AND PROSPECTING PROGRAM IN LEDUC TOWNSHIP, ONTARIO … · 42e12ne002a 2.11875 leduc 010 report on...

42E12NE002a 2.11875 LEDUC 010

REPORT ON THE GEOLOGICAL MAPPING

AND PROSPECTING PROGRAM

IN LEDUC TOWNSHIP, ONTARIO

FOR

CAVIAR RESOURCES LTD.

AND

DUBAWNT RESOURCES LTD.

1988

Date: November 1988 By: P. Lassila

42E12NE8828 2.1)875 LEDUC010C

CONTENTS

RECOMMENDATIONS . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

GENERAL STATEMENT . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

INTRODUCTION. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

PROPERTY. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

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

PREVIOUS WORK. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

WORK PROGRAM. . . . . , . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

GEOLOGY STRUCTURE AND LOCATIONS OF EXPLORATION INTEREST.

Kingston Island. , . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

Area East of Kingston Island and North of the Namewaminikan River . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

Area Between the Namewaminikan River and the Paint Lake Fault . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

Area Between the Paint Lake Fault and the Metoconglomerate Unit . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

Metaconglomerate Unit . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

Area South of the Metaconglomerate Unit . . . . . . . . . . .

GOLD ENRICHED QUARTZ CARBONATE ZONE AT TRENCH LAKE. . . . .

SUMMARY AND CONCLUSIONS . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

Geological and Structural Aspects . . . . . . . . . . . . . . . . .

Locations of Potential Economic Interest . . . . . . . . . .

AUTHOR'S NOTE. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

REFERENCES . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

Page

l

5

6

6

6

9

12

13

13

14

16

17

19

20

23

27

27

29

32

33

ii

CONTENTS (CONT'D)

Page

FIGURE 1.

APPENDIX 1.

APPENDIX 2.

APPENDIX 3.

MAP 1.

MAP 2.

MAP 3.

MAP 4.

LOCATION MAP

CLAIM MAP.

ASSAY REPORT.

NAMES AND ADDRESSES OF WORKERS.

GEOLOGY MAP , EAST SHEET

GEOLOGY MAP, CENTER SHEET.

GEOLOGY MAP , WEST SHEET

GEOLOGY MAP , TRENCH LAKE AREA.

,........ 7

, . . . . . . . . 34

, ........ 35

. ....... 37

. . . . . . . . . In MapPocket

Pocket

. . . . . . . . . In MapPocket

Pocket

ill

RECOMMENDATIONS

At least four areas which appear to contain potential for a gold

discovery should be thoroughly investigated. Detailed VLF electromag

netic (EM) and magnetometer surveys should first be conducted over these

zones of interest to provide information which will assist in defining

the parameters of geological units, and in the general evaluation of

these areas. Mechanical stripping should be subsequently conducted,

where feasible, to define and delineate the gold-bearing quartz

carbonate zone south of Trench Lake and the other three locations of

potential gold enrichment; followed by drilling those targets which show

encouraging results.

Many other locations, such as those with significant quartz veining

or old trench sites, should be prospected in detail and all sulfide

and/or quartz veined occurrences should be well sampled for assay.

Additional work at these locations would be subject to the results of

the prospecting program.

Specific recommendations are summarized as follows:

1. To complete the recommended work, it will be necessary to develop

about 14 km to 16 km of access road. A reasonably good route,

mainly along sand plains about one kilometer south of Paint Lake,

would provide access to the west boundary of the property from

Highway 801. Sandy plains can also be utilized to provide good

routes of access to the recommended work locations within the pro

perty area.

2. a) A picket line grid with 50 meter line spacing should be estab

lished, between the present lines 9+OOW and 2+OOE, over the

area which contains the gold-bearing quartz carbonate zone

just south of Trench Lake. A detailed magnetometer and VLF

electromagnetic survey should then be conducted over this

grid.

b) Where possible, this zone should be exposed by bulldozer

and/or backhoe stripping across its width and length to define

and delineate potential gold-bearing locations. Specific

locations of interest, exposed by the stripping, should

additionally be washed clean and sampled in detail for assay,

utilizing a diamond saw.

c) Lastly, the zone should be tested at depth by diamond drilling

at those locations where encouraging values are returned from

the results of the surface work.

3. The sequence of exploration outlined in the above section 2, should

also be carried out over the three other areas of interest which

are located as follows:

a) Within the highly foliated to schistose volcanics south of

the Paint Lake Fault in the area outlined by the present grid

co-ordinates of 1+OOE to 11+OOE, and 8+OOS to 13+OOS.

b) In the area along and north of the volcanic-metaconglomerate

contact, north of Contact Lake, outlined by the present grid

co-ordinates of 15+OOE to 25+OOE, and 9+OOS to 13+OOS. In

this area, the location of the east-west striking ridge of

high magnetic relief and the horizontal loop EM conductor,

depicted by the results of the 1980 Dome Exploration survey,

should be geophysically relocated and defined in detail. The

EM conductor should then be exposed by surface stripping, if

possible, or diamond drilled.

c) In the area of fault shearing and alteration along Baseline

20+OOS between lines 12+OOE and 23+OOE.

4. Locations of old trenches, quartz and quartz carbonate veining,

narrow cherty zones and those locations of intense saussurite clot

ting with associated quartz should be prospected in detail. At

least some of these might lead to more viable targets that would

warrant a more intensive exploration program.

A sufficiently large budget should be allocated to this promising

property to support an adequate and thorough evaluation of the property

potential. A summary of estimated costs for the program recommended

is submitted as follows:

1. Bulldozer and backhoe work for developing 8km of access road from Hwy. 801 to the west boundary of the property $ 16,000

2. Bulldozer and backhoe for developing 7km ofaccess road within the property area 15,000

3. Line cutting (in addition to the present grid) 2,000

4. Magnetometer and VLF surveys(including final reports and maps) 8,000

5. Bulldozer and backhoe stripping 70,000

6. Washing, sampling, mapping and blasting striptrenches 10,000

7. Prospecting and sampling 4,000

8. Diamond drilling 1000m at $80/m 80,000

9. Administrative costs 3 15,000

TOTAL ESTIMATED EXPENDITURES $250,000

GENERAL .STATEMENT

The Caviar-Dubawnt property is centrally located within the

Beardmore-Geraldton Gold Belt which contains some fifteen past gold pro

ducers and numerous gold occurrences. The property is bisected by the

Paint Lake Fault system which is considered to be a conduit for gold

occurrences in the area. The most recent significant development along

this system is the Metalore Resources gold discovery which is presently

on the verge of becoming a producer. The geology and structure under

lying the area of the Metalore discovery and that of the Caviar-Dubawnt

property are very similar: these two properties lie on strike with each

other and host the same general lithologic units (Map 2356, Macksey 1976

and Map 2294, Macksey 1975). Therefore, if gold-be'aring zones occur

on the Metalore property then it seems reasonable to assume that similar

zones could also underlie the Caviar-Dubawnt property. The present

prospecting and geological mapping was designed to investigate this

aspect, as well as any other possibilities which might lead to a gold

discovery.

A promising gold enriched quartz carbonate zone was located and

exposed at two old trench sites largely by the efforts of Jerry Bruce

and his assistant Doug Brackenridge. Encouraging gold values up to 0.30

oz/ton (verbal communication with Jerry Bruce) have been obtained from

this zone. Several other locations of interest, which warrant further

exploration, were also observed by the author during the geological

survey.

INTRODUCTION

This report documents the results of a detailed geological mapping,

prospecting and trenching program that was conducted jointly on the

Caviar Resources Ltd. property (54 claims) and the adjoining Dubawnt

Resources Ltd. property (27 claims) during the period May 16, 1988 to

August 31, 1988. Previous work, comments on the geological setting,

the work program and results of the mapping program are discussed. Con

clusions are presented and recommendations offered.

The results are also depicted on three geology maps and one trench

map.

LOCATION AND ACCESS

The 81 claim property area borders the south shore of Expansion

Lake and is situated immediately south of the north boundary of Leduc

Township, Ontario (Fig. 1). It lies about six kilometers north of

Jellicoe which is on Highway 11 about 180km east of the City of Thunder

Bay, Ontario. Expansion Lake may be reached via automobile by travel

ling 15km on the Kinghorn Road north from Highway 11 and then four kilo

meters east along a small dirt road. From Expansion Lake, waterways

allow boat access to various locations on the property.

PROPERTY

The area covered by the geological mapping program covers a group

of 81 mining claims in Leduc Township, Ontario as indicated on the claim

map under Appendix 1.

^ p/ AligogamaLake C;

RIVER; -- '

. -,,thy X-*Srft ^.Expansion

ON OF TH! TOWNSHIP OF

vners ike

Scale 1:100 000

PROPERTY LOCATION MAP

CAVIAR-DUBAWNT PROJECTOne centimetre represents one kilometre

: VINCENTMCCOMBER

Abstracts (Oct. 6, 1988) of the above 81 mining claims show the

ownership as follows:

Caviar Resources Limited

18th Floor, Royal York Hotel

100 Front Street

Toronto, Ontario

MSS 1E3

30 Claims: TB 813397

TB 815326

TB 830873

TB 907220

813402 inclusive

815331 inclusive

830881 inclusive

907228 inclusive.

TOTALS

(6)

(6)

(9)

(9)

TOTAL 30

Dubawnt Resources Limited

4 Austin Crescent

Toronto, Ontario

M5K 5E4

27 claims: TB 815313 - 815325 inclusive

TB 830882 - 830893 inclusive

TB 907254 and 907255 inclusive

TOTAL

TOTALS

(13)

(12)

(2)

27

Harold Watts

18th Floor, Royal York Hotel

100 Front Street

Toronto, Ontario

M5J 1E3

TOTALS

24 claims: TB 813393 - 813396 inclusive (4)

TB 813403 - 813412 inclusive (10)

TB 830910 (1)

TB 907211 - 907219 inclusive (9)

TOTAL 24

TOTAL ALL GROUPS: 81 MINING CLAIMS.

PREVIOUS WORK

Many old trenches located during the present survey attest to the

fact that considerable exploration, apparently mainly in the form of

prospecting and . trenching, was completed on the property some 20 to 50

years ago. The only record of this early work is a short article on

the seven claim Barker project (page 848 in the Dec. 1945 Canadian

Mining Journal). This showing is described to lie in a 10 ft. to 15

ft. wide shear zone which contains narrow quartz veins and bands of sul

fide, mainly pyrite, with chalcopyrite in places. Assay returns of

$40/t gold across two feet, $5/t across five feet and $3.75/t across

11 ft. are reported. (Gold at this time was priced at $35 per oz.)

The location is described as being east and south of Kingston Island

and situated in volcanics just south of a conglomerate unit which

strikes east-west across the property. This reported zone is believed

to be at the same location as the two old trench sites that were found

during the present exploration program. Several samples collected from

these trenches by Jerry Bruce during August, 1988 assayed low to very

encouraging gold values ranging up to 0.3 oz/ton (verbal communication

with Jerry Bruce). One representative grab sample by the author, from

the old trench at 4+91W, 15+25S returned a value of 0.224 oz/ton in

gold.

Assessment file research revealed two recorded geophysical surveys

over the eastern part of the property area; a horizontal loop electro

magnetic (EM) survey conducted by Hudson's Bay Exploration (HBED) in

1972, and a horizontal loop (EM) and magnetometer survey conducted by

Dome Exploration in 1980.

The HBED survey results depict a long formational EM conductor

which closely follows the Namewaminikan River, a weak but continuous

conductive zone along the Paint Lake Fault system, and two conductive

horizons south of the fault. All four EM conductors extend from the

east well into the Dubawnt property area. This survey covers an area

roughly from 11+OOE to 28+OOE, and 2+OOS to 15+OOS on the present grid.

HBED also delineated a short horizontal loop EM conductor within

volcanics which they drill tested with a 300 ft. hole in 1973. During

the present mapping, the drill hole setup was located at 18+30S and

3+25E. Andesitic volcanics with frequent quartz carbonate stringers,

tuffaceous sections, minor mylonite, a \h ft. chert section and several

narrow pyrrhotite mineralized zones are reported in the drill log. Two

10

sections were assayed for gold, silver, copper, and zinc with only trace

returns, except for one assay which returned Q.10% zinc across 2.5 ft.

The 1980 Dome Exploration survey covers part of the earlier 1972

HBED survey area. On the present grid it covers the area between the

co-ordinates 8+OOE to 28+900E and 7+OOS to 11+OOS. The Dome 1980 hori

zontal loop EM results closely duplicate the EM results of the HBED 1972

survey. The most significant feature characterized by the 1980 magneto

meter survey is a narrow east-west striking linear magnetic high of 400

gamma to 1500 gamma intensity. It is located from 8-fOOE to 28+OOE

between 10+50S and 11+75S on the present grid. The continuity of this

magnetic "ridge" is sharply broken at about 23+OOE, 11+OOS. A strong

horizontal loop EM conductor cuts ENE through this "magnetic" break.

A northeasterly striking structure (a fault?) is likely associated with

the EM conductor at this location. The magnetic "ridge" and conductive

horizon are both located within volcanics less than 100m north of the

contact with the polymicitic metaconglomerate to the south. Several

old trenches were located in this general area.

The most recent recorded work over the property area is a 1986 air

borne magnetometer, electromagnetic and radiometric survey that was con

ducted by Geoterrex for Murgor, Diplomat and Ark Energy. The airborne

EM anomalies closely correspond to the conductive zones delineated by

the earlier ground surveys. The airborne EM results also suggest that

nost of these conductive zones extend westward through the property

area. The airborne magnetic results depict the same magnetic "ridge"

as was outlined by the Dome 1980 ground survey. A strong magnetic high

indicated south of Trench Lake may be related to the diabase dike and

mafic intrusives in that area. The cause of a strong magnetic high

11

situated just east of Kingston Island remains unknown due to lack of

outcrop exposure in that area.

The Geoscience Report 149 (Mackasey, 1976) includes the property

area and outlines the general underlying geology and structure. Of

particular interest is the Paint Lake Fault system which cuts east-west

centrally through the property.

WORK PROGRAM

The field work was carried out during the period between May 16,

1988 and August 31, 1988. It included line cutting, prospecting and

detailed geological mapping over the whole property area. A cut and

chained picket line grid with 100m line spacing was utilized for loca

tion control. A total of 108 line km was covered by the geological sur

vey as well as several kilometers of shoreline mapping. Old trenches

were also searched for. Several of these were located. Two long

trenches were also mucked out, blasted, sampled and mapped. Additional

to the main grid, a short baseline and picket lines were established

at the area of the two trenches, for detailed location control.

All the geological mapping was completed by the author. Assistance

was provided by Rod Letang between June 28th and July 26th, 1988.

Jerry Bruce supervised the trench work and obtained samples for

assay. He was assisted by Doug Brackenridge and John Koski. This work

was carried out during various periods between July 20th and August

31st, 1988.

All the map work was completed from a tent camp at a road acces

sible site on the north shore of Expansion Lake. A canoe with a small

outboard motor was used for transport to various locations on the

12

property. A second canoe was portaged to some of the inland lakes to

provide access to across these lakes.

A total of 34 samples for assay was collected from various loca

tions of interest by the author. Several samples were also taken for

assay by Jerry Bruce from the two old trench sites which were blasted

and mucked out. These trenches cut a gold enriched, quartz-veined car-

bonatized zone located just south of Trench Lake.

GEOLOGY, STRUCTURE AND LOCATIONS OF EXPLORATION INTEREST

(Maps l, 2 and 3)

For the convenience of the reader, the following subject matter

is segregated into areas or sections, beginning with a discussion of

the area covered by "Kingston Island" and ending with a discussion on

the "Area South of the Metaconglomerate Unit".

Details of the gold-bearing quartz carbonate zone, located just

south of Trench Lake, is treated last.

Kingston Island:

The best outcrop exposure occurs along the north shore of the

island. Moderate exposure is found in the northwest and at a few loca

tions in the central part of the island. The remainder of this area

is covered ,by swamp or sand plain.

The island is underlain by mafic to intermediate volcanics includ

ing deformed pillow lavas, massive flows, flow breccias and minor amyg

daloidal lavas. The volcanics are weakly to moderately well foliated

with occasional very minor shears. Of interest is a pinkish medium

13

grain plagioclase porphyritic syenite which is clearly exposed on the

north shoreline between lines 16+OOW and 17+OOW. It "blends" eastward

into a greenish saussuritized feldspathic porphyry. A fine to medium

grain diorite (possibly a coarse grain flow) is exposed at the south

eastern tip of the island. A south striking diabase dike of about

twenty meters in width follows line 20+OOW south from Expansion Lake.

Minor quartz veining and locally minor disseminated pyrite was

observed at several locations. A 20cm thick quartz vein, mainly buried

under water, at the north end of line 22+OOW was sampled for assay and

returned 0.013 oz/ton gold. Another small quartz vein with associated

pyrite, located at 22+10W, 3+45N, returned 0.007 oz/ton gold. Four

samples from a small rusty silicified zone with pyrite, chalcopyrite

and malachite mineralization at 18+OOW, 1+OON returned gold values of

trace, 0.01, 0.008 and 0.009 oz/ton gold.

Area East of Kingston Island and North of the Namewaminikan River:

Most of this area is covered by deep glacial drift or swamp. The

best outcrop exposures lie along the shorelines of small lakes and along

the Namewaminikan River. The underlying rocks include dioritic to

gabbroic intrusives, mafic to felsic volcanic flows and minor related

volcaniclastics.

A medium to coarse grain pyroxene-amphibole metagabbro underlies

the area between Gabbro Lake and Lobe Lake. It grades into diorite to

the north. A medium grain diorite (possibly a coarse flow) is exposed

at the northeast corner of the property. Gabbroic to dioritic rocks

also occur along the north side of the Namewaminikan River. They appear

to be interflow intrusives which were formed contemporaneously or

14

penecontemporaneously with the volcanic flows. In most of these

intrusives the plagioclase feldspars are almost completely altered to

saussurite.

Mafic to intermediate volcanics are exposed at several sparsely

separated locations. They are generally weakly to well foliated and

locally contain minor shears. They exhibit considerable saussuritiza

tion, lesser chloritization and variable intergradations from andesitic

to dacitic composition. Minor pillow lavas, agglomerate, tuff, lapilli

tuff, and flow breccia apparently interlie between the massive flows.

Rhyolite flows are exposed in a few outcrops in line 2+OOE.

Minor (subsidiary?) fault structures and associated shearing were

observed at several locations. East northeast striking faulting is

clearly evident in a creek bed at 3+25S on line 9+OOE. Here the vol

canics have been sheared into a chlorite, chlorite-sericite and sericite

schist across at least ten meters of section. Quartz carbonate veining

occurs along the apparent fault line. Compositional variations across

section suggest that the original rock was likely composed of mafic to

felsic tuff. A sample from the quartz carbonate veining returned 0.005

oz/ton gold.

Quartz carbonate veining up to one meter thick is exposed in sev

eral old trenches at 0+50S between lines 22+OOE and 23+OOE. This zone,

which lies within well foliated to schistose mafic volcanics, was traced

for about 50 meters along strike. Additional trenches may exist in this

area. Therefore, it should be prospected in detail and all locations

of interest should be sampled for assay.

A sharply indented north striking draw between lines 4+OOE and

5+OOE could be underlain by a fault. A minor fault shear is indicated

15

by crenulate folded chlorictic schist with quartz carbonate seaming on

the east shore of Lobe Lake (line 1+OOE). Fault sheared chlorite and

chlorite-sericite schist with minor quartz carbonate veining was also

observed on a small island at about 7+OOS, 10+OOW and at the intersec

tion of stream and the river at about 5+OOS, 7+50E.

Area Between the Namewaminikan River and the Paint Lake Fault:

Most of this area contains moderate to abundant outcrop exposure

along an east-west trending ridge which lies between the Namewaminikan

River to the north and the lowlands along the Paint Lake Fault to the

south.

The underlying rocks are composed of weakly to moderately well

foliated volcanic flows of intermediate composition. "Intercalated with

in these flows are minor tuff, lapilli tuff, and occasional narrow

cherty beds. No intrusives were observed in this section. The section

pinches out in the west where the Paint Lake Fault and the Namewaminikan

River coalesce. It thickens to the east, and is about 300 meters wide

at the east boundary of the property.

Although the actual Paint Lake Fault line is not exposed on the

property, there is evidence of the faulting in exposed outcrop at 8+75S

just west of line 2+OOE on the northeast shore of a small lobate bay.

Here intermediate to felsic volcanics have been brecciated, sheared,

foliated and altered. Sericitization, chloritization, silicification,

quartz seaming and lensing, carbonatization and minor pyritization are

all clearly exhibited on what apparently is the north flank of the fault

zone.

16

Area Between the Paint Lake Fault and the Metaconglomerate Unit:

This portion of the property is underlain by mafic to intermediate

volcanics which have been strongly affected by the fault forming pro

cesses of the Paint Lake Fault system. This aspect is clearly depicted

in the area of relatively abundant rock exposure extending westward from

the northern part of Portage Lake (12+OOE to 4+OOE and 9+OOS to 11+OOS).

Here the volcanics are well foliated and, at many locations, have been

completely altered into chlorite and chlorite-sericite schist. These

schists commonly exhibit lensy banding which suggests a tuffaceous

origin. Minor carbonate and quartz seaming also generally occurs

parallel to the foliation. Crenulated folding of the foliation is

evident at some locations. A north-south fault displacement was noted

at one such location (5+OOE, 9+25S).

A notable exception to the generally well foliated character of

this zone is exhibited by the volcanics exposed on a knobby dome-like

hill between lines 5+OOW and 8+OOW just north of Trench Lake. Here

massive to poorly foliated mafic to intermediate volcanics, across some

300 meters of section have, for some reason, resisted the stresses which

so strongly deformed the rocks to the east.

West of Contact Lake, and in the areas between lines 4+OOE to 4+OOW

and 8+OOW to 14+OOW, thick glacial overburden covers the bedrock. This

section, as a whole, is characterized by flat to low topographic relief,

which is typical of erosional features that occur over broad shear sys

tems. This topographic feature, in conjunction with the foliated to

schistose volcanics, exposed south of the main fault line, suggests that

the Paint Lake Fault is not limited to a single horizon. Rather varying

amounts of displacement appear to have occurred at several locations

17

across some 300 meters of section south of the main fault line. Such

subsidiary fault systems are generally considered to be excellent poten

tial hosts for gold enrichment along this belt. For this reason, thi's

section of the property should be seriously considered for additional

exploration.

The area which lies between the co-ordinates 9+OOS to 11+OOS and

4+OOE to 9+OOE, and 11+OOS and 12+OOS on line 2+OOE, is particularly

amenable to surface exploration by mechanical stripping. Nearly all

of the outcrops in this area contain heavy rooty moss cover which

severely limits the scope of rock examination. Therefore, it is quite

possible that mineralized locations of interest, such as quartz and

quartz carbonate veins, could easily have been missed during the present

survey. The abundance of chloritization, sericitization, carbonate

seaming and thin quart lenses, which were observed, suggests that a

favourable environment for gold does exist in this area.

A second zone of interest lies between lines 16+OOE and 26+OOE

close to tie line 11+OS. In this area, the generally well foliated to

schistose volcanics are exposed only near the volcanic-metaconglomerate

contact. Deep overburden covers the area south from the Paint Lake

Fault to within 100 meters of the volcanic-metaconglomerate contact.

Of particular interest is a strong east northeast striking strong hori

zontal loop electromagnetic (EM) conductor (Dome Exploration 1980),

which cuts diagonally through a break in s long narrow east-west

striking zone of high magnetic relief. This geophysical feature sug

gests that a conductive horizon follows a structural break (fault?) at

an acute angle across the normal east-west strike of the stratigraphy.

The combination of the geophysical characterization with the geological

18

and structural environment makes this location an extremely attractive

target for surface stripping and/or diamond drilling. As nearly as can

be determined from assessment file data, the EM conductor lies within

the "magnetic break" between lines 22+OOE and 24+OOE and crosses tie

line 11+OOS at about 23+50E. The "magnetic ridge" apparently lies

within the volcanics some 50 to 100 meters north of the

volcanic-metaconglomerate contact. A detailed magnetometer and VLF or

horizontal loop survey is required to accurately define, relative to

the present grid, the locations of the above-mentioned electromagnetic

and magnetic features.

Metaconglomerate Unit:

A polymictic metaconglomerate, some 300 meters to 700 meters wide,

extends east-west across the central portion of the property. It is

well exposed in outcrops south and west of Contact Lake and west of

Trench Lake. The main body is a very distinct unit composed of closely

packed and poorly sorted pebble and cobble clasts of many lithologies.

The less competent clasts tend to be well flattened and foliated,

whereas the more competent clasts, such as granitic cobbles, have

retained most of their original form. Near both the south and north

contacts the unit is characterized by finer grained sediments, which

have been extremely flattened and usually altered into lensy banded

schists. At some locations where the composition is mafic, the original

sediment has been completely altered into chlorite schist. This

schistosy suggests that at least some faulting has occurred along or

near both the north and south metaconglomerate-volcanic contacts.

19

Old trenches were observed at several locations within the metacon-

glomerate unit. Quartz carbonate veining occurs in several of these.

The most economically significant presently known quartz carbonate zone

is the gold-bearing section rediscovered in an old trench, within the

metaconglomerate unit, at 15+25S just east of line 5+OOW, (just south

of Trench Lake). This zone is described in detail later in this report.

Several trenches were located within the conglomerate unit north

of Contact Lake. Most of these appear to be old strip trenches which

are now covered with slumped in soil and debris. In one sizeable

blasted trench, on line 13+OOE at 10+75S, sercite and sercite-chlorite

schist, along with minor quartz carbonate veining and seaming, is

exposed along the trench wall. A sample from the quartz vein material

returned trace gold. Quartz carbonate veining also occurs within the

metaconglomerate at two old trench sites at 15+OOS on line 13+OOW and

at 16+OOS on line 14+OOW. A sample from one trench assayed 0.01 oz/ton

gold.

Area South of the Metaconglomerate Unit:

This area covers roughly the south one-third of the property and

includes the section south from the conglomerate to the property bound

ary. The underlying rocks include intricately intergraded mafic to

intermediate flows, minor tuffs and flow breccias, intercalated with

occasional narrow interlayers of felsic f?ows and tuff. Many small

interflow intrusive phases are also irregularly interspersed within the

volcanic sequence. This lithological characterization of this area is

well exhibited across section in the abundant rock outcrops west of

Beaver Lake near the southwest end of the property (Map 1).

20

The intrusives vary from quartz diorite to gabbro in composition,

commonly contain well saussuritized feldspars, and often exhibit saussu

rite seaming and minor quartz veinlets along fractures. At some loca

tions, where the intrusives contact sharply with flow structured

volcanics, they grade from a fine grain fabric to a medium grain fabric

and, at a few locations, to coarse grain fabric away from the contact.

However, at many locations this distinction is unclear. Therefore, it

may be that some units interpreted to be intrusives may in fact be

structureless massive flows. The intrusive units are abundantly exposed

from 13+OOS to 20+OOS along the two lines 2+OOW and 3+OOW.

The majority of the volcanics within this section are composed of

intergrading flows ranging from andesite to dacite in composition, with

the overall average composition trending towards the mafic side. They

occur mainly as weakly banded flows, are generally foliated, and often

exhibit saussurite seaming and clotting parallel to the foliation.

Pillow lavas, which were observed only at a few locations in this

section, are well flattened and exhibit a well foliated lensy banded

surface texture. The more mafic (andesitic?) pillowed flows have com

monly been completely altered into chloritic schist. Minor flow breccia

also occurs at several locations. However, unlike the well preserved

breccias on the north shore of Kingston Island, the breccias south of

the conglomerate unit, are generally well foliated, well flattened and

often sheared into streaky banded structures. Intercalated within the

mafic volcanics are occasional narrow rhyodactic to rhyolitic flows and

tuffs which range from less than one meter to about fifty meters in

thickness. Some of these contain thin (less than 20cm) cherty horizons.

21

There is no clear evidence that any single lithological unit

extends more than a few hundred nleters in distance. Rather, the whole

volcanic sequence is characterized numerous compositional intergrada-

tions both across and along strike.

Three northerly striking diabase dikes cut through the sequence:

a forty meter wide dike along line 25+OOW, a thirty meter wide dike

along the east side of line 20+OOW, and a dike (unknown width) along

line 4+OOW.

A few significant shear zones as well as many minor shears are

evident at various locations in the area. Shearing and associated

schistosy is most pronounced in the central part of the property immedi

ately south of the metaconglomerate-volcanic contact south of Trench

Lake. Here, in a 100 meter wide zone, the volcanics are either well

foliated or altered into schist for a strike distance of at least 1000

meters. Another zone of schistose volcanics follows close to baseline

20+OOS from 12+OOE to 28+OOE. At 20+OOS, 13+75E handstripping exposed

a well foliated mafic flow containing massive saussurite clotting with

crosscutting quartz veining. Quartz carbonate veining up to 20cm thick

was also observed in an old trench which cuts across a small shear at

6+OOW, 21+45S. A sample from the veining returned 0.009 oz/ton in gold.

22

GOLD ENRICHED QUARTZ CARBONATE ZONE AT TRENCH LAKE

(Map 4)

A gold enriched quartz carbonate zone up to forty meters wide is

exposed in old trenches at two locations (4+91W and 3+62W) near the

southeast end of Trench Lake. The trench at 4+91W varies from one to

two meters in depth and from one to two and one half meters in width.

It is about twenty-three meters long (from 15+17S to 15+40S). The north

end of the trench was mucked out to bedrock over a length of nine meters

(from 15+17S to 15+26S). Five meters of this section was blasted for

assay sampling.

It is from this north part of the trench, between 15+21S and 15+25S

that the most encouraging gold values were obtained. This section con

tains many quartz veins ranging from a few centimeters to about ten

centimeters in width. The veins dip nearly vertically parallel to sub-

parallel to the foliation and stratigraphy of a well carbonatized

schistose metaconglomerate host rock. Fine heavily disseminated pyrite

occurs in lense-like stringers and bands adjacent to the quartz veins.

A 30cm wide quartz carbonate vein, containing about 607o quartz and 407o

carbonate, lies at the south edge of the quartz veined zone. Jerry

Bruce, who collected several samples from this zone, reported (verbal

communication) encouraging assay results ranging up to 0.30 oz/ton in

gold. Two representative grab samples, taken by the author, from

blasted rock which contained quartz and pyrite, returned values of 0.034

oz/ton and 0.224 oz/ton in gold, respectively. The section from this

quartz veined zone to the north end of the trench, is composed of com

pletely altered brown weathered carbonatized schist with only a few

23

minor quartz veins. This part of the trench was cleaned off but not

blasted or sampled.

In the south part of the trench, stripping exposed a 25cm wide

quartz carbonate vein in chlorite and chlorite-sericite schistose meta-

conglomerate. A well carbonated outcrop of completely altered, lensy

banded, schistose metaconglomerate across four meters of section was

also exposed by stripping an outcrop some seven meters east of the

central (buried) portion of the main trench. A small pit in a quartz

veined zone was blasted out from this exposure for sampling.

The quartz carbonate zone is also exposed, apparently across its

width, by a set of two old trenches (North Trench and South Trench),

located just east of the southeast corner of Trench Lake. Both trenches

were mucked out and parts of them were blasted for assay samples.

The North Trench, which is about ten meters long, has been blasted

along a steep bedrock slope at the east edge of an open swamp. The

trench exposed a carbonatized chlorite and chlorite-sericite schistose

polymictic metaconglomerate composed of well flattened and foliated

pebble and cobble size clasts. A three meter wide section contains

abundant quartz veining irregularly formed in a complex variety of

knobby clot-like veins, lensy veinlets and seams. Minor local concen

trations of disseminated pyrite occur close to the quartz veins. A grab

sample of the quartz-pyrite rock returned 0.006 oz/ton in gold. Jerry

Bruce also reported (verbal communication) that he received similar low

values in gold from his sampling at this trench.

The South Trench starts five meters south of the North Trench and

extends thirty meters to open outcrop at its south end. This outcrop

is composed of schistose, lensy bands formed by an extremely flattened

24

fine pebble metaconglomerate. Abundant rather lensy quartz veining

occurs near the south end of the trench. At this location a small pit

was blasted into quartz veining which contains associated seams of

pyrite. Four samples from this material, obtained by the author,

assayed 0.006/ton, 0.012 oz/ton, 0.008 oz/ton and 0.017 oz/ton in gold.

About five meters north of the blast pit is a three to four meter wide

section containing 307o quartz in the form of knotty veins and veinlets

which coarsely parallel irregularly folded foliation. Small cross

cutting quartz veinlets (tension fracture fillings) are also exhibited

in this zone. Minor pyrite was observed in places. This section has,

as yet, not been blasted out for assay. A grab sample of the quartz,

taken by the author, returned a value of 0.004 oz/ton in gold.

The remainder of the trench is mainly underlain by variably carbon-

atized chlorite schist and minor chlorite-sericite schist. Well foli

ated and flattened pebble and cobble clasts are clearly recognizable

only across seven meters of section at the north end of the trench.

At other locations the original fabric has been completely obliterated

during the alteration, foliation and recrystalization process.

Quartz carbonate veining and carbonatization is also exposed in

stripped bedrock, east of the trenches, at picket lines 3+50W and 3+OOW.

Except for the above-mentioned exposures, most of the carbonate

zone remains covered under shallow to moderate depth overburden. The

westward extension of the zone from the trench at 4+91W, and the east

ward extension from the line 3+OOW, remains undefined. The width of

zone also remains undetermined except for the one location along the

two trenches at 3+62W and 3+76W. Nothing is known about the strike

25

length of the very encouraging gold-bearing section encountered in the

exposure in the trench at 4+91W.

It is not unreasonable to assume that other significant

gold-bearing locations might underlie the overburden covered area within

this carbonated zone. Mechanical strip trenching would certainly be

the most cost effective method to expose and define such locations in

this area. It certainly could be well utilized to at least determine

the surface limits of the gold mineralized section discovered at the

4+91W trench.

26

SUMMARY AND CONCLUSIONS -

Geological and Structural Aspects

Most of the property area is underlain by a complex easterly trend

ing and nearly vertically dipping sequence of metamorphosed mafic to

intermediated volcanic flows, volcaniclastics and related interflow

intrusives, occasionally intercalated with narrow units of rhyodacitic

to rhyolitic flows and tuffs. This volcanic-intrusive system is inter

rupted by considerable dislocation along the Paint Lake Fault, and by

a 300 meter to 700 meter wide polymictic pebble-cobble metaconglomerate

unit which extends east-west through the center of the property. Sev

eral Proterozoic diabase dikes cut northerly through these Archean

rocks. Offsets of the dikes along the Paint Lake Fault system suggest

that fault movement continued well into the Proterozoic era.

The whole system has been subjected to considerable alteration and

deformation on a regional scale. The volcanic-intrusive units exhibit

pervasive saussuritization of plagioclose feldspars, which suggests that

an abundance of low temperature volatiles occurred during the rock form

ing process. This aspect may have been a significant factor in the

early stages of gold enrichment in the area.

In the less competent structures and compositionally more ductile

rocks, the original texture and fabric has been almost completely obli

terated at many locations. Flow structures in the more mafic volcanics

are flattened, foliated and often altered into mafic schists. Mafic

tuffs, lapilli tuffs, and flow breccias are commonly "blended" into

lenticularly banded schistose units, now essentially undistinguishable

from each other. These commonly exhibit secondary alteration in the

27

form of chloritization, carbonatization and saussurite seaming and clot

ting, often with quartzitic cores in the more sizable clots.

Small dioritic to gabbroic interflow intrusives occur at many loca

tions. Most of these are small, massive, fine to medium grained units

interlayered within the flow structured volcanics. Only rarely do they

grade into coarse grained centers. At many locations there is no clear

distinction between massive coarse flows and finer grained intrusives.

Therefore, some of the units which are mapped as intrusives might

actually be centers of massive flows.

The whole volcanic-intrusive sequence displays considerable and

intricate compositional variations across section. These variations

are related to primary differentiations upon which a complex variety

of secondary compositional changes and alteration have been superim

posed. Fault related stresses and the resulting structural dislocation

and deformation have no doubt played an important role in the secondary

alteration process. These structural dislocations also have provided

conduits for the flow and concentration of silica enriched fluids in

which gold has been entrapped. The quartz-veined, gold-enriched quartz

carbonate shear zone just south of Trench Lake is a good example of this

development.

A major zone of displacement occurs along the Paint Lake Fault sys

tem. From the Namewaminikan River, near the west end of the property,

the fault follows easterly through the. property along a linear topo

graphic low which is covered by a series of swamps and elongated lakes.

Subsidiary subparallel faulting is signified by a zone of well foliated

to schistose and, in part, carbonized volcanics extending as far as 300

meters south of the main fault line. East-west trending shearing and

28

schistosity, of varying intensity, also occurs at many other locations

within the volcanic sequence, suggesting that numerous minor disloca

tions have also occurred throughout the property area. Quartz and

quartz carbonate veining and lensy seaming is commonly associated with

these structures.

Some 200m to 400m south of the Paint Lake Fault line a polymictic

pebble-cobble metaconglomerate, about 300 meters to 700 meters in width,

extends east-west across the property. The main body of this unit is

characterized by variably deformed, closely packed, poorly sorted clasts

of many lithologies. The unit is also characterized by finer grained

extremely flattened and foliated sediments along both the north and

south volcanic contacts. Fault shears which occur along or near these

contacts commonly contain varying amounts of quartz and quartz carbonate

veining and seaming. Quartz carbonate veining also is evident well

within the conglomerate unit at a few locations west of Trench Lake.

Locations of Potential Economic Interest

Four main areas of interest are suggested for further exploration.

The most significant of these is the gold-bearing quartz veined, quartz

carbonate zone exposed in two trenches at the southeast end of Trench

Lake. The second and third areas of interest are underlain by well

foliated to schistose volcanics which lie between the Paint Lake Fault

line to the north and the metaconglomerate unit to the south. One area

is located between lines 4+OOE and 9+OOE and the other is situated

between lines 16+OOE and 26+OOE. Although no substantial quartz zone

was observed in these two areas, quartz carbonate seaming and lesser

thin quartz seaming and lenses were noted in several of the outcrops.

29

It is quite possible that more noteworthy quartz carbonate sections may

exist under the generally shallow overburden, which lends itself well

to bulldozer and/or backhoe stripping. The fourth area lies close to

Baseline 20+OOS between lines 12+OOE and 23+OOE. Along this zone

considerable shearing (minor faulting) is evident in mainly intermediate

volcanics and some poorly exposed rhyodacite and felsic tuff. This zone

is also characterized by rusty pyritic locations, quartz veining,

quartz-carbonate veining and seaming and heavy saussurite clotting with

cross cutting quartz veinlets.

In all the four above areas, mechanical stripping would not only

be a cost effective method to search for gold bearing zones, but it also

could be utilized to delineate the extent of these zones and expose them

for detailed sampling.

For a more informative evaluation, a detailed VLF and magnetometer

survey should first be conducted over these locations, particularly on

the area north of Contact Lake where results from an earlier geophysical

survey, by Dome Exploration, suggests that an underlying EM conductor

follows a structural break.-

A number of other less notable locations of interest such as quartz

veins, quartz carbonate veins (usually but not always associated with

shearing) and concentrations of saussurite clotting with associated

quartz veining were observed and recorded. Old trenches were found at

some of these locations. A prospecting and sampling program might

return sufficiently encouraging results to warrant additional and more

advance exploration in some of these areas.

Fault associated carbonatized volcanics, some of which contain

associated quartz and/or quartz carbonate veining, apparently occur at

30

many locations along the Paint Lake Fault system. From the author's

personal knowledge, three such areas with gold occurrences are noted

here: 1) several locations on the Metalore gold property in Irwin Town

ship; 2) the area just northeast of Bearskin Lake in Walters Township

(several gold-bearing quartz veins, either associated with carbonated

breccia or striking off from a quartz carbonate zone); 3) several loca

tions of gold-bearing quartz veining in quartz carbonated volcanics on

the "Missing Link" prospect in Lapierre Township. A fourth significant

zone should be considered to the gold-bearing quartz carbonate structure

located at the southeast end of Trench Lake on the Caviar Resources

Leduc Township property. All of these lie roughly on strike, and essen

tially within the same lithologic and structural units: along a length

of four townships. All have similar depositional characteristics and

structural relationships. All contain significant gold enrichment (at

least locally).

The point of this observation is to show that the Caviar property

is very favourably situated within a sizeable geological and structural

trend that contains several significant gold occurrences (one on the

property itself). To date, the property has only undergone a cursory

examination consisting mainly of geological mapping and the examination

of a few old trenches. Even so, a very encouraging gold occurrence was

located. Therefore, the property certainly deserves a more complete

examination by a more advanced exploration program.

A suggested exploration program and budget, for this purpose, is

submitted under "Recommendations".

31

AUTHOR'S NOTE

I, Pentti Lassila, hereby state the following:

That I am a qualified graduate geologist with twenty years experience

in minerals exploration.

That I was contracted by Harold Watts of Watts Mining and Development

Ltd. and Caviar Resources Ltd. to complete for Caviar Resources Ltd.

and Dubawnt Resources Ltd. the mapping program outlined in this report,

including the report and maps presented herewith.

That I completed all of the mapping field work, report and maps present

ly submitted.

That I am responsible for the presentation of report and maps.

Pentti Lassila.

32

REFERENCES

Mackasey, W.O.

1975: Geology of Dorothea, Sandra and Irwin Townships, District of Thunder Bay; Ont. Div. Mines, GR122, 88 p. Accompanied by Map 2294, scale l inch to h mile.

1976: The Geology of Walters and Leduc Tuwnships, District of Thunder Bay; Ont. Div. Mines, GR122, 83 p. Accompanied by Map 2373, scale l inch to k mile.

33

APPENDIX 2

(Caviar-Dubawnt Property: Leduc Township)

ASSAY REPORT

ATEBA MINES INC. (Sept. 1988)

To Watts Mining and Development Ltd.

Sample Number

14326

14327

14329

14330

14331

14332

14333

14334

14335

14336

14337

14338

14339

14340

14341

14342

14343

14344

14345

14346

oz/ton

.006

.012

.011

.005

.009

.007

.008

TR

.017

.017

TR

TR

.048

.029

TR

TR

TR

TR

.006

TR

Remarks

3+55W, 15+45S, 9 V., (S.

3+50W, 15+45S, Vol. with

26+OOE,

9+OOE ,

6+OOW,

28+20E,

26+OOE,

24+OOE ,

10+OOW,

10+OOE,

0+25E,

13+75E,

4+OOW ,

26+OOE,

22+OOE,

22+OOE,

4+OOE ,

8+OOW,

3+5 OW,

9+OOE ,

25+25S,

3+40S,

21+40S,

20+35S,

20+35S,

20+50S,

7+10N,

22+65S,

15+75S,

20+OOS ,

15+60S,

25+25S,

12+7 OS,

12+70S,

21+50S,

15+90S,

15+OOS,

16+2QS,

Qtz-carb

Qtz, (In

Qtz Carb.

Qv, (Old

Qtz-carb

Qtz-carb

Trench)

py. , (S. Trench)

V

Creek)

(Old Tr.)

Tr. )

V

(Lake Shore)

qtz, lenses in vole.

Qtz-Carb

Qtz-Carb

Qtz-Carb

Qtz Carb

Qtz Carb

Qtz Carb

Qtz V.

Qtz-Carb

Qtz-Carb

V

Vs

Vs (cliff face)

V (near diabase)

V, (Old Trench)

V, (Old Trench)

V, (Old Pit)

V, (Old Trench)

Qtz V, (From Old Campsite

35

APPENDIX 2 (Cont'd)

Sample Number

14348

14349

14350

14351

14352

14353

14354

14355

14357

14358

14359

14360

14361

oz/ton

.013

.007

.005

TR

.01

.01

.009

.008

TR

.008

.017

.004

.224

Remarks

22+OOW, 1+OOS, 8" 9V, (OC)

22+10W, 4+45S, Py, 9V, (OC)

26+OOW, 16+40S, Qtz-Carb Shear, (OC)

18+OOW, 1+OON, cpy,py,silc,qtz V, (OC)

18+OOW, 1+OON, cpy,py,silc,qtz V, (OC)

13+50W, 15+50 , 9v in qtz-carb (Old Tr.)

18+OOW, 1+OON, py (qz.cpy), (OC)

18+OOW, 1+OON, py, cpy, calc, wall rk, (OC)

3+76W, 15+15S, (North Trench)

3+62W, 15+50S, (South Trench)



4+91W, 15+25S, (Au Zone Trench)

14362 .034 4+91W, 15+25S, (Au Zone Trench)

Sampled by: P. Lassila

36

APPENDIX 3

NAMES AND ADDRESSES OF WORKERS (May 15 to August 31, 1988)

(Caviar-Dubawnt Leduc Township Property)

Linecutting: N. McBrideP. O. Box 112NOTRE DAME DU NORD, Quebec.

Mapping: P. Lassila 68 Albery Crescent AJAX, Ontario L1S 2Y3

Assistant: R. Letang366 Markland Street THUNDER BAY, Ontario P7B 2J1

Trenching: J. BruceGeneral Delivery JELLICOE, Ontario POT 1VO

D. Brackenridge2614E 20th Street, #L-6FARMINGTON, N.M., U.S.A.87401

J. KoskiGeneral Delivery BEARDMORE, Ontario POT 1GO

37

Northern Development r l ,and Mines (Geophysical, Geological, l WQQOA

Ontario ^ Geochemical and Expend!tunesr"

M

—If number o f^mining claims traversed

Type of Survey(s)

______Claim Holder(s)

at/ i t

&L jeoj. ~. O q J~ ' "

AddressLi

42E12NE8020 Z , 11875 LEDUC

i* JBL JL x.^* ^900

Survey Company

JL

,

Name and Address of Author (of Goo-Technical report)

Zt-rs. .Ala* .

[5ate of Survey (from Si to)3 f ] To7al Miles of line Cut /4 Ma;* imj/ A** M U* Day! MoT l Yr. t)av l MdflYr. —————-—l———^— 4.-- -.*.i—— .—————l————————l——————

Credits Requested per Each Claim in (Sflumfis at righ'tLI S-

Special Provisions

if For first survey:

Enter 40 days. (This includes line cutting)

For each additional survey: using the same grid:

Enter 20 days (for each)

Man Days

Complete reverse side and enter total (s) here

Airborne Credits

Note: Special provisions credits do not apply to Airborne Surveys.

Geophysical

- Electromagnetic

- Magnetometer

- Radiometric

- Other

Geological

Geochemical

Geophysical

- Electromagnetic

- Magnetometer

- Radiometric

- Other

Geological

Geochemical

Electromagnetic

Magnetometer

Radiometric

Days per Claim

ffi

Days perClaim

Days per Claim

Mining Claims Traversed (List in numerical sequence)

Expenditures (excludes power stripping)Type of Work Performed

Performed on Claim(s)

Calculation of Expenditure Days Credits

Total ExpendituresTotal

Days Credits

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

Total number of mining claims covered by. this report of work.

Date Recorded Holder or Agent (Signature!- -*~

Certification Verifying Report of Work

Total Days Cr.lDate Recorded Recorded

l hereby certify that l have a personal and intimate knowledge of the facts set forth in the Report of Work annexed hereto, having performed the work or witnessed same during and/or after its completion and the annexed report is'true. ^^^^

Name and Postal Address of Person Certifying

P fn ttV /-0j-3ilq 6 ft A/bfr&j As**, /sDate Certified

. CCertified by (Signature)

Ministry ofNorthern Developmentand Mines

Ontario

ReporvofWork(Geophysical, Geological, . Geochemical and ExnpnriituA'^A/RoOA'

uctl

Mining Act

If number or mining claims traversed exceeds space on this form, attach a list.

Note: — Only days credits calculated in the "Expenditures" section may be entered in the "Expend. Days Cr." columns.

— Do not use shaded areas below.Type of Survey(s)

Claim Holder(s)W.JW.

' ' ~ -

Town

L

Address

-"T.cj '

Pownship or Area o /**i/ ~J~

L e d u c TotA/nship j On t."kX

f OProspector'* Licence No.

ft M FiovY.fto^JPurvey Company f / of survey (from Si to)

/H3

Name and Address of Author (of Geo Technical report),-ij^V

A*** lin }t , fay /W.LM91 ! Y.r-J Day l Mo- i V r- l -

C-/V* j- 0*

ITotal Miles of line Cut

Credits Requested per Eacn Claim in Columns an rightSpecial Provisions

Jf For first survey:


For each additional survey: using the same grid:


Man Days

Complete reverse side and enter total(s) here

Airborne Credits


Geophysical

- Electromagnetic

- Magnetometer

- Radiometric

- Other

Geological

Geochemical

Geophysical

- Electromagnetic

- Magnetometer

- Radiometric

- Other

Geological

Geochemical

Electromagnetic

Magnetometer

Radiometric

Days per Claim

4-0

Days per Claim

Days per Claim




Total Expenditures

S -f- 15

Total Days Credits

=

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

Date Recorded Holder or Agent (Signature)



Total number of mining claims covered by this report of work.

l hereby certify that l have a personal and intimate knowledge of the facts set forth in the Report of Work annexed hereto, having performed the work or witnessed same during and/or after its completion andthe annexed report is true.

Name and Postal Address of Person Certifying

I en ffi L-OSfilo wij. A J** ii~ Dal* Certified Certified by. (Signatur


Report of Work(Geophysical, Geological,

Ontario(li

DOCUMENT No.

Geochemical and ExpenditJr^ygoQ/ 1tl^Mining Act

Type of SurveyU)

— If number of mining claims traversed exceeds space on this form, attach a list.

Note: — Only days credits calculated in the "Expenditures" section may be entered in the "Expend. Days Cr." columns.

- Do not use shaded areas below.

_____Claim Holder(s)

Address

Township or Area

W w

Prospector's Licence No.

5/70

Survey Company,f [Date of Survey (from Si fo)

' ~-

Name and Address of Author (of Geo-Technica! report)l l Yr.

Total Miles of line Cut

Credits Requested per Each Claim in Columns at right

OH f-r* f * J ^T,.

!^?__________

Special Provisions

7jf*For first survey:


For each additional survey.' using the same grid:


Man Days

Complete reverse side and enter toial(s) here

Airborne Credits


Geophysical

- Electromagnetic

- Magnetometer

- Radiometric

- Other

Geological

Geochemical

Geophysical

- Electromagnetic

- Magnetometer

- Radiometric

- Other

Geological

Geochemical

Electromagnetic

Magnetometer

Radiometric

Days per Claim

4-0

Days per Claim

Days per Claim




Total ExpendituresTotal

Days Credits

15 -

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

Date

"__S

Recorded Holder o^Agent (Signature)



Total number of mining claims covered by this report of work.

Total Days Cr. Date. Recorded Recorded

l hereby certify that l have a personal and intimate knowledge of the facts set forth in the Report of Work annexed hereto, having performed the work or witnessed same during and/or after its completion and the annexed report is true.

Name and Postal Address of Parson Certifying

r 6'8 A j a*, 0*t. A/SCertified bvtSlgnalure)Date Certified

Ontario


Ministere duDeveloppement du Nord et des Mines

December 29, 1988

Mining Lands Section 3rd floor, 880 Bay Street Toronto, Ontario M5S 1Z8

Telephone: (416) 965-4888

Your file: W8804-543.544& 545

Our file: 2.11875

Mining RecorderMinistry of Northern Development and Mines435 James Street SouthP.O. Box 5000Thunder Bay, OntarioP7C 5G6

Dear Sir:

Re: Notice of Intent dated December 14, 1988 - Geological Survey submitted on Mining Claims TB 815313 et al in Leduc Township

The assessment work credits, as listed with the above-mentioned Notice of Intent, have been approved as of the above date.

Please inform the recorded holder of these mining claims and so indicate on your records.

Yours sincere

y W/R. Cowar"7" Provincial Manager, Mining Lands

Mines S Minerals Division

SH:pl Enclosure

cc: Mr. G.H. Fergus Mining and Lan Toronto, Ontar

Caviar Resou 18th floor, R Toronto, Onta M5J 1E3

Resident Geologist Thunder Bay, Ontario

Mr. Pentti Lassila 68 Albery Cres. Ajax, Ontario L1S 2Y3

Ministry ofNorthern Development

/tinesOntario

Technical Assessment Work Credits

Oat*

December 14, 1988

Pila

2.11875Mining Recorder's Report ofWork S8804-543

Recorded Holder

Caviar Resources LimitedTownship or Area

Leduc TownshipType of survey and number of

Assessment days credit per claim

Geophysical

Other Hays

Section 77 {19) See "Mining Claims Assessed" column

Geological 34 days

Geochemical . rfcys

Man days | | Airborne [~]

Special provision (X] Ground K1

JT1 Credits have been reduced because of partial coverage of claims.

[~~1 Credits have been reduced because of corrections to work dates and figures of applicant.

Mining Claims Assessed

TB 815313 to 325 inclusive 830882 to 893 inclusive 907254-55

Special credits under section 77 (16) for the following mining claims

No credits have been allowed for the following mining claims

| | not sufficiently covered by the survey |~~| insufficient technical data filed

The Mining Recorder may reduce the above credits if necessary in order that the total number of approved assessment days recorded on each claim does not exceed the maximum allowed as follows: Geophysical-80; Geologocal - 40; Geochemical - 40; Section 77(19) -60.

828 (85/12)


Ontario;


Dete

December 14, 1988

File

2.11875Mining Recorder* Report ofWork hv8804-544

Recorded Holder


Leduc Township

Type of survey and number of Assessment days credit per claim

Geophysical

Radiometrir rifiyij

Induced pnlarJ7Atinn riayi

Other Hays

Section 77 (19) See "Mining Claims Assessed" column

Geological 33 ^y,

Geochemical Hayi

Man days Q Airborne Q

Special provision | | Ground l i

l l Credits have been reduced because of partial coverage of claims.

l | Credits have been reduced because of corrections to work dates and figures of applicant.

Mining Claim* Assamd

TB 813393 to 396 inclusive 813403 to 412 inclusive 830910 907211 to 219 inclusive



[ | not sufficiently covered by the survey l~~l insufficient technical data filed

The Mining Recorder may reduce the above credits if necessary in order that the total number of approved assessment days recorded on each claim does not exceed the maximum allowed as follows: Geophysical-80; Geologocal - 40; Geochemical - 40; Section 77(19)-60.

628 (85/12)


/linesOntario


Date

December 14, 1988

File

2.11875Mining Recorder'* Report of Work No.

U8804-545

Recorded Holder


Leduc TownshipType of survey and number of

Assessment days credit per claim

Geophysical

Magnetometer riays

Section 77 (19) See "Mining Claims Assessed" column

Geological ^3 days

Geochfitninal Hays

Man days l j Airborne l j

Special provision fc~j Ground Q

[x! Credits have been reduced because of partial coverage of claims.

l | Credits have been reduced because of corrections to work dates and figures of applicant.

Mining Claims Assessed

TB 813397 to 402 inclusive 815326 to 331 inclusive 830873 to 881 inclusive 907220 to 228 inclusive



| | not sufficiently covered by the survey [ | insufficient technical data filed

The Mining Recorder may reduce the above credits if necessary in order that the total number of approved assessment days recorded on each claim does not exceed the maximum allowed as follows: Geophysical - 80; Geologocal - 40; Geochemical - 40; Section 77(19) - 60.

B28 (65/12)

RicKobyTwp.. GrlGIJ H '

42M

v V/42 M Expansion Lake'

K i niya tf Dior aova 3 1 wtvi j o ava .

008 laMOIcN-' 618 /0121 81001* l 815016 l f'lftOJe"! '

6^66676J8666T5

' 8514611 83 l 464 .831 466 "86326

it , 8IS-P41'815069

~ *848233 I 86286S ( 682*60

E663 Tis a e 3720.

? Clist LxikeAr^*-i V - ' * ' ? (*- '- ' ' * *- ' ' . r * - j,-- *

l ,1* T J l *' *42EiaNE00a0 2.11875 LEDUC

NOTES

400' SURFACE RIGHTS ^RESERVATION, .ALONG ' THESHORE OF All LAK.ES RIVERS.

i AREAS WITHDRAWN FROM DISPOSITIONFT"*'' .---~ - - — - '—-•'•••~ -..-~,.. r . .r -..--.. , - , .., -- -" f ^-.

S.R. - SURFACE BIGHTS M.R.-- WNtNQ FI|tt'ltt,^

DESCRIPTION "•••-.'.prtQgR HO. ffATE DISPOSITION- FILg

(Ri) SEC. 36/60 W.29/63 20Y10/83 f S,f. , ~ - ' l 8852 8

@ SEC. 3a/ 60 W-14/82, B/ H/ 82 S.R. .'V985E8

LEGEND

PATENT, SURFACE ft MINING. RIGHTS-.^J^-w^.SURFACE RIGHTSONLY.^!:'.'.^.

" , .MINING RIGHTS ONLY I.. J.....'. LEASE. SURFACE ft MINING RlQHTS—— l

", .SURFACE RIGHTS ONLY-'^-^-— l" \MINING RIGHTS ONLY.r—;--.*.—,—..--j/H

LICENCE OF OCCUPATION ....* 1.^,1;;.,-—-..-lfe'''T

ROADS , v. V ' IMPROVED ROADS* - ' "^ , K/NG'S HIGHWAYS " . , , ; RAILWAYS '/! POWER LINES x ' ' . 4 x ••' MARSH OR MUSKEG ,

,,MINES .. . ''' ' -, : ;- J. CANCELLED .

SCALE: 1 INCH-40 CHAI MS

FEETO 1000 20OO 4OOO 6000 BOuO

' O 200 METRES

200011 KM)

"W "SH"DEC 01 W

LEDUCM.N.R. ADMINISTRATIVE DISTRICT

NIPIGON QMINING DIVISION ^^ . -v

^THUNDER BAY /ULAND TITLES/ REGISTRY DIVISION f"'

THUNDER BAY ^- Ministrypf , '"'Natural '

' Resources

Land '', ]

Management Branch ; ';

Ontario

0t1tFEBRUARY, 18th, I96I

G-169

i,

-O O

g G5

"n

"f

i P?

f -T

D so

^

r*

fk

r\

033

sy a ±1 w

OOt?oosooto

'310N

3 x v/1 wy v

l (.A l O

VI H 4-

pu o s v^.. :doc! ' ""

,s; ^tC^""^*soo-f o r

SOOfbf 18*JLM ) J. ^^———-^

l ('*uft*}*tf I^TH'

- -OtJ or!(7

/•j-d) fc we/V

oo 17 f j a

^J-s-^

p n c s j j

V/A 3 W \/ N 3 A i y

. ....(__t~ ; T

p w o 5

o y g g v 5

NOISN Vd X3

Oom

01-*- O O m

o o m

oo-K

o om

IM -t- O O m

O-h

Oo

Oorr.

O O

N-hOo

ooH-

O O

OO

01 -v- OO

O O

OoOD

-f- Oo

H-o-*- o o

-t-

3/53228/5 3/7

NAME WAM I NI RIVERXI53IS

^n X'*Js" 'C

S32"/

2 n o 5 f. w*wo x?3 ^ !*~r~*'x~-) -ti-—————*^-^

be,"dce1 t *ev fhit**rJ

8153/4

^..:'.'-

^t—r o 4*p*

; lfr-0

PORTA6E LAKE

- "S H not '

83087

830676 60NTAC T LAKE

,,U'-^

~^

7 ; K 30883i\;

\ \ 8 30862

830888**}'\tf?

Se o/e ' l .'2500NOTE! See ^op l ^oh Legend ond

/St

15 S

SO

UT

HW

ES

T

TR

EN

CH

t S

i- 2

0 S

c.o*-

to h

q-fv

a It

tt r

e c

J

^-oe

k

"l

J rn

w

i'-'

carb

**.

'fh

S

om

eat is

S.

Q"C

/ J*o

t-r*

j

J f 3

6 2

0

,23

4-

e**

/*

'l

caK

bonafi'i*c/

Ovevb

urd

en

c

o v*

r r

re*

k

j ur

*-tf

w

l 5

-f- 405

4-5

S

Li n

fi

IS4

50 S

TB

8

13 S

c Q

le!

l c ,

*

o|O

M e

t e

t- s

TR

EN

CH

M

AP

25"

S L

OC

A T

/ O

N oS

cale

1, l

cho.

s

5

2,5

M e

t e

h s

TR

EN

CH

L

OC

AT

ION

HS

T

TR

EN

CH

L

AK

E

TB

81

33

9^

42E

12h

C08

20

2.1

18

75

LE

DU

C2

40

NQ

RT

H

TR

EN

CH

Zone

, o

f "n

arro

w

qtz.

y

stn

5

f e

i M i

' n ^

, i'

n p e

fc

fc ft

- c

t. b

h l

e '

C 4

- p

m r

,

Old

pit

at.

'zfi

c/,

fois

ted,

h t f "

"*"

* " ^ ''

r'

A

''o

C a

H b

o r

i w ^

f z.

e J

ch

/or

C

K l

o*-

S

C k

t l!

/O

tt

e n

e J

,'M

t t

*-

rv,

e t/

i' Q

1 1

C h

lo

f-

SC

h f

loe k

s /ik

SOI;T

H TR

ENC

HT

hr'n

bo

nc/t

d

c T

z -

FI'

n--

/ly

b

O ^

,'^

fic/

5

^

h

( C

ar

o.

5 l

'C f

^i

i .

c. M

e f

, ^e t-

J

o /^

erat

ton

3 t

h to

S t

* t

*^

;

S *"

-. p

/,

o. 0

^4 o

t/t

cH

tot-

i-jn

d

c h

l c

-ser

Mf

tt-tqV

S.

Of o

-"-.

: r0

r "

'

t^-c

fr

o/,

,-,

Bo o

c^.

'r.

o.c

j e

- l.'k

*

c

an

d

i' r

-- i

cj u

le* r

e

U t -

* lo

t t

c1 r;

6 J

f

i' ne

-' : f

f - c

^

j cl c

c a

i i'

c r,

s

B L

IS-f

75

S

Sea

le

!IO

J

Mete

rs

TR

EN

CH

M

AP

3t6

0 W

,

15+O

OS

L

OC

AT

ION

TE

?

Se

e

M0p

l ^0

1-

Le

ge

nd

a

nd

S

y no

bois

CA

VIA

R

RE

SO

UR

CE

S

P

LED

UC

TW

P.

ON

T

TR

EN

CH

G

EO

LO

GY

TR

EN

CH

LA

KE

A

RE

A

Date

.1 N

ov.

'^8

8

By

: f?

/.o

'*sf

/a

Z m H

FT 33 ut

O

(f} O

D

o O

KJ U1 O O

o o

M \ ^ J ^ TJ *-*

a

o r*- Z

0

r0

-s

m

m

*

S

0

e-o

rn

r~

p.

ooo

W

o,

-i

ro

H

0

5

H

CTi

jj

o~r

^^

* 33

^

CRT

IT

-^-

U7ve

H

-^

X

Sfcrf

"^

—

-T -o

^

r -x -y

o c/i 51

; ?

j .•( 01.

i ii

i iff it

m

' a

M i

imti "* J

i^

m*f

f .a

^*i

i ^

*BH

ifcii*

i1*f

^*g

^^

Pi

DO >

0

j.

S

m

m

0(A

C

"D

P*JO

[T

O "D

>m

^J3

^

—

Orn

c

^

03 ^ J H

BH

B*

LEDuc

8/5323

.L A KE

8/5329

. r.,, j,, 8907228

v n c* l -L

815 3 24

8/53248 f 5 330

90722 7

RIVER1IN l KAN

'*,* (r"'k) ^9*5C"' ' ^^-^,/JrcMo.-

S a n c

-f a,, H brtct t o, kink fcirts \ **i.'m. qft

Lake

TU 1 0+Q.QSO c ^'or sch f

0722.6

. ^ 3*?x?^i,afooS a n J .-" F l o t

8/5-326

CO M T A

830878830879

g 3.6 (mas*

P O /ST D

813401

^30874

St 2Ot"QPS

fl 1 ORKI830875-

ARM L AKE5 +DOS

CAVIAR RESOURCES /AND D U B A V* N TRESOURCES P R op E R T/ es

co/ej i : 2500 LE D UC T OWNS HI P TARIO

MOTE.' See map L for Legend and Symbofe

G E OL06Y M APr CENTER SHEET)'

Dote! NOV. f*M8 By ; fi

MAP 2

13 L O fOO RICKABYLEDUC T WP.

8/53/7

907254

#15318

8153)5

LONGqt-l~tc

breccia (7o-*lto*k

8153/3

8/53/4/3r ( h

*P*I3 Tjr jt

ne1 /'So S

d- < ' ,830^85..'

83089/

ONTAC T LAKE

S^y^-V-2 ^^

V 8308?2

.SortcV P'^J rt s. ^e

So,^cJ \

3068222 + OOS

NOTE'. S*e Legend andSca/e ' l : 2500

roo 2^0 300 4-00

CAVIAR RESOURCES AND PU

R E SOURCES P ROPE R Tl fS

LEDUC TOWNSHIP

O N TA R f O

- G EOLOGY M AP (EAST S HEET;

Date 1. NOV. \ 388 B y! P L 055 i1 la

MAP 3

AND PROSPECTING PROGRAM IN LEDUC TOWNSHIP, ONTARIO … · 42e12ne002a 2.11875 leduc 010 report on...

Documents

Transcript of AND PROSPECTING PROGRAM IN LEDUC TOWNSHIP, ONTARIO … · 42e12ne002a 2.11875 leduc 010 report on...