41n16se8887 saunders 13a t saunders 010 file41n16se8887 saunders 13a t saunders 010 ... a jai...

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41N16SE8887 SAUNDERS 13A t SAUNDERS 0 10 THE CONSOLIDATES MINING AND SMELTING COMPANY OF CANADA LIMITED Exploration Division Eastern District 41N/16 ELECTROMAGNETIC SURVEY LOST LAKE PROPERTY TOWNSHIP 2 5, RANGE 2 1, ONTARIO j June 25, 1965 John M. Hamilton SUMMARY A horizontal loop electromagnetic survey was done to check a knwon conductive zone on a 14-chain group optioned by Cominco from the Algoma Central and Hudson Bay Railroad. One conductor was confirmed and a second one was found. A drill check of at least one of these is warranted. INTRODUCTION Fourteen claims, numbers SSM-67660 to SSM-67673 inclusive, are located in Township 25, Range 21, and can be reached by air from Wawa (32 miles). A one-half mile trail from an old campsite on the east side of Lost Lake provides access to picket line 1SE. The claims are held by Cominco under option from ACHBR, whose staff carried out geological mapping, a vertical loop electromagnetic survey, and a magnetometer survey over the entire group on lines spaced 400 feet apart. ELECTROMAGNETIC SURVEY The present survey was carried out with an ABEM Minigun horizontal loop electromagnetometer, frequency 3520 c.p.s., coil spacing 200 feet by J. Hamilton and R. Bentley on June 11, 1965. Reading interval was nominally 100 feet, and this was reduced to 50 feet over conductive zones. One-quarter mile of Line 16E and 20E were surveyed. Conductive zones apparently join in the manner shown. The strongest anomaly, at 16S on Line 20E, has excellent conductivity. Apparent depth to top is 60 feet at that point, and increases to 85 feet at 18S on Line 16E. Apparently this conductor dips steeply north. This conductor should be tested by collaring a diamond drill hole at least 300 feet long at 14+50S on Line 20E. Bearing of recommended hole is 175 0 , dip -45 0 . A short (400-feet?) conductor at 12S on Line 16E, which was not detected with vertical loop equipment, was found by the present survey. It has good conductivity. Indicated depth to top is 75 feet, and apparent dip is about 60 0 south. If results from the first drill are encouraging, this conductor should be tested by collaring a hole at least 300 feet long at 14+25S on Line 16E. Bearing of this hole is 355 0 , dip -45".

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Page 1: 41N16SE8887 SAUNDERS 13A t SAUNDERS 010 file41N16SE8887 SAUNDERS 13A t SAUNDERS 010 ... a Jai conduc'tlvo aono on ... nuri'ooi-a GS^T-GVCGO to SSK-C7073 inclusive^ avo

41N16SE8887 SAUNDERS 13A t SAUNDERS 010

THE CONSOLIDATES MINING AND SMELTING COMPANY OF CANADA LIMITED

Exploration Division Eastern District

41N/16

ELECTROMAGNETIC SURVEY

LOST LAKE PROPERTY

TOWNSHIP 2 5, RANGE 2 1, ONTARIO j

June 25, 1965 John M. Hamilton

SUMMARY

A horizontal loop electromagnetic survey was done to check a knwon conductive zone on a 14-chain group optioned by Cominco from the Algoma Central and Hudson Bay Railroad.

One conductor was confirmed and a second one was found. A drill check of at least one of these is warranted.

INTRODUCTION

Fourteen claims, numbers SSM-67660 to SSM-67673 inclusive, are located in Township 25, Range 21, and can be reached by air from Wawa (32 miles). A one-half mile trail from an old campsite on the east side of Lost Lake provides access to picket line 1SE. The claims are held by Cominco under option from ACHBR, whose staff carried out geological mapping, a vertical loop electromagnetic survey, and a magnetometer survey over the entire group on lines spaced 400 feet apart.

ELECTROMAGNETIC SURVEY

The present survey was carried out with an ABEM Minigun horizontal loop electromagnetometer, frequency 3520 c.p.s., coil spacing 200 feet by J. Hamilton and R. Bentley on June 11, 1965. Reading interval was nominally 100 feet, and this was reduced to 50 feet over conductive zones. One-quarter mile of Line 16E and 20E were surveyed.

Conductive zones apparently join in the manner shown. The strongest anomaly, at 16S on Line 20E, has excellent conductivity. Apparent depth to top is 60 feet at that point, and increases to 85 feet at 18S on Line 16E. Apparently this conductor dips steeply north. This conductor should be tested by collaring a diamond drill hole at least 300 feet long at 14+50S on Line 20E. Bearing of recommended hole is 175 0 , dip -45 0 .

A short (400-feet?) conductor at 12S on Line 16E, which was not detected with vertical loop equipment, was found by the present survey. It has good conductivity. Indicated depth to top is 75 feet, and apparent dip is about 60 0 south. If results from the first drill are encouraging, this conductor should be tested by collaring a hole at least 300 feet long at 14+25S on Line 16E. Bearing of this hole is 355 0 , dip -45".

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1^; : X-'V-: ; - 2 - ' -" : ; y

: , If drilling results are encouraging, the anomalous area should be electromagnetically surveyed in detail with a 200-feet coil spacing on Lines spaced 100 feet apart, in order to guide future drilling.

No magnetic anomalies are associated with these conductors. Magnetic anomalies in the are trend northeast, and suggest that depth to magnetic bodies is from 50 to 70 feet.

1.

2.

3.

CONCLUSIONS

Two conductors, having good to excellent conducitivty, were found. One of these had not been found by the previous vertical loop survey.

The position of the best conductor has been shifted along Line 20E, about 75 feet north of the position indicated by the vertical loop survey; the new position is believed to be more accurate.

Since drilling recommended on the basis of vertical loop data probably would have missed the conductor, horizontal loop checks are suggested for all future vertical loop anomalies before drill sites are chosen.

RECOMMENDATIONS

1. The conductors warrant investigation by one, and perhaps two diamond drill holes, positioned as indicated in the section entitled "Electromagnetic Survey".

2. Drill sites previously suggested on the basis of vertical loop data should be disregarded.

Submitted by

Endorsed by

JMH:hcJune 25, 1965Attachments (1)

Exploration Div, Mt.lTrail

Chief Exploration Geologist Eastern District Property file Toronto Office J.H.

John M. Hamilton Exploration Assistant.

George D. Tikkanon,Senior Exploration Geophysicist

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tiftfgK?''^*:^p:^;,;-:;;

...-* -' '' ---- T}r**Av: --'.--' , i*..- xiT*.:-- .r."t CXTLTIT;."/ CWW^Y c? CATICA

g t. 4X7X0 n*****7'*. s ve s f y

K f

n.? gpj i sea Jcira K,

A horisoatal loo;j olcctronssnotio s.u:-voy ^TIO dono to choc!: a Jai conduc'tlvo aono on a K-clnia croup optioned by Coainco frou Central nad KuOtoa Cay Jiall?oad 4

Cno conductor T.UO coni'liviod dnd a accord ono vaa i cbocU oi at least csa of thoso iu \vayra::tod ,

.. A drill

Fcurtcon claius, nuri'ooi-a GS^T-GVCGO to SSK-C7073 inclusive^ avo located in 'i07,753lii.p 23, fovijjc :;lj ami can Ijo a-caohcd by air Srca Vnua (32 nilco) . A cnc-huJ,^ niXo trail *rorj r*n olcl csr.psiwO ou tho cs.-t ci-Ju o2 Lost LaUo provides access to1 picket lino 1C3. 7Lo claims aro hold by Coaicco under oiiticn froa AC'.'.'ir^, uhcrio cta.fi: cr.rriod cut ^ooioaical cappitJSj, o vortical loop olceti'o.-ir.jyr.otio oui*vay8 and a uasr.otouotor cur- voy ovoi-'tho o:\tivo croup cii lir.as opaccci ^CD ioot apart,

?Uo proooat cr.rvoy vafl civi-icd out with aa ASir.i I*ini3i:i; I&rfcu loo? cloctrci'MicttOtesotc", frccjuc-ucy'352D c.;?.:;., coil Ci-ucin^ 2DO *o;

(,by J* llanllto,n ar.d R. Uot;tloy v.\ Juno II, 1002. r.ciiiir,;; it'corvul v/a: ncaisnlly 10^ i'cot, arid tbio vma rcch.:cod to 00 foot ovo? conductive

ciilo oi' Liuoo 1O3 arid :i32 uoro wurvoyod.

asaoc Oiir/f-roayly Jo to ir. tUs i^miar shows;. **J:oCUM?' ily, at 1C3 on Liso 20^3, fcus ecrcoilon't conductivity* /i:;^aro:.t depth to top la CD foot at that paint, and JJICIY~.-a to i50 2cct at 123 c:: Lii'iO 1C3. Apjaroatiy this couductor dipo otocpiy coriii. ?hlo couiluctoi* should bc tootod by coll&ytKS a fiianoncl drill holo ct lount SOO Jeot lo^a at l^SOS ou Lij;o SOS.

SJ3 oS voccesiondod holo is 173 0 . dip -3tt0 * f-

A cboi-t (tfOO-foct?) caaCisctoy at 12S en Lias 10S, ubicli was not

conductor* nhouid bo toatorl Uy collarirs o Solo at least 000 loot 14*2DS en Llr,o 102. Ucarias oi t'aio holo is 305", dip -400 *

il^^i ', ; '-'-'. -. ' * ||'^V^V : S ' , 2f driliir.s rcculta avo onco'itvasliiSj tUo anomlcuo urea choulti bo ^i^'i^ oloctrotsicnotically survoyod in detail with a 200-foot coil ot^cins en li "lil^ isuacocl 100 loot opart, la ordor to euldo iaturo driiliaz*

uflr;r''i':'..'.' , ..-.-. ' . . ,- :'^.--

sne&al&cs cro aacocia'cod v?ith tu-ei*o concSuctorc. i in tUo area tror/J northeast, or,d ou^acot tiut depth to K&S.

la from 00 to 70 foot.

S SM-7 3 6 j

' , ' -. ;-- ".'- , ' ';'-- .;- - ' - T',.'; "A, ' -

^'.'SVj -' ; --: ,'*^ :-i\-:^..-;:.C:'''; ;; , : ;-; ^ v-'^'^v;^

'^ * 'l**?|^ll^fe^ '

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-2-

it Two cosductora, l:avlr.3 C'^* to cscollro't conductivity, faro Swir.d. Oao o* tboso lujcl net boju *cu::;3 by wluj pvovlcao vortical loo^ curvoy.

. Vfco p^^ition of Clio Jx:^t cov/.&ctG? !^ia bocn clii*tccl alor^ Liao SGH:, alxwt VO foot tiortJi oi ti;o poc;tiicu ir-dlcatod by tho vor'tical lco^ curvoy; t bo now position to lx*iiovi-d to bo ao*-o accui-ato.

S* , Cteco drillitts rocciuc:icJc'tJ f/:: tho fcijirs ci vortical loo? c^.ts pro'ja5;ly voald loa\xi snicsioci tbc; ccc'-lcctor* hor^cr/val loo;? choci:y arc au,*;c'Ci2tccl for all futuro vorticxil leo;/ c:icur.lioo to2ovo drill oltoi oa-o cic-an.

l* 7ho coaUuctoi'o v/ari'cnt invcat Ration I/y cno, and porJ;av;j tvo tiicuxaddrill Ijolca, p-cultio:i0w us Indicated in tl:o sootioa ontitlod "Eloctrc-

j oasaotic Sui-voy".

2* Drill aitca proviouoly cuGjejtod oa the basis of vortical loop titita chould bo

Su'caittod by:

Jwr:o 25, 10G5 (1)

Exploration Div.. Ktl

. Ciiiof Exii raisto:*n District I*i'orx?i"ty Jilo Toronto W*ico

ioa Gcophyaicist,

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LEGEMDINSTRUMENT : ABEM MINIGUKJ

, \ COIL SPACING : 200 FEET.B 1?' FREQUE.NCY : 352O c.p.s.0^ ^ IN-* 1 L* * 1 ^* l f " * ^ — - *™ -— - | -^ - - . — . — — .•PHASE OKI THE LEFT

o OUT OF PHASE ON THE RIGHT.0 2

y g CONDUCTORS: —— ̂ c^- strong ——— Weak*l r* ~ O51 a ^^

sl h CONDUCTIVITY:. E- excellent F. fair1 O. good P. f^oorl MARSH:- ^

The Consolidated Mining and Smelting Company of Canada LimitedDRAWN DTI -, ^ TRACCO BYI

H- K.

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ZLECTftOMAGNZTtC SURVEY

'.OST LAKE PROPERTYAGAWA AREA, ONTARIO.

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Page 6: 41N16SE8887 SAUNDERS 13A t SAUNDERS 010 file41N16SE8887 SAUNDERS 13A t SAUNDERS 010 ... a Jai conduc'tlvo aono on ... nuri'ooi-a GS^T-GVCGO to SSK-C7073 inclusive^ avo

IliittP^DIAMOND DRILL GEOLOGICAL LOG

4O *CAUt

oaJecnvE: To deteroino cause of Z M. Conductor S/ ̂ ,* n -t-

LOGGED BY:S.R. Snodtn

DATE:

BLOCKi

18*

23 '

76*

RQ*

97'

18*

28*

76*

30*

97'

107'

18 August 1965seCT.,L2*20W

2*93S

SAMPLED: 120*-128*

COMPOSITES:

••LAC* Dave LakeR 21 Tu-p 25 S*-"*

Aff. B CAH.i327*

DISCARD! REASON:Sault Ste Jlario H.D.

Started Aug. nth/65 Finiched; Aug. IS/65

265'

Casing. - Overburden s^ey sand with boulders.

- Dark greea ?̂ eyf eediusi to flee, grained, fairly hard, BQderately veil foliated at S5O to core

Ions axis. A feu narrou quartz and calcite veins parallel to foliation* ChlorJtiacd around 27*. A few small blebs

of pyrite end pyrrhotite (Sat, trnce) disseminated throughout unit. A fea saall blebs of chalcopyrite around 23' in

calcite vein._____ ________________________________________________

Hornblende fabbro - Probably a dyke but s'nowir; mixing arouad contacts). Dark ftrcca. coorce nrcinedf hard ? massive*

Hell developed large interlocking crystals ci fibrous hornblende (Est 6Cfc) altered in places to...chlorite, and soaller

crystals of feldspar (Eot. 357.). Grades into finer grained rock around 33*..and between 60* and 42*. A fea trresular

quartz calcite vetno. Upper contact p.radotional, BetTvJcen 75*-75* horncbloido occurs concentrate*! in patches atnd anall

brown crystals cf plilogoptttc otca? coraaca. Pyrite (Est. trace) os caall Mcba dioscaiuatcd throughout l unit. A feu

pyrrhotite bctveca 70* and 75*, A fea saall blebs of chalcopyrite in a calcite vein around 48**, . . ^^^

mediua grained, soft, very uavy creaulatcd foliation at about 45O to coro long axis. HtpMy

chloritizcd. Upper contact ftradaticoal

Altcrfd Paslc Votccn5.c8 - Park grey netUtvi grained,, foliatc-.t at 45O to cora long ajjtis. Hore heavily chloritiscd Uian

18*-23*. Calcite occurs os a few voinleto and aa narrow visps parallel to foliation pyrrhotite (Est. trace) occuro aa a

few saall disseminated blebs throughout unit, a fca saall syccka of pyrite between 90* and 97** Top l ft, (SO'-Sl*) of

unit is chilled tasdiun nrey bro;jnf rxlaasyf hard* Op?er contact xxiyy,shagpf cUscordcuit at 60O to core long axio. -i

Pyrrhotite (Sst. trace between SO* - 81*) occurs as aaall veinlcta in chilled part.

I'ornblcndc i (vibbro - Probably dyke but shotting nixing around ccntacto). Satae as 28*-76*. 106*-107* finer grained and

slightly foliated at SO0 to core long axis* Ppper contact obscured (core broken) but appearsoharp and concordant with foliatioa of overlying unit. A feu flattened blebs of pyrrhotite

occur arouad 106*.

cone size

AXT

HOLE NO.

D.L-1PAGC

GroG

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;COMI*CO 2307— J..M. -

ip DIAMOND DRILL GEOLOGICAL LOGOBJECTIVE: SAMPLED:

LOGGED BY: DATE: COMPOSITES:

•LOCKt SECT.i PlACCi APP. BEAR. i APR.: DIP.:

FROM

107*

120*

128*

TO

120*

12S*

245*

DISCARD! . REASON:

-,;

LEHOTHi

AXtcrpd r-.iaic Volcanics - Dark p.reen Rreyt fine grained, fairly hard, foliated at 45O to core long axis. Upper contact

Crr^nfi"nal . *'™y n^r-rw r^Mf-o nnrl rhlnrfri* rich ln^nda nnrall**! to foliation, ryrrbotfte (Er,t. traca) occurs OSs-inll blebs diueeninnted throuriiout unit. A feu blebs (KTJ!!) of ci:alcopyrite occur around 113* in a calcite vein.

^Mtsrjrv"i i*-"."?*.**. Volc^Mcn -Sa™e aa 107 '-120* but contains Irresulcr veins (up to 0.2* wide) of pyrrhotite (Zst. 25^) .Chalcopyrite (Est. 0.37,) as czall vcinlets associated with pyrrhotite veining arcuad 123* and

Sw.plcd 120*-12S*

126*.

12S*-16*f- - Sase as 107*-120*. Foliation at 55O to core long axis. Pyrr-iot* -s (Eat. trace) occurs aa srull dicccr.iinatcblobs Hiro^Tic.it unit. Cnalco^vrite C2st. trace) occurs as o feu cnall blebs around 154* ond as snv.ll veinlet at 159* .

l^'-^yy'Rlu* grey fine (jreined-, very hard, foliated at 60O to core Ions axis. HicJily silicified except betceen 176*-17I!"p**r ear*tnct cb-irp and conrord^nt tjitli foliation. Pyrrhotite (Est. l7y2Z) ao cr^ail blcba dioccsiinatcJ throughout unit^nd as 0.2* veinlet et 167* and befcw.cn 173* and 174* no a.'.nller irregular vcinlcts. A few e:(tfst. tract*) a t in rtrrnr rttroi'.-hot.t unit. 177*-245*. S^c aa 107*-120*. Foliation at 60O to

yill blebs of pyritecore lens: axis. Upper

contact charp and concordant with foliation very little calcite vcinins bettreea 117* - 185* and 230*-245*. Pyrrhotite(Ect. trace) occurs oa sr^all blebs disseminated throuchcut unit. A few croal 1 spccha of chalcopyrite occur around 225*.

Core Recovery 93Z

CORC SIZC

HOLE NO. PAGE

J).L./ 2

1^^:-4O SCALC

COLO* n.OT k VIP* 1 OH* CI.AMI* * AV**.

O— pi —————— ——————————

llo.

406750

i

i*

Length

8*

1

CO CO

I

Cu Ut

03X trace

i

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\

LEGEND

OVERBURDEN

ALTERED BASIC VOLCANICS

HORNBLENDE 6ABBRO

CRENULATEDSCHIST

ALTERED BAS WITH PYRRHOT

CHLORITE

VOLCANICS E VEINS

SSM-736.-

Consolidated Mining and Smelting Company of Canada IgnitedDRILL HOLE SECTION DL- l

AGAWA PROJECT

TWP 25 R21 ONTARIO1965 ; 'Wtf:

Page 9: 41N16SE8887 SAUNDERS 13A t SAUNDERS 010 file41N16SE8887 SAUNDERS 13A t SAUNDERS 010 ... a Jai conduc'tlvo aono on ... nuri'ooi-a GS^T-GVCGO to SSK-C7073 inclusive^ avo

I

f;-

• BASE UNE

S,SM 67001

LEGEND

Claim Line Conductor Drill Hole o

SSM-736-^The Consolidated Mining and Smelting Company of Canada Limited

IlVrtl* tt l^jriOATt B, - - ttVIUOJT

TUCtD IY:

DAtfPLAN D.D.H. D.Lrl

AGAWA PROJECT TWP25; R21 ONTARIO

1965

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0/0

l.

/\'V5." M

26O

Page 11: 41N16SE8887 SAUNDERS 13A t SAUNDERS 010 file41N16SE8887 SAUNDERS 13A t SAUNDERS 010 ... a Jai conduc'tlvo aono on ... nuri'ooi-a GS^T-GVCGO to SSK-C7073 inclusive^ avo

flkVS ". Y ^ *^.-' ~ " "'•lCOMtNCQ 25O7-NJ

DIAMOND DRILL GEOLOGICAL LOG

'

SCALE

ftOGGED BY

•LOCKt

O

tr*.le SevTV ot t* f* fo^Jo^frojf

DATE: - l

TO DISCARD:

L 5oE 1^*90S.

SAMPLED:

COMPOSITES:

x -^ v-

r LwkfAPR. BEAR.: API": DIP: —— J-t-* LENGTH

REASON:-vt A fl/MtS -. . \ U t-U

S AJ)

*P ..r f AY S"/3 r.

^ STAJ"

^ ' )

——e

17.)gys

vtoccrMiA

l A ^A^ r edjjt-*.9i

JM

( f A* O-S"/, j

A-7.^ -

^Juy-w-a

M-gf

cv a)

J?.

fcy

L/l -A

(X C ̂ . pn^ ̂ ^ T gf- .tflMC-^x

st

,cAC 0 -Zcr

A.A^jfJJS J^C^O

. A ft If

-9ft c\JT ^0' "lo-

CORE SIZE

HOLE Nn PACE

1

COLOft ^VOT k oir* O*C C*Jfc**** tt AVC*.

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J -"' ""^ft-.-"^,;-' -SM

DIAMOND DRILL GEOLOGICAL LOGs-^rv .".•..

40 SCM.K

f-vi-

^OBJECTIVE:fe- tLOGGED BY:

•LOCKi

PHOM ' TO OISCAMOi

DATE:

SAMPLED:

COMPOSITES:

LO* H.OT * Dir* 0*K

APR. BEAR ;

g^? as?fll- ftQ* c*

(f JT'A-fi.ctJ XXQ

Q - O 2 C '

\( III

V^ 9.0^ - 1 0*^ 0.1^-220

^^ Q, JA -

A

i(|) txyvai

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CORE size

PACE

2

C

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i*5f^ DIAMOND DRILL GEOLOGICAL LOG^OBJECTIVE:

ED BY:

- BLOCKl

,PNOM

DATE:

SAMPLED:

COMPOSITES:

COCO* PLOT k DIP* 0*K CLASSK* k *V*K.

APP. BEAR: APP : DIP : LCNOTHi

DISCARD:

cv—e.

.

A f g rA^

M-

./i/v^yjtili -JStaJLMLk y/i/fi.M-CkSl&.Q foj. O^yCA^o^tA^^vv ^j/^Xx^tyv^ oJc. V " V p( ~ Wvcv ^•uiTk.^K.UY^*" CA^A±c^jpt J\L ris*\\ o^^A ^yvAMlX^MJA/^ f * p^U-ifo riT^fl

tl A A A^Xxli LAlli* fcLAAPA^^yy^^tg^i .vt^^f^-AA^/lwO-^ ^M^v^ .

. C^L^JJL QCvCo^t^ (XA AtAvCui^xA

^O' .^ C euotyua^CttlviL

( -S**- ®Q**U X^Cjt)

lo'/T) .^/^ fi J.^^* Q

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DIAMOND DRILL GEOLOGICAL LOG

.LOGGED BY:\. Tt i'^. *- -

DATE:

M.OCICI

SAMPLED:

COMPOSITES:

COIOII PLOT A DI** l O** CUkCX* t A***.

LKNOTHi

DISCAMDi MCASONi

flncVx

; r?*, i, very I Ut l a

aa 2i'-43f . flatly JnrVtr r*. l*?'. H7 1 .

vulii, In- .folieticn.

y JnrVtr rr^-r ar*5um!. !"**, frV. SnT*. l?7*. UV , U7*. ?53*. 162*, Tfi7*. 171*~ .-.ctw.M ins'-lll*. 117-12!*, l??*-!?^ 1 . IW'.lSn*, 2-4*-2ri^* 21R*-230', 23S*-

nn lA'.*-l:','i* .1 fnv crt.-irv*;r t AM:! .t (w* to .'!5 f *jtd^ o'? *chlot r-.-r.-silol Co foItAf•-L.-. ^Jm—— ——————— -.. ———-———————— - —————- -f\ ———-—————-—————————— .1—————————-————-^———————^———————— -——.———————.^.^^^ n - ^^^^^

* nrv:*r.sls. Volution *it '.1" t^ core Ion-. aK'.R. Uv-ft*sr cr^itsct jrra^attojal*ott^n contdinin; voll for:-"!.! cMorlc* nrv:*r.sls. Tollitlon *it '.1" t^ core Ion-("•.r'. ^'O ^ 9

234* cVAlcot.-yrlto occurs aa var-.- fau 1*^ ^ vein-:.

c.ilcltc (i'*t. 20r.) an.' tMn!*y^li*.f..t t f-i St r.^0 to lr-r-- ityff*- r-v-t*

as ti- V.lota nsacetate t vich calcic* veintnr api' rtt 7'iA.S 1 .is5. .ir.--! a (5-1 "3) -ftr.'illcl f* /"olfntf-wi. Cinlcv-yrUu (:^r. .it) occurs

(.•'•"5*) Irrrrtular vttlu.

4A *t AS t** c"rc oxin. tto (fntoccurs an a few flcttttno-i Ulch* i!i*sr::!n.net' tV-rctj.'V.out ui't. A of el: sil eckrite

jL

•5*rtffjFWQ7"ji..r..^* T."" t'- Cu. j4jj AU.

r~^ ^^4-

-gfy ."-i'HI H7

*f

cone size

C 'J

CD

-1 .'C

"N

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DIAMOND DRILL GEOLOGICAL LOG

;ED BY* DATE:

"299*

303'

TO

266

303

326

SCCT.I

SAMPLED:

COMPOSITES:

colon n.er * wr* | wtc CLAM** kl 0*1

APF.: OIP.i

OISCAMOl MEASONt

Silicified Schist;D JLU^ tjfiiy JL ii*ti , Irar'!, fol.tacffd flC A5 — to core loon otis. t:ontnr.t irtnh r-vorlytnf. unit sharp and con

cordant* Pyrite and pyrrhotite 0!.-;f:. *'oth trrtpy) aa ap.-ill ^rr-'r-t Ai-.r.i*r-*nntr*J

Srnne as 24*~43* 0hut v/itli vorv Httlfe gfll<'^^f• ---,— , ——Foliation at 50 to core lonjt ax In. Wopnr contact nVnrp md concordant with foliation. ?yritR rtnd pyrrhotite (fts*:.botli -- ~ ~na thi'ou^hout unit

Feldsar oognjiyry Rill

foldsnnr (Fnt 10!^) in .1 fine* — "^ — -— — ' — "Coliacca (ac AS to

. . ant witn foliation. A few snail crystal* of pyrite occur in trnft.

core lonj*. axis. Pcrrliyritic with uoil fomcd pJicnocrysts of white and1'^..^-^ ^...t t........ ,,^.i.^,i... ,t.-^— _ j - _ ̂ .— .' l'!'''* — r****1 — toner ctTuenccii cnarp ona ceticora-

Chlorite Schist ______________ o _________________________________ ^-^———-——-———^^—-—-——-— Saae aa 266 '-299*. Foliation at 50 to core lcmp. .-ctf-s. Pyrrhotite and pyrite (Ks. bctU trr.cc) aa srjll rttssentnatcd——g; — ft fug affall bleta of Chalcopyrite arour. an

Core recovery 96Z

cone size

HOLC MO. \ct

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LEGEND

CHLORITE SCHIST

SILICIFIED SCHIST

SCHIST WITH NARROWPYRRHOTITE VEINS

Consolidated Mining and Smelting Company of Canada Limited

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DIAMOND DRILL GEOLOGICAL LOGTo

^LOGGED BY: S .3

dctexaine caoac of E .H. Conductor A ^;^

, Soodin DATE.- 3th Aug. 765

•LOCKl

;FMOM TO

10'

.22!.

J13J

I

10*23*

33*

113'

114*

SECT., L 20E ^ 17 4- RO S

SAMPLED: 191-194 194-197

COMPOSITES:

DlSCAttOtSault Ste. Marie

APF. BEAK.:355"

Started Aug. 5/65 Finished Aug. 6/65

tKNOT*240 feet

rSClp.? ~ Overburden fine grey and brota* sand.

Oilcrtte gdlf Pt taeditta green Qtey fairly sof t, foliated at 65O to core long axio.

10*-19* rasdiura groined with a feu narrow calcite veins parallel to foliation and oany caall elougatc calcite streaks

parallel to foliation._______________________________________________________________19*-23' finer grained, riany calcite veina (narrow) parallel to foliation. 1Q'-19* more heavily chloritized than 19*-23*

Pyrite (cst, 0.5^) occurs no aaall crystalo 6c elongate blcbo tlirou^out ualts parallel to foliation. At 13* a fcv____

gaall blebs of chalcopyrite in a .25* vide, calcite vein.

-SiilelflpA.Schist, gale blue grey. Cine groined, hard, foliated at 4QQ to core long exis t Upper contact sharp con

cordant with foliation* Mahy calcite veins and elongate vicps of calctta parallel to foliation. Only very slightly

chloritized. Pyrite (EsQ trace) as soall dissealnatcd blebs and crystola.

Chlorite Schist - 33*-65* sarae aa 19-23. Foliation at 45Q to cere long axis. Upper contact obxcured (brofceo core).

57.) as e-.-all Meba .and crystals disgeaio-ctcd throe^iout unit. A few caall blcbo of chalcopyrite occur

37* in a rung t z calcite vein

grey, ginq grainedf fairly hard calcite ao very narrow tricpo parallel to foliation* Foliatioa at 40O to

long flxls. Upper contact r.radational . Pyrite (Eat, trace) as saall dtsscninotcd blebs ̂ A tea caall blebs

of chalcopyrite in a quartz calcite vein around 67*.

57*-113*. Satae ccncra.tly as 10*-19* but aiore coarsely foliated vtth long well developed chlorite crystals.

foliation at A5O to core Ions er.io. Upper contact gradationa!. Pyrite (Ect. 0.57,) and pyrrhotite (Ect. trace) occuro

os snail diseeainatcd blcbo throughout unit.

Sill ~ Rocdish bro\v-n. hard, slii?;itly foliated at A5O to core Ions axis.Porphyritic with uall daveloped pheaocrysts of piuU attd xAitc feldspar in a red broi-n, fine

rralnorl "rrnir.^ T""-- '^^ ̂ nt^r *to*™ and concordant with foliations. Pyrite (got Q.5%) 'da aaall"elonj;3tc bjeba parallel to foliation.

COME SIZE

AXX

CO

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DIAMOND DRILL GEOLOGICAL LOG

LOGGED BY: DATE:

mot* TO

.1351

160'

133*

191'

104*

UO*

133'

191*

1SV

197*

SAMPLED:

COMPOSITES:

APP. BEAM i APP.I DIP.: LCNOTMi

DISCARD!

- Sy-e aa fl5*-57* but fairly soft. Foltotc-J at to core IODJC a r. J. o. U-JTOQT coatact sharp and

ccacordeat vtth foliation. 3e^r lover ceatact thick calcite coining. Pyrite (Cst. trace) 03blebs.

Potrt'/ry Sill - Sasc os 113'*1I4' but Kith cere fclda^tr phc^.ocrysta ar.d also fine wlsoa of cblccite. Faintfoliation at 4S0 to core lou^ a*i3. C(?^cr cc^itact ccacurJatt vlth Ccliatioa but uith plight nialiy; baraccn

lyiaa schist. Pyrite 'tot. 5*.) aa eciall crystjlo tlttcasuout uait._______________________

SeSAgJr ~ Sg.:e aa 65*-57*. Cotvccj 17?*-tS3* cclctta ovcura aa ooay rooro rounOeJ lcaticlco. roliatlon at

to core o^ia. Upper ccatcct c&arp and ccneov*!aat alth foltattoa. Pyrite {Eat* O.S7Q as ec-nll diasoalnatcdunit. A f ga oc^ll btcl*s of chalcopyrite (Ssc. trace) olso occt:r*

~ S^jy; aa 23*-33* l?ut vcsy little calcite vetalnjy very hjrd. rolictloa ac /a50 to core* lencontact sharp concot'Jcat vith toliat?.oa. gyrite (ret. Q.5%) ao aoall dtss43fjlcati*d blabs. A fc-w caall blc';-o of

olao present. ___ ______________________________________. ' g;urc t* t9*"23*. Foliatlca at 45 to cere loos aala. Gppcr contact Pyrite (Cst

occugs ea iraall dles^-i^ntcd blct-s ood btt:-?eea Ul*-*'U,3* aa a gtrj irregular pecallcl to foliation. Pyrrhotite

as disseminate*! bltbs end *jctvs-n 191* - 191.3* c.id li2*-W2.5* cs tbia rc^ylar I\3.i0a parallel to foliation.

Chilccpyrlte cccurs aa a feu blel-a tn a talcite vc-inlnj grcttnd l?210*

Toio .^ bando cf cMorlte ocMccy pycehotite ami vginod c^lcttcy baa-Jo parallel to Collatloa at 4SO to coreaxis. Ujpcr contact O.lrly eliarp a^J co.icortla.it tilth foliation, i'yrrhotitc (Est. 5^-lGl) thcecd Itlcc and

of cblortto ec!)ist er.d calcite aro jeatrally tbickwr. A f au snail blcbo ol cholcopyrlicand ?yrrf\otlte. (Est. both trdcc) also occur.

194*-157* - il~7'

CORE size

HOUt No.

cm.0* PLOT k w**

PAGC

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DIAMOND DRILL GEOLOGICAL LOG

' LOGGED BY:

- BLOCK.

FROM

197

. ̂

TO

246

DISCAROi

DATE:

SECT.: PLACE:

SAMPLED:

COMPOSITES:

APP. BEAR.i APP.: DIP.:

^^JJE^JSSKSM

LENOTMt

REASONi

Chlctitc Schist - ?c~i- as 19 '-23Collation.(tt? to .075'

pyrite (r-t.

f . FoilaeC*tvcoa K7 l -2G2 t ana 20^-214*vide) of a cojcccr, cf(tr.ace) occ-jr es es-jtll

5.0i7 ac ASf Co corvc?rv feu :clc;c*.- ^

2 lcn- Jxli. UpP^r cr^^A.-.r r.J-,irn .*.^rJ .-^-*r*M-rV-j^f *.rl*f*

Vfrlns. S-i'-alL It-i-ith*: cF tht- vn?f -*? fr^

c^.i*r, r^re ehloe-lt Jscd ccM&t parallc-1 to foliation. PvcchotitcOlsscsfssa c r td b I c'-': i A frv !;rn?l blebs c- f r- li alt ^'i-tK. n^r,.

rr.-ft*n N^-i,

(F&t. 0."?") jo-ir ^ r,,,,,J ?."t?t

Cere clever* *77. ^7^ ^.^ y&r^xxtcs^vatcr at 103* 4.** r -r- w^-as-* y^T /OS"'

CORE sue

HIOL.C No. PAGE

3

140 SCAtX |

COLA* *VOT k DIP* 1 on cuk*ac* a AVM. 1

—————

—————

i

J

!

i

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DIAMOND DRILL GEOLOGICAL LOGSAMPLED:

COMPOSITES:

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rDIAMOND DRILL GEOLOGICAL LOG 40 4CM.K

b&lECTIVC:

CO BY: DATE:

•LOCKi

SAMPLED:

COMPOSITES:

APR. BEAM : LCNOTHi

DIBCAMDi

JL

)ctA

^ ("hJ. Ml g X^lf.fo

cl JLAAJgy^^^^JOAiL^I

colon nor m o*** l om cm****

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DIAMOND DRILL GEOLOGICAL LOGcot.0* PLOT * mrn ooc CLAM* a AV*R.

J" ctJ?yLfr CAA^JtftA^/^fAA^Jrr .flQS-'u^AyJ

ULjl ^hv- . LaJAjndG*^. to^

Page 23: 41N16SE8887 SAUNDERS 13A t SAUNDERS 010 file41N16SE8887 SAUNDERS 13A t SAUNDERS 010 ... a Jai conduc'tlvo aono on ... nuri'ooi-a GS^T-GVCGO to SSK-C7073 inclusive^ avo

i*'.'* M -* . .'i i i, -

ijji^-

mfapti®

IK.'' : -

•w' ^.4V,'V: ^

i -' : -:^, onsp-.*-s.-rV -,-,.' ~ -mK-w- * : -' ; A

LEGEND

OVERBURDEN

CHLORITE SCHIST

SILICIFIED SCHIST

FELDSPAR PORPHYRY

SSM-736.

;The,Consolidat^d Mining and Smelting Company of Canada LimitedTUCIDIY: ;

OATI ;^t)RILL HJOLErSECTiON LLS-2'.-^•'i-v'w

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^,

f? (?|;.

l

MM :̂ '**:,^f.m

mz-'i'Claim Line

Hole o

.iW'V-.' - ; P - - '-/'

10 S

S S M

67666

•C

SSM- '

Consolidated Mining and Smelting Company of Canada Limited

Mvnntt -''*TKACIO IT:

Btvnnrr OAT! PLAN ;D OH L L S- 1E c T, ' ' ;

ONTARIO

L L S -2

l200 FEEj|o*Tl'Auflott 19 65

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Page 26: 41N16SE8887 SAUNDERS 13A t SAUNDERS 010 file41N16SE8887 SAUNDERS 13A t SAUNDERS 010 ... a Jai conduc'tlvo aono on ... nuri'ooi-a GS^T-GVCGO to SSK-C7073 inclusive^ avo

41N16SEee07 SAUNDERS13A1 SAUNDERS

,- - . ^ - '•-•'•^.; - " ,';'.. , ,^ ''J.' OfflCt OP MINING RCCOftOCft

900 ^ ."2-

118. SAULT STE. MARIE MINING DIVISIONSAULT STE. MARIE. ONTARIO

ONTARIO

DEPARTMENT OF MINES

August 30th, 1965

The Consolidated Mining 4 Smelting Co. of Canada Ltd., Exploration Division, 1170 Beaver Hall Square, Montreal, Quebec.

Attn: Mr.S.R.Snodin

Gentlemen:

Further to your letter dated August 26th, 1965, I have this day filed work reports for diamond drilling as follows:

74 days on each of SSM 66988-96 inclusive

27.2 days on each of SSM 66997-67005 inclusive

40.8 days on each of SSM 67660-73 inclusive.

Yours truly,

/w A. Jodouin, Mining Recorder.

.* S .M - 7 3 G j '

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til (tut* l (tin

l - ,-!!j l ,

Ac!i^* i*!?2?J*.Z™iJ