on the property of...summary during the period december, 19b3, to mid-april, 198*4, pominex ltd....

42A18SW0285 63.4363 MACKLEM 010

GOLD DISCOVERY

on the property of

PQMINEX LTD.

Macklem Township, Ontario

Timmins, Ontario,

May 22, 19BU.

R. J. Bradshaw, P. Eng*,' .*'

Geologist.

42AieSWe285 63.4363 MACKLEM 010C

TABLE OF CONTENTS

Page

SUMMARY

INTRODUCTION . . . . . . . . . . . . . . . . . . . . . . . . 1

PROPERTY, LOCATION AND ACCESS . . . . . . . . . . . . . . . 1

PREVIOUS WORK . . . . . . . . . . . . . . . . . . . . . . . 1

DIAMOND DRILL PROGRAMMEGeneral . . . . . . . . . . . . . . . . . . . . . . . . 2Summary of Diamond Drilling . . . . . . . . . . . . . . 5Drilling Programme, Cost and Problems . . . . . , . . . 6

GEOLOGYRegional Geology . . . . . . . . . . . . . . . . . . . 6Local Geology . . . . . . . . . . . . . . . . . . . . . 7

ECONOMIC GEOLOGYGeneral . , . . . . , . . . . . . . . . . . . . . . . . 9Mineralization of Gold Zones in Feldspar Porphyry . . . 11 Structure of Gold Zones in Feldspar Porphyry . . . . . 12Distribution of Gold Zones . . . . . . . . . . . . . . 13

CONCLUSIONS . . . . . . . . . -. . . . . . . . . . . . . . . K*

RECOMMENDATIONS . . . . . . . . . . . . . . . . . . . . . . 16

General GeologyDrill Hole Plan fc GeologyGeology fc Gold ValuesSection 16+60USection 16+30UJ (A)Section 16+30U (B)Section 16+OOWSection

FIGURES 1A123 i*567

CERTIFICATE

REFERENCES

APPENDIX - Diamond Drill Logs

-

Feldspar porphyry t'.-':'| Serpentinite

[ l Volcanics f-'^3 Conglomerate

H^ MetasedimentsFault

Pominex drill hole, 1983-84Drill hole, pre-1983

POMINEX PROPERTY

POMINEX LTD.

General Geology of the 'Macklem Twp. Property Area

ScaleMay

1 : 15,000

1984f**~Y i 7 - 94

Figure 1A

SUMMARY

During the period December, 19B3, to mid-April, 198*4,

Pominex Ltd. drilled H* holes totalling 10980 feet on the Macklem

Township property, 2k miles east of Timmins, Ontario. Twelve

holes were drilled along the west boundary of the property.

Holes 83-1 and B**-? were drilled in the northeast and centre of

the property, respectively.

Of the twelve holes along the west boundary, nine drilled

a gold-bearing felsic feldspar porphyry dyke. A remarkably high

proportion of the 200 foot wide dyke contains uniformly low but

highly anomalous gold values ranging from 0.02 to 0.10 oz. of gold

per ton. The various gold intersections apparently form three or

more discrete zones, including a main central zone interspersed with

high grade concentrations generally associated with visible gold.

These zones appear to conform with the easterly strike of the dyke

and dip near vertically.

There is evidence for considerable length of these gold

zones. An Asarco drill hole 1200 feet west of the Pominex boundary

intersected 3** feet averaging O.OU5 oz. gold per ton which appears

to represent the central zone. The porphyry has been drilled for a

length of 1*00 feet on the Pominex property. Intersections in three

holes average 0.2^5 oz. gold for 210 feet over a true width of 27

feet. The most easterly hole intersected a true width of **9 feet

averaging 0,036 oz. Typical intersections of subsidiary parallel

zones include 0.11**, 0.111, and 0.066 oz. gold per ton over true

li

widths of 16, 26 and 11 feet respectively.

The better gold values and widths appear to occur at or

below the 575 foot level.

Gold is associated with obscure zones of silicification

containing about 1 per cent pyrite and 10 per cent or less quartz

stringers. Higher gold values occur with intense fracturing, parti

cularly obvious within the central main gold zone. Although the

mineralization associated uith the gold is not well defined,

dimensions of gold-bearing rock are impressive. It is expected

that future drilling will provide data for a better understanding

of the gold deposition and enhance this promising discovery.

Further drilling is, therefore, recommended. Up to

30,000 feet of drilling and perhaps more mill be required to evaluate

the gold deposition on the property. In order to facilitate

periodic evaluation of the drilling results, it is proposed that

the programme be undertaken in stages of 10,000 feet. It is esti

mated that each stage mill cost 8260,000. for a total of 8780,000.

if the entire programme is completed.

INTRODUCTION

Gold mineralization was discovered on the Pominex pro

perty in a drill hole completed in January, 198**. This hole uas

part of a programme of 1** holes, nine of uihich encountered gold

mineralization.

The following report is concerned uiith the results of

that drilling and proposals for additional work on the property

to evaluate the gold mineralization.

In conjunction with Company management, the writer

personally supervised and planned the project.

PROPERTY, LOCATION AND ACCESS

The property consists of nine contiguous patented

claims, totalling 369 acres, numbered P2555U to P25562 inclusive.

Situated in the northeast corner of Macklem Township, the

claim group is 36 kilometres east of the City of Timmins.

Highway 101 from Timmins is immediately north of the

property. The Gibson Lake road running south from highway 101,

about one kilometre west of the Pominex property, intersects a

tractor road about 1.5 kilometres south of highway 101. This tractor

road provided access to most of the drilling sites.

PREVIOUS UIORK

In 1981 Asarco, owner of the property immediately west of

Pominex, completed a series of overburden holes in the search for

anomalous gold in the bedrock till. One of these holes, 81-11,

- 2 -

encountered highly anomalous gold in the bedrock talus on the

mutual Asarco-Pominex boundary. Hole B**-2, the Pominex discovery

hole, uias subsequently drilled north, immediately below overburden

hole 81-11.

Prior to the start of the drill programme a magnetic

survey (November, 1983) was completed on the Pominex property which

basically outlined the south dipping ultramafic body striking at

07Q 0 through the northern sector of the claim group.

DIAMOND DRILL PROGRAMME

General

In late 1983, hole 83-1 was drilled in the extreme north

east sector of the property to investigate an area at the nose of

a prominent magnetic anomaly representing ultramafic rock. Shearing

and faulting trending east-northeast was expected to be confined to

the ultramafic rock. The target area uas, therefore, anticipated

to be sheared and faulted perhaps within a more competent rock. In

fact, as indicated by hole 83-1, the sheared ultramafic simply

narrouied substantially within the target area. Intermediate to

mafic volcanics, lacking significant mineralization, enclose the

ultramafic body.

Discovery hole 8*4-2 commenced drilling on the west

boundary of the property, just south of overburden hole 81-11, in

mid-January of 198**. Gold mineralization present in a feldspar

porphyry is associated with zones of fracturing and alteration.

While waiting for assay returns, hole 8**-3 was completed and BU-UA

- 3 -

uas started forming a north-south section along the Asarco-Pominex

boundary.

Holes 84-5 and 6 uere drilled 30 metres east of hole 84-2.

Although the favourable feldspar porphyry host rock uas intersected,

assay results uere less impressive than in hole 84-2.

A review of previous uork indicated that in 19*44, Broulan

Reef had encountered lout gold values over narrow widths within

felsite in a hole drilled from north to south near the centre of

the property. It was assumed that the felsite uas in fact feld

spar porphyry and that the hole had not fully intersected the

porphyry. It was, therefore, decided to investigate this area for

the presence of the gold mineralization in the feldspar porphyry.

In the meantime, holes 84-2, 5 and 6 uere revieued in order to

determine the most favourable locations for additional drilling in

the vicinity of the discovery.

Hole 84-7 over 750 metres (H mile) east of hole 84-2

confirmed the presence of the feldspar porphyry, of similar width,

with scattered low gold values.

The review of previous drilling suggested that more

representative results might be forthcoming by drilling from north

to south. At the same time because such holes uould essentially

be drilling down dip uiithin the feldspar porphyry, the potential of

the host rock uould be evaluated much quicker.

Holes 84-8 and 10 uere, therefore, drilled south in the

same section as 5 and 6, 30 metres (100 feet) east of hole 84-2.

Both holes provided better results than 5 end 6, particularly

8U-B uihich intersected a width of 85 feet (26 metres) assaying

0.328 oz. per ton (uncut).

Similarly, holes B**-9 and 11 mere drilled north to south

30 metres (100 feet) east of the section including holes B**-5, 6,

8 and 10. Comparitively mediocre results in these tuo holes

perhaps is caused by a fault, subsequently indicated by hole 8*4-K+,

Holes 8^-12 and 13 were drilled south on a section 60

metres (200 feet) east of BU-9 and 11. These holes generally con

firmed the presence of significant gold values over substantial

uiidths.

Throughout the drill programme it seemed apparent that

the better gold concentrations occurred at or beloui a depth of

about 175 metres (575 feet). Hole 8**-H* was, therefore, located

in the same section as holes 8^-9 and 11 to intersect the host

rock deeper. Apparently because of a cross fault, hole 8^-1^

remained within the volcanics in the footwall of the feldspar

porphyry.

- 5 -

Summary of Diamond Drilling

.Hole No.

B3-1

Bl*-2

Bl*-3

81. -l* abandoned

Bt*-i*A

8i*-5

Bl*-6

BU-7

BU-8

Bl*-9

Bi*-10

fll*-11

Bl*-12

Bl*-13

8i*-1i* Casing left in hole

Location

Line 1+OOW 1+1*0 South

Line 16+60U 5+20 South

Line 16+60U 3+1.0 South

Line 16+03U 2+53 South

Line 16+30UI 1.+99 South

Line 16+30UI 5+21* South

Line 9+OOUI 3+60 South

Line 16+30U) 3+Qi* South

Line 16+OOUJ 3+00 South

Line 16+30UJ 3+Qi* South

Line 16+OOW 3+00 South

Line 15+t.OW 2+91* South

Line 15+l.OW 2+59 South

Line 16+OOUI 2+60 South

Direction (Ast.)

North

North

North

North

North

North

North

North

South

South

South

South

South

South

South

Total

Dip

50"

50"

50"

50"

55"

50"

50"

50"

61"

61"

50"

50"

61"

61"

61"

rootage metres

Depth(feet)

550

973

808

71.6

71.3

835

700

750

981

691*

577

750

877

996

10980 331*7.6

- 6 -

Drilling Programme^ Cost and Problems

The diamond drilling uias contracted to Norex Drilling

and Bradley Bros., both of Timmins. Norex started the programme

and drilled the first seven holes and holes 9 and 11. Having

completed their contract and experiencing cost overruns they de

cided to leave the project. Bradley Bros, drilled holes 8^-8, 10,

12, 13 and W . Thus, for a period of time, two drills were used

on the property.

Norex drilled 6336 feet at a cost of 819.36 per foot.

Bradley Bros, drilled kBkk feet at a cost of 820.2B per foot.

Overall cost of drilling bias, therefore, S19.75 per foot or 861*.79

per metre.

Only hole 8**-** was lost because of deep overburden. Con

sidering the excessive depth of overburden the drillers, particu

larly Norex, performed very well.

Norex experienced excessive diamond costs because of the

extraordinary hardness of the felsic feldspar porphyry.

GEOLOGY

Regional Geology

The rocks which underlie the Pominex property are strati-

graphically equivalent to the Tisdale Group, an assemblage of

mainly volcanic rocks which to the west host a number of profitable

gold deposits. Similarly to the west the Porcupine-Destor fault is

genetically, if not spatially, associated with these gold deposits.

- 7 -

Apparently confined to an ultramafic body on the Pominex property,

a structure termed the Aquarius fault, striking D700 , eventually

merges to the east with the Porcupine-Destor fault striking about

08Q 0 just north of the Pominex property.

North of the Porcupine-Destor fault and the Pominex pro

perty is a uiide section of clastic sediments.

The Asarco gold mine, 2.6 kilometres to the west of the

Pominex property, recently commenced production.

Local Geology

The geology of the Pominex property, within a regional

setting, is displayed on Figure 1A; and a plan of diamond drilling,

figure 1, shouts the typical stratigraphy.

As indicated by a magnetic survey (November, 1963), the

most striking feature on the Pominex property is an apparently

conformable ultramafic body which strikes easterly and dips south

at about 70". A drill section formed by holes B**-2, 3 and l+A con

firms the ultramafic body and provides additional geological

information.

Hole B**-i*A was abandoned in a fault zone composed of

partially dissolved clay minerals which appears to be generally

conformable to the attitude of the rock assemblage. This fault

zone, which would reach the suboutcrop in the extreme northwest of

the property, is followed to the south by a narrow section of talc

chlorite schist about **5 feet (1** metres) wide. In turn the schist

is followed by a narrow felsic dyke about 30 feet (9 metres) wide,

- B -

intersected in both holes 6^-3 and **A. This dyke, containing

quartz stringers and up to **96 pyrite, but without significant gold

values, appears to be generally conformable to the enclosing

rocks.

To the south the dyke is in contact with a carbonate,

sericite or chlorite, talc rock which is schistose in part and 60

feet (18 metres) wide.

Intersected in both holes 8*4-3 and UA, a mainly carbonate

rock follows to the south. It varies from Ik feet (22 metres) in

hole 8*4-3 to 138 feet C*2 metres) wide in hole BU-t*A. Considerable

irregular quartz veining and minor crystalline pyrite is present

in this rock, particularly in hole 8*4-^. Albite, sericite and

fuchsite mineralization is also present. Significant gold values,

however, are lacking.

The carbonate rock is followed to the south by the above

mentioned magnetic, sheared and schistose ultramafic rock. About

330 feet (100 metres) wide, it is typically blue-black and serpen-

tinized but locally has characteristics of a serpentinized volcanic.

This unit appears to form the loci for the major movement in the

area which, to the west, coincides uith the Aquarius fault.

South of the ultramafic body is a unit about 100 feet (30

metres) wide which includes serpentinized massive and schistose

ultramafic rock and altered mafic volcanics of various types. This

unit forms the footwall of a generally conformable gold-bearing

felsic porphyry dyke.

- 9 -

Drilling by Asarco to the uiest and Dome to the east

(personal communications) indicates that the porphyry strikes at

OSO0 for some distance beyond the property boundaries. About 20Q

feet (60 metres) wide the unit dips near 700 to the south. The

existence of sharp contacts and numerous inclusions of recognizeable

pillow lava, which forms the hanging wall of the porphyry, are

evidence for its intrusive nature.

In general, this light grey to green rock is very hard

and aphanitic with scattered feldspar phenocrysts. The variable

colour appears to be influenced by ground water leaching, variation

of hydrothermal activity, and minor chloritization with intense

fracturing. Mineralization and structures associated with gold

values are described under Economic Geology.

The hanging wall pillow lava is more than 330 feet (110

metres) thick. Minor structures, including amygdaloidal selvages,

are remarkably well preserved in this unit particularly away from

the porphyry contact.

Numerous narrow intermediate to mafic dykes, generally

less than 10 feet (3 metres) wide, cut the above described sequence

of rocks.

ECONOMIC GEOLOGY

General

About 2.6 kilometres to the west of the Pominex discovery,

Asarco has commenced mining in a carbonate rock which contains ir-

- 10 -

regular quartz stringers and veins with free gold. This unit

corresponds uith the carbonate rock intersected in holes BU-3 and

**A north of the ultramafic body. However, significant gold values

were not encountered in the Pominex drilling.

Since discovery of the gold deposit by an overburden

drill hole, Asarco has covered most of their large property at

intervals of (*OQ to BOO metres (K to # mile). A line of four holes

extending westerly from the Pominex boundary for a length of about

1130 metres (about K mile) formed part of the Asarco programme.

Samples of the till from each of these holes returned anomalous

gold. Diamond drill hole 8**-2 by Pominex showed that the gold is

derived from a feldspar porphyry. Similarly, Asarco drilled at **QO

and 800 metre (H and fi mile) intervals from the Pominex boundary

and encountered the feldspar porphyry immediately north of the

anomalous overburden holes. In three holes the best gold value is

0.0*45 oz. per ton over 3** feet at a vertical depth of 530 feet

(160 metres).

Based on a regional study a major north-northwesterly

trending fault is interpreted to be situated at the joint boundary

between Asarco and Pominex. This right-handed fault, displacing

east side units south several hundred feet, may correspond to the

fault depicted on Figure 1. Alternatively, the fault on Figure 1

may be subsidiary to the main structure. Although the main break

crosses the major Porcupine-Destor fault, there is not yet any

definite evidence that it is genetically related to the distribution

of gold values in the feldspar porphyry.

- 11 -

Mineralization of Gold Zones in Feldspar Porphyry

Mineralization associated with gold values is not easily

recognized because of the comparitively minor variations of

alteration and also the substantial widths which may include

several boxes of core. A re-examination of hole B t*-8 which pro

vided the best gold values reveals the following.

A section of **7 feet (U.3 metres) from 650 to 697 feet

contrasts with the immediate wallrock. It is dominantly but ir

regularly silicified and has substantially more quartz stringers,

totalling about 10 per cent, than the adjoining rock. The colour

varies from grey-white from silicification to a darker grey where

chlorite-filled fractures have permeated the silicified zone.

Uithin the zone a slightly increased amount of pyrite as euhedral

grains or smears along fractures probably averages about 1X. Local

rusty weathering of the pyrite from ground water circulation is

notable considering the depth, A chlorite-quartz filled fault near

the centre of the zone may or may not be associated with the gold

values. An affinity for pyrite is indicated by gold replacing

euhedral pyrite in a quartz stringer. This characteristic is also

apparent elsewhere.

Of ten samples, all but one 5 feet wide, seven assayed

from 0.03 to 0.086 oz. per ton, two assayed 0.026 and Q.OK* re

spectively, and one assayed t*.79 oz. over 5 feet.

Both sides of the silicified fracture zone display

effects of hydrothermal activity. For about **0 feet (12 metres)

- 12 -

on either side, the rock is bleached to a light grey-green colour

and partially silicified. The rock is more massive and has less

pyrite and fewer fractures than the main silicified fracture zone.

Within this halo zone, gold values range from 0,02 to Q.10 oz.

gold per ton,except for 10 feet not assayed. This form of grey-

green alteration elsewhere in the hole also contains significant

gold values.

Structure of Gold Zones in Feldspar Porphyry

Gold in the feldspar porphyry may be associated with

pyritized silicification but more often is associated with frac

turing, with and occasionally without silicification. Fractures

may be filled with white quartz up to about a foot wide, very thin

seams of chlorite, pyrite, or graphite. Where fractures are

quartz-filled the gold is present in euhedral pyrite; where the

fractures form a shatter zone or breccia the gold is smeared on

a fracture surface and generally not visible. Three sets of

fractures within individual gold zones are recognizeable.

Perhaps because of the drill hole attitudes the set

which is most prominent strikes easterly and dips 50 to 55* north.

This fracture set is often filled with quartz and displays little

movement.

A second set occasionally filled with quartz but more

often chloritic or carbonaceous is conformable with the attitude

of the dyke, striking easterly and dipping about 68C south.

- 13 -

Finally a third uncommon set strikes easterly and dips

BO to 85" north. It is generally chlarite-filled, up to 2 feet

wide uith rusty pyrite, and displays shearing characteristics.

This set corresponds uiith the inferred attitude of the individual

gold-bearing zones.

At least one other fracture set is likely present but

there is insufficient drilling data to identify its attitude.

Distribution of Gold Zones

A comparitively limited amount of diamond drilling over

a length of **00 feet indicates the presence of one main central

gold-bearing zone and one or more parallel subsidiary zones within

the central portion of the dyke. This relationship is best dis

played on Figure 2, derived from the drill sections.

Again, limited data suggests that the individual gold

zones strike easterly conformable to the porphyry dyke and dip

vertically or steeply north. Within the area of drilling B cross

fault displaces the dyke and apparently individual gold zones.

Various widths of gold mineralization are shouin on the

drill sections ranging from about 5 to 85 feet (1.5 to 26 metres).

Because of the uide variance in gold values over exceptional

widths, establishing a particular uiidth in a drill hole is a some-

uihat subjective exercise dependent upon rock mineralization as

me!l as gold content in individual samples. Lacking a defineable

barren uallrock, widths can only be established after considerable

drilling has been undertaken. Similarly at this stage establishing

a cut grade, based on experience elsewhere, may be misleading.

Nevertheless, some impressive intersections are displayed

on the drill sections including 0.159 oz. over **1.2 feet (12.6

metres) in discovery hole 8*4-2; 0.326 oz. over 65 feet (26 metres)

in hole BU-8; 0.111 oz. over 30 feet (9 metres) and 0.036 over 66

feet (27 metres) in hole 8*4-13. These and other, intersections are

located over a length of **00 feet (122 metres), between the sub

outcrop and about 575 feet (175 metres) beloui surface.

Assuming a near vertical dip, individual mineralized

zones range from 3 feet (1 metre) to 50 feet (15 metres) in true

thickness. At the 575 foot level (-175 metres) the main zone,

apparently continuous for at least 210 feet (6U metres) and 27 feet

(6 metres) uiide, averages 0.21+5 oz. gold per ton (uncut). Some

other true widths at this elevation include 0.11*4 oz. over 16 feet,

0.111 oz. over 26 feet, 0.036 oz. over t*9 feet, and 0.066 oz. over

11 and 16 feet respectively.

CONCLUSIONS

1. A gold-bearing felsic feldspar porphyry dyke, about 200 feet

(60 metres) wide, strikes OSO0 across the Pominex property

for over a mile. Diamond drilling has confirmed that the

porphyry contains significant gold values for a length of t*OQ

feet (122 metres) on the Pominex property and 1200 feet (366

metres) on the Asarco property.

2. Uithin the porphyry a central main gold mineralized zone ranges

between 27 and **9 feet (6 and 15 metres) wide over the total

- 15 -

length of 1600 feet on the Agarco and Pomine* property. Only

one Asarco hole 1200 feet from the common boundary is evidence

for the continuity. Parallel subsidiary zones of lesser widths

are also present.

3. Diamond drill results suggest that greater concentrations of

gold occur at or belou the 575 foot (175 metre) level.

t*. At the 575 foot level where three holes have been drilled over

a length of 210 feet (6** metres) the main zone averages 0.21*5

oz. gold per ton (uncut) over an average true uidth of 27 feet

(8 metres). Considered representative of the main zone is a

true uidth of **9 feet (15 metres) averaging 0.036 oz. located

200 feet (60 metres) east and a true uidth of 32 feet (10

metres) averaging 0.0**5 oz. 1200 feet (366 metres) uiest on the

Asarco property.

Typical true uiidth intersections of subsidiary zones at

the 575 foot level include Q.1K* oz. over 18 feet, 0.111 oz,

over 26 feet, and 0.066 oz. over 11 and 16 feet respectively.

In many cases a reduction in uidth would enhance the average

grades.

5. Typically, the core of the main gold zone is silicified, grey-

white in colour, fractured, and contains about 10 per cent

quartz stringers and 1 per cent partially oxidized pyrite. If

present, higher concentrations of gold are preferentially

located within this zone. Although the higher concentrations

- 16 -

of gold are considered to be associated with fracturing, it is

not yet apparent which of three recognizeable sets is most

important.

A light grey-green, partially silicified, rather obscure

halo alteration adjoins the central mineralization. It is more

massive with feuier fractures and less pyrite than the central

core but, nevertheless, contains similar loui gold values.

6. Inasmuch as it is not yet known which of three sets of fractures

is most important for gold deposition, the preferred attitude

of drill holes is uncertain. If, however, the gold zones dip

near vertically, vertical holes will not likely provide repre

sentative results.

7. Some impressive gold intersections alternate uith comparitively

mediocre indications. Such results are normal for most gold

deposits. Probably most significant is the uniformly low (.02

to 0.10 oz.) but highly anomalous gold content of wide sections

in the feldspar porphyry. Only the odd higher concentration of

gold within these sections is required to categorize these

zones as potential ore.

Much additional diamond drilling will be required to

determine the economic viability of a mining operation on the

Pominex property.

RECOMMENDATIONS

It is recommended that sufficient funds be allocated to

provide for diamond drilling on the property in three stages of

- 17 -

10,000 feet each. This is likely to be a minimum requirement if

results from such a programme mere generally positive throughout.

Depending upon results, interruption of the drilling

between stages may or may not be necessary. However, it mould be

prudent to execute drill contracts of 10,000 feet or less so that

the programme may be evaluated periodically.

Hole 83-11*, the last hole of the previous programme, did

not reach its objective. However, the casing was not removed so

that the hole could be re-entered at a future data. Initially,

drilling should commence at this location which might involve one

or more wedges to intersect the projected gold zone at different

levels. Additional drilling from south to north should also be

contemplated at specific locations in order to acquire more infor

mation on the fracture pattern and determine the most favourable

attitude for drilling.

Cost of the programme is estimated as follows:

Stage One

Drilling 10,000 feet at 521 per foot . . . . . . . . . 1210,000.

Supervision, engineering and sampling , . . . . . . . 30,000.

Assaying . . . . . . . . . . . . . . . . . . . . . . . 10,000.

Contingencies . . . . . . . . . . . . . . . . . . . . 10 fODD.

8260.000.

- 18 -

Each additional stags of 10,000 feet is anticipated to

cost about the same amount. The entire 30,000 feet of drilling

if completed is, therefore, estimated to cost 8780,000.

Respectfully submitted,

SHIELD GEOPHYSICS LIMITED,

Timmins, Ontario,

May 22, 198**.

-O ~-

R. J. Sradahau, P. Eng.,

Geologist.

CERTIFICATE

I, Ronald J. Bradshaw, residing at R. R. 2, Airport Road, Timmins,

Ontario, a consulting geologist with office at R. R. 2, Airport

Road, Timmins, Ontario, do hereby certify that:

I attended Queen's University, Kingston, Ontario, and graduated

with an Honours B.A. degree in Geological Sciences in 1956.

I am a Felloui of the Geological Association of Canada, a Member of

the Canadian Institute of Mining and Metallurgy and of the

Association of Professional Engineers of Ontario.

I have no direct or indirect interest in the property, shares or

securities of Pominex Ltd. nor do I expect to receive any such

interest.

Timmins, Ontario f \ r ^ ~/ R. J. Bradshau, P. Eng.,

May 22, 19BU. ^^TTT^X Geologist.

REFERENCES

Shield Geophysics Ltd. November, 1983

Magnetic Survey on the Pominex Macklem Township Property

Leahy, E. J. 1971

Geology of Nighthauik Lake Area D.D.M. Report 96

Aquarius Project (Aaarco) 1983

Plan S Sections of Drilling

LEGEND

6

5

4

3

2

l

Aplitt

Feldspar Porphyry

Carbonate, Sericite or Chlorite, Talc Rock

Carbonate-Quartz Rock

Ultramafic Rock (Serpentine)

Mafic to Ultramafic Volcanic*

Felsic to Intermediate Pillow Lava

Re: Figures l to 7

-NORTH

POMINEX,—————

ASARCO

(M

S*o ———

\ S*-Vis — t* i—————— B ————— 1

9"

POMINEX LTD.

DRILL HOLE PLAN 8 GEOLOGY

AT SURFACE (Note 2) -5O METRES

O 2O 4O metres

: IOO

MAY, 1984 Figure

SYMBOLS

Vertical projection of hole

Gold value In oz./T over width in feet

Fault - interpreted

Rock contact - interpreted

84-8,10 84-9,11

POMINEX LTD.

EOLOGY a GOLD VALUES

PLAN'-175 METRES

l i 100

SYMBOLS

jn Gold value in oz/T over horizontal width In ftet

l| Diamond drill hot* No

;.v: Gold mineralized zone

84-2"

*

POMINEX LTD.

SECTION 16*60 W

l :KX)

ft o 5) g

•4-5 84-6

POMINEX LTD.

SECTION 16+30 W (B)

l :K50

Figure 5

POMINEX LTD.

SECTION 15+40 W

l : 100

Figure 7

AV

l ^^ APPENDIX

GO rsj (sj Diamond Drill Loga

{ Holes 83-1 to B^-j v\ O

in

^ s:o o

DIAMOND D ffi L L RECORDPROPERTYTOWNSHIP

LOT-ATTON Line 1+OOU

Station 1+UO South(metric grid)

ELEVATION

POMINEX LTD.

Macklem Township

CORE LOCATION-DATUMBEARING .DTP

MNR Timmins .

North (sat:)50 s

..-HOLE NO.......B3-.1......, PAGE NO. , 1

STARTED

. .,, mMPLETEr

I ftDecember 16, 1983

i December 23, 1983550 feetAQ core (1 1/16")

DEPTH FEET

n - 11*1U1 - 198.3

.^

198.3 - 230

230 - 238

238 - 2^6.5-

FORMATION

Casing (overburden).

Intermediate to Mafic Pillow Lava S/or Flows:

medium to pale oreen, v.f. or.". 1-iohtly fractured

and oartiallv carbonatized: flows S'pillous marker

by vesicles and dark qreen- chloritized interfaces;

some epidote; fractures filled by barren quartz an

carbonate.

1 5'37l*-"1 51* . ** grey vuggy: q tz @ 50" to c. a.

Intermediate to Mafic Volcanic Flow Breccia: ....:

dark green massive mafic. -sec-tians up to 2 1 ui.th ;^ ..1

pale green .sections of angular fractured inter

flow material; dark blue mafic sections and .

fractures are serpentinized.

Felsic (Aplite) Dyke: massive aphanitic, very

hard, siliceous rock; conchoidal fracture except

where low angle secondary cream coloured fractures

occur. ---.' ' .' ' . - . -'. .-^ -; ' -- J

Mafic Volcanic Flow*, dark green, massive, v.f. 'gr.

lightly fractured.

SAMW NO.

d

.

" *. .

f- '.

j '

" ""

.. t:.::

WIDTH Of SAAAHC

:-

* " - **T '

1 i

tt

-

i

By Signed.

DIAMOND D?ILL RECORDPROPERTY

TOWNSHIPLOTJkTTON

ELEVATirvM

CORF LOCATION

DATUMBEARING,,..',,, , .

DTP

HOLE NO. 83- 1 _ .

PAGE NO. 2 W

STARTPH

HEPTH

DEPTH FEET

7LA.R - 271*. 9

27U. 9 - 322.9

322.9 - 331*. 3

FORMATION

Intermediate Aqqlomerate (Pyroclastic Breccia):

Dale oreen. masses ranqinq from 3" to 3'; some

mav be pillows, upper contact at 3D0 ; some carb

in fine qash fractures, black mafic contact zones;

becoming more lightly packed deeper.

Intermediate Volcanic Flow: pale green, v.f.gr.,

more massive except for prevalence of serpentine-

filled gash fractures near top perhaps representin

flow top.

288. D becoming more massive

308.0 . becoming less massive with pale green

irregular masses perhaps representing

bombs

Intermediate Volcanic Breccia: upper contact at 'i*

pale green fragments with soft black serpentine

filling gash fractures and interstices, very

intense brecciation at start; rock becomes softer

deeoer.

31**. 7 2' nrev irreq, qtz stringer

SAMFU NO.

o ' t

WIDTH OF SAMFiE

-

Drilled By.

DIAMOND D {fi L L RECORDPROPERTYTOWNSHIP

LOTATinN

ELEVATION

CORR LOCATIONDATUMBEARING . ...,mo

HOLE NO. fl3- 1

PAGE NO. 3

STARTED -

COMPf.PTEn

nPPTH

' t.

DEFTH FEET

33**.3 - 370.5

370.5 - 1*00.5

t*00.5 - t409.3

t*Q9.3 - 513

FORMATION

Ultramafic: black, fairly soft, massive except

for irregular carbonate-filled fractures; probable

intrusive periodite although upper contact

gradational.

366. it-368. 3 soft, light grey-green talcose rock

366.8-368.0 core ground

369.B-370.3 light coloured xenolith ?

Intermediate Volcanic: comprised of breccia of

flow material, agglomerate and pillows, gash

fractures filled by serpentine."

Intermediate to Mafic Volcanic Flows: contact

poorly defined; medium green, fairly massive

with uniform fine dissemination of carb lathes.

Intermediate Volcanic Breccia: comprised of flows

agglomerate and pillows; pale green, v.f.gr.

dacitic pillows and fragments are extensively

fractured, gash fractures and interstices filled

by black serpentine; odd minor qtz and carbonate

stringer.

SAMflE NO.

i

WIDTH OF SAMHE

Drifted By. Signed..

DIAMOND oflLL RECORDPROPERTY. MOLE NO....

LOCATION.

ELEVATION-

TOWNSHIP. .PAGE NO..

CORE LOCATION. DATUM______

STARTED-

BEARING- DIP____

COMPLETED- DEPTH. ...,.

DEPTH FEET

513 - 550

550

FORMATION

^.9-^6.3 8" qtz-carb str. @ t*5 0 , feu grains

of py and cpy

**55. 0-1*82.0 minor brecciation of pillow lava

U82. 0-503.0 more intense brecciation; secondary

fractures filled uith carb, qtz and

occasionally clay mineral

Intermediate Amyqdaloidal Pillow Lava: contact

sharp at 7Q0 to c. a., med. green to brownish;

well defined pillows with variably sized green

amygdaloids in brownish matrix; some epidote,

few serpentine-filled fractures.

5^0.0 3" barren qtz-carb stringer @ **5 0

END.*

Dip test @ 550' - U1"

SAMPLE NO.

1-1

WIDTHor SAMPU

1.**

Au/ppb

15

Drilled By. Signed

DIAMOND DJflLL RECORDPROPERTYTOWNSHIP

LOTATTON LJne 16+60UStation 5+20 South(metric qrid)

ELEVATION

HUM1NLX LTD.

Macklem Township

, .. CORF I.OCATK

DATUMBFARTNODTP

HOLIPAGE

"jfj #3U Warehouse - AirooRoad

North (ast.)50"

STARTED ..

DEPTH

January 3'

12, 198**

17.

BQ core (-1 7/16")

DEPTH FEET

D - 200

200 - 512.8

-

FORMATION

Casino (overburden).

Felsic to Intermediate Amyqdaloidal Pillow Lava:

verv hard, v.f.ar. dacitlc pillows from 2 to B 1

with zoned qlobules in chloritic selvages of

pillows; lighter coloured amygdules ? up to H" in

diameter; selvages at about **5 0 forming zones up

to 3' wide with chlorite, yellowish carbonate and

quench textures similar to spinifex.

26**. 5-270.0 diabase dyke, orey f.qr. massive;

brecciated upper contact

272.5- over **" yellowish carbonate, aome py

in pillow selvage section

300.0 pink albite adj. to grey carbonate

in selvage over 6"

from 280 pillows becoming smaller and more

tightly packed

302.5-307.0 irreg. fractures filled with grey

carbonate and rock altered to green

colour by fuchsite

SAMfU NO. WIDTHor SAMPU

Drilled Oy-. Norex Signed

DIAMOND DhlLL RECORD

LOCATION.

ELEVATION,

PROPERTY. HIOLE

TOWNSHIP. .PAGE NO

CORE LOCATION.

DATUM______

STARTED.

BEARING. DIP___

COMPLETED. DEPTH

DEPTH FEET

512. B - 760.0

FORMATION

307.0-323.0 rock substantially softer

i.e. andesitic

339 little pyrite in gashes

1*19.0-1*22.0 W fractures @ 0" with carbonate-

hematite filling

1*68.0-512.8 darker, softer more mafic

1*67.0-1*88.0 1H" carb str. @ 20" with py-cpy diss

i*9B. 0-500.0 breccia of mainly carbonate @ 35" to

c. a. with sharp contact

500.0-512.8 more fractures and Di Hows not

recoanizeable: apparent silica

reduction

Felsic Porphyry Dyke: grey to pale qreen, very

hard, aphanitic, fractured rock with scattered

white phenocrysts generally rectangular in shape-

probable feldspar; fractures generally tight and

serpentinized uiith smeared pyrite.

51*1.0-51*6.0 1" fc B" white qtz strs. at 35 0 ,

crushed py at contacts, less than 196

SAMFtC NO.

2-1

2-2

WIDTH OF SAMHE

1.0

5.0

Au/ppb

15

1*87

Au/oz

.011*

Au/oz.reject pulp Swastika

nil.002

nil

euhedral pyrite diss. in dykes

Drilled By, Signed.,

LOCATION.

ELEVATION.

DIAMOND DlflLL RECORDPROPERTY. HOLE NO.

TOWNSHIP. ...PAGE

CORE LOCATION.

DATUM______

STARTED-

BEARING.

DIP___

COMPLETED-

DEPTH

DEFTH FEET FORMATION

551*. Q 1" white qtz str. @ 350

560.5 #" white qtz str. @ 45 0

567 3" dark green, soft, chloritic, mafic

xenolith

569.5-571.3 diabase or xenolith as above at 90"

597.8-602.0 l* - #" qtz strs. @ 2Q0 , 1 96 py in wlrk

609.0-611.0 fault with mud and black serpentine

at 20"

621.0-692.0 many more feldspar phenocrysts in

grey matrix; also fractured at low

angle with dull white carb filling

665.0-666.5 296 pyrite with irreg. silicification

677.0-681.0 numerous tight black fractures, less

than 196 pyrite

697.0-700.0 fractured with 196 pyrite

702.7-707.7 irreg. fractures with 196 pyrite

738 i*" diabase at BO0

7^+0.0-71*3.9 fractured, slight oyrite

7U3. 9-751.0 diabase, massive

SAMME NO.

2-3

2-i*

2-5

2-6

2-7

2-8

WIDTH OF SAMHE

U.2

1.5**.o

3.0

5.0

3.9

Au/ppb

278

670

Au/oz

.050

.008

.832

.372

.116

.02

Au/oz .rejectpi 1 1 n

Swastika

nil

nil.^b .21*

.39 •W* 1 fm

.11*

.uo

.02

Drilled By- Signed..

DIAMOND DffiLL RECORDPROPERTY. HOLE

TOWNSHIP. .PAGE

LOCATION. CORE LOCATION. DATUM——————

STARTED.

BEARING.ELEVATION.

COMPLETED. DEPTH....

DETTH FEET

760. D - 809.7

809.7 - 813.0

813.0 - 8^8.6

FORMATION

753.0 7" diabase

753.7-75*4.9 1" clot of Dvrite

Diorite: dark arev or brownish, fine to very f.

drained, massive, rock uhich shows occasional well

defined banding at **5 0 to 700 ; banding appears to

be secondary intrusion.

775.0-778.9 first 3" is black mafic volcanic

remnant, 1-296 diss. py throughout

778.2-780.9 mostly mafic volcanic, carbonatized

with gash fractures-

782 . 7" dark green mafic volcanic

783.5-76*4.5 dark qreen mafic volcanic

792 U n dark green mafic volcanic

Ultramafic Rock: grey-black, medium soft, numerous

irreg. carbonate filled fractures.

Intermediate Volcanic Breccia: medium green,

totally fractured, v.f.gr. rock; gash type fracture

filled with darker material; odd ovoid forms of

hematlzed grey silica uhich seems to partially

SAMFU NO.

2-9

2-10

3

WIDTHor SAMFU

1.2

3.9

Au/ppb

18

88

Au/ozAu/oz. re iectpulp

SuaBtikc.002

.002

surround bomb-like structures up to 2" uhich are

Drilled By. SignedflEOPHYSICS LIMITED

DIAMOND RECORDPROPERTY. JHOLB NO-TOWNSHIP. ..PAGE NO.. ...,. 5 ^

LOCATION. CORE LOCATION. DATUM______

ELEVATION-BEARING. DIP——

STARTED™-.

COMPLETED-

DEPTH.... .

DEFTH FEET

81*8.6 - 857.2

857.2-865.0

865.0 - 876.7

FORMATION

totally fractured; little secondary epidote;

may represent edge of volcanic vent.

839.0-8*48.6 rock more massive; seems to be

composed of large explosive bombs

having slightly different compositior

or perhaps pillows

835 carb-filled fault over 2" @ 350 to c

Intermediate Dyke: qrey, v.f.gr. massive R

uniform except deeper fractures filled by epidote,

etc., upper contact is sharp. -

Ultramafic . Intrusive: black, v.f.gr. soft highly

fractured rock; white carbonate fills fractures;

serpentinized.

Talt:-Clav Zone: arev-white, partially dissolved,

very soft, schistose rock at **50 , odd irreq. white

carbonate str. stands out, talcose to touch;

kaolinite likely present; probable fault.

SAMFUJ NO.

a.

WIDTH OF SAMFU

Drilled By. Signed-SHIELD GEOPHYSICS LIMITED

itDIAMOND DTMLl RECORDPROPERTY. MOLE NO^^-J^rl^-.-TOWNSHIP. ,PAGB NO..

LOCATION. STARTED..

DATUM.

ELEVATION.BEARING. DIP———

DEPTH FEET

676.7 - 973.0

973.0

FORMATION

Ultramafic Rock: black f v.f.qr. soft and schistos

at about 5D0 ; much white irreg. carbonate

possibly forming bouhdinaqe structures in otherwis

talcose matrix.

B96.0 very soft and powdery over 2"

901 3" grey qtz-carbonate

902 2" qrey qtz-carbonate

916.0-917.5 muddy and crushed

923.7 muddy sand for 8"

931.0-935.0 brownish serpentine ?

935.6 . 6" of mud

937.0-91*8.0 core lost

953.0-962.0 little more solid

96**;Q-966.0 core lost

End.

Din Tests

Deoth True Anqle

225' 55"

500' 57"

SAMTO NO.

i

f

WIDTH OF SAMFtE

973' 57'

Drilled By. Signed..

ADDITIONAL SAMPLING DIAMOND d&ILL RECORDPROPERTY .................POMI.INEX...LTD................TOWNSHIP ..............Mackl.Bn)...Toujn8hlB..

.HOLE NO...........8A-2.

.PAGE NO. ..................l

LOCATION

ELEVATION

CORE LOCATION

DIRECTION ..........

DIP ........................

DEPTH ..................

STARTED ......

COMPLETED

DIP TESTS ....

DEPTH FEET/METRES FORMATION - MINERALIZATION

FELSIC PORPHYRY DYKE: phenocrvsta are uidelv

scattered, fractures are all at low anqle of

20-300 to c. a.

512.D-517.0 contact zone; contact at 80"

517.0-522.0 feu chloritic S white fractures

522.0-527.0 as above

527.0-532.0 as ahove

532.0-537.0 as above S H" qtz str. @ 3D0

537.0-541.0 few fractures

541. 0-546.0 previously sampled


551.0-557.0 few fractures S 1" qtz str. S 70 0

557.0-562.0 few fractures, little ov * W q tz str

e 20 0562.0-567.0 few fractures

567.0-572.0 few fractures R 2 H diabase dvke


577.0-580.0 6" diabase, few fractures


SAMPLE NO.

2-11

2-12

2-132-14

2-15

2-16

2-2

2-17

2-18

2-19

2-20

2-21

2-22

2-23

2-24

WIDTH OF SAMPLE

5.0

5.0

5.0

5.0

5.0

4.0

5.0

5.0

6.0

5.0

5.0

5.0

5.0

3.0

5.0

Au/ppb

3

2

18

34

576

210

48T

775

683

605

192

30

7

15

25

Au/oz

.017

.006

.014

.023

.02

.018

592.

562.

Drilled By Signed.SHIELD GEOPHYSICS LIMITED

PAP - I-69

DIAMOND dblLL RECORDPROPERTY .

TOWNSHIP

.HOLENO...........BA-2..

.PAGE NO. .................Z..

LOCATION

ELEVATION

CORE LOCATION


DIP ........................

DEPTH ..................

STARTED ......

COMPLETED

DIP TESTS ....


565. 0-590.0

590.0-595.0 feu fractures

595.0-597.8

597.8-602.0 previously sampled


607.0-612.0 fault uith mud 8, black serpentine

612.0-617.0 feu pink carbonate-filled fractures


621.0-626.0

626.0-631.0

631.0-636.0 actually 7' of core marker to marker

636.0-61*1.0 tt" qtz str. //inq c. a.

61*1.0-61*6.0

61*6.0-650.0

650.0-657.0 2' serpentine fracture zone

657.0-662.0

662.0-665.0


666.5-671.0 feu uhite fractures

SAMPLE NO.

2-25

2-26

2-27

2-3

2-28

2-29

2-30

2-31

2-32

2-33

2-31*

2-35

2-36

2-37

2-38

2-39

2-1*0

2-1*

2-1*1

WIDTH OF SAMPLE

5.0

5.0

3.81..2

5.0

5.0

5.0

1*.0

5.0

5.0

5.0

5.0

5.0

t*. 0

7.0

5.0

3.0

1.5l*.5

Au/DPb

1888

1*89

1714-1*37

3151*31*

122

7

207

221*9

10

51*0

88251*

Au/oz

.011*

.05

.013

.09 L

.007

.01

.031*

•2\

.o&S

•4(,

• 73S

.155

.05^/I4.7J

tfcfe.S


PAP l 69

DIAMOND DRILL RECORDPROPERTY ..........................................................................................................................................HOLE NO..............?.{*~.?..

TOWNSHIP ....................................................................................^..................................................PAGENO. . ..................?...

LOCATION

ELEVATION

CORE LOCATION


DIP ........................

DEPTH ..................

STARTED ......

COMPLETED

DIP TESTS ....


671.0-672.7 very obscure visible qold smeared on

slip plane ad.1. to H" qtz str. @ 3D0 ;

broken core indicates possible fault

672.7-677.0 +5 1 of core

677.0-681.0 quarter split check sample

681.0-686.0 obscure very fine ooid on slip plane

686.0-691.0

691.0-697.0 feu fractures, sli. pyrite


700.0-702.7

702.7-707.7 2fc pyrite; previously sampled



716.0-722.0

722.0-727.0

727.0-732.0

732.0-735.0

735.0-71*0.0 3" diabase @ 80"

74*0.0-71*3.9 previously sampled

SAMPLE NO.

2-1*2

2-1*3

2-5

2-1*1*

2-1*5

2-1*62-6

2-1*7

2-7

2-1*8

2-1*9

2-50

2-51

2-52

2-53

2-5U

2-8

WIDTH OF SAM RLE

1.7

1*.3

1*.0

5.0

5.0

6.03.0

2.7

5.0

5.0

5.0

6.0

5.0

5.0

3.0

5.03.9

Au/ppb

8231*

25

18751*

1577

1303

68b

Au/oz

.389

.080

.832

.020

.022

.018

.372

.016

.116

.017

.01*6

.038

.02

.661

.344

3-328

.100

.HO

.106

(.lib

.642

.580

6.545

.Bft

.19

.328

.15941.2-

707-7

.04-18'

Drilled By SignedSHIELD GEOPHYSICS LIMITED

DIAMOND Df ILL RECORDPROPERTY POMINEX LTD.

TOWNSHIP .Macklem Township

LorATiON Line 16+60UJ . roan TOCATKStation 3+1*0 South HATVM

(metric grid) ' BEARINGELEVATTrtN HIP

"ija M.N.R. Timmins

North (ast.)50"

JHOLE NO.™ 8t*- 3 -..PAGE NO., , J .

STARTRD ,......

nFPTHDip Tests:

JanuaryJanuaryBOS'

- 260' -

li*.

56 0'500' - 57'

DET1M KIT

n - 253253 - 359

359 - 389

FORMATION


Ultramafic Intrusive: .soft blue-black serpentin-

ized and carbonatized; v. fine grained; white

carbonate forms qrains 8, fills gash fractures

generally at t*5 0 ; first foot looks like massive

mafic to intermediate volcanic in contact with

ultramafic at **5 0 .

300.0-359.0 verv soft, schistose i broken with

sections of mud - fault

312.0-317.0 core lost

317.0-322.0 v. soft schistose mud composed of

clay minerals

321*. 0-327.0 core lost

332.0-337.0 core lost

352.0-357.0 core lost

Carbonatized 8, Serpentinized Volcanic: fault

zone; med. grey, soft, fairly massive, in part

schistose and broken, with much lost core.

363.0-367.0 core lost

SAMMC NO. WIDTH Of SAMMf

Drifted By. Norex Signed..

DIAMOND D PILL RECORDPROPERTY

TOWNSHIP

LOCATION

ELEVATION

- CORE LOCATION.DATUMBFAPTNfrDTP

HOLE NO. BA-3 ;

PAGE NO. 2 1

' T, STARTED............... .,... , ,.,roMPf.ETPnDFPTH

.

DEPTH FEET

389 - 1*01

1*01 - 629

FORMATION

367.5-368.3 mud

372 3" carbonate stringer at **50

373. 0-371*. 0 core lost

381.0-382.0 soft and crumbly

382.0-383.0 core lost

Mafic Dyke: lamprophyre or diabase; mafic, soft

dark minerals in hematitic matrix giving brownish

colouration; blotchy carbonatized clots, uniform

and massive, feui chlori te-carbdnate strs. at UQ0 .

1*02.0-1*01*. Q core lost

Faulted Ultramafic Rock: blue-black to qrey,

schistose and broken, much carbonate in gash

fractures; talcose locally fc serpentinized;

schistosity at i*5 0 -9Q0 ; may be altered volcanic.

1*11.0-1*13.0 core lost

1*26.5 1" of green mud at **5 0

U28.5 2" irreg. white carbonate

1*31*. 0-t* 37.0 core lost

1*50.0-1*52.0 core lost

SAMNt NO. WIDTH OF SAMFU

Drifted By. SignedSHIELD GE

DIAMOND DTlLL RECORD

LOCATION

ELEVATTOM

PROPERTY

TOWNSHIP

-

CORR LOCATIONDATUMREARINGnip

HOLE NO. ^**rl ... .

PAfiE NO. . 3 W

STARTED

rOMPf.RTRn

DEPTH.

DEFTO FEET FORMATION

U50.Q-U96.0 increasing number of white carbonate

strs. and darker colour

500 3" carbonate str* @ 600

517.0-519.0 crushed rock

521.5-52U.O schistose rock

525.0-526.0 curved carbonate str. like selvage

of pilloij

529.0-531.0 core lost

531.0-592.0 core broken fc muddy after local

schistosity and faulting

572.0-576.0 core lost

565.0-587.0 core lost

591.0-592.0 core lost

592- generally schistose at about ^50 ;

much irreg. white carbonate

608 feui cubes of pyrite

616.0-62*4.7 very soft, muddy schist which is

partially dissolved - main fault

SAMttE NO. WIDTH OF SAMPUJ

Drilled By- Signed..r\ ncript-ivgffc i

DIAMOND DflLL RECORDPROPERTY. .HOLE

LOCATION.

ELEVATION.

TOWNSHIP. .PAGE NO-STARTED-

DATUM. COMPLETED. DEPTH

mo

DEPTH FEET

629 - 6U5

6*45 - 68**

FORMATION

Carbonate-Chlorite Rock: grey mottled colour,

soft, massive to schistose locally, odd quartz-

carbonate stringer; minor sulphides.

63U.O-635.0 2" qtz-carb str. 9 SO0 with

schistosity contains feu grains of

siderite? and lead-like mineral

Carbonate-Quartz Rock: irreg. white qtz veins

and strs. in med. arev carbonate rock with minor

albite, very minor fuchsite; sil. pyrite as large

cubes, slight siderite?

6*45-650 6096 white irreg. qtz, 296 py as large

xstals

650-655 1096 white irreg. qtz, 296 py as large

xstals

655-660 2056 white irreg. qtz strs., 296 py

660-665 7096 irreg. uhite qtz strs., some

albite, fuchsite, 296 pyrite

665-666.8 3096 irreg qtz-albite str., sil. py,

fuchsite

UMW NO.

3-1

3-2

3-3

3-U

3-5

3-6

WIDTH OF SAMPLE

1.0

5.0

5.0

5.0

5.0

3.8

Au/ppb

U

k

3

8

5

If

Drilled Bf. Signed..-SHIELD GEOPHYSICS LIMITED

LOCATION.

ELEVATION-

DIAMOND RECORDPROPERTY. MOLE

TOWNSHIP. .PAGE NO..CORE LOCATION. DATUM______BEARING. DIP___

STARTED.— COMPLETED. DEPTH... .

DEFTO FEET

681* - 703

703 - 76**. 7

FORMATION

67i*-679 **096 irrea. white qtz: albite in ulrk.

some fuchsite, 196 pv. minor cpv

678-66** 3096 qtz strs.; albite, fuchsite,

carbonate ulrk with sli. pv fc cpy

Carbonate-Fuchsite-Albite Rock: coarse grained,

green, fairly massive with qtz stra., 296 pyrite;

contacts gradational.

685-690 much fuchsite. 296 ov/rite

690-695 as above with 1" qtz str. //inq c. a.

695-701 as above: 10* qtz strs.

Carbonate-Sericite-Talc Rock: med. arevt massive,

occasionally schistose and softer deeper.

710 some fuchsite

725-730 1096 qtz str. @ 80 0 corresponds to

schistosity uiith 196 pyrite

730-7**7.3 occ. 1-2" qtz-carb strs. with 80"

schistosity, 196 pyrite

71*7. 3-76**. 8 more massive fc becoming harder deeper

towards dyke contact

SAMPU NO.

3-7

3-8

3-9

3-10

3-11

3-12

WIDTH OFSAMJ1E

5.0

5.0

5.0

5.0

6.0

5.0

Au/ppb

3

1*

10

3t*

7

DriKcd By. Signed..

DIAMOND DlflLL RECORDPROPERTY.TOWNSHIP.

.HOLE NO.

.PAGE NO.

Bt*-3

LOCATION. CORE LOCATION. DATUM______

STARTED..

DEPTH.

ELEVATION- DTP

DEPTH FECT

761*. 7 - 798.5

798.5

FORMATION

758.7-760.7, feu qtz-carb strs., 396 xstalline-py760.7-765 2096 white irreq. qtz strs., 296

xstallihe pyriteFelsic (Aplite) Dyke: light pink, f. to roed.grained, massive, hard intrusive with generallybarren white qtz strs., 3-596 euhedral pyrite,trace chalcopyrite.765-770 20* qtz str., 3* pyrite

770-775 1096 qtz str.. 396 pyrite775-780 5096 qtz str., t*96 pyrite780-785 . 1096 qtz str., 1*96 pyrite785-790 1096 qtz str., 1*96 pyrite790-795 596 qtz str., 396 pyrite795-798.5 1096 qtz str., 1*96 pyriteEND.

SAMPUNO.

3-133-U

3-153-163-173-183-193-203-21

WIDTH OF SAMFU

2.0

**. 3

5.0

5.05.05.05.05.03.5

Au/ppb3

11

1*9

5989

96131138

31*

By- Signed...SHIELD GEOPHYSICS LIMITED

DIAMOND dftlLL RECORDPROPERTY .................P^ML.^............^

TOWNSHIP ................y.?^!^ ....................l........

LOCATION ..........yLn.?...l6 P.3..!L....................................... CORE LOCATION ........M..N.,R......-...IA!n!niP.B............. STARTED ............F..Bbruary...1. ll ....19.8|*.

.................................SAati..?."...?.*.?..?.?.................................... DIRECTION ...................^P.rth...(ast.) COMPLETED ......E.B.bruary...5.a ....198f*.

.......................................................................................................... DIP ............................,..55L.....^. :...................................... DIPTESTS .......

ELEVATION .................................................................................. DEPTH .................71*6.!.......................................................... .............................

DEPTH FEET/METRES

0 - 300

300 - 307

307 - **66

FORMATION - MINERALIZATION


Core around.

Ultramafic (Serpentine) Fault Zone: blue-black,very soft to soft, locally muddy; schistose at80"; unite carbonate 8. feu qtz strs. and lenses

uhich are more resistent in soft seroentine orlocally talcose or muddy matrix.315.0-317.0 core ground


332.0-369.0 rock is more solid but apparentlybrecciated marked by rounded frag

ments of carbonate S uallrock in

erratic oattern

3^6.5 2" calcite stringer367 2" calcite stringer

369.0-385.5 qrev colour caused bv soft orevbrecciated mineral interspersed uith

numerous uhite very irreq. calcitestrs. and clots; average schistosity

SAMPLE NO.

WIDTH OF SAMPLE

-

Drilled By

seems to be developed at 50 to c.a.

Norex Signed,SHIELD GEOPHYSICS LIMITED

t .A.P. - 1-89

DIAMOND D^ILL RECORDPROPERTY................................................................................................................................ HOLE NO..........B.ff.rM.

.................................................................................................................................PAGE NO. ...................2.TOWNSHIP

LOCATION

ELEVATION

CORE LOCATION


DIP .....,,........,....,

DEPTH ,..............

STARTED ......

COMPLETED

DIP TESTS ....


362.D-3B3.0 core around38**. 5-385. 5 soft fc crumbly - fault?

385.5 brecciated as from 332-369

390-391 core ground

396 2" mud

1*07 1" mud

1*09-1*11 core ground

1*08.7 3" mud

1*11-1*13 as at 369

t*13-**25 numerous fractures and shears marked

bv white calcite strinaers

1*25-1*27.5 brecciated as above

1*36-1*37 core ground

1*1*0.3-1*1*5 brecciated schistose at 50", soft and

locally muddy

1*1*5-1*66 brecciated

1*52-1*51* partially dissolved breccia schist

at 500

1*1*8.5 2" irridescent purple soft mineral

SAMPLE NO.

WIDTH OF SAMPLE

-

following breccia cracks


PAP- 1-69

DIAMOND d&ILL RECORDPROPERTY .......................

TOWNSHIP .....................

LOCATION ..............................................................................

ELEVATION ...........................................................................

CORE LOCATION .............................

DIRECTION .......................................

DIP

DEPTH ...............................................

..............................HOLE NO. . ........o.*.-?.?................

..............................PAGE NO. ...................3................

........................................ STARTED ..........................

,...................................... COMPLETED ....................

,...................................... DIP TESTS ........................

9

DEPTH FEET/METRES

466 - 604


Carbonate-Quartz Rock: contact is knife sharp at70 0 to c. a. marked bv k * of massive talc:carbonate is qrev-qreen, roed, orained, soft to

medium hard with numerous irreg. qtz veins and

strs., rock has a pebbly texture after carbonatepseudomorphs; 2 ages of quartz veining.479. 7-484. 7 3096 white qtz strs. having sericite

contacts, very slight pyrite

484.7-489.7 7096 irreo. qtz veins S strs.4 89.7-4*94.7 5096 " " " " "

494.7-499.7 4Q% " " " " "

499.7-504.7 6096 irreo. otz veins fc strs. with

sericitic contacts

504.7-509.7 9096 irreq. qtz veins a strs. with

sericitic contacts

509.7-514.7 2096 qtz strs. with sericitic contacts514.7-519.5 2596 " " " " "

519.5-524.5 5096 qtz veins i strs. with sericiticcontacts

SAMPLE NO.

4A-1

4A-2

4A-3

4A-4

4A-5

4A-6

4A-7

4A-B

4A-9

WIDTH OF SAMPLE

5.0

5.0

5.0

5.0

5.0

5.0

5.04.8

5.0

Au/ppb

16

1011

25

4

a

24

2


DIAMOND DttlLL RECORDPROPERTY ......................................................................................................................^

.................................................................................................................................PAGE NO. .....................f*..TOWNSHIP

LOCATION

ELEVATION

CORE LOCATION


DIP ........................

DEPTH ..................

STARTED ......

COMPLETED

DIP TESTS ....


52t*.5-53D.5 10096 qtz veins S strs. with sericiticcontacts

529.5-550.2 rouqhlv banded carbonate at 50* withfeu conf. S crosscutting qtz strs.

537 2" qtz str.

550.2-555.2 U096 qtz-carbonate strs.

555.2-560.2 2596 irreq. qtz-carbonate strs.

560.2-565.0 3096 irreq. qtz-carbonate strs.:

carbonate is light brown colour;possibly ankerite

565.0-570.0 3096 qtz-carbonate strs.

570.0-57*4.9 3096 " " " . sli. ovrite

57*4.9-579.7 *4096 " " "

579.7-58*4.0 3596 " " veins a strs.

58*4-60*4 becoming more chloritic

58*4.0-589.0 2096 qtz-carbonate strs.

589.0-593.3 2096 " " "

593.3-598.1 2596 qtz-carbonate strs.. sli. ovrite

598. 1-600.0 1596 qtz-carbonate strs. banding at

SAMPLE NO.

itA-10

I*A-11

t*A-12

t.A-13

*4A-U

l*A-15

**A-16

i*A-17

i* A- 18

t*A-19

t*A-20

t*A-21

WIDTH OF SAMPLE

6.0

5.0

5.0

t.. B

5.0

t*. 9

t*. 8

i*. 3

5.0

t*. 3

t.. 8

1.9

Au/ppb

2

8**

5

———— J-7

3

29

7

2J*

760-70", 196 pyrite

Drilled By Signed,SHIELD GEOPHYSICS LIMITED

PAP t 69

DIAMOND d&ILL RECORDPROPERTY ...,..........................................................^

TOWNSHIP ........................................................................................................................................PAGE NO. ...................5.

LOCATION

ELEVATION

CORE LOCATION


DIP ...........,...........

DEPTH ..................

STARTED ......

COMPLETED

DIP TESTS ....

DEPTH FEET/METRES

6Qli - 657.8

657.fi - 681,. 8

66*4.8 - 730.0

730 - 739


600.0-60*4.0 intermediate dvke @ **50 : 1" white

qtz str. @ 20" @ bottom contact, odd

speck of reddish mineral throughout

perhaps potash feldspar

Talc-Chlorite-Carbonate Schist: dark green, very

soft, schistose li 50 0 , odd carbonate str., minor

euhedral pyrite.

6**9. 0-651.0 core around

Felsic Duke: lioht oink. siliceous, fine grained

S massive; chlorite fractures here and there.

657.7-661.0 feu irreo. flat chlorite fractures

661.0-665.0 as above

672.7-677.0 as above with 1" qtz str. and few

grains of pyrite

Talc-Chlorite Schist: dark green, very soft,

fairly massive rock with odd carbonate stringer.

697 some large crystals of pyrite

Intermediate Intrusive Dyke: arey. med. Drained.

massive except for sections up to about a foot of

SAMPLE NO.

UA-22

l*A-23

i.A-2^

l*A-25

WIDTH OF SAMPLE

U.Q

3.3

l*.Q

i*. 3

Au/ppb

8

7

8

7


PAP - 169

DIAMOND DHILL RECORDPROPERTY .

TOWNSHIP

.HOLENO........jB.(*-.f*A.

.PAGE NO. .................6..

LOCATION

ELEVATION

CORE LOCATION


DIP .........................

DEPTH ..................,

STARTED ......

COMPLETED

DIP TESTS ....

DEPTH FEET/METRES

739 - 7*46

7U6


nure chlorite: feldspar arains in matrix ofchlorite, some oyrite.Fault Zone: partially dissolved section of clayminerals developed after intermediate intrusive.END.

SAMPLE NO.

WIDTH OF SAMPLE

Drilled By Signed .SHIELD GEOPHYSICS LIMITED

DIAMOND ffrtILL RECORD

LOCATION

ELEVATION

PROPERTY .....................f I NEX ..L TD .^.................................................................................HOLENO..

TOWNSHIP ...................!1?.FM!E.~^^^

............................. CORE LOCATION .......

............................. DIRECTION .................

^..^..^.^.^ D IP .......................................................... DEPTH .....................

814-5

1

STARTED ..........EEhr.uar.y.......8.,.....19Bk.COMPLETED ...f.e.b.r.uar.y....1.3..,....i.9.fl'*..DIP TESTS .........SQD.!....-..5.2.0.......................

DEPTH FEET/METRES

D - 220

220 - 1465.0


Casino (overburden).

Felsic to Intermediate Amvadaloidal Pillow Lava:very hard, v.f.qr. dacitic pillows from 2 to 8'wide with zoned globules in chloritic selvages of

pillous: lighter coloured amygdules up to te" indiameter: selvaoes at about **5 0 includingchlorite?, epidote, pyrite; minor irreo. ciuartz-carbonate up tn t* ' uide; same as hole 8*4-2.256. 9-261. k

292. 6-293. 8 irreq. qtz S yellouiish carbonatein selvage

328 #" splash of oyrite

369.2-369.8 diabase S 80" to c. a.^12 3" irreq. brounish carbonate**29 1" banded carbonate @ 250 represent-

inq fault

1*29. i*-t*3 1.8 black diabase dyke @ 70 0^^0.6 5" black diabase dyke @ 60 0

SAMPLE NO.

5-1

5-2

WIDTH OF SAMPLE

*4.5

1.2

Au/ppb

10

5

Au/oz

Drilled By ............... J.P.r.e.X.. Signed.SHIELD GEOPHYSICS LIMITED

PA P. . 1-69

LOCATION

ELEVATION

DIAMOND LtrflLL RECORDPROPERTY ,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,.,,,,,,,,,.,,,,,,,.,,,,,,...HOLE NO...............BA-5,...

TOWNSHIP ........................................................................................................................................PAGE NO. ,.,,,,,,,,,2,,.

,.................................................... CORE LOCATION,,,,.,,,,,,,.,.,.,,,,.,.,,,,,.,,,,.,,, STARTED ,..,

,,.,,.,,,,,,,,,,,,,,,,,,,,,, DIRECTION .,,,....,,,,,,,,.,,,.,,,,,,,,.,,..,,,,.,,,,., COMPLETED

,,,,..,,,,,,,,,..,,,,,,,,,,,. DIP ,,,,...,,,,,,.,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,, DIPTESTS ,,

,,,,.,..,,,,,,,,,,,,,,,,,,,, DEPTH .,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,. ,.,,,,,.,,,,,,

DEPTH FEET/METRES

1*65 - 72U.8


Felsic Porphyry Dyke: liqht to med. preen to

qrey, very hard fc aphanitic; scattered white

rectangular phenocrysts; fractures marked by

straight and irreg. black lines of either

chlorite or carbonaceous material, some pyrite

locally and odd narrow qtz str.; contact is sharp

at 650 to c. a.

1*62. 7-U67.0 196 scattered pyrite

1*67.0-1*72.0 some irreg. black fractures

t*72.0-t*76.0

1*76.0-1*81.0

1*81.0-1*86.0 feu black fractures

1*86.0-1*91.0 feu black fractures

1*91.0-521.0 liqhter colour

1*91.0-1*96.0 liqhter colour fc feu fractures,

some chlorite

1*96.0-501.0 2 W uhite qtz strs. with some pyrit501.0-505.9 minor pyrite uith W q tz str. @ 200

505.9-511.0 2 W q tz strs. S pyritized fracture

SAMPLE NO.

5-3

5-1*

5-5

5-6

5-7

5-8

5-9

j 5-10

5-11

5-12

WIDTH OF SAMPLE

l*.3

5.0

t*. Q

5.0

5.0

5.0

5.0

5.0

1*.9

5.1

Au/ppb

3

51*

2

10

2

11

222

86731*3

Au/oz

-

Drilled By Signed ,SHIELD GEOPHYSICS LIMITED

8,DIAMOND DHILL RECORDPROPERTY .

TOWNSHIP

.HOLE NO.............BA-5.

.PAGE NO. ...................3.

LOCATION

ELEVATION

CORE LOCATION


DIP ........................

DEPTH ..................

STARTED ......

COMPLETED

DIP TESTS ....


511. 0-516. D 3 JMfe" qtz strs. 3 10-i*5 0 , some

fractures

516. 0-521. D M?" qtz str. S O 0

521.0-526.0 few black fractures

526.0-531.0 few black fractures

531.0-536.0 2-6" zones of irreq. fractured qtz

with pyrite

53*4-536.^4 light coloured intermediate dyke

@ BO 0

536.^-5^1.1 feu shadowy irreo. qtz strs.. sli.

pyrite

5*41.1-5^6.1 few fractures assoc. with poorly

defined qtz strs., sli. pyrite

5U6. 1-551.0 2096 shadowy qtz str. @ 200 , sli. py

551. 0-555. B 1.5" qtz str. 8 20 0 i 3 fractures @20" with pyrite

555.8-561.0 well fractured S few W to 1" qtz

str. . sliqht pyrite

561.0-567.0 2096 poorly defined qtz strs. with

SAMPLE NO.

5-13

5-K+

5-15

5-16

5-17

5-1B

5-19

5-20

5-21

5-22

5-23

WIDTH OF SAMPLE

5.0

5.0

5.0

5.0

5.0

*4.7

5.0

*4.9

*4.fl

5.2

6.0

Au/oob

W

*47B

158

117

67

260

2*4*4

791

5fc3

311

Au/oz

0.052

*

fractures, sli. pyrite


if.DIAMOND UrdLL RECORDPROPERTY .......................

TOWNSHIP .....................

LOCATION .............................................................................

ELEVATION ...........................................................................

CORE LOCATION .............................

DIRECTION .......................................

DIP

DEPTH ...............................................

HniFwn 8^-5 ^

..............................PAGE NO. ..............A................. ™

........................................ STARTED ..........................^............,.....................

........................................ COMPLETED ..........................................................

,...................................... DIPTESTS ..............................................................



572.0-576.8 fractured

576.B-5B1.0 feu fractures

581.0-587.0 first S last tuo feet well fractured;

60% irreg. qtz, some pyrite in last

tuo feet

587.0-592.0 feu qtz strs. S fractures

592.0-597.0 2 #" qtz strs. S 300

597.0-602.0 1" qtz str. @ 20", sliqht pyrite

602.0-607.0 several fractures @ 30" , some assoc.

uith narrow qtz strs., pyrite, 4

bleaching


612.0-617.0 feu fractures assoc. uith bleaching



627.0-632.0 1" qtz str. S 3D0 marks beoinnina of

bleaching to cream colour and

fractures uith pyrite

SAMPLE NO.

5-2U

5-25

5-26

5-27

5-28

5-29

5-30

5-31

5-32

5-33

5-3**

5-35

5-36

WIDTH OF SAMPLE

5.0

i*. 8

l*.2

6.0

5.0

5.0

5.0

5.0

5.0

5.0

5.0

5.0

5.0

Au/ppb

53

129

291

605

156

56

180

(.8

30

11

25

89

Au/oz

0.029

-


DIAMOND DTULL RECORDPROPERTY .

TOWNSHIP

.HOLE NO........... J.{!.-5.

.PAGE NO. .................. 5...

LOCATION

ELEVATION

CORE LOCATION

DIRECTION .........,

DIP ........................

DEPTH ..................

STARTED ......

COMPLETED

DIP TESTS ....


632.0-637.0 bleached, feu fractures fc fine qtz

strinqers

637.0-6^*2.0 as above with 3" chlorite section RK" pink calcite @ t*5 0

61*2.0-6^*7.0 bleached, fractured, 196 pyrite fc

vuggy pink calcite 6* 35 0 , #"

pyritized qtz str. @ 20"61*7.0-652.0 Vi b leached, fractured, sli. pyrite

652.0-657.0 Jt bleached, feu fractures

657.0-662.0 fractured, including W atz str. @

3D0 with adj. seam of oyrite

662.0-667.0 fractured. 1" orev otz str. @ 800Bd.1. to 1' intermediate dyke @ 80"


672.0-677.0 uell fractured, some shadowy qtz677.0-682.0 1" S 2" intermed. dykes @ SO0 ,

fractured, 1/8" narrou qtz strs.

//ing c. a., slight pyrite

SAMPLE NO.

5-37

5-38

5-39

5-1*0

5-**1

5-1*2

5-^*3

5-**i*

5-**5

5-4*6

WIDTH OF SAMPLE

5.0

5.0

5.0

5.0

5.0

5.0

5.0

5.0

5.0

5.0

Au/ppb319

i*i*5

263

1U

132

8

3

11

70

Au/oz

0.061


DIAMOND D?*ILL RECORDPROPERTY .

TOWNSHIP

.HOLE NO.............84-5..

.PAGE NO. ..................fi..

LOCATION

ELEVATION

CORE LOCATION


DIP ........................

DEPTH ..................

STARTED ......

COMPLETED

DIP TESTS ....

DEPTH FEET/METRES

72*4.8 - 7*43


682.0-687.0 7" intermediate dyke 8 80 0 .moderatelv soft 8, porphvritic like

others; porphyry is fractured withslight pyrite


692.0-697.0 1.2' interned, dvke @ BO 0 as above.

fractured, porphyritic697.0-70*4.0 sil. fractured, 2-1" int. dykes

70*4.0-709.0 1.2' int. dyke li 800

709.0-71*4.0 lightly fractured near perpendicular

to core71*4.0-719.0 3" S 1 1 sections of int. dyke 3 90";

rock becoming darker @ fractures @ *45719.0-72*4.0 darker; 6" brown chert-like rock @

90 0 . some irreg. unite .carbonate

72*4.0-726.8 contact zone

Mafic Conformable Intrusive: f. to m. grained.

dark oreen. moderately soft, havina multiple con

tacts suqgestive of zoned or multiple intrusion;

SAMPLE NO.

5-**7

5-**8

5-**9

5-50

5-51

5-52

5-53

5-5**

5-55

WIDTH OF SAMPLE

5.0

5.0

5.0

7.0

5.0

5.0

5.0

5.0

2. B

Au/ppb

53

22

7

11

10

1*4

11

60

3


PAP. - 1-69

DIAMOND drilLL RECORDPROPERTY .

TOWNSHIP

.HOLE NO...........J&-5..

.PAGE NO. ...........,.,...7,

LOCATION

ELEVATION

CORE LOCATION


DIP ........................

DEPTH ..................

STARTED ....,

COMPLETED

DIP TESTS ....

DEPTH FEET/METRES

7**3


some sections equivalent to dvkes in porphyry;contact knife sharp.END.

SAMPLE NO.

WIDTH OF SAMPLE


PAP. - 1-69

DIAMOND DftlLL RECORDPROPERTY ...............ZQmMO

TOWNSHIP ...............M.a.cl;:..T.8in...Jp.un9Mfl...........................................................................PAGENO. ...............I..

LOCATION ...linR-.1.6.tlQW.. CORE LOCATION


..SB".

ELEVATION

DIP

DEPTH ....................835.!......................BQ core (1 7/16")

STARTED .,...........fB.bruar.yCOMPLETED .......

DIP TESTS ...........

835' -

..|5ji..J9Bf* 2*

DEPTH FEET/METRES

0 - 23t*

21U - 5t*0


Casing (overburden) .

Intermediate to Felsic Amvodaloidal Pillow Lava:

pale to dark green, very hard, pillows UD to

several feet with amyqdaloidal selvaqes; selvaqesmarked by softer dark green chloritic zones,

carbonate, some epidote between pillows; very

occasional large clots of pyrite mostly inselvages.

215. S 'tf." purple otz str. @ kO0

23S.7 W massive pyrite @ ^O0 adjacent to

pillow selvage

251-257 dark green chloritic

320-323.5 fractured with qtz fillinq, minor pv

39^.8-397 19& pyrite in oash fractures

kQt* # " banded qtz in fracture @ 30"

*415.5 1" banded qtz-carb str. @ 3D0 to c. a,

MB 3 " pink qtz-carb in selvage

U39 10" intermediate dyke @ 70-80"

500-50** intermediate black, v.f.gr. banded

SAMPLE NO.

6-52

6-53

WIDTH OF SAMPLE

3.5

2.2

i- : .

Au/ppb

U10

Au/oz

-intrusive @ 80"

Drilled By ..........N.Qr.B.X.. Signed.SHIELD GEOPHYSICS LIMITED

PAP. - 1-69

DIAMOND e ILL RECORDPROPERTY ..........................................................................................................................................HOLE NO..

TOWNSHIP

LOCATION

ELEVATION

CORE LOCATION


DIP ........................

DEPTH ..................

.PAGENO. ...................2......

........... STARTED ......

........... COMPLETED

........... DIP TESTS ....

DEPTH FEET/METRES

51*0 - 5**3

5t.3 - 553

553 - 55**. 5

55*4.5 - 791.6


506.0-51Q.O a s above516 tt" S 2" qtz-carb str. @ 35"Intermediate (Dioritic) Intrusive: qrey-green,

med. grained with diabasic texture; much white

feldspar as lathes in green fibrous matrix, sharp

contacts @ 70" to c. a.

Intermediate to Felsic Pillow Lava: as above

51*3.3 t*" of sheared slightly vuggy qtz @

25" marks fault; little hematized

pyrite

551.5-553 buff green breccia zone (sericitic)

Serpentine: dark bluish, massive, soft, filling

fracture @ 1Q 0 to c. a.

551.2-555.0 #" irreg. qtz str. //ing c. a.

Felsic Porohvrv Dyke: yellowish green to green-

grey, aphanitic, massive with occ. white feldspar

phenocrysts; initial 1.2' shows fine oranular

texture with qhost-like fragments probable

xenoliths; then sharp contact @ 500 ; appears to bt

SAMPLE NO.

6-1

WIDTH OF SAMPLE

3.8

Au/ppb

27

Au/oz

-

actual contact since qtz str. stops at contact.

Drilled By ................................,............................................................... SignedSHIELD GEOPHYSICS LIMITED

PAP - 1-69

DIAMOND DTtlLL RECORDPROPERTY .......................

TOWNSHIP .....,..............

LOCATION ............................................................................

ELEVATION ..................................... ....................................

CORE LOCATION ............................

DIRECTION ......................................

DIP ....................................................,

DEPTH ..............................................

HOI F NO fl*t-6 ^fe

..............................PAGE NO. ....................3.............. ™

........................................ STARTED ................................................................

........................................ COMPLETED ..........................................................

........................................ DIPTESTS ..............................................................


555.0-560.0 *4096 uhite qtz as strs. //ino c. a..

1-296 pyrite as euhedral crystals in

ulrk S fine strs. and seams jnnstly

// to core axis560-56U 1" qtz str. @ 10 0 , 296 pyrite in feu

seams; seams @ 30-1+0 0 cut qtz

56*4-569 flat qtz strs. (#-1") form 2096; some

chlorite along contacts; less than

196 euhedral pyrite

569 - 57*4 a flat chlorite fracture @ 0" S one

@ *45 0 , minor euhedral pyrite

57*4-579 last foot contains irreg. grey

ghostly fractures, some yellowish

secondary mineral on flat fracture

579-561* little darker from ghost-like

fractures @ faded ovoid phenocrysts

5B*4-5B9 ragged irreg. fract. assoc. with

ghost-qtz fillings, late pink ft"qtz str. li *40 0

SAMPLE NO.

6-2

6-3

6-*4

6-5

6-6

6-7

6-8

WIDTH OF SAMPLE

5.0

*4.0

5.0

5.0

5.0

5.0

5.0

Au/ppb

260

9*46

1M

t*

59

Au/oz

.06*4

,0**6

.056 9'


df,DIAMOND DTiILL RECORDPROPERTY ..........................................................................................................................................HOLE NO..............B4-&.

TOWNSHIP ........................................................................................................................................PAGE NO. ...................A.

LOCATION

ELEVATION

CORE LOCATION

DIRECTION ...........

DIP ........................

DEPTH ..................

STARTED ......

COMPLETED

DIP TESTS ....


589.0-594.0 a s above with 3" dioritic dyke @ SO 0

594-62** generally darker (grey) with more

intense fracturing preferably @ 20-30"; euhedral S smeared pyrite on

tight chloritic fractures

594-600 8" S 5" diorite dvkes: moderate

fracturing and ghosty qtz600-605 3" diorite; moderate to good

fracturing assoc. with poorly definet

qtz

605-610 moderate fracturing as above; late

#" qtz str. cuts fractures

610-615 moderate fracturing


619-624 moderate fracturing assoc. with

ghosty otz strs., 1?6 py; obscure VG

in quartz str.

624-629 lioht fracturing at 300 . minor ov:

Mi" qtz str. 3 30"

SAMPLE NO.

6-9

6-10

6-11

6-12

6-13

6-14

6-15

6-16

WIDTH OF SAMPLE

5.0

6.0

5.0

5.0

5.0

4.0

5.0

5.0

Au/ppb

260

34

842

TR6

374

Au/oz

.033

.037

.085

.ofelto-


DIAMOND D3ILL RECORDPROPERTY .

TOWNSHIP

.HOLE NO.........BA-6...

.PAGE NO. ..............5.

LOCATION

ELEVATION

CORE LOCATION


DIP ........................

DEPTH ..................

STARTED ......

COMPLETED

DIP TESTS ....


629.0-635.0 feu fractures @ 1*5-30", minor py635-6W3 feu fractures, tt" qtz str. in fract.

@ 30"

6**0-6U5 moderate fracturing61*5-650 feu fractures

650-65** feu fractures

65^-658 2" arev to black banded qtz str. @3D 0 , black brecciated siliceousmineral at contacts

658-659. B feu fractures

659. 8-66**. 8 mod. fracturing, W q tz str. @ 20"uith some pyrite

66U. 8-667.0 light fracturing

667-672 mod. fracturing, minor fine pyrite

672-676 liqht fracturinq676-681 liqht to moderate fracturing

681-686 mod. fracturing, mostly @ 3D 0 assoc.uith alternating grey S buff green

colour fc #" qtz str.

SAMPLE NO.

6-17

6-18

6-196-20

6-21

6-22

6-23

6-2t*

6-25

6-26

6-276-28

6-29

WIDTH OF SAMPLE

5.05.0

5.05.0

t*. Q**.Q

1.8

5.0

2.2

5.0

t*.o5.0

5.0

Au/ppb

225905

**5

125

3215

5

3t*8

6926

8

Au/oz

.036

.1*70

-l

•'7\~~


PAP - 1-69

LOCATION

DIAMOND DftlLL RECORDPROPERTY ..................................................................... ^

TOWNSHIP ........................................................................................................................................PAGE NO. ....................6.......

............................................................ STARTED ...,..

..............................v............................ COMPLETED

CORE LOCATION


ELEVATION

DIP ......

DEPTH

DIP TESTS


686.0-691.0 feu fractures, 2-#" ghosty Ptz strs.

@ 3D0

691-696 feu fractures

691-733.2 generally lighter buff-green colour

696-701 feu fractures, minor pyrite

701-707 few fractures except in last foot

uhere more assoc. uith 2" qtz str.

@ 3D0

707-712 feu fractures, minor euhedral pyrite712-717 feu fractures S strs. of pink calcite

717-72**. 8 mod. fracturing mostly @ **0 0 , little

pink calcite filling fracture; 5"

diorite @ 90 0

72*4.8-729.8 feu fractures S 1" qtz str. //ing

c. a. , minor pyrite

729.6-733.2 feu fractures; 1X pyrite

733.2-791.8 generally darker to light grey

colour; portions shou a granular

texture

SAMPLE NO.

6-30

6-31

6-32

6-33

6-31*

6-35

6-36

6-37

6-38

WIDTH OF SAMPLE

5.0

5.0

5.0

6.0

5.0

5.0

7.8

5.0

3. ̂

Au/ppb

12

16

3075*.

AU/DZ

.035

.076

.055

.2145

.110

-

.11421. 2.

- ---. '


DIAMOND DfllLL RECORDPROPERTY .

TOWNSHIP

.HOLE NO..............8.1*.-6...

.PAGENO. ....................7..

LOCATION

ELEVATION

CORE LOCATION


DIP ...........,...........

DEPTH ..................

STARTED ......

COMPLETED

DIP TESTS ....



737-71*2 few fractures: ahost-like and ooorlv

defined

71*2-71*7 as above

7^*7-752 as above

752-757 as above

757-762 as above

762-767 as above, 1.2' diorite dyke @ 20"

767-772 as above

770.6-772.7 banded dioritic intrusive: sharp

contacts 9 ^O 0 S 90 0

772-777 verv feu fractures: 2" diorite

intrusive @ 900

777-782 feu fractures; 6" diorite intrusive

@ BO 0


787-791.8 1 1 , 2-6" gabbroic intrusive dykes,

sharp contacts @ 80-50"

SAMPLE NO.

6-39

6-1*0

6-1*1

6-1*2

6-1*3

6-1*1*

6-1*5

6-1*6

6-1*7

6-148

6-1*9

6-50

WIDTH OF SAMPLE

3.8

5.0

5.0

5.0

5.0

5.0

5.0

5.0

5.0

5.0

5.0

5.0

Au/DPb1*30

59

1*25

60

1*1*

69

267

3

?q

1*51*

5

2

Au/oz


PAP - 1-89

DIAMOND cftlLL RECORDBU-6.

B

LOCATION

ELEVATION

PROPERTY ..........................................................................................................................................HOLE NO.....

TOWNSHIP ........................................................................................................................................PAGE NO. ..

..................................................... CORE LOCATION.................................................................... STARTED ......

..................................................... DIRECTION .............................................................................. COMPLETED

..................................................... DIP ^^^^^^^^^^^^^^^^^^^^^^.^.^ D IPTESTS ....

......,............................................. DEPTH ...................................................................................... ..........................

DEPTH FEET/METRES

791.8 - 835

835


Mafic (Gabbroic) Intrusive: med. to dark qreen,

f. to m. grained, layered or banded, chloritic,

rock having sharp contacts; in part epidotized;

possible altered volcanic.

797.D-80Q.2 mostly pink to grey aphanitic felsic

intrusive, individual dykes and mod.

fractured with sharp 9D0 contact

805 V felsic aphanitic dykeEND.

SAMPLE NO.

6-51

WIDTH OF SAMPLE

3.2

Au/ppb

t*

Au/oz


DIAMOND RECORDPROPERTY ................. LTD. . . .........................................................................HOLE NO. .

TOWNSHIP ...............y.3.C.k.l.B!]n JP.un^

LOCATION ...MnB....O.BB.t..

ELEVATION

CORE LOCATION ......M.,.N., R.........Timmins..

DIRECTION ................MMb

DIP ...............................50!!......DEPTH .........................70.0..!...

STARTED ..................Fe.biu.ar.y...26. tCOMPLETED ...........M.a.rJGJl..fl.i..

DIP TESTS .............. 20lB.!...r.. A7".7DD' - U80

DEPTH FEET/METRES

0 - 206

206 - MB

M8 - 662.2



Felsic to Intermediate Amvqdaloidal Pillow Lav/a:

orey-areen, very hard except for selvage zone

which is chloritic, epidotized, and fractured:

uhite.qtz, carbonate in fractures, occ. clots fc

seams of pyrite S vesicles; see holes 8*4-2, 5 fc 6.

262 purple qtz str. //ing core axis

356.^7-36^.0 intermediate (diabase) dyke: dark gre

fine drained uiith sharp chilled

contacts @ BO 0

*416-**17 brecciated

Felsic Porphyry Dyke: liqht qrey-qreen, v.f.or.

to aphanitic, generally massive hard siliceous

rock uith occ. rectangular feldspar phenocrysts;

locally displays faded indistinct banding, upper

contact sharp at 80".

^17.6-^22.8 liqht irreo. fracturing marked by

tiqht chloritic seams and odd grain

of pyrite

SAMPLE NO.

y

7-1

WIDTH OF SAMPLE

5.0

Au/ppb

~ .

3'** V * ' -

, i-"'

, t .

Drilled By .......W.OJJBX.. Signed.SHIELD GEOPHYSICS LIMITED

CAP. - 1-69

DIAMOND DflILL RECORDPROPERTY .......................

TOWNSHIP .....................

LOCATION .............................................................................

ELEVATION ........,..................................................................

CORE LOCATION ..............................

DIRECTION ........................................

DIP ......................................................

DEPTH ................................................

............................HOLE NO. ..........flf*.r.7.................PAGF NO 2 ^ft

...................................... STARTED ................................................................

...................................... COMPLETED ..........................................................

...................................... DIPTESTS ..............................................................


1422.8-1427.8 light Fracturing as above

1*27. B-1459.14 massive uith only 2 or 3 fractures

1457.6-1459.1* moderately soft int. to mafic green

dyke at 80"

1*59. t* -146*4.14 l*" of brecciated fractures @ 90" ,

sliqht pyrite

14 6i4.i*-i4 69.14 light fracturing, slight oyrite

1459.** faded ovoid porohyroblastsi469.**-i475.Q core ground

1475.D-14BO.O light fracturing at about 3D 01*80.0-1485.0 " "

1485.D-149Q.O light to moderate fracturing

1490.0-1495.0 " " " "

1495.0-500.0 mod. fracturinn S bleached to cream

colour, some fractures are graphitic.

slight pyrite assoc. uith fracturing

500.0-506.3 mod. fracturing

508.8-513.8 light fracturing


SAMPLE NO.

7-2

7-3

7-14

7-5

7-6

7-7

7-8

7-9

7-10

7-11

7-12

WIDTH OF SAMPLE

5.0

5.0

5.0

5.0

5.0

5.0

5.0

5.0

6.3

5.0

5.0

Au/ppb

2

3

70

251

388

23

11

151

180

li

871

11

frl ^


DIAMOND DTilLL RECORDPROPERTY .

TOWNSHIP

.HOLE NO...........fi!*-.?...

.PAGENO. .................3,

LOCATION

ELEVATION

CORE LOCATION


DIP ........................

DEPTH ..................

STARTED ......

COMPLETED

DIP TESTS ....



523. 8-528. B mod. fracturing @ 30"


506.3-508.8 dark intermediate to mafic dyke,

contact @ U 5 0

533.8-537.0 1st 1.5' bleached to qrev-uihite

colour, moderate fracturing

537.Q-5U2.0 lioht fracturino

51*2.0-51*7.0 light fracturing assoc. with pyrite

seaming

5^*7.0-552.0 1" qtz str. with sericitic contacts

lling c. a.

552.0-559.0 mod. to good fracturing assoc. with

silicification and pyrite; locally

bleached

559.0-560.2 oreen int. to mafic dyke @ BO0


565.2-570.2 lioht fracturino

570.2-577.0 lioht fracturina

SAMPLE NO.

7-13

7-1*4

7-15

7-16

7-17

7-18

7-19

7-20

7-21

7-22

7-23

WIDTH OF SAMPLE

5.0

5.0

5.0

3.2

5.0

5.0

5.0

7.0

5.0

5.0

6.8

Au/ppb

11

59

151

513

329

700

583

111

22

2

3

. "V

,r;l-

-


PAP. - 1-69

DIAMOND DRILL RECORDPROPERTY .

TOWNSHIP

.HOLE NO. .............QA-?..

,.PAGE NO. ....................f*..

LOCATION

ELEVATION

CORE LOCATION


DIP ........................

DEPTH ..................

STARTED ......

COMPLETED

DIP TESTS ....


577.0-5B2.D light fracturina

582.0-596.5 verv feu fractures

596.5-598.8 one sulphide-filled fracture @ **0 0

598.8-602.1 mod. irreg. fracturing

602.1-607.1 good fracturing mainly @ 3D 0 assoc.

uith silicification i pyrite alongfractures

6D7. 1-612.1 mnrl. frarturing



622.1-627.1 good fracturing asspc. uith silicifi

cation S pv mainly @ 3D0627.1-632.0 lioht fracturina

632.0-637.0 liaht fracturing

637.Q-6**2.0 light to mod. fracturina

6**2. 0-6U7.0 liqht tp mpd. fracturinq

6^*7.0-651.0 good fracturing assoc. with irreg.

silicification B, pyrite along seams

SAMPLE NO.

7-2**

7-25

7-26

7-27

7-2fl

7-29

7-30

7-31

7-32

7-33

7-3**

7-35

7-36

WIDTH OF SAMPLE

5.0

2.3

3.3

5.0

5.n5.0

5.0

5.0

5.0

5.0

5.0

5.0

**.o

Au/ppb

t*

266

5

55

5

38

26

59

10

1*5

t* t*

l*

77



TOWNSHIP

LOCATION

ELEVATION

CORE LOCATION


DIP .................;......

DEPTH .................,

.HOLE NO.........of*.-/............

.PAGENO. ...............5...........

........... STARTED ......


........... DIP TESTS ....

DEPTH FEET/METRES

662.2 - 700

700


651.0 657.0 (good) heavy fracturing causing

bleaching S silicification; main

fracturing @ 3D0 ; minor pyrite

657. 0-660. t* liqht to mod. fracturina: but

bleached

Felsic to Intermediate Amvqdaloidal Pillow Lava:

as above.

697.3-698.9 mafic (diabasic) dyke

END.

SAMPLE NO.

7-37

7-38

WIDTH OF SAMPLE

6.D

3. i*

Au/ppb

37. *

18


PAP. - 1-69

DIAMOND DHILL RECORDPROPERTY .......E.Q!!1.INEX..L1P.A ................................................................................................HOLE NO...........84.-Q.................

TOWNSHIP .....^a.cMe.m. Jpu^ .................1................

LOCATION .......L ine....l6 30...Ljest.................................. CORE LOCATION J.3.k...W.axahnURB...^....AirpDrt STARTED ...........MSMlbL.......*..

.............................S.t.a..t.ion..3.l04...Sout.h......................... DIRECTION ..............S.Q.u.th....CaB.t.,.)..........?.o..a..d......... COMPLETED .....Mar.ch....19.^

.............................frnietric...^^!]:!.)........................................ DIP ...........................6.1^........................................................ DIPTESTS .........25.Q.!....-..6.rELEVATION ................................... ............................................ DEPTH ...,................75.Q..'.......(.BQ..l..Ag.).

DEPTH FEET/METRES

0 - 209

209 - 750


Casino (overburden) .

Felsic Porphyry Dyke: liaht arev to areen. hard.

uith uhite feldspar phenocrysts: initially rock is

variably rusty after minor pyrite S core is broken

209-215 rock is bleached to cream colour from

grounduiater

251-26*4 rock is bleached to cream colour from

grounduater

209-215 bleached uiith rust spots after pyrite

215-220 sliaht pyrite

220-222.9 partially bleached S 1" qtz atr. @ 80

222.9-231.5 bleached S feu fractures

226.4-230 core lost

231.5-236.0 feu fractures; 2 #" qtz strs. @ BO0

236.0-241.6 core broken after fractures241.6-246.0 2" qtz str. 9 800

2^6.0-251 moderately fractured

251-256 bleached uith rusty spots

256-260 bleached S fractured uith rust spots

SAMPLE NO.

B-1

8-49

1 8-2

8-3

8-1*

8-5

8-6

8-7

8-8

8-9

WIDTH OF SAMPLE

6.05-0

2.9

8.6

4.5

5.6k.k5.0

5.0

4.0

Au/ppb

.

9U6

636

69

420

365

713

Au/oz

0.004

0.07D

0.024

0.139

Drilled By .,Ir.adl ley.Brosi. Signed.SHIELD GEOPHYSICS LIMITED

DIAMOND RECORD

LOCATION

ELEVATION

PROPERTY ,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,, HOLE NO. .......Slf-.B.............

TOWNSHIP ........................................................................................................................................PAGE NO. ............,2......,,.,

,,,,....,,.,,,,,,,,,,,,,,,,,, CORE LOCATION ,,,..,,,,,,,,,,,,,,,,,,,,,,,,.,,,.,, STARTED ......

,,..,....,.,,,.,,,,,,,,,,,,,,,, DIRECTION ,,,..,,,,,,,,,,,,,,,,,,,,,,,.,,,,,.,,,,,, COMPLETED

,.,,....,,,,,,,,,,,,,,,,,,,,, DIP ..,,,.,,,...,.,,.,..,,..,,,..,,...,.,,,,.,.,,,,,,,,,,,,, DIPTESTS ,,

,,,.,....,,,,,,,,,,,,,,,,,,,,. DEPTH ,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,.,,.,.,,,. ..........................


260-265 bleached S fractured mainly @ SO0 .

rust soots

272. 1-275. t* core broken: mafic dark green

intrusive

275.^4-279.2 felsic porphyry

279.2-2B5.5 core broken; mafic dark qreen

intrusive

291-296 2" banded gtz str. @ b 5 0

296-300 mostly intermed. light green int.;

contacts partially X/ c. a.

296 core size changes from BQ to AQ

because of problem uith casing

309-312.3 some bleaching S fracturing @ 70"

321-327 bleachino fc fracturino @ 70 0 . sli.

pyrite

338-3*43.5 1" fc 2" gtz str. li 75 0 , feu fractures

slight pyrite

359 1" qtz str. @ 900

365.8-370.8 mod. fracturing, 1" qtz str. @ 700

SAMPLE NO.

8-1D

8-11

8-12

B-13

, 8-U

8-15

WIDTH OF SAMPLE

5.0

5.0

3.3

6.0

5.5

5.0

Au/ppb

(*61

27

128

622

Qkk

Au/oz

.026 ,


PAP - 1-69

LOCATION

ELEVATION

DIAMOND D~ ILL RECORDPROPERTY...........................................................................................................,................^

TOWNSHIP ........................................................................................................................................PAGE NO. ................3..........

,.................................................... CORE LOCATION.............................,..................................... STARTED ......

..................................................... DIRECTION ..................................,.......................................... COMPLETED

..................................................... DIP .................™........TO....^.........™TO..OT...............™.™.... DIPTESTS ....

,.................................................... DEPTH ..................................................................,................... ..........................


370.B-375.8 lioht fracturinq

393.5-39^ crumblv liaht areen int. intrusive S t*1*05 colour chanqes from qenerallv light

to med. grey-greenli t*5-**50

1*50-1*53 grey silicified, feu fract., sli. py1*53-1*58

t*96.5-501.5 1" brecciated qtz str. @ 3D0 followed

bv moderate fracturing501. 5-501*. 5 few fractures, slight pyrite

513 2" qtz str. @ 7Q 0

521.2-525.2 moderate fracturing over about a foot

@ 3D0 , slight pyrite

532.5-537.5 vuqqv pink qtz strs. @ 80* i 1 " qtzstr. @ 8D0

51*7-551 qtz str. @ 80", few fract., sli. py

551-553 1" qtz str. @ 70"

56^-569 silicified fract. following core,

mod. fracturing, slight pyrite

SAMPLE NO.

8-165 e

8-50

8-17

8-51

8-18

8-19

8-20

8-21

8-22

8-23

6-2(4

WIDTH OF SAMPLE

5.0

5.0

3.0

3.0

5.0

3.0

l*.0

5.0

1*.0

2.0

5.0

Au/DDb

260

233

796

651

590

kkB590

Au/oz

.032

.012

.060

.001*


DIAMOND cfilLL RECORDPROPERTY ..........................................................................................................................................HOLE NO........8f?.-B.

TOWNSHIP ........................................................................................................................................PAGE NO. ............A.

LOCATION

ELEVATION

CORE LOCATION


DIP ........................

DEPTH ..................

STARTED ......

COMPLETED

DIP TESTS ....

DEPTH FEET/METRES FORMATION - MINERALIZATION56 o.o -584.."?

58U.7-590.0 feu fractures. 1" qtz str. @ 80 0 .

sliaht pyrite

590-593 1" E 2" qtz str. S 70 0 . 196 pyrite

600 1" qtz str. S 75 0

601.2 1" pink vuqqy qtz str.

610-615 feu fractures S 3" qtz str. @ 75".

some pyrite

615-620 feu fractures mostly @ 7Q 0

620-625 3" qtz str. @ 70", feu pyritized

fractures

625-630 2" qtz str. 8 70". feu pyritized

fractures

630-635 3" qtz str. @ 70 0 , feu pyritized

fractures635-6^0 2 1" qtz strs. @ 70 0

6*40-6^5 3 1" qtz strs. @ 70 0 , sli. diss. py

6^5-650 3", 1" qtz strs. @ 70", feu pyritized

fractures

650-656 silicified fc bleached irregularly;

SAMPLE NO.

a -52.8-25

8-26

8-27

8-28

8-29

8-30

8-31

8-32

8-33

8-31*

8-35

WIDTH OF SAMPLE

4-- T5.3

3.0

5.0

5.0

5.0

5.0

5.0

5.0

5.0

5.0

6.0

Au/ppb

5in(.Qia

B97(.026

Au/oz

:1II!I.038

.026

.108

.026

.020

.050

.052

.076

Product

.51*

.13

.10

.25

.13

.26

.456.

.108/5

slight pyrite


DIAMOND D3ILL RECORDPROPERTY ..........................................................................................................................................HOLE

TOWNSHIP ........................................................................................................................................PAGE NO.

LOCATION

ELEVATION

CORE LOCATION


DIP ........................

DEPTH ..................

STARTED ......

COMPLETED

DIP TESTS ....


656.0-661.0 uell fractured mainlv @ 3 5". qrev to

areen colour

661-666 B" qtz str. @ 70", intersectinq str.

@ 1D0 contains 5 showings of VG all

uithin euhedral pyrite; moderately

fractured mainly @ 35-l*0 0

666-671 uell fractured S silicified, sli. py

671-676 silicified, feuer fractures

676-681 2" S 6" qtz str. @ 7D 0 , feu pyritizec

S chloritic fractures

681-686 3 1" qtz strs. P 7D 0 , 1" pink qtz

str. @ 70 0 , moderately uell fracturec

3" pyritized black chlorite

686-688 1' of chlorite-qtz marking probable

fault (i 3D 0 , 6" qtz str. @ **0 0 , sli.

pyrite

688-693 moderate fracturinq, 10" qtz str.

uith seam at bottom marked bv crumbly

chlorite

SAMPLE NO.

8-36

8-37

8-38

8-39

8-1*0

8-M

t

8-1*2

8-**3

WIDTH OF SAMPLE

5.0

5.0

5.0

5.0

5.0 -

5.0

2.0

5.0

Au/ppb Au/oz

.060

jljlgt.79

'nw- 052.030.082 n ap.0^0

.0^*2

.026

.011*

Product

.30

23.95

.26

.15

.1*3

.21

.052

.07

-

62D

.328B5'

705

.105 mi-85 to lo}


PAP - l 69

DIAMOND D&ILL RECORDPROPERTY .

TOWNSHIP

LOCATION

ELEVATION

CORE LOCATION


DIP ........................

DEPTH ..................

.HOLE NO........B.ft.-B............

.PAGE NO. ..............f?.............

........... STARTED ......


........... DIP TESTS ....

DEPTH FEET/METRES

750


693-698 2" S 7" atz str. @ 700 . rustv ov/rite:

last 2 1 silicified

698-705 3". 1" qtz stra.. partiallv silicif.:156 pyrite

705-710 2 1" R t*" atz strs. 9 70": 2' of

silicif.. less than 196 pyrite


720 B" of silicification

726-731

731-736 2" 8, 2 *" atz strs. @ 70 e . some

fracturing. 1X oy representative of

remaining core

736-7M

END.

SAMPLE NO.

8-^

8-1*5

8-1*6

8-1*7

8-53

8-1*8

8-51*

WIDTH OF SAMPLE

5.0

7.0

5.0

5.0

5.0

5.0

5.0

Au/ppb919

836

609

Au/oz

050

-Mb nu, nt*n gU^u

.028

.092

.030

-


PAP. - I-69

DIAMOND D" ILL RECORDPROPERTY .

TOWNSHIP

..8A-9. 1

LOCATION

ELEVATION ...3.a.!!!.6...a.8...8(t.-8..

CORE LOCATION J.?A. JajrjS.hoUBB..-.


DIP ............................SI*.

DEPTH .......i...........

STARTED .........Mar.ch....1.Q.i...l9.6A.

COMPLETED ...M.a.r.C.h....20.. t.....19.B(4.

DIP TESTS ........l 50.!....-.. 6.3.'.............

DEPTH FEET/METRES

0 - 15D

150 - 981


Casinq (overburden).

Felsic Porphvrv Dyke: lioht oreen to orev. hard

with uihite feldspar phencorvsts; rock is fracturec

having numerpus well defined and shadowy (pporly

defined) qtz stringers; mpst pyrite in uallrock;

quartz as silicification along tight central

fracture or well defined stringers @ 70 to 80" to

c . a .

150-156 core is badly broken with minor oy156-161 as above uiith t* tt" qtz strs. @ 90".

^ pyrite

161-167 i* #"-1" qtz strs. mainly @ t*5 0

167-172 2" a k tt" qtz strs. @ 50-300

172-177 k K" q tz strs. @ 500 -30 0 , ali. PVJ

secondary yellou mineral on 25" slip

planes

177-182 6 tt" qtz strs. mainlv @ 700 . 196

rusty pyrite

182-187 2 Vi" q tz strs.

SAMPLE NO.

-

9-1

9-2

9-3

9-t*

9-5

9-6

9-7

WIDTH OF SAMPLE

6.0

5.0

6.0

5.0

5.0 -

5.0

5.0

Au/ppb

125

885

260

500

670

672

67

Au/oz

Drilled By ..........N.9.r.B.x. Signed.SHIELD GEOPHYSICS LIMITED

DIAMOND DttlLL RECORDPROPERTY .

TOWNSHIP

.HOLE NO......8f*r.?...

.PAGE NO. ...........2.

LOCATION

ELEVATION

CORE LOCATION ,..

DIRECTION .............

DIP .............,............

DEPTH ....................

STARTED ......

COMPLETED

DIP TESTS ....


187-192 almost ^096 silicification @ 9D 0 -250 .

minor pyrite

192-197 6 y*" qtz strs. mainly @ 70"

197-202 2D% silicification, feu qtz strs.,

196 pyrite

202-207 3 M." qtz strs., 196 pyrite, partially

bleached

207-212 well fractured, 2096 silicif. as

irreg. strs.; 196 rusty pyrite

212-217 mod. fracturino. 6 Vi" to }fe" qtz strs.

196 rusty pyrite

217-221.5 broken core

221.5-226 1" rusty qtz str.

226-230.5 2096 silicif. mainly as qtz strs. @t*6 0

230.5-235 feu fractures, 1" qtz str.

235-239.5 1" qtz str. @ BO 0

239.5-2^1.3 5096 silicif. alono fractures i 35 0 .

sliqht pyrite

SAMPLE NO.

9-8

9-9

9-10

9-11

9-12

. 9-13

9-K*

9-15

9-16

9-17

9-18

9-19

WIDTH OF SAMPLE

5.0

5.0

5.0

5.0

5.0

5.0

t*. 5

t*. 5

li. 5

t*. 5

l*. 5

1.8

Au/ppb

681

1*52

676

271.

370

158

385

995

88

388

78

Au/oz

.Ok


PAP . 1-69

DIAMOND [ftILL RECORD

TOWNSHIP .....................

LOCATION .............................................................................

ELEVATION ............................................................................

CORE LOCATION .............................

DIRECTION .......................................

DIP .....................................................

DEPTH ...............................................

..............................PAGENO. ..............3.....................

....................................... STARTED ..........................

....................................... COMPLETED ....................

....................................... DIP TESTS ........................

9


24*1.3-24*6.0 few fractures 8 35 0

2^*6-253 12 fractures or atz strs. S 70-300 .

some pyrite

253-257.5 fractured, silicified S rusty; qtz

strs. are vuggy, 196 pyrite

257. 5-264*. 0 fractures 8. narrou qtz strs. are

vuggy, sli. rusty pyrite

262.5-264* core lost

264*-269 10" of irrea. qtz S vuoqy fractures

269-274* ix rusty pyrite

274*-280 rusty, feu fractures 8 20 0 with

silicification

280-286.8 qrey-cream colour after silicif icatio

throughout S pyritized black graphiti

fractures mainly at O0

286.8-289.8 uell fractured, slight pyrite

289.8-292.0 dark diabase dyke at l*5 0

292-297 moderately fractured, slight pyrite

297-303 lightly fractured

SAMPLE NO.

9-20

9-21

9-22

9-23

9-2**

9-25

9-26

i 9-27

:

9-28

9-29

9-30

WIDTH OF SAMPLE

t*. 7

7.0

4*. 5

6.5

5.0

5.0

6.0

6.8

3.0

5.0

6.0

Au/ppb

623

376

211*

1*02

1*66

579

352

391

773

Au/oz

.086

.096

086/4*. 7'

.096/6.8'


P.A.P. - 1-69


TOWNSHIP

.HOLE NO........S(t.rl.

.PAGE NO. ............A.

LOCATION

ELEVATION

CORE LOCATION


DIP ........................

DEPTH ..................

STARTED ......

COMPLETED

DIP TESTS ....


303-3Qfl lightly fractured

308-313 lightly fractured

313-318 5 V atz strs. @ 50-8D0 . 196 nyrite


322-337 feu fractures fc narrou qtz strs.,

sli. pyrite

337-31*2 3 1" qtz strs. @ 900 , sli. pyrite

350.7-357.0 feu irrea. fractures

367-372.5 feu fractures, little silicification

372.5-395 feu fractures, little silicification

395-i*00 variably silicified, 2 #" qtz strs.,

sliqht pyrite

f*QQ - t*05 feu irreg. fractures, variably

silicif .

**05-t*1Q moderate fracturing with silicif.

MO-MS 2" qtz str. @ 900 , moderate

fracturing

i*15-t*21.*4 variably silicified odd fracture.

sliqht pyrite

SAMPLE NO.

9-31

9-32

9-33

9-3U

9-35

9-36

9-37

9-38

9-39

9-i*0

9-M

9-U2

WIDTH OF SAMPLE

5.0

5.0

5.0**.Q

5.0

6.3

5.5

5.0

5.0

5.0

5.0

6.U

Au/ppb

59

1*59

152

515

122

276

267

96

i*57

255

Au/oz

.056

.036


PAP. - I-69

DIAMOND D3ILL RECORDPROPERTY .

TOWNSHIP

.HOLE NO........8.{*.-9...

.PAGENO. ..............5.

LOCATION

ELEVATION

CORE LOCATION


DIP ........................

DEPTH ..................

STARTED ......

COMPLETED

DIP TESTS ....


42 1.4-1*49. 5 feu fractures, odd qtz str.

448-449.2 inter, lioht areen dvke @ UQ0449.5-455.0 feu fractures S pink calcite strs.

@ 900

455-467.5 feu fractures and qtz strs.

467.5-472.5 4 fractures and qtz strs.

472.5-477.5 4 #" to 1" qtz strs. @ 8D0 , sli. py

k 77. 5-480. U 2 " BO 0 atz str. cuts W s tr. S 1 00 .

196 pyritei*8D.if-U83.9

'463.9-^88.9 feu fractures filled bv irreq. qtz

i*88. 9-^*92.0 feu fractures

^92-1*97 well fractured, sericitization,

silicification 8, qtz strs. @ 8Q 0 ,

IK pyrite*497-5D2 few fractures S 3" qtz str. @ BO0

502-507 2 1" qtz strs. i BO 0 , mod. fracturing

bleaching, 19o pyrite

507-512 feu fractures R strs. mainlu @ 80"

SAMPLE NO.

9-t*3

9-i*t*

9-**5

9-^*6

9-i*7

9-U8

9-U9

9-50

9-51

, 9-52

9-53

WIDTH OF SAMPLE

5.5

5.0

5.0

2.9

3.5

5.0

3.1

5.0

5.0

5.0

5.0

Au/ppb

162

30

717

236

(*8

1*55

699

747

398

Au/oz

.054

.068

054/2.9'

.068/5'


DIAMOND DrtlLL RECORDPROPERTY .

TOWNSHIP

.HOLE NO. ....8{*-?..

.PAGE NO. ..........1.

LOCATION

ELEVATION

CORE LOCATION


DIP ........................

DEPTH ..................

STARTED ......

COMPLETED

DIP TESTS ....


512-517 1" qtz str. S feu fractures @ 80 0

517-522 feu fractures @ BO 0522-527 feu fractures

527-532 silicified, few fractures, 196 pyrite532-537 silicified, feu fractures

537-51*2 feu fractures S strs. @ BO 05*47-552 2" qtz str. @ 70", feu fractures,

little silicif.552-557 2 1" qtz str. @ BO 0 , sli. pyrite557-562 some silicif., sli. pyrite562-567 3.5' silicified (bleached), k W

qtz str. @ BO"; 196 pyrite

567-572 3-1". 5" qtz strs. @ 75". 1ft pyrite572-577 feu fractures @ 75 0577-562 1*-1" qtz strs. @ 70 0 . sli. pyrite582-587 3-1" qtz strs. @ 70-50", 6 M silicif.

slight pyrite, chlorite seam587-592 2" qtz-chlorite, 9" qtz str. @ 70",

slight pyrite

SAMPLE NO.

9-5**

9-55

9-569-579-58

9-59

9-60

9-619-629-53

9-61*9-65

9-669-67

9-68

WIDTH OF SAMPLE

5.0

5.0

5.05.05.0

5.0

5.0

5.05.05.0

5.05.0

5.05.0

5.0

Au/DDb

59310

119513

2U681*

J62C.016

381

9601*1*1*

699

Au/oz.030

.01*6

.062

.01*8

Product

?T. C. J

.08

.

.21*

JU320 Y


PAP -1-69

DIAMOND Df(ILL RECORDPROPERTY..................................................................................................................................™

TOWNSHIP ........................................................................................................................................PAGE NO. ..............7.

LOCATION

ELEVATION

CORE LOCATION


DIP ........................

DEPTH ..................

STARTED ......

COMPLETED

DIP TESTS ....

DEPTH FEET/ METRES FORMATION - MINERALIZATION

592-597 1" qtz str. Q SO 0 , mod. fracturino

597-602 mod. to well fractured: tioht

chloritic fractures

602-667 dirty disuniform grey colour from

chlorite

602-607 6" silicif. followed by heavily

fractured S silicif. zone which is

grey colour after chlorite, ali. py

607-612 heavily fractured S silicif. orey

chloritic zone: 3". 1" R 8" otz strs.

S 70". sli. ovrite

612-617 as above S 2" qtz str. @ 70 0 . sli. ov

617-622 as above

622-627 1", 2 fc" qtz strs. 8 75 0 ; moderately

fractured @ 20" t 70"

627-632 2" K 1' qtz strs. 8 700 , moderately

fractured @ 700 , slight pyrite

632-637 moderately fractured, sli. pyrite

635.5-637 core ground

SAMPLE NO.

9-69

9-70

9-71

9-72

9-73

9-7**

9-75

9-76

9-77

WIDTH OF SAMPLE

5.0

5.0

5.0

5.0

5.0

5.0

5.0

5.0

5.0

Au/ppb

521

591

380

521

687

500

Au/oz

.01**

.018

.028HVB .U6b .nflfl.nflt.

.020

.020.020

.013

.066 5'


DIAMOND d&ILL RECORDPROPERTY .

TOWNSHIP

LOCATION

ELEVATION

CORE LOCATION


DIP ........................

DEPTH ..................

.HOLE NO........B(*.-?.............

.PAGE NO. ..............B..............

........... STARTED ......


........... DIP TESTS ....


637-6^*2 light tn mod. fracturing

6f*2-6**7 light to mad. fracturing T rusty after

pyrite in last foot

6U7-652 2" fc 10" qtz str. @ 70 0 . well

fractured, slight pyrite

652-657 3", 3", 5" qtz strs. @ 70 0 , fractured

to brecciated; oldest fracture at 3D0

?; angular fragments in grey-green

matrix; good VG in 5" white qtz

657-662 fractured to brecciated; most

prominent @ 30"

662-667 moderate fracturing, slight pyrite

667-672 V qtz str. @ BO 0 , light fracturing,

slight pyrite

667 colour changes from grey to pale gree

with odd fracture fc qtz str. R

slightly diss. pyrite; pale green

colour seems to result from bleaching

672-677 light to mod. fracturing

SAMPLE NO.

9-78

9-79

9-8D

9-81

9-82

9-83

9-BU

T

9-85

WIDTH OF SAMPLE

5.0

5.0

5.0

5.0

5.0

5.0

5.0

5.0

Au/ppb

351

166

58**

211

932

BBt*

265

Au/oz

.GOB

.not*

.020

.(*6B ,, .LVL -M

.010

.030

.037

Product

.10

i 2.23

.05

.15

.185

.^6

0.13zu-

.03310'


PAP - I-69

DIAMOND D^ILL RECORDPROPERTY .

TOWNSHIP

. HOLE NO........6!*-3..

.PAGE NO. .............?...

LOCATION

ELEVATION

CORE LOCATION


DIP ........................

DEPTH ..................

STARTED ......

COMPLETED

DIP TESTS ....


677-682 1" qtz str., feu fractures, sil. pv

6B2-6BU 3" a 3-1" qtz strs. @ 70*

695-697 3-1" qtz strs. @ 80*

712-717

717-720.1 light fracturing, alight pyrite

720.1-725.1

737.5 2" qtz str. @ 70"71*2-71*7

71*7-752 3" qtz atr. 8 70", 1-2X diss. pyrite

752-757 mod. fract.. mainly @ O0 . 1-2* DU

757-760 aliqht fracturing

760-799 colour chanqea to mainly roed, qrey

with local pala green bleached section795.2-797 well defined fract. @ 1*5* over 6"

filled with qtz; ulrk bleached to very

799-802 irreo. qtz str. oenerallv //ino c. a.with tourmaline

799 pale green colour

836-81*1 feu fractures causing cream bleaching,

SAMPLE NO.

9-86

9-99

9-87

9-100

9-1019-88

9-89

9-90

9

9-91

pale pi9-92

9-93

WIDTH OF SAMPLE

5.0

5.0

3.1

5.0

5.0

5.0

5.0

3.0

1.8

nk

3.0

5.0

Au/ppb610

218

3^4

71

106

521

Au/oz

.030

.062

-Tflfl* —

.008

.060

'slight pyrite

Drilled By Signed.D GEOPHYSICS LIMITED

PAP. - I-69

DIAMOND DTitlLL RECORDPROPERTY ..........................................................................................................................................HOLE NO........flk-9...

TOWNSHIP ........................................................................................................................................PAGE NO. ............ID...

LOCATION

ELEVATION

CORE LOCATION


DIP ........................

DEPTH ..................

STARTED ......

COMPLETED

DIP TESTS ....


8U2- 1.2' intermed. dvke at 3D0

8^*3-857 feu patchv roed, arev zones: suoaest

that pale preen colour is a product

of hydrothermal alteration

662-667 feui fractures mainly along c. a.

causing silicif; slight pyrite

B91.5-B93.5 porphyritic, hard, dyke @ **0 0

B9*t vuggy fractures with tiny qtz

crystals

897-912 colour little darker because of

incipient fractures and less bleachin

9D7-912 incipient tiaht fractures, sli. ov

912-917 feu fractures causing silicif. uith

little pyrite

928.6-935.1 mod. tight fracturing, slight pyrite

960-962 grey intermed. dyke @ **0 0

965-966.5 grey intermed. dj/ke @ **D 0966.5-971.5 pyritized fractures adjacent to dyke

rock which //s c. a. for a foot

SAMPLE NO.

9-9*4

j9-95

9-96

9-97

9-9B

WIDTH OF SAMPLE

5.0

5.0

5.0

6.5

5.0

Au/ppb

825

562

775

551

775

Au/oz


DIAMOND D^ILL RECORDPROPERTY.........................................................................................................................................

TOWNSHIP ........................................................................................................................................PAGE NO. 11

LOCATION ....................

ELEVATION ..................

DEPTH FEET/METRES

981

............................................................... CORE LOCATION ....................... .......... ...

............................................................... DIRECTION ..............................................

..,........................................................... DIP . ...........................................................

................................................................ DEPTH ......................................................


971.5-981.0 feu incipient fracturesEND.

SAMPLE NO.

WIDTH OF SAMPLE

STARTED ...

COMPLETED

DIP TESTS .

) ......................

•Vr


DIAMOND Cft ILL RECORDPROPERTY ,.........P.P.M.IJ!J.E.X....L!P........^^

TOWNSHIP

LOCATION ......L..in.B..16.t3p.,.UIest......

..T.Pyn8hip..................................................................................pAGENO.

CORE LOCATION*?.!? Warehouse -Airport - ^ t ^ . Road

DIRECTION .............Sp.g.th....(;.ag.t;.,J...............................

1

..........................Jmetric..^!:!^.!.ELEVATION ....B.amB. as. 6i*-6....

DIP ......DEPTH

..5.0.?..

STARTED ..........

COMPLETED .......M.a.r.c.h...2A,....

DIP TESTS ............2.2.Q.!... -....5.5.?.

DEPTH FEET/METRES

D - 217.5

217.5 - 691*



Felsic Porphvrv Dyke: qray to pale green,

aphanitic, very hard uith white feldspar pheno-

cryats, tight chloritic fractures at variousangles; may or may not bs filled uith pyrite or

form the loci for silicification.

217.5-222.5 modsratslv fractured at l*5 0 uith

silicif., some pyrite222.5-227.5 1" qtz str., feu fractures mainly

at BO 0

21*2.2-21*7.2 2-1" otz atrs. @ fl0 0 f moderate

silicified fracturing; SO0 fracture

later than 3D0 fractures

273.5-275.5 1" Qtz str. @ 80". 3" of fractures @

l*5 0 . slioht pyrite

278. 3-261*. 3 3" qtz str. S 700 . feu fractures

filled uith qtz-carbonate, ali. rusty

pyrite

292-296 dirty grey colour after chlorite

SAMPLE NO.

10-1

10-2

10-3

10-1*

10-5

WIDTH OF SAMPLE

5.0

5.0

5.0

2.0

6.0

Au/oz

0.021*

0.010

0.051*

0.031*

0.011*

.051*75

dissemination

Drilled By ......BTMJ,.e..y...8rO8..................... SignedSHIELD GEOPHYSICS LIMITED

DIAMOND Df ILL RECORDPROPERTY..........................................................................................................^

................................................................................................................................PAGE NO. ................2.TOWNSHIP

LOCATION

ELEVATION

CORE LOCATION


DIP ........................

DEPTH ..................

STARTED ......

COMPLETED

DIP TESTS ....


303.0-306.0 fc" atz-carb stra. @ 200 : 2" atz str.@ BO0 , sliaht ovrite

327-332 moderate fracturing, 5" qtz-chlorite

@ 35", slight pyrite

338 1" qtz str. S 70"

366 zone of rusty weathering after

ankerite 7

366.5 2" Qtz str. 0 700

372 fc" qtz str. 0 600

1*01-1*07.5 dark qrevt fairly soft, generally

massive rock having amygdaloids;

contacts sharp at 700 fc (*5 e , possible

pillow lava equivalent to hanging

uall unit

i*11. 1-1*13. 6 lighter grey but same as above.

contact sharp at 1*0*

1*28.5-1+39.0 as above but contacts at 3D0

1*1*7. 2-1*5**. 0 mafic grey f. or. dvke at 30"

i*5i*-i*59 6" ailicif. at start and slioht

SAMPLE NO.

10-6

10-7

10-7A

WIDTH OF SAMPLE

5.0

5.0

5.0

Au/oz

0.010

0.022

0.001* -

fracturing at 70-30"


DIAMOND DrULL RECORDPROPERTY .

TOWNSHIP

.HOLE NO..........fi!*.-1.0.

.PAGE NO. ...................3..

LOCATION

ELEVATION

CORE LOCATION


DIP ........................

DEPTH ..................

STARTED ......

COMPLETED

DIP TESTS ....


** 57-500 rock contains tiny ovoid greenDhenocrysts or oorohyroblasts

U73-t*76 6" silicif.. 1" qtz atr. 9 SO0 , few

fractures, slight pyrite

1*97.5-502.5 partially bleached, feu fractures

502.5-507.5 1' of fractured silicif.. oood

splash of VG in GO0 fracture, sli.py507.5-512.5 4" of silicif., few incipient

fractures, sli. py, 1" qtz-chloritestr. at 500

512.5-516.0 few fractures at 3D0

516-521 few fractures, slight pyrite

502.5-586 generally dirty grey-green colour.

variably chloritic, fractured

throughout, few qtz strs. and variablpyrite content

521-526 2*6" sections of intense chloritic

fracturing @ **5 0 with silicif. t sli.pyrite

SAMPLE NO.

10-B

10-9

10-10

10-11

10-12

10-13

10-U

WIDTH OF SAMPLE

5.0

5.0

5.0

5.0

3.5

5.0

5.0

Au/oz

0.036

0.020Q.M5

0.02U

0.006

0.018

0.016

Product

.10

2.225

.12

-

.16315'


LOCATION

DIAMOND DftlLL RECORDPROPERTY ...................................,.................^^

TOWNSHIP ..........................................................................................................................^ . .................k........

...............,.......................................... STARTED ......

............................................................ COMPLETED

............................................................ DIP TESTS ....

CORE LOCATION


DIP .........................

ELEVATION DEPTH


526.0-531.0 moderate fracturino Q 70-450531-536 1" qtz str. @ 80", 50* silicif. after

incipient fractures, alight pyrite536-5t*1 uiell fractured S silicified, It py

51*1-51*6 3 tt" atz stra. @ BO 0 . 1" chlorite@ 70 0 : moderate fracturing. ^ % pyrite

51*6-551 mod. fracturino @ 40 C -B0 0 . silicifiedslioht pyrite

551-556 mod. fracturing @ 80* fc 1" qtz str.,slight pyrite

556-561 moderate fracturing @ 40-80 0

561-566 moderate fracturino @ 4 0-800 . 6"ailicif.

566-571 moderate fracturing571-576 2' of dyke 7 @ 40" including 1' of

chlorite; last 1.5* well fractured 9700 a silicified

586-694 colour changes to pale green r less

fractured, odd well defined Qtz str.

SAMPLE NO.

10-1510-16

10-17

10-18

10-19

10-20

10-21

10-22

10-2310-24

WIDTH OF SAM RLE

5.0

5.0

5.0

5.0

5.0

5.0

5.0

5.0

5.05.0

Au/oz

n.nnuD. 269

0.008

0.014

n.nifl

n.024

0.008

0.004

0.002

0.002

t

269/5

@ 700


LOCATION

ELEVATION

DIAMOND DTtlLL RECORDPROPERTY.................................................................................................................................

TOWNSHIP ........................................................................................................................................PAGE NO. ................5..........

,................................................... CORE LOCATION.................................................................... STARTED ......

..................................,................. DIRECTION ....,........................................................................ COMPLETED

,.................................................... DIP ............................................................................................ DIPTESTS ....

..................................................... DEPTH ...................................................................................... ..........................


576.0-581.0 fractures cone. 9 1*Q 0 fc SO 0 . 1X oy

5S1-5B6 moderate fracturing 8 800

586-591 3" * 1" atz str. @ 800 r mod.

fracturlna, silicif., 196 pvrits

591-595.5 l*" atz str. @ BO 0 , mod. fracturing

595.5-597.5 1" i 2" atz str. 8 75 0 . sil. ovrite

597.5-601.5

601.5-607.0

601 2" qtz-chlorite str. S l*50

607-612 2' i 1" otz strs. Q 75 0 . feu chl.frac


616-621 2-2" qtz strs. 8 75 0

621-626 2-W q tz strs. 8 700 , good splash VG

in pyrite cube

626-631 3" qtz str. 8 75 0 , few fractures631-636 1" atz str. 8 75*. slight pyrite636-61*1

61* 1-61*1*. 6

6**i*. 6-651. 7 2-2" qtz strs. 8 75*. feu fract.sli.p

SAMPLE NO.

10-25

10-26

10-27

10-28

10-2910-1*1*

10-1*5

t. 10-30

10-31

10-32

10-33

10-31*

10-3510-1.6

10-1*7

M 1 0-36

WIDTH OF SAMPLE

5.0

5.0

5.0

1*.5

2.01*.0

5.5

5.0

A.O

5.0

5.0

5.0

5.0

5.0

3.6

7.1

Au/oz

0.026

0.031*

0.031*

0.056

0.127

0.021*

0.01*2

0.01*8

0 O1'i0.028

0.057

0.01*2

0.107

0.092

0.026

0.038

576

PHobUCT

O.'*

• ir• 17

.z*,z

.254

.096

• 231

• Z4-

.056

.14-

.285

•Zl

.53^

.46

.O94-

• 27

516'

.052.84-'

.,.,—.6feo'

VG

63/ 1

.074-29'

fefeo'

651.7-656.0

Drilled By ....................

moderate fracturing, sli. rusty py 10-37 l*.3

Signed .

0.021* ./oi

SHIELD GEOPHYSICS LIMITED

LOCATION

ELEVATION

DIAMOND DRILL RECORDPROPERTY ...................................................................^

TOWNSHIP ........................................................................................................................................PAGE NO. ................f?.

..................................................... CORE LOCATION.:..................................................................

.....™............................................. DIRECTION ..............................................................................

..................................................... DIP ...........,.......................................................................,......

,.................................................. DEPTH ......................................................................................

STARTED ......

COMPLETED

DIP TESTS ....

DEPTH FEET/METRES

694


656.0-660.0 10" Qtz v. @ 75 0 . slioht ovrite

660.0-666.5 only 5' core: uell fractured, sil. PV

666.5-671.5 6" qtz str. S 70". slioht ovrlte

671.5-675.5 3" qtz str. Q 70 0 , slight pyrite

678 2" qtz str. @ 70"

686-694 only 7' of core, well fractured, 1"

qtz str. @ 70 0

END.

SAMPLE NO.

10-38

10-3910-1*0

10-*.1

10-t*2

WIDTH OF SAMPLE

4.0

6.5

5.0

4.0

8.0

Au/OZ

0.173

0.0100.018

0.032

0.002

0.010

660

Product.

.692 II


DIAMOND DTfILL RECORDPROPERTY ...........fM?lE*..M^

TOWNSHIP ...........M.9.Ck..l..?!!)...J.P.U.n^ ................1..........

LOCATION .........y.nS..J.6.. W?.Bt...............................™..... CORE LOCATION J.3^ ...Idarehpuse......A.irpor.t STARTED ......rj --— -j

...............................s.ta t i on ...3+00. . South....................... DIRECTION .............Sg.g.1t.b....Ciaja.t.,J............................... COMPLETED

.............................J^ejtrl.c...g]pid)..................................,... DIP ...........................5.P.!!..................................................,...... DIPTESTS ....ELEVATION .....JMWS...9S.. B|*^........................................ DEPTH .....................577!...................................................... ..........................

...March..

DEPTH FEET/METRES

0 - 217

217 - 1*13

j



Felsic Porphyry Dyke: grey to pale green, very

hard aphanitic with scattered white feldsparphenocrysts, variably fractured throughout.

222.0-227.0 lightly fractured, some pyrite

227-232 moderate fracturing mainly at 80 0

232-237 moderate fracturing at 20-30", some

rusty pyrite

237-2**2 heavy chloritic fracturing with 1'

of brecciation, fracture fillingpartially leached

2U2-2U7 W q tz str. @ 3D 0 , some fracturing.

1X rusty pyrite2**7-252 2-1" vuggy gtz strs. @ BO0 8, feu

fractures, 196 pyrite252-257 in last ft. H" qtz str. @ 100 , light

fracturing, slight pyrite

257-262 K" 4 fc" vuggy qtz strs. @ 10", ali.

rusty pyrite

SAMPLE NO.

11-1

11-2

11-3

11-1*

11-5

11-6

11-7

11-8

WIDTH OF SAMPLE

5.0

5.0

5.0

5.0

5.0

5.0

5.0

5.0

Au/oz

0.002

0.032

0.006

0.022

0.016

0.016

0.006

0.016

Drilled By ......Npr.e*.. Signed .SHIELD GEOPHYSICS LIMITED

DIAMOND DT3ILL RECORDPROPERTY .

TOWNSHIP

.HOLE NO..........fi?*-..1.1

.PAGENO. ...................2.

LOCATION

ELEVATION

CORE LOCATION


DIP ...............,.......

DEPTH ..................

STARTED ......

COMPLETED

DIP TESTS ....


262-267 moderate fracturino S ailicif. #"

qtz atr. @ 1D 0 . alioht pyrite

267-272 feu fractures, partial ailicif. i

slight pyrite272-276 well fractured, alight pyrite276-280 broken and moderately fractured,

slight pyrite

2BQ-287 inclusion of med. oreen. speckledvolcanic 1 @ 40 0

285-287 core around287-289 obscure VG in dirty qrey K" qtz str.

@ 45* , remainder— volcanic inclusion

— uiell fractured with pyrite

289-292 volcanic inclusion: as above

292-297 few SO 0 fractures in porphyry

297-302 me 11 fractured, sliqhtlv VUQQV

302-307 ali. fracturinq

307-312 last foot is amygdaloidal volcanic

312-318 amyqdaloidal havinq sharp chilled

SAMPLE NO.

11-9

11-10

11-1211-13

11-11*

11-15

11-1611-1711-1811-19

11-2011-21

WIDTH OF SAMPLE

5.0

5.0

**.o4.0

7.0

2.0

3.05.05.05.0

5.06.0

Au/oz0.010

0.020

0.0020.002

0.004

0.224

0.0020.0080.0020.0020.002

Tr '

.224- l'

contact with P.P.


PAP - l 69


TOWNSHIP

.HOLE NO. ..,..BI*-I i..

.PAGE NO. ................3.

LOCATION

ELEVATION

CORE LOCATION


DIP ........................

DEPTH ..................

STARTED ......

COMPLETED

DIP TESTS ....


318-322 broken S moderate fracturina

322-327 fractured, partially ailiclf.

327-333 aliohtlv fractured * silicified

333-337 mafic dyke @ 35" for 1st 2';

remaining F. P. lightly fractured

K silicified

337-31*2 2 1 of brecciation including 3" of

cave represents fault followed by

uiell fractured porphyry

31*2-31*7 2 tt" otz-carb strs. @ 8D0 . 2' of

areenish-brouin (sericite ?) inclusiocontains abundant pvrite

31*7-352 highly broken 4 fractured at 0-l*5e

352-357 as above, alight pyrite

357-362 uiell fractured, slight pyrite

362-367 well fractured, some sericite

367-372 1.2' of mafic dyke @ l*0 0 r moderate

fracturing, slight pyrite

372-377 moderate fracturina. sli. pyrite

SAMPLE NO.

11-22

11-2311-21*

11-25

11-26

11-27

i

11-28

11-29

11-30

11-31

11-32

11-33

WIDTH OF SAMPLE

4.0

5.0

6.0t*.o

5.0

5.0

5.0

5.0

5.0

5.0

5.0

5.0

Au/oz

0.002

Q. DU

Tr

0.001*

0.016

0.066

0.002

0.002

0.030

0.022

0.038

0. 001*

,0b6. s-

.03IS'



TOWNSHIP

.HOLE NO..........Bf*-.11.

..PAGE NO. ..................ft..

LOCATION

ELEVATION

CORE LOCATION


DIP ........................

DEPTH ..................

STARTED ......

COMPLETED

DIP TESTS ....

DEPTH FEET/METRES

i*13 - 577


377-382 moderate fracturing mainly 9 350


387-392 last 1 1 is well silicif.t otherwise

mod. fracturing

392-397 well fractured, partially silicified

slight pyrite

397-1*03 90X secondary qtz mostly from

silicification, moderate fracturing,

1X pyrite

**03-**08 moderate fracturino mainly @ 800 . 1*

pyrite

i*08-**13 contact zone with F. P.; well

fractured contact parallels coreaxis for 3'; few spots of peculiargreen mineral (malachite) along

contact

Felsic to Intermediate Pillow Lava: dark to med.

green, very hard; initially pillows rather obscur

then marked by amygdaloidal selvages containing

SAMPLE NO.

11-31*

11-35

11-36

11-37

11-38

11-39

11-4*0

WIDTH OF SAMPLE

5.0

5.0

5.0

5.0

6.0

5.0

5.0

Au/oz

0.002

0.002

0.00/4

0.010

0.022

0.022

0.026


DIAMOND DftlLL RECORDPROPERTY .

TOWNSHIP

.HOLE NO.............Bft.-!l

.PAGENO. ......................5.

LOCATION

ELEVATION

CORE LOCATION


DIP ..L.....................

DEPTH ..................

STARTED ......

COMPLETED

DIP TESTS ....

DEPTH FEET/METRES

577


chlorite. BDidote. carbonate: odd fracture withabundant smeared Dyrite.END.

SAMPLE NO.

WIDTH OF SAMPLE


PAP . 1-69

DIAMOND Dft ILL RECORDPROPERTY ........rM!H!^...k".^............^

TOWNSHIP ......^.?P.!5..1.B.JL..T^ ..................H...............

LOCATION ,..L.tne....15.t.(*0..!i!.B8.t.................................... CORE LOCATION .l3..|*...Ma..r.e.!ip.u.s.8...-....A.ir.p..qrt STARTED ...........March...25., 198f*

...........................S.ta..t|l.p.n....2.t?A..!S.p..u.t;.h. - ............. - ... - ....... DIRECTION ..................S.quth...(ast.)..................o.f... COMPLETED ......!?.?.?.5.h.....?.li.....l?.?.f*..c i o *ii. nt-.*^Q®HID DI HIDTCCTC mu * 3.?.......................................................................................,.................. Ulr ................................TT.......................................................... Ulr l to l O .......,............................................

ELEVATION .................................................................................. DEPTH .........................750.1.................................................. ................................7.5..P..!...r....5.5..0..............

DEPTH FEET/METRES

0 - 135

135 - 750



Felsic Porphvrv Dyke: Dale green to arey. very

hard, aphanitic uith scattered white feldsparphenocrysts; pale green zones appear to be caused

by hydrothermal action.

135 mostly pale green, feu very narrow

up to Vi" q tz strs.

135.0-11*2.0 rustv catches after pyrite

15t*-158 rustv patches

15B.7-163.7 1.5' fractured * silicified with 196

pyrite

163.7-168.7 1/8" qtz-pyrite seam @ 80 0 , ali. py

168.7-173.7 feu fractures, ali. diss. pyrite

173.7-178.7 rust patch is after minor pyrite

178.7-183.7 2' rusty section after pyrite

183.7-188.7 feu tt" otz strs. i fracturino @ 50"

207.5-213.0 1' rust patch, some silicif.. ali.

pvrite

223 1' rust patch

SAMPLE NO.

12-1

12-2

12-3

12-1*

12-5

12-6

12-7

WIDTH OF SAMPLE

5.0

5.0

5.0

5.0

5.0

5.0

5.5

Au/oz

0.039

0.010

0.022

0.00*4

0.216

O.OK*

D. 018

.

Drilled By ........a.ra.d.l.B.y.. Jr.OS.. SignedSHIELD GEOPHYSICS LIMITED

PAP. - 1-69

DIAMOND D7ULL RECORDPROPERTY .......................

TOWNSHIP .....................

LOCATION ............................................................................

ELEVATION ...........................................................................

CORE LOCATION .............................

DIRECTION .......................................

DIP

DEPTH ...............................................

..............................HOLENO. ...........9.7..~..'..f.............

..............................PAGE NO. ....................?.............

........................................ STARTED ..........................

........................................ COMPLETED ....................

,...................................... DIP TESTS ........................

*


2^.0-21*9.0 silicif. with feu pvritizedfractures

256-261 rusty patches, some cave

300-305 rusty308-313 rustu patches313-318 6" silicif.. 6" rusty patch318-323 moderate pvritized fracturinq @ 20 C323-328 ali. pyrite disa.

351-35S 3' of silicif.. well fractured @ **5 0with pyrite

356-361 6" fracture zone361-366 feu pyritized fractures, ali. pv366-371 feu pyritized fractures, 1" qtz str.371-376 feu pyritized fractures376-381 2.5' bleached silicified section

uith diss. pyrite, vuggy contact @70", other contact @ 50 0 iscarbonaceous and pyritizsd; 1" qtzstringer

SAMPLE NO.

12-8

12-9

12-1012-1112-1212-1312-K*

12-15

12-1612-1712-1812-1912-20

WIDTH OF SAMPLE

5.0

5.0

5.0

5.05.05.05.0

5.0

5.05.05.05.05.0

Au/oz0.01*0

0.012Q. 0200.038

D. 002

0.006

0.030

0.010

0.002

0.022

0.070

0.036

0.020

0.35

o.tS

.053 1O 1



TOWNSHIP

.HOLE NO. .......*-...

.PAGE NO. ..................?...

LOCATION

ELEVATION

CORE LOCATION


DIP ............,...........

DEPTH ..................

STARTED ......

COMPLETED

DIP TESTS ....


381.0-386.0 2' fractured and rusty after pyrite1*02.5-1*07.5 moderate chloritic fracturingl*07.5-**22.7 pale green with sli. dies, pyrite

1*22.7-1*26.0 2 tt" atz atrs. @ 70" uhich cut oyseams @ 35 e : variably silicified

1*26-1*31 3 H" qtz strs. @ 70". sli. DV diss.1*31-1*36 2 W . 1 " qtz str. 9 75". sli. diss.

pyrite1*36-1*1*1 3 tt" qtz strs. @ 75", partially

silicified, sli. pyrite1*1*1-1*1*6 2" qtz str. @ 800 , 2 W pyritized

strs. @ 60" in grey mottled rock

1*1*6-1*51 196 pyrite, some incioient fractures1*51-1*56 10" of silicif. @ BO 0 . 2-1" atz strs,

@ 75 0 . feu Dvritized fractures 9 l*001*56-1*61 silicified a/or arev mottled.

pyritized fractures @ 1*0*1*61-1*77 feu fractures, sliqht pyrite1*77-1*82 diss. rusty pyrite, mod. fracturing

SAMPLE NO.

12-2112-22

12-23

12-21*12-25

12-26

12-27

12-2812-29

12-30

12-31

WIDTH OF SAMPLE

5.0

5.0

3.3

5.05.0

5.0

5.0

5.05.0

5.0

5.0

Au/oz0.0220.010

0.052

0.0300.01*1*

0.036

0.038

0.016

0.022

0.052

0.020

,|7I4)

. ISO

.^^

.I&

•rt.9IIG

23.3'

•**ys .

-

Drilled By SignedSHIELD' GEOPHYSICS LIMITED

DIAMOND DVilLL RECORDPROPERTY .

TOWNSHIP

.HOLE NO......flA.-12..

.PAGE NO. .............A.

LOCATION

ELEVATION

CORE LOCATION


DIP ........................

DEPTH ..................

STARTED ......

COMPLETED

DIP TESTS ....


1*82.0-1*87.0 grey to green, feu fractures, ali. D^1*87-1*92 as above1*91.2-1*93.0 soft orav mafic dvke @ i*5 01*92-1*97 fractured @ 10 0 , grey to green

colourt.97-502 2" grey qtz @ i*5 c , 2' of ailicif .

uiith mod. fracturing502-507 partially silicif.. lioht fracturino,

slight pyrite507-512 last 3.5' is soft grey intensely

fractured mafic dyke @ l*5 0512-517 slightly fractured i s ilicified517-526 as above526-531 2-2" otz atrs. @ 70 0 T partial

silicif.. slioht oyrite531-536 silicif.. mod. indolent fracturing

mainly @ 1*5"536-51*1 1" qtz str. @ 70". 10" silicif.. 1*

diss. pyrite

SAMPLE NO.

12-3212-33

12-31*

12-35

12-36

12-37

12-38

12-39

12-1*0

12-1*1

WIDTH OF SAMPLE

5.0

5.0

5.0

5.0

5.0

5.0

5.0

5.0

5.0

5.0

Au/oz0.01*1*D. 026

0.028

0.031*

0.052

0.010

0.001*

0.038

0.022

0.010



TOWNSHIP

LOCATION

ELEVATION

CORE LOCATION


DIP ........................

DEPTH ..................

.HOLE NO. ...J&-12............

.PAGE NO. ..............5............

........... STARTED .......


........... DIP TESTS ....


51*1-51*6 1" qtz str. @ 70". 3 1 of silicif . 9

3D0 , black pyrite seam5U6-551 1" qtz str. 9 700 . moderate chloritic

fracturing mostly paralleling core,

1X pyrite551-556 10" qtz str. @ 70", 10" silicif.,

1X pyrite

556-559 oartialv eilicif.. last 1' is darkgrey, slight pyrite

559-56** 3' is dark qrey with i*50 fractures.3" qtz str. @ 70* in pale green

section

56i*-569 1" S 3" qtz strs. @ 70" in pale greersilicif. section, slight pyrite

569-57^* silicif. along 600 fractures in dark

grey rock, carbonaceous oyriticseam @ 1*5" with silicif.

576-617 this section appears to represent

main gold zone; dirty grey colour

SAMPLE NO.

12-U2

12-1*3

12-1*1*

12-1*5

12-1*6

12-1*7

12-1*8

WIDTH OF SAMPLE

5.0

5.0

5.0

3.0

5.0

5.0

5.0

Au/oz

0.020

0.008

0.01*1*

0.030

0.111

0.011*

0.010

2Z

.oy

.555

.&6S-

.0^(3fi'

Drilled By Signed ..........r-sj............................................SHIELD GEOPHYSICS LIMITED

DIAMOND [frfILL RECORDPROPERTY ..........................................................................................................................................HOLE NO. .....8.4-1.2..

TOWNSHIP ........................................................................................................................................PAGE NO. ..............fi..

LOCATION

ELEVATION

CORE LOCATION


DIP ........................

DEPTH ..................

STARTED ......

COMPLETED

DIP TESTS ....


574—579 some chloritic fractures S some

silicif. fractures

579-582 ailicif. t 3" atz atr. 3 70", 196 py

582-587 10" ujhite qtz str. 9 70". 1" atz str,VUQQV fractures

587-592 dirty grey colour, broken core, wellfractured, rusty diss. pyrite

592-597 2", 1" qtz str. @ 75* , mod.fracturing pyrite seam 9 45*, 1X py

597-600 mod. fracturing, 194 pyrite600-605 2' well fractured with rusty euhedral

pyrite605-610 partially brecciated; 6", 3-1" qtz

etrs. @ 70"; vuggy fractures, rustypyrite

610-615 3" qtz str. @ 700 , mod. fracturing,some pyrite

615-621 2-1" qtz strs. @ 70 C , well fracturedsilicif., pyrite

SAMPLE NO.

12-49

12-5012-51

12-52

12-53

12-5**

12-55

12-56

12-57

12-58

WIDTH OF SAMPLE

5.0

3.0

5.0

5.0

5.0

3.0

5.0

5.0

5.0

6.0

Au/oz

0.008

0.020

0.036

0.010

0.061*

0.128

0.014

0.083

0.028

0.004

-•32.

-?04-.o~r

,4i?

•Oob'B'



TOWNSHIP

.HOLE NO. ........-...

.PAGE NO. ..................7..

LOCATION

ELEVATION

CORE LOCATION


DIP ........................

DEPTH ..................

STARTED ,....

COMPLETED

DIP TESTS ....


621-626 moderatelv fractured 9 6Q 0 ,silicif., some pyrite

626-631 moderately fractured, then 2 1of silicif with 1X pyrite

631-636 2' of silicif., sli. pyrite636-61*1 t*" otz str. @ 7Q 0 . feu fractures @

70 0

61*1-61*6 6" S 2" qtz str. @ BO 0 , partialsilicif., pyrite

61*6-651 1" qtz str. @ BO C , 2' of ailicif . @l*0 0 , slight pyrite

651-656 silicif. along old fractures, sli. p^656-660 1' of silicif. @ l*5 0 , some pyritefrom 653 aradual change to oale green colour660-665 feu pyritized fractures665-670 feu qtz seams @ 10 C * 90 0670-675.5 dark grey S unalteredfrom 675.5 greenish-grey colour675.5-6B0.5 mod. fracturing 8. silicified, 196 py

SAMPLE NO.

12-59

12-60

12-6112-62

12-63

12-6U

12-6512-66

12-6712-6812-69

12-70

WIDTH OF SAMPLE

5.0

5.0

5.0

5.0

5.0

5.0

5.0**.o

5.05.05.5

5.0

Au/oz0.01B

0.012

O.OUO.OU2

0.03U

0.026

n.nsD0.030

0.0600.0360.00 1*

0.0^*1*

o^,

'


DIAMOND RECORD

LOCATION

ELEVATION

PROPERTY ................................................:..................................................................^^

TOWNSHIP ........................................................................................................................................PAGE NO. .......................6...

........................................,........... CORE LOCATION ................................................................... STARTED ......


...................................................... DIP ............................................................................................ DIPTESTS ....

..................................................... DEPTH ...................................................................................... ..........................


680.5-685.0 3". 1" atz str. @ 80e . partialsilicif.. feui fractures, oyrite

685-689 for 1.8' atz str. //'s c. a.. 2" atz

str. @ BO 0 , slight pyrite689-69** for 2" qtz str. //'s c. a.; later thar

US a 70 0 fractures, 1X pyrite69U-698.5 fracture @ 700 filled with pale greer

soft mineral

698.5-703.0 2" 8. 7" of unite qtz @ 80 0 , 1.3' ofgrey silicif., feu pyritized

fractures

703-708 9096 orev silicif. i q tz //ino c. a.with pyrite S contacts

708-711 1" qtz str. @ 800

711-716 2 H 8. 2-1" atz strs. 3 80*. mod.fract. * silicif.. 1* owrite

716-721 mod. fracturinq. partial silicif..slight pyrite

721-726 1' of silicif., some fractures 9 30 0 ,

SAMPLE NO.

12-71

12-72

12-73

12-7**

12-75

12-76

12-77

12-78

12-79

12-80

WIDTH OF SAMPLE

l*. 5

t*.o

5.0

k. 5

t*. 5

5.0

3.0

5.0

5.0

5.0

Au/oz

Q. 02U

0.011*

0.036

0.0**0

0.022

0.022

0.0060.008

O.OQt*

0.006 .

pyrite


DIAMOND D ILL RECORDPROPERTY .

TOWNSHIP ..PAGE NO. ....................?.

LOCATION

ELEVATION

CORE LOCATION


DIP ........................

DEPTH .........,.......

STARTED ......

COMPLETED

DIP TESTS ....

DEPTH FEET/METRES

750


726-731 mod. fracturinq, some silicif..SliQht DVritB

731-736 mod. fracturing, irreq. qtz Ssilicif. over 1.5', 196 euhedral py

736-71*1 qtz seams fc strs. @ 0-30 0 , feufract. , ^% pyrite

71*1-71*6 fractured mainly @ 50-70 0 , ali. py

7i*2-7(*6 colour changes to pale green71*6-750 well fractured 10-80 0 , sli. pyriteEND.

SAMPLE NO.

12-B1

12-82

12-83

12-81*

12-85

WIDTH OF SAMPLE

' 5.0

5.0

5.0

5.0

l*.0

Au/oz0.020

0.020

0.011*

0.002

O.OQl*


PAP. - 1-69

DIAMOND DftlLL RECORDPROPERTY ...............?P.MM?.,k!9.V——^^

TOWNSHIP ...............?.i!L 0.V!. .LOCATION ..UjnJB..J.S*feQ...W.BJB.1l................................:..... CORE LOCATION Jl(f...W.B.rghpUB.B...- ...Airport STARTED ™.......Apr.i.O.i....l?.Bf*..

.........................S.1t.aMqn...2.t59...SQ.u.t;h............................. DIRECTION ................Sau.^!!...^.^.^...).................?1:18.11 COMPLETED

.........................(ffiB.^iq...9ri.tl)............................................ DIP ,...,...,..,.....,....,61*......................... ; ...;........................ DIPTESTS

ELEVATION .8.am8..ss.. 8|*.-12........................................... DEPTH .......................B?.?..1 ...................................................

DEPTH FEET/METRES

D - 126

126 - 877


Casing (overburden).Felsic Porphyry Dyke: Dale areen. very hard withwhite feldspar phenocrysts. occasional rusty

patch after pyrite, odd silicified fracture,qtz stringer, sli. pyrite, locally over a foot

or tuo colour is medium grey which apparentlyrepresents unaltered rock.

1^9-15** fractured @ 750 S rusty after pyrite

180-183 qtz strs. S 20" over about 5".chloritized, rusty, slight oyrite

184-187 light coloured after inclusion @20" to c. a.

220-225 Vi 'rusty, irreo. qtz 3 222.7'

252-257 liqht to med. chloritized fracturing

mainly @ 1*0"

257-262 pyritized 8, silicified fracturingalong core

262-267 as above

from 250-350 mostly med. grey colour, i.e.

SAMPLE NO.

13-1

13-2

13-3

13-1*

13-5

13-6

WIDTH OF SAMPLE

5.0

3.0

5.0

5.0

5.0

5.0

Au/oz

0.012

O.OCK*

0.130

0.002

0.016

0.002

unaltered

Drilled By ......tr.adley. Bros, Signed.SHIELD GEOPHYSICS LIMITED


TOWNSHIP

.HOLE NO. ...-.

.PAGE NO. .............2.

LOCATION

ELEVATION

CORE LOCATION


DIP ........................

DEPTH ..................

STARTED ......

COMPLETED

DIP TESTS ....


300—3^*6 core is highly broken along

unmineralized fractures318 1" barren atz str. @ 60*351.7 fe" qtz str. 0 75"350-^*21 generally pale green to light grey

colour372.5-377.5 well fractured fc silicified around

6" pals green inclusion, 1ft pyrite377.5-382.3 some fracturing, 6" rusty zone adj.

to 70* fracture

382. 3-387. D feu ovritized fractures @ 35 0


392-396 feu fractures, 196 pyrite396-^*01 bleached S silicified for k * adj. to

pyritized fracture 0 k Q*

**01-**06 10" rust zone, odd fracture

1*21-1*62 pale green to grey colour1*31.5-1*33.5 pale green speckled intermediate

dyke 0 1*5"

SAMPLE NO.

13-8

13-9

13-10

13-1113-1213-13

13-tt

WIDTH OF SAMPLE

5.0

(*.8

**.7

5.05.05.0

5.0

Au/oz

O.QK*

o.ooi*

0.016

0.276

0.018

0.008

0.006

•^

-


PAP. - 1-69


TOWNSHIP

.HOLE NO.............BA-1.3...

.PAGE NO. .....................3.

LOCATION

ELEVATION

CORE LOCATION


DIP ........................

DEPTH ..................

STARTED ......

COMPLETED

DIP TESTS ....


1*50.5-1*56.0 mod. fracturino @ 75-30 0 . somesilicif., sil. pyrite

1*56-1*60 ali. fracturing1*60-1*62 heavy chloritic fracturing @ 35*1*62-1*81 med. grey colour1*62-1*67 mod. fracturing, ali. pyritei*7i*-i*80 med. orey. silicified. 196 pyrite1*60-1*85 lioht orey. stronaly silicified 8

35"-, 396 pyritefrom 1*81 uniform light grey with occ. pale

green after sericite1*85-1*90 1" silicif., few fractures, 1* py1*90-1*95 2-1" qtz strs. @ 75 0 , 1* pyrite1*95-500 feui fractures ft pyrite seama marking

ailicif .500-505 oyritized fracture @ 35 0 . 2-1" otz

strs. @ 75 0505-510 sli. pyrite, sericite510-515 feu pyritized fractures

SAMPLE NO.

13-15

13-1613-17

13-1813-1913-20

13-2113-2213-23

13-21*

13-2513-26

WIDTH OF SAMPLE

5.5

1*.02.0

5.06.05.0

5.05.05.0

5.0

5.05.0

Au/oz0.008

0.0080.002

0.011*

0.0020.001*

0.0220.0120.036

0.022

0.01*1*0.021* -



TOWNSHIP

.HOLE NO............ B4.-1.3..

.PAGE NO. . ....................ft...

LOCATION

ELEVATION

CORE LOCATION


DIP ........................

DEPTH ..................

STARTED ......

COMPLETED

DIP TESTS ....


515-520 feu ovritized fractures 9 35*520-526 feu pvritized fractures526-531 1* disa. pyrite531-53** feu chloritic fractures53t*-5M mod. pyritized a chloritic

fracturing, 2" qtz str.5M-5U6 grey highly fractured silicif., some

sericite * 196 pyrite, 3-#" qtz strs.@ 75"

51*6-551 grey well fractured silicif., 2-te*qtz strs. @ 750 , less than 1X pyrite

551-556 1" qtz str. @ 75 0 , light fracturing,slight pyrite

556-561 lioht fracturino. 1" qtz str..sliqht pyrite

561-566 liaht fracturino. feu K" pink qtzstrs. @ 60"

566-571 mod. chloritic S pyritized fracturin571-576 mod. chloritic 8. pyritized fracturin

SAMPLE NO.

13-2713-2813-2913-3013-31

13-32

13-33

13-3*.

13-35

13-36

l 13-37l 13-38

WIDTH OF SAMPLE

5.0

6.0

5.03.07.0

5.0

5.0

5.0

5.0

5.0

5.05.0

Au/oz0.0100.0300.021*0.0160.01U

0.036

0.367

0.108

0.052

0.061*

0.01*00.011*

Pfoducf

./S

/.ass

.54

•26

•)i

•20

s+b

./4-820'

5-66

S+l

./t/——— 30'

571

@ 75'


DIAMOND DrfILL RECORDPROPERTY .

TOWNSHIP

LOCATION

ELEVATION

CORE LOCATION


DIP ........................

DEPTH .................,

.HOLE NO.......BA-13............

.PAGE NO. ................5...........

........... STARTED ......


........... DIP TESTS ....


579.5-581.2 intermed. dyke @ 20" to c. a.617-622 aoprox. 1' irrag. soft sericitic

zone with 2096 py, remainder lightlyfractured i silicif . mainly @ l*5 0

622-627 moderatelv fractured S silicif.,some pyrite

627-632 mod. fractured, J\K pyrite, silverymetallic

632-637 5" Qtz str. S 75 0 with ovritizedcontacts, mod. fractured with oythroughout

637-6**2.5 feu chlorite 4 pink qtz-filledfract. @ 75 e , 1* pyrite

61*2.5-64.7 1' qtz @ 70 0 with pyritic 4chloritized contacts, remainder wallsilicified with rusty pyrite

6** 7-652 moderately fractured, some rustyeuhedral pyrite

652-656 few fractures

SAMPLE NO.

13-39

13-*40

13-^.1

13-1.2

13-1.3

13-M*

13-4.5

13-1*6

WIDTH OF SAMPLE

5.0

5.0

5.0

5.0

5.5

1..5

5.0

1..0

Au/oz

0.205

0.020

0.028

0.050

0.011*

0.028

0.030

0.001*

l.ozS

.10

.14

.25

.077

,t26

.IS

.0/6.

bil

Drilled By .. SignedSHIELD GEOPHYSICS LIMITED

DIAMOND Dft ILL RECORDPROPERTY .........,......................................................^

TOWNSHIP ........................................................................................................................................PAGE NO. .................. 6...

LOCATION

ELEVATION

CORE LOCATION


DIP ........................

DEPTH ..................

STARTED ......

COMPLETED

DIP TESTS ....

DEPTH FEET/METRES

!


656.0-660.5 l*". 3-1" otz atra. S 75 0 assoc. withsilicif. f 196 dias. pyrite

660.5-665 i*-1" a 6" atz strs. @ 75 0 . ailicifiasome fracturing

665-670 1" a 2" qtz str. 0 75", irreg.silicif. a fract. @ 50", some py

670-675 mod. fractured, irreg. silicif.,some rusty pyrite, sericite

675-680 6" Qtz str. @ 75 0 . 1" chlorite withstrong vuqov fracturing, some py

680-685 7" qtz str. @ 750 , mod. fractured,IK pyrite

685-690 2-2" qtz strs. Q 750 , mod. fracturinia silicified

690-695 mod. fractured mainly @ 75 0 , partialsilicif., 1X pyrite

695-700 3-1" qtz str. @ 75", mod, fracturingslight pyrite

700-705 1" a ^ H qtz str., mod. fracturing,

SAMPLE NO.

13-1*7

13-i.B

13-^*9

13-50

13-51

13-52

l 13-53

13-5U

13-55

13-56

WIDTH OF SAMPLE

t*. 5

4.5

5.0

5.0

5.0

5.0

5.0

5.0

5.0

5.0

Au/oz0.021*

0.010

0.018

0.012

0.032

0.011*

0.022

0.021.

0.026

0.070

,/OB

-.045

.09

.06

.16

• 07

.11

.IZ

,'3

•K - 705Biignt pyrite


CAP. . 1-69

DIAMOND cfclLL RECORDPROPERTY..........................................................................................................................

TOWNSHIP ..........'..............................................................................................................................PAGE NO. ..................7..

LOCATION

ELEVATION

CORE LOCATION


DIP ........................

DEPTH .................,

STARTED ......

COMPLETED

DIP TESTS ....


705-710 **" qtz atr. @ 750 . mod. fracturino.sliQht pyrite

710-715 fc" R 1" qtz atr. @ 75C . ali. fract.fc pyrite

715-720 f BUI fracturea, alight pyrite

73*4.5-739.5 bleached S silicified, some Durite71*^-71*9 verv feu pyritized fracturea7t*9-75l* l*" grey qtz atr. Q U5* , mod.

fracturing mainly 9 75* , ^ % pyrite75^-759 feu fracturea, partially ailicif.

759-761* irreo. ailicif. cubea of ovritaalong fracturea

76**-769 feu fracturea769-773 5-fc" qtz atra. Q 75", 1X pyrite780.5-785.5 2" qtz atr. @ 75", bleached R

ailicif ., fractured mainly at 75C ,196 pyrite

785.5-790.5 odd fracture790.5-795.5 bleached ft ailicified, mod. fracturii

SAMPLE NO.

13-57

13-58

13-59

13-6013-6113-62

13-63

13-64*

13-6513-6613-67

13-68g 13-69

WIDTH OF SAMPLE

5.0

5.0

5.0

5.05.05.0

5.0

5.0

5.0**.o5.0

5.05.0

Au/oz

0.018

0.036

0.0160.012

0.002

0.0120.010

0.0160.020

0.012

0.0080.020 '

@ 75 0 , 1X pyrite


PAP. - 1-69

LOCATION

ELEVATION

DIAMOND DftlLL RECORDPROPERTY ..........................................................................................................................................HOLE NO

TOWNSHIP ........................................................................................................................................PAGE NO. ...................9........

..................................................... CORE LOCATION.................................................................... STARTED ......


..................................................... DIP .........................................................................,................. DIPTESTS ....

..................................................... DEPTH ...................................................................................... ..........................


795.5-800.0 2" soft oreen dyke or inclusion i45 0 . fractured @ 0*. some pyrite

600-805 partial silicif.. bleached.fractured, slight pyrite

805-810 3-tt" qtz-chlorite strs. @ 750 ingreen sericitic rock

810-815 3 Ytn shadowy qtz strs. @ 3D 0 , sli.py815-820 few fractures, slight pyrite820-821* bleached pale qreen for 2 1 with feu

fractures, slight pyrite82U-826 well silicified alonq // fracture.

1K pyrite826-831 BOX silicified S fractured @ M) 0 4

D 0 , sil. pyrite831-835 mod. pyritized fc chloritic fracturing

marking irreg. silicif.835-840 mod. fracturing causing silicif.8*40-845 mod. fracturino @ 4Q C . sli. pyrite845-850 mod. fracturing 9 35 C l 75 0 ,

SAMPLE NO.

13-70

13-71

13-72

13-73

13-7413-75

13-76

13-77

13-78

13-7913-8013-81

WIDTH OF SAMPLE

4.5

5.0

5.0

5.0

5.04.0

2.0

5.0

4.0

5.05.05.0

Au/oz0.018

0.006

0.020

0.010

0.0080.018

0.004

0.010

0.006

0.0100.014

0.008silicif. t some pyrite


PAP. - I-89

DIAMOND DT3ILL RECORDPROPERTY .

TOWNSHIP

LOCATION

ELEVATION

CORE LOCATION


DIP ........................

DEPTH ..................

.HOLE NO..........Bf*.r.l3........

.PAGE NO. ..................S........

........... STARTED ......


........... DIP TESTS ....

DEPTH FEET/METRES

877


650-855 as above fc also fract. 9 O 0 , sliqhtpyrite

855-863 light green a mod. fractured, tt"chlorite seam @ 1*5*

863-B6B uell fractured R silicif. grey rock

with 1H pyrite^ fractures @ O 0 , 70^,t*0 0

868-873 as above but not so uell fractured

873-876.5 green, soft, chloritized amygdaloidalpi Hou lava ? as inclusion with sharpcontacts @ 020"

876-877 about tt is silicified 4 ovritizedrock as above (13-80

END.

SAMPLE NO.

13-82

13-83

13-8^

13-85

13-86

WIDTH OF SAMPLE

5.0

8.0

5.0

5.0

1.0

Au/oz

0.02*4

0.022

0.010

0.008

0.006


PAP - 1-69

SAMPLING DIAMOND Dft ILL RECORD

LOCATION ................

ELEVATION ..............

PROPERTY..............:.^:.™:'':::...!:...!:.:................,...................,....................TOWNSHIP Macklem Touinship

.................................................................... CORE LOCATION ................... ..........

.................................................................... DIRECTION .......................................

DIP

................................................................... DEPTH ...............................................

..............................HOLE NO....... ..!^-.:.:L.............

PARPMn 10 ^

.....,................................. STARTED ................................................................

....................................... COMPLETED ..........................................................

,...................................... DIPTESTS .........................™.................................


612-617

576-581

581-586

586-591

591-596

596-601

601-606

606-612

SAMPLE NO.

13-87

13-88

13-89

13-90

13-91

13-92

13-93

13-9U

WIDTH OF SAMPLE

5.0

5.0

5.0

5.0

5.0

5.0

5.0

5.0

Au/oz

0.008

0.002

Tr

Tr

0.002

O.OOU

0.002

0.002

-


PAP. - l 69

DIAMOND DTULL RECORDPROPERTY ..........±9.MMAMP.^.........,.......™

TOWNSHIP ...........M.a.cklejn..J.p.wn^ ................I.................

LOCATION ...Un.8..16.t..QO...Ul88.1J...................................... CORE LOCATION ...M..^..^....-....!..^.^^.?................... STARTED .......ABrll..,5.*....l?.Bf*..............

.......................JMUmJ.tM.Jmth............................ DIRECTION .,.........South....(a8t..).............................. COMPLETED .AB.ril...l?.i....l?.Bf*..............

..................................._................................................,................... DIP ..........................61.!!......................................................... DIPTESTS ,...15^.'-620. 1...255'.-62 0

ELEVATION.................................................................................. DEPTH .....................??6!...................................................... .535.'-6i?.0. Jl ...755.!-62 0..,...?96.'-62'

DEPTH FEET/METRES

0 - 15**

15** - 263

[


Casino (overburden).Felsic to Intermediate Pillow Lava: grey-green,hard, margin of pillows display amygdaloidal

texture which merges into massive centre,

selvages display feather-like spinifex testures

marked by chlorite, carbonate, epidote.

160-161 t*" cream coloured felsic int. with

diss. pyrite173-176 almost black, v.f.gr., med. soft,

intermediate dyke @ kS*from 228-232 interstlal flow breccia developed

in wide selvage zone, fragments areup to 2" and include 1 N geode, quartz

black mafic rock ft uallrock in

matrix of much smaller fraoments

2**6 l*" of otz-chlorite 8 W*259-263 2-1' sections of flow breccia 9 350 .

c lasts up to 3" include ulrk (pillow

lava) serpentine and qtz; look likesiumpage rauits

JriliedBv Bradley Bros.

SAMPLE NO.

U-1

Sia

WIDTH OF SAMPLE

1.0

ned ..........*s

Au/oz

O.OOB

kSHIELD GEOPHYSICS LIMITED

LOCATION

DIAMOND oSlLL RECORDPROPERTY...........................................................................................................................

TOWNSHIP ........................................................................................................................................PAGE NO. ...................2........

,................................................... STARTED ......

,.......................................................... COMPLETED

,................................................... DIP TESTS ....

CORE LOCATION

DIRECTION ........,

DIP ,.,,....,.,.....,.

ELEVATION DEPTH

DEPTH FEET/METRES

263 - 671

671 - 71*2


Intermediate to Mafic Pillows 8. Pious: areen toblack, v.f.qr., massive with contacts @ 20".

deeper rock becomes darker, softer, more massive,uiith flow-like appearance i.e. amygdaloidal flow

tops similar to pillow selvages, other flow tops

display tiny vesicles; many contacts are at 1*0-

l*5 0 contrasting with normal 20-300 angle.

1*56-1*66 soft, oreen. semi-breccia ted

throuqhout

1*66-1*75 displays variation of flow structure

586-598 flow breccia i.e. top

636-6^*1 3X diss. pyrite

630-658 diss. pyrite, up to 31 locally

Mafic Flow Breccia: medium qreen. soft, massive

except for breccia structure almost throughout i

fractures filled with black chloritic mineral

or occasionally carbonate.

71.3-766 9 to 10 tt" to 1" qtz strs. @ 70C

SAMPLE NO.

U-2

WIDTH OF SAMPLE

5.0

Au/oz

Tr


f A P. . t-69

DIAMOND D^ILL RECORD

LOCATION

ELEVATION

PROPERTY ..........................................................................................................................................HOLE NO..

TOWNSHIP ........................................................................................................................................PAGE NO.

,.................................................... CORE LOCATION....................................................................

..................................................... DIRECTION ..............................................................................

,.................................................... DIP ............................................................................................

...................................................... DEPTH ......................................................................................

STARTED ......

COMPLETED

DIP TESTS ....

DEPTH FEET/METRES

7**2 - 826

826 - 638

838 - 858

858 - 903

903 - 929

929 - 95^


Mafic Volcanic Flows and Pillows: med. to darkgreen, soft, chloritic 8. carbonatized.

798.3 H" qtz str. @ 70 C

807.5-810.5 21 diss. pyriteVolcanic Pillow Lava: pillows or bombs marked bylight coloured banded partially brecciated

selvages; k occurrences of irreg. buff coloured

felsic rock with gradational contacts up to 5".

Mafic Volcanic Breccia: med. green, soft, massivwith mylonitic structure almost paralleling core

axis.

Felsic to Intermediate Flow Breccia: light grey-

green with dark chloritic matrix.

Felsic to Intermediate Breccia Tuff (Hvaloclastit

fine alternatina liqht green bands show abundantslumpaae fi cross faulting, beddino generally //to core axis.

Mafic to Volcanic Flow Breccia: dark, finely

fractured with abundant epidote, some pyrite

SAMPLE NO.

U-3

i

1s

WIDTH OF SAMPLE

3.0

Au/oz

0.002

probable carbonate.


DIAMOND dRlLL RECORDPROPERTY .......................

TOWNSHIP .....................

LOCATION ............................,...............................................

ELEVATION ...........................................................................

CORE LOCATION ........™..................

DIRECTION .......................................

DIP .....................................................

DEPTH

..............................HOLE NO. ......9.7.".!.*..................

..............................PAGE NO. ..............A.................

....................................... STARTED ..........................

....................................... COMPLETED ....................

DIP TESTS

t

DEPTH FEET/METRES

951* - 996

996


Ultramafic Flow Semi-Breccia: fine grained.black, numerous irreo. fractures filled bvserpentine or carbonate.END.

Survey Taq^

Deoth, Direction(T) D^p

200' 185 0 ——

1*00' 183 0

600' 180 0

800' 1850 63 0

Note: Casing left in hole and plugged.

SAMPLE NO.

WIDTH OF SAMPLE


Ontario

Ministry ofNorthern Developmentand Mines

42A18SW8285 63.4363 MACKLEM 900

Fouuou)it4^

IS

OH

GEOPHYSICS LIMITED TELEPHONE t7os) iswosAIRPORT ROAD, TIMMINS, ONTARIO *

MINING EXPLORATION CONSULTANTS & CONTRACTORS TIMMINS,

February 15, 198**.

Pominex Ltd.,1B16 - 29 Adelaide St. E.,Toronto, Ontario M5C 1Y2.

Attention: Mr. Don Rankin, President

Dear Sir:

Re: Hole No. 63-1Macklem Township Property

In mid-December, 1983, hole 83-1 was drilled in the northeast sector (claim P25557) of the property. Drilled in a northerly direction, this boring was located to test the area immediately adjacent to the nose of an ultramafic intru sive as reflected by a magnetic survey conducted by Shield Geophysics Limited in November, 1983. Based on the geophysics, this area uss interpreted as a potential zone of weakness perhaps hosting gold-bearing structures.

The drill log and appropriate section is attached. A thick series of intermediate to mafic volcanics, including massive f louis, pi Hou lavas, flow and pyroclastic breccia, was intersected. An eight foot wide felsic dyke was inter sected midway in the hole. Deeper, between 33**.3 and 370.5, a peridotite intrusive was encountered.

There were no structures or mineralization inter sected in the hole which might be associated with gold.

...2

OH63

- 2 -

Apparently, termination of the magnetic high in this area does not represent complete pinching out of the ultramafic intrusive. The lack of a high magnetic response may represent deeper overburden, a narrower width of ultramafic (magnetic) rock, carbonatization of the ultramafic or simply a combination of the above.

Respectfully submitted,

SHIELD GEOPHYSICS LIMITED,

RJB:pd R\ J. Bradshaw, P. Eng.

f* 4.0 S83-1

LE.GEHD

|T"| Felsic (.Aplite) Dyke

CPer*

/^ /o

/c Q re c c /o* /c/

I/a fact* t es 550'

^OFESS/oT

^S R.J.BRADSHAV/ * 01 a

lv/--^O.^***:-^ X/' "

l S- IS 84

POM/NEX Ltd.5ZCT/OH ~ HOLE

.5 C/* L E t t " w

DIAMOND DRILL RECORDPROPERTYTOWNSHIP

LOf^ATTON Line 1+QQE

Station 1+1*0 South(metric grid)

ELEVATION

POMINEX LTD.

Macklem Township

CORK LOCATION ,DATUM

. ^ pRAPTNft

MNR Timmins

North (ast.50 0

...... HOL,.^...PAG

)

HOLE N(X~J3*bl

STARTED

DEPTH.

December 16, 1983 December 23, 1983 550 feetAQ core (1 1/16")

DEPTH FEET

n - 11*1U1 - 198.3

198.3 - 230

230 - 238

238 - 24*6.5

FORMATION

Casing (pverhurden) .

Intermediate to Mafic Pillow Lava fc/or Flows:

medium to oale oreen. v.f. or., liohtly fractured

and oartiallv carbonatized: flouis R Dillous market

bv vesicles and dark qreen chloritized interfaces:

some epidote; fractures filled by barren quartz an

carbonate.

153.i*-15**.'* grey vuggy qtz @ 500 to c. a.

Intermediate to Mafic Volcanic Flow Breccia:

dark green massive mafic sections up to 2* uith

pale green .sections of angular fractured inter

flow material; dark blue mafic sections and

fractures are serpentinized.

Felsic (Aplite) Dyke: massive aphanitic, very

hard, siliceous rock; conchoidal fracture except

uhere low angle secondary cream coloured fractures

occur.

Mafic Volcanic Flow: dark green, massive, v.f. gr.

lightly fractured.

SAMW NO.

J

WIDTH OF SAMHE

Drilled By. Wo re x Signed

DIAMOND DRILL RECORDPROPERTY. MOLE NO-TOWNSHIP. .PAGE NO..

.B3-1. 2

CORE LOCATION. DATUM——————

STARTED.COMPLETED.

ELEVATION.BEARING. DIP

DEPTH FEET

7iifi.R - 27i*.9

27*4.9 - 322.9

322.9 - 33t*.3

FORMATION

Intermediate Aoalomerate (Pyroclastic Breccia):

pale areen. masses ranging from 3" to 3'; some

mav be pillows, upper contact at 3D0 ; some carb

in fine gash fractures, black mafic contact zones;

becoming more lightly packed deeper.

Intermediate Volcanic Flow: pale green, v.f.gr.,

more massive except for prevalence of serpentine-

filled gash fractures near top perhaps representin

flow top.

288. 0 becoming more massive

308.0 . becoming less massive with pale green

irregular masses perhaps representing

bombs

Intermediate Volcanic Breccia: upper contact at "t*

pale green fragments with soft black serpentine

fillinp pash fractures and interstices, very

intense brecciation at start: rock becomes softer

deeoer.

31**. 7 2' arev irreq. qtz stringer

SAMflE NO.

o ' *

WIDTH OF SAMPU

Drilled Dy. Signed..SHIELD GEOPHYSICS LIMITED

DIAMOND DRILL RECORDPROPERTY. JttOLE NO——J*liLTOWNSHIP. .PAGE NO..

LOCATION. CORE LOCATION. DATUM——————

STARTED-

DEPTH.

ELEVATION. DTP

DEPTH FEET

33U. 3 - 370.5

370.5 - ^00.5

1*00.5 - **09.3

1409.3 - 513

FORMATION

Ultramafic: black, fairly soft, massive except

for irregular carbonate-filled fractures; probablt

intrusive periodite although upper contact

gradational.

366.^-368.3 soft, light grey-green talcose rock


369.8-370.3 light coloured xenolith ?

Intermediate Volcanic: comprised of breccia of

flow material, agglomerate and pillows, qash

fractures filled by serpentine. "

Intermediate to Mafic Volcanic Flows: contact

poorly defined; medium green, fairly massive

with uniform fine dissemination of carb lathes.

Intermediate Volcanic Breccia: comprised of flows

agglomerate and pillows; pale green, v.f.gr.

dacitic pillows and fragments ere extensively

fractured, gash fractures and interstices filled

by black serpentine; odd minor qtz and carbonate

stringer.

SAMP1C NO.

i

WIDTH OF SAMPLE

Signed.,SHIELD GEOPHYSICS LIMITED

DIAMOND DRILL RECORD

LOCATION.

ELEVATION-

PROPERTY. .HOLE NO.. 83-1

TOWNSHIP. .PAGE NO-

CORE LOCATION. DATUM______

STARTED.

BEARING.

DIP___

COMPLETED. DEPTH———

DETTH FEET

513 - 550

550

FORMATION

1*1*1*. 9-1*1*6. 3 B" qtz-carb str. @ i*5 0 , few grains

of pv and cpy

1*55.0-1*82.0 minor brecciation of pillow lava

1*82.0-503.0 more intense brecciation; secondary

fractures filled with carb, qtz and

occasionally clay mineral

Intermediate Amyqdaloidal Pillow Lava: contact

sharp at 700 to c. a., roed, green to brownish;

well defined pillows with variably sized green

amygdaloids in brownish matrix; some epidote,

few serpentine-filled fractures.

51*0.0 3" barren qtz-carb stringer @ l*5 0

END,.

Dip test 8 550' - l*1 0

SAMTU NO.

1-1

WIDTH OFSAMHE

1.1*

Au/ppb15

v

Drilled By. Signed...SHIELD GEOPHYSICS LIMITED

BELL-WHITE ANALYTICAL LABORATORIES LTD.P.O. BOX 187. HAILEYBURY, ONTARIO TEL: 672-31O7

(UrrttfirateNO. B79-84

SAMPLE(S) OF: Core (11)

SAMPLE(S) FROM: M r. R. BradshawShield Geophysics Limited

DATE: January 27, 1984

RECEIVED: January, 1984

imple No .

1-1

2-1

2-2

2-3

2-4

2-5

2-6

2-7

2-8

2-9

2-10

Gold/ppb

.15 _ ̂?

15

487

278

670

18

88

Gold/oz .

0.050**

0.832**

0.372**

0.116**

** Checked

IN ACCORDANCE WITH LONO.C*TA*Llf MtO NORTH AMERICAN CUSTOM, UHLttI IT It •PCCIflCALLV *TATCO OTHERWISE OOLD AND SILVER VALUES REPORTED ON TMfir tHIITf HAVt HOT HIH A&JUtTfD T O COHftN. •ATI tOK LO*lCt AMP OAINt INHIfttNT IN THE n ut

BELL-WHITE ANALYTICAL LABORATORIES LTD.

BELL-WHITE ANALYTICAL LABORATORIES LTD.P.O. BOX 187. HAILEYBURY. ONTARIO TEL: 672-3JO7

ofNO. B79-84

SAMPLE(S) OF: Core (11)

SAMPLE(S) FROM: Mr. R. BradshawShield Geophysics Limited

DATE: January 27, 1984

RECEIVED: January, 1984

Gold/ppb••"-••^-p-——-

15

487

278

Gold/oz.

670

18

68

0.050**

O .832**

0.372**

0.116**

** Checked

IN ACCONOANCC WITH LONO-CSTACLIIHCO NONTH AMERICAN CUtTOM, UNLffl IT li IPtCIMCAkLV ITATCO OTHCMWIfC OOLO AND tlLVCH VALUtf Mt'ONTID ON Tfttt tffKrf HAft MOT VCCN *OJUfTtO TO COMriN. • ATI f OH LOMCt AND OAINJ INHIKtNT IN TM( fi*!

BELL-WHITE ANALYTICAL LABORATORIES LTD.

on the property of...summary during the period december, 19b3, to mid-april, 198*4, pominex ltd....

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