DIAMOND DF? ILL i MG 42A12NE0518 42 MACDIARMID
010
TOWNSHIP! Macdiarmid REPORT No,: 42
WORK PERFORMED BY: Norcen Energy Resources Ltd.
CLAIM No, HOLE No, FOOTAGE DATE NOTE
P 536908 TP-81-3 TP-81-2
566.0 184.1 m
July/81 June/81
(D (2)
NOTES: (1) 422-81 (2) 19-82
l F l f l p
*ji z oiesr-aois 5??o?o,5?i
u\ j
.1P , f P P
.J—..-.4___L,,,-4,-__-? M ''
•IP l p.-J-.-...
M.
B l c' ? 8
ON TWP - M.288
Moreen DIAMOND DRILL RECORDHotoMo TP-81-3
Hole No Property Township Location
Logged By .Core Location
TP - ffi - 3Mac south Groupwacaiarmid r OntarioGrid 650 W/ 200 N
L.A.BaldwinTimmins warehouse
Length 172.5 met Z fstfJj*- .
Beanng Az . 050DID - 55"Obfpctrve TO test MaxMi n
conductor 'A'
r ———— July 13,1981rompte,*d July 21.1981rv,rr,rv,r.o Bradley Bros. Ltd.
D^"\Ow* S'"1 Ji^
Cae-nr, 1 .ft .n MnU. 30 ft. BW
60 ft. Nw
Remarks
MetresFrom
'. 0To
53.0T TftfOTjjj.J.riUijOGY AND ALTERATION
BRECCIATED PILLOW BASALTBrecciated massive fine qrained to localy medium arained, buff coloured^ stronly altered by carbonate (probably dolo mitic) ; gritty, moderately hard; severalauartz-carbonate strinoers and veins to1 cm. ; characterized by intense cracklebrecciation with dark hard siliceous ancarbonaceous matrix as irregular swirlvstreaks and stringers and as matrix toirregular fragments; also several narrowzones of interpillow hyaloclastite withsmall angular fraoment-s IPSS t-han 5 cm.
riarlr ma-f-ri v - commnn -f-Vi-infinely variolitic* s^lvag^s; locallycommon qnar-t-^-car^onat^ amygrfnl e -(-o
after73.8:sl]Lghtly more uniformly mas-sive with sections of black matrix and/or hyaloclastite up to 60 cm. and lesspronounced crackle brecciation.
Dip
Etc
Collar - 55
NTest Depth Rog True106.7 m 62. 30 54OT *T *"* C ~* /"T CO C172.5 I" 61 S2-5
MINERALIZATION AND STRUCTURE
Less than 1?; pyrite as recry.- tallized clots in and ad-iaceT- to matrix material.
Several rusty fractures to65.5, common hemaritic slipsalong fragment margins.Matrix non-conductive but
j occasional graphitic slipsare locally weakly conductiv
.. -
after 77. 7: generally more abundantqiiartz- (carbonate) veins and stringers Jmostly in interpillow material. . ..88.2 - 88.6,90.1 - 90.6, and 99.9 -100.4:hvaloclastites with black matrix.
at 9 3. 4: several flecks browrsphalerite in local quartz-carbonate- (chlorite) patchy
- vein along pillow selvage.
Sample No
i —ffit
;.
From To Leogth
l.
1
J 1
i i' ; t
.™ ————— , ———— , ^i- —————— i —————— .
H
Location Sketch
)
3) S
l
i.
cu
NormtScale 1-1320'
1
1
,/^ v
/-7 'x*"' /IjL -— 43Z--
S7 /?
M(^Tj-
7/4
//JWA. ^— — -/ i
"pn—^—~
Norcen DIAMOND DRILL RECORD HoteNo TP-81-3
2
MetresFrom
53.0
To
137.2
J - ~^m-
^^ :
JjJL L fl\JLi\J\y3, AINI/ Alj^CtKjni J-v/IN
after 94.5:vaquely more common quartz-1 carbonate amygdules , f ine to irregularup to 5 mm. ; occasionally dark carbona ceous "i Py where cut by crackle frac tures.100.7 - 105. 5: slightly greyer massivesection, locally medium grained, withlittle brecciation and no interstitialmaterial; generally larger amygdules(including pipe amygdules) to about 102.and finer ones near lower selvage a large pillow or tube with narrow sel vages, indicates tops uphole (ie. , south)after 114.3:more obvious thin selvagedpillows from 15 cm. to several metreswith finely variolitic selvages; a de crease in carbonaceous interstitialmaterial, crenerallv more areen chloritecarbonate and rock has more fizz carbo nate.126.5 - 126.9 : carbonate bleaching arouramyadulesat 128.0: local stronq brecciation withseveral quartz carbonate veins over 15cm. .128.0 - 131.9:rock abruptly qreener.more chloritic and increasingly hardsiliceous or epidotic but still carbo nated a hornfels.at 129. 8 :a soft chloritic pillow inter stice.
MAFIC DYKEFine chilled to medium grained, darkgreen with pervasive carbonatizationand common chlorite-carbonate veinsand stringers.
MINERALIZATION AND STRUCTURE
to 102. 7: pipe amygdules flatto core axis .
7
at 109.0: graphitic slip incarbonaceous material, locallyconductive .118.0 - 121.0:one pillow withabundant amyqdules near uphol
-selvaqe to 2 cm. and relatively few near lower indicatetops uphole.
dat 119. 8: several flecks chalc(pyrite in quartz-carbonatestringer.
.
at 129. 8: locally "2-33 Py cube
Minor but common Py cubesin cnlorite-carbonate string ers.Upper contact chilled, irre gular at 2007C.A.Lower contact chilled butground .
Sample No. From To Length
J/
X//ts ' te.
/i /~c/yx/^X^zjb—iP*
7jf ' f-"5 f C.
s//J,G k/yt-*i
Norcen DIAMOND DRILL RECORD TP-81-3Sheet No
MetresFrom
.137.2
155.8
rm
To155.8
161.9
LITHOLOGY AND ALTERATION
ALTERED BASALTAs above, buff, strongly carbonated,massive with relatively less cracklingand generally chloritic and sometimesdark carbonaceous stringers; lesscommonly developed pillow selvages withchloritic interstices; sericitic inplace s; common fine carbonate grains andcarbonate wisps and stringers.at 140. 2: pipe amygdules near a selvage
143.7 - 144. 0 : chloritic shear over 5 cm
MINERALIZATION AND STRUCTURE
at 14 0.2: pipe amygdules flatto C. A.
. 143.7 - 144.0:shear at 20^/Cwith auartz-carbonate veinincr and 1brecciation; waxy to hard buff sericiticor soidotic fragmpn-hs. jat 146.0:5 cm. pillow interstice with 1 at 146. 0 :locally 2-^ Py cubedense moderately hard chlorite-strong land clots; locally moderatelycarbonate carbonaceous material, weaklygraphitic.146.6 - 146. 9: similar to 146.0; someoxidation on f ractures;weakly graphitic
146.9 - 148.1:patchily slightly darkergreyish-buff with increasing carbonateand some chlorite; several dark carbonaceous carbonate stringers and veins.
CHLORITIC TUFF AND SEDIMENTAbrupt from flow rocks above; an inter flow unit of predominantly finely lami nated chloritic and pervasively moderatly to strongly carbonated tuff and/orsediment ; topped by narrow section ofgraphitic sediment; passes downward intbasaltic fragmental and flow rock over all gradation and grading in some bedssucraest tops uohole (ie. .south) .
conductive .
146.6 - 146. 9: locally 3-5% Py.cubes to 1 cm. and clots;interstice 20-25 /GA but schistositv flat to CA? locallyweakly conductive.
-.
UDDer contact sharp fsliqh-Myground) at about I^/PA.
3
Sample No.
2211
-
From
146.
To
146.
Length
0.9
ppm Cu
ppm Zn
opm Ag
//S
JS 1
opb Au
' /^VX/f f fs
,, J•z-X/t
f
JfJ/ Vf'/ ffjAsfft/."9/^
s
/'s fSZf~#~7l
J
Norcen DIAMOND DRILL RECORD TP-81-3Sheet No.
MetresFrom
161.9
9 -* ^^^n
To
169.3
LITHOLOGY AND ALTERATION
155.8 -156.1:araphitic sediment .s treak-ily laminated with quartz-carbonate;slumped with several fraoments of basalcommon graphitic slips.
156.1 - 156. 4 : streaky chloritic tuffwith streaks and patches of chertysiliceous material.156.4 - 160.3: finely laminated chlori tic sediment or tuff; grading indicatestops uphole; beds thicken downhole;common convoluted slumping of beds.after 160.3: gradationally vaguelyfragmental with streakv basalt fragmentin carbonate-chlorite tuff matrix.
ALTERED BASALTAbrupt gradation through a few raggedgreyish-buff basalt fragments to 8 cm.into buff flow similar to above units;variably carbonated; massive to streakywith local thin selvages, in^placesvaguely fragmental with siliceouspatches and locally abundant chlorite-carbonate carbonaceous material ;variablquartz-carbonate amygdular, especiallynear selvages; unit of pillows to pillowbreccia.at 16 3. 4: local 10 cm. patch of irregu larly laminated carbonaceous materialafter 166.1: rock greyer, increasinglyhard, siliceous and relatively weaklycarbonated; amygdules have bleached rim168.5 - 16 8. 8: local interpillow hyalo clastite with steaky buff and whitesiliceous angular fragments in chlorite-carbonate matrix.
MINERALIZATION AND STRUCTURE
355 R - Tifi. l- locally S-8% PvulUtti , tTtrBa'Srs , and scattered
. cubes; one semimassive bandof cubes to 1 cm. ; schistositat 15 /CA. ; strong conductor.after 156.1: less than 11 Pycubes and clots
Bedding and schistositv at10-25wXr:A-
j
Minor Py
f
7
at 163. 4: locally 2-3% Py clotsand disseminations.
V
Sample No.
22l2
2213
2214
2215
From
155.
156.
157.
159.
To
156.
157.
159.
160.
Length
0.3
1.6
1.4
1.4
Cuppm
Znppm
Ag ppm
X
f '
"t
Au ppb
f /jy//^rvffi*' f '/S*/LZ^-—— —
X/fix
/r ,XA0//is^™ -^
?/^/
'
Norcen DIAMOND DRILL RECORD HetelMo TP-81-3
Sheet No..
MetresFrom169. 3
171.6
172.5
— m -
ToiVi.6
172.5
LITHOLOGY AND ALTERATION
BASALT HYALOCLASTITESimilar to 168.5 - 168.8; Streaky variably silicified basalt shards to 3 cm.in ragged matrix of finer fragments andchlorite-carbonate; several hard carbo nated buff basalt fragments to 10 cm. patchy silicification and ragged quartzcarbonate veiningi in places; one platyfragment of bedded chlorite-carbonatetuff with fine Py; an interpillowbreccia.
ALTERED BASALTMassive, buff, weakly carbonated,, vari ably siliceous t as for units above
EOH
————————————————————— -
MINERALIZATION AND STRUCTURE
Minor Py-
.
Sample No. From To Length
)/A
/d,//Wt ——————— ^
—2^
/7 -l^/7^'^Z&ky j.7 Q 7
/} /^2/r. rW
^3 —— — -— -
Loon77^-87 -3
: 25-00
Dff TP-Q l-3
n
Tl'l l ll l l
1322013 |3220W 1522015
52201J |32IQlt 1322070 132202?
MAC SOUTH GRCXJP MocDiarmid Township
Seal* : 1 H * 1/2 Mil*
MoreenDIAMOND DRILL RECORD
Hole NO.TP-81-2
.W,. NO. -L -t- 01-^
-.,,P,Mtv Mac North Group'mV'V.hlp
L"r,-ltifin
Macdiarmid Twp.Grid 188W/0+52N
(PEM line 25QW/04-90N)i.^-yicdOv L. A. BaldwinCo-0 1 ncniion Timmins Warehouse
p'-mnrks MaxMin grid oriented
184.1 Metres - , .. i nn-,Lonalh . .... Commr-ncpd June 15. 1981Bonrinq 22 2 0 Oomniotod June 23, 1981Dtp -58 0 ... ..... . .. . DriiiinaCo. Bradley Bros. Ltd.Objective tO tSSt MaxMin CoreSizp BO
conductor "A", also Casing 1 eft in Hole 4 0 ft. NWdefined by PEM 40 ft. BW
j
north-south; PEM lines cut at azimuth of 42 0
Metresfrom
(1
4 3 . 9
To
43.9
53.6
i
^L^p
L i f li o 1 o g y and Alteration
CASING
BASALT FLOWS:Mostly massive, light green,commonly variolitic, variablycarbonated; moderately hard,variably chloritic; likely apillowed unit; weakly amygdular(chlorite) ;brecciation
some cracklewith chlorite-
carbonate stringers; commonquartz - carbonate veinlets andstreaks .
at 48.8 and 49. 1-51. 2:strongly chloritic with abundantquartz-carbonate veining (30-504
51.7-52. 7: streaky flow laminate
53.^-53.6: open vuggy rustyqnnr-f-T: rrsrhon/ifn VP i n .
Dip: Collar -58 0
Etch Tesl Depth
44. 5 irRdg. True
i. 63^5" 55. 5 0108.5 m. 65. 5 0 58 0184.1 m. 59. 5 0 51 0
Mineralization and Structure
Minor Py in interstitial material ansmears on chloritic slips
at 52.7: local patch of vuggy Py inintertice.
-~
)
d
/' /l ,/) s////2 f /, \f/nrJ swffl wWSv^——l/ n /J^4^^j^^-v SZ^~--~~^
Sample No.
d
FrO'Ti
,
To Length
Location Stetch
TP-8/-1 (i
7No
1
Clairr
Scaie
/
rth
NoP 5369Q. r- .1320'
DIAMOND DRILL RECORD Hole No. TP- 81- 2 Sheet No. 2____—
M r:i ? vr^ c;' 'om TO
o i - b b 5 . b
v ' . b j 6 . 4
b b . 4
5 /' . 0
LI 0 . !J
57.6
Li 8 . 9
TT4 .5
- - - —— -
w
Lithology and Alteration
BASALT FRAGMENTALPredominantly green to buffragged to angular fragments ofbasalt in dark chlorite-ca'rbonate matrix; largerfVaaments UD to 10 cm.
MASSIVE (3 AS A f, TMa s s i ve, we a 1 y s i l i c i L i ed ( ? ) ;"Brecciated with common chloritecarbonate material
QUARTZ-CARBONATE VEINStreaky to massive with chloritand common rusty open Lracturcs
KOMATII'J'EGreen chloritic massive withmedium-grained spinifex texturecommon chloritic wisps; linergrained, more equigranular nearcontacts - probably a dyke.
BASALTMostly massive and stroakiiybrecciated with abundant dark"chlorite-carbonate clots, streakand patches; common fracturesand slips with carbonatestringers .
b X . 3 — b 2 . 5 and b 3 . i — b 4 . ^ :Strong shearing, gritty chloritwith ground and broken core(ground about 30 cm.)
Mineralization and Structure
i-2% Py dots in chloritic matrix
at 55.3: several flecks Pyrrhotite(Po) in amygdules within a largefragment.
No. From
1
To Lenglh
1!
2-3?;. fine Po disseminations in rockand 1-33 Py dots in chloritic
~V .breccia matrix ..........
p*w
Minor Py flecks
-
3 r
Le
1 /J
7 j/l^frffiv jf/f/r&lf /fi l^/lL^Lq/^l^Jr^-
1
...... ....
'f
DIAMOND DRILL RECORD Hole No. TP-81-2
Sheet No. 3_____
ri G t
r'rom
b '" . b
83.8
res1 To
y j . 8
85.6
KOMATIITE 1'LoW^Massive and streakily brecciatcsimilar T:o basalts but slightlysofter and abundant carbonate-chlonte wisps, clots, andstringers; local spinifexf'OV^ilt'-O' r^f\ri-f-r)r"*-f- v~i~*Trj*--iy"\i-x*-* -i ^-/--i
' 0 ot" J~vague, entire section may be afairly magnesian basalt.
64.6-6b.4 and b7. 1-68.1: stronc" sericite - (chlorite) shearingwith some quartz veinina andabundant around and. .brokencore (overall about 1.5 maround core) .
....at 68.1: spinifex blades inlocal fragmental
at 80.8: 8 cm. patch of chloritcarbonate material
after 81.7: vague to definitespinifex in breccia fragments.
FLOW TOP BRECCIA (?)Common ragged patches andfragments of basalt and blackcarbonaceous -carbonate materialabundant streaky and pervasivecarbonate; locally variolitic.
Minor Pyd,
-~
3 -
Upper contact sharp at about 50 0 7CA;lower vaaue and gradational - tops .uphole Ci. e., north)
1?; Pv dots.
-
J J S7 , s7 //f7*-s7S~i*j f /f sf' /l' J\jffl i^j^^^
/' i licl?--— ——
SamoleNo. Frorn To Length
'*
MwcenDIAMOND DRILL RECORD Hole No.
TP-81-2
Sheet No. ..JL
Mef rom
85.6
y j. 3
-9.6.-.3
t re sTo
95.3
96. b
-.J..0..4.,.2^.
BASALTMostly massive with localstreaky fragmental; likelypillowed.
85.6-88.7: soft chloritic withabundant cai ouna Le— quar L zveining and streaks pluspervasive carbonate; generallyvaguely fragmental.
88". 7-95.3: mostly massive,mottled dark and lighter green(patchy carbonate zation and soresilicification}; locallyvariolitic; some quartz-carBohcdots and streaks.
GRAPHITIC SEDIMENTBlack massive LO "finelyItiminated hard siliceous tographitic; abundant wliil'equartz-carbonate ' stringers andcrackling; strong pervasivecarbonate; a fewchloriticpatches.
KOMATIITE FLOWCommon fine spinifex texture invariably carbonated, slightlyharder unit.
96.5-98.8: vaguely fragmentalwith streaks and patches of blacarbona ceous-carbonate materiaa flow top?
Sharp lower contact at about bO"XCA.
--
te ——————————— : ————————————————
1-3?; Pv concretions and wisps
Strong .conductor
Schistosity at about 45 0 7CA.
Minor Py at . top., of unit.
ck1;
y /i ^ ^/ /^fyjfc}^ fl jfS *i //^/^/j/ffiffs&Mffite?----
(S
SamptoNo
2421
From
;
95.3
To
96.5
Lenath
1.2
Currm
163
ZnPpm
190
ACT"yPpm
0.2
AnPpfr'
30
DIAMOND DRILL RECORD Hot* No. TP-81-2 Sheet No. J?——————
i! -'fom
.1 i 1 4 . 9
-
e LI- e s " T^
122.9
b. . . ..
L i f h o 1 o g y o n d Alteration
9 .8^.8 -JL (13 , Q.:^iuo.s.tl;v^jn.a5.s.i:v..eJnoor.Ly.. carbonated., .fine sp in i f ctexture .
. 10 3..J3 -J- 03. .9: aradational sectico!; streaky alteration witheh J. or it:1 c wisp s in strong whitecarbon a t i z a t i o n ; a s s o e i a t e ciwith shearing and some quartz-carbonate vein ing.
103.9-104.9: mostly massive,.some quartz-carbonate veining.
PILLOWED TO MASSIVE KOMATIITEMostly massive with narrowsections of variclites andcjuartz-carbonate amygdules;lighter green; very fine grainccommon spinifex.
107.4-108.5: fine spinifexfexture.
at 110.2: 15 cm. quartz-car bonate-chTor i te veining.
110.2-119.5: mostly massive,less obviously pillowed; slightcoarser grained and Tiarcier;ge rierally pervasively carbonatcommon streaky pate ties ol quartcarbonate- (chlorite) veining —pillow Interstices (r'); commonline spinifex texture, sometimeetched by dark chlorite ingroundmass .
Mineralization and Structure
X
n
- -
.
d;
108.5-109.1: vuggy open shear.
iyed;z-
.S
7 4 S* sy /s,//!^? f jf "////^/j/fctf^jj/M/ZZ?-- —y ' t^-~— -— - — —~~^
Sample No. From To Length
f
rcenDIAMOND DRILL RECORD Hole NnTP-81-2
Sheel No. ^-—-——
Metresf r O'T?
— _
TO
li
.'.22.?
. .. ........
•"T -S';T
—— T35T^
J. 46.2
lji
" njpF
Litholoqy and Alteration
119. 5-122. y: spiniiex lessevident; mostly massive,mcdium-arained with quartz-carbonate ve in ing and streakychlorite in pillow intersticessome sections are baruer,s i ! ic.i J: 7. o d .
a rt e r T21 . 0": "SeVeraJr patchcB^J1 black carbonaceous-carbonatematerial in pi 1 lev/ inc'-j rsticie
MAbSIVE BAo/vLT I O KuwnTII j. c,j-'Iassive, fine Lu lucct.L.ly
jncdiura and coarse grained,- 3c.v.ej:al..R^tc,h.e.s... aad veins of. ..grey-white quartz-carbonate
... (weaklv pillowed?).
123.1-123.7: coarse arained wi'green chloritic spots(amygdulcs?) .
at 128.3, 129.7 and 132.0-132."some local fine spin j, f ex.
MIXED ULTRAMAFIC TUFF TOFRAGMENTAL AND GRAPHITICSEDIMENTMostly streaky to schistosechlorite-carbonate withabundant white carbonate-quartstringers and veins and commonnarrow sections and. bands ofblack graphitic sediment withsulphides; variable pervasivecarbonate; unit is an interflovor flow top
Mineralization and Structure
--
r
at 1 22.9: Upper contact eh illed,possiblv an intrusive.
Minor Po flecks.
at 135.8: fairly sharp contact at45 VGA.
h
' :
Generally minor Py
135.8-136.2: locally 2-31 Pyolots.
137.6-137.9: locally 2 -8*Z Poclotsand concretions, minor Py; locallystrongly conductive and magnetic.
145.1-145.2: locally i-2% Po and Pyclots
at 145.7: a few Py dots
Schistosity at about 45" (-65")7CA.
Sample No. From To Lcncilh
ii
1
,
f/l/
A^/rffy*/i/ /,i^
s?'j*/.WJ*— — ' ———— ~
———— --
7,W/l*— — — -^*
f
•'
1
DIAMOND DRILL RECORD HoioNoTP-81-2
Sheet No..
rio t re sI rom
l. '1 ^ . 2
.1.1)8. 6
........
- . .
- i
To
168.6
' "I5"9T'2
-- -
|W
Lithology and Alteration
S I L1C I F J. KD BASALTSimilar to flows above, mostlymassive to streaky but generalharder with greyish siliceousmottling and abundant butts 1 1 i c c o u s s t r x n g e r s a n c i b a n d sHSNOC:I a i. co wi. i.ii quartz vej.iu-.ngsome l: .me pervasive carbonate;
" Locally" variolitic-;'" commonpatch'es of quarTTz-caroonatevcining witn breccia t i oil andc i i e r t y c t r e y c a \ . b o n ,. 1 1 e -sil 1 c amaterial in probable pillowi n. t e i s 1 1 c e s .
at J (-ifi. J: local chlot. tlc tut fw. L th quar tz-eai. boiiato veininy
MIXED CAKBUNACEuUS M7\TERIALAND CHLORITIC TUFFO L- J. O ciiv JL -L y JL dill J, .1 lcl L. L^H V O L, Ci u L- W - )
— b-lacP. hciiG bll-Tceotrs-ecrrfaongostto gj.apliitj-c jtfatcj-iaJ- passingciownwa r u. to SUI.CCJK^' an.^.i luoL-Liexstiorig ciiloJi.Lte cai. bOiici t;j Lull
with abundant quartz-carbonate...v^ininq......^....^.^. ..^..^ ,,...,...
Mineralization and Structyre
jyiinor Py
Y at 1 fi R.I: local ] 3 Po .fj.p.cks. and .....brown. SphaJLexidet staining in guartz-
- .carbonate veinina.
LlLvocr. .contact sharp at about 65 0 7CA
•- -
168.6-168.9: S-5% Po, minor Py wispsand laminations in carbonaceousmaterial.
168.9-189.2: a few clots Po (Py)
Schistosity at 65-70VCA.
Strongly conductive.
Upper contact sharp and slightlycherty; lower gradational - topsuphole (i.e., North).
j/d,/? ,7 S
/;W/^///^/vj/^r^rt
Sample No.
242;
iL-~-
From
168.6
TO
169. i
Lonath
0.6
CuPPm -
111
ZnPPm -
312
Agppm.
0.2
Auppb.
20
c
-? — —— ——
DIAMOND DRILL RECORD Hole No. ^ Sheet No.
TP-81-2
Me Lue sI mrn l T^
i r; o j jj7 - ^ j- . - - ... 1
] 7 1 . 7
.1. 7 2 . y
1 7 .5 . J.
iiTi^r
•4
l 7 2.8
J. 7 3 . 1
1 73.9
T/^75'
l
J L i t K o 1 o q y an ci Alteration
m '^'O A A T.1 T i"1 nvVT/r;' J-' iXjtlx.JuA.1 i \^ J V1 i\i.
_ Mas.si.ve . to brecciated,, vacmelyC/iilledj softer^ locally talco:slips; abundant chlorite-carbonate a 1 1 c r a t i o n a n d a u a r t :carbo.na.-i-c ve i n i ncr .
Mirteralizafion and Structure
e
S(T"plC
No. Fro'Ti
1
i 11-59. 2-.TV).8: :-:; Lroncrlv scb is Los-:!:w i t h q r o u n d c ore.
CARBONACEOUS TO GRAPHITICMATERIAL,Similar to above sections,black liarcl siliceous carbonacecto graphitic.
171 . 8-171 . 9 : white quartz-carbonate v^in.
FLOW TOP BRECCIAC Lasts oi. underlying basaltin a carbonaceous matrix withquartz-carbonate veining.
MASSIVE BASALTMassive to locally brecciatedwith quartz-carbonate veining;flow morphology suggests topsuphole (i.e., North).
GRAPH 1 T 1 C BRECC i ARagged to rounded fragments ofbasalt xn a matrix o t blackcarbonaceous material; somegraphite slips; some cherty gresiliceous laminations near topof unit.
Several larqe catches Po and som^ P\arains In quartz-carbonate material.
us Stronqly conductive; locally maqneti
1-3?; Po.
Strongly conductive, locally maqneti
1-2? Po concretions and Py clots andflecks in quartz-carbonate veinmaterial .
{
J s? -V s/ 5c^~? j*s
//^/^/^Zf^ffl/fy—— ,- — ....... —— . ————————————— - ——— . ————
2423
c .
c .
2424
*"ft
171.7
— —— -
173.9
————
To
1..7J2.. 8
174.8
—————— -—— !
Lcnqlh
t. ra
0.9
,. — —
CuPPT"
JL03
100
. ———
Zn— ppm
^2.6..^
460
————
————
Agrr^
0^2
nil
Au Ppfr'
20
nil
-j ———
•vt-4 DIAMOND DRILL RECORD Ho'e No.. Shoot No.
TP-81-2
rrnm
^ rM.b
IB -T .T"
ol;rosr TO —184.1
Lithology an d Alteration
SILICIFIED MASSIVE BASALT TOKOMATIITESimilar to un.i. l;s above (e.g.,1 4 b . 2 - 1 6 b . b ) , ma s s i ve , g r e y ,usually harder silicified withchlorite rlecking; con'in.ongquar tz-ei^rho"- 1 .te vein '..'in ,
132.0-lco.^: j.',.)Cai Ime spini-Lc
END OF H.ULE
Mineralization and Structure
X ...
• -
^~7 s? /*/ ' 4r^,^^if' Jt^-f. — . ——
No.
^k
From To Lonqlh
A
MAC NORTH GROUP MocDiormid Township
f. C o l c . l " s l/? Mi Ir
LOCATION SKETCH
DRILL HOLE TP-81-2
NDKCEN g\ERGY RESOURCES LIMITED
MAC NORTH GROUP
LOCATION OF
DRILL HOLE TP-81-2
SCALE: 1:2500
