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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".
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
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^ '
-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,
firfc.* .-'h'-. :-.t.:-'
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'
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ffel*
f^HHsNEw
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4oi" ___ ̂ 2os^kl-o^^.u^-*V o•V 0 . _____ 22S^,lo
_________..__ __ —2^ S
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.
•tvint'D UT j OAT t ncviiCDnvj- o*'tJ.*A.M. jJ...HXlf X
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IJfeliiiffVii.fl.-fV.t.Xtm'. mM .
Iiite:s5*4,,,,,.,: .,
ZLECTftOMAGNZTtC SURVEY
'.OST LAKE PROPERTYAGAWA AREA, ONTARIO.
*u., '"-g^*p 7et ^MT /m '""'jgr&A1 *** *^ ̂ '-f "~ ( (5 (") RDMiNUO IHfcl
;V--,.A"f^.tfr.,w.,,w ., " - .-..- ',,,v;g;ife
!
;i
-'
;,V'v. ^•,
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
;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
\
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:
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
0/0
l.
/\'V5." M
26O
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*.
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
r.
-t^Q(fat
i Q/" ^
t i/f^x: x fx fei A A^ QA.vjbl A/ 3 c* /) n
O O T n i i ^.-J r~*
JTa
Q.
OA
O-/ C^ft*
.7.r. ^ A s^Uvi
JO! fiAt . A . CA-vv±j t f f t ikfL
C.ci J^ j^^-O
CORE size
PACE
2
C
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
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
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
LEGEND
CHLORITE SCHIST
SILICIFIED SCHIST
SCHIST WITH NARROWPYRRHOTITE VEINS
Consolidated Mining and Smelting Company of Canada Limited
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
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
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
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i
J
!
i
DIAMOND DRILL GEOLOGICAL LOGSAMPLED:
COMPOSITES:
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****
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^
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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67666
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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
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 '
til (tut* l (tin
l - ,-!!j l ,
Ac!i^* i*!?2?J*.Z™iJ