PRELIMINARY RPT ON OC STRIPPING

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42A04NW8553 3 .11712 KENOGAMING 010

PRELIMINARY REPORT on theOutcrop Stripping - Trenching Program

Reeves Joint Venture Propertyfor

GLEN AUDEN RESOURCES LIMITEDand

GOLDROCK RESOURCES INC.by

Ron Burk, M.Sc.Eng, August 10, 1988

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LANDS SECTION

M-223


42A04NW8553 Z . 11712 KENOGAMING 010C

TABLE OF CONTENTS

INTRODUCTION.

AREAS MARKED FOR OUTCROP STRIPPING/TRENCHING.

COMPLETED WORK.

CERTIFICATION

PAGE

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LIST OF FIGURES

Figure l Map l Map 2

Property Location Property Claim Map Trench Locations

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INTRODUCTION

l A program of mechanical outcrop stripping and trenching was

initiated by Glen Auden Resources and Goldrock Resources in June,

~ -1988 on their jointly held Reeves Joint Venture (RJV) property

B located in Reeves, Sewell, Kenogaming and Penhorwood Townships.

This work is being done to follow-up geologic mapping,

l geophysical surveying (ground magnetics and induced polarization

methods) and a limited amount of outcrop stripping done in

B November, 1987. Specifically, the trenching will attempt to

H expose areas marked by chargeability/resistivity (IP) anomalies

which ideally indicate concentrations of sulfide mineralization,

l Machinery being used for this work consists of a D7F Caterpillar

bulldozer and a 945 Caterpillar excavator. Bedrock exposed by

the stripping and trenching is being mapped and sampled for gold

content. High-pressure water pumps are being used to wash loose

dirt and rubble from the bedrock surfaces. In trenches where

l bedrock is not reached samples of glacial till will be collected

and analyzed for gold.

M AREAS MARKED FOR OUTCROP STRIPPING/TRENCHING

Geologic mapping and the interpretation of airborne and

l ground magnetics survey data suggest that within the mafic

volcanic sequences which underlie much of the RJV property there

' are westerly and southwesterly striking high strain deformation

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REEVES JOINT VENTURE

lo* BO*

REVISIONS ROBERT S. MIDDLETON EXPLOnATION SERVICES INC.

lor GOLDROCK RESOURCES INC./ GLEN AUDEN RESOURCES LTD. J.V.

Tilir

PROPERTY LOCATIONMAP Flq.l

i Oct. gf 1 Sf.jioil"*i60nil, 1U. L S.!_____

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lzones. These zones are considered to be prospective areas for

l gold mineralization. Chargeability anomalies located

coincidently with the interpreted positions of the deformation

zones represent the higher priority targets for the current

B trenching program (Map 2, see back pocket).

The southeast corner of Reeves Township is one area where

l mapping has identified a wide zone of highly sheared and

chemically altered rock which is also marked by a series of

B chargeability anomalies. Other target areas are located within

B 1500 meters northwest and southwest of Deerfoot Lake in

Kenogaming Township. A group of induced polarization anomalies

l in Penhorwood Township which are associated with a sheared

ultramafic unit altered to a talc-carbonate, and locally

B fuchsitic schist will also likely be trenched. Map 2 shows the

tt location of the more prominent chargeability anomalies which have

been targeted for trenching.

lCOMPLETED WORK

B As of August 5th, 1988, 15 days of mechanical stripping have

H 'been done on the property, and specifically on claims 932075 and

901334 in the southeast corner of Reeves Township (Map 2 in back

B pocket). This work completes about one third of the total amount

of trenching estimated to be done on the property. Trench

B locations are controlled by a cut grid which was used for

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YC^ 4W#^;# M#^\y^ . \

PENHORWOOD TWP.

LEGEND . '

Trench or S tripped- Outcrop

Proposed Trench

Chargeability Anomaly (Induced Polarization)

Zone of Shear Deformation

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KENOGAMING TWP.

REVISJOS ROBERT S. MIDDLETON EXPLORATION SERVICES INC,

for

JitleTR.EHCH LOCATION MAP

Fig. ZDale: Drawn:

Scale: j Approved:

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geophysical surveying. An east-west base-line follows the

l Reeves/Penhorwood and Sewell/Kenogaming township lines, with the

0+OOE/O+OON grid coordinate located at the mutual corner point of

B the four townships.

B The main area of stripping so far has been on line 7+OOW,

between 0+50N and 2+50N (see Map 2). An area of 1500 square

B meters which has been stripped between 7+OOW/1+75N and

7+OOW/2+OON has exposed highly deformed and altered mafic

B volcanic rock consisting of chlorite, sericite and iron

B carbonate. Narrow, discontinuous quartz veins (stringers) are

locally abundant. Schist rock hosting these veins contains

l appreciable concentrations of pyrite. There is also a number of

westerly trending ankerite-quartz veins, 20 to 50 centimeters

B wide, which are exposed in the outcrop.

m Trenches at 8+50W/2+75N, 7+OOW/2+25N and 5+80W/2+15N have

exposed a grey coloured, relatively massive rock which has been

l strongly ankeritized and is locally pyritic. This rock appears

to be highly altered greywacke. Spatially associated with this

B rock are narrow zones or units of dark grey, carbonaceous schist

B commonly containing 20 to 40 percent pyrite.

The trenching work done to date has been successful in

l uncovering previously unknown zones of shear deformation,

alteration, quartz veining and pyrite mineralization, as well as

B expanding existing exposures of such rock. Overburden

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lthicknesses have not exceeded the depth penetration of the

l excavator, however, eastwards from the completed trenches the

. overburden is expected to be thicker, and consequently sampling

l of glacial till instead of bedrock may have to be done.

l Respectfully submitted

lRon Burk, M.Sc.Eng.

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CERTIFICATION

I, Ron Burk of 29 Wardencourt Drive, Agincourt, Ontario certify that;

1. I am a graduate of the University of Toronto

with a Bachelor of Applied Science in Geo-Engineering

2. I am a graduate of Queen's University with a l Master of Science, Geological Engineering.

I have been practising my profession in Canada for 4 years.

4. I have no economic interests in the property M covered by this report.

Dated this August 10, 1988 l TIMMINS, Ontario

Ron Burk

C-C


42A04NW8553 2 .11712 KENOGAMING 020

REPORT on the OUTCROP STRIPPINGand

TRENCHING PROGRAMon the

Reeves Joint Venture Propertyfor

GLEN AUDEN RESOURCES LIMITEDby

Ron Burk, M.Se. Eng. October, 1988

n i: c; r. i v i: D

!i;!KG LANDS SECTION

M-223


42Ae4NW8553 2.11712 KENOGAMING

TABLE

SUMMARY.

INTRODUCTION..

PROPERTY LOCATION AND ACCESS..........................

GENERAL GEOLOGY

ECONOMIC GEOLOGY.

PREVIOUS WORK

AREAS OF OUTCROP STRIPPING/TRENCHING..................

RESULTS OF THE TRENCHING PROGRAM - GEOLOGY AND ASSAYS.

CONCLUSIONS

RECOMMENDATIONS

REFERENCES.

CERTIFICATION

LIST OF FIGURES

PAGE

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Figure l Figure 2

Map l Map 2

APPENDIX A:

Property Location Regional Geology

Location of Trenches and Stripped Areas Detail of Stripped Areas in SE Reeves Township

Assay Certificates

020C

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SUMMARY

A program of mechanical outcrop stripping and trenching was

carried out from July 14 to September 9, 1988 on the Reeves Joint

l Venture mining property located in Reeves, Sewell, Kenogaming and

Penhorwood Townships, Porcupine Mining Division, approximately 55

l km west of Timmins, Ontario. This work has exposed a westerly

trending zone of high strain deformation, 150 meters wide and

likely more than one kilometer in length, in southeastern Reeves

l Township. This zone is characterized by the development of

strongly foliated chlorite-ankerite schist, drag folding of the

f schist, and the presence of ankerite-quartz veins. More than 200

B - rock channel samples were taken from stripped areas along this

deformation zone. Assays show that sheared and carbonatized

l mafic volcanic rock rarely contains anomalous amounts of gold,

but that pyrite-rich, chlorite or sericite schist is weakly

enriched in gold.

The outcrop stripping has, however, uncovered a new gold

occurrence on claim 932074 in the southeast corner of Reeves

l Township. The showing consists of a narrow quartz vein with

visible native gold that dips at a moderate angle to the

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southwest apparently orthogonal to the plunge of a fold which is

l developed in the chlorite-iron carbonate schist, or host rock of

the vein.

' It is recommended that additional stripping/trenching be

H done in the immediate area of the gold-bearing vein. As well, a

number of short diamond drill holes are proposed to test for the

l presence of hidden veins oriented parallel to the known vein.

The major shear zone exposed by the stripping program also

B warrants more exploration work. A number of widely spaced,

H relatively long drill holes drilled northwards through the shear

zone would test for potential vein systems hidden by low-lying

l ground bordering a north-northeasterly flowing creek which occurs

north of the stripped areas.

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INTRODUCTION

l Mechanical outcrop stripping and trenching was done from

July 14 to September 9 1988 on the Reeves Joint Venture (RJV)l '" property located in Reeves, Sewell Kenogaming and Penhorwood

fl Townships. Porcupine Mining Division. Ontario. The property is

jointly held by Toronto-based junior mining companies, Glen Auden

l Resources Limited and Goldrock Resources Inc. This work was done

to follow-up geologic mapping, geophysical surveying (ground

H magnetics and induced polarization methods), and a limited amount

B of outcrop stripping done in October, 1987. The trenching has

exposed bedrock areas marked by chargeability (IP) anomalies

l which were interpreted as sites of disseminated sulfide

mineralization.

B The machinery used for the trenching consisted of a D7F

M Caterpillar bulldozer and a 945 Caterpillar excavator. A

high-pressure water pump was used to wash loose dirt and rubble

l from bedrock surfaces. Exposed bedrock was then mapped at 1:200

scale and sampled for gold content. Approximately 250 rock

l channel samples, cut with a power rock saw (using carbide blades)

H and typically one meter in length, were analyzed by Technical

Services Laboratories in Timmins using the fire assay/atomic

l . absorption method.

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PROPERTY LOCATION AND ACCESS

l The Reeves Joint Venture (RJV) property consists of 427

contiguous unpatented mining claims encompassing approximately

B 6,850 hectares which are broadly centred on the four-corner

B junction of Reeves, Sewell, Kenogaming and Penhorwood Townships,

some 55 kilometers west of Timmins, Ontario (Figure 1). Access

l to the property is via Highway 101 which skirts the northern

boundary of the property, and the main Kenogaming logging road.

B Branching northwards from the Kenogaming road is logging road #3

H which directly accesses the area of the property where most of

the trenching was done.

lGENERAL GEOLOGY

B The Reeves Joint Venture property lies in the northern part

fl of the Archean-age Swayze Greenstone Belt (Figure 2) and covers

typical sequences of mafic submarine flows and less abundant

l Intermediate to felsic volcanics (Milne, 1972: Burk, 1987).

Exposures of sedimentary rocks are sparse on the property, though

B two prominent units of oxide and sulfide facies banded iron

j formation have been identified. Intrusive sheets and pods of

ultramafic and mafic rocks are common, particularly in the

l western and southeastern portions of the claim group.

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85*-

REEVESVENTURE

PROPERTY

80*

REVISIONS ROBERT S. MIDDLETON EXPLORATION SERVICES INC.

for GOLDROCK RESOURCES INC./ GLEN AUDEN RESOURCES LTD. J.V.

TitlePROPERTY LOCATION

MAP Flg .iOjle: Oct. 87Drawn: B.S.B.

Scale: l s|60mi.Approved:

N.T.S.:File: M-223.

1 Mafic lo Intermediate Volcanic Rocks2 Felsic lo Intermediate Volcanic Rocks3 Clastic Sedimentary Rockt4 —*— Iron Formallon5 Mafic lo Ullromoflc Intrusive Rock*6 Felsic Porphyry7 Granitoid Intrusive RocksB Diabase

A Mineral Occurrence

" Mines

~~ Deformation Zone

—— Fault

—— — Geological Boundary—@- Highway '

— - Gravel Road

4—*- Railway

—— Properly Boundary

REVISIONS ROBERT S. MIDDLETONEXPLORATION SERVICES INC.

GLEN AUDEN RESOURCES LTD.

REEVES JOINT VENTURE PROPERTY AND REGIONAL GEOLOGY

2LUlt: Aug. 66 Solf.l" . 4ml. N.T.S.! Uriwn: Approved:___ fitt.' M-gg3

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ECONOMIC GEOLOGY

l Geologic mapping done in 1987 (Burk, 1987) and the

interpretation of airborne and ground magnetics survey data

l indicate that within the mafic volcanic sequences underlying much

m of the RJV property there are westerly and southwesterly

striking, high strain deformation zones which are deemed to be

l prospective areas for gold mineralization. Chargeability

anomalies located coincidently with these deformation zones

B constitute particularly attractive targets for detailed

m exploration work. One such target area is in the southeast

corner of Reeves Township (claims 932075 and 901334) where

l mapping has identified a wide zone of highly sheared and

hydrothermally altered rock which is also marked by a series of

B chargeability anomalies. Old reports from the files of the

m Ministry of Northern Development and Mines describe trenching

work done in this area of Reeves Township in 1935-36 by Erie

l Canadian Mines. This early work was done to locate the source of

black, pyritic quartz rubble evidently containing visible gold

l and assaying 0.14 ounces gold per ton which was discovered in the

m area. In addition, in 1946, Kalbrook Mining drilled 13 holes in

the vicinity of the "float" trench. Apparently no economic gold

mineralization was encountered, although drill logs are not

available.

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PREVIOUS WORK

The geology of the original 267 claims of the RJV property

was most recently mapped in the 1987 field season and is

described by Burk (1987). Early in 1988, eighty-six kilometers

of cut grid lines located within the limits of the original claim

group were surveyed with a magnetometer (Burk, 1988A). In June,

l 1988, an induced polarization survey was done on approximately 26

line-kilometers of the same grid, specifically in areas where

P geologic mapping and the magnetic data suggested good potential

M for shear zone-hosted sulfide mineralization (report in

progress),

l In addition to the geologic mapping and geophysical

surveys, mechanical stripping and trenching was carried out in

P October, 1987 in the southeast corner of Reeves Township, eastern

| Penhorwood Township, and just west of Deerfoot Lake in Kenogaming

Township (Garner, 1987). Two series of overburden pits were also

l excavated and sampled in these areas (Garner, 1987).

For a more comprehensive review of exploration work done on

l the Reeves Joint Venture property by Glen Auden/Goldrock as well

m as other mining companies which previously held claims in the

area the reader is referred to Burk (1987).

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AREAS OF OUTCROP STRIPPING/TRENCHING

l The majority of the stripping and trenching was done on

claims 932075, 901334 and 932074 in the southeastern corner of

l Reeves Township. Nine separate areas were stripped or trenched

m on these claims; their locations are 'tied' to the metric grid

which has its baseline following the Reeves/Penhorwood township

l boundary and its 0+OON/O+OOE coordinate at the junction point of

Reeves, Sewell, Kenogaming and Penhorwood Townships (Maps l and

l 2). Stripped areas identified as Trenches 1,3,8 and 6 were

B targeted on an easterly trending, strong chargeability anomaly

which extends at least 900 meters between lines 3+OOW and 12+OOW,

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(see Map 2, Back pocket). A second chargeability anomaly, south

of, and parallel to the other anomaly was investigated by

Trenches 2 and 5. Three areas on these claims were trenched

because of the presence of small outcroppings of sheared and

hydrothermally altered rock, and are exposed in Trenches 2,7 and

Elsewhere on the RJV property eight trenches were dug to

investigate chargeability anomalies on claims 933528, 933562,

933571, 933573, 987256 and 947253 (Trenches 10 to 16, Map 1). Inm

addition, two areas with known auriferous quartz veining located

on claims 798201 and 798202 (Trenches 17 and 18) optioned by R.

Tremblay of Timmins to Glen Auden Resources, were stripped to

determine the extent of the vein systems. Both of these showings

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can be accessed via an abandoned logging road which branches

southwestwards off the main Kenogaming road and passes south of

Sewell Lake.

RESULTS OF THE TRENCHING PROGRAM - GEOLOGY AND ASSAYS

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The trenching and stripping done during the 1988 field

l season was successful in uncovering previously unknown zones of

shear deformation, hydrothermal alteration, quartz veining and

8 pyrite mineralization. As well, existing outcrops of such rock

. were enlarged. Most important, however, stripping done in the

* northern part of claim 932074, southeastern Reeves Township, has

B led to the discovery of a new gold showing,

The new gold occurrence is located at about 2+90W/3+70N on

f the cut grid (see Trench 4, Map 2). The exposure consists of

^ tightly folded chlorite-ankerite schist which likely represents

* highly deformed and altered mafic lava rock. The rock is

8 strongly foliated and with the segregation of chlorite and iron

carbonate displays a thinly laminated texture. The configuration

B of asymmetric folds in the outcrop suggests the presence of a

M large-scale, westerly-verging fold. Based on the orientation of

the small, parasitic folds and crenulations, the larger fold

B plunges roughly 50 degrees northeast. Native gold occurs as fine

specks in a white quartz vein, 3 to 10 centimeters wide, which

B partially coats a fracture surface oriented at 125"/40"SW. The

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orientation of this vein-filled fracture is such that it is

l roughly orthogonal to the axial plunge of the large fold. The

best assays for 8 samples from the vein were 1.1, 0.13, 0.04 and

l 0.04 ounces gold per ton. Samples of chlorite-ankerite schist

mu f rom the immediate footwall of the gold-bearing vein (where the

vein rock has broken away from the fracture surface) yielded

l assay values of 550, 130, 40, 270 parts per billion (ppb) gold.

Several meters from the vein the altered mafic volcanic rock

l contains only marginally anomalous gold concentrations (10-40 ppb

m gold).

The stripped area in Trench l clearly reveals the source of

l the chargeability anomaly which has been delineated through the

centre of claim 901334 between lines 3+OOW and 12+OOW. The

l exposure (see Inset l, Map 2) shows a strongly foliated, and

m locally drag-folded, pyritic chlorite-ankerite schist.

Disseminated grains and foliation-parallel lenses of pyrite

l constitute between 5 and 15 percent of the rock. Where pyrite

concentrations are greatest, the rock is primarily composed of a

l blackish-green chlorite. Minor amounts of chalcopyrite were

mm observed in disrupted quartz veins hosted by the sulfide-rich

rock. Also observed in the stripped outcrop are a dioritic dike

l which strikes east-west and a 4-meter long pod of ankerite-quartz

rock which is believed to be a boudinaged segment of a

l carbonate-quartz vein. The pyritic rock, the precursor of which

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may have been a sulfide-bearing. fine-grained volcanic

l sedimentary rock, is not appreciably enriched in gold. Of 18

samples collected from this rock all but 2 samples gave assays of

l less than 50 ppb gold. A sample taken at the schist/dike contact

m had the highest gold content, 100 ppb.

The source of the chargeability anomaly which was uncovered

l in Trench l was also the target of Trench 3. At the second

location (see Inset 3, Map 2), three zones of pyrite-rich

l chlorite schist were determined to be the cause of the high

m chargeability. Two of the sulfide zones follow the margins of an

intermediate dike, about 1.5 meters wide, which in appearance

l resembles the dioritic dike exposed in Trench 1. The

intermediate dike is characterized by the presence of muscovite

l phenocrysts up to 20 mm in size, is pervasively carbonatized, and

m contains a minor amount of disseminated pyrite. The sulfide zones

consist of strongly foliated chlorite and laminated aggregates of

l pyrite, with sporadic, small pods of massive pyrite. The third

sulfide zone lies a few meters south of the dike and trends

l obliquely to the dike. It is suggested that with the intrusion

m of t he dike into a pyritic rock, pre-existing sulfide was

remobilized and concentrated at the margins of the dike.

l Seventeen samples were collected from this exposure. Only 3

samples contain slightly anomalous amounts of gold (120, 85, 60

l ppb), all of them being from the pyrite-rich zones.

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Trenches 6 and 8 (see Map 2) failed to reveal the eastern

l extension of the strong chargeability anomaly which was

investigated in the two previously described stripped areas.

l Instead, variolitic and locally pillowed mafic flow rock was

m exposed. Based on the shapes of variolites and pillows, it

appears that these rocks have undergone much less shear

l deformation than the rocks exposed in the stripped areas to the

west. Hydrothermal alteration is also less intense in the

l exposure of the pillowed flow. Weak to moderate iron

H carbonatization is, however, developed at the south end of Trench

6, and disseminated euhedral pyrite (chargeability source) occurs

l just north of this carbonate alteration. None of the 27 samples

taken from these exposures yielded gold assays of greater than 30

l ppb.

B The source of a moderate to strong chargeability anomaly

which strikes across the southern portions of claims 932074,

l 901334 and 932075 was the target of Trenches 5 and 9. At the

former location there had been previous stripping and blasting

l done, probably dating back to the late 1930' s. Detailed mapping

M of this area (Insets 5 and 6, Map 2) shows the presence of

moderately to well foliated chlorite-ankerite schist, i.e.

l sheared and altered mafic volcanic rock. Small-scale drag folds

and crenulations are commonly developed in the schistose rock.

l In addition, a folded unit of weakly foliated, medium-grained

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feldspathic rock has been identified. This rock is characterized

l by the presence of angular clasts or clots of chlorite (which are

altered to fuchsite close to quartz veins). The unit appears to

l be either an intermediate pyroclastic or an early dike with

mm widely dispersed mafic, xenolithic clasts.

Pods of massive pyrite, less than one meter long, and narrow

l zones of pyrite-rich, quartz-sericite rock which appear to pinch

and swell are found at 4+75W/0+80N and 4+95W/0+85N (see Insets 5

l and 6, Map 2). At the latter site narrow, smokey quartz veins

mm are common and the adjacent volcanic rock is bleached (altered)

and pyritic. Five samples were cut from sulfide-rich rock, and

l returned assay values of 100, 190, 900, 170, and 100 ppb gold.

An additional 12 samples were collected from the surrounding

l chlorite-ankerite schist, with gold values ranging between 10 and

mm 1 20 ppb.

The chargeability anomaly investigated by Trench 9 was shown

l to be caused by a 1.5 meter wide zone of highly foliated chlorite

schist hosting narrow, smokey quartz veins which contain

l coarse-grained pyrite. Five samples from this zone failed to

mm yield gold assay values greater than 25 ppb gold. A 30 cm wide

quartz pod located a few meters south of the sulf ide-bearing zone

l of veining does, however, contain appreciable amounts of gold,

with two samples assaying 450 and 1950 ppb gold.

P The trenching and stripping done just west of Line 7+OOW,

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between 0+60N and 2+10N (Trenches 2 nd 9) has exposed a zone of

l high strain deformation roughly 125 meters wide. Mafic volcanic

rock has been sheared and altered to chlorite-iron carbonate

l schist, where the foliation strikes 080 to 100 degrees and dips

M steeply north. Evidence of the shear deformation is best

observed in the large stripped area of Trench 2 (see Inset 2, Map

l 2). Here, there are numerous westerly trending ankerite-quartz

veins, 10 to 50 cm wide, which have been boudinaged and drag

l folded in a dextral sense. Another noticeable feature of this

M exposure is the local abundance of foliation-parallel quartz

stringers. Low concentrations of pyrite d-3% of the rock) are

l commonly associated with these quartz stringers. (Interestingly,

no chargeability anomalies were detected over these areas of

f sulfide mineralization). A total of 78 channel samples were

M taken from this stripped area. Of these samples only 5 returned

assay values greater than 100 ppb gold, the highest value being

m 240 ppb, with all of these samples consisting of weakly pyritic,

quartz vein-bearing chloite-ankerite schist. Several samples

f were collected from ankerite-quartz vein rock, however, none of

B these gave assay values greater than 100 ppb gold.

Outside of the southeastern corner of Reeves Township eight

l trenches were dug to test weak to moderate chargeability

anomalies. Trenches in claims 933562 (Trench 11) and 987256

l (Trenches 15 and 16) failed to reach bedrock and were abandoned.

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The bedrock exposed in Trenches 10,12,13,14 and 17 proved in each

l case to be only weakly altered or structurally deformed. Mafic

volcanic rock with minor amounts of disseminated pyrite or

l pyrrhotite, as is the case in Trench 17, appears to be the source

M of the weak chargeability anomalies investigated by the trenches.

Finally, the stripping which was done on claims 798201

l (Trench 18) and 798202 (Trench 19) southwest of Sewell Lake was

to examine two different styles of auriferous mineralization.

l Detailed mapping of these stripped areas is yet to be done,

B however, key aspects of their geology could still be recognized.

On claim 798201 (Trench 18) a quartz-ankerite vein containing

l coarse-grained pyrite has been traced discontinuously in a

northwest direction for about 30 meters, and is seen to be hosted

l by pyritic, and locally banded, chlorite-ankerite rock.

| Small-scale asymmetric folds in the vicinity of the vein and the

well developed foliation suggests the vein may be structurally

l related to a northwesterly trending fault shown to occur just

west of the stripped area. Grab samples collected from the

l pyritic vein rock has yielded assay values up to 1500 ppb gold,

M while samples of pyrite-rich wall rock generally run in the low

100's of ppb gold.

l The stripping done on claim 798202 (Trench 19) reveals a

very different style of mineralization, one which consists of a

l series of northerly trending, westerly dipping, quartz-filled

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fissures within a massive, medium-grained dioritic rock. Between

5 and 10 veins, l to 10 cm in thickness, occur across a distance

of about 15 meters. Trace amounts of pyrite and galena are

present in the veins which have iron carbonate alteration halos a

few centimeters wide. This system of veins has been located 200

meters to the north and an equal distance to the south. At the

northern end of their known extent the veins are exposed in a

number of old blasted pits and trenches. Grab samples recently

taken of the blasted rock which contain a few percent pyrite and

galena have assayed as high as 0.45 ounces gold per ton.

CONCLUSIONS

1. A major, westerly trending zone of high strain deformation has been identified in the central portions of claims 932075, 901334 and 932074 in the southeastern corner of Reeves Township. In places this zone is at least 200 meters wide and is characterized by a highly foliated chlorite-ankerite schist, right-handed drag folding of the schist, and the presence of boudinaged ankerite-quartz veins.

2. Pervasive hydrothermal alteration has affected the mafic volcanic rock within the shear zone, primarily in the form of iron carbonatization.

3. Within the broad zone of deformed mafic volcanic rock there are a number of westerly striking horizons along which small pods of massive pyrite and, more commonly, zones of laminated chlorite-pyrite rock have been identified. These zones of sulfide mineralization are the sources of strong, linear chargeability anomalies, and are believed to be narrow, structurally disrupted sulfide-facies iron formations.


- 14 -

4. Close to 250 rock channel samples were collected from the stripped areas in southeastern Reeves Township. Assays show that strongly carbonatized volcanic rock is generally not enriched in gold; typical gold contents being 5 to 15 ppb gold. Ankerite-quartz vein rock is only marginally enriched in gold, with assay values in the order of 50 ppb gold being most common. Samples from pyrite-rich rock contain geochemically anomalous amounts of gold, but rarely greater than 250 ppb gold.

5. In the northwest corner of claim 932074 sheared mafic volcanic rock has been folded into a west-verging, northeast-plunging structure. The deformation and alteration seen here appears to be separate from the major deformation zone passing 200 meters to the south. A narrow quartz vein oriented orthogonal to the plunge of the fold contains visible gold.

6. Trenching done in Kenogaming and Penhorwood Townships did not uncover zones of deformation and hydrothermal alteration comparable to those identified in south eastern Reeves Township.

7. Economic concentrations of gold occur in fissure-filled quartz veins hosted by dioritic rock southwest of Sewell Lake. However, stripping done on the trend of the veins shows them to be too widely spaced for an actual mineralized zone to be well defined.

RECOMMENDATIONS

1. The newly discovered gold-bearing quartz vein on claim 932074 should be the focus of future exploration work. Additional stripping/trenching could be done in the immediate area of the vein. A number of short drill holes collared in a crescent pattern around the fold, i.e. drilled at 50"NE, 50 e N and 50 0 E would test if a system of parallel veins transects the plunge of the fold in the sheared and carbonatized volcanic rock.

2. The intensity of deformation and alteration and the size of the shear zone identified in the central areas of claims 932075, 901334 and 932074 make it highly prospective for gold, even though the recent sampling program failed to identify economic mineralization. A number of widely spaced, relatively long holes are recommended to be drilled northwards through and


- 15 -

beyond the defined main shear zone. These holes will test for vein systems which might exist north of the exposed areas lying beneath a north-northeasterly flowing creek. The creek may be reflecting an unidentified structure, one which may be related to the folding and shearing seen in the exposure where the gold-bearing vein occurs.

A series of relatively short drill holes oriented due east are recommended to test the northerly trending system of quartz fissure veins along its 400 meter known strike length on claim 798202. If these veins pass from diorite rock into foliated volcanic rock they may increase in size and/or be concentrated into a more confined zone.

Respectfully submitted

Ron Burk, M.Sc.Eng.

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- 16 -

REFERENCES

BURK, R.1987 Geological Report on the Reeves Joint Venture

Property of Goldrock Resources Inc. and Glen Auden Resources Limited, Reeves, Sewell, Penhorwood and Kenogaming Townships, Porcupine Mining Division.

BURK, R.1988A Report on Magnetometer Survey on the Reeves

Joint Venture Property o f Glen Auden Resources Ltd. and Goldrock Resources Inc.

BURK, R.1988B Preliminary Report on the 1988 Trenching

Program on the Reeves Joint Venture Property of Glen Auden Resources Ltd. and Goldrock Resources Inc.

ll ^ CERTIFICATION

lI, Ron Burk of 29 Wardencourt Drive, Agincourt, Ontario certify

8 that;

1. I am a graduate of the University of Toronto

I with a Bachelor of Applied Science in Geo-Engineering

2. I am a graduate of Queen's University with a B Master of Science, Geological Engineering.

3. I have been practising my profession in B Canada for 5 years.

4. I have no economic interests in the property m covered by this report.

m Dated this October 4, 1988 B TIMMINS, Ontario

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Ron Burk

APPENDIX A

11 ^Sft

' Î^^^Hfl^V^1 p^^""^

iSAMPLE(S) FROM Robert B

1 P.O.BOX

TSL LABORATORIESDIV. BUROENER TECHNICAL ENTERPRISES LIMITED

2031 RIVERSIDE DRIVE, UNIT 2TIMMINS, ONTARIO

P4N 7C3TEL: (705) 268-4441 FAX: (705)268-4420

CERTIFICATE OF ANALYSIS

^Middleton Exploration REpQRT N Q

" 136 Cedar St. South W2055Timmins/

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Page 2 of 3

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TSL LABORATORIESDIV. BURGENER TECHNICAL ENTERPRISES LIMITED


P4N 7C3TEL:(705) 268-4441 FAX: (705)268-4420


SAMPLE(S) FROM Robert s. Middleton Exploration P.O.BOX 1637 136 Cedar St. South Timmins*Ontario P4N 7W8

SAMPLE(S) Orock

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Aug 21/88

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SIGNEDCTA

For enquiries on this report, please contact Customer Service Department. Samples, Pulps and Rejects discarded two months from the date of this report.

Page 3 of 3

TSL LABORATORIESDIV. BURQENER TECHNICAL ENTERPRISES LIMITED

2031 RIVERSIDE DRIVE, UNIT 21 W^1

SAMPLE(S) FROM

B

^^T TIMMINS, ONTARIO ^^ P4N 7C3

TEL:(705) 268-4441 FAX: (705) 268-4420


Robert S- Middleton Exploration j ————————— -iP.O.BOX 1637 REPORT No. 136 Cedar St. South W2091TimminSf OntarioP4N 7W8

INVOICE #: 1120SAMPLE(S) OFCHANNEL P.O.: M-223

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Page l of 2

l-' ; -~1 ^^Hflfci TSL LABORATORIES| jftn^f^^^^B^^m O IV. BUROENER TECHNICAL ENTERPRISES LIMITED

^^^^^^^^H|^^r 2031 RIVERSIDE DRIVE UNIT 2

1 P^^^"^ T IMMINS ' OJJNA™^ TEL:(705) 268-4441 FAX: (705) 268-4420

| CERTIFICATE OF ANALYSIS

SAMPLE(S) FRONbrihor f- Q Mi c\A~\ o hnn Rynl or Ai-i rm i ———————M i\uucLu o- rixuuj. CL.UII CMAJJ± UL a L. j. wu DCDOC 1 P.O.Box 1637 HtPUI"— 136 Cedar St. South W2091

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P.O.BOX 16^7 REPOP1 136 Cedar St. South W2070 m Timmins* Ontario

P4N 7W8 , , , r..

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CTA

DIV. BURGENER TECHNICAL ENTERPRISES LIMITED


PAN 7C3TEL:(705) 268-4441 FAX: (705) 268-4420

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. Middleton Exploration i ————————— i1637 E-*y*w- "w REPORT No.

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Ontario

INVOICE #: 1104P.O.: M-223

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Page l of l

TSL LABORATORIESDIV. lUanENEH TICHNIKAl ENTiRPAIfiy* l IMITIO

2031 RIVERSIDE DRIVE, UNIT 2 TIMMINS, ONTARIO1 ^

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enquiries on (his report, please contact Customer Setvice Department, pies. Pulps arid Rejects discarded (wo months from the date of this report.

TSL LABORATORIESDIV. BOBGENIH TECHNICAL ENTEMPRIfiCfe LIMIT* O

2031 RIVERSIDE DRIVE, UNl l 'i TIMMINS, ONTARIO

T E l.!(70fi) 268-44 41 FAX: (705)2684420


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Page l of L

TSL LABORATORIESOIV. BUROENEH TECHNICAL ENTERPRISES LIMITED

2031 RIVERSIDE DRIVE, UNIT 21 n1

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on this report, please contact Customer Service Department.Samples, Pulps and Rejects discarded two months from the date of this report.

Page l of


2031 RIVERSIDE DRIVE. UNIT 2TIMMINS, ONTARIO

P4N 7C3TEL:(705) 268-4441 FAX: (705) 268-4420

1 1 11


SAMPI F(S) FROM Robert S . Middleton ExplorationP.O.BOX 1637 REPORT No. 136 Cedar St. South W2047 Timmins^ OntarioP4N 7W8 ' —————————— '

INVOICE #: 1077 SAMPLE(S) OFGRAB SAMPLES P.O.: M-223

RON BURK

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Aug 17/88

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Page l of 6

*

TSL LABORATORIESDIV. BURQENER TECHNICAL ENTERPRISES LIMITED

l W^1

SAMPLE(S) FROM

^^^r T IMMINS. ONTARIO ^^^ P4N 7C3

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Robert S. Middleton Exploration i — RFPOBT M^ —— l P.O.BOX 1637 REPORT No.136 Cedar St. South W2047Timmins/ OntarioP4N 7W8

INVOICE #: 1077SAMPLE(S) OrV""DAn GAMOT i?c? n ** ** ** ~. \3t\t\o oArl.rlj.CiO P.O. * M~223

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SAMPLE(S) FROMRobert S. Middleton Exploration l ———— P.O.Box 1637 REPOF136 Cedar St. South W2047Timmins/ OntarioP4N 7W8

INVOICE t: 1077b M LE(S) 0GRAB SAMPLES P.O.: M-223

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For enquiries on this report, please contact Customer Service Department, Samples, Pulps and Rejects discarded two months from the date of this report.

Page 3 of 6



P4N 7C3TEL:(705) 268-4441 FAX: (705) 268-4420

1 1 11

SAMPLE(S) FROIVftObert S . P.O.Box 16 136 Cedar Timmins/ On P4N 7W8

SAMPLE(S) HSRAB SAMPLES

RON BURK


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TSL LABORATORIESDIV. BURGENER TECHNICAL E NTERPRISES LIMITED


P4N 7C3TEL:(705) 268-4441 FAX: (705)268-4420


SAMPLE(S) FROM Robert S. Middleton Exploration P. O.Boxl637 136 Cedar St. South Timmins/ Ontario P4N 7W8

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P4N 7C3TEL:(705) 268-4441 FAX: (705)268-4420


SAMPLE(S) FROM Robert S. Middleton Exploration P.O.Box 1637 136 Cedar St. South Timminsf Ontario P4N 7W8

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Page 6 of 6

Ministry ofNorthern Development

•and MinesOntario

Report of Work(Geophysical, Geological, Geochemical and Expenditures)

42ASI4NW8553 Z . 1 17 12 KENOGAMING 900

^^^ Wope f tClaim Holder(i)

f R.C . Poêf Stru? p/nq )i)

Township or Area

Prospector's Licence No.

Address

c ?b P.O.&OX.Survey Company

Name *nd Address of Author (of Geo-Technical report!

K-fevult i P o

Date of Survey (from A to) {Total Miles of line Cut

4- OuJaraoCredits Requested per Each Claim in Columns at right Mining Claims Traversed (List in numerical sequence)Special Provisions

For first survey:

Enter 40 days. (Thisincludes line cutting) .Jvfcgnupmaier

For each additional survey: using the same grid:

Enter 20 days (for efecfilt

Geophysical

- Electromagnetic

Geological

MINING lAMfl&nSECTION

Airborne Credits

Note: Special provisionscredits do not apply to Airborne Surveys.

Electromagnetic

Magnetometer

Radiometric

Expenditures (excludes power stripping)Type of Work Performed

PerfdrmecTon Claim(s)

Calculation of Expenditure Days Credits

Total Expenditures

Toial number of mining claims covered by this report of work.Instructions

Total Days Credits may be apportioned at the claim holder's choice. Enter number of days credits per claim selected In columns at right.

For Office Use OnlyTotal Days Cr. Date Recorded Recorded

Certification Vefifying Repora of Workl hereby certify that l have a personal and intimate knowledge of the facts set fbr-Uyn the Report of Work annexed hereto, having perf or witnessed same during and/or after its completion and the annexed report is true.

Name and Postal Address of Person Certifying

Minjstry of Report of Workhern Development and Mines _____ (Geophysical, GeologicaTOnlario

Type of Survey(s)

and Expe^jdityjas) . l < Mining Act AUC-. l l

Instructions: Please type or print. If number of mining claims traversed exceeds space on this form, attach a list. (Mote^ Only days credits calculated in the "Expenditures" section may be entered in the "Expend. Days Cr." columns.

Do not use shaded areas below.Township or Area

Claim Holder!

GLe.iv AudetA...,----Prospector's LicenceT- iqisAddress

P.O. focKib3?TiVv\mtnsSurvey Company

me and Address of Author (of Geo'technical report)

Date of Survey (from A to)

Day

Total Miles o' line Cut

. fi .s-HEs . fru r7. 0- 6ox fbS^ "Timmins OiAjtcun'pCredits Requested per Each Claim in Columns at right Mining Claims Traversed (List in numerical sequence)Special Provisions

For first survey:- ElectromagneticEnter 40 days. (This

includes line cutting) - Magnetometer

For each additional survey: using the same grid:

Enter 20 days (for each)

Man Days

Complete reverse side

Geophysical

,, - Electromagnetic(J - Magnetometer

Note: Special ErpiQ iofjs J-j credits doTiot apply

Magnetornetcf

TnStT/omM r i c

lo Airborne Surveys

MINING LANDSExpenditures (excludes power stripping) S

number of mining Claims covered by this report Of work.

For Office Use OnlyTotal Days Cr. Recorded

Recrded Hold/r or Agonti(Signature)

ftification Ve/fying Repqfjôf Work Sl hereby certify lhat l have a personal and intimate knowledge o( the facts jet forth in (he Report of Work annexed hereto, having performed the work or witnessed same during and/or after its completion and the annexed report is true.am* and Potial Ad ci r DM of Person Certifying

SCHEDULE BAMMENDMENT FOR REPORT OF WORK

AUGUST 11, 1988

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0

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CO a

REFERENCES

AREAS WITHDRAWN FROM DISPOSITION

M.R.O.-MINING RIGHTS ONLYS.R.O. - SURFACE RIGHTS ONLYM.+ S. - MINING AND SURFACE RIGHTS

OMCription Q rdmr No. DIM Dispnition Fit*

Ste 43/70 W3C'T7 H/3/77 S R. O i5i?*B

5EC.4J/TO W. l 9/7 B 10/4/76 S H. O ****0 l 8 854 3

SEC 43/70 W 1 0/78 14/11/78 SRO I35'48

DUMP ATTENUATION ZONE

SEC 36/80 W.46/8S 14/8/83 H * S

Nor oovn for troting AWAITING INSPECTION 71/66

"FILED ONLY- D-ze/86

NOT OPEN FOB STAKING- BON* rt DE APP L iCATION UNDER

PUBLIC LANDS ACT PENDING 2I/OI/87

MELROSE TWP FREY TWP

CRAvl

M T. C

M T. C

M-T C

M T C.

M.T.C

SAND AND GRAVE L

1*i T O? r

PIT 3H-I FILE '3ST4B

PIT 1576

PIT 3H-2 FI l. E 184702

PIT 1243

40J '074063. Of 40*4"" """ ~"

7 t N i ' ) I1 1074^69 J (07406* ^7*067 j O7*O66^3-|p~r .'""-!."- ", *174071. LroJ*?. jO**O

^"S^ **

-tk- --V

997tffcy*9*Bf i f5n . T |4*iaaa l*****il l " "-™-— w - r j j i i - *-nw| . mmfurv* f i v VWfV * ' M y tt**1———— ,^-. — —,—— -.^. —— —u.. — ^ , — .—E.I.—— ———— ——— --.jMLr-ft-p ;, p ' p i" | p "*i * o!;; p/ IP T p- iP 9JTS /i P --. '. : '- J ——WS

66121*

7 w 2*.26efn iG.JSchi

PHARAND TWR

KENOAMING TWP42A04NW8553 E.11712 KENOGAMING 210

LEGENDHIGHWAY AND ROUTE tec OTHER ROADS TRAILS SURVEYED LINES:

TOWNSHIPS, BASE LIKttS. ETC.LOTS, MINING CLAIMS f^RCELS, ETC

UNSURVEYED LINES.LOT LINESPARCEL BOUNDARYMINING CLAIMS ETC

RAILWAY AND RIGHTO^ WAY UTILITY LINES NON-PERENNIAL STREAM FLOODING OR FLOODIKiS RIGHTS SUBDIVISION OR COMPCSTE PLAN RESERVATIONS ORIGINAL SHORELINE MARSH OR MUSKEG MINES TRAVERSE MONUMENT

DISPOSITION OF CROWN LANDS

TYPE OF DOCUMENT SYMBOLPATENT, SURFACE Bt MlWJfigG RIGHTS

" , SURFACE RIGHfTSDNLY,...," .MINING RIGHTSONLY — . ..,

LEASE, SURFACE 8t M IWUIWG RIGHTS.." , SURFACE RIGHTS OWLY. __ .." . MINING RIGHTSOMLY.........

LICENCE OF OCCUPATlGWk __ ...™.. ORDER-IN-COUNCIL ______ RESERVATION __________ ,......CANCELLED __________ ,......SAND ft GRAVEL . ________ .... .

e e

—. B ™. B—. T—. OC

NOTE: MINING RIGHTS IF* ^*WCELS PATENTED PRIOR TO MAY C. 1913, VESTED IM OmtSINAt PATENTEE BY THE PUBLIC LANDS ACT. R.S-Q TBTO. CHAP 300. SEC. 63, SUBSEC 1.

SCALE: 1 I NCH = 40 CHAINS

FEETo 1000 2000 400O 6OOO aooo

O 200 METRES

20OO[3 K M)

TOWNSHIP

SEWELLM.N.R. ADMINISTRATIVE D ISTRICT

TIMMINSMINING DIVISION

PORCUPINELAND T ITLES/ REGISTRY DIV

SUDBURYISION

f LandManagement

Resources BranchOntario

DiliMARCHJ985

G-3247

MUS

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967293 l 367290997136 997140 ' 997163 n 997i63987292 \967291 '

-' -- -J---L-.^^, l997134 C 997133

93526 S 9472W

997f30 997129724554 l 947090 ;

901329 90(332 ' 901336

997122 l 937123 l 997R4

---f-- ——t901327 f 901333 l 901335929610 i 929611 l l 997114 9971* . 997t|2 '997111 '9971(0 997109

929606 9296071 92960ft 929609 929612997101 97102 (997103

REEVES TWP.PENHORWOOD TW i l 901345 f\ 944917 ! 944906

901344 .944897 i 94489044889 [944662 933343 .'933562 '933565,933570 .93357? 878419 893527

944S9I j 944688 | 944863933546 (933561 l 933566,9333*9 ;933573 ^933376 1^3528

901342 944913 : S449D8 i 9449^)3 , 944895 A MAM .l ) ' 9*4892 9448841 933559 i l 968364 , !l '967264,967265 967270 ! 987271

966367

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901341 , 9449,4 944909 l 94^902 i 9 44894 j 94483 944886 1944865 987259 (987256X

^0040 -944913 1-449.0 . .44.0, 1^. ^7251 947,48 987258 .987257947105 i 947102 901359 ' 901354i l 967247

949105 ! 549106 949095 949089 ,'S49094947101 l 901360 l 9DI353 9449r j 94491 944900 ' 944898

947109; 901352,, '901330

^ nncnl9/9062(949063949064 , 949065

949IW 1949100 949099' &9097

94918 j 949U3 l 949^2 ^49090'

949f23 ; 9 49f20

949121 949116, 949U5 l 949110

1 inch = '\/2 m ilet/2 l l I/2

REVISIONS ROBERT S. MIDDLETON EXPLORATION SERVICES INC

GOLDROCK RESOURCES INC. fi GLEN AUDEN R ESOURCES LTD.

REEVES JOINT VENTURE PROPERTY CLAIM MAP

Date: Oct. 87 Scale: t:325ooDrawn: a.S.B

9971

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NH

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D

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MP

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ch

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w

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num

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rite

lens

es

span

gly

anke

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, ch

lo-t

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, nte

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te

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py

rite

lens

esan

kerit

e-ch

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e sc

hist

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n an

kent

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h la

yers

se

para

ted

by

chlo

rite

lam

inae

ho

stin

g sm

all

lens

es

of

smok

ey

quar

tz

inse

t

anke

rite-q

uart

z-

chlo

rite

pod

gass

anou

s O

lccK

ch

lorite

sc

hist

w

ith 20X

pyr

ite

Sca

le

! :2C

C

chlo

rite

sc

his

t 1 0

70

pyr

ite

and

y narr

ow

quart

z

SA

MP

LES

a.2

zone

of

qu

artz

"st

ringers

an

d pyr

itel

47

quart

z

stringers

an

d pyr

ite

y.

quart

z-anke

rite

62

vein

quar

tz

strin

gers

an

d py

rite

zone

of

qu

artz

"1 st

ringe

rs

and

pyrit

e

boud

inag

e d

a n k

e r. l

e

05

pyrit

e ch

lorit

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e sc

hist

dior

ite

dike

s

\

TRE

NC

H l

anke

rite-

quar

tz

pod

see

inse

t l.

.-e

..*

quar

tz

s;.- ,

--ge

rs

and

pyrit

e

quart

z ve

ins

chlo

ritoi

d po

rphy

rob

SA

MP

LES

SA

MP

LES

A

ufpp

b)0020

002

0022

0023

^• o

*

Au(

ppb)

8246

- 15

mse

;S

ea e

l:

200

250

*:^

200

150

min

or p

yrite

\

-,r^

ir^—

:~

\

TRE

NC

H 2

anke

rite-

quar

li ve

ins

quar

tz \

:r ^

strin

gers

high

ly

folia

ted

chlo

rite

-ank

erite

sc

hist

anke

rite^

quar

tz

vein

sS

\ch

lorit

e\

S

100

SA

MP

LE

0008 -

0009 -

0010

-

0011

-

0012

-

0013

-

0014

-

0015

-

0044 -

8275

--7

6 -

77

-78

-79 -

80

-81

-

82

-83

-

84

-85

-86

-

87

-88

-89

-90

-91

-

92

-93

-94

-95

-96

-

97

-98

-99

-

8300

-0379

-0380

-03

81

-0382

-0383

-

Au(

ppb)

15 20 15 20

10 10 10 5 10 10 10 10 10 10 10 10 1019

50 35 35

25 20

20

20

20

25 20 15 20

30 10 15 10 15

410 80

10 20 15

450

85

, 00

15

"^

-

001

4i O

OI3

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012 l

OO

ID

— - t

l

see

inse

t 2

bush

ro

ad

ox

J hi

ghly

fol

iate

d ch

lorit

e-an

kerit

e sc

hist

-* lo

cally

qua

rtz-

anke

rite

boud

inag

ed v

eins

} tra

ce p

yrite

6299

l l

— c

hlor

ite-a

nker

ite

schi

st

with

ch

lorit

oid

porp

hyro

blas

ts

1-3^

l \-

94

l \

-93

~921

,. /,

..379 1

1-91

.'

dlM

. -''

" I-*

-

-891 38

311~

1-7

9 f

1-7

7

pale

gre

y,

fine

grai

ned,

m

assi

ve

to

wea

kly

folia

ted

inte

rmed

iate

to

m

afic

flo

wS

AM

PLE

S

Au(

ppb)

purp

lish

grey

, m

assi

ve

maf

ic flo

w v

lo

cally

va

riolit

ef

poor

ly

form

ed

vario

lites

are

fla

ttened

2:1

nter

^ned

iate

to

m

afic

, m

assiv

e

flow

Scal

e 1:

200

pyrit

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h zo

ne

med

ium

-gra

ined

, in

term

edia

te

dike

w

ith

mus

covi

te

phenocry

sts

(u

p to

20

mm

)i m

inor

fu

chsitC

i pe

rvas

ive

Fe

carb

onat

e altera

tion

and

/0py

rite

'pyr

ife-r

ich,

high

ly fo

liate

d

chlo

rite

schi

stf

sulfid

e

is

lam

inat

edm

ediu

m

grey

, fine-g

rain

ed

chlo

rite,

±ser

icite

, *

Fe carb

onate

; m

inor

p'y

-anke

rite

altera

tion

and

folia

tion

inte

nsity

in

crea

ses

tow

ard

s

dike

oxid

ized

, pyrite

-ric

h,

chlo

rite

anke

rite

schi

st;

adja

cent

rock

is

anke

rific

an

d str

ongly

fo

liate

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inse

t 3.

wea

kly

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riolit

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ic

flow

inte

rmed

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di

ke

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liate

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schi

st

stro

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ox

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ed,

pyrit

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h,

chlo

rite-

anke

rite

schi

st

SAMPLES

0073

-- ^4 -

- 75 -

- 76 -

- 77 -

- 78 -

- 79 -

- 80 -

- 81

-

Au(ppb)

2030

0082

- 10,

40

83

- 1C

5 - 84

520

r-

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30 i 0 4040

t /KJ ,

,1'*i-

f

^C.

'Or

''li

1 L,

see

inse

t 3.

\

flattened

pillo

w

chlo

ritic

rims,

anke

ritic

co

res

\ }

^~

,'-^

il .o'*

l

weakl

y ca

rbbo

natiz

ed

~ 62

~^t~

, ^

-83

TR

EN

CH

8

fine-g

rain

ed,

mas

sive

, va

riolit

ic

and

loca

lly

- pi

llow

ed

mafic

flo

w(

J -7

0

J-69

pillo

ws

poss

ibly

fa

ce

sout

h s

lack

of

ox

ide

wea

ther

ing

v su

gges

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Fe

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ate

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67

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l -

66^

92

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rite

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rite

sc

hist

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ith

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boud

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ed quart

z

vein

TRE

NC

H 7

' lN,_

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litic

, po

orly

fo

rmed

pillo

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wea

kly

stra

ined

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ows,

to

ps

sout

h ?

l-3cm

w

ide

boud

inag

ed

quar

tz

vein

gr

ey,

fine-

grai

ned,

mass

iv e

m

afic

w

eak

Fe

carb

onat

e altera

tion,

min

or

pyrit

e su

bhed

ral

x'Is

~~~

na

rrow

sh

ear

mod

erat

e Fe

ca

rbon

ate

altera

tion

tight

ly

fold

ed

chlo

rite-

anke

rite

schi

st (

0306

)w

hite

qu

artz

ve

in

4cm

w

ide

at

125/

45

s w

ith

trac

e py

rite

(0307,0

308)

shea

red

and

anke

rittiz

ed

maf

ic

flow

ro

ck

min

or

fold

s pl

unge

50

0 NE

SAMPLES

0302

- -303

-304

-305

-306

-307

-308

-309

- 310-

31!

-312

-313

-

0328

ch

iorit

e-

anke

rite

0329

sc

hist

wea

kly

folia

ted,

fr

actu

red

maf

ic

volc

anic

! w

eakl

y ca

rbon

atiz

ed

SA

MP

LES

A

u(pp

b)03

14 315

316

317

318

319

320

321

322

323

40

30

- 4680

- 38

890 35

75

35

25

35

i 5

whi

te

quar

tz

vein

3-I

Ocm

th

ick

fillin

g fr

act

ure

at

125/4

0

SW

, tr

ace

pyrit

etig

htly

fo

lded

S,

fo

liatio

n in

chlo

rite

-anke

rite

sc

hist

; ax

ial

surf

aces

at

85

g

shea

r su

rfac

e at

S

O"

SA

MP

LES

0324

-32

5 -

326

-32

7 -

328

-32

9 -

330

-

Au(

ppb)

i ^

. ^*

. J

l O

Sca

le

i 200

4.

-275

m

25O

m

see

inse

t 4.

high

ly

folia

ted,

fo

lded

ch

lorit

e-an

kerit

e sc

hist

w

ith

shal

low

di

ppin

g qu

artz

' l

vein

,- vi

sibl

e go

ld

;

TRE

NC

H

4

folia

tion

inte

nsity

an

d am

ount

of

car

bona

te

alte

ratio

n de

crea

ses

tow

ards

N

and

S en

ds

of

expo

sure

- 22

5m

TRE

NC

H 6

-4

iow

gro

und

smok

ey

quar

tzve

ins

high

ly

folia

ted

chlo

rite

-anke

rite

sc

hist

bo

udin

aged

qu

artz

st

ringe

rs

•sam

pled

!9

87j

see

Gar

ner,

19

87

SA

MP

LE

S0085

--8

6

-87

-88

-89

-90

-91

-

92

-93

-

94

-95

-

96

-97

-98

-

99

-0100

-

Au(

ppb)

10 15 15 15 10 15 10 10 10 5 15 10 (5 10 1 5 30

——

——

— —

i

Au

(ppb

anke

rite

-quart

z po

d (b

oudi

n)

SAMPLES

0393

394

395

396

397

398

399

400

narr

ow

anke

rite

bard

s pa

ralle

l ea

rly

folia

tion,

py

rite

cube

s

fold

ed

quar

tz

vein

35 25 30

50

170

40

100

10qu

artz

st

ringe

rs

perv

asiv

ely

anke

ritiz

ed

maf

ic tu

ff

or

brec

cia

chlo

rite

clot

s-^

s-

onia

l pl

anar

^T

^

^

cteo

voga

ol

050*

quar

lz

vein

di

ps

shal

low

W

sulfi

de

pod

quar

tz jj

ash

es

at

120'

Sca

le

l: 200

inse

t 6.

. 20

Om

o 17

5m

- IS

Om

low

gro

und,

ce

dar

bush

//

smal

l pyr

ite p

ods/

'

high

ly f

olia

ted

chlo

rite-

anke

rite

schi

stbo

udin

aged

, sm

okey

gr

ey

quar

tz-a

nker

ite

vein

ssa

mpl

e -9

1 fr

om

1.5m

w

ide

zone

of

qu

artz

ve

ins

loca

lly

cont

aini

ng

coar

se-g

rain

ed

pyrit

e^~

" da

rk

grey

ch

lorit

e sc

hist

w

ith

hum

erou

s qu

artz

le

nses

an

d po

ds^

trac

e py

rite

-No.

8283

J/om

30

cm

wid

e qu

artz

po

d

wel

l fo

liate

d ch

lorit

e-an

kerit

e ±

seric

ite s

chis

t

wes

t-dip

ping

, bl

ack

quar

tz

vein

y/

prev

ious

ly s

tripp

ed a

rea

,/

V

380

N— 3

81

382

80

-76

1827

5

^

\\

'dia

mon

d1 c

leav

age

at 80/9

0,

110/

90

—

mod

erat

ely

folia

ted,

w

eak

to

mod

erat

e an

kerit

e al

tera

tion

decr

easi

ng

folia

tion,

al

tera

tion

loca

lly

vagu

e,

stre

tche

d pi

llow

s

mod

erat

ely

folia

ted

chlo

rite-

t-an

kerit

± se

ricite

^ sc

hist

(m

afic

flo

w)

V \

\ \

\

sam

pled

19

87,

see

Gar

ner,

1987

\su

lfide

fa

cies

iro

n fo

rmat

ion

wea

kly

folia

ted,

car

bona

tlzeg

i' m

afic

flo

w

^ —

—--

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5O c

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hist

w

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shal

low

di

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visi

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l fo

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tens

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and

amou

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of c

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au

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NESAMPLES

Aulppb^

0324

-325

- J

326

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327

-328

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329

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330

- 5

med

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-gra

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, in

term

edia

te

dike

w

ith

mus

covi

te

phen

ocry

sts

(up

to

2Om

m)i

min

or

fuch

site

j pe

rvas

ive

Fe

carb

onat

e a

ltera

tion

an

d i"7

0 p

yrite

pyr

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, hi

ghly

fo

liate

d

chlo

rite

sc

hist

^ su

lfide

is

la

min

ated

m

ediu

m

grey

, fin

e-g

rain

ed

chlo

rite,

±se

rici

te,

* Fe

ca

rbo

na

te;

min

or p

y -

anke

rite

alte

ratio

n

and

folia

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nte

nsi

ty

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ease

s to

ward

s di

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— —

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e in

set

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PL

ES

boud

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nt

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nses

. ac

k ch

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sc

hist

w

ith

'Oy0

p

yrite

an

d o

c a ; i

y na

rrow

qu

artz

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rs

and

pyr

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; 02

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schi

st-t

hin

anke

rite-

rich

laye

rs

sepa

rate

dby

ch

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e la

min

ae

host

ing

smal

lle

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sm

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qu

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blac

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sc

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w

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28

chlo

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kerit

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29

schi

stbo

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aged

an

Ker

quar

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san

kent

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lorit

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dS

cale

!:2

0C

oxid

ized

, pyn

te-r

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chlo

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- an

kerit

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hist

; ad

jace

nt

rock

is

anke

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an

d st

rong

ly

folia

ted

Sca

le

i 2

00

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a

TRE

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H

4

SA

MP

LES

A

u(pp

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0020

- 5

00

20

02

2

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02

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-py

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chlo

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stdi

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di

ke

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pod

see

inse

t

—

high

ly

folia

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ch

lorite

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kerite

sc

hist

w

ith

narr

ow,

boud

inag

ed

quar

tz

vein

TRE

NC

H l

flatte

ned

pillo

ws;

ch

lorit

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rims,

an

kerit

ic

core

sse

e in

set

3.w

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EN

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7w

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liate

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flow

inte

rmed

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di

ke

wel

l fo

liate

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poor

ly

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ed

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pillo

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poss

ibly

fa

ce

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of

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tle

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stro

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chlo

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NC

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wea

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ps

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ide

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tz

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35 25 30 50 !70

40 100 10

narr

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folia

tion,

3

07o

pyrit

e cu

bes

SA

MP

LES

A

u(pp

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sh

road

grey

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e-gr

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ve

maf

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wea

k Fe

ca

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ate

alte

ratio

n,

min

or

pynt

e su

bhed

ral

x'ls

na

rrow

sh

ear

TRE

NC

H 2

anke

rite-

quar

tz

pod

(bou

din)

modera

te

Fe

carb

onate

a

ltera

tion

quar

tz

strin

gers

perv

asiv

ely

anke

ritiz

ed

maf

ic tu

ff

or

brec

cia

dike

; ch

lorit

e cl

ots

TRE

NC

Hfo

lded

qu

artz

ve

inqu

ariz

ve

inhi

ghly

fol

iate

d ch

lorit

e-an

kerit

e sc

hist

dips

sh

allo

w

Wsu

lfide

po

d

quar

tz

gash

es

at

120

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qu

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ve

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ank*

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ic,

trac

t py

rile

see

inse

t 2

Sca

le

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0

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ted

chlo

rite-

anke

rite

schi

sthi

ghly

fo

liate

d ch

lorit

e-an

kerit

e sc

hist

bo

udin

aged

qu

artz

st

ringe

rs

•sam

pled

19

87.

see

Gar

ner.

1987

loca

lly

quar

tz-a

nker

ite b

oudi

nage

d ve

inSj

tra

ce p

yrite

smok

ey

quar

tzve

ins

low

gro

und,

ceda

r bu

sh

smal

l pyr

ite p

ods/

- ch

lorit

e-an

kerit

e sc

hist

w

ith

chlo

ritoi

d po

rphy

robl

asts

wes

t-dip

ping

, bl

ack

prev

ious

ly s

tripp

ed a

rea

quar

tz

vein

wea

kly

folia

ted,

car

bona

tlzei

j m

afic

flo

w

old

over

grow

n tr

ench

50 c

m

tîa

ck q

uartz

vei

n

high

ly

folia

ted

chlo

rite-

anke

rite

schi

stbo

udin

aged

, sm

okey

gr

ey

quar

tz-a

nker

ite

vein

ssa

mpl

e -9

1 fr

om

1.5m

w

ide

zone

of

qu

artz

ve

ins

loca

lly

cont

aini

ng

coar

se-g

rain

ed

pyrit

e

over

grow

n tre

nch

dark

gr

ey

chlo

rite

schi

st

with

nu

mer

ous

quar

tz

lens

es

and

pods

* tr

ace

pyrit

e -N

o.

82

83

Ir

om

30cm

w

ide

quar

tz

pod

TRE

NC

H

5w

ell

folia

ted

chlo

rite

-an

kerite

±

serici

te

schi

st

chlo

rite-

anke

rite

sch

ist

\ al

tere

d m

afic

flo

w

inte

rmed

iate

tu

ff

or

brec

cia

dike

sam

pled

19

87,

see

Gar

ner,

19

87m

odera

tely

fo

liate

d

chlo

r it e

* a

nk e

r it

± se

rici

te

schi

st

(ma

fic

flow

)

'dia

mon

d'

clea

vage

at

80/9

0,

11

0/9

0

mod

erat

ely

folia

ted,

wea

k to

m

oder

ate

anke

rite

alte

ratio

n

\ se

e In

set

o.

sulfi

de

faci

es

iron

form

atio

n

sulfi

de-r

ich

cher

ty

laye

rsde

crea

sing

fo

liatio

n,

alte

ratio

n lo

cally

va

gue,

st

retc

hed

pillo

ws

see

inse

t 6

old

over

grow

n tre

nch

SA

MP

LES

A

u(pp

b)

TRE

NC

H 9

old

over

grow

n tr

ench

esin

term

edia

te

tuff

or

brec

cia

dike

s ch

lorit

e cl

asts

in

med

. gr

aine

d fe

ldsp

athi

c gr

ound

mas

s

\ m

oder

atel

y fo

liate

d,ru

bble

fr

om

trenc

hin

clud

es

pyrit

e-be

arin

g sm

okey

qu

artz

ve

in

rock

carb

on

ate

d,

i ol

d ov

ergr

own

tren

ches

\ \

(circ

a.

1942

) \

x \

x /x

\ m

afic

vo

lcan

ic

stoc

kwor

k of

sm

okey

qu

artz

blea

ched

vo

le,

pyle

nses

of

py

rite

in se

riciti

c an

d lo

cally

ch

erty

ro

ck;

sulfi

de-f

acie

s iro

n fo

rmat

ion

?S

cale

1:2

00

No.

i

- 9

44

89

92

- 90

1334

3 -

932074

4 -

94

48

62

old

blas

ted

pit

in m

oder

atel

y fo

liate

d rn

afi

volc

anic

ro

cKi

mod

erat

e Fe

ca

rbon

ati

grav

el

road

No

. 3

2.

11

71

2

oo w

2 *

50 W

alte

ratio

n,

quar

tz

vein

ing

and

sulfi

des

2 -t-

00 w

42

A0

4N

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3 S

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I2

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NO

GA

MIN

G

25

0

REV

ISIO

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for

RO

BER

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MID

DLE

TON

EX

PLO

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N S

ERVI

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IN

C.

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N A

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EN R

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UR

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LTD

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itle

SE R

eeve

s To

wns

hip

DE

TAIL

OF

STR

IPP

ED

A

RE

AS Map

2Da

te:

Aug.

88D

raw

n: R

B /S

PSc

ale:

l:

500

App

rove

d:N

T. S.

:Fi

le:

M-22

3

Documents

PRELIMINARY RPT ON OC STRIPPING