42Ae7SW8068 63.2635 LANGMUIR 010

INTRODUCTION . ' ' ' . -~ - : -.:,-y ; ''' 'O' ." ; ; : . -' . "' . .' '';,.-.; : ''' :.' ' " ' r :' : V""vv : -J-.--J r--. . -. '."' ' "' - ' '

During the period Oanueiry 11 tp 3^1^^ IS, 197D, a vertical

loop electromagnetic survey UJHB carried out 0n part of ths Langmuir

Township property df CI au Lake Molybdenum Mines Limited, ^05 - 67

Yonge Street, Toronto, Ontorlo by Shisld QeophyBica

A MqPhnr 8S15, IQDp/itbQQ.t^iiciit^lKonati.

for tho survey. . . : '^\. - 'S' ^ '' :' " : ^ ,.,-'/

Tha prtspsrty cDnsiatB of 12 contiguoufi unpotented raining

claims numbbrod aa ftillous: P97801, 97802^97603, 970[W, 97805, ,

97(i06, 9a66B, 98669, 9B67D, 98671, 9867*j anc l.1 .9606'..

Only nin0 of the claimo u/ere Ddvorad by the elBctromagnatio

survey aa followB! P978D^, 97805, 97806; 96666, 98669," 98670, 96671,

.90674, and 98675. " . \ - .- ^I'^f^ ' . ' ,-' '''.' . '' ' :

AND ACCCSS . .^'' ; '-: '"\ :' ! ' : : .- . '" ' v. ; ; ''. '. 'V

Thn claim group is located in the northutjot part of Langmuir

Township on the east ahorfii of Cardan Bay t ACCCBS to the property

for tha purpose of ths survey uaa via B ulntar road frow South

Porcupine to Langmuir Townahip, a distunca bf jappr0xitriat8ly 15 mi le a.

Portions of tho claim group '' wQr.^''ji'xiflyii.;piUilif.;hii'id...''by' Tiriax

Development Explorntlun Limited, fS'bvE* fxploratianH Limitad and

Con-Key Mines Limited, Magnetic arid C^tiitrnwegnBilb aurveya ware

completud by each company. Con-Hay Mines Limited perforfred an

induced polwrizatlnn survey and drilled one hole on the northern

portions of the group. Tha drill holB int(?raat:tfd mftflo. - . - '/' ' ' ' :' ' * :. :. ' Vwl/j.

rockB ond peridotitB with minor diaaaminatad

" : ' ' * '2 - ;: ''\. ' '. -'.

Langmuir Township yas mapped geologically by the Ontario

Department of Minea in 196T. A number of took "outcrop* occur on

the property with the main concentration of outcrops near tho north

property boundury. The rocks are mapped as mafic volcanic tuff* and

amphibolitas. Overburden thickness fin the proparty should bil in

the O to 75 feet ranyi?.

A magnetometer survey was completed on the proparty In

Novomber 19&) by Claw Lake Kolybdanum Fdnaa Limited* Th* conclusions

from Q report on this survey (Steers 1969) ware HB follows:

"Tha ujBBtern portion cf the group (not covered by the

BlDctromagnetic aurvay) ia underlain by apparently homogeneous rocks

of low magnetic susceptibility,

The eastern and central portions of the property are

underlain by mafic volcanic rooke which may, in part, hnvs been in

truded by sill * liki! bodies of ultramafic rocks.

The most prominent features are the contact areas between

the homogeneous rockn of low magnetic susceptibility."

sector of the property covered by the electromagnetic

survey is underlain by mafic metavolcanic rocks that have a north

to north-northeaaterly strike direction end have 60 e to 70" easterly

dips. The tr.nfic mettavoicanic rocks may have been intruded by Bills

of ultramzific composition,

At least one fault having en east-northeast strike direction

can be inferred an the basis of the magnetic dots. Other psrsllel

fuulta may also be present.

- 3 " : :. ' ' , ' , " ' : '' ''''' " .."

Up to 70 font of overburden occura on the property.

INSTRUMENT USED t Ml) aiKl/LY METHOD

A McPhar 8S15 vertical loop electromagnetic unit was employed

during the aurvoy (Ben Appendix 1 for 'instrument' data)*

The survey woe carried out LIB ing the "fan method" for

coverage of tha ground.

A total of '466 atBtii,nB were eatabliahad during the aurvay

on a total of 6.6 milae of picket linaa, '

SUHULY RESULTS ' •••. ' " , , ' ": : "; i ," '.;'-'- y '' ' :. ' '., ' ,-

The reaulta of thp, survey are preoanted on the wap accom-

panying thin report (in pocket). Fcur poaaible conductive zonea

wertt outlined during the survey (Conductors A to O on map).

None of the cnntiur;tore orf definito bedrock conductors,

houBvar, all merit detailed electromagnetic cheok aurveya.

Conductor A displays low anglea on the eaet aidn of tha

conductor axie with higher anglea to the waat. Tha conductor

displays a tjonBral corralntion with o broad 2QDD gamma magnetic

Conductor 8 is a poorly indicBted, poaaihiB cpnducUva

thot corrBlates cloaaly with a diatinct, narrow 13DC3 gawfisa

unomoly. The apparent conductivity way be due to a diabase*

volcanic rock contact. '

Conductor C la riominantly e high frequency response uilth:a

luoak low froquancy.raapQnaa on line. 28. ?

Conductor D ia weakly indicated on linea 4N,6N, BN, and

1UN. The poaaible^conductive zona ̂ 01^ ;fljt ih?;f*nd8 pf linea

read from transmitter locutions 1, 2, and 3, The apparent con

ductivity could be duti to mifloriantHtion.

CIWCLUSIDMS ' . . - :' '" . V ' v '- ' ' . ' ' ,. ' V '

Four possible bedrock conductive zones have bean outlined

by tho survey. Conductors A and C are the moat probable bedrock

conductors. Conductor B is of interest because of the clone correction

of tho conductors axis with a distinct magnetic anomaly. Conductor

D la tentatively indicated aa a bedrock conductor pending detailed

check work.

HECOHHENDATIDNS . ;

It ia recommended that the four coHductiVB zones outlined. ' ,i. ; .v. ' * -i , " :' - . i '- , ' - ' , ' . /, ; . :

during the survey be detailed in order to more properly validate"' .Vf." -. . ...; . - ; ' ' ' ,'V '.. S W- . .;'': - ' ' -

them prior to rscommending D drill program* ? v

Respectfully Bubmittadj

SHIELD QEOPHYSICa 1JMITCO,

Timmins , Ontario,

January 19, 1970.

RLFtRENCE

STLLRS, J.E. 1969

Consulting Geologict,

Report bn a Magnetic Survey on the jsrpperty of Clew Lake Molybdenum Limited, Langmuir Township, Ontario} private report.

I, Pater T. George, residing at 391 John Street, fiaiaina, Ontario,

a consulting geologic with 'off lo* tt 26 Plna Strept SoUth,

Timmine, Ontario, do haraby cartlfy thetr ;

I attended Uueon'a Univoraity, Kingston, qntarlp^isnd

with en Honours 8. Se. degreo:in QaologloaX Sciancsa In 196** and I

hove completed two yaws of post graduate atiiaitfl at Quwn' a

University. HinyBtoni Ontario. " :

I aw B Hamber of the Baologlcal of

Timmtna, Ontario,

JanuBry 19, 1970.

Peter T,, v ' " ' . " . ' '. i,: *. "-' 'f- , i. . " - - - '

Conauiiing Gaolagiot,

A, P P E N O

Scir vp y Mjf ̂ hod anc^ Ina trument Da ta

UURV/EY

Any alternating magnetic field will induce an electrical

eddy current in the medium through whioh the magnetic field

passes. If a source of en alternating magnetic field la located

near e conductive body anomalously strong eddy currents will be

induced in the deposit due to its high electrical conductivity.' , " ' r J ': ' "

electrical currents induced in the conductive body will produce a

secondary magnetic field proportional td the intensity of current

flOW. ; ' ; ' .-..- - ' ' "' : •••; ,. ' [ - ^ ' ,- ;

A receiver coil tuned to the frequBrtoy of the transmit

ting device will pick up both the directly transmitted eignai and

the eddy current signal.

The electromagnetic unit used in this survey is B McPhar

unit and consists of B vertically mounted* motor-generator

powered tranomittiny coil operating at frequencies of 5QQD and

1000 cpn. and B receiving coll, tuned to the tranamitting fra-. ' " ' ' f . - ' - . :

quenciea, an inclinometBr, a,n amplifier artQ \ -n helBidtBt,. "' . ^ A " *.' --:i '' '"t 'i' ;- . ;- "' ! - ' ' "" ' ' J ' "

Throughout the aurvny, the tranamitter and receiver were

aeparated by distances of- ADD* 600 ?nd ; 12dO,f^et. The plane of' - "' ' ' ^ '' ' '" •'•"l '''' '"' Ji '.'/* .' ' ' '. ' " / , . ' • -.'

the transmitter coil urn B oriented aa that the trarmmitter waa- . ' ;', ' "V.,. ;'. •'•' ' , ' '. . ''. - '

vortical and pointed toumrdd the fBCeiya?r. OriBntation was ob

tained using a plate on which predetermined receiver positions'' ::.:. ; .: " - ^ ' ^.. : T:.;,OO. ,-'-r'- v '\ ": - : ' ; ' . '-' : ''.-::were plotted. Stations ware read ut one Hundred 'foot intervale.

At all timaa, the receiver "faced" the transmitter. The results' ' , , ' .. F '" ! . '' ' " ' -, ' . '" '- .M '' t y":"" '

obtained are dip angles, meaaured in degress. The dip angles ara

obtained by first orienting the receiver coil in the plans of the

magnetic field by rotating the coil about a vertical axie until a

null or minimum signal is obtained, and then rotating the coil1 i*' ' , - - - '~ -' - ' ; . ' : . , ' ' . .

about a horizontal axia until a null or minimum aignal ia obtained.

The angle which the magnetic fiald makee with the horizontal ia

recorded ae a "dip" or "tilt" angle. In the absence of ,a con

ductor the dip angle will ho zero ainca rto secondary field le

present. In the presence of o conductor, the axia of the receiver

coil points towards the conductor and the plane of the, coil away" " . ' . -' .'. /- ' ' ;' ;',i, v '- '- ;- , -. ' ' - -. :' '' - - " . ' ' -.

from the conductor. In the preaence of e condgctor, tha eecondery

magnetic field IB usually dinplaceri frqfi the primary in-phnoo aa

uell as direction so that the total field ieellipticnlly polarized.

The receiver cannut then be nulled completely but a minimum aignal

can be obtained, the width of the''.ii^niiRum biting iti indication of

the phsoe displncement.

The tilt angles ero plotted as profilea,, the xero or

"croaB-over" point indicating the fociia of ̂ he.ACphdODtor axle. ;

Dnce a conductor axie haa bean established,the trans

mitter is set up over the conductor and linea are rend on both

sides of the transmitter and the conductor axle le traced out by"'* ' ' i "' ' V' -' i . ...i .. -. .' 'r . ' : :'.- .' . . : ' '' '

"leap frngging" from Mcrba;B-ovRr H t4o,?I QJlPi|B8*ovexiH . ;

Opera t(inq rrequenciBti t 1000 and 5000 cyalee per eecnnd.' i' .. ' . i '.'•'••'•*.- 4... , . '-'. i ' - ' '. . -;- r; i Y . - ' •-••^m,^. : -. --Kenrje; 2QUO foot separation betufieeh trrinawlttdr end receiver for

a i 10 degree null width.

Depth of Explore t i on t Roughly half the distance between'mitter and '' "'

Tranaroittor Poumr Supplvt 5DO watt alternator driven ijy a 1K H. P.englna. -,- /..- :; " - ,' ' :: - ;'..,;' /;; :

PaokbDard-mounted angina Qenerator ^^ J*B Ibs.TrbnBimltttr cbiJL on ^ackppard ' ;- **9 Ibt*.Coll mounting pnle artd 8pre0dBr ti*f 22 IbB.Receiver 7 Ibs.

42A07SW0068 63.2635 LANGMUIR 0S0

GENE HAL . . -.' . ' " '' : '' , . . ' ..' : - - •

During the period January 19to to January 23rd, 1970,

detailed electromagnetic survey work wna completed on the Claw

Lake property. Information concerningthe property ia described

in the attached report.

DETAILED ELLCTKDMACWLllC .SURVEY \ , J }.. ,., : . : -'."' *;-S'.'-; :, ': /'- ' ; . : :; '.-. : '

Three main conductive zonahav* been outlined on the

property. Theae are designated weat conductor which in part corree-

pondo to conductor fl on the general coverage plain, centre conductor}

and east conductor which generally eorreaponde to conductore A,

C and t) on the general coverage plan, the conductors ere described

aa follows: -: . ' ' -''' :;^'-' ' ..' -'.' ^ "'.'...' ' - '':-.-- '';- : " -""

uiest Ponductorai Almoet coinciding with B.L. t*OUI, this conductor ,

is at leoat 2^00 feat long, from Line AS to 2&S and strikes eHBBntia

north. For a length of 100D fafet, nb*rth of iinie 20^^ thia conductor; ' ' i ,; '. \ ' ~- \, . . ' ' ' j ' , ' i.

,, ; , t ..' ' '' '- ' " ! ,;' " * ' i.' '. jl " ' ' .' '

correepunde gtnerelly to a diabaee dyke (Bteore, November 18, 1969)*

Further north tha conductor ewingo east of the dyke into en area

of hiijh magnetic suaceptibility several hundred gatnmat above back

ground. Thia magnetic high probably represents ultramafic rocks. .

AB baaed on tha dip angle profilea, the conductivity ia

conaidered tu be of muderate to Btrong intensity with the oxcMptiqn

of Line 2'.5, neur an interprotad northeaat trending fault (Steera,

November 16, iyt9), uhere the conductivity is uiakj,

That purtitm of the conductor (approximately coinciding

with the diabase dyke is probably caused by a wet faulted contact.

Further north, the conductof, oroaaea a contact between rocks of'. , - i. .' -i' V ' ' - ' ' :',' v .' '-' ''- ' - -". -

'' ' * ' ' ^' r ' "' ' ' ' ' ' ;'. ,' " ' ' . . ' ' - .'. "' -' ' ' -' "-

IDUJ magnetic susceptibility, to the wBtt, und high roBgnetic

Buaceptlbility to tha east. Uhara the conductor entftra ;|he rpck^i pf

high magnetic susceptibility there IB an emhnymeht in thf contact,

This north portion of the conductor underlain by tpfiViB af hltjh

magnetic susceptibility may ne ctjuaad by aulphida mineralized

ultramafic rocks. . - ' . ; . "- , ;- '"vV:,.^:;v.:, ^ -' . :- ' ' '-i- , ' ' ' ' : '- v- ;, v:v -\ . '

... ."' " ' ' ' ,. ' ' ' -' :- '' ?.:--- !'' ' ' -' ,' ." ; '

Centre Conductor? This conductor ia at laaat 6DQ faet long oroaaing

Iin08 ZkS en ri ?fib. It almost coinciduB with the aaat edga of a l

lenticular maQnetic high Btrikirtg about no^'th* li? appears to be

terminatnd by B postulated northeast trBndihg faultV ' .

Although the conductivity. la valid, tha intenaity carniot ; ' ; ". . -' ' ' ' -'-'- ' -.'"-' ' .' . '' '"- , ,' -. i '- - 1 ' 'i . p

be BBcartnineri alnna the conductor is indicatBd oiii|y by atrong

inflections of the dip angle profilas. ;"

The conductivity may ba caUaad by a wnt fauitad rook

contact. ' . ' ' ' , ;' ' ;\ ' - , .' . ', -;: ' ''i"'.-':, : .,'-" : : .- .-'.^

Canductori This conductive ztina croaans tha /Bil ti^B propuriy in

a gsneral north-aouth diractiun for a length pfJBOO fuet. The zone' '-' " ."' '. r '- : "y ; '-,-.'v' .^';;W1 i-'^^' V - i;; '--- :- : '';'-' ;'.. t ' - ..-.V' 1

of conductivity croatiaa rocka ^ of variable magmatic Buncaptibility ,

ranging from abuut 1000 to 2200 gaifipiaB. "v j \' i

The north portion of 'thinj. t;pRduCtivB zonB, fqt 3PO faat,

is of wwok to moderate strength baaed on the ratioa of Ipw tp high' ' ' '

' ,- X , .' ' ' - - ,-', "'S - ' 'r . . ' i '- .-''

dip angle profiles. From Line 129 to iine 24*8, thBBputn portion v

of the conductor in of moderatB tp strong intensity, tha intBT"* '- ' ' ' . ' '"" - - ' i ' : . . ' ' ' ' ;.-'. - ';

' , :''\

vening portion of thn conductivB zone is flf ̂ wiiak tt3 modgratB '; ;-

intensity. Hare the variable iocationi i 0f tHc (sbndMctpr JBIKBB .way

indicate B wide zone . of u&ak conductivity i the pref erred intBrpratation,1 ' - ,' ' ' V - ' '' - : : : ''".'- ' ' '^'"' '- - ' - - - l ''" 1 "'" ' ; 1 '. "'' ' ' t "

or two approximately parallel conduqtpi'B 200 .fast -fijpart. 1 ^ ';; -

- ' -3 - ' J:'-'. . " . ' , . ',. '; Y -x- ' - ' " , ' - ' . ' ' ' ' '* " , -, r. '

Tha i?o'-;t conductor appears tn ba caused by a prominent

fault or ahuar zona. With a fHV/Qurablf geological environment ;

BBctitinn uf the conductive zonn nmy contain sulphide minnrolizatian

associated with ultramafic rocks. , ,

An iatjlatfid conductor crosses L ine 2QS at Station

Although this conductor appears to continu* northwards alantro-

magnetic traverses in this area were not uxtaiidecj far tnriutjfi i wiat

to crciaa tho projficted axis of the cbnducto.r^ ,|t ̂ la aKplc ted that

the conductor f ol louis the direction sif a probable diabasa dyk* in i- . - - ' "-'; ' -' '-- -'' ,~-' " ' - ; " , ' . ' ' -,;V

the area (Steurs, Nuvombar 16, 19fi?) andvtnat tna conductivity lav

caused by the cant , ut.' t TaultBd contact of the,. ' ; .;."-;- ' '. ' ' ''"' ; '";;.-^-:.'X^.;.";::

AND ' '

It is propoaed that ̂ BBCtiona of tni f *8ii ind uaat con- ; ;' '' " -* ' * j' . iV, . \ ''"- 1 '.' , f- ' ?'.'""'*' ~- ^ .. p '-

ductnre be' investiyatad by drilling. .' ? ;!, ' . ' ' ' .. '- '' -' i'. ''* , - : '-: ~ -' - , ' '. ' ' ' ''- 'r'--' ' '

The first hills IB located to investigate the north stctifcn

or tha went conductor, A cowbin8ti{|n of fBctdrB indicsatt tha

puaBibility of aulphidB mineralization. ThB cpniduiitoj' nroaoea li: ' ' '.' ' ' ' ' ''. " , - "' , ' ' ' " ' f f '

rock contact whern rocks nf low magnetic susceptibility am smbayad ,-

by rocka of high megnatlc susceptibility* The rockB of high Biapnatl.ts

Buacaptibility era probably ultramafic. ^ * ' i . v;

Hole No. 2 la located to inveatigote the centre portion

of the aaat conductor. Hera the axaa of waak conductivity bound

a magnetic low. Y. . ' ; ' .-'••,- ' - ' :"'"^''^.^ "'. : ' ''' ,. : "..- "' ,; -.".The north portion of the aa^t conductor^ lieai1 line 6N, Ip

of moderate intensity in an urea of high roaQnatic auacaptibllity,

Hole No. 3 ia propoued to invastiyate thia area for poaaiblB aulphide. '. , .t' i ' . -i'*, .-' '"'v'1''. ] ' ' ." " '- - :*. . ' ' ' ' . ' ' .' ; - 1 - , ' '

mineralization. ' ': '' -.f. 1 ' . '"-. /', , ' ,' '^ :- ' 'i' ' .' " '. : ^'' ' ' ; "V ,','-

' , - . ' - ,..

Hole No. k i s located to investiaBte the eouth faction of

the east conductor adjacent to a poatulatad northeast tfanlflin'sj "; t

fault a structural condition perhepp favour?biB to suiphlde

mineralization. ' , : - - " ;:'.-- . ' ; : / ; "-^'•:i '.\^' ^ ;-... :.:

Specific data concerninij the pyoppsad drilling is aa' ' '' '' "" - ' ' ' ' *' '

Hols Line Station Ofoaction Dip

1 88 39*25iii ulest 50" 250

2 W 3 1+OQul UJaii ; 50"

3 6N 31+BQN itJeat SO 0

Four holes . ,. . - - ' ". ; - /'. - ' ,,'\ -' .'. ' ; : ;-.; 1IOOV-:;-' ' " -' " ' ' - -'- i " ; : '* : v- ,' '- "'.' ". ' ' ' f-' ''

The BBtimntEri coat for this drill projsot including

Buperwiaion ia

SHlttO Qt

Timmlna, Ontario, R. J, BradaHBW,

January 3D, 1970. ;

42Ae7S*e*68 63.2635 LANGMUIR 030

INTRODUCTION . . ;

During the period November ** -7 inclusive, 1969, a

magnetometer survey was carried out on the property of Claw Lake

Molybdenum Mines Limited, Suite 405, 67 Yonge Street, Toronto,

Ontario. '. , ,

The property surveyed consists of 12 contiguous uhpatented/

mining claims numbered as follows: P97801, 97802, 97803, 97804,

97605, 97606, 98668, 9B&69,; 98670,, 98671, 96674, arid 98675,

LOCATION AND ACCESS . , ,. "";v . '" ,-: ;i - !,'\ -^ '. . ^, ' '

the claim group is Ideated in the northeast quarter of

Langmuir Township some,20 miles southeast of Timmins, Ontario.

Access for survey purposes was provided by boat on

Nighthawk Lake. . '-.*

PBEUIDUS UIDRK : . , .."- - '' '

Portions of the claim group were previously,held by Tinex

Development Exploration Limited, P.C.E. Explorations Limited and

Con-Key Mines Limited. -

Magnetic and electromagnetic surveys were completed by

each company. J

Con-Key Mines Limited performed an induced polarization

survey and drilled one hole on the northern portions of the group*

The drill hole intersected basic volcanic rocks and peridotite with :

minor disseminated sulphides* . ^

GENERAL GEOLOGY . ' :'- "":\ - '''-. . - ;.-,'

Geological mapping by the Ontario Department of Minesl'''," " ' ' :. ' ' '' -' \ . '

indicates that a few, scattered outcrops of mafic voTcanic tuffe

'. '' ~ 2 - ' ...' ' ;. ' : ; .--^:;;' '-'".'.-:... ,' 'Y' " ' '

and agglomerates occur on the property. Correlation -between the

outcrops and previously performed magnetic SMtvays IritiicatB that !thB

rocks have a northerly to northwesterly stfike.

It is thought that part of the property may be partially

underlain by sill-like bodies of*ultrabasic rocks. Some differentiated

ultrabasic sills in lanpwoir'fownshijpi containi signif iC'ant airipunte of v

sulphide mineralization having values in copper and nickel* '

INSTRUMENT USED 'AND SURVEY ̂ METHOD -Vi y ? f; \ : f;

The entire survey was carried but utilizing a fluxgate,

M.F.-1 magnetomBter manufaptured by ScintreX Limited* Sensitivity

of this unit is * 5 gammas. \ ; '. :'-i; .. , ; :

Base stations to facilitate diufnajL Corrections were

established on all baselines at iOO foot intervals. All picket- - " '- ! . . - : -.-' " -. v ' - ' ' -

lintis were read with a station interval of 50 feet. ';

A total of 1352 stations were read, 132** of which were :' . *'.' j...'- - - - -' --'' ; - , ; ' --.' -

within the confines df the claim group. ;,. ; ;

SURUEY RESULTS , ' ; ; ;"' './- /. ' ', .' . ^-, ••'. ; ^ ̂ ' - . . - -

The survey results are presented in plan form on the ;

accompanying map. lEiomagnetic contour linea havei'bfe'fth drawn ,at 1,00 .

gamma intervals between 200 and 1500 garnmaa and at 500 gamma intervals

between 1500 and UOOCi gammas. ' '

Maximum magnetic relief is in the order of 3900 gammas, '

There is a little magnetic relief ini the ebuthwest portipn

of the group indicating that the area is underlain by hOmogBrtBOUS

- 3 - \ v -- :,?"'^ : ' ' , ''••••"'•"' ' -' '''' 'i;/. -V. . ' - ,

rocks of loui magnetic susceptibility. ;

Tuo faulted diabase dikes are indicated between tie line

50 U and B,L. U O lij. ; .... -'

A sinuous gunerally northerly trending contact zone is

present near baseline i*Q UJ. j Cast of this zone the isomagnetic ctintours

exhibit a complex pattern of isolated highs and lows. It is

believed that this groa is underlain by mafic volcanic rocks which

may, in part, have benn intruded by narrow 8lli*like lenses of

ultrabasic., rocks* ; ;

In the extrnme southeast corner of the map area north- ;

easterly trending isarnagnetin contour lines are, believed to indicate

another contact area. The rocks to the southeest are believed to be

the same as those underlying the western portion of the property.

On line B N at 27 id a reading of 79frO gammas waei obtained*

It is believed that this is likely due to mari*made causes* As

nearly as can be ascertained from the data on file the drill hole by

Con-Key Mines Limited should have been in this general are?. . ;

SUMMARY AMD COIMCLUSIOfJS ' .;'"^ ] ''': :̂ '\ ''f. •^'•'. ;"--.''.

The western portion of the group is underlain by apparently

homogeneous rocks of 3ow magnetic susceptibility* , .' :,

The eastern and central portions of the property are under*- . ^ i :

lain by mafic volcanic; rocks which may, in part, have been intruded

by sill-like bodies of" ultrabasic rocks. ' , ,

The most prominent features are the contact .areas between"

the mafic volcanic roc:ks and the homogeneous rbcks; Df: low magnetic ̂ jV

susceptibility. ^ J; ; ' :

RECOMMENDATIONS ! ; .:h-

It is recommended that, the scattered pUttstQpings on V

property be carefully examined. It is ppssibl,^L thai:a touch

interpretation can be made, if better geological icpnirpl is

Since it is possible that petit^o'tite Sills (do exist tin

the property is is recommended that a dual frequency veftical loop

survey using the fixed transmitter fanl;'ffl'9tl^^.-j^la;,.C3.8ipplBd^out;'^iiJn^ thB

central and eastern portions of the property*^X :

Consideration should be given to.putting : additional lines

in order to perform the electromagnetic survey on iines spaced at

200 foot intervals. Should sulphide concentrations be present on

the property it is likely that they will have! limited strike length

and that they will b f. relatively poor conductors,;

Respectfully .submitted,

\ SHIEUD GEOPHYSICS ilMITEO,

Timmins, Ontario,

November 18, 1969.

J. E.

Consulting Geplogist

l

Type of Survey———

Chief Line Cutter or

Party Chief P. Young

Consultant J.E. Steers

SPECIAL PROV 42A07swae68 ea.aeas LANGMUIR

ASSESSMENT WORK DETAILS

MAGNETOMETER

NomeRR#1i Timmins

Address

NameCOVERING DATES Line Cutting

Address- / 3

Field Geology or Novembeg 4-7. 1969 inclusive

Office Mov/ember 1tt, 17, 16, 1969

900

A separate form Is required for each type o! surveyG. Gaqnon________Highuay 101. South Porcupine

Nome Address

__________199 Leiphton. South Parcupina__^_

INSTRUMENT DATA Make, Model and Type

Scale Constant or

Scintrex. M.F.-1 Fluxgate MagnBtomBtsr

j: 5 gammas_________________Or provide copy of instrument data from Manufacturer''s brochure.

Total Number of Stations Within Claim Group ——132n——Number of Miles of Line cut Within Claim Group——13*3

ASSESSMENT WORK CREDITS REQUESTED Geological Survey

Geophysical

Days per Claim

- Days per Claim

MINING CLAIMS TRAVERSED

P-97601. 976D2. 978D3. 976Dtt . 976D5. 97806, 96666 T 98669 T 9B67D r 98671 r

9867^*, 98675 ___ _________________

PATE Movember 16. 1969

TOTAL

SIGNED

Special provision credits do not apply to Radiometric Surveys

Submission of Geological and Geophysical Surveys

As Assessment Work

SPECIAL PROVISION

In order to simplify the filing of geological and ground geophysical surveys for assessment work, the Minister' has approved the following procedure under Section 84 (8a) of the; Ontario Mining Act. This special provision does not apply to geochemical, ground radiometric or airborne geophysical surveys.

If, in the opinion of the Minister, a ground geophysical survey meets the requirements prescribed for such a survey, including:

(a) substantial and systematic coverage of each claim(b) line spacing not exceeding 400 foot intervals(c) stations not exceeding 100 foot intervals or(d) the average number of readings per claim not

less than 40 readings,

it will qualify for a credit of 40 assessment work days for each claim so covered. It will not be necessary for the applicant to furnish any data or breakdown concern ing the persons employed in the survey except for the names and addresses of those in charge of the various phases (linecutting contractor, etc.). It will be assumed that the required number of man days were spent in producing the survey to qualify for the specified credit.

Each additional ground geophysical survey using the same grid system and otherwise meeting these requirements will qualify for an assessment work credit of 20 days.

A geological survey using the same grid system,and meeting the require ments for submission of geological surveys for maximum credits will qualify for an assessment work credit of 20 days. If line cutting has not previously been reported with any other survey and is reported in con j unction with the geological survey a credit of 40 days per claim will be allowed for the survey.

Credits for partial coverage or for surveys not meeting requirements , for full credit will be granted on a pro-rata basis.

If the credits are reduced for any reason,a fifteen day Notice of Intent will be issued. During this period, the applicant may apply to the Mining Commi ssioner for relief if his claims are thus jeopardized for lack of work or,if he wishes) may file with the Department,normal assessment work breakdowns listing the names of the employees and the dates of work. The survey would then be re-assessed to determine if higher credits may be allowed under the provisions of subsections 8 and 9 of section 84 of the Mining Act.

If new breakdowns are not submitted, the Special Provision credits , are confirmed to the Mining Recorder at the end of the fifteen days. '

ONTARIO DEPARTMENT of MINESRETURN AT POINT OF MAILING

Ontario Department of Mines, Parliament Buildings, TORONTO 182, Ontario.

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LOCATION MAPScale: l - 25 M iles

LEGEND-— Claim post and claim line

Lake

Swamp

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Magnetometer values in gammas

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REVISION DATE APF D

CAN-FER EXPLORATION SYNDICATE

MAGNETOMETER SURVEYOneman Lake Area

ONTARIO

Peer 2OO Oi i i

2OO 400 600 Fee!

SCALE: !,inch = 200 feet

DRAWN BY: L. Nagy

DATE: November 1969

APPROVED: J. Koski 1/1

N. T. S.

52 L 7