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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
•i-! i^:^-- '- i" i i- i-: -"••r.-'.' r-!--V;;,J ' 1.- 1 '- , i.-f-.' - 1 ' - :: : ".i-- ;:r
\ . ' . . :
:\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-- - --
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