42A10SE0137 2.2064 CURRIE

• : !S,".' r'f~"-:' - : ' . ; . 1'1 *,' V.' .. v..' - ;*

MAGNETIC * ..tk'?.CTfiC)MftGfl(ETIC

on,

FALCHNBHIDUE-. NJCHtL 'KINE^-r) t lMlTtD

Bond and Currie Twpa.,

"••J-'V.

010

. 12,

H., .., aradehaw, jj*,

':/'

42AI0SE0137 2.2064 CURRIE

TABLE, w. .ww...........

. . ,Introduction . . . . . . . . . . ,., .-.. . . , . .. . , . . . . , . . '. ;v^i*V* . .;. .' "I.-

PrapartiBa, Location and MccaSf ^ ' , , . l"' ;Group A . .,.,,,v,4v.,V, .^^.....vv^i'^V. .v^. ' 1Uroup O . . . . .•..;; ..-'i,'.V..*-.".t .Vy. . ..*y..*'*... iVii-V 2Group C . . . , . , , .. . .... , ,,.,;* ,.. . . . , . . .y....i.*y. . 2Group O . . , . . . . . . . . . . . . . . . . . . . . . . . . . . yy . . ,',y , 2

Previoun

Gaology ,

Magnetic Survey Heaul'ts anri Interpretation , . -•(; v Group A ..... . .,.......,....,,......,. i*-..,.. .'i-V- fc'iraup B . . . .|, ......,.....,,... -,.,.. .-. ^-^. ,^.. bGroup'C .'.. , l . ,,i. 4 i^-... t i ,-, .i ,-; . . i i.. |. ( '. | 4 ',L 4i||'i.^ * 5. Group O"-.'. . .'. . . ;. .v..',";. .V s. /... ;,y.7 TVv,r.lH..yv'. S

tluctromagnntic --iurvey ^f?8ultGroup a . /. i.' . . . ,". . : . /. . ; . t . .G.rOUp Q . . . . . . . | .-. ..?,-j f *.*r... .,*r . . . iV'.*'f*( **'j|i'V i;*i * . . . 7

LirOUP U . . . . t'. . . i . '* i . * . , . . . . .r/', t . * ,V . *V. t . . . . . B

Group D . . . . . . . . '. . . . . . . . . . . . .y ?;... 4, . . . .., 4,.. 9

Conclusions ,, , ,.Group A . . . . . , . .. ,. . . .*... , . . .. ,'v",.V.v ..j.* i.. . . 10aroup a . . . . . . . ... . . . , :... .y. , . . . . . . . y. .^V. . . . y. . ' 10Group C. . . . . . . ..^..s^.k^^^Vv.**^.,^.*:*.;*.,;.'. .... .11Group D . . . . . ., ...y. .''.',f.,.. : i-. , .. ..... . .y,*,. .... 11;

Racammendationa . . . . . . . . . . . . . . , . . . . . , . . . . ,* , , . , , , . * , . . . . 12- -" . - '. - - •"" ' ^' *-,' ' ~ i v" pi '.'- *

Certificate .'* '^

APPENDICES Appendix

Maps Property LocationGroup A Magnetic Mop

Llectromagnatic MapGroup d Magnatic Map

Clectrowagnatic Map'' ' ,.f. j f- '

firoup C Magnetic Mtp;vMap

Group D Magnetic Mapi-lectromagnetic Map ,

INTRODUCTION : \' "

Magnetic and electromagnetic surveys have baan conducted

an four claim groups in Currie and Bond Townships for FalConbridgt

Nickel Mines Limited.; This field i*iorlf wajs cpmpie^afl ,di|rintj the1 5 ' t. "' - f't.^./- -t.-..*- *-v* .',: i -' .' * li# ; ' . ''•-•' , .

period January 15 to FRbruary. 15, ...I^Tfc,!^ ;, .^ -;••~" it ..-i . : . "-f ''''H',, K Y;. '-" '-^ . '

ThH magnetic survey defines •wagrietioel'ly the vfrioua rock•l- , " '-- , . . . .. "-' ", . , - -. - "^4*fi: V ,- ' - :. ' ' ' :

types thereby Basiating an IntBrpretation tffr*^hf,, geological struc-

turs. Sulphide mineralii in Bufficiinit cortcantration to .form con

ductors are detected by the electromagnetic survey. Features such'" ; . - ' "'J ' - - ' ' ™* ' " " ' " . - " r ' -a'

as yet or graphitic shear zones may alao ba ponductivak

Various governmant publications ara Used in the inter-

pratation of tht; gaophyaical aurveye. ,

S. LOCATION AND ACCESS . :' v;';.

The individual properties ara with/ir* f lye milne of one

another and, as a group, are situated about 32 milaa east of down-'' : '^V ' . - "''' ". . - ' ' ' ' '" '-'

toun Timmins. The accow,panyinB plan i show a the relative location

of the individual claim gtoupa and their Bccaae,' '- -4 ,' ' : .' -' '"-. ' "' ' ' .

The four individual groups of claims ara daacribad aa' ' ' ', ' ' ^

follows:

Group A - Conaistiny of 6 unpatsnted claiaa in Lots i* and 5,:' ' s; V ---

Concession U, Currie Tounahip, the claims -are numbered LU22S93 to

Lt422596 inclusive and L k 21573 to L42257** InclaSiva. A gravel road

along the boundary of Lota ^ and 5, one and a half miles tputft of•: - ' . - - ' . ' - 1 ' . ,- . ., - ' ' '""VV- ..' '

highway 101, providaa acoesa to Qroup A.

f f ~ 2 -,,*v - -j .- V -

'* S-.'J x,.

Group B - In Lota 7V"B, and 9, CoritfB8a^n''|^an^*^:Curri8

Township, 19 unpatanted claims form Group Bj they lira

Li*22575 to LU22591 inclusiva, MZZSBi'*nd Lii259a. A gravel road

alony the boundary of Lota B and 9, two milsa south of highway

101, provides access to Group B.

C - Twelve claims numbered LU19B36 to U* 1981*7 inclusive,i ,

in Lots 3 end **, Concesaion II, Currie Touinahip, form Sroup C.

Situated 5 miles aouth of highway 101, tha property la two milaa

south of a gravel road along the boundary of Lots 4 and 5.

Group D - In Bond Township1 , this group of 6 unpatented claims

includes PM9S16 to PM9B1B incluilvB, P4l9S20, ^19821 and Pi* 19626.

Situated in Lot 1, Concession I and II, Group O in 5 miles aouth

of highway 101. ' ;

Although rock BxpOBursa in the area have bean examined

by prospectors, there ere -no records of any prevlOua detailed

exploratory work on the claim groups , ;T ,

Map No, t*Dh by H. C. Laird, published by the Ontario

Department of Mines in 1931, provldliB Ihe aaat datailed data of

the geology and topography of Bond i anjtl - Gurri*' TounahipS. Aero-

moynetlc maps 29U and 297 by the f edaral govsrniBanfe praaants ad

ditional information. Tha srea is part Of a regional study by

hutina and Fabbri described In B*St C- paper 71-9, Relationship" : i.'"*' ' '

of btructural Lineaments and MintjrBl Occurrences^ the Abitibi' ' -. - f '"" -. . ' ." - " . --

Arfia of the Canadian Shiald. : ',. ' ;,j ;

Map i*Db indicates that the f au rock 8XpbBur88 in the

arna are mainly altered mafic volcanics striking'gast and dipping-- *--~ -- ' '",.

steeply south intruded by north trending diabase dykes, granite,

felrispur and syenite porphyry.

Thers is an unusual amqunt of diabapfe in the urea aa' ' ' ^ ' ' ' : '

indicated several milne to the south where nope rock exposure is

presant. Qn aeromagnetic map 297, the predominance of diabase ia

reflacted by the north trending laoiwBQneticB in-the worth half of

Currie

ftbout the centre of t"8 fiend Sheraton Townshipi "' -' "-'.'-. '-.- I- ; '

! ' '- '' i" ' -' "' '

the uiriter conducted an exploration programme for Seaway Copper

Mines limited in 1972. Drilling indicated the presence of diseeoi-" '-', c.-;-' ' s , ' ' ' -',

inated sphBlsrite, gelena and chalcopyrite minerBlizetion in altered

carbrjn.5ceuu8 tuff i.e. alate, and feldspar porphyry. The. eltfte.'. .* . ' '.'"' \ ' - . .^'jT

horizon, about 5QCJ fact wide, ie bounded by intermediate to mikfic

altered vnlciinice and ie intruded by confoi?fi,able feldaper poriihyry.

This rock assemblage strikes alightly north of Mftt'-and dtps 75 13

south. The BBStuard uninterrupted extension of this horizon would

come close to, or cross, Groups C -end D. Tht mineralized zona that

ham bRBn drilled by "Braacan et al", about the centre of the Currie-•. ' -v. ;. ' ".' ' : ~' ' ; '

Touinships boundary, appears to correspond to the seme horizon.

-k - . - ' ,- .

Paralleling the north tranding diabase jiykaa, a major

fault extending north from Gowganda crosses the area betuaBn

Brassy and MGDSB Lakes. AB indicated on regional maps mi nqr laft-

hand displacement has qccurrad along this fault. The seat trending

Porcupina-DBBtor fault a feu miles to ths north of this claim groups' if. . p . " '' i * ' - \ '

is the other major fault in the aria. . ;; , .

M.\GNLTIC SUi.'V/r.Y HISULTS

Plans at a scali.of ons inch to four hiihdredj feat show

the magnetic survey resulta on the four groups of clairas. ThB

instruiwent and survey wethpd are described in tha 4pppndlx. To

BliminatB the prBaence of negative magnetic valuBiH an Groupa C and

D, it UJBS necessary to add 1500 gammgs to the mBtiaurements on

Group C and 700 gammas to ttiii measurements on SrdUp 0.' ' ' -' .. ?~ \' ' . ' , ' ; ' '' '" ' - •

Group A: ' - :' '- - ' ,. v . .^- , : ..; -

Magnetic background on the property ia in the ZOtl to '3DC(f

gamma ronya and the iaamagnBticB trand north, yeak noith trBndifig

linear enomalies along the wist boundary artd near tha centre of

Lot b a ttnin peak values of about 500 flamwas. Thaae faaturaa ara4 i - : - ' ' ' . - ' " •""' ;" ~ . ''.' ' * "K

thought to repreeent diabaaa dykas, ^ : , * ,' r

The a raa of magnetic fbackf round la interpreted to raprB*

eant east trending felaic to intarwodiatB volcanica.

Graup 0: 'v.., . . --i -- - - - '- ;*1.v'-" ' !

ThB major trend of the iBatoaonsjlsifciB on thia proparty la

north with the magnetic background in the 100 to 250 gamma rang**i; - ' f r"* , - . ,- ,{"V:" t ''j-"-' *fi . :-.i -"^. ..-t/' ' ~',' -:

The trend of the iBom^grtBtJis it-fi rffiajetitin ijf;in|affB\tic d iabase: . . :,.i - : j A*'" ]:'- 4 . '-V. '. . ,, !'V . ,. V i ,, ,i\ ", : - '-. 4, ''..^ t,: ' ' - '

-J,

on the property. 4 l * a . .

T'5 - -: -•- vy -. . "'i--* .:-'^-jf- Y'-"'. : - '

Five generally north trendingmagnetic diabase dykes,

termed U, w, X, Y and ^, ara identified on tha Magnetic plan.

The presence of tha moat westerly dyke, termed V, ia questionable

becausR of tha relatively poor magnetic o?efinit;iiWv

The diabase probably i*Urudas felsic to intermediate:

volcanic rock which strikes easterly. '

Croup C: - ' '. :,

A magnetic background in the 100 to **QQ gamma range is

apparent on this claim group with the dominant trend bf the

isomagnBtics being easterly.. The broad range of magnetic values

and complex magnetic pattern 'presents sowa difficulty in Identi**

fying rock units. T ,

Diabase dykes, however, termed X, Y and 2, trending

north, are interpreted from the linear magnetic features and

geology shown on map **Qb. , - ,

The easterly trending 700 gamma isomagnetic seems to mark

a contact between rock typss. The area below 700. gammaa may repre-

aent intcrmediats volcanics or granitoid intruaiyfS, epeclfically,

syenite porphyry. That area flbove 700 gawmas ai^||fttaining peHkB -,.

of over ^000 gammas is interpreted tlj be largely undeillSin by '

altered mafic: volcanics, termed hornblende schist on map i*Qb.

Vertical OR hpri*ontal die^l^cremant fflltmg ttie pre-existing

diabase; filled faults' ia suggested by the"complex magnetic pattern.

There is insufficient dpta, ho^e^ff, ,t^ Inttrpr'et magnitude or ;•"'•^

direction of movemgnt}. , --; ;. " i.**. ' - ;'-- V!.'"'' ; ? V'-,,. :--' 3- ; ; ' V . ' "''

Group D:

The magnetic background On the property Ttsngea from ^00

to BOO gammas. The most dominant trend of thdiUilPwagnetics it

northerly; less pronounced but well defined la an easterly trend.

Dirbase dykes account for the magnetic BnomallaB oriented

northuards. These ara designated '*'V V and ^ "ani-.th*accompanying

plan. Dykea x and Y tend ;ta merge In the vicinity ^kitte 12 NprtN;

The easterly trend of the iaomagnetiCB 4f pctountad for\ V ' '"'J''" . * -'J 1 -. ' " r' : - ' ' ' ''" '

by the older Precambrian rock assemblage. A half Wila to the east

altered volcanic rocks ara indicated to strike eaet und dip Btaaply

south according to Map Mo. ^Ob. A contact between rocks of high

magnetic ausceptibility to-the south end louer mmgnetic BUBcapti-

bility to the north approximately coincides viith tine 28 North.

The area north of Line 28-Worth way be underlain by faldapar por

phyry or alternatively altered intermediate volcanicB. Hock expo

sure suggests thnt the area of .relativaly higher magnetic values,

to the south of Line 28 North, is underlain by altered intermediate

to mafic volcanics.. J.,he-pjiBrly, defined rdir*.ctiDp f f the iBomagne-

tics to the south' sUgges-t'aX:.thB -r6iclfo"''d!ipr stilltttV ,!" f*--''''^'.'' ; " : /r-. ' :'

Offset magnetic T|0tur^3 jbetkftien diabflyBe dykes X and Y- - \ - :.- ^ ..;,' *' .'' '' , .-:-i-' t , rJk 9.K-,Ai':," - ' ' '-.' '- . . i ; ....

indicBtea th, t dyke ,Y f ill*,a/eultn/^th- la|ft-handBd diaplacement

in the order of 12UD feet. '-i

.~ 7 ,-

i:LECTRI-MMUNLTIi: iiUHV/EY RESULTS AMD

Plans at a scale bf ona inch-to foiir huflfjratf 1*1

the electromagnetic survey results on the four groupjt Of claims.

The instrument and aurvay matnod ara daacribad in tha flppfrtdl)*A ,

Apparently because of conductive ovarburdan, tfia inatru*

went could not be calibrated lo zero per cani W?tha* 4n-phi|ji*;

control. It UIBB, tharefora, rtecaaaary to eubtract 10 units fro?*

the readings to achieve an average zero par ^B,nl:l8V8l for thf

in-phase fneauurBmsntB. ,

Group A; "- ,^v- 'V^'v';,' ,. ' :- ' "' , ; '- -.,.''-' -

Conductor A - Trending nprthatly abovit tHs tyantra of Lot IJiHHiia

diecontinuous zone lacks good definition.: the uaak conductivity,

if located in rock, is likely, cauaed by tha wet nxldi?ad contacta

of a nonmagnaUe diabeac dyke. , Aitaindtlw^ly^ phji {scj|jn|uctivity way

be caused by a b reak, in the conriuc^iv^ pvf*,l|ur.J^n **hara tha diabaaar" M ' ' : t . - * ' - i,-, i ' *- T- - . a -.'-j ' ' : •-i y|- i'-v"'-1* j ' ' -' .

fonriB a relative topograplfio

Conductor S ~ Trending north fallaui'rig 'ti^^Vaa^i'i'.tHif dlBoontinUQua.- , ' .-;r ' . .. -" -1^;:*".,,^;,;' . "••^•,;-^' i '. -' '" ' - - "' '

zone ia marked by ita diaunlforroity,. fha f^rwliicifclylly la attri- ^

buted to a combinatipn of powa* and tal^phona lina ;intarf8rBnca.. ,, ,. ; . : ." v- .^ ^ .( x... ,., .;:-,y |

LocBtion C - Tha poaitivB ii^-Rhaaa and .oilt^of-'philiB maaBuramanta————————" , ' \ '::''' ' " • ;-"- "' 'V '- ' ' - ''"''.t ' '. . ' f t:.'-'

at the bieat (2nd of L i na 2+35 South are apatially related to pone r

and tBlephono lines and alparallal uira fanes.- " i -i 'ri* . r , . " ' '" r - ,,\ '."-' ' J '

. . i- fl . ---r '. ' . . t,.'. w.. - . , ' i . -- ' ' r;

, " . - : , . -; * '.Group B: '; : ..^T-;,^,'. , ;,, ^^^;//-: ^ -

There uare nu conductive zonaa detectad on this claira

-, - - '- - . . - ,group of particular significance. Large deflections of the gut- '

1 ' ' ."'.-i ' ' , i 1***

of-phaae component along the south andre of ^tiraafyjiaka; way be C,- - -' - ' ' -- - . -. '- ' ' ' : ''- 1''' v -* - 4 tt* - ' : ' '"

attributed to a break in the Conductive overburden tiauBiid by more

resistant diabase dykes fprmirifc eubsurface

Group ...i; i . , ' . ' '"- . v: ., . - .' ; - ' .- -:--:.. : • :^ ; :vAv^.':;.:'--"" : : '/''' ^

A number of ueak| ganeraily ahort and diacontlnMoua ,

conductive zones arn present on this c laim group lifiBcribBd as i

folloua: . , ;" ' ' ' ' -' '^ ;-;\. . ; . -- ' .. - :-- - ' ; - ,

Conductor A - This anomaly in the central nort^weat aector pf tWo *

claim group is marked 'by , the., ^ disjjAiCfi^Wiliy If ' .ln4riWi [to '" ' '

phase profiles. Unly the out-pf-phaBq^prOjfi^pdiaplays uniformity

from line to line. Wo-sviftisnca'of softttoctitfity'ttae apparent Ot* I

renurvoying the conductor ijeilVia,/tfijiWfcPWar vertical loop unit.

The uBHk conductivity en detected by the horizdrttel loop is Attri

buted to old rivur channels Ini the conductive overburden. . 'H

Conductor b' - This short cpntjiictof on i.ina i* Cast uaa alao chack|i4X |f

with the Mci j har vertical loop. , A i*iet{ pafajLlil conductive ion* ^1 ?

about 50 feet south, aa ahowp on the accompanying plan, uaa out** , * L

lined. A shear zone possibly uith diaaaminatad aulphides mey :'

represent the conductivity/.]'"; ; t " ' "^ "' -

Conductor C - Three different Ibcat^ris along tiiafa Q ttnti k Cast C ;

are designtitnri C, These locations approximately'corraapond to the

crntscts of a poatulatecl diabaaa .tfvkf" tiiandlna .ridfth. jiTha condun- ;;••. ' "f ' . ' - ' " , : . . .. ;: ' ' ' - ' ::' ' ' - .' '- 4". -. ' ]-

tivity iQ attributed to tho wet oxidized contacts of thf diabase.

- . - . , , ,

L oca t i on D - There is insufficient date sveilatele to interpret

thB cause of the positive in-phase measurements'rit thia location.

Conductor E - This ona line conductor le - loifeiSao^jiBar the' south..-.- - 1 ; A ' ' ' '' '' ' ' *

end of Line 16 test. Although tht conductor corriiafJondB to tha

axin nf a magnetic high, the short length and proximity to the ,

river suggests that the conductivity if tfluBffd-l|y'.:lh*te^f"-riyar ' v, ,/' , ' .^'•',- '.., .' • :r'\-^\ * ^ .. .; .:-.S. "f ''" J*-. ' ' ' ' - ;^-'

channel cutting the conductive overburden.

Conductor F - Thia diacont;ihU(^i8*ltilinit of a^doctivity extends *

from Line 16 East to 4S fast. 't^fe|i|^t*l,ilea'''cif5^1r|*^hB8B^;4nd out* i*-.':-.v*':''

of-phase measurementa indies ttfffiipf^conductiv^ty^^

that the cunductivity ia caused Jjy shearing ^n iiNf^ ;isltBJ?8d waf ic

volcanics which have been cut by north trending diabase dykes.

Conduo|ora G and H - ThesB are on* iina features ipn iUIfiea 42 East

and 3? Last respectively. Conductor G may repreBgnt a shear zona

along the altered mafle volcanic contact. There ia. insufficient

data to poatulato the tiWuse of aonductor H. - , ' ^ VI ^

Group D: ' ; - ":;' ' "--: . ,"V . -' .,,'''-" '

Only ana conductor, daaignotad A, is shown oh the plan.

This weak north trending feature likely rwpresfihts tha contacta iif

a postulated diabase dyke.

Considerably .yar'jLatitin. of the out-of-phaaa prbfil^'a^'lifrii-'

noted. These anumelous conditions forHtha moat paTt coincide With

postulated diBbsse dykes. At these locations, it ia likely that

the conduct i vti overburden ia much shallouejr beeaus'e of the roerft

resiatant diabase.

The magnatlGj3nfi?lapti'o*Pflr'8ti: urVB.fbrk ,and 'inter-' ' - , i-...* -i " ' .'-' -l ? ^v' ;. ' ^----i ' x**..?. l;.,'.''" : :. .

pretotion on each of ..the qj^jin groupBjte ,{i4Cf^full 6eoei|ll|*of the' -- ; i-.';- :s- ^i^-1 *''-^.^-*;-;^^^--. 1 . ,.;.large numher of diabase dykea -and .deiefi conduct i ve •ovttyfeMrder*^, i; ^,

Although a large number of diabaSB dyWis have been•' ' ,tvv ;- ;'' ' "•'••* '. . .-' ^'^-'.;., ;. - . '; : . defined and outlined by their viaghs'tic -ai^lBeptiijifljtle'e many wore

•. '*^,-- '' . '' f -~ , -- ' " * " ' "' ' ' "' v nonmognatlc dykes are likely -pftitatni-. ; |Jie8B wagnetic antf lion-.'•••V'''.'': -"":'jf,i ;{ ?. -- .•••••- ' " ; . •-'••. ' '.': f .' magnetic dykes interrupt conductive z&Waa in thi plder' *aat

Precambrian rocks thereby lesegning the pOBaibiiity of their''.'•• : ',:' ' ' ' J i - ' vS r f** .' :. ', .. .' ' ' '' •"''.•., *

detection. ' -\ ,,i,X - Li :'\*v " ' : - ^ - - '.'" . . ; . : . .-^^ *

Aa a cunaequenca of the deejsi ^onductiye ovBrbutijan, the r-'- •"•;"', ,". --vi^Vy"' - 1 ' .•^•••'f v' •"^vv horiznntel loop elactroBBgnati^ unit .way no^ ;fcp the *dat "auitabl* '

survey aquipmRnt. ' '?~ s- ' , '. ' " ^' . ,;' •' : ' J ' ' ' '- ' '\': fi'f,' . . ' 'V * '.

Tht; concluaiona derived f Fpm tha aurvay reaultiiori

apecific claim yroupa are aa fallows: ( ,

Orpup A ' : ..' ' ' \ i .-.•,. ' ':--:\ ' ,;: '; ; • '"' :

The property la Interpreted to be unberliin by easti ' •" ' "' ' : . ' ' * " ' ' ' " ' " ' ' '

striking felsic to Intermediate volcanic rock* /intruded tjy north t

trending diabaso dykaa. The q^ientatiort of ^ne'ai'tii^ thersfore,' ' *. ." w '''"t- : ' ' ' V

i a not aui table for exploration of the ^Ide^ vplfianitjs utilizing

common electromagnetic survey msthods. :[t ^t ;

Group B.

The magnBtic expreaaion on thl*; le elmoet

. - , .. . . , . * ' ,

reflcKtsd by north'.trending d jLatia||i..-^|*B which'-at*-' - .

interpreteii to cut B i* s t striking felslq to irtt*rrt*diotB volcanics,i. t " , -' ' - - ' |)4 .V ' ' \ ,, ^ ' ';..; • •^•- - , ,;.,,,The lack of conductive zones on the^ (iropierlty w**j 4b*

attributed to the deep conductive overburden cond i titans, l|f simply

the lack of conductive mineralization. - ,; : ; :

Group C ' , . -. ' '••'^•i - . . : -, .', ;- '; : ' - ., ,v

This property ia interpreted to bewlindsrlaln by ^ast

trendinrj altBreri mafic volcanics represented t?y broad tBagnetic

highs intruded by generally confqrwBblB feldspar porphyry and

ayenita intrusivGo. North trending diatjase dykes intrude tha

volcHnic-granitoid intrusive assemblage.

Limited vertical loqip, survey uork to chttck' conductdra

W and li indicHtc most nf the eonductive zones on the pyo0erty arsr

probably rc;lBted to fsatures of noneconowic luportancB Including

diabase dyke contocte and old river channela in the conductive

overburden. Some conductive zones, namely F and S, merit further

attention.

Group .P -

The metjnetic survey indicates th.at the property ia

underlain by altered mafic volcanicB l ri. conforrottliia contact with

granitoid intrusivns or alter||d interiBBdiate volcanicB whJ,i|H

strike Rest end clip eouth. Thie asBBmblBQa la intruded by north

trending diabase dykes. " i-'•l '..'' '•''•' . ' ' -

A grid uith north oriented picket Unas is moat suitable

for geophysical survey work, pprticulariy elactfiiinsQnetlc wethdd*.

-12 -

Rf.CCMMENDMTIUNS

To provide a more complete evaluation of Qroupe A and O,

it is rncommendBd that qriria ba aatBbliahed with picket linas

orientad north nt UUO foot intervals. In view cf.tha overburden

conditions and type of mineralization being aaarchsd for, a vertical' . i' . .':'

loop ulsctromeignetic survey method is considered preferable for :.'. i- " ' '' . -

investigation of the propertiea. Cost of ^his wpirkV totalling

approximately 12 miles, is eatimated' at 03500. ,

Dn Group Q, it is recommended that a liroiteti amount of

vertical loop electromBgnetic survey work bt uhdajplakan to elk

least determinK thut the completed aurvay has tjBftn iff active : S !i;, .

enough to penetrate tho conductive overburden*' ".'.FijSke'lf linaa

obviously underlain by diabase may be aliminatad. Asauping that

10 milfsa of survey uork would atiaquBtaly avaluata tha claiis ,

group, a cost of S150Q is as'timatad. . ' "o- -" .•'-•:, -.. 'V^^- "v-/ .^'" "-.'- ' ' J -v.

Finally, it IE rBcowmended that conductors F and B on: f '' - . - , i -' ' f-' '-

Group C be checked utilizing vertical loop electromagnetic equip

ment to determine whether or not these anomalies merit a drill ,

investigation. Cost of thin work is eatiwated a:t I60D to 81000*:. :

^eapectfully auhmittad,

SHIELD GEOPHyeips XJMJTED, :' ' . ' - - . -. . . ,.

Timmins, Ontario,

March 12, 1976.

R. J; BrBdsKa*, F. Eng. f

Consulting Geologists

A F f'' S M O.I X

i -.' .. ;f r ' ' ' '

KLTMrJD AMD IMRVCY DATA

LlectromaQnctic Survey .

Any alternating magnetic field ulii.'induC8 en

cal eddy current in the medium thirouoX uhichflho SMSflftetic field

passes. If a source of an alternating magnetic field ia locattd

near a conductive body anomalously strong vddy torrents WilJ. he1 . , - I - . ~ ' : - ' t; ' '

induced in the deposit due to ita high electrical conductivity.

t-lectrical currents induced in the Cft|fHiuiBil^ 1-^cjly;',WHi';''.'pr.ailuo*^il

secondary magnetic field proportional -tlHtha .intii'ty']: Q' curran t''

A receiver coil tuned to the frequancy of

ting device will pick up both the directly transmitted

eddy current signal. . v .-•-. : .•-^-,., Jsj::. V -'.\ . •• :.'}-'...'-. '

The electromagnetic unit uoed in thi^ ayrvey la a

y/HEtf. This horizontal loop ayatem constati* of a recBiver and , .

transmitter connected by a reference cable with a capability of

operating at 6QG and 2**00 ops. " - "

The in-phase and out-of-phasa coraponanta^of the iacondary

field from ti conductor, enargizad by the priw^yy fitid fro^ tha

transmitter, mill vary aa-the Bp,iJ ayitBm paaaea over the conductor.

The equipment i3 calibrated to compare the in^phace end out-of-

phase Field at the receiver witH tbs in-phaaa fia^d at that point

in the absence of a conductor. Tfta measurements nira raad dira,ctlf 4

off the dials a f; a percentagej of vtha^prij^bryvfilill i\ the receiver.

The in-phnse and oiitMJf-phfisB anoRialies avftr a glvsn' ' '*: \ ' * 'V \ :'" i - '"'-'i' . " •'.,.,'" . - , - "•"'•' .

conductor when profiled will have the" same atjapa 8lthdugh';theii*

relative magnitudes uill depend upon ifchis alza and conductivity

of the conductor and ths frequency •i*ojtoyjiisi *

In this survey, e 30(3 foot cable arjej a ^frequaticy of'••#\\ ,. J' ; ' , " * ' , -'."

600 cps. were used. -' V

.' ..' . -' .: 1 .•••-•-.:-- i'' .. .i' :?.: , Magnetometer Bur ve y :.\'-fv ': '' v f l:/ .-.• i-"- - .^..v, .•; -.. b . ,. i"' . ' ''.'-^: -':'^'"''^: ' -:

A ijharpe H.F.-1 fluxga'ta. magna tome tar, model miwiber- ;' - ' ' ' ::', ' ' .- ' * ' , y'~ ;'-'''

. ' ' ' ' - ' ',: " '"', ' ' ' '.' ; ; ' ' - ; ,, ' ;- .'^t 1 ' .321, ujaa used in the magnetic survey. This ''Itiatrupant waaaurBB•;-.v- ;'j . ' ~'' " . v;-rn--- •.•••;Ji " : ' v '"' : \ '-' ;the vertlGBl component of the ieHh'a mBgnetiC f!itW tn Q8BimB8 kl "•••-. "' ' "'"- : -' "- . ' :'-^~ "; - / :'' : '-.- Basa stations for determining ttt| rtognetic diu^a^; :0j*iati0rtestahliBhed nt convenient locatij&ne on base lines or tia linea 'aa

shown on the acccmpanying plans. Magnetic readings mere taken at 50 foot intervals, alnng the cross lihaa.

l-.: , . ' - ;i ; '' - ' . • : :' •••'^'•:"^'ri'

GKOPHYSICAL GKOL( TECHNICAL D;

42AI0SE0137 2.2064 CURRIE 900

TO BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORTi-ACTS SHOWN HERE NEED NOT HE REPEATED IN REPORT

TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.

Type of Survey___Magnetic 8* Electromagnetic Township or Are;. Currie; Touinahip_________Claim holder(s) Falconbridge Nickel Mines Limited

Author o C Report R, J. Bradshauj___^ ——— A fid rcss 26 P ine. Sjki S.. Timmins, OntarioCovering Dates of Survy January 15 - February 15. 1976.

(lincLUttin^ lo office)

Total Miles of Line cut___A * B * C s 35.5 milea_______

Sl'KClAL PROVISIONS CRKDITS RKQUKSTKl)

KNTKR -K) days (includes line cutting) i or first survey.

KNTKR 20 days for each additional survey iisint; same iind.

Cieoplu'sical

l''.leetroinanetie.

DAYSper claim

\2D i

Radiometric

-Other -^^^

(ieolo"ical.

(ieochemieal.

AiRBORNl'. C RKDl IS (Special provision credits do not apply to airborne surveys)

Magnet o mete r ____Klectroma'jnetic . Radiometric(enter clays per claim)

1) An.; : Jterch 12, 1976 sif ;\ ATI IRK: iAuthor of Report or Agent

PROJKCrsSKCllON

Res. Geol. ________

Previous Surveys ___

Onalif if::

(r St. '-•3---.-f.

"' - . ( /''- t

XO

Checked bv_____ .date

GKOI.OCilCAL HRANCII.

Approved by___.______———

GKOLOC;K:AI, BRANCH_____.

Approved by—.

MINING CLAIMS TRAVERSED List numerically

.....SEE..SCHEpL)LE............(prefix) (number)

TOTAL CLAIMS-

Show instrument technical data in each space for type of survey submitted or indicate "not applicable"

GEOPHYSICAL TECHNICAL DATA

GROUND SURVEYSMagnetic - 3760

Number of Stations———!???_______________________Number of Readings EM " 1 70DStation interval

Line spacing_________nDDM^———————.—..^——-——————.^^—^——^^^—..^^—^—-——^—^—-—————.Profile scale or Contour intervals 1" ^ 20X EM profile seals; 1 DD gammas - magnRtin nnntnnr

(specify for each type of survey) Interval

MAGNETIC

Instrument____ Scintrex M.F.-1 fluxgate magnetometer_____- _____________ Accuracy - Scale constant__* or - 10 gammas____________.^______^_____^__^^______Diurnal correction method, check of base station at no greater than one hour intervals Base station location_____along base line at **00' intervala from LO_^^____^____^_____

ELECTROMAGNETIC

Instrument________McPhar VHEM serial no. 33-7M33Co.lconfumralion horizontal

Coil separation_____3UD^————— Accuracv_________-t- or - 1X

Method: Q Fixed transmitter CH Shoot back S] Inline CH Parallel lineFrequency___________6DO cps.______________________________________________

(specify V.L.F. station)Parameters measured____in-phase and out-of-phase components in per cant_________ GRAVITY

Instrument_______________.____^-^——-——^.——.^————^^...^^-——-.^—^—...—.^^^..—.^-^^..—.^—.——Scale constant ——Corrections made.

Base station value and location.

Elevation accuracy___________________ INDUCED J'OLAKl/.A'l ION RESISTIVITY

Instrument________________________Time domain______________________________ Frequency domain. Frequency___________________________________ Range -——.—^^——. P o w e r ________________________________________________Electrode array—— Electrode spacing. Type of electrode .

—

File. 'ts O (-GEOPHYSICAL GEOLOGICAL - GEOCHEMICAL

TECHNICAL DATA STATEMENT

TO HK ATI ACHED AS A N APPENDIX TO TECHNICAL REPORTI ACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT

TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.

.J:lyuUl'l.in i. i-IoctrnninynoticType of Survey__

Township or Air,i__tiond Township

Claim h olfli-r(s)Talconbri(lyp L'ickel Mi inns L imited

Au l kor ol Report_EL. -A^AddressJLCL. 11 np,iitHRPtJ;AJ .. Umnins, iCovering Dates ol Survey January 15 - February 27, 1976

(liiiccutting t o office)

Tola! M iles ol Line cut 6.2

SI'KCIAM'ROVISIOXS CRKD11S RKQUKS'l'Kl)

KNTKR 10 days (iiu-kuli-s line rutting) lor lil si survey.

KXTKR 20 days lor radi additional survey same grid.

DAYS

Geophysical

Electromagnetic—.

\l:i(i;ncl nincl fi- ' 20 : :

Radiometric —————————— '

C) l her _______________

(icocheniical

AIRBORNE CREDITS (Special provision credits do not apply to airborne surveys)

Magnetometer

Author of Report or Agent

PROJECTS SKCTION

Res. Geol.

Previous Survey;

.j/ . 'X -————!———______^- Qu;ilir!r:ii!nns .P'^ - '-. ' V

,,J__, ,r .^^:,^jy i/', l

5O

Checked by—-—. .date.

*^

lGKOlX)C;iCAL BRANCH.

Approved by-

Gl'X)l,0(;iCAI,15RANCII.

-date.

- ;

Approved l)y- -date.

MINING CLAIMS TRAVERSED List numerically

.190.16-

TOTAL CLAIMS.

Show instrument technical data in each space for type of survey submitted or indicate "not applicable"

GEOPHYSICAL TECHNICAL DATA

GRUUXILSURVKYS.^ Magnntic - 660

Number of Stations________^^____________________Number of Readings_ Station interval_________ ion'

Line spacing ________ _____ 4 L "- 1 ___________ ——————————————————————————————————————————— Profile scale or Contour intervals 1 " a 20* ^ profile scale; 1UO gammas - magnetic nnntnur in

(specify for each type of survey) tOPX/El

MAG.N'LTIC

Instrument __ _________ Lidntrex K.F.-1 fluxgate magnetometer -.——.—^—-^..,^.^.^^— Accuracy - Scale constant ____ * or - 1 0 qammaa _______________________________________ Diurnal correction method nhock of tiasn stations at no nreater than one hour intervals Base station location ______ alnn-j biine linn at **CJC1 ' intervals from LO -—————————^

KLF.c:rROMA(i.\'LHc:Instrument ____________ Mc^har UHL'M serial nn 33-7403 -^-^———-—^———-———————-Coil configuration _________ harJ7nntal ____________________________________________ Coil separation ____________ 300 _____________________________________________________Accuracy _______________ -f or -

Method: LTJ Fixed transmitter CH Shoot back [S Inline CI! Parallel line Frequency_______________()t.iiJ OPS.———-^----^—---^^^^——-^^-———.^^^—-^———.^^——————

{specify V.L.F. station)Parameters measured jn-phasB and nut-of-phaae campnnenta i n per cent_________ GRAVITY

Instrumenl^^

Scale constant.

Corrections made.

Base station value and location —-

Elevation accuracy____——^^-^-———^——L\DUC:LD I'OLARI/.AUON RKSISMVITYInstrument_____________,_________

Time domain________________________________ Frequency domain. Frequency___________________________________ Range.,-—^-^—-—. Povver_____________________-__________________________Electrode array—^.

Electrode spacing—

Type of electrode —

TAYLOR TWPHwy. 101

BOND TWP

D

CURRIE TWP

B

V.JS-

x

PROPERTY LOCATION PLAN

FALCONBRIDGE NICKEL MINES LTD.

SCALE-. l inch ^ l mile

BOND TOWNSHIPONTARIO

MINISTRj RSURVEYS AND MAPPING B

MAR 181976

SURVEYS AND MAPPING IRANCH.

SOURCESANCH

PORCUPINE MINING DIVISION

DISTRICT OF COCHRANE M.33ISCALE 40 CHAINS TO ONE INCH

STOCK TWR

o:

uJ

Do

8 7 6 '5 SHERATON TWR

p

42A13SE0137 2.2064 CURRIE 200f 9.

PATENTED LANDS . . . . . . . ©CROWN LAND SALES . ....©LOCATED LANDS ....,... .L o^LICF.N5E OF OCCUPATION.. L.O.L

Taylor Twp.

427062fe) 427063

SRO1 L. l

424710 " 42470642689WR* 4Z6900

"- S. P WITHDRAWN FROM l STAKING

424709 ! 424707

424708426995 l 426994

400047 l 400046

437615 l 437614 400043 14000

421929 (P)42I928

422597 422596

L L

4I0896' 4 |0897 410900 MI09OI vK- - - -."! — — ™- — 'J4* t'j'jjJS-

L

41 0696 |4I08 7.9

—— r---/-

122101 '^422102 SRO 422124 i 42I9S4 421947 i 421938 421962 421963

388938 1368539

L. i L.

381585 .581588421950 l 421951

/til. REISER47*953 1.421952

368*33 I3B8437 400055 40005*/42I94SL421940 388943 388542

422121 1421997-l —~ —

t L

421968 j 421967

rL421977 l 421976

429127 1-429129

L 429I28 ! L

429131 I4Z9I33 -— --L : L.TL

ll

426688 1426667420190 420193 420194 i 420197 420714 1420709•H

L.

420713 ' 420710 — ~ —-f- — — — — L.

42690t i 426775

L iL

426884 426888~" ~~ 420686 420689•*co (ID -r t ut' •^cvcui

420204 420203 420639'420684 l i C

420712 I 4207114^^687^420690

L. l L.

429200 '429199420200 4201199 426B85J 426^89^ LT — L~~"

426975 (42697^4

~ "li I f

426980 i 4269/6

4269T7 426976 426896 426895 426886,426890 420688420691**vwt i •feoyi o

426680)426679 426978 426979 426904 l 426905 426887,426891 427052 427053 427054 427055

7 6

Egan Twp

2.2054 CURRIE 310

Q.

c oEo

OD

THE TOWNSHIPOF

CURRIEDISTRICT OF COCHRANE

LARDER LAKE MINING DIVISION

SCALE- 1- INCH" 40 CHAINS

LEGENDPATENTED LAND

CROWN LAND SALE LEASESLOCATED LANDLICENSE OF OCCUPATIONMINING RIGHTS ONLYSURFACE RIGHTS ONLYROADSIMPROVED ROADSKING'S HIGHWAYSRAILWAYSPOWER LIMESMARSH OR MUSKEGMINES

l t t l H l

NOTES

MARKED THUS Files; 11593

21312WITHDRAWN FROM STAKING UNDER SEC. 3 9(0) OF MINING ACT

IA

400' Surface rights reservation around all lakes and

rivers.

FT?-/ 7 f/ f '

C.?) 106 fe^

DATE OF ISSUE

MAR 181976

SURVEYS AND MAPPING

PLAN NO.- M.34!ONTARIO

MINISTRY OF N ATURAL RESOURCES^URVcTi'C AINU MAPPING BRANCH

•o o o

-J rr, -J

24 NV* "* V\ y V\ IE "*T T T 7 7 T i

* ^

O•— o O o

mj f^J^-^-J^-^'C1 ^ 'C1 C — a

o -"~

20 N -~-I-J T 7 T E^L-^^1*"1?O^o ^r^\*"''r 7' * r-V," v' -

J -l ^*vJ-Ji|^C*A^ 1^'iC^rJ iC*Vtv* w J rv\Avi SAP* - ^ N

16 N

rl l

12 N

8 N

4 N

rj M J w t: j ^ o *" ~~^ r z *fi\9* ** ^ - t w w s jj^i VC ^p0 0 ^ i/^"^""0""^ — :'^~V t - i * f * 0 *~ * 3

' ' A V ,-4 . '

n^ m m r* J -*———. T --. T r——sr""-

1^ 5 *^jC^ r*X^* .J vi V. *n O K. J "V, rft f*-* ^U| *V,f l - .STT.T^AT.. vT.7.7v T^s— sj/* ...^ jr^

I *' IV

"'1 /S l -' t 1l/ '*......-.-...-'-'-*' 'l

t''^

......--/l\

l

-*- vi^-*Nir: 1*...!-^vft 9- wv- v- ™—J" ' ' ~ T - ~T. T* "~

;i\ s\ i

road2+35 S

power l ine* ?s

l l "-i* '' l\

la i^^ T T r r

\ B

fcAA^-^^ifi O^-^^^*" "^^'Sy'w)^ 6J *J Vi f^ ^T^^" " "^ T *****'i ,-^**^^ 0 Q -4.1— Q *^i^***'A^X^'^O Q t^ -*^ O ^ O *Jl

vx LOT 5 /\ f\ CONC./

,'— — ' \ . /' i /' l, C,ONC7/l f f ""~— S V v "" "^.' \ i' ' 'X* \ t

*^ *H? *T * "*|w " ~~-*- 0o0ft O~-0[)9 ft~™^^^"5 -OO^OOO*

^•y\^\L LOT 41 IV 1 *' *s "", -— " — "^

O

LEGEND

Measurement station along picket line

In-phase component reading (0Xo)

Out - of - phase component reading (Vo)

In-phase component profile - l" - 200Xo

Out-of-phase component profile - l" =

Conductive zone

Claim post

v v

O)

oCL

GROUP A ELECTROMAGNETIC SURVEY

on the property of

FALCONBRIDGE NICKEL MINES LTD.CURRIE TOWNSHIR ONTARIO

BY

SHIELD G EOPHYSICS LIMITED

INSTRUMENT: McPhor VHEM

FREQUENCY : 600 cps

COIL SEPARATION: 300 feet

SCALE400 800 1200

FEETFEBRUARY 1976

42A10SEB137 2 .2064 CURRIE

Base Line

rood

"^" Je

"3 ? V ^ i' a.

\

\ \• la .0

't- \-7 - o-

-7 0

r f ?ris'^ ' M

} I!,

,' | " ! or-N

—j j 49 * u-^ : \1 r , i;-'5

*-1

yy

f i 'l l? ,i ^X P

^

n-12 y f

^ "-'li j (

,, o*.,3 *.

i i "i -'vt 1 t

f' \ - f" J-1 * 0-/S ;

' ! v ! /" 0 + -/U

-,is ' O J--II - n4 -IJ -

1 1 '

\

o

o

\

"-(1 0

j 3 ' 0-.2. ,

-'3 j

t a

^"II 1 O" 1

•-(l i t.v

-ij '. u

-IS V o

1 C- i -Ij1

l *H}l

,' s-if-IP '

. 0-14--M ^

O "-I if

-is-If

t o *( f

-Jfc

"t-) 1/

-f3

24W 20W

LOT

-'3

-'-T"

). ±I2W

0 -f*

..-T

O

i

t"'-ff

o -IS

8W

a -to

ti *

4W

yOT-I 1/

o- .15

oy 3-I-'IL

w*-ye

ort

-/t

o'-15

-IS

is

-2

-iO H5

iS

-is

-

4-14

^t^is

\zo*-l S

o--/S

o--i f

f--IS

o--|f

0*1.5

,L

1.1- r

l

/s

• Hs

," 0-15

l (\ :fj o,..,j,

-a

^

I

OT-IV

o -/y

-i5

-'f

-^

"'*

-17

-it

-/f

j o -is

- Jr^\ -;}".^.i-^.L-a- 4iE

fS

-/f

l toHT

0

J o.-ij

-IfT

i-*

power line

8E

; J -H

-If

-IS

-IS

-/s-(5

^5

o -i

- -is

0-/S

; o'-rt

2 "3

ol-lj

-/t

-,l J.,

•, 4-s

^•-13

?

I2E

I.. -

LOT 8

- ' l'

rt

o -'li,

-li

GRASSY

'"''-S

-7

T'1*

-?

..1 o/-,,

*-iy-

0+-S

-'J

Ot-l

; - 'T -a i

,( -itrii

-H -/L

,' 0--/6

t i

-s

7\ /-.3

^ of/3

to r'\-|*

70---/J

Oi-lf

sp^ . o-t-jy y w.

'-.1 1 o

\'•-^ i -ii

-/f l o

16 E1 Sf Jo

1•-it i oL l 0.r |^j i O

;20E-1] j o

y i

-II j'

i "* /' y•-.r f

IHI lL \\(J i p

'l !-/i -^ 1

V J

\- -If o

1C "'1 "If l!

-rt o

, -14 ' ~\

1-II ' O

1-lo ^ o

\t

-|^ O

-li ^1f''* ,! r\

-h i ^)1

-fZ' \ L?

t \

•-ii i 0ii1

" f ^ o

l i•J3 l i-

-/5 ; oi-It f Ci

i-,i ; 0 ,

-'0 ' ~ 1

\24E.11 - a

V

-li - 01 j1 l-14 i i.

V I\ l

*1} * t

\4 1•t" r

M 5 0X

/^ V o

j

-li ,'

-If ( J

-W o

\ •'S ) o

,, y. .^ o * -i ji

-j c j oJ^i? Oi v

'i1 3j"'3

-IS f o i-if /* ol-/^/l s ' ',

L-'I.-t--.^ .x ?1.'9 -*- -^ .-^...oifz-..

2^E \32E-If -( or-Po \ O"-q

. \.1 \

-ft f o --Ji J 0*-fl

' ' I

-1,3 (- o --a s ;. i*

•'

-li J o J - to ! 1 4 -i.

X \•-13 i o " ~7 -s o

x v

-IS , o '-ti ") c-

^\\

Y } .y-i? - 1 -Vi j, ; il

L ''-If "/'t ; 1\

-q

-7

•*

..,j; ' 1-/' i-i? i f-i \ y

' ' 1 -' /1-rt t 4 -.f l- 1-1 i, i•-li

i-

\ 0 .-,^1 V1 l- -i" li-

"("

iJ'-li

.Y,

-a

-it

7L

-"i

-T

-a

r(3. - li-

! \,-i

, -7 -ICJ r/

0--IZ

o ;-)i.

0 •-li'

o- -li

LMftC

O - 1 !, ! -1-1-) . rt -C - . -- — ~—

-1

-^ ;U l ./.

•S \ o\

1^ l ^

I

o -rt ," -i|^ 7 o•* . . f\ ,l. (2 f -1. , ^

1 ' i ~*f i i \\ Ot -'i ^' o l -13 i u

X Oi- - (r \ 0 J- 1 j \ 0

\ \

0 1 |l

-s, j^ i•-S ;

t

-5 1 oi o

^

-if-

-y-if-' cJ~^~

-9 -v -M -/p \ - :-fV

-IT, ^ of -t ti

0 + -IJ N -lin- ^ Ut- 1 ,' ^^-1*.l/ 7

o ^s j--S

- ltu\

-;y \-1.-IU i-

1 1 L" fc^ ^r/ :^7 !\; ot-ji* . t'u- o* ' T T "*

; . -1--K.f o*-J \ - i 1*1 1 0

; V\

o 4^5 \ -V-

11

H. i 0

l ^? /"f f'

\l *^ i o f, i 2-^^^^^ '

i O^TV**. ^ p r ^l a -^ ^"

i 1 /'; i:\ - i-' -i*J-s - x - ii

^~Tj**"*^ \ - t

U \ o\ \

1

TitJls ^-^..^1 f

10--I? J- ( i 13 \ Q

; \' 0 4-'i y -|-Uj 5 ,' oii o

J ~'J; Mf

— i . 1 \

40 E

1

r/S i -

Lrt i o

,, 1 *-If 1 0

* ' iif 10'

i i

;' i i D i f '

44 E0 |-rt j -r

(/ i* i

t\ O 1t i

t; - 1 -ii *

-/f ; -l,'

-13 1 -f

,

-'3 ( 0ic i . .",

4&E•O o

IS

1 Lf \ 1 t

-/o -x - 1\\

-'3 /' -

r/^

j-Ij -v o E-iy

A

-If -^ -1 tV)V

-is ; o l-ii1 l1 \

M ^U-^U-L^THT/

1 * Q J^-if ;*iiij ; o*-W '-

f-15 J ~-*

l /'

li : o -'5

/ :- (jt '.^ o-,j

T S ] 0,

,s rr , 1

T o

-'3 ;' 0i-O \ oi ari 1/ 1-1

1

' 52E

"f**

-'i

-j y

^

-i*t ; -i-Hffi-if -,

-IS c* -'"f i

ii-li ' 01

t 1

.-/3 -1 i '4 Joff'i3 \ ~ i -

r *

/' 't

' O '^\

V

1

J o\.

oti "l! 0

1

i ?1 1

'l ftr*

i oi

i oi

i O J11i! o.jiii\i( i

*' a *

ii i

\ l

i

1•(4 ; o

\\

-15 - Q11

-l 1^ ' - 1 T *'4 . ot

Ji

1

-'3 \ -\f-IJ i oi

-14 l. ,i-f.

l,J11

•'3 ; -i * '} \ o j i j 'i

-(3 ,! 0'/

-li ; -i ''

-B ^ 0'i

-'3 \ - i-y

j

-rt /' -i

-•s *. oL iri S ; D

;-rt ; 0

-rt o

•i? i ;^ '

t \-H | Q1

-12- *- -i

|-'2- ; -,

*\ -,\

•IS ; o 1ii

~!S ; o '

-'3 ^ o-

-'S ; -i-i

-rt i -i-

"'T O 1

t-fif o

N ' o1

'l\ ' 0r-13 o

-fi (Oi

- 1 1 l o\•rt J o

'

13 ; o..J. l ,, ".r li v- ,'

-if o,

-li j oi

-13 | ol

-'3 \ 0'i\

-fi - oii-if ,- o

^

•-(J yii

-li ; o\

-13 u

-i? o

•'5 i' o ^ r

''Z. 0

-'X. ' o\\ "l

-'3 l-.

-12. ; 0

-" \ -'

\-li- i O 1

i^

,,

" ' 3 i O

-15 j -1 1

-'3 ; *\

-;4 \ i'

1

-uJ-13

-if

-li

-'i

-fc

-rt

-U

-iii

-13

-i^t

-B

-'3

-rt

-rt

-13

i ,ri-'3

*'5

-io

L-* 1*

- ^

LOT 7

*" ^* ^ 1

i j1 f

1 l\ \

1 B

,' \\ 1

* 1\ l' *

1t

'^ ~*^

r*'

•^^

\ i

1

^

ii i

ii t

r X1

\\

\

;coNc. iv\ii

.(

r\\iii iiiJ

i\\iii

iiii i\

\i

ii

i ii

\1i f1

i it

iii

ti-

s/\\ \

\ \ \ii!

LEGEND

Measurement station along picket line

In-phase component reading {"/o)

•-B Out - of - phase component reading ("/o)

K In-phase component profile - l" - 20*Vo

Out -of - phase component profile - l" a 20 0Xo

~ — ~ Conductive zone

O Claim post

INSTRUMENT: McPhar VHEH

FREQUENCY : 6OO cps

COIL SEPARATION: 300 fee

42MCSE0137 2.2064 CURRIEE30

GROUP B

ELECTROMAGNETIC SURVEYON THE PROPERTY OF

FALCONBRIDGE NICKEL MINES LTD.CURRIE TOWNSHIP ONTARIO

BYSHIELD GEOPHYSICS LIMITED

1200

FEET

FEBRUARY 1976

•T

M -17

O

V' yaf KX /*~~~^1 ': 0.x^ \.'/p )•^ ;

- T5^^*^ -' a."^ f' '*-t- i C?* s vC \l Ito

'

s ,'' \, i

; i ^i

J ;j H/i M^i A

' v-v1 C

;/*j- ^20 e wJ Ni\

? \* ^Ifr ^'of '

l ;" -ii - i

6 \ -J

-,i-15 ,.-'-J ,/-'-7 -'

" ? "

•44 ' oi

-tf y "

-, /" o"7 ;•* i-t ;** *^ ^B

'l* ""*^,-,, V,..

-l? ?1

-li 't"5 !• 19 O-IS-J "^ OJ

5 X ,•/l ' l-1} \ ' !"j "' 'i ! \•IS \ o*,

~" ***\l -*? 24 E /*•t*- i \-t . i v ix' -.t f -i-li l "A

" " s.

-lo ^ "ft

y oi 'V ,.*

-'Ji"l-17"rL 0It

-O

'7

't

-17

-'7

't?

-n }/

''i {\-w i

i

-i? 4^ -jsM-Zi o yis

-1 J.,4f ( I ] n

~" j i

- ( 7 \ ~, ! n

i 0-17

i r-if

""

OH?

l SG

', o -o

O

o -i?

O t -t?

o V' t\-l t-17

V'7"

t''6

Vi-i?"

32 Er1 T"

fi-(f -l?to

/•H?

-;5

36 E 4OE 44 Ey -H

-/t-l*-li

48 E

4

\,1 77; o i -i

-(i

-'3

-H-.lt

A"! O' -2*

--

-*t

w f'J

r r

-2

-15

LEGEND

Measurement station along picket line

In-pnase component reading (0Xo)

Out - of - phase component reading CVb)

In-phose component profile - l " r 200Xo

Out-of-phase component profile - l" -

Conductive z one

Claim post

INSTRUMENT: McPhar VHEM FREQUENCY : 600 cps COIL SEPARATION: 300 feet

42A10SEC137 2 .2064 CURRIE

GROUP C ELECTROMAGNETIC SURVEY

on the property of

FALCONBRIDGE NICKEL MINES LTD.CURRIE TOWNSHIP ONTARIO

BY

SHIELD GEOPHYSICS LIMITED

SCALE 400 600 1200

FEETFEBRUARY 1976

240

BOND TWP CURRIE TWP

LEGEND

Measurement station along picket line

In-phase component reading ("/o)

Out-of-phase component reading (0Xo)

In-phase component profile - l" r 200Xo

Out-of-phase component profile - l" * 200Xo

Conductive zone

Claim post

INSTRUMENT: McPhar VHEM

FREQUENCY : 600 cps

COIL SEPARATION: 300 feet42AI0SE0I3?

GROUP D ELECTROMAGNETIC SURVEY

on the property of

FALCONBRIDGE NICKEL MINES LTD

BOND TOWNSHIP, O NTARIO

BY

SHIELD GEOPHYSICS UVIT f- ;-

SCALEo h--L. .

FEBRUARYCURRIE

350

?vnO D i B " " .2. ** G f.s fffr * S SU5 A ? 5yff ^

o 0 *"llliA a oi/i^cy, OvioOutO'^in^iinv.o/n^HID M 'J '^Ss'-fi^'isirn.I "J.K'J'f*-'^ 1", *3- *^/" .J./* *-?*iNN NjJpiMNNrtJi *l N r'rt^'l ^ N *!"/* "T^f^

power H neLOT 4

LEGEND

Measurement station along picket line

Relative value of the vertical component of the earth's magnetic field In gammas

O)

oQ.

if o*Magnetic contour

iMagnetic depression

GROUP A MAGNETOMETER SURVEY

on the property of

FALCONBRIDGE NICKEL MINES LTD.

CURRIE TOWNSHIR ONTARIO

BY

SHIELD GEOPHYSICS LIMITED

INSTRUMENT; Sharpe M.F. - l fluxgate

Contour Interval: 100 gamma intervals

SCALEO 400 800 1200"J

FEETFEBRUARY 1976

42A10SE0137 2.2064 CURRIE 260

BaseLine

LOT LOT 8

LEGEND

Measurement station along picket line

Relative value of the vertical component of the earth's magnetic field In gammas

Magnetic contour

Magnetic depression

INSTRUMENT: Sharpe M.F. - l fluxgate magnetometer

gamma intervals

GROUP B

MAGNETOMETER SURVEYON THE PROPERTY OF

FALCONBRIDGE NICKEL MINES LTD.CURRIE TOWNSHIP ONTARIO

BY

SHIELD GEOPHYSICS LIMITEDBase station location SCALE

O Claim post1200

(976

42AI0SE0137 2.2864 CURRIE

z o(/) (fiLU OZoo

•Mo

LEGEND

Measurement station along picket line

Relative value of the vertical component of

the earth's magnetic field in gammas

Magnetic contour

Magnetic depression

INSTRUMENT.- Sharpe MF.-l fluxgate magnetometer

Contour Interval: IOO gammas up to 1000 gammas

500 gammas up to 3000 gammas

IOOO gammas over 3000 gammas

GROUP C MAGNETOMETER SURVEY

on the property of

FALCONBRIDGE NICKEL MINES LTD.

CURRIE TOWNSHIR ONTARIO

BY

SHIELD GEOPHYSICS LIMITED

SCALEO 400 8OO

FEETf K

42A10SE0137 2 .2064 CURRIE

40 N

36 N

32N

CURRIE TWF?

LEGEND

Measurement station along picket line

Relative value of the vertical component of

the earth's magnetic f ield i n gammas

f ~2 Magnetic contour

Magnetic depression

INSTRUMENT: Sharpe M.R-l fluxgate magnetometer

Contour Interval: 100 gammas up to 1000 gammas

500 gammas up fo 3000 gammas

Base station location

GROUP D

MAGNETOMETER SURVEYon the property of

FALCONBRIDGE NICKEL M INES LTD

BOND TOWNSHIP, ONTARIO

-\*-**\^—^^

BY

SHIELD GEOPHYSICS LIMITED

SCALE4OO 800 I20O

FEET1976