arctic red resc corp omep rpt on ddh ar-1 … (up to 1 cm) set in a fine grained, uniform, ......

42CI2NW8181 63.4489 BOMBY010

ARCTIC RED RESOURCES CORP,

OMEP REPORT ON DDH AR-1

OM83-4-C-35

HEMLO AREA, ONTARIO

42C12NW8181 63.4480 BOMBY

TABLE

010C

INTRODDCTION

THE PROPERTY

LOCATION AND ACCESS ,

PROPERTY GEOLOGY

PREVIOUS EXPLORATION

CURRENT PROGRAM

FINANCIAL REPORT

1

1

1

2

2

3

4

APPENDICES

I DRILL LOG AND LEGEND

II ANALYTICAL RESULTS

III HOLE DEVIATION SUMMARY

IV TECK EXPLORATIONS LIMITED INVOICES AND OMEP FORM 2

ILLUSTRATIONS

Figures

12

3

Location Map...., Property Map. Property Geology,

After Page

112

Drawings (in pocket)5498 DDK AR-1, Vertical Section

5499 Surface Plan

G RQ-86

INTRODDCTION

The Michano property consists of nine claims presently

under option from Grant Michano of Heron Bay, Ontario, to

Arctic Red Resources Corp. Arctic Red Resources Corp.

submitted a proposal for a mineral exploration program which

was subsequently approved and registered as Designated

Program OM83-4-C-35.

THE PROPERTY

The claims occur in Bomby Township, District of Thunder

Bay, Ontario (Fig. 1, 2):

____Due Date____TB 645171-173, inclusive April 21, 1985

TB 656742-744, inclusive September 24, 1985 TB 614189-191, inclusive October 5, 1984

The claims are held in escrow by National Trust Company

Limited.

LOCATION AND ACCESS

The property is in the Molson Lake area 1 km northeast

of Hemlo.

Michano Optionx*-~CeJai

ARCTIC RED:PINE BELL JOINT VENTURE

MICHANO OPTION

PROPERTY LOCATION MAP

Hemlo,Ontario

Dec..1982

7oi7?5 I70i7se 4701757 [701753 701757

it lv IGI5I2T 615)28 1615129 615130 614750^^ i i . j . i ^^——— ———— -~ -f-. .———. l——— . M j————— ~. M .f—— ^ . ————.

!TB JTB J645897 [645895)545893 J_^.70I7J? [701686 J70I738 J70I7CO J70l75"p

7'jieee 1701737 1701690 [687197-.i -i. . ' 4873 674874)

__ . . - — J ______ . __ - ___ if-"

Michano Option ^67-Q57? J674876 J674876 I 6 e5964 J686983 \66S98270I689 |70I692 70I69I 687I96^68406 j6084 ' 7 L

'-^l— — T— ,-' ~ "" ~io— L. -. ^ —L — _ L. — — J—

ITB ITB JTBl l ' l 701684 701683 J70I682 {701681 687195 674870 '.674871 1685985 .635986,685987

613970 1613972

" '"""-—--|653859 .,'',/;

——i^L.————— - . s*.r.fina ™-it^ Xi.vS- i .b a b b aa L^l.; ; l ra •-|^W^j^^92^|i-C69L|6J66S2j -.^ e \-

TB f/ '\JB

i-^.GoJ den SceptreIT8 -?

''S35S04,— — —^ .. L.' SSM \ 8SM

ARCTIC RED-PINE BELL JOINT VENTURE

MICHANO OPTIONj SSM~] SSM l SSM

j674863;C'74769 J65634S———^*i———————p—————l CLAIMS LOCATION

Hemlo, Ontario

"* mile

J2MSSMISSM |SSM JSSM j|^ .

CC5560 *yw*i 1 625562 j 625563 | 625564675105 6 74" " ~~~ -.675106 (675107 j l

l674486;6744fi5 July 1983.. .. .f5**68 l 62 S5666

- 2 -

The TransCanada Highway (Hwy. 17) crosses the property

and Highway 614 forms the east boundary of the northeastern

claims (Pig. 2). All parts of the property are easily

accessible from either the TransCanada or Highway 614.

PROPERTY GEOLOGY

With the exception of the southwest portion of the

property, the claims are underlain by massive equigranular

grey granite which comprises the Cedar Lake pluton. A

diabase dyke trending north-northwest cuts across the

central part of the property, and metasedimentary rocks

underlie the western sections of claim TB 614189. These

metasediments, consisting predominantly of metasiltstones,

strike north-northwest and dip 50"-60*E.

PREVIOUS EXPLORATION

No known exploration work was conducted on the property

prior to the 1982 geophysical, geochemical and geological

surveys carried out by Arctic Red Resources Corp.

Diabase

Granite

Mctasediments

ARCTIC RED:P!NE BELL JOINT VENTURE

MICHANO OPTION

International Corona——o

Dec.,1982

- 3 -

Magnetometer and VLF-EM surveys were completed during

the period November 23 to December 9, 1982.

Geological mapping was carried out concurrently with

the geophysical surveys and a B horizon soil geochemical

survey was conducted on the southwestern portion of the

property.

CDRRENT PROGRAM

In 1983, DDH AR-1 was drilled to test for the extension

of the Corona gold-bearing horizon at a projected depth of

approximately 1,800-1,900 m.

The hole was collared vertically on March 6, and was

completed August 2nd, 1983 at a depth of 1,952.7 m. The

drill log appears in Appendix I.

A vertical section (Dwg. 5498) illustrates the

structural and stratigraphic features observed in core.

The hole was collared 85 feet southwest of the

northwest striking contact of the Cedar Lake pluton. It is

located 1,350.79' on a true bearing N44 0 2'33"E from post #3

- 4 -

of mining claim TB614189. The only interesting

mineralization encountered in the hole was intersected

between 1,833.6 and 1.834.1 m, in which a sericitic

siliceous unit contained minor molybdenite mineralization.

No economic gold values were associated with this sulphide

horizon.

Twenty-three wedges were necessary to a depth of

1,225 m to keep the hole from flattening beyond 80 e

(Appendix III). At a depth of 1,272 m, the inclination of

the hole reached an unacceptable angle of 78 e and the Navi

system had to be employed (between depths 1,272-1,372 m) to

steepen the inclination to 84". At the end of drill hole,

the inclination of the hole was 69*.

The average azimuth of the hole is 225*, approximately

perpendicular to the strike of the strata.

The hole was drilled using NQ diameter bits. The drill

core is presently stored on the property of International

Corona - Teck Corporation joint venture.

FINANCIAL REPORT

Teck Explorations Limited managed the exploration

program on behalf of Arctic Red.

The total eligible Exploration Expenditures for the

period April 1, 1983 to December 31, 1983 amounted to

5259,152.16. Copies of Teck Explorations' invoices and the

OMEP Form 2 are included in Appendix IV.

TECK/EXPLORATIONS LIMITED

M. Blecha, P. Eng. /January 11, 1984"

#915T:42 C/12 G RQ-86

LEGEND

ARCTIC RED RESOURCES CORP.

12 DIABASE DYKES

11 (LATE) FELSIC DYKES AND SILLS

11A PEGMATITE

11B GRANITE

11C GRANODIORITE

10 MAFIC SILLS AND DYKES

10A MAFIC SILLS AND DYKESt Fine grained, massive to moderately schistose chlorite rich sills and occasional dykes. Some contain calcite. All show sharp unchilled contacts.

10B AMPHIBOLITE DYKES: .Coarse grained, rather massive dark green amphibole and chlorite rich dykes and occasional sills.

9 PORPHYRY SILLS AND DYKES

9A INEQUIGRANULAR FELDSPAR PORPHYRY: 10 to 301 coarse feldspar porphyroblasts (up to 1 cm) set in a fine grained, uniform, massive, weakly magnetic, biotite, chlorite, feldspar-quartz rich groundmass.

9B QUARTZ FELDSPAR PORPHYRIES: Medium to coarse grained sills. Light grey to rather dark grey-green matrix. Feldspar and quartz phenocrysts account for up to 401 of the unit. Contacts show no chill margins and are generally very sharp.

9C PSEUDOPORPHYRIES: Vague dark grey, weakly porphyritic, fine grained groundmass with 5 to 201 silicate phenocrysts which possess a perfect cleavage.

8 HETAVOLCANICS AND METASEDIHENTS

8A Interbedded amphibole-rich flows and tuffs.

8B Massive quartz-biotite-feldspar unit with grain size ^0.5 mm. Unit is foliated and exhibits gross bedding features on weathered surfaces.

8C Massive quartz-biotite-feldspar unit as above but coarser with minerals jC2 mm. Unit generally occurs as interbeds in 8A.

8D A quartz-biotite-feldspar unit with interbands OO cm of white quartz-feldspar+minor mafics.

8E Similar to 8D but bands are MO cm thick.

- 2 -

MBTASKDIMKNTS

7A Pine to medium grained, dark brown to black biotite gneisses and schists containing pervasive garnet porphyroblasts (almandine) . Unit may contain minor sericite and/or amphibole inter beds.

7B Fine to medium grained , dark grey to black biotite-sericite schists minor gneisses containing abundant staurolite and garnet with less frequent chloritoid and sillimanite.

7C Fine to medium grained/ light grey to brown sericite-biotite schists sericite interbeds give distinctive thinly laminated appearance.

7D Fine to coarse grained, dark grey to green well banded unit containing biotite-sericite gneisses and schists alternating with coarse grained calc-silicate beds. Calc-silicate beds typically range from 1 to 40 cm in width and comprise less than 3(tt of unit thickness.

7E Very fine grained, light grey to grey-green finely laminated siliceous sediments (may in part be chemical sediments - cherts) containing narrow biotite schists interbeds. Finely disseminated pyrite H-3%) along bedding planes.

7F Fine to medium grained, brown to black quartz-biotite schists and gneisses, typically thickly bedded metasediment s with minor sericitic interbeds. May in part be gradational into Unit 5.

7G Quartz-feldspar-biotite-tremolite (OOt) with 5-10 cm wide bands of bluish actinolite.

7H Amphibolite with pervasive magnetite.

6. VOLCANICLASTIC ROCKS

6A Black to dark green, calcareous volcaniclastic unit composed of ash to lapilli size leucocratic fragments and/or phenocrysts and less common lenticular mafic fragments (biotite rich). Matrix typically mafic and schistose.

6B White to light grey, calcareous volcaniclastic unit containing abundant quartz eyes and/or crystals and reworked felsic pyroclast ic/volcanic material.

5 METASEDIMKNTS

Fine to medium grained, dark grey-blue banded to fragmental siliceous unit may contain pyrite and MO&2*

4 VOLCANICLASTIC ROCKS

Medium to coarse, intermediate to felsic volcaniclastic material set in a chlorite groundmass. The groundmass contains minor magnetite .5 to 51 pyrite, biotite, feldspar, minor sericite and minor oellacherite

- 3 -

MOSCOVITE SCHISTS

Foliated muscovite and quartz eye rich pale yellow schist containing .5 to 21 pyrite and up to 21 fine brown tourmaline crystals and rare oellacherite wisps.

HETASEDIMENTART BOCKS

2A Fine to medium grained, pale grey to dark green black, metasedimentary unit composed of intercalated biotite-garnet rich beds and amphibole-pyroxene (?) beds.

2B Fine to very fine grained, pale grey green siliceous metasediment containing fine pyrite lamination (2-101

2C Rather massive fine grained, brownish grey pelitic metasediment containing abundant biotite, feldspar and chlorite. Generally capped by 1-5 cm magnetite, chlorite, pyrite rich interbeds.

BDRHBLEHDE SCHISTS

1A Medium to coarse grained, dark green hornblende-chlorite schist, locally magnetic.

1B Fine to medium grained, dark grey green biotite gneisses to schists. More massive textured than Unit 1A.

X PJD-330 15/2/84/cs

R PJD-2l3(a) 5/12/83 TECK EXPLORATIONS LIMITED DIAMOtO DRILL LOO

AR-1HoleSheet 1 of 27

Job 1419 N.T.S. 42 C 12Property ARCTIC RED/PINE ELLTownship BOMBf Twp. On t.Location: Line 20+23*

Station 7+84NElevation 318.5 m

Logged R, Quartern* In

Remarks

Objective To test for the extension of theCorona mineralization at depth

Drilling Co. Midwest Drilling, Winnipeg

Commenced March 6/63Completed July 31/83Length 1952.7 m

Core Location - Corona core shack1

Distance to waterCasing Lost 4 m

Core Size NO

TestsDip Azimuth

At Collar 90* 197*

Depth (m)From

0

4.0

5.2

5.95

7.25

B.I

To

4.0

5.2

5.95

7.25

6.1

9.75

Rock Type

Casing

6A

1IC

8A

ne

6A

Description

Remark; Hole AR-1 collared on Feb 28/83 at 90*. At 71,5 m, hole off 3 degrees, terminated and recol lared6' to the northwest on Mar 6/83,

Dark green, silicified amphibolite. Intermixed flows and tuffs with flows predominating. Binding andfoliation Is erratic, but generally at 50* to core axis. Unit has patches of blotlte/garnet and ^f calcitebands and W magnetic pyrrhotite occurring as bleb* and disseminations. Trace pyrite. The pyrrhotite Isresponsible for the mag high and the gossan at the granite contact.

Massive, medium gray granodiorite with 5-101 biotite, ^OJf quartz and 75? feldspar/plagloclase dominant.The unit has a slight porphyritic appearance with OJf phenocrysts. It Is not like unit 96 of Corona - It Ismore massive and equigranular. The unit lacks a strong foliation, Trace garnet end pyrite.

Typical,

Typical, Contact at 45* to C. A.8.0 Muscovite mlcroveln ' :

Typical.8.4 - 9.1 Ojt garnet porphyroblast*.9.73 - 9.75 Quarti vein.

R PJO-2l3(a) 13/7/83 TECK EXPLORATIONS LIMITED DIAMOND DRILL LOO

Hole AR-1Sheet 2 of 27

Depth (m)From To Rock Type Description

9.75

19.9

21.3

20.67

33.95

35.35

37.7

38.4

42.35

19.9

21.3

28.67

IIC

8A

ne

33.95

35.35

37.1

38.4

42.35

56.5

BA

11C

8A

IIC

8A

ae

Typical. Unit has OJ quartz veins and biotite xenolith* <3 cm. 10.8 - 10.85 Quartz vein 19.9 - Contact Irregular

Typical. - * 20.5 - 20.52 Quartz vein

Typical.26.4 - 26.43 8A27.0 - 27.04 8A ' 28.67 Contact at 30* to C.A.

Typical, tending at 50* to C.A. 29.95 - 30.2 IIC with calcite velntng 30.85 - 31.2 IIC with coarse muscovite vein 33.47 - 33.6 IIC

Typical.Contacts at 57* and Irregular.

Typical. 36.9 - 37.2 10| disseminated pyrrhotite

Typical,

Typical.Lower contact at 35* to C.A,

Massive black blotlte-quartz-feldspar siltstone. Minor banding, minor quartz velnlng, abundant chlorite- sericite mlcrovelns with random orientations. Weak foliation developed at 40* to C.A. Minor pyrite Minor pyrite mlcrovelns,

47,6 - 48.45 IIC at 30* to C,A. Contacts are IIC porphyritic while center of unit Is good granodiorite49.0 - 49.03 Quartz vein

R PJD-213(a) 13/7/83 TECK EXPLORATIONS LIMITED DIAHOM) DRILL LOO


Depth (m)From

56.5

57.9

58.5

61.0

65.05

68.3

69.23

71.63

74,2

74.55

75.3

75.7

76.0

76.6

82.2

87.9

To

57.9

58.5

61.0

65.05

68,3

69.23

71.63

74.2

74.55

75.3

75.7

76.0

76.6

82.2

87.9

91.3

Rock Type

98

80

9B

8B

80

8B

9B

80

96

BB

9B

80

9B

80

BB

80

Description

Porphyritic sill. Dark green with 501 white phenocryst* of feldspar In a finer chlorlte-rlch matrix.Unit Is foliated. '

Banded metasediment with *t cm white and black Interbands at 40* to core axis.

Typical.

Typical.

Typical,

Typical.

Typical.

Typical, fended at 50* to C.A.

Typical.

Typical,

Typical.

Typical.

Typical. Contacts at 35* to C.A.

Typical. Banded at 45* to C.A.81.0 Ground core . -,

Typical.84.0 - 84.25 9B at 40* to C.A.86.8 - 87.2 Epldote/chlorlte velnlng

Typical.86.85 - 89.0 9B and quartz vein69.2 - 69.4 9B

R PJD-213(a) 1 3/7/83 TECK EXPLORATIONS LIMITED OIAHOM) DRILL LOG

Hole AR-I Sheet 4 of 27

Depth (m)From

91.3

92.5

97.0

98.1

101.4

104.5

112.0

115.85

125.46

126.9

138.5

141.6

To

95.5

97.0

98.1

101.4

104.5

112.0

115.65

125.46

126.9

138.5

141.6

143.8

RocK Type

98

88

96

80

ee

Lost core

8C

6B

9B

88

8C

88

Description

Typical. Strong foliation at 45* to C. A.

Typical,

Typical.

Typical,

Typical. 101.5 - 101.65 Quartz vein

Drilled with a blast bit - no core.

Dark, black, massive metasediment* Coarse grained with quartz * \ mm, feldspar j(\ mm and biotite ^2 mm. The unit Is foliated and very homogeneous.

Typical. 118.2 - 118.6 98 122.9 - 123.4 9A at 45* to C.A.

Typical. Lower contact at 40* to C. A.

Typical. 131.9 - 132.8 10| chlorite mlcrovelns at 30* to C.A. 134.0 - 138.0 101 chlorite mlcrovelns with random orientation

Typical.

Typical. 142.3 - 142.9 98 142.9 -143.5 Veined with chlorite mlcrovelns

R PJD-2l3(e) 1 4/7/83 TECK EXPLORATIONS LIMITED DIAHOM) CHILL LOO

Hole AR-1 Sheet 5 of 27

Depth (m)From

143.8

145.7

147.4

148.85

153.1

155.25

156.0

161.0

161.4

166.1

168.0

173.6

To

145.7

147.4

148.85

153.1

155.25

156.0

161.0

161.4

166.1

168.0

173.6

175.4

Rock Type

8C

se9A-B

88

8E

98

No core

98

6E

9 B

8E

No core

Description

Typical.144.9 - 145.2 12A

Typical. Foliated at 45* to C. A.

Typical.

Typical.150.0 - 150.2 98150.2 - 150.66 Veined150.66- 150.80 I0e amphibolite vein at 42* to C.A.151.1 - 151.2 98151.6-151.95 98 at 46* to C.A. '152.5 - 152.7 10| quartz blebs152.7 - 152.75 5* pyrite

Typical. :'

Typical. '

Wedge. ;

Typical.

Typical, tended at 40* to C.A.

Typical.

Typical.168.0 - 190.0 Chlorite mlcrovelns '172.0 - 173.6 Veined ' i

Wedge.

R PJO-2l3(a) 14/7/83 TECK EXPLORATIONS LIMITED DIAMOND DRILL LOS

AR-1Hole

Sheet 6 of 27

Dopth (m)From To Rock Type Description

175.9

191.65

221.5

227.5

240.9

191.85

221.5

227.5

240.9

242.5

8E

9B

SB

10A

Typical. Eonded at 50* to C.A. 10* chlorlte/serlclte mlcrovelns.180.15- 180.9 98184.1 - 184.4 Silicified, brecciated section198.8 tending at 45* to C.A.

Typical, Core blochy.197.5 - 197.6 9B200.1 - 200.15 Quartz vein212.0 - 213.0 Core blochy. Cut by diabasic mlcrovelns215.5 Possible fault zone217.0 - 217.15 9A218.3 - 219.5 I2A contact at 15* to C.A.219.8 - 220.2 98221.0 - 221.15 9B221.4 Bunded at 40* to C.A.

Typical. Foliated at 49* to C.A. Has minor sections of 9A and 10A(7). 223.2 - 223.9 12A 224.2 - 224.4 12A 225.0 - 225.2 I2A

Typical.230.5 - 231.0 5J epidote mlcrovelns and brecciated areas237.0 - 237.3 9B

Typical. Dark greenish gray porphyritic dyke. Fine (O mm) groundmass of fxspar with green amphibole chlorite augens ( 4i1), 30)1. '

R PJO-213(a) 1 3/7/83 TECK EXaORATIONS LIMITS) DIAMOND DRILL LOG


Depth (m)From

242.5

301.0

305.7

319.7

To

301.0

305.7

319.7

321.2

Rock Type

88

BC

ea

9B

Description

Typical, Some carbonate-rich bands ^2j().249.6 - 250.0 IOA252.7 - 252.76 108255,9 - 256.4 8C256.7 - 256.8 98257.0 Banding at 40* to C.A.260.2 - 260.4 IOA263.0 - 263.5 Epidote, chlorite altn with M d isseminated pyrite.265.2 - 271.3 5j( hematlte/epldote microvelns at random through the Interval, minor calcite. Some epidote

veins remained with hematite at 30* to C.A,271.3 - 275.0 2jf hematite/op I dote microvelns279.4 - 279.6 Epidote microvelns262.8 - 283.3 Epldote/calclte vein at O* to C.A.264.9 Quartz/calclte/epldote patch285.8 - 286.5 lOo286.7 - 287.7 60 with hematlte/epldote300.2 - 301.0 diorite

Typical. Altered by epldote/calclte/hematlte to light green colour.

Typical. Cut by numnerous calcite microvelns. From 305.7 to 310.1 looks like unit 8A (andesite).307.2 Epidote vein with breccia Infilling307.9 - 308.3 Pink calcite vein with 20*1 hematite stain and cut by microvelns of specularite hematite.

Vein at 80* to C.A,308,7 - 308.9 Pink calcite vein - Irregular contacts309.1 - 309.7 Pink calcite veins - Irregular contacts -310.1 - Typical 88308.9 2 blebs of chalcopyrite In an epidote vein313.8 - 319.7 7 calclte/quartz/f luorlte veins (^jf fluorite) with a random orientation

Typical. Contact at 48* to C.A. Foliated.

L

R PJD-213(a) 1 3/7/63 TECK EXPLORATIONS LIMITED DIAMOND (RILL LOG


Depth (m)From

321.2

324.55

325.65

336.65

337.45

386.1

392.0

To

324.55

325.65

336.65

337.45

386.1

392.0

394.2

Rock Type

68

98

66

IOA

8B

BE

98

Description

Typical,

Typical.

Typical. Wedge at 33*.

Typical.

Typical. Black, massive. Minor epidote mlcrovelns and quartz veins. Minor 8C,353.5 - 344.0 9E344.5 - 346.0 5* quartz veins354.0 Foliation at 42* to C. A.355.8 - 356.3 BC357.2 - 357.7 B-eccla zone. Silicified. 2* dark red hematite stain with W d isseminated pyrite.

Zone at 15* to C.A.360.1 - 260.13 Quartz vein i .363.2 - 363.25 Quartz vein367.0 Epidote mlcrovelns at 7* to C.A.371.8 - 372.4 9A with epidote mlcrovelns374.3 - 374.33 Fluorite veins378.38 Wedge384.9 - 384.97 Quartz vein384.97- 385.4 1* disseminated pyrite

Typical.387.0 0.5 cm chloritic slip390.0 Epidote mlcrovelns at 13* to C.A.391.0 Banding at 40* to C.A. ;

Typical .

R PJD-2l3(a) 1 3/7/63 TECK EXPLORATIONS LIMITED DIAMOND DRILL LOG


Depth (m)From

394.2

396.5

409.6

412.6

To

396.9

409.6

412.8

542.65

Rock Type

BE

88

8E

68

Description

Typical.

Typical.399.0 0.2 cm pyrite band400.0 - 400.5 Epidote ml cr eve Ins (with chlorite)401.5 - 402.0 Epidote microvelns (with chlorite)402.3 - 403.0 BC403.0 - 403.5 10| quartz velnlng with chlorlte/epldote microvelns405.0 - 405,3 Epidote/chlorlte microvelns405.3 - 406.0 80407.75- 407.79 (Juertz vein

Typical.

Typical. Some banded areas. Generally dark green. K SI quartz veins.412.8 - 415.8 51 chlorlte/epldote microvelns414.05- 414.15 Epldotlzed aplite with If cubic pyrite415.8 Hematite microvelns420.6 - 420.7 Epldote-rlch section ,421.4-422.1 Silicified epldote-rlch section. Very hard423.5 - 425.0 10* epidote chlorite microvelns at 10* to C.A.427.0 B-own colour with KlOjf pyrite438.4 - 438.6 Quartz vein445.7 tending at 42* to C.A.446.1 - 446.3 Silicified breccia zone445.0 Ebndlng at 45* to C.A.456.7 - 459.5 102 erratic quartz velnlng, minor epidote microvelns463.0 Banding at 45* to C.A.Comment: Unit very massive homogeneous. Minor calcitic patches.487.0 - 489.0 3 graded beds fining down the hole* Either a metamorphic feature or beds are overturned -

bending at 46* to core axis*

rR PJD-2l3(a) 1 3/7/83 TECK EXPLORATIONS LIMITED

DIAMOND DRILL LOO



412.6

542.65

554.6

560.65

566.4

569.6

561.3

. .continued

554.4

560.65

566.4

569.6

581.3

503.6

ec

88

88

BC

8B

9B

495.3 - 496.5 Zone of sillclflcaton with 10* epidote, 91 amphibole and a moderate blue mineral Inmlcrovelns cutting the core at 12* to C.A. and 20* to foliation. 1* disseminated pyrite.

498.2 - 498.5 201 quartz-calclte volnlng. Looks Ilk* o fragmental but only optical. 503.5 - 504.0 Minor silicification . ' . 519.3 - 520.5 Epidote alterations522.5 - 523.5 Coarse silt/sand with 5 mm sized fragments523.8-526.2 Epldote-cMorlte mlcrovelns at 25' to C.A. i527.2 - 527.4 Disseminated pyrite < \il m inor pyrite vein :533.1 - 534.1 10} epidote veins534.5 - 542.0 Numerous quartz calcite veins. Section contains silicified patches with a cherty appearance,

Typical. Equigranular, massive with 1-2 mm quartz-fxspar grains. Minor lenses of 88 (6*). Minor quartz- calclte velntng (40)1) with purple fluorite. . :

Typical. With 10)1 quartz calcite veins. 552.4 - 552.7 Zone of silicification along a quartz vein558.9 - 560.65 Zone of silicification with 25jf carbonate, minor epidote along a chert band l cm wide at

^90* to C.A. Appears to cross cut mineral foliation, so not a primary structure.

Typical. Note contact Is Irregular, cross-cutting the foliation. 565.4 - 566.4 Epidote along fractures almost parallel to core

Medium ground blotlte-feldspar foliated, massive sediment with a few thin quartz-feldspar bands.

Fine-grained, typical, with minor epidote along fracture, and some bleaching, a few ptygmatic quartz-feldspar velnlets, gradatlonal, coarser grained sections. ' 570.6 - 570.8 Quartz-feldspar-epldote alteration with a disseminated py halo 0.2 m from bottom. 575.7 1 cm quartz-feldspar vein at 5*

Upper contact 52*; lower contact 50*. Minor barren quartz velnlets, trace Kspar along fractures.

R PJD-2l3(a) 13/7/83 TECK EXPLORATIONS LIMITS) OIAHOND DRILL LOG


Depth (m)From

583.6

(595. 5)

603.0

607.5

671.0

673.5

To

605.0

605.0

607.5

673.5

673.5

683.2

Rock Type

se

BB

8 B, C9A

9B

9B,ee

BC, B

Description ' '

Typical.585.7 - 588.0 Coarser foliated blotlte-feldspar-amphlbole unit 6C(?) with a few epidote spots and fractures582.2 5 cm Kspar alt. t 20*592.9 15cm OJ'Z-epl-emphlbole zone

Typical. With abundant qtz-carb-chl bleached fractures and minor granitic patches at 599;bleached fractures to 601 ,

Lost core, wedge.

Continues typical, minor 8C beds with minor ...608.5 - 608.8 Medium gray slag porphyry) upper contact at 48*, lower contact 1 55*} 0.5Jf py608.9 - 612.0 Very blocky core, 8C Interbed614. 0 8C, 88 bedding 1 18* to C. A., somewhat Irregular619.0 - 623.0 Foss abundant qtz-carb-chl -epl In fractures628.5 Goudlnaged q.v, 1 approx 10* to C. A. .632.0 - 637.0 Bedding at 46*. 49*634.1 - 634.9 80 ted with prob If py, and a 2 cm py+mag+qtz pebble641.0 - 642.9 Abundant plag-pheno-porph, upper contact poss foliation 0 45*; lower contact obliterated by

abundant q.v. In lower 0.5 m ,655.1 Approx 10 cm zone In foliation with abundant calcite velnlng, poss brecciation657.3 1-2 cm fluorite * calcite vein i660,7 - 666.65 Abundant plag-pheno dikes, 6 separate dikes of 20-120 cm thick with 88 screens with possible

rare xenos; dikes prob 90-60* of 1 nterva I.*. contacts general ly sharp at 45-60* to C. A. |668.3 20 cm calcite velnlng * brecciation j

Lost core, wadge* j

Typical, medium to coarse grained grits; grain size changes give some bedding - 51* f 679 m. \ '681.1 - 681.4 Fine-grained mafic dike, 2 xenollths within j679.9 py * mag patch approx 2 cm (disrupted layer?) ,683.2 Bedding 1 73* to C.A. ! ;

* *.R PJD-2l3(a) 14/7/83 TECK EXPLORATIONS LIMITED

DIAMOM) WILL LO3



663.2

745.9

765.0

607.0

821.0

634.0

652.7

765.0

607.0 (805*)

621.0

634.0

652.7

1050.2

8 B, C

Wadge

BC, B

BB

68

8C,B

9C

90

Typical. Flne-to-medlum grained massive blo-chl-qtz-feldi, -695.3 - 697.6 Pinkish Kspar/hem?) * chloritic alteration, with epl along hairline fractures699.6 - 700.6 Pinkish alteration as abovei pervasive chloritization703.1 - 707.7 Hore Intense, localized zones of pink-orange alteration, brecciated zones with blue-green

chloritic gange at 703.5 * 705.5} q.v. for 20 cm at 705.2 Bedding prob 51* at 712 m. Irregular/wavy prob 23* at 725 m Probable graded bed at 749-74 m , tops up, S0 prob 12* to C.A, 742.7 - 743.2 and 744,0 - 745.0 post moderately chlorltlzed rock, due to epl *.chl-qtz filled fractures

745.9 - 746.4 prob 2.5 cm lost core (only 0.4 m lost)752.4 Quartz vein (759.04765 Bedding (S0 ) prob 5-6* to C.A.

Typical medium to coarse grit...hole Is approx downdip so very little lithologic variation i 791,0 - 792.0 and 804.0 -805.0 Bidding at prob 5* to C.A..... , Typical... lower contact poss 10 cm quartz vein

Typical, with a few coarser-grained, quartzose patches, and a few buckled q.v's (O cm); lower contact Is bedding, jcS* to C.A. for approx l m, then changes to approx 30* to C.A. (came contact).

Typical, no change*822.0 Wedge, approx 2 m lost core. Contact l 834 m Is approx 5* to C.A.

Typical, no change. , ; 835.5 5-10 cm Irregular quartz vein l 45*-SO* to C.A.

Typical, upper bedding contact prob 8* to C.A,i gradual change over approx 2 m from fine 80 to typical e.g. grit... variations over Interval primarily due to presence of dikes and local bleaching - epidote zones ... 864.8 - 865.2 Mod-gray, 10-201 small plag phenos (1-2 mm) porph dike, contacts prob 40* to C.A, (lower

one with quartz) 869.2 - 370.5 Hed-to dark gray, otherwise as above) texture i colour variable due to Included 8 and later

quartz vein '

ft PJO-21i(a) 1 3/7/63 TECK EXPLORATIONS LIMITED DIAHOM) DRILL LOG


Depth (m)From To Rock Type

9C

9CWedge

se

se

BCec

ec

Description '

678.1 - 678.4 Highly Irregular, lensold, dark green, coarse-grained amphibolite slices within Intervalapprox 1 0* to 29* to C.A.

880.4 - 880.9 Neakly to typically porphyritic dlkes(s), with slice of 8 within; Irregular lens of py * eplat upper contact, 0-2 cm j lower contact prob 49* to C.A.

888.3 - 688.8 Med -* dark gray typically porphyritic, contacts at 45* to C.A.891.0 - 894.0 Prob 2.2 m lost core895.5 sil * epl fracture zone/F.Z. 1 approx 45* to C.A.903.7 and 904.2 Grain-size variations * colour changes suggest bedding, 9 60* to C.A. i 32* to C.A.....?

No other bedding dlscernable until ^934.5 - 935.1 Typ gray, small plag pheno porph dike) upper contact Irreg approx 6 70*; lower 9 4 5* sharp938.5 10-15 cm of hem alteration from cal * eh) fractures943.5 - 944.7 Typical, upper contact 9 50*j lower obscured '944.7 - 945.6 Silicified and partially hematlzed fine-grained hornblende porph dike, lower contact 9 1 5*

to C.A. Gadding axes .., probable (laminations) " 20* t 931.5 m, 3056'.Definite C/F contact - 30* 9 934.1 m, probable (lams) - 0*-14*. Variations 9 938.5 m.contorted laminations prob 35* 1 99,3 m -* looks like a flame structure...

Largely 6B but gradations of 8&-8C are subtle*959.2-959.3 Qtz vein959,4-959,7 0.2-0.9 cm qtz-calclte veln-ptygmatlo, parallels core axis ,962.7-962.9 Coarse Interval with qtz-feldspar <3 mm ''963.3-963.6 Coarse Interval with qtz-feldspar <3 mm erratic contacts '964.0 Biotite rich bands (7) at 38*-91* to C.A. .966.4 Calcitic patches oriented at 49* to C.A,968.6 Possible bedding at 26* to C.A. !969.0-978,0 Typical981.36 Contact between BC and 68 at 95* to CA. fining upwards982.5 Chlorlte-serlclte veins983.4 Quartz vein - U shaped '985,5-985.9 Minor S fold Indicates fold axis of synform In up hole. This observation Is at best tenuous

banding of biotite at 39* to C.A. :

R PJD-2I3U) 14/7/63 TECK EXPLORATIONS LIMITED DIAMOND DRILL LOO '


Depth tw)From To Rock Type DeterIpt lon

852.7 1050,2 Cont'd

1050.2

1053.l

1053.1

1097.3

8C

8C

ec

8E

986.1 ' Foliation at 40* to C.A. ,990.7 Godding at 20* to C.A., minor ptygmatic folding992.2-992.8 t cm qtz vein para l le l s C.A. '999.35 fed dIng at 25* to C.A,Note: Although bedding Is not obvious tt appears that the mineral foliation Is at an angle of 66* to bedding

on a face of core cut perpendicular to the core axis,1003.8-1004.0 Erodlc bedding

0.5 cm ptygmatic quartz vein parallel to C.A.Quartz vein with minor calcite ' : \Ptygmatic quartz vein at 12* to C.A.Coarse unit with 5* feldspar phenos (t) contacts at 40* to C.A. |Biotite banding at 35* to core axis ' 'l cm ptygmatic quartz vein at ,Quartz vein at 90* to C.A. iFeldspar phenos and carbonate-rich porphyoblasts (patches). Possible a tuff band. Feldsparphenos are rt mm In size .

1033.2 Contact of BC and 8E at 50* to C.A.1037.4-1037.6 Ptygmatic quartz vein Vj1036.0 fending at 25* to C.A. i1047.0 Mineral foliation at 47* to C.A.

1010.8-1011.51013.1-1013.251016.5-1016.91017.1-1017.351021.01030.51031.4-1031.51031.5-1032.0

Typical. Equigranular* carbonate augoout (601 of unit) and sedimentary clasts rt similar to 86 and 8C.

Typical. 15-201 8B throughout.1053.5 Contact of 8&/8C at 53* to C.A.1055.7 Lacks carbonate patches but has scattered silt fragments1057.0 Mineral banding at 18* to C.A.1060.0-1065.0 Foliation at 56* to C.A. but erratic mineral bending (bedding 7}1079.5 8B/8C contact at 54* to C.A.1089.4-1090.2 Erratic blotlte/chlorlte banding S folds

cm. Compositional l y

•/•"t"

R PJD-213(a) 13/7/81 TECK EXPLORATIONS LIMITED DIAHOM) DRILL LOO


Depth (m)from To Rock Type Description

097.3 Cont'd

1097.3 1225.3 68

80ec

1095.5-1096.5 10* carbonate patches1097,3 Irregular contact at 25* to core axis. Contacts due to compositional variation between a

chlorlte-amphlbole unit and blot 11 le unit, If bedding the contact Is a slump feature Indicating tops up hole ' . i !

Typical. Sections of BC throughout. i '1099.0-1100.0 5JJ carbonate spots

Ptygmatic quartz veinBiotite rich section35* to C.A. (compositional banding - bedding) 'Quartz vein ,fending at 45* to C.A. i -' 'From this point down the holt there are numerous green chlorlte-quartz mlcrcvelns cuttingthe biotite unit. The veins are at random directions to the C.A. but generally less than25* to C.A. Stop at 1174 m. '301 chlorlte-slllea velnlets :5 cm quartz vein !Quartz vein (bull quartz)Quartz vein

1101.31102.0-1102.71102.71105.4-1105.471105.51105.5

1127.5-1128.01130.51139.5-1139.61156.8-1157.61157.77-1157.791159.01162.3-1162.81163.01165.01170.7-1170.91173.5-1173.61174.8-1174.651175.75-1175.91176.5-1177.851178.01192.9-1193.0

Bedding 70* to C.A. Tops up hole.

Contact between 8B/8C

3 cm cherty band.Quartz veinBedding at 67* to C.A.Bedding at 64* to C.A.Quartz veinHealed breccia zone with epldote/chlorlte 'Milky quartz veinBanded at 63* to C.A.Typical. Mass lv. Irregular contacts.Binding In core Is more abundant, 2-3 bands every metreQuartz vein

*

R PJD-2l3(a) 13/7/83 TECK EXPLORATIONS LIMITED DIAMOND DRILL LOG

Hole AR-ISheet 16 of 27


097.3

1225.8

1272.0

1372.0

1374.1

22S.3

1272.0

1372.0

1374.l

1380.5

Cont'd

Navl

7

70

7C 7F 7 7F

6B

1193.4 tending at 68* to C.A. '1195.0 Appearance of garnetiferous epidote rich bands and calcitic patches at 35* to C.A. 1224,0-1225.3 Unit has a granitic appearance. Coarse (2 mm) feldspar, quartz and biotite. Unit Is ! '

equigranular* '

Corona hanging wall unit, Typical banded metasediment with bands < ^ cm. Contact with overlying unit Is verysharp, fending results from lighter sericitic sections between darker sections. The dark sections arebrown to black In colour reflecting variations In the changes In biotite colour. Minor amphibole bands givethe unit a 70 appearance, X-beddlng at 1249,5 Indicates tops down the hole. !1258.5-1258.7 Quart* vein1260.0 fending at 52* to C.A.1265.0-1267.0 Of garnets '1270.0 fending at 52* to C.A.5-10 cm calc-silicate bands, t every 30 cm r

No core recovery . ,

Unit below navl approaches 7C.1372.0-1372.5 Not typical1372.5-1373.1 Not typical, unit consists of blotlte-chlorlte-feldspar-garnet1373.1-1373.3 Light grey/brown colour, silicified ;1373.3-1373.87 Not typical. Unit consists of blotlte-chlorlte-feldspar-garnet In a masslve-homogenecus-

equlgranular unit 1373.87-1374.1 Elongated fragments O cm x .9 cm of a siliceous-feldspar rich composition. Contacts at 55*

to C.A. * ' ' i

Typical. Contains II calc-silicate bands In centre of Intervals, :1374.5-1375.0 51 andalusite1379.0-1379.3 Amphibolite s ill1379.9-1380.1 Coarse metased with 20* feldspar 2 mm In site1379.4 Q.V. at 20* to C.A.

R PJD-213(a) 13/7/83 TECK EXPLORATIONS LIMITED DIAMOND GRILL LOO


Depth (m?From To Rock Type Description

1360.5 1385.0

1385.0

1365.0

1383.83

1367.63

1366.23

1369.95

1391.6

1392.2

1393.5

1385.63

1387.83

1388.23

1389.99

1391.8

1392.2

1393.5

1394.9

Note

7D

6A

Not typical. Has a gneissic appearance In places. Silicified unit light brown/grey colour with feldsparphenos (?) throughout. Fragmental In places* Patchy Kspar/amphlbole alterations.1380.7-1380.75 quartz veinUnit has a bleached blotlte-qtz-feldspar metasediment between fslc u nits

From 1385 the stratigraphy Is ery erratic with Intermixed maflc/felslc rich and fine/coarse units. There Is minor pyrrhotite throughout both as fine disseminations and In mlcrcvelns. Trace chalcopyrite occurs and massive garnet-amphlbole sections may Indicate l.F, There are finely lamlated siliceous sections that look like a chemical sediment. ' -. .

Not typical, More massive than finely banded 7D. Minor pyrrhotite.-, ' ii

Massive green amphlbole-garnet unit...Silicate Iron formation* Silicate Iron formation with disseminated pyrrhotite Of.

Cherty tuff. Eelge coloured banded unit with chert (T) bands layered with sericitic quartz rich bands. , Banding at 52* to C.A.

, i. Coarse, massive, blotlte-qtz-feldspar rich unit* Pyrite occurs In mlcrofractures through unit. '

Not typical. Good flattened silicified fragments. Feldspar O mm pervasive through unit as clasts Ci), 2 very fine cherty sections.

Cherty tuff. Same as 1387.83-1388.23. Efended sillclfled unit with tiger stripe appearance.i -

Silicate Iron formation with abundant garnet-amphlbole. 1392.7-1393.0 Massive pyrrhotite vein with O* chalcopyrite.

Chert, fended at 50* to C.A.

R PJD-2IJ(a) 13/7/83

i! .A

h ;ji

TECK EXPLORATIONS LIMITED

DIAHOM) DRILL LOOHole AR-1Sheet IB of 27


1394.9

1402.7

1412.0

1413.6

1416.1

1402.7

1412.0

1413.6

1416.1

1421.3

1419.75 1425.7

7/6

7B

76

7B

7C/6

70

7C

70

Medium brown colour unit with Interbedded finely laminated metasediment* and some siliceous patchescontaining feldspar eugans O mm* Clastic sedimentation predominates with some chemical sediments and 'lesser fragmental material*1396.9 Pyrrhotite1398.4 Pyrrhotite mlcroveln1399.34-1400.0 Silicate Iron formation. Massive green band of garnet end amphibole with OOjf matasedlments.

At 1399.36 2 cm of stringer pyrrhotite. - HOI.7-1402.1 68 not typical. Chert? fragments. 80* In a biotite feldspar matrix.

Typical. Green-brown banded with emphlbole/calclte bands separated by biotite rich bands at 55* to C.A. Minor pyrrhotite In the calc-silicate bands. The unit contains e few i garnet and a few f s illimanite. The sillimanite occurs In layers and Is not as pervasive as the garnets. Mlonr staurolite as of 1410.0 m. : 1402.7-1405. Typical. Lacks calc-schtsts bands but Is assumed to be part of the 70 unit1410.1-1410.2 Pervasive garnet ^2011410.2-1410.65 Grit unit contactT at 40* to C.A.

Not typical. Massive block biotite rich unit with OO lathes of tremolite (?). 1412.9-1413.6 Massive amphibole (tremolite unit) 1413.3-1413.4 freed o tone with 70* fragments 301 calcite

\

Typical. Not crenulated - no muscovite. Abundant ga-bl-sl- (andaluslteT)-st.1414.3-1414.35 tourmaline rich band!414.91kyanlteT

Not typical. Siliceous qtz-feldspar rich unit with 20]f 7 (blotltlc) sediments* Seme sericitic laminations. 1418.4-1419.0 Silicified. Not typical. Few ghost calc-sllleate bands. 1419.3-1419.4 Pyrite 1419.75 Pyrite

Not typical. Silicified, fended at 55* to C.A.

R PjO-21i(a) 14/7/83 TECK EXPLORATIONS LIMITH) DIAMOND DRILL LOO



1425.7

1430.4

1438.85

1442.6

1456.6

1430.4

1438.65

1442.6

1456.6

1476.5

7B

7B

7F

6A

6B

7F 7F

Typical. Ehnded. Not cranulated.1429.0-1429.3 Grit unttT Looks Ilk* pseudo 98 , . '1429.17-1429.27 Q.V. at 70* to C.A. at 50* to foliation !

Typical. Massive. Abundant st (OO*)-ga(40jf)-sir(Ojf).1431.4-1431.7 Chloritoid?, disseminated O|1434.95-1435.4 4 veins have a ye MOM mineral stain (carbonate?)1437.8-1438.8 Ipf andesite (?)

Banded unit with calcitic rich bands O cm. Banded at 56* to C.A. 1438.9-1439.0 fi-eccla lone cemented with calotte 1439.2-1439.4 B-eccle Zone cemented with calcite

Not typical. Btotlte-feldspar rich section* These are occasional fragments and the Interval as a whole has an appearance of a unit approaching anatexis. This may b* due to large granitoid fragments In the unit. Some calsts approach 5 cm In size. ,1442.7-1442.7 Typical. Good fragments1455.4-1455,7 Good fragments ,

t r*~~~ - — '~^

Typical. Light gray unit, very siliceous with abundant porphyry and chert clasts. Contains minor 7F bandsas carbonate rich, homogeneous, sandy (T) Intervals* The unit Is weakly calcareous throughout and hasdisseminated pyrite K2|,1456.6-1459.0 Epidote and chlorite through Interval OOJ1463.5-1464.0 With 5J finely laminated pyrite1464.9-1465.4 With 5J finely laminated and patchy pyrite1475.0 Banding at 56* to C.A.1469.8 Calclte-quartz vein - ' ,1470.4-1470.43 Q.V. at 35* to C.A. Large garnet crystal O cm :'1473.8-1473.9 Fault gouge . ' .)475.8-1476.3 Massive quartz vein , .

,*,

R PJO-2li(a) 14/7/83 TGCK EXPLORATIONS LIMITED DIAMOND DRILL LOO



476.5

1490.0

1494.7

1508.7

490.0

1494.7

1506.7

1551.65

7/6

7F

7/6

7F

7F Foul t

7C

676B

Interval Is dominant l y a finely laminated 7F with sane sericite (7E/7C). 30* of Interval Is slllceous(6) bands which are KlO cm In length and weakly calcareous* There are a few bands of coarser 6B-typlcal. 1476.5-1477.1 ! 1462.48-1482.85 Heterolithic breccia. Fragments are angular K| cm, 90jf of Interval. Zone Is conformable

to bedding but there are no sediment fragments In breccia. They are all exotic and chertyIn nature. ' . . ,

1483.7-1484.6 Calcareous sand with 51 chlorite spots. 1468.0-1490.0 Not typical. Unit has < ^0t sericite and 5* pyrrhotite as fine lamellae throughout unit.

Ebnded at 55* to C.A.

Typical. Has some serlctte-pyrrhotlte rich sections. '1490.8-1491.5 Andalusite rich1493.9-1494.5

Siliceous bands of quartz-feldspar-carbonate O cm are Interbedded with 7F.unit. Ebnded at 55! to C.A. 40J "6. .1502.7-1504.1 Send with calcite end OOf pyrite (1502.7-1503.1)1504.1-1505.6 O0| disseminated pyrite . " j1507.2-1507.6 Good fragments ' ( . " ;1505.6-1505.7 Coarse calcite vein. Calcite crystals O cm

Typical. Some sericitic bands. Some bands of 68 fine grained. White fibrous augens (andalusite?) throughout occur Ing concentrated as patches account for OOJf* In places unit has a crenula ted appearance. Minor garnet. .

30| quart* vein with epidoteAndalusite Is white and pervasive 10* i i fending at 57* to C.A.Quarts vein - 51 green chloritoid? . j l Quarts vein at 30* to C.A. '

Disseminated pyrtle throughout

1524.1-1524.31533.0-1541.51545.01547.8-1547.851548.0-1550.01553.3 1553.4

R PJD-213(a) M/7/83 TECK EXPLORATIONS UNITED DIAMOND DRILL LOO

Hola , AR-1Shaet 21 of 27


1553.65

1569.2

1571.7

1583.0

1594.7

553.65

569.2

1571.7

1583.0

1594.7

1613.2

9A

7F

70

7G

76

76

70

7A 76

Typical. Phenocryst* aligned along foliation at 45* to C.A. ,

Typical. With 5|* andalusite.1556.5-1560.0 Hora or lass typical1560.15-1559.25 Agmatite vain 20J muse - 60* feldspar - 205 qti :1569.0-1560.1 Pegmatite vain at 52* to C.A* Crystals jOS cm, equigranular ,i1561.5 Appearance of garnets Of . '1561.5-1561.6 Minor tremolite i1568.2-1566.5 Core Is blotchy, calcite cemented breccia - fault -

1 - - ' ' i Transition from 7A-76. lOf garnet with 101* amphibole.

Typical - ganded. 10 cm blue actinolite bands separated by 25 cm of tremolite rich ^20jf) metased. fending at 45* to C.A. l j ,

i

Typical massive. Unit Is massive with biotite ^ tremolite ** actinolite. Vary few adlnollte bands.Section has some silIceous-cherty(T) segments. '1584.7 5 cm tourmaline (i20|) vein ,1585.0 EbndIng 35* to 25* to C.A. '1585.6-1586.1 Siliceous cherty Interval, contorted banding {T), largely quartz-amphlbole (chlorite) '1588.1-1589.6 fended cherty Interval of 45* to C.A. '1589.6-1590.4 Cherty section '1589.7-1584.8 Ptygmatic quarts vain 1594.1-1594.16 Quartz vain

Typical massive. BlotIte-tremollte-garnet-tourmallne unit. Foliated but locking banding. 1603.0-1603.4 White andaluclte (7)

R PJO-2l3(a) 14/7/83 TBCK EXPLORATIONS LIMITBO DIAHOM) DRILL LOO

Hola AR-1Sheet 22 of 27

Depth (m)To Rock Type Description

1616.1

1652.8

1660.7

1669.2

1694.7

1695.6

1699.7

76

7G

7G

7G

7G

11A

76

9A 9A

Typical banded. 301 blue actinolite In bands ^30 cm at 45* to C,A,1615.8-1615.63 pegmatite Kspar * qtx16)6.9 Tourmaline i ,

Typical massive. 3| garnet. Minor staurolite. Minor tourmaline throughout. Binding at 65* to C.A. Fewquartz veins,1635.0-1637.0 To-q.v. 5*1651.2 Fault zone ,

Typical banded. Garnet-tourmaline In massive material. Blue actinolite Is devoid of ga-to. '

Typical massive, tended at 70* to C.A. . 1666.9-1668.95

Typical. Massive Tremolite < \Qf, pervasive garnet OOjf end tourmaline Of, Tourmaline occurs In veins as well.1676.2-1676.25 To-q.v.

•1671.1-1671.M To-q.v. II cpy 4 disseminated po 1671.5-1671.54 To-q.v.1679.8-1680.0 Tourma lIne-garnet-tremollte section* Tourma11 ne altered to biotite. 1687.0-1690.0 76 banded. Blue actinolite 1687.6-1687.65 Qtz-to vein 1687,9-1688.15 Typical at 69* to C.A. 1689.7-1689.9 Typical

Coarse pegmatite. Kspar t qtz * lime green mineral O0|. Contacts Irregular but at approx 27* to C.A.

Garnetiferous.

JkT*l J

R PJD-213(a) 13/7/83 TECK EXPLORATIONS LIMITED

DIAMOM) DRILL LOOHole AR-1Sheet 23 of 27


699.7

1710.1

1717.45

1722.9

1751.9

1757.3

705.65

710.1

1717.45

1722.9

1751.9

1757.3

7HO)

7

7H(?)

7F

7F

7F

7F Fault

Amphibolite. Magnetite pervasive. Mata-andeslte(T) with Interbedded garnet rich section. Amphibole richsections are generally absent of garnet, Magnet11*jMOf,1701.3-1701.8 MX garnet (20f) - silicate Iron formation. Magnetic banded at 64* to C.A.

Silicate IF (?), Dark grey blotltlc metasediment wlthjOOX coarse (*1 cm) garnet porphyroblast* throughput.

Amphibolite with pervasive magnetite. (Magnetite l.F.), Epidote mlcrcvelns throughout, fended at 64? toC.A.1714.5-1714.95 Pegmatite contact at 20* and 70* to C.A. with 60* Kspar ±2 cm In size1715.3-1715.9 Blotltlc metasediment ~"1715.7-1715,8 Quartz vein1717.45 Contact at 30* to C.A,

Garnetiferous motasedlment-blotlte rich. Garnet jHSjJ.1719.65-1720.6 Massive1722.2-1722.25 Clay gouge at 50* to C.A.

Massive blotlte-rlch metasediment. Homogeneous. Cut by random ehlorltlc-serlcltlc mlcrcvelns.1733.5-1733.7 Core fractured due to lithostatic pressure release1736.05-1736.15 Pegmatites green due to spodumene!*) contacts at 22* to C.A some disseminated pyrrhotite1739.1-1739.15 Minor breccia llthlfled1745.0-1747.5 Interval Is altered (serlcltlzed-chlorltlzed) .1746.7-1747.3 Massive milky quartz vein1748.8-1749.9 Large breccia zone *IOJf quartz Infilling. Fragments are angular end have not been rotated a

great deal. At 1749 some open space cavity fillings (zeolites?) Last few metres of Interval has some bands.

Not typical. Unit appears anatectic. Is genlsslc with a black-green-plnk banding due to alteration. There Is hematltlc altn as well as Kspar. The Interval It finely banded (K4 mm) at 64* to C.A. Sane qtz velnlng.

Typical. Massive, sericitic, cut by epidote mlcrovelns, 1758.4 Llthlfled breccia over 3 cm

R PJD-213(a) 10/8/83 TECK EXPLORATIONS LIMITS) DIAMOM) DRILL LOO


Depth (m)From

1789.2

To

789.2

1801.2

Rock Type

2C

909Cse

IIA

9A

9A9C9C9A

9C9B9A9A

9A9B

2

i

Description ,

Not typical. Locks magnetite bands) however, It Is cut by a number of 9A/9B porphyries as seen elsewhere.to 1767.0 Unit Is biotite rich) below 1767.0 unit has pervasive chlorlte-serlclte.1762.7-1762.75 Carbonate healed breccia - fresh.1765.0 Foliation at 57* to C.A.1764.9-1765.11765.17-1765.471765.52-5765.57 9C with 1 cm q.v.1766.6-1766.8 Epidote filled crackle breccia.1767,0-1768.7 Pink - abundant Kspar and pervasive hematite stain M, minor Ojf pyrite.1773.6-1773.62 Breccia. ,1774.8-1775*4 Phenos have an augen shape.1775.7-1775.75 Breccia - 1 Ithlf led.1776.1-1776.21776.3-1776.351776.55-1776.651777.1-1777.4 ;1777.4-1780.0 Brecciated, healed with epidote mlcrcvelns.1781.1-1781,41781.6-1781,8 i1782.1-1782.31782.4-1782.61782.0-1783.0 Breccia - healed with epidote, breccia displaces 9A/9B minor calcite.1784.1-1784,21784.4-1784.551785.1-1785.4 Brecciated 9 B.

Typical, fended with 1-2 cm bands at 60* to C. A., minor dlssem pyrite) hematite mlcrovelns, patchy epidoteand carbonate.1791.2-1791.3 Quartz vein.1795.5-1796.8 Grit unit - coarse ^2 mm.1793.4-1793.7 Chert. ~"

R PJD-2l3(a) 10/8/83 TECK EXPLORATIONS LIMITED

DIAMOND DRILL LOO

AR-IHoleSheet 25 of 27

DopTh (m)From

1769.2

1801.2

1805.7

1818.0

1623.0

1831.2

1633.6

1634.1

1636.4

1643.5

To

801.2

805.7

1818.0

1823.0

1831.2

1833.6

1834.1

1636.4

1843.5

1848,0

Rock Type

cont'd

9B

2

2A

2 MA MA

2A

5

2A

29090

)A

* Fault

1 Description

1795.0-1795.2 Chert.1798.0-1798.3 Sericitic.

Typical. As seen In lower zone of Corona stratigraphy..

Laminated metasediment s. Some felsic sections and some gneissic portions.

Typical. Dark green amphibolite banded with brown biotite rich sections, fended at 60* to C. A.

Blotltlc metasediment. Some calc-silicate bands but more massive than typical 2A, 1825.3-1825.6 Light grey pegmatite with minor pyrite * garnet at 12* to C.A. 1826.15-1827.25 Light grey pegmatite with Kspar 30* and pyrite. 1830.0 fending at 65* to C.A.

Not typical. Gneissic appearance. Abundant chlorite * epidote, fended at 65* to C.A.

Not typical (72416). Light grey Interval with disseminated molybdenite *O.J*. From 1833.85-1834.0 more typical 5 very siliceous. Minor O! pyrite and no V.O. This mo-mlneral Izatlon Is at a new stratigraphic position at the base of 2A above unit 2.

More or less typical.*

Typical. Black banded metaseds with gnelsslc/sll lceous sections. 1839.3-1834.518 JO. 0-1840.251842.0 fending at 65* to C.A.

Typical. Dark green amphibole - chlorite Interval with patchy magnetite. Interbedded tuffs. 1844.8-1845.0 Chlorite schist - may be faulty zone seen along highway * 239. 1846.1-1846.15 Fault zone.

' . -n-Hf t w* (n.1

*

R PJD-2l3(a) 10/8/83 TECK EXPLORATIONS LIMITED DIAMOM) CRILL LOO


Depth (m)from

1848.0

1848.35

1851.5

1851.8

1858.55

1891.2

1892.6

1905.5

To

1848.35

1851.5

1851.8

1858.55

1891.2

1892.6

1905.5

1910.9

Rock Type

16

MA

IB

1A

2

9B

10A

11A

2IIAI1A

1 IA

Description

Coarse tuff with fxspor K2 mm. '

Typical. Pink with abundant large Kspar and disseminated pyrite. Contact at 38* to C.A. Fractured contact.1851.2 Hematttlc slip with sllcken sides.

Dark green foliated emphlbolltlc sediments. .

Typical. Dark amphlbollte-metabasaltic tuff(?)j Is well banded at 60* to C.A. Some augened fragments. Theunit Is coarser and locks the magnetite seen In unit 1 on the Corona property. Contact with the underlyingmetasediment Is quite sharp.

Massive tuffaceous me t as od. Foliated at 55* to C.A. Has a gneissic appearance and consists of feldspar-quartz-hornblende (altered to chlorite). Has a pervasive hematltlc alt'n Of and ^f calcite.1861.6-1861.75 Altered, ter vos 1 ve hematite.1863.3-1863.35 Hematite-quartz vein at 25* to C.A, minor epidote In mlcrovelns.1864.5 Epidote mlcrovelns over 1 cm.1869.15-1869.20 Pegmatite.1880.75-1884.0 Coarse wacke unit. Has Ojf pervasive hematite.1889.5-1889.8 - - ,1891.1-1891,2 Calcltlc-chlorltlc cement OO/J, Angular fragments.

Typical, coarse fxspar-quartz-hematlte (O cm crystlas) at 40* to C.A.

Massive wacke with epidote mlcrovelns and pervasive calcite.1900.75-1901.3 fervaslve hematite.1902.0-1902.95 Typical.1903.2 fending at 50',1904.8 tending at 70*,

Massive. Pervasive hematite < \0%, dominated by white Kspar. cut by epldote/chlorlte mlcrofractures.

R PJD-213(a) 10/8/83 TECK EXPLORATIONS LIMITED DIAMOND DRILL LOO


Oupth (m)From To Rock Type Description

1910.9

1917.75

1920.9

1952.7

1917.75

1920.9

1951.4

1952.7

1IA

t 10

END OF HOLE

HA

9B

Massive, thick bedded metased. 1915.4 tended at 40* to C.A. 1912.2-1912.6 HA. 1912.8-1913.11913. l 1914.4

Contorted bedding. Tourmaline vein.

Typical. Red, blotchy, lower contact at 40* to C.A.

Massive matased. Metamorphic grain size ^2 mm. cut by chlorite t epidote mlcrovetns. Unit is biotite richbut In places has been altered to chlorite. Alt'n hole around the pegmatlte(?).1924.5-1926.1 Silicified section, Finely banded at 65* to C.A. May be chemical sediment. Abundant

epidote mtcrovelns display slip. 1932.0-1934.7 Pervasive garnet. 1934.7-1935.2 Typical. 1939.5 tending at 65* to C.A.1941.0-1942.5 Pervasive hematite, some brecciation and faulting. 1949.0 tending at 75* to C.A.

Granite gneiss. Transition from 2 to 110 over 0.5 m. Gneiss Is light grey, dominated by white/grey feldspar/quartz. Pervasive biotite 4 chlorite. Some amphibole rich mlcrofrectures. Possibly granite contact!?).

Jul 31/983 1400 hrs.

APPENDIX II

Sample Number

54727

54728

54784

54887

54888

54889

54886

54895

54896

54897

54898

54899

54900

72347

72348

72349

72350

7235272351

72414

72415

7241672417

72418

72419

ARCTIC RED RESOURCES CORP.

RESULTS OF CORE ANALYSIS FROM BELL-WHITE ANALYTICAL LAB. LTD.

Gold (oz/ton)

0.002

0.002

tracetracetracetrace0.002trace0.0020.002trace0.0020.002trace0.0020.0040.002

0.002trace0.0020.002

0.0020.002

trace0.002

From (m)

413.5

428.0527.1

1,386.01,387.51,389.01,392.2

1,464.5

1,465.5

1,488.0

1,489.0

1,502.7

1,504.1

1,767.0

1,789.2

1,793.4

1,797.5

1,804.71,815.5

1,826.15

1,832.6

1,833.61,834.1

1,848.35

1,849.4

To (m)

414.5

429.0

528.11,387.5

1,389.0

1,390.01,393.2

1,465.5

1,466.5

1,489.0

1,490.0

1,504.1

1,505.6

1,768.6

1,790.2

1,795.2

1,798.5

1,806.51,816.5

1,827.25

1,833.6

1,834.1

1,835.11,849.4

1,850.5

Width (m)

O OO

1.5 1.5

O O O O

1.0 1.0

1.51.6

1.0

1.8

1.0

1.8

1.0

1.1

1.0

0.51.01.05

1.1

G RQ-86 Jan 18/84

: S P

b*

0. 5" X^ XLMSl/kr ST

~ 88-J* Sc&.o fi/O

.S"

Q 't 'f* r -'S 33 M**- -81.4-

r //X 5. TT 3/9 -K9.+

JLLtsx.12 / '/*l t :'l

533tot.*

M, S, T, ^ S 35?/D'l //.C, T,

J 0?/*.331

d&l,, -f. st w . r -87-3

Sk Mt* -W*. K t'i

/V IS P3X Ab 303./ - 32 f - 97-gr /.i, TT

A/. S, TT - w085 c?

/A A/srA/r /b? //-s /T: -85"

'T7 {•s 3/W-r /' M JftO.to "Z?, /o o.? X/* r S&4

233 /.o. r

/?y, x MO A k./l z? z

X ^ * 3 X t 221 ste242. ss* Q 9 /.o

-J t '33

y* tfAtf S.

W* 4*" M

?/&T7 *W7l~T"

//11 Vd

vyhi til*~7?~tt 'z yt*V}.f Q/

J

oy-SitT v yOSrsr

7- fs-0/t//

Q(,f//rrt*?77TT3T f f ffi 1/0

-f4z tr

oyrijnr ''*u~~?r •*?~rr-

*O'/1-h?o

yto/•'f iyz

^O1/

/Xoy/SZJ/**

VT"7.^-7- ftIf 4 '

vnf-1 1

8't evoetO'lSfr

S'r*00-6)!

tJ-Mt

, /*^

A-R-l'b

-fci-2.i? l*- '

nw 22- Zl l v *1 /LSsiy. W j -

.——L!l*2*u

J* * S ^ f

.. 3 a•J

ft- rjro-o* *c /J*/

4}

r t^J\*f.l*S-\T ^ //t,

80*1.0

t?r

/W Bh62, r' r- '

T v i*' k

AO&Tttttfl

63 "/S"* 62-2:8V, 0

W t 'z, 5/6,g A f A PI

. 0,lui,.', /'X O ' J*0

a -f ̂ , c /ft/Ait AV'.," ;- 2/3 .s

A/.m ",T - If

Jtao o./ z

4sLJ^m .*-.M ^^.^.14^ - rl.uk111 .y

B H:'' u^b '*

to C(ftr :tt* f-i*\i

#3**

/Ci t /t.f ^.V

,A^1 ^* r* f '

frll.O

-iXvj:-L-

-3*L

73. rlo

f -8.. f! L.

d i. .

-.JifckJ-Jje

6

A.

m/

mi

73 * ! /.o...j______.

IZP v ' ̂3'*^ ' /v

-** rf ..-zz

j JicAL-5-i-

JUh_JHL

IS&W

r^ r*

/?97 /.oH 10

3.ot

LIM

ITE

DM

N

ES

GO

LDG

OL

IAT

H

LA

C

MIN

ER

AL

S

LIM

ITE

D

TR

AN

S-C

AN

AD

A

HIG

HW

AY

CO

RO

NA

NT

ER

NA

TIO

NA

L LIM

ITE

DR

ES

OU

RC

ES

TEC

K

EX

PLO

RA

TIO

NS

LIM

ITE

D

Arc

tic

Red-P

ine

Bel

l Jo

int

Ven

ture

DDH

AR

-1

SU

RFA

CE

P

LAN

42

C1

2N

W0

18

1

63

.44

80

B

OM

BY

ARCTIC RED

N

N89 - 3I-3SE -D

GOLIATH

5,000 m

W-3,4.

W-7.

4,800

\• 20C

W-9

W-IO-

NAVI-DRILLED (NO CORE RECOVERED)

3,000

42CiaNWdl81 63.4460 BOMBY

2,800210

N44-02-33E 1350-79'

N

ARCTIC RED

N89 -3I-36E

5,000 m

x

W-I.Z

\

W-3,4-

W-7.

\

w-eJ4,800

W-9.

W-IO-

NAVI-DRILLED (NO CORE RECOVERED)

4,600

4,400

4,200

4,000

3,800

3,600

3,400

3,200

12

10

LEGEND

DIABASE DYKES

FELSIC DYKES AND SILLS

MAFIC DYKES AND SILLS

PORPHYRY DYKES AND SILLS

METAVOLCANICS - METASEDI M E NTS

METASEDIMENTS

VOLCANICLASTIC ROCKS

METASEDIMENTS

VOLCANICLASTIC ROCKS

MUSCOVITE SCHIST

METASEDIMENTARY ROCKS

HORNBLENDE SCHISTS

SYMBOLS

O DIP AND/OR AZIMUTH TESTS

w-21 WEDGE

"\ CORE ANGLES

J,000

TECK EXPLORATIONS LIMITED

Arctic Red - Pine Bell Joint Venture

VERTICAL SECTION

DDH AR-100 m J

tOO SCALE

?OO200

300 fi

DRAWN BY CHECKED BY NTS 4? C/l Z JOB NODWG NO

arctic red resc corp omep rpt on ddh ar-1 … (up to 1 cm) set in a fine grained, uniform, ......

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