37304749

302

*9121111919^

.02

.03•03.05.05

1212141110

NilNilNilNilNil

High*at aseayai 167*170 *04?S Cu, .03 OB Ag172-175 .222* Ou, .05 OB Ag175*177 .064* Ott, .02 OB Ag253*255 .077* Ou, .05 OB Ag292*294 .145* Cu, .05 OB Ag295*300 .069* Ou* .03 OB Ag

310*315 .06* Ott, .04 OB Ag320*323 .066* Ctt, .a OB Ag

330*335 .01* Ou, .07 OB Ag355*360 .09* Ott, .06 OB Ag

APPENDIX 111 Shoot 3

A-12-73 (continued)

Moat of tht grab aanplaa in thia hola yioldod background values, except for two aa follows t

275'300*

Cuppsi

573170

Znpym3460

d5

Hippei

35idd

Agos.3

2.6

PbPPM

id3d

AUosNilNil

In tha light of high aaaaya for split samplas shown above, it thua appaars that tha interval 275* to 360' is characterise! by valuta whleh ara high background or slightly abova.All aaaaya for gold values waro Nil*

DDH A.14-73 Cu(pjw) Zn(ppa) Ni(ppsi) Ag(oi) Pb(ppai) Au(oa)

200*360 10d d3 97 .02 19 Nil640-695 500 40 50 .04 10 Nil(640*655) 1240 5d 54 .07 U Nil720*745 450 4d 59 *04 11 Nil760*7dO 523 32 40 .03 12 Nil

liighaat aaaayat 315*320 .03^ Cu, .02 os Ag640*645 *W Cu, .10 os Ag645*650 .13* Cu, .06 os Ag650-655 .0#, Cu, .05 os Ag732-735 .0# Cu, .07 os Ag737*740 .13* Cu, .Od os Ag764*765 .32* Cu, .17 os Ag76d*770 .09* Cu, .04 os Ag770*771 .07* CU, .03 os Ag

All grab aanploa yioldod background valuaa.Although thia hola intoraaetad Taniskaning eongloaarata and arkoaa which onhaaood tha prospoot of finding gold, all aaaaya for gold waro Nil. Tha aadiaonts would appoar to bo barron unlaaa affootod by a aajor atructural foaturo and/or host to ona or mora atringar sonos.

'7.s f—/7

'SNIWW11 S3NIW M39NmOH

/.d S ST 7 ' 6rf z- 7*2

J

'•"/s'ff^'FORM 522 "

EAST. .

FI f",AZ'M. , . , ,, ,nip L/IKiC.C

31-i-OOSj 9-;-;; oy;29,^3

collar 'i - ^q - ,

rv?

:eTP^J-T

voftt

/v^/

. 300' .- '\ f L ^ '

DIAMOND DRILL REPORTHOLE NO. A-l/i-73

COMMENCED^ FINISHED-^——

PROPERTY- VIIQr: OPTIOl!PURPOSE OF______———HOLE_'fist ;ri;.::':;^

.Ashmore township .y'-iril?:'''

FROM

0

126

TO

1266 M). 3

DESCRIPTION

CAoino.Coneloi.ierate - /I'enisknr.inr in age. .

UD to ISO the conglomerate is slightly

frfienish fcrav to grev in colour. After

1^0 1",*i" rort^ 1'! n^Av^tf*' i -^ r "Ppy i ^ fnloUT1

with numerous fragments or pebbles. The

more sedimentary nature of the con'-lonera!

is not truly noted until further down the

hole where the pebbles are much more

rounded.

Aftor ISO we start to ret a few smoky

rmarts RVP.S and the conglomerate tends to

Ion],- ri ft ,o ri y i ri on t. i r, T 1 t-i thp niit.prop on

t.ViR T'alsori , i-,t.i nr,, '"^n t.evhiirp nlnn

changes s one v/h at ?fter ISO from the su&arj

nature over the first 60' to a more

inar.Kivfi groimdpi.iss \-nA;h t.hp ounrt,?, pyes.

Ahciiit. -i.hp 'inlv o-f-.hpr rii Rt.iprn-i shaVil P.

rdneral in the matrix is biotite which

occurs in vorv tiny brownish flecks. The

amount of biotite decreases after 1#0.

The pebble sif.e is f enerallv 'in the

^ to J" ranpe althouf'li some fra;-.nents are

greater than an inch. The larger pebbles

are usually e Ion rat e at approximately 4 5to the core axis. The smaller fragments

FROM

Q

t

CO

TO

RE SAMPL

RECOV.

ES

WIDTH ASSAYDESCRIPTION OF SAMPLE

FORM S22

NORTH EAST. - ELEV. - AZIM. — DIP___

DIAMOND DRILL REPORTHOLE NO. A -1A.-73

PROPERTY- Uilson Option :.-l

COMMENCED- FINISHED——— PURPOSE OP- HOLE——————

Ashr-'ore "i.p e

PROM TO DESCRIPTION

are fenerally more angular although this

tyne of occurrence is also seen in the

outcrop on t. h R iC.ilson property. The

pohhlor, nrp nf ssvnral types - the dominan

tvpe ceinff blue grey and cherty - in some

instances almost translucent; E**ey to buff

cherty pebbles; black siliceous pebbles -

fv?'ther dov;n the hole sorie of these look

r"i,!-jpr slaty; olus some dark brownish to

"T..pniRh pphblfis \;hj.ch often contain

r* 1 op -i t. A -h -i nt. -i t. A t

153.4-153 and 167-180 are nore massive

sf.'-itions - d -ir k ^rev rreen in colour -

ne n-i pt.i n^ii-i f?hahl A pjnftra^s. The pebble

sj v e and number .lust generally decreases

ir'jo these zonos - arkosic?

; After ISO the pebble size r.radually

increases over 2' and then we start to

r,et some better conglomerate and the

quartz eyes begin to occur.

rineralization is only minor with a

f AW tinv h .1 ab F. of Rijl-jhides in the early

p:^rt 'if t.bft hole - mostly pyrite - some

pyrrhotite and rarely chalcopyrite. The

pyrrhotite ip onlv iveakly ma^'iieti^c - and

the chalcopyrite is generally associated

FROM

CO

TO

-

RE SAMPL

RECOV.

ES

WIDTH

*

ASSAYDESCRIPTION OF SAMPLE

}'[.

'-.

('

NORTH. EAST. - ELEV. - AZIM. — DIP———

DIAMOND DRILL REPORT

PROPERTY- V/IL30I! OTTI01! -:?1

HOLE NO.

COMMENCED. FINISHED— PURPOSE OF- HOLE———————

•.-l!; -75

Ashmore Twp,

FROM TO DESCRIPTION

.••i t h it in tinv solashos. After 210 thereis a general increase in the amount of

sulphides - here vre have raostly dissemin

ated blebs of pyrrhotite and the rock is

more r-iarmfitie. fip ir, vsry m nor hfii*e t

Ar^un^ ?rt? i-.he p j 7," flnd r"mho^ nfpebbles gradually decreases into a short

zone of arkose from 30i..5 to 330. In the

G.ojTv lorip.r At.fi up t.o t, 'IR qrko.qe f.liA frapwrts

ir f- fi" in TV of t. h p Muiph frey t.ypo-

similarly at the lov/er contact after 330

althouc-'h the rradation here (330) is much

faster.

Ths arkose is rreener in colour than

the rrey conglomerate and contains a few

noticeable grains of ouartz and feldspar.

pTMct.i nnlly iinaJt.Ar'p.d - very I'n'nnr-

chlorite-sericite nearly the same as the

alteration in the conglomerate. Very

,-iinor pyrite in the arkose - solash of

chalcopyrite at 319.5. There arc a few

carbonate strinrers in the arkose unlike

the conglomerate r.u}d thore is some minor

brecciation and alteration with a few

narrov: carbonate. Rt.Hnr^rs f-rn^ ^n.^,^ t-n310.5.

CORE SAMPLES

FROM

200

205

210

215230225

230

235

240

2t5

250

255

260

26,5

270

275

22028-5

2902Q5

TO

205

JJ10

21^

220

225

230

23^

?;,n2L5

2^0

255

260

265

270

?7^2!sO

2^5

200

. 29.5300

RECOV. WIDTH

5t

5r,

5

5

*;*;

^5

5

s*5

S

•5

q

5

5

5

5

5

ASSAYDESCRIPTION Of SAMPLE

gl - very ninor sulnh.

ii ir it it

It It '.t IT tj, ^

" minor rjo i..y

tt Tt r^ ^ Tiy t, ̂ f ri

" ! t po py

II 11 r,,, y

" '' Tip ^V tv . C P1

" " no r'V tr. c*'

Tt It ^ 3 .-.y

If It T,,j r,y

" very •••I o ir f-,;;' -.'i.

TT It '1 If

It It !t If

" ninor mvrite

" " pyrite

vprv ,,inor ^

tt It tt ^y

" r^inor nv

FORM S22

NORTH— EAST. __ ELEV. —— AZIM. —— DIP____

DIAMOND DRILL REPORT

PROPERTY- \,'1LJO:J or'i'IOL? -'l

HOLE NO.

COMMENCED- FINISHED-—— PURPOSE OF- HOLE______

Ashriore 1'wn.

FROM TO DESCRIPTION

After the arkose v.re are into a eood

conglo.-r.erata before "tyO. There i? a

not.ahlfi iT'p-rpHRfi ^n py pn h^rp r - K i/oll

Schistosity due to frarincnt ,, elongation at

55 0 t o the core. Similar lithology aaprp.vi nnpl.y rlep.f.rihfiri nongl ni^erar.^ ,

^if^^r ^^0 "I'.li^ r, 3 A t. "p "i ir of1 t.hp ^ni"\c' i (ij'^y^p

becomes ,t;reeuer...and there are very numerouv/el.l rounded pebbles, llostlv blue prey

cherty, some white, some porphyry, some

black, none brown and some dark green.

Fvrit.fi -pyrrl-inr.il-.fi r.nnt.Pnt. rapirtly

rlonr'pnppp ft -f i-, o 37 ^Sn.

/t06-407.5 - short arkosic band}

speckled nature of ot^-feldsoar.

419.4-445 r rat.hnr sharp. .upper contao.tnt. J|.0 O t,o dark ^rov fairly manK3Vf! ( vf)ry

Rlifht.1v nlt.PT-fid nrlfrtse,

;, J, *; -I|J, f* - v^^y rt&rk- {jr-ny pnncT opo-^at .c.

vr..ry nnn 1 1 Vii\io r r^y fmr.-nontp p nmo nyrit

- contacts Kradational.

Wj.S-^56.7 - Fradation to greenish

arkose, fairlv passive, Minor nyrite.

^A.y.^m , ? - ^rflriat.inr, t" a Cnnri

conglomerate - mostly bluish grey and

CORE SAMPLES

FROM

300

305

310315

320

.^325

^30•ns

Mfi

345350 .

- 355

TO

305310315320

325

330

335

™.n

31.5iw

355360

RECOV. WIDTH

?

5

55

5

5

5

5

^

H

55

ASSAYDESCRIPTION OF SAMPLE

Ofl - very ninor ^y ^o

irkose - vary ninor r'v n o

it it it n v ., 0

It II It r,y T^ o p,,

It . !t !1 r)V -: 0

If It ' It ,r . l Q

)r"l r. i nor ;v no

" " ny r,Q

" ^ ; pv no" ITT nor r'y ~n

11 *} j r.v nn

" 3 'j pv v)0

rORM S22

'NORTH EAST. - ELEV. - AZIM. — DIP———

DIAMOND DRILL REPORT

PROPERTY- soi: nmo:; --"i

HOLE NO.

COMMENCED, FINISHED- PURPOSE OF- HOLE——————

Ashnore Tv;p.

FROM TO DESCRIPTION

whitish cherty fragments, minor py po.

Lineation of frarr.ients at about 75 O to the

core.

501.2-509.1 - short shear (I'M at

401,2 at. 60 to core then conglomerate

vi t, h a more arkosic: matrix. Pra^ments are

ri f"1 li f^Wpr ^n PHt'ih^T* t'. ban ot.ViPT f*oriP"l divier.*

h:rizons. ......, -,, . — ..- . ,,-,...509.1-521 - short band of co&rse con

glomerate - more brov;nish chloritic alter

ation. Traces of sulphides.

521-5L.3.f3 - some arkose but mostly

n'.ru'l o- -IP. rat i n fra^t.-.fint. fi in a rioi'fi arkosic

rr.;',t.rix ^ s irniLir t,.n thp. unit 501r-5Q9 ^"t,

l"V : re there is some areas with no fragments

T! fit h contacts fjraclatipiial - lov;er is more

r fp 1'^' ^ lit.t.lR piorp. alteration here -

chlorite, sericite. Lineation at 60 to

cors.

54^ T f5-605.S - return to conglomerate

H-inoat.p.d at 60 flonf axis of frajJT'fintfi) .

l-'uch more highly altered than previous -

matrix is ouite brovmish. Larpe number

of nebbles as before - mostly blue Krey

chertv,. some white, Rprao buff chertv, sonit

brov/nish and aandv. At 554.9 trace of

FROM

hf^

.

CO

TO

'

RE SAMPL

RECOV.

ES

WIDTH

t

ASSAYDESCRIPTION OF SAMPLE

FORM 622

NORfH- EfcST. —

ELEV. - AZIM. — DIP___

DIAMOND DRILL REPORTHOLE NO.

COMMENCED-

A-l/i-73

PROPERTY- UILGOi; OPTIOI? :rPURPOSE OF- HOLE ———.——

FROM

.

'

~ ^^W^•' ! Sfk

TO DESCRIPTION

chalcopyrite - otherwise very little sul

phides. -\round 565 we "•rade into a less

r.ltarcd conglomerate and the colour ehangr

from brownish t.o r-rey. Vnrther a] nnn- t.hp

zone the conglomerate also becomes more

.605.3-609.8 - contacts at ^5 0 - con-

.vnr^'iiir- to a short Dyke of gabbro??

Yer^ 'fine groundiiass i/ith soine fairly lar'

i rrp^'iil ar blph^ of brov;n5 tCn b i ot.i t.i r.

m,*} t.pTM ^i 1 ^nr! ^OT!!P TarlA rr^^n pp^t-^ nf

chlorite. It appears to have no effect

on the arkosic material at either contact

although the rivke seems to be slightly

c.hillRd and brownish at its contacts.

i'T on-!"aLnetiCj carbonatized.

609.8-611.3 - arkosic, grey green as

before. *

611.3-623 - sharp contact at 1+5 0 to

band of conglomerate , grey, hard, numerous

pabble.q- T;-inn-r RnlphiripRj traofi of np ^

612.1. Lover contact is quite abrupt at

80O to core into the much finer conglomer*tfffot* **S."w i ?s'*- 6 23-6W.5 - gradation from the con-clonerate for the first 2' then quite a

CORE SAMPLES

FROM

ft

be.

TO RECOV. WIDTH ASSAYDESCRIPTION Of SAMPLE

FORM 522

NORTH EAST. - EL6V. — AZIM. -. DIP———

DIAMOND DRILL REPORT

PROPERTY- ^O;-:' OFTIOi! j,''

HOLE NO.

COMMENCED- FINISHED—— PURPOSE OF- HOLE——————

A-l/,-73 7.

Ashr:iore ri'v;p.

FROM

640.?

TO

7QO

DESCRIPTION

dark r.rey f;reen arkose, llassive. Very

minor sulphides. Lower contact al one a

fiuartz Btrinrer.

Hornblende diorite dvke, upper contac

along- a quart. K stringer. Rather high per-

rent.^c-o nf feldspar VIOVA ,inH 1 really the

feldspar content is extrene. The rock is

medium ;:reen in colour with fairly numerou

hlehs of psp.iidomorphie chlorite after horn

blende, The roi^k is v^ry slightly magnet. -i

Hp t.n A6? t-h^rp nrp onit.e a f^w quart- 7-

stringers - usually at a low angle to the

norfi - nftst.ly hlinsh in colour, Assoftiated

.-"ronnrl thfiSfi n1-.rin 0^r,c' are ftor\A Rnlphlrinn

py pii v/it-h 6 nn0 f; 0^"^ sized splashes ofchalcopyrite.

667.5-670.3 - few quartz-carbonate

stringers hore, making the diorite quite

altered. The diorite becomes finer grains

r.iora silicified, v;ith sortip. brink red

staining of the felriRpnr, Arr.pr.f.nry ^hT^r

vdth the stringers - less than normal

chlorite .vdthin the diorite.

Sone chalcopyrite around a quartz

stringer at 6S6.

Around 9??-1 t.hel rli nr-i ta hoflnme-R .1 hit

CORE SAMPLES

FROM

640

, 6L5

6506^5660

j 66S

. 670

:. 6756rtnArtc6 on

l, ———

It-0

TO

64-5

6-50

6^

660

665

670

6756rtn

6ft5

690^95

RECOV. WIDTH

^

^

555•5

*;i5

5

5

ASSAYDESCRIPTION OF SAMPLE

T,^ - vpry r^-innr rp p. -i r.y

' minor py j.io .cptf " en roy

" n pv cp

" " py np

" very riiinoT- py } t.r. r.^

" t. T A r A py

" np^li^ihTo piilph.

!1 ——— minor ".y c P ————————————•* ** *

-.'J

FORM S22

NORTH—. EAST. —— ELEV. —- AZIM. —— DIP————

DIAMOND DRILL REPORT

PROPERTY- VJLS01: OPTIOH j/

HOLE NO.

COMMENCED,. FINISHED——— PURPOSE OF- HOLf-————.—

A-14-73

Ashmore Tv/o.

FROM

-

TO

7QO

DESCRIPTION

finer trained and then -around 728.8 the

rock becomes very brownish and micaceous,.

After 728.8 to 741.3 the rock looks some.

vrtiat like the matrix of the brownish con

glomeratic. Thnrfi la so much bint.-it.P an ri

ouart.7. arminrf t. h i s 7.nnn t. hat. it. -j p v^ry

rii f. f iciilt, to inte7?pret. There is about30,3 bluish qtz strinp'ers here and some

sulohides associated v/ith them.

741.3-790 - p:rever diorite than

nrevious - contfict alpnr; stringer zone

v.dth above. Hathnr mottled apnearanon

vnt.h t.hfi hi ^ h fplr^npqr rnrit.^nt. , On'ly ^

pt."pj n^'^rs her^ — ^'Tiiitj© nu^rti?— c3.rbonntGi.^, - - .- j ^ ---,- ,. ^ -, - ,^ with very minor sulohides:- 764.8, 778.2

and 7o3.

ra TD OP TTOLT!

fifrk K . CWo/rtrft/HOLLINGER HIKES LIMITED

TIMMINS, ONTARIO

CORE SAMPLES

FROM

720

725

7^0

7^9.735

737

740742

745

760764

765

768

770771775

777779788

TO

7?-5

730732735.737

740

74274 fi7^n

764765

768770771775777779780789

HECOV. WIDTH

5

*5

•y

l

2

3

2

3

r.

41

32142

2

1

1

ASSAY jDESCRIPTION OF SAMPLE

LI - traces of py no CTJ

" ninor qt.K, n-inor -y po

tt it H n-i ^n-r -v rio r- r:

" SO 5, " t r . py C^

" 30 j ; t rr.ino:V-y no cri

" 20 .r " rrp nor -'V "'j c^

" minor !t " py oo c ~)

'.L nfiglSf- 'sulph or qtc

it tt it ir it

LI mass, (slightly magnetic)fl/L mass., 1" str. 1" 20O to C.A.-

bordered by heavy black tourma line with minor cp throughout.

Mass LI - minor py @ 300 to C. A. {magnetic).

Slightly min. - qtz Xi w. small tourmaline strs. -w. cp 6: py (ra^ndi

••lass. alt. LI with py fc cp (magnetic )

Coarse grained LI massive ̂

Coarse gr. LI - slightly min.1" green qtz str 200 to,.C.A.. cp * py, shear plain @ lo0 to fi. A.

3tz diorite - chloritic and pyritic (magnetic)

2n qtz calcite str. in an un- mineralized diorite.

NORTH EAST. — ELEV. - AZIM. — DIP.. .

DIAMOND DRILL REPORT

PROPERTY-

HOLE NO.

COMMENCED FINISHED PURPOSE OF- HOLE-——^

A -14 -73

Ashnore

FROM

r*U

G -r T3

Gr, * T.--i

G

G H- T3

G

G -i- T3

rt 4- V:"!

GG * T3

G

G -t- T3

G

G v T S

r.

G * T 3

G

G -i- T S

G

G i m ^ v i o

TO

126

150

.175

?nn225

250

2?5

. 300..,.

3?5•3.f.n

375400

425

450475500

r,2 r,

550

.57.5

600

60S

62?

650

DESCRIPTION

Geochemistry and Thin Section

"emiskar.iinf conr/loraerate - biotitic

Ijiotitic conglomerate

; 'OT'n n,Ts.RTVP. spriinipnt. - nrkosfi? .

it

11

li

" 'ara n rkpRir: pnrt of r.rr.ri.it.a on

Coarse, conglomerate

Finer conglomerate

Dark rrev arkose

^rkose vi t h a few dark f r arpent s

Gorij^lonerate, blue trey pebbles

f,.5r': r rny non^ lorisrptft

flrnv'T oi •-•.Pi'fll'.n - fpvj pphViTpR - avkoRT^ mnt.^ J

Conf lornerate - more hirhly altered --- py

Oonflornerate - e-revish

nnnf;1 nr^pr?it,p. - rinTp arko.oic nat.rix

To Dr. Koddle - rabbro?

Grev crfiRn arkoss

' :uite hlshly altered diorite, py cp

CORE SAMPLES

FROM

X

1

TO RECOV. WIDTH

*

ASSAYDESCRIPTION OF SAMPLC

FORM SZ2

NORTH EAST. — ELEV. - AZIM. — DIP———

DIAMOND DRILL REPORT

PROPERTY- •JILSOII OI-TIQi: :''

HOLE NO.COMMENCED. FINISHED- PURPOSE OF-HOLE——————

A-i;,-73

Ashnorc Twp

FROM

G

G H- TS

G

n v T3r.

G -i- T3

TO

675

700

72^

750

775

790

DESCRIPTION

Geochemistry and Thin Section

Diorite with hirh feldspar content

Diorite - RONR ny

^io'n'1'.p' ~ r ^ }-\p p'T^/^Tn^d v7 "*^"n ^u-'^rt-E

Greenish diorite - aoiiie po

Greyish biotitic dioriteH 11 H

.

CORE SAMPLES

FROM TO RECOV. WIDTH

*

ASSAYDESCRIPTION Of SAMPLE

KENOGAMISIS

LAKE

0 + 00 B.L

L

AST.

CL

I-

(T 10

~ l mi

iflUJNGER MINES LIMITED x 11WHS, ONTARIO

WILSON OPTION No l

ASHMORE TWP

Scale : l "s lOOO'

16 ASHMORE200