42ceaNwaees ee11 LALIBERT 010

Discussion of Anomalies Wa-2-4 and Wa-2-4a

Anomalies Wa-2-4 and Wa-2-4a (Fig. 6) are located approximately half a kilometer south-west of Big Marsh Lake in township 30, Range 26 and are accessible^ by truck from an old road which leaves highway j? 17 some 35 kilometers north of Wawa.

i

Five linns of anomaly Wa-2-4 and- all of anomaly Wa-2-4a are underla: by a small lake, however, the few exposures examined indicate that th^ area is almost totally underlain by metasediments - argillite, slate, chlorite-biotite schist, and a felsite - some of which coulcl be reworked intermediate to felsic metavolcanics (personal communi cation - F. Van Thournout). Metabasalt outcropped only on line 12 west, 4 south. r

Pyrite is present in trace amounts in all units.

Conclusions

Geological mapping failed to, explain other Wa-2-4, a seven line weal to moderate conductor with a'moderate flirting magnetic anomaly or Wa-2-4a. a four line moderate 'to strong conductor with a moderates flirting magnetic association.

To determine the exact nature of these conductors and their magneti* associations, the scheduled hole on line 'O, 3*40 north, bearing 220 at -45 should be drilled:

The geological environment does not seem to have high base metal potential and hence this drill' hole should have a low priority.

S SM-2044

UMEX AREA WAWA

ANOMALY NO. Wa-2-4 Wa-2-4A

District and Province Algoma, ONT

Party Leader_M. Gagnon—-—-—————- Dates of Examination Jan.17,18,19,23Assistants B.Macparland, P. Kennedy, J. Charlton,H.J.????????Location details? li miles east of i.^y 17 - l mile south-west of Big Marsh Lake

Topography Rolling Hills and Lake_______Overburden 10 to ?—————-—,.———, f Timber Spruce, Poplar________________Water supply conductors mpstly on^ ^ Accessibility Summer road - snowmobile in winter. |

Samples collected_ Thin Sections

Description 6 location

Assay

Representative Type

Water

Foliage_____________________________________________________ - Supervision Remarks_____________________________________^.——— ^Geophysical An Wa-2-4 - A sevenline weak-moderate conductor with a moderate

fluting mag assoc.An Wa-2-4a - a 4 line modest-strong conductor wit.h a moderate tluting

Geology ' a ssoc '

Drilling see page LwoPROGRKSSION OF WORKS

WORK DONE10 linesSE- !b(J-EM 7 lines

DATE SIGNATURE21/L/lb 23/1/75

line

i

REMARKS Wa 2-4, 4a

#i. GENERAL GEOLOGY

ECONOMIC VALUE

GEOPHYSICS From the vertical and horizontal survey , several parallel

conductors were located ;

On line 4W - the conductor at 4 + 30N has a Js of 160 -————--.-——-— The conductor @ 2N has a JS 20 mhos with a low mag between them.

On line O, there are two other conductors, 0-fOQ, 2+OON, 3+OOS____ The one at 0+00 has a better Js and magnetic assoc. and therefore a D.-e-5-Hr—io propooed fco intoraGot this oonduotoro.————————————————

' CONCLUSIONS D. D. H. L-0 1+OON Bearing * 220—— 0=250'Dip s

5+40N D=450orDip ~-- 45 0

•(to intersect 2 conductors)-

_Signature

Date

UMEXAREA

ANOMALY No

District and Province ,

Party l ^nrfpr /sfxj/LffK

n 'tefPt.Assistants

Location details ../.

, /C/^LA^ xA.#Dates Df Examination

17v.^/***

. ,-/ 7 — X ^g^tVV.

^ . y7.x.f,/^ :

. /7i J'^4^C-i'aa3*^

Topography

Timber

Qverfaurrfpn

{Accessibility . •-f, ~~..vater suppiv - t'^-vj^-l.i+is&SV A-t^-^^^y g^t ̂ ^.X^J

y*->^ix^^7xl ^^^ JtK^^*?-^ S ^^^^^

Samples Collected

Thin Sections .

Description and Location.

V-J

Assay.

Representative Type

Water ^.

Foliage ..

Remarks

Geophysical

, .^rf T^X^

y

T17PROGRESSION OF WORKS

WORK DONE

TT

DATE

'

-m- SSM-2044

REMARQUES

YOLOGIE GENERALE

ALEUR ECONOMIOUE

EOPHYSIOUE -^Ts.W /fa S^^* f̂tf'X^^^-^

y

^r^'^ G) &V Jto 4. CTS

O t-tt &-T.C-. .^

sX^oD -O

,

tf

CONCLUSIONS

'T'P.//. /-Qk.'JT

,

NOTE: (U Signaler possibilite's on cau, bois de construction ct donner les renseiQnements utiles pour one campagna

do Bondages,

'(21 Etoblir one cone montrnnt Ins routes, nffleurements, directions et pondages, o'aclation. cchantitlonnage

levee non-*ro des prises).

••iA

UMcX CORPORATION LTD.

l935L*ili* 5i'**t,

Dan Mill*. Onlo'io, Conode.

Hoi* No: Wa-1

Af.o: Wawa Twp: Twp. 30 R 26Coordinji.j: L~0 3+40N

DtptS: 478' Diom.r.f. EX.

StorUd: 11/9/75 Com^.lpd: 1 6/9/75

Anomoly: Wa~2~4, 4'

Conlroctor;

D.jcrib.d by:P. Kennedy

Depth {(o.l) Lithology App.Dip. Mincrolixotion

o12 ..O

37.4

75.0

82.4

444.0

467.0

12.0

37.4

75.0

82.4

444.0

467.0

478.0

Casing

Metasediment: .GraywackeMetasediment: -Interbedded and laminated graphitic shales/ silt: stones and mudstonesMetasediment: GraywackeMetasediment: - Interbedded and thinly laminated black graphitic shales, siltstones and mudstones;

10"

C.N,

Sulphides:minor specks and cubes of I li Sulphides

Oxidesminor erratic thin magnetite bands are pre sent througho'. the black gra phite-rich sh ies

Metasediment: GraywackeMetasediment: Interbedded thinly laminated black graphitic! shales, siltstones and mudstones C.N

Note: Conductor is explained bygraphite-r ..eh zones throughout the hole. ' Magnetic anomaly explained by minor erratic thin magnetite bands.

S f2 o ^ ,.

v , t- -,i

DRILL RECORD.

AREA Wawa

ANOMALY: Wa-2-4

CLAIM:

Hole No. Wa-1

Bearing and Dip: 220 @ -45 5

Local Coord. X^r.-0

Depth: 478.0'

Started: 11/9/75

Completed: 16/9/75

Described By:Drilled By: UMEX

Machine: Longyear 24

Diam Drill: EX. P. Kennedy

1i;:^'; Depth

r 'From To

27.4

'5.0

811.4

75.0

82.4

144.0

Core

Description St Lithology Mineralization O.p

CasingMetasediment; Graywacke

The rock is fine-grained, grey, massive and is composed of detrital quartz and feldspar with minor chloritized mafics and carbonates. Locally, the rock is weakly banded (5 C.N.). Minor thin bands of interbedded and thinly laminated graphitic shale and siltstone occur in this section.

Sulphides - a few specks of py.Metast -Hment: Interbedded and thinly laminated graphitic shalesilts tones and mudstones.

This section if mainly composed of graphitic shale. The laminations vary in thickness from 0.2 mm. to 4mm, are white to grey to black, have a banded structure 10 C.N. and locally exhibit intrastratal flowage. Calcite occurs throughout the section in the form of streaks, patches and films along shearing and bedding planes.

Sulphides.:- minor specks and fine disseminations of py, po and minor cpy, sph.

Metasediment; GraywackeThis unit is similar to the above graywacke and has a weakobanding (5-10 C.N.)

Metasediment; Interbedded and thinly laminated graphitic shale,siltstones and mudstone

This section is almost entirely composed on black graphitic shale. Laminations vary in thickness from 0.2 mm. to 5 mm. and give a banded appearance (10 C.N.). Locally, intrastratal flowage structure is prominent. Numerous 3 cm,, 0.3 m. and l m. grey wacke dykes occur throughout the section. Calcite is presentUas - streaks, patches and oval blebs throughout the section.

Sulphides - minor specksy. cubes and fine disseminatio

magnetite is ^resent as ninor errati chin bands.

J.% Sulphides

nagnetite is ^resent as ninor erratic :hin bands

r

fc

D *ti*

1

Depth

From

444.0

4G7.0

To

67.0

78.0

- .

9iof

CoreDescription S Lithology

M3tasediment: GraywackeThe unit is fine-grained, gray, has a general spotty massive

appearance and is similar to "the graywacke described above (2.0'-37.4').

Metasediment: Interbedded and thinly laminated black graphiticshale, siltstone and mudstone.

The rocks .are fine-grained, whitish to gray to black and banded(5 -100C.N.). The graphite content is much lower in this sectionthan in the above graphitic zones.

Sulphides - odd specks

End of Hole

Note: Conductor is explained by graphitic-rich zonesthroughout the hole. Magnetic anomaly explainedby minor erratic thin magnetite bands.

Mineralization

-

Dip

1 1

cSor

l M*

U Wk Lt, X CORPORATION LIMITED

1035 LESLIE STREET

DON MILLS

SM-p A i ^

ir/-.---;.F"/-;:-

. .j -y--. :' if: l -^ • •- V

^v

ii- ^ s

...-. - ., ., :.1 ' ' , ' - ' - -\- . ; .- ! :- ' v: : -;V-:'-.!r-:,: ;.\..'-:.- . hfj--;-::^-;'.

\.-! l -. ..-..;.. ..' ;-i-: i : :y

- - - - - . - -. v - - .- . ^ -j ., . :..r-.. ' -.-:

. ; : ;: : : . - : .- ; -Vi".,;,.!,'-'i-'-..-.;- ;. ; - ".i-rr!|-i: :1--s-!-

•~^^ ' ' '

- - T -- . :.-..i .

v : .: 1 ; i ' ••-. ! ; •••••r.-. ' - - - 'i.-; ! ' '.'' H ; .j

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\ . ' . . :

:\ii, ::.:;/ '.: V,k,iM^•m/x.•::.\^/.-

- i .i . ;

...;, '--X^-';^;:.f : -:r;-r^-i-^fe:?a:r:^ :^:- ; T:;7.vhn:fKT ! 3.- -! - ;' : i :: 'T:| i!

' ' - 1 - ' . ". . - i ! 'O '.;. : ' -' l :.;.: ; i-',-:.''---'::^.-/•'.: j ' - - -.-•.'..-•:. :.'.-:v-. . ' 4-.A-..- ;-.- . v t ' - -r - - ' - L ' l ; . v • ...•.~1 i , . ,. , ,;.,/...,

^:-.ifwi te'^v-^:

m:rv.;

• !

i l..; .: -.

:- l -i - - ,- - I - : - .r; p .,-:. .j;-,.n,}/;:r -:-,-!.i..v-. l

- ;:i : ;;rvi-r!.iJ-;:. ; .U ,:-..,..... :-......... .- j.:.-..

•-•..;; '.-,;:-.-

T-rc * - ,Wfc- '"r"m.^:'-:- l .•Ji'*"':- -

'mw : #is--.;-:JcB; Anomaly l'?a-2-6

Introduction

The purpose of the ampping was to explain a 7-line conductor with a moderate magnetic association.

Location

The anomaly (fig. 5) is located in Township 30, Range 26, east of Big Marsh Lake, near the Magpie Mine Road.

Trenchr

An 18 foot trench located on BL-O, 6 15N has been opened during a previous exploration programme.

Disseminated pyrite occurs throughout and makes up 5-10% by volume of the siliceous banded magnetite formation which is striking .275 and dipping 70 .

The introduction of hydrothermal fluids causing strong silicification and some sericilization has probably been facilitated by shearing of the rock.

Conclusion and Recommendations

The magnetic association is probably due to the iron formation. The observed disseminated pyrite and the associated cilteration may indi cate a more important massive mineralization along the shear zone at depth causing the E.M. conductor.

The exposures in the trench have been sampled (no. 09 05) and shoulc be assayed for base metals. If positive (anomalous) results are obtained, the conductor should be drilled.

DEC 11 1979

RESIDENT GEOLOGISTSTE. MARIE

SSM-2044

i i * B r- v - ^UMEX ,AREA

ANOMALY No. ^O.2~6

•"s, 'i.f-' cW iy , * \ I r . i

)istrict and Province

Party s H v~ Dates ofA? ' ' J ̂ 4

^cation details S 7^ /

lo AZCsS'

Topography 5" /i-. * X/ A i f' * Overburden . O ~ 7

^Syri' w 1LTimber ____-..y.... ..,. , ^.Accessibility 7-QOO t^A/A

Water Supply JTW^^, .T* /*?c;(? ^. /..i J r ? opt.

ft.

iption and7. 3*-,^/'*

. 7. * a ••i"' f

Thin Sections.

Assay.

lepresentative Type

o! i age

upervision Remarks

j 7 x; ruL. M-^/m^/c. a ft?c t*-/-!t

'•-•'t'// n

X ^^^c^-f^S . J2 ~f-re^{Ar.

PROGRESSION OF WORKS

Tilling WORK DONE

c /i-wrDATE SIGNATURE

/J

REMARKS

GENERAL GEOLOGY

ECONOMIC VALUE

GEOPHYSICS___Conductor appears to be brokenup by N-S faulting /____

———————————forming an—"on echelon" pattern-?——The -faot that -the———

———————————vcrticoL-loep-f ixcd Tx method worked ouggoobs-that wo————————————arc dealing-with- one conductor -br-okon up i—r-at-hor- than—

———————————oovoral oopogato -lonoooi—Conti-nuity would -bo- provided-———————————through-and-Qlon^ faulto botwoon pioooc.—The magnotio-

CONCLUSIONSsupport this interpreation also. magnofeio oorolation.——————————

Medium to strong

The tronohoc chould bo camplod.

Signature

January 2, 1975 Date

Remarkstncral Geology

y* 2-

conomic

UOKj'jfophysical b* b+uL-f*- i .,' L b- M - S'

_ l Jr •f ^^ij^ y ^r M-*-^ V^aV ^ r ,?.———— —— ——— —^ ^ *—————————————i-

f• '•'f-.

//y,.

f \* j t s //y -j 1 ,VO V V- j-....

rf f t-i','U w , -/ to

onclusions

T..

j S, f7 LV-*-

_____________•'•:- ^ y^J______ Date

lil.: (1) In remarks re timber, wnu-r supply and accessibility the data required for planning a drilling program should be kept in m i r.

(2) Submit a map of the area .showing traverse route, outcrops, strikes, dips, glacation, location of samples, etc. Sample's number should be prefixed with the anomaly number.

2044 - I

UMEX CORPORATION LTD.

WS Loli-Stre.t, -"

Dan Mills, Ontario, Conodo.

Hoi .No: W a-2

Aroo: V7awa Twps Twp. 30 R26 Coordinot.*:L-8N 2+60E

295. O 1 Diom.t.,: EX.

12/9/75 Compl.ud: 15/9/75

SS..tNo: 2 Anomaly:

An 9U: ~450W

Controcter; UmSX

by: P. Kennedy

D.pt'n ((-.t) Lithology App.Dip. Minvroli lotion

. O

6.0

108.5

6.0

108.5

295.0

Casing

Metasediment: Interbedded and thinly laminated black graphitic shales, siltstones and mudstones

'6.0'-64.5' predominantly, siltstones, mudstones

and graywackes64.5'-92.5' predominantly black

. graphitic shales andsiltstones.

92.5'-108.5 predominantly . grayvackes and siltstones

Metagabbro carrying finely dis seminated magnetite.

Note: Conductor explained by graphitic '/.one @ 64.5- 92.5'.Magnetics expDained by finely disseminated magnetite Q lOb',5'-295.0

Sulphides: odd specks o PY, PO, CPY

From ToDescription Si Lithology

Casing

Metasediment: This section is composed of interbedded and thinly laminated siltstone, black graphitic shale, mudstone and weakly b nded to massive greywacke. The laminations vary in thickness from 0.2 mm. to 4 mm, are light grey to green to black, form a banded structure (50C.N.) and locally exhibit intrastratal flowage Minor bands or pinkish-white to creamy-gray cryptocrystalline quartz and white carbonate patches, streaks and films, are present throughout the section. The graywacke occur as minor bands (7cm to 3 m. in thickness) is light gray, fine-grained, has a subcon- choidal fracture, is composed mainly cf detrital quartz and felds par with minor argillitic fragments and locally, exhibits weak banding and graded bedding.

6.O '-64.5' predominantly siltstone, mudstone and graywacke 64.5'-92.5' predominantly black graphitic shale and

siltstone. 92.5'-108.5' predominantly graywacke and siltstone.

Sulphides - odd specks of oy, po, cpy

Me tag abb rp: The rock is fine-grained, composed of GO'S mafics and 401 feldspar, has a ophitic texture and carries finely dissemina ted magnetite throughout.

Sulphides - -a few specks po, cpy@ 174' thin massive sulphide stringer @35 C.N. in a highly chloritic matrix

End of HoleNote: Conductor is explained by graphitic shales from 64.5'-92.5'

Magnetic anomaly^explaine^by finely disseminated magnetite

Mineralization

Sulphides-95

Dip

\ po

'* *-V***J*c. -r. * -*^.-3(-^^-*

-•Sttf*nr,Sft'K* ,t*ti*Mii"mtranttvntninva*,f, lif,,i.i, tfl n'*'m**{r *"~t— •••••" - - ———— - ——————————————— — - -- '

LJ M EX CORPORATION

1933 LESLIE STREET DON MILLS

SAMPLE No.

0.9/89

LOCATION ,

7fe.o - 8/f.o

-

r

.

LIMITED

n... S-p. 22,75-

OESCRIPTION

DDW (Ja- 2

,

1

SSM" 9 Av

ASSAY FOR

^C*

O.Oi

-4-J•*L n)]

%-Zn

O.oz

inTr

or/t A3.

Mil

-

-

—

UMEXwlAREA WAWA -

ANOMALY No. U/A 2" 7

i and Province CXnW\\O

.fojs.KA.v7 . ..."DrnrhrovicV) Dates of Examination

Hiistants

ion details \jWys-J7

ccgraphy Overburden O"- poplar Water Supply

feasibility

roles Collected

bisections ———

Description and Location.

)™sentative Type

ision Remarks

cphysical Tb

t 'C3v . Ma^.c rov.-(o.\;ulcrvvA 1 c.sJ b^-

di L.Q

c

PROGRESSION OF WORKS

WORK DONE

Mo.

DATE SIGNATURE,i

St 7r

UMEX

til/ict and Province

:y Leader JU^d

Assistants . T-

JMtion details

fr

AREA

ANOMALY No.

Dates of Examination , . aq.-* horacwW

Tography tt"! vW

,r.,cihilify W l 000 3vvc* -fi

Overhurrfftn S B|

Water Rnnply lOOO ' M

K

rples Collected . mDpsnription anH 1 nratinn IP

Bf fi"''I

™* 1B^-

cresentative Type , . . .... . .. , 1i"age

envision Remarks .

'.physical

mg 2cci. x- ^ 4fJ-^PROGRESSION OF WORKS

WORK DONE DATE

vj-r 2 r c'-.tj. XJL Z.

Wawa 2 - 7AREMARKS

GENERAL GEOLOGY

ECONOMIC VALUE

GEOPHYSICS T^e response on line 4W is too narrow on the horizontal loop survey to accurately register the conductor. (Response should be = cable length - conductor width, at the background level) It is likely that we are dealing with a short conductor falling between lines O and 4W.

CONCLUSIONS if this conductor is to be drilled then it should be

between lines O and 4W.__^_______^^__^_^^_^^__^_^^^^^_______^____^____.

Signature

February 2 , 1 975. Date

seral Geology J

^' ;?'i^W^'' -' f'-r*-;:. '';?lA: V*'-^..';if':;,''' -" Remarks''' ••'.^•^•••: -- —— ~ o -7 y.2- 7/4

anomc

•xophysical ^L O"*- 7 tJ

/ u.:*w(.. j -/

)y

o

Conclusions

O.. ,V .r/. ;.. '.

VOTE: (1) In remarks re limber, water supply and accessibility the data required for planning a drilling program should be kept in n

(2) Submit a map of the area showing traverse route, outcrops, strikes, dips, glacation, location of samples, etc. Sample's number should be prefixed with the anomaly number.

Discussion of Anomalies V'a-2-7 and Wa-2-7a !

Anomalies Wa-2-7 and Wa-2-7a (fig. 7) are located in Township 30, Range 26, some 6 kilometers east of highway i? 17 along the Magpie Road. Mapping revealed that the area is underlain by mafic meta- volcanics, tuffs and lapilli tuffs, and metasocliments. A mafic intrusive with d orj.te and gabbro phases trends north-south and cuts these units. The mafic metabasalt is silicified in places generally close to the mafic intrusive. However, this could be a contact metamorphic affect.

Pyrite and pyrrhotite are present in trace amounts in most of the units, but anomalous amounts v/ere not seen.

Conclusions '

Anomaly Wa-2-7 is located in a low swampy area. The conductor transects the metasediment, metavolcanic, and mafic intrusive units and could be interpreted as a fault.

Anomaly Wa-3-7a lies again within all those units, however out crop was not found along the conductor.

It is recommended that both conductors be drilled to determine the exact nature of the conductive material. It is conceivable that sulphides could be concentrated along the contact of the mafic intrusive.

The recommended drill hole is located on line 2 west, l north at -45 , be:aring

044

l 1735L.*li.

, Dan Mill*, Ontario, Conodo.

j

Hoi. No: Wa-4

Af.o; Wawa Twp: Twp. 30 R 26Coofdinol.*: L-3+20W 3+-10N

Dapth: 524.0' Diom.ter: EX.

S.ort.d: 16/9/75 Compl.f.d: 22/9/75

Anomaly:

Controctor:

ky : p. Kennedy

D.pth {f**t)

'o 4.0

. 4.0 66.0

66.0 219.7

219.7 260.0

j 260.0 286.0

! 286.0 524.0i

-

Lithology

Casingr

Mafic intrusive: magnetite bea ring metagabbro

Metavolcanic: basalt Minor sections are brecciated

Metasediments: interbedded graphitic shale, siltstone, mudstone and thin magnetite bands

Metasedimenu: argillite

Metavolcanics: basalt

End of Hole

Note: Conductor and magnetic anomaly explained by graphitic shale, magnetite and minor po, py.

.

S SM-

App.Oip.

5-10 0C.N.

5-100 C.N.

S 0"

C.N.

5-150C.N.

? 0

M'ncroliiotlon

•li nor specks po,cpy-linor specks po

IS po, py '

lv.2% po, py

Minor po, cpyt

*

44 '

'AREA Wawa Hole No. Wa-4ANOMALY: Wa-2-7, 7a3earing and Dip: . 200

CLAIM: Local Coord.

Depth

From

4.0

66.0

219.7 l

260.0

219.7

Tor:. i-.-:

4.0 G6.0

260.0

?86.0

Core

W

Depth: 524'

Started: 16/9/75

Completed: 22/9/75

Described By:Drilled By: Umex

Machine: Longyear 24

Diom Drill: Ex . p. Kennedy

Description Si Lithology

Mafic intrusive: MetagabbroThe rock is fine-grained, composed of amphibole,and plagio

clase feldspar and has a greenish-white salt fi pepper massive appearance. Finely disseminated magnetite is present throughout the section.

Sulphides: minor specks of po.Metavolcanic: Metabasalts . -

The rock is fine-grained, light to dark greenish-grey, banded and schistosed 5 - 10 C.N. Minor thin brecciated zones comprised of greenish-grey ellipsidal fragments in a greyish- white matrix are present.

90.O'-107.6' Metasediment: greywackes.The unit is fine grained, light-dark gray faintly schistosed 5 C.N. in sections and is composed of biotite-hornblende-guartz and feldspar. Lower contact is 5-10o C.N.

Sulphides - specks of po, py minor cpy.

Metasediment: Interbedded graphitic shale, siltstone, mudstone and thin magnetite bands. The unit is fine grained, light-dark gray, banded 5-10 C.N. and contains patches and concordant stringers of py minor po. Upper contact is O C.N.

Sulphides: py minor po ( li Sulphides)Metasediment: Argillite

The unit is fine grained, greenish-grey, lighty banded and schistosed 5 C.N. Minor section are brecciated and some contain highly chloritized mafics with subordinate biotite.

@ 280' thin graphitic shale.

Mineralization Dip

Description 8c Lithology

Sulphides: po, py are present as fine disseminations and patches X-2% Sulphides.

Metavolcanic: Basalti i-

schistosed 5 -15 C.N. in sections.The rock is fine-grained, greyish-green , faintly banded and

Numerous sections are brecciate

Miner Jtizatlon Dip

1and chloritized. Minor bands consisting of biotite-chlorite-quartz feldspar occur and are considered to be metasediments. Zones high in chloritized mafics and biotite are considered to be ultra-basic in composition. Upper contact assumed to be 5 C.N.

286.O'-306.0* Transition Zone

Sulphides - minor specks po, py minor cpy.

End of Hole

Note: Conductor and magnetic anomaly explained by graphitic shale, magnetite and minor po, py.

i i*l

Sal fer

U lV/ tl X CORPORATION LIMITED 1033 L ESLIE S TREET DON MILLS

091^0 2.1)5.0 -

g5?.5 - 255.0

09192 Z9Q.O - 295-0

O9/93 3 85.0 -368.0

^•lOsiriJi E-HtS

~rt ' "'.i..' . . -. i- .-f-'-- -I-- - --

—: . y.4444;: :.LL: J±ti

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