4IN01SW0861 NORBERG 010

Diamond Drilling

Area NORBERG(Former Twp.27 R.13)

Work performed by: Tribag Mining

Report N9 f O

Claim NQ

SSM.62209

SSM.62194

Hole NO

EB-22 EB-23 EB-24

X-23

Footage

553' 560.7 1 321'

105'

Date

July/64 July/64 Aug/64

Nov/64

Note

VH-

Notes:

•-WL 005(7 69" fcv 9 72

DIAMOND DRILLING

Contractor: Continental Diamond Drilling Co. Ltd. P. p. Drawer 250 Rouyn, Quebec

Core Size: AX 1-5/16""

Hole No.

EB-20

^EB-21

'EB-22

) EB-23

l EB-24

Angle

-90 o

-90 0

-90 0

-90 0

.550

Length

541.0

762.5

553.0

560.7

321.0

Total: 2,733.2'

Dates

May 3-6, 1964

May 7-13,1964

July 14-21,1964

July 2S-Aug.9764

Aug.6-Aug.10/64

Claim

62209

PROPERTY:

LOCATION:

DIAMOND DRILL LOG

Tribaq Mining Co. Ltd. HOLE NO. EB-22

Batchawana Bay. Ontairo

LATITUDE: 6750'E DIP; 89"

DIP COLLAR: 90 0

FOOTAGE

DIP TEST

READING CORRECTED

DEPARTURE: 2250'S

ELEV.:

DEPTH: 553.0*

AZIMUTH:

COMMENCED:July 14/64

FINISHED; July 21/64 LOGGED BY; M. Blechc.

SAMPLE NO. DESCRIPTION

0.0 Casing 6.0

6.0 Brecciated Zone- 60% fine grained green volcanic material; 35%-reddish acidic, felsitic and rhyolitic fragments (l^"-2"); 2-3% incerstitial quartz carbonate. Low chloritization and carbonatization; weakly mineralized with trace chalcopyrite, pyrite, aCnd minor traces of MoS a associated with quartz. Minor epidotization. The chalco pyrite occurs in small widely scattered blobs and specks, and finely disseminated in basic fragments. Minor scattered patches of magnetite.52.0 - Rhyolite? Pinkish grey, aphanitic, faintly banded at 30 0 c.n. Probably a large fragment. No mineralization. 54.5 - Brecciated Zone. An abrupt decrease of acidic material to less than S'i; rock consists of fine grained fragmented, green, volcanic material, with S-4% quartz carbonate; S-7% epidote stringers and patches; low-medium chloritization and carbonatization. Locally vuggy. Trace chalco pyrite throughout with concentration between 59.4-60.7 (51 cpy). The zone contains long relatively massive sections of volcanic rock.72.0 - Fragmented volcanics. Relatively low fragmentation, low alteration. l * quartz carbonate stringers, minor epidote, trace chalcopyrite.76.0 - Fragmented Volcanics. Fragmentation increases, rock becomes lo-medium chloritized, carbona-ized and epidotized. Note 0.5' of high wet-type chloritization at 97.0-97.5. Trace chalcopyrite throughout. 100.5

100.5 Felsophyre - Pale green, medium sericitized porphyritic dyke, with 10% rounded, sericitized phenocrysts 11-5 mm.); finely disseminated pyrite throughout. Note: galena and sphalerite in a 1/16" wide carbonate stringers at 101.1. 100.4 As above - sericitization decreases, rock becomes pink, relatively fresh and massive. 111.5

111.5 Fragmented volcanics, as at 76.0.119.0

119.0 Fault Zone. High shattering, high chloritization, carbonatization and hematite staining. Numerous striated slip planes.

DUPLICATE COPYPOOR QUALITY ORIGINAL

TO FOLLOW

PROPERTY:

LOCATION:

Latitude:

Departure:

Elevation:

Azimuth:

9DIAMOND DRILL LO(

Tribag Mining Co. Ltd.

Batchftwana Bay, OntarioDip at collar

6750 'B Dip: at 55090

Footage

HOLE NUMBER: EB-22

DIP TESTS

Reading Corrected

2250*3

SAMPLE NUMBER

C.O

6.0

100. 5

111,5

119.0

Depth: 553-0*

Commenced: July 14, 1964

Finished: July 21, 1964 Logged by: M,

DESCRIPTION

Caning 6.0Breeeiated Zone - 60# fine grained green volcanic taiterial; 355S-reddish acidic, felsitic and rhyolitic fr (lX8*-2")s 2-3# interstitial quart* carbonate. Low chloritization and carbonatiaation; weakly mineralised with trace chalcopyrite, pyrite, and rainor traces ol associated with quarts. Minor epidotization. The chalco pyrite occurs in small widely scattered blobs and sjecks, and finely disseminated in basic fra^nonts. Minor scattered patches of nagnetite.52.0 - Rhyolite? Pinkiah srey, aphanitic, faintly landed at 300 c.n. Probably a large fragment. Wo mineralisation 54.5 - Brecciated Zone. An abrupt decrease of acidj material to less than 5#; rock consists of fine grained frafjmented, green, volcanic material, with 3-45^ quarts carbonate! 5-7# epidote stringers and patches5 low-eodiuachloritiaation and carbonatization. Locally vuggy, pyrite throughout with concentration between

cpy.). The zone contains long relatively masoive aectio:of Volcanic rock,72.6 - Fragraented volcanics.low alteration.

Relatively low fragnenbatlon,quarts carbonate stringers, mino r epidote

trace chalcopyrite.76.0 - Fragmented Volcanico. rraipaentation increases, rock beconeo low-raedluia chloritiaed, carbonatlxed and epi iotiaed. Note 0.5* of high wet-type chloritization at 97.0-97-5. Trace chalcopyrite throughout.100.5Fol.oophyre - Prle ffreen, D^diua serlcitiaed porphyritic dyke,with 10?. rounded, aericitised ph*nocrysts (1-5 ran.) j finelydlaeerainated pyrite throughout. Kotei galena and sphaleritein a 1/161* wide carbonate otringera at 101.1.100.4 As above - sericitization decreases, rock bocoaeapink, relatively fresh and laaaslve.ill. 5Fraswentod volcanics, ao at 76.0.119.0Fault Zone. High shattering, high chloritiaation, cirbonatiiatioiand hematite staining. Numerous striated slip plane a,

Trace ci* .7

alco-

Sheet No. 2.___________________________________________Hole HO- EB-22

DESCRIPTION ______ ^^^^

121.0 - Carbonate vein, coarse grained, heavily stainedby hematite. Fracturing at 80 0 c.n.122.5 - As at 119.0124.0

124.0 Fragmented Volcanics. Low-medium patchy chloritization,carbonatization and epidotization. Minor traces ofchalcopyrite and magnetite throughout. 1-21 quartzcarbonate. Note: 11 chalcopyrite between 141.3-145.0.143.0 - Fragmented Volcanics. Fragmentation and alterationdecrease to low. Trace pyrite. The zone includes weaklymineralized medium fragmented and carbonatized zonesfrom 148.0-149.0 and 152.5-152.0.154.7

154.7 Mineralized Fragmented Zone. 1-21 chalcopyrite in a highlyfragmented, predominantly fine grained volcanic rock3-41 quartz carbonate, low chloritization, mediumcarbonatization and epidotization. Trace MoSj l11 red acidic fragments.172.5- As above, but red acidic (felsitic and rhyolitic)material increases to 30-401, with corresponding increasein mineralization to 1-21 chalcopyrite, trace MoS 2 ,5-7* quartz carbonate.194.5

194.5 Andesite - green, fine-medium grained, amphibolitized andfoliated at 75-80 0 c.n.197.0

197.0 Brecciated Zone- Predominantly volcanic material, withless than 51 felsitic fragments. 2-31 quartz carbonat,minor epidote, trace chalcipyrite, minor traces MoS 2associated with quartz carbonate. Note: 21 chalcopyritebetween 212.8-214,1. Low chloritization throughout.214.1

214.1 Fragmented Volcanics (Andesite). Low-medium fragmentation,low-medium carbonatization, minor eipdote, trace chalco pyrite throughout. Low chloritization.256.0

256.0 Felsophyre, greenish pink, low-medium sericitization.101 dark green sericitized anhedral phenocrysts.Upper contact brecciated the dyke contains an inclusionof fragmented volcanics from 260.2-261.3.261.3

261.3 Green Dyke - Probably a sericitized phase of the abovefelsophyre. 51 very finely disseminated pyrite.Medium sericitization massive. Trace sphalerite andchalcopyrite. Becoming pinkish and relatively fresh nearend.281.5

281.5 Zone of Fragmentation - green, predominantly volcanicmaterial, medium chloritization, carbonatization,1-21 quartz carbonate, minor epidote, trace chalcopyrite,MoS, .

DUPLICATE COPYPOOR QUALITY ORIGINAL

TO.FOLLOW

Sheet No. 2. Hole NO- EB-.

DESCRIPTION

121.0 - Carbonate vein, coarse grained, heavily stained by hematite. Fracturing at 80 0 c.n. 122.5 - As at 119.0 124.0

124.0 Fragmented Volcanics. Low-medium patchy chloritization, carbonatization and epidotization. Minor traces of chalcopyrite and magnetite throughout, l-2% quartz carbonate. Note: l* chalcopyrite between 141.3-145.0. 143.0 - Fragmented Volcanics. Fragmentation and alteration decrease to low. Trace pyrite. The zone includes weakly mineralized medium fragmented and carbonatized zones from 148.0-149.0 and 152.5-152.0. 154.7

154.7 Mineralized Fragmented Zone, l-2% chalcopyrite in a highly fragmented, predominantly fine grained volcanic rock S-4% quartz carbonate, low chloritization, medium carbonatization and epidotization. Trace MoS a / ^ red acidic fragments.172.5- As above, but red acidic (felsitic and rhyolitic) material increases to 30-40%, with corresponding increase in mineralization to l-2% chalcopyrite, trace MoS 2 , S-7% quartz carbonate. 194.5

194.5 Andesite - green, fine-medium grained, amphibolitized and foliated at 75-80 0 c.n. 197.0

197.0 Brecciated Zone- Predominantly volcanic material, with less than 5% felsitic fragments. 2-3% quartz carbonat, minor epidote, trace chalcipyrite, minor traces MoS a associated with quartz carbonate. Note: 2% chalcopyrite between 212.8-214.1. Low chloritization throughout. 214.1

214.1 Fragmented Volcanics (Andesite). Low-medium fragmentation, low-medium carbonatization, minor eipdote, trace chalco pyrite throughout. Low chloritization. 256.0

256.0 Felsophyre, greenish pink, low-medium sericitization. 10% dark green sericitized anhedral phenocrysts. Upper contact brecciated the dyke contains an inclusion of fragmented volcanics from 260.2-261.3. 261.3

261.3 Green Dyke - Probably a sericitized phase of the above felsophyre. 5% very finely disseminated pyrite. Medium sericitization massive. Trace sphalerite and chalcopyrite. Becoming pinkish and relatively fresh near end. 281.5

281.5 Zone of Fragmentation - green, predominantly volcanic material, medium chloritization, carbonatization, 1-2% quartz carbonate, minor epidote, trace chalcopyrite, MoS, .

DU PLICATE COPYPOOR QUALITY ORIGINAL

Sheet N-? 2. Ho.* No. KB.2.DESCRIPTION

124 O

7

194 5

197 O

214 l

256 o

261 3

121.0 - Carbonate Tain,'coarse grained, heavily stainedby hematite. Fracturing at dOo c.n.122.5 - As at 119.0.124 OFragmented Volcanics. Low-medium patchy chloritization,carbonatization and epidotization. Minor traces ofchalcopyrite and magnetite throughout. 1-2*6 quartscarbonate. Note: 1?C chalcopyrite between 141-3-H5.0.143-0 ~ Fragmented Volcanics. Fragmentation and alterationdecrease to low. Trace pyrite. The sone includes weaklymineralised nediun fragmented and carbonatlsed zonesfrom 148 0-149-0, and 152.5-153.0.154-7Nflneralized Fragmented Zone. 1-2*4 chalcopyrite in a highlyfragmented, predominantly fine grained volcanic rock.3-4# quarts carbonate, low chloritization, mediumcarbonatization and epidotization Trace MoS2/1# red acidic fragments172 5 - An above, but red acidic (felsitic and rhyolitic)material increases to 30-40**, with corresponding increasein mineralisation to l-2# chalcopyrite, trace MoS2,5-7^ quarts carbonate.

Andesite - green, fine-medium grated, amphibolitised and foliated at 75-300 c.n. 197 OBrecciated Zone - Predominantly volcanic material, with lean than 5# felsitic fragments 2-3# quartz carbonate, minor epidote, trace chalcopyrite, minor traces MoS2 associated with quarts carbonate. Note: 2# chalcopyrite between 212 8-214.1 Low chloritisation throughout. 214 lFragmented Volcanics (Andesite). Low-medium fragmentation, low-modium carbonatization, minor epidote, trace chalco pyrite throughout. Low chloritization.256 oFelsophyre, greenish pin):, low-medium sericitization.10# dark green sericitised anhedral phenocrysts.Upper contact brecciated the dyke contains an inclunionof fragmented volcanics from 260.2-261.3,261 3Green Cyke - Probably a seru-citised phase of the abovefelsophyre 5# very finely disseminated pyrite.Medium sericitiaation massive. Trace sphalerite andchalcopyrite. Becoming pinkish and relatively fresh nearend281 5Zone of Fragmentation - green, predominantly volcanicmaterial, medium chloritisation, carbonatization,1-2*3 quarts carbonate, minor epidote, trace chalcopyrite,MoS2 .

•\"-\D ,S^~ 7 : ^.

Sheet No. 3____________________________________________Hoi** j fR-

DESCRIPTION________________________________________^^^^^___^ - ^ -________ --

290.3290.3 Volcanics? Medium grained, amphibolitized, low chlorit

ization, massive. Less than I* quartz carbonate and eipdote stringers. No mineralization. 299.0

299.0 Zone of Fragmentation, as at 281.5. Predominantly fine grained and medium grained, amphibolitized volcanic material, 2-3% quartz carbonate, minor epidote, less than Q.5% pyrite and chalcipyrite in widely scattered blobs Low chlorite, epidote.

. 320.7 - Mineralized Epidote - rich Zone. Less than Q.5% chalcopyrite, pyrite, in a siliceous, highly epidotized rock, probably originally volcanic, i-2% carbonate-hematite filled fractures. 325.0

325.0 Fragmented and Shattered Zone, green basic host, medium shattering, high chloritization, 2-3% quartz carbonate, 2-3% hematite stringers and patches, minor epidote, trace sulphides. 329.3

329.3 Volcanics? Fine-medium grained, amphibolitized,locally faintly foliated at 45 0 c.n. l * quartz carbonate and epidote stringers, few short, highly epidotized zones, with minor associated traces of chalcopyrite. li hematite-stained stringers. Note: 4" siliceous, epidote-rich zone with trace chalcopyrite at 365.8. Becoming slightly chloritized, from 365.0 on. Note a 4" highly brecciated zone at 374.6.385.8 - Mineralized Zone, l-2% MoS 2 , trace chalcopyrite in a quartz carbonate stringer at 7G 0 c.n. 387.3- Volcanics!?) Gabbro{?) as before. Green, fine to medium grained, relatively fresh and massive, amphibole- rich. Spotted texture due to darker colour of stubby amphibole crystals. ^ hematite stained narrow quartz carbonate stringers, occasional short epidotized zones, with minor associated sulphides. 421.8

421.8 Shatter Zone. High shatter, high chloritization,considerable hematite staining, l-2% white carbonate, locally with embedded fragment. Medium grained basic (gabbroic) host.428.0 - Shatter Zone. Becoming silicified, only local high chloritization. S-4% hematite, 10% quartz carbonate fine grained, green, basic host. Minor epidotization. Trace chalcopyrite, pyrite, with short local concentration.456.5 - Shattering decreases to low. Less than l * quartz carbonate stringers, some stained red by hematite, irregular epidote and hematite stringers. 474.0

474.0 Gabbro-Volcanics? Medium grained, amphibole-rich "spotted" texture, due to dark colour of stubby amphibole xals.

DUPLICATE COPYPOOR QUALITY ORIGINAL

•mcruinw

Sheet No. 3 HokNoJB-22DESCRIPTION

290 5 290 3 Volcanics? Medium grained, aTphibolitited, low chlorit-

1 vat i on, aassive Less than 1JC quart* carbonate and epidotestringers. No olnaralisatlon.299.0

299 O Zone of fragmentation, as at 261.5. Predominantly fin* grained and nedium grained, amphibolitised volcanic material, 2-3^ quarts carbonate, minor epidote, less than 0.55* prrit* and chalcopyrite in widely scattered blobs. Low chlorite, epidote.320.7 - Mineralised Bpidote-rich Zone. Less than 0.39& chalcopyrite, pyrite, in a siliceous, highly epidotised rock, probably originally Tolcanic. 1-2* carbonate-hematite- filled fractures. 325 O

325 O Fragmented and Shattered Zone, green basic host, medium shattering, high chloritization, 2-3# quarts carbonate, 2-3# hematite stringers and patches, minor epidote, trace sulphides 329 3

129 3 Volcanics? Fine-mediun grained, amphibolitiaed,locally faintly foliated at 450 c.n 1# quart* carbonateand epidote stringers, few short, highly epidotiaed sones,with minor associated traces of chalcopyrite.1^. hematite- stained stringers. Note: 4" siliceous,epidote-rich zone with trace chalcopyrite at 365.8.Becoming slightly chloritiaed, from 3^5 O on. Note a 4 nhighly brecciated aone at 374 6.385 ^ - Mineralised Zone. I-2& MoS2, trace chalcopyritein a quartz carbonate stringer at 70O c.n.3^7 3 - Volcanics{?) GabbroT?) as before. Green, fine tonediura grained, relatively fresh and massive, amphibole-rich Spotted texture due to darker colour of stubbyamphibole crystals 1?5 hematite stained narrow quartzcarbonate stringers, occasional short epidotiaed zones,with niinor associated sulphides.JV21.3

421 B Shatter Zone High shatter, high chloritiaation,considerable hematite staining, 1-2JC white carbonate, locally with embedded fragment. Medium grained basic (gabbroic) host. 423 O - Shatter Zone.

474 O

Becoming silicified, onlylocal high chloritization. 3-4# hematite, 10^ quarta carbonate, fine grained, green, basic host. Minor onidotiaation Trace chalcopyrite, pyrite, with short local concentration456 5 - Shattering decreases to low. Less than l!?5 quarto carbonate stringers, some stained red by hematite, irregular epidote and hematite stringers 474 OGabbro- Volcanics? Medium grained, aaphibole-rich "spotted11 texture, due to dark colour of stubby amphibole xals.

t 14 Bole IEB-22

SAHPLEHO. DESCRIPTION

Relatively massive and fresh - possibly recrystalllzedvolcanics? Minor epidote, less than I\ quartz carbonateand hematite stringers.490.5

490.5 Andesite - Fine grained, green, locally well foliated at35-40 0 c.n. Foliation accentuated by parallelism ofepidote stringers; same type of volcanics as encounteredin lower half of EB-6. Minor local carbonatization,occasional trace of chalcopyrite, associated with epidote,

. less than ^ hematite-stained carbonate stringers; increasein intensity of foliation near end.525.0

525.0 Shear Zone. Medium epidotization, carbonatization,hematite staining, local silicification and amphibolitization.Volcanic hols. Distinct schistosity at 45-50 0 c.n. Tracechalcopyrite throughout.529.0 - As above, but carbonate-rich, medium chloritized,and high hematite staining.530.0

530.0 Andesite - Schistosity decreases, rock is still mediumepidotized and carvonatized, locally silicified, withoccasional traces of chalcopyrite.537.3 - Becoming massive and relatively fresh; decreasein epidote to 2-3% minor local carbonatization.553.0

553.0 END OF HOLE

DUPLICATE COPYPOOR QUALITY ORIGINAL

TO FOLLOW

No. 4 Hok No,DESCRIPTION

Relativ**, -*. -*w and fresh - possibly recrystallized voli*"' . iinor epidote, less than 1J( quarts carbonate

. . .,-ve stringers.

490.5 Andesite - Tine grained, green, locally well foliated at 35.400 c n Foliation accentuated by parallelism of epidote stringers; sane type of volcanics as encountered in lower half of EB-6. Minor local carbonatization, occasional trace of chalcopyrite, associated with epidote, less than 1# heir at it e-stained carbonate stringers; increase in intensity of foliation near end. 525-0

525 O Shear Zone. Medium epidotization, carbonatization,hematite staining, local silicification and amphibolitizationVolcanic host Distinct schistosity at 45-500 c.n. Tracechalcopyrite throughout.529 O - As above, but carbdnate-rich, medium chlorltized,and high hematite staining,530.0

530.0 Andesite - Schistosity decreases, rock is still medium epidotized and carbonatized, locally silicified, with occasional traces of chalcopyrite.537 3 - Becoming massive and relatively fresh: decrease in epidote to 2-3^ minor lO'-al carbonatization 553 O f

553 O End of Hole

l*X

DIAMOND DRILL LOG PROPERTY; Tribag Mining Co. Limited

LOCATION: Batchawana Bay, Ontario____uip ac. conar -90*

LATITUDE:______________ DIP:-,* nn - ft Q o FOOTAGE

DEPARTURE: -

ELEV.:

HOLE NO. EB-23

DIP

AZIMUTH: 13!!

READING CORRECTED

_____ COMMENCED: July 28/64

(magn) FINISHED: Aug.6/64 LOGGED BY:_M.Blecha

SAMPLE NO. DESCRIPTION

0.0 Casing6.5

6.5 Highly fragmented, altered zone. Dark green, basic host.High patchy chloritization and carbonatization, minorepidote. Trace pyrite throughout.10.0 - Andesite(?) dark green, fine grained, massive.No mineralization.12.2

12.2 Rhyolite - fractured and locally fragmented. Greyish red,locally well banded at 5-45 0 c.n. Minor quartz carbonateand epidote, stringers and patches.24.4

24.4 Fragmented andesite. Dark green, fine grained. Lowfragmentation, low chloritization, local carbonatization.2-3% epidote. Contains relatively massive sections from25.0-28.0, 34.0-42.7.42.7

42.7 Fault Zone (?) Andesitic host, high chloritization andcarbonatization and fragmentation.43.2 - Carbonate - rich fault breccia, 45 0 c.n.43.5 - as at 42.744.0

44.0 Andesite, dark green, fine grained, massive, minorepidotization, relatively fresh.53.5

53.5 Mineralized Zone, l-2% chalcopyrite, finely disseminatedin fragmented andesite. Medium patchy carbonatization,chloritization. 1-2!* quartz carbonate, 2-3% epidote.58.7

58.7 Fragmented Andesite. Dark green, fine grained. Mediumfragmentation, l-2% reddish -cidic fragments, generallylow alteration, except for few short highly fragmented,chloritized and carbonatized phases, l-2% epidote stringersand patches, with associated traces of chalcopyrite.Includes a relatively massive seciton from 93.0-102.5, andfrom 105.0-112.8.120.5

120.5 Zone of Foliation (Shearing?) Andesitic host, high chloriteand epidote, medium-high shearing at 50 0 c.n.

DUPLICATE COPYPOOR QUALITY ORIGINAL

TO FOLLOW

DIAMOND DRILL LO(PROPERTY, Tribag Mining Co. Limited

LOCATION: Batchawana Bay, OntarioDip at collar -90-

latitude: Dip: at 270 -39*at 535 37*

Departure: Depth: 560.7*

Footoge

HOLE NUMBER: BB-23

DIP TESTS

Reading Corrected

Elevation:

Azimuth: 270 S46*W

Commenced: July 23,

Finished: A^ f t, , /Vi V Logged by: M.

SAMPLE NUMBER

^^

^P

4t

DESCRIPTION

0.0 Casing6.5

6.5 Highly fragmented, altered cone. Dark green, basiHigh patchy chloritization and carbonatization, miepidote. Trace pyrite throughout.10.0 - Andesite(?) dark green, fine grained, massiHo mineralisation.12.2

12.2 Rhyolite - fractured and locally fragmented. Greylocally well banded at 5-45* c.n. Minor quartz eaand epidote. stringers and patches.24.4

24.4 Fragmented Andesite. Dark green, fine grnlned. Lf ra rae nt at i on, low chloritization, local carb on* t2-3* epidote. Contains relatively massive section25.0-2S.O, 34.0-42.7.42.7

42.7 Fault Zonet?) Andesitic host, hi*h chloritizationcarbonatization and fragaentation.1*3.2 - Carbonate-rich fault breccia, 45* c.n.43.5 - as at 42.7.U.O

44.0 Andesite, dark groen, fine grained, massive, minorepidotization, relatively fresh.53.5

53.5 Mineralized Zone. l-?ji chalcopyrite, finely dissetin fragmented andesite. Medium patchy carbonatizachloritization. 1-2* quarts carbonate, 2-3# epido58.7

53.7 Frvgnwnted Andesite. Dark green, fine grained. Mfragmentation. 1-25* reddioh acidic fragments, genlow alteration, except for few short highly fragmechlorltized and carbonatized phases. 1-21C epidotean-* patches, with associated traces of chalcopyritIncludes c relatively massive section from 93.0-10from 105.0-U2.3.120.5

host.or

e.

.sh red,rbonate

yw.zation.

from

and

ilnated.ion,i to*

Hilumnrallyited,stringert.!.5, and

t

120.5 2one of Foliatim (Shearing?) Andesitic host^ higm chloritand epidote, medium-high shearing at 50 0 c.n.

^ i '"' -f- - - . ,

B

e

Sheet 12______________________________________________Hole t EB-23

DESCRIPTION

-122.5122.5 Fragmented Andesite - low fragmentation, low alteration,

minor epidotization, becoming highly chloritized from 127.5 on. 128.8

128.8 Fault Zone(?) Carbonate-rich, higly chloritizedbrecciated zone. 3(^ quartz carbonate - andesitic host. 129.5

129.5 Zone of High Fragmentation. Predominantly fine grained volcanic fragments, with 2(^ pinkish grey rhyoliti-.- and felsitic fragments. Medium patchy chloritization, carbonatization and epidotization. S-4% quartz carbonate. Q.5% chalcopyrite throughout. Note: l.O 1 highly foliated zone (45 0 c.n.) at 138.5-139.5.146.0 - Andesite, dark green, fine grained, massive Trace chalcopyrite. 150.0

150.0 Zone of Fragmentation, as before, but acidic material less than 5%. Low-medium chlorite and carbonatization. D.5% chalcopyrite throughout. 166.0

166.0 Andesite - dark green, fine grained, massive. Note flow structures and minor flow breccia between 168.5-170.0. Becoming medium grained and amphibolitized near end. 185.7

185.7 Mineralized Zone. lS-17% chalcopyrite, 45% magnetite : in a amphibole-rich green rock. Mino- epidotization.

186.0 186.0 Zone of Fragmentation. Highly fragmented, predominantly

andesitic, with 7-10% acidic fragments, 31 epidote. j Medium patchy carbonatization, low chlorite. j Trace chalcopyrite throughout, mostly associated with l epidote.

205.0205.0 Fragmented Volcanics. Dark green, low-medium fragment

ation, less than l 5* acidic fragments, l-2% epidote, less than l * quartz carbonate. Medium patchy carbonatiz ation, low-medium chloritized throughout. Mineralized with less than Q.5% chalcopyrite.245.5- Shatter Zone - volcanic host, high chlorite, lQ-15% white carbonate and red hematite stringers. 246.2

246.2 Andesite - dark green, fine grained, massive, 5% epidote stringers and patches, low chloritization. Same as in lower half of D.D.H. EB-6. 258.5

258.5 Fragmented volcanics, low fragmentation, 7-8% epidote,l-2% quartz carbonate, low-medium patchy carbonatization. Mineralized with Q.5% chalcopyrite. Note: 20% magnetite in a silicified and epidotized zone from 263.0-263.5. 278.5- Quartz-rich, epidotized zone, 80 0 c.n. Trace magnetite and chalcopyrite.

DUPLICATE COPYPOOR QUALITY ORIGINAL

TO FOLLOW

Sheet No. 2. Hole No. KB-23DESCRIPTION

122.5 122.5 Fragmented Andesite - low fragmentation, low alteration,

minor epidotization, becoming highly chloritized from127.5 on.128.8

128.8 Fault Zone(?) Carbonate-rich, highly chloritizedbrecciated zone, 303& quartz carbonate - andesitic host.129.5

129.5 Zone of High Fragmentation. Predominantly fine grainedVolcanic fragments, with 20# pinkish grey rhyoliticand felsitic fragments. Medium patchy chloritization,carbonatization and epidotization. 3-1,7* quartz carbonate.0.5# chalcopyrite throughout. Note: l.O 1 highly foliatedzone (45 0 c.n.) at 138.5-139.5.146.0 - Andesite, dark green, fine grained, massive.Tracw chalcopyrite.150.0

150.0 Zone of Fragmentation, as before, but acidic materialless than 5*. Low-medium chlorite and carbonatization.0.5# chalcopyrite throughout,166.0

166.0 Andesite - dark green, fine grained, massive. Note flowstructures and minor flow breccia between 168.5-170.0.Becoming medium grained and amphibolitized near end,185.7

185.7 Mineralized Zone. 15-17^ chalcopyrite, 45* magnetitein a amphibole-rich green rock. Minor epidotization.186.0

186.0 Zone of Fragmentation. Highly fragmented, predominantlyandeoitic, with 7-10# acidic fragments, 3'.* epidote.Medium patchy Xftv****ii***K carbonatization, low chloriteTrace chalcopyrite throughout, mostly associated withepidote.205.0

205.0 Fragmented Volcanics. Dark green, low-medium fragment-ati^n, less than 156 acidic fragments, 1-2^ epidote,loss than l* quartz carbonate. Medium patchy carbonatiz ation, low-medium chloritized throughout. Mineralizedwith loss than 0.5# chalcopyrite.245.5 - Shatter Zone - volcanic host, high chlorite,10-15,* white carbonate nnd red hematite stringers.246.2

246.2 Andesite - dark green, fine grained, massive, 5S& epidotestringers and patches, low chloritization. Same as inlower half of D. D. H. EB-6.258.5

258.5 Fragmented volcanics, low fragmentation, 7-8* epidote,l-2# quart?, carbonate, low-medium patchy carbonatization.Mineralized with 0.5# chalcopyrite, Note: 20# magnetitein a silicified and epidotized zone from 263.0-263.5.278.5 - Quartz-rich, epidotized zone, magnetite and chalcopyrite.

80* c.n. Trace

Page 3.____________________________________________Hole No. EB-23

^^^^^ DESCRIPTION ______ ^^^^

280.3 - Fragmented Volcanics. Fragmentation and carbon atization increase to medium with corresponding increase in chalcopyrite to 11. Trace pyrite. Local patchy medium chloritization. 5-71 epidote. 1-21 quartz carb. 298.3

298.3 Andesite - dark green, fine grained, with 10-151 fine magnetite parallel to foliation (45 0 c.n.). Core broxen up from 301.0-302.0. 302.5

302.5 Highly Fragmented Zone. Predominantly basic volcanic material. 25% acidic fragments. Medium patchy carbon atization and epidotization. 5% quartz carbonate. Trace chalcopyrite throughout. 312.1

312.1 Andesite-green, fine grained, massive, fresh. 3-41epidote, minor magnetite (less than 5%) . Trace chalco pyrite; locally well foliated at 75 0 c.n. 316.0

316.5 Fragmented Andesite. 1-21 acidic fragments. Medium patchy carbonatization, locally medium chloritized, 3-41 epidote. D.5% chalcopyrite throughout. Minor magnetite. 2-31 quartz carbonate. Mote foliated (55 0 c.n.) zone with parallel carbonate stringers and associated 5% pyrite from 339.0-340.0. The zone contains sections of massive andesite from 360.0-362.0, 364.0-369.5. l-2% acidic fragments, relatively fresh. Less than 11 quartz carbonate, minor epidote, trace chalcopyrite, MoS 2 associated with quartz. Medium patchy carbonatization. 403.4

403.4 Weakly Mineralized Zone, l-2% chalcopyrite, trace MoS ain fragmented andesite, with less than 11 acidic fragments. 51 epidote, l-2% quartz carbonate. Medium patchy carbon atization. Low-medium patchy chloritization. 417.5 - As above, quartz carbonate increases to 3-41. 21 chalcopyrite, trace MoS, .423.0 - Trap Dyke, grey, aphanitic, massive. Cut by 1/16" quartz 'carbonate stringers with MoSj (50 0 c.n.) Sharp contacts at 45 0 c.n.424.5 - Mineralized Zone, as at 403.4. Medium patchy chloritization and carbonatization. 5% quartz carbonate. Hematite stringers. Only minor epidotization. The basic fragments gradually becoming slightly coarser (medium grained), possibly gabbroic? Q.5% chalcopyrite, traces MoS 2 throughout, with lo ;al concentration. Less than 11 acidic fragments. 448.6

448.6 Fragmented Andesite - low-medium chloritization, lowfragmentation, low patchy carbonatization. 2-3% epidote, less than 11 quartz carbonate, minor chalcopyrite and MoSj throughout. Most rock locally becoming medium grained (gabbroic?). Chalcopyrite mostly associated with epidote and quartz. Note short highly epidotized sections from501.0-501.5, DUPLICATE COPY

POOR QUALITY ORIGINAL TO FOLLOW

Sheet No. 3. Hole No.EB-23

DESCRIPTION

c.n.)

280.0 - Fragmented Volcanics. Fragmentation and carbon atization increase to medium with corresponding increase in chalcopyrite to 1#. Trace pyrite. Local patchy medium chloritization. 5-7# epidote. l-2# quartz carb. 293.3

298.3 Andesite - dark green, fine grained, with 10-15* finemagnetite parallel to foliation (45 0 c.n.). Core brokenup from 301.0-302.0.302.5

302.5 Highly Fragmented Zone. Predominantly basic volcanicmaterial. 25# acidic fragments. Medium patchy carbon atization and epidotization. 5# quartz carbonate. Trace chalcopyrite throughout. 312.1

312.1 Andesite - green, fine grained, massive, frosh. 3-42*epidote, miner ma&netite (less than 5/*}. Trace chalco pyrite; locally well foliated at 75 0 c.n. 316.0

316.5 Fragmented Anr'-site. 1-21& acidic fragments. Medium patchy carbonatization, locally medium chloritized, 3-4^ epidote. 0.55* chalcopyrite throughout. Minor magnetite. 2-3;* quartz carbonate. Note foliated (55 zone with parallel carbonate stringers and associated 5# pyrite from 339.0-340.0. The zone contains sections of massive andesite from 360.0-362.0, 3&4.0-369.5. 369.5 - Fragmnntod Andesite - low-medium fragmentation. 1-2/i acidic fragrxmta, relatively fresh. Less than 1# quartz carbonate, minor epidote, trace chalcopyrite, MoS2 associated with quartz. Medium patchy carbonatization. 403,4

1*03.4 Weakly Mineralized Zone. l-2fe chalcopyrite, trace HoS2in fragmented andesite, with less than 1^ acidic fragments. 5# epidote, l-2# quartz carbonate. Medium patchy carbon atization. Low-medium patchy chloritization. 417.5 - As above, quartz carbonate increases to 3-4^. 2'* chalcopyrite, trace MoS2*423.0 - Trap Dyke, grey, aphanitic, massive. Cut by 1/16" quartz carbonate stringers with MoS2 (50 0 c.n,) Sharp contacts at 45 0 c.n.424.5 - Mineralized Z^ne, as at. 403.4. t Medium patchy chloritization and carbonatization. 5# quartz carbonate. Hematite stringers. Only minor epidotization. The basic fragments gradually becoming slightly coarser (medium grained), possibly gabbroic? 0.5^ chalcopyrite, traces MoS2 throughout, with local concentration. Less than I# acidic fragments. 448.6

448.6 Fragmented Andesite - low-medium chloritization, lowfragmentation, low patchy carbonatization. 2-3^ epidote, less than 1# quartz carbonate, minor chalcopyrite and MoS2 throughout. Host rock locally becoming medium grained (gabbroic?). Chalcopyrite mostly associated with epidote and quartz. Note short highly epidotiied sections from 501.0-501.5,

mPage 4 ___ Hole IEB-23' — : —————— : ————————————— ~~ ————————— " ———————— : : ———

DESCRIPTION . .

511.0-512.0 - Minor hematitie filled fractures and hematite staininq. Occasional patches of magnetite. 547.5

547.5 Andesite - becoming relatively massive, green, fine grained, with l-2% quartz-epidote stringers, trace magnetite. 560.7 - END OF HOLE

DUPLICATE COPYPOOR QUALITY ORIGINAL

TO FOLLOW

Sheet No. i Ho'e No, EB-22

DESCRIPTION

511.0-512.0 - Minor hematite filled fractures and hematite staining. Occasional patches of magnetite.547.5Andesite - becoming relatively massive, groen, finegrained, with l-2;i quartz-epidote stringers, tracemagnetite.560.7 - End of Hole. .

M

1

DIAMOND DRILL LpG

PROPERTY:_____TRIBAG MINING CO. LIMITED -' HOLE NO. EB-24

LOCATION; Batchawana Bay, Ontario ' ' DIP TEST—-—-.—.-—-—

LATITUDE:_______________ DIP;at collar -55* FOOTAGE READING CORRECTED- . ." at collar -b3 0

DEPARTURE: DEPTH: 321'

ELEV. :___________^_____ COMMENCED: August 6/64

AZIMUTH;at collar S30 0E FINISHED; August 10/64 LOGGED BY;M.Blecham. \ - ~.T 1 j. i- Ci 7 *". n T?CL \f IM-V^ J. i CI 1. ±3 i. J d

S^LE DESCRIPTION

0.0 Casing 5.0

5.0 Highly Fragmented, weakly Mineralized Zone. Q.5% chalcopyrite, in a predominantly volcanic fragmented zone. lQ-15% acidic fragments, S-7% quartz carbonate, medium-high patchy chloritiz ation and carbonatization. 11.8

11.8 Dyke. Dark grey, aphanitic, very hard (siliceous), massive. Sharp, irregular contacts. 15.2

15.2 Phyolite - Pinkish grey, well banded at 60 0 - 70 0 c.n., fine grained. Core broken up from 18.5-20.0. 20.0

20.0 Basic Volcanics (?) Dark greenish grey, fine grained, massive. Relatively fresh with short slightly chloritized sections. 1-2!* very finely disseminated pyrite throughout. Minor chalco pyrite in fractures at random angles, l-2% carbonate stringers. Chilled lower contacts at 40 0 c.n. 44.9

44.9 Rhyolite - as at 15.2. Locally porphyritic and banded at 40 0 c.n. Note: 4" epidotized and silicified section with trace chalcopyrite at 47.0 1 . Minor local fragmentation. 50.3

50.3 Dyke - as at 11.8. Sharp contacts at 65 0 c.n. 51.5

51.5 Basic Volcanics(?) Dark greenish grey, fine grained, fresh and massive. 55.0

55.0 Zone of Fragmentation. 50% acidic (rhyolitic) fragments,50*^ basic volcanic, (medium patchy chloritization and carbon atization. Size of fragments i"-3". Trace MoS 2 . 2-3% epidote. 60,0

60.0 Basic Volcanics (Andesite?) Dark cjreen, fine grained,relatively fresh and massive. Cut by 5 % epidote and quartz stringers, with traces of associated chalcopyrite. Note short (few inches) zones of high epidotization and silicification. Mineralized with minor chalcopyrite at 66.1-66.5 and 71.3 -71.5 75.5

75.5 Tuff? Brownish green, well banded (30 0 c.n.) rock, consisting of lense-like 1/8"-!^" alternating bands of soft, medium

DUPLICATE COPYPOOR QUALITY ORIGINAL

TO FOLLOW

DIAMOND DRILL LO(PROPERTY: Tribag Mining C o. L imited

'LOCATION: Batchawana Bay, Ontariolatitude:

Departure:

Elevation:

DiP' *t collar -55' * at 318 -53'Depth: 321*

HOLE NUMBER: Kg.;

DIP TESTS

Footage Reading Corrected

Commenced: AugUSt 6, 1964

Azimuth: at Collar E30*E Finished: August 10, 1964 ^W*6 bX! K Bl*eha _______Ut 31** 52S*E_________ _____ .—-....-..———-—— u-fcgon*

SAMPLE NUMBER

9

9

at

0.0

5.0

11.8

15.2

20.0

U.9

50.351.5

55.0

60. c

75.5

"ab W — —————— ••^••X —— ** ———————————————————————————————————————————————————————— —————————————————————————

DESCRIPTION

Casing5.0Highly Fragmented, weakly Mineralised Zone. 0.5* ciin a predominantly volcanic fragmented none. 10-151fragsents, 5-7?* quarts carbonate, medium-high patch)atlon and carbonatization.11.3Dyke. DnrV grey, aphanitic, v*ry hard (siliceous),Sharp, irregular eontactn.15.2Rhyolite - Pinkish grey, well banded at 60" - 70* c.Brained. Core broken up from 18.5-20.0,20.0Haslc Volcanics(?) Dark greenioh groy, fine grainedJJ.elativ*:y fresh with short slightly chloriti**d seel-2# very finely diseaminatod pyrite thi^onrlmut. Mlpyrite in fractures at rnndon nnglea. 1-2* carbonstChill ttd lovr*r contacts at 40* c.n. ^4.9Rhyolite - AB at 15.2. Locally porphyritic and bandc.n. note: 4 W epidotised and silicified section witchalcopyrite *t /k7.0*. Minor local f ra mentation.50.3Dyke - aa at 13.8. Sharp contacts at 65* c.n.51.5Baric VolcMnicn(?) Dark greenish xray, fine grainedftnd massive.55.0Sone of Fragmentation. 50jt acidic (rhyolitic) fra^a5O,i basic volcanic. (meditM patchy chloritization aatisation. Sine of fragnenti l72lf -3". Traee MoS2.2-3^ epidote.60.0Basic Volcanics (Andooitc?) Dark groen, fine grain*relatively fresh and suisaire. Cut by 5^ epidote andetr infers, with traces of nnaociated ohalcopyrite.(few inches) cones of high epidotization and siliciMineralized with ainor chalcopyrite at 66.1-66.5 And75.5Tuff? Brownich Kreon. wall banded (30* c.n.) rock,of lenst-like 1/5" -1/4" alternating bands c^f soft, B

/—i

alcopyri^acidicchlorit:

uaeaive.

n., fine

, mn se i y*t ions.nor chai*e string*

ed at itO'i trace

, fresh

mto,id carbo

i,quarts

fote shoLoation.71.3-71

consist iidlum

•ix-

*

o-rs.

-

t

.

S"S" f. ' .--j

Sheet No. 2 Hole #EB-24

SAMPLE NO. DESCRIPTION

chloritized material, pale green epidotized bnads, and bands of brown micaceous alteration.78.5

78.5 Andesite - as at 60.0. Grandational upper contact2-31 epidote stringers, some with minor associatedchalcopyrite.87.8

87.8 Mineralized Zone. 3-41 chalcopyrite, 5% magnetite in ahighly fragmented zo.ie. Medium-high patchy chloritizationand carbonatization. Fine grained basic host.88.8

88.8 Zone of Fragmentation. 70-80% fractured and fragmentedpinkish grey rhyolitic material. 20% basic volcanicfragments and masses. Some highly chloritized.l-2% epidote, 3-41 quartz carbonate. Locally banded at45-50 0 c.n. Trace chalcopyrite and MoS 7 . Note 4" greyaphanitic dykelet at lower contact.110.3

110.3 Andesite - Dark green, fine grained, relatively freshand massive, except for minor local (flow?) brecciation.51 epidotized and silicified patches with traces ofassociated chalcopyrite.122.6

122.6 Rhyolite - Reddish grey, banded at 75 0 c.n. 1-21 quartzstringers parallel to banding.125.0

125.0 Fault - Strong fault breccia. 10% white carbonate;rhyolitic host.126.5

126.5 Rhyolite - as at 122.6. Locally fragmented, less than 11quartz carbonate stringers, trace MoS 2 .136.2

136.2 Zone of Fragmentation. Predominantly basic volcanichost, with 203; rhyolitic fragments. Medium patchycarbonatization, low chlorite, 2-31 epidote. 11 quartz.Contains massive andesitic sections from 140.0-141.5 andfrom 144.3-148.4. Less than Q.5% chalcopyrite inwidely scattered blobs. Trace MoSj150.0 - Rock becomes predominantly rhyolitic, stillfragmented, .locally well banded at 65-70 0 c.n. 1-21quartz. Localy high carbonatization. Occasional blobsof chalcopyrite. The zone contains sections of massive,but banded rhyolite from 160.3-163.0, 164.2-165.0.167.8 - Andesite - Fine grained, green, massive,3-41 epidote. Sharp, upper contact at 40 0 c.n.170.0 - As at 136.2.171.5 - Rhyolite, as before, banded at 45-50 0 c.n.11 quartz carbonate stringers.176.6 - Zone of Fragmentation - Rhyolite host.1-21 quartz carbonate, locally stained blue, by molyb denite .184.0 - Zone of Fragmentation - becoming increasinglybasic, medium chloritization, 51 quartz carbonate,trace chalcopyrite.

Sheet No. 2. Hole No.DESCRIPTION

chloritized material, pale green epidotlzed bands, and bands of brown micaceous alteration.73.5

76.5 Andesite - as at 60.0. Oradational upper contact,2-3# epidote stringerj, some with minor associatedchalcopyrite.87.8

87.8 Xineralized Zone. 3-4* chalcopyrite, 5* magnetite in ahighly fragmented zone. Medium-high patchy chloritizationand carbonatization. Fine grained basic host.88.8 ^

88.8 Zone of Fragmentation. 70-805& fractured and fragmented pinkish grey rhyolitic material. 20# basic volcanic

fragments and masses. Some highly chloritizod.l-2?l epidote, 3-4# quartz carbonate. Locally banded at45-50* c.n. Trace chalcopyrite and MoS2. Note 4" greyaphanitic dykelet at lower contact.110.3

110.3 Andesite - Dark groen, fine grained, relatively freshand massive, except for minor local (flow?) brecciation.5# epidotized and silicified patches with traces ofassociated chalcopyrite,122.6

122.6 Rhyolite - Reddish grey, banded nt ?5 C c.n. 1-2^ quartz?trinfers parallel to banding,12 5-0

125.0 Fault - Strong fault breccia. 10?* white carbonate;rhvolitic host.12&.5

126.5 Rhyolite - as at 122.6. Locally fragmented, less than l* quartz carbonate stringers, trice ?!oS2. 136.2

136.2 Zone of Fragmentation. Predominantly basic volcanic hoot, with 2O/S rhyolitic fragments. Medium patchy carbonatization, low chlorite, 2-3^ epidote. 1^ quartz. Contains massive andesitic sections from 140.0-141.5 and from 144.3-143.4. Loss than 0.5;* chalcopyrite in widely scattered blobs. Trace Ko5 2 . 150.0 - Kock becomes predominantly rhyolitic, still fragmented, locally well bnnded at 65-700 c.n. 1-2* quartz. Loc^ly high carbonatization. Occasional blobs of chalcopyrite. The zone contains sections of massive, but banded rhyolite from 160,3-163.0, 164.2-165.0. 167.8 - Andesite - Fine grained, green, massive, 3-4^ epidote. Sharp, upper contact at 40 C c.n. 170.0 - fts at 136.2.171.5 - Rhyolite, as before, banded at 45-50" c.n. 1^ quartz carbonate stringers. 176.6 - Zone of Fragmentation - Rhyolitic host. 1-2^ quartz carbonate, locally stained blue, by molyb denite, q 184.0 - Zone of Fragmentation - becoming increasingly basic, medium chloritization, 5# quarts carbonate, trace chalcopyrite.

Sheet 13___________________________________________Hole IEB-24

DESCRIPTION

190.7 - As at 176.6. Includes a predominantly basicsection from 195.5-198.0.208.0

208.0 Shatter Zone (Fault) High shattering and brecciation,7-10% quartz-carbonate and hematite. Rhyolitic host.Locally highly chloritized.211.2 - As above, but mineralized with 1-2% chalcopyriteblobs. High chlorite. 101 carbonate.212.4 - Highly shattered chloritized. predominantly basicrock. Only trace chalcopyrite, MoSj.218.0 - Mineralized Zone - 4-5% chalcopyrite, associated 'with quartz-carbonate in a shattered zone, as above.219.3 - Shattering decreases to low, but rock is stillfractured, mostly at 80 0 c.n. Core broken up from221.2-222.0.222.0

222.0 Rhyolite - Pinkish grey, fine grained, banded at 80-90 0c.n. Less than li quartz carbonate stringers, stainedred by hematite. Trace chalcopyrite along fractures.263.9

263.9 Mineralized Zone. 1-2** chalcopyrite, in a sheared(75 0 c.n.), silicified and highly chloritized zone.Andesitic (?) host.264.9

264.9 Andesite - dark green, fine grained, medium chloritized,locally sheared at 65-70 0 c.n. Minor chalcopyrite alongslip planes. Sharp lower contact at 70 0 c.n.268.5

268.5 Rhyoliye - as at 22.0 Cut by 3-4* quartz stringers,less than 11 carbonate. Generally massive, except forminor local fragmentation. Locally banded at 80-90 0 c.n.Minor traces of chalcopyrite and MoS, associated withquartz stringers.321.0 END OF HOLE

Samples Taken

Assay Results

Sai.ip leNo. Footage Length

9644 5.0-11.8 6.89645 60.0-83.8 23.8 0.10

6 83.8-87.8 4.0 0.187 87.8-88.8 1.0 1.388 88.8-95.8 7.0 0.17

R^ICATE COPY

Shtet No. 3 . Hole No.DESCRIPTION

208.0

222.0

263.9

264.9

263.5

190.7 - As at 176.6. Includes a predominantly basicsection from 195.5-193.0.203.0Shatter Zone (Fault) High shattering and brecciation,7-10* quartz-carbonate and hematite. Rhyolitic host.Locally highly chlor *.",ized.211.2 - As above, but mineralized with 1-2* chalcopyriteblobs. High chlorite. 10** carbonate.212.4 - Highly shattered chloritized, predominantly basicrock. Only trace chalcopyrite. MoS2.213.0 - Mineralized Zone - 4-53* chalcopyrite, associatedwith quartz-carbonate in a Shattered zone, as above.219.3 - Shattering decreases to low, but rock is stillfractured, mostly at 800 c.n. Cor** broken up froa221.2-222.0.222.0Rhyolite - Pinkish grey, fine grained, bunded at 80-900c.n. Less than 1# quartz cnrbonata stringers, stainedred by hematite. Trace chalcopyrite along fractures.

^ Mineralized Zone. 1-2* chalcopyrite, in a sheared(75 0 c.n.), silicified and highly chloritized rone. *mdesitic{?) host.

Andesite - dark green, fine grained, medium chloritized, locally sheared at 65-70 e c.n. Minor chalcopyrite along slip planes. Sharp lower contact at 70* c.n.263.5Rhyolite - as at 222.0. Cut by 3-4r* quartz stringers,less than l'/* carbonate. Generally massive, except forminor local fragmentation. Locally banded at 30-900 c.n.Minor traces of chalcopyrite and KoS2 associated withquartz stringers. (321,0 End of Hole. ;- 'i 'f]h

Samples Taken

Assay Results

Sample Ho.

9644

9645673

Footn Re

5.0-11.3

60.0-33.3 33.3-37.8 37.3-33.3 38.3-95.3

Length

6.3

23.3 4.0 1.0 7.0

0.14

0.100.131.330.17

DIAMOND DRILL LOG

PROPERTY :

LOCATION :

LATITUDE:

DEPARTURE:

ELEV.:

\ AZIMUTH:

Tribag Mining CoClaim SSM 621941150'S7800'E

-

. Ltd.

DIP: -90 0 . -

DEPTH: 105.0*

COMMENCED: Nov.

FINISHED: Nov.

HOLE NO.

DIP TEST

FOOTAGE READING

21/64

X-23

CORRECTED

23/64 LOGGED BY: Matthew Blecha

! SAMPLE i NO. DESCRIPTION

0.0 Andesite, dark grey, fine grained, massive, cut by lQ-15% narrow epidote stringers. Locally foliated at 45 0 ; minor local flow (?) brecciation. 64.2

64.2 Quartz vein, white, massive, barren quartz. 66.5

66.5 Fault Zone. A 3" mud seem, followed by a highlysilicified and epidoteized fault breccia. No minerali zation. 69.5

69.5 Andesite, as at 0.0 Decrease in epidote stringers to 2-3 !4. Minor local flow (?) brecciation, trace py. 93.0

93.0 Rhyolite (?) or possibly silicified andesiteDark grey, aphanitic, locally brecciated, becoming slightly paler and brownish near end. No min. 105.0

105.0 END OF HOLE.

lAM*DI&XOND DRILL LOGPROPERTY, Tribag Mining Co. Ltd., HOLE NUMBER,

w? TESTS

Footoge Reading

LOCATION: Claim SSM Ilfl 62194Urtitvdei 1150*3 Dip: -990

Departure: 7#00*g Depth: 105.0*

Elevation: Commenced: Nov. 21 1964

Azimuth: —— Finished: Mov. 23, 1964 Lowd ** Matthew Blecha

Corrected

SAMPLE NUMBER DESCRIPTION

0.0*

6i 9

66.5*

69.5*

93.0*

105.0*

Andesite, dark grey, fine grained. massive? cut by!10-155f narrow epidote stringers. Locally foliatedat 45 ; minor local flow (?) brecciation.64.2Quartz vein, white, ttassive, barren quarts.66.5*Fault Zone. A 3" raud seem, followed by a highly lsilicified and epidotized fault breccia. Ho mineralfl-zation.69.5Andesite, as at 0.0* Decrease in epidote stringers2-3#. Minor local flow (?) brecciation, trace py.93.0Rhyolite (?) or possibly silicified andesite.Dark grey, aphanitic, locally brecciated, becomingslightly aler and brownish near end. No min,105.0End of Hole

- l 586

Matthew Bleoha

AS3E5SMEWT WORK

x

* \x\\ 1 \ \

\

G* ro 5 •f*f