32D04NWe293 63.7 LEBEL 010

KliP'Jf?

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A cool o(;l cal fcz;d ReorjaGnetic eurvoy of tbe Ftoouroaa

property has outlined ou Etr*a V el lev od lo bo

Kreenstoue on the mu then ft cornur contuiRlni

which w&rrunt diamond drilling* . ?l-io xone oppeare moat

n*;: bc emu o c of ft poor i Vie coimcctlnii v/lth gold

an roc i Q ted v/J th f. heor'ii^ l .M Gauthie..r Tv/p.

rt;;ilt, /;or^h Wjd v/o^t of thi a ^ono iiau

*t of Turtle U*ko ond osia or U#o oxplor-

utory Ixslos aro Pusc^stod. ^{railarly, X-roy drilling of

the altered ctir\'';^utt:1 iona on ohe north fferj'.in of the

eyojalto lo 8Utii:o:ito'v* to explore* ttrlffc oovorod ora&s alcng;

tiiia VAclt . 'Ihofio tvo ^"vnt;s ju-e not boliovod to be parti

cularly promlelnp, iut Bbould be oxploixidi at stroteglo

loootloiiB Indicated by ^eofeucnotlo r*ssal Is.

I fir*i, \T.1 ti"" 'l-'-i XT -H . j\ i , .K;y j J . - a

I'tc chief object of t ho eurvey wuc to oetdbllsh the

ooBnoctlon, J f ary, !;i'U,eeti tht* csrb'mti tjiod f&ult iioiio

v,'hlch o i ten**; n across the 'vicsitorii pert of ftoowsoa propertyi

euDtv/ard frosi t Jit* :'uMlo Liite feu It, i^ud tho Koltl-boarliig

oht;ar iouu vMeh h?s(! boiun locijti.^ ftorutif;wt,ttloally In tho

Urlft-txivortiCl v/ortorii v^rtlon of Cjautblcir Township.

The guooficnotlc imrvwy '..n:: eonfinod ler{*ftly to the

southern pert of U;o property of oewfifiu KJnos Ltd. t oo'a-

prlelng claims 31X^7* 5^* ^'yC, UC^, 905^, 27721, if

. 2 -

, 27140, 14555, 27510, 27511, uiid tho eouth*ra

portions of olei&a 7751, 526, 527, 8550, 15658, and

three treveraoa vero node northward to th* trons-

line of t ho Kor the wu Ontario Light and Pow or Co.

In till cai eroa of about l c^utro mile: vms curveyod geo*

North-oouth picket lino a turned off by transit at

400* Intervale alortg u eturvoyed bfiiso-liiis ruardng between

the 8outh-vt,*t corner of olaia 3097 fi oft o point 504* north

of the oouth-oar.t oornar of oloin r2?142, provided tbe,;^ -

Jbr tlxf aurvfcy. ?:lovctn Lui*3rod oiid ^l^ty-eight

dotorwliiutions of vertical csagrietlo Int^oeity

vere miuao v.lUi (.n .'.arr^nlb vertical vrrlosteter et

Intei-vule of cot laorfc U.an KX fa e t til one 15 *Qlli*o of

llueo. CloBor IntorvclP, (bvo to 25 fe*st vore observed to

record dttti.il ou Irriport^t MI om til i os. Jvovorol additional

oaot-wtit}t ti'i.verfo liauu \to-ro run to verify tho existence

of a north-south tn;*K*!nr, t.nor,ta\y* All results Krcro cor

rected for diurnal mid jnntruiaonttil varietion by ohdok ob-

servo t ion s on ^ane stutio&s at In tor val s of two houi'S or leas*

q;x)UiOV OF ?i ir. MAP A**^.

Outoropo era nuraeroua in the western part end along

the northern fringe of the nop ereu. To the south and tmst

however, in oli-Jcfia 27U1. 27140, 27511, 27142 end 14355, a

- 3 -

of sand obeeurea t ho roclc surface. Ctand rld&ea

rarely riso wore than 5^ feet above the cener*.! level

of the country*

Over &0& of tho exposed rock in the urea le

oy en i U* V.M oh, to the narth, is lit intrusive contact

with tuff e of tlio Tenlsksialne oorleo. Tho contact

eycjnite tind tuff In rnout plttcen connot be ohorply

due to ititeraotioQ teuton tuff tind ayfculte, or

emanations f mat it, which txiva produced a ^ona of

ayeuitliicd tuff up to 200 fewt in v/idth* In the vicinity

of 600U*.26003 eftrboiifitUfttion 5;iis atf;5ort to t to difficulty

of dofiiiiuf tho. contact.

Ttw ptitawB of tuff wore rccr^yijjcufi in the outcrops.

A fiutt.grttinefl, utric ttftolo tuff occurs ifaaecUcttely oorth

of tho Bycfiit in b t or. d f row 10DO to 1^00 faet wide.

Tlieee dark tufCo tire hlehly rao ^/k^ t i o, contttlnir^ bonds

visibly rich Ju w&jjinuiltG. To tl*c north t* lifjht (;rey to

pink diljkoooua tuff prevollfi vh'ch t'^"d**s corths.ard Into

nohlBtooo tufftiooous pobble oonfloaer&ttta in the vicinity

of thfe 2*o2'thttrn i'mtarlo M eh t cind rower Co* transmission line

The tuff e tuid Btidlsaonto Btrik^ ttpjiroxirsa tcly eaet-v/o^t

d bins 774*1, 7741* 77 (''7 ^n*l 1^G^7 but **t the eeatorn

of L r* 41^6 ^itt strike* ch^i^tiB qul to abruptly to

tho Houthttunt.

In tho \-crtwrn p- rt nf the c*rou the tuffs dip (tenor*. 11 y

but In ci t* IK l^W^* ^* jC ^* P i^ to tiio north.

Tho Dodiraonte am! the {siliceous tuffs In contact

v/lth thexa tiro ^uite hJr.itly schistose tind curbonutl2,etion

and silicification vero neon In places notably around

2400f W . 4000*11. No definable shoe r /one was observed,

however*

Ojj tlio v/uiit bautt'3uiy of ci ala t/lO^:), about 200 foet

south of the ohort; of Vurtlo LtJ;;o {.iid outside thu mop

old oloo v/ork:1 1\K& u&posu G tv/o foot quurt^ voln in a zone

of carbonated syunKti. Thio frrjcture ct:,n be traood eorao

4000 faot iK.;itwariJ fjl^j-i to the v/oot boundary of oluita

5096 by ocourrofioea of o.jrbiM.tofl ayonito, ^ucirta veins

arid Bn&ulur CKrbowoto floct.

A f cult BtrikUiJ. norti,et58t, Is mispoctod It* the vicinity

of GOOw - 2600K. A fi-ijotured i**!* v/ec* observed in tlio north

end of u troiich fiour 400*/ . 2700;J ftnd on close inapoctlon

it wt*e dutorftiftdd that the rookt? on c-i t ho r aide of the

Bucpeotod fiiult differ in orlcln, blthough now rather aim-

llto* in churocter duo to ct.rboi^^tJi'.atSon. lUiuded structure

Jn Hit* flDe-^rolnod, dijjt'k frotiii rocks to the ea*;t

thw groon oorboijjj to rooh to the i;ost grades into fairly

fresh jmpure ayenjte.

- 5 -

liooulta of thti cyoiatifinttlo wurvey wre conplled in

the cjep vhicL nocoiiptmlas this report. Linos of equal

vortical tibctictic Intensity {{jeoMe&tititlc contouro)

Illustrate tho t rond of uijofaulltja.

,i north to south tho outotundinr magnetic feature o

(a) lil the o.trof.o jiorth of the taup-aroa, u ^ono of

unlforfn very lov ru.rnoti c iritimaity v.hich extoiida

northward beyond tfie liuite of the eurvoy.

(b) A ollc^t fiO{;utlvo nnonfily trocdlng south of east.

(o) A Siono of irre(yui^r, h l eh rat.ynetlo iutonsity.

(fi) A sono of rwtLor irro^ul^r, ood orate, maf^etlo

IhteiiSity i/hicJi, v^ct of liLO 2000 U, uxtotide to the*

southern Unit of tho property.

(c) A cUatinot t- 1 1 (t pu r e Its t en t no^fitjvt) onocuily, \vMob

truvortiea tone (d) betveon oOCOU- COOK imfi COO*.' . 1700!5

\;liei'O 1 1 o ppt,rcr, tl y t c ir; l u';. tu r..

(f) i,rrcitlo ra^r.notic Jii/^iu itjc-iodltitoly ijouth of onoDuly (e).

(g) Lust of 2000'.,', Viitvxoi; tho lit-;tjollno and the couth

bound ury, u i^nnc of Lifh rxi {;LO t it) intenoity.

(h) I'sctwttcn /,QG . Kiirt 600i; find otrlkinc slightly v/oet

of tiorth, a ivonc of M^h rausnotlc intajsJiy v/hich ox-

toudo from the mutfc bnun^m-y to ebout 600* *Jorth.

- 6 -

Geological bo'.mdk.rlos, fi iructureo and roci: typos as

Intorprotud TJ^W the Cbowucnutio detu are Indicolucl on the

accompany l ne aa p.

( n ) Connet of rh:slo ruffs D; Hi 33I3conuo 'xiffs

i'iie aoiit* of uniform Irv ra'.r/joti c Intensity vvfaloh

uxtondo i:oj"of?st the norton* Ifr^lto of '..he rwp-Dreu cor-

rtj.'jpojj v.-3 th D belt of oillcnrmn tuffs arid tuffaCDOUB Bod-

ijyont. VliO onMnct; nf thin ^cl t \.1tL t ho brjsic tuff o wuo

olourly t^rf.^ by o liuckion li-.on.:uofi 5 1, r.:;, ; jiotic luterio) tloo

ar;d vms triicod bcijcuth t ho iirjft to tJ;y etistcrn boundary

of t ho property.

( b )

. 2,011 o o l* c r.i rb .'.*j 10 1 3 i- 1; 1 1 on So i nO letted by a nofju t i vo

In thf) vlclnjiy of t,\,j traistilor'lon Uno. Thio

to K 6000

46001? (lirln baticlJnt;}. Tt Jc not pronounced i.txl no liapor-

cho a r voiio 10 lrj;*l ci, t ud.

(o) uwl (iO ^ti tuc t oi -'ii o,^r.i? J 'a f f

'i'ho contact tctwcon oy on i tti arid bo t; i c tuff is rariccd

by un liufrouoe l ri nti^notio ii-tuv :ity fro a syenite to tuff

and \7t:o followud 1/3 the llnJto of tho property. In the

vicinity of li G400 ~ 5^,00'.,', tJtu c-'intf.ct owin(;o shorply

BDUtliv;fjrd follo'.vjii(; tl.io trcjfl of the con toot bctvetiC tuff o

tind tseditionts to the north.

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oyVhe i/iiifhutonotur Lt*s proved of vuluo In prepar! ng

i* oociprohenrfJvo ^ool'^lt'^l euip, tui h&s yjoldud ci cioro

useful ploturo of ttub-eurffcC6 ^colony tli&K could htavo

boon Inferred fjv*n purely feolo^ioul ofc at rv tit l on e of

outozops til ouc. Jr* iho oa ut hoc o turn purt of the property

when* no outoiops tiro unovm lo occur, iroortajjBatio oappiDg

LQB iDdlctitud the prtjj:cMjcc of a cliabuot* dike) t)Dd a bolt

of ulterod croonatorio south of the isyenito, Thin urea

rauy cctbtuiii o elio^'^d J6OU& r&l tiled to tdterod nodiraonto

and turf o ID Oituthltr TownaMp, but not related to tbo

Kooaeica fault \vhloh ti-cn*}® cvrtv.-^rdfi frori the couthora

of 'Air tlc L-ui;c, fi.*:) cpptwe to tor-filmito r.ortlj of

tdtexi^l ^rt oi.st^Ltj. J'oivot! ou^l an-3 ntruotural

ff, im.M.uu? w. t 'Of:iJMfc ;. f *rv s of tiLt-nrSrvf: ^ ara

v/ii on Ihe .';uolo,f!et.l ru-p rtiM'wCvn'.Jrit* our

tlon of the ct^w ".f'.Motic dutti.

A iiono of otU"b:'tiii t J ic t", t i or. r.e^r tho j-jov^s

Hiifi Is 3 li d J c ut od by a j :;U; lively vrofJ: n^gnetlo unomaly,

but no lup.^rtcxnt i'.ojio of tlicti'liiC GI^. MJncrcll^atlon i c

^Jli.oo, i.D'.*evM;r, l-vv/ cold vtluos have boen ob-

in tho oarb^ijotjiitid K, cho in^r thin cnoniily, and

oirioo tho taa&t fiivouiritilo j^;rt of thin iojiue lo now looutod,

of the wiowuly by ti f ow sh^rt holoo rw^y b©

wit f xj o i oil y x /ho r e it ie moat pronounced* If

drilling result e warrtmt It, tho pnaitlou of the utiomuly

~ 10 -

tho linos tslixutly curvuyod can bo dott mined

by o f.oj-i} dotiillod (jeori.ucnotlo ourvoy of thia tiroe.

The curbontitiituS altered t, yen i to and tuffa sh^wu

OB the o up In the vicinity of lac fnult lione on the north istirrln of UK; Byoriittj tb Lot tonour to bo

lculttrly piWtlsJiit' for t* o l'.7 ir.lnvr^lli-.iutlon, but B

ahort J;^lofi, porh;;pn V'l th tin M X~i\f ;y" drill totay be

warrantuA to cx';ilor*j r l*^ d rjf t-cove-rod oxtcnr4ono of

thlB zone, Dhown on t ho i'oor.* (;i.ol3o-.. ; -ool^.'lCftl wap.

The liocaRint fault oa^t. of Vurtlo Lckfe is revealed

by c oonapiououfj f i^r^f^u-3 o for. lure ^a fur tjo lino

8-0, no Moll-lllur, tr^tfci! 3z: this pl.M.o^rtir'h of the

solid rxidtil. (Plt.10 1), VMii Tf.ult lo tiowoietod

locally \d th eorhoruit* i;^d :*DOi;, l^u t it 3o not folt tlmt

it 10 of ve. r tl cult, r 'ioori'^lo 5nto;*o* t. .'f ney the ftiult

hue boon c*oourotoly tn;cofl foaf4a{-ne t3 c;.lly, aov/ovor, end

the lOCdiMllty of ^.olc; i.ilncn:*li^:.U.on ;vni:Jnn, it. le

Euiurotitod that short J.olt-.e Ve c* ri lit rt at strotogio apotts

in oi'dur to oxplore t3;oi'our.lily 13;B oro poooiMlltfoe of

thici ftsult y o ne,

If out* or*nffi*idore thw f:*;.'Wifcf',r.utl P chtirtiOter of the

drift-covcrud tiltorod ^roonotano t;ml ttyoMtifccxl ond&

iiiid tuffa itidjcutoa !n the nouthof.oturn corner of the

property, rulttJvoly .••tj^nf; f.jvirial iof vi t h tin o&ftt-.v^iBt

strike suf.T^'*t t ho ^rusu.-noi, of atriioturtU futAuroo t'.tri!,

J . rn.vc Li.o.-i, to

In 'Jauthlor .o1.; j i ?c Ip tind eij^?lnc von-le^Hy or steeply

{jOUtJj. '^htf rc'-K-'.t.^iJt'U C i/rofllt-;.; i.;,-!-.,1 i, J j., t

of ovorbiu vjou j. tt i.'it t r j o fUA-:^ for ^crnior.ic t31a;soi.fl

drilling, MiK'i t:uctiiK;;-t of M.e ])-.n;-,J Ml T, v of .;..

r.iiiiurt*lii.'f,tjoji J:: this ^ilt, :a; ox-l m-a lory li-Ju to toot

i.y St; i-oo'v. •-•of.dul.

, ' 'r.'yfj - .-' ' - ' ' ^ M'r-. -." - -.. s T r '. If "f . .- - U. . ( . . . . - . J . . . ' ., . . i . . .1 l i., J. , ', -. l

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tit ui r oo rt* ;,o i /o ft.

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includes lUidcKlto, undo M t jo tuff;*, tllorlU-,

e.nd dilorliiwOd r.npturm*phoftod dorlvtit jvoo of iheao irooka,

Minor syenite) and fultfup&r porphyry, unc! VMlfcblo

eulphldo i:iSuv;n;l Iv-otl on, i ri too eixvplex association to

* It Jc llkoly t lw t

Of thi W I'ul t V';.,'., oil f l JV td) y l. Ir:" i; S J to t*Ii(3 tuff, 1,'hich

ht*o been fcltorv-ri, l c: o.. li y, ;u.rt3clly f..-;;l ,'-,1 la tod tiiid (K)

cloaely lntruO!c.1 V-y Vi.lj.o uii. 1: i.lfCvD iiu5 y^iall ntooke of

fei sir 5 *M- porphyry 3i3 ;*li.c^B, thit !:ifiro tlitii^

of thy rot'l'i i-o^rorst.p.lo irttcrli.1 li^.roducocl from tbo

In true! vo. J-inn; i'Jfhly ciltorml i.rttn: vlth'n thin bolt,

p5rtl*y-.ilt..rly chiral t!*;,ud ?^n^ nchli^tcd zojv-o p.'otluood by

-i c hlrfta, 6riS to

bo ^conotjlcolly J -.'vrt^nt t..:,, w^iioti thi t v;oi-o titruc-

turully fcvoruble f^r the pt*r?t*{tc of oro-! otirit,i;;. oolutlone

i.i of M{-:h C

tho tjoutliobtttoiti colour ip J ;? ,;vud to luit duo to

, noof.lbly the t f, r^i lv:, t i on of ts iinrtlwsouth

which ciULcroj'?. thro o-nuiir tore of 6, ,'.-Jlo tsouth of Uie

Koo,,jrm4ti f.roj^jrty. ' hllti of no ticon'mJo Intorcnt, the

delineation of ihw dl'.;V'tso Sri t?. Ir f:ri;o lo uooful in out-

futile f^r tfrlill:^-.

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