010

EXPLORATION FOR ZINO IN SOUTH-EASTERN ONTARIO

SLAVE LAKE AREALITTLE MUD LAKE AREA

KALADAR AREA

BY

OR. WINFRIED BRACK

OPAP 91-782

JANUARY 1992

31C108W0009 01*1-782 SHEFFIELD

TABLE OF CONTENTS010C

SUMMARY ................. ............................ i

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

2. PROJECT A: SLAVE LAKE ......... ..... ........ 32.1 Description, location and access ....... 32.2 Geology ............. . .. .... ...... ..... . 42.3 Previous exploration activities......... 52.4 Exploration activity: prospecting ...... 6

3. PROJECT B: LITTLE MUD LAKE .... ........... ... 83.1 Description, location and access ....... 83.2 Geology and previous exploration activity 83.3 Exploration activities:

3.3.1 air photo lineaments ......... 103.3.2 orientation survey ........... 113.3.3 grid line establishment ...... 113.3.4 prospecti ng ...... . . . . . . . .. . .. 123.3.5 geochemical soil sampling .... 13

4. PROJECT C: KALADAR .......................... 224.1 Description, location and access ....... 224.2 Geology ................................ 224.3 Previous exploration activity........... 224.4 Exploration activity:................... 24

4.4.1 air photo lineaments ......... 244.4.2 grid line establishment ...... 254.4.3 radiometric survey ........... 254.4.4 prospecti ng .................. 264.4.5 geological mapping ........... 264.4.6 trenchi ng .................... 284.4.7 rock geochemistry ............ 314.4.8 thin section description .... 36

5. CONCLUSION AND RECOMMENDATION ............... 40

REFERENCES 41 CERTIFICATE

PICTURES

Picture 1 SW tip of the south-eastern marble unitat Donahue Lake ........................ 27

Picture 2 Trench 2, NW corner concession VII, lot 2 30

TABLE OF CONTENTS (CQNT'D)PAGE

LIST OF FIGURES

Figure 1 General location mapProject areas ............................ 2

2 General location mapLittle Mud Lake and Slave Lake projects .. 9

3 General Location mapKaladar project .......................... 23

4 Kaladar projectTrench 2 ................................. 29

5 Kaladar projectPosition of trenches ..................... 29 A

LIST OF TABLES

Table 1 Rock sample description for the LittleMud Lake area ............................. 12

2 ICP atomic emission spectroscopy,detection limits for 28 elements .......... 15

3 Geochemical analysis: statistical data ... 154 Sample description for 75 soil samples

from the Little Mud Lake project.......... 185 Sample description of 55 rock samples

from the Kaladar project ................. 31

APPENDIXAnalytical results (geochemistry)

MAPS

Map 1 Slave Lake project, prospecting traverseswithin the north-western claims .......... 7

2 Little Mud Lake project, grid lines, soilsample locations, prospecting traverses .. 14

3 Little Mud Lake projectAir photo l i neaments ..................... folder 1

Geochemical contour maps for the Mud Lake folder 2 area:

4.1 Contour map for calcium ................... 24.2 Contour map for magnesi urn ................. 24.3 Contour map for zinc ...................... 24.4 Contour map for copper .................... 24.5 Contour map for lead ...................... 24.6 Contour map for manganese ................. 2

5. Kaladar projectAir photo lineaments ..................... folder 1

6. Kaladar projectGeological map ........................... folder 3

7. Kaladar projectRadiometric map .......................... folder 4

SUMMARY

Three different sub-projects were investigated. The Slave Lake project, which was partly investigated in 1990 (OPAP-435) was optioned by Willow Resources Limited. The executed prospecting of the north-western claims eliminated this area for further mineral exploration.

The Little Mud Lake project was a follow-up project of the Slave Lake project. The anticipation of occurrences of further unmapped marble lenses in this particular area was not confirmed.

Within the Kaladar project area three distinct bands of marble occurrences were mapped. The discovery of a 350 metres long quartz vein with an elevated gold value (25 ppb Au) is encouraging. The north-west corner of the property with the recorded high zinc value of 27X zinc remains unexplained.

The Slave Lake area is optioned to Willow Resources Limited, therefore no further work on the claims is possible under the umbrella of the OPAP program. The Little Mud Lake area is eliminated as a potential target area. The Kaladar project merits a follow-up program. The described gold bearing quartz vein should be investigated by trenching and detailed sampling. The old trench area on Concession VII lot 2 should be generously opened up by blasting to create a larger observation area in order to clarify the geological and mineralogical situation.

INTRODUCTION

This report summarizes the results of the exploration efforts completed by Dr. Winfried Brack in south-eastern Ontario. These activities were supported by the Ontario Prospectors Assistance Program (OPAP) and registered under the file number: OPAP 91-782.

The objective of the exploration activities was to locate zinc-sphalerite mineralization of economic interest hosted by marble occurrences within the Grenville rock suites of south eastern Ontario.

Although the objective remained the same, the completed exploration work differs from the original program proposal (see application OPAP 91-782). Due to the successful negotiation of an option agreement with WILLOW RESOURCES LIMITED for the Slave Lake claims (Sheffield and Hinchinbrooke Twps.), further exploration had to be abandoned. Confirmation for the program change was obtained by the Incentive Office by phone on September 9, 1991 for the Little Mud Lake area (Hinchinbrooke Twp.) and by facsimile on October 20, 1991 for the Kaladar project (Kaladar Twp.).

The Kaladar project is a joint project with W. Holmstead (OPAP 91-433). Originally an 8 unit claim had been staked for the Kaladar project (Kaladar Twp., concession VII, Lot 1 and 2). However, a staking error led to the refusal of these claims by the mining recorder. The claims were not restaked.

45* r

44*

GENERAL LOCATION MAR PROJECT AREAS

W.BRACK OPAP 91-782

L

2. PROJECT A: SLAVE LAKE

2.1 Description, location and access

The Slave Lake zinc property is located in the east-central part of Sheffield Township and the west central part of Hinchinbrooke Township in the Southeastern Mining Division of Ontario (see fig. 2). The claim numbers listed on the next page are recorded on Claim Maps M150 (Sheffield Twp.) and M104 (Hi nch i nbrooke Twp).

The property may be located by taking Concession Road 6 north from Highway 401 at Interchange 599 near Odessa. Slave Lake is located in Sheffield Township about 35 kilometres north of Highway 401. An all-weather gravel access road runs from Enterprise to Parham and the prospect is accessible from a vehicle trail which passes south of Slave Lake and joins the access road approximately 10 road kilometres north of the CPR crossing in northeast Camden East Township. Logging roads which are passable by pick-up truck in dry weather, provide good access to the claims east of Concession Road 6.

The area is marked by rolling hills and ridges of minor elevation intersected by narrow, shallow lakes and swamps. The vegetation is dominated by hard-wood such as oak, beech, maple and birch with minor stands of spruce and pine. Especially on exposed ridges and underlain by granite, patches of sumach bushes are common. The area was previously farmed but is now used for recreational purposes such as hunting and fishing. The investigated claims are on Crown land.

4

2.2 GEOLOGY

The geology of the property was described by Carter (1981).

The Slave Lake zinc prospect "occurs within a narrow north-to- northeasterly trending belt of marble that is completely contained within the Hinchinbrooke Gneiss, a large circular granitic intrusion. Calcitic and minor dolomitic marble, granite and amphibolite-biotite-plagioclase gneiss are exposed in the vicinity of the deposit."

"The calcitic marble is a white, medium to coarse grained (2 to 6 mm) rock composed essentially of calcite with accessory dolomite, graphite, phlogopite, serpentine, and tremolite-ntp. The marble is massive to poorly layered, the layers being defined by variations in the grain size and shades of grey. Dolomitic marble occurs in only a few outcrops and is similar to the calcitic marble in appearance."

"The granite is pink, fine to medium grained (1-3 mm) foliated to massive rock. It is characterized by "augen" of pink feldspar 15 to 25 mm long."

"The amphibolite-biotite-plagioclase gneiss is a grey to black, fine-grained (0.5 to 2 mm), massive to poorly foliated rock. The mafic mineral content varies from 15 to 50 percent. It may represent the metamorphosed equivalent of either mafic volcanic rocks or pelitic clastic sediments."

"The geological relationships of the different rock types are complex. The marble forms northwest striking units within granite that are closed around northwest-trending axes. The amphibole biotite plagioclase gneiss generally occurs as isolated xenoliths within the granite and forms a mappable unit in the east. Layering in the marbles and foliations in the granite generally dip consistently to the southwest at 20 to 85 degrees, with only local variations."

2.3 Previous exploration activity

Past work on the property was summarized by Malczak, Carter and Springer (1985) and is included with additional information below. The larger part of the work was done on the east half of Lot 10 which is not part of the subject property.

pre-1916 two pits were opened on the Slave Lake occurrence by unknown operators (Uglow 1916, p.48).

1935 Mr. Beausoleil acquired the property, carried out some exploration work and optioned the property to Lennox Mines Ltd.

1936-1937 Lennox Mines Ltd. optioned the property and excavated a shaft on the east half of Lot 10 to a depth of 50 feet, and 60 feet of drifting was completed. Two other shafts were also deepened, and 1000 feet of diamond drilling was completed. About 20 tons of high grade material was extracted from the No. 2 shaft and No. 4 Pit. In 1936, a 540 pound bulk sample was tested at the Mines Branch in Ottawa and was found to contain large disseminated grains of sphalerite in calcite gangue and assayed 57* zinc.

1938-1948 An unspecified amount of trenching was carried out by Lennox Mines on the east half of Lot 10. In 1947-48 a diamond drilling program brought the total drilled on the property to 5000 feet. At the same time the shaft was de-watered and surface mapping and prospecting were carried out.

1967 Paul Kingston (present Resident Geologist for southeastern Ontario) owned the claims and produced a report and geological map on the west half of Lot 10.

1990 W.Holmstead and W.Brack carried out an extensive exploration program in the Slave Lake area (OPAP 90- 435). It successfully outlined an area that is highly anomalous in zinc in the B horizon soils. The anomalous area is considered a valid anomaly and measures approximately 800 meters long and 100 to 200 meters wide. A magnetometer survey, a VLF electromagnetic survey, a surficial conductivity survey, geological mapping, an air photo lineament study and thin section description were completed.

2.4 Exploration activity: prospecting

On July 12 an 13, 1991 prospecting was performed on the north westerly claims of the Slave Lake property. These claims were not investigated in the previous exploration program in 1990. The prospecting focused on locating marble occurrences as the potential host rock for zinc-sphalerite mineralisation. No marble occurrence was located within the northerly claim boundaries. Several reference rock samples were taken but abandoned since they had no significance for the project. All the samples were of granitic composition.

The traverses and the area covered by observation are shown on map 1.

Subsequently to the prospecting the entire claim block was optioned by WILLOW RESOURCES LTD. Therefore no further exploration activity was warranted within the claim boundaries.

SCALE: 1 : 10,000

TRAVERSE 1 TRAVERSE 2

S BO

SLAVE LAKE PROJECT

PROSPECTING TRAVERSESWITHIN THE NORTHWESTERN

CLAIMS

W.BRACKOPAP 91-782

\\V"

8

3. PROJECT B: LITTLE HUD LAKE

3.1 Description, location and access

The Little Mud Lake prospect is located in the north-western part of Hinchinbrooke Township in the Southeastern Mining Division of Ontario (see fig. 3). It covers concession XI, lot 11 and 12 and concession XII, lot 11 and 12. No claims have been staked. The NTS is 31C/10SW. The hydro power line straddles the northern boundary of the prospect area.

The prospect may be reached from Kingston going north on highway 38 to Parham. From there a secondary paved road leads to the west. Approximately 14 kilometres from Parham towards the west end of Fifth Depot Lake an unmarked trail leads towards the south-east to Little Mud Lake. The trail may have been used as a power line access road. It reaches the north- central portion of the investigation area after approximately 2.5 kilometres.

The area is marked by rolling hills and ridges of minor elevation intersected by narrow, shallow lakes and swamps. The vegetation is dominated by hard-wood such as oak, beech, maple and birch with minor stands of spruce and pine. Especially on exposed ridges and underlain by granite, patches of sumach bushes are common. A hydro power line intercepts the investigation area in a east-westerly direction and is an excellent marker for orientation. The investigated lots are Crown land.

3.2 Geology and previous exploration activity

The geological framework is the same as described in paragraph 2.2 The prospect is part of a rock sequence, which contains granitoid intrusive rocks, meta-sediments and marble overprinted by metamorphism of Grenville age.

No records of past exploration work have been found. However, past work in the vicinity of the prospect to the south-west indicated sphalerite mineralization along a major marble- granite contact. Within this area previously unmapped marble lenses with potential sphalerite mineralization have been discovered (see OPAP 90- 435 Slave Lake Project).

The objective of the work program is to define the possible extension of the known mineralized zones in the Slave Lake area towards the north-east into the Little Mud Lake area and explore for the presence of additional undiscovered mineralized marble zones.

(SLA

VE LAKE PROJECT^

- NORTH-WEST CL

AI

PROJECT AREA

GENERAL

LOCA

TION

MAP

LITTLE MUD

LAKE

PR

OSPE

CT

W.BRACK

OPAP

91-782

10

3.3. Exploration activities

3.3.1 Air photo lineaments

The basis for this study are air photos at a scale of 1:10,000. The air photos used were numbered 78-4441-141, photos 118 to 124. A TOPCON table stereoscope was used for the stereoscopic viewing of the air photos. All recognized lineaments were plotted on transparent paper with the exception of areas where the density of lineaments with the same directional pattern would have distorted the importance of such lineaments. Streams and lakes were plotted for reference.

The above described method for the extraction of the air photo lineaments has to be considered as a quantitative approach, since distortions are unavoidable. However, the accuracy should be sufficient for a lineament interpretation and the selection of potential prospective target areas.

In principle, an air photo lineament is a line which may or may not have any geological significance. The geological importance of such lineaments increases with the recognizable regional directional pattern or the length of such lineaments, especially in cases where such lineaments have significant morphological or topographical expressions.

Results and Interpretation:

The density of the air photo lineaments in the Little Mud Lake area is rather thin compared with similar areas within the region. With a few exceptions the lineament pattern is regular and the individual lines are short. Longer lineaments often curve. The dominant configuration is a regular cross pattern of lines trending NE/SW ( 45 degree) and NW/SE ( 135 degree). E/W lineaments represent the third most frequent population. These lineaments deviate in their direction more than the above described line patterns. The fourth group of lineaments are directed N/S (approximately 05 to 15 degree and 165 to 175 degree), however they are rarely observed. Other lineament directions are either to scarce to have any significance or are deviations of the above described patterns. Only a few of the lineaments have a strong topographical expression and are recognizable in the field. One such lineament is the NE/SW directed Little Mud Lake fault at the north-west shore of Little Mud Lake. 700 metres to the east a similar fault occurs cutting the southeast corner of the concession XI lot 11.The air photo lineaments show a rather consistent cross pattern. Such a regular pattern can be expected within igneous (plutonic) rocks and is related to the cooling and shrinking fractures of plutonic rocks. Another general observation is

11

the curving of lineament trends which may also be characteristic of an intrusive environment. The patchy, amoebic shape of the lakes in the area indicates a weak stress pattern for this area which is typical for an intrusive environment.

3.3.2 Orientation survey

An orientation survey was necessary in order to evaluate the accessibility to the investigation area. Initially the shortest possible access through the bush was chosen. Coming from the north from the Fifth Depot Lake Road, the access appeared to be difficult, due to swamps and densely vegetated low land. However the traverse intersected the power line access trail which leads to the north central portion of the investigation area. The access trail was then followed towards the Fifth Depot Lake road. After approximately 2.5 kilometres to the north-west the access trail intersects the Fifth Depot lake road.

From the north-central portion of the investigation area the power line access trail continues towards the east and should connect to a permanent bush road at Loon Lake (see fig. 2) However the latter possibility was not fully explored.

3.3.3 Grid line establishment

Within the Little Mud Lake prospect area a flagged grid was established. The base line direction is 90 degree E/W and follows the Hydro power line. The grid lines are perpendicular at 180 degree N/S. Grid line separation is 100 metres and station distance 25 metres. After an initial systematic grid in the north-central portion of the prospect it appeared to be appropriate to restrict the grid lines to establish orientation lines only.

A total of 7.7 kilometres of grid lines were established on the Little Mud Lake prospect.

12

3.3.4 Prospecting

Prospecting was executed in areas were no grid lines were established in order to verify the possible existence of marble lenses. The prospecting was selective and targeted the edges of lakes, swamps and topographical lows (depressions). The prospecting efforts were concentrated towards the southern border of the investigation area.

Since no marble occurrence was encountered sampling remained restricted to 7 rock samples as reference samples (see listing below). No analysis or thin sections are planned for these samples.

Table 1

SAMPLE

RMS-01

RMS-02

RMS-03

RMS-04

RMS-05

RMS-06

RMS-07

Rock sample description for the Little Mud Lake area

LOCATION

B.L. 5+00 E

B.L.

B.L. 14-1-00 E

10+00 S 14-1-00 E

10+00 S 14+00 E

1+50 S 1+00 W

9+00 S 9+00 E

DESCRIPTION

milky quartz

11+00 E medium to fine grained pink granite

biotite, hornblende granite fine grained, equigranular fine grained, aplitic granite

mafic, fine grained dioriticrockmilky quartz

medium grained, equigranular, pink granite

13

3.3.5 Geochemical soil sampling

Objective: The objective of the geochemical soil sampling survey was to detect sphalerite (zinc) mineralization within possibly hidden marble lenses as well as other potential base metal mineralization. Since no marble outcrop or boulder was discovered within the Little Mud Lake prospect the geochemical survey is considered to be crucial to evaluate the potential for mineralization in this area.

Method: The selection of the sample medium is of importance for a meaningful geochemical survey. An orientation study over a known mineralization may determine the sampling technique to be applied. However, such orientation surveys are time- consuming and expensive. In case of the Little Mud Lake prospect the survey could be related to the successful geochemical survey at the Slave Lake property (OPAP 90- 435). Preferred sample locations were depressions or at the base of slopes. The upper "B" horizon within the soil profile is considered the proper sample medium.

During the geochemical soil sample survey great attention was given to the consistency and uniformity of the sample medium. In order to control the sampling a short protocol was noted for each sample. Locations with water saturated thick organic layers were disregarded for sampling, since no comparable "B"- horizon could be obtained and leaching effects may be expected through circulating ground-water.

The sample extraction was done with a narrow bladed garden spade. First the top layer (grass, mulch etc.) was turned over and then a soil profile was extracted. After determining the upper "B"-horizon approximately 150 to 200 grammes of soil was filled in a pre-labelled geochemical soil sample paper-bag. A short description of the sample was given (location, depth of sample, colour, composition, humidity as well as significant topographic features). Each sample location was fully restored in filling the sample holes in the reverse order for environmental consideration. Before shipping the samples for analysis they were laid out for drying for several days.

Analysis: The geochemical soil samples were analyzed by BONDAR-CLEGG ft COMPANY LTD. in 5420 Canotek Road, Ottawa, Ontario K1J 9G2. As for the most cost effective analytical method the 28 element IPC-atomic emission spectroscopy was chosen. The analytical extraction method is based on the Aqua Regia Digestion. The analyzed elements and their detection limits are shown in table 2 (by Bondar-Clegg 1991). The elements marked with an asterisk may be incomplete in their analysis for certain mineral forms. In addition 12 samples were selected at random and analyzed for uranium.

c ON

c es

s i o

iv) x

i^

CO

NC

gS

SIO

JV

X

II

PR

OS

PE

CT

GR

ID

LIN

ES

SO

IL

SA

MP

LE

L

OC

AT

ION

S

PR

OS

PE

CT

ING

T

RA

VE

RS

ES

W.B

RA

CK

O

PA

P 91-7

82

15

Table 2: ICP-atomic emission spectroscopy detection limirs

ICP-ATOMIC EMISSION SPECTROSCOPY

3— UOOOppat 5- 2,000pirn

0.01-10.00*

l- 2400pp.10- 2,000|i|n 2- 2jOOOpiMi l— 20400 ppm l- 2400 ppm

W* . Se* .Al* .Mg*a*.Ml*.K*.ST* .Y*-

20- 2.000 ppm20- 2,000pp-5- 2.000 ppmaoi — 10JOO%001 —IOLOO% Ml — 10.00 % 0.01 — 1000 % OLOI — 10.00 % l— 2.000 ppm l- 2400)

The loan orthose dements marked with

Technical data: A total of 75 geochemical soil samples were collected within the Slave Lake project area and were analyzed. The analytical results were subjected to a statistical interpretation. Only elements with some variations were considered.

Table 3: Geochemical analysis: statistical dataHean value (top), standard deviation (bottom)

i cu T PB i MN 2A , MG '

| 52.04 j

35.92 i

;

AL i

2.26 i

' 1 .38.

iGR j

29.29 |

j 15.85 l

i ;l BA ,

139.79 j

j 98.09 j

17.2 .

17.61 |

iFE j

1.96

1 .33 j:

co i10.21 j

11.16 j•-

LA j

27.61 j

22.08 !

18.08

12.51

NA

0.06

0.01

NI

23.07

25.85

j 352.92

l 832.61! 1:

! K

i 0.07

1 0.05i

j SR

j 29.27

i 28.63

i

!

-i ——————i

22.29

15.48

se6.24

5.84

Y

12.49

10.74

117.04 j

69.29 iJK

J

v !34.99 |

2C.78 [•t t

CD !

0.47 i

0.38 ?

——————— l

*

j

16

Results: The geochemical data indicate rather uniform geochemical conditions in the sample area. This may be explained by a homogenous and non-mineralized lithological unit, such as the encountered granitoid rocks. The zinc values (max. 192 ppm) as well as indicator elements for zinc mineralization such as copper and lead are not anomalous in comparison to a previous survey over the Slave Lake area (OPAP 90-435). According to this study calcium values ^.5X Ca are indicative for marble occurrences. Seven values fulfil this criterion (sample: M-3,M-9,M-28,M-33,M-68,M-70,M-73). The true occurrence of marble within the described sample locations would have to be further examined, since prospecting did not reveal any outcrop of marble. Only two samples appear to be slightly distinguished. Sample M-17 is enriched in iron and manganese which most likely relates to local weathering conditions. Sample M-34 has an elevated nickel value (211 ppm) which may indicate a more mafic unit within the granitoid rock suite. Any other occurrence of mineralization in the investigation area is very unlikely since all the indicator elements analyzed give rather uniform and flat values. The analytical results for the samples tested for uranium gave low background values only.

Out of the 29 elements analyzed the analytical values of 6 elements were selected to be plotted on contour maps in order to detect even minor geochemical l y anomalous areas. The selected elements are: calcium, magnesium, zinc, copper, lead and manganese. These elements appear to be the most relevant ones in regard to sphalerite mineralization in marbles.

CALCIUM:A very weak calcium high is indicated in the central portion of the observation area. It stretches NNW to SSE starting at the base line 400 E and widens to the south at 900 S to 1000 S and 1000 E to 1400 E. A second calcium high is located at 400 W from 300 S to 800 S. According to field observations both highs are not related to marble lenses and may reflect differences in the composition of the underlying granitic rock.

MAGNESIUM:The elevated magnesium values correspond very well to the above described calcium highs. They are more pronounced but do not indicate any underlying marble.

ZINC:The indicated zinc anomalies are spotty. The trend lines indicate a NNE to SSW direction. This does not correspond to the calcium and magnesium directional trend, although there is some overlapping with these elements mainly at 200 W and 425 S.

17

COPPER:The anomalous copper values correspond very well to the elevated zinc values. The directional trend of the copper values is similar to the one for zinc in the eastern portion (NE to SW) of the prospect but reverse for the copper values in the west (NW to SE).

LEAD:The lead values are rather flat, and the directional trend within the central portion of the observation area is N to S. It does not correspond to all the above described trends and may be coincidental. Some of the isolated higher lead values however do overlap with the copper and zinc highs such at 200 W and 450 S and 1400 E 200 S.

MANGANESE:The manganese anomalies are truly of erratic nature and do not indicate any directional pattern. Two of these anomalies overlap with the area of influence of high values of zinc and copper and partly with lead. The match is very good at 200 W and 450 S and fair at 1250 E and 100 S.

Conclusion: The results of the geochemical survey lead to the conclusion that the prospect area does most likely not contain any mineralization of economic importance. The elevated values of the above selected and graphically presented elements (see appendix) appear to generate patchy clusters and pseudo- trends. The few spots were some overlapping of different high values of elements does occur, may be explained by a preferred drainage location and ideal deposition conditions (reducing soil condition etc.). Other conditions may apply as well but are not important in relation to the objective of the project. The results may be used as reference for other projects in the area since the underlying geology is uniformly of granitic composition and the geochemical data represent a single population medium.

18

Table 4: Sample description of 75 soil samples from the Little Hud Lake project

Legend:SPL r SAMPLE NUMBER

(THE LABORATORY ADDED THE PREFIX ML- (MUD LAKE) TO THE SAMPLE NUMBER

COLOUR - SOMETIMES TWO PROMINENT COLOURS ARE GIVEN

BLK - BLACKGRY = GREYBRW = BROWNDK = DARKLGT = LIGHTCOMP = COMPOSITIONORG ^ ORGANIC SOILHUM = HUMIDITYD = DRYM = MOISTW - WET

19

SPL

1

2

3

4

5

6

7

8

i 910

1112

13

14

15

16

17

18

19

[ 20

j 21

22

j 23

24

25

l 26

i 2 728

29

STATIO N

10+00

9+40

9+00

7+00

6+00

5+00

4+00

3+00

2+00

0+15

00+00

00+00

00+00

1+00

3+00

4+00

4+75

00+00

1+00

5+75

5+50

5+50

10+00

10+00

7+75

6+75

sssssssss

POSITI ON

2+75 E

3+00 E

4+00 E

4+00 E

4+00 E

3+75 E

4+00 E

4+00 E

4+00 E

S i 4+00

00+00 W

sscss

INssssssssss

2+25 W

4+50 W

2+00 W

2+00 W

2+25 W

2+00 W

, 1+00 W

: 1+00 w2+00 W

3+00 W

4+00 W

7+00 W

7+00 W

7+00 W

t 5+00 ! W

3+75 ! W

3+50 j W

4+50 ' W

DEP i COLOUR 1 ! TH—i ———— ———————

10 j BLK.GRY

! 20 GRY

' 20 : DK.BRW

25 ̂ MED.BRW

j 15 i MED.BRW

15 GRY— ———— i ——————— j 20 j GRY

20 DK.BRW

30

! 15

i 30l 30

30

BLK

DK . BRW

GRY

DK . BRW

MED.BRW

20 DK . BRW

i 30 DK . BRW

30 j GRY

30 CK.BRW

20

35

! 30

30

30

40

25

30

BRW, GRY

MED.BRW

BRW , GRY

GR Y, BRW

DK.BRW

DK . BRW

LGT.BRW

GRY

35 MED.BRW

! 25

i 20

20

GRY , BRW

BRW

MED.BRW

COMF1 | COMP2i'

ORG CLAY

SANDY

HU M

MD iORG CLAY ' M f

SANDY

SANDY

SANDY

CLAY

SANDY

ORG

loID

CLAY j M

W

ORG j D |

SANDY ORG

W (

M

CLAY l W

ORG CLAY M j

SANDY ORG D—————— —————— ————SANDY l ORG D

CLAY

CLAY

ORG

SAND

ORG

SAND M

i D

SAND

ORG

D

D

SAND D

CLAY i ORG ' M j

CLAY ORG

CLAY ORG

ORG

ORG

SAND

CLAY

M

M

M

CLAY j M

ORG

ORG

ORG CLAY

( ORG

ORG SANDY

D

D

M iM t-MH

D l

20

30 [ 5+75

31 j 4+75

32 l 3+00

33 i 1+50

34 j 1+50

35 j 1+00

36 i 1+00J

37 j 2+00

38 j 1+00

39 ! 2+50

40 j 3+25

41 ! 5+25

42 i 6+00

43 ; 7+50

44 i 10+00

45 j 7+50

46 j 8+00

47 j 5+50

48 ' 5+50

49 j 4+50

50 s 2+75

51 j 00+00

52 j 1+00

53 | 2+00

54 j 00+00

55 | 1+00

56 j 1+75

57 ; 1+00

58 i 0+75

59 ; 0+50

S j 6+00 : W——— ! ———————— ! —— S j 6+75 j W

S j 8+50 ! W

S j 8+50 W

S j 5+75 j W1 —— i ——————— ! —— S ; 5+00 ! W

N ! 4+00 j W

N j 4+00 i W

N j 8+00 | W

S ; 4+00 ! W

S j 3+25 i W———— j ———————————— i ———

S I 1+50 ! W

S ! 1+25 j W

S j 2+50 | E

S j 1+00 | E

s S j 0+50 E

S j 2+00 j E

L S j 3+00 i E

S j 2+00 l E——— l ———————— j ——

S l 2+00 | E

S l 2+00 ! E

j 18+00 E

S i 17+50 \ E1 —— ' ——————— ! —— S j 1 7+00 E

' 16+00 E

N ; 14+75 j E

N j 14+00 E

S | 12+50 j E

S | 11+50 j E

S j 10+50 j E

25

' 30

30

! 30

30

40

25

25

10

—22,40

d. O*rv/

30

30

35

40

30

35

j 40

30

' 15-i ———— j 20

30

25

30

20

25

25

20

30

BRW

BLK, GRY

GRY

GRY , BLK

GRY, BRW

BRW

DRK . BRW

GR Y, BRW

BRW

GRY

BLK

BRW

GRY

BRW

GRY , BLK

, LGT. BRW

GRY

LGT. BRW

LGT. BRW

DRK.BRW

GRY

GRY

BRW

GRY

GRY , BLK

GRY

GRY

GRY

GRY , BLK

BLK, GRY

CLAY j ORG j W

ORG SANDY ! W

CLAY ! ORG j M

CLAY ORG i M

CLAY ORG j M

ORG j Di —————— —————— i ————ORG CLAY j M

SANDY ORG D

SANDY D

SANDY | D

ORG CLAY D !

ORG SANDY D

CLAY ORG M

ORG CLAY M

CLAY j ORG W

SANDY ORG D

CLAY SAND D

SANDY D

CLAY ORG D——————— ! — —— ——— —— —— SANDY ORG D

SANDY CLAY j D

CLAY | W

ORG ! CLAY j 0—————— i —— i ——— 1 ————CLAY ! | W

CLAY j ORG j W j

CLAY ! j D

CLAY SANDY \ D

CLAY j M

SANDY ORG ! M

ORG j CLAY ; W

en CO -si en CO 00 ro en co 0 CD r i co o r > "* z

* * -si

en CO 00 en O m CO o CD r T? V CO 3Q K o 5 o o

CO en en O CO CO o o m ro on CO f- v CO JO "* o r- * 0 CO z

ro -j ro en CO to en 0 m ro en CD •rt X i CO w" z 0 0

.^ CO o o CO to o m CO 0 CO ^ o r * .... z

U-W

BI

O 00 -J en CO ^ o o o m ro en CO •^ v CO r~ * o < o CO z

O)

CO 00 en o CO — •f o o m CO o 0 t CO 3J -4 CO z o o CO z

0

00 to o o CO CO o o m CO o CD r o r * "i" (D

O O ro en CO * ro en m CO o CO -f. o CD * O "* ,...

Z

^IB

MH

ail

0)

O)

CD ro en CO co CO 0 m ro en

CD C

OZ

-n -n o r- *

W.. . .

. H

Z

0) en -J o o CO co -j en m ro en CO ^Q ^ O r~ * ,. Z

o* •^ O) ro en CO •^ o o m ro en Z m o m CD TO X CO z o i CO o

O)

CO * O) o CO * o 0 m ro en CD r~ M CD X) X i CO "" z

O) ro ro CO en CO * o o m ro en CD r o CO z

o - en o CO * 0 0 m CO o CD 2(J x z 5 i" Q O

O)

O O 0 o o 00 -J m ro o CO < f CO r~ 7*.

CO z 5 o r- > "* *

ro

22

4. PROJECT C: KALADAR

4.1 Description, location and access

The Kaladar project is located in the most south-central portion of Kaladar Twp. within the Southeastern Mining Division of Ontario. The project covers concession VII, lot 1 and lot 2 (see map 4).

The accessibility of investigation area is excellent. Coming from Kaladar where highway 7 is intersected by highway 41 and following highway 41 approximately 7 kilometres to the south, the property can be reached from the intersection with the Racoon Lake road or approximately 700 metres further to the south were two private trails reach the property. One trail leads to the northeast and north of Donahue Lake to the central portion of the investigation area, whereas the second trail is to the south of Donahue Lake and intersects the southern portion of the property.

The area is marked by elongated ridges of minor elevation intersected by narrow, shallow lakes and swamps. Most of the lakes are created by the activity of beavers. The vegetation is dominated by hard-wood such as oak, beech, maple and birch with minor stands of spruce and pine. Patches of sumach bushes and alders are common. A hydro power line intercepts the south-west corner of concession XII lot 1 of the investigation area. The investigated lots are Crown land.

4.2 Geology

The investigation area is part of the Central Metasedimentary Belt, Hasting Basin as defined by Wynne-Edwards(1972), and is composed of Late Precambrian meta-volcanic and meta-sediment of the Grenville Supergroup, and Late Precambrian granitic intrusive. Late tectonic pegmatite sheets and dikes cut the supracrustal rocks locally (J.M.Wolff,1982).

4.3 Previous exploration activity

Very limited records do exist of previous exploration activities in the area and particularly on the target area. However, a report by J.D.McCannel l for Glenshire Mines Limited (1975) describes a trench within the northwest corner of concession VII, lot 2: "Heavy sphalerite is exposed in an eld trench in crystalline limestone in the northwest corner of lot 2 concession VII. A large sample of well mineralized rock from this trench returned an assay of 29.29* zinc, 0.007* lead and 0.04 ounces of silver. The sphalerite was difficult to identify as such with the result that better mineralized pieces were selected more to establish the presence of zinc mineralization than to determine the grade of the material."

j^TTTTl

r? l H

1C7 •/Ir r^^k

PROJ ECT AREA

GENERAL LOCATION MAP KALADAR PROJECT

W.BRACK OPAP 91-782

24

4.4. Exploration activity

4.4.1. Air photo interpretation

The basis for this study are air photos at a scale of 1:10,000. The air photos used were numbered 78-4442-142, photo 108 to 112 and 78-4441-141, photo 97 to 101. A TOPCON table stereoscope was utilized for the stereoscopic viewing of the air photos. The technique applied is described in paragraph 3.3.1 of this report (see page 10).

Results and interpretation:

The air photo lineament pattern indicates two tectonically different sub-areas. The north-western portion covering approximately 2/3 and the south-eastern covering 1/3 of the observation area. The separation is precisely defined along the south-east shore of Donahue Lake and along the Donahue valley to the north-east.

To the south-east of Donahue valley the air photo lineaments are dominated by NW/SE ( 135 degree) lines. These lines tend to occur in dense patterns and they are usually short. With a few exceptions they do not intersect into the adjacent area to the north-west. The NW/SE lines form a cross pattern with lines directed NE/SW ( 40 to 50 degree). Superimposed on this pattern are north-southerly lineaments with a wide angle range (165 to 180 and O to 10 degree). These lines intersect the entire observation area. A more subdued lineament is directed 70 degree ENE/WSW.

The air photo lineaments south-east of the Donahue valley form a consistent cross pattern. Such a regular pattern can be expected within igneous (plutonic) rocks and is related to the cooling and shrinking fractures of plutonic rocks as it was described in chapter 3.3.1. This area compares very well with the Little Mud Lake area, even the lake contours have a similar patchy, amoebic shape which indicates a weak stress pattern for this area which is typical for an intrusive environment.

A rather dramatic change occurs to the north-west of the Donahue valley, where the line pattern is denser. The dominant lineament stretches NE/SW ( ± 40 to 50 degree). These lineaments tend to be long and consistent. They have a strong topographical expression in narrow valleys which are frequently filled with water (beaver lakes). Between the elongated lakes are ridges which are just as consistent and follow the same 40 to 50 degree lineation. The cross lineaments are sharp angled and strike 65 degree. The N/S lineaments are more frequent and form a swarm pattern in the central part of the observation area. A suppressed lineament

25

appears to be the ±135 degree direction with lines that have very weak contours and are of short distance. In the field the strong and frequent ± 40 to 50 degree lineaments are quite obvious with the best example being the Donahue valley, a graben-!ike feature which probably forms the south-eastern suture line of the Clare River syncline. This syncline with its metasedimentary rock suites is a significant tectonical feature visible on satellite photos.

4.4.2 Grid line establishment

A total of 13.6 kilometres of grid lines were established or. the property. In order to comply with environmental concerns and to keep the disturbance of the land at a minimum all lines were marked with flagging tape. A major difficulty to establish a grid system on the property are numerous long but usually narrow beaver lakes and swamps.

Within the central portion of the investigation area a 15CO metres long base line v/as established wi^h the direction of 040 degree NE/SW. The distance between the perpendicular grid lines (130 degree) is 100 metres and the station distance measures 25 metres. Some of the grid lines were extended across the property. The distances across lakes was either measured or estimated and then later, after freeze up, readjusted. Two tie lines were established, one in the northwestern corner of the property at 8 -H 00 NW with a distance of 400 metres and a second at 3 * 25 SE with a distance of 1550 metres (the grid is shewn on the geological map).

4.4.3 Radiometric survey

The objective of the radiometric survey was to test the area for possible uranium mineralization and to use the scintillorneter as a mapping tool. The later objective appeared to be appealing since the marble formation should be contrasted in their radiometric response from the surrounding igneous rocks (granite and pegmatite) as well as the gneiss. The instrument used was a SCINTREX BGS-3 gamma-ray scintillometer.

Results: Numerous high readings were encountered within the igneous rock suites with a background of ± 300 cps (counts per second). Locally, especially over granitoid intercalations within the meta-sediments, readings from 500 to 2000 cps were quite common. The best value was discovered at highway 41 with 6000 cps. The source is a coarse grained pegmatitic dyke. The marble outcrops gave readings of 10 to 35 cps with the bulk of the readings being 20 to 25 cps. Unfortunately some of the metasedimentary gneiss responded with the same background values. However, other gneiss especially those enriched in

26

feldspars and biotite had background values of 40 cps. It therefore can be concluded that the scintillometer can be used as a mapping tool under favourable conditions as long as its limitations are recognized. The encountered radiometric anomalies had very much a point configuration and therefore do not warrant a follow up.

4.4.4 Prospecting

Prospecting was completed over the entire project area but concentrated on intermediate lines and the gneiss regimes on the property. The latter were not mapped in as much detail as the marble zones. The surrounding of the property was prospected as well, namely along the Racoon Lake road where several samples where taken along road cuts and around an old shaft (with the permission of the present land owner). Part of the prospecting efforts was to map topographical features and in particular the shore lines in relation to the flagged grid.

4.4.5 Geological mapping

The emphasis of the geological mapping was to concentrate on the occurrence of marble lenses and their l ithological boundaries.

Three principle lithologies occur within the project area. These are bands of marble in contact with gneiss of various composition and granite. Three marble units were observed on the property and mapped in detail as they are the potential host rock for sphalerite mineralization.

The most north-westerly marble unit forms a significant cliff (45 feet drop) and is the location with several former pits and trenches (see geo!.map and fig.5). The width of the marble band reaches much further to the north-west exceeding the limits of the observation area and is part of the Clare River Synform. The marble is medium grained and mostly white with various degrees of impurities. The marble unit dips steeply to the SE and is in contact with gneiss.

Approximately 750 metres to the south-east another marble lens occurs (central marble band). It is a continuous band with several layers of marble with intercalations of meta-sediments and granitic material as well as pegmatite. The marble band is relatively narrow as it appears at line 1+50 E and widens towards the north-east. The marble forms ridges and slopes towards the NW. The marble unit is framed by gneissic rocks to the NW and SE. The marble shows a great variety in its appearance such as white, grey, ochre, buff, brownish, yellowish and banded. The marble is fine to medium grained with occasional coarse grained varieties. Various impurities are common such as tremolite, white mica and others.

27

The th:rd marble band occurs SCO metres to tre south-east of the central marble band. Again it forms a high ridge with intercalations of narrow (dyke like) granitic intercalations. The south-west tip of this marble unit is wel"! exposed (see photo i J. The exposure is just 200 metres outside the property limit (approximate position 4+00 SW 1+00 SE). It shows clearly the dark grey to black weathered marole and one majo r granite ba^d Hn the centre (white.) and two smaller ones to the right.

^uence is quite consistent over the entire length of the CLSTT' , ation area along r-? "-ne 3+25 SE. At the picture site (see picture 1) the dv i s nearly vertical and tne unit abruptly disappears. narble unit is framec by gneiss tc the NE and granite to -.'t ^E. Fresh broken maro^e of t-ns unit is mostly white and with alterations as described within the central marble band. At the contact of the marble unit ^o the north-west, from 11 ne 3+00 ' 'r 7+00 NE and 3+00 SE a continuous quartz-vein occurs quartz TS porous, dense and dark grey (smoky). It is strc ^titized (rusty). Only a few samples have been take- - * "- ~ " ~ ~~:~d sold value (25 ppm Au).

Picture i: SW tip of the south-eastern marble unit a

Tne marble weathers dark grey to b":ack, the weathering surface of the granite is white. Three granite bards are reccgnzable en the picture with the marble squeezed in between, the left flank of the rock face cons*sts entirely of marole. Donahue Lake is in the back of the observation point.

28

The observation of the marble units forming ridges is contradicting previous observations where the marble units covered the very low areas (Slave Lake). This may be explained by sub-anticlinal structures as it was observed at the tip of the central marble band. In addition the marble units within the Kaladar area are sometimes quite rich in quartz and have sub-parallel intercalations of ridged granite.

The meta-sediment or gneiss unit is generally characterized by low radiometric response which confirms the sedimentary origin of this unit. The mineralogical composition is variable. The gneiss range from quartzite, quartz-feldspar gneiss, quartz- feldspar-biotite gneiss to biotite gneiss. Muscovite and biotite as well as hornblende and sometimes pyroxene are main components. Garnet accumulates locally and along foliation planes.

The granite forms a large body south-east of the Donahue valley and contains the most south-easterly marble band. The central marble band contains some granite and pegmatite, especially towards the north-east. Local granitization of the gneiss are frequent but do not extend over any large distance.

The tectonic features are quite consistent. The units strike 30 to 50 degree NE/SW and dip from vertical to 50 degree to the SE. Dipping to the NW was observed but less frequently. At the tip of the central marble unit within the gneiss a fold axis was observed with 45 degree strike and a dip of 15 degree to the north-east. The fold indicates an anti-form. This possibly may explain the widening of the central marble unit.

4.4.6 Trenching

Within the very north-westerly corner of concession XII lot 2 a series of former pits and trenches is exposed within a large band of marble. One previous sample of these workings assayed 29,29 X zinc. It was recorded that the ore carrying mineral sphalerite was hard to recognize. Examination of the pits did indeed not reveal any sphalerite mineralization. The main pit (T-3) however contained a stockwork of beige-brown siderite. Some meta-volcanic rocks were observed in the old trenches and rock debris surrounding the pits. These rocks however had no surface expression. Therefore it was decided to open up additional trenches in order to evaluate the geology in detail. Trench 1 was opened south-west of pit 1 and was entirely exposing regular marble. This trench was abandoned after a survey of its location revealed it was just outside the concession on private land. The second trench was placed 4 metres east of the main pit. The trench is 6 metres long and 1 to 1.5 metres wide (see fig, 5). The trench revealed a single lithology: marble. No indication of a mineralization was recogn i zed.

TRENCH-1

TRENCH

2

l

**T-5

6T59

KALADAR PROJECT

POSITION OF TRENCHES

SAMPLE LOCATION

W.BR

ACK

OPAP

91

-782

A

ALL CXPOSC9 ROCKS AU HARBLC

HCTttft

KALADARPROJECT

TRENCH 2

W. BRACK O PAP 91-782

30

Picture 2: Trench 2, NW corner of concession VII, lot 2The marble forms small ridges, due to the changes in its mineral composition.

31

4.4.7 Table 5:

Rock geochemistry

?j.i

\ ROCK SAMt 3t3

SAMPLEt

} NUMBER1 iD-01

P

D-02

i lD-O3

D-04

D-05

D-06

D-07

D-08

D-09

D-10

PLES

S

S

A

A+S

S

A

A

A+S

A+S

A

SAMPLE RECORD j j

i fTHIN SECTION: S GEOCHEMICALLY f

ANALYZED: A t

LAB LOCATION l DESCRIPTIi ON i

NUMBER ; l i j

15+OONE ' 0+25 SE ; MED./COAR (i i SE ;j | GRANITE i

12+OONE 0+75 SE DENSE j i l BIOTITE ] j GNEISS l

D-03 12+OONE 0+10 NW BUFF , i MARBLE

D-04 10+OONE j 0+90 NW GREY i BANDED j MARBLEj

5+00 NE j 2+20 NW QTZ/BIOTI j TE GNEISS

6711 ! 5+25 NE j 2+00 NW QTZ-VEIN, 1 j i RUSTY

6712 j 3+00 NE j 0+60 NW MARBLE, i j WHITE

6713 ; 3+00 NE ' 0+25 NW MARBLE, i YELLOWISH j ALTERATIO

————————— ' ———— h5 ———6714 6+00 NE j 1+25 NW MARBLE,

i DIRTY i GREY

6715 6+00 NE i 1+00 NW \ MARBLE,; i j TINY s

' 1 RUSTY j ! SPOTS j

32

D-11

D-12 E

D-13

D-14

ED-15

D-16

D-17

D-18

D-19

l

D-20

D-21

D-22

D-23

D-24

D-25

i

A

A+S

A+S

S

S

A+S

A' ————————— A

S

A

A

S

f\

S

A+S

6716 8+00 NE

i

6717 j 9+35 NE

6718 10+OONE

10+OONE

: 11+OONE

6719 11+OONEi i1

6720 2+50 NE

6721 2+50 NE

; 10+25NE

6722 j 8+00 NE'

6723 j 6+00 NE

i

7+00 NE!

6724 | 3+00 NEi j; 3+00 NE;

6725 4+00 NE

0+17 NW

0+10 NW

1+25 NW

0+00 BL

1+25 NW

1+45 NW

0+50 NW

0+50 NW

0+00 BL

1 ————————— 0+15 NW

3+12 SE

3+00 SE

3+15 SE

4+00 SE

3+00 SE

MARBLE, WITH RUSTY SPOTS

GRANITE, WITH GARNETS

MARBLE, DIRTY

QTZ/FLSP/ BIOTITE GNEISS

PEGMATITE j

MARBLE, ] DIRTY, WITH HEM.

MARBLE, IMPURE .;

MARBLE, j WITH HEM, i SULPHIDE

PEGMATITI C GRANITE, l GARNET j

MARBLE, DIRTY

QUARTZ, RUSTY, HEM, PY, CHL

FLSP/BI/G ARNET GNEISS

BI-GNEISS RUSTY

COARSE BIOTITE GNEISS

QUARTZ, RUSTY,

33

D- 2 6 ; A 6726 j 4+00 NE 3+00 SE

|

l \ j—————— i ——————— ; ——————— ——————— i ———————D-27 j A j 6727 4+00 NE 3+50 SE

i'. si i

D-28 A 6728 5+00 NE 3+60 SEi 11 ——— i ———— , ————————— ' ————D-29 ] A j 6729 ROAD CUT 41

D- 30 A i 6730 ROAD CUT 41* 1

11 D- 31 A+S 6731 ROAD CUT 41i it ; i i i iD-32 A 6732 10+20NE 3+25 SE

i iD- 3 3 j A 6733 15+OONE 0+40 NW

D- 34 A+S 6734 13+OONE 1+95 NWi 1

j D-35 j A 6735 1 14+OONE 0+50 SE

i ij D-36 i A+S 6736 i 7+75 NE 0+00 BL1! :fi ! }t ; i

D-37 j A+S 6737 j MAIN PIT

D- 38 A+S 6738 R. C. RACOON L.ii

QUARTZ , DENSE. SMOKY, RUSTY

MARBLE, j GREY LENSES, COARSE j

MARBLE, DIRTY

MARBLE, BANDED WHITE/ORE Y

QUARTZITE , DARK GREY, SULPHIDE2* ^* i

PEGMATITE

RADIOACTI VE

MARBLE, IMPURE, YELLOW, ROSY

DIRTY MARBLE j

PYROXENIT E(?)

RUSTY QUARTZ VEIN

LIMONITIC j META-SEDI MENT

ULTRAMAFI C ROCK

RUSTY (RED) MARBLE

34

D-39 A+S 6739 R.C.RACOOL LAMINATED QUARTZ

D-40 l A+S 6740 R. C. RACOON L RUSTYMETA-SEDIMENT

D-41 A+S 6741 R. C. RACOON L. j META-QUAR TZITE

D-42 A+S ! 6742 R. C. RACOON L l RUSTY BIOTITE p GNEISS

D-43 A+S i 6743 7+90 NE i 3+75 SE GRANITIOD E ROCK

D- 44 6744 j R.C.RACOON L. PINKISH MARBLE

D-45 6745 R. C. RACOON L RUSTY MARBLE

D-46 6746 T-1 | CALCITIC STOCKWORK

D-47 i 6747 T-3 SELECTIVECALCITICMATERIAL

D-48 i A 6748 T-3 ! COARSE j GR. MARBLE

D-49 6749 T-3 SELECTIVE i CALCITE MATERIAL

D-50 A l 6750 BANDED MARBLE

D-51 i 6751 R. C. PIT GREY 1 MARBLE PY

D-52 6752 R. C. PIT j DK.GR. DENSE MARBLE

D-53 * i 6753 R. C. PIT j GREY MARBLE,

l

j D-54 j A ; 6754 R. C. PIT j CONGLOM., j i QUARTZ i i PEBBLES [

j D-55 j 6755_____j TRENCH 2 j MARBLE

35

From 55 rock samples collected within the Kaladar project area and its immediate surrounding 47 have been geochemically analyzed by Bondar 8. Clegg company in Ottawa (see 3.3.5). The samples were analyzed for 29 elements and gold. The applied method and the detection limits are explained in paragraph 3.3.5.

Results: Due to the limited number of rock samples and the large variety of lithologies analyzed a statistical and quantitative approach to evaluate the data might be misleading. Therefore a quantitative approach is chosen where anomalous values are related to the specific rock sample. The analytical data are shown in the appendix. The most interesting rock sample is D-25 (6725), a rusty and porous quartz at 3+00 NE and 4+00 SE. The sample shows an elevated value for Au (25 ppb) and Cr (227 ppb). Sample D-17 (6720) has a weakly anomalous gold value (25 ppb). Sample D-24 (6724) is elevated in lead (58 ppm) and Sn (25 ppm). Other samples with increased background values are D-39 (6739) with 39 ppb Hg, D- 40 (6740) with 28 ppm Sn, D-42 (6742) with 276 Cr, D-45 (6745) with 295 ppm Cr, D-6746 (6746) with 182 V and D-51 (6751) with 257 ppm Zn.All the described anomalous samples have to be considered of marginal interest with the exception of sample D-25. The considerable width of the quartz vein (up to approximately 10 metres) and a length of approximately 350 metres as well as the -elevated gold value may be indicative of a possible gold mineralization of economic interest.

36

4.4.8 Thin section description

The purpose of the thin section description was to identify mineral compositions and especially accessory minerals in marble.

D-01 Granite: feldspar 75*quartz 20Xbiotite 3*accessory minerals 2%

medium to coarse grained granular texture, plagioclase, microcline twinning, perthitization, myrmekitization, sericitization, quartz is fresh and intergrown with feldspar, biotite is strongly corroded, some decaying hornblende and calcite.

D-02 Gneiss:

lattice grained amounts

D-03 Marble:

work

diopside 79* feldspar 10* quartz 10* accessory minerals 1*

of greenish hypidiomorphic, medium to smalldiopside intergrown with quartz and feldspar, minor of calcite and sericite.

calcite 80* quartz 15* accessory minerals 1*

flaky corroded calcite with some grains reflection (dolomite?).pattern of tiny aggregates, muscovite as small isolated

which have higherundirected quartzlath and corroded,

minor amounts of opak mineral as individual grains (pyrite?).

D-04 Marble: 95*calcitemica 2*accessory minerals 3*

large grains of non corroded calcite, isolated slates of mica and chlorite, minor amounts of quartz and feldspar, fine, disperse opak mineral.

D-05 Gneiss: quartz 35*feldspar 35*diopside 20*accessory minerals 10*

fine grained mosaic texture of quartz and feldspar, disperse diopside, radial aggregates and sheets of chlorite, minor calcite, disperse opak mineral (5*).

D-08 Marble: calcite 98* accessory minerals 2*

large, corroded grains of calcite with isolated muscovite slates, minor amounts quartz, traces of opak minerals.

twinning f small of feldspar and

37

D-09 Marble: calcite 65*muscovite 3056accessory minerals 5*

medium grained calcite, slightly foliated mica predominately muscovite and sericite, mica are frequently chloritized, relictic feldspars (3*), occasional small fresh quartz grains.

D-12 Granite: quartz 58*feldspar 40* accessory minerals 2*

inhomogeneous quartz and feldspar assemblage, perthit, minor calcite, biotite (1*) as isolated small aggregates, traces of opak mineral.

D-13 Marble: calcite 70*muscovite 30*

inhomogeneous assemblage of hypidiomorphic calcite and muscovite, traces of feldspars and minor traces of opak mineral.

D-14 Gneiss: feldspar 50*quartz 40* chlorite K calcite 3*

fine grained equigranular slightly foliated gneiss, feldspars are sericitized.

D-15 Pegmatite: feldspar 64*quartz 34*accessory minerals 2*

large feldspar crystals, perthit twinning, sericitication of feldspars, larger crystals are surrounded by a matrix of smaller feldspar and quartz aggregates.

D-16 Marble: calcite 99*accessory minerals 1*

medium grained, granular calcite with some corroded boundaries, isolated slates of chlorite, minor traces of opak mineral, hematite staining on twin lamella of calcite.

D-19 Gneiss: quartz 50*feldspar 45*garnet 3*accessory minerals 2*

inhomogeneous and foliated, large crystals of quartz with ondulous extinction, feldspar shows frequently flame twinning, some quartz and feldspar crystals are twisted indicating a stress, ground matrix inhomogeneous from very fine to fine grained, garnets are corroded from the canter and filled with quartz, sericite and biotite as narrow seems along the foliation plane.

38

D-22 Gneiss: quartz 39*feldspar 29*biotite 15*sericite 10*muscovite 5*garnet 2*

fine grained and homogenous, quartz is intergrown with feldspar, flame texture in feldspars, biotite as narrow short lath stretched within foliation and rarely interconnected, muscovite forms slates (not as narrow as the biotite), garnet is locally accumulated and strongly corroded and filled with quartz, traces of chlorite and minor traces of opak mineralization

D-24 Gneiss: feldspar 30*quartz 20* muscovite 25* biotite 20* accessory minerals 5*

medium grained, foliated, inhomogeneous, feldspar quartz assemblage, intergrown network of partly corroded biotite, and elongated muscovite, 3-5* opak mineral, large elongated grains and fillings, cross cutting crystal boundaries.

D-25 Quartzite: quartz 99*accessory minerals 1*

inhomogeneous assemblage of medium to large quartz crystals, isolated small lath of chloritized biotite, cracks filled with opak mineral (hematite?).

D-31 Pegmatite: feldspar 65*quartz 30*sericite 4*accessory minerals 1*

igneous texture, inhomogeneous assemblage of porphyritic feldspar and quartz within medium to fine grained ground matrix, feldspar shows flame texture and sericitization, biotite as isolated elongated lath, minor chlorite minerals occur.

D-34 Pyroxenite:mixture of large decayed pyroxene, muscovite, relictic garnet, sericite and calcite. Further evaluation of this thin section i s recommended.

D-36 Gneiss: feldspar 35*quartz 40*pyroxene 20*hornblende 15*

inhomogeneous, large feldspar crystals surrounded by fine ground matrix and mortar texture, rich in opak minerals,

39

locally up to 5X, fade greenish pyroxene aggregates and green hornblende occur.

D-38 Marble: calcite 99*accessory minerals 1X

medium to coarse grained, minor occurrence of white mica and individual quartz crystals, hematite staining along twinning lamella of calcite.

D-40 Gneiss (mylonite): feldspar 55*quartz 30*muscovite 10*accessory minerals 5*

very fine and homogenous ground matrix of feldspar, quartz and muscovite, some isolated larger relictic grains as white mica, up to 5* disseminated opak mineral.

D-41 Quartzite: quartz 92*inter granular filling 8*

homogenous, fine grained, equigranular assemblage of rounded quartz, inter-granular filling cannot be identified

D-42 Marble: calcite 80*quartz 15Xaccessory minerals 5*

medium to fine grained, banded, narrow bands of medium seized calcite is interlocked and surrounded by fine grained calcite, the fine grained bands of calcite have intercalations of quartz and an opak mineral, occasional white mica occurs.

D-43 Granite: feldspar 45*quartz 50*accessory minerals 5*

inhomogeneous porphyritic texture, the medium to fine grained matrix is formed out of corroded feldspars overgrown by a younger generation of large and fresh quartz crystals, garnets is an accessory mineral (1*) as well as biotite and chlorite.

40

5.0 CONCLUSION AND RECOMMENDATION

Three different sub-projects were investigated. The Slave Lake project, which was partly investigated in 1990 was successfully optioned to Willow Resources Limited. The executed prospecting of the north-western claims eliminated this area for further mineral exploration.

The Little Mud Lake project was a follow-up project of the Slave Lake project. The anticipation of the occurrence of further unmapped marble lenses in this particular area was not confirmed by prospecting, a geochemical soil sampling survey and by means of an air photo lineament study. The result of the geochemical survey may be useful as a reference for further studies in this area.

Within the Kaladar project area three distinct bands of marble occurrences were mapped. The discovery of a 350 metres long quartz vein with an elevated geld value (25 ppb Au) is encouraging. The north-west corner of the property with the recorded high zinc value of 29,29* zinc remains unexplained. The result of the air photo "lineament study was the separation of two distinct geological terrains within the investigation area separated by the NE/SW striking Donahue Valley. The trenching work did not resolve the complex geological situation in the area of the old workings. The radiometric survey defined several high point anomalies and proved to be useful as a mapping tool. The rock geochemistry revealed only very weak mineralization. The thin section description was helpful to determine the accessory minerals of marble and for the definition of some of the rocks collected in the area.

The Slave Lake area is optioned to Willow Resources Limited. Therefore no further work on the claim is possible under the umbrella of the OPAP-program. The Little Mud Lake area is eliminated as a potential target area. The Kaladar project merits a follow-up program. The described gold bearing quartz vein should be investigated by trenching and detailed sampling. The old trench area on Concession VII lot 2 should be generously opened up with blasting to create a larger observation area in order to clarify the geological and mineralogical situation.

41

REFERENCES

Boyle, R. W. and Cragg, C. B.1957: Soil Analyses as a Method of Geochemical

Prospecting in Keno Hill-Galena Hill Area, Yukon Territory, Geological Survey of Canada Bulletin 39.

Fenton, J. O.1975: A Geochemical Orientation Survey over the Long Lake

Deposit of Lynx-Canada Exploration Ltd., Queens University Bachelor Of Science Thesis.

Holmstead, E.W.Brack, W.1991: Exploration program on the Slave Lake Zinc

Prospect, Sheffield Township, South-eastern Ontario,OPAP report 90-435

Kingston, P. W.1967: Report of a Geological Survey of the West Half of

Lot 10 Concession XV of Sheffield Township, OGSAssessment Files, 12 p.

Malczak, J., Carter, T. R., and Springer, J. S.1985: Base Metal, Molybdenum and Precious Metal Deposits

of the Madoc-Sharbot Lake Area, OGS Open FileReport 5548, 394 p.

Uglow, W. L.1916: Lead and Zinc Deposits in Ontario and Eastern

Canada, OBM Annual Report Vclume 25 Pt. 2.

Wolff,J.M.1982: Geology of the Kaladar Area, Lennox ans Addington

and Frontenac Counties, OGS report 215

CERTIFICATE OF QUALIFICATION

I, Winfried Brack do hereby certify:

1. that I am a geologist and reside at 34 Birch Hill Rd., Baie d'Urfe, Quebec, H9X 3H8

2.. that I graduated from the University in Munich (Germany) in 1972 with the degree of "Di p l om-Geo "i oge" in geology (approx. equivalent to a Master of Science) and from the University of Munich (Germany) in 1977 with the degree of "Doctor rerum natural iurn" in mineralogy (equivalent Ph.D.),

3. that I have practised my profession continuously since 1978 and since 1980 in Canada,

4. that I have frequently visited the Slave Lake project area and executed the exploration work as stated in the daily report sheets,

5. that the report is based primarily on personal observations,

6. that I have no personal interest in the property (with the exception of the Slave Lake property, which was optioned by Willow Resources Limited).

January 21, 1992

Winfried Brack, Dr, Di plom-Geologe

Td: (613) 749-2220 ,: (613) 749-7170

Geochemical

BONDAR*CLEG6 wwiwww WM.WV

(EOBRKKUC. IR. NILFRID BRACK 34 BIRCH HILL RD. BALE D'lRFE, QUEBEC H9X3HB

BondarCkcg A Company Ud5420 Cai*** RoadOttawa. OntarioKIJ9G2(613) 749-2220 Ibex 053-3233

Lab Report

UE PRINTED: 25-OCT-91REPORT: 091-42919.0 ( COMPLETE ) JECT: NONE PAGE 1A

SMPLE NUMBER

ELEMENT UNITS

Al Fe Tot PCT PCT

Mn PPM

Ng PCT

Ca PCT

Na PCT

K PCT

Se PPM

V PPM

Cr PPM

Co PPH

0-3 0-4

0.140.03

0.680.16

617113

10.00 no.oo3.75 HO.OO

0.060.06

0.050.03

2

GeochemicalRoadOaawa. OntarioKIJ9G2(613) 749-2220 lefex OM-.12.U

DATE PRINTED; 2S-OCT-91REPORT; 091-42919.0 ( COMPLETE ) | PROJECT; HOME________PAGE IB

SAHPLE ELEMENT Hi Cu Zn As Sr Y Ho Ag Cd Sn Sb NUMBER UNITS PPH PPH PPH PPH PPH PPH PPH PPH PPH PPH PPH

D-3 4 l 39 ^ 68 4 3 ^.2 4.2 4Q 32 0-4 4 ^ 4 ^ 142 4 3 ^.2 0.5 *20 20

OoawaOn^no

(613) 749-2220 Telex 05.1-3233

Geochcmtal

REPORT; 091-42919.0 ( COMPLETE )DATE PRINTED; 25-OCT-91PROJECT; MHE PAGE 1C

SAMPLE HUNBER

ELENENT UNITS

Te PPN

Ba PPN

La PPN

H PPN

Pb PPN

6i PPM

D-3 IH

4040

40 11

Lid.5420 Cawtek Road Ottawa. Ontario KIJ9G2

^(613) 749-2220 lefex 053-3233

Lab Report

REPORT: 091-42988.0 ( COMPLETE )

SAHPIENUMBER

ELEHEKT AlUNITS PCT

Fe TotPCT

PROJECT: KALADAR

MnPPM

KgPCT

CaPCT

KaPCT

KPCT

StPPM

VPPM

PAGE 1A

Cr CoPPM PPM

67116712671367146715

0.040.120.070.420.05

0.350.920.470.980.55

25775926847497

0.0340.00no. oo

6.7140.00

0.1340.0040.0040.0040.00

0.010.010.02O.G50.01

0.020.080.040.190.02

3^3^4

^328^

145 ^13 q

7 ^12 9

6 ^

67166717671867196720

0.020.350.030.050.02

0.640.480.46

393242430

0.78 17160.61 649

40.001.059.649.619.35

40.000.75

40.0040.0040.00

0.010.060.010.010.01

4.010.230.01

4.014.01

fl3tf^tf

41

452

4 3113 ^

15 5cl3 ^6 *1

67216722672367246725

0.100.060.153.910.20

0.83 7500.40 18852.953.571.83

131232133

40.008.861.191.280.17

40.0040.00

1.683.170.27

0.010.020.010.470.03

0.020.040.030.110.02

3S3^3

42

224026

5 ^<l ^

199 470 17

227 6

^ 67266727672867296730

0.100.020.230.083.57

1.420.34

81384

1.06 10510.446.07

263311

0.12HO. 0040.00

8.104.50

0.1040.0040.0340.00

1.22

0.010.019.02

4.010.32

0.024.010.11

4.011.26

tf^iS^18

925^

122

173 66 'l9 *1

<l ^97 17

67316732

0.56O.C8

3.690.31

93499

9.5940.00

0.:7HO. M

O.iD0.02

0.35O.C*

'5^

?2

111 25 ^

BoHte-OegB A Carnpny Ud 5420 Canon* Rcwl Ottawa. Ontario KIJ9G2

i (613) 749-2220 Idex 053-3233

Lab Report

REPORT: 091-42988.0 ( COMPUTE )

SAMPLE ELEKENT Hi CuNUS6ES UNITS PPH PPH

PROJECT: KALADAR PA&E 18

Zn As Sr Y MoPPM PPH PPM PPM PPM

A9PPH

CdPPM

SnPPM

SbPPM

6711 3 36712 ci ci6713 2 26714 5 46715 ci ci

ci c5 2 ci 19 c5 68 4 55 c5 77 6 6

11 c5 62 7 33 c5 46 33

C0.2cO.2cO.2cO.2cO.2

cO.2cO.2cO.2cO.2cO.2

c20c20c20c20c20

c537411939

6716 1 46717 2 36718 ci ci6719 2 26720 ci ci

2 c5 47 2 417 c5 4 16 ci2 c5 34 356 c5- 137 7 54 c5 49 3 3

cO.20.2

cO.2cO.2cO.2

cO.2cO.2cO.2cO.2cO.2

c20c20c20c20c20

32c5333729

672i 2 ci6722 ci <l6723 6 186724 58 596725 9 11

3 c5 50 5 44 c5 112 8 3

10 c5 7 ci ci41 c5 134 13 323 8 7 4 ci

cO.2cO.20.50.40.5

cO.2cO.2cO.20.3

cQ.2

c20c20c2025

c20

38326

c5c5

6726 7 B67?7 d ac-^c 2 ci6729 <l ci6730 28 35

19 c5 3 1 110 c5 103 ci 4iO -5 105 3 4ci c5 303 2 21

294 *5 43 5 ci

0.3cO.2cO.2cO.20.4

cO.2'0.2<9.2cO.20.5

c20c20^20c20c20

cS3?3616c5

6731 3 56732 ci ci

35 '5 9 19 ci11 '5 59 i 6

0.4cO.2

cO.21.2

c20*20

'5i]

3420Gnttek toriOttawa. OncarioKIJ9G2(613) 749-2220 lelex 053-3233

Geocfaemkal Lab Report

REPORT: 091-42988.0 ( COMPLETE )

SAMPLENUMBER

ELEMENT Te BaUNITS PPM PPM

La KPPM PPS

Pt)PPM

SBi

PPM

tOJECT: KALADAR PAGE 1C

Hg Aupro PPB

67116712671367146715

40 740 1340 37 .40 4540 9

4 402 402 403 40

4 40

44444

^26271127

3 4^ ^c5 ^6 tf^ ^

67166717671867196720

40 840 1140 1140 1540 8

4 403 40

4 403 401 40

4li444

21^201719

3 ^3 ^*5 ^4 ^13 25

67216722672367246725

40 3340 11640 12

13 1040 7

1 403 40

4 401 401 40

44145811

251886^

6 tf^ ^4 ^6 ^6 25

67266727672867296730

40 10440 157

~ -

40 2313 188

4 404 40

" ~-

4 404 40

104r?

433

^2329109

6 S3 ^^ -S^ <5<5 <5

67316732

40 3840 11

4 404 40

474

^29

^ <5 '

5420 Canotek Road Ooa*a. Omarin KIJ9G2Td: i6!3i 749-2220

-Fas: 16131 749-7170 BONDAR CLEGG

Geochemical Lab Report

KPOXT: 091-43314.0 ( COMPLETE ) : fi

SAMPLEMMEft

ELENENT AlUNITS PCT

FeTotPCT

NnPPN

NgPCT

CaPCT

NaPCT

me rmmcy; ii-vci'ji MUECT:MNE

KPCT

Se VPPH wu

PAGE 1A

CrPPN

j

CoPPN

67336734673567366737

0.040.050.201.093.12

0.240.250.822.344.02

1977392149267389

3.393.040.442.174.50

HO.OO4.770.730.972.70

0.010.020.030.260.51

0.020.010.050.110.12

*5 5^ 4^ 3

8 607 105

429

238115143

M. i

1 i8 i

23

673867 *9574067416742

0.320.281.530.340.15

0.741.422.671.000.76

443768135269

70

0.867.272.742.980.30

HO.OOno.oo

1.16HO.OO

1.10

0.050.030.020.020.01

0.06o.n1.130.320.05

4 135 199 98

(5 15*5 25

25358529

276

4^3 i41

67436744674567466747

0.480.090.152.622.40

0.310.691.004.533.09

49980182442210

0.118.270.705.252.77

0.36HO.OO

0.905.582.08

0.200.030.010.140.44

0.250.050.020.040.05

4 3^ 5^ 518 1828 78

17944

295198122

4 '4 i4 '-2615

^ 67486749675067516752

0.311.800.120.080.13

1.433.050.370.640.46

1158478229437471

1.552.965.512.002.71

^0.001.87

HO.OOHO.OOHO.OO

0.050.290.030.030.02

0.010.060.020.020.07

4 1421 126^ 74 4(5 4

13190

103

11

411 '4 'ci4 !

675367546755

0.070.160.11

0.540.420.27

525259200

2.390.233.23

no.oo4.66

HO.OO

0.020.010.02

0.040.090.02

c5 24 8*5 3

326015

444

:Ol Canoiek Road

Ottawa. Ontario KIJ9G2Tel: (613) 749-2220 Fax: (613) 749-7170

Ltd.

BONDAR-CLEGG

Geochemical Lab Report

KPttT: 091-43314.0 ( COMPLETE ) 1 R

SMPLE MMBER

ELEMENT Ni UNITS PPN

Cum

Zn PPH

As PPN

Sr PPN

V PPN

IL rmnii OJECT: NI

No PPN

J. U UUME

*9 PPN

rsi

Cd PPH

PAGE 16

Sn PPN

Sb PPN

6733 6734 6735 67X 6737

53 4

20 39

4 4

4 5

45

10 18 20 50

114

9 3 3 315

113 13 3

11 33

8 3 46 5

9 4 44 3

4.2 4.2 4.2 0.4

4.2

0.9 1.7 1.4 0.5 0.9

^ 24 21 ^ 30

23 8S 6

21

6731 6739 6740 6741 6742

5 10 12 10 U

4 12 4 15 4

26 18 3651 10

3 S 3 17

6

61 455

97 7

2 13 11

7 4

7 5 4 5 4

4.2 4.2 0.2

4.2 4.2

0.8 4.2 4.2 1.3

4.2

40 40 28

40 40

18 23 11 U 3

6743 6744 6745 6746 6747

43 6

3826

a 4 fl 8

112

24 6 7

122 69

3 3

7 15 G

4 61 5

43 69

26 11

1 8 5

9 7

4 4 3

4.2 4.2 0.2

4.2 0.2

0.5 1.4 0.3

4.2 0.6

40 40 40 40 40

3 32 S 19 U

^ 6741 5'49 T58sol 6752

4 IB 2 3 3

4 4a20a

19 91 14

257 24

9K5

3 S 6

394 27

325 165 149

10 8 3 4 3

6 1 7 6 8

4.2 0.4

4.2 4.2 4.2

4.2 4.2 4.2 0.9

4.2

40 40 40 40 40

19 9

22 18 20

6753 6754 6755

47 2

304 4

150 18 49

10 6 3

132 73

335

6 64

7 4 6

4.2 4.2 4.2

4.2 4.2 4.2

40 40 40

21 418

5420 Camnek RoadOnawa. OntarioKIJ9G2Td: (6131 749-2220Fax: (613) 749-7170

Ltd. Geochemical Lab Report

BONDAR CLEGG

KPttT; 091-43314.9 ( CQNIIETEiTE PmHTEDi U-OK-91WKE-W

ffOJECT: WOE PACE 1C

SAMPLE MJMER

ELEKNT Te UNITS PPN

Ba PPN

La PPN

N PbPPN PPN

Bi PPN

Hg m

Au 1 PPB l

6733 6734 6735 6736 6737

40 40 40 40 16

25 9 7

17 24

6 11 7 3

30 5 30 10 30 5

7 8

12 15

7 7 5 7

10

8 i! i75 i

6738 6739 6740 6741 6742

40 4140 40 40

21 36 57 27 13

17 20 64

30 3

30 4 30 3 30 3

22 5 6

17 94 17 10 8

5 ! 8 j

11 j

6743 6744 6745 6746 6747

40 40 40 19 40

7 24 73 12 17

8 8 4 5 3

30 11 30 3 30 3 30 3 30 7

24

16 11

10 10 10 17 13

5 ii

5 14

^ 6748 6749 6750 6751 6752

40 10 40 40 40

9 15 147 5

5 41 4 3

30 3 30 3 30 3 30 3 ^ 3

6 7

13

6

10 13 7

10 7

5 :6 :

6753 6754 6755

40 40 40

7 tfOOO

12

5 8 2

^ 4 30 3 30 3 6

18 10 29

s i6 :

Bondar-Cfcgg A Compmiy Ud 5420 Canutek Road Ottawa. Ontario KIJ9G2

^613) 749-2220 lekac 053-3233

Geochemical Lab Report

REPORT: 091-42918.0 ( PARTIAL ) |

CLIENT: 6E08RACK INC. PROJECT: HONE

REFERENCE INFO: j

SUBMITTED BY: H. SACK DATE PW1ED: 28-OCT-91

ORDER

12

A1Fe

ELENENT

AT MimaTot Total Iron

NUKBER OFANALYSES

7575

LOVERDETECTION LIMIT EXTRACTION

0.01 PCT0.01 PCT

HCL-HN03,HCL-HM03,

(3:1)(3:1)

i

HEThDD j

Ind. Coupled Plasna -Ind. Coupled Plasaa

34567

MnNgCaMaK

ManganeseHagnesiimCalcianSodiunPotassiim

7575757575

1 PPH0.01 PCT0.01 PCT0.01 PCT0.01 PCT

HCL-HN03,HCL-HH03.HCL-HN03,HCL-HN03,HCL-HH03,

(3:1)(3:1)(3:1)(3:1)(3:1)

Ind. Coupled PlasaaInd. Coupled Plasma ;Ind. Co-jpled Plasna 'Ind. Coupled Plasma |Ind. Coupled Plasna !

i

89

101112

SeVCrCoHi

ScandiuHVanadiiBChroaiunCobaltNickel

7575757575

5 PPM1 PPH1PPH1 PPH1PPH

HCL-HS03,HCL-HN03,HCL-HN03,HCL-HN03,HCL-HN03,

(3:1)(3:1)(3:1)(3:1)(3:1)

Ind. Coupled Plasna ;Ind. Coupled Plasca 'Ind. Coupled PlasaaInd. Coupled PlasiaInd. Coupled Plasia

^ 1314151617

CuZnAsSrY

CopperZincArsenicStront^unYttriuB

7575757575

l m.1 PW5P?H1PPH1PPH

HCL-HH03,HCL-W03,HCL-HN03,HCL-HN03,HCL-HH03,

(3:1)(3:1)(3:1)(3:1)(3:1)

Ind. Coupled PlasaaInd. Coupled Plasnafad. C:,'?.2Q P'-asnaInd. Coupled PlasaaInd. Coupled Plasna

1819202122

232425l;'

27

*oAgCdSnSb

TeBaLa

Pb

HolybdenunSilverCadniuaTinAntioony

TelluriumBariunLanthanumT. . ,

Lead

7575757575

757575~C

75

1 PPH0.2 PPH0.2 PPH

20 PPK5PM

10 PPH2 PPH1 PPK

i*, ----(j

2 PPN

HCL-HN03,HCL-HN03,HCL-HM03,KCL-HN03,HCL-HS03,

HCL-HH03,HCL-HM03,HCL-HNOJ,..- ... --.

HCL-HH03,

(3:1)(3:1)(3:1)(3:1)(3:1)

(3:1)(3:1)(3:1)

(3:1)

Ind. Coupled PlasnaInd. Coupled PlasmaInd. Coup'-ed PlasmaInd. Co-jpled PlasnaInd. Coupled Plasia

Ind. Co-jpled PlasnaInd. Coupled PlasnaInd- Coupled P'asra.

InG. Copied P'asra

28 Bi Bismuth 75 5 PPH *CL-HS03, (3:1) lid. Coupled Plasna

RESULTS TO FOLIO* FOR: U

Bandv-CkK&Ca 5420 Omoldc Road Ottawa Ontaiio KIJ9G2

k (613) 749-2220 Tdex 053-3233

Geochemkal Lab Report

SEPOST: 091-42918.0 ( COSPLETE )

SAMPLEM'S&ER

ELEKEsT U A 1 FeUNITS PPfl PCT

Tot KnPCT PPH

KgPCT

\Ca

PCT

IQJECT: N!

KaPCT

AE PAGE 1A

KPCT

SePPS

VPPM

CrPPH

H-lH-2H-3H-4H-5

1.7 0.28 0.30 572.251.17

1.85 761.14 63

2.42 2.84 1G81.8 1.15 3.12 122

0.121.010.680.780.51

0.240.100.520.080.08

0.050.050.050.050.05

0.030.040.050.040.04

<5<5\'5<5<5

831154459

821152417

H-6H-7H-8K-9H-10

0.27 9.49 350.44 0.35 340.82 0.11 20

1.1 0.68 0.36 311.77 2.63 1742

0.100.130.110.180.71

0.050.050.020.660.33

0.050.050.060.050.05

0.020.020.030.030.05

<5<5*5<5<5

141457

57

56

i

6 i32 ;

K-llH-12K-131-14K-15

1.473.24

1.13 1411.85 85

2.2 4.06 3.34 2690.62 1.65 22560.72 0.20 90

1.371.061.980.320.12

0.290.130.080.100.03

0.050.050.050.050.05

0.050.070.100.040.03

^76

*5<5

22305326

9

252841118

^ -H6H- i?w. p

-19ft-23

2.13- 0.95 652.9 4.30 3.00 650i

J. 242.45l.SG

1.53 :011.70 1672.62 ?6i

0.851.850.831.631.69

0.320.360-130.350.35

0.06C.OCG.D5C.05O.G6

0.040.20O.Qi0.030.15

<55

-5-5

5

161-9i?3950

23f.-. 637 :33

"-:. 2.0 i.93 i.;l 83".-22 -2Jf- 24*-25

3.563.5?2.55

1.9 1.72

:.:S 572.2? 2.1.97 1DOn.86 57

1.05}.I90.251.220.75

3.2i3.100.200.090.24

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Geocbemical Lab Report

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Geochemical Lab Report

REPORT: 091-42918.0 ( COMPLETE )

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Geochemical Lab Report

REPORT: 091-42918.0 ( COMPLETE )

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MINISTRY OF NATURAL RESOURCESSURVEYS AND MAPPING BRANCH

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Lot And Concession Lines Shown Hereon Are Projected From The Best Information Available, But Their True Position Is Not Guaranteed For Official Survey Purposes Consult The Original Survey Plans And Field Notes Of Records In The Uept Of Londs S Forces

4OO' Surfoce Rights Reservation Around All l akps And Rivers

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MARBLE Outcrop

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PEGMATITE

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