the results of am integrated exploration program ... · the results of am integrated exploration...

LAKE010

1990 SUMMARY REPORT

THE RESULTS OF AM INTEGRATED EXPLORATION PROGRAM (GEOLOGICAL MAPPING. LITHOGEOCHEMICAL SAMPLING.

GROUND GEOPHYSICS, AND POWER STRIPPIHGVTRENCHING) OH THE MISSING LINK PROPERTY

(CLAIMS TB90755Q et all LAPIERRE AMD LEGAULT TOWNSHIPS THUNDER BAY MINING DIVISION

ONTARIO

NTS:LATITUDE:LONGITUDE:OWNER:OPERATOR:DATE:AUTHOR:

42EM449 45'N87 24'WHOMESTAKE MINERAL DEVELOPMENT COMPANYHOMESTAKE MINERAL DEVELOPMENT COMPANYSEPTEMBER, 1990DUNCAN MCIVOR

4SE146MMI 63.6*36 LAPIERRE LAKE

TABLE OF CONTENTS

O10C

PAGE

1. SUMMARY AND RECOMMENDATIONS

2. INTRODUCTION

2.1 SCOPE OF REPORT2.2 LOCATION, AREA, AND ACCESS2.3 PROPERTY DEFINITION2.4 REGIONAL GEOLOGIC SETTING2.5 GOLD DEPOSITS OF THE BEARDMORE - GERALDTON AREA2.6 GENERAL GEOLOGY OF THE MISSING LINK PROPERTY2.7 PREVIOUS VORK2.8 1990 PROGRAM

3. DETAILED TECHNICAL DATA

3.1 GEOLOGICAL MAPPING AND LITHOGEOCHEMICAL SAMPLING1) METHODS EMPLOYED

11) RESULTS AND INTERPRETATION

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1010101314181921

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232324

3.2 GROUND GEOPHYSICAL SURVEYS(VLF-EM, TOTAL FIELD MAGNETICS) 1) METHODS EMPLOYED


3.3 POWER STRIPPINGXTRENCHING PROGRAM i) METHODS EMPLOYED


323232

3535

36

4. COST STATEMENT

5. SELECTED REFERENCES

40

41

6. STATEMENT OF QUALIFICATIONS

7. TECHNICAL DATA STATEMENTS

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LIST OF FIGURES

FOLLOWS PAGE

1. GENERAL LOCATION MAP, MISSING LINK PROPERTY 10

2. DETAILED LOCATION MAP, MISSING LINK PROPERTY 10

3. CLAIM SKETCH, MISSING LINK PROPERTY 12

4. GEOLOGY OF THE BEARDMORE-GERALDTON AREA 17

5. GOLD DEPOSITS AND GEOLOGY OF THE BEARDMORE-GERALDTONAREA 17

6. GOLD PRODUCTION IN THE BEARDMORE-GERALDTON AREA 17

7. SCHEMATIC DIAGRAM ILLUSTRATING FORMATION OF THEBBARDMORE-GERALDTON BELT 17

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LIST OF APPENDICES

1:2000 GEOLOGY (SOUTH SHEET) 1:2000 GEOLOGY (CENTRAL SHEET)

2000 GEOLOGY (NORTH SHEET)

1:5000 GEOLOGY-GEOPHYSICS-GEOCHEMISTRY COMPILATION

1:5000 CONTOURED TOTAL FIELD MAGNETICS 1:5000 VLF-EM LINE PROFILE PLOTS

1:2000 LOCATION MAP, STRIPPED AREAS 1-61:2000 LOCATION MAP, STRIPPED AREA 7

2000 LOCATION MAP, STRIPPED AREA 8 2000 LOCATION MAP, STRIPPED AREA 9 100 DETAILED GEOLOGY, STRIPPED AREA l 100 DETAILED GEOLOGY, STRIPPED AREA 2A 100 DETAILED GEOLOGY, STRIPPED AREA 2B 100 DETAILED GEOLOGY, STRIPPED AREA 3

RAW GEOCHEMICAL DATA

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1. SUMMARY AND RECOMMENDATIONS

l The Missing Link property is located 12 kilometres northeast of the town of Jelllcoe, in north-central Ontario. The property is comprised of 54 contiguous, unpatented mining claims, located in

l Lapierre and Legault Townships, of the Thunder Bay Mining Division.

The property straddles the Paint Lake Fault/Deformation Zone, a regional transcurrent structure that separates the Onaman-Tashota Terrain to the north, and Beardmore-Geraldton Terrain to the south.

The Onaman-Tashota Terrain, which underlies most of the property, is predominantly comprised of calc alkalic to tholeiitic metavolcanics. The Beardmore-Geraldton Terrain is a metavolcanic -metasedlmentary assemblage within which lithologic units have been tectonically transposed into thin alternating slices.

Prior to acquisition of the property by HMDC in early 1990, the property had seen only limited surface work. The property was held by Golden Earth Resources during the period 1986 to 1989, who completed an airborne magnetics and VLF-EM survey, and some limited ground geophysics over those portions of the property covered by water. The vendor, Mr. Nolan Cox, completed a stripping/trenching program over portions of the ground in 1989.

During the 1990 field season, HMDC completed a program of line- cutting, detailed geological mapping, lithogeochemical sampling, and ground magnetic and VLF-EM surveys over the entire property. A power stripping program was also completed, at 9 target locations. Detailed geological mapping and channel sampling of the stripped areas completed Homestake's initial program on the property.

The results of the geological mapping indicated that the property was underlain predominantly by intermediate to mafic metavolcanics, locally intruded by conformable, sill like gabbroic bodies. Within the mafic volcanics were distinct strongly magnetic flow horizons, that defined the generally east- west trend of the stratigraphy. Varying degrees of shearing within the mafic metavolcanics resulted in the use of descriptive field terms that are associated more with tuffaceous and

epiclastic rocks, though true sediments are not thought to constitute a significant proportion of the stratigraphy. Also intercalated within the mafic metavolcanics are interformational exhalative horizons. The presence of these horizons/ not observed in outcrop, is based on interpretation of the ground geophysical data, which defined several strong, long strike length VLF-EM anomalies, often with associated magnetic signatures. The horizons are thought to be massive pyrite/graphitic argillite interflow sediments, or, in the case of the coincident mag - VLF-EM anomalies, chert- pyrrhotite/magnetite exhalatives.

A major contact with sediments of the Beardmore-Geraldton terrain is interpreted as crossing the southern portion of the property, beneath Jory Lake. Polymictic paraconglomerates of the Beardmore- Geraldton belt were observed in outcrop south of the lake, and the contact is interpreted based on the airborne magnetic data.

The mapping also defined, within the mafic metavolcanics, two distinct zones of intense shearing and associated hydrothermal alteration, to an assemblage of Fe carbonate, sericite, and chlorite. The zones, up to 25 metres in width, and strike lengths in excess of 1000 metres, are thought to reflect an anastomosing shear system that may be the Paint Lake Fault itself, or a related subsidiary splay. These zones became the focus of the exploration program. Initial lithogeochemical sampling of the zones, where exposed, was disappointing, with only 5 of 49 samples collected returning anomalous gold values in excess of 50 ppb. The best initial assay of 1.968 gpt was returned from a sample of arsenopyrite bearing quartz vein blast rock proximal to an old pit within the shear.

Despite the initial poor analytical results, the setting of the property, and in particular the shear/alteration zones proximal to the interpreted major Paint Lake Fault System, is analogous to the Brookbank Deposit, thirty kilometres to the west (1.3 MT at 0.30 OPT). Given the poor exposure along the strike length of the shear, a stripping program was designed to better evaluate the system at several locations along its strike length.

The program, comprised of 121 hours of backhoe work, and an additional 16.5 days of outcrop washing, targeted 9 areas, 3 as major clearing programs, and 6 as thin, strip type trenches

across target zones. Over the extensively cleared areas, detailed 1:100 scale geological mapping, and extensive rock saw channel sampling programs were completed (325 samples).

At Stripped Area l, a broad shear/alteration zone, to 25 metres in width, is exposed over 130 metres of strike length. Within the shear zone are several thin, contorted to brecciated quartz and quartz - Pe carbonate veins, carrying variable amounts of pyrite and arsenopyrite mineralization. Analytical results from the detailed channel sampling program were poor, with only 7 of 180 samples returning significantly elevated gold values of ^00 ppb. Best results came from a 3 metre wide quartz - carbonate stockwork zone, which carried 1.22 gpt/3.0 metres, including 2.06 gpt/1.0 metres.

Stripped Areas 2, 3, 4, and 6 also exposed the shear/alteration system along strike, though no significantly elevated gold values O500 ppb) were returned from the channel sampling programs at these locations. The results of all sampling to date, then, indicate a very sporadic, and low grade gold content hosted within secondary veining within the shear system. Again, however, the analogy to the Brookbank Deposit holds, in that surface sampling there returned only low grade and sporadic gold values, and ore was not encountered within the shear system until drilling began to probe beneath the 800 foot level.

A 1500 metre, eight hole diamond drilling program is therefore proposed for the 1991 fiscal year, to evaluate the shear systems defined on the property at depth and along strike, as well as secondary geophysical targets. Specific collar locations are outlined below.

DDH ML-91-01

COLLAR: L5+OOE, 10+OOSAZIMUTH: O DEGREESDIP: -45 DEGREESDEPTH: 200 METRESTARGET: The first of a two hole fence designed to test thecontact between the paraconglomerates to the south, and maficmetavolcanics to the north, a zone interpreted as being a majorfault and potential sight of significant hydrothermal alterationand associated gold mineralization. This hole will also test aweak VLF-EM anomaly in the vicinity of the interpreted contact.

DDH ML-91-02

COLLAR:AZIMUTH:DIP:DEPTH:TARGET:above.

L5+OOE, 8+70SO DEGREES-45 DEGREES200 METRESThe second hole of the two hole fence, as outlined

DDH ML-91-03

COLLAR: L6+OOE, 2+50SAZIMUTH: O DEGREESDIP: -45 DEGREESDEPTH: 300 METRESTARGET: This hole is designed to test the down dip extensionsof two parallel shear/alteration zones defined by surfacemapping/ in the vicinity of surface channel samples to 2.06gpt/1.0 metres. The hole will also penetrate a strong VLF-EManomaly, thought to be a massive pyrite horizon.

DDH ML-91-04

COLLAR: Lll+OOE, 1+50SAZIMUTH: O DEGREESDIP: -45 DEGREESDEPTH: 140 METRESTARGET: This hole is the first of a two hole fence designed totest the eastern strike extension of the two parallelshear/alteration zones encountered during surface mapping, 500metres to the west.

DDH ML-91-05

COLLAR: Lll+OOE, 0+50SAZIMUTH: O DEGREESDIP: -45 DEGREESDEPTH: 140 METRESTARGET: This hole is the second of the two hole fence,designed to test the target described above.

8

DDH ML-91-06

COLLAR: L19+OOE, 5+258AZIMUTH: O DEGREESDIP: -45 DEGREESDEPTH: 180 METRESTARGET: This hole is designed to test a strong coincidentmagnetics\VLF-EM anomaly thought to be a chert-pyrrhotite/magnetite exhalative horizon. It is the first of athree hole fence testing the stratigraphy in an area of stacked/repetitive anomalies that may be the result of local complexfolding.

DDH ML-91-07

COLLAR: L19+OOE, 4+OOSAZIMUTH: O DEGREESDIP: -45 DEGREESDEPTH: 200 METRESTARGET: This hole is designed to test two moderate VLF-EManomalies, with an associated magnetic response, that are thoughtto reflect a folded chert-pyrrhotite/magnetlte exhalativehorizon. It is the second of a three hole fence crossing thestratigraphy in an area interpreted as having been folded.

DDH ML-91-08

COLLAR: L19+OOE, 2+75SAZIMUTH: O DEGREESDIP: -45 DEGREESDEPTH: 140 METRESTARGET: The third hole in a three hole fence, designed to testa strong VLF-EM/magnetics anomaly in an area of inferred folding.

Total anticipated costs for the 1500 metre diamond drilling program are approximately S150,000.

2. INTRODUCTION

2.1 SCOPE OF REPORT

This report serves to summarize the results of the 1990 exploration program carried out by Homestake Mineral Development Company on the Missing Link property.

2.2 LOCATION. AREA. AND ACCESS

The Missing Link property is located approximately 12 kilometres northeast of the town of Jellicoe, midway between the communities of Beardmore and Geraldton, in north central Ontario (see Figures l and 2).

Access to the property is via the all weather gravel Kinghorn Road, which extends north from the Trans Canada Highway 11, at a point approximately 7 kilometres east of Jellicoe. The Kinghorn road crosses the western edge of the property, approximately 10 kilometres north of the Highway 11 turn off. From the Kinghorn road, a 4WD bush road extends east through the south central portion of the property, providing reasonable access to most portions of the ground.

The property is one of low relief, rarely exceeding ten metres. The majority of the claim block is covered by spruce swamp, underlain by a thick exotic glacial till and outwash assemblage known as the Wildgoose Glaciofluvial Complex. Outcrop exposure is limited to a broad, east - west trending ridge that crosses the south central portion of the claim block, and where locally the glacial sediment cover is less than 3 metres.

Two large lakes, Jory in the south, and an un-named lake in the east-central portion of the property, cover approximately 15* of the claim block. Three smaller, un-named lakes straddle the western edge of the property.

2.3 PROPERTY DEFINITION

The Missing Link property is comprised of 54 unpatented mining claims, all located within Lapierre and Legault Townships of the Thunder Bay Mining Division. Outlined below is a summary of the claim status, including the work filed for assessment credit summarized in this report.

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CLAIM STATUS

CLAIM

907485907486907487907488907489907490907491907492907493907494907495907496907500907507907508907509907510907511907512907513907514907515907550907851907852907853907854907855907856907857907858907859907860907861907862

REG. DATE.

MAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAY

20,8620,8620,8620,9020,8620,8620,8620,8620,8620,8620,8620,8620,8620,8620,8620,8620,8620,8620,8620,8620,8620,8620,8620,8620,8620,8620,8620,8620,8620,8620,8620,8620,8620,8620,86

MISSING LINK PROPERTY

ASSESSMENT CREDITSGPHY.

8080808080808080808080808080808080808080808080808080808080808080808080

GEOL.

4040404040404040404040404040404040404040404040404040404040404040404040

GCH.

00000000000000000000000000000000000

DR.

00000000000000000000000000000000000

EXP.

23.23.33.43.23.23.23.23.43.53.23.23.80.23.23.23.23.23.33.38.43.43.

52525252525252525252525274525252525252525252

100.0080.80.80.80.80.80.80.80.43.90.95.85.

747474747474747452525252

TOT

143.143.153.163.143.143.143.143.163.173.143.143.200.143.143.143.143.143.153.158.163.163.220.200.200.200.200.200.200.200.200.163.210.215.205.

EXPIRYDATE

5252525252525252527852527452525252525252525200747474747474747452525252

MAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAY

20,20,20,20,20,20,20,20,20,20,20,20,20,20,20,20,20,20,20,20,20,20,20,20,20,20,20,20,20,20,20,20,20,

919191919191919191919191929191919191919191919292929292929292929192

20,9220, 92

11

CLAIM REG. DATE ASSESSMENT CREDITS EXPIRYGPHY. GKOL. GCH. DR. EXP. TOT. DATE

907867907868907869907870907871907872907873907875907876907877907878907879907880907881907882907883907884907885907890

MAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAYMAY

20,20,20,20,20,20,20,20,20,20,20,20,20,20,20,20,20,20,20,

86868686868686868686868686868686868686

80808080808080808080808080808080808080

40404040404040404040404040404040404040

0000000000000000000

0000000000000000000

90.5223.5243.5223.5223.5223.5223.5280.7499.3290.5285.5299.5233.5228.52100.0099.5223.5243.5255.52

210.52143.52163.52143.52143.52143.52143.52200.74219.32210.52205.52219.52153.52148.52220.00219.52143.52163.52175.52


20,9220,9120,9120,9120,9120,9120,9120,9220,9220,9220,9220,9220,9120,9120,9220,9220,9120,9120,91

* Note that credits listed as greater than 200 man days are in anticipation of Notices of Reduced Assessment Credit for geological mapping on partially water covered claims. This Claim Status Summary will be updated upon acceptance of all filed work.

Figure 3 illustrates the locations of the claims that comprise the property.

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2.4 REGIONAL GEOLOGIC SETTING

The following description of the general geology of the area comes predominantly from Mason and White (1986), to which the reader is referred for an excellent overview of the geology and gold deposits of the Beardmore - Geraldton area.

The area has been geologically subdivided into two belts; the southern Beardmore - Geraldton belt, and the northern Onaman - Tashota belt. The belts are separated by a regional, transcurrent fault/deformation zone, known as the Paint Lake Deformation Zone (PLOZ), and are differentiated on the basis lithology, structural style, and age.

The PLDZ is an east - west trending lineament, approximately 50 kilometres in length, and up to l kilometre in width, comprised of an early ductile component termed the Paint Lake Shear Zone, and a late brittle component known as the Paint Lake Fault (Reilly, 1988). Movement along the PLDZ was in a dextral sense, consisting of an early differential motion with south side down, and a later strike slip motion.

The southernmost Beardmore - Geraldton belt is situated within an east - west trending isoclinally folded metavolcanic - metasedimentary sequence, within which lithologic units have been tectonically transposed into a series of thin alternating slices. The belt has been divided lithologically into: the Southern Metavolcanic Sub-belt, and the Southern Metasedimentary Sub-belt.

The Southern Metavolcanic Sub-belt is comprised predominantly of massive, pillowed, amygdaloidal and variolitic magnesian to iron tholeiitic flows. Intercalated with these flows are thin tuffaceous equivalents, as well as thin clastic and chemical metasediments. Regional foliations are 075 to 090 degrees, dipping vertically to steeply north.

The Southern Metasedimentary Sub-belt is comprised of interbedded clastic and chemical metasediments, predominantly wackes, conglomerates, siltstones, and oxide facies (magnetite - hematite) iron formations. Isoclinal and tight drag folding have affected much of the sedimentary sequence, and fold structures generally plunge to the west at 30 to 40 degrees.

13

The northern Onaman - Tashota Metavolcanic Belt is comprised predominantly of calc-alkalic to tholeiitic felsic to mafic raetavolcanics. These rocks have been deformed into arcuate shapes by the emplacement of several intervening granitic intrusions. Regional fault structures, and much of the stratigraphy, trend north and northeasterly.

Gabbro, diorite, granodiorite, quartz-diorite, monzonite, feldspar porphyry, and quartz-felddppar porphyry intrude rocks of both the Onaman - Tashoda Belt and Beardmore - Geraldton Belt. Late Precambrian diabase intrudes all rock types. Metamorphic grade throughout both belts is generally greenschist, but locally ranges to amphibolite facies, usually proximal to large granitoid intrusions.

The general setting of the two belts described above suggests that the Beardmore - Geraldton Belt is an accretionary prism of repetitive sequences of northward younging basaltic volcanic rocks, and predominantly clastic marine sedimentary rocks, which is developed on the southern margin of an early Archean volcanic arc complex (the Onaman - Tashoda Belt). The two terrains can be equated with and are part of the Wabigoon Sub-province to the north, and the Quetico Sub-province to the south, again separated by the regional Paint Lake Deformation Zone. Figures 4 through 7 illustrate the general geology of the Beardmore - Geraldton area, as well as schematic illustrations of belt formation.

2.5 GOLD DEPOSITS OF THE BEARDMORE - GERALDTON AREA

The Beardmore - Geraldton gold camp ranks among the top five gold producing regions of the Canadian Shield, with approximately 4.12 million ounces of production from 19 mines over the past 55 years.

The following summary of styles of gold mineralization is adapted from Mason and White (1986), and Burk (1989).

Gold mineralization within the camp can be classified according to stratigraphic location, and host lithology.

1. Southern Volcanic Sub-belt, Beardmore - Geraldton Belt

As previously discussed, this sub-belt consists of massive,

14

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pillowed, and amygdaloidal and variolitic magnesian and tholeiitic flows. The flows are intercalated with thin but stratigraphically continuous oxide facies iron formations, comprised of chert, magnetite, iron carbonate, and and iron amphibole bands. The sub-belt is separated from adjacent metasedimentary packages by the Empire Fault in the north, and the Blackwater River Fault.

A) Mafic volcanic host rock (Northern Empire Mine, Spooner Prospect, Mcwilliams - Beardmore Prospect, Buffalo - Beardmore Prospect, Pichette and Maki East Occurrences).

The Northern Empire Mine (located 1.5 kilometres northeast of Beardmore), produced 149,500 ounces of gold from 1934 to 1941, at an average grade of 0.35 OPT. It is to date the only gold producer from the Southern Metavolcanic Sub-belt. The deposit consists of a 0.6 metre (average width), boudinaged quartz- carbonate vein hosted within a l to 3 metre wide shear zone in mafic metavolcanics. Gold is associated with arsenopyrite, pyrite, chalcopyrite, and galena. The chlorite-carbonate wallrock marginal to the vein, while often carrying appreciable sulphide concentrations, carry no significant gold values.

B) Iron formation host rock (Craskie-Vega Prospect, Oelbridge, Maki Main, and Lattimer Occurrences).

Gold mineralization is associated with two persistent east-west trending chert-magnetite-carbonate iron formations in Vincent Township. The sub-parallel iron formations, stratigraphically approximately 40 metres apart, have been traced for strike lengths of 600 metres, and average 2 metres in width. The iron formations are hosted within strongly sheared and variably altered mafic flow rocks. Gold is associated with arsenopyrite, pyrite, pyrrhotite, and chalcopyrite bearing discordant quartz veins cutting the iron formation, as well as sulphide replacement bands of the iron rich amphiboles within the iron formation. Average grade at the Craskie-Vega prospect is 0.19 OPT\Au over 2.0 metres, though tonnages defined to date are uneconomic.

2. Southern Metasedimentary Sub-belt, Beardmore - Geraldton Belt.

As discussed, this belt is comprised predominantly of clastic

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metasediments, primarily feldspathic wackes and argillites, and polymictic conglomerate, which tends to occur near the northern margin, or stratigraphic top of the sedimentary sequence. Interbedded with the clastic metasediments are oxide facies iron formations. In the Beardmore area, the sub-belt is bounded by the Watson Lake Fault to the north, and the Empire Fault to the south. In the Geraldton area. The Bankfield - Torobill Fault, and Little Long Lac Fault, are the two most prominent structures

i within the sub-belt, and bound all gold deposits in the Geraldton l area. The majority of gold production from the Beardmore -

Geraldton camp has come from the Southern Metasediroentary Sub- I belt.

A) Clastic metasediment host rocks (Leitch, Sand River, Little Long Lac, Magnet Consolidated, Hard Rock, and Jellicoe Mines).

* Lithologies generally found on these mine properties areinterbedded wackes, arkosic sandstone, argillite, and minor conglomerate. Iron formation is typically interbedded with the clastic metasediments, approaching widths of 25 metres. Narrow sill-like bodies of diorite and feldspar porphyry are also commonly present. Ore consists of sheeted fissure - type quartz veins rarely exceeding 0.5 metres in width, with associated carbonate, pyrite, arsenopyrite, scheelite, tourmaline, chalcopyrite and sphalerite. Wallrocks (generally feldspathic wackes) are variably sheared and altered, to an assemblage of sericite, carbonate, and locally silica, over widths rarely greater than l to 2 metres. The ore zones appear to be spatially and probably genetically related to tight isoclinal drag folds, plunging 30 to 40 degrees to the west, proximal to regional transcurrent faults (eg. Bankfield-Tombill, Little Long Lac, Watson Lake Faults).

B) Iron formation host rock (Hardrock Mine, MacCleod-Cockshutt Mine, Soloman's Pillars Prospect).

The most significant production from an iron formation host in the camp comes from the North Zone of the Hardrock Mine. This orebody is located within a westerly plunging 7. shaped drag fold on the north limb of a tight isoclinal fold. Mineralization consists of quartz-carbonate-sulphide veins localized by shearing, and quartz-carbonate-sulphide replacement bands within the chert-magnetite iron formation. Sulphides present include

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pyrite, arsenopyrite, pyrrhotite, chalcopyrite, and sphalerite. Pervasive iron carbonate alteration is associated with the ore zone.

The Soloman's Pillars Prospect, located 7 kilometres west of Jellicoe, consists of quartz-pyrite-arsenopyrite veins that cut and replace chert-magnetite iron formation near the northern margin of the Southern Metasedimentary Sub-belt. The deposit is less than 300 metre from the regional Watson Lake Fault, to which the mineralization is probably genetically related.

C) Felsic intrusive-metasediment contact hosted mineralization (Bankfield, Hardrock, MacCleod-Cockshutt, Consolidated Mosher Mines).

One of the largest orebodies in the Beardmore - Geraldton Camp is the F Zone of the MacCleod -Cockshutt and Consolidated Mosher Mines. The deposit, located along an albite porphyry - metasediment contact, contained approximately 10 million tons at an average grade of 0.15 OPT Au. The zone consists of a quartz vein stockwork within a wide, 100 degree trending, steeply dipping intensely fractured and sheared horizon in wackes and lean iron formation, along the north limb of a tightly folded albite porphyry body. The ore zone follows the plunging nose of the porphyry, at 30 degrees west. Gold occurs in quartz veins and fractures with associated pyrite and arsenopyrite mineralization, in variably carbonatized and sericitized wacke. Where the veins pass into iron formation, sulphide replacement of magnetite becomes the most prevalent ore type.

At the Bankfield Mine, Approximately 10 kilometres northwest of the MacCleod-Cockshutt Mine, mineralization consists of sheared and brecciated wacke and albite porphyry, impregnated by silica, pyrite, arsenopyrite, and pyrrhotite. The orebody sits in a flexure or roll along the northern margin of the west-northwest trending albite porphyry body. The Bankfield-Tombill Fault passes' less than 500 metres north of the orebody, to which the deposit is probably genetically related.

D) Regional transcurrent fault/shear zone hosted mineralization (Brookbank, Cherbourg Deposits, Metalore Resources)

At the Brookbank and Cherbourg deposits, currently being explored

17

LEGEND

Diabase Gramlc SedimentsLJVolcanics Mica schist

\. Hard Rock Gold Mines. Ltd. 2. MacLeod-Codnhun Gold Mines Ud. l LW* Long Lac Gold Mines Ltd. 4. Elmos (Tombill Gold Mines UdJ. SL Ma(net Comobdaled Mines Ltd. 6. BanhlieM Consolidated Mines Ltt 7. TombiU Gold Mines Ltd. a Jellicoe Mine* (19391 Ud. 9. Orph (Oik-O&l Mine. 10. Sturgeon Rim Gctt Mines Ltd. 11. Nonhern Empire Mines C&Ud. 12. Leitch Gold Mines Ltd. 13. Sand River Gold Mining CaLtl

____________________________________ 6.S.C

Fig. 4.—Geological outlioe map of Little Lung Lac-Sturgeon River area.

Tatil

a 1.

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1934

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1949

1941,

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1936

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68

1934-54

1956

1938

, 19

68

1938-43

1946-52

1937

1946-47

1962-66

1934-35

1937

-42

1936

-42

1942,

1948

1935,

1938

1935-38

'MJ1-.I4 .

1044

Ounces G

old

Ounces silver

66,417

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" 149,493

134

269,081

4,23

8

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.

605,499

*

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8

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089 73 792

330,263

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50,063

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19,803

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9

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1,51

8

2,710,65

7

3,525

157,870

143,

123

6,63

4

31,200

26,120

0.29

0.33

2.91

0.18

0.40

0.92

0.34

0.14

0.42

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0

0.52

0.12

0.70

0.32

0.51

0.21

0.24

0.18 i

0.03

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0.01

0.01

0.03

0.03

0.09

0.05

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0.03

0.01

0.44

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0.01

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1950

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1938

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05

ri) Archaean (c.2770 my.)

SUBDUCTION OBLIQUE. TO MARGIN?

b) Post accretion (c.2600 my.)

- GERALDTON - BEARDMORE BELT

Figure - Schematic diagrams of tho arc-accretlanary prism model during prism lormatlon and subse quent to accretion to wawa terrain to the south.

ll l l l l l l l l l l l l 2.6 GENERAL GEOLOGY OF THE MISSING LINK PROPERTY

M The Missing Link property is underlain predominantly by mafic

i

by Placer Dome and Metalore Resources, gold mineralization is associated with an east-northeast trending shear/fault system known as the Brookbank Fault. This fault is a secondary splay off of the transcurrent east-west trending Paint Lake Fault, which demarcates the boundary between the northern Onaman - Tashoda Belt, and the southern Beardmore - Geraldton Belt. Then Brookbank Fault juxtaposes mafic metavolcanics to the south, against a thin slice of polymictic paraconglomerate to the north. The fault/shear zone is characterized by intense carbonatization, sericitization, hematization, and local silicification of both lithologies along the contact, over widths to 20 metres. Gold mineralization is associated with disseminated pyrite to 20* within the shear zone, as well as distinct quartz-tourmaline veins developed at the contact. At the Brookbank deposit, reserves in excess of 1.5 million tons at 0.27 OPT Au have been outlined to date, most of which come from below 800 feet of surface. The potential for other, similar deposits along the entire strike length of the Paint Lake Deformation Zone is relatively good, and is the target model for the Missing Link property exploration program.

3. Onaman - Tashota Belt

A) Felsic volcanic\intrusive hosted gold (polymetallic) mineralization (Quebec Sturgeon River, Dik Dik, Crooked Green Creek Mines).

Typically high grade and low tonnage in nature, gold deposits of the Onaman - Tashota Belt are fissure type auriferous quartz - sulphide - carbonate veins in sheared intermediate to felsic metavolcanics, usually proximal to felsic intrusive stocks. For example, at the Dik Dik or Orphan Mine, auriferous quartz veins are hosted by a thin shear zone which crosses the contact between intermediate metavolcanics and granodiorite of the Kaby LakeStock. The quartz veins are mineralized with pyrite, chalcopyrite, pyrrhotite, sphalerite, and galena, and the average grade mined at the deposit was 0.70 OPT Au.

f18

metavolcanics of the Onaman - Tashota Belt. Along the southern margin of the property are polymictic paraconglomerates of the Beardmore - Geraldton Belt, and the contact between the two terrains, the regional Paint Lake Fault/Deformation Zone, is interpreted as crossing through Jory Lake, along the southern boundary of the property. The Jellicoe Fault, a northeast trending, sinistral structure, appears to have dislocated regional stratigraphy by as much as 1.5 kilometres north, immediately west of the property. Prior to recognition of this dislocation, based on high resolution airborne magnetics, the eastern continuation of the Paint Lake Deformation Zone was poorly defined.

Intercalated with the predominantly mafic metavolcanic pile are thin interflow graphitic metasediments, as defined by previous drilling immediately east of the property (Amax, Hudbay, Inco - see following section of this report). Locally small conformable gabbroic sills intrude the mafics, as do thin quartz-feldspar porphyry dykes.

Recent geological work on the property is described in the following section of this report.

2.7 PREVIOUS WORK

Prior to the 1986 staking of the current claim block, there is no recorded work on ground that now constitutes the Missing Link Property. The discovery of several overgrown trenches on the property during staking, however. Indicates that the ground has seen at least some previous work, probably during the initial exploration rush in the camp, in the early 1930's.

During 1986, the property vendors discovered several trenches and pits north of Jory Lake, which exposed a zone of shearing and associated carbonate-sericite-silica alteration within mafic metavolcanics. Grab samples from sheared material collected that summer returned assays to 0.075 OPT Au. Samples from a thin quartz - arsenopyrite vein collected from one trench also returned gold values to 0.52 OPT Au. On the strength of these assays, and because of news of significant deep intersections on the Metalore Property 30 kilometres west and along strike, the property was optioned by Golden Earth Resources in late 1986.

During 1987, Golden Earth Resources contracted an Airborne Magnetics and VLF-EM survey over the property. The survey, completed by Terraquest Ltd., delineated two, east-west trending linear magnetic lows crossing the southern portion of the claim group, both thought to reflect zones of underlying carbonatization within the predominantly mafic metavolcanic terrain. Two parallel linear strong magnetic highs were also defined by the survey, both attributed to zones of magnetite enrichment within the mafic metavolcanics.

Also in 1987, ground magnetics and VLF-EM surveys were completed over the ice on all lakes on the property. These surveys identified several VLF-EM anomalies, all of which however were attributed to conductive lake bottom sediment effects (Lassila, 1987).

The property remained inactive through to 1989, when Golden Earth Resources terminated their option on the claim block. At that time, the vendors completed limited power stripping programs proximal to and along strike from the initial discovery trenches. These stripping programs delineated the east-west trending zone of shearing and associated alteration within the mafic metavolcanics over a strike length of almost 2000 feet.

In December, 1989, Homestake Mineral Development Company optioned the property, and commenced work on the ground in May, 1990.

Adjacent to the property, several exploration programs by various companies has taken place since the early 1970's.

In 1971, Inco drilled two holes, totalling 326 feet, in the Delisle Lake area, immediately east of the current claim block. Both holes targeted EM conductors, and intersected graphitic andsulphide (Po,Py) interflow horizons within intermediate to mafic metavolcanics. No assays were reported with the drill logs on file.

In 1972, Hudson Bay Exploration and Development Company Ltd. completed an 8 hole, 2,629 foot drilling program in the Lapierre Lake area, approximately 5 kilometres east of the Missing Link property. Again, all holes targeted EM conductors, and encountered barren graphitic and sulphide interflow horizons within intermediate to mafic metavolcanics. No significant gold

20

assays were returned from the drilling program.

i In 1973, in the same area, Amax drilled three holes totalling 1,175 feet. All three holes targeted EM responses, and

- intersected graphitic and Py-Po interflow horizons within n*afic metavolcanics. No significant gold assays were reported from the drilling program.

H In 1980, Dome Mines Ltd. completed a 3 hole, 899 foot drilling program between Delisle and Lapierre Lakes, approximately 3

kilometres east of the property. Again, these holes intersected

- barren graphitic and sulphidic interflow horizons within mafic metavolcanics, from which no significant gold assays were reported.

Immediately southwest of the property, in 1986 through 1987, Rampart Resources completed a 9 hole, 4,570 metre diamond drilling program. All holes intersected metasediments of the Southern Metasedimentary Sub-belt, predominantly wackes, argillites, and some polymictic paraconglomerate. Several holes encountered zones of significant shearing and associated carbonatization/silicification within the metasediments, though no significantly elevated gold values were returned from the drilling program.

1990 EXPLORATION PROGRAM

During the period May l through August 10, 1990, Homestake Mineral Development Company Ltd. completed an integrated exploration program on the 54 claims that comprise the property, including;

- establishment of a 72 line kilometre cut line grid over the entire property.

- detailed 1:2000 scale geological mapping over the entire property, with collection and subsequent analyses (Au, 30 element ICP) of 48 rock samples.

- completion of 66.0 line kilometres of total field magnetics, and VLF-EM surveys over the entire property.

l

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l

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l

l

l

l

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l21

lllIlI

- 121 hours of power stripping, in eight areas of the property, employing a 215 Caterpillar Excavator, and 11 days of Wajax pump outcrop washing.

- detailed 1:100 mapping and channel sampling of stripped areas, with analyses of 325 rock samples for gold.

The results of this work is summarized in the subsequent sections of this report.

22

l l l l l

3.0 DETAILED TECHNICAL DATAf

3.1 GEOLOGICAL MAPPING AND LITHOGEOCHEMICAL SAMPLING

i) METHODS EMPLOYED

To facilitate access and provide control for the geological mapping program on the property, a 72 line kilometre cut line

( grid was established in late April and early May. An east-west trending, 2.3 kilometre base line was cut across the southern portion of the property. Shorter, east-west trending control tie-

1 lines were cut at 2+50S, 10+OOS, 7+50N, 12+OON, and 20+OON, primarily to provide control points for lines cut between the several lakes on the property. North-south trending cross-lines

. were established at 100 metre intervals , between 10+OOS and l 20+OON, providing detailed grid coverage over the entire

property. Pickets on all base, tie, and cross lines were established at 25 metre intervals, with the station co-ordinates

l clearly inscribed on each.

The grid was employed in providing control during the geological mapping of the property. All outcrops encountered during line, and between line traverses were accurately tied into the grid employing a hip-chain and compass. Similarly, all topographic and geomorphic features were tied into the grid during mapping the property.

l l l l l l l

At each outcrop, detailed notations as to lithology, structure, alteration, and mineralization were recorded. Where warranted, specifically at all outcrops exhibiting significant alteration and/or mineralization, samples were collected for gold and 30 element ICP analysis.

The results of the geological mapping appear in Appendix l, as the 1:2000 scale North, Central, and South Sheets (Maps l to 3), as well as in Appendix 2 on a 1:5000 scale Geology-Geophysics- Geochemistry Compilation (Map 4). All sample locations, as well as detailed descriptions and resultant Au analytical results, also appear plotted on the 1:2000 scale Maps l to 3. Raw geochemical data appears in Appendix 5.

23

RESULTS AND INTERPRETATION

LITHOLOGIES

The mapping identified six major lithological groups on the property, as outlined on the legend appearing on each of Haps l through 4. Below are general descriptions of each.

1. INTERMEDIATE TO MAFIC METAVOLCANICS

This is the most prevalent lithological group encountered during mapping, outcropping extensively in the southwest portion of the property, and interpreted as covering the majority of the claim group. Where possible, subdivisions within the group were recorded, and contacts drawn, but for the most part minor textural and alteration/shearing variations were local to the degree that individual sub-units were difficult to trace over any significant strike continuity. As such, sub-units 1A, IB, and 1C are all incorporated within the confines of one contact.

1A. ANDESITE

This sub-unit outcrops sporadically throughout the southwest portion of the property, and is best exposed in the vicinity of Lines 12E to 15E at baseline. The lithology is usually massive to very weakly foliated, light green, and aphanitic to very fine grained. It appears to grade laterally at this location into unit 5 (locally a diorite), and may be a very fine phase of the intermediate intrusive rock. Elsewhere, several "andesitic" appearing outcrops are intermixed with "basaltic" appearing outcrops, and the two terms were often employed simultaneously in lithology descriptions. The term andesite, in the field sense, was used to describe less chloritic (and usually less foliated), lighter green, slightly harder zones within the predominantly basaltic appearing terrain. The variation is, again, probably the result of shearing\alteration intensity, as opposed to a primary magmatic difference.

IB. BASALT

This unit outcrops throughout the southern portion of the property. It is usually moderately foliated, and weakly to

24

mfeiiiiii

moderately chloritized. Usually aphanitic, there are zones in which feldspar crystals are visible, and this coarser unit often grades into sub-unit 1C. Primary textural features are rarely observed. In some places, severely stretched pillow selvages can be seen, but the pervasive fabric developed in the rock has obliterated most readily identifiable textures.

1C. BASALT TO GABBRO

This sub-unit outcrops sporadically throughout the basaltic terrain, as a crystalline equivalent to the predominantly aphanitic basalt. It is for the most part only locally present, as coarser portions of the mafic flows. Typically the rock is moderately foliated and chloritized, with weak to moderate sausseritization of the plagioclase. In some cases, specifically along a prominent south facing ridge between Lines 4E and 8E, at 5+OOS, the distinct coarser flows can be followed with some confidence. This sub-unit differs from the Unit 5 gabbros in that it can be clearly related to adjacent flows, is rarely coarser than 2mm, and exhibits the same degree of alteration and shearing as the adjacent flows. The distinct diorite to gabbro unit (5) is usually massive, and much' coarser grained.

ID. MAGNETITg PEARING BASALT

This very distinct unit occurs as thin bands paralleling stratigraphy across the southern portion of the property. It is characteristically very black, aphanitic, and fissile, and in many places appears to be laminated to the extent that initially the sub-unit was thought to be a tuffaceous equivalent. Where well exposed, however, it is a distinct flow, and can be followed with a very degree of confidence both in outcrop, and via its strong magnetic signature. Typically the rock carries 5 to 10* very fine grained disseminated magnetite. The unit provides good stratigraphic control through the southern portions of the property.

25

2. INTERMEDIATE TO MAFIC TUFFS/LOCALLY DERIVED METASEDIMEWT3

l

2A. ANDESITE TO BASALT (T/S)

In several locations throughout the stratigraphy, the degree of foliation becomes intense, causing the mafic metavolcanics to become thinly laminated, and extremely fissile. This "field term" was employed to describe such zones, which, in many poorly exposed locales appeared to be locally derived metasediments or tuffaceous equivalents to the intermediate to mafic metavolcanic flows. In retrospect, and as a result of the stripping program on the property, it became apparent that this unit is simply an intensely sheared equivalent to Unit 1. As such, it is incorporated within the contacts defining Unit 1.

2B. QUARTZ EYE INTERMEDIATE TUFF

This sub-unit was noted only at two locations, one in the vicinity of L2+OOW, 2+75S, and the other in a thin slit trench at L1+50E, 2+50S. At both locations, the unit is thin ^5 metres), and comprised of an aphanitic andesitic appearing matrix with 5 to 15% small (O mm.) elongate quartz crystals\fragments. The unit is concordant with stratigraphy, and probably represents a thin interflow tuffaceous horizon.

2C. OXIDE FACIES IRON FORMATION

This sub~unit does not outcrop on the property, but rather is interpreted as being present based on geophysics. In the central portion of the claim block, three parallel, east-west trending coincident linear magnetic highs and VLF-BM conductors were defined by ground geophysical surveys. The responses are typical of either a massive pyrrhotite exhalative interflow, or an oxide facies iron formation with a significant sulphide (sulphidlzed) component. It is interesting to note the apparent disruption and repetition of the otherwise very linear features in the vicinity of Lines 15+OOE to 22+OOE, between 8+OON and 10+OON. This may be a zone of complex folding within the exhalative, and represents an interesting drill target, as proposed in section l of this report.

26

l l

2D. PYRITICVGRAPHITIC INTERFLOW

l This sub-unit does not outcrop on the property, but rather isinferred based on the interpretation of geophysical data, and the

. discovery of massive pyrite float in some of the trenches l completed on the claim block.

A strong VLF-EM conductor, with no associated magnetic response,

I trends east-west across the property along Baseline 0+00. Immediately south of this anomaly, in the vicinity of L5+

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l

Immediately south of this anomaly, in the vicinity of L5+OOE, 0+75S, several large boulders of massive pyrite were discovered in basal till in an old trench. The conductor is therefore interpreted to be an interflow massive pyritic/graphitic horizon, with little economic potential for gold.

3. EPICLASTIC METASEDIMENTS

3A. POLYMICTIC PARACONGLOMERATE

This unit outcrops sporadically south of Jory Lake. It is

( typically comprised of a poorly sorted graywacke matrix, with predominantly quartz, chert, and dioritic to granodioritic clasts to 10 cm. and 40* by volume of the rock. Where observed in

l outcrop, the paraconglomerate showed no indications of strong l foliation or significant alteration. The contact with the

northern volcanic package is inferred from airborne magnetic data to cross the central portion of Jory Lake, trending at

I approximately 080 degrees. The contact, as with most in the Deardmore-Geraldton belt, is felt to be tectonic, and may be the locus of significant hydrothermal alteration/mineralization,

l analogous to the Metalore Brookbank deposit. Two holes areproposed to fence through the interpreted contact area in the vicinity of a moderate VLF-EM anomaly.

4. LITHOSTRUCTURALVALTERATION UNIT

4A. CHLORITE-SERICITE-Fe CARBONATE SCHIST

Three distinct zones of intense shearing and related alteration were defined on the property during mapping. All zones cut intermediate to mafic metavolcanics, and are characterized by an

27

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lassemblage of sericite, Fe carbonate, and remnant chlorite. The

I criteria used in classifying a shear within the mafics volcanics as Unit 4, was a combined sericite-carbonate content of ^0*. In fact this classification was redundant, as the zones of alteration were extremely well defined, with sharp contacts over

I the width of l to 2 metres with the less altered and sheared metavolcanics. Typically the zones are comprised of Fe-carbonate bands along schistosity planes, to 20 to SQ* of the rock, within

I an assemblage of sericite and chlorite. The central, most intensely sheared portions of the zones are almost exclusively sericite-carbonate, with chlorite content increasing at the

(expense of sericite outwards towards the alteration zone margins. Shear fabric within the zones is intense, trending subparallel and parallel to stratigraphy at 075 to 090 degrees. Strong S kink banding is prevalent throughout the shear, as are north-south

l trending extension fractures, indicating that probably the shears " are cutting zones of axial planar weakness within a broad fold

structure. Direction of fold closure is not known. Secondary

( quartz, quartz-Fe carbonate, and Fe carbonate veins are sporadically present throughout the shear zones, almost exclusively as thin, very discontinuous, boudined to brecciated

I and rotated foliation parallel features. Only a very few of these veins carry associated disseminated pyrite and arsenopyrite mineralization. A more detailed discussion of the economic significance of the shears appears later in this report.

The northernmost zone defined by mapping trends at 080 degrees between LO+00 and L8+OOE, at approximately 1+OOS, and is best exposed in an old trench on L5+OOE, 1+OOS. At this location, the alteration zone is at least 15 metres in width.

The central shear zone is exposed in a series of pits from L5+OOE at 1+50S, to L9+OOE at 1+OOS, again trending at 080 to 085 degrees. This zone is of appreciable width, to 20 metres.

The southern zone is exposed in a series of trenches between L2+OOE, at 2+75S, and L5+OOE, at 2+25S. The zone initially appeared to trend at 070 degrees, slightly oblique to stratigraphy, but as will be discussed in the Power Stripping section of this report, is actually comprised of a series of sinistrally offset en echelon zones trending at 085 degrees.

28

Several thin and apparently discontinuous zones of similar alteration were discovered elsewhere on the property. Between L4+OOE and L5+OOE, at 3+25S, a thin 5 metre wide zone can be traced in relatively good outcrop exposure for only 20 metres.

Immediately west of the property/ two thin zones are exposed along the Kinghorn Road on ground held by a competitor, and trend at 075 degrees on to our property. The immediate extensions of these exposures could not, however, be located on our ground, due to very poor outcrop exposure in the immediate area.

The three major zones of alteration and shearing all are probably the result of a broad anastomosing shear system related to and along the Paint Lake Fault.

5. MAFIC INTRUSIVE ROCKS: DIORITE. GABBRO

This unit outcrops in the east central portion of the property. Between L9+OOE and L14+OOE, at approximately 0+50S, a major ridge of diorite to gabbro is well exposed. South of this zone, between L6+OOE and L16+OOE, at approximately 2+OOS, a series of exposures define a 080 degree trending gabbro horizon. Both zones are conformable to stratigraphy, indicating emplacement as sills within the sequence of volcanics. The unit is characterized by its relatively coarse texture (predominantly medium grained), and relatively weak fabric development in relation to the encompassing volcanic terrain. Compositionaly the unit varies locally from dioritic to gabbroic appearing (based on ferromagnesian mineral content). The unit is non-magnetic.

6. LATE PROTEROZOIC INTRUSIVE ROCKS - DIABASE

Thin (>l metre) strongly magnetic, and characteristically porphyritic diabase dykes were noted at only one location on the property, in an old pit at L7+25E, 1+25S. Locally the dyke was extremely contorted, and offset by 030 degree trending fractures/faults. Generally in the area, and based on the regional airborne magnetics, these dykes trend north-south as a swarm across the central part of the property.

29

lll

STRATIGRAPHY

Based on the geological mapping, as well as the geophysical definition of interformational stratigraphic exhalative horizons, the stratigraphy trends at approximately 085 degrees across the property. Local minor variations, between 075 and 090 degrees, are probably the result of gentle flexural folding of the sequence.

A major stratigraphic break between the younger, polymictic paraconglomerates of the Beardmore-Geraldton Belt, exposed south of Jory Lake, and the predominantly mafic metavolcanic assemblage of the Onaman-Tashoda Terrain, encountered during mapping on most of the property, is envisioned as crossing through Jory Lake, at approximately 075 degrees. This break, west of the property, is occupied by the regional Paint Lake Fault/Deformation Zone. Splays from this regional fault are associated with significant gold mineralization west and along strike from the property, at the Brookbank deposit.

STRUCTURE

The aforementioned Paint Lake Fault is inferred as crossing the property proximal to the contact between the sediments, to the south, and volcanics to the north, as just discussed. With no exposure of the contact zone, it is Impossible to determine if the defined zones of Unit 4 are actually expressions of the anastomosing Paint Lake Fault/Shear system, or subsidiary splays off of a contact hosted shear/fault system. As outlined in Section l, a drill fence is designed to test the contact zone.

A pervasive fabric is developed throughout the volcanics exposed on the property, trending parallel to stratigraphy at approximately 085 degrees, and dipping steeply to the south at 075 to 085 degrees. Throughout the property, small scale S kink banding, and north-south extensional fractures, indicate that the stratigraphy is situated on the limb of a fold structure, though closure direction is not known.

*

Several 030 degree trending cross faults sinistrally transpose stratigraphy on a small scale (^ metres) throughout the property. These faults are consistent with an interpretation of dextral movement on a regional shear system, reflecting antithetic slip along the 030 degree trend within the broad deformation system.

30

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SAMPLE WO. Au (PPB) LOCATION

38415 262 L3+40E, 2+25S

38422 820 L4+OOE, 2+20S

LITHOGEOCHEMICAL SAMPLING RESULTS

During first pass mapping/ a total of 49 samples were collected on the property, and forwarded to Min-En Laboratories for Au analysis, and 30 element ICP analysis. Subsequent re-analysis of all samples for gold was completed by Chemex Laboratories, also of Vancouver. As mentioned, all Au results appear plotted on the 1:2000 scale geological maps, with detailed sample descriptions. The raw geochemical data appears in Appendix 5.

Only 5 of the initial 49 samples collected from the property returned anomalous gold values of ^0 ppb. They were;

DESCRIPTION

Pit exposing Fe carb-ser altered shear, with tr. diss Py.

Pit, exposing a 2H wide quartz vein. Sample is from mineralized wallrock (5* Py, 3* AsPy) immediately adjacent to vein.

Pit exposing qtz-carb veining in Fe carb-ser altered mafics. Grab is of qtz vein blast rock with 31 Py, 3\ AsPy.

20 metres east of above pit, grab of ser-Fe carb schist with tr. AsPy,Py.

Fe carb - sericite altered shear zone west of property, with 40* thin quartz-carbonate stringers and 3* diss. Py, l* AsPy.

38437 1968 L5+10E, 1+50S

38439

38449

465

310

L5+30E, 1+50S

Kinghorn Rd.

31

All other samples failed to return appreciable gold values. The ICP data failed to define broad zones of any pathfinder element (As, Sb, B, V,) enrichment within the sampled alteration zones. Arsenic was obviously elevated in samples in which arsenopyrite was noted, but again most samples returned only background level values. A discussion of the economic significance of the sample results appears in Section 4 of this report.

i ™

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3.2 GROUND GEOPHYSICAL (VLF-EM. TOTAL FIELD MAGNETICS) SURVEYS

i) METHODS EMPLOYED

During the period May 26 to June 03, 1990, 66 line kilometres of VLF-EM and total field magnetics surveys were completed on the property. The work was performed by Northwest Geophysics Ltd., a Thunder Bay based contractor.

Instrumentation for the survey was an E.D.A. Omni IV, which reads VLF-EM and total field magnetics simultaneously. Total field magnetic readings were taken at 25 metre intervals along all cross lines. All readings were corrected for diurnal drift employing a base station magnetometer cycling at 30 second intervals, established at Ll+OOE, 1+OOS. The data appears plotted on the enclosed 1:5000 Contoured Total Field Magnetics Map (Map 5) in Appendix 3. A base value of 59,000 nT was subtracted from all readings, and the data appears contoured at 100 nT intervals. VLF-EM readings were also taken at 25 metre spacings along all cross lines, employing the transmitter at Cutler, Maine (NAA, 24.0 KHz). The in-phase and quadrature components of the VLF-EM field were measured at each station, and appear plotted as line- profiles at l cm. * 50* on the enclosed Map 6 in Appendix 3.

RESULTS AND INTERPRETATION

TOTAL FIELD MAGNETICS

The majority of the property is characterized by a moderate magnetic signature in the 59,500 to 59,800 nT range. In the southern portion of the claim group, several thin, linear magnetic highs cross the property at approximately 080 degrees. These correspond well with outcrops of Unit ID, a strongly magnetic basalt, and the magnetics data was useful in defining the limits of these stratigraphic markers.

32

l l l

In the central and northern portion of the property, the thin,

linear east - west trending magnetic highs correlate well with strong VLF-EH conductors, and probably reflect the presence of interformational chert-pyrrhotite/magnetite exhalative horizons, as discussed in the following section of this report.

There is no apparent signature to the inferred contact between the metasediments to the south of Jory Lake, and the northern

volcanic package, though obviously this due in large part to the lack of coverage over the lake.

Similarly, there are no definitive north-south trending highs that would correspond to crosscutting Proterozoic diabase dykes, though there is an apparent airborne magnetics feature so

M interpreted. Because of the orientation of the grid, it is very H likely that the dykes were missed between lines.

VLF-EM

Eight distinct conductive horizons were outlined on the property by the VLF-EM survey, and appear labelled as A through H on the enclosed profile plot. Below are interpretive continents as to their cause.l

lCONDUCTOR A

This short strike length anomaly, located in the extreme southwest portion of the property, trends at 070 degrees into

Jory Lake, where obviously it is lost. It is located proximal to the inferred contact between the polymictic paraconglomerate to the south of Jory Lake, and the predominantly volcanic package to

' the north. The conductor may reflect shearing at that contact, or more optimistically, a horizon of significant sulphide mineralization. As previously mentioned, a two hole fence to test

the contact zone and this VLF-EH anomaly has been proposed in Section 1.

CONDUCTOR B

This long strike length, property wide east - west trending strong conductor is interpreted to be a massive pyrite exhalative

horizon, or a pyritic-graphitic interflow sediment, due to its long, interformational character, the lack of any associated

33

l l l l l l l l l l l l l l l l l l l

magnetic response, and the discovery of massive pyrite boulders in trenches immediately south of the axis of the anomaly. All samples of the massive pyrite float failed to return any elevated precious or base metal values, and as such the horizon is not seen as having economic significance. A deep hole designed to test the parallel carbonate shear zones immediately south of this conductor will pierce the anomaly, however, as the additional drilling required to truth the interpretation is minimal (25 metres).

CONDUCTOR C

This strong conductor trends east-west across the entire central portion of the property, and has a coincident moderate magnetic response. It is clearly an interformational horizon, and because of the magnetic association is interpreted as being a chert- pyrrhotite or pyrrhotized oxide facies iron formation.

CONDUCTORS D. E. F

These shorter strike length conductors, immediately north of Conductor D, all also exhibit a coincident and contorted magnetic signature. They are interpreted as being folded equivalents of Conductor D, and a three hole fence is proposed to test all four conductors in an area of inferred complex folding. This area represents an interesting target, as there is very real potential for sulphidized iron formation hosted gold mineralization in this setting.

CONDUCTOR G

This east-west trending strong conductor crosses the property in the vicinity of TL12+OON. Again, it is associated with a moderate magnetic anomaly, and is interpreted as being a chert-pyrrhotite exhalative horizon. Drilling, by Dome and HUdbay east of the property appears to have intersected the eastern extension of this conductor, encountering thin chert-pyrrhotite bands within andesites.

CONDUCTOR H

This short strike length, weak conductor, situated in the extreme northwest corner of the property, is probably an overburden related anomaly as opposed to a truly conductive bedrock response.

34

ft i i i i i i i i i i i

3.3 POWER STRIPPING/TRENCHING PROGRAM

3.1 METHODS EMPLOYED

During the peziod June 13 through July 15, 1990, a power stripping program was completed on the Missing Link property by Nelco Equipment, a Beardmore based contractor. The program involved 121 hours of backhoe work, employing a 215 Caterpillar Excavator, and 16.5 days of outcrop washing employing a Wajax pump. Prior to the stripping program, all major areas to be stripped were cleared of timber by Mr. Dave Kindla, a Beardmore based contractor, employing a Timberjack skidder. The cleared timber has been limbed and stacked on the property.

Following the stripping program, detailed geological mapping, at a scale of 1:100, was completed over all trenches in which outcrop was exposed. All major areas of interest were channel sampled at 10 metre line intervals, with collection of l metre saw cut channel samples across the zones of potential mineralization. A total of 325 channel samples were collected, and forwarded to Chemex Laboratories in Vancouver for gold analysis by fire assay.

Appendix 4 contains Maps 7 through 14, as follows;

Map 7 1:2000 Location Map, Stripped Areas l to 6Map 8 1:2000 Location Map, Stripped Area 7Map 9 1:2000 Location Map, Stripped Area 8Map 10 1:2000 Location Map, Stripped Area 9Map 11 1:100 Detailed Geology, Sample Locations, and Gold

Geochemistry, Stripped Area Number l Map 12 1:100 Detailed Geology, Sample Locations, and Gold

Geochemistry, Stripped Area 2A Map 13 1:100 Detailed Geology, Sample Locations, and Gold

Geochemistry, Stripped Area 2B Map 14 1:100 Detailed Geology, Sample Locations, and Gold

Geochemistry, Stripped Area 3

All raw analytical data appears in Appendix 5.

The following section of this report summarizes the results of the stripping program.

35

ll l l l l l l l l l l l l l

3.2 RESULTS AND INTERPRETATION

STRIPPED AREA l

This stripped area, approximately 125 metres in length, and 30 metres in width, was excavated in the vicinity of a series of small hand pits and trenches that exposed quartz-carbonate veining within Unit 4, the chlorite-sericite-Pe carbonate altered and sheared mafic metavolcanics.

The stripping exposed an east-west zone of intense shearing and associated chlorite-sericite-Pe carbonate alteration, approximately 25 metres in width, hosted within less altered, predominantly massive mafic metavolcanics. Within the shear zone, are several irregular, discontinuous, boudined to brecciated quartz and quartz-carbonate veins, carrying sporadic pyrite and rarely, arsenopyrite mineralization. A total of 180 l metre channel samples were cut across the exposed zone, at ten metre intervals. Only 7 of the 180 samples returned significantly elevated gold values of ^00 ppb. They were;

SAMPLE NO.

39086

ASSAY (GPT)

1.78

LOCATION

L5+10E

39115 0.620 L5+20E

39157 1.16 L5+50E

DESCRIPTION

l metre channel across shear with thin qtz-Aspy stringers to 10* rock. Grabs from this location had previously returned values to 1.96 GPT.

l metre channel sample across ser-chl-Fe carb shear. No significant veining or mineralization noted.

l metre channel across shear, with a 20 cm. discontinuous quartz vein.

l l 36

ll l

SAMPLE NO. ASSAY LOCATION DESCRIPTION

f 39164 0.96 L5+60E l metre channel acrossshear, with a 20 cm. qtz.

- vein.

l

l

l

l

l

l

l

39165 2.06 L5+60E l metre channel acrossshear with a 25 cm. gtz. vein.

39166 0.65 L5+60E l metre channel acrossshear with a 20 cm. gtz. vein and trace Aspy.

39177 1.16 L5+70E l metre channel acrossshear, with a 20 cm. gtz. vein.

The best results came from three contiguous samples crossing a zone of guartz veining in the extreme east section of the stripped area. The 3 metre interval averaged 1.22 gpt, though only 5 metres along strike, the same zone of veining returned values of 30 to 100 ppb. The low values, and sporadic nature of the gold mineralization encountered in this area warrant them uneconomic. It is worth noting the increase in vein density moving east through the stripped area, and the potential for more significant mineralization along strike in the shear system.

STRIPPED AREA 2

This stripped area, centred around L7+OOE, 1+25S, was designed to expose the shear zone east and along strike from Stripped Area l, in the vicinity of an old pit exposing significant guartz veining within the shear. Two areas were exposed as a result of the trenching/stripping, and appear as Maps 12 and 13 in Appendix 4. Both areas exposed the shear zone, and associated chlorite- sericite-Fe carbonate alteration. In Area 2A, significant guartz veining was present within the shear, though sulphide mineralization was extremely rare. No significantly elevated gold values were returned from the 82 channel samples collected from the zone.

37

l i i i i i i i i i i i i i i i

STRIPPED AREA 3

This stripped area, approximately 90 metres in length, by 15 metres in width, was designed to better expose zones of shearing and related alteration within the mafic metavolcanics uncovered by Hr. Nolan Cox in 1989. The stripping exposed two zones of shearing, and associated chlorite-sericite-Fe-carbonate alteration within the mafic metavolcanics, both very discontinuous in nature. Within the shears, quartz veining is rare, with the exception of a Z folded, 2 metre thick vein at the nose of a tight Z fold on L3+90E. The strike extent of the vein, however, is only 2 metres, as the fold nose host plunges steeply east at 55 degrees. No significantly elevated (}500 ppb) gold values were returned from the 53 channel samples collected from the zones of shearing and alteration.

STRIPPED AREA 4

This small trench, centred around L4+25E, 3+25S, was designed to better expose a small zone of shearing and related alteration within mafic metavolcanics discovered during the mapping program. The trench, approximately 25 metres by 10 metres, exposed a 4 metre wide zone of intense shearing, trending at 075 degrees, across its length. The shearing, hosted within mafic metavolcanics, was accompanied by pervasive Fe carbonate and sericite alteration. No significant quartz veins were present in the shear. Minor (<5%) disseminated pyrite was present locally within the shear zone. Grab samples from the zone failed to return significantly anomalous gold values, the highest being only 270 ppb Au.

STRIPPED AREA 5

This trench targeted a strong VLF-EM conductor. Unfortunately, the trench did not reach bedrock, as the overburden was locally in excess of 7 metres in depth.

STRIPPED AREA 6

This thin trench, located on Line 7+OOE between 0+50 and 1+OOS, exposed a broad zone of intense shearing and associated Fe carbonate-sericite alteration within mafic metavolcanics. Only one thin 10 cm. quartz vein was present in the shear, from which two grab samples returned values of 450 and 210 ppb Au.

38

4.0 COST STATEMENT

The following is a summary of costs incurred in completing the 1990 exploration program on the property.

1. Option Payment: ................................... S15,000.

2. Line cutting: (72 km. ^245\km.)................... $17,640.

3. Geophysical surveys: (66 km. ^169.\km)............ $ll / 154.

4. Pre stripping tree clearing (Kindla)............... $2 / 400.

5. Total Power Stripping Costs: (including labour for tree falling, wajax pump operation, channel sampling, fuel)

....................................................$20,227,

6. Analytical: .........................................55,786.

7. Geological Salaries and Supervision:................515,210,

8. Miscellaneous Field Support: ........................S3,528,

TOTAL ; 590^945,

40

111

5.0 SELECTED REFERENCES

1

1

1

1

1

1

nli1~

Burke, R.1989

Lassila, P.1987

Mason, J., andMatthews, M.1980

Mason, J., andWhite, G.1986

Reilly, B. A.

Terraquest1987

,

-EXPLORATION CRITERIA AND TARGETS FOR THEBEARDMORB-GBRALDTON BELTRobert S. Middleton Exploration Services Report

REPORT ON A VLF-EM AND MAGNETOMETER SURVEY FORGOLDEN EARTH RESOURCES, LAPIEERE AND LEGAULTTOWNSHIPS, ONTARIO1987 Assessment Report, MNDM Files, Thunder Bay

LAPIERRE LAKE AREA, DISTRICT OF THUNDER BAYOGS Prelim Map P. 2070, Thunder Bay Data Series,Scale: 1:15,840

GOLD OCCURRENCES, PROSPECTS, AND DEPOSITS OFBEARDMORE-GERALDTON AREA, DISTRICT OF THUNDERBAY AND COCHRANEOntario Geologic Survey OFR 5630

STRUCTURAL ANALYSIS OF THE PAINT LAKE 1988 DEFORMATION ZONE, NORTHERN ONTARIOBrock University, Unpublished M. Se. Thesis

REPORT OF AN AIRBORNE MAGNETIC AND VLF-EMSURVEY IN ... LAPIERRE AND LEGAULT TOWNSHIPS,THUNDER BAY MINING DIVISION, FOR GOLDEN EARTHRESOURCES1987 Assessment Report, MNDM Files, Thunder Bay

41

n l

6.0 STATEMENT OF QUALIFICATIONS

* I, Duncan F. Mcivor, do hereby state that;

I - I am a graduate of the University of Waterloo, with an H.BASc. (Co-operatve Earth Science).

I - I have been employed in the mineral exploration industry since 1974, holding positions with Esso Minerals Canada, BMP-Utah Mines Ltd., BMP-Utah International, and Homestake Mineral

Development Company.

- -I am currently employed by Homestake Mineral Development Company, in the capacity of Regional Exploration Geologist,

l Northwest Ontario District.

- I have personal knowledge that the information contained in m this report is complete and correct.

l __________l Duncan F. Mcivor Date and Place

lll

lll

42

7.0 TECHNICAL DATA STATEMENTS

l

l43

n n li n li

rMinistry ofNorthern Developmentand Mines

Geophysical-Geological-Geochemical Technical Data Statement

Ontario

TO BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORTFACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT

TECHNICAL REPORT MUST CONTAIN INTERPRETATION. CONCLUSIONS ETC.

Type of Survcy(s) Township or Area Claim

Survey CompanyAuthor of Report.Address of AuthorCovering Dates of Snrwy Mifi

Total Miles of Line Cut

- AiV^XT eT el,{EncoittiDf lo office)

7g lidE-

SPECIAL PROVISIONS CREDITS REQUESTED

ENTER 40 days (includes line cutting) for first survey.ENTER 20 days for each additional survey using same grid.

Geophysical—Electromagnetic.—Magnetometer.——Radiometric———Other—————.

DAYSpcrdiim

GeochemicaLAIRBORNE CREDITS

Electromagnetic———(oMcrdqrspcrcfaim)

do not apply to aiibume Mfw

—™Radiometric

SIGNATURE)*!

Res. Geol.. .Qualifications.Previous Surveys

File No. Type Date Claim Holder

BONING CLAIMS TRAVERSED List numerically

••••JWMOTh***K***3*55W?9nVf******MJBKl*********ifcwefe) (anter)

l

CLAIM STATUS MISSING LINK PROPERTY

CLAIM REC. DATE.ASSESSMENT CREDITS

GPHY. GEOL. GCH. DR. EXF? TOT .

907485 907486 907487 907488 907489 907490 907491 907492 907493 907494 907495 907496907500 907507 907508 907509 907510 907511 907512 907513 907514 907515 907550 907851 907852 907853 907854907855 907856 907857 907858 907859 907860 907861907862

MAY 20,86 MAY 20,86 MAY 20,86 MAY 20,90 MAY 20,86 MAY 20,86 MAY 20,86 MAY 20, 86 MAY 20,86 MAY 20,86 MAY 20,86 MAY 20,86MAY 20,86 MAY 20,86 MAY 20,86 MAY 20,86 MAY 20,86 MAY 20,86 MAY 20,86 MAY 20,86 MAY 20,86 MAY 20,86 MAY 20,86 MAY 20,86 MAY 20,86 MAY 20,86 MAY 20,86MAY 20,86 MAY 20,86 MAY 20,86 MAY 20,86 MAY 20,86 MAY 20,86 MAY 20,86MAY 20,86

80 80 80 80 80 80 80 80 80 80 80ftAo v80 80 80 80 80 80 8O 80 80 80 80 80 80 80 8080 80 80 80 80 80 80finOU

40 40 40 40 40 40 40 40 40 40 4040 40 40 40 40 40 40 40 40 40 40 40 40 40 40 4040 40 40 40 40 4040 40

0 0 0 0 0 0 0 0 0 0 00 0 0 0 0 0 0 0 0 0 0 0 0 0 00 0 0 0 0 0 000

0 23.52 0 23.52 0 33.52 0 43.52 0 23.52 0 23.52 0 23.52 0 23.52 0 43.52 0 53.52 0 23.520 23.52 0 80.74 0 23.52 0 23.52 0 23.52 0 23.52 0 23.52 0 33.52 0 38.52 0 43.52 0 43.52 0 100.00 0 80.74 0 80.74 0 80.740 80.74 0 80.74 0 80.74 0 80.74 0 80.74 0 43.52 0 90.520 95.520 85.52

143.52 143.52 153.52 163.52 143.52 143.52 143.52 143.52 163.52 173.78 143.52143.52 200.74 143.62 143.52 143.52 143.52 143.52 153.52 158.52 163.52 163.52 220.00 200.74 200.74 200.74200.74 200.74 200.74 200.74 200.74 163.52 210.52215.52 1205.52 1

EXPIRY DATE

MAY 20,91 MAY 20,91 MAY 20,91 MAY 20,91 MAY 20,91 MAY 20,91 MAY 20,91 MAY 20,91 MAY 20,91 MAY 20,91 MAY 20,91 MAY 20,91 MAY 20,92 MAY 20,91 MAY 20,91 MAY 20,91 MAY 20,91 MAY 20,91 MAY 20,91 MAY 20,91 MAY 20,91 MAY 20,91 MAY 20,92 MAY 20,92 MAY 20,92 MAY 20,92 MAY 20,92 MAY 20,92 MAY 20,92 MAY 20,92 MAY 20,92 MAY 20, 91 MAY 20,92 MAY 20,92 MAY 20,92

CLAIM REG. DATE ASSESSMENT CREDITS EXPIRY GPHY. GEOL. GCH. DR. EXP. TOT. DATE

907867 MAY 20,86 80 40 O907868 MAY 20,86 80 40 O907869 MAY 20,86 80 40 O907870 MAY 20,86 80 40 O907871 MAY 20,86 80 40 O907872 MAY 20,86 80 40 O907873 MAY 20,86 80 40 O907875 MAY 20,86 80 40 O907876 MAY 20,86 80 40 O907877 MAY 20,86 80 40 O907878 MAY 20,86 80 40 O907879 MAY 20,86 80 40 O907880 MAY 20,86 80 40 O907881 MAY 20,86 80 40 O907882 MAY 20,86 80 40 O907883 MAY 20,86 80 40 O907884 MAY 20,86 80 40 O907885 MAY 20,86 80 40 O907890 MAY 20,86 80 40 O

0000000000000000000

90.23.43.23.23.23.23.80.99.90.85.99.33.28.10099.23.43.55.

5252525252525274325252525252.0052525252

210.143.163.143.143.143.143.200.219.210.205.219.153.148.220.219.143.163.175.

52525252525252743252525252520052525252


20202020202020202020202020202020202020

ifi,ititt,ttt*i,*tt

92919191919191929292929291919292919191

* Note that credits listed as greater than 200 nan days are In anticipation of Notices of Reduced Assessment Credit for geological napping on partially water covered claims. This Claim Status Summary will be updated upon acceptance of all filed work.

Figure 3 Illustrates the locations of the claims that comprise the property.

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STRIPPED AREA/TRENCH 7

This thin trench, located on L12+OOE, between 0+25N and 0+75N, was designed to expose a strong VLF-EM conductor. The trench failed to reach bedrock, as overburden was locally in excess of 7 metres.


This thin trench, located between L3+OOE and L4+OOE, at 6+75N to 7+25N, was designed to expose a strong coincident magnetics/VLF- EM anomaly. The trench failed to reach bedrock, as locally the overburden was in excess of 7 metres.


This thin trench, located on L5+OOE between 11+50N and 12+OON, was also designed to provide exposure over a strong coincident mag/VLF-EM anomaly. Again, due to overburden depths in excess of 7 metres, the trench failed to reach bedrock.

39

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DATE : 6/ 5/90 NTS : 42 E/14FREQ.: 24.0 KHz.

LTT).

-- w itr—- . - *-

CMOo

o o UJo oLJ OoCM

LJ Ooro

LJ o oU Ooin

UJo o(O

LJ O O

LU O O OD

LU O O en

LJo o o

LJ Oo

LJ Oo(N

LJ O O

LJ o o

LJ Oo m

LU o oCO

OoLJ o o00

LJ Oo

LJ O OoCM

LJ OoCM

LJ O O CM (N

O O COCM

Oo-CM

2000N TL 2000 N

1800N

1600N

1400N

BASELINE 1200N

1000N

800N

600N

400N

TL 250 N

200N

0+00

200S

400S

600S

800S

1000S

1200S

TL 400 S

63 6*36 LAPIEHfit LAKE 330

ln*trum*nt i OMNI IVn.W i TOTALDatum i 58000.0 nT

Contour Interval : 100 nT

Conductor Axis i

ip.,

HOMESTAKE MINERALS CO.MAP 5 MAGNETOMETER SURVEY

PROJECT: MISSING LINK PROJECT # : 5608 BASELINE AZIMUTH : 90 Deg.

SCALE = 1 : 5000 SURVEY BY : NWG

DATE : 6/ 4/90 NTS : 42 E/14

NORTHWEST GEOPHYSICS LTD.

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