DIAMOND DRILLING29 PAYS PLAT LAKE
010
AREA: PAYS PLAT REPORT NO: 29
WORK PERFORMED FOR: MINNOVA INC.
RECORDED HOLDER: SAME AS ABOVE (x]
: OTHER
CLAIM NO.
TB 535914/TB 9361
TB 386767/TB 386768
TB 646433
HOLE NO.
WL-08
WL-26
' WL-43
FOOTAGE
694.6 M
1,458.0 M
438.0 M
DATE NOTE
OCT-NOV/83 (1)
JULY-SEPT/85 (1 )
JUNE/88 - (1)
NOTE: d ) #W9140.180, FILED OCT/91
New Gesic GridCORPORATION FALCONBRIDGE COPPER
2+42N 3+48 E DRILL HOLE RECORD : -i-'~X METRIC UNITS
... IMPERIAL UNITS
HOLE NUMBER GRID
WL-8 Old Gesic GridPROJECT CLAIM a j., J
PN 070 TB 53591,0 -
pints'COORDS
SURVEY COORDS.
PURPOSE
Test Gesic Horizon at 500 m vertical
L AT.
7+94S^pprox. on!' 7730N
(nuL uii bur
ACID TESTS
DEPTH ( m)
5
30
60
90
120
150
180
210
240
270
300
330
360
390420
CORRECTED ANGLE
88.5
88.0
87.5
87.0
86.5
85
84
83
81
79
78
77
76
7675
DEPTH ( m )
450
480
510
540
570
600
630
660
690
CORRECTED ANGLE
73
73
73
74 73?
72
71
70
69
69
DEP.
1 5+80Wt
10117EVtiy tU y i t u j
ELEV.
N/A
COLLAR f - -w /L~ S BRNG. l g() o 2 ( ^
DATE STARTED: Oct . 19/83 N/A i 9jn DATE COMPLETED: N QV . g/83
Multishot Data X-XtfW&tXf&ra
DEPTH ( HI )
20 2938 4756 6574 8392101no119128133142 151160 169178 187196 205214 223232 241250 259
AZIMUTH
219 240223 245227 227219 220219 229230 220219 225227 224224 223224 225225 224223 223220 224214 219
DIP
89 8989 88.588 8887.5 87.587.5 8787 86.58685 . 585 8585 8584.5 8483.5 8382 8281 8180 an
COLLARDIP -89 0
———————————————— ———————— ̂ p —————————— . HOLE FINAL SIZE B Q DEPTH 6 94i6 ^
CONTRACTOR: McKpight Diamond Drilling CORE STORAGE: Q leaver Lake CASING: BW
ROD LOG . PULSE EM SURVEY X COLLAR SURVEY MULTISHOT SURVEY x
MULTISHOT DATA
DEPTH ( m )
280
310
340
370
400
430
460
490
520
550
580
610
640
670. . 687
AZIMUTH
218
218
217
219
218
X 214 X
221
221
221 '
221
223
224
224
224224
DIP
80
78
76.5
76.5
74
75
74.5
74
74
73.5
73
72.5
72
70.570.5
HOLE NO.Printed by Wester PRINT
WL-8 ^ COGGEDsyW.Smith,R. Ramshaw,F.Sal in-
rROM TO
O to 4.2
4.2to13.0
13.0to19.9
ROCKTYPE
Casing
Gabbro
COLOUR
Grey green
Int. dyke Dark green
GRAIN SIZE
mg-cg
mg-fg
TEXTURE and STRUCTURE
Typical 'Zenmac Gabbro' feldspars
ANGLE TO CORE AXIS
70% amphibole
4.2-10.2:Massive to weakly foliated C 38-40 0equigranular gabbro
10.2-10.5: Well foliated @ strong chlorite altered dyke. Sharp contacts.
10.5-10.8:Badly broken ground.Some chloritic muddy faultgouge at 10.5
10.8-13.0:Same gabbro as that at 4.2to 10.2
13.0-17.0:mg-fg intermediate dyke
13.3-13.4:Qtz-carb vein hostingangular lmm-3cm fragmentsof int. dyke.5% iron carbonate.
13.4-13.7:Badly broken ground.Fault zone.
ALTERATION SULPHIDES REMARKS
Weak chl.alt. locally
Strong to pervasive chlorite alt.
SO-60% chl.alt.
20% qtz-carb veinina
10% qtz-carb veins
Weak chl.
Trace diss py.
Trace py From ;10.2 to 24.5:~ -~- a major structural zone hosting dykes and faults
Fault
Fault zone
HOLfc NO -——-
PuitwJ by WisliT PRINT
WL-8LOGGED BY . WKS
PROM ^ TO
19.9to22.0
22.0to24.5
24.5to167.3
ROCKTYPE
Feldsparphyricint. dyke
Int. dyke(gabbro?)-, y f . ^ ,- :
Gabbro- ' -*" 1
COLOUR
Darkgreenwithwhitespeckles
Darkgreen
Greygreen
GRAIN SIZE
Porphy ritic
f g -mg
mg-cg
TEXTURE and STRUCTURE
17.0-17.4:Section of mg-cg equigranulgabbro.Sharp contacts, lower @
17.6-17.7:Rounded fragments of mg-cg
gabbro in f g int. dyke
Massive feldspar phyricgabbro.15^ white subhedral feldspai
Massive, weakly feldsparphyric int. dyke.Could be finer phase ofgabbro.Upper contact irregular.Lower contact @
24.5- :Massive to weakly foliatedequigranular gabbro.
27.4-27.6:Brecciated zone in gabbro.2mm-4cm chloritic frags are set in a matrix of qtz-carb.
36.3-36.6,:Badly broken ground.Possible fault.
ANGLE TO CORE AXIS
ir
10 0
•s
14 0
Foliation60 0 @ 38.561 0@ 4358 0 (? 4660 0 (? 5340 0 (? 5648 0 @ 71.464 0 @ 82.5C A C O "1 Ol
52 0 @ 15656 0 @ 164.
ALTERATION
Unaltered
Unaltered
Weak chl. 10'^ locally20fo qtz-carb veins.Patchy granitization.2% leucoxenes
Strong to perv.chl .alt.
5
SULPHIDES
17.0-17.05:40% py over 0.1 m assoc.with qtz vein
Diss pyrite along fragmentboundaries.
Tr py.
Tr py.
Trace pyrite
REMARKS ^^
Xenolith of gabbro withinint. dyke.
Fault Breccia
Fault
HOLfc NOWL-8
LOGGED BV. WKS
tfO bv Misltf PRINT
PROM " TO
ROCKTYPE COLOUR
GRAIN SIZE TEXTURE and STRUCTURE
40.4-40.7: Same as above but contains talc-chl along fractures.
41.5-41.8: Badly broken ground.
57.1-57.3: Fg int dyke in gabbro. Sharp contacts, upper @
lower @
60.4-60.7: V.c.g. section of gabbro. Feldspars are up to lcm.
75.0-90.0: Gabbro gradationally becomes more mafic. Contains lcm blotches of amphibole.
-, r
^103.5-103.9:- Badly broken ground. Possible fault.
112.8-114.6: Fg section of mafic equigranular gabbro.
123.1-123.8: Massive feldspar phyric int. dyke. Sharp contacts, upper @
lower @
-141.7-142.8: L Badly broken ground. Fault zone.
ANGLE TO CORE AXIS
18 0 30 0
49046 0
ALTERATION
Strong talc chl alt.
Unaltered
Unaltered
25 0̂ chl. alt.
SULPHIDES
*Trace cp, po.
Trace pyrite
Trace pyrite
Trace pyrite
REMARKS ^^
MOLfcNOWL-8
LOGGED BY . WKS "AGE.
Pinned bv Vistw PRINT J
FROM ^ TO
167.3to172.0
172.0 to180.2
ROCKTYPE
Garnetaltered?banded tuffor sedimentL:e-.- ---'-"~7
Mafic intrusivediabase?- - i -,-,
COLOUR
Grey togreen
Dark green tojlack
GRAIN SIZE
fg-mg
fg
TEXTURE and STRUCTURE
142.8-143.5:Bleached section of gabbro.Riddled with qtz-carbveinlets.
140-150:Gabbro gradationally becomeless mafic.Feldspars increase.
154. .4-154. 7:F. g. int dyke.Sharp contacts, upper @
lower @
154.7-167.3:Massive to weakly foliatedequigranular gabbro.
Banded, garnetiferous,mafic to intermediate tuff-sediment.Upper contact @Banding @Lower contact @ Contains 10-1 5^ lmm-2cmanhedral light pink garnets
1QX s ubtle ammoeboid shapesup to 3cm in size which aremafic (biotite, chlorite?)with siliceous haloeslocally up to 40% of sectioi
Massive, equigranular mafic, Upper contact @Lower contact @ 80/^ dark black-orppn amnhilv
ANGLE TO CORE AXIS
;
65 068 0
58 055-60 052 e
-
*-
-*
52 070 0
IP
ALTERATION
60% qtz-carb veinlets.
Riddled with qtz-epveinlets (20 0̂ )
Up to 20X biotitelocally.10'^ chl. locallylQ-15% garnets up to 2cmsubhedral to stretched.
strange relic xylls ofsome type, some aresubhedral , probablycordierite altered tochlorite.
Weak biotite alt. locally
SULPHIDES
Trace pyrite
Trace diss pyrite
168.05-168.1:Trace cp in siliceous band.
168.2: 1 . 5mm magneti teband conformable tobedding.
Trace diss pyrite
REMARKS ^^
**Garnetiferous banded tuff.Pause in volcanism.Raft in gabbro?
167.3-169.8:Strongly magnetic.
f. g. gabbro?? or possibly diabasic dyke??Locally magnetic
HOLfc NOWL-8 feldspar LOGGED BV . FB/WKS PAGE.
tcd by Mister PRINT
FROM TO
180.2to 190.3
190.3to194.7
'
ROCKTYPE
Bandedmafic to in termed i at tuff withminor chert} b s phaleritmineralized exhalative component
'i- r (c '~~s ~^
Biotitecordieritechloritealterationzone
o* fa- r~
COLOUR
Bands ofgreen S
grey
Darkgreen toblack
GRAIN SIZE
f g -mg
mg
TEXTURE and STRUCTURE
Well banded mafic to inter mediate tuff with 5-1 0% cherty beds locally.
mm scale bedding @ ^
Contains lenticular felsic clots which concentrate sulphides (diss py) alongtheir perimeters from 180.8 to 181.1
187.05-188.15:Massive mafic dyke whichcontains 1 07o e longate clotsof biotite-chlorite.
188.15-190.3:Tuff is more intermediateto felsic.Contains more siliceouscherty bands (20 0̂ )
Well foliated biotite+ quartz with white toFlue cordierite rimmedchloritic pseudo cord xyllsup to 1.5cm
191.0-191.2:Section of massive int. rockSharp contacts, upper @
lower @
ANGLE TO CORE AXIS
62 0 (3180.5 62 0 @180.857 0 @182.5 60 0 @184.7 62 0 @186.064 0 @188.0
65-70 0
60 066 0
ALTERATION
Weak (pervasive)biotite-chlorite alt. (TO-15%)
lQ7o grid alteration (silica veinlets)
183.15-183.35: 105^ pink garnets
507o b iotite20^ cordierite + qtz30% chloritecordierite xylls alterirto chlorite
SULPHIDES
180.2-183.15: tr py.
183.15-184.4: T-2% diss py throughout, tr po diss.
184.4-185.4: Tr diss po.
185.4-187.05:V/o very fine dusting of sphalerite, locally moreconcentrations in certainbands
187.05-188.15:Barren dyke
188.15-188.45:V/o f ine sph dusting as abo 1
188.45-190.3:Tr py-po.
None.
g
REMARKS ^k
Locally this materialresembles Winston Lake Horizon, possibly with a more mafic tuffaceouscomponent.
*NOTE: Zn mineralization probably exhalative Zn ina tuffaceous section,possibly 1 7o z inc from185.9-1S5.0
e
Patch of tuffaceous materialin biotite altered zone.
c------- -' ^ r
HOLfc NOWL-8
LOGGED BY . FB/WKSht) by Mis!tf PRINT J
FROM ^ TO
194.7to201.6
201.6to224.1
224.1to240.2
ROCKTYPE
Intermediatmassivetuff
6L IT 77
Mafic unit(footwallmafic flow)
Intercalatebedded Smassivemafic ashtuffs
-
COLOUR
i Greygreen
Green
Green
GRAIN SIZE
fg
Aphan iticto fg
Ashtof .g.
TEXTURE and STRUCTURE
Massive, nondescript tuffwith local signs of weakbedding.
197.1-197.3:Section of pervasive shearechlorite alt.Sharp contacts, upper @
lower @
Massive mafic material withID-20% feldspars micro phyric in texture 1mm up to2mrn.No pillow selvedges evidentLocally f g massive.
Overall 30% of sectionshows fine mm scale beddingRest of section is a f. g.massive rock of mafic tointermediate composition.
Banded sections are slightlmore felsic.Banded sections:224.1-226.5229.5-231.7233.5-235.5
Last 1 m section 20%clotted rhyolite ash bands.
ANGLE TO CORE AXIS
I
72 o83 0
(9 65-70 0
ALTERATION
Weak chl alt, S-10%locally.57o grid alt.
Chlorite shear
None
224.1 to about 226.0:507o of section is verysilicified.
SULPHIDES
Trace py
iNo sulphides
Tr py occasionally.Very occasional tr speckof sph noted.
None to trace diss py.
REMARKS ^^
Similar to tuff sectionabove alteration but moremassive.
Probably footwall maficflow in that it is on topof clotted rhyolite
Similar bedded maficsediment/tuff seen onsurface intercalated withclotted rhyolite near road.
Two geochem samples(bedded vs massive)
HOttNOWL-8
LOGGED Bv . FBPrmtcd bv Mistit PRINT
FROM TO
ROCKTYPE COLOUR
GRAIN SIZE TEXTURE and STRUCTURE
ANGLE TO CORE AXIS ALTERATION SULPHIDES REMARKS
240.2to356.6
Clotted rhyolite
Creamy grey to grey pirrt with green clots
Aphan itic
Pink withgreenstreaks
Massive rhyolite withstreaky green amphibole-magnetiteSulphide clots from mm to2cm scale.About 10 to 20% clots.Clots all elongate mm to2cm sized defining foliatio
242.3-242.6:Banded mafic tuff as abovesection.
Foliated mafic dykes with ragged contacts. 247.3-247.4 249.0-249.95
From 268.7 to about 274.2: ID-20% l-2mm clear quartz eyes in matrix to clotted rhyolite.
Z-3% magnetite cubes up to 3mm occur throughout sectior
274.2-287.0:y/o d iscrete clots in pinkgrey matrix.
287.0-304.5:(streaky clotted rhyolite) 20-305& mafic streaks rather than clots, otherwise same as above.Intermediate to felsic biotite bearing massive pink green dykes @ 280.2-28C^JD/PO' 7 284.1-286.0
1_____2S7.Q-?aa n p.,
2-3^ epidote veinlets No hydrothermal altera tion apparent.
52-55'
Trace py diss in clotsthroughout.Locally up to Vh pyrite.Trace cp in clots foundoccasionally throughoutsection.Very occasional speck ofsph also noted.
65 !
NOTE: clotted rhyolite can be 'quartz eyed'
Section variably magnetic,
.5 55V5545V45 0ged Conta
More pink colour through out this flow.
278.5-279.0:10^ epidote in fracturesystem
bis——————————————
**NOTE: individual clotted rhyolite flows
Less sulphides apparent down section, i.e. by 280, trace diss py in some clots
Contact within rhyolite betweenflows??Check difference
clotted individual
in chemistr
HOLfc NOWL-8
LOGGED BY . FB PAGE. 8Pinned Ov Misttv PRINT
FROM* TO
1
ROCKTYPE COLOUR
Grey wit dark green clots
Pink witf dark green streaks
GRAIN SIZE TEXTURE and STRUCTURE
293.7-294.8:Very biotite rich foliated mafic dyke @ Clotted fabric @
304.5-318.3:Grey clotted flow again S-10% l-3mm clots in a grey aphanitic Fabric @
316.5: lcm fault gouge @
315.9-316.5: mafic dyke
317.8-318.1: mafic dyke
318.3-339.2:Streaky S clotted pink clotted rhyolite as above 304.5 Foliation of clots S streaks @
30% green clots S streaks 3mm to 2cm.
331.5-333.2:Very broken core, fracture zone.
334.6-334.7:Epidote filled fracture zone @
337 to 339.2:Very banded looking zone, probably flow banding?
ANGLE TO CORE AXIS
30 0
55 0 @ 293
55 0
30 0
55 0
20 0
ALTERATION
50 0̂ black biotite
Weak pink staining locally
matrix pervasively pink stained
Chlorite-epidote filled fractures ID-20%
2Wo epidote
SULPHIDES
Tr py.
No sulphides
No sulphides
None
REMARKS ^^
Again compare chemistry with flow above
Contacts abrupt. Another flow. No grading or sorting of green clots within any individual flow.
Possible fault, no orientation evident
Very steep fault zone
WL-8LOGGED BY .
FBPAGE.
Ov Visltf PRINT
FROM" TO
ROCKTYPE COLOUR
Grey witpink grepatchesgreenclots
GRAIN SIZE
fg
TEXTURE and STRUCTURE
339.2-356.6:Sharp contact at about
Grey clotted rhyoliteS-10% green clotslmm-4mm in scaleFabric @
Hybrid mafic- intermediatefg-mg massive dykes @
339.5-339.75340.95-341.05343.3-343.55343.85-344.3344.7-345.8
349.7-356.6:Dyked section.
F. g. mafic dykes @:349.7-350.0352.25-252.45352.9-353.85353.95-354.25354.30-356.1
'351.0-352.0:Fault, very broken fracture*ground = fault zone?Fractures @
ANGLE TO CORE AXIS
30 0
52 0
Contactsat
50-60 0
45V45 050 0 750 050V50 050V50 050V50 0
0-5 0
ALTERATION
Epidote, silica S pinkstaining along veinletsmarginal to dykes.
*341. 05-348. 9:garnet altered clotsbegin at 341.05By 345.8 green clots areall altered to a lightpink garnet S magnetitewith a weak pink halo.
Epidote veinletsbleaching St pyritichaloes to dykes.ID-20% epidote S pinkveining of dykes.
SULPHIDES
None
Diss pyrite apparentlyas haloes to dyked section:
349.3-349.7:~\7o d iss py.
350.4-352.25:~\ 0h d iss py.
356.2-356.6:27o d iss py.
REMARKS ^^
,'339.5-345.8:Strongly dyked zonerepresents structuralzone??
*NOTE: garnet alteredclotted rhyolite
HOLfc NOWL-8
LOGGED BY . FB PAGE. 10v Mislif PRINT
FROM TO
356.6 to395.1
395.1 to433.0
ROCKTYPE
Mafic intrusive?Flow?
^ ^/i yVc -~
Clotted rhyolite
~ ~//g P p"7 ) 77
^
COLOUR
Green
Creamy grey tolightpink
GRAIN SIZE
fg to aphan iticlocally with2-320.5 m
feld spars
Aphan iticwithgreenclots
TEXTURE and STRUCTURE
Massive to weakly foliated locally. Mafic intrusiveor flow.
,J361. 0-364. 0:-
Di abase dyke @with good chills, weaklymagnetic.
361.3-361.4:fault gouge @
361.7-361.9:fault gouge @
387.7:4cm pink silica-quartzvein let
Overall 202 of sectionweakly foliated @
Lower contact sharp @
Grey clotted rhyolite foliated with 5-1 02 darkgreen clots ^ s treaksconsisting of amphiboleand magnetite (approx 202clots)
Modest fabric @1-22 Irnrn feldspar xyllsSharp contact with overlyinmafic @
ANGLE TO CORE AXIS
45 0
20 s
70 0
50-55 0
55 0
50-60 0
55 0
ALTERATION
52 fine hairline silica- epidote veinlets.Intensely chloritizedsection 359 to 361
12 pink silica veinlets
Occasional rusty redhematite in veinlets
Light pink staining in streaks b mottlesthroughout.1-22 epidote veinlets
SULPHIDES
Trace pyrite in vein
Trace diss py in matrix and in clots
REMARKS (̂
Probably a micro gabbroic intrusive as it appears tohave identical clottedrhyolite above S below it??
Note: faults post diabasedyke
Strongly magnetic throughout
The clotted rhyolite becomesvery similar to the campQFP flow in that maficstreaks are magnetic and thepi nk colour.
' f^.-sA,^t"~. -' "~"
,. s . - *
MOLfcNOWL-8
LOGGED BV .FB
PAGE.n
Ptmh-d bv Mistcf PRINT
FROM " TO
433.0 to 477.8
ROCKTYPE
Gabbrof- '^
COLOUR
Green
GRAIN SIZE
fg-mg
TEXTURE and STRUCTURE
1414.2-414.8:'- ^' j
Broken, blocky ground with chloritic slip planes
415.0-415.2: F. g. massive mafic dyke @
419.3-420.0: Blocky fractured core
420.7-420.9: Fractured ground
428.3-428.4: f. g. chloritic mafic dyke
429.0-430.2: Fractured core
430.0-430.2: f. g. chloritic mafic dyke
4433.0-433.8: -^ r ' Severely chloritized fault zone with fabric @
433.8-434.2: Pink Si green mg gabbro
ANGLE TO CORE AXIS
55 0
40 0
ALTERATION
S-4% hairline chloritic fractures
y/o hairline chloritic veinlets
2-30̂ chloritic veinlets
5% chloritic joints S veinlets
Hematite staining
SULPHIDES REMARKS ^^
415.5-418.0: 2.5 m ground core
HOLfcNOWL-8
LOGGED BY .FB 12
Pimtwi by Mistf PRINT
FROM TO
ROCK TYPE COLOUR GRAIN
SIZE TEXTURE and STRUCTURE
434.2-436.3:Very fg massive intermediatedyke, contacts @
Chloritic fault at 434.5-435.0
Gabbroic xenolith in dyke at 436.0-436.2
ANGLE TO CORE AXIS
45'
438.0-441.2:Mg gabbro with 20% ofsection chloritic fracturezones.
441.2-443.8:Fg intermediate dykestrongly foliated @
443.8- :mg to eg weakly foliatedgabbro 30-40 0̂ whitefeldspar, 70% greenamphiboles.
448.6:Chloritic gouge @
of section consist of short O.lm to 0.3m sections of very foliated (sheared) gabbro
468.0-469.0: f. g. epidote altered mafic dyke @
Fabric@ 45 0
20'
45 :
hearing 40-45 0 ei ning 30-45 070 0
ALTERATION
Severely chloritized at fault zone
436.3-436.6 and 436.8-438.0: Severely chloritized sections 907o chlorite
Moderately chlorite throughout (ID-20%) ^0% pink silica vein- lets up to 6cm at random angles to CA
epidote quartz filled veinlets from 1mm -15m wide 10^ weak pink staining of feldspars
SULPHIDES
None
REMARKS
Note: from 433.0 to 443.8 Strong fault zone.
Very typical gabbro.
HOLfc NO WI.-8LOGGED BV . FB 13
Pr*rt(*d by Mistot PRINT
FROM * TO
477.8 to 491.0
i
ROCK TYPE
Mixed fault breccia shear zoneuT P-~ ^o-j'-
COLOUR
Variable black green
Black to green
Green S white
Green
Pink
Creamy pink S green
Green
GRAIN SIZE
aphan itic
fg
TEXTURE and STRUCTURE
477.8-478.1: Shear
478.1-480.9: Altered zone
481.1-481.3: Intense chloritic clay fault gouge @
481.3-482.7: M. g. gabbro
482.7-483.7: Strongly foliated sheared gabbro Sharp contact @ 483.7
483.7-486.5:Massive pink siliceous rock, altered
486.5-486.7: Sheared pink S green siliceous rock
486.7-486.9:Massive mafic dyke. Contacts @
ANGLE TO CORE AXIS
45 0
30 0
40 0
ALTERATION
477.8-478.1: Intense chlorite alterec zone.
478.1-480.9: Bleached light green intense epidote silica altered zone brecciatedID'% red hematite.
480.9-481.3:90-100'^ chlorite
Moderate chlorite alt.
482.7-483.7: Bleached b s trongly silica epidote altered
Silicified 'Pinked up' rhyolite?
None
SULPHIDES
None
None
None
None
None
None
None
REMARKS 4b
Assayed for Au because of hematite
HOLbNOWL-8
LOGGED BY . FBPAGE. 14
Printed bv Mtsttff PRINT
..FROM TO
491.0to518.0
^
ROCK TYPE
Severelybrecciatedmafic flow(LadderFlow)
i* r X .
COLOUR
Green
GRAIN SIZE
fg
TEXTURE and STRUCTURE
486.9-491.0:Severely mottled brecciatedaltered felsic rock or verysilicified mafic?
491.0 to about 498.6:Apparently massive maficbrecciated and injected byepidote silica pink veinmaterial 2 07cchloritic veins 10^
Extremely fractured ground,locally sheared.
498.6:Mafic becomes feldsparphyric up to 3Q70
503.0-503.4:f. g. mafic dyke @
504.3-41)5.9: - 'M. g. massive hybridintermediate dyke @
ANGLE TO CORE AXIS
10-20 0
80 0
ALTERATION
Strong epidote altera tion locally 2 Q7o o fsection.207, white siliceouspatches S veins
485.5-490.6:Strong muscovite biotite~\07o gnt alteration
490.6-491.0:500̂ epidote2070 p ink silica
491.0- :Strongly chloriticepidote silica veined
Feldspars stained greenand/or pink 205S ofsection.
SULPHIDES REMARKS ^^
Actual rock unitquestionable.
**Tectonic breccia zone
i. e.) 'Ladder Flow 'typefeldspar phyric nature.
HOLt NOWL-8
LOGGED BV . FBPAGE . 15
Printed bv Mistor PRINT
FROM* TO
518.75 to 581.4
ROCKTYPE
Intensely altered, pyritemineralizedfelsic rock
-, --,; -?7z' l- -
COLOUR
Grey with pink bbrownmottling
Bleachedpalegreen
GRAIN SIZE
fg
fg
TEXTURE and STRUCTURE
i 512.0-513.2:Strong chlorite-clay faultgouge, fabric suggests
513.2-518.75:Severely brecciated fspphyric maficContact obscured by shearin^
Strongly altered, garnet staurolite muscovite, quart, felsic rock of some type.Brecciated S sheared zone518.75-524.0
Moderate fabric throughout t
519.3:chloritic fault gouge,shear zone @
521.95-522.4:Massive to sheared Sbrecciated intermediatedyke, contacts @
Overall 5# network veinletsof quartz with tracesulphides
ANGLE TO CORE AXIS
50 0
J
i 52 0
55 0
Upper @20 0 S60 0
ALTERATION
510.7-512.0:Intense epidote silicaveining S bleaching
Intense chloritization
Moderate to strongchloritization
Intense garnet 205S staurolite 1025 muscovite 30^quartz 307,,chlorite-biotite? 10 0̂possibly anthophyllitepossible resorbed orpartial resorbed remnant3-4 mm quartz xyllsnoticed occasionally.
Pervasive pale greenbleached look:
chlorite, sericite orserpentine?
Chlorite filled veinlets10-1 5 7o
SULPHIDES
None
Trace diss py.
Diss pyrite throughout overall T-2% locally up to S-4% as noted below.*See estimates forsulphides specificintervals on assay sheet
-
None
REMARKS ^^
**Very strong fault zone
**Note: this alteration is very strong, obscures rock type. It is identical tothe altered felsic (QFP)immediately under the LadderFlow in WL-2 S 3
i.e.) same as core alt qfp
JHOLfcNOWL-8
LOGGED BY . FB PAGE . 16if**d bv Misttf PRINT
FROM TO
ROCKTYPE COLOUR
Greygreen
Pink
GRAIN SIZE
fg
TEXTURE and STRUCTURE
523.3-523.6:30% quartz filled brecciazone
From about 524: strongshearing brecciation givesway to massive to weaklyfoliated alterationmineralogy.
525.55-526.3:Feldspar phyric(y/o l -3mm white xylls)massive intermediate dykeContacts @
534.7-535.4:Same dyke as above @
Weak fabric chill @
ANGLE TO CORE AXIS
80V80 0
60V60 0
52 0
ALTERATION
None
None
Change in alterationmineralogy at about 536.Staurolite ends.,cordierite begins.
Mineralogy from around536.1 down:ID-20% pink gnt asxylls up to lcm30-40^ cordierite bluexylls30^ micas * anthophyllitqtz - 10-2^??
SULPHIDES
2 0fo cp in quartz veining
None
At 526.7:Pyrite mineralizationbecomes less to aboutQ.5%
None
3
541.1-541.5:S-4% streaks of diss pyrifl
REMARKS ^^
Note: staurolite cordieritechange, check geochemabove b below 536 m.
j.-H-'z cJ^*-~ •-'-*-
e
WL-8LOGGED BY . FB 17
Praitcd Dv Misttt PRINT
FROM" TO
ROCK TYPE COLOUR
Green
Lightgreen
Green
Green
GRAIN SIZE
fg
fg
fg
fg
TEXTURE and STRUCTURE
542.0-542.6:Massive fresh mafic dyke.Contacts @
i-^ 542. 6-547. 6 r *r - /:
Feldspar phyric mafic tointermediate dyke.S-10% l-3mm fsp xylls.
548.55-548.7:F. g. mafic dyke @
549.35-549.5:Altered zone.
549.85-550.5:Massive mafic dyke.
550.5-550.75:Foliated chlorite quartzcontact zone with maficdyke.
556.1-556.2:Weakly foliated mafic dyke '
ANGLE TO CORE AXIS
80 0
Shearedcontactsat 60 0
60 0
70-80 0
Sulphidebands
55 0Conformatto fabric
80 0
ALTERATION
None
Contacts sheared andchlorite altered,546.2-546.3 and547.3 to 547.6.
Intense pink stainedzone surrounding quartzfilled hairline fracture
Unaltered.
le
SULPHIDES
None
None
Trace diss py.
554.4-555.5:Two lcm bands of massivepyrite
REMARKS ^^
iL^Jb-?
Possible sulphide beds?Both beds are veryconductive with cm ohm-meter
WL-8LOGGED BY . FB PAGE . 18
tfd by MistiK PRINT
FROM * TO
ROCKTYPE COLOUR
Green S white speckled
GRAIN SIZE
fg
fg
TEXTURE and STRUCTURE
7557.3-558.5: " 7? Fsp phyric mafic to intermediate dyke. Massive
564.0-564.4: Open spaces 5% Vugs fi]led with quartzT Co/
1 3 /0
573.6-575.4: 5% open space filled vuggy quartz vein network.
575.4: 2-3cm chloriticgouge zone
-575.4-576.7:;- * Massive intermediate to mafic dyke. Sharp contacts @
ANGLE TO CORE AXIS
55 0
75 0
ALTERATION
T-3% epidote veinlets. Weak saussuritization of feldspar xylls.
None
SULPHIDES
None
From 559: sulphides in crease to T-2% diss pyrite (see assay sheets)
560.6-560.7: 5# diss pyrite in streaks in chlorite rich band.
560.7-561.3: y/o d iss py in chloritic bands S irregular streaks
No sulphides
By 569: sulphides reduce to Q.5% diss pyrite
Trace pyrite
None
REMARKS ^^
MOLbNOWL-8
LOGGED BY .FB 19
bv Vistur PRINT
^FROM TO
581.4to583.8
ROCKTYPE
Intenselyalteredmafic unit/"/' - -
COLOUR
Darkgreen toblackwithpinkspots
Darkgreen
GRAIN SIZE
fg
fg toaphan itic
TEXTURE and STRUCTURE
-'577.7-578.8: 'Faulted brecciated shearedsection includes:577.7-578.2: brecciatedmafic dyke
578.2-578.4: chloriticfault gouge with fabric @
578.4-478.6:Brecciated altered felsicas above.
578.6-578.8:Strong chloritic gouge zone
From 578.8-581.4:Gnt-cordierite mica qtzaltered felsic.
581.4-582.0:Streaky biotite-chloritegnt alteration zone.Foliated @Sharp contacts with felsic
582.0-583.0:Massive fresh lookingmafic.
ANGLE TO CORE AXIS
55 0
@ 55 0
60 0@ 60 0
ALTERATION
Strong chlorite
Strong chlorite
As before
581.2-581.4:10 0fo s taurolite nearcontact co-exists withcordierite.
2Q7o p ink euhedral tosubhedral garnets up to2cmS0y0 b iotite,305^ chlorite
Hazy contact withalteration (halo?)above and below.
SULPHIDES
Trace py.
Trace py.
Trace diss py.
Trace diss py.
REMARKS ^^
Note: 577. 7-578. 8, faultzone
Streaky chlorite biotitealt. look similar to 27 AuZone type material.i.e. altered mafic.No magnetite.
Assayed for Au.
HOLfc NOWL-8
LOGGED BY .FB
PAGE.20
i.il.^3 bv Misflf PRINT
FROM TO
583.8 to 588.0
588.0 to 640.0
ROCK TYPE
Vuggy altered felsic
intensely altered "el sic (altered QFP?)
COLOUR
Grey
3rey to blue grey with pink b yellow specks
GRAIN SIZE
fS
mg
TEXTURE and STRUCTURE
583.0-583.8:Streaky biotite chlorite alteration. Zone much thesame as first zone butwithout garnets and with a severely brecciated zone from 583.2-583.5
583.5-583.7:hybrid dioritic like dyke?
583.7-583.8:Streaky eh! -bio alt.
30% of section consists of of qtz-qtz epidote filled veinlets (approx. 10^; open spaces - vugs)
Rock appears to be musc- bio-cord altered felsic
Foliated rock consisting of cordierite, gnt, staur. (biotite-chl-musc)
593.0-593.2: vuggy fault? zone 107o open spaces
ANGLE TO CORE AXIS
Fabric @ 60 0
60 0
ALTERATION
Massive chl -biotite
10% white carbonate fi 11 i ng spaces between chloritic fragments
Qtz-epidote veinlets 20% qtz, 1 0X epidote Trace carbonate noted.
Intense pervasive alteration obscures original rock textures Proportions of individua minerals vary locally. Generally 50^ cord-blue to grey xylls in matrix up to 3mm. 20-305^ micas b chloritebetween all minerals^0% gnt-porphyroblasts up to lcm, occasionally up to 207o l ocally 1070 s taur-finequartz ??
SULPHIDES
Trace diss py in alteration
Barely trace diss pyrite
Only occasional diss py.
REMARKS ^^
Assayed for Au
lHOLfcNO WL-8
LOGGED BY . FB PAGE. 21Pr Kited bv Mster PRINT
TOROCKTYPE COLOUR
Greygreen
Greenwithwhitexylls
GRAIN SIZE
fg
fg
TEXTURE and STRUCTURE
611.6-611.95:Chloritic mafic dyke.Foliated sheared contacts @
617.2-618.2:Massive to weakly foliatedmafic dyke. Contacts @
i j619.7-622.2: ^ 'Mafic dyke.
qtz veined 621.2-620.3620.6-620.9
Fault gouge @ 621 .2Contacts @
i"633.2-636.4: r " "-^?Feldspar phyric to massivemafic dyke.Inlcudes from 634.0-635.0a hybrid gram' ti zed f g dyke,Sheared contacts.
ANGLE TO CORE AXIS
60 0
60 0
60 0
ALTERATION
Strong pervasive chlorit
Weak pervasive chlorite
At 611: mineralogy ofalteration changes to:50* cord + qtz30% colourless-whitemineral amphibole likeanthophyllite?10^ gntW0/, bio
**Staurolite is replacedby colourless whitemineral (anth) which hassame type of distributioas staur did.
Unaltered
Anthophyllite increasesdownhole by 623 20-300̂Some anth xylls havegarnet cores.
Weak saussuritizationof feldspars but other wise unaltered.Pink staining in hybriddyke.
SULPHIDES
s None
T
Tr py.
None
None
REMARKS ^^
Check geochem above S below611
HOLfcNOWL-8
LOGGED BY .FB 22
Pruned Oy Misttf PRINT
^FROM TO
640.0to641.0
641.0to644.0
644.0to648.7
648.7to653.3
^
ROCKTYPE
Mafic dyke&.-T
Quartzfeldsparporphyry(unaltered)
.- : ri: ~7
Mafic dyke
^ ' . - -
PatchyalteredQFP
' -7
COLOUR
Dk green
Greywithwhitespots
Dk green
Grey
GRAIN SIZE
fg
fg
fg
fg-mg
TEXTURE and STRUCTURE
Massive mafic dyke, sharpcontacts @
Feldspar porphyriticrhyolite - rhyodacite?l-3mm tabular subhedralcrystals (200̂ )Subtle quartz crystalsl-2mm evident throughout1056??Very weak fabric @
Massive with short weaklyfoliated section 20%Fabric @Vfc feldspar xylls.Lower contact brecciatedover 0.2m.
305^ of section relativelyunaltered QFP patches (asabove)70% of section consists ofcordierite, garnet, biotiteanthophyllite alteration.Weakfabric @
GRADATIONAL C
ANGLE TO CORE AXIS
65 0
60 0
65 0
65 0
0 N T A (
ALTERATION
]-20,'o hairline epidotefilled veinlets
Weak alteration biotiteS possible cordierite??blue grey qtz?
T-3% pink or greenveinlets
647-648.7:Intensely chloritized.
70% of section strongalteration hazy patchesor windows of lessaltered to unalteredQFP.Alteration increasesdown section.
T
SULPHIDES
None
None
None
Trace diss py.
REMARKS ^^
Fresh window? of QFP
HOLfcNOWL-8
LOGGED BY .FB 23
Ptmtecl by Misltf PRINT
TO
653.3to694.6
E.O.H.
694.6
E.O.H.
ROCKTYPE
Intenselyalteredfelsic(QFP)
COLOUR
Bluegreywithwhiteflecks
Green
GRAIN SIZE
mg
f g.
eg
TEXTURE and STRUCTURE
Weakly foliated cordieritebiotite anthophyllite andminor gnt.Cordierite eyes from l-4mmwrapped in anth-bio.
659.1-659.6:Wormy qtz vein 3cm
664.5-664.8:Foliated chloritic altereddyke.Similar dyke from 665.9-666.1
.684.4-685.3 and-j 689. 0-690.1:.,- ' ' S/
Massive to weakly foliatedmafic dykes.
684.6-685.3:2cm qtz pegmatite veinalong core axis.
693.5-693.7:White milky qtz vein.
Hole ends in strongcordierite anthophyllitebiotite alteration
ANGLE TO CORE AXIS
20 0
BO 0
Fabric bContacts
@ 60 0
ALTERATION
50% cordierite30^ anth + muse20 0̂ biotiteZ-3% garnet porphyro-blasts l-4mm
Bleached pink stainsurroundinggarnets disappear by 660
Strong chloritealteration.
673.3-677.0:Feldspars preserved ina short section of lessalteration.
Incipient to strongchlorite.
SULPHIDES
*at 656.5: a 1mm chloriti*veinlet at 30 0 to CA ishaloed by sphalerite andpyrite as ragged veinlikematerial over O.lmEst. of 4% sph.
None
n.
Trace to ~\ afo d iss pyrite
None to trace py.
None
REMARKS flfc
f ' t -*Xj- i, rf 4. r f ^ -^J* J f -~-^
HOLfcNOWL-8
LOGGED BY . FB PAGE. 24Piot.-d Ov Mister PRINT
O ^S^r
;jrn r *niM?l t \.: ±t Li i t ^ i l t UL-26
CORPORATION FALCONBRIDGE COPPERDRILL HOLE RECORD IMPERIAL UNITS: METRIC UNITS: X
PROJECT: PN370 WINSTON LAKE FIELD COORDS: LAT 5 + 10S /^ ", " .'- COLLAR BRNG: 300 sDEP 12+25E ^-•--•. - COLLAR DIP: -89"
GRID: SELCO IDEAL ELEV 9997 (EXPLN)'-"" HOLE SIZE: 30CLAIM NUMBER: SURVEY COORDS: LAT L8700N FINAL DEPTH: 1458m
LOCATION: PICK LAKE DE? 90 J-74EDATE STARTED: JULY 23. i9ss GEOD. ELEV 10415 ROD LOG:
riATprnMP'rTri'ersT'io i a o ̂ piirq^cMQMtitrv-v
CONTRACTOR:CORE STORAGE:
CASING:PLUGGED:
MULIISHOI SURVEY:COLLAR SURVEY:
ST. LAMBERT DRILLINGCLEAVER LAKE3m BU
X
PURPOSE:
ACID TESTS IROPARI TESTS
Depth \ni) Anqle Dsoth (m) Anqie Denth 'inu Asinvjth DID Deoth
'"-. -39"100 -85.5"2 0 0 - S I ljr? A r. - T o o
400 -70 0500 -i7'"'600 -64 0700 -51*300 - ?i 3 09 0 0 -57*1000 -54'1100 -53* 1200 -50 sL O V v' . j
~*1 ''"" ~'
1280 310 i-^ -48 01343 303 ^Vi -48'140S 316 VJ-T -47"
^- -^"^ ' ""'-"-^ - r3:x. . -".- , ---' 7
J^c. "..s -j'/x."-*"-'."
J •'"/-^ ^
•J— "^ J ' "* . ^ ^ ^ r j. -~^ -y ^ . ,
O^-- '^^ *^^- -1 '-.-^ \ \ .,- j ^-^ , - -
' -i^O'r ' f* ' ** i .*- \ '\\i. *J .^ * i-.
^
^
' J\o- i ' -, - ;lVi-j^ C - " ^ -^ .. " —
^J \ t~\ *^r — 7 s~~\ \\ O— C^ V-Av^j Zli ( ^ — ' \*
305784
111133147174201228255282309336408471534597650713776839902965102810911154
1 - f j 1217
MULTISHOT DATA
(m) Asisuth
293270261259261259260261262263 26426526626926927027227627823128328528629329823-5/^7^7
Dip
-S3 0-87*-86"-84*-P3 0-OOO \J *J-82"-30*-79 0-77 0 -73"-7 ~ o— 79 o-70"'
-68 s-66"-64 o-62"-60"-58 0-57 0-56'-54 0-53 0-52 0
J/2^7 ~^Q5
HOLS NO: UL-2S LOGGED BY: S.C.SIM
DRILL HOLE LOG
FROMTO
0 to3.0
3.0to46.5
ROCKTYPE
CASING•"3*:.~
ALTEREDQFP
e- . C - '^f t" -*v * '
GRAINCOLOUR SIZE
Blue/qrey mqwithmottledcreamypatches
ANGLE TOTEXTURE AND STRUCTURE CORE AXIS ALTERATION
Moderately foliated (? 45 0 Intense alterationdefined by micas and 20% biotiteweak flattened cordierite 5% muscovite
0-27. anthophylliteUp to 60% blue cordieritelS-20% recrystallisedsugary qts - patchy weakepidote stained givingcreamy colour
SULPHIDES REMARKS
131 pyrite in localisedangular clots oftenenveloped in biotite(up to 2mm)
Grey/green
10.7-10.9: White qts dyke 0
30.8-31.3: Qts/eoidote healed breccia sone.
31.3-32.6:Weak mineralised locally well foliated intermediate dyke. Sharp contacts ?
31.5-51.8:Unite qts dyke with20X host fragments
70 0
57. muscovite, cut by 351 qts veins
27. pyrite clots in dyke tr-1% cp in qts veins.
10-15*
38.7-38.8:Well foliated int dyke.same as 31.3 @
38.7-40.0:Blocky ground, possiblefault sone.
40 0Cut by 103: qts veins
Below 32.6: pyrite content in QEP increases to 2-331 (up to 5mffl) with localised tr-1% pyrrhotite
431 pyrite clots
;38.7-40.0: ~ r '~ Possible fault?
HOLE NO: WL-26 LOGGED BY: R.C.SIM PAGE:
DRILL HOLE LOG
FROM TO
ROCKTYPE COLOUR
GRAIN SIZE TEXTURE AND STRUCTURE
ANGLE TO CORE AXIS ALTERATION SULPHIDES REMARKS
3.0 to46.5 (cont'd)
Mottled mo -42.1-43.2: - ^ i '-~ -"- ' ' brown S to Weak foliated feldspar grey fg glomeroporphyritic
altered mafic xenolith/ dyke ?Contacts somewhat gradational over lcm due to alteration @
Intense biotite (202) Cordierite (up to 402) with up to 2 7. anthophyllite
17. po, 1 7. py, IX magnetite in clots
Possible Ladder Flow Xenolith
44.7-44.9:Mineralized well foliated altered mafic xenolith (? Sharo contacts.
37. qts veins S clots often 40 0 py mineralised
+602 biotite/anthophvllite
32 py in streaks parallel to foliation
44.9-46.5:37. pyrite, 22 pyrrhotitein clots over section.
46.5to52.6
UEAKALTEREDFELDSPARGLOMERO-PORPHY-RITICMAFICFLOW/XENOLITH
Green to fggrey withwhitespots
Massive to locally weakfoliated.Sharp upper contact markedby 5cm intense to pervasivebio/anth/cord alt. in mafic @ 50"
Fg dark green to 47.5m 5 7. biotite 12 diss py.
47.5-47.9:Irregular gts/ep dyke.
47.9-52.6:Fg greyish weak alteredmatrix with 52 round whitefeldspar "glows* up to4mm.Gloms commonly have tramphibole or magnetite incores.Lower contact somewhatgradational with weak felsicbanding from 52.4-52.6 l? 50 0
52 biotite1-32 anthophyllite
12 diss pyrite 1-22 diss magnetite
Banded zone weak eoidote bleached
22 py, 12 po in banded material.
HOLE NO: UL-26 LOGGED BY: R.C.SIM PAGE: 3
DRILL HOLE LOG
FROM TO
52.6 to 666.1
ROCKTYPE
ALTERED QFP
GRAIN COLOUR SIZE
Blue/grey mg
TEXTURE AND STRUCTURE
Same as above.
ANGLE TO CORE AXIS ALTERATION
5-72 muscovite 202 biotite +502 cordierite
17.Ir-
SULPHIDES
pyrite throughout 17. pyrrhotite
REMARKS
71.6: 3-5cm irregular mineralised qts vein (?
Gradational increase foliation angle 8 75m =
98.4-99.0:Massive fg highly feld. phyric (202) intermediate dyke @
112.6-117.9:Well foliated dark greenfg mafic dyke @
"35"
50 0
65"
50'
114.4-116.3:- ^-- - Multiple dykes in fault sone.
114.4-114.5: fg mafic dyke similar to above114.5-114.9: chloritic, grungy fault sone 9 60" 114.9-115.4: qts/ granitic dyke
Very intense alteration 1-37. anthophyllite
59.2-60.0:White highly siliceoussone in QFP
107.9-111.4: Creamy white highly siliceous sone with 102 musc/sericite 37. s illimanite
57.6 S 60.3:Clots of non-magnetic (?) pyrrhotite up to 152 over 5cm sections
52 pyriteTr sphalerite
py cubes X clots
3Z py streaks over section
diss py.
,114.5-114.9i Fault
32 py clots up to lcm
'-OLE NO: UL-26 LOGGED BY: R.C.SIM PAGE: 4
DRILL HOLE LOG
FROM ROCK GRAIN ANGLE TOTO TYPE COLOUR SIZE TEXTURE AND STRUCTURE CORE AXIS ALTERATION SULPHIDES REMARKS
52.6to666.1(cont'd)
115intcut116
.4-116.3:
. dyke -by mafic.0-116.15
feldsanedyke
.ohyricas 98.4at
10Z irregular qts clots from 118.5-119.5
Grey fg 145.3-147.5: with Weak altered feldspar phyric white intermediate dyke. Massive, spots fg matrix with 10Z anhedral
white feldspar phenocrysts.Sharp chilled contacts, top l? 80 0
bottom 5 55 0
147.6-148.3:Fg massive weak feld.mafic dyke.Sharp contacts 8
phyric
60'
102 biotite157. cordierite in matrix
None2Z disseminated magnetite
Weak chloritised 1Z py * po associated with crosscutting q.tz veinlets Tr-lZ magnetite
Uell e 150m: QFP altered to: foliated 15-20Z biotite 0 SO0 5-7Z muscovite
+50Z cordierite Rare anthophyllite 1-3Z sillimanite 20-30Z recrystallised qts partially or wholey gone to cordierite
Rare trace diss py S po.
156.7-157.0:Dark green weak foliatedmafic dyke.Sharp contacts G? 35*
Intense biotite developed in dyke for 5-10cffl at upper X lower contacts
160.3: 5cm qta veining at 45' giving 1Z py, 1Z po for 0.2m above and below.
HOLE NO: WL-26 LOGGED BY: R.C.SIM PAGE:
DRILL HOLE LOG
FROM ROCK TO TYPE
52.6 to 666.1 (cont'd)
GRAIN COLOUR SIZE TEXTURE AND STRUCTURE
163.6-164.2: Well foliated mafic dyke, similar to 156.7
ANGLE TO CORE AXIS ALTERATION SULPHIDES
Intense carbonate developed at contacts Also biotite as in above dyke.
REMARKS
165.2-165.4:Very fine grained massive (chilled) mafic dyke. Sharp contacts 9
Dark green
182.9-184.4: 6.*"*-^ Well foliated and highly crenulated altered mafic dyke. Sharp biotite rich contacts 9
204.0-204.2:Well foliated Mineralisedint/aafic dyke 0
SO 5
166.3-166.5:Grungy, blocky shearsone cut by 152 qtz veins 8 45*
166.5-167.1:Very blocky fg massive dark green mafic dyke. Contacts fractured.
Dark Aphan--178.7-180.0:- ^ D6;7 green itic Carbonate soaked diabase to black dyke.
Sharp chilled contacts l? 45 C
50"
70 0
204.2-204.4:Well foliated felsic dyke 8 70 l
intense carbonate Qtz veins partially altered to corderite
22 pyrite introduced in qtz veins
-71&6.3-166.5: Fault
152 biotite,102 anthophyllite fromhornblende.
22 diss pyrite
Epidote bleached in centre
HOLE NO: UL-26 LOGGED BY: R.C.SIM PAGE: 6
DRILL HOLE LOG
FROM 10
ROCK TYPE COLOUR
GRAIN SIZE TEXTURE AND STRUCTURE
ANGLE CORE
TO AXIS ALTERATION SULPHIDES REMARKS
52.G to666.1 (cont'd)
QFP changes character gradationally from 190m to 210m.It becomes lighter grey in colour and more sugary matrix with a well defined foliation marked by aiicas, anthophyllite and sillimanite S Rts eyes altered to cordierite (avg. 3mm)
208.7-208.9 S211.6-212.4:Well foliated alteredintermediate dykes @
65*
65 s
230.7-230.9: Altered int. dyke, same as 208.7 0 60 (
e 210ra QFP altered to:15-202,biotiteUp to 5051 cordierite52 muscovite22 sillimaniteTr gahnite1-42 anthophyllite27. garnet"202 sugary q iz.
Increased sulphides at200m average:12 py, 12 po disseminatedRare tr cp.Rare tr sphal from gahnite
302 biotite42 garnet
152 cordierite
Garnet content has increased to 42 3 225m. also anthophyllite increases locally up to 52
Ir diss.-pyrite Probably synvolcanic intrusive dykes
240m: Garnet has increased - to 62, patchy sillimanite up to 42 locally, increased gahnite to 12 - possibly tr staurolite?
Increased sulphides also. 32 py * po clots with tr-12 cp also tr sphal from gahnite
Very altered QFP !! !
244.4 - 5cm X244.6-244.9:Well foliated fg maficdykes ? 65 s
HOLE NO: UL-26 LOGGED BY: R.C.SIM PAGE:
DRILL HOLE LOG
FROM ROCK TO TYPE
52. S to 666.1 (cent 'd)
GRAIN COLOUR SIZE TEXTURE AND STRUCTURE
252.4-253.0: Olive green mafic dyke with dark green chloritic clots (751) stretched e Sharp contacts @
ANGLE TO CORE AXIS ALTERATION
65" 65"
SULPHIDES
Several clots pyrite over 2cm at bottom contact.
REMARKS
253.5: lOca zone with 122 irregular veined sulphides approx. parallel to foliation. 27. c p 42 py62 pyrrhotite (non
magnetic)
NOTE: between 253.5 and 265.6 rocks highly alt ered 42 total po+po+cp with abundant gahnite (1-22, up to 1.5mm). May be a result of intense perculation of hydrothermal fluids rich in sulphides (Cu.Zn.Fe, etc).
Dark fg -'270.3-272.2*-^ /D ̂grey Massive feld. phyricwith (32) int. dyke withwhite sharp contacts, top (?spots bottom (?
265.6-266.9:Gradational contacts over 3ca delineate this intense sone of alteration consisting of: 352 biotite52 garnet
+12 gahnite22 sillimanite22 muscovite
502 cordierite No visible qtz.
52 sulphides over section mainly irregular clots of weak to non-magnetic pyrrhotite and orange/ rusty sphalerite from gahnite.
266.7-266.8:402 sulphides in massiveveins/bands similar to253.572 cp
102 pyrite232 pyrrhotite (non
magnetic)
NOTE: estimate overwhole section 12 Zn(from gahnite) 0.52 Cu
50" 75"
HOLE NO: WL-26 LOGGED BY: R.C.SIM PAGE: s
DRILL HOLE LOG
FROM TO
ROCK TYPE COLOUR
GRAIN SIZE TEXTURE AND STRUCTURE
ANGLE TO CORE AXIS ALTERATION SULPHIDES REMARKS
52.6 to666.1 (cont'd)
285.4-285.6:Light green well foliatedsynvolcanic altered dyke(QFP)Sharp contacts (? 75'
Intense bio/cord with 77. garnet
5 291m: begin to see a decrease in garnet content to 1 -27. avg.
Probably intrusive QEP dyke into main flow 8 subsequently altered.
296.0 - 3cm X296.2-296.4:Irregular white qts clotsand dykes.
Green/ grey
308.5-309.0:Massive fg mafic dyke (?
J315.2-318. 2:'r ^ .Massive, weakly feld. phyricintermediate dyke.Sharp contacts 9Similar dyke at:
333.8-337.1 cut by mafic dyke at 335.3-336.8
338.0: 5cm blocky ground possible joint plane.
354.4-354.7:Blocky epidote bleachedpossible fault zone (?
296.4-"301m:37. pyrrhotite clots ov.er section (irregular up to lcm) also 12 py, 12 cp Tr sphal from ̂ gahnite.
65*e 313m: sillimanite increased to 42 avg
has
65
~/ 354.4-354.7: f 'Possible fault?
30'
HOLE NO: UL-26 LOGGED BY: R.C.SIM PAGE:
DRILL HOLE LOG
FROM 10
ROCKTYPE COLOUR
GRAIN SIZE TEXTURE AND STRUCTURE
ANGLE TO CORE AXIS ALTERATION SULPHIDES
Tr-12 diss py * po.
REMARKS
52.6 to666.1 (cont'd)
Light grey/blue
Blue/ grey to
mg
360.0-360.3:Blocky weakly chloriticgroundPossible fault ?
365.4-365.5:Light green mafic dyke Q
365.5-369.4:Highly qts/calcite veined,blocky, fault zone.Most fractures alongfoliation ?Very broken up from367.2-367.5
Below 369.4: QFP is patchy weak to well foliated and much darker in colour
60 0
55 1
60"
65 C
373.2-373.7:Eg foliated feld. phyric dyke, int. dyke 9 also at 383.8-384.1 e
65"65 0
0 357ra QFP altered to:52 muscovite22 sillimanite patchy)15-202 biotiteRare tr anthophylliteTr-22 garnet402 cordierite"302 recrystallised qts.
360.0-360.3: Possible Fault?
352 cloudy white recrystallized clots of qts K5mm) in fg biotite matrix. 102 qts/carbonate veins and vugs (up to lcm)
365.5-369.4:Fault zone
102 biotite1-22 sillimanite (locally
up to 52)2-32 muscovite (locally up
to 52) 0-22 garnet Up to 202 qts 0-22 anthophyllite 50-602 cordierite
Non-magneticTr pyrite throughout (diss)
QFP seems to change across fault. Alteration is similar but visually it is different
MOLE NO: WL-26 LOGGED BY: R.C.SIM PAGE: 10
DRILL HOLE LOG
FROM ROCK TO TYPE
52.6 to 666.1 (cont'd)
GRAIN COLOUR SIZE TEXTURE AND STRUCTURE
384.7: lOcffl sillimanite rich (152) qts dyke/vein
Black/ fg 385.3-387.1:
ANGLE TO CORE AXIS ALTERATION
S 75"
SULPHIDES REMARKS
brown with white spots
Massive feld. phyric (52) int/mafic dyke Sharp chilled contacts l? 12 diss magnetite.
65
Fg dark green well foliatedmafic dykes at:392.4-392.7 S 70" 395.4-395.8 S 70" 400.0-401.0 e 65"
9 399.0: Gradation sone from 398m to 403m where QFP is less altered.37. b iotite 102 cordierite12 muscovite
Tr-12 garnet (no visible feldspars)
e 405n: QFP becomes same as above.
27. d iss S clots pyrite 402.0-403.0
Black, white X pink
406.2-406.5: Fg mafic dyke, sane as 400.0 S
407.0-407.3: Qts/carbonate/hematite/ chlorite healed breccia zone
407.3-408.4:Massive hematite stained intermediate dyke. Contacts, top @
bottom l?
65 C
-/407.0-407.3TPossible healed fauli
75' 50"
HOLE NO: WL-26 LOGGED BY: R.C.SIM PAGE: 11O
DRILL HOLE LOG
FROM TO
ROCK TYPE COLOUR
GRAIN SIZE TEXTURE AND STRUCTURE
ANGLE TO CORE AXIS ALTERATION SULPHIDES REMARKS
52.6 to666.1 (cont'd)
Brown
403.4-408.8 S409.8-409.9:Light green fg massivesiliceous felsic dykes.Irregular contacts, also5cm clot at 409.7 probableedge of similar dyke.
414.6-415.1: Well foliated fg mafic dyke with sharp contacts,
top e bottom l?
17. magnetite.
40 0 05"
433.5-434.2Fg patchy foliated weak feld. phyric int/mafic dyke e
442.8-443.0:Blocky core along crenulated pervasive biotite zone. Probably drill induced.
70'
e 420m: QFP 2-52 sillimanite 32 garnet 152 biotite 5-102 qtz 1-32 muscovite C-2% anthophyllite •t-60% cordierite
Beginning at 432m: Pervasive biotite bands (2-5cm) become quite common at various core angles (avg. 1-2Z of section)
Upper contact at 5cm biotite sone
Commonly 1-22 diss pyrite
HOLE NO: HL-26 LOGGED BY: R.C.SIM PAGE: 12
DRILL HOLE LOG
FROM ROCKTO TYPE
52.5 to 666.1 (cont'd)
GRAIN COLOUR SIZE TEXTURE AND STRUCTURE
445.8-446.0: Fg mafic dyke 2 Siailar dyke at 454.4-454.6 0
ANGLE TO CORE AXIS ALTERATION
45 0
80"
SULPHIDES REMARKS
455.5-459.0:Blocky core with fracturesalong qts/carb veins.
462.4-462.9:Eg patchy foliated mafic dyke, top @
bottom 0
462.5: lOcffl sons with 1003: qts clots @
464.4-464.7: Well foliated mg mafic dyke. Sharp contacts @ contains 20Z chlorite clots K2mn)
Pink S white qts veins S clots at:
474.7-474.8475.0-475.1475.3-475.4476.3-476.4476.5-476.6
all with irregular contacts.
Gradational change in QFP from 465m to 485m.
40" 85"
50"
70 C
Tr-1% diss pyrite Rare tr magnetite
HOLE NO: WL-26 LOGGED BY: R.C.SIM PAGE: is
DRILL HOLE LOG
FROM TO
ROCK TYPE COLOUR
GRAIN SIZE TEXTURE AND STRUCTURE
ANGLE TO CORE AXIS ALTERATION ' SULPHIDES REMARKS
52.6 to666.1 (cont'd)
Mottled fg e 485m: Weak to moderately 70"Ii3ht 8 dark grey/ blue
foliated defined by amphi- boles and lighter coloured siliceous/cordierite clots. Avg. ^cra x 5am, 5Z of section) (Note clots exist only from 485m to 489m)
489.8-490.5:Fg weak foliated mafic dyke
top 8 70" bottom e 50"
490.5-491.4:Pink stained granodioritedyke.Sharp lower contact 8 40®
491.4-491.6:Fg massive mafic dyke.Lower chill l? 50 0
Siliceous clots similar to 485m at 503.0-505.0
516.3-516.5:Well foliated graniticstained mafic dyke 2 70 0
519.2-519.5 8524.2-524.6:Blocky chlorite/carbonate/qts rich fault zones 9 60-70"
3-7Z anthophyllite(up to 3mm)
15-20Z biotite 17. sillimanite Ir muscovite 0-3Z garnet +50Z cordierite Clots contain 30Z cord, 70Z qts - recrystallised NOTE: no garnets where
clots present.
489.8-491.6: Composite mafic/ granitic dyke.
5Z muscovite 3Z diss. pyrite
e 511.0: QFP has become slightly lighter in colour due to increased light green anthophyllite (5-7Z) also 3-5Z garnet.
519.2-519.5524.2-524.6:Faults
HOLE NO! WL-26 LGGGES BY: R.C.SIM
DRILL HOLE LOG
FROM ROCK TO TYPE
52.6 to 666.1 Ccont'd)
GRAIN ANGLE TO COLOUR SIZE TEXTURE AND STRUCTURE CORE AXIS ALTERATION
0 525m: QFP altered to: patchy 2-57. s illimanite 3-52 garnet (anhedral) 207. b iotite
SULPHIDES REMARKS
Slight change in QEP across fault (staurolite, sill imanite, biotite)
Grey with white spots
544.1-546.0:Fg massive mafic dyke.Sharp contacts ?
547.0-547.9 :r -f FT- 7 ~ Intensely altered and crenulated zone around qts vein at 547.1-547.3
550.2-550.7:Ueak altered sy.nvolcanic dyke, well foliated l? Eg, foggy contacts.
565.0-567.9:Massive feld. phyric int.dyke. Sharp contacts l?
55 C
85'
75'
576.3-577.0:Blocky sone slightlybleached (dry fractures)
2-37. anthophyllite (clots) 1-22 staurolite (•Clmm) 10-202 recrystallised qts
8 qts eyes K102) ± 502 cordierite
P.ervasive biotite/antho- phyllite enveloping qts S cordierite fragments
37. pyrite in 2cm qts vein at 546.1m
37. py in, qts vein 27. i n pervasive sone
Fault?
52 biotite, 102 cordierite '22 pyrite, tr-12 po.
Consistently +S2 sillimanite in QFP below 552m.
Sillimanite decreased .to22, 2m above and 1m belowdyke
568.2: lea zone in QFP with 202 streaky bands pyrite
(? 575m: patchy sillimanite 5-72
595.6: 10cm pervasive/biotite cordierite band
HOLE NO: UL-26 LOGGED BY: R.C.SIM PAGE: 15
DRILL HOLE LOG
FROM 10
ROCK TYPE COLOUR
GRAIN SIZE TEXTURE AND STRUCIL'RE
ANGLE 10 CORE AXIS ALTERATION SULPHIDES REMARKS
52. S to666.1 tcont'd)
600.1-600.3: Blocky qround (dry)
602.9-603.0!402 irregular qts clotsover section.
Massive to weak foliated S 65-70 0
618.2-618.3:Fg mafic dyke 5 50"
620.4-520.6:Sillimanite rich (102)siliceous dyke l? 50 0
624.7-625.0: 602 irregular qts clots over section up to 10cm Enveloped in biotite with minor anth.
625.0-625.5:Fg massive mafic dyke.Sharp contacts (? 65"27. d iss. magnetite.
8 603.5: we see gradationalchange in QEP over 2m to:Tr-1% sillimanite15-202 biotite2-52 anthophyllite(no garnet)1-22 muscovite+702 cordierite(qts eyes qone to cord)
Rare trace diss pyrite
627.S-62S.2:white qts dyke withirregular contacts.
HOLE NO: WL-26 LOGGED BY: R.C.SIM PAGE: 16
DRILL HOLE LOG
FROM TO
ROCK TYPE COLOUR
GRAINSIZE TEXTURE AND STRUCTURE
ANGLE TO CORE AXIS ALTERATION SULPHIDES REMARKS
52.6 to666.1 (cont'd)
630.2-630.9:Fg weak fol. to massivemafic dyke (2?i magnetite)with sharp contacts 8 80"Cut by weak garnetiferous(27.1 granodiorite dykeat 630.3-630.5
631.3-631.6:Irregular granodioritedyke - same as 630.3
632.0-632.1: Blocky ground along irregular qts clots. Dry fractures.
632.5-632.9:Muscovite richJlOX)qts dyke @ 30 s
633.5-633.6:Sillimanite rich (7%)siliceous granodioriticdyke @ 80"Similar dyke at634.5-634.7
631.2: 5cm sone with 102 garnet around 10X irregular qts clots.
636.3-636.7: Fg mafic dyke, same as 630.2. sharp biotite rich contacts, top @
bottom ?55" 80"
HOLE NO: UL-26 LOGGED BY: R.C.SIM PAGE: 17
DRILL HOLE LOG
FROM TO
ROCKTYPE COLOUR
GRAIN SIZE TEXTURE AND STRUCTURE
ANGLE TO CORE AXIS ALTERATION SULPHIDES REMARKS
52.G to66.1 (cont'd)
636.7-636.9, 637.0-637.1 S 637.2 - 5cm: Sillimanite rich grano diorite dykes. Intense biotite in QEP at irregular contacts.
637.4-638.3:Eg massive magnetic mafic dyke, same as 636.3 Sharp contacts, top (?
bottom l?•^4oi6
640.4-644,5:Qts clotted biotite rich garnetiferous (52) sone in GFP
642.0: 3cm qts healed breccia sone
648.3-648.4:Qts clotted (102) biotite/cord rich sone in QFP
655.0-657.0:52 qts clots (up to 2cm)over section causingintense biotite/cord atcontacts.
55' 25 0
fg anthophyllite over bottom 10cm in dyke.
652.0-653.0: Gradational sone in QFP with 52 sillimanite wisps
658.0-661.5:Patchy sillimanite (32)locally up to 52
Gradational decrease in alt. froa 661.5-662.0 to: 52 cloudy feldspars K2on) 202 cordierite
MOLE NO: ML-26 LOGGED BY: R.C.SIM PAGE: 18
DRILL HOLE LOG
FROM ROCKTO TYPE
52.6to666.1(cont'd)
GRAIN ANGLE TOCOLOUR SIZE TEXTURE AND STRUCTURE CORE AXIS ALTERATION SULPHIDES
3-5Z biotiteTr-17. anthophyllite25! muscovite255! qts eyes
REMARKS
665.6-666.4: Blocky ground with smooth fractures along
Possible fault zone
666.1 GABBROto862.0 .̂ J
Darkgreenwithwhitespots
fstoeg
chloritic joints 9 40-60"
Sharp upper contact l? 70 0Generally a massive mgtypical gabbro occasionallygrading to more coarseror finer grained varieties.
Typically chloritised Locally up to 1Z diss py.Epidote bleached feldsparsup to lOcffl
Locally up to 32 magnetite in irregular clots
667.8-668.1: Qts-granitic dyke with irregular top contact S 2nm hematite vein along sharp lower contact 9
668.9-669.0:Fg massive light greyfeld. phyric int. dyke 9
669.4-669.8: Fg massive mafic dyke, similar to 637.4 but no magnetite 8
669.85-670.5: White qtz dyke with sharp contacts, top (?
bottom l?
In finer grained ntat'l Mt has gone to leucoxene In coarser aat'l leucoxene is present in white rims aroung magnetite.
e
e
20'
80"
80"
85" 35"
HOLE NO: WL-26 LOGGED BY: R.C.SIM PAGE: 19
DRILL HOLE LOG
FROM ROCKTO TYPE
666.1toS62.0(cant 'd)
GRAIN ANGLE TOCOLOUR SIZE TEXTURE AND STRUCTURE CORE AXIS ALTERATION
677.5-680.0:Fg zone in Gb gradinqto eg at 680.0-681.5
SULPHIDES REMARKS
681.6-681.7: Siliceous granodiorite dyke e 70-75"
-J&83. 1-664. 684.2-685.0:Fg mg aassive wore evolved dioritic dykes with sharp chilled contacts @ 80 0
9 687.0m: gabbro becomes consistently medium grained,•assive 2 non-magnetic.
695.9: 5cm garnetiferous qtsvein 9 60"
27. qnt
1-23: leucoxene
diss py
5Z pyrite in l x 3cm chloritic vein at 684.95
Ir diss py.
Darkgreenwithwhitespots
-699. 2-700. 2:rFg massive mafic dyke, sane as 669.4 l?
704.9-705.7:Fg massive highly epidotebleached int dyke 9
Massive int/gabbroic dyke with sharp contacts 3 cut by granitic dyke at 720.6-720.9
724.9-725.8: Fg dyke, sane as 702.3 Contacts, top 0
bottom e
80"
75"
80 0
65" 75"
55C qts/ep/carb veinlets
HOLE NO: WL-26 LOGGED BY: R.C.SIM PAGE: 20
DRILL HOLE LOG
FROM ROCKTO TYPE
666.1to862.0(cont'd)
COLOUR
white8 pink
GRAINSIZE
mgtoeg
TEXTURE AND STRUCTURE
-;729. 5-730. 6:V tgr&A^Massive granitic dykeSharp contacts, top @
bottom @
ANGLE TOCORE AXIS ALTERATION
60"35"
SULPHIDES REMARKS
White
732.9-733.3:Fg int/gabbroic dykewith sharp contacts @ 70 (same as 720.3
Irregular qts/granitic clot/veins @
733.8 - 2cm734.2 - Sen
S 734.5-735.0
741.7-741.85:Banded felsic dyke cut by1031 ep veinlets.Sharp contacts "S 85 0
Aphan- 745.4-746.2: itic Massive qtz dyke, contacts @ 35-45"
l x 2cm py/cp clot at 734.6 associated with qts ve-ining
None
-1746.9-747.2:- ^ TL~ ̂ Blocky chloritic fault zone 8
O
e
-747.4-748.5:- ^ Granitic dyke with Gb xenolith at 747.7-748.2
748.5-748.6: Very blocky chloritic ground minor fault grunge Also 2cm similar nat'l at 748.7
'SO 0
70 C
747.1-747.2: Epidote vein
Fault
Note: intense qts/ep/ carb veinlets froa 747.2-751.5
Fault - looks very similar to zone which got rods stuck in UL-25
HOLE NO: WL-26 LOGGED BY: R.C.SIM PAGE: 21
DRILL HOLE LOG
FROH TO
ROCKTYPE COLOUR
GRAINSIZE TEXTURE AND STRUCTURE
ANGLE TO CORE AXIS ALTERATION SULPHIDES REMARKS
666.1 to862.0 (cont'd)
Unite S pink
755.7-755.9:Intense qts/carb veins f? 35 0
757.2-757.3:Blocky ground withfractures along qts/carb/ep veins ? 50"
760.0-760.6 S760.9-761.0:Fg massive int/ma dykes @Similar dykes at:768.1-769.0 (23! magnetite) 8 45"770.2-770.7 9772.0-772.1 l?777.4-777.7 9780.0-780.6 0
80'
40" 70" 20" 50 0 27. py over lower 10cm
777.0-777.1: - Granitic dyke l?
782.2-782.6:602 qts clots S veinsover section.
80'
75'
SO 0
-784.9-786.2:"Locally foliated qranitic dyke 9 '
783.8-789.6:Fq massive chloritic•afic dyke 9Similar dykes at: 790.6-790.7 790.9-791.5 8 799.0-799.5 (2Z Mt)
803.0-803.4:Feld. phyric int/mafic dyke 5 65"cut by 7 7. white qts veinsX clots
HOLE NO: WL-26 LOGGED BY: R.C.SIM PAGE: 22
DRILL HOLE LOG
e
FROM ROCK TO TYPE
666.1 to 862.0 (cont'd)
COLOUR
Dark green
GRAIN SIZE TEXTURE AND STRUCTURE
803.0-803.2: Pink i white granitic dyke ?
Fg massive chloritic mafic dyke (saae as 788.8) at
ANGLE TO CORE AXIS ALTERATION
75 0
SULPHIDES REMARKS
All with tr-lZ magnetite Dykes noted are probab syn-intrusive chilled
iy
e
c
e
e
Dark green
c
c
o
fg
803.9-809.6(10cm mg gabbro xenolith at 809.3)
809.8-809.9:
810.2-812.4:With gabbro xenoliths at 811.0-811.2 and 811.2-811.5 Lower contact marked by 7cm qta vein.
813.5-813.8 8
814.5-814.7:Siliceous granitic dyke,sane as 803.0 l?
817.1-817.9:Mafic dyke - same as above l?also at 819.9-820.0 ?
75
80"
SO 0 SO 0
825.5-826.0:Mg weak foliated intermediate SO 0 granitic dyke with 5cm gabbro xenolith at 825.9
829.7-829.8:Carbonate rich qts vein 1?
i831.2-832.6:r Massive weakly feld. phyric (32) chloritic mafic dyke ? 17. magnetite
40 0
80 0
gabbroic dykes or sills
Cut by 102 epidote veinlets
Eoidote bleached from 8io. 2-811.0
131 diss pyrite
HOLE NO: UL-26 LOGGED BY: R.C.SIM PAGE: 23
DRILL HOLE LOG
FROM TO
666. 1 to 862.0 (coni 'd)
ROCK TYPE
GRAIN COLOUR SIZE TEXTURE AND STRUCTURE
Similar dykes at 835.2-835.3 2 835.7-834.9 0
ANGLE TO CORE AXIS ALTERATION
20" SO 0
SULPHIDES REMARKS
Salt S pepper
mg
Whitewithorangewisps8 greyclots
f g
837.8-838.3:Massive granodioritedyke l?Similar dykes S veins at:839.3 - Scat !?839.9 - 3cn840.1 - 5cm840.3 - 3cm842.7 - 3cm
"70"
80"
.843.7-845.2:-Massive granodiorite dyke with 5Z orange hematite wisps in fractures 8 3 7. chlor/amphibole clots Klcm) with dif-fuse boundaries.
849.0-849.6:Fg mafic dyke, same asabove cut by granodioritedyke at 849.05-849.1 8849.3-849.35
J 850.2-851.4: - tzrt-ry? Very blocky ground with chloritic fractures l? Grungy fault mud at 851.2-851.3
852.3-852.8: Fg mafic dyke Q
849.5: Tr-lZ phlog wisps beqin in qabbro
Eaull70"
SO 09 853m: phlog content has increased to ± 57. defining foliation l? 80"
HOLE NO: WL-26 LOGGED BY: R.C.SIM PAGE: 24
DRILL HOLE LOG
e
e
e
e
e
FROM ROCK GRAIN ANGLE TO TO TYPE COLOUR SIZE TEXTURE AND STRUCTURE CORE AXIS ALTERATION SULPHIDES REMARKS
666.1 to 862.0 (cont'd)
362.0 TRANSITION Mottled i
854.4: 5cm granitic dyke l? SO 0
854.8-855.0: Feld. phyric int/mafic dyke @ 80"
Eg massive mafic dyke at 856.6-857.2 Q 80" 859.7-860.5 (? 70 0 2 7. diss po.
:g Gradational upper contact 5 7. w iscy clots of Noneto ZONE light S 864.0 GABBRO dark
green
marked by decrease in feldpsars to
phlogopite defining weak foliation S 80 0
863.0-863.1:Granitic dyke supporting502 host fragments
e
c
o864.0 MEIA-
c to PERIB-917.4 OTITE
e ^
0
c
c
c - ———— -HOLE NO:
C
Steel mgblue/grey towith egblackspots
Light fggrey
WL-26
bnarp contacts e so"
863.5-863.8:Composite fg massiveintermediate dyke cut . . - .by 202 granitic veinlets.Sharp contacts (? 30"
Typical massive magnetite Typically chloritic Nonerich (±20Z) ultra-maficunit. Upper contactgradational over 0.2mmarked by colour changeand occurrence ofmagnetite.10cm blocky ground atupper contact.
870.9: ICB chloritic mud P 85"Possible minor joint plane.
884.8-886.0:." *xib-?? ,Moderately foliated, locallyfeld. phyric (52) int. dyke @ 80"
LOGGED BY: R.C.SIM PAGE: 25
DRILL HOLE LOG
FROM ROCK TO TYPE
864.0 to 917.4 (cont'd)
GRAIN COLOUR SIZE TEXTURE AND STRUCTURE
S86.7-S86.85: Weak feld. phyric int. dyke
Zones often very blocky
ANGLE TO CORE AXIS ALTERATION
5 80"
Green S black intense
SULPHIDES REMARKS
Altered zones in Px maywith 3radational contacts over ±5cra
898.9-899.8:Salt S pepper massivegranodiorite dyke 9
904.1-904.4: Dark green magnetite rich (15X) mafic dyke. Sharp contacts (?
905.3-905.6:Mafic dyke, same as 904.1 with 5cm micaceous fault at 905.4 e
906.1-909.2:- -z^~ Intercolated intermediate feld.phyric X chloritic aafic dykes with px, very blocky over section Fault sone ?
80"
60"
50"
60 0
chlorite/biotite zones in Px. Patchy magnetite at
887.0-887.1"892.5-892.8893.4-893.7894.2-394.4894.8-895.4
901.3-901.5: Bio-chlor sone, sane as above
3-5ca biotite at contacts
represent selective alterations of cumulate layers in sill (regional alteration)
Fault zone P-895.2-895.4
7 -
fault
Chlorite/biotite rich zone, same as above at 911.0-911.5 S 912.6-913.3
HOLE NO: WL-26 LOGGED BY: R.C.SIM PAGE: 26
DRILL HOLE LOG
FROM TO
ROCK TYPE COLOUR
GRAIN SIZE TEXTURE AND STRUCTURE
ANGLE TO CORE AXIS ALTERATION SULPHIDES REMARKS
864.0 to917.4 (cont'd)
915.0-917.4:Fg non-magnetic maficto gabbroic chill soneto sill.Sharp lower contact @ 50
C
e
917.4 WEAK-MOD to ALTERED 1010.6 QFP
Greywithlightgrey towhitespots
Darkgreenwithwhitespots
e
c
c
c
c
mg Weak to moderatelyfoliated unit definedby qts eyes and biotite 3 75-80 020-252 qts eyes up to 3om
917.G-918.0:Fg chlorite/biotite richnon-magnetic mafic dyke.Probable related toupper chill sone 5 80"
919.4-919.6 8920.7-920.9:Massive, mg granodioritedyke @ - 40'
-922.1-923.6:!- f V b~ Massive weakly feldspar phyric O2) chloritic mafic dyke 8 80" Non-magnetic.
927.7-927.S:Composite mafic/graniticdyke 9 80"
Patchy visible feldspars(up to 32)Very weak altered to 928.3m72 biotite
202 cordierite Rare tr muscovite
None
e 928.3: Gradationally over 0.2m QFP becomes more intensely altered and has a more light grey colour. 5-72 biotite 30-352 cordierite 2-32 muscovite Tr-2% anthophyllite
Ir diss pyrite
HOLE NO: WL-26 LOGGED BY: R.C.SIM PAGE: 27
DRILL HOLE LOG
FROM ROCK TO TYPE
917.4 to 1010.5 (cont'd)
GRAIN - ANGLE TO COLOUR SIZE TEXTURE AND STRUCTURE CORE AXIS ALTERATION SULPHIDES
5 923.3 (cont'd): All qts is recrystallised in matrix giving lighter colour. Still patchy visible feldspars, locally up to 3X
REMARKS
r
Pink 8 white grantiic veins S dykes 8
933.4 - 3cm934.4 - 5cm935.0 - 5cm939.5-939.8 5 45"940.0 - Sen941.3 - 5cm
941.2-941.3:Eg chloritic mafic dyke
946.5: Sen sillimanite/•use rich siliceous dyke S 85"
947.2-947.5:Mg massive granitic stainedintermediate dyke 5 85"
Pink to white granitic to pegmatitic to granodiorite dykes at:
948.0-948.6
l-2% diss pyrite
37. muse.
948.6-94.89 (949.9-949.0:mafic dyke) 950.1-950.5 950.95-951.2 (951.35-951.4:•afic dyke) 951.4-951.8
garnetiferous
garnetiferous
HOLE NO: UL-26 LOGGED BY: R.C.SIM PAGE: 28
DRILL HOLE LOG
EROM ROCK TO TYPE
917.4 to 1010.6 (cont'd)
GRAIN COLOUR SIZE TEXTURE AND STRUCTURE
951.8-952.15: Moderately foliated weak granitic stained int. dyke
ANGLE TO CORE AXIS ALTERATION
S 80 0
SULPHIDES REMARKS
C
c
e
c
c
e
c
c
c
c
c
952.6-953.3:Eg massive chloritic,magnetic mafic dyke ? 80 0
954.0-954.1: Granitic dyke
956.2-956.4:Granitic stained int.dyke, same as 951.8 8 85"
Granodioritic to granitic dykes at:
956.9-957.2 0 75'957.5-957.65 0 75"957.7 - 5cm957.8-958.0958.2-958.7959.4 - Sen -961.3-961.3 !? 30-40'965.2 - 7cm966.7-966.8
: 967.1-968.5:'- 4? i b y Feld.phyric (102) massive intermediate dyke (? 80"
968.6-969.5:Grandodiorite dyke 9 60 0 Granitic to granodiorite dykes at:(irregular contacts)970.2-970.5971.8-972.1972.4-975.9 with 52xenoliths of host (-ClOco)
HOLE NO: UL-26 LOGGED BY: R.C.SIM PAGE: 29
DRILL HOLE LOG
FROM TO
ROCKTYPE COLOUR
GRAIN SIZE TEXTURE AND STRUCTURE
ANGLE TO CORE AXIS ALTERATION SULPHIDES REMARKS
917.4 to1010.6 (cont'd)
Mottled black i white
mg to eg
- 979 .5-981 . 0:-Coiaposite and highly mixed mafic X granodiorite dyke. Sharp contacts S
981.0-981.8:Well foliated fg int/raafic dyke with 5 7. chloritic clots (Onrn) defining foliation 9
J981. 8-984. 7:L ^IDT? Clotted to mottled well foliated intermediate dyke 0 Elongate siliceous clots up to lcm with cloudy edges eveloped in dark biotite/ amphibole matrix.
984.7-985.5: Weak feld. phyric •assive int. dyke
985.9-986.3: Granitic dyke Q
986.5: 7cm granitic dyke 9
986.6-987.1:Massive fg int/mafic dyke with 1 57. irregular grano- dioritic clots
987.3-987.4: Pegmatite dyke @
988.2-988.5:32 feld. phyric int/aafic dyke with 1051 granodiorite clots - same as 986.6
60 e
Rounded cloudy feldspar 'gloms* up to 5mm (3Z)
80 0
80"Tr-1% diss pyrite
85 0
25'
25"
350
HOLE NO: UL-26 LOGGED BY: R.C.SIM PAGE: 30
DRILL HOLE LOG
FROM ROCKTO TYPE
917.4to1010.6(cont'd)
GRAIN ANGLE TOCOLOUR SIZE TEXTURE AND STRUCTURE' CORE AXIS ALTERATION
988.&-989.0:257. i rregular granodioriteclots in QFP
SULPHIDES REMARKS
Orange/ pink with black spots
989.3-989.5:Massive fg chloritic maficdyke (? 85 C
994.8-995.1: Massive fg weak feld. phyric int. dyke Sharp contacts, top @
bottom l?
1002.0-1002.7:Massive fg chloritic maficdykeBlocky with fracturesalong 3Z carb veinlets
fg/ -1002.7-1006.0:- .'^ :---- nq Massive granitic/syenite
dyke e
85" 35"
80 0
9 990m: QFP composed of: 1031 qtz eyes Oiam altered to cordierite 20-35Z cordierite 3-57. anthophyllite 1-3X biotite 27. muscovite Patchy up to 2Z angular magnetite blebs Klmm) 3Z cloudy visible feld sparsAll qtz in matrix fg recrystallised Feldspars commonly weakly, pink stained.
Bottom contact narked by Sen granitic vein with 2 x O.Scn dark purple fluorite clot S 15Z epidote veins.
Rare trace diss pyrite Patchy 1-2Z rounded magnetite blebs *Qmn
Tr-1% diss pyrite 1Z magnetite '
HOLE NO: WL-26 LOGGED BY: R.C.SIM PAGE: 31
DRILL HOLE LOG
FROM TO
ROCK TYPE COLOUR
GRAIN SIZE TEXTURE AND STRUCTURE
ANGLE TO CORE AXIS ALTERATION SULPHIDES REMARKS
917.4 to1010.6 (cont'd)
Grey
1006.7: 5cm siliceous3ranitic dyke/vein ? 85"
1007.4-1007.S: Massive dark green mafic dyke fg matrix supporting 57. l ight green anthophyllite wisps ^cm
- 1007.8-1009.6:^ ^,D^ Moderate to well foliated weakly feld. phyric int. dyke (? 75" Cut by highly granitised int. dyke 5 1008.3-1009.0
1010.6 INTENSELY Mottled mg Mottled unit varying into ALTERED dark blue/ alteration intensity over1101.4 POSSIBLY grey to spaces of ^'0.5m.
MORE black Locally well foliatedMAFIC with defined by anthophylliteSEDIMENT light and micas ?
green but nore commonly a * ^i?"--"- ' wisps massive aggregate of
'.-.r, -5 a lteration minerals.
Generally: 40-502 cordierite 25-302 biotite/phloqopite 103: anthophyllite 10-302 recrystallised qtz
75-80* (similar to intermediatesediments)More intense zones are common (gradational) composed of: 10-152 anthophyllite •t-252 cordierite Up to 602 biotite/phloqopite
ots
1-22 pyrite blebs U2mm) NOTE: similar raat'l seen intermixed with sili ceous garnetiferous sediments in other holes Other mat'l of similar texture S composition has been seen at top of •ain QFP associated with Ladder Flow (UL1-4) (Pervasive altered sediment)
US0631 - whole rock
1010.7-1011.0:Massive coarse pegmatiticgranitic dykeIrregular contacts.
1020.7-1020.8: Granitic dyke with 10Z chlorite along fractures
52 muscovite 12 garnet
32 garnet
HOLE NO: UL-26 LOGGED BY: R.C.SIM PAGE: 32
c
c
c
c
FROM ROCK TO TYPE
1010.6 to 1101.4 (cont'd)
DRILL HOLE LOG
GRAIN ANGLE TO COLOUR SIZE TEXTURE AND STRUCTURE CORE AXIS ALTERATION SULPHIDES REMARKS
1023.1-1023.6: Weakly feld. phryic 5 7. anhedral garnets garnetiferous intermediate dyke. Sharp contacts 0 80-85"
C
c
c
c
c
c
Grey
1025.2-1026.1:Altered int/mafic dyke,massive with sharp contacts 5 75 0
f g -1031.5-1035.9^ ^ '^7massive weak altered feld. phyric int. dyke. Sharp contacts,- top 0 SO 0
bottom 5 45 0
Siliceous granitic dykes at: 1045.3-1045.4 @ 85 e
1047.6 - 5co l? 80"
32 diss py over top 0.2m57. garnet over top 0.2mwith poorly developedsiliceous rims.57. anthophyllite oversection.
1030.6-1031.5: Example of gradational intense to pervasive altered sone. Bio/cord/anth with O2 qt2
Rare tr gnt. 17. anthophyllite Garnetiferous qts veins at 1032.5 S 1033.0 K2cm)
1038.6-1039.0:Gradational sone containing42 anhedral pink garnets^lcm)
1048.3-1052.1:Gradational intense to perv- 2-3Z diss pyriteasive altered sone with Tr-1% po152 anthophyllite302 cordierite0-32 garnet502 biotite/phlogopite ,Up to 22 qts.
HOLE NO: WL-26 LOGGED BY: R.C.SIM PAGE: 33
DRILL HOLE LOG
FROM TO
ROCKTYPE COLOUR
GRAIN SIZE TEXTURE AND STRUCTURE
ANGLE TO CORE AXIS ALTERATION SULPHIDES REMARKS
1010.6 to1101.4 (cont'd)
Garnetiferous qranodioritic dykes at 1051.1-1051.15 and 1052.1-1052.6
e 1055m: begin to see siliceous cordierite altered zones with distinct but irregular boundaries average l-2cm up to 10cm in matrix same as above.
1070.9-1071.1:Eg massive mafic dyke @
1074.3-1075.9: Gradational zone of siliceous garnetiferous sediments, similar sone at 1079.2-1080.0
85"
1088.2: 15cm granitic dyke. Top contact marked by 5cm chloritic shear @
37. garnet
'Windows' contain:^52 cordierite3-57. garnetTr-12 magnetite inrecrystallined qts matrix.
17. pyrite in fragments
1066.5: 2cm x 0.5cm py clot in siliceous 'fragment'
Appear to be windows of siliceous patches in completely blitzed rocks
52 garnets with typical white silica rims
1080.0-1080.3:Anthophyllite pooraltered sone30-402 biotite/phlogopite502 cordieriteO2 anthophyllite
Variation in original composition?
9 1083m: gradation back to 10-152 anth. (as above)
65 0
HOLE NO: WL-26 LOGGED BY: R.C.SIM PAGE: 34
DRILL HOLE LOG
FROM TO
ROCKTYPE COLOUR
GRAIN SIZE TEXTURE AND STRUCTURE
ANGLE TO CORE AXIS ALTERATION SULPHIDES REMARKS
f
C
1105.6-1106.3:Feld. phyric int. dyke
1106.3-1106.6: Sediments
1106.6-1107.1: Feld. phyric dyke
1107.1-1111.4: Intercalated sedimentary xenolith ^Ocm in siliceous spotted dyke, similar to 1103.3 (very mixed)
1111.4 SILICEOUS Blue/grey fg Typical massive fg matrixto GARNET- 1276.3 IEEROUS
SEDIMENTS
with pink supporting up to 1 07. silica S white rimmed anhedral garnets, spots Gnts S silica often banded
1-2Z fine disseminatedmagnetite.
1113.1-1113.5: Spotted dyke, similar to above 5
1114.0-1115.3: Garnet free altered sediment (light seds) same as mat'l above.
1116.1-1116.2: Granodioritic dyke 9
1117.9-1119.5:-**- '.D/FD^ Spotted dyke, similar to above (altered int/felsic dyke)
80'
75"
Matrix composed of +50Z cordierite 103S biotite/phlog. 2-32 anthophyllite "305: qtaUp to 102 garnet Some localized zones contain no garnet but increased aiaphiboles S micas avg. 15-202 biotite/phlog Up to 52 anth. +502 cord "252 qts
27. pyrite in'clots S bands often associated with most intense garnet formation Tr-1% po in clots (very localized)
Magnetic !
US 0635 Whole rock
85"
Weak altered 37. gnt5Z anthophyllite 15Z cordierite Minor biotite
HOLE NO: WL-26 LOGGED BY: R.C.SIM PAGE: 36
DRILL HOLE LOG
c
*
t
c
FROM ROCKTO TYPE
1111.4to1276.3(cont'd)
COLOUR
Darkgreenwithwhitespots
GRAINSIZE TEXTURE AND STRUCTURE
fg -T1119. 9-1121. 6: - A ib^Massive feld. phyricint. dyke 2Similar dyke at1123.4-1123.7 @
ANGLE TOCORE AXIS ALTERATION
80 s
50"
SULPHIDES REMARKS
1125.4: 2 rare 5vm bands
C
c
c
c
t
c
c
c
c
c
of pyrrhotite at 70 0 to CA
Grey with white spots
fs
Dark grey with white spots
fg
1128.6-1128.9: Spotted int/felsic dyke, same as 1117.9 @
1129.1-1129.4: Weak foliated feld. phyric int. dyke (?
-1138.5-1139.6:'- # ,r,y Massive feld. phyric (102) intermediate dyke Sharp contacts (?
1159.1-1159.4:Salt S pepper massive mggranodiorite dyke 9
1159.7-1159.9:Feld. phyric int. dyke,same as 1138.5 S
1161.0-1161.8 S 1162.7-1163.0: Massive garnetiferous granodiorite dykes, same as 1159.1 but with irregular sharp contacts
-1170.0-1171.4: r Massive feld. phyric (72) int/nafic dyke. Sharp contacts l? Sediment xenolith at 1170.8-1170.9
85 0
70*
75 s
80
SO 0
75"
1153.8: 3cm x .5cm pyrrhotite clot/vein in sediments
35: anhedral 3arnetK4iBm)
HOLE NO: UL-26 LOGGED BY: R.C.SIM PAGE: 37
DRILL HOLE LOG
FROM 10
1111.4 to 1276.3 (cont'd)
ROCK TYPE
GRAIN COLOUR SIZE TEXTURE AND STRUCTURE
1173.9-1174.5: Weak foliated highly fcld. phyric (15Z) int. dyke @
ANGLE TO CORE AXIS ALTERATION
80"
SULPHIDES REMARKS
Grey withwhitespots
fq
Dark green
Grey withwhitespots
fg
-1176.6-1178.8:- 4 Massive weakly feld. phyric (2-3Z) int. dyke with sharp contacts 8 Sediment xenolith at 1177.8-1178.0 S qts veins at:
1178.0-1178.1 S1178.5-1178.6 e
ill81.8:*3cm chloritic blocky shear sone (?
1181.95-1183.0:Massive to weak foliatedchloritic aafic dyke 9
1186.5-1187.9: 502 sranitic to grano- dioritic clotting and veining over section.
^1187.9-1190.2:- ^: Massive weakly feld. phyric (331) int. dyke Sharp contacts 9
1199.1-1199.4: Massive garnetiferous granodiorite dyke with sharp contacts 8
80*
80"
75-80"
85 C
22 py clots in qtz
Possible shear
SO 01193.0: 2 - ICB x 1.5cm pyrite clots associated with garnet development in sediments
*60 0
HOLE NO: UL-26 LOGGED BY: R.C.SIM PAGE: 38
DRILL HOLE LOG
c
c
f
c
c
t
c
c
c
c
c
c
c
c.
c
FROMTO
1111.4to1276.3(cont'd)
ROCKTYPE COLOUR
Blackwithwhitespots
GRAINSIZE
f3
TEXTURE AND STRUCTURE
-1205.0-1206.8:;- *2t*:??Massive diabase dyke withsharp contacts, top 9
•bottom P
ANGLE TOCORE AXIS ALTERATION SULPHIDES
*57. carbonate spots85"40"
REMARKS
1213.7-1214.1: Massive eg garnetiferous granitic/granodioritic dyke S
1224.1-1224.4: Massive fg chloritic mafic dyke 8
1232.3-1232.9:Weak foliated, fg weakfeld. phyric int. dyke ?
1242.1-1242.4: -Granitic to granodioriticdyke @also at 1248.2-1248.3
8 * 1247m: silica rimmed garnets begin to fluctuate in occurrence and content example: 8.1248m seds composed of massive fg recrystallised mass of lS-20% amphibole, 10-15Z cord, 3 7. biotite, 2 7. magnetite, GO-70% qts. @ 1249m grades over 20cm to:30Z garnet * silica rims, often in bands f?
85"
85*
80 0e 1235n: silica rims about garnets begin to become pink granitic stained (to " 1251B)
Py content has increased to avg. 2-331 in clots associated with garnet development.
45*
Rare tr pyrite
Possible turbidite fluctuations in sedi ment composition or texture causing fluctuation alteration on IB scale, i.e. fg less to unaltered mat'l at top grading into more altered coarser nat'l below.
80"Ir-1% pyrite ^
HOLE NO: WL-26 LOGGED BY: R.C.SIM PAGE: 39
DRILL HOLE LOG
ROCK GRAIN TYPE COLOUR SIZE TEXTURE AND STRUCTURE
ANGLE TO CORE AXIS ALTERATION SULPHIDES
(? 1242s (cont'd): In fg mass of 5-10/J biotite, +202 cord. 22 magnetite, 502 qts. with abrupt change to similar mat'l as above at 1252.5si (pattern on rough scale exists to 1275m)
I255.8-125S.4: Garnetiferous (42) qranodioritic dyke @ also at 125S.4-125S.3 S
1259.9 - 7cm S 1260.&-I260.7: Garnetiferous grani- dioritic dykes.
12&3.4-1263.5 S 12&4.5-1264.S: White siliceous granodiorite dykes
85 0 65"
1254.1: 7cm sone with 122 pyrite in angular clots, seems to be associated with qts veins S clots
•1256.9-1259.0: 2-32 diss pyrite throughout
2 " 12Glra: begin decrease in garnet tc 3-52 'i locally o7.1~. Matrix grades from weak altered amoh 2 qts with minor bio/cord to 15-202 bio and +3S2 cord, (no magnetite)
2-42 oarnet
1274.0: 20cm sone with 82 oarnet with "banded* silica rims at 35" to CA
Gradational sone to int sediment unit, suggest: possible alteration variation defining different unit (?)
HOLE NO: UL-2S LOGGED BY: R.C.SIM PAGE: 40
n T? T 7 T unT r Ti.1 A A JL. i. n u M u jUl
FROM SOCKTO TYPE
1111 4to1276.3(cont'd)
GSAIM COLOUR S IZE
Dark qrev f qwithwhite/pink spots
TEXTURE AND STRUCTURE
1275.0-1276.3: " I r*'-'Massive weakly tsaqneticweak f eld. phvric ( 37.)int/aiafic dyke.sharp contacts, top @
bottom 8
ANGLE TO CORE AXIS
60"75 0
ALTERATION SULPHIDES
Cut by y/, e p/qts veinletsM mm uo to 2cm 2 1275.2
REMARKS
1276.3 INTER- to MEDIATE 1299.0 SEDIMENTS
Grey fg Generally a massive, equigranular, non descript unit with localised weak foliated patches defined by amphibcles or biotite. "602 unit composed of weak to unaltered amph S qtz (40X/60Z) with" minor bio S cord (same as 1248m) with altered patches C'40%) containing up to 20Z biotite +40Z cord1-2Z anthophyil-ite "407. qts recrvstallised
Ir diss pyrite
1286.5-1287.3: 152 qts veins ove: section Klcm)
20;: epidote ± qts veins over section KSinn)} also at 1291.5-1291.6
@ 129.2: several pink
2 1291m: seds begin to contain patchy magnetite 0-27. { rounded ';lmm)
silica rimmed ted 1garnets are present recrystallised pink garnet4. nW — utl
HOLE NO: LOGGED BY: R.C.SIM PAGE: 41
DRILL HOLE LOG
FROM TO
SOCK TYPE
GRAIN COLOUR SIZE TEXTURE AND STRUCTURE
ANGLE tO CORE AXIS ALTERATION SULPHIDES REMARKS
3 1297.2m: lOca section with 102 garnet shaped chlorite/ qts ± magnetite (retrograde garnets ?) with pink stained siliceous rims
1299.0 SILICEOUS Grey with fg 152 section comoosed of pinkto GARNET- 1309.0 IFEROUS
SEDIMENTS
pink S white bands S clots
stained silica rimmed garnet or partially retroqrade garnets (as in 1297.2) Garnetiferous zones avg. \0.2m separated by int. sedimentary mat ''l.
1300.0-1301.0: Granitic dyke @
1304.0-1304.1:Blocky, chloritic, qts veined possible minor fault sone ?
1304.9-1305.2: Granitic dyke S
Tr-12 pyrite disseminated in garnetiferous zones Patchy 0 -27. magnetite
27. gnt
Possible fault 7
SO" 32 qnt
1309.0 INTE8- to MEDIATE 1368.3 SEDIMENTS
Grey fg Contact marked by lastgreen to gnt/siiica patcheswith dk mg (Mineralogy chl-qtz-green hornblendeifeldspar)bands Local fabric (bedding?) @ 80-85 0occasion- marked by more chloritically streaks.
Predominantly a massive to weakly bedded (foliated) intermediate rock(greywacke) Magnetite 1-32 locally
1310.0-1310.5:Quarts healed (902)breccia vein 9 80"
Patches S sones of weak pervasive pink staining (hematite ?) 1-32 qts veinlets Minor epidote in vein- lets and in 1-lOcm oatches (x'12)
None Bedding appears to be alternating more chloritic bands S less chloritic bands on a mm scale.
No sulDhides
HOLE NO: UL-26 LOGGED SY: R.C.SIM/F.BALINT PAGE: 42
DRILL HOLE LOG
FROH TO
1309.0to 1368.3
ROCK TYPE
GRAIN COLOUR SIZE TEXTURE AND STRUCTURE
1312.6-1312.9: Granitic dyke @
ANGLE TO CORE AXIS ALTERATION
S5 0
SULPHIDES REMARKS
From 1317-1332.8: c -- -Numerous minor chloriticgouges S clay filledseams i.e. \lmni thick(57.) at various angles.At 1324.4: lcm clay gouge SS 1325.8: 0.5cm clay gouge i?
9 1325: bedding fabric 2
From 1325.0 down section, quarts veinlets prefer 30" to core axis, these veins make up about 10X of section (Icm-lOcm wide) and have horsetail like style.
Granite dykes at: 1328.6-1329.01330.3-1331.1 1331.5-1331.3 1333.5-1334.0 1335.0-1335.2 1346.0-1346.2 1347.0-1347.2
1350.0-1368.3: ^..-i.'V Numerous clay gouge zones •aaira 5 7. a t all "angles 10X veinlets of qts 8 OJD to 3cm)
1359.5: 3cm clay gouge S
1360.3-1360.4: Clay gouge
1360.8: lcm clay gouge
SO 0
Continued patches locally of mild oink silicification
Green chloritic patches l-4mm some with pyrite or pyrite gnt cores (0.5X ant)
Ir diss py locally (I mean only trace)
Granite dykes always have 5 7. quars veinlets associated
None From 1350 down section. numerous broken up zones Start of major structure
SO 0
HOLE NO: iJL-26 LOGGED BY: R.C.SIM/F.BALINT PAGE: 43
DRILL HOLE LOG
FROM TO
ROCK TYPE COLOUR TEXTURE AND STRUCTURE
ANGLE 10 CORE AXIS ALTERATION
1-27, c c veinlets
SULPHIDES REMARKS
1368.3 DIABASE to DYKE
Dark grey fg Massive diabase, good to black aphanitic chills.
Contacts @
None
1371.3 MAJOR to FAULT 1402.1 BRECCIA
ZONE
Green fg Massive to weakly foliatedwith intermediate sediment aswhite above with severeveinlets brecciation 8 quarts Quarts
veining. veiling Overall about 10-202 at quarts filling breccia 0-20 0 sones. to CA mm chlorite veinlets 5-102
Same as in above int. sed.Minor 'pinking up" weaksilicificationDoes not appear to besignificant alterationrelated to structure
None at all Literally O ROD entire section
Minor clay gouge zones l-2tnni. 1-22'at" 70-80 0
None General feeling that structure is at 20 0 to CA
52 granitoid dykelets- very pink-orange colourwith irregular -contacts.
From 13S6 down section to1402.1:Quartz filling increasesto 20-402 of section.
At about 1391: a marked increase in hematite vein lets.
From 1391-1400: 52 red brown hematite fractures lam scale Mild pervasive epidote alteration associated with hematite
None 1398-1401: assayed for Au
From 1391-1402.1: Rock is epidote altered fragments shot with quarts S hematite veininq
1402.0 DIABASE to DYKE 1404.9 ^
Bark grey fg to black
Massive with good Contacts aphanitic chills at Contacts sub-parallel 0-20 0 to core axis
Minor carbonate Possibly sane dyke asintersected higher inhole.Diabase definitely po;fault breccia intrude;quarts heal breccia.
HOLE NO: UL-2S LOGGED BY: F.BALINT PAGE: 44
DRILL HOLE LOG
FROM TO
1404.9to1430.7
ROCK TYPE
QUARTZHEALEDFAULTBRECCIA'T'--' -'
"' ' '
COLOUR
Palegreenwithwhiteveining
GRAIN SIZE TEXTURE AND STRUCTURE
fg 302 quarts filling voidsbetween epidote alteredangular fragments of cmscale proportions
ANGLE TO CORE AXIS
No realfabricto 1413
From 1413down
pr e domin ance ofveininqat 30 o"
ALTERATION SULPHIDES REMARKS
Pervasive epidote-silica Virtually no sulphidessoaked throughout brecciatedfragments.
Only very minor hematiteveinlets (marked differencefrom above diabase in lackof hematite)
From 1421 down section:2-37. very red pink stained.
1430.7 INTER-to MEDIATE1454.1 SEDIMENTS
Green Massive to weaklyfoliated (foliationresembles beddinqlocally)Identical to materialabove fault zone.
Granitoid dykelsts lcm to 10's of cm 5-102 of section, most near 90 0 to CA
Epidote in patches at top of section (20-307.) decreasinq down section. By 1434: 2-32 epidote
veinlets1-27. garnets locally Weak silicification with minor pink staining increasing down section.
Silicification appears to be granite related. A granitization of the sediments
More significant dykelets at: 1433.6-1433.8
1436.1-1436.61439.5-1440.0
At 1437.15: a 2cm band of J402 specular hematite semi- ]conformable ^L", probably ]a vein. l
Run for Zn S Au
Chloritic fractures 1 -57. still persist throughout the section.
Calcite vein 2mm-lcm from 1451.8-1454.0 S
angles
0-10"
Silicification (granitiza tion) intensifies down section
From 1440.0-1443.0:1-22 diss pyrite in blebsand along irregularstreaks
Geochem.
HOLE NO: WL-26 LOGGED BY: F.BALINT PAGE: 45
DRILL HOLE LOG
FROH ROCK TO TYPE
1454.1 GRANITEto1458.0 ^-^'
GRAIN COLOUR SIZE
Grey with mgwhitesoecklesfaintpink h ue
TEXTURE AND STRUCTURE
Weakly foliated qts-feldspathic granite-granodior iteCut by very massiveeg pink granitic dykes.Contact is very hasywith overlying silicifiedsediments
ANGLE TO CORE AXIS ALTERATION
Fabric Noneat 85 0
SULPHIDES REMARKS
None Typical of materialintersected inPick Lk. holes
other
E.O.H. End of Hole
LOGGED BY: E.BALINT PAGE: 46
G? V
HOLE NUMBER: WL-043MINNOVA INC.
DRILL HOLE RECORD IMPERIAL UNITS:DATE: 23-May-1991
METRIC UNITS: X
PROJECT NAME: WINSTON LAKE (NORTH) PROJECT NUMBER: PN370 CLAIM NUMBER:
LOCATION: N.OF WINSTON DEPOSIT
PLOTTING COORDS GRID: WINSTON MINENORTH: 12200.DONEAST: 10130.OOEELEV: 10502.00
COLLAR GRID AZIMUTH : 270* O' O"
ALTERNATE COORDS GRID:NORTH: 0+ O EAST: O* O ELEV: 0.00
COLLAR ASTRO. AZIMUTH : 250* O 1 O"
COLLAR DIP: -87* O 1 O"LENGTH OF THE HOLE: 438.00m
START DEPTH: 0.00mFINAL DEPTH: 438.00m
DATE STARTED:DATE COMPLETED:
DATE LOGGED:
June 12, 1988June 22, 1988June 18, 1988
COLLAR SURVEY: NOMULT I SHOT SURVEY: YES
ROD LOG: NO
PULSE EM SURVEY: NOCAPPED: NO
HOLE SIZE: NO
CONTRACTOR: MORISSETTECASING: 3.65m INTACT
CORE STORAGE: CLEAVER LAKE
PURPOSE: TESTING RAFTED WINSTON STRATIGRAPHY BELOW SURFACE DEEPEM LIMITS.
COMMENTS
Depth (m)
0.0078.30130.10182.00224.60285.60328.30360.00392.30428.9021.9067.60113.40159.10204.80250.50296.30342.00387.70433.40
Astronomic Azimuth
.---------
250* 0'266' 0'244' 0'236' 0'234* 0'233* 0'230* 0'228* 0'230* 0'233* 0'
Dip degrees
-87* 0'-86* 0'-83* 0'-79* 0'-75*30'-72* 0'-71* 0'-69* 0'-67* 0'-62* 0--86* 0'-85* 0'-82* 0'-80* 0'-76*30'-74* 0'-71* 0'-68* 0'-64*30'-61* 0'
Type of Test
ACIDACIDACIDACIDACIDACIDACIDACIDACIDACIDMULT I SHOTMULT I SHOTMULT I SHOTMULT I SHOTMULT I SHOTMULT I SHOTMULT I SHOTMULT I SHOTMULT I SHOTMULT I SHOT
FLAG Comments
OKOK DOUBLE LINEOKOKOKOKOKOKOK WOWOK
OKOKOKOKOKOKOKOK
Depth Astronomic (m) Azimuth
Dip Type of FLAG Comments degrees Test
^ i i i i dzfzHOLE NUMBER: WL-043 DRILL HOLE RECORD LOGGED BY: D. COURTNEY PAGE:
HOLE NUMBER: WL-043MINNOVA INC.
DRILL HOLE RECORD DATE: 23-May-1991
FROM TO
ROCK TYPE TEXTURE AND STRUCTURE
ANGLE TO CA ALTERATION MINERALIZATION REMARKS
0.00TO
1.00
OVERBURDEN
1.00TO
281.60
PILLOWED MAFIC FLOW Fine grained, dark green, mafic flow. Nicely
preserved pillows. Hb, plag and qtz, distinct selvedges every 10cm-1m consisting of laminated (mm-cm) bhle: qtz/plag with minor calc and local epidote.Mild to strong fabric 3 ........................
1.0-2.2Blocky Fe stained core (close to surface).
21.85-22.2Two barren white qtz veins (3cm) S
37.0-37.15 Barren white qtz.
66.2-66.5Barren white qtz irregular contacts.
73.45-74.55Barren white qtz - ragged - irregular bleb.
90.5-103.5Flow becomes more massive, fewer selvedges. Homogeneous, almost medium grained - starts to look like GB. Strong foliation a ............................
103.5Material becomes pillowed again as described
above (1.0-90.5) typical BMA. Strong fabric a .............................
28
35
41
44
Unaltered hydrothermally, IX qtz/carb veinlets.Epidote bleaching of some pillow coresMinor carb'n in pillow selvedges.Local minor chlorite.Local pink punky gnt (mm-cm) in some
selvedges representing inter-pillow sediment.
13.3-13.35Strong epidote bleaching with qtz (selv ?).
31.215X punky pink gnt in hb rich
selvedge - over 4cm.
55.6Gnt as above over 6cm.
Trace Py (diss). Typical BMA.
Geochem 23.5-26.5.25.13X Py with qtz in selv.
Geochem 54.0-57.0.
HOLE NUMBER: WL-043 DRILL HOLE RECORD LOGGED BY: D. COURTNEY PAGE: 2
HOLE NUMBER: WL-043MINNOVA INC.
DRILL HOLE RECORD DATE: 23-May-1991
FROM TO
ROCK TYPE TEXTURE AND STRUCTURE
ANGLE TO CA ALTERATION MINERALIZATION REMARKS
132.7-132.8 S, 133.4-133.5Barren white qtz veins - crosscutting 3
154.3-154.4Qtz/fsp/chl 'bleb 1 - selvedge.
163.1-163.35Irregular coarse white qtz/fsp 'bleb'.
175.7-175.85Irregular 'blob' of very coarse fsp.
179.4-179.55Very coarse irregular fsp-qtz blob.
193.7-194.0Very coarse irregular patch of qtz and fsp.
J203.8-203.9|.Brecciated carb, chlorite and minor qtz. Probable healed fault, attitude ?
225Strong fabric persists a ................
227.6-227.7Pegmatitic calcite vein - irregular.
248.0-281.4Flow becomes more massive - fewer pillow
selvedges.
281.4-281.6Qtz/chl breccia, attitude = ?Chosen as contact which is otherwise ambiguous.
45
3X Po here (clotted) < IX Cpy diss. Geochem 133.2-136.2.
Geochm 179-182.
201.3-209.53-5X mostly random 1-4mm calc/qtz veining.
203.5-204.5 Carb'd.
Geochem 218.6-221.6.
42
Broken core.
Fault bound contact.
HOLE NUMBER: WL-043 DRILL HOLE RECORD LOGGED BY: D. COURTNEY PAGE: 3
HOLE NUMBER: WL-043MINNOVA INC.
DRILL HOLE RECORD DATE: 23-May-1991
FROM TO
ROCK TYPE TEXTURE AND STRUCTURE
ANGLE TO CA ALTERATION MINERALIZATION REMARKS
281.60TO
315.70
GABBROMedium grained, dark green, mafic intrusive. Mild to moderate fabric a ..................Hb, plag, qtz, leucoxene. Typical Zenmac GB. Homogeneous, equigranular.
298.0-298.1Qtz vein crosscutting 3 ....................
308.85-308.9 Qtz/chl vein 3
49
60
50
T-3% qtz/carb veining, 1-25J leucoxene, local tr hem staining.
Trace disseminated Pyrite.
315.70TO
317.20
BEDDEDINTERNEDTUFF
Fine grained, grey green, bedded and massive felsic to intermediate ash,Ashy looking under magnification, mm-cm siliceous fairly coarse beds 3 .............................
315.7-316.3 Nicely bedded.
316.3-317.2Massive, homogeneous, fine sugary siliceous groundmass. Sharp intrusive contacts a ......................
57
Local epidote (near upper contact).Chloritized.Biotitic mafic component 5-8X.No obvious hydrothermal alteration.Minor secondary carb'n.
diss Primary bedded Pyrite. Sawn and geochemed raft.
4060
317.20TO
347.95
GABBROFine to coarse grained, dark green mafic intrusive, homogeneous, equigranular. Typical Zenmac Gabbro. Local cm round hb 'knubblies 1 .
347.95-348.0, 348.4-248.45 Z 349.2-349.25 Chlorite grundge filled faults a ..........
IX qtz/carb veining, trace leucoxene.
341.2-247.955X wispy chlorite.
Trace Pyrite.
Gradationsl lower contact.
406090
HOLE NUMBER: WL-043 DRILL HOLE RECORD LOGGED BY: D. COURTNEY PAGE:
HOLE NUMBER: WL-043MINNOVA INC.
DRILL HOLE RECORD DATE: 23-May-1991
FROM TO
347.95 TO
354.30
354.30 TO
355.40
355.40 TO
385.45
385.45 TO
389.05
ROCK TYPE
TRANSITION ZONE *TZ*
GABBRO ttGBn
PILLOWED MAFIC FLOW *BMA7BSF*
GABBRO *GB*
TEXTURE AND STRUCTURE
Fine to medium grained, dark grey green mafic to nearly ultramafic intrusive. < 105S fsp, mostly massive, locally -cbl spots C1cm) typical Tz. Gradational contacts.
Material returns gradationally to medium grained, mildly foliated gabbro fabric a ....... ...........Dark green, homogeneous, equigranular. Sharp
Fine grained, and locally medium grained, dark green pillowed mafic. Well developed fabric a .........................Local irregular qtz/fsp gloms 1-3cm (BS's ?) Distinctly pillowed with mm-cm laminated hb vs.
qtz/fsp, material also locally displays 30X mm blue qtz spots over 20cm (function of pillows ?)
361.45-361.6 Pink massive GR peg a ...........................
377.55-377.75 Coarse grained white GR dyke 3 ..................
4382.0-382.3l- *ALT CRT* 4382.85-383. 1(. *ALT CRT* Intermediate composition. Bedded mm-cm with siliceous laminae.
Medium grained, dark green, mafic intrusive, moderate fabric a ................................Homogeneous, hb "knubblies 1 5-8mm.
387.2-387.4 35X injected white qtz. Sharp contacts 3 ................................
ANGLE TO CA
45
45
60
60
65
67
65
ALTERATION
Chloritized amph.
Unaltered hydrothermal ly 1-2/K hairline qtz/carb veining. Local very weak epidote bleaching. Trace leucoxene.Local pink punky gnt in interflow
sed/tuffs. Local weak bio development (hydrothermal ?)
3-5X transluscent fibrous anth. Cord, eh l, hydrothermal ?
Trace leucoxene.
MINERALIZATION
Nil.
Nil.
Trace - 1X diss Py.
2X bedded disseminated Pyrite and approximately 5X fine bedded sph, trmt.
Nil.
REMARKS
Geochem 361.8-364.8.
Altered seds in fresh host ? Sawn and geochemed. 2070 t 2020 Zn.
HOLE NUMBER: WL-043 DRILL HOLE RECORD LOGGED BY: D. COURTNEY PAGE:
HOLE NUMBER: WL-043MINNOVA INC.
DRILL HOLE RECORD DATE: 23-May-1991
FROM TO
ROCK TYPE TEXTURE AND STRUCTURE
ANGLE TO CA ALTERATION MINERALIZATION REMARKS
389.05TO
391.65
BEDDED, ALT INTERNED TUFF *ALT CRT*
Fine grained, grey green, with beige, blue and pink. Bedded intermediate tuff (mm-cm) fairly coarse bedding with local delicate beds -'ashy 1 looking.Intermediate overall composition. Moderate fabric
coincident with bedding 3 ........................
Unaltered to 390.5 then material displays, 1-3X fine anthophyllite. 3-8X pink gnt/qtz knots (nm-2cm). 8-12* ph log, cord ?
1-3X bedded disseminated Pyrite, 1X fine bedded Po., Tr bedded fine sph, tr mt.
Two geochems sawn.
389.05-390.5 S, 390.5-391.65
472 -t- 480 Zn68
391.65TO
392.80
PILLOWED MAFIC FLOW Fine grained, fresh foliated mafic, probably
pillowed (one or two) with laminated selvedges and spotted qtz rich cores ? Identical to material in 385.45-389.05. Dark green, hb rich.Fabric and conformable contacts 3 ...............
No hydrothermal alteration, 1X mm-cm punky pink gnt.
1X fine disseminated Pyrite. Thin flow intercalated with tuffs. Tuffs are preferentially altered !? Geochemed.
69
392.80TO
394.00
ALTERED BEDDED FELSIC TO INT TUFF wALT CRT*
Fine grained blue grey bedded tuff. Intermediate composition. Nicely bedded mm scale but not cherty. Moderate fabric, bedding and contacts alla ................................................
Hydrothermally altered. > 15X muse/ ph log fine grained, cord? 5X fine blades of transluscent anth.
Trace fine Pyrite. Trace very fine sph ?
70
Sawn and geochemed.
366 Zn.
394.00TO
395.85
PILLOWED MAFIC FLOW Fine grained, dark green, fresh mafic. Possibly
pillowed.Very similar to material seen at 355.4-385.45. Moderate to strong fabric and contacts a .......
No hydrothermal alteration. Local weak epidote bleaching, IX fine leucoxene.
IX disseminated intrafolial Pyrite. Another thin intercalated flow geochemed.
70
395.85TO
400.25
ALTERED BEDDED INTER MEDIATE ASH *ALT CRT*
Fine to medium grained altered tuff, quite homogeneous.Blue grey beige. Bedding probably obscured by
alteration, or otherwise poorly defined.
396.0-396.1Qtz fsp vein a ...............................
397.4-397.55 White qtz vein a
397.7-398.9Material becomes medium to coarse grained (function of alteration ?)
Somewhat diffuse lower contact 3
70
75
70
Strong hydrothermal alteration up to 50X cord.5-15X phlog/bio, 5-15X phlog/bio. 10-20X anth, up to 15X punky pink gnt. 2-6X muse, local chlorite.
396.1-396.615X punky pink gnt < cm.
Trace Pyrite. Trace Po.
Intercalation of rock types suggests two source areas. Unit is sawn.
395.85-397.65 397.65-398.9 ft 398.9-400.25
IX Po, tr Py with vein.
HOLE NUMBER: WL-043 DRILL HOLE RECORD LOGGED BY: D. COURTNEY PAGE:
HOLE NUMBER: WL-043MINNOVA INC.
DRILL HOLE RECORD DATE: 23-May-1991
FROM TO
400.25TO
438.00
ROCK TYPE
PILLOWEDMAFIC FLOW•KBMA/GB ?*
E.O.H.
TEXTURE AND STRUCTURE
Fine to medium grained, foliated mafic flow.Pillowed with diffusely laminated mafic vs felsic
zones 10-30cm. Also displays epidote bleachedpi l low cores ?Moderate to strong fabric 3 .....................
416.5-438.0Material becomes homogeneous, ie. pillowevidence dissappears.
428.2-438.0Fairly leucocratic.
End of Hole.
ANGLE TO CA
72
ALTERATION
Weak patchy hydrothermal alterationPatchy bio development up to 30/t.Local <cm punky pink gnt -(hosted in
hb rich fresh mafic ?).Local epidote bleaching.WU leucoxene.1-2X qtz veining (1-4cm).
Trace local bio.Trace local gnt.
MINERALIZATION
Trace Pyrite.Rare tr Cpy.Locally spotted with 1-3X 1-3mn
subhedral mt (20cm zones).
416.4Mm spots of Cpy in silicified pillow
core ?
438.0Trace 'clotted 1 Cpy with qtz bleb.
REMARKS
Geochem 404.5-407.5.
Geochem 432.0-435.0.
HOLE NUMBER: WL-043 DRILL HOLE RECORD LOGGED BY: D. COURTNEY PAGE:
WL-26
h-(X)[^CD 00K)
11
ootD
1 (^
7i
(D 00K)
CD m
DRILL SECTION( in the plane of the drill hole )
WL-26
SCALE: 1:5000
TB 386770
TB 386767
TB 386769
TB 386768
TB 38676
enLO
C\i
roin CN
DRILL HOLE LOCATION PLAN
WL-26
SCALE: 1:5000
TB 9317TB 535914
35m
WL-08
l85m
l
TB 535915
TB 9301 TB 9300
DRILL HOLE LOCATION PLAN
WL-08
SCALE: 1:5000
WL-08
O K) O)
m
T̂—
O)
K)in00
DRILL SECTION( in the plane of the drill hole )
WL-08
SCALE: 1:5000
-
TB 646434
TB 646432
WL-435m—*""—-.
125m
TB 386802 TB 646433 TB 646427
TB 386799 TB 386800
DRILL HOLE LOCATION PLAN
WL-43SCALE: 1:5000
Ministry ofNorthern Developmentand Mines
•(ructions
Ontarioho.
W9140* 16042DMNW0eil 29 PAYS PLAT LAKE
Mining Act Report of Work900
Name and Address of Recorded Holder
MINNOVA Inc.
SUITE 700, 4 KING STREET, WEST, TORONTO, ONTARIO M5H 3X1
Prospector's Licence No.
T-556Telephone No.
(807)623-1511Summary of Distribution of Credits and Work PerformanceMining Division
THUNDER BAY^^j^!-A[eanOPE LAKE AND
CPAYS PLANAREATofok&ssfissmerTTCredits Claimed
(Check one only)
[~] Manual Work,— Shaft Sinking Drifting or other U Lateral Work
f] Mechanical equipmentr—. Power Stripping other than Manual 1 _ 1 (maximum credit allowed - 100 days
Qjj Diamond or other Core drilling
[ ]Core Specimens
KPrefix
lining ClaimNumber
WorkDays Cr.
KPrefix
lining ClaimNumber
WorkDays Cr.
MPrefix
ning ClaimNumber
WorkDays Cr.
Dates when work was performed
To: AUGUST^! 988Total No. of Days Performed Total No. of Days Claimed
0
Total No. of Days to be Claimed at a Future Date
Qf^O OO L I 1?
All the work was performed on Mining Claim(s): indicate no. of days performed on each claim. ^JSee note No. 1 on reverse side)fining Claim
TB 646435No. of Days! Mining Claim No. of Days
2196I TB 646438 381
Mining Claim No. ol Days
TB 386768J 1312Mining Claim
TB 646439No ol Days
996
Mining Claim No. ol Days
TBL5359H 1378Mining Claim No. of Days
Mining Claim
IB. 646431Mining Claim
No. of Days
—.328.No. ol Days
Mining Claim
JB-64fi433Mining Claim
No. of Days
- 1437..No. ol Days
Required Information eg. type of equipment, Names, Addresses, etc. (See Table on reverse side) If space below is insufficient, attach schedules with required information and location sketchesDDH WL-08 TB 535914 1378 Ft. Oct. 19th- Nov. 8th, 1983 MCKNIGHT DRILLING CO. Ltd.DDH WL-26DDH WL-43
-DDH WL-44
DDH WL-46
TBTB
TBTBTBTBTB
386768
646433646435646438646439646431646435
13121437
984381996328
1212
Ft.Ft.
Ft.Ft.Ft.Ft.Ft.
JulyJuneJune
23rd12th25th
- Sept. 13th, 1985- June- July
22nd,22nd,
11
Total Footage DDH-WL-44July 25thTotal Foe
- Aug. 30th,
988988
ST. LAMBERT DRILLING CO. LTD.N. MORISSETTE CANADA Inc.N. MORISSETTE CANADA Inc.
2361'1988
)tage DDH WL-46 1N. MORISSETTE CANADA Inc.
540'
^KNIGHT DRILLING co. LTD.,'11 BRUCE STREET, P.O. BOX 906, iAILEYBURY, ONTARIO POJ 1KO
ST. LAMBERT DRILLING CO. LTD.,P. 0. BOX 473VALLEYFIELD, QUEBEC J6S 4V7
N. MORISSETTE CANADA Inc. 310 NIVEN ST. P.O.BOX 789 HAILEYBURY, ONTARIO POJ IK
:ertification of Beneficial Interest * (See Note No. 2 on reverse side)1 hereby certify that, at the time the work was performed, the claims covered in this report of work were recorded in the current recorded holder's name or held under a beneficial interest by the current recorded holder.
Date
MAY 28th,
''1
1991RecoMl&rfH^Mer fif A lent (Signature)
serlification Verifying Report of Work IAN R.MORRISON - AS AGENT
i hereby certify that l have a personal and intimate knowledge of the facts set forth in the Report of Work annexed hereto, having performed the work jr witnessed same during and/or after its completion and the annexed report is true.Jame and Address of Person Certifying
IAN RJ MORRISON -AGENT FOR -MINNOVA Inc. 2606 VICTORIA AVENUE, EASTTHUNDER BAY, ONTARIO P7C 1E7 Telephone No.
807-623-1511Date
MAY 28th, 1991or Office Use OnlyWork Assignments ONTARIO
GIS- ASSESSMENT HLF.S
JUN 1 8 B91
IAN By' MORRISONReceived Stamp rv*
CO
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