Footage/ ; Date^- , r , .,w.-,,, ^^.-.- . ,,- : B-25-71 -i ... · Baraa-m Prelect: (88) BILLET LAKE AREA GRID 30-25 5 Pro-tec By--— j . EDWARDS ST*ertO JULY 20/71 22/71 Ko-3-25-71-1

Diamond Drilling

Area or KAWASHI: I.AKI:

Work performed by: COCHENOUR wniANS

Claim N9 Hole NQ

B-25-71

?OeiGS,E 931,7 11 KAWASHE LAKE

Footage/ ; Date"^- , r , .,w.-,......,, ^...^.-.- . ,,- :. ,v.,. :.ir '..'"''..' .- i' '* " *-.' ',- .iv'.r,1 ;.,.,' v "* -:-"v"^.':-v,-.,-": -^; A - - .*-'" •'••"' '. .-X'--, '" --'' Vi'''-4 ":-;^'.^..". ! "-'.•"J. S-'^.'V.''- 1''.' •'•••'• l - :-i ' '.: loi*.--. v -' -July/71 -- :"^v. ;.i -i- ^ -. ;.;.' .^-' •••;:,' i:; f' '-- ::- - :-i35! : -' ;Juiym- ^i.iv-oV|;.- v V- :v --" vJ: "'-"'135* July/71

Baraa-m Prelect: (88)

BILLET LAKE AREA GRID 30-25

Pro-tec 5 By--—j . EDWARDS ST*ertO JULY 20/71 22/71 Ko-3-25-71-1

i 45 .101.0 R-MCGULLOCH JULY 22/71

O

14

H^L

14' Casing - Overburden

15'4" Mafic tuff - (chloritized)

Mineraloev(a/ calcic? placrieclase {about 65%) minor quartz(b) dark mineral

amphibole (hornblende?) biotite 25*

(c? Chlorite (alt of dark mineral) about 5*;(d) ovrite and ovrrhotite 2% to 5% (massive and disseminated)

Texture;

*- -v-w

Medium grained crystaline euhedral to subhedral amohitole

Moderately foliatedirregular hair line to 2 mmwide white mineral layers of (quartz and feldspar)contact with next rock type broken but suspect it toue sharo

DUPLICATE COPYPOOR QUALITY-ORIGINAL

7 : TO FOLLOW

LOGAT tONs?

TT*i*ct*

CORP SIZECORw^IPpOi

VATION

S. *4w*rdi ^ly

A7'Tl'D

PROM j TO j G E Q L O G t C A Lr̂ e-i*^pARTi'RF—m*- P f E

NO - j ~Q lyytOTH

ASSA

j v , AW i w*f--,t - vTwx-.u-**a

i i Ji —— 14 —— ; — 15M*^ —— Mjtfie tuff" (cklwritimcm) ————————————————————————————————l . 1

; j ; Ki.**-*l.*7

1 ——————— i

!

.

^

L -, -.

BILLET LAKE AREA GRIP 25 Mo- B-25-71-1

15'4" 61*1" Interlayered morfic tuffeous graywacke (siliceous-tuffsite?)

Mineralogy;

(A) Morffic tuff(chloritized layers) about 65%)(b) calcic plagioclase (about 65*)(c) dark mineral amphibole and biotite about 3(H(d) chlorite {qlteration o 4: dark mineral (about 5%)

(B) Tuffaceous graywacke (about 45*4)

(a)- Calcic? plagioclase (about 65%)(c) dark mineral ambibolis and biotite 'about 35%)

(C) Pyrite (about 5%massive and disseminated throughout both A) and B) but consentrated along foliation planes

( j) Felsic layer

(a) Plagioclase(b) quartz

Texture

(E) Quartz lens (between 26'11" to 27'2")

Fine grained to medium rrained (cyclic)

47866 75'6" 61*1" 2*7" Tr. 30. Metal

DUPLICATE COPYPOO^jQUAUTYoRIGINAL

{v TO FOLLOW

~ - " *- - - ""

':^m*

53Ss

*

F . jx,- r* t*--m

DIAMOND DfrtLl- HOLE LOG LOC AT tON^r*-** l*fc* A*** " B**4

15'4" 61*1 (continued)

Structure: Well foliated layering between mineralogy (A and B) is not well defined (ghostly but seems to follow parallel to foliation) Also felsic layers are irregular and often discontinuous. Contact with next rock type below is sharp but irregular (jagged), where there is concentration

of pyrite)

61*1" 67*1" Dark gray argillite (Tuffaceous argillite

Mineralogy:

(a) dark mineral mostly clay minerals (biotite muscovite etc)

Texture:

(b) white minerals felsic 10* as irregular layers is argillite

(c) pyrite 5%

(d) pyrrhotite (15%)

Very fine grained to aphanitic

47856 61*1" 63*8'

' r*",'i- :

"

DUPLICATE COPYPOOR QUALITY ORIGINAL

TO FOLiOWC

T tm*tCOPE SIZE nr

NO.;

VATIQNBEARING

xns—-cfu-ta-

FROM j TO j C- E Q L Q G i C A L EC-CPIPT iCN!P lj TO IVNJQTH

BILLET LAKE GRID 25

-67'l" 75'

Texture: Continued)Pyrite pebble (l mm l on in diameter massive pyrrhotite

Structure Well feliated irregular layers 9.5 mn to l cm of white felsic materialPyrite and pyrrhotite concentrated along foliation and contact with above rock type contact with next rock below is sharp but jagged

Tuffaceous graywackevery sinilar to rock of 15' 4" to 61"l" but lacks chloritized layers (mafic, tuff) and has about 5* pyrrhotite and 51 pyrite Contact with rock below is gradational

75' 87'3" Interlayered Tuffaceous graywacke and mafic tuff.As described for 15'4" to 61*1" but only a trace of pyrite.

87*3" 88' Mafic tuff chloritzedAs described for 14' to 15'4"

DUPLICATE COPYPOOR QUALITY ORIGINAL

TO FOLLOW

NO. P-15-71-1

r16'EPTH M* H

t* lea of

Wl^tr 1. rf^rn Vmt

18*4* t^ On* tat •ttly a trac* *f pyrit

Structure:

w r"" foliated. "Snd leveredr t e corjceri.tratec. alone: foliatio

DUPLICATE COPYPOOR QUALITY ORIGINAL

TO FOLLOW

t ix r "~\ r .rj r* P : i f f—.~j' cIUI*t.I***JfridL*SXRF '.:~A-.vrt OS

BttKlJ&.FMjaet.

45. . ^IS-fKt^f

*l——:——r

gg.O lOlJg Jtl&LjUEJttJLS.Xix*rai*gj-

C*) Calele fix f?)

joa. -XS5L

"i ' : ' ' t——— . ———————————————————————— —————————————— . —————— , ————————— . ————————— ; ————————— , ————————— ; ————————— ' ————————————————————

. ^*- '

J f

1

^J*^^

T*xt*r* tFis* t* **4im

Alf*g f^Z

101.0 of 1*1*

'

OD;i LQ51 PtOJJCTON. Lak N

j ice-- --7C- m i?^A^tNG CrHr*f0 -T p -4S*:|DePrH 13C^?4i ' ^feL c vA-'o^ ! ' A" '•.••:- r fr*oo* fcpoApnfpp tot m ' -•v ~| ' C POV ' "O ^ 0 E O ' C G : C A r ' 'D '"E-" i? C S ! PT *5 0.0 '9.0 : Casing " " " - ' :

V LC^'---^ ^ v L.C.Caastko le*,*' 25/7/71! S A V ?. \ ' ^ ' A S V A v :,

; j j ; ;i : 9.0 ,6S.3 Mafic Heta Tolcaale* (aade*lte) fia* f*aland, dark greea, i ; ^l - \ 'massive to Hod foliated. 5-fjC fractures *it2i o^nurts-csrV ' : ' ' ' , t ;j . , l toTJKaline f illiaf . S**-ear*-teur* *trtsser coetalai ; ; : *trisg*rs mp to *6 feet la vidta. ~

Andesite - moderately aa^aiWlitised* Is *t 1.5 feet; : fractured - 25? qt* eartif 1-^C Po-pr -' - -! . - ' -

f trace* F.^r ': : s l ! l

addevlte '. ". : ' - :' r^~ ;

; ; : ; ' i J ?^f 7^7 :58. 3 !7C.S i L- ^, -li Tuff (Kayo dacitie eoH9o*itioa) Jiar4^ des* e, fin* i i 't'Ssj? ^ - -if

: . grained, siljLceoa*. creyika fracteats W t9- sereral c* ia ; ' ; : iO^^" G^ ' r^l\ length, .3 c* in vidta, Jttxed vita liehter sr*efil*a fiae : ! , ' i l?t-^ . ^ 1^1

: ; .grained, siliceous fragseat* of *ame frlse, ka* ^aaded ; - '- ' ! l*? ^ Q^ ;~/; : appearance at 35* to C^l.^ dis*voinated Po— Py app. '

; ; taarp npper and lover eoataet*.' - ' ~ ' - -fit , -

70.6 ,i±fcc Kafic Keta Tolcaaie* — fine tralced, ved frees* "cal

,* - ' : 1 '~ jfj; ^^ e i : tt : ; ! l f ^ v) B' -SB- -,' i , : ' ' ^^ **| :

srltised S- : i f ; ~~"r~~~~~— - M :. ^11. s ' ? uniform a?pearaaee eoceept for fellatios at 450 to C. A. : ; - i l : ^

; fractured - 3? quarts ear* f iliac*; last 5 feet 10*; 111.8 -114.0 Massire Sulfide* - 75-50^ svlflde*! 6OO-75^ EjPflre

ea ro stringer. . -; ; 'Pr 5* Po 1 : l - ? ' "

15? alt^d rhyolite* frai^eate or baads - frapeeat* k?867 i 111. s' 114. ol 2.2* i 30 ..|al .pectro !i ; greyish browa sard cilleeoa* foliated cerleitised 5? Qts ; **4 ' j l : crai.hie anil-r*i. 1

t ' and Carb bl*fc* la Py. - " : - " ' " '-'"' ' . ' - ' ' '- . - ' -- .. t ! j, ^ j ^

' 114.0 134.6 iXafic Agglomeratej 65?C aadesitic fraffieat* *urr9vaded l(y '" '- ' \ ' s I30? biotitic amterlalt fraga*srt ore^ xed freea^

j ' grained ara s sire raagiac la ali* from under a eafiae ! - ; p /^ tla least* - ; \ T- \ ! ^ \ 1 i i/ l

. , ; to 10-15 cm la taielDBe***/ fracveat* eloagate vita ; ; ; i i 'i f— S (C^J^^5*^:::::':::1t long ? ^ Diotite f oliatiea of •aterial parallel f /' J^l^-L" !: ^ ! to 450 to CJL. ": C--" : -— - - : ; " , "- ; :. •••." :- .. :: : ."••' ' ".--.V •— - : \ i t ' —— t* —— "1 i! ' - - 1 -1 i*4 * : fOOT OF *"^TU " : ~~ '- : '; ' "' -? ' '•'"•'•"•'•- -' ' ."'V-'--'-:-.:-::-.l-.'^- ^ j i ' j ! i ' t- t i"--

i-ri

t)

JH*!

S-f .JW'*'.''-'. v -- '. ''-^ov-; .'.'•;*,.a)v';,V"i BS. *"^! : .*.l. r ,M,4^fml

!.. , ,- ' , t'- 3. f -.-i . "' .-••" 1 . 1 ,/ tl-ftri'' -.y *-,-* t -" ^B*'"-.v v. { ,;- r^^^'M'xm

B-2S71V2

;.^cc^^: j'v^c6^.v^'X^-'i: :--''. '^••/•v'.i :'.-'V ." Cs''-'5 '''-''' 1i'1'r . ,'-- - " ' v'; '.' ,' *' :-^' - -" -'7 \- '"' -- '':' .'':t \ii. V."''- i;;*, T-M ; ' , - '. ' v^'"'-*v; ,-;,'^^x ,. rt: i".^,' ^v,' , .-.' /A ,. -' ''\'.* ^ U*; 1 .'. .mj''',*-'.* - 1 '"* 11 ' .'..ti^jK-^^f' -rV,-^.:-i,-VA * !'. 'V-*^''v r^y v;).;*f t'*' * r t - *' ' ' .' '; . , -' i* , ' ," -' ''J 1 v ,- . V * -" " '*t'.H'5''"^.': ii'.""-,e''.r*^ ; i 1 s : -' "'"'*, . \'-A -- J' r t ;.

1^)'^?^^'^^^m^iWj:^m^^f^ ' :.-- V'^?;Ma:^te\'^ -'M'^•te :^ t^^v-'^i^l^'-'f;^'^'.;flfc'*i'i8, 1V'.'^-AM*';iVi':'*. 4.'"-tK'-r-Jnn ' - .3 f.H '.^^:.*:;fef^^1S*it*'ltt'^''5 :'tl:;'; ;!.-: 'iV'

TT,. T. .••..• :,\" .,'.-. -','. J .' L'-ii--.',:- :-.-' - "iVr.;;-v-ki-(v^,; . iVc-l

':;.'.-'':^ i 7."W'vtfo'Cri'.X.,-;. •/••- 'vs .H-.Vvr^X'^V

.'•'t ^ ' - ' ' - ''. 1 V * ' , , , 1 ".- ; N , '

••• : \ •,,- : vf 1 ' 1'' ; ' - i,'''' V; '.'. ^'if;'., v i"1ii' i';S.;i^^;},;:i^.,^, :.';'-;'v^"'jt f,/, 1 '/ ^-d''/^.^^.;, 1 "^?",:-;; : ?:'.-,:;'j;^ V jS*f:-;,.'vi:;-Vf

''- '.' '. . V f ' . ' '\'V ?^'i'i * *(WT . V l , ' '' ; '

^m'&fA^SEutiviiniJur^&jrf&S y.^|SEp46:Wfp

,; ' ;. Cv ,;,.-. .;- v* .iiM'a vi' k t**u\^,'A ', l. 'N.tfc.;^;*i:^ ' : i-t.ll jMtfV'AiferVS.iS'J

*S.i KJPSS'.^Si-/!**^!"WJf^WMfSS.iW

"***Sws^-*•p.feimm mm 'Kif. y^KKtA1 ^-fcfMS M\''*V'?FWf rfMi-W,; ^.ji^cASM. J3iii.VMviv 4

itfA.tyM.*

Wtft^c-.'.; ^f:*M M*sem:*: K?y^

•Wvife

Ki ^s:*ay"i

!i^•M

"PIfAp.'

ito: yp

LOCATION " BlliSf lAXS - CrtLd 25-2 -IWiW^ttbAi i^y?cdr*lT 27Aa ftr^l^WPtfily ^/*n.lHCLE-NO.""B-25-71-'? "*W.COQt vzEHtt !prAq!N"^-B !D ! ^ -^50 :o'crtl35* u, K/ }I C ^^CD oy-^i-'MeCtOloeh !CA~ C •J*1?' 29/71 ;^hLEVATfON'- c -?O V ' "*" OD,0 ' 10.OuO.O .IA.&

t' A" * t"t' r' I2^*OOV -(^COAQTI .pc 270 W ^AVO'' r ^!A c'SAY^ ̂-'-"i"

; G C O'OG'CA' oc^cqto-" ! O^ ! 'NO. i F9CM - "^ -w t Dru i 1 ^ ! 1'— v'Caslaic 1 : : ! ! 1 , S ^ -^JIX&Tlc to Istsmcdlate Xcta Tolcanic? Cande?lte) i i i i j i : ' ;^^

i j ! Mineralogy s ' ; i i i j 1 i -—i-.1 ; aj dark nine-rails (hornblendt. fr biotite?) chloritized i '', . l

*b) plagioclase ' ' ' [

Texture: -rery fine grained, equigranular. , . : '' , ' Structure i Flov banding? Some bands are distinct color : : , '*

j bands (light Ii3se green) 0.5^^ to leo wide - bands are due -\ to , plagioclase concentration. Other bands are indlstinctl-re . ' . :

1 ! -"'-^1 ! "*:*-.-

f ! " ' '""1

t ; 'Vri.V

. ' ' color bands •-itJi only 3ilnor color difference from one : ,: ; 1 ' , f"—- *^^1 ! -~- '' band to another. These bands are fairly Irregular in ' : , i ; :l Ozj^i sI^T' ""' : -'

outline and rary greatly' In vldth O.Szan to 2ca; d*rkerbands resnlt Troc biotite concentration

rtg layers - talnor quart* reinlets (about Rrsa vide -5 *J!

parallel to foliation) ~-| l

Rock is foliated^ contact ylth pext rock is lost as CO, 1.1

a result of no core froa 1A.6 to 15.6 - Lost Core. j* ac,

tL5.6 ;36.0 * Internediate Meta Volcanics. Tery sinilar to rock of - i i 1 ^ 1 ~~ ^*~~^ J -' "'- :--

! ; 1O. O to 14.6 but vlth generally less chloritic alteration j ; t [ i

;

:of dark Minerals and aore ^ilte feldspar. Also banding ! j I 1

i ; all indistinct. Grades into next rock. 1 i i i 1

J '. l 20.1 - 20. 6 and 25.1 - 25.Zf - Lost Core. i i l l \

36.0 ;55.O 'Mafic to Intermediate Keta Volcanics. As described for 10.0 to 1 ! - \

i i "- "

l 1 -;-l i ---; '

but slightly higher percentage dark minerals and

chloritic alteration of dark minerals; banding all indistinct.

Contact vlth neoct r^ck Kratdatlonal .

jLOCATION'

P""""~~")CCt~C Oc"ACJ f ?SX^ S —————— , ——————— i ——— &AJSG ———————

VATtO* 'LAT'TUCEr^pQv j TO ii 55.0 t 59.6 |

G c O ? O G f C A tKafic Met*. Volca&ies

jUKiui — u ^T -j^j^pp- - - -|t;^\^per* -' " ' 'WCLE1 NO. B-25-71-3 'L*" " r- ' t I* ' — *- Pi^e WO 2 '" ~

f-^AT^'^ f^ AV PrCq ; A ^^AY^ 4:r-,,^- " f " ; -o i ' ^r* kx. u ' ' ' ' -'v 'r-

Ccorase erftlsed asdesite) Slailar '' i \ \ l \ \ \ ^ :f i ' to rock of 1O. O — 1^.6 but very coarse graiaed and ; r - - \ \

; - banding less distinct. Contact with next rock type gradational. ' ' . i ', J

: 59.6 L SO-*1 i

^ ' i

Kafic Meta Volcanlcr (andesite? Slstllar to rock of 55-O-59-6 but i . } r ;' 'with tnterbands of fine grained raafi- zaaterial. : t ' - ; ; i ;Contact with next rock type fairly isharp. j ' - ', ; ! r

' ; ' Mineralogy: ; - : ' ! :

•; *

t . i"

w ————— f —————— L

t , i ' ii i

: 1 ff V

; 81. "3 ; 88.0 !

a) dark minerals - hornblende at biotite - 50?, highly chloriti^ed ! : : \ \ * : '^b) plagioclase - 2O— 40^ f ; ' ' ', ^ ' '

c) siliceous pebbles - 2O-30^ ' i . . ; f^ \d) at 82.7 - trace pyrrhotite S' chalcopyrite. . | - - ' ; / /?5^""'"""'-—tfcr ^.'"'"

Texture: Siliceous pebbles (2rm to 3cn) statix — verr coarse grained ' t '. - ' /*r f.1 **6/ "—————————————————————————— C ————————————————————————————————————————————————————— . —— , ———————— i —————————————————————————— , ———————— . —— i^, fVVg —— —— —— cff ——— .

Structure: moderatelr foliated, stretching of pebbles parallel, to i i - ' l '0-^*^ ^ t*?y; ' ; ', f /"*r? '5::5* i *^ ^ lf^^ntfor^^ Contact with next rock type sharp. ; j ' ; 5 l-t?^,, : ^o *^|

Mafic Keta Volcanic (andesite? very slssllar ro^v type to ; : i ''•It* "^ 'IT* ^n: i 36.0-55.0. Contact with next rock type gradational. : \ - ' if"" ^ fef *7 L

f 88. C ! 90.6 j Brecciated Mafic Volcanics. Slailar to 83.3-88.O but slightly t i s \ ^^ f ,^/ T ' :.---: ! brecciated. Contact with next rock type gradational. - -is "~--— ̂4,.^^-^

' 90.6 i 92.0 ' Brecciated Mafic Aggloioerate . Similar to rock of 80.6-83.3 but | j t -j

i f j KtTiirhtlr brecciated. Contact with next rock cn*(4*tif*^*lL ! ' l t 1 "

i 92.0 ; 106.2J Brecciated Mafic Volcanics. Stellar to rock of 36. 0-85. 0 but with j ' f j | "; j ! quartz veinlets (up to l*ca) \ i ' i t

' 106.2 135.0: i i1 t i

Mafic Meta Volcanics (andesite). As described for 59.7-8C.6 bbt i . l . { \ :noted also were irregular sharp discordant (to foliation?! | j i '- \ - - \ - - jbleb g e? m* rf ̂

andesite (blebs

^ ^ . . ,, . ( , f - i ! | /7 1 *)Sy i

especially noted near 106.2?. These- blebal ssay | ! ' V * —^^^2^6^^ \ ~;' -| - l represent fragments of an agglomerate (aafic) -or they-Kay |only-be - --j--- -- . - ^— -. - ~ ;i. --.. ~-. .........j -. :-

irregularities brought on by the flow oT andesite? f EJTD OF EOLB ^

LOG BAJULJZ PIOJICTLOG AT t CM Billet Ldce Crktl 25-2 i*i^lL4wue4ji 2^/7/71

v . KeCnlloef.W 1 CVA

l COOK-QQV1 ! "'"C210 V ^.-J^.

Cio.o r 10.o casing'10. O Xafie Met* Volcanic* (And**!!*)

*) eMeritt**4 biotite - SOJt

b) elaclcc)4) Pj-rlt* - Tr*c*.

Texturefine crained to coarse trained (cyclic)

Street-are tveil foliated? distinct groen fr vhito layers of dark ft light

concentration* respectively (lim to Sem) through

vbite layer P aro often ditcoatiBvov*, *(M4rvkat irregpilar

in *hap* they tend to follov foliation. Layer* alvo rary

13.2 .65.4 i Mafic Keta Toj Mineralogy s

a) Slightli b) calcici | c) Quarts

: d) Pyrite

; - Textile;i l medium to

; Structure s

' . '". .. KAg*v* *-*7rf * —————————— i ————————————t -

; i ; ; ; jfcj^ ^* ^1 l --:lcanic. (Ande.ite) i . . , ; tl^ g- j ^7 \ y

• - — t r t f f fTx" ^* I *f~l ' T*

! i ! ! i 1 fc^v-j ^ ' e?/ "* i :y chloritixed biotite and aJiphibole - 50JS i ; i i t -— -iZ^ ^S/ i '-'-'placi*cla*e - 45/C : s i ! ; j " T~^ ;———————————————————————————————————————————————— i —————— i —————— t ————————————— ; —————— ( ————————————— ( ———- sjc i i i i : ' ; i , .O pyrrhotite — trace *o*tly along break* in core^ :- \ ', - | j

f i ! t - ' t l :fine t^*ined (cyclic) , 1 t 1 i [ | )

i i j j /l \ J^ S?^ I.. -- ;

foliated " vfrlte. and dark layorg ae in rook ——— i ————— '- ——— ..-i ——— . \- . ./—^^—^- ^^^'^^^' \ . "-- - - t i -1 eonelnne^. . '*. . . . i '

........ .... .-. . ... .... .j.-...-., i L . } . . . j li . . i . . .. j ,:^

ON3 OPLo c A T ? o \' ; ' "' '" L " L ~- " IfcJ&Wpff*?*'1 s ' ' l i . .. " . -(COR- 3"Z^ - S r A ̂ 'N-'G- : D'^ '^.cc:~'ri ; H . U/ LC

[E. LEV AT ' O*^ ' A "^ ' *" U D E Ccc'Ay"r! 'n- ~ ~; r r?CV ' T C ' G c O ' C G ? C A ' ^ c 3 C 3 ' P T -CM' ! ' immediately abor-e rock but lasers aot s? r*i?*titi*us or

*; -i^^cwcn JHC' E NO. w ?^-7?-4 - :GC- PD ov ;: CA~- Pac* *** 2^AV^'^^!A5-SA V S ;

l ' - : j ' 1

f ; j ! ; ( | l

t , . numerous? also layers here are not as ob-rieus by rar iati*a i* '- \ ! ; ; ' t- ' ' grain vise, as ia abore rock. Tery fine layering alsw as.* fi ^ ~

' . : f 1 i ' i"

' result of fiotit* concentration variation. ' " ' ; : :-' 65.4 :. 75.4 . Felsic Tolcanics: L i Kiaeralo^y:

a) dark minerals 5 to 10* mostly biotite: '. b) quarts and f*ld*?*r (vfcite) aboat 75*| i c) Sericite (about 15 to 20?)

- ' ] Texture:1 medium to fin grained plates of mica

: ' Structure:

t . , ;

1':

.

i ! " ^ ' ' i' - ' finely layered as a result of rariations ia c one eat rat ioa* - ; : (/ /^^^^^^ t'.- ' ' of dark minerals and rariation in grain size. Kodermt*ly , ; t ' - /^ ^^ *^/ ~-

1 ; foliated (parallel to layerings);75.4 ^78.7 ' Feldspar Quarts Porphyry (Felsic Tuff)

1 ' i- ! ? ^CJ^^ 8 /^ ^f -'l f i- J O f*1*^ ^" A f

j ; ; ; '/?? ^ ;^T ^Y* ^. i rery similar to rock of 65.4 to 75.4*e*cept for less distinct . ' l fei ^ ̂ Z/ \ i; ' layering aad except for texture.

: ' : Tezturer . ;-' j ] ; l 7 j. "^ c^ c 7 ! ;r ; l ' 1 i -C^s? i c 7 i1 . ' l ' ! — -^ ^/*: l

! ; Porphyritic, phenocrysts of quarts and feldspar (10J *f r*Ck) i j ; ^*^-^.^i -rt I \: ! : and about 1mm in diameter. Contact vith next rock typ* sluirp. i l i i | ;, 78.7 -81.8 ' Xafic Keta Tolcaaics - Andesite. 75.7 *o 7?.? - Con^t^tw

as described for rock of 13.2 to 65.4 but irith 3"vri4* mm-J ————— .i . ...j..... ... .1—.... .. —— L..... . .. t ! ;

4 i ! i t : i i i; : of massire pyrrhotite - 80* in *pper 3* of rock along cratAct ; i j i 1 1, vith rock immediately abore. Also lesser amounts abotrt S**tO* i l j /? j! /f^7

• - - - - - — i ———— TtAssiyp p-rrrhotito la ropt of rook. —— Coatae* vi t k aeait -f+i

! .

1 i - ' /x iii ^ f~ 'ff1 ^~~y' ' ^^ilt it grftdatiega.il ——— ' ————— ?'*~JL~~^^ — **^~~r^~''^ —— i ———-' i ! - icoatiased.. J . . . ; ..•1 i 1 ' i :i 1 f

•" ;: *"'sT~-- -*f'- - * --t

DtAVONP 'QPtll 'HOL LOGLOG AT r ON, vi-ULLED &V

.CORE •S& TNG,t r i ' i-- r1 S A V

TO j G E O O NO.A v

gj.S F*Id*yar For?!t7Titic Kafic Tolcaaie ~ similar to rockbttt eoataia* pJieaecrrst*. T of brok*at vtiit* f*ld*par about"

0.5 to le* la dia**t*r makiac about of rock,03.2 7.01.6 i Mafic K*ta TolcanCJi (Aad**it*)

similar to rock 13.2 t* 65.4 but twxtar* i* fin*to coars* grained (cyclic) Mid l*7*riag dop*nd* mor* apon

t*xtnr* than graia sis

o

r-.Ol f" l GC /VI ION

KAV\7\c4iE l /..K?: P, AN MO..IvV3

25-71-1 ^ B-25-71-3 B-25;71-4 -4S0 135' -45*102*

•. is-v-.'Jf, .f" :^IV,'* IIIv v--;y,yy|* 'k, .yyyyy^. ^ c'.v

r**cft(PATRICIA

MININO ofv.

SEP l fi 1971

•t -'

:v;y":^i| p ;.v^-i*^ mi-' s:*\';tm' -n'*,

ki\-'^^^;*;W :ii; •;' 'V.'^v** ^''iw^rti 'f?^ ; ': . : . :-- v ;'^' '' -.••- ' - ,' : l ' .-- ,' -"-, ; ''-, : '"';1 ^•'^'^^'iVt^M'ijm.'^f^-' 'V y--'' 1 '.- /'' :-.- '''''-: ' ; -'y : ';'^ -y'''i ^^'I^^I^S'iii-'pi-•, v s '••'A.y^.- -'...- -.-'? " ; ' ''--;- y..' .^./'V'.-vv^vi •^•^^W^M^a-^f'.'..•':V ': v','iJ ^-,, : " ' ' ..v', . : .,.-r-.:', ,;iv-:':i X?A ;**4^f^*^"^^*'^*-

•- i'-ki'^t'S-'ii^i; ' ^ - -''-''''--'''--"-t'1 ' 1 '" -^ v*'* *- f-'' ' ;:'' : -' : * ^^AlffiSJI

\A KAWASHE l AKI

"N1 AMT-

l Ml MINING ACT RtPOfeT OF WOKK

it^w'ltt^ (M totl,l,f l 1.1 Vi tt H It r* (, f J* rf,

ra

'f;Tij0iii|i^ Oi vi ilon

^|iv|^WJ1,'.;r : g:; jilW|r : \ fKtftii of Rttwdid Hold*, Mini,'.! lic*nci(^^iMf^fevfc-:.,:.^';" . ''- . ' f'ott Oflic*

ftfubflfd tfe I't 0|'{.lii(? th'i ttii follo*.inQ conliguoui tloin.t

|r; Poyi Ctoirti Me.. l*oyijKv -. ,

Piiial|^":- V! .M. t ,,,...,,ltefei^.i^MK, ; -^ ..

typ* of *wk

Cloitt. No.

e-v-

pil^iiir''' •*a -lifife^'Mfti^AII rtti'iDfti wet p*f'win4d oft M|(ili||;|^irt^;ti|(t d j-'"'-* - -1 '--Cn.d'fr

n, (i) ....(i)

l*

*.CH'* tl.of. 16 t loin,i or* Involvtd otlocK o t(htduU)

HIN1K& MCWt'.tK

i on i - Nc.n,**|^||fj*;f J'*'',i'.!- : : Fftr WttriW|J|(('rli| Stil/f Iftf w Optfilr.j, tif ef Min*t ( Sinking SKoft* of O^ifc A; tool Mlrjlng C^roli

otitii Cot* tMllinj, ' ^oc.tjvi, No. Ofid onrttt of hoUi ot.d diomtttr of to?*. Noiti* ont! oddi*i* of t! drill. Dot*l vlitd tbillirvQ v til dont. Sio'.td cor* IOQ Oivd tl.*Uh iii doplicoi*.

i M *i^'pSiK.t. NoriiM t;.ri oddftlltl of ftitri *,.ft.{,*d in Of^-olirig *qoif.rP ,*.,l ond td* dot*t ond IK:^MI of

M. Proof of OC(iK)! tot! i*,v.1 L* lul.ri.ilt*v viO,ir. 30 0*0/1 of recording.

tt ttolftiJ*oll. Ift li* tfii* of dioft.ofid 01 othn tw* diillir.j Hi* *k*lcii wuil b* iut.tniiud In d^.licolt.

t; M. d in tli* coit of tr6c.|4.)*icol *f.f .*/. f;*;.c-11 ond L.OJ.I in do|.lkii* ir, ut l b* filtd vi t!, ike M.it.iilt t of t*cwdlf.f.

tnfoiinalloh it o* f ollov. t: (Ailfr:!. o lin iftl.it i/oc* ii intuf)ir!*rit)

t*l

hi^Sfe1 fi :?i-.

, tl*4

CO li ft K.,

*ft(*1 fi; Ii*,'sM5i

13S ^ July 27-29/71 I* 2*39909 102 \ July 2f;.I*ii\^771 I'** iiiKiMHUd, ttfcorii, Onltrio.

n

At iof W

^..ft(:*....Ci^MW.W^4....0*UUftA (Poil Off le* Addr*ii)

l l-.Bv* n f-tut-wl o .d Inliit.Dli knc.wltd{|t of t),t foe li Ml fvrlK In Hit r*pori of work onfi***d nti*1 tilt Vrtwlk Of ^ i In* II* (f tOii.* dv'flnQ Ofid/M ofitt ill COr,,pUliC"..

t u fe---"St f l C 1971

. a

iirs

!3TWJ ' r -v;r~~7 ' V