REPORT ON THE FALL, 1999 DRILLING PROGRAM, CEDAR ...

GM 57567REPORT ON THE FALL, 1999 DRILLING PROGRAM, CEDAR RAPIDS PROJECT

http://gq.mines.gouv.qc.ca/documents/examine/GM57567

http://gq.mines.gouv.qc.ca/documents/sigeom/Licence.pdf

http://gq.mines.gouv.qc.ca/documents/sigeom/license.pdf

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2 PM 1999

BUREAU REGIONAL ROUYN-NORANDA

CAMECO CORPORATION

REPORT ON THE FALL, 1999 DRILLING PROGRAM

CEDAR RAPIDS PROJECT

QUÉVILLON, LAAS AND TONNANCOURT TOWNSHIPS

QUEBEC, NTS 32C/14, 32F/02 and 32F/03

December, 1999

Dominic Babin Geologist

NI?tN-GÉOINFORMATION 2000

GM 57567

2

SUMMARY

The Cedar Rapids Project is located at the junction of Quévillon, Laas, and Tonnancourt Townships, approximately 10 kilometres south of Lebel-sur-Quévillon, and about 150 kilometres north of Val d'Or, Quebec. The project consists of 162 mining claims covering an area of 3134.72 hectares. Cameco has the option to earn 87.5% interest in the property, while, the Société de développement de la Baie James holds 12.5% interest in the property.

The Cedar Rapids property is underlain by dominantly southeast to East-southeast striking, steeply dipping, greenschist facies, Archean volcanic and sedimentary rocks within the Abitibi greenstone belt. Lithologies present include: ultramafic, mafic, intermediate and felsic volcanic and volcaniclastic rocks, greywacke, argillite, carbonaceous argillite ("graphite") and minor iron formation. The volcanic and sedimentary rocks are intruded by aphyric, feldspar porphyritic, and quartz feldspar porphyritic mafic, intermediate and felsic dykes, sills and plugs. A massive biotite granodiorite pluton underlies the west end of the property, and this is cut by two northeast striking diabase dykes. Three gold occurrences are known on the property. The Village Zone and the Zone 1 (or Discovery Zone) occurrences are historic showings. The Dyke Zone was discovered by Cameco drill hole CDR98-07 in 1998.

The fall 1999 drill program at Cedar Rapids, totalling 2,204.8 metres in eight holes, was carried out from September 8th to October 15th, 1999. Hole CDR9937 intersected the best mineralized interval of the 1999 drill program and the widest mineralized interval showing significant gold assays on the property (2.0 g/t Au and 0.15% Cu over 31.4 m or about 18 m true width). The mineralization consists of a series of chalcopyrite-pyrite-quartz-calcite-magnetite stringers located generally between strongly chloritized fractures or pillow selvages within a succession of variolitic mafic flows, moderately to strongly epidotized, carbonatized and biotitic. Visible gold was observed for the first time on the property in one of the chalcopyrite-pyrite-quartz-calcite stringer and the returned 13.9 g/t Au over 0.3 metres. This type of mineralization is very similar to the other mineralized intervals intersected in previous drill programs at the Village Zone. The stratigraphic and structural relationships suggest that the stringer mineralization could represent a large feeder system to an economic gold-rich massive sulphide deposit. Available historic data and results from this program indicates that gold grades are increasing to depth and that the system is open along strike and at depth. It should be considered as the highest priority target for future drilling program.

Holes CDR9932 and CDR9936 intersected feldspar-quartz porphyry, variably epidotized, locally carbonatized, and cut by vuggy chlorite-calcite (+/- anhydrite)-epidote-quartz stringers containing variable percentages of pyrite and chalcopyrite. Molybdenite was recognized in a few of these stringers (highest assay was 671 ppm Mo/0.7 m). These observations suggest that an intrusion related alteration and mineralization system could have affected part of the stratigraphy in the area between the Village Zone and the Dyke Zone, in addition to the interpreted hydrothermal volcanogenic mineralization found at the Village Zone (Mouska-Bousquet type of setting). However,

Cameco Corporation Cedar Rapids Project Report on the Fall, 1999 Drilling Program

3

the locally strong presence of epidote (i.e. in matrix, veins, joint, planes, plagioclase overgrowths), presence of calcite (+/- anhydrite) veinlets with chlorite alteration haloes and absence of significant quartz veins may suggest that the intersected intrusive intervals are relatively removed from an area of strong alteration and mineralization.

The intermediate volcaniclastic sequence (mudstones, siltstones, sandstones and conglomerates) hosting the Dyke Zoné mineralization was intersected in all holes, except CCDR9933. In the upper half of hole CDR9934, weakly to moderately chloritized, epidotized and mineralized zones were intersected and returned significant assays of 1.3 g/t Au over 2.8 metres (including 6.0 g/t Au/0.5m) and 0.9 g/t Au over 3.4 metres (including 2.0 g/t Au/ 1.0m). These zones appear to grossly represent the extension at depth of the upper mineralized zone intersected in hole CDR9818 (0.7 g/t Au/4.3 m). A similar altered and mineralized sequence was intersected downhole, at the contact of a 35 metre-wide feldspar-quartz porphyry, representing the depth extension of the Dyke Zone (24.3 g/t Au/1.1 min CDR9807 and 3.4 g/t Au/2.0 min CDR9818). The only significant assay obtained from this 11.8 metre wide alteration zone was 6.4 g/t Au over 1.0 metre. Other similar mineralized alteration zones were intersected in holes CDR9935, CDR9936 and CDR9937 of the 1999 drill program, and holes CDR9922 and CDR9923 of the 1998 drill program. The work completed so far suggest that at least three or more sub-parallel mineralized alteration zones crosscut the volcaniclastic stratigraphy, but more work (petrography, geochemistry and more drilling) is needed to identify the orientation and the true nature of these zones or pipes. The mineralized system is still open along strike and at depth, although it should represents a lower priority target than the Village Zone mineralization.

Following these results, a 1000 metre drill program is recommended to test the strike and depth extension of the mineralization intersected in hole CDR9937. Geological, petrographical structural and lithogeo chemical compilation work should be carried out prior to the start of the drilling program. Borehole T.E.M. survey is suggested in hole CDR9937 to search for a gold-rich massive sulfide target in the vicinity of the hole.


4

TABLE OF CONTENTS

Page

SUMMARY

2

1.0 INTRODUCTION 6

1.1 Property Location, Access, Infrastructure and Topography 6

1.2 Property Sensitivities 8

1.3 Claim Ownership and Land Status 8

1.4 Previous Work 9

1.5 Previous Cameco Corporation Work 11

2.0 GEOLOGY 13

2.1 Regional Geology 13

2.2 Property Geology 13

3.0 Fall 1999 CAMECO CORPORATION DRILLING 20

3 1 Purpose of the1999 Drilling Program 20

3.2 Drilling Results 20

3.3 Lithogeochemistry 33

4.0 DISCUSSIONS AND CONCLUSIONS 35

5.0 RECOMMENDATIONS 39

6.0 REFERENCES 41

CERTIFICATE OF QUALIFICATIONS 43


5

LIST OF FIGURES

Figure 1

Claims and Drill Holes

7

Figure 2

Geology and Drill Holes

14

Figure 3

Geology, Drill Holes and Significant Assays

28

Map 1:

Map 2:

Map 3:

Map 4:

Map 5:

Map 6:

LIST OF MAPS

1:500 Section for DDH CDR97-2, CDR97-6 and CDR9933

1:500 Section for DDH CDR9932

1:500 Section for DDH CDR9807, CDR9818 and CDR9934




In pocket

In pocket

In pocket

In pocket

In pocket

In pocket

LIST OF TABLES

Table 1. CDR9937 Summary Log. 27

Table 2. 1999 Cedar Rapids Project Drill Holes 29

Table 3. Cedar Rapids Project, 1999 Drill Program, Summary of Significant assays 30

APPENDICES

Appendix 1 Diamond Drill Hole Logs

Appendix 2 Au and ICP Assay Certificates for Drill Core

Appendix 3 Whole Rock Analysis Certificates for Drill Core

Appendix 4 Diamond Drill Hole Sections

Cameco Corporation Cedar Rapids Project

Report on the Fall, 1999 Drilling Program

6

1.0 INTRODUCTION

This report describes the results of diamond drilling carried out by Cameco Corporation (Cameco)

on the Cedar Rapids Project between September 8th and October 15 h, 1999. The property was

acquired in 1997 because of two historic gold showings suggested potential for gold-rich, volcanic-

hosted, massive sulphide mineralization similar to that observed in the Bousquet-LaRonde-Doyon

Camp. The 1999 drill program was carried out to explore for extensions to the Dyke and Village

zones. Eight drill holes totalling of 2,204.8 metres were completed by Forage Val d'Or of Val d'Or,

Quebec.

1.1 Property Location, Access, Infrastructure and Topography

The Cedar Rapids Project is located at the junction of Quévillon, Laas and Tonnancourt Townships,

within the Val d'Or mining district, on NTS sheets 32C/14, 32F/02, and 32F/03. The coordinates

for the centre of the property are longitude 77° 04'W and latitude 49°N (349000E and 5430000N, in

Nad 27 Zone 18). The property is situatedl0 kilometres south of Lebel-sur-Quévillon, Quebec, and

150 kilometres north of Val d'Or (Figure 1). Access to the property is provided via Highway 113,

power lines, trails, and the Bell River.

Electrical power can be obtained from a high voltage transmission line crossing the East half of the

property. Skilled labour and mining equipment are available in Lebel-sur-Quévillon and Val d'Or.

The property lies within the Hudson Bay watershed. The topography is generally flat due to a thick

clay cover and is punctuated by rolling hills, local moraines and eskers. Till is absent or deeply buried

in low lying areas. Water ways on the property consist of drainage channels up to 10 metres in depth

that flow into the Bell River (Figure 1, 2 and 3). Vegetation includes poplar and birch forests, spruce

swamps, and cut over areas overgrown with poplar and alder.


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Cedar Rapids Project

CLAIMS AND DRILL HOLES

Compiled: Dominic Bob n Dwg. No.: CDR99_cIaim

Drafted: Chris Halchuk, Clayton Durbin Date 99/12/14

Scale: 1:50,000 Geo. Ref.: NAD 27 — UTM Zone 18

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Figure 1

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Montreal 34, Fall 1999 Cameco Drill Hole ---- Cedar Rapids Claims

USA

8

1.2 Property Sensitivities

The site of an old sawmill is located on the north shore of the Bell River, 500 metres North of the

Highway 113 bridge. Domtar has top dressed and seeded the upper surface, but scrap wood and

metal are still visible on slopes and edges.

A groomed snowmobile trail follows an east-northeast trending hydro line across the south central

portion of the property to Highway 113. From there it heads northeast to Lebel-Sur-Quévillon.

Drilling equipment cannot be moved on this trail during winter. During the summer, care must be

taken not to destroy the trail surface, and permission must be obtained from Lebel-Sur-Quévillon

town office before moving equipment on the trail.

There is a house 1 kilometre North of the Bell River bridge on the West side of Highway 113. There

are also several cabins, occupied by families belonging to the Lac Simon Indian Band, located north

of the Bell River approximately 700 metres northwest of Highway 113.

MRN approved work permits were obtained through the services of Mr. Gaston Lacroix of La Sylve

de la Haute Harricana Inc., and drilling plans were discussed with Mr. Serge Woods of the Lebel-sur-

Quévillon town office, prior to drilling. All drill sites were inspected after all equipment had been

removed following completion of the drill holes.

1.3 Claim Ownership and Land Status

The Cedar Rapids project consists of 162 mining claims (Figure 1) covering an area of 3134.72

hectares. One hundred and sixty-three claims were optioned from Explorations Minières Hervé

Blondeau Ltée in 1997. Sixty claims were added to the property through staking by Cameco in

February, 1997, in July, 1997 and in December 1998. Cameco's option on 61 claims was terminated

October 1998. Cameco has the option to earn 87.5% interest in the property, while, the Société de


9

développement de la Baie James holds 12.5% interest in the property. Claims on which drilling was

performed are listed in Table 2. These claims are also recorded in the header data for each drill log

(Appendix 1), and on drill sections (Appendix 4).

1.4 Previous Work

The Quebec Bureau of Mines (QBM) completed regional geological reconnaissance work along the

Laflamme River to the west of the property in 1934 (QBM Annual Report, 1934, Part C). The area

was then mapped by W.W. Longley in 1937 and 1938 for the Government of Quebec (Auger and

Longley, 1939; Longley, 1938). He produced a map at a scale of 1:63,360 often townships including

Quévillon and the north half of Laas and Tonnancourt. In 1981, the Government of Quebec flew the

Comtois-Cavelier A.E.M. (INPUT MK VI) survey (DP-819) and also created regional geological

compilations at a scale of 1:250,000.

Previous exploration work on the property, completed by several companies between 1959 and 1988,

includes limited geological mapping, trenching, drilling, and various geophysical surveys. From 1958

to 1961, Quebelle Mines Limited carried out prospecting, trenching, and drilled 22 diamond drill

holes. These exploration programs were the first detailed work on two gold showings namely, Zone

1 and the Village Zone (Figure 3). Exploration work on the Zone 1 showing returned up to 72.8 g/t

Au over 0.3 metres in chip samples. The work on the Village Zone returned values up to 300.9 g/t

Au in grab samples which contained pyrite and chalcopyrite, and returned up to 3.76 g/t Au over 6.1

metres from drill core (GM 8802, 9271,10518-A, 10518-B, 10559, 10580, 10890). In 1959,

Quebelle Mines Limited also flew an airborne magnetic and electromagnetic (Rotary Field System)

survey over the project area (GM 9340). A few airborne anomalies were identified on the property

and were mostly located at the Village Zone area.


10

In 1965, the Government of Quebec drilled two vertical holes on the south shore of the Bell River

along Highway 113. Simplified drill core descriptions are filed under GM 21490 and GM 21509 and

geochemical analyses are reported.

In 1977, Maurice Latùlippe, MERQ Resident Geologist of the Val d'Or district wrote a summary

report for the Village Zone and Zone 1 (GM 32671). In the same year, Shell Minerals flew airborne

EM and magnetic surveys over a large area including Comtois, Laas, Quévillon, Tonnancourt, and

Verneuil Townships (GM 38810). This new airborne survey outlined similar anomalies to the

Quebelle's 1959 survey and the anomalies were confirmed by a later survey done by the Government

of Quebec in 1981. Also in 1977, the Cedar Rapids project area was withdrawn from staking by the

government due to the James Bay hydro development projects.

In 1984, Teck Exploration completed line cutting and diamond drilling in the north central part of the

property. They encountered a graphitic argillite conductor. A small grid was also cut and a

H.L.E.M. survey was carried out at near a former float plane base, but no drill targets were defined

(GM 41432, and 43434).

In 1988, Butte Canyon Resources Inc. carried out line cutting, H.L.E.M. surveying, and diamond

drilling on the north shore of the Bell River to the west of the float plane base (GM 46150). No

encouraging results returned from the drilling program.

In 1988, Explorations Minieres H. Blondeau Ltd obtained an exploration permit from the Societe de

Developpement de la Baie James (SDBJ) to do prospecting work on the Cedar Rapids property. In

1988, H. Blondeau completed property evaluations, prospecting, and backpack drilling. All the data

remained private due to the nature of the exploration permit. In 1994, the permit areas were staked

in order to conform with the Quebec Mining Act. In 1995, minor geophysical and prospecting work

was carried out. In 1996, 281 line kilometres were cut and VLF-EM surveys were done on the entire

property. The survey outlined numerous conductors.


11

1.5 Previous Cameco Corporation Work

In 1997, Cameco completed 255 line kilometres of geological mapping, detailed mapping of shoreline

outcrops at the Village Zone, and excavation of one trench at the Zone 1 showing (Faber et al, 1998).

Drill core from H. Blondeau's 1988 drill holes was relogged and sampled (Faber et al., 1998). The

Village Zone is characterized by gold and copper mineralization hosted in sulphidic pillow selvages

and fracture fillings in intercalated variolitic mafic flows and ultramafic flows. Grab samples with up

to 43.8 g/t Au and others with up to 5.6% Cu were obtained from Village Zone outcrops. Sampling

of the 1988 drill core returned intervals with 4.57 g/t Au over 4.2 metres and 2.54 g/t Au over 4.6

metres. The gold mineralization observed at Zone 1 is characterized by chlorite-pyrite rich shear

zones cutting a feldspar porphyritic felsic rock. Trenching and channel sampling on this showing

returned up to 13.7 g/t Au over 1.0 metre.

During 1997 and 1998, ground geophysical surveys were completed prior to each phase of drilling

as new target areas were selected based on the results of the previous drilling phase. All geophysical

surveys completed for Cameco were carried out by GÉOLA. In August, 1997, 251 line kilometres

of magnetometer surveys were carried out along existing north-south lines on the Blondeau option

(Lavoie, 1997a). Due to an almost complete lack of outcrop away from the Bell River, this

magnetometer data was used extensively in preparing the initial geological interpretation for the

property.

In November, 1997, a new rotated grid (with 100 metre spaced lines at azimuth 050) was established

northwest of the Village Zone, and 15.0 kilometres of H.L.E.M. surveying was completed (Lavoie,

1997b). This survey was used to delineate, on the ground, positions of a number of A.E.M.

conductors defined during airborne geophysical surveys by Quebelle Mines, Shell Minerals and the

Government of Quebec. In March, 1998, 12.4 kilometres of magnetic surveying were completed on

the rotated grid. Dipole-dipole I.P. surveys were completed over 15.6 kilometres covering small

portions of the rotated and north-south grids in six separate locations on the property (Plante, 1998a).


12

A further 8.2 kilometres of dipole-dipole I.P. were completed over the newly expanded rotated grid

south of the Bell River in July, 1998 (Lavoie, 1998). In November 1998, 11.6 kilometres of dipole-

dipole I.P. were completed over seven north-south grid lines and one east-west tie line in the south

central portion of the property. Several new I.P. targets were defined (Plante, 1998b).

Cameco completed a total of 5,704.8 metres of diamond drilling in thirty-one diamond drill holes

during four phases of drilling carried out between November 18t, 1997 and December 7 h, 1998. The

results indicate that the best potential for gold mineralization on the Cedar Rapids property lies in the

area between the Village Zone, Dyke Zone and Zone 1 gold occurrences (Brisbin, 1998; Babin and

Brisbin, 1999). The Village Zone and the Zone 1 (or Discovery Zone) occurrences are historic

showings. The Dyke Zone was discovered by Cameco drill hole CDR98-07 in 1998. The highest

gold values intersected by Cameco drill holes at the three known gold occurrences are 24.3 g/t over

1.1 metres (CDR98-07) in the Dyke Zone, 6.0g/t Au over 1.0 metres (CDR97-02) in the Village

Zone, and 0.8g/t Au over 1.5 metres at Zone 1 (CDR97-03). All three zones occur within a south

facing, east-southeast to east-striking, steeply north-dipping package of volcanic and volcaniclastic

rocks. These include pillowed and massive (locally variolitic) mafic volcanic flows, massive (locally

spinifex-textured) ultramafic volcanic flows, and mafic to intermediate monolithic and polymictic

volcaniclastic rocks. Feldspar porphyritic felsic dykes (Village Zone, Dyke Zone) and plugs (Zone

1) intrude the volcanic rocks, and are themselves mineralized at the three known gold occurrences.

Gold is associated with chlorite-carbonate-pyrite-chalcopyrite veinlets (Dyke Zone, Village Zone),

pyrite-chalcopyrite-magnetite-carbonate assemblages in epidotized and chloritic pillow selvages

(Village Zone), and east-southeast striking chloritic-pyritic foliated zones (Zone 1).


13

2.0 GEOLOGY

2.1 Regional Geology

The Cedar Rapids project is located in the Joutel-Quévillon corridor of the Archean age Abitibi

greenstone belt. The area is underlain by greenschist metamorphic facies ultramafic to felsic volcanic

rocks, intermediate and felsic volcaniclastic rocks, and sedimentary rocks. Several younger

monzodiorite, hornblende granodiorite and syenite plutons intrude the supracrustal rocks (MERQ-

OGS, 1981). The Sleeping Giant Mine (1,814,662 tonnes at 10.35 g/t Au) currently being operated

by Cambior, is located 70 kilometres West of the Cedar Rapids project. Cambior also operates the

Gonzague-Langlois Mine (10,673,000 tonnes at 8.41% Zn, 0.46% Cu, 37 g/t Ag and 0.09 g/t Au)

35 kilometres to the northeast. Two significant gold exploration projects in the area are at the

advanced stage. GeoNova Explorations has outlined a resource of 1,215,5000 tonnes at 6.95 g/t Au

in the Discovery Zone on its Desjardins property 30 kilometres North of the Cedar Rapids property.

Teck Corporation and Murgor Resources have defined a drill indicated resource of 555,000 tonnes

at 6.86 g/t Au in Barry Township 95 kilometres to the East.

2.2 Property Geology

Outcrop is scarce on the Cedar Rapids property, and with the exception of two outcrops, it all occurs

along the shores of the Bell River. The geology of the property, as summarized below, is based

largely on the interpretation of geophysical data constrained by available outcrop and diamond drill

holes (Figure 3). A detailed description of lithologies that outcrop is provided by Faber et al (1998).

The central and eastern portions of the property are underlain by east-southeast to southeast striking

volcanic, volcaniclastic and sedimentary rocks. A unit of mafic and ultramafic schists, representing

tectonized Mg-rich volcanic rocks, occurs in the extreme northeast portion of the property. It is

characterized by a high magnetic susceptibility. Both carbonaceous argillite ("graphite") and sulphide


North

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Quevillon Township

Cameco GEOLOGY AND DRILL HOLES

Compiled: Dominic Bab n Dww. No.: COR99_geology

Soda: 1:50,000 0e0. Ref.: NAD 27 — UTM Zone 18

'LEBEL-SUR-0UEVIUAN

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2000 2500m

James Bay

ONTARIO 1Matagami

A Cedar Rapids Timmins* Nor,ndo Val—d'Or Cuebec

• Kirkland QUEBEC

I Lake

^. Ottawa ~ Sudbury • —;

Symbols Lake shoreline or stream — — Transmission Line H-H- Railroad

Highway

6/ Previous Cameco DDH 34•f Fall 1999

Cameco Drill Hole

Legend I1 B Felsic Intrusive Rocks V1 Felsic Volcanic Rocks V2 Intermediate Volcaniclastic

Rocks V3 Mafic Volcanic Rocks V4 Ultramafic Volcanic Rocks S Sedimentary Rocks

S10 Iron Formation — Geological Contact

.,. Fault /(Montreal

~J / USA

LOCATION MAP

n

Scale 1:50000


Drafted: Chris Halchuk, Clayton Durbin Date: 99/12/14 Figure 2

NTS Ref.: 32F02, 32F03, 32C14, 32C15 Source:

0 100km

15

facies iron formation have been intersected in drill holes in the vicinity of a 300 to 500 metre wide

belt of formational A.E.M. conductors that occurs along the south contact of this unit.

To the south lies a 2 kilometre wide package of undifferentiated volcanic rocks characterized by

moderate magnetic susceptibility. A.E.M. conductors within this unit are confined to two areas in

the north-central portion of the property. One 1.5 kilometre long conductive trend is due to graphite

present along the contact of this unit with sedimentary rocks to the south. An interflow graphite is

also the source of a second, 600 metre long, conductive trend within the volcanic package.

A 1.5 kilometre wide package of interbedded greywackes and argillites strikes southeast across the

central portion of the property. Felsic volcaniclastic rocks and graphites are interbedded with the

wackes and argillites near their contact with volcanic rocks to the south. The graphites are the source

of a cluster of A.E.M. conductors along the Quévillon River in the southeast end of the property.

A.E.M. conductors that occur in the central portion of the property along the contact between these

sedimentary rocks and Village Zone volcanic rocks (see below) to the southwest are due to weakly

conductive graphite and narrow massive pyrite beds hosted in the southernmost felsic volcaniclastic

unit in the dominantly sedimentary package.

A southeast striking package of intercalated mafic and ultramafic volcanic flows and sills,

characterized by high magnetic susceptibility, roughly follows a southeast trending portion of the Bell

River in the central portion of the property. This rock package is 4 kilometres long and up to 750

metres wide. The historic Village Zone gold occurrence is hosted in chloritized, epidotized, pillowed,

locally variolitic, mafic flows exposed where the Highway 113 bridge crosses the Bell River. Gold

values of up to 2.0g/t over 31.4 metres (including 20.0 g/t Au/0.3 m) in drill core (1999 drill

program), and up to 43.8g/t Au and 5.6% Cu in grab samples, (Faber et al, 1998) have been obtained

from pyrite-chalcopyrite-chlorite-carbonate filled pillow selvages and veinlets. In two drill holes

(CDR07-06 and CDR98-30), the upper part (20 to 70 metres thick) of the Village Zone stratigraphy


16

consists of angular mafic breccia, where the interstices between the fragments are filled with aphanitic

silica and sericite (low temperature hydrothermal activity?).

A package of intermediate volcaniclastic rocks overlies the Village Zone stratigraphy. The extent

of this unit is poorly defined as it is only known from a few outcrops and drill holes, but it is at least

600 metres wide. It is composed of a coarsening upward sequence of siliceous, chloritic, tuffaceous,

dark green to light grey sandstones interbedded with polymictic volcanic conglomerates and breccias.

The latter are composed of lapilli to block sized, angular to sub-rounded, dominantly dacitic and

andesitic fragments in a green chloritic matrix. The first 0.9 to 1.3 metres of this package,

comformably overly the Village Zone stratigraphy and is weakly anomalous in gold (values up to

122ppb Au over 1.3 metres in CDR97-01). It is composed of siliceous tufchert containing 5 to 10%

bedding- and fracture-controlled pyrite. The middle part of this package hosts the Dyke Zone. Gold

values of up to 24.3g/t over 1.1 metres have been intersected in drill core associated with pyrite-

chalcopyrite-chlorite-carbonate veinlets, in proximity to a quartz and feldspar porphyritic dyke.

Similar mineralization has been found in other parts of this package, where dykes are narrow (less

than 2 metre wide) or absent. The sulphide-chlorite-carbonate veinlets are either pyrite-rich or

chalcopyrite-rich and are grouped within 0.3 to 8.3 metre wide intervals. The alteration associated

with the mineralization generally consists of moderate to strong pervasive chlorite alteration

associated with variable amount of disseminated biotite specks, that gradually decreases outwards

from the stringer zones. Moderate to strong patchy epidote alteration is usually seen enveloping the

chlorite-biotite alteration. This zonation pattern is also observed with the stringers. The stringers

near the centre of the mineralized zones are richer in chalcopyrite and gold, while away from the

centre, the stringers are mainly composed of pyrite with little chalcopyrite and only anomalous gold.

The best gold values are found associated with the chalcopyrite-rich veinlets and are up to 1.3g/t

over 2.8 metres (including 6.0 g/t Au/0.5 metres) in hole CDR9934. There are at least three or more

sub-parallel mineralized alteration zones within the intermediate volcaniclastic assemblage. The

orientation and nature of these zones or pipes is not yet fully understood.


17

The south-central portion of the property is underlain by a folded package of mafic and ultramafic

flows characterized by generally high, but variable, magnetic susceptibility. The western part is

intruded by a layered, feldspar porphyritic gabbro sill (>110 metres wide) containing plagioclase

phenocrysts up to 2 centimetres long. The phenocrysts are concentrated in 70 centimetre to 11.5

metre thick layers. There is no outcrop and only a small portion of this package has been explored

by drilling. The sources of I.P. anomalies tested by drilling have proven to be interflow graphitic

argillite and sulphidic chert horizons, pyritized intervals and graphitic fault zones. The volcanic flows

are variably carbonatized, sericitized, fuchsitic and foliated, but no significant gold mineralization has

been intersected.

Throughout the property, aphyric, feldspar porphyritic, feldspar-hornblende porphyritic and quartz-

feldspar porphyritic, intermediate to felsic dykes, less than 1 metre to more than 35 metres wide

intrude the volcanic and sedimentary rocks. Feldspar porphyritic intrusive bodies of similar

composition are closely associated with mineralization at all three known gold zones. The Dyke Zone,

described above, is localized in proximity to the East contact of a 35 metre wide, quartz-feldspar

porphyritic dyke, 400 metres south-southwest of the Highway 113 bridge (Figure 3). Auriferous

sulphide-chlorite veinlets extend into the dyke, and gold grades of up to 2.2g/t over 1.0 metre have

been intersected in drill holes (CDR9807). Dykes/sills of very similar composition and textures have

been intersected in holes CDR9822, CDR9932, and CDR9936 and are interpreted to represent strike

extensions of the quartz-feldspar porphyry present at the Dyke Zone (holes CDR9807, CDR9818,

and CDR9934). The quartz-feldspar porphyry in holes CDR9932 and CDR9936 are variably

epidotized, locally carbonatized and cut by vuggy chlorite-calcite(+/- anhydrite)-epidote-quartz

stringers usually rich in pyrite and chalcopyrite. Molybdenite was recognized locally in some stringers

(up to 671 ppm/0.5 m in hole CDR9932). A crescent-shaped massive to fragmented feldspar

porphyritic felsic plug, 600 metres long with two east-southeast trending arms each 100 to 200

metres wide, intrudes mafic flows and polymictic intermediate volcaniclastic rocks on the north shore

of the Bell River, 1.5 kilometres east of the Highway 113 bridge. This porphyry hosts the historic

Zone 1 (Discovery Zone) gold showing where gold grades of up to 13.7g/t over 1.0 metre have been


18

obtained in channel samples from east-southeast striking, strongly foliated, chloritic and pyritic

structures that cut the porphyry body. Feldspar porphyritic dykes, intruding the mineralized mafic

and ultramafic flows, were also intersected in drilling at the Village Zone and gold values up to 0.5g/t

over 6 metres (including 1.4g/t over 1 metre) were obtained from chloritized and epidotized alteration

zones within a feldspar-hornblende porphyritic dyke.

The western third of the Cedar Rapids property is underlain by massive biotite granodiorite that

makes up a portion of a 10 kilometre wide pluton centred in southwest Quévillon Township.

Structural data is confined, almost entirely, by the distribution of outcrop and drill holes, to the area

of the Bell and Quévillon rivers in the central portion of the property. In that area, lithologic contacts

(SO) strike East-southeast and have dips that range from subvertical to 70°N. Two foliations have

been observed in outcrop and drill core. A varuably developed S1 foliation strikes east-southeast and

dips 70° to 85°N, subparallel to lithologic contacts. The dominance of the east-southeast trending

structural grain on the eastern two thirds of the property is supported by a similar trend on total field

ground magnetic maps. Both SO and S1 are rotated in a clockwise fashion in the vicinity of the

Highway 113 bridge to a North-northwest strike, a change that is readily visible on magnetic maps.

A southwest striking, steeply South dipping S2 foliation occurs in the bridge area. It is weakly

developed compared with the more penetrative S1 fabric, and it takes the form of a spaced or

pressure solution cleavage. Its orientation relative to the flexure in the SO and S1 fabrics suggests

that the southwest-trending axis of an open F2 fold may pass approximately 300 metres East of the

bridge. A North striking S1 fabric cuts East-southeast striking lithologic contacts at a high angle on

outcrops on the south shore of the Bell River at the Highway 113 bridge. This relationship suggests

that a F1 fold closure may also occur in that area.

All stratigraphic younging directions recorded in outcrop and drill core, with one exception, are to

the South. The geology of the area is characterized by south facing, steeply north dipping,


19

homoclinal lithologies and that the possible fold hinges described above merely crenulate this

homoclinal panel.

A series of northwest trending brittle-ductile reverse faults appear to have duplicated the mineralized

horizon and the stratigraphy in the bridge area. Higher gold values found in the vicinity of these faults

may indicate that they have played an important role in the emplacement or remobilization of the

mineralization (and alteration) found at the Village Zone and the Dyke Zone.

A later East-West striking, anastomosing network of subvertical, brittle, gouge-filled faults is

observed in drill holes and outcrop in the Highway 113 area. An unfoliated, hematitic, red

sandstone/grit was intersected along the main fault plane during drilling. Locally, the sandstone

intervals appear normally graded indicative of a southwest facing direction, similar to all the other

units. This same sandstone-filled fault was intersected in a drill hole 600 metres east of the bridge.

The "Sandstone fault" appears as an East striking lineament on magnetic maps and is expressed

topographically by a bend in the Bell River towards the East in the Highway 113 bridge area. In holes

CDR9706 and CDR9937, the "Sandstone Fault" appears to become wider at depth and gold

mineralization is located just at the margins of the fault. A similar magnetic and topographic

lineament occurs 900 metres further South, and probably reflects another fault in the same set.

Although the origin of this fault system is not fully understood (nature and age of the sandstone?),

the faults appear to be post-mineralization structures, which have sinistrally offset the stratigraphy

(less than 200 m displacement).


20

3.0 FALL, 1999 CAMECO DIAMOND DRILLING

3.1 Purpose of the 1999 Drilling Program

A total of 2,204.8 metres was drilled in eight holes between September 8 h and October 15 h, 1999.

Three of the eight holes (CDR97-6 extension, CDR99-32 and CDR99-37) were drilled to test strike

and depth extensions of the Village Zone. One hole (CDR99-33) was drilled to test an Enzyme Leach

geochemical anomaly (copper, lead, arsenic and molybdenum) 200 metres northeast of the Village

Zone mineralization, at the interpreted contact between the mafic-ultramafic and felsic volcanics

underlying the Village Zone mineralization. The remaining four holes (CDR99-34, 35, 36 and 38)

were drilled to test the strike and depth extension of the Dyke Zone mineralization.

3.2 Drilling Results

The results of diamond drilling completed by Cameco are discussed below and are summarized in

Tables 2 and 3. The target selection, overall supervision and part of the core logging was provided

by the author and the remaining holes were logged by Jacques Samson of Timmins. Core sampling

was completed by Louis Perron, a geological technician from Rouyn Noranda. The crew stayed at

the Motel du Lac in Lebel sur Quevillon. All drill core is stored at M.D. Entreposage in Lebel-sur-

Quévillon, Québec.

Drill logs for all holes are in Appendix 1, and interpreted drill sections are in Appendix 4. Drill hole

locations are shown on Figure 3. For this report, the terms felsic, intermediate, mafic and ultramafic

are based on field observation criteria. Alternatively, the terms dacite, andesite, basalt and komatiite

are used respectively when lithologic classifications could be refined using whole rock and trace

element geochemistry.

Cameco Corporation Cedar Rapids Project Report on the Fall. 1999 Drilling Program

21

CDR9706 (drilled in 1997; Brisbin, 1998) was extended from 336.0 to 421.6 metres, to test the

upper part of the mineralized mafic volcanic sequence and the prospective contact with the pyritic

chert intersected in holes CDR9701 and CDR983 0. The hole went through a carbonatized and

massive ultramafic unit from 336.0 to 347.7 m. It was followed downhole by a massive to pillowed

mafic flow, weakly mineralized to 356.4 m by 0.1% quartz-calcite-chlorite stringers containing 25

to 50% pyrite and minor chalcopyrite. Below 356.4 m, the weakly carbonatized mafic flow becomes

strongly altered to chlorite and it is cut by about 10% quartz-calcite-chlorite stringers containing of

10 to 80% sulphides. In these stringers, pyrite is found associated with minor pyrrhotite and

magnetite from 356.4 m to 359.6 m, while below 359.6 m, pyrite is associated with 1 to 5%

chalcopyrite (magnetite and pyrrhotite are not seen). From 364.3 to 372.0 m, the hole intersected

a mafic and variolitic breccia/hyaloclastite horizon showing a cherty aphyric matrix. This horizon is

mineralized with 10% pyrite-quartz-calcite-chlorite stringers, containing up to 5% chalcopyrite, from

364.3 to 367.4 m. The breccia/hyaloclastite is followed downhole by a pyritic (1 to 20% vol.) felsic

tuff/chert horizon from 372.0 to 376.0 m, then the hole traversed a series of volcaniclastic sandstones

interbedded with

siliceous mudstones and/or tuffs to the end of the hole. The best assay obtained from this hole was

0.6g/t Au over 0.6 metres from 366.0 to 366.6 metres.

CDR9932 was drilled to 352.2 metres to test the projected strike extension of the Village Zone, 400

metres southeast of hole CDR9830. It required two attempts to reach bedrock. The first attempt

(CDR9932A) was terminated at 57.9 metres, when the casing broke. The hole was then redrilled at

a steeper angle (-55 degrees instead of -45 degrees). The second attempt reached bedrock at 58.3

metres, then traversed a medium grained, epidotized dioritic rock to 80.3 m. Subsequently, a medium

grained gabbroic unit, showing 10 to 20% cumulate-like pyroxene-rich horizons (less than 20 cm

wide), was intersected from 80.3 to 128.8 metres. The gabbro is moderately altered to epidote,

mainly concentrated along fractures. From 128.8 to 317.9 metres, the hole traversed an epidotized

quartz-feldspar porphyry, intruded by an amphibole-feldspar porphyritic dyke from 164.2 to 171.1


22

metres. The porphyritic unit is cut by about 5 to 10% strongly foliated, moderately sericitized and

chloritized deformation zones, between 2 and 60 cm wide. Up to 2% disseminated and fracture-

controlled pyrite is observed in these diffuse zones, while only traces of pyrite are seen in the host

rock. A weakly bleached section located from 179.5 to 180.2 metres contains less than 1%

molybdenum concentrated in three quartz-calcite stringers (671 ppm Mo over 0.7 metres). From

262.5 to 317.9 metres, the moderate epidote alteration is accompanied by weak and pervasive

ankerite. The alteration is accompanied by 1 to 2% disseminated pyrite and traces of chalcopyrite

throughout. In addition, the porphyry contains locally up to 5% pyrite and up to 2% chalcopyrite

associated with a stockwork of vuggy calcite-quartz-epidote (+/- anhydrite and chlorite) fractures.

The most abundant chalcopyrite mineralization (1 to 2%) was observed from 269.8 to 271.15 metres.

This section returned the only assays anomalous in gold (0.1g/t Au and 0.1% Cu over 4.0 m, from

267.5 to 271.5 m). The lower contact of the porphyry is marked by a strongly foliated and chloritic

deformation zone from 317.9 to 318.3 metres, followed by a sequence of volcaniclastic sandstone

and cherty mudstone beds to the end of the hole. The volcaniclastic unit contains 2 to 4% pyrite

disseminated throughout and also concentrated along cherty laminae. Another quartz-feldspar

porphyritic dyke was intersected from 320.4 to 332.5 metres.

CDR9933 was drilled to 276.5 metres to test the prospective contact between the dacitic and the

mafic-ultramafic volcanics, stratigraphically below the Village Zone (to the northeast), coincident

with the best copper anomaly from the 1999 geochemical soil survey (enzyme leach method). The

hole traversed 16.9 metres of overburden followed by a sequence of foliated, thickly bedded crystal

tuff, crystal lapilli-tuff and lapilli-tuff, all dacitic in composition, from 16.9 to 179.7 metres. They are

interbedded with laminated to thinly bedded graphitic argillite horizons encountered from 113.3 to

121.4 m and 147.4 to 179.7 m. From 131.2 to 147.0 m, fine-grained pyrite is partially or totally

replacing some of the dacitic clasts and two massive to semi-massive pyrite horizons were intersected

from 139.50 to 139.55 metres and from 147.0 to 147.4 metres. The dacitic unit was followed

downhole by a foliated and carbonatized tuffaceous horizon, intermediate to ultramafic in

composition, interbedded with siliceous graphitic argillites to 202.6 metres. Thin massive pyrite


23

horizons (5 cm to 30 cm thick) were encountered from 180.7 to 180.7 metres and from 198.1 to

194.4 metres. The rest of the hole intersected a foliated and carbonatized mafic rock to 212.1 m,

followed by a carbonatized ultramafic flow/sill present to the end of the hole. An intense deformation

zone is present at the contact between the two units from 212.1 to 233.4 metres. This major

structure contains about 2% pyrite and the strong foliation within the zone is oriented at less than 20

degrees to core axis. Several quartz only and quartz-feldspar porphyritic dykes/sills intrude the

ultramafic unit below 237.3 metres. One of the quartz porphyritic dykes containing about 5%

disseminated pyrite returned the only gold anomalous assay (0.3g/t Au over 1.4 metres from 274.2

to 275.6 metres).

Since none of the lithologies encountered in this hole were anomalous in copper (>1000 ppm), it is

possible that the copper anomalies obtained from the soil survey in the area might originate from the

Village Zone mineralisation approximately 200 metres to the southwest. Alternatively, the anomalies

might be due to culture (there is an old concrete foundation just 100 metres to the south of the copper

anomalies).

CDR9934 was drilled to 325.2 metres, in order to undercut previous mineralized horizons (Dyke

Zone) intersected by drill holes CDR9807 and CDR9818. The hole went through 50m of overburden

and started coring through a thick volcaniclastic sequence, comprised of pebbly sandstone to

polymictic conglomerate, and minor mudstone beds. In the upper half of the hole, weak to

moderately altered and mineralized zones were intersected between 94.00 to 115.75m, 128.55 to

133.20m, and from 147.00 to 154.50m. One of the zones is accompanied by a weakly altered

intermediate feldspar porphyry dyke located between 133.20 to 135.00m. The alteration zones

generally display weak to moderate epidote-chlorite-calcite±biotite alteration, with pyrite±pyrrhotite

1-3%, 5% locally, accompanied by up to 1% chalcopyrite in places. The sulphides usually occur as

fine disseminations to wisps and stringers infilling micro-fractures, often crosscutting the foliation and

apparent bedding. Two of the alteration zones returned significant assays of 1.3 g/t Au over 2.8 m

(including 6.0 g/t Au/0.5 m) from 129.7 to 132.5 metres and 0.9 g/t Au over 3.4 metres (including

Cameco Corporation Cedar Rapids Project Report on the Fall. 1999 Drilling Program

24

2.0 g/t Au/1.0 m) from 150.0 to 153.4 m. These zones and the associated porphyry dyke appear to

grossly represent the extension at depth (75 to 125m vertical depth) of the "upper zone" previously

intersected at the top of CDR98-18 (aver. 1.5 g/t Au/4.3m, including 4.4 g/t Au over 1.1m).

Another similar sequence of moderately altered volcaniclastic rock was intersected from 212.50 to

258.30m (approx. 190m vertical depth), comprising the hangingwall to a quartz-feldspar porphyry

dyke/sill, intersected from 258.3 to 294.8 metres and also present in drill holes CDR9818 and

CDR9807 ( "Dyke Zone"). The mineralization, consisting of 2-10% pyrite (aver.3%), is located

between 226.7 to 238.5 m, and diverts away from the porphyry contact at depth. The only

significant assay in this altered zone returned 6.4 g/t Au over 1.0 m, from 236.0 to 237.0 metres.

Except for a moderate chlorite and carbonate alteration at the upper contact, from 258.3 to 259.8 m

(pyrite 2%, trace chalcopyrite), the porphyry is relatively unaltered and undeformed. The footwall

to the porphyry consists of a monotonous, barren and unaltered sequence ofpolymictic volcaniclastic

conglomerate intersected to the end of the hole.

CDR9935 was drilled to 279.5 metres to test the projected strike extension of the Dyke Zone, 140

metres to the northwest of holes CDR9807, CDR9818 and CDR9934. After drilling through 38.4m

of overburden, the drill hole essentially remained in a thick sequence of volcaniclastic sediments from

top to bottom, with only occasional dyke intersections. A moderately chloritized and moderate to

strongly carbonatized reworked volcaniclastic sequence was intersected between 38.4 to 81.00m,

including an altered gabbroic dyke located from 41.80 to 47.10m. The zone contains 1 to 3% locally

disseminated to wispy pyrite, accompanied by trace chalcopyrite. A similar but weaker zone of

alteration, weakly epidotized, with less than 1% pyrite was intersected between 96.25 and 156.00m.

This second zone is crosscut by a moderately saussuritized and carbonatized intermediate quartz-

feldspar porphyry dyke, 8m wide, located from 103.2 to 111.2 metres. The main porphyry dyke

which characterized the footwall to the Dyke Zone in previous drill holes (CDR9807, CDR9818 and

CDR9934) further to the southeast was not intersected by CDR9935. Instead, the rest of the hole

intersected relatively unaltered volcaniclastic sandstone, pebbly sandstone and conglomerate, except


25

for a moderately schistose interval, moderately to strongly altered to pervasive sericite and carbonate,

observed from 248.00 to 276.00 metres. This zone also displays weak to moderate patchy

hematization, and is accompanied by two small intermediate porphyry dykelets, less than lm wide.

The only significant assay was obtained from the altered gabbroic dyke, from 44.0 to 44.3 m and

returned 0.6 g/t Au over 0.3 metres.

CDR9936 was drilled to 264.3 metres to test the extension of the Dyke Zone, between holes

CDR9822 and CDR9823, at the intersection with a possible east-west structure inferred from the

ground magnetic survey. Bedrock was intersected at 17.4 metres, followed by a weakly epidotized

and carbonatized, mineralized feldspar porphyritic intrusion to 83.2 metres. The mineralization

consists of less than 1% pyrite and about 0.5% chalcopyrite, concentrated in microfractures. The

feldspar porphyry is very similar in composition and texture to the other porphyritic intrusions

intersected in holes CDR9932, CDR9807, CDR9818 and CDR9934 (Dyke Zone). One significant

assay grading 0.9g/t Au over 0.5 metres was obtained from this dyke from 21.0 to 21.5 m. Other

feldspar porphyritic intrusions, similar in composition, but significatively less mineralized and altered,

were observed from 88.8 to 95.0 m, and 106.5 to 152.3 m. Nevertheless, from 135.5 to 137.0

metres, the feldspar porphyritic intrusion returned 1.0 g/t Au over 1.0 metre. The dykes/sills are

intruding a volcaniclastic sandstone sequence, which is weakly to moderately silicified and

carbonatized from 83.2 to 88.8 m. Below 152.3 metres to the end of the hole, the drill hole

intersected a sequence ofpolymictic volcaniclastic conglomerates interbedded with about 20% pebbly

volcaniclastic sandstone beds. From 152.3 to 182.2 m, the volcaniclastic sequence was moderately

carbonatized and 2 to 3% pyrite with traces of chalcopyrite were found locally. Weighted average

of the assays from 152.3 to 156.5 metres returned 0.6 g/t Au over 4.2 metres (including 1.1 g/t

Au/l.1 m).

Hole CDR9937 required two attempts to collar into bedrock. The first attempt (CDR9937-A) was

drilled at an inclination of 45 degrees (azimuth of 050) and was stopped at a depth of 67.1 metres,

without reaching bedrock. The hole location was subsequently moved 10 metres to the southwest


26

(12+90 E, 8+10 N, Rotated grid) and the second attempt at an inclination of 50 degrees (azimuth

050) reached bedrock at 47.5 metres downhole. The geological summary is presented in table I. This

hole intersected the best mineralized interval of the 1999 drill program and returned 2.0 g/t Au over

31.4 metres of core length (including 13.9 g/t Au/0.3 m), which corresponds to about 18 m true

width measure from the drill section at about 300 metres vertical depth. The mineralization consists

of a series of chalcopyrite-pyrite-quartz-calcite stringers located generally between strongly

chloritized pillow selvages within a succession of variolitic mafic flows, moderately to strongly

carbonatized and biotitized. Two specks of visible gold were seen in one of the stringers at 386.2

m.

Hole CDR9938 (14+18 E, 23+30 S) was abandoned at 92.0 m when the casing jammed before

reaching bedrock. No other attempts were made.


Table L• CDR9937 SUMMARY LOG

From To Lithologies

Comments

(m) (m)

52.6-71.4 m: Epidotized section with 5% epidote-silica patches up to 10 cm in diameter.

133.5-146.3 m: Moderately to strongly carbonatized deformation zone.

197.2-222.5 m: Moderately to strongly foliated interval (deformation zone?), mineralized with <1% pyrite and chalcopyrite concentrated in quartz-carbonate-chlorite stringers, 2 mm to 2 cm thick and oriented sub-parallel to core axis.

Strongly foliated interval made of alternating sericitized and chloritized laminae.

297.2-302.0 m: Pyrrhotite and pyrite concentrated along chloritic laminae

302.0-302.5 m: 15 to 20% massive to semi-massive pyrrhotite laminae with 1% pyrite and chalcopyrite.

Moderately to strongly chloritized and moderately carbonatized. <5% pyrite and <0.5% chalcopyrite concentrated in quartz-calcite-chlorite stringers.

1 to 2% pyrite and trace chalcopyrite concentrated in quartz-calcite-chlorite stringers.

Trace pyrite and chalcopyrite concentrated in rare quartz-calcite-chlorite stringers.

Bounded by blocky brittle fault.

359.0-365.6 m: Mineralized section containing 1% chalcopyrite and <0.5% pyrite concentrated in quartz-carbonate stringers with chloritic alteration halo.

Weakly carbonatized and epidotized throughout, strongly chloritized along pillow selvages. 2 to 3% chalcopyrite and pyrite concentrated in quartz-carbonate stringers (< 6 cm thick), located between pillow selvages.

2 to 3% pyrite, 1% chalcopyrite concentrated in stringers as above. Two specks of Visible gold were seen in one of the stringers at 386.2 m.

387.6-388.3 m: Sandstone-filled fault.

1 to 2% pyrite and up to 0.5% chalcopyrite concentrated in talc-carbonate stringers.

395.5-399.3 m: Sandstone-filled fault zone.

OVERBURDEN

INTERMEDIATE VOLCANICLASTIC ROCK

PYRIl'h AND PYRRHOTITE-RICH INTERMEDIATE TO FELSIC TUFF/MUDSTONE

MINERALIZED, ALTERED AND PILLOWED MAFIC FLOW

MASSIVE MAFIC FLOW/SILL

CARBONATIZED AND BIOTITIC MASSIVE MAFIC ROCK

MASSIVE ULTRAMAFIC TO MAFIC FLOW/SILL

CARBONATIZED AND BIOTITIC MASSIVE MAFIC ROCK

MINERALIZED AND VARIOLITIC PILLOWED MAFIC FLOW

MINERALIZED, CARBONATIZED, BIOTITIC, PILLOWED AND VARIOLITIC MAFIC FLOW.

TALCOSE AND CHLORITIC MASSIVE ULTRAMAFIC ROCK

0 47.5

47.5 276

276 303

303 322

322 327

327 337

337 356

356 366

366 378

378 390

390 405

27

Cameco Corporation



N N N N NN N N N,J,..N N N N N N N N N N N N N N N N N N N N

7

N N N N

I •

4 4,45 -08

Scale: 1:10,000 PITS R. 32F/03

Osa. Ref.: NAD 27 - UN Zona 18 Source:

Legend

NNNN

CDR98-23 1.1g/t Au/0.3m 1.4g/t Au/0.5m

u n, N

r~ti~NNNN~a

CDR99-37A

CDR99-37 13.9 t Au/0.3m 2.0 Au/31.4m

2.3g/t Au/0.2m 2.6g/t Au/0.7m

R99-35

24.3g/t Au/ .0m

CDR99-06X

O CD

CDR974,,.

3.4g/t Au/2.0m

CDR98-22 - - \I 1 B

6.4g/t A 1.3g/t A

•L 1, :L__

V3 CDR98-

'8 30 u/1.0m

Au/1.0m

V1,S1OD

T,NNNNNNNn ~ 6.0: • u/1.0m

g/t A 5m 3.5g/t Au/O.

/ \ _~.. /

1.7g/t Au/3.9m 2.2g/t Au/2.7m 0.7g/~ An/12.7m

CDR99-33 II / /

• n, N N n, N N N N N N

1. z

9-32, 3'

Nn„

R98-10

V1,FT,TU,S3,S6 ~NNNnnnnnnnnNNnn

~n,Nnv NNN NNN N

to

N-41a_N

N N N n.W n, ^a.12! ti =~ M 1. N N. n,1R n, 1,

CDR98-11

V1,F'T \~

s

N ,V N N N N N N N N N N N N N

CDR98-12 V3,V4

.~ ----- -~----~ z t

0 100 200 ~

3401-1

400 500 m 1 1 3 I 1

Scale 1:10000 1,,P ti

Cedar Rapids Project GEOLOGY, DRILL HOLES

AND SIGNIFICANT ASSAYS Cameco Complied: Dominic Bobin

Drafted: C. Durbin, C Halchuk Dwg. No.: CDR99_10000

Dots: 99/12/14 Figure 3

V1,S1OD

CDR98-18

-

I1B FT V1 V2 V3 V4 S

S10

Felsic Intrusive Rocks Felsic Tuff Felsic Volcanic Rocks Intermediate Volcaniclastic Rocks Mafic Volcanic Rocks Ultramafic Volcanic Rocks Sedimentary Rocks Iron Formation

Old Drill Holes

~COR98-18 Previous Cameco Drill Hole

~R99-33 Fall 1999 Cameco Drill Hole

- N N N- Geological Contact Fault Transmission Une Highway North

-L

a

zt

\`

V2 VS .~

29

TABLE H: 1999 CEDAR RAPIDS PROJECT DRILL HOLES

DDH Claim No. Northing* Easting* Azimuth Dip Length (m) Casing (m)

CDR9706 5126394 -11+15 9+20 215 -45 85.6**

CDR9932 5126361 -15+35 13+20 230 -55 352.2 58.3

CDR9932A 5126361 -15+35 13+20 230 -45 57.9 57.9

CDR9933 5126394 4+65R 12+97R 230 -50 276.5 16.9

CDR9934 5126360 8+75R 16+00R 229 -55 325.2 50.0

CDR9935 5126359 7+90R 14+00R 229 -55 279.5 38.4

CDR9936 5126334 7+58R 18+14R 230 -55 264.3 17.4

CDR9937 5126359 8+10R 12+90R 050 -50 404.5 47.5

CDR9937A 5126359 8+00R 12+90R 050 -45 67.1 67.1

CDR9938 5126337 -23+30 14+18 230 -50 92.0 92.0

Total: 2204.8 445.5

* "R" denotes collar co-ordinates on the rotated grid on which grid north is azimuth 050.

** Extension of hole CDR9706 from 336.0 metres to 421.6 metres.


30

TABLE III CEDAR RAPIDS PROJECT, 1999 DRILL PROGRAM, SUMMARY OF

SIGNIFICANT ASSAYS (Au > 0.5 g/t)

DDH Length (m) Interval (m) Width (m) Au Grade (g/t) Weighted Average

CDR9706 222.0-336.0 312.0-313.1 1.1 0.4 0.7 g/t Au /12.7 m

(Infill 313.1-313.5 0.4 3.8*

Sampling) 313.5-315.0 1.5 0.1*

315.0-315.5 0.5 0.7*

315.5-317.0 1.5 0.5*

317.0-318.0 1.0 2.4*

318.0-319.5 1.5 0.6

319.5-321.0 1.5 0.1

321.0-322.5 1.5 0.5

322.5-323.5 1.0 0.2

323.5-324.5 1.0 1.0

324.5-324.7 0.2 2.4*

CDR9906 85.6 366.0-366.6 0.6 0.6 0.6 g/t Au /0.6 m

(Extension) (421.6 total)

CDR9932 352.2 No significant values

CDR9933 276.5 No significant values

CDR9934 325.2 129.7-130.2 0.5 6.0 1.3 g/t Au /2.8 m

130.2-131.2 1.0 0.1

131.2-132.0 0.8 0.2

132.0-132.5 0.5 1.3

150.0-151.0 1.0 0.4 0.9 g/t Au/3.4m

151.0-152.0 1.0 2.0

152.0-153.4 1.4 0.5

236.0-237.0 1.0 6.4 6.4 g/t Au /1.0 m

Carneco Corporation



31




CDR9935 279.5 44.0-44.3 0.3 0.6 0.6 g/t Au /0.3 m

CDR9936 264.3 21.0-21.5 0.5 0.9 0.9 g/t Au /0.5 m

135.5-137.0 1.5 1.0 1.0 g/t Au /1.5 m

152.3-153.2 0.9 0.3 0.6 g/t Au /4.2 m

153.2-154.3 1.1 1.0

154.3-155.3 1.0 0.1

155.3-156.5 1.2 1.1

CDR9937 404.5 212.6-214.1 1.5 1.0 1.0 g/t Au /1.5 m

219.5-220.5 1.0 0.3 1.7g/t Au /2.1 m

220.5-221.6 1.1 3.0

359.0-360.7 1.7 3.1 2.0 g/t Au /31.4 m

360.7-361.3 0.6 1.1 (18 m true width)

361.3-361.9 0.6 0.4

361.9-362.6 0.7 3.4

362.6-363.2 0.6 1.5

363.2-364.2 1.0 1.9

364.2-364.7 0.5 1.9

364.7-365.6 0.9 3.6

365.6-366.4 0.8 0.9

366.4-367.0 0.6 6.2

367.0-368.0 1.0 1.2

368.0-369.0 1,0 2.1

Cameco Corporation



32




369.0-369.7 0.7 2.3

369.7-370.7 1.0 3.7

370.7-371.7 1.0 0.6

371.7-372.7 1.0 5.7

3.72.7-373.7 1.0 1.3

373.7-374.3 0.6 3.9

374.3-375.8 1.5 0.7

375.8-376.8 1.0 1.3

376.8-377.3 0.5 1.0

377.3-378.2 0.9 6.1

378.2-379.3 1.1 2.8

379.3-380.3 1.0 3.0

380.3-381.3 1.0 1.0

381.3-382.3 1.0 0.3

382.3-383.0 0.7 0.1

383.0-383.3 0.3 1.6

383.3-384.3 1.0 0.1

384.3-385.3 1.0 0.3

385.3-386.0 0.7 0.3

386.0-386.3 0.3 13.9**

386.3-387.6 1.3 0.6

387.6-388.3 0.7 0.2

388.3-389.3 1.0 0.2

389.3-390.4 1.1 3.0

* Sample collected and analyzed during the 1997 drilling campaign. Lab results reported in ppb have been

converted to g/t and rounded to one decimal place. No significant values (ie. no values >0.5 g/t).

** Assay obtained using the weighted average between Pulp Metallic and regular fire assays.


33

3.3 Lithogeochemistry

Geochemical analyses for gold and 34 additional elements were performed on a total of 769 sawed

core samples from the 1999 drilling program. Sixty infill samples (analysed for gold only) were taken

from hole CDR9706 (97 drilling program), between 222.0 and 336.0 metres. In addition, three infill

samples were taken from hole CDR9930 (1998 drilling program), from 42.3 to 46.3 metres, and

analysed for gold and 34 other elements. One hundred and twenty-nine of the total samples,

representing 15.5% of the population, returned gold values of at least 100ppb. Gold was analyzed

by FA-AA on 30g samples. The remaining elements were analyzed by ICP following an aqua regia

digestion. For all initial assays which returned 2.0 g/t Au or more, another cut of the reject was taken

and analysed for gold by FA-Gravimetric on 30g samples. In hole CDR9937, a suite of 34 sample

rejects from the mineralized zone between 359.0 and 390.4 metres were also re-analysed for gold

by FA-Gravimetric method, regardless if the initial assay was higher than 2.0 g/t Au. Sample

CDR9937-1996 taken from the mineralized zone (from 386.0 to 386.3 m), contained visible gold and

was first analysed by FA-AA on a 30g sample. The remaining of the sample (pulp+reject) was re-

analysed by FA-Gravimetric following a metallic screening preparation method (150 mesh). The

average assay value for this sample, reported in Table III and Annexe I, corresponds to the weighted

average between the two assays.

Whole rock analyses were completed on 38 samples. Each sample was typically composed of three

to five pieces of whole core, each 5 to 10 centimetres long, collected over a 3 metre long interval.

In cases where the lithologic or alteration unit being sampled was less than 1 metre long only one or

two core samples were collected. Veins, sulphides and other heterogeneities were excluded from

samples whenever possible, except for the samples taken to characterize the alteration (As noted at

the end of each log in Appendix 1). Major oxides, Ba, Cr and Sr were analysed by borate fusion-ICP.

Y and Zr were analysed by pressed pellet-XRF. A statistical evaluation of the whole rock data has

not been undertaken, but all analyses were examined and used to refine lithologic classifications made

in the field.


34

All analytical work was done by Intertek Testing Services (Chimitec) of Val d'Or. Sample rejects

and sample pulps are stored temporarily there. Gold, silver, copper, lead, zinc, molybdenum and

arsenic analyses from the multi-element data are recorded in the drill logs in Appendix 1. Gold

analyses of the reject (in g/t) and the average value between the initial assay and the re-assay (in g/t)

are reported for holes.CDR9934 and CDR9937. Complete analytical reports for all multi-element

data are in Appendix 2, and complete analytical reports for all whole rock samples are in Appendix

3.


35

4.0 DISCUSSIONS AND CONCLUSIONS

Hole CDR9937 intersected the best mineralized interval of the 1999 drill program and the widest

mineralized interval showing significant gold assays on the property (2.0 g/t Au and 0.15% Cu over

31.4 m or about 18 m-true width). All assays within the mineralized zone were anomalous in gold

(>100 ppb) and two third of the assays were equal or higher than 1.0 g/t Au. The mineralization

consists ofa series of chalcopyrite-pyrite-quartz-calcite-magnetite stringers located generally between

strongly chloritized fractures or pillow selvages within a succession of variolitic mafic flows,

moderately to strongly epidotized, carbonatized and biotitic. Visible gold was observed for the first

time on the property in one of the chalcopyrite-pyrite-quartz-calcite stringer and returned 13.9 g/t Au

over 0.3 metres. This type of mineralization is very similar to the other mineralized intervals

intersected in previous drill programs at the Village and Dyke Zones. The stratigraphic and

structural relationships suggest that this stringer zone is most likely linked to the other mineralized

zones intersected in holes CDR9701, CDR9702, CDR9706 and CCDR9830, which together could

represent a large feeder system to an economic gold-rich massive sulphide deposit. Available historic

data and results from this program indicates that gold grades are increasing to depth and that the

system is open along strike and at depth. It should be considered as the highest priority target for

future drilling programs.

The mineralized zone intersected in hole CDR9937 is bounded to the northeast by a red, hematitic,

sandstone-filled sinistral fault. This fault was also intersected in holes CDR9701, CDR9702,

CDR9706, CDR9810 and CDR9831. The width of the fault appears to increase with depth (similarly

to the mineralization?). Although the fault is interpreted to postdate the mineralization, it is possible

that it may have played an important role by remobilising the early mineralization and/or by displacing

part of the stringer zone (there could be up to 200 metres horizontal displacement).

The extension of hole CDR9706 intersected variably mineralized and altered variolitic mafic flows

and breccias at the contact with the pyritic cherty tuffs/mudstones. The best assay was 0.6 g/t Au


36

over 0.6 metres. Similarly to hole CDR9930, the mafic breccia in contact with the pyritic cherty

tuffs/mudstones showed evidence ofhydrothermal activity interpreted from the presence of aphanitic

silica-sericite infilling the fractures and spaces between the mafic fragments. This contact could be

prospective for the presence of an economic massive sulphide deposit along strike or at depth.

Hole CDR9932 failed to intersect the projected strike extension of the Village Zone. Instead, it

drilled through 189.1 metres of feldspar-quartz porphyry, very similar in texture and composition to

the one observed in holes CDR9807, CDR9818 and CDR9822. Similar porphyries were also

intersected in holes CDR9934 and CDR9936 and are interpreted to be part of the same intrusive

facies. Hole CDR9935 did not intersect the projected strike extension of the main porphyritic

intrusion, but few minor porphyritic dykelets were observed.

The porphyries in holes CDR9932 and CDR9936 were variably epidotized, locally carbonatized, and

cut by vuggy chlorite-calcite (+/- anhydrite)-epidote-quartz stringers containing variable percentages

of pyrite and chalcopyrite. Molybdenite was recognized in few of these stringers (highest assay was

671 ppm Mo/0.7 m). These observations suggest that an intrusion related alteration and

mineralization system could have affected part of the stratigraphy in the area between the Village

Zone and the Dyke Zone, in addition to the interpreted hydrothermal volcanogenic mineralization

found at the Village Zone (Mouska-Bousquet type of setting). However, the locally strong presence

of epidote (i.e. in matrix, veins, joint, planes, plagioclase overgrowths), presence of calcite (+/-

anhydrite) veinlets with chlorite alteration haloes and absence of significant quartz veins may suggest

that the intersected intrusive intervals are relatively removed from an area of strong alteration and

mineralization.

Hole CDR9933 intersected variably pyritized dacitic volcaniclastics and wide sections of

argillaceous/graphitic sediments with pyrite, in contact with ultramafic flows/sills of the Village Zone

stratigraphy. Best gold assay was 0.3 g/t Au over 1.4 metres within the ultramafic flow/sill sequence.

The copper anomaly from the soil survey was not explained and could originate from the Village


37

Zone mineralization 200 metres to the southwest or from cultural contamination (old concrete

foundation in the area). No further work is recommended along this contact zone.

The intermediate volcaniclastic sequence (mudstones, siltstones, sandstones and conglomerates)

hosting the Dyke Zone mineralization was intersected in all holes, except CCDR9933. Hole

CDR9934 undercut the Dyke Zone mineralization (hole CDR9807 and CDR9818) by about 100

metres. In the upper half of the hole, weakly to moderately altered and mineralized zones intruded

by a small porphyritic dykelet were intersected and returned significant assays of 1.3 g/t Au over 2.8

metres (including 6.0 g/t Au/0.5m) and 0.9 g/t Au over 3.4 metres (including 2.0 g/t Au/1.0m).

These zones appear to grossly represent the extension at depth of the upper mineralized zone

intersected in hole CDR9818 (0.7 g/t Au/4.3 m). A similar altered and mineralized sequence was

intersected downhole, at the contact of a 35 metre-wide feldspar-quartz porphyry, representing the

depth extension of the Dyke Zone (24.3 g/t Au/1.1 m in CDR9807 and 3.4 g/t Au/2.0 m in

CDR9818). The only significant assay obtained from this 11.8 metre wide mineralized alteration zone

was 6.4 g/t Au over 1.0 metre. Gold is associated with pyrite-chalcopyrite-chlorite-carbonate

stringers. The surrounding volcaniclastic sequence is usually moderately to strongly chloritized and

biotitic near the stringer zone and it becomes more epidotized (patchy) and less chloritic-biotitic

away from the mineralization. Stringers tend to be richer in chalcopyrite and gold near the centre of

the alteration zones and away from the centre, they usually become richer in pyrite with little

chalcopyrite. Other similar mineralized alteration zones were intersected in holes CDR9935,

CDR9936 and CDR9937 of the 1999 drill program, and holes CDR9922 and CDR9923 of the 1998

drill program. Best assays in these zones were 1.0 g/t Au over 1.5 metres in hole CDR9936 and 1.4

g/t Au over 0.5 metres in hole CDR9923. The work completed so far suggest that at least three or

more sub-parallel mineralized alteration zones crosscut the volcaniclastic stratigraphy, but more work

(petrography, geochemistry and more drilling) is needed to identify the orientation and the true nature

of these zones or pipes. Similarly to the Village Zone mineralization, gold values and intensity of the

alteration in these zones appear to increase with depth. The mineralized system is still open along


38

strike and at depth, although it should represents a lower priority target than the Village Zone

mineralization.

Hole CDR9938 did not reach bedrock because of ground conditions and no other attempts were

made. The overburden is very deep in the area and it is composed of large boulders in a sandy matrix.

It should be considered as a low priority exploration sector, although there is no geological data

available for the area.


39

5.0 RECOMMENDATIONS

Following the 1999 drill program, the following recommendations are outlined to further investigate

the mineralization intersected in hole CDR9937;

1. Available lithogeochemical data from outcrop and drill core samples should be compiled and

analysed to characterize and define the epidote-chlorite-carbonate alteration associated with the

mineralized zones, also to ensure that no other significant alteration zones have gone unrecognized.

2. A detailed compilation of the area comprising the Village Zone and the Dyke Zone using G.I. S

should be carried out, including all geochemical, lithological and structural data collected by CGI and

by previous operators. The area is geologically complex and a complete compilation is necessary

before planning the next drill program.

3. A selected number of mineralized samples (10 to 15) should be sent for petrographic studies to

help better understand what controls the gold mineralization and the alteration. A sample of the red

sandstone filling the "Sandstone Fault" should also be sent to help identify the true nature of this

sandstone.

4. Consideration should be given to carrying out a borehole T.E.M. survey in CDR9937 to search

for a gold-rich massive sulfide target at depth or along strike in the Village Zone. Optimal positioning

of the transmitter loop may be difficult because of the Bell River.

5. Pending the results of the borehole T.E.M survery, a minimum 1000 metre drill program should

be planned to test the strike and depth extension of the Au-Cu stringer mineralization intersected in

holes CDR9937 and CDR9706. All drill holes should be planned to test the complete Village Zone

stratigraphy (hosting Au-Cu stringer mineralization) and the contact zone between the mafic volcanics

and the overlying pyritic cherty tuffs/mudstones, which are both prospective to host an economic


40

gold-rich massive sulphide deposit. The lack of airborne E.M. anomaly in the area suggests that a

conceivable conductive massive sulphide deposit would be located below 200 metres vertical depth.

If possible (cultural interference), borehole T.E.M. surveys should be subsequently carried out in all

new holes.


41

6.0 REFERENCES

Auger, P.E., Longley, W. W., 1939, Région de la Rivière Laflamme Inférieure, Territoire d'Abitibi,

part 2, Ministère des Mines, Rapport Géologique 2.

Babin, D., Brisbin, D.I., 1999, Cameco Corporation, Report on the Fall 1998 Drilling Program,

Cedar Rapids Project, Quévillon, Laas and Tonnancourt Townships, Quebec, NTS 32C/14,

32F/02 and 32F/03, Marsh, 1999.

Brisbin, D.I., 1998, Cameco Corporation, Report on the 1997-98 Drilling Program, Cedar Rapids

Project, Quévillon, Laas and Tonnancourt Townships, Quebec, NTS 32C/14, 32F/02 and

32F/03, October, 1998.

Faber, A., Boiridi, M., Valade, J., Brisbin, D., and Burga, D., 1998, Cameco Corporation, Report

on the 1997 Field Exploration Program, Cedar Rapids Project, Quévillon, Laas and

Tonnancourt Townships, Quebec, NTS32C14, 32F/02, 32F/03.

Lavoie, C., 1998, Induced Polarization Survey For Cameco Gold Inc., Cedar Rapid Project, Laas &

Quévillon Twps, July, 1998.

Lavoie, C., 1997a, Magnetic Survey Performed on a Property of Cameco Gold Inc., Cedar Rapids

Project, Quévillon, Laas & Tonnancourt Townships, September, 1997.

Lavoie, C., 1997b, Horizontal Loop Electromagnetic Survey Performed on a Property of Cameco

Gold Inc., Cedar Rapids Project, Quévillon Township, November, 1997.

Longley, W. W., 1938, Advance Report on the Laas-Frase Map Area, part 2, Department of Mines

and Fisheries, PR-122.


42

Ministère de l'Energie et des ressources, Quebec, 1981, Gites des Minéraux de Québec, Région de

l'Abitibi, Feuille Lac Waswanipi (32F, M-306), and Feuille Sennette (32C, M-309).

Ministère de l'Energie et des ressources, Quebec, 1981, Levé EM par INPUT MK VI: Région

Comtois-Cavelier,

Plante, L., 1998a, Geophysical Surveys - IP & Mag for Cameco Gold Inc., Cedar Rapids Project,

Laas, Quévillon & Tonnancourt Twps., April, 1998.

Plante, L., 1998b, Induced Polarization Survey for Cameco Gold Inc., Cedar Rapids Project,

Quévillon Twp, QC, November, 1998.


CERTIFICATE OF QUALIFICATIONS

I, Dominic Babin, residing at 5 Cypress St., Sudbury, Ontario, P3C 4G2, do hereby certify that:

I am currently employed as a Geologist by Cameco Gold Inc., 1349 Kelly Lake Road,

Unit #6, Sudbury, Ontario, P3E 5P5;

I attended l'Université du Québec à Chicoutimi, Quebec and graduated with a B. Ing.,

(Geological engineering) in 1995;

Since June, 1995, I have worked continuously as a geologist in exploration and

postgraduate research;

I was on the property when the work was being carried out, and personally supervised

the exploration activities.

Signed at Sudbury, Ontario, this 31th day of March, 1999

Dominic Babin

Geologist


CERTIFICATE OF QUALIFICATIONS

I, Jacques Samson of 806 Denise Street, Timmins, Ontario, do hereby certify that:

1) I hold a Bachelor of Science (Honours) Degree in Geology (1986) from the University of Ottawa, Ottawa, Ontario.

2) I have been practising my profession in Ontario and Quebec since 1986.

3) I have worked for Newmont Exploration of Canada Ltd., Homestake Canada Inc., Major General Resources Ltd., and am presently employed by Cameco Gold Inc.

4) I do not have directly or indirectly, nor do I expect to receive, any interest in the subject property.

Dated this 14th day of December 1999, at Sudbury, Ontario

Jacques Samson, B.Sc.H. (Geology), Geologist III

APPENDIX 1

DIAMOND DRILL HOLE LOGS


Cameco Gold Inc.

PROPERTY: Cedar Rapids HOLE No.: CDR97-6

Collar Eastings: 920.00 Collar Northings: -1115.00 Collar Elevation: 290.00 Grid: rotated south Benoit Drilling

DIAMOND DRILL LOG

Collar Inclination: -45.00 Grid Bearing: 215.00 Final Depth: 421.60 metres Claim#: 5126394/5126360 Test Village Zone down dip of CDR97-02

Logged by: Dan Brisbin Date: 11/29/97-12/02/97

Down-hole Survey: Acid Test Core size: NQ

ASSAYS FROM TO

LITHOLOGICAL DESCRIPTION

0.0 7.0

OVERBURDEN

7.0

152.8 MASSIVE ULTRAMAFIC ROCKS

Medium grey to greenish-grey, fine grained, massive,

featureless, hard, nonmagnetic. 3% greyish-white

carbonate (very weak fizz) veinlets 0.3mm to lcm wide. Most of these are subparallel to a weak foliation at 401 to

core axis. Speckled with 5 to 20% grey carbonate grains

0.5 to lmm across. 0.5 to 2% subhedral pyrite in carbonate

veinlets and disseminated in host rocks.

7.0 - 23.0m: Locally silicified and intruded by felsic dykes.

Some dyke contacts are sharp. Others are gradational and it

is hard to discriminate dyke from silicified country rock. 0.5% white quartz veins 0.5 to 4cn wide at 201 to 501 to

core axis.

7.0 - 7.9m: Ultramafic with 1 to 2% pyrite. Patchy

silicification from 7.8 to 7.9m. Lower contact sharp at 251

to core axis.

7.9 - 9.2m: Felsic Dyke. Light grey, very fine grained,

massive, featureless. 1% disseminated pyrite, mostly

within 20cm of upper contact.

SAMPLE No. FROM TO WIDTH Au (ppb) Ag (ppm) Cu (ppm) Pb (ppm) Zn (ppm) As (ppm) Ba (ppm)

1 7.00 7.90 0.90 40 TRACE 260 3 57 TRACE 4

2 7.90 9.20 1.30 32 TRACE 57 4 28 TRACE 42

3 9.20 10.20 1.00 55 TRACE 33 2 31 TRACE 29

4 10.20 11.50 1.30 52 TRACE 36 2 33 TRACE 27

5 11.50 12.50 1.00 TRACE TRACE 113 3 18 TRACE 20 6 17.50 18.50 1.00 TRACE TRACE 26 TRACE 33 TRACE 6 7 18.50 19.50 1.00 76 TRACE 89 TRACE 30 TRACE 9 8 19.50 20.50 1.00 21 TRACE 288 3 39 TRACE 8

9 20.50 21.40 0.90 47 TRACE 142 4 38 TRACE 10

10 21.40 22.60 1.20 6 TRACE 50 TRACE 27 TRACE 33 11 22.60 23.00 0.40 TRACE TRACE 153 2 43 TRACE 12 12 35.50 37.00 1.50 55 TRACE 18 2 31 TRACE 33 13 37.00 38.50 1.50 7 TRACE 182 3 43 TRACE 4

14 38.50 40.00 1.50 TRACE TRACE 16 3 13 TRACE 85

15 40.00 41.00 1.00 TRACE TRACE 32 TRACE B TRACE 28

16 41.00 41.90 0.90 17 TRACE 113 2 9 TRACE 27 17 41.90 43.50 1.60 32 TRACE 147 TRACE 47 TRACE 10 18 43.50 43.90 0.40 7 TRACE 77 TRACE 42 TRACE 30 19 54.60 56.10 1.50 54 TRACE 76 TRACE 44 TRACE 15 20 56.10 57.10 1.00 TRACE TRACE 51 TRACE 43 TRACE 7 21 59.80 60.30 0.50 61 TRACE 416 5 36 TRACE 5

22 72.20 73.70 1.50 26 TRACE 241 14 56 6 7

23 101.80 103.30 1.50 19 TRACE 176 6 53 TRACE 4

No: CDR97-6

Cameco Gold Inc.

DIAMOND DRILL LOG PROPERTY: Cedar Rapids HOLE No.: CDR97-6 Page 2

ASSAYS FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM TO WIDTH Au (ppb) Ag (ppm) Cu (ppm) Pb (ppm) Zn (ppm) As (ppm) Ba (ppm)

24 110.40 111.00 0.60 13 TRACE 36 3 42 TRACE 76 9.2 - 11.5m: Ultramafic interval. Light to medium grey due to pervasive but patchy carbonatization and silicification. 0.5% disseminated and fracture-hosted pyrite. Lower contact sharp at 401 to core axis.

11.5 - 12.5m: Felsic Dyke. Light grey, massive, featureless, very fine grained, weakly foliated with 0.5% disseminated pyrite. Lower contact sharp at 551 to core axis.

12.5 - 17.0m: Ultramafic interval. Relatively unaltered.

17.0 - 20.5m: Ultramafic interval. Patchy buff alteration in bands <2cm mostly subparallel to foliation (silicification and carbonatization) has affected 60%. 3 to 5% white quartz veins. 0.5 to 2% pyrite, mostly in buff carbonate- silica alteration features but also in host rocks. Lower contact sharp at 301 to core axis.

19.8 - 20.4m: Fault? Badly broken.

20.5 - 21.4m: Felsic Dyke. 2% disseminated pyrite.

21.4 - 22.6m: Ultramafic interval. Weak pervasive bleaching. 1 to 2% disseminated pyrite.

22.6 - 23.0m: Felsic Dyke. Massive, very fine grained, featureless. Pink-grey, probably due to weak pervasive hematization. 1% disseminated pyrite. Lower contact

No: CDR97-6

Cameco Gold Inc.

DIAMOND DRILL LOG

PROPERTY: Cedar Rapids HOLE No.: CDR97-6 Page 3

ASSAYS

FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM TO WIDTH Au (ppb) Ag (ppm) Cu (ppm) Pb (ppm) Zn (ppm) As (ppm) Ba (ppm)

broken.

38.5 - 41.9m: Felsic Dyke. White, massive, featureless,

very fine grained, weakly sericitic and weakly foliated at 451 to core axis. Blocky and broken, particularly from 38.7

to 39.7m where 5% light green sericite veinlets 1 to 2mm

wide, and 10% grey to white quartz veins 1 to 2cm wide

are at 201 to core axis. 2 to 3% disseminated pyrite

<0.5mm. 5% irregular black chlorite-filled fractures from

39.6 to 39.7m. Both contacts broken.

41.9 - 43.5m: Ultramafic with 2% pyrite and 5 to 10%

quartz-carbonate veins.

43.5 - 43.9m: Fault. Broken and ground core with gouge.

Grey-white irregular carbonate veining and 3% pyrite in

lowermost 10cm.

43.9 - 54.6m: 1 to 2% pyrite, both disseminated and in

quartz-carbonate veinlets.

54.6 - 57.1m: 3 to 5% pyrite, mostly in quartz-carbonate

veinlets.

59.8 - 60.3m: 3 to 5% pyrite and 5% white quartz-calcite

veins, both aligned at 301 to core axis in a weakly to

moderately chloritic interval. 62.2 - 152.8m: Typical medium grey, massive, featureless,

fine grained, moderately carbonatized ultramafic rock.

Green-grey core uphole of this interval could be mafic, but

No: CDR97-6

Cameco Gold Inc.


ASSAYS FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM TO WIDTH Au (ppb) Ag (ppm) Cu (ppm) Pb (ppm) Zn (ppm) As (ppm) Bs (ppm)

downhole of 62.2 metres the rock is definitely ultramafic. 5 to 10% irregular, greyish-white carbonate veinlets <2cm wide at 101 to 401 to core axis. Moderately hard. Nonmagnetic. Weakly foliated at 301 to 401 to core axis. <0.5% disseminated pyrite.

65.2 - 65.7m: Fault. Broken and blocky, black chloritic interval.

72.2 - 73.7m, 1 to 2% pyrite in grey carbonate veinlets. Weak patchy buff sericite alteration.

101.8 - 103.3m: 1 to 2% pyrite in carbonate veinlets.

110.5 - 110.7m: Banded white and grey quartz-carbonate vein with 3% 0.3mm pyrite grains. Banding is parallel vain contacts at 301 to core axis. Vein occurs in a broken and blocky core interval from 110.4 to 111.Om.

143.9 - 150.4m: Increase in white quartz-carbonate veining to 10 to 15%. Veins are up to 10cm wide, parallel foliation at 301 to core axis. Both veins and foliation are locally folded with fold axes nearly perpendicular to core axis (e.g. 149.3m)

144.5 - 145.6m: Fault. Soft, punky core with green gouge/breccia sections comprising 60%. Foliation at 401 to core axis.

Lower contact broken.

No: CDR97-6

Cameco Gold Inc.

DIAMOND DRILL LOG


FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM TO WIDTH Au (ppb) ASSAYS

Ag (ppm) Cu (ppm) Pb (ppm) Zn (ppm) As (ppm) Ba (ppm)

152.8 216.6 MASSIVE MAFIC VOLCANIC ROCKS 25 152.80 153.60 0.80 17 TRACE 35 4 52 TRACE 3 26 153.60 154.40 0.80 584 0.4 998 9 50 19 7

Medium green, massive, very fine grained, chloritic 27 154.40 155,90 1.50 78 TRACE 71 3 42 TRACE 6 groundmass speckled with 5 to 20% euhedral grey dolomite 28 155.90 157.40 1.50 24 TRACE 86 2 47 TRACE 2 grains. Moderately hard, nonmagnetic. Nonfoliated to 29 157.40 157 .80 0.40 620 1.0 2792 2 53 23 10 weakly foliated at 501 to core axis. 1 to 3% irregular 30 178.00 179.50 1.50 108 0.8 705 TRACE 49 15 10 greyish-white dolomite veinlets 0.5mm to 1cm wide, 39 179.50 180.80 1.30 26 TRACE 196 2 50 TRACE 2 mostly at <501 to core axis. <0.5% white quartz veins. 31 180 .80 181.30 0.50 1135 1.5 13000 6 95 17 2

32 181.30 183.00 1.7056 TRACE 365 4 50 TRACE 9 153.6 - 154.4m: 10% pyrite in pyrite-dolomite bands/veins 33 183.00 183.50 0.50 136 0.7 806 9 70 9 2 up to 5cm wide at 401 to 501 to core axis. These are cut by 34 183.50 185.00 1.50 109 0.3 301 666 TRACE 6 unmineralized white quartz veins. 35 185.00 186.50 1.50 125 TRACE 266 9 46 TRACE 45

36 186.50 187.50 1.00 38 TRACE 140 7 50 TRACE 73 154.4 - 157.4m: Trace pyrite. 37 187.50 188.50 1.00 184 TRACE 200 8 45 TRACE 62

38 188.50 190.00 1.50 364 1.0 1175 8 56 15 56 157.4 - 157.8m: 3% pyrite and 1% chalcopyrite with grey carbonate in 0.5 to 3cm wide bands and patches at 501 to core axis.

158.8 - 159.8m: Blocky and broken.

162.6 - 163.1m: Fault. Three gouge-filled slips 3mm to 2cm wide at 501 to core axis.

178.0 - 178.2m: White quartz vein with black chlorite seams and margins at 451 to core axis. Minor pyrite.

178.5 - 190.0m: 1 to 5% pyrite and minor chalcopyrite in sulphide-carbonate veins 5mm to 5cm wide at 301 to 501 to

No: CDR97-6

Cameco Gold Inc.


ASSAYS SAMPLE No. FROM TO WIDTH Au (ppb) Ag (ppm) Cu (ppm) Pb (ppm) Zn (ppm) As (ppm) Ba (ppm)

1184 222.00 223.50 1.50 TRACE N.A. N.A. N.A. N.A. N.A. N.A. 1185 223.50 225.00 1.50 8 N.A. N.A. N.A. N.A. N.A. N.A.

1186 225.00 226.50 1.50 14 N.A. N.A. N.A. N.A. N.A. N.A. 1187 226.50 228.00 1.50 TRACE N.A. N.A. N.A. N.A. N.A. N.A. 1188 228.00 229.50 1.50 TRACE N.A. N.A. N.A. N.A. N.A. N.A. 1189 229.50 231.00 1.50 TRACE N.A. N.A. N.A. N.A. N.A. N.A. 1190 231.00 232.50 1.50 TRACE N.A. N.A. N.A. N.A. N.A. N.A. 1191 232.50 234.00 1.50 TRACE N.A. N.A. N.A. N.A. N.A. N.A. 1192 234.00 235.50 1.50 TRACE N.A. N.A. N.A. N.A. N.A. N.A. 1193 235.50 237.00 1.50 9 N.A. N.A. N.A. N.A. N.A. N.A. 1194 237.00 238.50 1.50 TRACE N.A. N.A. N.A. N.A. N.A. N.A. 1195 238.50 240.00 1.50 TRACE N.A. N.A. N.A. N.A. N.A. N.A. 1196 240.00 241.50 1.50 TRACE N.A. N.A. N.A. N.A. N.A. N.A.

FROM TO LITHOLOGICAL DESCRIPTION

core axis. Includes 40% pyrite and 20% chalcopyrite over 5cm at 180.9m.

187.6 - 188.0m: Grey siliceous varioles 5mm in diameter.

Lower contact broken, but appears to be at 601 to core axis. Location of contact is uncertain as there is only a subtle difference between the mafic and ultramafic rocks. The ultramafic rocks are slightly less green and less chloritic.

216.6 225.0 MASSIVE MAFIC/ULTRAMAFIC ROCK

Medium grey to greenish-grey, massive, very fine grained to fine grained, featureless, soft, nonmagnetic. Weakly foliated at 50I to core axis. 2 to 3% white calcite veinlets 0.5mm to 5cm wide at 201 to 501 to core axis. Minor disseminated <0.5mm pyrite, mostly near calcite veinlets. Lower contact gradational.

225.0 263.0 MAFIC VOLCANIC FLOWS

Medium green-grey to medium green, massive, featureless, very fine grained, moderately hard, nonmagnetic. Nonfoliated to weakly foliated. 1 to 36 white calcite veinlets similar to those in ultramafic unit uphole. <0.5% pyrite.

242.5 - 263.Om: Variolitic? Poorly developed coalesced variole textures locally present. Minor red hematitic coatings on some fractures.

No: CDR97-6

Cameco Gold Inc.



1197 241.50 243.00 1.50 9 N.A. N.A. N.A. N.A. N.A. N.A. 255.3 - 261.4m: Major Fault. Gouge and fault breccia 1198 243.00 244.50 1.50 8 N.A. N.A. N.A. N.A. N.A. N.A. comprise 70% of this unit. Calcite and hematite veinlets 1199 244.50 246.00 1.50 18 N.A. N.A. N.A. N.A. N.A. N.A. are dismembered. Hematite veinlets <lmm (<0.5%) cut 1200 246.00 247.50 1.50 TRACE N.A. N.A. N.A. N.A. N.A. N.A. calcite veinlets. 0.5% pyrite, mostly along irregular 1201 247.50 249.00 1.50 6 N.A. N.A. N.A. N.A. N.A. N.A. chloritic fractures at <l01 to core axis. 1202 249.00 250.50 1.50 TRACE N.A. N.A. N.A. N.A. N.A. N.A.

1203 250.50 252.00 1.50 TRACE N.A. N.A. N.A. N.A. N.A. N.A. 261.4 - 263.0m: Red grit sandstone identical to that 1204 252.00 253.10 1.10 5 N.A. N.A. N.A. N.A. N.A. N.A. intersected adjacent a strong fault in CDR97-01 and 40 253.10 254.10 1.00 3013 0.4 294 6 53 22 39 CDR97-02. Lower contact marked by a <1mm chloritic 563 254.10 255.30 1.20 2212 0.1 105 1 49 3 22 slip at 601 to core axis. This fault slip cuts a clast in the 564 255.30 257.00 1.70 580 0.1 95 1 53 3 14 grit, i.e. it post-dates the sedimentary rock. 565 257.00 258.30 1.30 79 0.1 35 1 53 3 7

566 258.30 259.40 1.10 19 0.1 25 1 49 3 7 41 259.40 260.40 1.00 478 0.3 1230 4 53 7 3

1205 260.40 261.30 0.90 33 N.A. N.A. N.A. N.A. N.A. N.A.

263.0 290.0 MASSIVE ULTRANAFIC/MAFIC ROCK 1206 265.50 267.00 1.50 TRACE N.A. N.A. N.A. N.A. N.A. N.A. 1207 267.00 268.50 1.50 5 N.A. N.A. N.A. N.A. N.A. N.A.

Medium grey to green-grey, massive, featureless, very fine 1208 268.50 269.60 1.10 TRACE N.A. N.A. N.A. N.A. N.A. N.A. grained, soft to moderately hard, nonmagnetic. Nonfoliated 42 278.00 279.00 1.00 171 TRACE 190 TRACE 33 TRACE 1 to weakly foliated. 1 to 2% irregular white dolomite 43 279.00 280.00 1.00 2917 TRACE 166 2 30 TRACE 8 veinlets <1cm1 wide, mostly at 301 to 501 to core axis. Trace 44 280.00 281.00 1.00 72 TRACE 94 2 27 TRACE 7 disseminated pyrite. The lower half of this unit is definitely _ 45 281.00 281.70 0.70 4248 0.5 74 TRACE 25 TRACE 30 medium grey, weakly carbonatized massive ultramafic 1209 286.70 288.00 1.30 76 N.A. N.A. N.A. N.A. N.A. N.A. rock. Lower contact sharp at 601 to core axis. 1210 288.00 289.00 1.00 52 N.A. N.A. N.A. N.A. N.A. N.A.

1211 289.00 289.90 0.90 167 N.A. N.A. N.A. N.A. N.A. N.A. 263.0 -265.5m: Network fracturing, probably related to fault uphole.

274.5m: Fault. 2cm of green chloritic gouge at 301 to core

No: CDR97-6

Cameco Gold Inc.


ASSAYS FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM TO WIDTH Au (ppb) Ag (ppm) Cu (ppm) Pb (ppm) Zn (ppm) As (ppm) Ha (ppm)

axis.

277.5m: Fault. 5cm of gouge and fractured rock at 501 to core axis.

278.0 - 281.7m: 1% pyrite as anhedral/subhedral grains <2mm, mostly in white carbonate veins and patches.

290.0 296.5 FELSIC DYKE

Light grey to buff, massive, very fine grained, hard, nonmagnetic, nonfoliated with nil to 5% ghosty 1 to 2mm feldspar phenocrysts. Patchy buff to light green colour due to weak sericite alteration along fractures <0.5mm, adjacent quartz veins, and as patches several cm across. 1% white, unmineralized 1cm wide quartz-carbonate veins in various orientations. Trace disseminated pyrite <0.5mm. Black tourmaline veinlets from 294.7 to 294.9m. Lower contact broken.

296.5 306.6 MASSIVE ULTRANAFIC ROCK

Massive, medium grey, very fine grained, featurless, soft, nonmagnetic. Nonfoliated. 1 to 2% irregular, white carbonate veinlets <2cm wide. <0.54 pyreite, associated with carbonate veinlets. Lower contact sharp at 301 tO core axis. Ultramafic is chilled, dark green, chloritic and aphanitic for 10cm adjacent contact. Could the felsic units be contemporaneous tuffs?

1212 289.90 291.00 1.10 18 N.A. N.A. N.A. N.A. N.A. N.A. 1213 291.00 292.50 1.50 8 N.A. N.A. N.A. N.A. N.A. N.A. 1214 292.50 294.00 1.50 19 N.A. N.A. N.A. N.A. N.A. N.A. 1215 294.00 295.50 1.50 18 N.A. N.A. N.A. N.A. N.A. N.A. 1216 295.50 296.40 0.90 20 N.A. N.A. N.A. N.A. N.A. N.A.

1217 296.40 297.40 1.00 5 N.A. N.A. N.A. N.A. N.A. N.A. 1218 297.40 298.50 1.10 436 N.A. N.A. N.A. N.A. N.A. N.A. 1219 298.50 300.00 1.50 6 N.A. N.A. N.A. N.A. N.A. N.A. 1220 300.00 301.50 1.50 6 N.A. N.A. N.A. N.A. N.A. N.A. 1221 301.50 303.00 1.50 TRACE N.A. N.A. N.A. N.A. N.A. N.A. 1222 303.00 304.00 1.00 49 N.A. N.A. N.A. N.A. N.A. N.A. 1223 304.00 305.60 1.60 15 N.A. N.A. N.A. N.A. N.A. N.A. 1224 305.60 306.60 1.00 18 N.A. N.A. N.A. N.A. N.A. N.A.

No: CDR97-6

Cameco Gold Inc.

DIAMOND DRILL LOG


ASSAYS


306.6 309.9 FELSIC DYKE 1225 306.60 307.60 1.00 193 N.A. N.A. N.A. N.A. N.A. N.A.

1226 307.60 308.80 1.20 189 N.A. N.A. N.A. N.A. N.A. N.A.

Light grey, massive, featureless, fine grained, hard,

nonmagnetic, nonfoliated. 0.5% disseminated pyrite. Up to

1227 308.80 309.80 1.00 133 N.A. N.A. N.A. N.A. N.A. N.A.

5% subhedral white 1 to 2mm feldspar phenocrysts. 10 to

20% subhedral green-grey phenocrysts 1 to 2mm long -

chloritized amphibole? Lower contact sharp at 751 to core

axis.

309.9 324.2 MAFIC VOLCANIC FLOWS 1228 309.80 310.80 1.00 TRACE N.A. N.A. N.A. N.A. N.A. N.A.

1229 310.80 312.00 1.20 50 N.A. N.A. N.A. N.A. N.A. N.A.

Medium green to medium green-grey, massive, very fine 1230 312.00 313.00 1.00 394 N.A. N.A. N.A. N.A. N.A. N.A.

grained to fine grained. Poorly developed coalesced variole 46 313.10 313.50 0.40 3832 4.1 7731 6 89 11 36

textures are locally present. Individual varioles are lighter 47 313.50 315.00 1.50 52 TRACE 48 TRACE 48 TRACE 52

green than groundmass and are lmm or less in size. Rare 48 315.00 315.50 0.50 727 1.0 1106 6 61 29 41

poorly developed pillow selvages (e.g. 316.7m). 1% 49 315.50 317.00 1.50 492 1.0 2067 9 70 6 64

irregular grey and white carbonate (no fizz) veinlets <1® 50 317.00 318.00 1.00 2386 3.4 1590 7 59 TRACE 42

wide. <0.5% pyrite and chalcopyrite overall. These are 1231 318.00 319.50 1.50 581 N.A. N.A. N.A. N.A. N.A. N.A.

concentrated locally in patches in the carbonate veins. 1232 319.50 321.00 1.50 80 N.A. N.A. N.A. N.A. N.A. N.A.

Lower contact indistinct - gradational? 1233 321.00 322.50 1.50 533 N.A. N.A. N.A. N.A. N.A. N.A.

1234 322.50 323.50 1.00 202 N.A. N.A. N.A. N.A. N.A. N.A.

309.9 - 318.4m: Deep green, moderately chloritized with

2% patchy light grey silica/carbonate alteration (e.g. 315.0 -

315.2m).

324.2 336.0 ULTRAMAFIC ROCK 1235 323.50 324.50 1.00 959 N.A. N.A. N.A. N.A. N.A. N.A.

51 324.50 324.70 0.20 2419 6.2 14000 3 58 8 88

Massive, very fine grained, featureless. 1 to 5% irregular 1236 324.70 325.70 1.00 163 N.A. N.A. N.A. N.A. N.A. N.A.

grey and white carbonate veinlets. Trace pyrite, except for 1237 325.70 327.00 1.30 TRACE N.A. N.A. N.A. N.A. N.A. N.A.

3% pyrite and 2% chalcopyrite associated with carbonate 1238 327.00 328.50 1.50 72 N.A. N.A. N.A. N.A. N.A. N.A.

No: CDR97-6

Cameco Gold Inc.

DIAMOND DRILL LOG


ASSAYS


from 324.5m to 324.7m.

Start of hole CDR9906 extension Logged by: Dominic Babin from 08/09/99 to 09/09/99

336.0 347.7 (MASSIVE ULTRAMAFIC ROCK)

Same as from 334.2-336.0 m. Very soft, talcose, fine grained, massive rock, non magnetic. Weakly to moderately foliated at

about 45 deg. TCA ( ROD >95). 5 to 10% irregular calcite

veinlets with rare quartz, less than 1 cm thick. They are

oriented anywhere from 5 to 45 deg TCA. The matrix is strongly altered to micro specks of ankerite and calcite. Trace to nil

pyrite.

339.4: Ground core.

342.7-347.7: The rock still appears to be ultramafic in

composition, but the matrix gradually becomes medium grained. It contains about 50% very dark irregular blebs, 1 to 5 mm long,

composed of biotite and probably chlorite. The rest of the rock

is composed of carbonate, calcite and probably chlorite+talc.

Still about 5% calcite+-quartz veinlets. Traces of fine grained

disseminated pyrite concentrated around 343.2 m.

342.7 356.4 (MASSIVE TO PILLOWED MAFIC ROCK)

Dark green, relatively soft, homogeneous, non magnetic, fine to

medium grained mafic rock. The rock is not to very weakly

SAMPLE No. FROM TO WIDTH Au (ppb) Ag (ppm) Cu (ppm) Pb (ppm) Zn (ppm) As (ppm) Ba (ppm)

1239 328.50 330.00 1.50 32 N.A. N.A. N.A. N.A. N.A. N.A.

1240 330.00 331.50 1.50 12 N.A. N.A. N.A. N.A. N.A. N.A.

1241 331.50 333.00 1.50 TRACE N.A. N.A. N.A. N.A. N.A. N.A.



1244 341.20 342.70 1.50 5 TRACE 50 TRACE 53 TRACE 62

1245 342.70 344.20 1.50 TRACE TRACE 88 TRACE 57 TRACE 100

1246 344.20 345.70 1.50 6 0.3 74 TRACE 58 TRACE 94

1247 345.70 346.80 1.10 TRACE 0.3 71 TRACE 44 TRACE 32

1248 346.80 347.80 1.00 21 0.3 47 TRACE 47 TRACE 8

1249 347.80 348.80 1.00 10 0.3 87 TRACE 48 TRACE 5


1251 349.70 350.70 1.00 19 0.3 155 TRACE 37 TRACE 8

No: CDR97-6

Cameco Gold Inc.

DIAMOND DRILL LOG

PROPERTY: Cedar Rapids

HOLE No.: CDR97-6 Page 11

ASSAYS


foliated and RQD > 95. The upper contact with the ultramafic unit 1252 350.70 351.70 1.00 8 TRACE 69 TRACE 33 TRACE 8

is very difficult to see (transitional?) and it could be located 1253 351.70 352.70 1.00 51 0.4 341 TRACE 39 TRACE 17

anywhere from 346.0 to 348.0 m. The rock is composed of 30 to 50% 1254 352.70 353.70 1.00 31 TRACE 332 TRACE 39 TRACE 12

irregular dark specks, 1 to 2 mm in size, which are composed 1255 353.70 354.70 1.00 6 TRACE 69 TRACE 36 TRACE 5

probably of biotite and chlorite. The matrix between the specks 1256 354.70 356.40 1.70 9 TRACE 89 TRACE 38 TRACE 6

is aphyric and probably composed of chlorite and feldspars. The rock is weakly altered to pervasive calcite and ankerite. There are 1-2% white calcite veinlets, <5 mm thick, oriented from 10 to 40 deg. ICA. From 347.7 to 349.9 m, the unit is altered to about 5% subhedral specks of calcite and ankerite. The alteration decreases gradually away from the ultramafic contact. The pillowed texture is not obvious and possible pillow selvages could correspond to the darker mineralized chloritic bands found at 349.7, 352.4, 352.5, 352.6, 353.1, and 356.0 m. These bands/pillow selvages are 2 mm to 4 cm thick and are oriented at 45 to 70 deg. TCA. The bands are composed of about 25 to 50% pyrite, less than 1% chalcopyrite, <1 to 50% white quartz-calcite, and the rest is occupied by chlorite. There is a 1 to 3 cm wide chloritic halo around each mineralized band, where the crystalline texture of the host rock has been completely destroyed. The rest of the unit contains no significative sulphides.

356.4 364.3 (MINERALIZED MASSIVE TO PILLOWED MAFIC ROCK) 1257 356.40 357.40 1.00 61 0.5 688 TRACE 50 8 22

1258 357.40 358.40 1.00 114 0.7 1165 TRACE 51 9 16

Similar rock as from 342.7 'to 356.4m, but it is mineralized with 1259 358.40 359.60 1.20 147 0.9 1154 TRACE 67 11 27

about 10% semi-massive sulfides stringers, 2 mm to 10 cm thick. 1260 359.60 360.20 0.60 289 1.7 2729 TRACE 68 15 8

The host rock is aphyric, strongly chloritic and weakly altered to 1261 360.20 361.20 1.00 5 TRACE 58 TRACE 54 TRACE 1

ankerite and calcite. No well defined hyaloclastite or fragmental 1262 361.20 362.30 1.10 60 0.7 734 TRACE 70 10 35

textures are seen, but the unit is probably pillowed. There is a 1263 362.30 363.30 1.00 89 0.5 648 TRACE 65 10 2

No: CDR97-6

Cameco Gold Inc.

DIAMOND DRILL LOG


ASSAYS


faint, relatively sharp contact with the previous interval oriented at about 30 deg. TCA. 1 to 2% late, calcite-filled fractures, <5 mm thick and oriented at 5 to 45 deg. TCA. Rare buff, quartz-sericite-carbonate veinlets, <1 cm thick, crosscut the mineralized stringers at high angle (>70 deg.) The sulphide stringers are oriented from <5 to 80 deg. TCA and are composed of 10 to 80% sulphides, 0 to 60% quartz-calcite and variable amount of chlorite and magnetite. From 356.4 to 359.6 m, the sulphides within the stringers are dominated by pyrite, with up to 15% pyrrhotite and variable amount of magnetite. After 359.6 m, the sulphides are still dominated by pyrite, but it is associated with

up to 5% chalcopyrite and no magnetite is seen.

364.3 367.4 (MINERALIZED MAFIC BRECCIA/HYALOCLASTITE)

At around 364.3 m, the mafic rock becomes lighter green, and it is cut by an intense network of yellowish buff fractures, up to 2 cm thick, filled with aphyric silica and sericite? The host rock is not aphyric (similar to 342.7 to 356.4m), and contains up to 50% coalescent varioles/spherulites 1 to 2 mm in diameter. Chloritic, angular (triangle shape) hyaloclastite fragments are common. Similar breccia/hyaloclastite is seen in hole CDR9830. The mineralization is similar to previously, but it is concentrated from 366.0 to 367.4 m. There is a 15 cm thick mineralized band from 366.4 m, composed of 50% pyrite and 5% chalcopyrite.

367.4 372.0 (MAFIC BRECCIA/HYALOCLASTITE)

Same as from 364.3 to 367.4 m, but it is only weakly mineralized from 371.2 to 372.0 m with 2 to 3% disseminated and stringer cubic

1264 363.30 364.80 1.50 7 0.4 461 TRACE 54 TRACE 7


1266 366.00 366.60 0.60 561 3.0 5511 11 68 110 5






No: CDR97-6

Cameco Gold Inc.

DIAMOND DRILL LOG


ASSAYS


pyrite concentrated in chloritic +/- quartz-carbonate stringers 1272 371.30 372.00 0.70 17 0.2 200 TRACE 64 TRACE 7

<5 cm thick.

372.0 376.0 (FELSIC TUFF) 1273 372.00 372.30 0.30 55 0.4 608 2 40 22 10


Medium grey, relatively soft, thinly laminated (<1 cm bands), 1275 373.80 375.40 1.60 17 0.2 154 TRACE 25 TRACE 36

felsic tuff/chert. It is probably a felsic tuff since it is too 1276 375.40 376.00 0.60 5 0.3 234 3 962 TRACE 53

soft to be a chert? The rock is relatively blocky (RQD of about 60). The contact with the mafic rock is very sharp and oriented parallel to bedding at 55 deg. TCA. From 372.0 to 372.13 m, the rock is very siliceous and contains about 20% coarse cubic, banded pyrite The amount of pyrite decreases gradually away from the mafic contact. From 372.13 to 375.4 m, the felsic tuff/chert is weakly to moderately sericitized and contains 1 to 2% disseminated, fine grained cubic pyrite. There are rare irregular beds?, darker in colour and more chloritic, containing up to 5% disseminated pyrite. From 375.4 to 376.0 m, the felsic tuff/chert contains abundant (>20%) chloritic laminae? and the interval is mineralized with 5 to 10% finely disseminated pyrite and pyrrhotite (+/- magnetite) with <1% chalcopyrite.

376.0 421.6 (VOLCANICLASTIC SANDSTONE, MUDSTONE/TUFF/CHERT) 1277 376.00 377.50 1.50 TRACE TRACE 51 4 38 TRACE 23

1278 377.50 379.00 1.50 TRACE TRACE 61 4 50 TRACE 32

Medium grey, relatively soft, non magnetic, laminated to thickly 1279 379.00 380.50 1.50 15 0.2 131 4 525 10 44

bedded, fine to very coarse lithic sandstone, interbedded with 1280 380.50 382.00 1.50 5 TRACE 135 3 64 TRACE 50

thinly laminated aphyric, medium grey felsic tuff/chert/mudstone, 1281 382.00 383.50 1.50 10 TRACE 42 TRACE 81 TRACE 8

very similar to 372.0 to 376.0 m (RQD >95). The mudstone and 1282 383.50 384.50 1.00 13 TRACE 130 TRACE 94 TRACE 7

sandstone intervals are anywhere from 30 cm to 5 m thick. Some of 1283 384.50 385.60 1.10 48 0.3 111 TRACE 58 TRACE 1

the mudatone/tuff beds are strongly sericitized. From 376.0 to 1284 385.60 387.00 1.40 12 TRACE 92 TRACE 92 TRACE 4

402.6 m, the sandstone beds contain 1 to 2% disseminated cubic 1285 387.00 388.00 1.00 6 TRACE 91 TRACE 71 TRACE 12

No: CDR97-6

Cameco Gold Inc.

DIAMOND DRILL LOG



Ag (ppm) Cu (ppm) Pb (ppm) En (ppm) As (ppm) Ba (ppm)

pyrite up to 3 mm in size. Within the same interval, the 1286 388.00 388.50 0.50 7 0.3 163 4 50 8 24

mudstone/tuff beds contain 1 to 5% finely disseminated pyrite and 1287 388.50 390.00 1.50 7 0.3 88 TRACE 77 TRACE 2

also rare stringers of pyrite and trace chalcopyrite. There is 5% 1288 390.00 391.50 1.50 9 0.2 85 TRACE 72 TRACE 4

pyrite from 388 to 388.3 m. The rest of the unit is relatively 1289 391.50 393.00 1.50 44 0.2 125 TRACE 51 TRACE 5

barren except from the intervals mentioned below. Bedding is 1290 393.00 394.50 1.50 255 0.4 346 2 43 TRACE 1

oriented at 60 deg. TCA. The beds are crosscut by about 1% 1291 394.50 396.00 1.50 74 TRACE 121 3 33 10 20

calcite-filled fractures, < 2-3 mm thick and oriented in all 1292 396.00 397.50 1.50 TRACE TRACE 105 9 29 6 30

directions. They are also cut by rare, white quartz-calcite- 1293 397.50 399.00 1.50 11 0.3 221 TRACE 38 TRACE 13

chlorite veins oriented from < 5 to 80 deg. TCA. The veins are 1294 399.00 400.50 1.50 TRACE TRACE 52 2 39 TRACE 6

usually barren and 1 to 2 cm wide, but as described below, one 1295 400.50 402.00 1.50 TRACE TRACE 97 TRACE 32 TRACE 27

vein is up to 80 em wide. The coarser beds contain up to 20% 1296 402.00 403.00 1.00 25 TRACE 13 TRACE 30 TRACE 2

light grey, angular to sub-angular, aphyric fragments, 1 to 5 mm 1297 403.00 404.50 1.50 10 TRACE 1 2 28 TRACE 19

in size, which may represent felsic volcanic cleats or feldspar 1298 412 00 413.00 1.00 5 0.3 50 2 35 TRACE 18

fragments. Most of the sandstone beds contain also up to 5% 1299 413.00 413.60 0.60 5 0.3 307 TRACE 37 TRACE 10

biotite specks, less than 0.5 mm in size. No top indicators could 1300 413.60 414.50 0.90 10 0.3 132 TRACE 24 TRACE 3

be found. 1301 414.50 415.50 1.00 9 0.4 166 TRACE 46 TRACE 4

1302 415.50 416.50 1.00 73 1.1 1312 2 41 TRACE 14

384.6-385.2: White quartz-calcite-chlorite vein, oriented parallel 1303 416.50 417.50 1.00 244 TRACE 71 TRACE 42 TRACE 23

TCA and containing traces of chalcopyrite and pyrite. 1304 420.60 421.60 1.00 TRACE TRACE 22 TRACE 37 TRACE 6

391.0-391.3: Barren, white, quartz-calcite-chlorite vein, oriented at about 40 deg. TCA.

413.2-416.5: Fine grained sandstone section, relatively darker in colour (more chloritic?) From 413.5 to 416.0 m and intruded by a white quartz-calcite-chlorite vein from 413.6 to 414.5 m. The contacts of the vein are sharp and oriented at about 45 deg. TCA. The vein contains traces of pyrrhotite, but from 413.2 to 413.6 m and from 414.5 to 416.5 m, the host rock contains about 2 to 3% disseminated and stringer pyrrhotite with minor pyrite and traces

No: CDR97-6

Cameco Gold Inc.

DIAMOND DRILL LOG PROPERTY: Cedar Rapids

HOLE No.: CDR97-6 Page 15

ASSAYS


of chalcopyrite. From 414.5 to 416.0 m, there are four, quartz- calcite-hematite veins, oriented at 30 to 40 deg. TCA, all about 1 cm wide, which contains 1% specks of chalcopyrite and pyrrhotite. Also, from 415.6 to 416.5 m, the pyrrhotite stringers contain up to 10% chalcopyrite and they are associated with white calcite veinlets up to 3 cm wide.

418.4-419.8: Series of sandstone beds with strongly altered felsic clasts/feldspar fragments, which are buff in colour ( probably sericitized). The matrix of these beds is also more biotitic than the rest of the unit. Bedding is oriented at 45 deg. TCA.

420.7: 1 to 2 mm thick pyrrhotite-pyrite stringer.

421.6: EOH

Whole Rock Samples:

CDR9906-A: 337.0-340.0: Carbonatized ultramafic rock. CDR9906-B: 350.0-353.0: Relatively unaltered mafic flow. CDR9906-C: 358.0-361.0: Weakly chloritized mafic flow. CDR9906-D: 368.0-371.0: Mafic flow breccia with cherty matrix.

Representative Samples:

337.9 m: Carbonatized and massive ultramafic rock. 349.6 m: Relatively unaltered mafic flow. 358.6 m: Chloritized and mineralized mafic flow. 266.2 m: Mafic flow breccia with cherty matrix 266.4 m: Semi-massive sulphide stringer for thin section.

No: CDR97-6

Cameco Gold Inc.



DOWN-HOLE SURVEY DATA

DEPTH INCLINATION BEARING

60.00 -47.00

180.00 -48.00

240.00 -48.00

300.00 -46.00

398.50 -46.60

No: CDR97-6

Cameco Gold Inc.

DIAMOND DRILL LOG

PROPERTY: Cedar Rapids HOLE No.: CDR9932 Collar Eastings: 1320.00 Collar Northings: -1535.00 Collar Elevation: 290.00 Grid: N-S Claim#:5126361

Collar Inclination: -55.00 Logged by: D. Babin Hole Bearing: 230.00 Date: 12/09/99-18/09/99 Final Depth: 352.20 metres Down-hole Survey: DIP METER/ACID TEST Val d'Or Drilling Core: NQ Test the SE extension of the Village Zone.

ASSAYS FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM TO WIDTH Au (ppb) Ag (ppm) Cu (ppm) Pb (ppm) Zn (ppm) Mo (ppm) As (ppm)

58.3 80.3 (DIORITE?) 1386 58.30 59.30 1.00 43 TRACE 195 11 30 1 TRACE 1387 71.00 72.00 1.00 51 TRACE 209 2 32 1 TRACE

Medium-dark greenish grey, hard, non magnetic, very blocky (RQD 1388 72.00 73.00 1.00 27 0.2 92 9 30 1 TRACE <50) and heterogeneous, non to weakly foliated, medium grained 1389 73.00 74.00 1.00 26 TRACE 157 TRACE 23 2 TRACE intermediate intrusive rock. The unit is composed generally of 20 1390 79.30 80.30 1.00 22 0.2 75 3 20 3 TRACE to 40% anhedral to subhedral, stubby, mafic minerals (probably altered pyroxenes?), 1 to 6 mm in diameter, floating and intertwined with a groundmass of feldspars, <1 to 2 mm in size. Quartz could be present in the groundmass, but no megascopic crystals were seen. The intrusive rock is moderately altered to epidote, which is present in 1 to 3 mm wide fractures (10%/vol.) and also as anhedral specks, 1 to 2 mm in size. There are about 3 to 5% grey quartz veinlets, <2 cm thick, showing biotite(+/- chlorite)-rich margins. Minor calcite is also present in the veinlets. They crosscut and displace about 1%, 1 to 5 mm wide, fractures filled with calcite, quartz, and tourmaline?(black and hard mineral), which crosscut the earliest epidote-filled fractures. All fractures ire oriented between 25 and 40 deg. TCA. Traces of very fine grained pyrite are seen.

80.3 128.8 (GABBRO) 1391 80.30 81.30 1.00 47 0.3 169 TRACE 52 1 TRACE 1392 95.00 96.00 1.00 31 TRACE 63 3 33 11 TRACE

Dark grey-green, very heterogenous, hard, non magnetic, blocky 1393 99.90 101.00 1.10 40 TRACE 212 TRACE 35 10 TRACE (RQD=50-70), medium grained gabbroic rock. The contact with the 1394 101.00 102.00 1.00 23 TRACE 204 TRACE 38 25 TRACE previous intrusive interval is relatively sharp and oriented at 1395 102.00 103.00 1.00 12 0.2 104 TRACE 38 25 TRACE

No: CDR9932

Cameco Gold Inc.

DIAMOND DRILL LOG

PROPERTY: Cedar Rapids HOLE No.: CDR9932 Page 2


about 30 deg. TCA. It is marked by a 1.5 cm thick, very fine 1396 106.00 107.00 1.00 39 0.3 330 TRACE 37 29 TRACE grained, diffuse and dark horizon, probably rich in mafic minerals 1397 107.00 108.00 1.00 59 TRACE 382 TRACE 34 38 TRACE (pyroxene?). The gabbro is composed of 30-80% altered subhedral 1398 108.00 109.00 1.00 8 0.2 107 TRACE 41 24 TRACE pyroxene?, <1 to 8 mm in size and 20 to 70% plagioclase laths, up 1399 125.40 126.40 1.00 7 0.2 107 TRACE 45 17 TRACE to 2 mm long. The rock is generally equigranular (1 to 2 mm grain 1400 126.40 127.00 0.60 13 0.3 237 2 31 6 TRACE size), but from 80.3 to 95.2 m, there are about 20% "cumulate" 1401 127.00 128.00 1.00 TRACE 0.2 18 TRACE 41 7 TRACE horizon, <20 cm wide, which are composed of at least 80% euhedral pyroxenes (5 to 8 mm in size). The contacts of these horizons are relatively diffuse and oriented at about 40 to 50 deg. TCA. Within the same interval (80.3 to 95.2 m), there are about 30 to 40%, darker grey, diffuse, fine grained sections, up to 1 m long, which probably represent finer grained facies of the gabbroic rock. All phases are weakly to moderately altered to fracture- controlled epidote, similarly to the diorite above. These fractures are also crosscut by about 5% quartz-biotite-calcite- carbonate veinlets, <2 cm wide and oriented generally at about 30 deg. TCA. Traces of pyrite and very rare chalcopyrite is seen in places.

86.6-87.1: Lost core.

91.9-92.0: Strongly biotitic section intruded by a 2 cm wide, pink, fine grained veinlet, probably composed of K-spars and quartz. <1% disseminated pyrite within and around the veinlet.

95.6-95.8: Darker section (biotitic?) cut by 10% epidote-filled fractures, 1 to 3 mm wide and oriented in all directions. No visible sulphides.

99.0-99.5: 1 cm wide, pink veinlet, oriented sub-parallel TCA.

No: CDR9932

Cameco Gold Inc.

DIAMOND DRILL LOG

PROPERTY: Cedar Rapids HOLE No.: CDR9932 Page

ASSAYS FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM TO WIDTH Au (ppb) Ag (ppm) Cu (ppm) Pb (ppm) Zn (ppm) MO (ppm) As (ppm)

Very similar veinlet to 91.2 to 92.0 m. It is crosscut by the late quartz-biotite veinlets, but it crosscuts the epidote-filled fractures.

99.9-102.2: Section containing 2 or 3, 1 to 2 mm wide pyrite stringers, associated with some black mineral (biotite?) and minor quartz. Epidote is also seen along one stringer margin. Few specks of chalcopyrite and <0.5% disseminated pyrite are seen within a blocky, more dioritic looking section, from 101.4 to 101.9 m.

104.0-105.0: This section contains three stringers, 2 mm to 1 cm wide, composed mainly of biotite?, magnetite and pyrite, with minor quartz, calcite, carbonate and epidote. They are oriented at 40 to 50 deg. TCA. Overall, the interval contains maximum 1% pyrite, but each stringer contains up to 25% disseminated subhedral to euhedral pyrite, 1 to 2 mm in size.

111.3-128.8: At 111.3 m, the gabbroic rock becomes gradually (over 20 cm) darker in colour probably due to a decrease in feldspar content? >30% subhedral to euhedral pyroxene? <5 mm in size. The moderate, fracture-controlled epidote alteration stands out more. There are still about 5% quartz-chlorite/biotite-carbonate-calcite stringers oriented at about 30 to 45 deg. TCA.

115.8-116.6: Coarse grained section/dyke composed of 60% tabular plagioclase crystals, 2 to 3 mm long, with 40% black, interstitial and chloritized mafic mineral (amphibole?). Contacts are diffuse, with grain size increasing and decreasing rapidly over 5 to 10 cm. No visible sulphides.

No: CDR9932

Cameco Gold Inc.

DIAMOND DRILL LOG


HOLE No.: CDR9932 Page 4

ASSAYS

FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM TO WIDTH Au (ppb) Ag (ppm) Cu (ppm) Pb (ppm) Zn (ppm) MO (ppm) As (ppm)

119.5-119.6: Dark grey, hard, feldspar porphyritic dykelet,

oriented at 80 deg TCA. It is composed of about 20% very diffuse,

subhedral, feldspar phenocrysts, 1 to 2 mm long, in an aphyric

siliceous matrix. No visible sulphides.

126.5: 4 mm wide stringer, composed of 50% pyrite, within a

chlorite-quartz-calcite-carbonate matrix.

121.8-122.0: 20 cm wide, white, quartz vein oriented at 30 deg.

TCA and containing one subhedral bleb of pyrite, 1 cm in diameter.

128.8 262.5 (EPIDOTIZED FELDSPAR PORPHYRY) 1402 128.80 130.30 1.50 25 TRACE 90 TRACE 23 7 TRACE

1496 130.30 131.50 1.20 TRACE TRACE 15 TRACE 21 5 TRACE

Medium grey, non magnetic, very hard, non to weakly foliated, 1497 131.50 133.00 1.50 7 TRACE 66 TRACE 22 37 TRACE

feldspar porphyritic intrusive rock. It is composed of 20 to 40% 1498 133.00 133.50 0.50 11 TRACE 29 TRACE 26 2 TRACE

euhedral white plagioclase crystals, 1 to 5 mm long, <5% 1499 133.50 134.60 1.10 TRACE TRACE 29 TRACE 22 10 TRACE

subhedral, greenish mafic mineral (chloritized amphibole?), 1 to 2 1500 134.60 136.20 1.60 8 TRACE 65 TRACE 34 7 TRACE

mm long, very rare quartz specks, <1 mm in size, and 60 to 80% 1501 136.20 137.30 1.10 10 TRACE 93 TRACE 30 6 TRACE

aphyric and siliceous matrix. Sulphides are rare (traces) are 1502 137.30 138.50 1.20 TRACE TRACE 42 TRACE 28 18 TRACE

associated with fractures. The unit is moderately altered to 1503 138.50 140.00 1.50 9 TRACE 68 TRACE 32 13 TRACE

epidote, seen along fractures and partially to totally replacing 1403 145.00 146.00 1.00 20 TRACE 101 TRACE 29 4 TRACE

10 to 30% of the feldspar phenocrysts. The interval is very 1404 148.40 149.40 1.00 TRACE 0.2 11 TRACE 25 3 TRACE

blocky (RQD=50-60), with several section with lost core (indicated 1405 172.90 173.90 1.00 13 TRACE 135 TRACE 26 4 TRACE

below). 2 to 3% white quartz-chlorite-calcite-carbonate 1406 173.90 175.00 1.10 24 TRACE 119 TRACE 27 8 TRACE

stringers, < 1 cm thick (but generally <5 mm thick) and oriented 1407 175.00 176.00 1.00 11 TRACE 67 TRACE 30 3 TRACE

at 30 to 70 deg. TCA. Rare fine grained mafic xenoliths up to 1408 178.50 179.50 1.00 11 TRACE 76 TRACE 29 4 TRACE

3 cm in diameter. The upper contact with the gabbro is undefined 1409 179.50 180.20 0.70 9 TRACE 94 TRACE 27 671 TRACE

since it is located in a very blocky section of core. 1410 180.70 181.70 1.00 10 TRACE 83 TRACE 26 3 TRACE

1411 181.70 183.20 1.50 8 TRACE 52 TRACE 25 4 TRACE

No: CDR9932

Cameco Gold Inc.

DIAMOND DRILL LOG



FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM TO WIDTH Au (ppb)

ASSAYS Ag (ppm) Cu (ppm) Pb (ppm) Zn (ppm) Mo (ppm) As (ppm)

133.6-137.3: Medium grey, very fine grained siliceous section,

with very rare feldspar crystals, < 1 mm in size. It has the same

1412

1413

183.20

195.80

184.70

197.20

1.50

1.40

TRACE

11

TRACE

TRACE

47

69

TRACE

TRACE

27

25

2

5

TRACE

TRACE colour and texture as the matrix of the feldspar porphyry. It is 1414 197.20 198.20 1.00 9 TRACE 83 TRACE 25 18 TRACE cut by a network (10 to 20%) of dark silica-chlorite-carbonate 1415 211.40 212.40 1.00 15 TRACE 220 TRACE 46 3 TRACE stringers, <2 mm wide. Traces of molybdenum in these fractures 1416 212.40 213.40 1.00 20 TRACE 171 TRACE 30 3 TRACE from 134.0 to 134.6 m. Weak to moderate, fracture-controlled 1417 224.00 225.00 1.00 9 TRACE 123 TRACE 27 7 TRACE epidotization. The upper contact with the porphyritic facies is 1418 225.00 226.00 1.00 26 0.2 263 TRACE 32 9 TRACE diffuse, while the lower contact is marked by a 15 cm wide,

strongly foliated shear zone, oriented at 45 deg. TCA. There is a

1419

1420

232.50

240.10

233.20

241.10

0.70

1.00

14

13

TRACE

0.2

160

142

TRACE

TRACE

23

27

7

3

TRACE

TRACE 5 cm wide gouge section from 137.25 to 137.3 m. Only very rare 1421 247.50 248.50 1.00 21 TRACE 229 TRACE 28 8 TRACE pyrite and chalcopyrite. 1422 248.50 249.30 0.80 12 0.3 187 TRACE 28 15 TRACE

1423 249.30 250.30 1.00 25 TRACE 283 TRACE 33 7 TRACE 138.6-142.0: Finer grained section composed of at least 50% 1424 254.30 255.30 1.00 51 TRACE 467 2 32 6 TRACE feldspar < 1 mm long, in a similar matrix as the main porphyritic 1425 255.30 256.20 0.90 15 0.3 211 TRACE 19 5 TRACE facies. It is probably a different facies of the main porphyritic 1426 256.20 257.20 1.00 62 TRACE 702 2 30 4 TRACE body. The upper contact is very sharp and marked by a chloritized 1427 261.00 262.50 1.50 22 TRACE 155 TRACE 28 10 TRACE "shear" plane, less than 5 mm wide, oriented at 40 deg. TCA. The

lower contact is less obvious and more transitional. No

significant sulfides. Possible anhydrite in one of the calcite-

quartz-chlorite stringer at 139.3 m.

143.9-144.1: Shear zone. Feldspars have been destroyed or

stretched at 45 deg. TCA. The zone is moderately altered to

pervasive epidote. Contacts are transitional. 5% calcite-quartz-

carbonate fracture network with chloritic margins, crosscut the

foliation. No visible sulphides.

145.8: Pyrite-calcite-carbonate-chlorite-quartz stringer, 3 mm

wide, oriented at 40 deg. TCA. It is crosscut perpendicularly and

offset by a series of fractures filled with quartz, chlorite and

No: CDR9932

Cameco Gold Inc.

DIAMOND DRILL LOG



ASSAYS

FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM TO WIDTH Au (ppb) Ag (ppm) Cu (ppm) Pb (ppm) Zn (ppm) Mb (ppm) As (ppm)

carbonate.

148.0-156.0: The interval contains more feldspar than the main

porphyritic facies. There is about 50 to 60% feldspars, up to

3 mm in size, but mainly < 1 mm long. There is also 5 to 10% dark

grey, angular mafic crystals/xenoliths, generally less than 5 mm

in size, but some xenoliths are up to 3 cm across. Contacts with

the main facies are undefined (blocky core).

148.7-149.2: Possible shear zone. Darker grey, fine grained

section, where the feldspar phenocrysts have been destroyed by

chlorite and sericite. At about 149.0 m, the rock is strongly

sericitized and foliated at 50 deg. TCA over 15 cm of core length.

150.5-150.9: Blocky section with few foliated and brecciated

zones, probably representing small shears. Traces of pyrite.

152.8-152.9: Fine grained, dark grey, soft, chloritic section,

probably a mafic xenolith. Contacts are undefined, but appear

sharp.

156.35: 1 cm wide, strongly sericitized minor shear oriented at 40

deg. TCA.

159.5-160.5: Fine grained, feldspar porphyritic facies, very

similar to 138.6 to 142.0 M. From 160.0 to 160.1 m, there is a

block/dyke of the main porphyritic facies. It has very sharp but

variable contacts with the finer grained facies. No chilled or

cooked margins.

No: CDR9932

Cameco Gold Inc.

DIAMOND DRILL LOG




161.0-163.5: Very blocky section with 1.22 m of lost core. In that section, there is a 8 cm long block composed of 90% white, barren quartz and about 10% fracture-controlled chlorite.

164.2 171.1 (Hornblende-feldspar porphyry) Medium-dark greenish grey, moderately hard, non magnetic, non to weakly foliated, amphibole (hornblende) and feldspar porphyritic dyke/sill. Upper and lower contacts are sharp, but irregular. It is composed of 10 to 20% subhedral black amphibole phenocrysts (hornblende?), 1 to 3 mm in size, 5 to 10% feldspar phenocrysts, <1 mm long, partially to totally altered to epidote. The matrix is moderately hard and aphyric. The dyke is cut by the same epidote and quartz-calcite-carbonate-chlorite stringers and fractures as the main feldspar porphyritic facies.

166.7-167.2: Section/block showing same composition and porphyritic texture as the main description.

167.2-167.5: Lost core.

167.5-168.0: Section/block with the same fine grained porphyritic texture as the interval from 138.6-142.0 m. Contacts with the Hp- Fp porphyritic dyke are sharp and oriented at 80 deg. TCA.

168.9-169.1: Pervasively carbonatized? interval, overprinted by a moderate, fracture-controlled epidote alteration. The interval contains 10 to 20% irregular quartz-carbonate-filled fractures/stringers, with amphibole/biotite-rich margins, oriented in all directions. Traces of disseminated pyrite is seen in some of the fractures.

No: CDR9932

Cameco Gold Inc.

DIAMOND DRILL LOG



ASSAYS

FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM TO WIDTH Au (ppb) Ag (ppm) Cu (ppm) Pb (ppm) Zn (ppm) Mo (ppm) As (ppm)

173.9: <5 mm wide irregular stringer, composed of 25% pyrite,

quartz, carbonate and chlorite?, with 1 to 2 mm thick epidotized

margins.

174.9: Similar pyritic stringer (<5 man thick) as described above

oriented at 15 deg. TCA.

178.0-178.7: Very blocky section with 20 cm of lost core.

178.5: Strongly foliated and sericitized shear, 4 am thick and

oriented at 45 deg. TCA. Traces of disseminated pyrite.

179.0-179.2: Weakly chloritic, moderately sericitized and strongly

foliated interval, where all feldspar phenocrysts have been

destroyed. Probably a shear zone oriented at 50 deg. TCA. <1%

fine grained pyrite is seen.

179.5-180.0: Moderately epidotized and may be weakly carbonatized

(bleached) feldspar porphyritic interval, similar to main description, but it is cut by about 3 quartz-carbonate stringers,

<3 mm thick, containing >20% molybdenum/galena and traces of

chalcopyrite+pyrite+sphalerite. The stringers are oriented at 30

to 45 deg. TCA and present no significant alteration along their

margins. The only difference with the rest of the unit is that

the matrix seems weakly bléached.

180.2-180.7: Lost core.

181.0-186.9: Weakly bleached section, which is more epidotized

No: CDR9932

Cameco Gold Inc.

DIAMOND DRILL LOG



ASSAYS


(fracture controlled) from 181.0 to 184.6 m. The epidote-calcite-

filled fractures are oriented at very low angle (<10) TCA. Trace

pyrite.

186.9-262.5: The main porphyritic facies contains about 5 to 10%

strongly foliated, moderately sericitized and chloritized zones,

oriented at 35 to 45 deg. TCA, where most feldspar phenocrysts

have been destroyed (small shear zone?).. The zones are 2 cm to

70 cm wide. The contacts of these sections are relatively abrupt,

but slightly diffuse (not sharp). Calcite-carbonate+/-quartz

stringers, with chlorite+/-tourmaline? margins are often located

in the middle of these zones and are oriented sub-parallel to

foliation . They are <1 cm thick. Traces to 2% disseminated,

fine grained pyrite is seen almost exclusively in these zones (no

sulphides in the main porphyritic facies). The pyrite is

stretched along the foliation planes.

196.0-196.2: Finer grained feldspar phyric dykelet, oriented at 30

deg. TCA. <1% pyrite seen in a calcite-carbonate stringer, 3 mm

thick.

197.7-197.9: Fine grained intermediated dykelet oriented at 50

deg. TCA. The upper contact is marked by a 7 cm wide foliated

zone similar to above.

208.0-208.5: Medium grey, fine grained dykelet, intermediate in

composition and oriented at 45 deg. TCA. The contacts are very

sharp and straight. The dykelet is moderately epidotized

(fracture controlled). No visible sulphides.

No: CDR9932

Cameco Gold Inc.

DIAMOND DRILL LOG




211.9-212.4: Brownish, aphyric, intermediate dykelet, with sharp

but irregular contact with the main porphyritic facies. Trace pyrite.

214.4-217.7: Finer grained felspar porphyritic facies/dyke,

composed of 50% euhedral feldspar phenocrysts, <2 mm long and 20%

green (chloritized), subhedral mafic phenocrysts, also <2 mm in

size. The matrix is aphyric and similar to the main porphyritic

facies. Contacts appear sharp, but they are hard to see. There

are two white quartz veinlets, 1.5 and 2 cm thick, oriented at 25

to 30 deg. TCA. Trace pyrite.

224.0-228.5: Moderately fractured interval where the feldspar

phenocrysts become diffused. The rock seems weakly chloritized?

The hairline thin fractures oriented in all directions are filled

with yellowish-buff siliceous material, probably a combination of

silica, epidote, sericite and may be carbonate? Trace amount of

pyrite.

231.0-231.9: Medium-dark grey, hard, non magnetic, fine grained,

feldspar phyric dyke. Two white and barren quartz veinlets, 1 and

3 cm wide.

232.5-233.2: Dark grey-green interval where the felspar

phenocrysts are very diffuse. The interval is moderately

chloritized and sericitized, but only very weakly foliated. 5%

calcite-carbonate-quartz stringers, <1 cm wide and <1%

disseminated pyrite. Contacts are relatively sharp.

248.5-249.2: Fine grained, strongly foliated, moderately

No: CDR9932

Cameco Gold Inc.

DIAMOND DRILL LOG



ASSAYS FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM TO WIDTH Au (ppb) Ag (ppm) Cu (ppm) Pb (ppm) Zn (ppm) Mb (ppm) As (ppm)

chloritized and sericitized interval, containing about 1% very fine grained pyrite and traces of molybdenum (shear zone?).

255.5-256.0: White, blocky quartz vein, containing about 1% very fine grained disseminated pyrite associated with 15 to 30% chlorite/biotite stringers/fractures. Contacts of the vein are sharp but it is hard to measure their orientation since the core is very blocky. Over 15 to 20 cm on each side of the vein, the feldspar porphyritic texture is more diffuse and the host rock contains about 1 to 2% disseminated and fracture-controlled pyrite. These margins are weakly foliated and weakly altered to sericite+/-carbonate and may be chlorite?

262.4-262.5: Section with 2 or 3 calcite-chlorite-quartz filled fractures containing about 1% molybdenum. Could be part of the carbonatized section?

262.5 317.9 (CARHONATIZED FELDSPAR PORPHYRY)

Same porphyritic rock as above, but the style of mineralization and alteration gradually changes around 262.5 m (approximately). The rock is still composed of 20 to 40% euhedral feldspars, 1 to 5 mm long, rare quartz (<5%) phenocrysts, 1 to 2 mm in diameter, and <5% brownish mafic mineral (amphibole?), 1 to 5 mm long. The matrix is medium grey and aphyric. The unit is pervasively weakly carbonatized (ankerite?) and it is weakly epidotized, mainly along fractures but also partially to totally replacing some feldspars. The epidote alteration seems to be weaker than previously. The interval is cut by 2 to 3% calcite-carbonate+/-quartz and tourmaline stringers, <5 mm thick and oriented from 5 to 50 deg.

1428 262.50 263.50 1.00 18 TRACE 208 TRACE 31 4 TRACE 1429 263.50 264.50 1.00 22 TRACE 321 2 31 5 TRACE 1430 264.50 266.00 1.50 16 TRACE 276 TRACE 30 4 TRACE 1431 266.00 267.50 1.50 12 TRACE 144 2 29 5 TRACE 1432 267.50 268.50 1.00 134 0.3 1167 TRACE 30 6 TRACE 1433 268.50 269.50 1.00 TRACE TRACE 185 TRACE 23 7 TRACE 1434 269.50 270.50 1.00 252 0.3 1394 TRACE 30 8 TRACE 1435 270.50 271.50 1.00 99 0.5 2395 2 30 20 TRACE 1436 271.50 273.00 1.50 68 0.3 871 TRACE 26 23 TRACE 1437 273.00 274.40 1.40 49 0.3 398 2 24 14 TRACE 1438 274.40 275.50 1.10 7 TRACE 178 TRACE 18 5 TRACE 1439 275.50 276.50 1.00 43 0.2 715 TRACE 23 9 TRACE 1440 276.50 270.00 1.50 14 TRACE 168 2 27 5 TRACE

No: CDR9932

Cameco Gold Inc.

DIAMOND DRILL LOG



FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM TO WIDTH Au (ppb)

ASSAYS

Ag (ppm) Cu (ppm) Pb (ppm) Zn (ppm) Mo (ppm) As (ppm)

TCA. Rarely, these stringers contain pyrite and minor 1441 278.00 279.50 1.50 43 0.3 987 3 29 8 TRACE chalcopyrite. Like previously, there are about 5% strongly 1442 279.50 280.90 1.40 12 TRACE 163 3 25 3 TRACE foliated zones (50 deg. TCA), which are moderately to strongly 1443 280.90 282.00 1.10 38 0.3 506 3 27 4 TRACE sericitized and weakly to moderately chloritized. These 2 cm to 1444 282.00 283.00 1.00 10 TRACE 453 3 24 6 TRACE 50 cm wide zones contain less than 1% pyrite. The core is still 1445 283.00 284.00 1.00 13 TRACE 219 TRACE 21 2 TRACE blocky from 262.5 to about 274.2 m (RQD<50), but after 274.2 m,

the RQD is higher than 90.

1446

1447 284.00

285.00

285.00

286.00

1.00

1.00

38

22

TRACE

TRACE

502

461

TRACE

TRACE

20

15

2

5

TRACE

TRACE 1448 286.00 287.00 1.00 26 TRACE 349 TRACE 25 2 TRACE

262.5-267.5: Weakly bleached (carbonatized) and epidotized 1449 287.00 288.50 1.50 26 TRACE 553 TRACE 25 3 TRACE interval, very blocky (RQD<50), with only traces of very fine 1450 288.50 290.00 1.50 29 TRACE 333 TRACE 25 3 TRACE grained pyrite. From 267.0-267.3 m, there is a finer grained,

feldspar porphyritic dykelet oriented sub-parallel TCA.

1451

1452

290.00

291.00

291.00

292.50

1.00

1.50

34

21

TRACE

TRACE

608

278

TRACE

TRACE 20

26

7

3

TRACE

TRACE 1453 292.50 294.00 1.50 6 TRACE 96 TRACE 30 3 TRACE

267.5 317.9 (Mineralized feldspar porphyry) 1454 294.00 295.50 1.50 16 TRACE 199 TRACE 27 2 TRACE Same as the main description, but in addition, the whole interval 1455 295.50 297.00 1.50 9 TRACE 152 TRACE 32 5 TRACE contains 1 to 2% disseminated and fracture controlled pyrite,

mixed with minor («0.5%) chalcopyrite. The sections with more

1456

1457

297.00

298.00 298.00

299.00

1.00

1.00

12

11 TRACE

TRACE

158

146

TRACE

TRACE

31

30

9

10

TRACE

TRACE sulphides are described below. In theses more sulphidic sections,

the pyrite and chalcopyrite are concentrated along thin fractures 1458

1459

299.00

300.00

300.00

300.60

1.00

0.60

40

22 TRACE

TRACE

519

303

TRACE

TRACE

30

29

4

1 TRACE

TRACE (< 5mm wide) oriented at 5 to 40 deg. TCA. The fractures have a 1460 300.60 302.00 1.40 30 TRACE 432 TRACE 28 3 TRACE vuggy texture and in addition to the sulphides they are filled 1461 302.00 303.50 1.50 14 TRACE 142 TRACE 31 3 TRACE with calcite, carbonate, epidote, chlorite and 1462 303.50 305.00 1.50 11 TRACE 172 TRACE 29 4 TRACE +/-anhydrite/gypsum. 1463 305.00 306.00 1.00 12 TRACE 193 TRACE 28 3 TRACE

1464 306.00 307.00 1.00 13 TRACE 163 TRACE 25 1 TRACE 267.5-267.7: Section with about 2 to 4% fracture controlled 1465 307.00 307.60 0.60 31 TRACE 243 TRACE 27 2 TRACE sulphides, mainly pyrite, but minor chalcopyrite (0.5-1%) is seen. 1466 307.60 308.60 1.00 23 TRACE 248 TRACE 28 3 TRACE

1467 308.60 309.10 0.50 42 TRACE 580 TRACE 31 5 TRACE 266.7-269.3: Finer grained, feldspar porphyritic dykelet, similar 1468 309.10 310.10 1.00 18 TRACE 444 TRACE 32 2 TRACE to 267.0-267.3 m. It is oriented sub-parallel TCA. 1469 310.10 311.00 0.90 6 TRACE 42 TRACE 33 3 TRACE

1470 311.00 312.00 1.00 22 TRACE 223 TRACE 26 3 TRACE

No: CDR9932

Cameco Gold Inc.

DIAMOND DRILL LOG




269.8-270.2: Interval containing about 5% fracture-controlled chalcopyrite and 1 to 2% pyrite.

270.8-271.15: Same as 269.8 to 270.2 m, 5% chalcopyrite, about 2% pyrite.

271.5-276.0: Interval containing at least 60% strongly foliated sections, 10 cm to 50 cm wide. These sections are moderately sericitized and chloritized and contains about 1% disseminated pyrite. Foliation at 50 deg. TCA. From 274.4 to 275.5 m, there is a fine grained feldspar porphyritic dykelet, similar to 267.0-267.3 m and oriented sub-parallel TCA.

277.0: 8-9 mm wide, quartz-calcite-carbonate stringer, with <1% disseminated chalcopyrite. It is oriented at 35 deg. TCA.

277.8: 8 mm thick, vuggy, calcite-quartz stringer, containing <1% disseminated chalcopyrite. The stringer is oriented at about 15 deg. TCA.

278.0-278.1: 5% fracture-controlled chalcopyrite and 1 to 2% pyrite.

278.6-279.0: 2% pyrite and 1 to 2% fracture-controlled chalcopyrite. Fractures are oriented at 5 to 10 deg. TCA. One quartz-calcite stringer, <'1 cm thick, contains 1 to 2% blebs of chalcopyrite. It is oriented at about 30 deg. TCA and crosscuts the mineralized epidote-chlorite-calcite-filled fractures.

279.5-280.9: Fine grained, feldspar porphyritic dyke, similar to

1471 312.00 313.20 1.20 TRACE TRACE 120 TRACE 30 5 TRACE 1472 313.20 314.20 1.00 24 TRACE 89 TRACE 27 8 TRACE 1473 314.20 315.40 1.20 39 TRACE 209 TRACE 31 3 TRACE 1474 315.40 316.30 0.90 11 TRACE 196 TRACE 51 2 TRACE 1475 316.30 317.90 1.60 20 TRACE 171 TRACE 32 2 TRACE

No: CDR9932

Cameco Gold Inc.

DIAMOND DRILL LOG




267.0 to 267.3 m. Sharp contacts at 55 deg. TCA. Weak fracture- controlled epidote alteration. Traces of disseminated pyrite.

280.9 286.0 (Foliated zone) Darker grey, foliated zone containing 1 to 3% disseminated pyrite and 0.5 to 1% disseminated chalcopyrite throughout. Minor tourmaline needles are seen in patches. The foliation is oriented at 40 deg. TCA. The section is moderately sericitized and carbonatized, and weakly to moderately chloritized. Feldspar phenocrysts are very diffuse or completely destroyed. Contacts with the less deformed porphyry are diffuse. There are about 2 to 3% white, calcite-carbonate+/-quartz stringers, <1.5 cm thick and oriented sub-parallel to foliation. Chalcopyrite blebs are often found within or near these stringers.

290.1-291.0: 5% disseminated and fracture controlled pyrite. Traces of chalcopyrite.

299.3-299.7: 3% pyrite and traces of chalcopyrite and molybdenum, mainly fracture controlled (vuggy epidote-calcite-quartz+-chlorite and anhydrite/gypsum).

300.6-302.0: Section showing 2 to 3% fracture controlled and disseminated pyrite associated with 1% chalcopyrite.

307.1-307.3: Section with 5% pyrite and traces of chalcopyrite.

307.3-307.6: Moderately sericitized, strongly foliated deformation zone. Weak chlorite. 1-2% disseminated pyrite and minor tourmaline.

No: CDR9932

Cameco Gold Inc.

DIAMOND DRILL LOG




313.2-314.2: Interval containing 50 to 60% strongly foliated, sericitized deformation zones, 5 cm to 20 cm wide. 1% disseminated pyrite and traces of chalcopyrite. Foliation is oriented at 50 to 60 deg. TCA.

315.4-316.3: Medium greenish grey, sedimentary interval (greywacke). The rock is composed of feldspar phyric sandstone interbedded with cherty mudstone, similar to the interval from 318.3 to EOH. 1% disseminated pyrite. Contacts are very sharp and oriented at 55 and 30 deg. TCA. Chilled margins are very thin (<1-2 mm) or absent. Could be a block in the porphyry?

316.3-316.45: Moderately foliated feldspar porphyritic section, weakly sericitized and moderately carbonatized. Foliation is oriented at 40 deg. TCA. 1-2% disseminated pyrite.

316.45-317.9: Weakly to moderately carbonatized feldspar porphyry, similar to main description. 1-2% disseminated pyrite and traces of chalcopyrite are seen. Feldspar are still 1 to 5 mm long (no grain size reduction).

317.9 318.3 (DEFORMATION ZONE) 1476 317.90 318.30 0.40 19 TRACE 203 TRACE 31 2 TRACE

Medium-dark green, strongly foliated, fine grained deformation zone. The foliation is oriented at about 50 deg. TCA. The rock is composed mainly of chlorite, with weak to moderate sericite, and about 20% calcite-carbonate+/-quartz stringers, <1.5 cm wide, oriented generally parallel to foliation, but also crosscuting it. The upper contact with the porphyry is very diffuse over 7 or 8

No: CDR9932

Cameco Gold Inc.

DIAMOND DRILL LOG




cm, where the feldspar phenocrysts gradually disappear. The lower

contact is also transitional over 2 or 3 cm. <1% very fine grained

disseminated pyrite is seen.

318.3 352.2 (VOLCANICLASTIC SANDSTONES AND MUDSTONES) 1477 318.30 319.30 1.00 5 TRACE 73 TRACE 31 3 TRACE

1478 319.30 320.30 1.00 15 TRACE 90 TRACE 33 3 TRACE Medium grey, competent (RQD>90), moderately hard, weakly magnetic, 1479 320.30 321.80 1.50 15 TRACE 55 TRACE 28 1 TRACE non foliated (well preserved), fine grained to pebbly sandstone 1480 321.80 323.30 1.50 15 TRACE 143 TRACE 31 4 TRACE interbedded with 20 to 30% laminated cherty mudstone beds. 1481 323.30 324.80 1.50 32 TRACE 108 TRACE 31 3 TRACE Bedding is oriented at 40 deg. TCA around 319.0 m, but it changes 1482 324.80 326.30 1.50 48 TRACE 164 TRACE 29 4 TRACE to about 10 deg. TCA below 332.5 m. It is hard to establish a 1483 326.30 327.80 1.50 9 TRACE 86 TRACE 30 2 TRACE facing direction, but it seems to be downhole (core angle are too 1484 327.80 328.80 1.00 14 TRACE 256 TRACE 29 4 TRACE low). Above 336.0 m (approximately) The beds are cut by 5% 1485 328.80 330.30 1.50 16 TRACE 112 TRACE 33 2 TRACE hairline thin siliceous fractures, with 2 to 5 mm epidotized halo. 1486 330.30 331.80 1.50 17 TRACE 208 TRACE 35 2 TRACE These fractures axe oriented in all directions and are crosscut by 1487 331.80 332.50 0.70 18 TRACE 178 TRACE 34 2 TRACE about 5% calcite-carbonate-quartz stringers, <5 mm thick and 1488 332.50 334.00 1.50 12 TRACE 86 TRACE 36 4 TRACE showing a 1 to 2 mm wide chloritized halo. These later stringers 1489 334.00 335.50 1.50 18 TRACE 168 TRACE 28 6 TRACE are present from 318.3 to EOH. Some sandstone beds contain up to 1490 335.50 337.00 1.50 TRACE TRACE 179 TRACE 23 5 14 5% white feldspar crystals 1 to 3 mm in size and some show rare 1491 337.00 338.50 1.50 TRACE TRACE 106 TRACE 28 2 TRACE feldspar porphyritic diffuse clasts 1 to 2 mm in size. The whole 1492 338.50 340.00 1.50 8 TRACE 79 TRACE 28 2 TRACE sedimentary interval contains about 1 to 2% very fine grained 1493 340.00 341.50 1.50 TRACE TRACE 53 TRACE 24 4 6 disseminated pyrite and about 1 to 2% additional pyrite and minor 1494 341.50 343.00 1.50 TRACE TRACE 98 4 47 3 TRACE pyrrhotite is seen concentrated along 1 to 3 mm thick laminae 1495 343.00 344.50 1.50 13 TRACE 407 3 35 10 17 within the cherty mudstone beds. Traces of chalcopyrite and

molybdenum are also seen locally in fractures.

320.4 332.5 (Feldspar porphyry)

Medium grey, weakly carbonatized and very weakly epidotized

(fracture controlled) feldspar porphyritic dyke, slightly

different from the main intrusion above. The dyke is composed of

No: CDR9932

Cameco Gold Inc.

DIAMOND DRILL LOG




30 to 40% weakly diffuse feldspar phenocrysts, 1 to 5 mm in size, <5% quartz crystals, < 2 mm in size, and about 15% of brownish amphiboles and/or mafic xenolith, usually less than 4 mm long, but some xenoliths are up to 2 cm long. There are still about 5% chloritized and sericitized deformation bands, <10 cm wide, containing about 1 to 2% pyrite and rare chalcopyrite. Foliation in those bands is oriented at about 50 deg. TCA. Upper and lower contacts with the sediments are sharp and oriented at 15 and 35 deg. TCA respectively. No significative chilled margins are seen. Very rare disseminated pyrite is seen from 320.4 to 327.8 m, but below 327.8 m, there are about 1% disseminated and fracture controlled pyrite and traces of chalcopyrite. Very often, the epidote-filled fractures have a darker chloritic halo. They are crosscut by less than 1% calcite-carbonate-quartz stringers, <5 mm wide.

352.2: EOH.

Whole rock samples:

CDR9932-A: 60.0-63.0 m: Epidotized diorite. CDR9932-H: 103.0-106.0 m: Epidotized Gabbro. CDR9932-C: 122.0-125.0 m: Epidotized finer grained gabbro. CDR9932-D: 130.0-133.3 m: Feldspar porphyry CDR9932-E: 168.0-171.0 m: Hornblende-feldspar porphyry. CDR9932-F: 185.0-168.0 m: Feldspar porphyry. CDR9932-G: 236.0-239.0 m: Relatively unaltered feldspar porphyry.

Representative samples:

No: CDR9932

Cameco Gold Inc.

DIAMOND DRILL LOG




59.9 m: Diorite.

91.0 m: Gabbro "cumulate"

104.8 m: Equigranular gabbro.

122.2 m: Finer grained epidotized gabbro.

133.1 m: Feldspar porphyry.

135.4 m: Aphyric feldspar porphyry facies.

140.5 m: Fine grained feldspar porphyritic facies.

168.45 m: Hornblende-feldspar porphyry.

234.5 m: Feldspar porphyry with chloritic zone.

350.8 m: Volcaniclastic sandstone and cherty mudstone.



30.50 -56.20

61.00 -57.40

91.46 -59.00

121.95 -59.40

152.44 -59.50

215.50 -59.50

246.00 -59.60

No: CDR9932

Cameco Gold Inc.

DIAMOND DRILL LOG



ASSAYS FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM TO WIDTH Au (ppb) Ag (ppm) Cu (ppm) Pb (ppm) En (ppm) Mb (ppm) As (ppm)


276.50 -59.70

307.00 -59.80

349.70 -58.00

No: CDR9932

Cameco Gold Inc.

DIAMOND DRILL LOG

PROPERTY: Cedar Rapids HOLE No.: CDR9933 Collar Eastings: 1297.00 Collar Inclination: -50.00 Logged by: D. Rabin

Collar Northings: 465.00 Hole Bearing: 230.00 Date: 09/09/99-11/09/99

Collar Elevation: 290.00 Final Depth: 276.50 metres Down-hole Survey: DIP METER/ACID TEST

Grid: Rotated

Val d'Or Drilling Core: NQ

Claim#: 5126394

Test soil geocheminal anomaly at felsic-mafic cont

FROM

0

TO

16.9

LITHOLOGICAL DESCRIPTION

(OVERBURDEN)

SAMPLE No. FROM TO WIDTH Au (ppb) ASSAYS


16.9 62.1 (DACITIC CRYSTAL TUFF/LAPILLI-TUFF) 1305 32.70 33.70 1.00 TRACE TRACE 20 TRACE 51 1 TRACE 1306 33.70 34.40 0.70 TRACE TRACE 8 TRACE 18 1 TRACE

Light to medium grey, very soft, strongly foliated, non magnetic 1307 34.40 35.40 1.00 TRACE TRACE 19 TRACE 64 1 TRACE

homogeneous felsic to intermediate cyrstal tuff interbedded with 1308 55.00 55.80 0.80 TRACE TRACE 20 TRACE 108 1 TRACE

crystal lapilli-tuff. The bed contacts are hard to see due to the 1309 55.80 56.90 1.10 TRACE 0 20 2 63 1 TRACE

blocky nature of the core (RQD <70). Foliation is generally 1310 56.90 57.70 0.80 9 0 83 3 56 1 TRACE oriented at 40 to 50 deg. TCA. The matrix and fragmets are 1311 57.70 58.10 0.40 TRACE 0 51 6 212 5 TRACE

strongly altered to pervasive sericite and ankerite. The matrix is also weakly altered to patchy and streaky chlorite. From 16.9

1312 58.10 59.10 1.00 TRACE TRACE 19 2 53 TRACE TRACE

to 32.2 m, there are about 10% oxidized intervals, 4 to 15 cm wide, which probably represent oxidation of the ankerite along fractures.

16.9-40.7: granular looking section composed mainly of crystal lapilli-tuff, made of fragments of sericitized and ankeritized feldspar crystals and aphyfic whitish flatted felsic? cleats, generally less than 5 mm long, some are up to 2 cm long by 5 mm wide. There is about 50% fragments and 50% matrix, but it is hard to define (rough estimate). Rare irregular pyrite blebs up to 1 cm in diameter are seen.

33.7-34.4: White, blocky , barren, quartz vein. Upper contact is blocky, while lower contact is sharp but undulates.

No: CDR9933

Cameco Gold Inc.

DIAMOND DRILL LOG PROPERTY: Cedar Rapids HOLE No.: CDR9933 Page 2

ASSAYS


SAMPLE No. FROM TO WIDTH Au (ppb) Ag (ppm) Cu (ppm) Pb (ppm) Zn (ppm) Mo (ppm) As (ppm)

40.7-55.0: More homogeneous, finer grained, crystal tuff section

composed of 5 to 20% sub-rounded quartz crystals, up to 4 mm in

diameter. No obvious fragments are visible and the matrix is very

fine grained and strongly altered to sericite, ankerite and weak

streaky chlorite. From 40.7 to about 46.3 m, the rock is more

heterogenous with darker more chloritic bands and patches. It may

represent a fragmental horizon (tuff-breccia), but it is hard to say.

55.0-62.1: Very heterogenous interval, still containing feldspar

and quartz crystals, but some sections appear to be fragmental in

nature and others are chloritic to graphitic. From 57.7 to 58.1,

the interval is dark grey-green and is strongly chloritic and may

be very weakly graphitic? It contains about 5% large pyrite cubes up to one centimeter in diameter. The contacts of this interval

are sharp and oriented parallel to foliation at 35 deg. TCA.

Another similar zone, without the pyrite cubes is seen from 59.9

to 60.2 m. From 61.0 to 62.1 m, the rock contains 10 to 20%

angular feldspar crystals, 1 to 3 mm in size and more visible

within the chloritic bands 1 to 3 cm wide (elastic texture?)

56.0-57.3: The interval is intruded by three, fractured, white

quartz veins, 10 to 20 cm wide. At 57.0 m, the edge of one quartz

vein contains few blebs of pyrite and chalcopyrite located in

fractures crosscutting the foliation and the quartz vein contact.

62.1 113.3 (DACITIC LAPILLI-TUFF)

Strongly foliated, blocky (RQD = 70 to 80), very homogeneous and

1313 79.70 80.70 1.00 TRACE TRACE 17 TRACE 56 2 TRACE 1314 80.70 81.30 0.60 5 TRACE 16 2 39 TRACE TRACE 1315 112.30 113.30 1.00 TRACE TRACE 20 3 57 1 TRACE

No: CDR9933

Cameco Gold Inc.

DIAMOND DRILL LOG



massive sequence of felsic to intermediate lapilli-tuff. Foliation is oriented generally at 50 to 55 deg. TCA. The upper contact with the previous unit is not well defined, but it is located around 60.0 to 62.1 m. The fragmental texture is define by the presence of <50% light grey flatten, oval shaped lenses and bands composed of <5% quartz crystals, 1 to 2 mm in diameter, floating in an aphyric, strongly sericitized and may be ankeritized matrix. The matrix between the clasts is dark grey, and is composed of <5% quartz crystals, 1 to 2 mm in diameter, floating in a strongly sericitized and chloritized aphyric groundmass. Only rare cubic pyrite, 1 to 3 mm in size, is seen in places.

80.7-81.3: Crowded, quartz-feldspar porphyritic dyke. Non magnetic and hard. Contacts are sharp and oriented parallel to foliation at 55 deg. TCA. It is composed of >50% diffuse pinkish feldspars and 10 to 20% angular to rounded quartz crystals up to 5 mm in size. The weakly foliated matrix is strongly sericitized and weakly chloritic. Traces of disseminated and fracture- controlled pyrite.

81.8-82.1: Same dyke as from 80.7-81.3 m.

82.5-84.4: Fold nose. The foliation becomes gradually parallel to core axis and it becomes very disturbed from 82.7 to 84.3, where it is parallel TCA. Regularly spaced kink bands 1 to 5 cm apart crosscut sub-perpendicularly the foliation at 45 deg. TCA. From 84.3 to 84.4 m, The rock is very soft and "creamy", which probably indicates a shear zone. On the other side of this shear, the foliation abruptly change back to its original angle (55 deg.

No: CDR9933

Cameco Gold Inc.

DIAMOND DRILL LOG


ASSAYS

FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM TO WIDTH Au (ppb) Ag (ppm) Cu (p(m) Pb (ppm) Zn (ppm) Mo (ppm) As (ppm)

TCA), but it seems oriented in the opposite direction.

88.0-88.8: Very fractured and disturbed section. Fault zone?

100.1-100.2: Similar dyke as from 80.7-81.3 m

108.5-110.6: Crowded porphyritic dyke identical to 80.7-81.3 m.

113.3 121.4 (GRAPHITIC ARGILLITE) 1316 113.30 114.30 1.00 TRACE TRACE 50 5 92 2 5

1317 114.30 116.00 1.70 TRACE TRACE 53 6 81 2 TRACE

Black, very soft, non magnetic, strongly foliated graphitic argillite. Upper and lower contacts are relatively sharp and oriented parallel to foliation generally at 45 deg. TCA. However, from 115.8 to about 116.7 m, the foliation is disturbed and oriented at 10 deg. TCA (fold?). 10 to 15% calcite+/-quartz seams are located along the foliation planes. They are generally less than 3 mm thick, but some are up to 1 cm thick. An intense cleavage is oriented sub-perpendicular to the foliation and produces small undulation of the foliation and the calcite seams. There is about 3-5% large pyrite cubes, averaging 5 mm in diameter (max = 2 cm in diameter). There is also 2 to 3% white, barren, quartz+/-calcite vein, oriented sub-parallel to foliation and ranging from <1 cm to 5 cm thick.

113.3-113.4: At the upper contact, there is About 10% pyrite cubes concentrated in a series of laminae < 5 mm thick. The interval is lighter grey and less graphitic than the rest of the unit.

121.4: The lower contact with the lapilli-tuff is occupied by a 1

cm wide gouge zone.

No: CDR9933

Cameco Gold Inc.



121.4 147.0 (DACITIC LAPILLI-TUFF) 1318 130.20 131.20 1.00 TRACE TRACE 21 3 54 1 TRACE 1319 131.20 132.30 1.10 TRACE TRACE 23 TRACE 72 3 TRACE

Individual sections described below. 1-2% white calcite-quartz- 1320 132.30 133.30 1.00 TRACE TRACE 24 TRACE 70 1 TRACE filled fractures, 1 to 5 mm wide, crosscut the foliation at 1321 133.30 134.60 1.30 TRACE TRACE 22 TRACE 58 1 TRACE various angles. Blocky core (RQD <80) 1322 134.60 135.60 1.00 11 TRACE 22 TRACE 61 1 TRACE

1323 135.60 136.80 1.20 TRACE TRACE 25 4 68 2 9 121.4-126.0: Quartz phyric lapilli-tuff very similar to 62.1-113.3 1324 136.80 137.80 1.00 TRACE TRACE 25 TRACE 47 1 TRACE m. Foliation oriented at 40 to 45 deg. TCA. 1325 137.80 139.00 1.20 TRACE TRACE 23 TRACE 42 2 7

1326 139.00 139.50 0.50 TRACE TRACE 21 TRACE 129 4 10 126.0-131.2: The lapilli-tuff becomes slightly more siliceous with 1327 139.50 140.50 1.00 5 0 26 5 68 2 16 lighter grey to buff quartz phyric clasts, and about 30 to 40% 1328 140.50 141.70 1.20 7 TRACE 23 3 65 2 9 darker, more chloritic clasts/matrix containing 10 to 30%, 1-2 mm 1329 141.70 142.70 1.00 5 TRACE 15 3 53 1 TRACE feldspar crystals. Some sections look like lapilli-stone (>70%

clasts). Still strong sericite and ankerite alteration. The

darker, feldspar phyric clasts? could represent metamorphosed

1330 145.90 146.90 1.00 TRACE TRACE 21 TRACE 57 2 TRACE

vitric clasts? Traces of disseminated pyrite.

131.2-132.3: Same lapilli-tuff as above, but most of the darker,

chloritic, feldspar phyric clasts become replaced by very fine grained pyrite. The pyrite content within those cleats varies from 1% to 80%. Overall, the section contains about 5% pyrite.

132.3-135.6: Still quartz and feldspar phyric fragmental section, but it looks more like a lapilli-atone. The upper and lower

contacts of this section are relatively sharp and parallel to foliation (45 deg. TCA)_

135.6-139.0: Same kind of lapilli-tuff as from 131.2 to 132.3 m,

with fine grained pyrite replacing the more chloritic cleats

No: CDR9933

Cameco Gold Inc.



averaging 4 cm in length and 1 cm in width. Overall this section contains possibly 10% pyrite (hard to evaluate), but the interval from 136.0 to 136.7 m, must contain at least 20% pyrite.

139.0-147.0: The lapilli-tuff sharply becomes darker in colour, very similar to 121.4-126.0 m. It is still quartz phyric (5-10%, 1-2 mm in size), and the clasts are strongly sericitized, floating in a more chloritic, but still sericitized fine grained matrix. Compared to 121.4-126.0 m, in this interval, the clasts are more diffuse and hard to see. The strong foliation outlined by the stretching of the clasts is oriented at 50 deg. TCA. The upper contact with the previous unit is sharp and oriented parallel to the foliation. There is less than 2% pyrite, generally as partial replacement of chloritic cleats, but also as fracture filling (exceptions are mentioned below).

139.5-139.55: Semi-massive pyrite horizon composed of about 50% massive, very fine grained, irregular pyrite "fragments" in a white quartz-calcite matrix. The horizon seems discontinuous and is oriented parallel to foliation. The pyrite "fragments" are generally less than 1 cm across, but some are up to 4 cm long. They are composed of very fine grained, dull, pyrite+/-chlorite goundmass and the clasts are outlined by very shiny, still fine grained, pyritic corona, less than 1 mm thick. The same shiny, probably recrystallized pyrite is also seen filling thin (<1 mm) fractures within the massive sulphide "clasts".

139.55-141.7: Interval containing between 5 and 10% very fine grained pyrite, as partial replacement of darker, more chloritic "clasts", similar to 135.6-139.0 m.

No: CDR9933

Cameco Gold Inc.


ASSAYS

FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM TO WIDTH Au (ppb) Ag (ppm) Cu (ppm) Pb (ppm) Zn (ppm) MO (ppm) As (ppm)

147.0 147.4 (MASSIVE PYRITE HORIZON)

1331 146.90 147.40 0.50 40 1 19 44 121 2 155

Very similar horizon as from 139.5-139.55 m, but this section

contains more than 70% pyrite. The clastic texture is less

obvious since the sulfide horizon is more massive. There is still a quartz-calcite matrix and shiny pyrite filling fractures and outlining pseudo-clasts. The contacts of this interval are sharp

and parallel to foliation, but there is about 15 to 25%

disseminated pyrite replacing more chloritic clasts over 2 to 5 cm within the host rock, on each side.

147.4 179.7 (GRAPHITIC ARGILLITE) 1332 147.40 148.40 1.00 8 TRACE 31 2 64 2 TRACE 1333 169.20 170.20 1.00 TRACE TRACE 59 3 90 2 12

Similar, black graphitic rock as from 113.3 to 121.4 m. The core 1334 170.20 170.60 0.40 7 TRACE 51 4 101 3 35 is not very blocky (RQD >90). There are about 5% pyrite cubes up 1335 170.60 171.60 1.00 5 TRACE 62 6 99 2 15 to 2 cm in size and about 5 to 10% calcite +/- quartz seams 1336 173.50 174.60 1.10 TRACE TRACE 48 8 76 2 31 parallel to foliation (45 deg. TCA). 1% late quart-calcite filled 1337 174.60 175.60 1.00 TRACE TRACE 42 9 91 2 28 fractures (<5 mm thick) crosscut the foliation at high angle (80 1338 175.60 177.10 1.50 TRACE TRACE 35 5 90 2 6 to 90 deg.). A strong cleavage crosscuts the foliation at about 1339 177.10 178.60 1.50 TRACE TRACE 35 5 96 2 36 30 to 40 deg. The unit is thinly "bedded" with slightly more 1340 178.60 179.60 1.00 TRACE 0 54 2 95 2 TRACE siliceous horizon alternating with more graphitic ones (1 to 5 cm

thick beds). The upper 2 metres appears to be more siliceous in

composition and the rock becomes gradually more graphitic

downhole. 1 to 2% white, barren, quartz-ankerite veins less than

3 cm wide, crosscut the foliation at various angles.

149.2-149.6: Shear zone. The graphitic horizon is intensely

foliated and contains more than 25% pulled-apart calcite-quartz

seams, < 7 mm thick. Foliation is still oriented at 45 deg. TCA

No: CDR9933

Cameco Gold Inc.

DIAMOND DRILL LOG


ASSAYS


and 5% coarse pyrite cubes are observed.

156.2-156.23: Disturbed gouge section oriented parallel to foliation.

162.1-162.3: Blocky section.

170.2-170.6: Laminated interval, slightly more felsic looking, with about 10 to 15% cubic pyrite, concentrated in horizons, 2 mm

to 1 cm thick, oriented parallel to foliation (40 to 45 deg. TCA.

The upper and lower contacts are relatively sharp and parallel to

foliatiion.

172.24-172.7: Very blocky section (RQD = 0). Could be a fault

zone?

173.5-178.6: The interval contains about 10% pyrite concentrated

in bands as from 170.2 to 170.6 m.

177.4-177.9: Blocky section where the foliation is very disturbed

(fault zone?)

179.3-179.7: Transitional lower contact where the graphitic

horizon becomes gradually lighter grey because of increasing

ankerite alteration. The ankerite is seen as <1 mm disseminated

euhedral specks and it is also associtated with the calcite seams

parallel to foliation.

179.7 196.0 (FOLIATED AND CARBONATIZED DACITIC TUFF?) 1341 179.60 180.10 0.50 TRACE TRACE 30 3 103 2 TRACE

1342 180.10 180.70 0.60 35 1 14 20 98 3 156

No: CDR9933

Cameco Gold Inc.

DIAMOND DRILL LOG


ASSAYS

FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM TO WIDTH Au (ppb) Aq (ppm) Cu (ppm) Pb (ppm) Zn (ppm) Mb (ppm) As (ppm)

Medium greenish grey, soft, strongly foliated, fine grained rock. 1343 180.70 181.40 0.70 TRACE TRACE 23 2 111 2 TRACE

Foliation is generally oriented at 50 deg. TCA, except when 1344 181.40 182.40 1.00 TRACE TRACE 22 TRACE 185 2 TRACE.

mentioned below. It is composed of 75% light grey, strongly carbonatized and sericitized laminae alternating with 25% dark grey, chloritic to possibly graphitic laminae, showing a weak to moderate carbonate alteration. Laminae are 1 mm to 1 cm thick. The carbonate (ankerite) is seen as aphyric groundmass and also as diffuse subhedral specks, < 1 mm in size. No quartz crystals are seen. The unit does not show any evident cleats, except from 189.2 to 190.1 m as mentioned below. It could be a tuffaceous or a massive intermediate to ultramafic rock? 1-2% ankerite-calcite stringers, < 5 mm thick, oritented parallel to foliation. They are crosscut by later ankerite-quartz veinlets, <5 mm thick, oriented sub-perpendicular to foliation at 45 to 80 deg. TCA. A strong cleavage is seen crosscutting the foliation at a 10 to 20 deg. angle (45 to 50 deg. TCA). Below 181.4 m, rare pyrite is seen, as thin (<1 mm thick) seams stretched along the foliation.

179.7-181.4: Mineralized zone. From 180.1 to 180.7 m, the interval shows two massive sulphide horizons, 10 and 30 cm wide. They are very similar to the one seen from 147.0 to 147.4 m (two kinds of pyrite within a quartz-carbonate matrix). The section in between contains about 5 to 10% disseminated and stringer pyrite. Overall this interval contains about 50 to 60% fine grained pyrite. From 179.7 to 180.1 m and from 180.7 to 181.4 m, the tuffaceous(?) rock contain, 2 to 5% disseminated and stringer fine grained pyrite, stretched along the foliation plane. The stringers are <5 mm thick. Sulphide content increases gradually towards the massive sulphide horizons.

No: CDR9933

Cameco Gold Inc.



184.2-185.3: Fold nose/deformation zone. At 184.2 m, there is a 2 cm very soft, chaotic section, probably representing a fault zone. Then the angle TCA of the foliation decrease suddenly to about 20 25 deg. and becomes gradually parallel TCA. It gradually changes back to 50 deg. around 185.3 m. Probably a fold nose.

189.2-190.0: The interval looks like a dacitic lapilli-tuff, very similar to previously. The medium grey "fragments" are harder than the more chloritic matrix and tiny quartz(?) crystals are visible. The "clasts" are 1 to 4 cm long and <5 mm to 2 cm wide. Contacts of this zone are undefined and appear transitional.

190.1-190.8: Blocky core.

193.1-194.0: Blocky section, 30 cm of lost core.

196.0 202.6 (CHERTY, GRAPHITIC ARGILLITE AND MAFIC TUFF?) 1345 196.50 198.00 1.50 TRACE TRACE 21 3 144 2 TRACE

1346 198.00 199.50 1.50 12 0 38 11 105 3 16

196.0-200.5: Dark grey to black, non magnetic, strongly foliated 1347 199.50 201.00 1.50 TRACE TRACE 24 TRACE 232 2 15

(45 deg. TCA) sedimentary rock. The interval is made of 60 to 70% 1348 201.00 202.60 1.60 TRACE 0 56 TRACE 114 2 TRACE

dark grey, very hard, cherty laminae, interbedded with 30 to 40% black, graphitic laminae. Laminae are usually less than 5 mm thick, but some are up to 2 or 3 cm thick. Upper and lower contacts are transitional and they are hard to locate with precision. 5% pyrite is seen as coarse cubes and as fine grained stringers, 1 to 5 mm wide,'oriented parallel to foliation. The core is relatively blocky (RQD < 70). 1-3% white quartz-carbonate veinlets, <1 cm wide, cross cut the foliation at 70 to 80 deg. TCA.

No: CDR9933

Cameco Gold Inc.



198.1-198.4: There are two semi-massive sulphide horizons, about 5 cm wide, oriented parallel to foliation. The section contains about 15-20% fine grained pyrite, similar to the zone described from 147.0 to 147.4 m.

200.5-202.6: Similar section as described from 179.7 to 196.0 m. There is about 5% pyrite seen as disseminated coarse cubes (up of 2 cm in size) and also as fine grained stringers, oriented parallel to foliation. A 5 cm wide, white, barren, quartz- carbonate vein, crosscuts the foliation at 202.5 m. It is oriented at about 30 deg. TCA.

202.6 212.1 (FOLIATED AND CAREONATIZED MAFIC ROCK)

202.6-212.3: Medium-dark grey, soft, strongly foliated, intensely carbonatized (mainly ankerite), fine grained mafic rock, looking alike the mafic tuffaceous rock described above. The main difference is that the rock is more evenly carbonatized and the more chloritic (graphitic) laminae are rare to absent. The rock matrix is pervasively and intensely altered to very fine grained carbonate and sericite, associated with moderate(?) chlorite. The interval is intruded by at least 20 to 35% carbonate (+1-quartz) veinlets oriented parallel to the foliation (45 deg. TCA.). The upper and lower contacts of this interval are transitional and hard to locate with precision (+/- 1 m?). Traces of pyrite as thin seams, parallel to foliation.

207.9-208.1: Chaotic and brecciated fault zone. The foliation and the carbonate veinlets are broken up in angular fragments averaging 1 cm in diameter. There is very little matrix, made

No: CDR9933

Cameco Gold Inc.



mainly of calcite. The contacts of the fault zone are relatively sharp and seems oriented parallel to foliation.

209.3-209.4: Fault zone similar to 207.9 to 208.1 m.

211.3: 2 cm wide brecciated band, similar to above.

211.4-211.6: The foliation becomes parallel to foliation (kink band?).

212.1 233.4 (DEFORMATION ZONE) 1349 215.00 216.50 1.50 5 0 53 2 105 2 8 1350 216.50 218.00 1.50 6 0 121 TRACE 58 3 9

212.1-212.4: Brecciated fault zone. Contacts seems parallel to 1351 227.00 228.50 1.50 5 0 95 TRACE 65 2 TRACE foliation, but it is hard to say. The matrix between the fragments appears to be composed mainly of chlorite and calcite.

1352 232.00 233.40 1.40 5 0 61 TRACE 47 2 21

212.4-233.4: Very blocky and weakly chaotic interval. The foliation is generally oriented at less than 20 deg. TCA. The rock is brownish grey, still fine grained, strongly foliated and very soft. It may represent a major deformation zone or a fold nose. It is intruded by pulled-apart, calcite-carbonate veinlets, often associated with bluish-grey quartz. There is about 2% pyrite, seen as anhedral dull blebs, 2 to 5 mm in diameter. From 212.4 to about 221 m, the core is not blocky and the foliation is well defined and parallel. Below 221.0 m, the core becomes blocky (RQD < 40), and the carbonate veinlets are going in several different directions. This section is intruded by about 5% white, barren, very irregular quartz-carbonate veins, up to 5 cm wide.

233.4 247.6 (FOLIATED AND CARBONATIZED ULTRAMAFIC ROCK)

1353 233.40 234.30 0.90 TRACE 0 80 TRACE 54 2 5

No: CDR9933

Cameco Gold Inc.

DIAMOND DRILL LOG




1354 234.30 235.30 1.00 TRACE 0 84 TRACE 55 2 8

More homogeneous, not blocky (RQD >95), non magnetic, fine grained, ultramafic interval moderately to strongly

1355 1356

235.30 236.50

236.50 237.30

1.20 0.80

TRACE TRACE

0 0

61 72

2 TRACE

51 51

TRACE 1

6 6

foliated at 50 deg. TCA. The rock is still intensely carbonatized 1357 237.30 239.00 1.70 32 0 333 TRACE 22 6 5

and moderately chloritized and sericitized (?). There is 10 to 1358 239.00 240.10 1.10 TRACE 0 81 2 54 TRACE 7

20% carbonate +/- quartz veinlets, < 1 cm thick, oriented parallel 1359 240.10 241.60 1.50 TRACE 0 75 TRACE 48 1 9

to foliation. Throughout the interval there is 2 to 3% 1360 241.60 243.10 1.50 TRACE 0 78 TRACE 46 TRACE TRACE

disseminated pyrite, < 1 mm in size. From 241.0 to 244.5 m and 1361 243.10 244.60 1.50 TRACE 0 238 TRACE 46 1 TRACE

from about 245.2 to 247.6 m, the foliation is weak and the 1362 244.60 246.10 1.50 TRACE 0 101 3 43 1 TRACE

carbonate veinlets are oriented in several directions. 1363 246.10 247.60 1.50 TRACE 0 99 2 44 TRACE TRACE

237.3-239.0: Medium grey, strongly foliated, moderately hard, quartz phyric, felsic dyke/tuff. The rock is composed of <5 to >20% angular quartz crystals, <1 to 3 mm in size, floating in an aphyric matrix, strongly sericitized, carbonatized and moderately chloritic. It contains about 3 to 5% pyrite, disseminated throughout and also within the foliation planes. No clastic texture was observed. The contacts are sharp and parallel to foliation at 55 deg. TCA. The first 3 cm at the upper contact is brecciated (small fault?). No chilled or cooked margins were seen.

238.0-239.0: 17 cm of lost core.

247.6 251.8 (QUARTZ-FELDSPAR PORPHYRY)

light grey, hard, non foliated, non magnetic, quartz-feldspar porphyritic dyke. It is composed of 25 to 35% white euhedral plagioclase crystals and about 15 to 20% angular to irregular quartz phenocrysts, both 1 to 5 mm in size. There is <1%

1364 247.60 248.80 1.20 TRACE TRACE 55 3 55 TRACE TRACE 1365 248.80 250.30 1.50 TRACE TRACE 22 3 54 TRACE TRACE 1366 250.30 251.80 1.50 TRACE TRACE 12 3 24 TRACE TRACE

No: CDR9933

Cameco Gold Inc.



disseminated cubic pyrite and about 5% white quartz veinlets oriented at less than 30 deg. TCA. The veinlets contain minor amount of chlorite, carbonate and rare pyrite. The dyke is weakly silicified near the quartz veinlet margins and the rest is weakly altered to sericite/carbonate? Contacts are very sharp and very irregular. From 248 to 248.25 m, there is a weakly foliated mafic to ultramafic section, similar to the description above (enclave).

251.8 276.5 (MASSIVE ULTRAMAFIC FLOW/SILL) 1367 251.80 253.30 1.50 TRACE 0 108 2 51 1 TRACE 1368 253.30 254.80 1.50 9 0 118 TRACE 46 1 TRACE

Very dark grey-green, very soft, weakly to non-foliated, massive 1369 254.80 255.60 0.80 47 TRACE 11 3 12 TRACE TRACE fine grained ultramafic rock. Probably a flow or a sill. The 1370 255.60 256.10 0.50 36 0 203 2 43 1 TRACE textureless matrix is strongly chloritic and moderately altered to 1371 256.10 257.60 1.50 TRACE 0 112 TRACE 46 1 TRACE anhedral ankerite specks, up to 2 mm in size. The interval is 1372 257.60 259.10 1.50 26 0 206 TRACE 45 2 TRACE. intruded by 10 to 20%, very irregular, discontinuous calcite- 1373 259.10 260.60 1.50 5 0 62 TRACE 53 3 TRACE carbonate (+/- quartz) stringers, <1 cm thick and oriented in all 1374 260.60 262.10 1.50 6 0 59 TRACE 49 TRACE TRACE directions. 2 to 3% pyrite is found mainly associated with the 1375 262.10 263.40 1.30 26 0 222 TRACE 51 1 TRACE calcite-carbonate veinlets, but there is also <1% pyrite which is 1376 263.40 263.90 0.50 61 TRACE 136 TRACE 20 TRACE TRACE disseminated throughout. Some of the calcite-carbonate veinlets 1377 263.90 265.40 1.50 TRACE 0 82 TRACE 39 2 TRACE contain up to 50% pyrite, <1 mm in size. Rare grey, irregular, 1378 265.40 266.90 1.50 TRACE 0 55 TRACE 38 2 TRACE discontinuous quartz veinlets, <3 cm wide. 1379 266.90 268.40 1.50 11 0 103 TRACE 37 4 TRACE

1380 268.40 269.90 1.50 TRACE 0 51 TRACE 37 TRACE TRACE 254.8-255.6: Quartz-feldspar porphyritic dyke similar to 247.6- 1381 269.90 271.40 1.50 26 TRACE 76 TRACE 31 TRACE TRACE 251.8 m. 1382 271.40 272.90 1.50 TRACE 0 57 TRACE 34 1 TRACE

1383 272.90 274.20 1.30 82 0 119 TRACE 36 TRACE TRACE 255.6-255.8, 263.4-263.9, 274.2-275.6: Medium grey, hard, weakly 1384 274.20 275.60 1.40 345 TRACE 321 TRACE 20 2 TRACE foliated, quartz physic felsic dykes, containing 5% disseminated and patchy, fine grained pyrite. 5-15% very diffuse, angular quartz crystals, 1 to 2 mm in size. <5% angular mafic specks

1385 275.60 276.50 0.90 10 0 146 TRACE 46 5 TRACE

(biotite or chlorite?), 2 to 3 mm in size. Contacts are very

No: CDR9933

Cameco Gold Inc.



sharp and irregular.

258.0-258.3, 268.1-268.8, 276.0-276.3: Blocky sections.

276.5: EOH

Whole Rock Samples:

CDR9933-A: 22.0-25.0: Sericitized and ankeritized dacitic crystal lapilli-tuff.

CDR9933-B: 51.0-54.0: Sericitized and ankeritized dacitic crystal Tuff.

CDR9933-C: 100.0-103.0: Sericitized and chloritized dacitic lapilli-tuff.

CDR9933-D: 143.0-145.0: Sericitized and chloritized dacitic lapilli-tuff.

CDR9933-E: 192.0-195.0: Carbonatized, intermediate/ultramafic tuff?

CDR9933-F: 208.0-211.0: Carbonatized, mafic to ultramafic rock. CDR9933-G: 252.0-255.0: Massive, carbonatized ultramafic rock.

Representative Samples:

25.4 m: Dacitic crystal lapilli-tuff. 52.4 m: Dacitic crystal tuff. 102.8 m: Dacitic lapilli-tuff. 144.3 m: Dacitic lapilli-tuff. 191.2 m: Carbonatized intermediate/ultramafic tuff?

No: CDR9933

Cameco Gold Inc.


ASSAYS

FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM TO WIDTH Au (ppb) Ag (ppm) Cu (ppm) Pb (ppm) En (ppm) Mo (ppm) As (ppm)

209.9 m: Carbonatized mafic to ultramafic rock. 252.3 m: Massive and carbonatized ultramafic rock with small

pyrite stringer.



17.10 -49.80

47.90 -49.80

78.40 -49.60

122.00 -50.00

183.00 -50.00

276.50 -50.00

No: CDR9933

Cameco Gold Inc.

DIAMOND DRILL LOG PROPERTY: Cedar Rapids HOLE No.: CDR9934

Collar Eastings: 1600.00 Collar Inclination: -55.00 Logged by: J. Samson Collar Northings: 875.00 Hole Bearing: 229.00 Date: 19/09/99-21/09/99 Collar Elevation: 290.00 Final Depth: 325.20 metres Down-hole Survey: DIP METER Grid: Rotated

Val d'Or Drilling Core: NQ Claim#: 5126360

Test the depth extension of the Dyke Zone


0 50.0 (OVERBURDEN)


Au re gt Au av gt Ag (ppm) Cu (ppm) Pb (ppm) Zn (ppm) Mb (ppm)

50.0 133.2 (VOLCANIC SANDSTONES, CONGLOMERATES AND MUDSTONES) 1504 94.00 95.00 1.00 24 N.A. 0.024 TRACE 160 2 31 2 1505 95.00 96.00 1.00 8 N.A. 0.008 TRACE 43 TRACE 21 TRACE

Medium grey to greenish grey volcaniclastic sediments, consisting 1506 96.00 97.00 1.00 150 N.A. 0.150 TRACE 261 3 29 2 of over 90% thickly bedded sandstone, 1-5 m thick, moderate to 1507 97.00 98.00 1.00 106 N.A. 0.106 TRACE 192 TRACE 31 2 poorly sorted, of intermediate composition, with feldspathic 1508 98.00 99.00 1.00 58 N.A. 0.058 0.2 427 TRACE 31 3 pebbles, and occasional lapilli size clasts, subrounded, increasing locally into conglomeratic beds, matrix supported.

1509 1510

99.00 100.50

100.50 101.60

1.50 1.10

23 17

N.A. N.A.

0.023 0.017

TRACE TRACE

102 84

TRACE TRACE

24 29

2 2

Minor <50cm thick mudstone intervals are also found. Apparent 1511 101.60 102.60 1.00 9 N.A. 0.009 TRACE 39 TRACE 30 TRACE bedding is defined by change in colour and grain size, and is 1512 102.60 103.60 1.00 TRACE N.A. TRACE TRACE 18 TRACE 29 2 subparallel to the foliation. It is locally graded and may 1513 103.60 104.60 1.00 22 N.A. 0.022 TRACE 177 2 20 1 display flame structures, suggesting top direction downhole (ie. 1514 104.60 105.60 1.00 90 N.A. 0.090 TRACE 979 2 34 TRACE 108.0m). Foliation is generally weak, at 45 deg. TCA. Core is 1515 105.60 106.70 1.10 28 N.A. 0.028 TRACE 100 TRACE 19 8 fairly massive, not blocky. Alteration is weak to calcite, and 1516 106.70 108.00 1.30 11 N.A. 0.011 TRACE 62 TRACE 15 5 chlorite, with mudstone beds preferentially sericitized. Quartz- 1517 108.00 109.40 1.40 7 N.A. 0.007 TRACE 107 TRACE 11 9 calcitetepidote stringers, 1-2%, <5mm, occur at all angles from 1518 109.40 109.75 0.35 248 N.A. 0.248 0.6 1995 3 28 167 subparallel to 65 deg. TCA.' Later quartz-calcitethematite 1519 109.75 110.75 1.00 102 N.A. 0.102 TRACE 648 TRACE 24 3 stringers are also found, 1%, within chloritized margins up 3 mm 1520 110.75 112.25 1.50 47 N.A. 0.047 TRACE 230 TRACE 24 4 wide. All stringers show disruptions, or weak folding. 1521 112.25 113.25 1.00 15 N.A. 0.015 TRACE 120 TRACE 25 7

Moderately magnetic where fine pyrhotite disseminations and blebs 1522 113.25 114.25 1.00 65 N.A. 0.065 TRACE 541 TRACE 22 18 are found, up to 1% locally. 1523 114.25 115.75 1.50 62 N.A. 0.062 TRACE 310 2 24 8

1524 115.75 117.25 1.50 12 N.A. 0.012 TRACE 99 TRACE 19 4 50.0-74.4: Monotonous sandstone interval. 1525 127.05 128.55 1.50 38 N.A. 0.038 TRACE 30 3 28 2

1526 128.55 129.65 1.10 21 N.A. 0.021 TRACE 104 TRACE 26 1

No: CDR9934

Cameco Gold Inc.

DIAMOND DRILL LOG




Au re gt Au av gt Ag (ppm) Cu (ppm) Pb (ppm) Zn (ppm) Mo (ppm)

64.4-64.0: Quartz-calcite-chlorite veinlet, 5cm wide, at 10 deg. 1527 129.65 130.20 0.55 6334 5.620 5.977 1.8 3188 3 26 3 TCA, barren. 1528 130.20 131.20 1.00 148 N.A. 0.148 TRACE 242 TRACE 19 4

1529 131.20 132.00 0.80 156 N.A. 0.156 TRACE 383 2 19 2 74.4-77.7: Polymictic conglomerate unit, with 5-25% subrounded 1530 132.00 132.50 0.50 1309 N.A. 1.309 0.8 2112 3 20 9 clasts, generally pebble-size. Approximately 40% of clasts are 1531 132.50 133.00 0.50 29 N.A. 0.029 TRACE 149 3 16 2 light grey and cherty, and 60% are greenish grey, of intermediate to felsic composition, occasionally biotite-phyric and probably intrusive. Matrix is similar to previously described sandstone beds.

77.7-94.0: Sandstone is somewhat better sorted and fine grained, locally grading into mudstone. Weak to moderately chloritic locally, with minor carbonatization (calcite). Quartz-calcite stringers, and later quartz-calcite-biotite-chlorite stringers, at all angles, 1-2%. Pyrite and pyrrhotite 0.5%, disseminated to stringers, with trace chalcopyrite.

80.8-81.1: Pyrrhotite 1% and trace chalcopyrite, in close association with quartz-calcite blebs and patches (like nodules, ie.81.0m). Pyrite <1% disseminated.

94.0 115.8 (Weak to Moderate Altered/Mineralized Zone) Interval consists of sandstone, with <5% argillaceous intervals, <30cm wide. Locally weak to moderate epidote and chlorite-calcite alteration, accompanied by disseminated to stringer biotite. Quartz-calcitetepidote-chlorite stringers and veinlets, 3 to 4%, at various angles. Pyrite, chalcopyrite, and pyrrhotite stringers and wisps, 1 to 3%.

94.0-95.0: One cm wide quartz-calcite stringer, disrupted, at 10

No: CDR9934

Cameco Gold Inc.

DIAMOND DRILL LOG



ASSAYS FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM TO WIDTH Au (ppb) Au re gt Au av gt Ag (ppm) Cu (ppm) Pb (ppm) Zn (ppm) Mb (ppm)

deg. TCA, accompanied by 1 to 5cm wide epidote-biotite-calcite margins. Fine pyrite and pyrrhotite wisps and blebs and occasional stringers, at all angles TCA, 2% locally, 1% overall.

95.0-96.0: Disseminated to stringer pyrrhotite and minor pyrite, 1 to 2%.

96.0-99.0: Chlorite and epidote alteration pervasive, weak to locally strong. Notably, biotite disseminations to stringers and wisps are common, parallel to the moderate foliation, at 35 to 40 deg. TCA. Quartz-calcitetepidote-chlorite stringers and veinlets are crosscutting, disrupted. Pyrrhotite, pyrite and trace chalcopyrite up to 3% locally, 1 to 2% overall, occur as disseminations, seams and stringers, often crosscutting foliation.

99.0-102.6: Mineralization and alteration decreases to very weak, with <1% pyrrhotite and pyrite. Quartz and carbonate stringers <1%. Biotite is very minor.

102.6-108.0: Epidote alteration is very weak, with moderate chloritization locally. Quartz-calcite-epidote stringers and later quartz-calcitetchlorite stringers are hairthin, 1-3%, at all angles. Up to 2% pyrite and 0.5% chalcopyrite and lesser pyrrhotite occur mostly as seams and stringers at 45 to 90 deg. TCA, often crosscutting foliation. Notably, chalcopyrite is mostly in association with the quartz and carbonate stringers.

108.0-108.4: Apparent bedding parallel to foliation, at 48 deg. TCA.

No: CDR9934

Cameco Gold Inc.

DIAMOND DRILL LOG



ASSAYS FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM TO WIDTH Au (ppb) Au re gt Au av gt Ag (ppm) Cu (ppm) Pb (ppm) Zn (ppm) Mo (ppm)

108.0-109.4: Pyrite <1%, with trace chalcopyrite.

109.4-109.8: Moderately sericitic mudstone, with a 10cm wide quartz-calcite-chlorite-epidote stringer band, at 45 deg. TCA, with 2% pyrite and chalcopyrite patches and seams.

109.8-112.3: Epidote alteration weak, in association with 1-3% quartz-calcite-epidote stringers, diffuse and parallel to the weak foliation at 45 deg. TCA. Mineralization <1%.

112.3-115.8: Epidote decreases from very weak, and is only observed within the quartz and carbonate stringers, <1%. Pyrite wisps and seams 1%.

115.8-117.8: Polymictic conglomerate unit, as previously described, with lapilli-size subrounded clasts. Approximately 50% are light grey to medium grey, cherty, of probable sedimentary origin, whereas the rest appears felsic and varies from aphyric to feldspar phyric. Unit is matrix supported, light grey, relatively unaltered. Quartz-calcitetepidote stringers <1%, disrupted, at all angles. Pyrite <1% disseminated.

117.8-128.6: Monotonous sequence of sandstone, moderately sorted, pebbly, as previously described. Less than 10% conglomeratic intervals, <lm wide. Apparent bedding parallel to weak foliation at 46 deg. TCA.. Weak to moderate carbonatization (calcite), and weak sericite and chlorite alteration.

128.6 133.2 (Altered/Mineralized Contact Zone)

No: CDR9934

Cameco Gold Inc.



ASSAYS

FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM TO WIDTH Au (ppb) Au re gt Au av gt Ag (ppm) Cu (ppm) Pb (ppm) Zn (ppm) Mo (ppm)

Pebbly sandstone to mudstone, as previously described, weakly

bleached by silicification and weak sericitization, in apparent

contact near 132.50m with an intermediate feldspar-porphyry dyke,

moderately sheared. Pyrite and chalcopyrite (ratio 70:30) wisps and seams, scattered throughout, 4-5% locally, 2% overall,

subparallel to foliation, locally cross-cutting it. The sulphides

are closely associated with quartz-calctie-chlorite seams, as

fracture infillings. Foliation/schistosity weak to moderate, at 45 deg. TCA.

131.3-131.6: Ground core.

132.0-132.5: Cherty/silicified mudstone, sheared, broken core,

accompanied by narrow mudseam pyrite-chalcopyrite (ratio 95:5) 4 to 5%. Probable contact with underlying unit.

132.5-133.0: Quartz-phyric phase to the underlying feldspar-

porphyry(?). Moderately sheared, near 40 deg. TCA. Displays

diffuse mineralogy of fine quartz, chlorite, sericite, schistose,

with apparent fine quartz phenocrysts(?) still visible. Weakly

blocky core. Includes only one 2cm wide quartz vein, barren.

Coarse pyrite cubes, 3-4mm, recrystallized, disseminated, 1%, and

fine pyrite seams parallel to schistosity, 1%.

133.0-133.2: White quartz-chlorite-tourmaline vein, with minor

calcite, trace ankerite, at 50 deg. TCA. Pyrite disseminations

and seams, 1%.

133.2 135.0 (INTERMEDIATE FELDSPAR PORPHYRY)

1532 133.00 134.00 1.00 228 N.A. 0.228 TRACE 36 3 17 2

No: CDR9934

Cameco Gold Inc.




1533 134.00 135.00 1.00 35 N.A. 0.035 TRACE 31 3 17 TRACE Greenish grey feldspar porphyry, moderately sheared to weakly

foliated downhole. Lower contact sharp at 46 deg. TCA. Contains

over 60% greenish white feldspar phenocrysts, averaging 1.5mm,

weakly to moderately saussuritized, within a fine grained greyish

groundmass of intermediate composition, weakly chloritic to

sericitic. Occasional mafic xenoliths. Quartz-calcite stringers

<1%. Pyrite 0.5%.

133.2-134.0: Moderately sheared, locally sericitic along discrete

shear planes, at 47 deg. TCA. Feldspar phenocrysts are weakly

epidotized, to strongly saussuritized. Fine pyrite disseminations

and seams, 1%, decreasing rapidly downhole.

135.0 212.5 (VOLCANIC SANDSTONE TO CONGLOMERATE, MINOR MUDSTONE)

Interval consists of volcaniclastic sediments similar to the unit

previously described and located between 50.0-133.2m.

135.0-147.0: Monotonous and massive section of sandstone to pebbly sandstone, thickly beded. Quartz-calcitetepidote stringers <1%,

at all angles, disrupted. Alteration and foliation very weak, at

52 deg. TCA. Fine disseminated biotite, <lmm in diameter, is

locally disseminated within the matrix of the sediments, up to 15%

locally. Pyrite 1%, fine disseminated to seams and wisps, mostly

parallel to foliation, and closely associated with chloritic

fracture infillings.

135.0-138.0: Preferential weak epidote alteration of the felsic

1534 135.00 136.50 1.50 8 N.A. 0.008 TRACE 45 3 26 TRACE 1535 136.50 138.00 1.50 10 N.A. 0.010 TRACE 52 3 27 TRACE 1536 147.00 148.50 1.50 TRACE N.A. TRACE TRACE 7 TRACE 16 2 1537 148.50 150.00 1.50 38 N.A. 0.038 TRACE 3 TRACE 17 1 1538 150.00 151.00 1.00 369 N.A. 0.369 0.9 2036 3 24 98 1539 151.00 152.00 1.00 1988 N.A. 1.988 3.4 6506 3 29 45 1540 152.00 153.35 1.35 474 N.A. 0.474 0.7 1459 3 23 7 1541 153.35 154.50 1.15 73 N.A. 0.073 TRACE 19 TRACE 21 2 1542 154.50 156.00 1.50 9 N.A. 0.009 TRACE 11 TRACE 21 2 1543 156.00 157.50 1.50 14 N.A. 0.014 TRACE 5 TRACE 22 3 1544 166.00 167.30 1.30 38 N.A. 0.038 TRACE 113 2 46 2 1545 167.30 167.55 0.25 TRACE N.A. TRACE TRACE 34 3 36 TRACE 1546 167.55 168.80 1.25 82 N.A. 0.082 TRACE 414 TRACE 26 3 1547 168.80 170.10 1.30 TRACE N.A. TRACE TRACE 62 3 25 TRACE 1548 186.70 187.30 0.60 TRACE N.A. TRACE 0.2 52 2 20 1

No: CDR9934

Cameco Gold Inc.


HOLE No.: CDR9934 Page


pebbles, generally decreasing downhole. Matrix is weakly 1549 211.00 212.50 1.50 8 N.A. 0.008 TRACE 69 2 28 1 chloritic, giving the rock a mafic appearance.

146.3-146.5: Laminated cherty mudstone, at 45 to 46 deg. TCA.

Pyrrhotite wisps 1%, and trace pyrite.

147.0 154.5 (Weak to Moderate Altered/Mineralized Zone)

Sandstone, and 5% narrow intervals of cherty mudstone, less than

30cm wide. Rock shows weak silicification and carbonate

alteration (mostly calcite), and contains radiating to acicular

green and vitrous needles locally, up to 5%, possibly actinolite.

Minor fine biotite is visible locally as well (<0.5%). The

interval is characterized by the presence of epidote-calcite-

quartz stringers and "balls" or pseudonodules, generally less than

lcm across, scattered throughout the interval, up to 15% locally,

3-4% overall, mostly in association with the cherty mudstone

beds. Weakly chloritic to sericitic. Quartz-calcitetepidote-

chlorite stringers and bands, 2%, at various angles. Pyrite is

less than 1%, but increases up to 2-3% between 150.00m to 153.35, and is accompanied in that interval with about 1% chalcopyrite. The sulphides occur as stringers, seams and wisps, in close

association with calcite-quartz-chlorite, as fracture infillings,

at various angles often cross-cutting the foliation. Foliation

weak to moderate at 45 deg. TCA.

154.5-157.0: Sandstone, locally laminated, to cherty mudstone,

similar to the interval above, but with much less mineralization.

Calcite-quartz-epidote "nodules" still locally present. Pyrite

disseminations, seams and blebs, 1% overall.

No: CDR9934

Cameco Gold Inc.




157.0-163.5: Thick sandstone bed, weakly pebbly, relatively

unaltered. Quartz-calcite-epidote stringers and bands, 1 to 2%, at various angles up to subparallel TCA. Pyrite <1%, as

disseminations and occasional stringers.

163.5-167.3: Polymictic conglomerate, grading downhole into pebbly

sandstone. Clasts are pebble to cobble-size, 50%, matrix

supported, subrounded to subangular, greenish white, medium to fine grained, intermediate to felsic, most with discernible fine

feldspar phenocrysts, other with minor mafic phenocrysts

(chloritized), and may be of intrusive origin. Less than 5%

appear to be of sedimentary to mafic volcanic origin. Quartz-

calcitettourmaline(?) stringers, 1 to 2%, at various angles. Pyrite 1% wisps and disseminations.

166.0-167.3: Weak epidotization of the matrix, increasing to

moderate downhole, near contact with mafic dykelet. Alteration is

accompanied by increase in fine disseminated to wispy pyrite, 2%

locally.

167.3-167.6: Mafic Dykelet

Upper and lower contacts sharp at 64 deg. TCA. Dark grey, fine

grained, non magnetic, massive and essentially non-foliated. Less

than 1% very fine feldspar(?) phenocrysts discernible, pinkish

white, <1mm, possibly hematized. Weakly chloritic, moderately

carbonatized (calcite). Contains dusty greyish black mineral,

possibly very fine biotite (see thin-section). Contains <1%

disseminated dusty pyrite. Quartz-calcite stringers <1%, hairthin.

No: CDR9934

Cameco Gold Inc.




167.6-170.1: Sandstone(?), very homogenous, <1% pebbles, dark

green over most of interval, moderately chloritized, weak epidote

alteration patches. Displays fine black minerals disseminations,

probably fine biotite. Pyrite fine disseminated to occasional wisps and stringers, 1-2% overall.

170.1-212.5: Sandstone to conglomerate.

Interval consists of a thick sequence of bedded sandstone to

pebbly sandstone (70%), locally grading into polymictic

conglomerate. Beds vary in thickness from 2m down to laminations,

and generally fine downhole (ie. 189.1m), and are subparallel TCA

at 50 to 55 TCA. The pebbles and cobbles which increase up to 50% within the conglomerate, are similar to previous descriptions,

with subrounded intermediate to felsic clasts, greenish grey, with

chloritic mafic phenocrysts (probably intrusive), some with fine

feldspar phenocrysts, others aphyric. About 25% of the clasts are

cherty grey to ghostly grey (hard to distinguish from the matrix),

like strongly bleached mafic clasts. The matrix is light greenish

grey, and the rock appears moderately bleached. It is moderately

carbonatized by calcite, and is weakly sericitic. Quartz-

calcitetepidote-chlorite stringers are less than 3%, at various

angles, often disrupted, infilling fractures often subparallel

TCA. Foliation is weak at 50 deg. TCA. Pyrite <1% fine

disseminated to occasional wisps and stringers.

186.7 187.3 (Fault/Sheared to Brecciated Core)

Rock is strongly sheared at 44 deg. TCA.. Brecciated to gouged

core locally. Moderately sericitized and weakly chloritic,

schistose. Quartz-calcite stringers 4%, barren. Pyrite <1%.

No: CDR9934

Cameco Gold Inc.

DIAMOND DRILL LOG




212.5 258.3 (MODERATELY ALTERED VOLCANICLASTIC ROCK) 1550 212.50 214.00 1.50 49 N.A. 0.049 TRACE 158 2 31 2 1551 214.00 215.50 1.50 174 N.A. 0.174 TRACE 212 2 43 2

Interval consists of interbedded volcaniclastic sandstone to 1552 215.50 217.00 1.50 281 N.A. 0.281 TRACE 87 TRACE 33 2 pebbly sandstone (95%), with minor conglomeratic units, and 1553 217.00 218.50 1.50 55 N.A. 0.055 TRACE 19 TRACE 29 2 occasional mudstone laminae. Notably, the interval is relatively 1554 218.50 220.00 1.50 195 N.A. 0.195 TRACE 42 TRACE 30 5 darker green as a result of weak to locally strong chloritization, 1555 220.00 221.50 1.50 70 N.A. 0.070 TRACE 7 TRACE 26 1 and weak patchy epidotization.. Carbonatization by calcite is 1556 221.50 222.75 1.25 85 N.A. 0.085 TRACE 24 TRACE 36 2 moderate, and is expressed by moderate bleaching in places. 1557 222.75 224.25 1.50 TRACE N.A. TRACE TRACE 2 TRACE 35 1 Sericitization is confined to the mudstone or argillaceous 1558 224.25 225.15 0.90 TRACE N.A. TRACE TRACE 19 TRACE 26 2 laminations. A fine black mineral, most likely biotite, varies 1559 225.15 226.65 1.50 10 N.A. 0.010 TRACE 9 TRACE 39 2 from <1% to 2-3% locally, as fine disseminations to wisps parallel 1560 226.65 227.60 0.95 95 N.A. 0.095 TRACE 5 TRACE 29 1 to foliation. The foliation is weak to moderate, at 54 deg. TCA. 1561 227.60 228.40 0.80 42 N.A. 0.042 TRACE 6 TRACE 31 2 Quartz-calcitetepidote and trace hematite, 2 to 3%, at all angles. 1562 228.40 228.90 0.50 74 N.A. 0.074 TRACE 4 TRACE 30 1 Rock is non-magnetic. Pyrite varies from <1% to 10% locally, 2% 1563 228.90 230.00 1.10 61 N.A. 0.061 TRACE 5 TRACE 30 TRACE overall, as disseminations to wispy stringers closely associated 1564 230.00 231.00 1.00 44 N.A. 0.044 TRACE 4 TRACE 33 2 with the quartz-calcite-chlorite stringers, and sometimes 1565 231.00 232.00 1.00 35 N.A. 0.035 TRACE 4 TRACE 35 2 crosscutting the foliation as fracture infillings. 1566 232.00 233.00 1.00 16 N.A. 0.016 TRACE 4 TRACE 33 2

1567 233.00 234.00 1.00 30 N.A. 0.030 TRACE 2 TRACE 19 1 212.5-218.5: Very weak and gradual increase in chloritization, 1568 234.00 235.00 1.00 51 N.A. 0.051 TRACE 2 TRACE 26 2 accompanied by very weak saussuritization/epidotization of the 1569 235.00 236.00 1.00 176 N.A. 0.176 TRACE 1 TRACE 34 1 feldspathic material within the sediments. Pyrite 1-3%, 2% 1570 236.00 237.00 1.00 6588 6.250 6.419 TRACE 3 TRACE 33 1 overall. 1571 237.00 238.50 1.50 16 N.A. 0.016 TRACE 4 TRACE 37 TRACE

1572 238.50 240.00 1.50 TRACE N.A. TRACE TRACE 2 TRACE 42 1 218.5-222.8: Weak pervasive epidotization. Pyrite 1%. 1573 240.00 241.50 1.50 TRACE N.A. TRACE TRACE 43 TRACE 46 1

1574 241.50 243.00 1.50 38 N.A. 0.038 TRACE 53 TRACE 43 TRACE 222.8-224.3: Vuggy quartz-calcite-epidote stringers and veinlets, 1575 243.00 244.50 1.50 TRACE N.A. TRACE TRACE 21 TRACE 41 2 3%. Pyrite <1% disseminated. 1576 244.50 246.00 1.50 TRACE N.A. TRACE TRACE 20 TRACE 46 TRACE

1577 246.00 247.50 1.50 27 N.A. 0.027 TRACE 35 TRACE 45 1

No: CDR9934

Cameco Gold Inc.




Au re gt Au av gt Ag (ppm) Cu (ppm) Pb (ppm) Zn (ppm) Mo (ppm)

224.3-225.2: Weakly chloritized, very weakly epidotized, similar 1578 247.50 249.00 1.50 17 N.A. 0.017 TRACE 91 TRACE 45 2 to 212.50 to 222.75. Pyrite <1% disseminated to wisps. Biotite 1579 249.00 250.50 1.50 33 N.A. 0.033 TRACE 100 TRACE 61 TRACE disseminations and wisps locally visible. 1580 250.50 252.00 1.50 16 N.A. 0.016 TRACE 207 TRACE 51 1

1581 252.00 253.50 1.50 78 N.A. 0.078 TRACE 231 TRACE 48 TRACE 225.2-226.7: Moderate and pervasive epidote alteration, starts and 1582 253.50 255.00 1.50 32 N.A. 0.032 TRACE 118 TRACE 55 2 ends abruptly, but interval displays apparent bedding (sandstone 1583 255.00 256.50 1.50 12 N.A. 0.012 TRACE 66 TRACE 76 1 to pebbly sandstone) indicating it is not a dyke. Fine black 1584 256.50 257.50 1.00 TRACE N.A. TRACE TRACE 25 TRACE 46 1 mineral is scattered throughout, up to 10%, most likely chloritic 1585 257.50 258.30 0.80 18 N.A. 0.018 TRACE 99 TRACE 50 1 biotite (see photo by P. Code, and thin-section). Pyrite 1%, fine disseminations to cubes aver. 2mm across. Pyrite also occurs in association with a quartz-calcite-biotite stringer at 35 deg. TCA, crosscutting foliation.

226.7 238.5 (Moderately Mineralized Interval) Pyrite 2 to 10%, 3-4% overall, fine disseminated to wisps and wispy stringers. Alteration as previously described, with weak to moderate chloritization, patchy bleaching by calcite and weak epidotization.

226.7-227.6: Pyrite up to 10%, 5% overall.

227.6-228.4: Pyrite 2%.

228.4-233.0: Pyrite 3-4% overall. Bleaching by calcite, in association with weakly vuggy quartz-calcite-chlorite bands and stringers, 3-4%.

233.0-238.5: Pyrite 1-2%. Weak hematization preferentially along minor sericitic mudstone laminations. Epidote is weak, occurring as occasional "balls" as previously described.

No: CDR9934

Cameco Gold Inc.




238.5-258.3: As previously described, moderately chloritic, with

very weak patchy epidotization. Fine biotite is still scattered

throughout. Calcite alteration is moderate and pervasive.

Quartz-calcitetepidote-chlorite stringers 1-2%, at all angles.

Foliation is weak to moderate at 55 deg. TCA. Pyrite <1% overall,

with occasional stringers in association with quartz and calcite-

chlorite seams.

256.5-258.3: No change in alteration nearing contact with porphyry. Foliation still moderate at 57 deg. TCA. Pyrite <1% disseminated. Quartz-calcite stringers <1%.

258.3 294.8 (INTERMEDIATE QUARTZ-FELDSPAR PORPHYRY) 1566 258.30 259.00 0.70 59 N.A. 0.059 TRACE 119 TRACE 36 1 1587 259.00 259.80 0.80 93 N.A. 0.093 TRACE 121 TRACE 45 1

Medium grey, non magnetic, intermediate quartz-feldspar porphyry 1586 259.80 260.50 0.70 TRACE N.A. TRACE TRACE 19 TRACE 47 1 dyke or sill. The feldspar phenocrysts vary from 50 to 75%, are 1589 260.50 262.00 1.50 9 N.A. 0.009 TRACE 46 TRACE 47 2 euhedral to subhedral, aver. 1.5mm, are yellowish white and weakly 1590 291.25 292.75 1.50 TRACE N.A. TRACE TRACE 7 TRACE 50 2 saussuritized to locally green and pervasively epidotitzed. The 1591 292.75 293.75 1.00 TRACE N.A. TRACE TRACE 3 TRACE 46 1 quartz phenocrysts are grey, aver. lmm, are subangular, are only

locally developed and appear to be inversely proportional to the

feldspar phenocrysts. They are contained within a grey groundmass

1592 293.75 294.75 1.00 TRACE N.A. TRACE TRACE 22 TRACE 41 4

of fine quartz, feldspar, <3% chloritized mafic minerals, and

other accessory minerals (epidote, carbonate, sericite). Overall,

alteration is weak to moderate by pervasive calcite, accompanied

by weak local sericite, chlorite, and epidote. Foliation is

mostly weak at 50 deg. TCA. Fine grained mafic to argillaceous

xenoliths are common, lapilli-size, approximately 2-3%. Quartz-

No: CDR9934

Cameco Gold Inc.




calcitetepidote-chlorite stringers at all angles, 1%. Pyrite <1% fine disseminated.

258.3-259.8: Cloudy, greenish grey and weakly to moderately chloritic, moderately carbonatized. Moderately foliated at 56 deg. TCA. Mineralized with about 2% finely disseminated pyrite and trace chalcopyrite. Very minor wispy sulphides in association with chlorite fracture infillings. Upper contact with volcaniclastic sediments is sharp, at 50 deg. TCA.

270.4: One 2-3mm quartz-calcite stringer, at 35 deg. TCA, contains <1% pyrite and two specks of chalcopyrite.

292.8-294.8: Porphyry gradually becomes predominantly quartz- phyric dowhnole, and is accomapanied by a gradual increase in finely disseminated pyrite, from <1% to over 1%, with the occurrence of a trace wispy stringers. Foliation is moderate at 70 deg. TCA. Lower contact between porphyry and sediments is sharp at 65 deg. TCA.

294.8 325.2 (POLYMICTIC VOLCANICLASTIC CONGLOMERATE)

Unit consists of a monotonous sequence of polymictic conglomerate as previously described. The rock contains 50 to 60% clasts of pebble to cobble size, weakly flattened, average width around 3 cm, with a maximum size up . to 8cm. The clasts are yellowish white to ghostly grey, and appear to be of intermediate to felsic composition, others appear to be sedimentary, and minor ones are probably of mafic volcanic origin. The clasts are supported by a pebbly sandstone matrix similar to that previously described

1593 294.75 296.00 1.25 TRACE N.A. TRACE TRACE 87 TRACE 55 2 1594 296.00 297.50 1.50 TRACE N.A. TRACE TRACE 37 TRACE 53 2

No: CDR9934

Cameco Gold Inc.




further uphole. Alteration is generally weak by chlorite and carbonate, but is sufficient to give the rock a greyish green color similar to a bleached mafic volcanic. Epidote is very minor, and occurs as weak patches, often preferentially altering felsic cleats, or along the margins to some quartz-carbonate stringers. Foliation is weak to moderate at 60 to 65 deg. TCA. Quartz-calcitefchlorite-epidote stringers, <1%, very irregular, diffuse. Pyrite occurs as very fine disseminations and occasional wisps and stringers, <1%.

294.8-296.0: No notable changes in alteration or schistosity. Pyrite <1% fine disseminated, and trace of chalcopyrite specks.

310.7-310.9: Quartz-calcite-hematite-chlorite veinlets and stringers, 40%, at 45 deg. TCA. Wallrock is chloritized, and contains leucoxene. Pyrite blebs and disseminations 1%.

318.0-325.2: Weak but gradual increase in chlorite alteration, locally moderate. Rock is weakly schistose, at 60 deg. TCA.

325.2: EOH.

Whole rock samples:

CDR9934-A: 133.2-135.0: Intermediate feldspar porphyry. CDR9934-H: 260.0-263.0: Intermediate quartz-feldspar porphyry. CDR9934-C: 289.0-291.0: Intermediate quartz-feldspar porphyry.


No: CDR9934

Cameco Gold Inc.



ASSAYS FROM

TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM TO WIDTH Au (ppb) Au re gt Au av gt Ag (ppm) Cu (ppm) Pb (ppm) Zn (ppm) Mo (ppm)

133.4 m: Intermediate feldspar porphyry.

225.8 m: Epidotized volcaniclastic sandstone, fine disseminated

biotite, crosscut by qtz-cal-chl-biot-py stringer. 262.2 m: Quartz-feldspar porphyry.

288.7 m: Quartz-feldspar porphyry.

301.3 m: Polymictic conglomerate.

For thin-sections:

CDR9934-1527: 129.65, Mineralized volcaniclastic rock (py, cpy),

within porphyritic clast/dykelet.

CDR9934-1539: 151.60, mineralized (cpy, py) volcaniclastic rock. CDR9934-1545: 167.40, Mafic dykelet, biotitic.

CDR9934-1559: 225.65, volcaniclastic sandstone, pervasively

epidotized, biotitic.

CDR9934-1570: 235.50, Altered and pyritic volcaniclastic

sandstone.


DEPTH INCLINATION HEARING

32.60 -55.50

63.10 -54.80

93.60 -54.60

124.10 -54.20

No: CDR9934

Cameco Gold Inc.





154.60 -53.90

185.10 -53.60

215.50 -53.20

246.00 -53.00

276.50 -52.90

325.20 -52.50

No: CDR9934

Cameco Gold Inc.

PROPERTY: Cedar Rapids HOLE No.: CDR9935 Collar Eastings: 1400.00 Collar Northings: 790.00 Collar Elevation: 290.00 Grid: Rotated Claim#: 5126359

DIAMOND DRILL LOG

Collar Inclination: -50.00 Grid Bearing: 229.00 Final Depth: 279.50 metres Val d'Or Drilling Test the NW strike extension

Logged by: J. Samson Date: 22/09/99-25/09/99 Down-hole Survey: ACID TEST Core: NQ

of the Dyke Zone.


0 38.4 (OVERBURDEN)

38.4 81.0 (MODERATELY ALTERED VOLCANICLASTIC SANDSTONE TO PEBBLY SANDSTONE)

SAMPLE No.

1595

FROM

42.50

TO

44.00

WIDTH Au

1.50

(ppb)

41

ASSAYS Ag (g/t) Cu

TRACE

(ppm)

20

Pb (ppm) Zn

TRACE

(ppm) Mo

52

(ppm)

2

As (ppm)

TRACE 1596 44.00 44.30 0.30 565 1.8 4644 TRACE 51 2 TRACE

Greenish grey to green, fine grained sandstone, with gradational 1597 44.30 45.80 1.50 10 0.3 6 10 27 3 TRACE bedding into subtle pebbly intervals, generally less than 1m 1598 45.80 47.10 1.30 TRACE 0.4 6 4 26 3 TRACE thick. The felsic looking clasts are mostly <lcm, aver.2-3mm, and 1599 47.10 48.50 1.40 11 TRACE 27 TRACE 38 3 TRACE are preferentially epidotized. The matrix is moderately 1600 48.50 50.15 1.65 7 0.3 88 2 46 3 TRACE chloritized, and moderate to locally strongly carbonatized 1601 50.15 51.65 1.50 39 0.5 241 2 51 3 TRACE (calcite), gives rock a predominantly "mafic" appearance. Epidote 1602 51.65 52.65 1.00 141 1.7 1392 TRACE 73 5 8 alteration is weak, mostly patchy, locally pervasive. Foliation 1603 52.65 54.00 1.35 22 0.5 249 TRACE 68 3 TRACE is weak to moderate at 47 deg. TCA. Core is moderately blocky 1604 54.00 55.50 1.50 14 0.2 78 2 50 3 TRACE down to 72.0m, ground in places. Quartz-calcitetepidote stringers 1605 55.50 57.00 1.50 24 0.3 64 2 61 3 TRACE 1%, at various angles.. Weak to locally strongly magnetic, due to 1606 57.00 58.50 1.50 57 0.3 147 TRACE 60 4 TRACE the presence of fine disseminated to wispy stringers of magnetite 1607 58.50 60.00 1.50 189 0.5 317 TRACE 61 4 TRACE to magnetic biotite(?). Pyrite very fine disseminations 1%, locally up to 2-3% as wisps and stringers, in association with

1608 1609

60.00 61.50

61.50 63.00

1.50 1.50

16 146

0.2 0.3

51 4

TRACE TRACE

50 38

3 2

TRACE TRACE

<0.5% chalcopyrite. 1610 63.00 64.50 1.50 19 0.3 47 TRACE 44 3 TRACE 1611 64.50 66.00 1.50 20 0.3 24 TRACE 45 2 TRACE

38.4-41.8: Mafic pebbly sandstone. Pyrite <1% disseminated to 1612 66.00 67.50 1.50 13 TRACE 24 TRACE 47 3 TRACE stringers. 1613 67.50 69.00 1.50 172 0.3 20 TRACE 57 3 TRACE

1614 69.00 70.50 1.50 18 0.4 171 TRACE 53 3 TRACE 41.6 47.1 (Gabbroic Dyke) 1615 70.50 72.00 1.50 TRACE 0.3 50 TRACE 50 2 TRACE Medium green, lighter colored interval, relatively coarser, with 1616 72.00 73.50 1.50 26 TRACE 58 TRACE 50 3 TRACE yellowish-green feldspar phenocrysts, over 60%, moderately 1617 73.50 75.00 1.50 12 0.4 20 TRACE 56 3 TRACE

No: CDR9935

Cameco Gold Inc.




Ag (g/t) Cu (ppm) Pb (ppm) Zn (ppm) Mb (ppm) As (ppm)

1618 75.00 76.50 1.50 TRACE 0.4 12 TRACE 58 3 TRACE 1619 76.50 78.00 1.50 58 0.4 8 TRACE 52 3 TRACE 1620 78.00 79.50 1.50 72 0.3 6 TRACE 49 5 TRACE 1621 79.50 81.00 1.50 10 0.3 77 3 44 3 TRACE


saussuritzed to epidotized, aver. lmm. Moderately fractured, weakly foliated. Moderately altered, chloritic, carbonatized, patchy epidote. Pyrite <1% overall.

41.8-44.0: Upper contact sharp, at 22 deg. TCA. Pyrite <1%.

44.0-44.3: Pyrite 1-2%, includes one 1cm band with 1% chalcopyrite, associated with chlorite and epidote, at 56 deg. TCA.

44.3-47.1: Pyrite 1%, locally 2%, dusty disseminations and wisps. Lower contact of dyke is not well defined.

47.1-51.7: Epidote alteration locally weak, pervasive to patchy. Moderately chloritized. Foliation at 45 deg. TCA. Pyrite <1%, fine disseminated to occasional wisps.

51.7-52.7: Pyrite-chalcopyrite (ration 95:5) stringers, wisps and dusty disseminations, 2-3%, mostly subparallel to foliation, in association with quartz-calcitetchlorite stringers, at 51 deg. TCA.

52.7-64.5: Moderately chloritized, locally strong, moderately magnetic in places. Pyrite 1-2%, as dusty disseminations, to occasional stringers in association with trace chalcopyrite within 1% quartz-calcite stringers

64.5-66.0: Epidote-quartz-calcite stringers, 3%., along fractures, broken core. Dusty pyrite to coarser dissemnations, 1-2%.

No: CDR9935

Cameco Gold Inc.



ASSAYS FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM TO WIDTH Au (ppb) Ag (g/t) Cu (ppm) Pb (ppm) Zn (ppm) Mo (ppm) As (ppm)

66.0-72.0: Core appears weakly less chloritized than above, very weak epidotization.

72.0-81.0: Epidote and carbonate alteration moderate, pervasive. Chlorite alteration perhaps weaker than overlying intervals. Fine biotite locally discernible. Foliation moderate at 47 deg. TCA. Core is only weakly fractured. Pyrite 2% disseminated mostly, with occasional wisps and stringers.

81.0 96.3 (VOLCANICLASTIC CONGLOMERATE TO PEBBLY SANDSTONE) 1622 81.00 82.50 1.50 7 0.3 77 TRACE 50 2 TRACE 1623 82.50 83.50 1.00 TRACE 0.3 59 TRACE 49 2 TRACE

Greenish grey interval of intermediate volcaniclastic 1624 83.50 84.40 0.90 7 TRACE 43 TRACE 47 2 TRACE conglomerate, polymictic, grading to pebbly sandstone locally. 1625 84.40 85.00 0.60 5 0.3 8 2 32 3 TRACE Clasts are pebble to cobble size, up to 8cm thick, average 2cm, greenish grey and preferentially weakly epidotized to

1626 85.00 86.50 1.50 6 0.3 35 TRACE 60 2 TRACE

saussuritized, others strongly carbonatized, subrounded, weakly flattened. Their composition appear mostly intermediate to felsic, with some ghostly grey in color, probably of sedimentary origin. Overall, alteration is weak by chlorite, moderate by calcite, and weak by epidote. Foliation weak to moderate at 44 deg. TCA. Quartz-calcite stringers <1%. Pyrite ,1% fine disseminated.

81.0-84.4: Epidote and sulphides rapidly decreasing relative to overlying interval. Epidote occurs mostly as diffuse patches, of clasts preferentially, up to 10cm across. Pyrite <1% very fine disseminated.

84.4-85.0: Up to 50% of interval consists of quartz-calcite-

No: CDR9935

Cameco Gold Inc.



ASSAYS FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM TO WIDTH Au (ppb) Ag (g/t) Cu (ppm) Pb (ppm) Zn (ppm) MO (ppm) As (ppm)

tourmaline and quartz-calcite-epidote veining, at 45 deg. TCA. Pyrite <1% dusty disseminations.

85.0-96.25.0: Pyrite <1% disseminations.

96.3 103.2 (MODERATELY ALTERED VOLCANICLASTIC CONGLOMERATE)

Same as previously described interval between 81.00 to 96.25m, but unit displays moderate chloritization, with moderate to strong and pervasive calcitic alteration. Foliation moderate at 51 deg. TCA. Moderately blocky core. Quartz-calcite stringers <1%. Pyrite <1% fine disseminated and trace stringers.

100.8-101.7: Quartz-calcite stringers and veinlets, up to 3cm wide, 8%, at 50 deg. TCA, accompanied by sericite and chlorite wisps. Moderately blocky core. Pyrite 2% locally, 1% overall. Trace chalcopyrite.

103.2 111.2 (INTERMEDIATE QUARTZ-FELDSPAR PORPHYRY)

Yellowish green quartz-feldspar porphyry, of intermediate composition. The feldspar phenocrysts are moderately saussuritized, subhedral, aver. 1 to 2mm, >50%. They are contained within a grey groundmass, fine grained, moderately to strongly carbonatized, with 3 to 5% chloritized mafic minerals. Foliation is weak to moderate at 42 deg. TCA. Locally, the foliation or schistosity is stronger, and marked by an overall

No: CDR9935

Cameco Gold Inc.



ASSAYS FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM TO WIDTH Au (ppb) Ag (g/t) Cu (ppm) Pb (ppm) Zn (ppm) Mb (ppm) As (ppm)

grey colour where only fine quartz phenocrysts may be distinguished. Weakly blocky core. Late white quartz-calcite veinlets, irregular, at various angles to core, mostly very oblique TCA, 3%. Pyrite 1% locally, generally less than 1%, disseminated to wisps.

103.2-104.2: Upper contact with volcaniclastic rock is sharp, at 45 deg. TCA. Porphyry is light grey, strongly carbonatized, weakly chloritic, finely quartz porphyritic. Moderately sheared at 51 deg. TCA, making rock cloudy, with diffuse mineralogy. Pyrite 2% locally, 1% overall, disseminated to wispy.

104.2-106.0: Similar to interval at 103.20 to 104.15 m, includes a 20 cm sliver of volcaniclastic sediments. Pyrite 1-2%.

106.0-111.0: Dominantly feldspar-phyric interval. Weakly foliated. Pyrite 0.5% disseminated.

111.0-111.2: Moderately sheared at 45 deg. TCA. Contact sharp at same angle. Moderately carbonatized and chloritized. Pyrite 0.5%.

111.2 156.0 (WEAKLY ALTERED VOLCANICLASTIC CONGLOMERATE) 1627 86.50 138.00 51.50 TRACE TRACE 7 TRACE 50 2 TRACE 1628 130.00 148.50 10.50 TRACE 0.2 15 TRACE 76 2 TRACE

Same as previously describéd volcaniclastic conglomerate located 1629 148.50 150.00 1.50 TRACE TRACE 12 TRACE 55 2 TRACE above the porphyry, between 96.25 to 103.20, but alteration 1630 150.00 151.00 1.00 13 0.3 50 TRACE 56 7 TRACE consists of weak chloritization, and more notably, patchy 1631 151.00 152.00 1.00 5 TRACE 17 TRACE 51 2 TRACE epidotization. The epidote has preferentially altered the felsic 1632 152.00 153.35 1.35 TRACE TRACE 56 TRACE 73 2 TRACE clasts, or occurs as rounded patches/pseudoclasts(?), up to 10 cm 1633 153.35 154.50 1.15 TRACE TRACE 13 TRACE 95 3 TRACE

No: CDR9935

Cameco Gold Inc.




across, where it is very strong and pervasive, accompanied by 1634 154.50 156.00 1.50 TRACE TRACE 14 TRACE 51 2 TRACE quartz-stringers which do not continue into the matrix, and therefore predate sedimentation. Carbonate alteration is pervasive, moderate to strong. Foliation is weak to moderate at 51 deg. TCA. Quartz-calcite stringers <1%. Pyrite 0.5% fine disseminated.

137.0-156.0: Most intensely epidotized interval, locally strong, patchy, overall weak.

141.6-142.3: Epidote moderate to strong, in association with a narrow quartz veinlet, oblique to the core. Barren.

147.1-147.4: Pervasive and strong epidote alteration of a pseudoclast, accompanied by narrow translucent quartz stringers, 10%. Weakly silicified. Fine pyrite, <1%, disseminated within the clasts and within the quartz stringers.

147.4-148.7: Fine sandstone to mudstone, with 1% hairthin quartz-carbonate stringers infilling fractures at all angles TCA, irregular.

156.0 248.0 (VOLCANICLASTIC SANDSTONE TO CONGLOMERATE) 1635 156.00 157.50 1.50 8 TRACE 4 TRACE 52 2 TRACE 1636 157.50 167.30 9.80 TRACE TRACE TRACE TRACE 55 2 TRACE

Light grey sandstone, monotonous, grading locally into pebbly 1637 167.30 167.55 0.25 TRACE TRACE 1 TRACE 56 2 TRACE sandstone to conglomerate (<15%). Betweeen 198.0 to 215.50m 1638 167.55 168.80 1.25 TRACE TRACE 20 TRACE 57 3 TRACE downhole, conglomeratic intervals are predominant, comprising over 1639 168.80 170.10 1.30 6 0.3 TRACE TRACE 58 2 TRACE 70% of interval. Thickly bedded, parallel to foliation, locally 1640 170.10 187.30 17.20 TRACE 0.3 31 TRACE 98 2 TRACE graded, with fining downhole observed at 197m, 202m, and 209m. 1641 187.30 212.50 25.20 TRACE 0.3 28 TRACE 111 2 TRACE

No: CDR9935

Cameco Gold Inc.



ASSAYS FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM TO WIDTH Au (ppb) Ag (g/t) Cu (ppm) Pb (ppm) En (ppm) Mb (ppm) As (ppm)

Calcite alteration pervasive, moderate, giving rock a weakly 1642 212.50 214.00 1.50 TRACE TRACE 48 TRACE 110 2 TRACE bleached, cloudy texture. Chlorite and sericite weak. Foliation 1643 214.00 215.50 1.50 TRACE 0.2 53 TRACE 97 2 TRACE is weak at 54 deg. TCA. Quartz-calcite stringers <1%. Pyrite <1%, 1644 215.50 217.00 1.50 TRACE 0.3 13 3 53 3 TRACE disseminated to occasional wisps. 1645 217.00 218.50 1.50 TRACE TRACE 69 TRACE 103 TRACE 6

1646 218.50 220.00 1.50 TRACE TRACE 24 TRACE 108 TRACE TRACE 163.0-169.0: Weak fault zone. Moderately fractured core, 1647 220.00 221.50 1.50 TRACE TRACE 74 TRACE 116 TRACE TRACE locally strong. 1648 221.50 222.75 1.25 TRACE TRACE 47 TRACE 102 1 TRACE

1649 222.75 224.25 1.50 TRACE 0.2 56 TRACE 31 2 TRACE 168.8-169.8: Fine grained, weakly laminated, with moderate 1650 224.25 225.15 0.90 9 TRACE 14 TRACE 61 1 TRACE chlorite alteration. Laminations parallel to foliation, weakly 1651 225.15 226.65 1.50 TRACE TRACE 51 TRACE 80 1 TRACE crenulated, at 49 deg. TCA. Pyrite 1% disseminated. 1652 226.65 227.60 0.95 8 TRACE 59 2 86 TRACE TRACE

1653 227.60 228.40 0.80 TRACE TRACE 58 TRACE 100 TRACE TRACE 187.3 187.6 (Intermediate Feldspar Porphyry Dykelet) 1654 228.40 228.90 0.50 TRACE TRACE 11 TRACE 116 TRACE TRACE Grey dykelet, with 40% fine feldspar phenocrysts, lmm aver., 1655 228.90 230.00 1.10 TRACE TRACE 29 TRACE 104 TRACE TRACE weakly saussuritized, within a weakly carbonatized groundmass. 1656 230.00 231.00 1.00 TRACE TRACE 2 TRACE 60 1 TRACE Similar and probably of same generation as previously described 1657 231.00 232.00 1.00 TRACE TRACE 39 TRACE 137 2 TRACE porphyry dykes. Chloritized xenoliths, <lcm, 2-3%. Foliation 1658 232.00 233.00 1.00 TRACE TRACE 55 TRACE 88 3 TRACE weak. Upper and lower contacts sharp at 38 deg. TCA. Trace of 1659 233.00 234.00 1.00 TRACE TRACE 71 3 135 TRACE TRACE hairthin quartz-calcite stringers. Pyrite <0.5%, fine 1660 234.00 235.00 1.00 TRACE TRACE 28 TRACE 117 1 TRACE disseminated. No increase in alteration of wallrock noted. 1661 235.00 236.00 1.00 20 TRACE 783 TRACE 80 TRACE TRACE

1662 236.00 237.00 1.00 TRACE TRACE 5 TRACE 131 TRACE TRACE 198.0-210.0: Weak pervasive epidote and chlorite alteration 1663 237.00 238.50 1.50 TRACE TRACE 18 TRACE 65 TRACE TRACE locally. Pyrite <1% disseminated. Bedding and foliation 1664 238.50 240.00 1.50 7 2.2 7 TRACE 23 3 TRACE parallel, at 58 deg. TCA. 1665 240.00 241.50 1.50 TRACE TRACE 10 TRACE 78 1 TRACE

1666 241.50 243.00 1.50 12 TRACE 47 TRACE 67 TRACE TRACE 210.0-211.0: Weak epidoti'zation, pervasive, along a narrow 1667 243.00 244.50 1.50 9 TRACE 171 7 76 5 TRACE quartz-carbonate stringer parallel to ca. over 30cm, associated 1668 244.50 246.00 1.50 TRACE TRACE 35 TRACE 66 2 TRACE with 1% fine disseminated pyrite. 1669 246.00 247.50 1.50 TRACE TRACE 42 TRACE 71 TRACE TRACE

212.5-215.5: Moderate schistosity, at 61 deg. TCA.

No: CDR9935

Cameco Gold Inc.



ASSAYS FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM TO WIDTH Au (ppb) Ag (g/t) Cu (ppm) Pb (ppm) 2n (ppm) Mb (ppm) As (ppm)

215.5-214.3: Includes 5.5cm quartz-calcite-chlorite stringer

band, with 1% pyrite and trace chalcopyrite.

215.5-236.5: Monotonous section of sandstone to pebbly

sandstone. Alteration weak by epidote, chlorite, and moderate by

carbonate. Foliation weak at 56 deg. TCA. Pyrite <1%.

236.5-237.0: Quartz vein, moderately sheared at 38 deg. TCA,

with minor carbonate, chlorite, and wisps of tourmaline infilling irregular fractures at all angles. Pyrite trace.

237.0-248.0: Similar to interval between 215.50-236.50m.

248.0 276.0 (MODERATELY ALTERED VOLCANICLASTIC ROCKS) 1670 247.50 249.00 1.50 TRACE TRACE 50 3 68 2 TRACE 1671 249.00 250.50 1.50 TRACE TRACE 8 2 43 1 TRACE

Fine grained volcaniclastic sandstone to pebbly sandstone, weakly 1672 250.50 252.00 1.50 5 TRACE 37 2 75 1 TRACE to moderately bleached by pervasive weak to moderate carbonate 1673 252.00 253.50 1.50 10 TRACE 23 3 76 1 TRACE (calcite), sericite and hematite alteration, with moderately 1674 253.50 255.00 1.50 7 TRACE 20 TRACE 85 TRACE TRACE chloritic intervals. Rock is moderately foliated, schistose, at 1675 255.00 256.50 1.50 TRACE TRACE 14 TRACE 79 1 TRACE 63 deg. TCA. Quartz-calcite stringers <1%. Pyrite 0.5% to trace, fine disseminated. At least two narrow intermediate feldspar

1676

1677 256.50

257.50

257.50

258.30

1.00

0.80 TRACE

TRACE

TRACE

TRACE

29

6 TRACE

TRACE 78

19

TRACE

2 TRACE

TRACE porphyry dykelets also cross-cut the zone. 1678 258.30 259.00 0.70 TRACE TRACE 47 3 135 TRACE TRACE

1679 259.00 259.80 0.80 TRACE TRACE 4 TRACE 186 TRACE TRACE 248.0-249.0: Moderately carbonatized interval. 1680 259.80 260.50 0.70 TRACE TRACE 8 TRACE 75 TRACE TRACE

1681 260.50 262.00 1.50 TRACE TRACE 65 TRACE 73 1 TRACE 249.0-249.4: Moderate to strongly sheared, with pervasive 1682 262.00 262.75 0.75 TRACE TRACE 11 TRACE 74 TRACE TRACE quartz-calcite-chlorite stringers, sheared, deformed, weakly 1683 262.75 263.75 1.00 TRACE TRACE 19 TRACE 77 1 TRACE folded, at 69 deg TCA. Pyrite 1-2%, disseminated to wisps. 1684 263.75 264.75 1.00 TRACE TRACE 20 TRACE 95 2 TRACE

No: CDR9935

Cameco Gold Inc.




1685 264.75 266.00 1.25 TRACE TRACE 11 TRACE 81 2 TRACE 1686 266.00 267.50 1.50 TRACE TRACE 27 TRACE 74 1 TRACE 1687 267.50 269.00 1.50 TRACE TRACE 40 TRACE 67 TRACE TRACE 1688 269.00 270.50 1.50 TRACE TRACE 42 3 72 TRACE TRACE

249.4-251.5: Schistosity weaker. Weak to moderately chloritic. Pyrite trace.

251.5-253.0: Moderate to strongly schistose, at 63 deg. TCA. Moderately chloritic, carbonatized, weakly sericitic. Schistosity gradually increasing downhole, nearing contact with porphyry, accompanied by 3-4% sheared/brecciated quartz-carbonate stringers and veinlets. Pyrite trace.

253.0 253.5 (Intermediate Feldspar Porphyry) Upper contacts sharp at 65 and 62 deg. TCA respectively. Grey, relatively fresh looking, with 40% subhedral and white feldspar phenocrysts, 1 to 3mm, within a groundmass of quartz, feldspar, carbonate, weakly sericitic, and 2-3% chloritized wispy mafic minerals. Rock is weakly foliated, schistose, at 45 deg. TCA. No quartz-carbonate stringers are noted. Pyrite trace.

253.5-261.0: Fine grained to pebbly sandstone, moderately chloritized and carbonatized, schistose at 62 deg. TCA. Fine specks of ankerite locally discernible, up to 15% fine disseminations in places. Pyrite trace.

259.5-261.0: Becoming moderately bleached by sericite and carbonate (calcite).

261.0 261.8 (Hematized Quartz-Feldspar Porphyry) Contacts sharp at 60 deg. TCA. Rock is light pink, moderately hematized, with over 70% pinkish feldspar phenocrysts, 2mm aver., and 5% greyish quartz eyes (<1-2mm), within a fine groundmass of

No: CDR9935

Cameco Gold Inc.




quartz-feldspar-carbonate-saussurite. Weakly foliated. Quartz- carbonate stringers, 1%. Pyrite trace.

261.8-263.8: Moderately schistose at 65 deg. TCA. Moderately sericitized and carbonatized, weakly chloritic, bleached. Ankerite specks locally developed. Weak silicification over one narrow 30cm interval. Pyrite trace.

263.8-266.0: Bleached, pinkish grey interval of quartz- sericite-carbonate-hematite schist, possibly a highly altered sediment, or dyke, although contacts are not well defined. Fine quartz eyes and chloritic wisps are still discernible. Fine ankerite specks in places. Overall, fairly homogenous, moderate to strongly carbonatized, sericitic and hematized, with no quartz stringers. Pyrite trace.

266.0-274.5: Moderately bleached interval, light yellowish grey, due to pervasive moderate to strong sericitization, and carbonatization (calcite and ankerite specks). Hematization is patchy, moderate in places, pervasive. Weakly magnetic in places. Rock is essentially a quartz-chlorite-sericite-carbonate schist, moderately foliated at 61 deg. TCA. Quartz-calcite stringers <1%. Pyrite trace, to <1% in association with occasional quartz- carbonate stringers.

270.0-272.5: Patchy hematization weak to moderate, pervasive.

274.5-276.0: Fine ankerite specks disseminated throughout, over

No: CDR9935

Cameco Gold Inc.




15% locally.

276.0 279.5 (VOLCANICLASTIC PEBBLY SANDSTONE)

As previously described, but relatively much less altered, with

weak chloritization, and weak to locally moderate carbonate

(calcite) alteration. Foliation is less defined, weaker, at 65

deg. TCA. Quartz-calcite-epidote-hematite stringers, 1%. Pyrite trace.

279.5: EOH.

Note: No whole rock samples or representative samples were taken.



215.50 -39.50

265.00 -38.00

No: CDR9935

Cameco Gold Inc.


HOLE No.: CDR9936

Collar Eastings: 1814.00 Collar Inclination: -50.00 Logged by: J. Samson Collar Northings: 758.00 Grid Bearing: 230.00 Date: 26/09/99-27/09/99 Collar Elevation: 290.00 Final Depth: 264.30 metres Down-hole Survey: ACID TEST Grid: Rotated

Val d'Or Drilling Core: NQ Claim#: 5126334

Test the SE strike extension of the Dyke Zone.


0.0 17.4 (OVERBURDEN)


Ag (g/t) Cu (ppm) Pb (ppm) Zn (ppm) Mo (ppm) As (ppm)

17.4 83.2 (MINERALIZED INTERMEDIATE FELDSPAR PORPHYRY) 1689 17.44 18.75 1.31 TRACE TRACE 43 TRACE 35 1 TRACE 1690 18.75 20.00 1.25 11 TRACE 95 TRACE 42 2 TRACE

Light greenish grey intermediate feldspar porphyry, locally 1691 20.00 21.00 1.00 46 0.3 67 TRACE 44 1 TRACE brecciated, with pyrite and chalcopyrite stringers often infilling 1692 21.00 21.50 0.50 890 1.3 998 TRACE 50 1 6 microfractures. The porphyry contains over 60% yellowish white 1693 21.50 23.00 1.50 16 TRACE 9 TRACE 31 1 TRACE feldspar phenocrysts, subhedral to euhedral, aver. lto 2 mm,

weakly saussuritized to strongly epidotized in places. The 1694

1695

23.00

24.50

24.50

26.00

1.50

1.50

72

151

TRACE

TRACE 91

153

TRACE

TRACE

34

30 1

1 TRACE

TRACE groundmass is grey, fine grained, moderately carbonatized, cloudy,

with chloritized mafic minerals varying from <1% to 5% locally. 1696

1697 26.00

27.45

27.45

28.75

1.45

1.30

TRACE

19

TRACE

TRACE

22

13

TRACE

TRACE 33

25 1

1 TRACE

TRACE Fine grained mafic to sedimentary(?) xenoliths are very common,

angular, moderately carbonatized and chloritized. Foliation is 1698

1699 28.75

30.15 30.15

31.50

1.40

1.35

TRACE

12 TRACE

TRACE

20

21 TRACE

TRACE 42

30

TRACE

TRACE TRACE

TRACE generally very weak to absent, but accompanied by narrow (<30cm) 1700 31.50 32.75 1.25 56 TRACE 44 TRACE 25 1 TRACE moderately sheared intervals scattered throughout the core. These 1701 32.75 33.50 0.75 105 0.3 675 TRACE 20 TRACE TRACE narrow shears, at various angles from 25 to 65 deg. TCA, are 1702 33.50 34.50 1.00 116 TRACE 425 TRACE 20 1 TRACE accompanied by stronger carbonate alteration, sometimes very weak 1703 34.50 35.50 1.00 108 0.3 689 TRACE 19 1 TRACE sericitization, and are oftén characterized by the presence of 1704 35.50 36.50 1.00 113 0.2 253 TRACE 22 2 TRACE quartz-calcite-chlorite stringers, generally mineralized with 2-3% 1705 36.50 37.50 1.00 25 TRACE 25 TRACE 20 1 TRACE pyrite and 1% chalcopyrite, as fine disseminations to wisps and 1706 37.50 38.50 1.00 11 TRACE 16 TRACE 26 1 TRACE stringers. The sulphides are also infilling chloritic 1707 38.50 39.50 1.00 12 TRACE 32 TRACE 33 1 TRACE microfractures at all angles to core axis. Overall, the core 1708 39.50 41.00 1.50 TRACE TRACE 10 TRACE 30 2 TRACE contains si% pyrite, and less than 0.5% chalcopyrite (more than a 1709 41.00 42.50 1.50 20 TRACE 45 TRACE 24 2 TRACE trace). Quartz-calcite-chlorite stringers are overall less than 1710 42.50 44.00 1.50 126 TRACE 43 TRACE 27 1 TRACE 1%. 1711 44.00 45.00 1.00 251 TRACE 90 TRACE 48 TRACE TRACE

No: CDR9936

Cameco Gold Inc.




1712 45.00 46.00 1.00 60 TRACE 18 TRACE 36 2 TRACE 17.4-21.0: Pyrite seams <1%, trace chalcopyrite. 1713 46.00 47.00 1.00 210 TRACE 33 TRACE 34 1 TRACE

1714 47.00 48.00 1.00 54 TRACE 63 TRACE 32 1 TRACE 21.0-21.5: Interval includes a 1cm wide calcite-quartz- 1715 48.00 49.50 1.50 69 TRACE 40 TRACE 37 TRACE TRACE chlorite-epidote stringer, at 30 deg. TCA, with over 50% pyrite, 1716 49.50 51.00 1.50 108 TRACE 84 TRACE 34 2 TRACE and 5% chalcopyrite. Overall, pyrite 1%, trace chalcopyrite. 1717 51.00 52.50 1.50 22 TRACE 35 5 44 TRACE TRACE

1718 52.50 54.00 1.50 26 TRACE 67 TRACE 34 1 TRACE 28.8 30.2 (Gabbroic Dyke) 1719 54.00 55.50 1.50 31 TRACE 73 TRACE 37 2 TRACE Green, medium grained mafic dyke, with chloritized mafic minerals 1720 55.50 57.00 1.50 9 TRACE 30 TRACE 32 2 TRACE contained within a finer groundmass of feldspar and carbonate. 1721 57.00 58.00 1.00 TRACE TRACE 28 TRACE 28 1 TRACE Moderately altered, very weakly foliated. Upper and lower contacts 1722 58.00 59.00 1.00 7 TRACE 32 TRACE 28 1 TRACE sharp at 67deg. TCA. Quartz-calcitetepidote stringers, hairthin, 1723 59.00 59.70 0.70 TRACE TRACE 27 3 32 2 TRACE very oblique TCA, 1%. Hematite on some fractures. Pyrite up to 1724 59.70 61.00 1.30 TRACE TRACE 29 TRACE 29 2 TRACE 1% finely disseminated. No pyrite-chalcopyrite stringers or seams 1725 61.00 62.50 1.50 TRACE TRACE 30 3 29 1 TRACE noted. 1726 62.50 64.00 1.50 TRACE TRACE 27 TRACE 30 1 TRACE

1727 64.00 65.50 1.50 TRACE TRACE 52 TRACE 24 TRACE TRACE 30.2-32.8: Pyrite <1%. 1728 65.50 67.00 1.50 TRACE TRACE 32 TRACE 28 1 TRACE

1729 67.00 68.25 1.25 TRACE TRACE 9 TRACE 31 1 TRACE 32.8-38.5: Notably, this interval displays more abundant 1730 68.25 69.50 1.25 15 TRACE 51 TRACE 25 1 TRACE microfracturing or weak brecciation, with chlorite infilling, at 1731 69.50 70.50 1.00 116 0.3 590 TRACE 24 2 TRACE various angles to core axis. Core also appears more bleached, 1732 70.50 71.80 1.30 TRACE TRACE 40 TRACE 25 1 TRACE more carbonatized, accompanied by grain-size reduction locally due 1733 71.80 72.80 1.00 35 TRACE 180 TRACE 23 4 TRACE to shearing. 1734 72.80 73.50 0.70 TRACE TRACE 15 TRACE 24 1 TRACE

1735 73.50 75.00 1.50 TRACE TRACE 65 TRACE 22 4 TRACE 32.8-33.5: Pyrite 1%, with 0.5% chalcopyrite splashes. 1736 75.00 76.50 1.50 TRACE TRACE 61 6 32 1 TRACE

1737 76.50 78.00 1.50 6 TRACE 71 4 32 2 TRACE 33.5-38.5: Pyrite <1%, seams and disseminations, with trace 1738 78.00 79.50 1.50 24 TRACE 263 3 24 2 TRACE chalcopyrite. 1739 79.50 81.00 1.50 66 0.2 534 TRACE 18 3 TRACE

1740 81.00 82.00 1.00 163 0.2 430 TRACE 16 2 TRACE 38.5-59.0: Pyrite <1% disseminated, with trace of pyrite seams. 1741 82.00 83.15 1.15 58 TRACE 337 TRACE 17 4 TRACE

No: CDR9936

Cameco Gold Inc.



ASSAYS FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM TO WIDTH Au (ppb) Ag (g/t) Cu (ppm) Pb (ppm) Zn (ppm) MO (ppm) As (ppm)

59.0-59.7: Weakly bleached core, in association with a lcmt wide quartz -calcite veinlet at 35 deg TCA. Pyrite blebs within the stringer. Overall 1% pyrite.

59.7-71.8: Fairly homogenous interval of porphyry, with less than 1% hairline thin quartz-calcite-epidote stringers. Pyrite less than 1% fine disseminated.

71.8-72.8: Includes 40% narrow shears, grey, carbonatized, fine grained, at 66 deg. TCA, with 2-3% quartz-carbonate-chlorite stringers infilling fractures. Pyrite as recrytallized blebs, stringers and disseminations, 1-2%, 1% overall, with trace chalcopyrite.

71.8-83.2: As before, hairthin chloritic fractures at various angles, with occasional pyrite seams and fine disseminations mostly along their margins. Pyrite <1% to 1%, trace chalcopyrite.

82.0-83.2: No notable increase in alteration or mineralization. Lower contact of porphyry with sediments sharp but irregular at less than 30 deg. TCA.

83.2 88.8 (ALTERED VOLCANICLASTIC SANDSTONES) 1742 83.15 84.25 1.10 125 TRACE 380 TRACE 27 8 TRACE 1743 84.25 85.50 1.25 26 TRACE 325 TRACE 24 2 TRACE

Light greenish grey, fairly homogenous section of fine 1744 85.50 86.75 1.25 17 TRACE 132 TRACE 20 TRACE TRACE volcaniclastic sandstone(?). No definite bedding, but subtle 1745 86.75 88.00 1.25 33 TRACE 231 TRACE 26 4 TRACE pseudolaminations at 41 deg. TCA suggest this interval is 1746 88.00 88.75 0.75 6 TRACE 53 TRACE 24 TRACE TRACE sedimentary. Locally, the core is medium grained, and presents a

No: CDR9936

Cameco Gold Inc.




texture somewhat similar to a highly altered feldspar porphyry.

Core appears weakly to moderately silicified in places, with weak

carbonate and very weak sericitization. Trace of very weak and

pervasive patchy hematization. quartz-calcitetepidote-chlorite stringers, mostly hairthin, sometimes vuggy, <1%. Pyrite finely

disseminated, to wisps and occasional seams, in association with

carbonate stringers, 2-3% locally, overall <1%. Chalcopyrite trace. Foliation is diffuse, locally moderate at 53 deg. TCA.

83.2-84.3: Appears moderately silicified locally. Includes one

<lcm wide quartz veinlet, with chlorite and tourmaline, cross

cutting foliation at 25 deg. TCA, accompanied by blebs of pyrite. Overall, pyrite <1%.

85.5-86.8: Moderately silicified interval, with very patchy

hematization. Includes one 5cm wide band of quartz-carbonate-

epidote, with 5-8% pyrite and 1-2% chalcopyrite. Also other sulphide wisps and seams. Overall, <1% pyrite, and more than a trace chalcopyrite.

86.8-88.8: No notable increase in alteration or mineralization.

Apparent bedding or laminations at 54 deg. TCA. Pyrite <1% fine

disseminated.

88.8 95.0 (INTERMEDIATE FELDSPAR PORPHYRY) 1747 88.75 89.50 0.75 20 TRACE 184 TRACE 36 2 TRACE 1748 89.50 90.75 1.25 6 TRACE 33 TRACE 23 2 TRACE

Very massive and homogenous but relatively fine grained 1749 90.75 92.00 1.25 7 TRACE 40 TRACE 27 2 TRACE intermediate feldspar porphyry. Rock is greenish grey, appears 1750 92.00 93.00 1.00 11 TRACE 24 TRACE 31 TRACE TRACE cloudy, with diffuse mineralogy of fine feldspar phenocrysts (lmm, 1751 93.00 94.00 1.00 12 TRACE 190 TRACE 28 2 TRACE >50%, moderately saussuritized to weakly epidotized) contained 1752 94.00 95.00 1.00 42 TRACE 99 TRACE 23 1 TRACE

No: CDR9936

Cameco Gold Inc.




within a fine grained grey groundmass of quartz, feldspar, and carbonate, with fine chloritic mafic minerals. Overall, of same generation as previously described feldspar porphyries, but finer grained, perhaps more altered, weakly sericitized. Foliation is weak locally at 52 deg. TCA. Trace of hairthin quartz- calcitetepidote-hematite stringers. Pyrite <1% very fine disseminated, to occasional seams and blebs. No chalcopyrite observed.

88.8-89.5: Upper contact sharp at 51 deg. TCA. Pyrite fine disseminations to wisps, up to 1%.

94.0-95.0: Lower contact sheared, obscure, at 52 deg. TCA, and is accompanied by 1% dusty pyrite disseminations over the last 20cm interval.. One 3mm quartz-calcite stringers cross cuts the contact at 70 deg. TCA, and contains 20% pyrite. Overall, <1% pyrite.

95.0 106.5 (VOLCANICLASTIC SANDSTONE TO PEBBLY SANDSTONE)

Greenish grey and relatively unaltered and monotonous sequence of volcaniclastic sandstone to pebbly sandstone. Apparent beds vary from 1.5m to less than 10cm, are mostly gradational suggesting possible tops downhole (ie. 99.0 to 100.0m), and are subparallel to the weak foliation at 48 deg. TCA. Alteration is very weak, characterized by weak sericite within the finer grained "argillaceous" sandstone beds. Quartz-calcitetepidote stringers are hairthin, <1%. Pyrite 0.5% disseminated to seams.

96.5-97.0: Weak to moderately sheared, including one <lcm

1753 95.00 96.50 1.50 8 TRACE 47 TRACE 43 TRACE TRACE 1754 96.50 97.00 0.50 8 TRACE 34 TRACE 44 TRACE TRACE 1755 105.00 105.95 0.95 TRACE TRACE 2 TRACE 40 1 TRACE 1756 105.95 106.45 0.50 82 TRACE 124 TRACE 42 2 TRACE

No: CDR9936

Cameco Gold Inc.




gouge, at 45 deg. TCA. Interval also includes one 3cm quartz-

calcite-epidote-hematite veinlet, parallel to the schistosity. Pyrite <1% disseminated.

106.0-106.5: Weakly sheared at 42 deg. TCA. Moderately altered

by carbonate and silicification. Weakly chloritized. Contains

over 5% sheared epidote-quartz-carbonate stringers. Pyrite disseminations and wisps up to 1%.

106.5 152.3 (INTERMEDIATE FELDSPAR PORPHYRY)

Green grey intermediate feldspar porphyry as previously described

near the top of the hole. The alteration consists of weak to

moderate and pervasive carbonate (calcite), locally bleaching the

core. Foliation is nearly absent to very weakly developped.

Quartz-calcite stringers, trace. Microfractures locally infilled

by quartz-calcitettourmaline, sub-parallel to very oblique TCA,

<1%, often display 0.5cm sinistral displacements. Pyrite trace.

117.8 118.0 (Fault)

Ground core. No mineralization or veining, except for a 1cm<

quartz-calcite-tourmaline stringer at 118.1m, oriented at 22 deg. TCA, barren.

120.5-128.5: Fractures parallel TCA, infilled by quartz-

calcite-epidote-chlorite, and accompanied by 1% disseminated

pyrite. Overall, pyrite <1%. Trace of molybdenite along fracture

planes. Weakly blocky core, with moderate bleaching by carbonate.

1757 106.45 108.00 1.55 91 TRACE 36 TRACE 22 TRACE TRACE 1758 119.00 120.50 1.50 TRACE TRACE 2 TRACE 18 TRACE TRACE 1759 120.50 122.00 1.50 22 0.2 15 TRACE 27 TRACE TRACE 1760 122.00 123.00 1.00 197 TRACE 7 TRACE 22 TRACE TRACE 1761 123.00 124.00 1.00 179 TRACE 48 TRACE 31 TRACE TRACE 1762 124.00 125.50 1.50 5 TRACE 22 TRACE 29 3 TRACE 1763 125.50 127,00 1.50 TRACE TRACE 13 TRACE 25 1 TRACE 1764 127.00 128.50 1.50 47 TRACE 68 TRACE 25 TRACE TRACE 1765 128.50 129.75 1.25 18 TRACE 37 TRACE 29 TRACE TRACE 1766 129.75 130.75 1.00 47 TRACE 44 TRACE 26 TRACE TRACE 1767 130.75 132.00 1.25 96 TRACE 54 TRACE 26 1 TRACE 1768 132.00 133.10 1.10 TRACE TRACE 4 TRACE 27 TRACE TRACE 1769 133.10 134.10 1.00 135 0.3 860 TRACE 30 6 TRACE 1770 134.10 135.50 1.40 20 TRACE 5 TRACE 26 1 TRACE 1771 135.50 137.00 1.50 994 TRACE 120 TRACE 27 TRACE TRACE 1772 137.00 138.50 1.50 TRACE TRACE 4 TRACE 25 TRACE TRACE 1773 149.50 151.00 1.50 6 TRACE 10 TRACE 20 TRACE TRACE 1774 151.00 152.30 1.30 56 TRACE 123 TRACE 23 1 TRACE

No: CDR9936

Cameco Gold Inc.

DIAMOND DRILL LOG PROPERTY: Cedar Rapids HOLE No.: CDR9936 Page


127.5-128.0: Strongly fractured core, locally ground.

133.1-134.0: Dark grey interval, with strong pervasive carbonate (calcite) alteration. Weakly chloritic. Pyrite 1% disseminated. Trace of chalcopyrite, in association with a quartz-calcite stringer, lcmti wide.

134.0-137.0: Bleaching by carbonate is gradually decreasing, to weak. Weak saussuritization of the feldspars, as before.

137.0-151.0: Fairly homogenous interval of porphyry, relatively fresh looking. Pyrite trace, fine disseminated.

151.0-152.3: Gradual increase in schistosity to moderate nearing contact, at 50 deg. TCA.

152.0-152.3: Rock is light grey, quartz porphyritic, pervasively carbonatized, and contains up to 1% finely disseminated pyrite. Lower contact sharp at 47 deg. TCA.

152.3 182.2 (MINERALIZED VOLCANICLASTIC SEDIMENTS)

Unit consists of volcaniclastic pebbly sandstone to polymictic conglomerate, thickly bedded, gradational, light grey to medium grey, and mostly displaying pervasive moderate carbonate alteration (calcite), with gradually decreases to weak downhole. Epidotization is very weak, preferentially of feldspathic to felsic clasts. Sericitization is also very weak, mostly of the matrix. Rock is weakly to moderately foliated, parallel to

1775 152.30 153.20 0.90 301 0.3 319 TRACE 50 6 TRACE 1776 153.20 154.25 1.05 950 0.5 669 TRACE 47 4 TRACE 1777 154.25 155.25 1.00 127 0.3 318 TRACE 48 6 TRACE 1778 155.25 156.50 1.25 1062 2.3 5265 TRACE 54 36 15 1779 156.50 157.50 1.00 88 TRACE 185 TRACE 35 3 TRACE 1780 157.50 158.50 1.00 86 TRACE 201 TRACE 40 2 TRACE 1781 158.50 159.50 1.00 173 TRACE 268 TRACE 41 3 TRACE 1782 159.50 160.50 1.00 55 0.2 86 TRACE 38 2 TRACE 1783 160.50 161.50 1.00 96 0.3 105 TRACE 50 7 TRACE

No: CDR9936

Cameco Gold Inc.




Ag (g/t) Cu (ppm) Pb (ppm) Zn (ppm) Mo (ppm) As (ppm)

apparent bedding, at 43 deg. TCA. Quartz-calcite stringers <1%. 1784 161.50 162.25 0.75 53 TRACE 3 TRACE 38 6 TRACE Pyrite occurs as fine disseminations to wisps and stringers, 2 to 1785 162.25 162.80 0.55 TRACE TRACE 2 TRACE 29 4 TRACE 3% locally, 1% overall. Chalcopyrite trace. 1786 162.80 163.80 1.00 TRACE 0.2 3 TRACE 37 20 TRACE

1787 163.80 164.80 1.00 196 0.3 400 TRACE 41 26 TRACE 152.3-155.3: No notable increase in alteration associated with 1788 164.80 166.00 1.20 35 TRACE 13 TRACE 34 18 TRACE the proximity to the contact with the porphyry. Pyrite <1%. 1789 166.00 167.50 1.50 15 TRACE 120 TRACE 37 TRACE TRACE

1790 167.50 169.00 1.50 14 TRACE 55 TRACE 51 TRACE TRACE 155.3-156.5: Includes a 25cm band of quartz-calcite veining and 1791 169.00 170.25 1.25 15 0.3 92 TRACE 44 TRACE TRACE mineralization, with 15% pyrite, semi-massive, and 2-3% 1792 170.25 171.70 1.45 5 TRACE 70 TRACE 45 TRACE TRACE chalcopyrite. Overall, pyrite 2%, chalcopyrite 0.5%, as stringers 1793 171.70 172.50 0.80 TRACE TRACE 7 TRACE 55 1 TRACE and seams, at various angles, cross cutting foliation, mostly at 1794 172.50 173.50 1.00 297 0.5 810 TRACE 52 2 TRACE 63 deg. TCA.. 1795 173.50 175.00 1.50 40 0.3 171 TRACE 32 TRACE TRACE

1796 175.00 176.50 1.50 TRACE TRACE 24 TRACE 32 TRACE TRACE 156.5-162.3: Pyrite 1%, as stringers and seams. 1797 176.50 178.00 1.50 15 TRACE 68 TRACE 31 TRACE TRACE

1796 178.00 179.50 1.50 TRACE TRACE 2 TRACE 32 TRACE TRACE 162.3-162.8: Quartz veinlet, 15%, with minor calcite, about 1cm 1799 179.50 180.50 1.00 TRACE TRACE 4 TRACE 35 1 TRACE wide, but subparallel TCA. Moderate silicification to margins 1800 180.50 181.15 0.65 TRACE TRACE 4 TRACE 37 1 TRACE of vein, with <1% finely disseminated pyrite. 1801 181.15 182.15 1.00 36 0.3 277 TRACE 36 TRACE TRACE

162.8-163.8: Pyrite <1%.

163.8-166.0: Pyrite 10% locally, but 2% overall. Trace chalcopyrite.

166.0-169.0: Pyrite <0.5%.

169.0-170.3: Includes a 30cm wide patche of quartz-calcite veining, with fine tourmaline and/or chlorite, and epidote. Oriented very oblique TCA. Pyrite <1%, as blebs and disseminations.

No: CDR9936

Cameco Gold Inc.




170.3-173.5: Pyrite 1% as wisps and stringers.

173.5-181.2: Pyrite <0.5%, as occasional wisps and stringers.

Bleaching by carbonate is absent, rock is relatively unaltered.

181.2-182.2: Quartz veining, 15%, parallel to ca, with calcite

and epidote. Interval also includes one quartz-calcite

stringer/veinlet with 5% pyrite and 2% chalcopyrite. Overall, pyrite <1%, and trace chalcopyrite.

182.2 264.3 (VOLCANICLASTIC CONGLOMERATE TO PEBBLY SANDSTONE) 1802 182.15 183.50 1.35 7 TRACE 11 TRACE 37 2 TRACE 1803 202.00 203.30 1.30 TRACE TRACE 3 TRACE 52 1 TRACE

Rock type is the same as previously described volcaniclatic 1804 203.30 204.00 0.70 17 TRACE 6 TRACE 60 TRACE TRACE sediments, comprising over 80% polymictic conglomerate and 20% 1805 204.00 205.50 1.50 16 TRACE 35 TRACE 55 TRACE TRACE pebbly sandstone. The clasts are up to 20cm wide, aver. 2c, 1806 205.50 207.00 1.50 71 TRACE 83 TRACE 39 TRACE TRACE appear intermediate to felsic, subrounded, quartz-mafic phyric, 1807 207.00 208.50 1.50 5 TRACE 35 TRACE 33 TRACE TRACE quartz-feldspar phyric, and aphyric. The clasts are 1808 208.50 210.00 1.50 TRACE TRACE 53 TRACE 58 TRACE TRACE preferentially epidotized, which varies from moderately 1809 261.60 261.80 0.20 17 TRACE 361 TRACE 94 TRACE TRACE pervasive near 182.15m, gradually decreasing to occasional patches

beyond 203m downhole. This is accompanied by a gradual decrease

in alteration of the matrix from weakly chloritized to essentially

non-chloritized. Quartz-calcite stringers essentially absent,

trace. Pyrite <0.5%, 1% locally as fine disseminations to

occasional seams. Foliation weak, at 55 deg. TCA.

199.5-199.8: Weak shistosity at 60 deg. TCA, with moderate

chloritization, very weak sericitization, and trace hematite

within 1-2% quartz-calcite stringers parallel to schistosity.

Pyrite 0.5% wisps.

No: CDR9936

Cameco Gold Inc.



ASSAYS FROM

TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM TO WIDTH Au (ppb) Ag (g/t) Cu (ppm) Pb (ppm) Zn (ppm) Mo (ppm) As (ppm)

203.5-210.0: Weakly chloritized, carbonatized (calcite)

interval, with 1% very fine disseminated to seams and stringers of pyrite. No chalcopyrite noted.

210.0-264.3: Monotonous interval of polymictic volcanicalstic

conglomerate as previously described, relatively unaltered (very

weakly carbonatized and chloritic to sericitic) and unmineralized, with less than 0.5% pyrite, mostly as fine disseminations.

Quartz-carbonate stringers and veinlets <1%. Foliation weak, at 63 deg. TCA.

261.7: Amygdaloidal clast, 3 to 4 can wide and about 7 or 8 cm

long. The clast is fine grained and intermediate in composition.

It contains about 20% amygdules, up to 5 mm in diameter, mainly

filled with epidote and/or chlorite, minor calcite, <1% pyrite and trace chalcopyrite.

264.30: EOH

Whole rock samples:

CDR9936-A: 18.0-21.0: Weakly altered feldspar porphyry.

CDR9936-B: 32.7-35.7: Fractured, mineralized and chloritized

felspar porphyry.

CDR9936-C: 44.0-47.0: Weakly altered and non mineralized feldspar

porphyry.

CDR9936-D: 71.0-74.0: Non mineralized feldspar porphyry.

CDR9936-E: 91.0-94.0: Intermediate felspar porphyry.

CDR9936-F: 109.0-111. 0: Intermediate feldspar porphyry.

No: CDR9936

Cameco Gold Inc.




CDR9936-G: 148.0-151.0: Intermediate feldspar porphyry.


21.2 m: Mineralized (cpy, py) feldspar porphyry for thin section.

33.0 m: Mineralized (cpy, py), fractured and chloritized felspar porphyry for thin section..

46.3 m: Mineralized (py) feldspar porphyry for thin section.






93.60 -52.00

124.00 -52.00

166.80 -50.00

258.20 -52.00

No: CDR9936

Cameco Gold Inc.

DIAMOND DRILL LOG PROPERTY: Cedar Rapids HOLE No.: CDR9937 Collar Eastings: 1290.00 Collar Northings: 805.00 Collar Elevation: 290.00 Grid: Rotated Claim#: 5126359

Collar Inclination: -50.00 Logged by: D. BABIN Grid Bearing: 50.00 Date: 28/09/99-03/10/99 Final Depth: 404.50 metres Down-hole Survey: ACID TEST Val d'Or Drilling Core: NQ Test depth and NW strike extension of Village Zone


0 47.5 (OVERBURDEN)

SAMPLE No. FROM TO WIDTH Au (ppb) Au rej.

ASSAYS

Au ave. Ag (g/t) Cu (ppm) Pb (ppm) Zn (ppm) Ho (ppm)

47.5 276.2 (INTERMEDIATE VOLCANICLASTIC ROCK) 1810 51.10 52.60 1.50 15 N.A. 0.015 0.4 86 TRACE 70 2 1811 52.60 54.10 1.50 18 N.A. 0.018 0.3 10 3 81 2

Medium dark green, moderately hard, non magnetic, competent 1812 54.10 55.60 1.50 8 N.A. 0.008 0.3 6 TRACE 79 1 (RQD>90-95), weakly to moderately chloritic, intermediate 1813 55.60 57.10 1.50 TRACE N.A. TRACE 0.3 13 TRACE 74 1 volcaniclastic sequence composed of thickly bedded, matrix to 1814 57.10 58.60 1.50 TRACE N.A. TRACE 0.2 6 TRACE 62 1 clast supported, granule to cobble conglomerate, fine to coarse 1815 58.60 60.10 1.50 TRACE N.A. TRACE TRACE 4 TRACE 59 TRACE sandstone and laminated tuffaceous mudstone beds. Beds are <1 cm 1816 80.50 81.50 1.00 9 N.A. 0.009 0.3 113 TRACE 49 1 to >2 metres thick. Above 95 m, the sequence comprises 50% 1817 81.50 82.50 1.00 13 N.A. 0.013 0.3 112 TRACE 48 1 conglomerate and 50% fine to coarse sandstone beds, with only very 1818 82.50 83.50 1.00 TRACE N.A. TRACE 0.2 20 TRACE 42 1 rare mudstone laminae. Below 95 m, the sequence is composed of 1819 83.50 84.50 1.00 TRACE N.A. TRACE 0.3 13 TRACE 46 2 90% very fine to pebbly sandstone beds, 5% granule conglomerate 1820 84.50 86.00 1.50 TRACE N.A. TRACE 0.2 18 TRACE 44 1 beds and 5% laminated mudstone intervals. Foliation is weak to 1821 86.00 86.90 0.90 18 N.A. 0.018 0.2 54 TRACE 54 2 moderate and is oriented parallel to bedding at 30 to 35 deg. TCA. 1822 86.90 87.40 0.50 395 N.A. 0.395 2.0 2605 TRACE 69 2 Most of the clasts seen in the conglomeratic units and pebbly 1823 87.40 88.40 1.00 TRACE N.A. TRACE 0.3 37 2 57 1 sandstone beds are light grey to buff, fine grained and relatively 1824 94.10 95.10 1.00 30 N.A. 0.030 0.4 134 3 49 2 hard. They seem intermediate to felsic in composition. There are 1825 95.10 95.40 0.30 309 N.A. 0.309 0.7 462 TRACE 60 1 only traces of disseminated to fracture-controlled, fine grained 1826 95.40 96.40 1.00 225 N.A. 0.225 0.4 90 2 54 2 pyrite throughout (exceptions are mentioned below). About 1 to 3% 1827 98.70 100.20 1.50 25 N.A. 0.025 0.2 12 TRACE 50 1 grey quartz-calcite+/-chlorite stringers, oriented generally at 40 1828 105.20 106.20 1.00 6 N.A. 0.006 0.2 11 TRACE 56 TRACE to 45 deg. TCA, crosscut the foliation. Some of these stringers 1829 106.20 106.60 0.40 99 N.A. 0.099 0.9 505 TRACE 64 2 have a chloritic alteration halo up to 5 mm thick. It is possible 1830 106.60 107.60 1.00 15 N.A. 0.015 0.2 20 TRACE 61 2 to see several generations of these stringers, crosscutting and 1831 107.60 108.10 0.50 8 N.A. 0.008 0.5 35 7 73 2 offsetting each other. 1832 112.00 113.00 1.00 35 N.A. 0.035 0.3 88 3 43 2

No: CDR9937

Cameco Gold Inc.


FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM TO WIDTH Au (ppb) Au rej. ASSAYS

Au ave. Ag (g/t) Cu (ppm) Pb (ppm) Zn (ppm) Mo (ppm)

1833 113.00 114.00 1.00 88 N.A. 0.088 0.5 119 4 39 3 52.6 71.4 (Epidotized volcaniclastic rock) 1834 114.00 114.80 0.80 118 N.A. 0.118 0.2 34 TRACE 42 3 Same as main description, but there are about 5%, sub-rounded, diffuse to sharp epidote-silica patches, few millimetres to 10 cm

1835 1836

114.80 115.30

115.30 116.30

0.50 1.00

240 12

N.A. N.A.

0.240 0.012

0.5 0.2

33 9

4 TRACE

44 49

5 2

in diameter. Foliation seems to divert from these patches. No 1837 132.50 133.50 1.00 TRACE N.A. TRACE 0.2 29 TRACE 55 1 significant sulphides (trace pyrite only) are seen in this 1838 133.50 135.00 1.50 TRACE N.A. TRACE 0.2 25 TRACE 49 1 interval. 1839 135.00 136.00 1.00 TRACE N.A. TRACE 0.2 2 TRACE 45 1

1840 136.00 137.40 1.40 TRACE N.A. TRACE 0.3 30 TRACE 60 2 81.5-82.5: Interval with 1% disseminated, medium grained euhedral 1841 137.40 138.40 1.00 TRACE N.A. TRACE 0.2 43 3 35 1 pyrite (cubic), some concentrated within the alteration halo 1842 138.40 139.70 1.30 TRACE N.A. TRACE 0.3 43 3 45 1 (chloritized) of a 2 mm wide quartz-carbonate-chlorite stringer. 1843 139.70 141.40 1.70 TRACE N.A. TRACE 0.2 11 2 28 1

1844 141.40 142.20 0.80 TRACE N.A. TRACE TRACE 5 3 44 1 86.9-87.4: 5 mm wide quartz-calcite-carbonate-chlorite stringer 1845 142.20 143.70 1.50 156 N.A. 0.156 0.7 261 8 66 2 oriented at 10 deg. TCA and containing about 20% chalcopyrite with 1846 143.70 144.70 1.00 TRACE N.A. TRACE TRACE 2 3 101 1 minor pyrite. Redistributed over the 50 cm interval, there are 1847 144.70 145.80 1.10 TRACE N.A. TRACE TRACE 1 TRACE 92 2 about 2% chalcopyrite and <1% pyrite_ 1848 145.80 146.30 0.50 TRACE N.A. TRACE TRACE 2 TRACE 50 2

1849 146.30 147.30 1.00 TRACE N.A. TRACE TRACE 1 2 97 2 93.3-95.8: Coarsest, non magnetic conglomeratic bed, one of the 1850 153.00 153.40 0.40 188 N.A. 0.188 0.5 293 3 120 2 rare clast-supported and polymictic interval. Maximum width of 1851 176.00 177.00 1.00 TRACE N.A. TRACE TRACE 6 TRACE 38 3 the angular to sub-rounded cleats is 5 cm, but the average is 1852 178.80 179.80 1.00 TRACE N.A. TRACE TRACE 10 TRACE 33 2 about 1 to 2 cm. The clast size increases downhole within the bed 1853 179.80 180.80 1.00 100 N.A. 0.100 0.5 255 TRACE 46 2 (probably a graded bed indicating a top uphole). All clasts are 1854 180.80 181.80 1.00 60 N.A. 0.060 0.5 310 2 47 1 fine grained and vary in colour from very light grey (felsic 1855 181.80 182.80 1.00 89 N.A. 0.089 0.5 336 TRACE 43 2 clasts), to medium grey (intermediate clasts), to very dark green 1856 196.20 197.20 1.00 TRACE N.A. TRACE TRACE 9 TRACE 40 2 (chloritic mafic clasts). Most clasts and the matrix are altered 1857 197.20 197.50 0.30 14 N.A. 0.014 0.2 278 4 44 3 to about 5% elongated biotite specks 2 to 3 mm long. The biotite 1858 197.50 199.00 1.50 TRACE N.A. TRACE 0.4 231 TRACE 54 2 alteration does not extend more than 40 cm outside this bed. Only 1859 199.00 200.50 1.50 TRACE N.A. TRACE TRACE 21 TRACE 45 2 traces of pyrite are seen, except from 95.1 to 95.4 m, where 1 to 1860 200.50 201.00 0.50 138 N.A. 0.138 0.9 369 TRACE 54 4 2% medium grained, disseminated euhedral pyrite is observed. This 1861 201.00 202.00 1.00 TRACE N.A. TRACE TRACE 3 TRACE 49 2 latter pyritic zone is intruded by two dark grey, quartz- 1862 202.00 203.40 1.40 TRACE N.R. TRACE TRACE 19 TRACE 46 1

No: CDR9937

Cameco Gold Inc.


FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM TO WIDTH Au (ppb) Au rej.

ASSAYS

Au ave. Ag (g/t) Cu (ppm) Pb (ppm) Zn (ppm) Mo (ppm)

carbonate-biotite stringers, 2 mm and 1 cm wide. 1863 203.40 204.40 1.00 73 N.A. 0.073 0.2 85 TRACE 65 2 1864 204.40 205.50 1.10 208 N.A. 0.208 0.6 539 TRACE 66 5

96.05-96.15: Light pink quartz-carbonate vein, with minor chlorite 1865 205.50 206.80 1.30 8 N.A. 0.008 0.5 68 TRACE 48 2 and pyrite. The vein is oriented at 35 deg. TCA. Less than 1% 1866 206.80 208.10 1.30 18 N.A. 0.018 0.4 69 TRACE 47 3 medium grained cubic pyrite is disseminated near the margins of 1867 208.10 209.60 1.50 TRACE N.A. TRACE TRACE 40 TRACE 43 2 the vein. 1868 209.60 211.10 1.50 9 N.A. 0.009 0.4 174 TRACE 45 3

1869 211.10 212.60 1.50 112 N.A. 0.112 0.5 403 TRACE 65 5 98.7: 3 am quartz-carbonate-chlorite vein very similar to 96.05 to 1870 212.60 214.10 1.50 1038 N.A. 1.038 0.5 205 TRACE 49 2 96.15 m. 1% cubic pyrite near the margins of the vein. 1871 214.10 215.60 1.50 TRACE N.A. TRACE 0.2 104 TRACE 48 2

1872 215.60 217.10 1.50 TRACE N.A. TRACE 0.4 53 TRACE 73 1 100.15: Same as 98.7 m. 1873 217.10 218.50 1.40 TRACE N.A. TRACE TRACE 45 TRACE 41 1

1874 218.50 219.50 1.00 70 N.A. 0.070 0.6 343 TRACE 99 2 106.3-106.6: Weakly biotitized interval (5 to 10% biotite specks, 1875 219.50 220.50 1.00 338 N.A. 0.338 2.5 1735 TRACE 71 2 <2 mm in size) cut by a 2 mm quartz-carbonate-biotite stringer 1876 220.50 221.60 1.10 2857 3.06 2.959 5.5 3133 TRACE 82 3 oriented at 10 deg. TCA (crosscut the foliation) and containing 1877 221.60 222.50 0.90 96 N.A. 0.096 0.5 376 TRACE 48 2 10% chalcopyrite and minor pyrite. Overall, the interval contains 1878 222.50 223.50 1.00 7 N.A. 0.007 0.3 43 TRACE 43 TRACE <0.5% chalcopyrite and pyrite. 1879 225.20 225.50 0.30 112 N.A. 0.112 1.5 861 TRACE 78 1

1880 229.30 230.50 1.20 115 N.A. 0.115 0.2 115 TRACE 44 2 107.8-108.1: Interval containing 2 quartz veins, 3 cm and 8 cm 1881 234.70 235.60 0.90 17 N.A. 0.017 0.4 209 TRACE 58 2 wide, and oriented at 45 deg. TCA. The 8 cm wide quartz vein 1882 235.60 237.00 1.40 35 N.A. 0.035 0.4 290 TRACE 60 1 contains abundant carbonates, minor chlorite and about 10% albitic 1883 237.00 238.50 1.50 15 N.A. 0.015 0.4 244 TRACE 45 2 bands? Traces of medium grained, cubic pyrite are seen in the 1884 238.50 239.70 1.20 118 N.A. 0.118 1.0 1384 TRACE 45 3 veins and in the host rock near the margins of the veins. 1885 244.60 245.60 1.00 TRACE N.A. TRACE TRACE 40 TRACE 44 3

1886 245.60 247.20 1.60 152 N.A. 0.152 1.6 2054 TRACE 74 6 113.0-114.0: Fine to very fine grained sandstone interval cut by 2 1887 247.20 248.20 1.00 382 N.A. 0.382 4.3 6090 TRACE 136 5 quartz-calcite-chlorite/biotite stringers, less than 2 mm wide and 1868 248.20 249.70 1.50 221 N.A. 0.221 2.3 2752 TRACE 92 3 containing 10 to 20% pyrite with minor chalcopyrite. The 1889 249.70 251.20 1.50 21 N.A. 0.021 0.3 241 TRACE 62 2 stringers are oriented at 10 to 15 deg. TCA and crosscut the 1890 263.20 264.20 1.00 5 N.A. 0.005 TRACE 37 TRACE 24 2 foliation and bedding. Overall, <0.5% pyrite and traces of 1891 264.20 265.20 1.00 349 N.A. 0.349 0.4 723 TRACE 100 1 chalcopyrite are observed. 1892 265.20 266.20 1.00 6 N.A. 0.006 TRACE 97 TRACE 28 1

No: CDR9937

Cameco Gold Inc.


ASSAYS FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM TO WIDTH Au (ppb) Au rej. Au ave. Ag (g/t) Cu (ppm) Pb (ppm) 2n (ppm) Mo (ppm)

1893 266.20 267.20 1.00 218 N.A. 0.218 TRACE 76 2 26 7 114.85-115.3: Laminated mudstone interval, moderately chloritized 1894 267.20 268.20 1.00 13 N.A. 0.013 TRACE 49 TRACE 27 3 and containing 2 to 5% very fine grained pyrite concentrated along 1895 268.20 269.20 1.00 8 N.A. 0.008 TRACE 41 TRACE 26 4 the chloritized laminae and at the margins of quartz-carbonate- 1896 269.20 270.20 1.00 11 N.A. 0.011 TRACE 9 TRACE 32 TRACE chlorite veins and stringers, 1 mm to 3 cm< wide, oriented parallel 1897 270.20 271.00 0.80 75 N.A. 0.075 0.2 24 TRACE 30 TRACE to bedding and foliation at 35 deg. TCA. 1898 271.00 272.00 1.00 8 N.A. 0.008 TRACE 10 TRACE 28 TRACE

116.0-120.0: More blocky section (RQD=50-70).

127.7-128.3: Very blocky section (RQD=0).

133.5 146.3 (Bleached deformation zone) The volcaniclastic sequence is mainly composed of matrix supported pebbly sandstone, but at about 133.5 m, the rock becomes gradually bleached up to 137.4 m, where the interval becomes more chaotic and very blocky (RQD <30). The alteration consists of weak sericite, weak to moderate chlorite, 5% biotite specks (1 to 3 mm in size) and moderate to strong pervasive carbonate (little ankerite, more dolomite). The rock is strongly foliated at 20 deg. TCA from 137.4 to 139.7 m. From 139.7 to 142.2 m, the section is intruded by 40% very chaotic veins, 1 to 20 cm wide and oriented from 10 to 80 deg. TCA. The veins are mainly composed of milky quartz, associated with 10 to 30% (?) ankerite+dolomite, <5% chlorite and tourmaline, and 5 to 30% of a buff coloured, moderately hard, needle-like mineral (7). The rest of the interval is less foliated and altered, and only one major quartz- carbonate-chlorite-tourmaline vein (containing the unknown needle- like mineral) is seen from 145.8 to 146.2 m. <1% anhedral pyrite is seen throughout. Lower contact is approximate since the alteration and foliation decrease gradually downhole.

No: CDR9937

Cameco Gold Inc.


ASSAYS FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM TO WIDTH Au (ppb) Au rej. Au ave. Ag (g/t) Cu (ppm) Pb (ppm) Zn (ppm) Mo (ppm)

153.2: 1 to 2 mm wide quartz-calcite-pyrite-chlorite-filled fracture oriented at 10 to 15 deg. TCA.

159.9-160.0: Blocky core.

166.5-166.7: Very blocky core.

176.3-176.7: Laminated siliceous "mudstone" interval oriented at 10 deg. TCA, while above and below, the sandstone beds are oriented at 35 deg. TCA. It is crosscut by two, very irregular, 1 to 2 cm wide, quartz-carbonate-albite? veinlets. Trace pyrite.

179.0-179.6: Blocky core composed mainly of laminated siliceous mudstone beds, oriented at 25 deg. TCA. A rip-up clast at the interface between a mudstone and a sandstone bed indicates a paleostratigraphic top uphole.

179.8-181.7: Pebbly sandstone horizon, weakly epidotized and weakly to moderately chloritized/biotitized. The intensity of the pervasive alterations is very variable throughout the interval. 1% medium grained cubic pyrite (1 to 2 mm in size) is seen throughout.

197.2 222.5 (Weakly mineralized and deformed zone) From about 197.2 to 222.5,'the core becomes blockier (ROD <70) and the foliation/bedding orientation gradually changes to about 20 to 25 deg. TCA. The interval seems slightly more foliated than previously? The mineralization consists of quartz-carbonate- chlorite-sulphides stringers oriented at less than 15 deg. TCA and

No: CDR9937

Cameco Gold Inc.

DIAMOND DRILL LOG PROPERTY: Cedar Rapids HOLE No.: CDR9937 Page

ASSAYS FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM TO WIDTH Au (ppb) Au rej. Au ave. Ag (g/t) Cu (ppm) Pb (ppm) Zn (ppm) Mb (ppm)

often following the core axis. Stringers are 2 mm to 2 cm thick and are described below. Overall, the interval contains <1% pyrite and chalcopyrite.

197.3: 2 mm thick chlorite-quartz-carbonate stringer, oriented at 15 deg. TCA (parallel to bedding) and containing about 30% medium grained pyrite.

200.5-201.0: Quartz-dolomite+/-chlorite stringer, oriented parallel TCA. It is 2 mm thick at 200.5 m, but it becomes gradually thicker (2 cm) near 201.0 m. It contains about 1% pyrite and 0.5% chalcopyrite. The host rock is strongly chloritized over 2 to 3 mm at the margins of the stringer. The core is very blocky (fractured along the stringer).

203.4-205.5: Very blocky section of polymictic, granule to pebble conglomerate, cut by a 5 mm to 2 cm thick quartz-chlorite-dolomite stringer oriented parallel TCA. The stringer contains usually less than 5% fine-grained pyrite, but at 205.2 m, it contains 2 to 5% chalcopyrite. The host rock is strongly chloritized over 5 mm to 2 cm on each sides of the stringer.

206.9-208.0: White quartz-dolomite-chlorite stringer oriented parallel TCA. It is 2 mm thick at 207.0 m, but thickens to 2 cm about 207.5 m. It contains only traces of pyrite (chalcopyrite?). The host rock is strongly éhloritized over 2 to 4 mm on each sides of the stringer.

208.0-218.5: More competent interval, not mineralized and less foliated. Bedding is oriented at 25 deg. TCA. The sequence

No: CDR9937

Cameco Gold Inc.



consists of relatively unaltered coarse to pebbly sandstones

interbedded with laminated mudstones/siltstones. Only traces of

pyrite are found, mainly concentrated near 214.8 m, where a

chlorite-carbonate stringer just touches the edge of the core. It is <5 mm thick and oriented sub-parallel TCA.

218.5-222.5: Interval cut by a 5 mm thick quartz-chlorite-dolomite

stringer, oriented parallel TCA. The stringer is vuggy in places and contains 5 to 30% pyrite and <5% chalcopyrite. The core is very blocky and fractured along the stringer. The chloritic alteration halo is very thin (<3 mm). The stringer crosscuts the

bedding (10 to 15 deg. TCA)and earlier, non mineralized quartz-

carbonate-filled fractures. Below 222.5, the bedding and

foliation are back at 35 to 40 deg. TCA.

225.3-225.5: 1 cm thick, quartz-carbonate-chlorite stringer,

oriented parallel TCA and containing about 10 to 15% pyrite and

minor chalcopyrite. The core is very blocky.

229.3-230.5: Interval containing about 1% pyrite cubes up to 5 mm

in size. They are concentrated along tiny chloritic fractures and

near the margins of grey quartz-carbonate veinlets. These

veinlets are 1 to 1.5 cm wide, oriented at 20 to 40 deg. TCA, and

exhibit a light grey, strongly silicified+carbonatized alteration

halo, up to 4 mm thick. From 230.1 to 230.3, the core is strongly

fractured and chaotic. Its probably represents a weak brittle

fault.

234.7-235.6: Interval intruded by about 10 to 20% white, very

irregular, 5 mm to 5 cm wide, quartz-carbonate-chlorite veinlets,

No: CDR9937

Cameco Gold Inc.



crosscutting foliation and bedding at various angles. Trace cubic

pyrite, disseminated in the host rock and in the chloritic part of the veinlets.

235.6-239.7: Relatively unaltered volcaniclastic section, cut by

less than 1% hairline thin chloritic fractures containing medium

grained (2 to 4 mm) pyrite cubes. The fractures are oriented at 10 to 20 deg. TCA. Overall, the interval contains about 1%

pyrite, mainly in these fractures but also disseminated throughout.

239.0-239.5: Very blocky core.

245.6-247.2: Moderately to strongly chloritized section (pervasive

and fracture-controlled alteration) containing about 5 to 10%

medium grained, anhedral to cubic disseminated pyrite (<1 to 4 mm in size), located along and near the margins of a dark grey

quartz-chlorite+/-carbonate stringer oriented sub-parallel TCA (<1

cm thick). Minor chalcopyrite is also observed within the

stringer. <5% biotite specks are also present within this section.

247.2-259.0: Relatively unaltered volcaniclastic section

containing maximum 1% medium grained (2 to 4 mm) disseminated

cubic pyrite throughout.

259.0-276.2: The volcaniclastic sandstones and mudstones gradually

become more and more chloritic and finer grained from 259.0m

downhole. The rock becomes darker and darker as the pervasive

chloritic alteration becomes stronger. From about 266.2 to

271.4 m, the rock is cut by a network of hairline thin chloritic

No: CDR9937

Cameco Gold Inc.


ASSAYS SAMPLE No. FROM TO WIDTH Au (ppb) Au raj. Au ave. Ag (g/t) Cu (ppm) Pb (ppm) Zn (ppm) MO (ppm)

1899 278.00 279.50 1.50 6 N.A. 0.006 TRACE 69 4 57 2 1900 279.50 281.00 1.50 14 N.A. 0.014 0.4 198 12 193 2 1901 281.00 282.20 1.20 11 N.A. 0.011 TRACE 97 2 65 1 1902 282.20 283.00 0.80 32 N.A. 0.032 0.3 104 TRACE 119 - TRACE 1903 283.00 284.50 1.50 18 N.A. 0.018 TRACE 113 6 45 2 1904 284.50 286.00 1.50 25 N.A. 0.025 TRACE 137 TRACE 72 2 1905 286.00 287.50 1.50 19 N.A. 0.019 TRACE 148 TRACE 72 2 1906 287.50 289.00 1.50 25 N.A. 0.025 0.4 192 3 99 3 1907 289.00 290.00 1.00 12 N.A. 0.012 0.3 169 TRACE 50 3 1908 290.00 291.00 1.00 5 N.A. 0.005 0.2 91 TRACE 26 1 1909 291.00 292.00 1.00 TRACE N.A. TRACE TRACE 81 TRACE 41 2 1910 292.00 292.60 0.60 TRACE N.A. TRACE 0.3 181 TRACE 65 TRACE 1911 292.60 294.00 1.40 6 N.A. 0.006 TRACE 130 TRACE 23 TRACE 1912 294.00 295.50 1.50 TRACE N.A. TRACE TRACE 205 TRACE 29 2 1913 295.50 297.00 1.50 38 N.A. 0.038 TRACE 565 2 65 1 1914 297.00 298.50 1.50 TRACE N.A. TRACE TRACE 319 TRACE 21 2 1915 298.50 300.00 1.50 TRACE N.A. TRACE TRACE 270 TRACE 22 2 1916 300.00 301.00 1.00 TRACE N.A. TRACE 0.3 336 TRACE 32 2 1917 301.00 302.00 1.00 TRACE N.A. TRACE 0.3 394 TRACE 32 2 1918 302.00 302.50 0.50 9 N.A. 0.009 1.1 1770 TRACE 46 9


fractures containing very fine grained pyrite and minor pyrrhotite. Minor pyrite and pyrrhotite anhedral blebs within a quartz-chlorite-carbonate matrix, <5 mm across are seen throughout. Overall there are less than 1% pyrite and only traces of pyrrhotite.

269.0-282.0: The core is very blocky (RQD<50).

276.2 302.5 (PYRITE/PYRRHOTITE-RICH FELSIC TO INTERMEDIATE TUFF/MUDSTONE)

Light to medium grey, blocky (RQD<80), non to moderately magnetic in places, strongly foliated and laminated felsic to intermediate aphyric rock (tuff or mudstone?). The sequence is made of light grey, +/-sericitized siliceous laminae (70-80%) interbedded with dark green chloritic ones (20-30%). The laminae/beds are <1 mm to >20 cm thick, but average about 1 cmi. Foliation is parallel to bedding and oriented at 40 deg. TCA at 276.5 m, but it gradually shallows to about 10 to 15 deg. TCA at 302.0 m. There is about 2 to 5% pyrite +/-pyrrhotite concentrated along chloritic laminae, chloritic fractures and as euhedral cubes, up to 1 cm across, showing quartz-carbonate-chlorite-filled oval shadow structures, up to 2 cm long.

282.2-282.9: Dark brownish green interval, intensely chloritic, with very sharp contacts oriented parallel to bedding (bed?). 1% very fine grained disseminated pyrite. 2 to 3% dark chloritic fractures oriented parallel to bedding. 2 to 3% discontinuous quartz-carbonate stringers, <5 mm wide and oriented parallel to foliation.

No: CDR9937

Cameco Gold Inc.


ASSAYS FROM TO LITHOLOGICAL DESCRIPTION

SAMPLE No. FROM TO WIDTH Au (ppb) Au rej. Au ave. Ag (g/t) Cu (ppm) Pb (ppm) Zn (ppm) Mb (ppm)

282.9-289.0: Section looking slightly more sericitized than the

rest of the sequence. There are about 5 to 10% yellowish

sericite-rich laminae/bands, 1 mm to 4 cm thick, interbedded with

the chloritic and more siliceous laminae. This section is also intruded by 5% quartz-carbonate stringers, <1.5 cm thick and

oriented parallel to foliation.

269.0 289.5 (Fault zone)

The upper 30 cm is composed of a chaotic brecciated zone composed

of grey quartz, white carbonate (dolomite? and minor ankerite) and

chlorite. <0.5% pyrite in chloritic fractures. The rest of the interval is strongly foliated, very soft (gouge) and composed of

sericite, chlorite and may be carbonate. Foliation is oriented at

30 deg. TCA.

291.4: 3 cm wide brecciated band, oriented perpendicular to

foliation. Bedding and foliation are completely disturbed.

Silica, sericite and minor chlorite are filling the numerous hairline thin fractures.

292.0 292.6 (Chloritic shear zone?)

Dark greenish brown, non magnetic, soft foliated interval,

composed mainly of chlorite, crosscut by about 10 to 20%

irregular, discontinuous, grey quartz-carbonate stringers, <1 cm

thick. The zone is oriented parallel to bedding at 30 deg. TCA. It could represent a mafic'tuffaceous bed? 2 to 5% fine grained

disseminated pyrite, mainly concentrated in the upper 6 cm of the

zone. Very sharp contact with the felsic tuff and some rip-up

clasts of the felsic tuff are seen within the upper 6 cm1.

No: CDR9937

Cameco Gold Inc.



292.6-298.6: The felsic tuff sequence is crosscut by a network of hairline thin chloritic fractures containing very fine grained pyrite. The fractures often exhibit the dendritic growth of chlorite and pyrite at their margins.

297.2-302.0: The core becomes weakly magnetic because of the presence of pyrrhotite associated with the pyrite, within the chioritic laminae. Maybe some traces of chalcopyrite.

302.0-302.5: Strongly magnetic contact zone showing may be 15 to 20% massive pyrrhotite (+/-magnetite) laminae, <5 mm thick, interbedded with 80 to 85% light grey, weakly sericitized siliceous laminae, up to 1 cm thick. 1% pyrite and <1% chalcopyrite are also seen in the sulphidic laminae.

302.5 322.0 (MINERALIZED AND PILLOWED MAFIC FLOW) 1919 302.50 303.50 1.00 82 N.A. 0.082 1.4 2192 TRACE 98 12 1920 303.50 304.50 1.00 20 N.A. 0.020 0.9 1413 TRACE 97 16

Dark green, competent (RQD>99), moderately soft, fine grained 1921 304.50 305.60 1.10 TRACE N.A. TRACE 0.6 300 TRACE 103 2 mafic rock generally non magnetic except from 302.5 to about 305.6 1922 305.60 306.60 1.00 21 N.A. 0.021 0.8 610 TRACE 98 3 m. It is very similar to the pillowed unit observed in holes 1923 306.60 307.60 1.00 23 N.A. 0.023 0.6 642 TRACE 84 7 CDR9701, CDR9702, CDR9706 and CDR9830. The interval is moderately 1924 307.60 308.60 1.00 61 N.A. 0.061 1.1 1172 TRACE 86 3 to strongly chloritized and moderately ankeritized seen as 1925 308.60 309.60 1.00 21 N.A. 0.021 0.6 286 TRACE 83 4 subhedral specks < 1 mm in size. The rock is relatively weakly 1926 309.60 311.00 1.40 122 N.A. 0.122 2.3 1805 TRACE 88 5 foliated and the orientation of the foliation is very variable 1927 311.00 311.50 0.50 5 N.A. 0.005 0.4 189 TRACE 78 2 (follow the selvages). It is cut by about 5% quartz-dolomite- 1928 311.50 312.50 1.00 430 N.A. 0.430 2.5 5229 TRACE 103 5 ankerite stringers, <1 cm thick, oriented in all directions. Over 1929 312.50 313.50 1.00 43 N.A. 0.043 1.1 823 TRACE 78 2 all, the mineralization consists of <5% medium to fine grained 1930 313.50 314.50 1.00 75 N.A. 0.075 1.3 1183 TRACE 75 TRACE pyrite and <0.5% chalcopyrite, concentrated in stringers, up to 1931 314.50 315.50 1.00 55 N.A. 0.055 1.1 938 TRACE 87 1 2 cm wide, between pillow selvages. About 1 to 2% additional fine 1932 315.50 316.50 1.00 96 N.A. 0.096 1.5 1423 TRACE 84 TRACE grained pyrite is seen disseminated throughout. The stringers 1933 316.50 317.50 1.00 55 N.A. 0.055 0.8 558 TRACE 74 1

NO: CDR9937

Cameco Gold Inc.




contain up to 80% sulphides within a matrix of quartz-chlorite- 1934 317.50 318.50 1.00 53 N.A. 0.053 1.1 967 TRACE 74 1 carbonate (dolomite?+ankerite) and minor black specks of biotite? 1935 318.50 319.50 1.00 TRACE N.A. TRACE 0.4 59 TRACE 71 1 less than 1 mm in size. They are oriented anywhere from 10 to 70 1936 319.50 320.50 1.00 10 N.A. 0.010 0.5 173 TRACE 68 TRACE deg. TCA. Pillow selvages are seen as laminated, strongly 1937 320.50 321.50 1.00 16 N.A. 0.016 0.8 522 TRACE 74 1 chloritic bands, <2 am thick, sometimes forming triple junctions. The mafic flow could be weakly variolitic, but possible varioles are very faint and small (1 mm).

302.5-303.7: Upper contact zone with the tuff is very irregular and shows two "fingers" of mafic rock coming into the sediments sub-parallel to foliation at 10 deg. TCA. Between the mafic "fingers", there is a 1 cm wide horizon composed of 50% massive pyrrhotite, 1 to 2% chalcopyrite, and 45 to 50% quartz-carbonate and felsic tuff fragments.

303.7-305.5: Moderately magnetic interval mineralized with only 1 to 2% very fine grained disseminated pyrite and pyrrhotite, and minor magnetite.

305.5-309.6: <3-5% fine grained pyrite, disseminated throughout and concentrated in 3 or 4 very faint, strongly chloritic pillow selvages, 1 to 2 cm wide.

309.6-317.5: Between 5 and 10% medium grained pyrite and about 1% chalcopyrite concentrated in sulphide-quartz-carbonate-biotite stringers, up to 3 cm wide'and located between pillow selvages. The main stingers are located at 309.75 m, from 310.1 to 310.3 m, at 310.85 m, from 311.6 to 311.75 m, at 312.0 and 312.4 m. All of them contain 1 to 2% chalcopyrite, except from 311.6 to 311.75 m, where about 5 to 10% chalcopyrite is present in the stringer.

No: CDR9937

Cameco Gold Inc.



317.5-321.0: Maybe 5% fine to medium grained pyrite and <0.5% chalcopyrite concentrated in chloritic pillow selvages? Not as much quartz and carbonate as before between the pillow selvages.

321.0-322.0: 5% pyrite and <0.5% chalcopyrite in pillow selvages. 5% medium grey, siliceous material is also seen near the pillow selvages. It looks like the material filling the spaces between the mafic clasts in holes CDR9706 and CDR9930. Maybe a low temperature hydrothermal silica event?

322.0 327.1 (MASSIVE MAFIC FLOW/SILL)

Very similar rock as before, but pillow selvages are less obvious. Could be a massive facies of the flow above? 1 to 2% stringer pyrite and traces of chalcopyrite.

327.1 337.4 (CARBONATIZED AND BIOTITIC MASSIVE MAFIC ROCK)

Very dark green, soft, non magnetic, very weakly to non foliated, massive mafic rock (RQD >95), strongly altered to ankerite, dolomite and biotite seen as euhedral to subhedral specks <1 mm in size. The alteration intensity is very variable (comes and goes) The rock is crosscut by a network of quartz-carbonate stringers, generally <1 cm thick, representing from 5 to 10% of the rock. The matrix of the rock is éphyric and mainly composed of chlorite and biotite? (not much talc). There are only traces of sulphide (pyrite and chalcopyrite), except in few stringers as mentioned below. Upper contact with the mafic flow is very sharp and straight, and it is oriented at 45 deg. TCA. When foliation is

1938 321.50 322.50 1.00 43 N.A. 0.043 1.3 1155 TRACE 82 TRACE 1939 322.50 324.00 1.50 TRACE N.A. TRACE 0.5 102 TRACE 58 TRACE 1940 324.00 325.50 1.50 9 N.A. 0.009 0.4 105 TRACE 61 TRACE 1941 325.50 327.10 1.60 10 N.A. 0.010 0.6 216 TRACE 63 TRACE

1942 327.10 328.10 1.00 8 N.A. 0.008 0.6 79 TRACE 64 TRACE 1943 328.10 329.10 1.00 TRACE N.A. TRACE 0.6 112 TRACE 61 TRACE 1944 329.10 330.50 1.40 7 N.A. 0.007 0.5 76 TRACE 52 TRACE 1945 330.50 332.00 1.50 10 N.A. 0.010 0.5 79 TRACE 57 TRACE 1946 332.00 333.50 1.50 TRACE N.A. TRACE 0.4 81 TRACE 57 TRACE 1947 333.50 335.00 1.50 6 N.A. 0.006 0.4 84 TRACE 61 TRACE 1948 335.00 336.50 1.50 TRACE N.A. TRACE 0.3 106 TRACE 71 TRACE

No: CDR9937

Cameco Gold Inc.



visible, it is oriented at 20 to 25 deg. TCA.

327.25: 5 mm stringer composed of 20 to 30% pyrite, 50 to 60% quartz-calcite-carbonate and 10 to 20% chlorite/biotite.

328.3: Traces of chalcopyrite in a 5 mm thick stringer similar to above, oriented at 20 to 30 deg. TCA.

337.15 337.4 (Fault Zone) Very blocky core. Fault zone?

337.4 355.7 (MASSIVE ULTRAMAFIC TO MAFIC FLOW/SILL) 1949 336.50 338.00 1.50 TRACE N.A. TRACE 0.4 84 TRACE 66 TRACE 1950 338.00 339.50 1.50 9 N.A. 0.009 0.3 90 TRACE 65 TRACE

Very similar rock as above, but it appears more mafic to 1951 339.50 341.00 1.50 TRACE N.A. TRACE 0.3 34 TRACE 65 TRACE ultramafic in composition. Upper and lower contacts are bounded 1952 341.00 342.50 1.50 8 N.A. 0.008 0.3 41 TRACE 61 TRACE by blocky core, probably brittle faults. 1953 342.50 344.00 1.50 TRACE N.A. TRACE 0.2 37 TRACE 62 TRACE

1954 344.00 345.50 1.50 10 N.A. 0.010 0.2 70 TRACE 58 TRACE 345.7: 3 cm wide strongly foliated gouge core, intruded by 2 1955 345.50 346.90 1.40 TRACE N.A. TRACE 0.3 26 TRACE 59 TRACE quartz-carbonate veinlets <1 cm thick. Foliation at 28 deg. TCA. 1956 346.90 347.10 0.20 20 N.A. 0.020 1.0 90 TRACE 68 TRACE

1957 347.10 348.50 1.40 TRACE N.A. TRACE 0.2 60 TRACE 60 TRACE 347.0: Series of 6 parallel, pyritic quartz-carbonate stringers, 1958 348.50 350.00 1.50 TRACE N.A. TRACE 0.2 4 TRACE 48 TRACE <5 mm thick, oriented at 25 deg. TCA. From 346.9 to 347.1 m, 1959 350.00 351.50 1.50 9 N.A. 0.009 0.2 67 TRACE 49 TRACE there is about 5% pyrite overall. 1960 351.50 353.00 1.50 TRACE N.A. TRACE TRACE 34 TRACE 53 TRACE

1961 353.00 354.50 1.50 48 N.A. 0.048 0.5 498 TRACE 60 TRACE 347.9-348.0: Similar foliated gouge section as from 345.7 m. Quartz-carbonate veinlets ire up to 2 cm wide.

355.7 365.6 (CARBONATIZED AND BIOTITIC MASSIVE MAFIC ROCK) 1962 354.50 356.00 1.50 56 N.A. 0.056 0.6 391 TRACE 63 TRACE 1963 356.00 357.50 1.50 9 N.A. 0.009 0.5 97 TRACE 54 TRACE

Same description as from 327.1 to 337.4 m. 1964 357.50 359.00 1.50 38 N.A. 0.038 0.4 238 TRACE 61 TRACE

No: CDR9937

Cameco Gold Inc.


FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM TO WIDTH Au (ppb) Au rej. ASSAYS

Au ave. Ag (g/t) Cu (ppm) Pb (ppm) Zn (ppm) Mb (ppm)

1965 359.00 360.70 1.70 2867 3.28 3.074 1.5 31 TRACE 55 TRACE 355.7 356.5 (Brittle fault?) 1966 360.70 361.30 0.60 1114 1.09 1.102 1.7 1611 TRACE 75 TRACE Very blocky section. Part of the core seems brecciated. Could be 1967 361.30 361.90 0.60 454 0.40 0.427 0.8 812 TRACE 78 1 a brittle fault? 1968 361.90 362.60 0.70 3741 3.03 3.386 4.7 9710 TRACE 93 1

1969 362.60 363.20 0.60 1448 1.64 1.544 0.9 544 TRACE 87 1 357.5-358.6: Blocky section (RQD <20) with about 0.5 to 1% pyrite 1970 363.20 364.20 1.00 1937 1.86 1.899 0.9 1266 TRACE 79 1 and traces of chalcopyrite in quartz-carbonate stringers <5 mm 1971 364.20 364.70 0.50 1230 2.58 1.905 0.8 540 TRACE 77 2 wide. 1972 364.70 365.60 0.90 3065 4.14 3.603 1.6 2073 TRACE 71 2

360.7 365.6 (Mineralized mafic rock) Same massive mafic/ rock as in main description, but it is mineralized with maximum 1% chalcopyrite and <0.5% pyrite concentrated in quartz-carbonate stringers mentioned below. The stringers appear to be associated with a chloritic alteration halo, <1 cm wide. The stringers are oriented anywhere from 40 to parallel TCA.

360.77 and 361.2: Series of four stringers, <5 ram thick, containing between 10 and 25% chalcopyrite and <1% pyrite.

361.2-361.3: Strongly foliated chloritic section intruded by 25 to 30% quartz-carbonate stringers, <5 mm thick (some are mineralized as mentioned above). Foliation and stringers are oriented at 28

deg. TCA.

361.9-362.6: Section with about 5% chalcopyrite and 1% pyrite concentrated in quartz-carbonate stingers, <2 cm wide. There are little sulphides in the host rock. Some of these stringers could occupy the spaces between pillow selvages, specially the irregular one following the core axis from 362.36 to 362.6 m. The stringers

No: CDR9937

Cameco Gold Inc.



are composed of 50 to 60% dark grey quartz, 10 to 40% white

ankerite and calcite, and 10 to 30% disseminated anhedral chalcopyrite and <5% fine grained cubic pyrite.

363.2-365.6: Weakly magnetic section, probably due to minor

disseminated magnetite present in the matrix of the rock.

364.6: 1 cm wide stringer, as described from 361.9 to 362.6 m, but containing about 20% fine grained pyrite with less than 1% chalcopyrite.

365.3-365.6: Very blocky section. Could be a fault zone at the

contact between the ultramafic? unit above and the variolitic

mafic flow below. From 365.5 to 365.6 m, the rock is strongly

foliated and intruded by 80% white, quartz-carbonate-chlorite veinlets, <1.5 cm thick. Foliation and veinlets are oriented at 40 deg. TCA.

365.6 378.2 (MINERALIZED AND VARIOLITIC PILLOWED MAFIC FLOW)

Dark green, moderately soft, very weakly foliated, variolitic,

fine grained mafic rock. The rock is weakly carbonatized and

epidotized throughout, except along possible pillow selvages, where the rock is strongly chloritized. The chloritic selvages,

<3 cm wide, contain minor magnetite (weakly to strongly magnetic) and represent about 15 to 40% of the section. The mineralization is located between these chloritic zones and consists of irregular

quartz-sulphide-carbonate stringer up to 5 or 6 cm thick as

described from 361.9 to 362.6 m. Overall, the section contains about 2 to 3% chalcopyrite and pyrite. The orientation of the

1973 365.60 366.40 0.80 877 0.88 0.879 0.9 217 TRACE 78 TRACE 1974 366.40 367.00 0.60 6159 6.30 6.230 4.0 4364 TRACE 108 1 1975 367.00 368.00 1.00 1388 0.94 1.164 0.7 839 TRACE 90 TRACE 1976 368.00 369.00 1.00 2116 2.16 2.138 1.3 1870 TRACE 91 1 1977 369.00 369.70 0.70 2012 2.58 2.296 1.6 2069 TRACE 82 TRACE 1978 369.70 370.70 1.00 4273 3.12 3.697 2.4 2937 TRACE 78 TRACE 1979 370.70 371.70 1.00 812 0.48 0.646 1.3 1772 TRACE 79 TRACE 1980 371.70 372.70 1.00 7154 4.23 5.692 4.2 6771 TRACE 113 1 1981 372.70 373.70 1.00 1215 1.36 1.288 2.4 2098 TRACE 90 1 1982 373.70 374.30 0.60 3953 3.85 3.902 9.4 3411 TRACE 86 1 1983 374.30 375.80 1.50 1052 0.40 0.726 0.4 368 TRACE 73 1 1984 375.80 376.80 1.00 1069 1.47 1.270 1.0 1305 TRACE 63 2

No: CDR9937

Cameco Gold Inc.



stringers is very variable and they are usually spaced every 30 to 70 cm of core length. There are also another 5% very similar quartz-carbonate stringers <1 cm thick, which are oriented in all directions. They are not associated with pillow selvages, but also contain up to 5% chalcopyrite and pyrite. All stringers are crosscut and displaced by minor chloritic/calcitic fractures oriented at about 20 deg. TCA. Varioles are faint and weakly epidotized. They are usually <1 cm in diameter, but in places they reach 1 cm in diameter.

374.5-374.6: Moderately brecciated section showing buff colored fracture network. The fractures are probably filled with sericite, carbonate and silica? The zone is oriented at 20 to 25 deg. TCA.

378.2 390.4 (MINERALIZED, CARBONATIZED, VARIOLITIC PILLOWED MAFIC FLOW)

Very dark grey, carbonatized unit, very similar to the interval from 327.1 to 365.6 m, but it appears pillowed and it is weakly to moderately magnetic throughout. The spaces between the chloritic selvages (<3 cm thick) are filled with quartz-carbonate and up to 80% fine grained pyrite and up to 20% chalcopyrite. Overall there is about 2 to 3% pyrite and may be 1% chalcopyrite. Visible gold was seen in one stringer as described below (386.2 m). The matrix of the rock is strongly biotitic and chloritic, and it is moderately to strongly altered to subhedral specks of carbonate (calcite+ankerite). The rock is cut by about 10% white carbonate-quartz stringers, <1 cm wide, oriented in all directions. These stringers are not mineralized as in the mafic flow above. Contact with the upper flow is not well defined. Rare carbonatized

1985 376.80 377.30 0.50 1040 N.A. 1.040 1.4 837 TRACE 69 TRACE

1986 377.30 378.20 0.90 4190 7.96 6.075 1.3 470 TRACE 52 1

1987 378.20 379.30 1.10 2270 3.26 2.765 2.8 2287 TRACE 82 TRACE 1988 379.30 380.30 1.00 2834 3.26 3.047 0.9 571 TRACE 69 1 1989 380.30 381.30 1.00 1070 0.88 0.975 0.8 249 TRACE 65 TRACE 1990 381.30 382.30 1.00 484 0.11 0.297 0.6 306 TRACE 58 TRACE 1991 382.30 383.00 0.70 92 0.08 0.086 0.9 720 TRACE 82 TRACE 1992 383.00 383.30 0.30 2411 0.74 1.576 3.5 2889 TRACE 95 1 1993 383.30 384.30 1.00 62 0.16 0.111 0.7 163 TRACE 83 TRACE 1994 384.30 385.30 1.00 319 0.26 0.290 0.5 99 TRACE 76 1 1995 385.30 386.00 0.70 270 0.24 0.255 0.7 542 TRACE 87 TRACE 1996 386.00 386.30 0.30 39004 12.75* 13.900 2.5 3164 TRACE 82 TRACE 1997 386.30 387.60 1.30 436 0.74 0.588 0.4 772 TRACE 79 1 1998 387.60 388.30 0.70 123 0.24 0.182 0.3 380 TRACE 30 1 1999 388.30 389.30 1.00 144 0.31 0.227 0.7 284 TRACE 64 1 2000 389.30 390.40 1.10 3243 2.68 2.962 1.4 1856 TRACE 93 TRACE

* Assay of the entire sample (after metallic sieving) except the 30g sample taken for the initial assay.

No: CDR9937

Cameco Gold Inc.



varioles, up to 1 cm in diameter are seen in places (specially from 383.6 to 383.9 m).

378.2-379.3: Section containing 3 sulphide-rich stringers, 1 to 5 cm wide, clearly located between pillow selvages (triple

junction). The stingers are composed of about 80% fine grained pyrite, <5% chalcopyrite and <20% carbonate and chlorite. Quartz is rare or absent.

379.3-383.0: Section with only traces to 0.5% pyrite and chalcopyrite.

383.15: Very irregular series of small stringers, <5 mm wide, between chloritic pillow selvages and composed mainly of fine

grained carbonate, 20 to 25% chalcopyrite, minor dark grey quartz and minor pyrite. The stringers have very diffuse edges.

383.2-386.2: Section with only traces of chalcopyrite and pyrite.

386.2: Very irregular mineralized quartz-carbonate patch, from 1

to 9 cm wide, probably located between pillow selvages (triple

junction). The stringer/patch is composed of 80% dark grey quartz, 5% white carbonate and 10 to 15% splashes of chalcopyrite with very minor pyrite. Two specks of visible gold, 1.5 mm and <0.1 mm in diameter, are seen floating in the dark quartz by themselves. There is not a lot of chloiitic alteration near the edges of the stringer/patch.

387.2-387.6: Fractured section with no carbonate specks and cut by

10% carbonate stingers oriented in several directions. Some

No: CDR9937

Cameco Gold Inc.



crosscut and displace others. Edges of a brittle sandstone fault.

387.6 388.3 (Sandstone-filled fault) Dark reddish brown, non foliated, hematitic and polymictic grit (pebbly sandstone) probably filling a fault zone (very similar to holes CDR9701, 9702, 9706 and 9929). The sediment appears to be graded uphole (top indicator?). It contains a 10 ca wide clast of mafic to ultramafic rock oriented at 45 deg. TCA. The clast contains minor pyrite and chalcopyrite. Upper contact is very sharp and oriented at <10 deg. TCA, while lower contact is oriented at 40 deg. TCA.

388.3-390.4: Fractured interval very similar to 387.2 to 387.6 m. Very little specks of carbonate. 0.5% chalcopyrite and traces of pyrite in few carbonate+/-quartz stringers, <5 mm wide.

390.4 404.5 (TALCOSE AND CHLORITIC ULTRANAFIC ROCK) 2001 390.40 391.40 1.00 86 N.A. 0.086 0.3 52 TRACE 68 TRACE 2002 391.40 392.40 1.00 TRACE N.A. TRACE TRACE 8 TRACE 66 TRACE

Dark greenish grey, competent (RQD>95), weakly to moderately 2003 392.40 393.40 1.00 49 N.A. 0.049 0.9 1138 TRACE 67 TRACE foliated (30 to 35 deg. TCA), very soft, non magnetic, massive 2004 393.40 394.40 1.00 12 N.A. 0.012 0.3 582 TRACE 81 TRACE ultramafic rock. The upper contact with the pillowed flow is very 2005 394.40 395.50 1.10 101 N.A. 0.101 0.5 209 TRACE 70 TRACE sharp and oriented parallel to foliation. The rock is intruded by 2006 395.50 397.10 1.60 171 N.A. 0.171 0.2 167 TRACE 60 TRACE 5 to 10% irregular stringers, oriented generally at less than 40 2007 397.10 398.60 1.50 21 N.A. 0.021 0.4 187 TRACE 79 TRACE deg. TCA, but in several different directions. They are composed 2008 398.60 399.30 0.70 32 N.A. 0.032 0.5 271 TRACE 38 2

'carbonate mainly of talc, with minor and up to 40% sulphides 2009 399.30 400.30 1.00 19 N.A. 0.019 0.3 39 TRACE 56 TRACE (pyrite and chalcopyrite). From 390.4 to 393.7 m, the stringers 2010 400.30 401.50 1.20 183 N.A. 0.183 0.6 376 TRACE 59 TRACE contain up to 10 to 20% chalcopyrite, while below 393.7 m, 2011 401.50 403.00 1.50 24 N.A. 0.024 0.3 58 TRACE 59 TRACE chalcopyrite is absent. Overall, the unit contains 1 to 2% pyrite and traces to 0.5% chalcopyrite (only from 390.4 to 393.7). The

2012 403.00 404.50 1.50 33 N.A. 0.033 0.3 128 TRACE 61 TRACE

No: CDR9937

Cameco Gold Inc.



matrix of the rock is fine grained, strongly chloritic, strongly talcose and weakly to moderately altered to pervasive carbonate, seen as very tiny anhedral and diffuse specks.

395.5 399.3 (Sandstone-filled fault zone) The more blocky section (RQD <80)is composed of hematitic, polymictic pebbly sandstone intervals (as described above), 20 to 50 cm wide, alternating with ultramafic intervals, 80 and 1.5 cm wide, identical to the main description (also with 5% pyritic talc-rich stringers). The contacts between the intervals are very sharp and oriented at 10 to 40 deg. TCA. From 398.9 to 399.2 m, the foliated ultramafic rock is intruded by 90% milky white, dolomite?-quartz veinlets, up to 3 cm wide and oriented at 25 deg. TCA. Minor pyrite is seen near the margins of the veinlets.

404.5: EOH

Whole rock samples:

CDR9937-A: 304.5-307.5: Mineralized and chloritized mafic pillowed flow.

CDR9937-B: 328.0-331.0: Carbonatized and biotitic mafic to ultramafic rock.

CDR9937-C: 297.0-300.0: Siliceous and weakly sericitized tuff/mudstone.

CDR9937-D: 361.0-363.0: Mineralized carbonatized and biotitic mafic to ultramafic rock.

CDR9937-E: 370.0-373.0: Mineralized and weakly epidotized-

No: CDR9937

Cameco Gold Inc.



chloritized, pillowed mafic flow. CDR9937-F: 383.0-386.0: Mineralized, carbonatized and biotitic,

variolitic pillowed mafic to ultramafic rock.

CDR9937-G: 391.0-393.0: Talcose ultramafic rock.


302.4 m: Mineralized tuff/mudstone in contact with mafic flow. 311.5 m: Mineralized and chloritized mafic pillowed flow. 328.5 m: Carbonatized and biotitic mafic to ultramafic rock. 403.4 m: Talcose ultramafic rock with talc-carbonate-pyrite patch.

Thin section:

370.15 m: Dark grey quartz-carbonate-chalcopyrite-pyrite stringers in variolitic pillowed mafic flow.

388.30 m: Hematitic pebbly sandstone horizon filling a fault zone.



63.10 -50.00

154.60 -50.00

188.10 -50.00

No: CDR9937

Cameco Gold Inc.



DEPTH INCLINATION REARING

273.50 -52.00

322.30 -51.00

No: CDR9937

Cameco Gold Inc.

DIAMOND DRILL LOG PROPERTY: Cedar Rapids HOLE No.: CDR9938 Collar Eastings: 1418.00 Collar Northings: -2330.00 Collar Elevation: 290.00 Grid: N-S Claim #: 5126337

Collar Inclination: -50.00 Logged by: D. BABIN Grid Bearing: 230.00 Date: 04/10/99-05/10/99 Final Depth: 92.00 metres Down-hole Survey: ACID TEST Val d'Or drilling Core NQ Did not reach bedrock, was abandoned at 92.0 m

ASSAYS FROM TO LITHOLOGICAL DESCRIPTION SAMPLE No. FROM TO WIDTH

0.0 92.0 (OVERBURDEN) 94 0.00 0.00 0.00



HOLE No: CDR9938

APPENDIX 2

AU AND ICP ASSAY CERTIFICATES FOR DRILL CORE


mannimmonssamsamossimamanne

Intertek Testing Services Chimitec

CLIENT: CAMECO GOLD INC. PROJECT: CEDAR RAPIDS REPORT: C99-61052.0 ( COMPLETE

DATE RECEIVED: 20-MA7-99 DATE PRINTED: 27-MAY-99 PAGE 1 DE 1

SAMPLE

NUMBER

ELEMENT Au30

UNITS PPB

SAMPLE

NUMBER

ELEMENT Au30

UNITS PPB

CDR9906-1184 <5 CDR9906-1224 18 CDR9906-1185 8 CDR9906-1225 193 CD89906-1186 14 CDR9906-1226 189 CDR9906-1187 <5 CDR9906-1227 133 0DR9906-1188 <5 CDR9906-1228 <5

CDR9906-1189 <5 CDR9906-1229 50 CDR9906-1190 <5 CDR9906-1230 394 CDR9906-1191 <5 CDR9906-1231 581 CDR9906-1192 <5 CDR9906-1232 80 CDR9906-1193 9 CDR9906-1233 533

CDR9906-1194 <5 CDR9906-1234 202 CDR9906-1195 <5 CDR9906-1235 959 CD89906-1196 <5 CDR9906-1236 163 CDR9906-1197 9 CDR9906-1237 <5 CDR9906-1198 8 CDR9906-1238 72

^.DR9906-1199 18 CDR9906-1239 32 DR9906-1200 <5 CD89906-1240 12

CDR9906-1201 6 cDR9906-1241 <5 CDR9906-1202 <5 CDR9906-1242 <5 CDR9906-1203 <5 CDR9906-1243 <5

CDR9906-1204 5 CDR9906-1205 33

CD19906-1205 <5 CD29906-1207 5 cDR9906-12(18 <5

CDR9906-1209 76 CDR9906-1210 52 CDR9906-12I1 167 cDR9906-1212 18

CDR9906-1213 8

CDR9906-1214 19 CDR9906-1215 18 CDR9906-1216 20 CDR9906-1217 5 CD10906-1218 436

CD89906-1219 6 CDR9906-1220 6 CDR9906-1221 <5 -089906-1222 49 )R9906-1223 15

Rapport Lab Geochimie Geochemical Lab Report

Intertek Testing Services Chimitec Bondar Clegg

REFERENCE: 170408 REPORT: C99-62643.0 ( COMPLETE )

SUBMITTED BY: D. BABIN

DATE RECEIVED: 16-SEP-99 DATE PRINTED: 23-SEP-99

CLIENT: CAhECO GOLD INC.

PROJECT: CEDAR RAPIDS

SAMPLE TYPES NUMBER SIZE FRACTIONS NUMBER SAMPLE PREPARATIONS NUMBER

50 -150 50 CRUSH/SPLIT 8 PULV. 50 TRANS FROM POLY BAG 31

DRILL CORE

DATE APPROVED ELEMENT

NUMBER OF ANALYSES

LOWER DETECTION EXTRACTION METHOD

990921 1 Au30 Gold 50 5 PPB Fire Assay of 30g 30g Fire Assay - AA 990921 2 Ag Silver 50 0.2 PPM HCL:HNO3 (3:1) IMDUC. COUP. PLASMA 990921 3 Cu Copper 50 1 PPM HCL:HNO3 (3:1) IMDUC. COUP. PLASMA 990921 4 Pb Lead 50 2 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 5 Zn Zinc 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 6 Mo Molybdenum 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990921 7 Ni Nickel 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 8 Co Cobalt 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 9 Cd Cadmium 50 0.2 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 10 Bi Bismuth 50 5 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 11 As Arsenic 50 5 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 12 Sb Antimony 50 5 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990921 13 Fe Iron 50 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 14 Mn Manganese 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 15 Te Tel 50 10 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 16 Ba Barium 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 17 Cr Chromium 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 18 V Vanadium 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990921 19 Sn Tin 50 20 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 20 W Tungsten 50 20 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 21 La Lanthanum 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 22 Al Aluminum 50 0.01 PCT HCL:HNO3 (3:1) IMDUC. COUP. PLASMA 990921 23 Mg Magnesium 50 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 24 Ca Calcium 50• 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990921 25 Na Sodium 50 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 26 K Potassium 50 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 27 Sr Strontium 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 28 Y Yttrium 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 29 Ga Gallium 50 2 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 30 Li Lithium 50 1 PPM HCL:HNO3 (3:1) IMDUC. COUP. PLASMA

990921 31 Nb Niobium 50 1 PPM HCL:HNO3 (3:1) IMDUC. COUP. PLASMA 990921 32 Sc Scandium 50 5 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 33 Ta Tantalum 50 10 PPM HCL:HNO3 (3:1) IMDUC. COUP. PLASMA 990921 34 Ti Titanium 50 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 35 Zr Zirconium 50 1 PPM HCL:HNO3 (3:1) IMDUC. COUP. PLASMA

REPORT COPIES TO: MR PAUL CORD INVOICE TO: MR PAUL CORD

This report oust not be reproduced except in full. The data presented in this report is specific to those samples identified under "Sample Number" and is applicable only to the samples as received expressed on a dry basis unless otherwise indicated

ITS - Chimitec - Bondar Clegg, 1322-B Harricana, Val-d'Or, P.Quebec, J9P 3X6, (819) 825-0178

Rapport Lab Geochimie Geochemical Lab Report MUMI


CLIENT: CAMECO GOLD INC. REPORT: C99-62643.0 ( COMPLETE )

PROJECT: CEDAR RAPIDS DATE PRINTED: 23-SEP-99 PAGE 1 OF 5 DATE RECEIVED: 16-SEP-99

G8! Na

PCT PCT.

K` Sr yy. PCTPPM PPM

Ga Li;:: Nb Sc::: Ta .. T'i : Zr

PPM PPNEs:PPM PPM:PPM PCT;PPM

4 4 4

8: 8 6

23.

27 25 15 17

8 20:;i<10 0:1i1:: <1 9 . 25;I:<10 0.21:: <1 11 27'<10 0.21< <1 9 18:::<10 0.21`' <1 10 14<10 0.21;:i <1

2.16 ::0.04 0,28 40 5; <2 5:;: <1 <5;<10 043 24 3.66 <:0.02 0.03 : 60 5>; 4 .12 6 7:;:<10 0.29 <1 :1 62 0.02 0.05 50 5;:: 4 12:i 5 5;<:<10 0.41:; <1 2.66 <.01 < 01; 74 4;: <2 6:: 3<5<:<10 0.38 <1 3.76 0.02 Q 04< 50 5:: 5 13;;: 7 5::<10 0.27 <1

1.421 0.62 2.75 2.65 4,07

3 1(1:: <1 <10 0.11G; 6 <5:;<10 0.01'1 22

5 20':' 1 <5;<10 < 01;'.; 13 4 18:: <1 <5;:<10 <.01: 15

~ 10< <1 <5: ><10 <..01:i. 23

0.07 0.14';: 49 0.03 0.20: 18 0.07 Q.11 70 0.07 0.15: 75 0.03 0.22:;119

SAMPLE NUMBER

ELEMENT Au30 Ag UNITS PPB PPM

Cu Pb! Zn Mo. Ni Co Cd Bi As Sb Fe

PPM PPM PPM PPM PPM PPM:: PPM PPM:: PPM PPM PCT Mn Te

PPM PPM

CDR9906-1244 5 <.2>> 50 <2 ' 53 <1232 47: <.2 <5 <5. 6.71 954:<10 CDR9906-1245 <5 <.2 88 <2 57 <098 45. <.2 <5 <5 6.99 980 <10 ŒR9906-1246 6 0.3 74 <2 : 58 <1 165 44 <.2 <5 7.26 959. <10 ŒR9906-1247 <5 0.31 71 <2 44 <1 134 37;<.2 <5 <5',6.41 810<10 ŒR9906-1248 21 0.3 47 <2;i 47 <1':130 34<.2 <5 <516.27 748:<10

ŒR9906-1249 10 0.3> 87 <2>;: 48 <1 126 37 <.2 <5 <5 6.59 723 <10 ŒR9906-1250 <5 <.21 8 <2( 37 <1. 102 26:!<.2 <5 <5 <5;4.65 540 <10 ŒR9906-1251 19 0.3: 155 <2 37 <1 155 35::<.2 <5 <5 <5 4.32 458 <10 ŒR9906-1252 8 <.2> 69 <2 33 <1 121 27>:<.2 <5 <5 <5 3.84 422 <10 ŒR9906-1253 51 0.4 341 <2'' 39 <1 150 40.2 <5;:; <5 <5:!4.41 436 <10

ŒR9906-1254 31 <.2 332 <2 39 <1':129 45 <.2 <5;;I <5 <5. 4.23 457<10 ŒR9906-1255 6 <.2'i 69 <2. 36 <1 137 31:<.2 <5:::

<5 4.29 443:<10

ŒR9906-1256 9 <.2: 89 <2 38 <1;' 145 31 i!<.2 <5:: <5 <5; 4.16 445: <10 ŒR9906-1268 5 <.2; 80 <2: 31 . <1274 37'<.2 <5' <5 <5i 3.20 406` <10 ŒR9906-1269 <5 <.2. 77 51 . <1:355 45 <.2 <5» <5 <5: 5.78 751,<10

ŒR9906-1270 <5 <.2< 41 c2>: 37 <1:296 <.2 <5 <5 3.75 543 <10 ŒR9906-1271 <5 <:2< 64 <2 : 44 1:364 .59! <.2 <5: <5 <5 4.28 585 <10 ŒR9906-1272 17 0 2; 200 <2;; 64 <.2 <5 <5 6.48 907 <10 03R9906-1273 55 608 2 !' 40 % 2:::106 199i <.2 22 <5 9.05 232 <10 ŒR9906-1274 10 4.Z. 41 <2;1 19 1 : 27 16.: <.2 <5 <5 <5 s 1.92 132 <10

ŒR9906-1275 17 0., 2:'. 154 25 42 17:i:<.2 <5<;: <5 <5:2.73 109:;<10 ŒR9906-1276 5 0,3:' 234 962 2 49 30:::2.2 <5:> <5 <5 ;:5.40 56;:<10 CDR9906-1277 <5 < 2. 51 38 <1.: 20 12:;<.2 <5:; <5 <5 3.08 290:<10 ŒR9906-1278 <5 <, 2': 61 50 26 16<.2 +5:: <5 <5:3.58 264?i<10 ŒR9906-1279 1502 131 525 33 26 0.9 .45!: 10 <53.36 96::<10

0)R9906-1280 5 <.21; 135 642;; 32 23<.2 <5. <5 ÇS: 3.49 93<10 ŒR9906-1281 10

<,2 42 <2' 81 <1;:94 34><.2 <5 <5 <5 7.31 942<<10

ŒR9906-1282 13 <:2 130 <2 94 <1: 84 42::<.2 <5:: <5 <5 7.67 871`<10 ŒR9906-1283 48 0,3: 111 <2. 58 <1::i 48 26::<.2 <5 <5 3.75 584 <10 ŒR9906-1284 12 <:2:! 92 92 Al': 67 35:0.4 <5: <5 <5 7.36 1010 <10

Ba Cr

PPM PPM 'V Sn :>N La Al< Mg

PPM PPM PPM PPM PCT :> PCT

::62 966 13.7. <20 <20 <1 4;53:5.89 .100.642 147 <20 <20 <1 4:916.04

94 552 161 <20 <20 1 4.73 5.40 32 471 152 <20 <20. 1 4.10 4.65 8 472 146 <20 20 1 3.774.10

5 474 143 <20 <20 1 3:773.76 2 449 112 <20 <20 <1 .2.:85;;2.77 8 511 77 <20 <20 <1 2:.60>2.48 8 495 78 <20 <20 <1 2.47 2.40

. 17 556 71 <20 <20 <1 2';62;2.54

12 519 74 <20 <20 <1 2.58;2.58 5 549 74 <20 <20. <1 2.77>2.80 6 538 74 <20 s20 <1 2:742.85 2771

• Z988 63:,<20 107 <20

40. 40

1 1.90 1.49

1 304;2.54

1:783 84:<20 <20 <1 2:21::i:1.90 2 840 72<20 <20 <1 2:22:1.89 7988 1.Ox <20 Q0 1 3:192.63

:10.234 45.<20 <20. 9 1:350.87 2:1 68 .113.<20 <2#t 12 1.34..0.84

36 88 1:9'<20 <20 12 1.41:0.78 a3.. 94 9 <20. <20 . 16 1.02 : 0.51

88 26 <20 <20 26 2.00 1.43 32. 81 24 <20 <20 23 1;86<1.29 44 105 8 <20 <20 12 1.25 <0 .81

i.~ 84 :10 <20 40 14 1.04 0.53 8 236 116.<20 <20. 2 3:80 3.21 7. 217 103 <20 40 <1 $94 3.15 ;1,.174 .61.<20 <20 <1 Z35 1.54: 4 193 122.<20 <20 <1 373 3.04

ITS - Chimitec - Bondar Clegg, 1322-B Harricana, Val-d'Or, P.Quebec, J9P 3X6, (819) 825-0178 ~

3.99 <.01 1.19: 61 4.48 <.01 1 76i: 65 4.79;!0.01 1..64: 61 5.080.02 0.56 53 5.10 0.02 0,13 43

4.60.;;0.04 OAT 36 2.80 ';:0.05 0:02s' 22 1,47;0.04 0.11! 19 1.38 0.05 0.13 18 0.86.;:0.04 0,26: 15

9 12!:<10 0.21: <1 7 61: <10 0 24;' <1

13 4 <5 <10 0.19 <1 13 ! 5 <5<i<10 0:22 ` <1 14: 4 <5;!:<10 064: <1

8:;i 6 4

4! 3 1% 2 3: <2

17 14

1.48:''0.04 0 16; 18 3' 2 14 4 0.99.:'0.03 16 3' 2 15' 4 1.00.:0.04 006 12 .4 3 15 4 1.56 0.06 0.01;< 27 4:: <2 5 4 362:0.03 0.01,!; 40 4 3 91 7

<5<100.181ü<1 <1

<5<10 0.21: <1

0.22:: <1 6<10 0,18 <1

2.55s:0.06 <.01• 27 1:88 0.07 0 01;' 23 3.90 ',:0.03 0.04: 44 1 94;0.08 0.04. 23 2 13;0.07 0,16 40

d!> 5 7><10 0.21::: <1

4 5;:<10 0.21: <1

6 7:<10 0:17: <1 2 <5<10 p:44:: 9

8:! <1 .<5..<10 0.12' 9

5<' 3 5 ;! <2 4; 3

<2 3




PROJECT: CEDAR RAPIDS DATE RECEIVED: 16-SEP-99 DATE PRINTED: 23-SEP-99 PAGE 2 OF 5

SAMPLE NUMBER

ELEMENT Au30 Ag; Cu .Pb: Zn Mo: Ni Co...i Cd Ai As Sb. Fe UNITS PPB PPM PPM PPM PPM PPM :PPM PPM PPM PPM PPM PPM:: PCT

t Te PPM' PPM

B8 Cr

PPM PPM V: Sn .'U La

PPM PPM PPM PPM PCT Mg

PCT

Ca Na

PCT PCT (C:: Sr

PCT,;PPM

Y;: Ga Li:: Nb Sci! Ta

PPM PPM PPM: PPM T'I; Zr

PCT PPM

(DR9906-1285 6 <,2 91 <2. 71 54 29<.2 <5 <5 <5'i5.31 630 <10 12 160 93 <20 <20 4 2.72 2.26 2.09. 0.06 045'; 38 5 5 10. 6 5;I:<10 0:4i <1 CDR9906-1286 7 0.3' 163 41 50 .2! 57 44<.2 8 <5 5.32 590'. <10 24 184 76 <20 <20 3 2.34 1.95 2.82! 0.03 0.111: 36 5' 3 1.0 5 6i:<10 0,18, 4 CDR9906-1287 7 0.3. 88 2:1 77 <1' 72 <5 ' <5 <5 6.41 913 <10 2 206 119 <20 <20 <1 3.61 3.02 3.60 0.02 0.03; 81 E.02 4 7 13. <10 0.34: <1 CDR9906-1288 9 0.2% 85 <2 72 <1 63 32 <.2 <5:!: <5 <5 5.59 827 <10 4 205 82 <20 <20 <1 2.94 2.25 3.18 0.03 0.0 ( 81 4' 2 4 . 4-<10 0.34" <1 CDR9906-1289 44 0.2: 125 <2 51 82 27::<.2 <5 <5 <5 6.04 728 <10 5 214 109 <20 <20 1 3:31:2.81 3.04 0.03007' 65 61 7 15 7 7''<10 0.35- <1

CDR9906-1290 255 0.4 346 2 43 1:;; 66 25. <.2 <5. <5 <5 4.99 539 <10 1.172 107 <20 <20 8 2:57 2.45 3.80 0.06 < 01;; 59 5 10>: 7 13::<10 0.23>; 4 CDR9906-1291 74 <.2:: 121 3 ' 33 2'r: 44 38 <.2 <5 10 <5 3.33 316 <10 20 103 60 <20 <20 13 2.00 1.85 2.60 0.08 0 09!: 40 6 9.; 3 7:<10 CDR9906-1292 <5 <.2 105 9 ; 29 1 ': 41 35 <.2 <5. 6 <5 2.97 236 <10 30 77 25 <20 <20 11 1.89 1.66 2.06 0.07 0,16:: 34 4!: 5 10: <1 <5;::<10 0.08;; 11 CDR9906-1293 11 0.3 221 <2 : 38 <1 > 48 20. <.2 <5 <5 <5 3.87 397 <10 13 98 52 <20 Q0 4 2.29.;2.15 2.96 0.06 0.08 62 4:: 4 11: 3<s:<10 0.15>'. 3 CDR9906-1294 <5 <.2>' 52 2!:39.<1i'.50 12: <.2 <.5: <5 <5 3.43 . 466 <10 6 117 65 <20 <20 4 2.52 ',I2.38 2.64 0.07 0.05 66 3`! 4 10» 4 <5;<10 0.18;: 2

CDR9906-1295 <5 <.2" 97 <2 32 <1:; 40 21;;<.2 <5::: <5 <5;2.86 347?<10 27 105 35 <20 <20 6 2:08;;1.81 2.61 0.07 0,13 66 31<: 3 9;: 1 s5;::<10 0.14:! 2 CDR9906-1296 25 < 2;' 13 <2 30 1:; 69 Z0: <.2 <5:1i <5 <53.15 ..432<:<10 2 .137 49 <20 <20 3 2.39 2.27 3.20 0.07 < 01 81 3;; 4 11: 3 :.<5:<10 0 15.,;: 2 CDR9906-1297 10 <.2': 1 28 1 52 13 <.2 <5 <5 <5:2.46 384.:<10 19 107 37 20 <20: 2 2.09 1.95 3.38 0.06 0.08 69 3 < 4 10>; 2 <5:<10 (65;;: 2 CDR9906-1298 5 0.3 50 2 35 <1!: 58 25<.2 <5; <5 <5:3.48 458 <10 . 18137 57 <20 <20 4 2.54 2.33 2.95 0.07 0.15:` 59 3i; 3 3 <5<10 0.20 <1 CDR9906-1299 5 0;3.. <2 37 7: 62 107;<.2 <5:; <5 . <5:4.95 400':<10 :10 133 60.20 <20 4 2.19 2.00 3.09 0.07 0.06 44 4;: 3 9 3 <5<10 0.15> <1

CDR9906-1300 10 0.3:' 132 2: 24 19 76 <.2 <5 <5: 2.23 309<10 3 167 32 <20 <20 2 0.95 0.88 4.11 0.03 0.02 51 3: 2 2 0.05;: <1 CDR9906-1301 9 0.4: 166 2 46 2 i 63 77:':<.2 <5 <5. !4.36 423<10 4:124 80 <20 <20 5 2.46 2.27 4.16 0.07 0.04 45 10::<10g14'; 2 COR9906-1302 73 1 1)312 2!I 41 <1<:109 227:<.2 <5 <5,::5.40 404<10 t4 91 52 20 Q0 . 5 2.00 1.77 3.95 0.06 0.07 50 5::<10 2 CDR9906-1303 244 <.2:: 71 <2>i 42 ~1:: 66 35;<.2 <5 <54.04 4$9:::<10 23 145 67 20 <20 3 2.53 2.17 1.52 0.06 0 21';: 55 4<5 ;<10 0 27;: <1 CDR9906-1304 <5 <.2'; 22 <2 :: .... 37 <1?: 59 :19<.2 <5 <53.36 528:<10 6 142 53 <20 <20 4 2.35. 2.05 2.71 0.07 0.04 55 3 <5<10 <1

ITS - Chimitec - Bonder Clegg, 1322-B Harricana, Val-d'Or, P.Quebec, J9P 3X6, (819) 825-0178

CLIENT: CAMECO GOLD INC.

REPORT: C99-62643.0 ( OOMPLETE ) PROJECT: CEDAR RAPIDS

DATE RECEIVED: 16-SEP-99 DATE PRINTED: 23-SEP-99 PAGE 3 OF 5

ELEMENT Au30 Ag, Cu Pb<:: Zn Mo Ni CoG Cd Bï; As Sb Fe

UNITS PPB PPM. i: PPM PPM PPM PPM PPM PPM PPM PPM i;PPM PPM PCT Sr Y Ga Li': <' Nb Sc::

PCT ;;PPM Fr* PPM PPK:;PPM

Ta T Zr

PPM :PCTsPPM

STANDARD

NAME

ANALYTICAL BLANK <5 <.2': <1

ANALYTICAL BLANK <5 <.2'r: <1

ANALYTICAL BLANK <5 - -

Nurber of Analyses 3 2 2

Mean Value 3 0.1 <1

Standard Deviation - -

Accepted Value 5 OZ.

<.01 < 41'; <1

<.01 <.01I: <1

2 ....2!: 2

<.01 <,01: <1

<2 <1;:) <1 a5><10 <.01f <1

<1 <2 <1 '' <1 <5:1<10 <.01 <1

2.2:> 2 2`: 2 2' 2

3 ' 5 01:! <1

Oxide (Feldspar & 3053

Number of Analyses 1

Mean Value 3053

Standard Deviation -

Accepted Value 2940

STD GEOCHEM STD 6

Nutter of Analyses

Mean Value

Standard Deviation

Accepted Value


Nuttier of Analyses 1

Mean Value 184


Accepted Value 186

2 126 30 0.3

I' 1 1<! 1

126 30 0.3

135 35:0.2

7.13 1351 7 206

1 1< 1 1 1

7.13 1351 5 7>206

7.20 1450: <1 6'251 _

49 <20 <20 2 1.95 2.61 3.68;:!0.02 0.05 79

11 >1 1 1< 1. 1:;: 1 ..... 10 ;10 2 1.95 2.61 3.68 0.02 0 05!;; 79

:80:2.70 4.00 t).01 Q 04:: 70

<2 20;_ 2 $;:!<10 <,01>:' 5

1 1: 1 ..T 1 ...>1:> 1 5 <,01

1 <.:0:1::: 24



Mean Value 465


Accepted Value 465

<1

<1

2




- <.2 70 14 89 1 26 11 0.3 ' <5 11

- 1 1 1 1 :.1 . 1

- 0.1 70 '14 89 ;:l 26 '110.3 :3: 11

- - - - - - -

- 0.3 66 :15.: 82 2 23 11.0.6 11

31 56<20<20' 15 1:38 0.81 1.35:0.05 0.12' 73 -12. <2 AO: 5 <5'<10 0;09: <1

Yli • 1 ::11! 1 1 1 1:: 1 1 -

31 : 56 10 10 151.380.81 1.35..0.05 0,12. 73 12 1 10 5 3 5 0.09 <1

<5.2.94 1313' <10 1125

1 1: 32.941313.. 51125

_ - - -

'.4..12.60 1200 -

II Intertek Testing Services Chimitec Bondar Clegg


CLIENT: CAMEO° GOLD INC. PROJECT: CEDAR RAPIDS

REPORT: C99-62643.0 ( COMPLETE ) DATE RECEIVED: 16-SEP-99 DATE PRINTED: 23-SEP-99 PAGE 4 OF 5

STANDARD ELEMENT Au30 Ag. Cu Pb: Zn Mo Ni Co" Cd . Bi- : As .Sbc. Fe Mn Te ...la: Cr V Sn .:- It La .* Al Mg Ca Na K Sr Y Ga Li Nb Sc Ta Ti Zr

NAME UNITS PPB PPM PPM PPM PPM PPM PPM PPM PPM PPM PPM PPM PCT PPM PPM PPM PPM PPM PPM PPM PPM PCT. PCT .PCT. PCT PPM PPM PPM PPM PPM PPM PPM :PCT PPM

GANNET STREAM -SED 4

Number of Analyses

Mean Value

Standard Deviation

_

Accepted Value ..•.•••...•..•..•••••;.....

• • - ••••••• •••••••• ........„.

.,.....,................ .............,...„.... ..... :•••••••••••••••••••-.-.• •••••••.• ..,...... ....... ........ •••••••••.••••••

........... ...,................ ................ .................

.......... .......... .......

.......... ........ .••••-•••••••••••••• ........... .....••••• ........ •-•••••••••••• .......... •••••• ••• .......... ........ ......... ..........

••"•••••• ........... ... ...

•••••••••••.,.•••••• .••••••••••••• .................... ......... ........ ••••• ••••• "'"""' '•••"•• .......... ..........

........

.......... ........ '''''••••••••••••••• •-...:-:::.•-•....:"...•,...".:.-.....•.::•...:.

.........

......••••• ..........

.......,.. ,.......

„........ ........

... •...'...

.......... ............,....

.......... ......

.......... ........ .......... •••••••••• ........... . .....

..•....... .. .. ••••••.•••.••••••••••••••.:':.••••••••••

........

........ .......... ........

••••••.... . • ...

• ""•••• ""' "

.......... ......

.......... ........ "'••••••• .........

.....,............

.........

........ ........... .......... ........

.......... ...... .-...1.-."..."•.'..•..-..•••"•••••••• ......... ..........

....... .......... ........ ..........

.......... ..... .......... ......... .. .....

.......

. .. ..

........ ..........

.......... .. .

.......... ........

•••.•••••.,...•••••• ...-....•.••

.......... ........

•••••••"' •• ••••-

.......... ........ .---,••••••,...".•••••:,....•:.••:"••••••••••••:::............1.."..,'

•••....... ...... •••••••••• ........... ....... • ...... .......... ........

........

........ ........... ..........

.......... ........

......... ...„...

1.-.::.: .•:".::.: .•:...:::..i.,:;: "..... .....E.,::. •...... .•::',.::: .".. •••::: ••••:. •::•: •:'. ••1

.......... ....... .......... ...... .

........ .......... ........

.••••••••. ....... ..........

.....,... ........

........ .......... ........ ..........

•••••••••• .. • .. •••••••••• .•..• . .. ..... ........... .......... ........

........ .......... •••••••••• ••••••••

........

........ ........... ..........

:....,....••.....•......••••,,..... .•••••••.•....••••••••••••

......... .......

......... ........ .-':.....'..-•:'.....'....".-.'....."....•••••••••••

........ ........... .... ... ........... ..........

:••••:',.:•.•".....:........••••••••••••••••••••:: •••,' •• •••-.•E•••,- ..'•....• .-.•..-'

..','...'........... .'...-.'..-.-.- ••-•••];:-..1•:. •,.. •::::-..•'..•:."':-.::'•:. ."'•:::.•:

........

........ .......•.... . ...... ..........

••• ••• ••• ••••''.1"..''.•'....•.'".•.1.... :•11• .•• •11..".•- •.........:."...."....--•.." .:

::••• ••••::"•....'"'"...:• ••--...:".1....1.

.......... ........,. .,......

.•••:."...."•-•••••:.•'•,•'.".-...-."..-••••• .........,.. .........''......."..•••.... ..........••••-•••••••..

1,.............''..,.....•• •••.- •• ........

........... ..........

••:''.••••••••••••.•••'..•::'.. ••••••••••••••••,.....•••••:.•

......... ......,.

........ ........

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........„ •••••••...........•'.••••••-.. .-....-'•••••••••.•••'- :::,.."::.........::••••,:"....::: ".-:.-,-....':'::'' ':...'":!- •••-••••1:-.

.......... ::":"....":: :•.."..•.".• ........

........ ........... ••••••..,•..'....."..•-••••• •••••••••••••••"..".••

........... ........ .......... ........ ........... ........ .......... ......... ........

........

........

........

....... ........... ..........

..........

.•••••••,"!...... :".".":::

-,•.•-:•.•."..•-•.•:-•-: .••::-.••.•-••-••-.••

......... ........

.......... ........ ••••••••'••:••••••,-,i'.."-......•...,:......-'.•:::::,,:•.",..."....: .••.-.••••••••••••••••••••.•

........

......,. ........... ........ .......... i.....' ........•...•...........;...... :•........... ,...i..... -- .1

.......... ........

...._...,....... .............,.. •,•.......„....,.........„•....:

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........

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........ ........... ........... .......... ......... •

.......... .......

..........

•...'..............'•••••:•: ••:•••'.....,•..•..

••••••:••••••."... .•;.....•••••••

.......... .......

.......... ........ •••••••••.........",..••••••••,.....::•...........',„ ••••••••:::::.

....... ........... .......... ••••••••••••••••••.',.•........•••••••••••:•.••• ........... ••.•:•••••••:•••:••••••••• :•••••••:••••••:•:•

,.......,. ...,.... •••••••••:•:•,••:•:•.••:-

........

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........ ........... ........... -......... .......... .......... ........

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•••••••••• ••••••••

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•••••••••••••.•..............•

•••••••••• "••"••••

........... ••••••••....................• .•.......•••••••••••

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........ .•••:.",,..•••,......•'•:•.",•-•••.•-..•..:-.",•••.,':.

.......... ........ "••.••••• .......... ........ ...... ........

::,:•••:::::.::::.,:•..:::,'.:....'•••'::••••••••••:.!..!

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....... ........... •••••••..•••.••••••• ••••••••••••.•,•

.......•••• .•.....•••••••••'.•,..........•••'..••-•••••'..•:..,•'. ...••••••••••••••••••••••••'....•.....••...•,' .......... ,, .,............. ........... ........... ••••••••.• ••••"••

........ ...,,..... ........

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........... .......... ........... ......... .......... .......... .......... ••••••••,.. '''.'... :-. •••••••'. ..-...:' •••••••••:.•••:::.••••••••••••••••,.'.........:,::•••-•••''.•.',••••-••:,•:'••:,-'....": ..........

.....„. .........

........ ........... .......... .......... ........

..... ........... .......... :.....,..,..::..,,,....,.::

........ .......... .......... ........... ..........

........ ...........

....... ...........

........ ...•.•.•.•••••••••..

........ .......... ••:,........1....,.:•••••]•.:::::.',E..•.:•,....'•••••:..:...::'::' ,..::.: '.........:......•:,...,:..1.1•:::..::::........:•-.!,•....::

..,...::::,..:::::•.......,.............,::.;::,,,,.., ........ ........

....... ........... ........... ...........

.......... ......... .......... .......... ..... .... .......... ........

.......... ........

.......... ........ .......... ........... ........... ••••••••,•••••.••••• ..,.......

........ :.'..• •:.. ••• ••• •.:,•• • -... ..- ,'-::" •:- .. •-••••••

........ .:',.......,.'.....'..'..: ..-,,,•,-...:•:•:•

........ ...,,:',....:::::::::::,....

....:.'.:.'..,....•••••.... -..•..•........,,,..,,

........ .................. ....... ........ ...... ... ... ... .. .......

........

........ ........... .....•-.:,:•:::...".•..:....-.:::.:::.:.?...... .•'...-.....:.;.:.......:..:.:.:.,:.: ..........

... .. ......... .......... .......... .. . •::::.•:-.• .....•::::: . ..... . .......

.......... ..... ,--.,.:.:,.•.....'..:,'..•.,:•...:::. ........ .......... ........ „.:...,,...........:. ........ ...... ........ ........... .......... .......... .....

..... .. .

.....•...•.::-.• .:::::::

......... ........ • • •-• • ----

.......... ......

.......... ........

...... ........ ... .. ........ :::••:_•,:•.:...:•••••.:.•,:.:

.......... " "--- ................ ..............

....;.<................::: :',:...,-,-.'•,',

.........:....:„ :: : ::

.......... ........ i......1.::::::•,....:: ,:.:••••••,...........,"..:.•

......_ ...:. ..........


.......... ........... ••••• •

.......

.......

........ ...........

....... ........... .........

.......... ........... .......

........ ........

Fe Mrj;: Te

PCT PPM PPM

6.41 810'' <10 6.80 832 <10

4.16

<10

3.90

<10

2.73 109:<10 36 88 '.:19 <20

2.80 112 : <10 : ;::35: :: 89 <20 i20 12 <20 12

3.49 <10 50. 84 <?10::<20 14 <20

3.43 466 <10

3.49 473 <10 117 65 <20 <20 4

120 65 <20 <20 4

<5.

<5'

Cu Pb Zn Mo Ni Co Cd 9i: As Sb

PPM PPS PPM PPM PPM PPM PPM PPM: PPM PPM

71 <2 44 <1<;134 37>`<.2 <5 <5 71 <2 :! 46 <1 ''139 38''<.2 <5 <5

89 101

38 <1 :145 31 !'<.2 55-: <5 37 <1 ;,144 33:<.2 <5. <5

CDR9906-1247 Duplicate

CDR9906-1256

Prep Duplicate

17 0.2'; 154

0.2 153


173<.2 25 42 <5

<5 25 42 17<.2

64 32 <.2 <5

CDR9906-1294

Duplicate

CDR9906-1301

Duplicate

<5 <.21 52

X.2

9 0.4'i' 166

9

39 50 <5

<5

<5 c5:

<5 <5: 53 40 50

46 63

<.2

<.2

<5

CDR9906-1280 5 <.2: 135 Duplicate 6

<5

SAMPLE ELEMENT Au30 Ag:

NUMBER UNITS PPB PPM

<5 <5:

EGO Intertek Testing Services Chimitec Bondar Clegg



REPORT: C99-62643.0 ( COMPLETE ) PROJECT: CEDAR RAPIDS


Ba Cr .1'V Sn <iU La PPM PPM. PPM PPM PPM

At

PCT

Mg

PCT PCT';

Na

PCT ~

PCT

Sr Ga Li' Nb Scj; Ta PPM PPM :PPM PPM>PPM PPM:PPM PCY

Zr

PPM

32 471 152 <20 <20 1 34. 503 161 <20 <20 1

6 538 74 <20 <20 <1 6 456 74 <20 <20 <1

4.10 4.65 5.08 0.02 0.56 53 5 18 9 18.'!;<10 0.21',; <1 4.21 4.78 5.11 0.02 0.59 55 6 19: 10 19';<10 0.22: <1

2.74 2.85 1.00 0.04 0.06 12 4 3 4 <5::<10 0.21':> <1 2.69 2.77 0.05 0.07 13 4" 3 4 15:<10 0.20 <1

1.41 0.78 1.42 0.07 0,14' 49 3 <1 ~ <10 g4.1„: 6 1.44 0.81 '1 47 0.07 0.14 > 52 4. 3 <1 <5 <10 0.11 6

1.04 0.53 2.16:'0.04 _ 0.28:' 40 <2 <1 <10 0.03!:: 24

2.52 2.38 2.64 0.07 0.05 66 4 10;: 4 <5;:<10 0.18::i 2 2.55 2.42 2,72 0.07 0.05i 66 5 10 4 <5:<10 0.17> 1

2.46 2.27 4.16 0.07 0.04 45 6 5 103:'<10 0.14? 2 4.36

<10

4:124 80 <20 <20 5





SUBMITTED BY: D. BASIN


11 -150 11 CRUSH/SPLIT & PULV. 11 DRILL CORE


NUMBER OF ANALYSES


990913 1 Au30 Gold 11 5 PPB Fire Assay of 30g 30g Fire Assay - AA 990913 2 Ag Silver 11 0.2 PPM HCL:HNO3 (3:1) 1NDUC. COUP. PLASMA

990913 3 Cu Copper 11 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990913 4 Pb Lead 11 2 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990913 5 Zn Zinc 11 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990913 6 Mo Molybdenum 11 1 PPM HCL:HNO3 (3:1) 1NDUC. COUP. PLASMA

990913 7 Ni Nickel 11 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990913 8 Co Cobalt 11 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990913 9 Cd Cadmium 11 0.2 PPM HCL:HNO3 (3:1) IMDUC. COUP. PLASMA

990913 10 Bi Bismuth 11 5 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990913 11 As Arsenic 11 5 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990913 12 Sb Antimony 11 5 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990913 13 Fe Iron 11 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990913 14 Mn Manganese 11 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990913 15 Te Tellurium 11 10 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990913 16 Ba Barium 11 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990913 17 Cr Chromium 11 1 PPM HCL:HNO3 (3:1) IMDUC. COUP. PLASMA 990913 18 V Vanadium 11 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990913 19 Sn Tin 11 20 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990913 20 W Tungsten 11 20 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990913 21 La Lanthanum 11 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990913 22 Al Aluminum 11 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990913 23 Mg Magnesium 11 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990913 24 Ca Calcium 11- 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990913 25 Na Sodium 11 0.01 PCT HCL:HNO3 (3:1) 1NDUC. COUP. PLASMA 990913 26 K Potassium 11 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990913 27 Sr Strontium 11 1 PPM HCL:HNO3 (3:1) 1NDUC. COUP. PLASMA

990913 28 Y Yttrium 11 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990913 29 Ga Gallium 11 2 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990913 30 Li Lithium 11 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990913 31 Nb Niobium 11 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990913 32 Sc Scandium 11 5 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990913 33 Ta Tantalus 11 10 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990913 34 Ti Titanium 11 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990913 35 Zr Zirconium 11 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA


REPORT COPIES TO: #6-1349, KELLY LAKE RD. INVOICE TO: #6-1349, KELLY LAKE RD.

** ewe***** * tan *********** k****************** r*win*******,k, *******-k,k **** ********

This report must not be reproduced except in full. The data presented in this report is specific to those samples identified under "Sample Number" and is applicable only to the samples as received expressed on a dry basis unless otherwise indicated




CDR9906-1257 61 0,5 I 688 <2;: 50 2 136 79 <.2 <5; '. 8 <5 6.95 557 <10 22 457 74 <20 <20 CDR9906-1258 114 0.7 1165 c2 51 : 2 135 162 <.2 <5. ' 9 <5 8.19 584. <10 16 321 74 <20 <20 CDR9906-1259 147 0.9:1154 <2> 67 7184 182;<.2 <5 ; 11 <5 >10.00 736'. <10 27 324 106 <20 <20 CDR9906-1260 289 1.72729 <2 68 2?104 221 <.2 <5 15 <5 >10.00 826. <10 8 401 130 <20 <20 CDR9906-1261 5 <.2 58 <2 54 1 119 35:<.2 <5 <5 <5 7.57 855. <10 1 432 139 <20 <20

CDR9906-1262 60 0.7I'; 734 Q;; 70 163 148 <.2 <5:: 10 <5>10.00 816 <10 ':35 613 .173 <20 <20 CDR9906-1263 89 0.5 1 648 <2'. 65 198 191':<.2 <5<: 10 <5>10.00 827 <10 ' 2 :722 .137 <20 :;<20.. CDR9906-1264 7 0.4' 461 <2' 54 252 54<.2 <5<; <5 <5:' 8.14 861 <10 ::7 901 151 <20 <20 CDR9906-1265 <5 <.2 61 <2 1 39 1' 271 40:<.2 <5:!i <5 <5 5.16 597 <10 5 778 101 <20 Q0. CDR9906-1266 561 3.(0511 11<> 68 17 219 575 1.1 <5('110 <5 I> 10.00 613 <10 ; 5 586 ::87 <20 <20

CDR9906-1267 12 <.2 199 41 2!:308 62:'<.2 <5 4.68 446. <10 773 64-<20 <20 :

_ .. .

_ _.. 1,87 0.02 0.32' 17 2 <2 9 4 <5 <10 0;13;' <1 1.66 0.03 0.20' 15 2 <2 6 3 <5.<10 0.12 <1 2.50 0.01 0.34 20 2 <2 5. 5 ..:7;<10 0.12; <1 4.55 <.01 0.08 39 3 2 9 6 :14.<10 0.09> <1 5.79 '<.01 <J11 52 4 4 .14 8:19<100.10I<1

3.89 <.01 0;37: 34 5. 4 13: 11 22 <10 0.12':: <1

4.09''0.01 <.01 34 4 3 13 8 24 .<10 0,08' <1 6.40 0.01 0.05

3.88 0.02 0.05 62 38

5

4',.

5

4

10

8

9

7

26 <10

11: <10 4;13;<1 3.14 0.02 Q 02:j: 32 2:. <2 6 3 <10 0.~0.': <1

1,04 0.03 0 0i 17 2 <2 61 3 <5 <10 0.12;; <

3 2.58 2.02

6 2.39 1.77 4 3.14 2.01

5 3.82 2.92 1 4.12 3.98

11 4.36 2.92

6 4.26 2.92

2 3.64 3.06

1 2.64!2.48 5 2.47 1.87

<1 2ï1 2 1.80

ions Intertek Testing Services Chimitec Bondar Clegg





SAMPLE

ELEMENT Au30 Ag Cu Pb. Zn MR :< Ni CO. Cd BI ; As Sb Fe

Te 8a Cr V Sn W La AL Mg Ca: Na K'. Sr my. Ga.L; Nb Sc Ta :: T1: Zr NUMBER

UNITS PPB PPM PPM PPM PPM PPM PPM PPM 'PPM PPI1 PPM PPM PCT

PPM PPM PPM PPM PPM PPM PPM ':PCT< PCT PCT: PCT PCT PPM PPM PPM PPM PPM 000 pm PCT;; PPM


Mg Cas Na PCT .PCT: PCT

<K:

PCT:

Al

PCT:

<1 <20 <20

1

10 I10

<1

1

<1

<1. <1

<1

Mink Te AO: Cr '; W Sn W. La

PPM PPM PPM PPM PPM PPM PPMPPM

<1. <10 ..........

Sr Y Ga :I„V Sc> Ta PPM PPM PPM PPM PPM PPM PPM

<1 <1> <2 <:1! <1 5:<10 <:01 i: <1

1 1> 1 1: 1 1 1 1;'? 1 <1<1i; 1 .<.1; <1 3. 5 <.01;> <1

<.01 <,01:<.01 <,01

.01':<.01 <.01 <.01 <.01

.::1I: <1 <1 4.01; i><.01 r

42

<20 <20 52

1 ::1! 1

10 18r 52 1.51:

1840<; 29 ;48»

17,82 ;:<10 201 27

1 1 ;:1;: 1

1782 5 201 27

0.62 0.61 0.03 0.19 ...... 1 1> 1

0.62 0 61 0.03 0.;19






STANDARD ELEMENT Au30 Ag; Cu Pb' Zn Mo Ni Ca Cd BI As Sb: Fe NAME UNITS PPS PPM: PPM PPM :PPM PPM:?PPM PPM,PPM PPM PPM PPM PCT

ANALYTICAL BLANK <5 <,2> 2 . <2',; <1 <1: <1 <.2 <5 <5 ( <0.01

Number of Analyses 1 1 1 1: 1 1 1 1I 1 Mean Value 3 0.1 <1 <1 <1 0.1 3 3i <0.01 Standard Deviation

Accepted Value 5 0.2. 1.0 5 . 5> 0.05



Mean Value 465

Standard Deviation

Accepted Value 465

CANMET LAKE-SED 2 - 0.4:: 34 35::179 21 15;:;0.7 <5 10 <5. 3.60

Number of Analyses 1 1. 1! 1 1:: 1 1

Mean Value - 0.4> 34 35`179 21 15>'0.7 3;i: 10 3.60

Standard Deviation

Accepted Value - 0.8I 36 40200 23 17,:;0.8 9 3.50




CLIENT: CAMECO GOLD INC. PROJECT: CEDAR RAPIDS

REPORT: C99-62542.0 ( COMPLETE )


SAMPLE

NUMBER

CDR9906-1259

Duplicate

__. _.. _.. _.,...

ELEMENT Au30 Ag', Cu Pb;: Zn Mo;:; Ni Co:: Cd Bi As Sb; Fe

UNITS PPB PPM PPM PPM !PPM PPM I PPM PPM PPM PPM PPM PPM PCT

147 0,91154 <2: 67 184 182';<.2 11 >10.00 <10 ;;27 324 106 <20 <20 4 3.14 2.01 2.50 0.01 0.34 20

164 0.91112 <2 . 65 178 180 10 >10.00 <10 :27 322 104 <20 <20 5 3.07 1.97 2.44 0.01 0.331:: 20

Z> <2

5

<10 0;12. <1

Z; <2

5

<100.12'<1

PPM

Te Ba Cr V Sn Y La

PPM PPM PPM PPM. PPM PPM PPM PCT

Mg

PCT Ca Na

PCT

~s Sr Mri! Ga AE Nb Sc: Ta 11-6 Zr

PCF;;PPM PPM:': PPM PPM';:PPM PvMi;PPM PGI''::PPM

ITS - Chimitec - Bondar Clegg, 1322-B Harricana, Val-d'Or, P.Quebec, 19P 3X6, (819) 825-0178

DRILL CORE 58 -150 58 CRUSH/SPLIT & PULV. 58 TRANS FROM POLY BAG 58


NUMBER OF ANALYSES

LONER DETECTION

990928 1 Au30 Gold 58 5 PPB 990928 2 Ag Silver 58 0.2 PPM 990928 3 Cu Copper 58 1 PPM 990928 4 Pb Lead 58 2 PPM 990928 5 Zn Zinc 58 1 PPM 990928 6 Mo Molybdenum 58 1 PPM

990928 7 Ni Nickel 58 1 PPM 990928 8 Co Cobalt 58 1 PPM 990928 9 Cd Cadmium 58 0.2 PPM 990928 10 Bi Bismuth 58 5 PPM 990928 11 As Arsenic 58 5 PPM 990928 12 Sb Antimony 58 5 PPM

990928 13 Fe Iron 58 0.01 PCT 990928 14 Mn Manganese 58 1 PPM 990928 15 Te TeL 58 10 PPM 990928 16 Ba Barium 58 1 PPM 990928 17 Cr Chranium 58 1 PPM 990928 18 V Vanadium 58 1 PPM

990928 19 Sn Tin 58 20 PPM 990928 20 W Tungsten 58 20 PPM 990928 21 La Lanthanum 58 1 PPM 990928 22 Al Alunirxm 58 0.01 PCT 990928 23 Mg Magnesiun 58 0.01 PCT 990928 24 Ca Calciun 58 0.01 PCT

990928 25 Na Sodium 58 0.01 PCT 990928 26 K Potassiun 58 0.01 PCT 990928 27 Sr Strontium 58 1 PPM 990928 28 Y Yttrium 58 1 PPM 990928 29 Ga Galliun 58 2 PPM 990928 30 Li Lithium 58 1 PPM

990928 31 Nb Niobiun 58 1 PPM 990928 32 Sc Scandium 58 5 PPM 990928 33 Ta Tantalus 58 10 PPM 990928 34 Ti Titanium 58 0.01 PCT 990928 35 Zr Zirconium 58 1 PPM


EXTRACTION METHOD

Fire Assay of 30g 30g Fire Assay - AA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) IMDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA

HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) IMDUC. COUP. PLASMA

HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) IMDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA

HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA

HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) IMDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA

HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) IMUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA


REPORT COPIES TO: MIKE KOZIOL INVOICE TO: MIKE KOZIOL

******* r tir*****************ir****ir*******,r******** ****ir+r*rti ***w****************

This report must not be reproduced except in full. The data presented in this report is specific to those samples identified under "Sample Nurber" and is applicable only to the samples as received expressed on a dry basis unless otherwise indicated

******w************************************************************#********* **

mol Intertek Testing Services Chimitec Bondar Clegg



REFERENCE: 170410

CLIENT: CAMECO GOLD INC. SUBMITTED BY: D. BASIN



Effli Intertek Testing Services Rapport Lab Geochimie Chimitec Bondar Clegg Geochemical Lab Report


PROJECT: CEDAR RAPIDS DATE RECEIVED: 22-SEP-99 DATE PRINTED: 29-SEP-99 PAGE 1 OF 5

SAMPLE ELEMENT Au30 Ag Cu Pb Zn Mo Ni Co Cd Bi As Sb. Fe NUMBER UNITS PPB PPM PPM PPM PPM PPM PPM PPM PPM PPM:PPM PPM PCT

Mn ' Te ..Be: Cr . . V Sn . ,N La PPM';PPM PPM PPM PPM PPM PPM PPM

All Mg CB; Na

PCT. PCT PCT::; PCT [~ Sr Y; Ga ,L1;

PCT: PPM PPM PPM PPM::PPM Nb Sc:; Ta

PPM;:PPM Zr

PCT'; PPM

WR-9932-1386 43 <.2; 195 1'' 30 32 17 <.2 <5';! <5 <5 2.40 264: <10 441141 .30 <20 x20 20 1.85 1.43 :1,3ü::0.070.1a 152 4 <2 7::; 2 <5:;<10 p' 0?: 8 WR-9932-1387 WR-9932-1388

51 27

<.2> 0,2:

209 92

2 9:

32 30

42 38

17 <.2 16;<.2

<5 <5:;1

<5 <5

<5 2.60 <5 (2.38

312 <10

329 <10 56 144 22:145

.391.<20 40-<20

<20 <20

9 8

1.95 1.72 1,52 0.070 26:'122 1.96 1.83 :1,71 0.070,09i'115

.3.. 2 3'. <2

3<5:i<10 3 <5::;<10

0 13?: 5 5

WR-9932-1389 26 <.2: 157 <2. 23 33 17:<.2 <5 <5 .<5:!1.97 288 <10 31:117 29<20 <20 13 1.56..1.37:1..86>:0.09 0.10:: 91 4: <2 6: 2 <5<10 0.09:: 7 WR-9932-1390 22 0.2!: 75 3 20 38 16 <.2 <5 <5 <5 1.70 194 <10 28112 29-<20 <20 5 1.39 1.32 1.44 ::0.08 0.11 ` 47 <2 5 2 <5::<10011:: 14

WR-9932-1391 47 0.3 169 <21'<: 52 1i'i 77 361I:<.2 <5 5.32 646 <10 37 176 84 <20 <20 4 3:54 3.56 3.21 0.03 0,24.> 91 <2 141: 6 4<'<10 0 14: <1 WR-9932-1392 31 <42' 63 3:' 33 11:! 73 25:<.2 <5 <5 <5 3.35 318 <10 . 86 180 70 <20 <20 2 2.39 2.24 1.28 0.05 0,67 66 <2 8 5 <5:<10 0.19: 1 WR-9932-1393 40 <42 212 <2 35 10:>: 57 45;;<.2 <â; <5 <5 3.34 .388f<10 39 168 60 <20 <20 6 2,52 2.57 1.95 0.05 0.26;: 72 <2 10! 4 <5:<10 0,.161 5 WR-9932-1394 23 <.2 204 <2 38 .25'' 50 22>I<.2 4 <5 <5 3.23 40.0. : <10 . .31: 150 40 <20 <20.. 5 2.21 2.22 2.86 0.06 0.13:! 63 <2 9> 3 <5.1<10 6.11a: 5 WR-9932-1395 12 0.2I 104 <2 38 25:' 54 20:<.2 <5 <5 <5 3.49 392 <10 22 175 47 <20 <20. 6 2.50 2.42 2.45 0.05 0.10': 78 2 .10 3 <5>:<10 0..13 5

WR-9932-1396 39 0.3 330 <2; 37 29si 53 25<:<.2 <5 ` <5 <5 3.11 381:':!:<10 37 168 55 <20 <20 6 2.38 2.49 2,26 0.06 020; 58 4 <2 9' 4 <10 0.15 4 WR-9932-1397 59 <.2' 382 <2!! 34 38_:! 65 26<.2 <5ü <5 <5 3.88 362 <10 74 162 60 <20 <20 5 2.34 2.30 1.98 0.05 0.43 66 3! <2 9.: 4 i5 <10 0.1k 3 WR-9932-1398 8 0.2 ' 107 <2 41 24:: 64 21';:<.2 <5 > <5 <5 :3.52 422;><10 65', 176 63 <20 <20 5 2.66 2.64 2.12 o.o6 0,35 ` 72 3'! 2 10 5 5 <10 007!;' 3 WR-9932-1399 7 0.2 107 <2 45 171:: 36 21>:<.2 <5 <; <5 <5 < 4.24 496:ü<10 27 113 42 <20 <20 13 2.65 2.32 3.48::0.04 0.13 112 4. <2 10< 3 <5 <10 0.08> 2 WR-9932-1400 13 0.3 237 2<; 316: 32 15<.2 <5 <5 <5 2.76 366 <10 211 175 27 <20 <20 9 1,68 1.49 3.28 0.04 0.11< 94 4 <2 <5 <10 0,06: 3

WR-9932-1401 <5 0,2<I! 18 2 41 .7 65 18;' <.2 <5:` <5 <5_3.44 415: <10 24::162 34::<20 <20: 8 2:46:2.33 3,25;:0.05 0.11:: 86 4: 3 1 2 <5;;<10 (149 2 WR-9932-1402 25 <.2: 90 <2. 23 7:: 29 13<.2 <5>: <5 <5>1.44 176: <10 43:> 97 20:: <20 <20': 5 1.47 1 09 20.08 .1'.53 0.14 > 84 3 2 5:: : 1 <5:00 0.12': 3 WR-9932-1403 20 <.2': 101 <2 29 4:: 29 .13<.2 <5 ;: <5 4:4.90 232 <10 97:: 99 20:<20 <2Q; 5 1.6.7 1.29 1:$4;;0.08 0 11; 80 3i <2 7; 1 . K5::<10 0.11;; 5 WR-9932-1404 <5 0.2 11 <2: 25 3:: 32 10 <.2 <5.:: <5 <0.72 272: <10 53:: 86 12;:<20 <24: 81.57 1.10 2 0.04 0 Z0:: 67 2 <2 7: <1 <5 ;<10 0 05 ;: 7 WR-9932-1405 13 1.21 135 <2 26 4;' 32 14;!<.2 <5 !: <5 <5:1.73 195: <10 32 : 95 20;: <20 <20 5 ? ô0 1 2s 1.39 ;0.07 0 10, 75 2< 2 7 1 <5(;<10

WR-9932-1406 24 <.2;I 119 <2.:I 27 8: 31 14;:;<.2 <5 <5::1.77 1510 411 92 18 <20 <20: 5 1.56 1.18 126_0.07 012.: 78 2.: <2 . 7 <1 <5::<10 0,11;i! 5 WR-9932-1407 11 <.2 ` 67 <2:> 30 3:: 30 13<.2 <5 <5:::1.70 220;<10 33105 24 <20 <20 5 1.74 1.34 1.22 0.08 0.09 96 <2 . T 1 <5<:<10 0.13:: 6 WR-9932-1408 11 s 2i` 76 <2:: 29 4 :: 28 13:<.2 <5 . <5 1.71 88 15 <20 <20 4 1.58 1.09 2,13 ;0.06 0.18 i 65 2 { <2 Hf1; <1 <5,<10 0.10: 6 WR-9932-1409 9< 2`::' 94 .<2: 27 671 31 13:::<.2 <5; <5 <51.61 190;<10 34> 97i 18 <20 <20 4 1.64 1.24 1.39::0.08 0.12' 70 2< <2 7: <1 <5:::<10 0.11 6 WR-9932-1410 10 <.2 83 . 26 .3z 30 14:1:<.2 <5 ''<511.70 1.70 184 ;'<10 36!; 97 22 <20 <20 5 1.78 1.31 1.21 0.08 0.11 91 .. 3> 2,7: 1 <5::<10 0,13;:; 6

WR-9932-1411 8 <.2I:: 52 +2: 25 29 14::<.2 <5:; <5 <5;:1.72 227;<10 13: 103 233;; <20 <20! 4 1';64 1.24; 1;85:0.09 0 04:::106 2 8:: 1<5s:<10 0 12; 6 CDR-9932-1412 <5 <,2; 47 <2 27 z 28 12:;<.2 <5:>: <5 <5;1.64 .207:<10 29 103 20 <20 <20'; 5 1.56 1.22 1>.490.08 0.88 78 2:: 2 T: 1<5:1<10 p..11:] 7 WR-9932-1413 11 <,2;: 69 <2> 25 51; 29 .12;!<.2 <5 <5 <5:s2.04 227<10 38 109 14::<20 <20 4 1.67.1 22 2;07:0.05 0.14: 51 <2 10< <1 <5 <10 4:.,44 7 WR-9932-1414 9 <.2; 83 <2 25 18: 28 9: <.2 <5;: <5 <5 :1.69 217:<10 32 91 14i<20 <20 5 1:.55 1.16 2:19<0.05 0.1.2`. 64 Z:: <2 11Y <1 <5's<10 p.0.. 7 WR-9932-1415 15 <.2;!; 220 <2:!: 46 3:: 28 19<<.2 <5; <5 <5::2.99 400<10 48: 71 .40<20 <20: 24 09:1.84 2.29:0.05 0.11172 4;: <2 2 <5::<10 0.14.;: 9

ITS - Chimitec - Bonder Clegg, 1322-B Harricana, Val-d'Or, P.Quebec, 39P 3X6, (819) 825-0178 re3

Intertek Testing Services Rapport Lab Geochimie

Chimitec Bondar Clegg Geochemical Lab Report CLIENT: CAFECO GOLD INC. REPORT: C99-62736.O ( COMPLETE )



. _ _ _. .. __. _... SAMPLE ELEMENT Au30 Ag Cu .Pb:. Zn:Mo- Ni Co:: Cd 81.': As Sb< Fe

NUMBER UNITS PPB PPM: PPM PPM:PPM PPM: PPM PPM::PPM PPM :PAM PPM PCT Mn: Te B8' Cr V Sn W La

PPM: PPM PPM PPM PPM PPMPPM PPM Ai> Mg Cs: Na ,...If' Sr Y;: Ga L#;: Nb Sc:: Ta T1 Zr

PCT :PCT PCT: PCT PCT ;':PPM PPFI;PPM P1'!#:'PPM PPM :PPM PCT :PPM

CDR-9932-1416 20 <.2: 171 <2:;, 30 29 <5 <5 <5 1.79 271: <10 45; 92 ;.4.<20 <20 6 t.74 ;1. 32 1.58 ::0-07 0.10 103 3'; <2 7;: 1 ti5,':i<10 0.13: 5

CDR-9932-1417 9 4.2: 123 <2 27 30 13:<.2 <5:;: <5 <5. 1.74 266'. <10 39. 94 16 <20 <20 3 1.68:1.20 1.92 0.07 0.11 66 . 2:: <2 . .9. ; <1 <5 <10 0.10:< 4

CDR-9932-1418 26 0.2 263 <2 : 32 9!: 32 14?<.2 <5 <5. 2.09 246 <10 40 98 19 <20 <20 4 1.90 1.42 :t 63 ;0.08 0.10; 65 2 <2 11;; <1 <5;,<10 1:01.:: 4

CDR-9932-1419 14 <.2. 160 <2: 23 7: 29 12;!;<.2 <5 45. 1.69 266' <10 44 84 12 <20 <20 41.:490.98 2.81:':0.06 0.16: 59 2` <2 9<: <1 .<5::<10 0.04? 7

CDR-9932-1420 13 0.2,. 142 <2.;,; 27 3; 27 <5<; <5 <5, 1.78 231: <10 33 90 16 <20 <20. 4 1.73:1.14 2.21 0.06 0.13. 79 2!: <2 10i: <1 <5::<10 4.47;!i 5

CDR-9932-1421 21 <.2 229 <2 ; 28 8: 30 13::<.2 <5:; <5 55!;:1.72 187 <10 34:108 19.<20 <2U 5 1"031.04 ;1:33 :;0. 07 1:107.: 87 2 <1 <10 0.08 6

CDR-9932-1422 12 0.3 187 <2 28 15< 28 12'<.2 <5: <5 .<51.94 364 <10 45; 77 10 <20 <20 3 1.52 1.00 3.96:0.03 0.19>' 38 <2 9. <1 15 :<10 6

(DR-9932-1423 25 <,2: 283 <2 : 33 7 29 12<.2 <5: <5 42.14 205<10 24'115 21.<20 <21I 4 1.85 ;1. 27 1.26 ;10.07 0.47:: 77 3 11 1 <5:<10 0,08: 5

CDR-9932-1424 51 <.2 467 2i 32 6 34 )4:::<.2 <5!: <5 <5 2.07 2351 <10 46:. 85 14:<20 <20 5 1.791.17 2.11 :i0.06 0.19:I 65 <2 1:0 <1 0.05:: 8

CDR-9932-1425 15 0.3 211 Q ;; 19 5; 22 9;:<.2 <5;; <5 <51.43 231 <10 27:177 .7. <20 <20 3 1;01.:0.68 _.. 3.82::0.04 0,12:1 57 <2 6 <1 0.03: 6

CDR-9932-1426 62 <,2 702 2;; 30 4:> 33 15::<.2 <5:: <5 <5'. 1.89 184'. <10 24 114 20 <20 <20 6 1.75 1.11 1.43 0.10 0.0-:; 94 <2 <1 4,16: 5

CDR-9932-1427 CDR-9932-1428

22 <,2

18 <.2 155 208

<2: 28 <2`:31

10 4

33 13(:<.2 32:13.;<.2

<5 :: <5:

<5 <5

<51 1.77 <5 1.79

187'. <10 208 <10

34%106 28104

20 <20 21: <20

<20. ~20

5 5 1.74 1.10 1.76 1.29

1.47 0.09 0.08:? 96 ;1.56 0.09 0.07:i 86

<2 2 8

10: 1

1

s5:;<10 <5::;<10 0,12>

5 5

CDR-9932-1429 22 <..2. 321 2i 31 :::5:: 31 16::<.2 <5: <5 <5: 1.68 189 <10 35111 21:.<20 <2Q 6 1.721.32 1.28 0.09 0.09 68 2: <2 9 ...5 .<10 0..12 7

CDR-9932-1430 16 <.2 276 <2,:: 30 4;; 30 20i<.2 <5.I;: <5 <5 1.86 203. <10 29: 97 20.. <20 <20 6 1.66 1-26 1-69 OM 0.49:: 72 <2 <1 <5;!:<10 0.11:i

0)R-9932-1431 12 <.2 144 2!: 29 5::: 27 <5 2001 .<10 40 102 W<20 <20 7 1.72:1.17 :1,61;:;0.09 0,12;: 87 <2 <1 <5(:<10 0,11 6

CDR-9932-1432 134 0.3 1167 <2: 30 . 6: 32 13:<.2 <5<; <5 <51.61 169:<10 47.102 21' <20 <20 6 1.53:1.18 1.18::0.09 0.11:: 57 <2 <1 <5i <10 0.12:: 8

CDR-9932-1433 <5 <,2 185 <2;; 23 7• 27 12':;<.2 <S`:'. <5 <5::I1.51 153:<10 51108 17 <20 <20 10 1.45 0.95 1.24>'0.09 0.11'1: 76 <2 <1 5;:<10 4.12I< 10

CDR-9932-1434 252 0.3 1394 <2:: 30 832 <5 <52.05 164.<10 36 103 23 <20 <20 7 1.65 1.24 1.48 0.10 0.10 67 2 1 .<5><10 0 12<'' 7

CDR-9932-1435 99 0.5 2395 2 30 20::: 29 15::<.2 <5'_i <5 <5>i1.98 159.<10 36 90 19 <20 <~0 6 1081 1.21 1.64<,0.09 0.12 59 <2 <1 <5::<10 0.11> 7

CDR-9932-1436 68 0,3. 871 <2:1; 26 23:; 30 21i::<.2 H<5..- <5 <5 1.91 188::::<10 40 86 16 <20 <20 6 1.62 1.13 2.34:>0.08 0.16;: 58 <2 <1 55::<10 4;49<: 7

CDR-9932-1437 49 0.3. 398 2>: 24 14 :: 31 31<.2 . <5 > <5 <5::!2.02 191' <10 42:101 13<20 <20 5 1.63.1.12 2.43:!0.07 0.17:: 58 <2 10; <1 <5::<10 0.06:: 8

CDR-9932-1438 7<.2 178 <2 :: 18 5 : 20 1.2 <5::; <5 <51.43 120:<10 37:129 13 <20 <211 8 1",45-0.89 1.34:0.08 0.11:: 81 <2 . 7.; <1 <g <10 0.06:: 8

CDR-9932-1439 43 0, 2, 715 <2:: 23 9: 30 16<.2 <5:: <5 K51.90 16p:<10 32 87 16 <20 <20. 5 1.À2: 1.13 1 7:0.08 01::: 73 <2 10s <1 . <5::<10 0.10> 7

CDR-9932-1440 14 <.2. 168 2:: 27 5':: 30 11;<<.2 <5 > <5 .<51.90 170 <10 28 100 262o <20 5 1.82 1.31 .142.!0.09 0.08: 83 <2 Al,< 1 '..i:.<5::::<10 4.10:; 6

CDR-9932-1441 43 4 3: 987 29 32 16;<.2 <$:f: <5 <5 2.13 214-<10 31:101 20 <20 <20: 7 100.28 28 1.770.09 04c 18;: 77 2 11: <1 <5<<10003: 8 CDR-9932-1442 12 <2i 163 25 20 10:<.2 <5 <5 <5 1.91 22$;<10 37 116 17. <20 <20 10 1.820.07 Ii 77;:0.08 0015 2 10 <1 <5<10 < 01' 7

CDR-9932-1443 38 0,3:> 506 27 31 18:<.2 <5 <5 <5 2.33 248 <10 41 94 15 <20 <21:r 1.76:1.09 334;:0.08 0.15: 57 2 <1 <5''<10 < 01 8


23 17 1 0.8

Al

PCT Mg Ca Na

PCT iPCT ` PCT

STANDARD

NAME

ELEMENT Au30 .Ag, UNITS PPB PPM

Cu Pb Zn Mo': Ni .Co> Cd Bi: As Sb: Fe

PPM PPMPPM PPM{: PPM PPM.PPM PPM PPM PPM; PCT

Mti;< Te Be;: Cr V: Sn : u: La PPM:PPM PPM;::PPM PPM PPM PPM,.PPM

Sr Y' PPM PPM

Ga Li;: Nb St.,; Ta Tfi:' Zr

PPM PPlF ;PPM PPM1.::PPM PCT;PPM

<1 3>: <1 <1;> <1 <1;;'<.2 <5.:: <5 <5 <.01 <1:!;:<10

1 3:: <1 <1 > <1 <t<.2 <5 <5 <5 <.01 <1!::<10

2. 2: i 2 2::: 2 2 I', 2 21' 2 Z.:' 2

<1 <1';i <1 <1 0.1 3 ;i 3 3 !:<.01

Standard Deviation - <1

Accepted Value 5 0 2 1 2' 1 1: 1 4::;1.0 2I 5 5:';0.05

<20 <20I <1 <.01 <.01 x 01;':i<.01 < <20 <20:. <1 <.01 <.01 <.01'':<.01 <

2

10 1t) <1 ;01'6.<.01 < 01<.01 <

<1 <:0.1 <.01F.01';:<.01

*1

Oxide (feldspar & 957

Number of Analyses

Mean Value 957

Standard Deviation

Accepted Value 968

CANMET LAKE-SED 2

Number of Analyses

Mean Value

Standard Deviation

Accepted Value

Oxide (Feldspar &

Number of Analyses

Mean Value

Standard Deviation

Accepted Value


Nunber of Analyses 1

Mean Value 446

Standard Deviation

Accepted Value 465

<20 <2.0: 55 1;76 0.69 0.70 0.04 0.24 30 28 <2

1 1: 1 1 1 1 1 1; 1

10 10: 55 1.76 0.69 0.70`:0.04 0 24<: 30

23 :16;0.7

1 1> 1

23 16::0.7

ANALYTICAL BLANK

ANALYTICAL BLANK

ANALYTICAL BLANK

Number of Analyses

Mean Value

<5 <i;?

<5 < Z' <5

3

3 0;

<5:.<10 <,01:; <1 <3<10 <..01:: <1

<1

<10 0,03:: 2

1 1:; 1

5(108:; 2

- 0.4

- 04

- t1:8?

178

1

178

186








19 3

1 1

7'<10 <, 0i: < 4

19 3 7;

Elge Intertek Testing Services Rapport Lab Geochimie Chimitec Bondar Clegg Geochemical Lab Report

CLIENT: CAMECO GOLD INC. PROJECT: CEDAR RAPIDS REPORT: 099-62736.0 ( COMPLETE ) DATE RECEIVED: 22-SEP-99 DATE PRINTED: 29-SEP-99 PAGE 4 OF 5

I'n Te ' Bs . Cr A Sn Y La Ai

PPM: PPM PPM PPM PPM PPM P151:0 )PM

Mg : Ca Na ~; Sr y: .': Ga MI: Nb Ta Zr

PCT ::PCT:: PCT PCI:PPM PpF1::PPM PPlt:_PPM 1444 .:4441 PCT _PPM

STANDARD ELEMENT Au30 Ag Cu Pb Zn Mio! Ni Co Cd Bi: As Sb Fe

NAME UNITS PPB PPM'.; PPM PPM: PPM PPM: PPM PPM PPM PPM:: PPM PPM:: PCT

1332 <10 6: 172 44 <20 <20 2 1> 1 1:: 1 1> 1

1332: 5 6 172 44i: 10 10 2

1454: <1 :6 251 .:50 5

1::83;2.45 3,45 0.01 0 05;:; 74 <2

1 . 1 1 1$3 2.45 3.45 0.01 0,05 ? 74 ;. 1

1i80 2.70 4.00 0.01 0.04 70

STD GEOCHEM STD 6 - <.2i 145 16127. 2:113 29 0.4

Number of Analyses - 1:i 1 1: 1 1 1 i 1

Mean Value - 00 145 16::127 2;113 0.4

Standard Deviation - -

Accepted Value - 0',.2 148 20148 4;::135 35 0.2

127 <5 7.13

1. 1:!: 1 127 3 7.13

7.20


63

66 . 2 <2

2 2

2!' <2

2;1; <2

70

61

77 2 <2 1 <10 0;'11`: 6

64 2' <2 <1 <5:><10 O:fL#';: 7

<10 04 5

<10 O 12: 5

86

88 2 .1'0 1

2 .1.0> 1

<5 81

84

<2 <10 0.06 8

<10009 8 <5 <2

31 <.2. 63 3 33 71 73 25 <.2 A5: <5 <5 3.35 318-00 86 180 70 <20 <20 2 2.39''2.24 1.28 0.05 0.67: 10 < 2: 62 2< 32 11,? 73 25<.2 <5 <5 <5'3.34 316. <10 86 182 70.<20 <2Q 2 2:362.24 1.249.05 0 66:

9 <42 94 <2 27 671 31 13.:'<.2 <5 <5 <5:1 61 '::190 <10 34 97 18 <20 <20 4 1.64;: 1.24 '1 390.08 0.12' 5 <,2 93 <2 27 679 30 13 <.2 <,5 <5 <5?1.58 185.:<10 31 94 16 <20 +Q0 4 1.53 1.21 1,33 0.07 0 11:::

<.2 103 <2:1; 29 704: 32 14'<.2 <5: <5 <5>1.70 195 <10 35i!103 <20 4 1,67 1.23 52 0.09 o,12

9 <.2 83 <2` 25 18 28 <5I <5 <5:'1.69 217-00 :321; 91 <20 ::<2O 5 .55::1.16 2.19 0.05 0 12;::1 <5

18 <;2; 208 <2; 31 4:i' 32 13;:<.2 5; <5 <5 1.79 208.<10 28 104 21..<20 <20 5 1;761.29 1.56: 0.09 0.07:'. <.2: 213 <2:.' 32 4< 33 14 <.2 <5: <5 <5::'1.83 215 <10 29 106 22 <20 <20 5 1:.01.1.34 :1 630.09 0.08:

99 0;5 2395 2; 30 .20 29 15'<.2 <5:i1 <5 <5;:1.98 159 <10 36` 90 19 <20 <20 6 1.:61::1.21 1.64 0.09 0.12» 98

7 <.2 178 <2; 18 5;; 20 11i<.2 <5 <5 <5<1.43 120 <10 37 129 13 <20 r20 8 1,45:0.89 1.34 0.08 0,11:: 9 0.2 189 <2!: 19 5> 21 12';<.2 <5` <5 <5.?1.49 125 <10 38 121 14 <20 <20 8 1:52 0.94 :1 41 0.09 0.11

CDR-9932-1392 Duplicate

CDR-9932-1409 Prep Duplicate

Prep Duplicate

CDR-9932-1414

Duplicate

CDR-9932-1428

Duplicate

CDR-9932-1435 Duplicate

CDR-9932-1438 Prep Duplicate

59 3': <2

5 5<10 0,14;: 1

6 <5 (;:<10 0 19.;: 1

<1 <5:<10 0.11 6 <1 <5 <10 0.19 6






SAMPLE ELEMENT Au30 Ai:.Cu Pb Zn :Mo Ni Co

NUMBER UNITS PPB PPM: PPM PPM:PPM PPM:; PPM PPM::

Cd Bl As Sb Fe MnTe . Ba Cr Y Sn W La PPM PPM:: PPM PPM: PCT PPM PPM PPM PPM PPM PPM PPM PPM PCT

Mg Ca > Na

PCT ;PCT PCT

Sr Y:; Ga .L#; Nb Sc;; Ta Ti'::: Zr

PCT::PPM FFIR::PPM PPM;.PPM PPIl,:PPM PG1'::;PPM

ITS - Chimitec - Bandar Clegg, 1322-B Harricana, Val-d'Or, P.Quebec, 39P 3X6, (819) 825-0178



REPORT: C99-62737.0 ( COMPLETE ) REFERENCE: 170410

CLIENT: CAMECO GOLD INC. SUBMITTED BY: D. BABIN

PROJECT: CEDAR RAPIDS DATE RECEIVED: 22-SEP-99 DATE PRINTED: 29-SEP-99


NUMBER OF ANALYSES



DRILL CORE 60 -150 60 CRUSH/SPLIT & PULV. 60 990928 1 Au30 Gold 60 5 PPB Fire Assay of 30g 30g Fire Assay - AA 990928 2 Ag Silver 60 0.2 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990928 3 Cu Copper 60 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA REPORT COPIES TO: MIKE KOZIOL INVOICE TO: MIKE KOZIOL 990928 4 Pb Lead 60 2 PPM HCL:HNO3 (3:1) INDUC. CCUP. PLASMA 990928 5 Zn Zinc 60 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA **********************************'"`********************************************* 990928 6 Mo Molybdenum 60 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA This report must not be reproduced except in full. The data presented in this

report is specific to those samples identified under "Sample Number" and is 990928 7 Ni Nickel 60 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA applicable only to the samples as received expressed on a dry basis unless 990928 8 Co Cobalt 60 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA otherwise indicated 990928 9 Cd Cadmium 60 0.2 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA ******************************************************************************** 990928 10 Bi Bismuth 60 5 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990928 11 As Arsenic 60 5 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990928 12 Sb Antimony 60 5 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990928 13 Fe Iron 60 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990928 14 Mn Manganese 60 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990928 15 Te Tellurium 60 10 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990928 16 Ba Barium 60 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990928 17 Cr Chraniun 60 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990928 18 V Vanadium 60 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990928 19 Sn Tin 60 20 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990928 20 W Tungsten 60 20 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990928 21 La Lanthanum 60 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990928 22 Al Aluminum 60 0.01 PCT HCL:HNO3 (3:1) IMi)UC. COUP. PLASMA 990928 23 Mg Magnesiun 60 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990928 24 Ca Calcium 60. 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990928 25 Na Sodium 60 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990928 26 K Potassium 60 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990928 27 Sr Strontium 60 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990928 28 Y Yttrium 60 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990928 29 Ga Gallium 60 2 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990928 30 Li Lithium 60 1 PPM HCL:HNO3 (3:1) IM)UC. COUP. PLASMA

990928 31 Nb Niobium 60 1 PPM HCL:HNO3 (3:1) IMDUC. COUP. PLASMA 990928 32 Sc Scandium 60 5 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990928 33 Ta Tantalus 60 10 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990928 34 Ti Titanium 60 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990928 35 Zr Zirconium 60 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA


PROJECT: CEDAR RAPIDS DATE PRINTED: 29-SEP-99 PAGE 1 OF 5

Ca; Na Sr Y'; Ga Li: Nb . Scl1: Ta Ti Zr PCT :: PCT PCT. PPM PPM PPM PPM PPM PPM;: PPM PCT: PPM

3.06:'>0.13 0.11 65 3.85';0.13 0.14 74 3.,83 0.15 0,11I: 80 3.00 0.12 0.19 71 1.80 0.16 0.09 61

1.55 0.15 0.10 72 .1.78:0.14 0.14 69 1.53 0.12 0.11. ; 66 1%46'0.14 0.11 73 1.34 `: ;0 .13 0,08 i: 77

1.73 0.14 0.12 70 1.39 0.15 0.10 81 1.46 0 .11 0.10 .: 77 1.31 0.16 0.09 ; 76 1.31 0.15 0.09 69

1.55 0.14 0.10 i: 62 1.77:0.13 0.12 66 1.30 0.13 0.08 79 1.47 0.14 0.10 84 1.11 0.14 0.07 81

1.37> 0.14 0.08 68 192:0.11 0.14::: 81

1.55;0.14 0 O5> 79 2.18 0.14 0 06;: 65 1;40 0.14 0.07:: 85

1:25:i<0.13 0.05 89 1.73:0.15 0.08< 63 1.67 0.14 0.07 85 2.66'.0.09 0.14 59 2.00 0.13 0,09: 68

4 10;': <1 <2 10::i <1 <2 8 <1 <2 10: 1 <2 10.: 1

<10 c.41'<' 7 <5<<10 <01.. 6 <5<10 c,01;: 6 <5:<10 <.0.1<: 8 <5:`<10 <.01,1: 9

<5::<10 0,02 10 0.06' 8

i5;<10 0.07 9 ô::<10 0410. 7 <5;:<10 0.11 7

<5 I:;<10 0.10>;; 7 <5>:<10 0.12: 7 <5S:<10 0.11:: 7 <5.':<10 0;4: 7

..<5.<10

1 <5:;<10 0,1 1. 7 1 <5.;<100.11: 7 1 <5:<10 0.12: 6 1 <5<:<10 041Q!! 7

<1 <5;:<10 0.10;; 7

<5<100.06 <5::<10 0 01i 9 <ÿ::<10

2 11::: <1 4.c10 0.06'; 9 <2 0.10. 9

1 <5;<10 0A1. 8 Q. <1

10; <1 <5'::<10005; 10 8' <1 <5::<10 9<; <1 <5<:<10 0408>: 10




SAMPLE ELEMENT Au30 Ag Cu Pb'I Zn Mo Ni CO,< Cd Bi As Sb Fe NUMBER UNITS PPB PPM PPM PPM PPM PPM PPM PPM PPM PPM PPM PPM PCT

DATE RECEIVED:

Mn: Te Ba: Cr V Sn PPM: PPM PPMPPM PPM PPM

22-SEP-99

u La Al ; Mg

PPM' PPM PCT;; PCT

CDR-9932-1444 10 <.2 453 3 24 30 11 <.2 <5; <5 <5 2.15 226 <10 291 59 14 <20 <20 6 1.86 1.10 CDR-9932-1445 13 <;2:219 <2 21 28 14 <.2 <5.;I <5 <5 2.03 238'. <10 36! 56 11; '. <20 <20 6 1.76 0.93 CDR-9932-1446 38 <.2 502 <2 20 32 16 <.2 <5 <5 <5 2.12 229'. <10 29 74 11 . <20 <20 5 1.700.88 CDR-9932-1447 22 <.2.461 <2 15 22 10 <.2 <5 <5 <5 1.56 189. <10 68 ': 93 <20 <20 10 1.61 0.73 CDR-9932-1448 26 <.2<349 <2 25 32 13 <.2 <5 <5 <5 2.18 187: <10 37 82 24: <20 <20 5 1.80 1.27

COR-9932-1449 26 <.2 553 <2 25 3::: 32 14 <.2 <5 !' <5 <5 2.06 181'. <10 39'i:99 20 <20 <20 5 1.75 1.21 CDR-9932-1450 29 <,2 333 <2 25 3:I 33 14 <.2 <5 <5 <5 2.08 183 <10 42 S 88 20 <20 <20 5 1.79. 1.21 CDR-9932-1451 34 <.2608 <2 20 7 34 19 <.2 <5 ' <5 <5 2.03 144 <10 41 ': 86 17 <20 <2i 4 1.49 0.98 CDR-9932-1452 21 <.2 278 <2 26 3 34 16 <.2 <5 <5 <5(1.87 188 <10 43 ` 90 21'. <20 <20 5 1.77 1.27 CDR-9932-1453 6 <.2 96 <2 30 3 ; 31 12 <.2 <5 <5 <5 ;11.72 215 <10 41;I 92 22' <20 <20 5 1.81 1.36

CDR-9932-1454 16 <,2199 <2 27 2> 31 14 <.2 <5 <5 1.66 209;, <10 45', 83 19.:'<20 <20; 5 1.68 1.19 CDR-9932-1455 9 <.2 i152 <2:! 32 5 : 32 12':<.2 <5 <5. 1.75 215 <10 47: 100 . 211: : <20 <20 5 1..85 1.34 COR -9932-1456 12 <.2:i158 <2s, 31 :9. 1 32 13<.2 <5 1.79 208 <10 4 88 19:<20 20 5 1.79 1.33 CDR-9932-1457 11 <.2 146 .<2: 30 10 33 16 <.2 <5 <5 1.82 209 <10 99 2d,,. <20 <20j 5 1.76 1.26 CDR-9932-1458 40 <.2519 <2.: 30 4'I 36 22<.2 <5 <5 2.14 199 <10 39 98 21..<20 <20;( 7 1.68 1.27

CDR-9932-1459 22 <.2303 <2!L 29 31 16 <.2 . <5<: <5 <5 1.72 215 <10 39 106 .20:<20 <20: 6 17 60:1.22 CDR-9932-1460 30 <.2432 <2> 28 3; 29 17 <.2 <5 <5 <5 1.87 224 <10 43 78 19:<20 <20> 5 1.621.19 CDR-9932-1461 14 <.2`142 <2.'! 31 3 31 13 <.2 <5:! <5 <5 1.77 <10 37! 103 .21:;!<20 <20 5 L80 1 31 CDR-9932-1462 11 ,c.2 172 <2 29 4< 31 14: <.2 <5 <' <5 <5::! 1.84

213<10 207: 42i:101 21;<20 <20: 5 1.85.1.26

CDR-9932-1463 12 <4193 c2>' 28 3: 30 12 <.2 <5 <5 <5i;1.76 190 <10 31107 20:<20 20'i 5 1.84 1.30

CDR-9932-1464 13 <.2s163 <2: 25 1`:; 29 15:i:<.2 <5<:: <5 <5::1.79 191 <10 Al 96 20 <20 <20 6 1.73 1.26 CDR-9932-1465 31 <.2243 <2:> 27 21.> 33 24r:<.2 <S;: <5 <5::2.21 202:<10 30:::89 15, <20 <20 6 1.85 1.23 CDR-9932-1466 23 <.2248 <2, 28 .3:: 31 14><.2 <5: <5 <5 !:1.97 194 <10 17;i 99 18'<20 <20; 5 '05.1.23 CDR-9932-1467 42 <4 580 <2. 31 5 : 37 29: <. 2 Y.<5 : <5 <5::!2.79 25L<10 <10 ..27:::104 2.1H20 <20'i 5 1.67. 1.30 CDR-9932-1468 18 <42444 <2;: 32 2: _..... 35 21<.2 <5i; _._.. <5 <5 1.86 212::<10 .28:104 22,:<20 <20: 6 1.76 1.26

CDR-9932-1469 6 <4 42 <2:: 33 3;3i 32 <.2 <5 <5 1.67 209:<10 22 107 21>;:<20 <20: 51.80 1.28 CDR-9932-1470 22 <.2223 <2'i 26 3,;' 31 <5 <5 2.16 181<10 30 96 21:::<20 <20 5 1.57 1-17 CDR-9932-1471 <5 <.2 120 <2:;z 30 . 5:: 30 <5 <5 1.86 204::<10 19 106 19 <20 <20 6 1.78 1.21 CDR-9932-1472 24 < 2 : 89 <2 27 8<: 28 <5 <5 1.62 241.::<10 31 76 12 <20 <20 5 1.49 0.98 CDR-9932-1473 39 <.2:209 <2! 31 3;:: 29 <5 <5' 1.78 243<10 26 78 18 <20 <20 8 1,E6 1.15

(") ITS - Chimitec - Bondar Clegg, 1322-B Harricana, Val-d'Or, P.Quebec, J9P 3X6, (819) 825-0178

Rapport Lab Geochimie Geochemical Lab Report 1[10 Intertek Testing Services

Chimitec Bondar Clegg CLIENT: CAMECO GOLD INC.



AL

PCT.

Ca. Na

PCT PCT

Mg

PCT PCT::

SAMPLE ELEMENT Au30 Ag" Cu Pbai Zn MG 'I Ni Co! Cd Bi As Sb Fe NUMBER UNITS PPB PPM PPM PPM PPM PPM PPM PPM; PPM PPM PPM PPM PCT

Te Ba Cr Y Sn Y La PPM PPM PPM PPM PPM PPM PPM

Mt1 Zr

PPM

Ti PCT

CDR-9932-1474 11 <.2196 <2:. 51 2 54 CDR-9932-1475 20 <.2:171 <2 32 2::' 30 CDR-9932-1476 19 <4:203 <2 31 2 36 CDR-9932-1477 5 <.2. 73 <2.' 31 3 43 CDR-9932-1478 15 <.2.: 90 <2 33 3 37

CDR-9932-1479 15 <.2 55 <2 28 22 CDR-9932-1480 15 <.2I'143 <2 31 20 CDR-9932-1481 32 <.2 108 <2: 31 20 CDR-9932-1482 48 <.2164 <2 29 19 CDR-9932-1483 9 <.2 86 <2: 30 20

CDR-9932-1484 14 <.2 256 <2 29 21 CDR-9932-1485 16 <,2 112 <2 33 2? 22 CDR-9932-1486 17 <.2208 <2 35 2: 18 CDR-9932-1487 18 <4,178 <2 34 2; 23 CDR-9932-1488 12 <.2: 86 <2 36 4` 34

CDR-9932-1489 18 <.2:168 <2;:: 28 6i 36 CDR-9932-1490 <5 <.2179 <2 23 36 CDR-9932-1491 <5 <.2106 <2 28 2i 38 CDR-9932-1492 8 <.2' 79 <2: 28 2 43 CDR-9932-1493 <5 <.2 53 <2 '3 24; 4 35

CDR-9932-1494 <5 <,2 i 98 4:; 47 3 37 CDR-9932-1495 13 <.2407 3 35 10:105 CDR-9932-1496 <5 < 2' 15 <2: 21 5;i 29 CDR-9932-1497 7 < 2; 66 <2 22 37; 30 CDR-9932-1498 11 < 2 29 <2; 26 2>• 32

CDR-9932-1499 <5 <.2 29 <2;;: 22 10;; 25 CDR-9932-1500 8 < 2:' 65 <2;; 34 7;' 33 CDR-9932-1501 10 < 2: 93 <21; 30 6;: 30 CDR-9932-1502 <5 ‹.2 . 42 <2:: 28 18: 31 CDR-9932-1503 9 <2; 68 <2',i 32 13'; 38

61 94 14 <20 <20 9 1.58.0.99 1.67 0.12 0:16;; 83 48. 77 11 <20 <20 9 1.52 1.05 1.70 0.11 0.153 57 44 80 12 <20 <20 10 1.44 1.04 1.21 0.13 0-10 59 45 82 12 <20 <20 10 1.340.95 1.21 0.12 0.11 59 42 73 12 <20 K20 9 1:48 1.03 1.16 0.13 0.11 il 65

<2 17:i: 3 <5;<10 0;1,4:: 6 <2 10 ` <1 <5;<10 0.09:> 10 <2 12 I <1 <5<10 0.04' 5 <2 12>: 1 <5 <10 0.13!s 6 <2 11 1 <5';<10 0.12 6

2:: <2 <1 +É5 ;<10 0.09.;,' 13 2> <2 <1 <5:<10 0.07: 8 2 I <2 <1 6<10 0,07: 8 2 <2 <1 <5;><10 0.07: 8 2 ; <2 <1 <5::<10 0.07: 10

<2 7 <1 <5 <10 0.05'{ 10

<2 7i: <1 <5 <10 Q 09';' 9 <2 6;:: <1 <5`:<10 0,061. 11

<2 6 : <1 -;.<$'/<10 0 08:: 9

<2 8: 1 <5<<10 0 09:: 6

: 3> <2 5; <1 <5:::<10 0,00 5 <2 5;; 1<5:<10 0* 4

3 <2 5>: <1 <5 <10 6,0; 5 2 <2 6::! <1 <5;`<10 0 08; 5 2 <2 5.> <1 . ..<5.c10 0.08!; 5

2: <2 <1 <5'::<10 0,0& 7 4 :; <2 4: <1 <5'>:<10 0:09:: 12 2<: <2 <1 <5<1001f< 4 2 <2 1 :<5.<10 04A, 3 ,2;: <2 6 ; <1 . 5'::.<10 0 U9 : 3

3;;; <2 4'.: <1 <5 <10 0.'3W 5 3;? <2 4 <1 . ô.<10 0.09:; 4 31: <2 8,: <1 <5;<10 0 07 4 4 <2 7: <1 4::<10 0* 6 2::i <2 8.:.: <1 ''.'<.5.:f<10 0.11 i: 6

: 18,';<.2 <5 <5 12:: <.2 <S J <5 15'<<,2 <5; <5 14.''<.2 <5:' <5 12 <.2 <5': <5

<5 3.06 421 <10 3 155 42 <20 <20 6 2.60 2.29 2.11 0.09 0.01. !I 69 <5 1.97 246 <10 22 96 21 <20 <20 6 1:791.26 1,58 0.14 0.08 74 <5 2.55 535 <10 48 88 12 <20 <20 4 1.89 1.40 6.79 0.02 0.25 35 <5 2.24 278 <10 26 111 .,26 <20 <20 8 2.061.60 2.12 0.12 0.09`' 85 <5:;1.83 273: <10 31 101 25.<20 <20 8 .94 1.56 1.68 0.12 0.08`; 89


<5 <5 1.66 <5 <5 1.66 <5 <5:1.58 <5 <5.1.45 <5 <5 1.61

12;<.2 <5 <5 <5:!;1.87 263. <10 52 75 11 <20 <20 8 1;46.0.93 :1.95:i0.13 0.16:: 52 11><,2 <5i: <5 <5:'1.63 258 <10 44 94 15 <20 <20 10 11:53: 1.06 1;116:0-14 0 10!.: 68 12 ;:<. 2<5 !; <5 <5 ' 1. 58 250i <10 34 94 .13. <20 <20 12 0.96 ;1 13 ;0.13 0.49 ; 57 13 ;<.2 <5 <5 <5 ::1.81 244i <10 49 97 14; <20 <20. 11 1..39 1.03 1 341;0.12 0.12'i; 62 11 `;<.2 <5 <5 <5.1.89 308i <10 64; 87 20 <20: <20 9 1.69 1.37 1.4T0.13 0.13 ; 67

15 <.2 <5` <5 <5 1.70 14 <.2 <5 14 <5 1.61 15 <.2 <5 <5 <5 2.13 12 <.2 : r5 : <5 <5 !!2.32 11 <.2 <5 6 <5 2.12

261 <10 64. 77 238 <10 69 92 270 <10 67> 88 256<10 644 90 229;<10 54; 80

19. <20 <20 9 1:41 ?1.15 1.--;';0.12 0,13 60 18:<20 <20 9 1.24 0.92 1.46' ;0.11 0.15::' 50 18 <20 <20 10

11

58.1.25 1,71;0.11 fl 16:; 52 19 <20 <20 10 1.72 1.40 1 71 ;0.10 0.17:: 50 14 <20 <20 11 1,61 1.32 109 4;0.1U 0 12`: 51

19::0.3 <S i <5 .62><.2 <5:i 17 11<.2 <5: <5 13><.2 <5: <5 15 <.2 <5 <5

2.43 213 <10 67 99 17 <20 <20 12 1,60:1.26 1.35 0.11 0.15 48 3.82 177 <10 53 84 16: <20 <20 14 1.4:1 1.03 8.85 :0.11 0.13 > 41 1.21 152 <10 37. 89 16: <20 <20: 1.39 <; 63 1.25 166::<10 35; 80 17:<20 <20: 5 1.43 1.07 1.17'0.13 .13 7 0':; 69 1.36 191 <10 40 81 15 <20 <20 5 1,39;1.11 1534).10 0.13 65

<5. <5. <5: <5

<5:

1ü<.2 <5`;' <5 <5<:1.01 459:<10 .58!; 70 12<.2 <5:f; <5 <5:1.55 197<10 13><.2 <5. <5 <5:;1.51 212 <10 .45' 69

<5:3; <5 <5:<1.56 240::<10 29::118 14:i<2 <5: <5 <5;';1.87 222`<10 39: 94

7 1.10'::0.79 t:644.10 04t 55 7 f;521.27 1 52 0.11 0* 61 6 1 45 1.20 1,$9 : ,16j; 0.09 0 59 5 445).15 1.750.120.12 : 61 4 1491.41 1j 61 9.11 1:413 : 67

4 <ZO <20.

14::<20 <20; 4e<20 <20 16<<20 <20

Sr Y ; Ga JV Nb Sc>; Ta

PPM PPM PPM PPM:PPM PPM:PPM

143<.2 10:<.2 12:<.2 11.1:<,2 11:<.2

<5 <5

<5 <5

<5

232 255 244 226 238

<10 <10 <10 <10 <10




STANDARD

NAME

ELEMENT Au30 Ag Cu Pb> Zn Mo.

UNITS PPE] PPM PPM PPMIPPM PPM'.

2

ANALYTICAL BLANK <5 <,2 <1 <2`j <1

ANALYTICAL BLANK <5 <.2.' <1 <2': <1

ANALYTICAL BLANK <5 - -

Number of Analyses 3 2 2

Mean Value 3 0.1 <1 1 <1

Standard Deviation

Accepted Value

Mn Te Ba Cr V Sn W La All Mg

PPM PPM PPM PPM PPM PPM PPM PPM PCT PCT

<10 <1 <1 <1 <20 <20 <1 <,01 <.01 <.01

<10 <1 <1 .<:1 <20 <20 <1 <.01 <.01 <.01

2 2 2 2> 2

5 <1 <1 <1 10 10 <1 <.01 <.01 <.01

Ni Co. Cd Bi : As Sbl; Fe

PPM PPMsPPM PPM PPM PPM! PCT

__..., _. __...

Nb 'Se Ta i: T! Zr

PPM PPM::PPM PCT;>PPM



Mean Value 177


Accepted Value 186

STD GEOCHEM STD 6

Number of Analyses

Mean Value

Standard Deviation

Accepted Value

<.2'141 16 135

- 1 ? 1 1: 1

- 0;.1.:141 16,1;135

148 , 4:135

7.22 1395 <10

1 1::. 1

7.22 1395 5

7.20 1450:, <1

8; 194 46 <20 <20 3 1.89,;2.64 3.76 0.02 0.05 82 3 4

1 1: 1 1 1 :!: 1;: 1

8 194 46 10 10 3 1;89 2.64 3.76 0.02 Q 05:;; 82 3;:: 4

251 :50 5 12 - 1.80 2.70 4.00 0.01 0.04 70

2;124

- 1

2;:124



Mean Value 412


Accepted Value 465



Mean Value 2758


Accepted Value 2940

Igne Intertek Testing Services Chimitec Bondar Clegg








STANDARD ELEMENT Au30 Ag Cu Pb Zn Mo<: Ni Co; Cd 81 As :SI). Fe NAME UNITS PPB PPM '.PPM PPM I' PPM PPM PPM PPM :PPM PPM': PPM PPM: PCT

CANMET STREAM-SED 4 - <.2;i 62 11'' 79 s: 23 0.3 13 <5. 2.83 Nuîber of Analyses 1 1 1' 1 1 1' 1 Mean Value - 0.1 I' 62 11 79 '< 23 11 0.3 13 3'2.83 Standard Deviation

Accepted Value - 0.3. 66 13` 82 23 0.6 11 4 2.60

Te

PPM PPM

B Cr V Sn i :W La

PPM PPM PPM PPM PPM PPM

>;Al ; Mg Cai Na PCT PCT PCT PCT

K Sr Ys Ga Li': Nb Sci; Ta PCT PPM PPM PPM PPM:::PPM PPM:PPM

1229<10 787> 30 <20 <20 12 .1:12 0.71 :1;20;!0.04 0.09 57 10 <2 5 <10

1! 1 1: 1 1 1 1 ;1 : 1 z 1:: 1 1; 1 1229 5 787 30 4s 10 .10 12 1.12 0.71 1.20 0.04 0.09 57 5 5

1200 - - 30 ;51s'

Tfi<:I Zr

PCT:PPM

006.;; <1

1 0.06< <1







SAMPLE ELEMENT Au30 Ag Cu Pbr: Zn Mo Ni Co::: Cd Bi; As Sbr;' Fe Mn:; Te Ba; Cr V Sn W!;I La

NUMBER UNITS PPB PPM PPM PPM PPM PPM PPM PPM PPM PPM ;PPM PPM PCT PPM:IPPM PPM PPM PPM PPM PPM PPM

Ca

PCT

Na AÇ Sr . Y": Ga Li : Nb i$0. Ta

PCT PCT<:PPM PPM:PPM PPM PPM PPM<:PPM

Tr.

PCT

Zr

PPM

CDR-9932-1446 38 <.2 502 20 2 32 16':<.2 <5 <5 2.12 229 <10 29 74 <20 <20 5 1.70 0.88 3,83 0.15 0.11 80 3 <1 <10 <.01 6 Prep Duplicate 30 <.2 444 <2''' 18 2; 32 17;<.2 <5 . <5 2.12 231 <10 26 60 <20 <20 5 1.59 0.86 3.90 0.13 0.10 73 3 <1 <10 <.01

CDR-9932-1451 34 <.2 608 <2'.: 20 7> 34 <.2 <5 <5 2.03 144 <10 41 86 <20 <20 4 1.49 0.98 1.53 0.12 0.11 66 2 <2 <1 .<5<10 0.07: 9 Duplicate 39 <.2 627 <2`. 21 7 33 <.2 <5 <5 2.02 143 <10 39 87 <20 <20 4 1.45 0.98 1.55 0.11 0.11 65 2 <2 <1 <5,;<10 0.07'; 9

CDR-9932-1468 18 <.2 444 <2 32 35 21 <.2 <5 •<5 1.86 <10 28 104 <20 <20 6 1.76 1.26 1.40 0.14 0.07:': 85 3:; <2 10: 1 <5 <10 0.10 9 Duplicate <.2'421 <2 31 34 <.2 <5 <5 1.81 <10 274 98 <20 <20 6 1.70 1.23 1.39:0.13 0.07% 82 2: <2 10:. 1 <5 <10 0.10:: 9

CDR-9932-1473 39 <.2 209 31 29 <.2 <5 1.78 <10 26"` 78 <20 <20' 8 1:66::1.15 2.00:0.13 0.09:: 68 2::: <2 . 9>; <1 <5:'<10 0.08::: 10 Duplicate 28

CDR-9932-1487 18 <.2>178 34 23 13 <.2 <5 <5 1.81 249! <10 49> 97 14 <20 <20 11 1.39 1.03 1.34 0.12 0,12 62 . 3':: <2 6> <1 :<5..<10 0.08 9 Duplicate <.2 183 34 23 14 <.2 <5 <5: 1.85 257: <10 501' 97 14: <20 <20 11 1.40 1.06 1.36 0.12 0.12 61 3; <2 6;: <1 <$:<10 0.08:: 8

CDR-9932-1494 <5 <.2 98 47 37 19';:0.3 <5 <52.43 <10 99 17 <20 <20 12 1.60 1.26 1.35 0.11 0.15 48 2:: <2 5'> <1 <5€<10 0.08< 7 Duplicate <5

CDR-9932-1496 <5 <.2;; 15 21 5 ; 29 11 :<.2 <5- • <5 <5 1.21 <10 89 16 <20 <20 5 1.39 1.07 1;28;;0.12 0.14 63 2:; <2 5; <1 <5 <10 0.11< 4 Prep Duplicate 6<,2114 21.5: 29 11i:<.2 <5(' . <5 <5i1.19 _ <10 90 16 <20 <20 5 1.361.08 __.... 1:28'0.12 0.14 61 . 2 <2 ' 5 ' <1 <5<10 0.11.', 4

Prep Duplicate 6 <.2 14 21 5: 29 11>%<.2 <5:; <5 <5:1.19 153:<10 37 90 .16 <2O <20. 5 1:36 1.08 1.28 0.12 0:14 61 2;; <2 5::i <1 x5<10 0.11; 4 Duplicate <,2: 14 21 , 5 '' 29 11 <.2 <5.'' <5 <51.21 155 :<10 37 92 .16<20 <20' 5 1.38. 1.09 1.29 0.12 0,14 61 x;l <2 6'; <1 <5.i;<10 0,W 4




REPORT: 099-62644.0 ( COMPLETE )

REFERENCE: 170409

CLIENT: CAME00 GOLD INC. SUBMITTED BY: D. BASIN




NUMBER OF ANALYSES


990923 1 Au30 Gold 50 5 PPB Fire Assay of 30g 30g Fire Assay - AA 990923 2 Ag Silver 50 0.2 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990923 3 Cu Copper 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990923 4 Pb Lead 50 2 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990923 5 Zn Zinc 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990923 6 Mo Molybderxm 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990923 7 Ni Nickel 50 1 PPM HCL:HNO3 (3:1) IM)UC. COUP. PLASMA 990923 8 Co Cobalt 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990923 9 Cd Cadmiun 50 0.2 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990923 10 Bi Bismuth 50 5 PPM HCL:HNO3 (3:1) IMDUC. COUP. PLASMA 990923 11 As Arsenic 50 5 PPM HCL:HNO3 (3:1) 1MDUC. COUP. PLASMA 990923 12 Sb Antimony 50 5 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990923 13 Fe Iron 50 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990923 14 Mn Manganese 50 1 PPM HCL:HNO3 (3:1) IM)UC. COUP. PLASMA 990923 15 Te Tel 50 10 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990923 16 Ba Bariun 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990923 17 Cr Chromium 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990923 18 V Vanadium 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990923 19 Sn Tin 50 20 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990923 20 W Tungsten 50 20 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990923 21 La Lanthanun 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990923 22 Al Aluminum 50 0.01 PCT HCL:HNO3 (3:1) IM)UC. COUP. PLASMA 990923 23 Mg Magnesium 50 0.01 PCT HCL:HNO3 (3:1) 1MDUC. COUP. PLASMA 990923 24 Ca Catcha 50- 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990923 25 Na Sodium 50 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990923 26 K Potassium 50 0.01 PCT HCL:HNO3 (3:1) IMDUC. COUP. PLASMA 990923 27 Sr Strontium 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990923 28 Y Yttriun 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990923 29 Ga Galtiun 50 2 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990923 30 Li Lithium 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990923 31 Nb Niobium 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990923 32 Sc Scandium 50 5 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990923 33 Ta Tantalus 50 10 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990923 34 Ti Titaniun 50 0.01 PCT HCL:HNO3 (3:1) 1MDUC. COUP. PLASMA 990923 35 Zr Zirconiun 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA


DRILL CORE

50 -150 50 CRUSH/SPLIT & PULV. 50 TRANS FROM POLY BAG 50

REPORT COPIES TO: #6-1349, KELLY LAKE RD. INVOICE T0: #6-1349, KELLY LAKE RD.

******sirk **Onk sinle*le ******i v* k************** **Ink r*stir,tir*************,r*****,k**, ****



Eno Intertek Testing Services Chimitec Bondar Clegg


CLIENT: CAMECO GOLD INC. PROJECT: CEDAR RAPIDS REPORT: C99-62644.0 ( COMPLETE )


SAMPLE

NUMBER

ELEMENT Au30 Ag,' Cu Pb': Zn Mo Ni Co Cd B1;1; As $bil Fe : Mn Te IBa UNITS PPB PPM!<PPM PPM iPPM PPM PPM PPM; PPM PPM::; PPM 1411. PCT PPM PPM PPM

Cr V> Sn U :. La PPM PPM;PPM PPM PPM

At; Mg

PCT:;: PCT Na

PCT' PCT

Sr ;' Y Ga ;Li Nb ::i5c Ta :: Tt' : Zr

PPM PPM PPM PPM PPM PPM:PPM PCT::PPM

CDR9933-1305 <5 <.2:!! 20 <2:; 51 1:'; 6 5 <.2 <5 <5 <5 1.05 247 <10 33' 68 5;;<20 <20 14 0.67:0.25 3.52!:0.10 0,09 55 :; 4 <2 : 4 <1 :i<5 :<10 <.01 10 CDR9933-1306 <5 <.2<' 8 <2' 18 1> 7 2 <.2 <5 <5 <5 0.73 ..138':<10 23 229 4;;<20 <20 5 0.42i0.10 2 15'':0.05 0.06 37 i: 1 <2 €:3 <1 :<<5 <10 <.01 4 CDR9933-1307 <5 <.2` 19 <2?' 64 1I 7 5 jl<.2 <5 : <5 <5 1.31 219 <10 31 81 6 <20 <20 i 11 0.77 0.26 3 42.;0.10 0:09 57 :: 3 <2 : 5 <1 ;:<5 <10 <.01 11 CDR9933-1308 <5 <.2! 20 4108 :1?' 14 9 <.2 <5 <5 <5<': 2.88 558 <10 23 56 11 <20 <20 18 1.14 0.80 3.74<'::0.10 0.08 40 <:4 2 .:!:10 <1 ! 5 <10 <.01 8 00R9933-1309 <5 0 3:i 20 2; 63 1`. 7 4 <.2 <5 <5 <5 1.33 344 <10 23:: 100 8 <20 <20 18 0.72:0.31 3.85:0 10 0.08 44 ;4 <2 '<5 <1 „<5 <10 <.01 8

CDR9933-1310 9 0.2 83 3 56 6 3E<.2 <5 <5 <5`` 1.08 :293>!<10 30 140 7';<20 <20;? 15 0.62 0.24 2.70;0.09 0;10 31 :!i3 <2 ;':41 <1 4%<10 <-.01H 7 CDR9933-1311 <5 0.4: 51 6212 5 13 13:<.2 <5 <5 <5 > 8.17 1154:!<10 6 56 .38:<20 <20 7 3.02).37 5.63:0.05 0:03 44 i<3 5<30 <1 21 <10 < 01< 5 CDR9933-1312 <5 <.2 19

.2:< 53 <1 5 4<.2 <5 <5 <5;: 1.20 3<10 31;. 57 6;<20 <20 17 0.6610.38 3.51 0.11 0:09 45 . i3 <2 :.4 <1 <5 <10 < 01:I 7

CDR9933-1313 <5 <.2 17 <2>: 56 11 9'.<.2 <5 <5 <5 1.82 478::<10 36 69 11 <20 <20<: 16 1.330.58 3..31.0.07 0.11 62 3 4 ;115 <1 <5 <10 <.01;' 7 œR9933-1314 5 <.2 16 2:': 39 4 3<.2 <5 <5 <5'! 1.08 .237<10 46 106 . 4;:<20 <20;; 10 0 80:0.26 1-4.0.06 0.14. 51 2 3 : 6! <1 <5 <10 <.01: 10

œR9933-1315 <5 <.2 20 57 7 6. <.2 5 < : <5 <5. 1.49 384 <10 :;:; 28?! 76 9::<20 <20:;: 14 1.01 0.31 2.48:-0.09 0.10:; 51 2 <:: 7 <1 ;<5.:<10 <.01. 16 CDR9933-1316 <5 <::2- 50 92 79 26: !0.2 <5 5 <5:- 5.89 1002 <10 I;25.:' 121 28?<20 Q0:< 7 2.46!:1.21 2.45.0.04 0.11;; 53 3 ;i'28 <1 <5 <10 <.01i: 20 œR9933-1317 <5 <,2ç 53 81 86 29 <.2 <5 f: <5 <5 5.26 1291 <10 22 153 26:<20 <20:< 6 2,42 1.28 3. 29>:0 03 0:11 I; 62 3 29 <1 <5 .<10 <..:01 25 œR9933-1318 <5 <.2:: 21 54 11 <.2 <5: 1.55 301 <10 '> 35:I 87'14 <20 <20:i 12 1.06::0.33 1,80 0.06 Oî11":: 37 3 ;!10 <1 ::.<$<10 0: 12 5

œR9933-1319 <5 <.2.' 23 72 14 12: <.2 <5i: <5 <5: 3.18 . 338.<10 > 42 88 14 <20 <20:(: 13 1 15 :0.35 2.10<0 07 0.>14:1: 40 3 10 <1 ':<5 <10 0 11:: 9

œR9933-1320 <5 <.2: 24 <2. 70 12 .9:<.2 <5I;; <5 <5; 1.95 366 <10 :::37;: 89 14 <20 <20 11 1.24 0.42 1.87!:0.06 0;12',;: 53 3 3';i10 <1 <5X10 0 12; 3 œR9933-1321 <5 <.2: 22 <2, 58 11 8:<.2 <5 <5 <5, 1.44 298 <10 ::43:i: 89 13 <20 <20 14 1.12 0.34 2 02.:0.07 0.14 45 4 3 ::8 <1 <5:<10011;: 4 œR9933-1322 11 <.2 22 <2i 61 10 7;<.2 <51;: <5 <S1 1.60 270 <10 i 41 `: 104 13 <20 Q0 : 16 1.16 0.42 1,79 0.07 0.13 < 34 4 3 <;9 <1 <5<10 0.11':: 6 œR9933-1323 <5 <.2-: 25 4 s: 68 20 19;:<.2 <5<. 9 2.82 157 <10 ;: 44 : 99 12 <20 <20 : 13 0.91 0.20 1 80 ;0 08 0.12 :; 34 4 3 <1 ':<.5..<10 013: 8 1DR9933-1324 <5 <..2 25 <2!: 47 9 7;<.2 . <5.;;: <5 1.07 113 <10 :;i:53;:; 91 11 <20 <20 13 0.7$ 0.16 1,61`;0 08 0,12:I: 34 4 3 :4 <1 .;<5'<10 0.12:': 8

œR9933-1325 <5 <.2:< 23 <2(< 42 . 2 „ 12 11 <.2 <5 7 <5 2.09 ;164;::<10 48'? 81 8::<20 <20 13 0.78 s 0.16 1.72:>0 08 0,13 33 3 2 ; :: 7 <1 :<5.<10 01i2;: 12 œR9933-1326 <5 <.2` 21 <2 129 4 20 17;:0.2 <5 10 <5 4.33 301 <10 65 . 13 <20 <20 : 11 1.35 0.41 1.58 ::0.07 0.13 : 32 4. 2 ::t4 <1 .<10 <10 4011 18 œR9933-1327 5 0,2 26 5 68 2 19 17 <.2 <5 16 <5 4.76 371 <10 : 83 12 <20 <20 12 1.00 f).31 2 .18 0.07 0.12 37 <1 <ri <10 <:.01 .: 12 œR9933-1328 7 <.2ü 23 3 65 2 19 ..18:<.2 <5 9 <5 3.62 :.305:'<10 42. 72 11 <20 <20 15 0.99 0.30 21Q:>0 08 0.12 36 4 3 :; 9; <1 '0.<10 r:.01 :: 12 œR9933-1329 5 <.2 15 3 53 1: 11 8 <.2 <5 <5 <5 1.72 403 <10 44: 89 10 ::<20 <20 ` 14 0.92. 0.29 2,61 0 08 0,13 ' 44 3 7 <1 ':::<5.<10 <.t)1:`: 11

œR9933-1330 <5 <a: 21 <2; 57 2,: 12 9: <.2 5>: <5 <5 2.40 489 <10 62 9 <20 <20 14 1.13 0.43 2,19 0 09 0.09 46 3 :<10 :<5 <10 <:01:: 15 œR9933-1331 40 1,2! 19 44:121 2 33 51> 0.5 .<5:155 <5 >10 00 600 <10 72 11 <20 <20; 5 1 21;;0.33 1.98 0 03 0:03:: 24 <2 12 <11M!'<<1100 <1 <5.<10 <>01' 8

00R9933-1332 8 <4: 31 2 64 2:< 40 14 <.2 <55 :: <5 <5 3-93 .. 620:<<10 90 14 <20 <20 ; 10 149 0.99 2.02 ::0 06 0.12 ; 49 3 21 <1 <5 <10 <:;01:: 16 œR9933-1333 <5 <.2:> 59 3. 90 2: 94 311i: <.2 <5:: 12 <5:i' S 47 1169:<10 _,..... 144 25 <20 <20 7 2.20 1.29 2.83 0.04 0.13: 73 3 ;29 <1 :<5 <10 1;01 :: 26

00R9933-1334 7 .42; 51 101 4 45 21 0.3 <5 35 <5 >10 00 941 <10 107 26 <20 <20 6 3.03;1.36 1,95.:0.03 0.08 : 47 2 32 <t .; c5 <10 <;01;; 32

(÷) ITS - Chimitec - Bondar Clegg, 1322-B Harricana, Val-d'Or, P.Quebec, 19P 3X6, (819) 825-0178

SAMPLE NUMBER

CDR9933-1335 CDR9933-1336 œR9933-1337 CDR9933-1338 CDR9933-1339

œR9933-1340 œR9933-1341 œR9933-1342 œR9933-1343 œR9933-1344

œR9933-1345 œR9933-1346 œR9933-1347 œR9933-1348 œR9933-1349

œR9933-1350 œR9933-1351 œR9933-1352 œR9933-1353 œR9933-1354

<5 <,2 21 3 144 12 0.4 38 11ü105 <5 <.Z 24 <2232 <5 04.21 56 <2114 5 0.2; 53 2105

6 0,4 121 5 0.3 95 5 0.3 61 <5 0.2! 80 <5 0.2: 84

<5 <5 1.44 315::<10 16 <5 6.82 .186 !<10 15 : <5 :! 2.89 490 <10 <5 <5 : 5.28 ..692 ;<10 8 . <5 :' 4.79 918::'<10

<5;'; 9 <5 5.8610.44:;;<10 <5 <5 <5 6.72 1302;><10 <5 : 21 <5 5.68 1194I<<10 <5 5 <5; 7.63 10.11::<10 <5 ' 8 <5;; 6.36 935:;<10

<2; 58 65 47

<2 54 i::

<2 55

6.

ELEMENT Au30 Agl', Cu Pb'. UNITS PPB PPM PPM PPM.

5 <.2 62 <5 <.2: 48 <5 <.2' 42 <5 <.21 35 <5 <.2 35

8 9. 5

5 <5 <5

<5

5

<5 <10 <10 <10 <10 <10

078: 709 490 5511 7226

5.80 >10.00 5.02 2.60 5.36

<5

<5 <5 <5

<5 <5 5.10 1159 <10 <5 <5 4.73 1198 <10 156 <5''>10.00 1094 <10 <5 .<5' 1.86 522 <10 <5 <5 1.75 385 <10

2 95 103 98 111 185

3

20 2

<2,

<5 0.2 54 <5 <.2': 30 35 0.7 14 <5 <.21. 23 <5 <.2 22

90 26 <.2 57 22 0.2 36 38 0.5

2 22 16 <.2 2'i 13 11 <.2

Cd 8i'; As Sb '.

PPM PPM ::PPM PPM::

34 <.2 <5 15 25 <.2 <5 31 27 0.2 <5 28 18'<.2 <5 6 24 <.2 <5 36

Fe PCT

Mn:

PPM Te

PPM

38 56

2 : 73 2: 59 2114

464 176 525 339 580

13 <.2 39`0.3 2310.3 23:.<.2

27 <.2

47 43 51

<.2 <.2 <.2

60<.2

24. 134 22 97 34': 98 36 > 77

31;'; 101

24:> 117

27.. 68

<1 72

311 81

42!:i ' 96

36:: 107 33; 139 16;! 138 17! 185

<1;;

3: <1 i

<1':

<1:

1049 760

1186 959

1224

mijo Intertek Testing Services Chimitec Bondar Clegg


CLIENT: CAMECO GOLD INC. PROJECT: CEDAR RAPIDS REPORT: C99-62644.0 ( COMPLETE ) DATE RECEIVED: 16-SEP-99

DATE PRINTED: 24-SEP-99 PAGE 2 OF 5

30'<20 <29:: 8 2.32<11.40 2,51:: 0.05 0;12; 58 5: 3 30 <1 <5 <10 <.01''. 28 17. <20 20 7 1.85:!0.94 1.82 0.06 0;:10' 58 4 2 19 <1 <5. <10 <.01: 35 14:<20 <20 8 1.46 0.83 1 42:: 0.07 0;12: 51 4 <2 <1 <5 <10 <.011 42 9<20 <20': 10 1.01i:0.80 2.04 0.07 0.13 43 4 <2 8 <1 <5,. <10 K.01' 28 11<20 <20 7 1.18;:0.75 2.58 0.06 0.14! 54 4 <2 12 <1 4 <10 30

27 <20 <20I: 8 2.22: 1.46 3.54 0 06 0.12 56 ':i 4:;i 3 <1 <5 '. <10 <:01 26 9 <20 <20;;; 13 1.02 1.06 3.22:.0 06 0.13 47 ;14> <2 <1 <5. <10 <.01 24 10 <20 Q0; 3 1.06. 0.39 2.84 0.02 0.02 51 :2 <2 11. <1 <5. <10 <.01 8

<20 20.' 11 0.79. 0.58 2.51 0.09 0.11 48 <4:. <2 <1 ''<5. <10 <.01 22 9 <20 <20 12 0.99 0.68 2.14:0 08 0.12 37 :I 3:i 2 <1 ::<5 <10 <,01 17

6; <20 <20 13 0.71 0.16 2 98;i 0.06 0;15,< 62 4 <2 :';; 7 <1 :i<5<10 <.01 19 .9 <20 <20 9 0.96 0.18 1.98 0.06 0.13::46 3 3 <> 9 <1 :::<5 <10 <.01:: 24 25I <20 <20 9 1.38 1.45 3.19i0 06 0.11 55 3 <2 <17. <1 :<5k10 <.01 >: 14 24!'. <20 <20 ; 4 2.36 1.97 4.53;1:0 07 0.09';: 80 3. 2 29.. ..'.<5.<10 <1 6 35 <20 <20 3 2.13:!3.59 5.47 0.02 0.10:;:105 3 2 :25

102.:;:20 20:' 1 3.67:7.42 6.13 < 01 ~:0.1:;1222 5 39 5 :!18<10 <41 1 148;:20 <20 :6.02 5 31;; 0 01 0 ::02::237 4 -341 8 26<10 <1 104;20 40:: 2 3 34 i7.74 6,b8ij < 01 <:01277 3 ;i2t. 4 151 i20 20':: <1 4 42'!7.70 5 02:! < 01 <'.01 i215 5,i33 8::28<10ï01;:.<1 111 `I20 20`: <1 3 39` 8.13 5..91< <•Ot <:01 227 4 .'24 5

PPM I Cr Vï:: Sn .0 PPM PPM PPM

La At:' PPM

Mg Na PCT PCT:;,: PCT

Sr A Ga <ILi PPM PPM PPM PPM

Nb

PPM PPM: Ta

PPM PCT

Zr

PPM





Ga <Li

PPM PPM

Nb >: Sc', Ta '4.C: Zr

PPM PPM::PPM > PGT:;PPM

<1

ANALYTICAL BLANK

ANALYTICAL BLANK

ANALYTICAL BLANK

Nuirber of Analyses

Mean Value

Standard Deviation

<5 <,2I'

<5 <.2:'

<5

3 . 21

3 0.1

<1

<1

2

<1

<2I <1

<2:' <1

- -

2' 2

.1 <1

<1i <1

<1 <1

21: 2

<1> <1

Accepted Value 5 0'


Nutter of Analyses 1

Mean Value 171


Accepted Value 186

CANMET STREAM-SED 4 - <.2 64 11<' 76 25 Number of Analyses - 1.:: 1 1 1

Mean Value - 0.1 64 11;! 76 25

Standard Deviation

Accepted Value - 0,3 66 13 82 23



Mean Value 432


Accepted Value 465



Mean Value 954

Standard Deviation

Accepted Value 968

STANDARD ELEMENT Au30 Ay !_ Cu Pb Zn No Ni .Co Cd Bi As Sbl Fe

NAME UNITS PPB MM. PPM PPM: PPM PPM;:: PPM PPM :PPM PPM PPM PPM PCT

<2 <1 <1

<2 <1 <1

2

<1': <1

<5><10 <-01-i <1

<5:<10 <.01;:: <1

2: 2! 2.:< 2

3 5<01::<1

<1 <.)1 : <.01 <.011: <.01 <:01 <1 ?;<1 <1 !I: <1 <1

<1'<.2 '<5 <5

<1..<-2 <5 <5 -

2'' 2 2:I 2

<10.1 3 3

11;;0.6 ... i 1

<0.01 <1 <10 : <1': <1 <9>i<20 <20;! <1 <.01 <.01 <,01 <.01 <,01;; <1

<0.01 <1 <10 !; <1 ! <1 <1;:<20 00 ` <1 <.01 , <.01 <.01',. <.01 <.01 <1

2 2 2< 2 2 2> 22r 2 2 2 2; 2

<0.01 K1 5 <1 <1 <1 <: 10 10 <1 <.01 i'< 01 <.01i <.01 <:01 1

Mg

PCT

Ga.

PCT.

0.76 1.27 0.05 0.11 72 :;;11 <2 ': g 4 <5 <10 0,08:< <1

1 1 1>1 1:1 1'>1 1:1' 1: 1: 1

0.76 1,27 0.05 0.11 72 ;:11 1;¢ 4 3` 5 0.08 : <1

2.93 1201 <10 1029 29

1 .:; 1 1;;: 1 ü 1

2.93 1201. 5 1029:i: 29 52' 10

10 0.3 <5 12

10>0.3 3;:12




Imo Intertek Testing Services Chimitec Bondar Clegg



REPORT: C99-62644.O ( COMPLETE ) DATE RECEIVED: 16-SEP-99 DATE PRINTED: 24-SEP-99 PAGE 4 OF 5

STANDARD ELEMENT Au30 Ag Cu Pb Zn Mo Ni Co Cd Bi As Sb Fe Mn Te Sa Cr V Sn W La Al Mg Ca Na K Sr Y Ga Li Nb So Ta Ti Zr

NAME UNITS PPG PPM PPM PPM PPM PPM PPM PPM PPM PPM PPM PPM PCT PPM PPM PPM PPM PPM PPM PPM PPM PCT PCT PCT PCT PCT PPM PPM PPM PPM PPM PPM PPM PCT PPM

BCC GEOCHEM STD 5 - 0.7 93 6 73 2 38 18 0.2 <5 7 <5 4.70 707 <10 203 47 131 <20 <20 8 3.37 1.77 1.13 0.06 0.33 42 8 7 25 9 11 <10 0.21 9 Number of Analyses - 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1

Mean Value - 0.7 93 6 73 2 38 18 0.2 3 7 3 4.70 707 5 203 47 131 10 10 8 3.37 1.77 1,13 0.06 0,33 42 8 7 25 9 11 5 0.21 9

Standard Deviation

Accepted Value - 0.7 90 11 80 2 40 18 0.1 1 8 1 4.74 720 <1 200 54 153 4 1 5 3.09 1.83 1.06 0.06 0.32 39 9 - - 1 18 1 - 9







SAMPLE ELEMENT Au30 Agf Cu Pb'I Zn Mo: Ni Co1' Cd Bt( As Sb' Fe Mn: Te

NUMBER UNITS PPB PPM::;PPM PPM ! PPM PPM<PPM PPM PPM PPM: PPM PPM';: PCT PPM PPM

Baa Cr

PAM:- PPM PPM

Sn W

PPM PPM::

La

PPM

AL

PCT:

Mg Ca: Na

PCT PCT:> PCT PCT

Sr :.y Ga Li Nb : Sc:. Ta

PPM PPM. PPM PPM.PPM PPMPPM Ti:

PCt:

Zr

PPM

CDR9933-1309 <5 0,3:' 20 63 1;: 7 4:::<.2 <5;I' <5 <5i!; 1.33 '344<10 100 <20 <20 18 0.72i<0.31 3,85; 0.10 0':08 44 >I::4: <2 <1 >'<5;:<10

Duplicate <5 <.2: 20 65 1:'I 7 4 ><.2 <5 <5 <5 1.36 353:<10 99 <20 <20? 19 0.71 ':0.32 3.92 0.10 0.08 46 ,: 4 <2 5 <1 :<5 <10 <.01:, <; 9

Prep Duplicate <5 <.2 21 70 1 ' 7 4 <.2 <5.; <5 <5 1.37 .564:X10 94 <20 <20 20 0.72 0.33 4.09 0.10 0:08 48 ;; 4 <2 <1 <5.<10 < 0T<< 9

œR9933-1326 <5 <.2 21 <2z:129 4 20 17'0.2 <5':: 10 <5;f 4.33 301 <10 65 <20 <20 11 1.35 0.41 1.58 0.07 0:13 32 ; 4 2 ;14 <1 >i:<5 <10 <.01 18

Duplicate <.2 23 <2::131 4 21 18i'0.3 <5;: 10 <5 4.40 .306!<10 66 <20 <20! 11 1.35 0.42 1.61 0.07 0;13 33 'i 4 2 <14 <1 <5 <10 <.01 18

œR9933-1331 40 1,2 19 44`121 2:4: 33 51 0.5 <5 155 <5(I>10.00 600 <10 72 <20 <20 5 1.21 0.33 1.98 0.03 0.03. 24 2. <2 12 <1 .I:<5 <10 <.01 8

Duplicate 40

œR9933-1345 <5 <.2`I 21 3144 2; 38 13i:<,2 <5; <5 <5 1.44 315 :<10 ;42`,' 96 <20 <20;: 13 0.71 0.16 2.98 0.06 0.15 62 i'4 <2 ,:; 7 <1 >:45 <10 <.01 19

Duplicate <.2 21 4:133 2' 36 13 <.2 <5 <5 <5.: : 1.36 300 <10 •!i 4CY 96 <20 <20I: 13 0.68 :0.15 2 891:0.06 0.14 58 ; 4 <2 ,: 6 <1 <5 .<10 <.01 ; 18

œR9933-1352 5 0.3 61 : <2::': 47 2:525 51 <.2 r5>: 21 <5:(' 5.68 1194 <10 1186 <20 <20:;: 2 3.34 7.74 6.68:<.01 <.01 277 >:4 3 :::21 4 ,!.:;19:<10 <1

Duplicate <5




REPORT: 099-62645.0 ( COMPLETE ) REFERENCE: 170409



SUBMITTED BY: D. SABIN



NUMBER OF ANALYSES

LOWER DETECTION EXTRACTION METHCO

990921 1 Au30 Gold 31 5 PPB Fire Assay of 30g 30g Fire Assay - AA 990921 2 Ag Silver 31 0.2 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 3 Cu Copper 31 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 4 Pb Lead 31 2 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 5 Zn Zinc 31 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 6 Mo Molybdenum 31 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990921 7 Ni Nickel 31 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 8 Co Cobalt 31 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 9 Cd Cadmium 31 0.2 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 10 Bi Bismuth 31 5 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 11 As Arsenic 31 5 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 12 Sb Antimony 31 5 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990921 13 Fe Iron 31 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 14 Mn Manganese 31 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 15 Te Telluriun 31 10 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 16 Ba Barium 31 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 17 Cr Chromium 31 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 18 V Vanadium 31 1 PPM HCL:HNO3 (3:1) IMDUC. COUP. PLASMA

990921 19 Sn Tin 31 20 PPM HCL:HNO3 (3:1) IMDUC. COUP. PLASMA 990921 20 W Tungsten 31 20 PPM HCL:HNO3 (3:1) IM)UC. COUP. PLASMA 990921 21 La Lanthanum 31 1 PPM HCL:HNO3 (3:1) 1MDUC. COUP. PLASMA 990921 22 Al Alumirun 31 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 23 Mg Magnesium 31 0.01 PCT HCL:HNO3 (3:1) 1NDUC. COUP. PLASMA 990921 24 Ca Calcium 31' 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990921 25 Na Sodium 31 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 26 K Potassium 31 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 27 Sr Strontium 31 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 28 Y Yttrium 31 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 29 Ga Gallium 31 2 PPM HCL:HNO3 (3:1) IMDUC. COUP. PLASMA 990921 30 Li Lithium 31 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990921 31 Nb Niobium 31 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 32 Sc Scandium 31 5 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 33 Ta Tantalum 31 10 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 34 Ti Titanium 31 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990921 35 Zr Zirconium 31 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA


DRILL CORE



r****Inir* ***k,kk,k****+r****,k*,k*rt*M,r**1t,Nk*** rk*,r*,r**** k*** k**** *****,k**********


ITS - Chimitec - Bondar Clegg, 1322-B Harricana, Val-d'Or, P.Quebec, ]9P 3X6, (819) 825-0178

IffleIntertek Testing Services Chimitec Bondar Clegg





SAMPLEELEMENT

NUMBER

Au30 Ag; Cu Pbi: Zn Mo; Ni Co:: Cd Bi: As Sb Fe Mn;, Te Ba: Cr . V. Sn u La Al Mg Ca;:: Na K:: Sr Y:: Ga Lt; Nb Sc.!. Ta UNITS PPB PPM PPM PPM PPM PPMPPM PPM:PPM PPM PPM PPM PCT PPM :PPM PPM::: PPM PPM PPM PPM PPM PCT PCT ;:;PCT: PCT PCT PPM PPM PPM PPM :PPM PPM ::PPM

Ti Zr

PCT>PPM

CDR9933-1355 <5 0.31 61 2 51 <1:486 45':<.2 <5; 6 <5 6.52 920j.:<10 2;1228 116 <20 <20 <1 3,42 7.96 6:24 <.01: <:01. 247 2:;' 5 . 23;; 7 19::<10 <.01; <1 CDR9933-1356 <5 0.3 72 <2 51 1 458 46':<.2 <5; 6 <5 6.58 854''::<10 2;1171 116 <20 <20 <1 3.43 7.38 6.12 ;:<,01 <:61 ;°:240 2:' 5 22::: 7 19 ::<10 <.0 1:; <1 CDR9933-1357 32 0.4 333 <2 I 22 6: 39 20 <.2 <5 ': 5 <5'3.58 203:<10 : 28€ 104 .36 <20 <20 8 1:251.71 :1.47:0.09 0.09:: 32 . 3:: 3 9: 2 <5::<10 <.01; 24 CDR9933-1358 <5 0.3 81 2 54 <1 <578 55.<.2 <5; 7 <5:'.6.91 926«10 1:1:1300 117 <20 <20 <1 3.63 8.28 6..11':<.01 <.01.202 . 2:' 6 28> 7 20<10 <.01;> <1 CDR9933-1359 <5 0,3 1 75 <2' 48 1 518 57::<.2 <5; 9 <5`;6.44 878:<10 2 1221 109 <20 <20: <1 3.26 8.21 6 16r<.01 <:01 136 2 4 25:: 6 18'!<10 <.01i:i <1

CDR9933-1360 <5 0.2' 78 <2 46 503 52. <.2 <5 <5 <5'::6.61 841 <10 3 1181 113:<20 <20 <1 3.00 8.55 5.770 1;; 91 4 21?: 7 20. <10 <,01; <1 CDR9933-1361 <5 0.2 238 <2 46 526 99 <.2 <5 <5 <56.97 794 <10 3.1173 111 <20 <20 <1 3.22 8.12 5.55:i<.01 <411 ,0 100 5. 25 ü 7 19. <10 <.01> <1 CDR9933-1362 <5 0.3'101 3 43 471 45. <.2 <5 <5 <5 5.85 847 <10 32 1124 109 <20 <20 <1 3.14 7.47 3 ;: 3 . 23 ' 7 18 <10 <41: <1 CDR9933-1363 <5 0.4> 99 2 44 484 51. <.2 <5 <5 <5 6.58 905 <10 4 1153 114 <20 <20

6,70I'<.01 tl

0

151

1

:x1

17238 6.

6

79:<,01 <Q,

4!: 4 24' 7 20 <10 <.01 <1 CDR9933-1364 <5 <,2:' 55 3 55 156 20 <.2 <5 <5 <5 2.54 391. <10 65 426 33,<20 <20

<19 3

1.3226:>726

2 <2 9;i 2 5. <10 <411!; 9

CDR9933-1365 <5 <.2 22 3 54 <1 < 5 4 <.2 .<5: <5 <5 1.08 212 <10 91'> 99 4.<20 <20 14 0,38.':0.36 :1.62' 0.08 0.21 - 64 .2 <2 <1 <5,<10 ‹.01. 11 CDR9933-1366 <5 <,2- 12 3.: 24 <1 : 5 3:<.2 <5:' <5 <5 1.10 208 <10 102 95 5; <20 ..52.0.. 15 0.43 0.34 1.88>0,08 0.23 : 84 2 < <2 <1 <5::.<10 <.01!>. 12 CDR9933-1367 <5 04.108 2: 51 1 448 47' <, Z <5 xi <5 <5 6.68 825 <10 3>1285 114 <20 <20. <1 3.50 7.90 5:66 <:<,01 0.02;.148 2:: 4 • '2Q: 7 19x<10 <.01,! <1 CDR9933-1368 9 0.018 <2,; 46 1468 45:<.2 <5>: <5 <5. 7.05 837!.:<10 7 1225 124 <20 <20; <1 3.66 8.03 5.76 <.01 0.04;:;149 2;:: 6 .28' 8 21:<10 0 02 : <1 CDR9933-1369 47 <.2i: 11 3i' 12 <1 8 4;<.2 <5 >! <5 <5 1.06 245:<10 83: 92 8:.<20 <20 14 0,42 0.66 1.47 0.08 0.19>: 50 . 2 : <2 21!. <1 r5>:<10 <.011; 11

CDR9933-1370 36 0.2:<203 2 43 1:<338 39 <.2 <5; <5 <5 5.25 666 <10 32 884 106 <20 <20 4 2.71 6.38 5.25 0.02 0.26 169 5 19;: 7 16;1;<10 0,01 7 CDR9933-1371 <5 0,3<112 r2! 46 1 427 37:?<,2 <5: <5 <5;;6.11 758:::<10 72;;1222 115:;<20 <20; <1 3.27 7.82 608:<.01 0.31 152 6 22:< 7 19>:<10 0.:014: <1 CDR9933-1372 26 0,31206 <2 45 2.'441 44::<.2 <5 <5 6.46 784 <10 53 1178 116 <20 <20 <1 3.24 7.79 6.08 <.01 0 27:;111 5 7 19;<10 0 04 <1 CDR9933-1373 5 0.3': 62 <2 53 3>453 42:<,2 c5: <5 <5 6.27 848 <10 29 1322 114 <20 <20 <1 3.45 7.90 5.90 <.01 0.21; 90 4 21 , 7 19x!<10 0 03;i <1 CDR9933-1374 6 0,31 59 49 ,<1>452 39:<.2 <5: <5 <5 6.68 946 <10 147 1227 122 <20 <20 <1 3.41 7.79 6.78 <.01 0.46 165 5 24! 8 20:<10 0 07<: <1

CDR9933-1375 26 0.3 222 <2 51 1 <522 52! <.2 <5;;i <5 <5 7.87 925 >: <10 44 259 119;< <1 3.40 7.14 5 65'<.01 9;38'144 5 7 20<10 0:40, <1 CDR9933-1376 61 <.2;>136 . <2>: 20 <}'! 48 .12:><.2 <5 <5 <5 2.86 336 <10 5 111 4 $!: 3 A6H10 .00e 12 CDR9933-1377 <5 0.2> 82 <2!;i 39 2304 43 <.2 <5 <; <5 <5 6.40 891 ' : <10

1:12179158

65;

841':0.14

1285 <1 6' 7 8 17!:<10 0,13= <1 CDR9933-1378 <5 0.4:: 55 <2:I 38 <5 <5 6.17 903 <10 157 1 <20:

31.'<,011178 <1 3 62 .5 41 5 90;;<.01 0.79:;143 6 9 17;<10 0.14: <1

CDR9933-1379 11 03...103 <2<; 37 4.f:308 40:j<,2 <5'€ <5 <5 6.06 780 <10 . 88 1286 107 <20 <203 <1 3 32 5.12 5;54:<.01 0.12::142 5 31 !' 7 14><10 0.10; <1

CDR9933-1380 <5 0:a: 51 <2`. 37 <3!>27741;:<,2 <5.;;; <5 <5 6.00 783,00 .42:j1216 125 <20 <20:: <1 3.545.39 4-.60 <.01 Q 07434 ..5!;; 7 32i: 8 15:<70 Q,13:: <1 11)R9933-1381 26 <.2;i 76 <2:: 31 <1:274 37<.2 <5;: <5 <51!5.58 862;:<10 24;;1281 11.6<20 <20; <1 3.435.24 477:<.01 0:26.173 6 6 30::: 7 1%.<10 0 14:: <1 CDR9933-1382 <5 0.3;! 57 <a 34 1290 35:<.2 <5;: <5 <5 5.50 934<10 17::1238 117<20 <20: <1 3.48.5.28 40.6 ..01 0 14176 6:< 5 AO.: 7 19<100.13> <1 CDR9933-1383 82 0:2119 <Z 36 <1<322 43. <.2 <5:: <5 <5:5.68 906;<10 i91258 118<20 40 1 3,52:5.43 6 19<.01 0;05:105 5:i' 5 30< 7 20<:<10 0 07: <1 CDR9933-1384 345 <4:321 <2 20 2> 28 17:i:<.2 <5 _ <5 <5;3.38 208><10 2; 95 .45.<20

~'. 8 1 27 1.72 1 35;0.15 0 02 : 18 :..il. 5 9`:: 5 . 7^:<10 <.01' 18


Ga Li;: Nb Sc>: Ta

PPM PPM:PPM PPMPPM

6

8

<10






SAMPLE ELEMENT Au30 Ag, Cu Pb Zn Mo Ni Co:' Cd Bi As Sb Fe Mnf Te Ba< Cr V Sn W La Al Mg li Ca! Na K> Sr Y NUMBER UNITS PPB PPM; PPM PPM' PPM PPMiPPM PPM PPM PPM PPM PPM • PCT PPMiPPM PPM PPM PPM PPM PPM. PPM % PCT PCT !PCT.€ PCT PCT :PPM PPM

CDR9933-1385 10 0.3 146 <23 46 5!450 44';<.2 <5 <5I;6.66 930 <10 10:'1256 1 <20 <20 1 3,547.50 5.90 <.01 0,01<127





ANALYTICAL BLANK

ANALYTICAL BLANK

Number of Analyses

Mean Value

Standard Deviation

<1 <.2 <5>! <5 <5z<.01 2i><10 <1 2

1 1:! 1. 1: 1

0.1 3 3; < 01 2:' 5 <1 ! 2

0.05 1 <1

<.01 <.01f:: <

1 <.01 <.01::;: <1

<.01 c.01:; <1

ELEMENT Au30 Ag; Cu Pb: Zn MO.: Ni Co Cd Bi:> As Sb!' Fe Mi Te Be' Cr V Sn . ;FI La AL> Mg

UNITS PPB PPM PPM PPM PPM PPM PPM PPM PPM PPM PPM PPM: PCT PPM PPM PPM: PPM PPM PPM PPM PPM PCT.' PCT

Sr Y ; Ga Lu . Nb Sc! Ta

PPM PPMPPM PPM ;PPM PPM<:PPM

STANDARD

NAME



Mean Value 416


Accepted Value 465

BCC GEOCHEM STD 5

Number of Analyses

Mean Value

Standard Deviation

Accepted Value

- 0.6_: 87

- 1` 1

-06::87

- 07;;90 1

__.... _, .. 5.23 755 <10 208 46 128

1 1'': 1

5.23 755>: 5 208i:; 46

4.74 720 <1 200;: 54 133 4

<20 <20. 8 3...39-1.86 :1 21;0.06 033.

1 :1 1 1 1 1:! 1 1 10 10 8 3:3g 1.86 1 210.06 0.43

5 4:P9:1-83 1,080.06



Mean Value 983


Accepted Value 968




SAMPLE

NUMBER

ELEMENT Au30 . Ag. i Cu Pb> Zn Md :i Ni Co; Cd Bè: As Sb!: Fe Mn:: Te Ba Cr V Sn ':W. La UNITS PPB PPM;:PPM RPM .PPM PPM; PPM PPM PPM PPM;;PPM PPM;: PCT PPM I: PPM PPM PPM PPM PPM PPM PPM

AL.'. Mg

PCT PCT Cal: Na

PCT : PCT

CDR9933-1360 <5 0.2 78 <2 46 <1;503 52'!:<.2 <5;! <5 <5i!6.61 841 <10 3::1181 113 <20 <20 <1 3.00 8.55 5.77 <.01 Duplicate <5 0.3 74 <2' 44 <1 486 49::<.2 <5' <5 <5 6.23 798 <10 2:1154 109 <20 <20 <1 2.87 8.14 5.61 <.01

CDR9933-1377 <5 0 2 82 <2>' 39 2'304 43'<.2 <5; <5 <5 6.40 891 <10 65!;1285 130 <20 <20 <1 3.83 5.86 5.31 <.01 Duplicate <.2: 75 <2 37 2 290 41 <.2 <5;! <5 <5 5.98 844 <10 62 1214 122 <20 <20 <1 3.59 5.51 5.08<<.01

CDR9933-1382 <5 0.3II!; 57 <2: 341:290 __. 35,<.2 <5''< <5 <5. 5.50 934:<10 17.1238 11:7 <20 <20 <1 3.48:5.28 606(:<.01 Duplicate <5

K'i Sr Y::; Ga AL Nb Sc: Ta Ti Zr

PCT ;PPM PPM:PPM PPM-RPM PPM PPM PCT:PPM

4.01:: 91 4 21:i 7 20 <10 <.0:1! <1 <.01:: 88 4 20; 7 18 <10 <.C1': <1

0.31132 7 31'; 8 17 <10 0.13 <1

0.29;;125 5 29> 8 16 <10 0,12':: <1

0-14 i! 176 5 7 19"<10 0.13' <











DATE RECEIVED: 24-SEP-99 DATE PRINTED: 5-OCT-99

47 1

47

47 -150 47 CRUSH/SPLIT & PULV. PULVERIZATION TRANS FROM POLY BAG

DRILL CORE

DATE APPROVED

NUMBER OF ELEMENT ANALYSES


990930 1 Au30 Gold 47 5 PPB Fire Assay of 30g 30g Fire Assay - M 990930 2 Au rej Gold assay on rejet 1 0.03 G/T FIRE ASSAY FIRE ASSAY 990930 3 Ag Silver 47 0.2 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990930 4 Cu Copper 47 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990930 5 Pb Lead 47 2 PPM HCL:HNO3 (3:1) 1MDUC. COUP. PLASMA 990930 6 Zn Zinc 47 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990930 7 Mo Molybderxm 47 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990930 8 Ni Nickel 47 1 PPM HCL:HNO3 (3:1) 1MDUC. COUP. PLASMA 990930 9 Co Cobalt 47 1 PPM HCL:HNO3 (3:1) IIDUC. COUP. PLASMA 990930 10 Cd Cadmiun 47 0.2 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990930 11 Bi Bismuth 47 5 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990930 12 As Arsenic 47 5 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990930 13 Sb Antimony 47 5 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990930 14 Fe Iron 47 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990930 15 Mn Manganese 47 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990930 16 Te Tellurium 47 10 PPM HCL:HNO3 (3:1) IMDUC. COUP. PLASMA 990930 17 Ba Barium 47 1 PPM HCL:HNO3 (3:1) IMDUC. COUP. PLASMA 990930 18 Cr Chromium 47 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990930 19 V Vanadiun 47 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990930 20 Sn Tin 47 20 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990930 21 W Tungsten 47 20 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990930 22 La Lanthanun 47 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990930 23 Al Alunirxm 47 0.01 PCT HCL:HNO3 (3:1) INDUIC. COUP. PLASMA 990930 24 Mg Magnesium 47' 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990930 25 Ca Calciun 47 0.01 PCT HCL:HNO3 (3:1) IMDUC. COUP. PLASMA 990930 26 Na Sodiun 47 0.01 PCT HCL:HNO3 (3:1) IMDUC. COUP. PLASMA 990930 27 K Potassium 47 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990930 28 Sr Strontium 47 1 PPM HCL:HNO3 (3:1) IMDUC. COUP. PLASMA 990930 29 Y Yttriun 47 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASM 990930 30 Ga Gallium 47 2 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990930 31 Li Lithiun 47 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990930 32 Nb Niobiun 47 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990930 33 Sc Scandium 47 5 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990930 34 Ta Tantalum 47 10 PPM HCL:HNO3 (3:1) IM)UC. COUP. PLASMA 990930 35 Ti Titaniun 47 0.01 PCT HCL:HNO3 (3:1) IMDUC. COUP. PLASMA 990930 36 Zr Zirconium 47 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA



***** art**** ,r**** t,Heir******** k,t**,lair** air****************** **** n ****** r*,t*,t**** t


**************************r***t********************* *********************** ***







PROJECT: CEDAR RAPIDS DATE RECEIVED: 24-SEP-99 DATE PRINTED: 5-OCT-99 PAGE 1 OF 4

SAMPLE MAIMBER

.............. ... ........... ELEMENT Au30 Au rej Ag

UNITS PPB Pb ;;Zn Mo ;:.1W Co ;:ad Bi AS:: Sb

PPM PPM PPM PPM;PPM PPM::PPM PPMPPM Té;: Ba 3r ; V 5[t ; N

Ca PCT < PPM PPM: PPM PPM::PPM PPM;PPM PPM: PCT PCT: . PCT

K: Sr: PGT; PCT PPM:PPM PPM;PPM PP1I;PPM PPM: PCT F

CDR 9934-1504 24 CDR 9934-1505 8 CDR 9934-1506 150 CDR 9934-1507 106 CUR 9934-1508 58

<.2 160' : 2 <.2 ::43 : <2 <.2 261 3 <.2 . 192:1 <2 0.2 427; <2

39 4,2.; <5 :i <5;

21. <1 ;;!57 22

29 2 10b' 64 � 2 <5 31 2 '::69 24 :<.4 <5 :;:<5;

31 3:::63 18 4 2; <5 ;.<5;

<5 4•54. ; 369 <10 : 9 166 : 43 <20 <20 4 2.08 1.44:: 2.07 0.06 <0.03 <5 2.72 ; 236 <10 :; 5 119 : 36 <20 ;<20 5 1.55 1.03 1 36 O .:0$;0.02 <5 5..00'.: 324 <10 38 144.; 39 <20 <20 5 2.18 1.42 1 88 0.05 0.14 <5 3.95 368 <10 ; 12 160s:. 45 <20 <20 5 2.16 11.69 2.11 0.07 0.04 <5 3.51 369 j10 : 2 167 39 <20 <20 ¢:2.00 1 63 2 31 0:06;<.01

62 ; 3 ; Q;: 6 58; 4 4 82!! 4 51 . 3 : <'L:i 6 44: 3

<5 <10:0-18 <5 <10:0-19 <5 <1i1;0.20 <5 <10 0.18 <5 <10 0.1

CDR 9934-1509 23 CDR 9934-1510 17 CDR 9934-1511 9 CDR 9934-1512 <5 CDR 9934-1513 22

102 <2 24 2 ;52 15 < 2 < 5 i <5 <5 322 ;: 3 171::< 30

B4 <2 ;29 2 :64 16 ~ 2 <5 <5 3.19:: 407 41 <zO; <20 ; 39 <2

<10;

30 <1 '<65 15 4 2 <5 :: ~ ; <5 3 32:(I 459 S10 : 7 202 ; 47 ~20 :<20 >18 <2 <:2! 2 :65 17 ~ 2 <5 <5 : <5 458 <10; 13 176; 177 2 20 1 51 16 c

4::'!<5 ,':<5 ; <5 2 67.> 329 <10:: 2 174::

5 1.87 1,50 1. 95 0.117;: <.01 4 2.12 1,88 2 40 0.06 <.01 6;;2.16 2,01 2.58 0.05;:0.03 8 1.95 1.73 2.01 0'06i0.06 11 1.45 1,33 2.22 007; <.01

<5 410;0.18 <5 <10 0.18

3 <5 <10'0.17 <5 <10 0.17 2 <5 <10;0.15

85':

:55 50 44. 99

CDR 9934-1514 90 CDR 9934-1515 28 CDR 9934-1516 11 CDR 9934-1517 7 CDR 9934-1518 248


<.2 :::97'9 2 :34.< <1 X.2 :100 <2 .:19.: 8 <2 62 . <2 15. 5 x.2 A07 <2 '>91' 9 6 1995 3 '4067

20 < 2 <5 ::<5:: <5 3 91<: 456 <10>: 3 277<: 63 <20 21 X.* <5 4$i . <5 2 47 .: 280 <10 :: 27 152 ; 34 <20 11 4 2 ' <5 j $•. ; <5 Me 219 <1Q :: 26 123>; 31 <20 12 <5 <5 i.23 ;: 156 <10:.: 26 107 ; 27 X2018 z 2, <5 ';.<5 <5 373 <1{l ; 24 rl 34 f.0:6

<20 16 2.34 2.$9 3.03 0;05 0.01 ; 47 3 <20 4:;1.69 1.61 2 67 O06>0 09 :;52: 3 <20 4 1.40 1.15 ;2 06 047 0.09 ; 63; <20 3 1.12 0.82 1 50 D=07 0.09 ; 56 : 3 <20 3 1.50 1 65 4.82 0,g5;0 07 63 3 <2

<5 +ç10':0.15 <5 {10 :0.14 <5 410 ;0.16 <5 <10;0-1 <5 <.14:0-1

<5 <100.2 <5 <10;0.19

<5 <10:0.16 <5 <i0::0.14 `

<5 <10;0.15

< 2 6413 <2 ::24 3 ::58 17 < 2 <5 '::<5:; <5 2 69,;; 354 <10[ 4.161 40 <2D;<ZD 6;:2.02 1 94.:1 82 0;'blr;:0.01 < 2 230 <2 24 4 52 16 ~ 2 <5 ;.<5 : <5 2 i3;; 388 <10 < 2 144.; 42 <20 :40 04 i„.81.2.41 0, ~17<.01 < 2 1~0 <2 25 7 55 15 ~ 2 <5

<5 <5 2~: 402 3 l71 45 <20 :<20 10:2.04 2.263.17

< 2 â41 <2 22 18 :54 17 ~ 2 <5 <5 <5 2 4d; 319 <10. 5 132; 37 ~0 ;<20 1T:1.7o 1,84;2 72 0;.0b;0.02 < 2 314 2 24 8 58 16 ~ 2 <5 :<5 <5 2.63. 370 <10;; 9 34 <20:<20 11.2.00 2,1:1'2 59 0.06<0.03

<5 <5

CDR 9934-1524 12 COR 9934-1525 38 CDR 9934-1526 21 CDR 9934-1527 6334 COR 9934-1528 148

2 ;19' 4 ;53; 13 <4 <5 3 28 2 44:d 24 '<.2 <5

04:. <2 46 1 4.0 29 4:2 <5 62 1 8 3188 3 ..26 3 129. 84 <:2 <5

X.2 242 <2 49 4 ,:53 43 <:2.: <5

<5 2 17: 312 c1#1:; 5 149.; 33 <5 3..* ;: 302 <10.. 10 154.; 41

<5 3 59 224 410 14 1230 34 <20.1<20 <5 3.89:; 167 ~6 22 118:; 24 <20: ,:<20 <5 341 146 <10 19 . 98,; 25 .Q0

1.76 1,73 2.24 0;08:0 02

2.50 2,59.;1 67 0:05 0.09 ;:59::'

2.40 2.145 0 90 0.05 0.10 .71; .94 1,57 1 00 0:a40 12 69 .09 :1,90.;0 71 0-05 0.11 ::;72:;

CDR 9934-1529 CDR 9934-1530 CDR 9934-1531 CDR 9934-1532 CUR 9934-1533

156 < 2 ;:383 ; 2 19 2 ;;52 74 4.2 : <5

1309 0.8 2112 3 20. 9 148 221 z:2 <5

29 <.2 149 3 16 2':25. 33<:2'<5

228 <.2 36 3 17 2 :27 11 <.;2 <5

35 <.2 31 3 17 <1 21 15 <.2.: <5

7 :

:<55

5 3 61 :: 130 <1i1; 17 113 :: 26

I:2200

c.00 30 5 21> : 162 19 . 7 1.39 <5 . 2.49: 150 <1 Q :' 28 105 11 11 :1.44 <5 <5 2 40 ; 203 <141. 22 106 : 15 <LO .QO 8;;1 .54

147 31 43; 14 <20 ;<20 11 1.68

1,90:0.92 0.45 0.11 :49: 2 1.26 3 08 0.04 0.16 > 50 : 3 1.13 LW 0;04 0-25 :39 2 <2 1.12 2 71 0.04 0.16 ;:77 2 <2 1,13 1 37 0.06 0.16 ;;87; 3

<5 410:.0.14 <5 <10:;0-10 8;;

5 ;;<1 <5 +s10':0-06 5 ;; <1 <5 <10 :0.07 5 : <1', 6 410:;0.08


Rapport Lab Geochimie Geochemical Lab Report Iwo Intertek Testing Services

Chimitec Bondar Clegg CLIENT: CAMECO GOLD INC. REPORT: C99-62784.0 ( COMPLETE )


28

:31 <5;> <5 494:':: <5 : <5

1 49 13<.2.:<5 2 .:70 29 <:2.: <5

368 <10 351 <10.;'

Y ; Got Li Nb Sc ;: Tit Ti .c Zr.' PPM PPM PPM PPM PPM PPM PCT PPM

4 : d <10 i:0.1 4' t5 410:;0.15 8.: 3> <5 ;t10:;0.19 3: <5 :<1Q;:0.19 3 <5 s10. 0.1

2` <5 <10::0.16 2 <5 <10;0.13 1 <5 <10 0.14


< 2 113 2 46. 2:88 34 <,:2 <.2 34 3 :36 <1 128. 18 <.2 4.2 .414 Q ;.26 3.,:71 66 c 2

3 25 <1 107 20 <.2 0.2 52 2 20 1 37 . 17<2

.4 6506 ;i 3

0.7 1459 3

<.2 19 <2 <.2 11: <2

<2

<5 <5;; <5 $011 504 <10 _; <5 ô <5 2.37:< 365 <1(T> <5 :$ <5 2.90:: 74 <10; <5 ::<5 <5 1.87:: 274 <10`i <5 292

<5 :4=1; ; 267 ~10:;

<5 3 14::; 256 <10;: <5 2-79;; 363 <10<: <5 2.69s 332 . <5 ~ 77;; 368 <10

11 147 39 <20 <20 5;:2. 2.71:>0 99 0.05 0.05 94 2 ;: <2;; 9 15 158<: 48 a40::<20 . 5 2.86 2.80.;1.03 0.05 0.18 12 16 105 31 <20 <20 5 1.85 1,79;2 79 0,06<0.10 64 3 :;42: 10 9 120> 40 <20 <20 6 1.75 1.85 3.05 0.07 0.05 b2 4 ;:<2:! 10 8 124 :: 43 <20: i:Q0 14 ::1.27 1,58 :4 08 0.06 0.05 63: 3 : Q:: 8

3 94 `: 43 <20:.<20 .15 ;0.90 1.10:;6 05 008..0.04 123 3 :; ~2 ` 5 20 109:; 49 Q0;>QO 4:1.54 1.84.;2 93

0.07 ::53 4

6 106>: 48 <20Q0 10::2.02 2.293 31 0:.06.0 02 .;7,! 3 ;:~; 11 <10: `: 2.79 0:06 .0.03 >55 4 .: ~': 71

2 16U: 46 <20:<20 3<2.02 W<.01 2:28'2.62 ; 0:06 '61 3;<2;: 10

14 1!~3 34 <20 <20 2;:2.51 2 88.2 79 O';t13 0.04 i:92 3:<2> 12 74 185 26 <20 <20 35 1.67 1.87 2 42 0.05 0 27 :;85 3 <2 8 18 15ô 26 <20 ;<20 4 1.61 1.53 1 19 044 0.05 129 2 <2 . 7 74 150 27 <20 <20 29 1.31 1.52 2 96 0.09 0.23 156 3 6 33 $8 22 <20 <20 4:::1.63 1,50;2 62 002 0.20 :36 2 ;~:; 8

11 112 33 <20 ;<20 2.02 2.09 2.59 0.04 0.07 ,::54 ` 3 ~.: 8 > 5 149 41 <20<20 2.21 2.48::2.32 0.05 0.04 .<.54:: 2 9 ':

2 <5 <10 0.14 1; <5 o0: 0.10

2: <5 <10;0.15 3.; <5 <10 0.15

Mg Ca PCT;: PCT

Na:: K PC)~: PCT PPMF

CDR 9934-1534 8 CDR 9934-1535 10 CDR 9934-1536 <5 GDR 9934-1537 38 CDR 9934-1538 369


COR 9934-1544 38 CDR 9934-1545 <5 CDR 9934-1546 82 CDR 9934-1547 <5 CDR 9934-1548 <5

CDR 9934-1549 8 CDR 9934-1550 49

<2 45i 3 .2 52;: 3

<•

2 ~; <2

<.2 3; <2 09 2036 3

27' 16 17: 24:

<1 <1 2 1 98

79. 79

48- 48 T1

36 4,2 <5 <':<5:: <5 5.01'::; 225 <10i 39 <.2 <5 ::<5'. <5 5.32: 234 <10: 12 {,2 : <5 ::<5 ,; <5 2 â3>: 258 <.10: 12 <.2 <5 ;:.<5 : <5 2.17: 299 63 S.2 <5 <5 411,- 251 <10

45 ;102.:100 <•2:: 7 :.51 41 <-2: 2 :44 15 ~ 2;

:21 2 .:52 14 .<.2 22 3 :59 15 14

~9 23 21

2 <5 <10#0.17 '. 3 <5 <10,0.18 2 <5 <10 0.1 3 <5 <10;0.18 3.

<5 <10 0.1

<5 <5 <5 <5 <5

<5: <5.

<5: <5.

SAMPLE NUMBER

ELEMENT Au30 Au t•el AgCt1 Pb iZn Mo N# Co !Cd Bi :As Sb Fe Mn 4 UNITS PPB G,(:1' PPM 4.44 414 PPM PPM PPM

Ba Cr.; V W 1.8' At PPM PPM PPM PPM PPM PCT PPM PPM PPM PPM;PPM PPM PPPM PPM PCT

Imo Intertek Testing Services Chimitec Bondar Clegg



REPORT: C99-62784.0 ( COMPLETE ) DATE RECEIVED: 24-SEP-99


DATE PRINTED: 5-OCT-99 PAGE 3 OF 4

ELEMENT Au30 ,..-i tlre1-:--'i As Cu Pb -.-.:;- P1) Mo .:.:::::N1:-. Co ',:.,.::Cd-: B1 ::.......04.::: s ,...„..,.. ,,,......:„. STANDARD •••••- -,::::•,.:<-, ::::.,:--:•,.ff!..: . ::.':::

b ?Si-i Mn '-.4*.: 8a Cr v .:.:: Mi:.: W ..::--*,1::F..

.... ....„,........ „,.....„...i-,:i,.,

Al :::-,..141' Ca ..::.;' '....:.:..-t;*:-. : K .:.::*:::::::::-. Y %6-i.!-i,. Li '.'' ':'ITi:'" -I

2 :,ili, Sc ,-.4c .1 ff.gx....,, NNE UNITS PPB :i...,rii2i,pm ::gPP14 i'00PPm 0(FPM .IPPM !r1rPIN :q6A:

i

PPM PCT

PPM

PPM PPM

°11 :::PPM !.....!1)PM 1...." PCn: !Ill'

PCT

lill<i).:: !"111:11 11:r13:41

-::-:,M,::::•.-:::..1 ',.- M-:'.]i]:.,. '-:::::.T-.0 :::::::::::::::',:,.. .:0:::?,::::::: :.---,,':,].,.:: :::::.,':,U.:.:-.:,, ...:::!',:::::::',','. ::i.::.: <1 :40'::::.<20 1.,.:-:-51'::::::<.-. 'Z,..7‹..:':......-'::: 1 :•:,4., <1 '....‹.r. <5 ..,---* :::::::::..

...:.','..!:•::.. PiT <1 ig <5 ..q.:<5 <5 ;0.J. <1 '1:!:::.: < 1 1..,:i 1 ',...,/i <20 ,...6.01 61:.::::,:<.01

:..,...177;.7...1.-'1.. PPM‹5 :..,:,.. PPM.:1in, , I ,‹ PCT.noil :::,,...,4: PPMi):111

ANALYTICAL BLANK <5 :,--:.:MR4:<.2 .0.i.C1 <2 q.'....:g'. <1 ........a 7.,••••••:.• <5 :..:ir <5 01 <1 5101 <1 .',."...li <1 <20 aV.1 2 '',..M......:i. 2 .?..:P:::,.. 2 :4.: 2 ::.:...:.:::

:< 01 .::;4-:::::::

ANALYTICAL BLANK <5 ..i.g!NI-2 ::J'.2:40.1 <2 :1.:' 1...i <1 -4.-..!' : 1,:.;;.:.:i.i 2 1:•!.P, 2 ggiiM 2 '..i:','.:'::'.:'.•.2 2 . g 2 " 2 IS pi .01<.01 I.

,.ill<'°1 ll" <1 iti

<1

.:.-11 3 III *

•..::,;.,::: 1 •:::.??..4.-:::-. 2 <,•::: - --',..•::::...-:•:]

.....,. <1 ?•::::.w, <1 Atr.: 10 ,:.::.--.<-

1'Pt... <.°1 .:'. 1.! < :: ii 2 '" 2 q.--i.i];•i 2 BC

NuTter of AnaLyses 2 Kg:-....., ,: : 2 ::,::,,4 , ..',•:',,,-:.:;,] 3 i-.,::::3. 3 '.,<Oli <1 ',:..'5: .:::::::.- '....'-.:.:-,,::::::: ':::::??::.:.„::::i:. ':::::.e:&: - ';'.:-.::::::::::::::::: - :,..:::....-7.: :•:-:.-..:::i: ::::-ga =•:.--:. '-.::::::::::.,.::,

•,:,•:::::.-..., , ::.:-. ..,,i, 1 ::4.1:• <1 .::.-.,<I'. <1 !4*1:::] ::;:•:•:.:.:..,, :.».,::::::.::-. ::::::::::::: _ ',,,.::-:•:,..:::: - '-,:•:'..'.. -:i...:::: - ;:...a.,.7.....::: - ],..,-..,?....Tw a...., -.,,.,.,...,..,,,:: .., -:,?.=::: 'a,:::,.:::, ::::,,.....,....?..0 :-..,::::::,,:gi ... ,.ma:

Mean Value

- :::::-.-:,,., - -.--.,,...,:-..-.::: ,g,...?..,.-.,.-:-.-<,-.:: :::-.,-.,:.::.• :,::.:•,:...i,-.n ,,..-:.,:.:::-..,:.,. :::::.:.:?.?::::,... ::::::,::::::.-.%:::::: :-.....,:-.....g.::: .:.:.,,,,:., ..:,..,.-......,.,: -.4..., 1 ,,,..0,< 01 ..,..,..-1,

3 -...::::::::::::::,:::.p.. ..,,,,:, ,..,,..:,,,,.......„...:„ ......,..•,.:..,".•:::::::. :,..,..,, . ....,......i....: : - :::.•.-.•,... -.:::......... h,.... ,.,:...,.....:-. ::,..•.:...,,,, ,-.:,.,,.......,:...; :,....:::::::::, ..-.::,...::.. ,.... :.z.,,,,, ::::..,...,,,:: ...,: .,:...;0:. Accepted Value

Standard Deviation

5 <0.01 0.2 Eil 2 Mi 1 g" 1 1.:.:;o.: 2 ::6$,,, 5 Y'..Y':- . • : • ::-

...... -. -,....--

........ ... _ .._ 1011‹.01 III <1 illl <1 1.71.1...

<1

IIII . Mil

IgE: ill . 1 .11 <1 .111 1 Ell <1 l''....41•01

::::::::::-....• :.,,,,,,, ,,,..,..: .,,...„,. :•.--, .. .....- %_•.....- ::,:..........: :::::••••H:

.......... .:,...._. . ::: .:::,:::::::: .;•,...:;•.:..:,........ •••••••:::•::::::,•:: •••::::•-::::::. .. •

1.01<.01

.. .

•.:..:.: i .-..:,-,::-,.,i-.

- •••

•••.••, ..-„,:• .:.:.•:,•:

- ---• .........

_....... .

.•••••• ....

••••••••

....... .• - .. ...

....... ........

Oxide (Feldspar &

Mean Value


186 U0A1(

184

Nurber of Analyses

gg-4

184 .:.'.::.-••.--J'•., :-:

1 ::!MMa':',

...,..............::::.•

...............

...............

............... •-•-•••••---- ...........-.............. ------•-••••

..............

- :.-.?.*:::: - ,--..::::','•,--. - ",---..-,.:::!!:::::::::. - :

. .:.,:,,,,,,,,,,,::, - : -..:::•7!: - '..,-.'..,:.:',7:: '.i:';':,:::,:,,,-.

- - • ' . ,....,,,,::.

- - :',....'.J.4.%.: ,....1..n TEM. '•::'''A' :q:;'•.: . ....aja - ::.r..:..e:i;:: :::::!.:::::.: - n!..7.:.... ' ''''''''';:'''

_ ..... . .,,.....,.....•.. . .... _ ..,,,. . ... . ....,...„„ _ . . ..,...... . . . ........ . . . . . ......7 _ ... .

. ...,...,...,........:...,...,... - .:,..:„.,...i..,..,:.:i.....,...i, . ...:...,..,...,..i.. . .....,....,,.., - ...,,,,,,, - :.:•:•:,..,... - .....:•:,•:,•:.:, . y.....,,,..:•: - .......;••••• .... -..".••..•.•• - -- • " - -

.:.:.,.,,.:...,. .,.......,. 7..:.: ... .. , , . ...,.......,.; . .,,,,,,,,:,,,:;:: - :,:•:::::::.:7:::,.. :':'•,,',,,,• -..":•••''''.: .'

•:'.':.M.,•-::

..:...,,....:,,,.:

............ .• • • - • - •

...........

................

.......... ....

.......... - • • • •

.••••••• ....- ....-.•:,-.• • ••••••• • -

......,..„. . „„,..:,::::: - •••'•:.;••••• - ----- - ....-7. - ....- -- - ......T....' ......:' : Accepted Value

....

•••• •- ........ ....

•••• ••- •-•-•-- ••••-• ----• --•

............„ ..........:.... .....:•:••.:......

::::.:.::::...............,. -......."..

' .. . ...... """-,:. ••.•.

......... .........

:: .•• I.::: : :

......... .........

.••••••••:.:•:•:. „:„....:.:.:.:. ----- "•:.--

....... ..„

............. . .

. ... .... • ... .. .. ... .••• . ...„ ..

......... •-•-•- ........ ........

. . „„,.. 't,-..•: .:.1. : - al!ii 7 E:f5 --------------

- .07 - °1'.

".". ---••••••• - - •••

........ ...... ........ ... . ........

..:::.:.:.:.': ........ ......."....'•...::

. •-• •• .. ........ .. ..

•••••••••

.::.,.....:.:„...,...:.: ---

-""•-•

...

y..,......„... ............

.."-"•• ........ ...........

.......... •••• ,..:,::::: ::::::....: •••-••• • - -, •:...:::::,..,.:::::. ,,,,, ---• , „......, v „.„.......„ •• •••

-- •• .. ..„ .. ........ .. .. ••.•••••

....... ........ ....

..... ........ ....... •••-•-•

............„. ••- .... ,!........:.„... ........ ....„.. .. . . .. .... ...... ••••••••• -•

.......... •••••••••••

,:„.„,„.:,„:„.•::, •••-•-- •.„,•:::::, .....,...... ........ . ....... .......... .... .. •• .. ••••••• . . ........

........ .. .

". •-• ••"""

--•••• ---" ................

.............. _ ....-- - „---......, ,...,...-..:: ,,,.,,,-. ..,,,,, ,.-..,..,....., -„....„„. ...,,„ ..„......... .„.....„ ,_,,. „„......

Mean Value

Nurrber of Analyses

CAPIIET STREAM -SED 4

- •":::::*:-.0.1 ',,.', 63.: 13 -.:!lv 1 ',23.:r'.. 10 04--.?::

46 <20

.:,....:,,,::•,, 1 --..•!::::.1::::•: 1 2Y 1 .1 ., 1 MI.::',•-• 1 Mt: 1 .:•'-',:MI: 1 •?!1.: 1 :':::-1 1 '14 1 ili::::, ':,-,',g,:i::..„,„i,

6640 10 :,., 4i.::. 10 Oi...

.. • • •• . .... . •••••..: • •.......„:•:. .• ••••• ...• .: •:: 14 018:,:i 24 664.--0.10 ....:.6...1..........,:. 10 --.,.r,;::.: ii.:::.:-..:-,-:.......

3 ::..13.:.,, 3 48,4 ,1159 -i,. ]...: -,...-.,923.. .-..i!:.... 46 8 :::-:4 3 a4.-:',.0.07 ::„W

Accepted Value

Standard Deviation

- -6.- '-Ut.-i.9.3 g'..0003 ;j0C 2 4;$... 11 ();:4 - ',11.. 4 Z401200 :,..::: - :.:.1W 51 :-..•':::i

- ]•':::::a.:] - i:-.:::::e:•- - :::':'-'''-''' ' '-'- - ' '' - '' -

10,...:: 10: ',,..1;...:.;.,.., r..14. ',i7::,,,,,:.24.. ....::::i. ....;:..:,.... • :::.

:.:.......:;:,::::......,:

::-..:,„•:::::::::::: .....••• - -

... .

Nurber of Analyses

436 ]::::::::-,•:,---,-------

.1 : ,.:-..,--,,-.:7,.,,-•-• - ...-.•:.......

•: . ..'..'?::',' '::::::':'''• - .-:::'.'i.-. - ..-..- -:'.:4'.:',

i.,.:.. 1,; _ ..,..,,.,::.-,::.:,,. : ....,:,,...::::„.. - K..,%i - ::i,•:n:. ,..::••• - ,:.-:•:;.''.-:: - ..:',•:::',...:-...: - !:..'.'"...:•••••:.-:.'.:•'•:.' - -.•:••••-.....: ..:::.::::: - •„„„„•,-,,,,,, : ::::,

•-•- •••••-• „........... Oxide (Feldspar & 436 •:'-.U.:.:i.:- - .:,-.::::::,..:.- .„.....„ .

._........ - ,..:....,..,- ::::.i...:.... - .....' .. -

.. ..

Mean Value

....:i„ ---------. Standard Deviation _ :::,......,.i..:;.:4 - •::,, :i,-.:,..„-....„... ::„............. : !,..:.....i.7-,..-.:.....: - ,..!..7...?.::::

...

465 ::i..:.iP.;?7!..• - , E.:',.,!'::.. ,.:. - .!•:::,...'.,..:7-. - !..,.. ,i!, - !!-:::::.:'• 4'.:.. :, .. :,:,,... :::.:„,......... ..,.,,:.....,... .......:..... ::.......:::: - .:: - .::!:".i-..:. - .--.:-..:,.,7::::7:-...7. - i!,.........,...!.::- .... ::-. ..-,:..'::::,::,.:,1,:.-7,:...:,' - :::::.1i...,]:•...11:.. ,,,,.::: ----- ••,.....- ---,-. .•-•••• .•.-.........• ........ .•••.... .-....-.......,•, ••••-.•:•:•,,,, .....•••...•.••• ........•.•..... .•.--.... .......• :::::':: ".•••:••••:::: :""::: -•-•-•••:-:-:-:.."-'-',---•::.- :•:7--,,i':. .'-:-'--•

Accepted Value '-..i.:

':•::-..--:

.':::!':i',.. :-•ii :','-':•:!... - :•:',..-.'•:.......;... ''"::::::.-:, :::::,:::::',,,,,. ,,,,::::,„: _ ,,,,...., •-•:,,,!...,,,.

- 4A.4 90 8 ,.- 6.0 -: <1 '14• 18 ',k2-:::; <5 -...,::':.:',13:: <5 45.0... 662 .,00180.::50115'?..;20,..?,..e.20 NI.:.3.02 14701.10 0450.30 .:. .. 7<2 21 10....... <iÔ, 0.20

ITS ITS - Chimitec - Bondar Clegg, 1322-B Harricana, Val-d'Or, P.Quebec, 19P 3X6, (819) 825-0178

BCC GEOCHEM STD 5

Nurber of Analyses - .:g!] ,i-:Z 1 ,'.4i.i 1 ::f 1 iPii! 1 !!IRC; 1 .4. 1 R4 1 g1.:1! 1 .M1-.. 11 1 FV 1 01:: 1 o::.v 1 ','..-:it 1 Rt 1 iA. 1 m 1 :4:, Mean Value - -': -. -::.:'....,..0.490. 8 '..69': <1 .-:',$4:. 18 0.1?::: 3 '':',41. 3 4.5.9:: 662 ':A .: - 180 .?:!P.115 : 1.0.:'!.:i 10 :'•:1•:.':3..02 Tal$ 1.10 (t......050.30 . 4.0. 7 i:']':G 21 :,:10 9 :,'N'.:0.20 i'..-10 Standard Deviation - l.':::::7 - .Z.::•'7 - '1:7• -.: - ''.::.'::'-':'.': - :.:: - '!':'.':'•"'' ' !':!::!'"'''.: • :::Y"--' - !'."'!-':':': - '-''''!• - ''.:: - .',71.::'''' - ::::•::'""'! - '"' - '.:j.:!:''''''• - :::::::::". - '•••:•:••:*•:' - ••:-: •:. Accepted Value - 0.7 '- ',. 90. 11 80(:::: 2 :4.0:, 18 0.1 1 --,',:l3'.::. 1 4;74. 720 <1200 :.;54,:,.133 MC 1 -:0$'1.09 1.83 1.0 0460.32 ':'.:.P:]: 9 :.::a;'..., - g-4::: 18 i:i-:]'..4:::: - .:'..: 9::,.;

,„„ „„: „,„ „„,„ „„„,: :,.,,,m,::: ,.:-,..,...„-:,, ,,•,:-„, „:,:,:,,,i, ::: u,,.,

jki!° Ag Pb Zn Mo Bi _:- ,i.:.! co Cd. As Ba Cr

PPM.FFkopN rom:ppm PPM +/* w La.: Al Mg Ca r ELEMENT Au30

PPB UNITS

............„ •..............

.............. .............. ............... „ ............

.......... ............ .............. .• ....... .............. . ........

....... ........... ........ ............... .............. ............... ....... ............. ..............

186 -

............... ........ ......... .......... ........

184

1

184

, . <5 <0 <1 <10 <5 <.OU <1 <10 2 2 2 2

- 0.1 <1 1 <1 <1 <1 <1 0.1 3 3 3 <.01 <1 5

5 <0.0.1 0.2 2 1 .1 1.0 2 8 50.05 1 <1

<1 <-2 • < -

<1 <2 2 <1 <2 <1 <1

* <5 <5 <5 <5 2 3

-• • _. •

_ - - -

<5 4.59::::]. 662 <10oso .g.02 1111 1 1 1 R:U; 1 1

,1

3 4.59 662 a5.1130 .50.115 10 10 M71.02 17B 1.10

4.14 720 <1 200 54 133 4 1 53.09 1.83 1.08

•

10 <2

1 1

10 1

0.05 0.30 40. 1 1

0.05 0.30 40

21 10 9 <10 0.20 I

1 1 1 1 1 •1

21 10 9 50.20 •10

9 - - 1 18 1 -1 9

04.04:].0.10 61

1 11

0.04 0.10 61

8 5 <5 <10 0.07 <1

8 15= ; 1 0.07 <1

moo Intertek Testing Services Chimitec Bondar Clegg




DATE RECEIVED: 24-SEP-99


Na K Sr YGa Li lib Sc Ta Ti Zr

PCT• PCT PPM PPM PPM PPM PPM PPM PPM PCT PPM

4,01 <.01 <1 <1 <2 <1 <I <5<10 <-01 <1 <,01 <.01 <1 <1 <2 <1 <1 <5 <10 <.01 41

2 2 2 2 2 2 2 2 2 2 2 ‹.01 <.01 <1 <1 1 <1 <1 3 S. <.01 <1

436 1

436

465 Aiat't,

STANDARD

NAME

ANALYTICAL BLANK

ANALYTICAL BLANK

Number of Analyses

Mean Value

Standard Deviation

Accepted Value

Oxide (Feldspar &

Number of Analyses

Mean Value

Standard Deviation

Accepted Value

CANMET STREAM-SED 4 Number of Analyses Mean Value

Standard Deviation Accepted Value

oxide (Feldspar &

Number of Analyses

Mean Value

Standard Deviation

Accepted Value

BCC GEOCHEM STD 5 Number of Analyses Mean Value Standard Deviation

Accepted Value

- -

<1 18

<5

1 13 8

14., 18 0.1 0.; 1 a

69 8

18

1 ‹./.1

40 ; 00, 11 2 80

- #4.1! 13 .:J77 1 23 10 0;5.4 <5 13

W* 1 1 1 1 1 1 13 77 1 23 10 0.4 3 13

- - -

- 44.3 66. 1382 2 4V 11 4;e6 - 11

<1 <1 <1 46213 <1 <1 <1 . 20<20 2 2 2 222 2 HZ: 2

<1 <1 <1 10 10 . 6.01 . .

<5 041159 <10923 30 46 00.<20 1

1 EJA 1 1 1 Riv 1 a1i 1 3 2...84 1159 V4.92330 46 10 10 .j

4 2.601200 iHR - 51 -

2 1.14 0.78 1.24

1 1 1 2 1.14 OA 1.24


REFERENCE: 170413




DRILL CORE 44 -150 44 CRUSH/SPLIT & PULV. 44 TRANS FROM POLY BAG 44 PULVERIZATION 1


r***** *************** t* r**at* ***** ****** **** ********* t*** ta**** e*****


********************************************************************************






DATE NUMBER OF APPROVED ELEMENT ANALYSES


990930 1 Au30 Gold 44 5 PPB Fire Assay of 30g 30g Fire Assay - M 990930 2 Au rej Gold assay on rejet 1 0.03 G/T FIRE ASSAY FIRE ASSAY 990930 3 Ag Silver 44 0.2 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990930 4 Cu Copper 44 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990930 5 Pb Lead 44 2 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990930 6 Zn Zinc 44 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990930 7 Mo Molybderun 44 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990930 8 Ni Nickel 44 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990930 9 Co Cobalt 44 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990930 10 Cd Cadmium 44 0.2 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990930 11 Bi Bismuth 44 5 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990930 12 As Arsenic 44 5 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990930 13 Sb Antinany 44 5 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990930 14 Fe Iron 44 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990930 15 Mn Manganese 44 1 PPM HCL:HNO3 (3:1) IMDUC. COUP. PLASMA 990930 16 Te Tellurium 44 10 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990930 17 Ba Barium 44 1 PPM HCL:HNO3 (3:1) INDUC. COIF. PLASMA 990930 18 Cr Chromium 44 1 PPM HCL:HNO3 (3:1) IMDUC. COUP. PLASMA

990930 19 V Vanadium 44 1 PPM HCL:HNO3 (3:1) IMDUC. COUP. PLASMA 990930 20 Sn Tin 44 20 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990930 21 W Tungsten 44 20 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990930 22 La Lanthanum 44 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990930 23 Al A lumi rum 44 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990930 24 Mg Magnesium 44' 0.01 PCT HCL:HNO3 (3:1) IMDUC. COUP. PLASMA

990930 25 Ca Calcium 44 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA. 990930 26 Na Sodium 44 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990930 27 K Potassium 44 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990930 28 Sr Strontium 44 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990930 29 Y Yttrium 44 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990930 30 Ga Gallium 44 2 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

990930 31 Li Lithium 44 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990930 32 Nb Niobium 44 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990930 33 Sc Scandium 44 5 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990930 34 Ta Tantalus 44 10 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990930 35 Ti Titanium 44 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 990930 36 Zr Zirconium 44 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA


ELEMENT Au30 AU rej: Ag .lx UNITS PPB 0/t: PPM PPI PPM PPM PPM PPM. PPM PPM. PPM PPM

fe: PCI

Pb 7ii Mo . Ni! Co Cad Bi As Sb PPM

<.2 2.12 <2 87.

<.2 19 <.2 .42 <.2 : ;7

2 ,43:. 2 <2 .33 2 <2:29 2 <2 30. 5 <2 26 1

W.162 <; 2 <5 <5 71 .360 <.2 <5 6 50:141 <.2 <5 . <5 46:116 <:2 <5 153.: 21 <.2. <5 <5

36 2 1:1:1 30 <::2: <5 .<5 <5 3:78:i:! 35 1 105 19 <:2 <5 <5 <5 284-

26: 2 80 17 r.2 <5 <5. <5 39. 2 ..53. 43 <:2 <5 <5 <5 4:28::

29 1 .64.210 <.2 <5 <S <5 6:53:

488 <10.:: 23 440 <10: i 28 364 <10>; 48 480 <10: 61 500 <10 :: 31

68.:108 <.2 <5 <5 <5 6';09:: 552 <10<: 12 63 252 <.2 d :<5. <5 6:77i 502 <10:!: 55 57 82 <:2 <5 s5 <5 5:05:: 287 <10.:i 32 52 61 <:2 <5 <$ <5 ?4 `44;; 270 <10 :: 34 55 54 4.2 <5 x5 <5 4.53::: 295 <10' 27

<.2 <2 <.2 <2 <.2

Q <.2 <2 <.2 <2

2 30. 1 3Q. <1 33 2

35. 2

58 63 <:2 <5 36 18 <:2 <5 50. 35 c:2. <5 68 16 K.2 <5 62 28 4: i,<5

<5 <5 4.30 : 271 ;<10 :1 30 <5 <5 2:10-- 241 <10 : 40 <5 <5 34.1 : 319 :<10 ; 29 <5 <5 4.16: 511 ..<10 : 29 <5 <5 4.50i 464 <10'? 30

63 19 <:2 <5 ':<5 <5 4:.49 :: 531 <10 : 28 74 17 <.2. <5 <5 <5 4.04;:: 565 :<10:: 18 95 20 <.2 . <5 ,<5 <5 4.74 ; 696 <10 . 35 74 24 r,Z <5 .:<5 <5 4:45 644 <' ;ie 50 Ai 26 K..2 <5 .s5 <5 4.:73 < 605 <10 i: 55

<.2 <.2 <.2 <.2 <.2

<2 <.2 <.2 <.2 <2

<2 33 2 <2 19. 1 <2 26. 2 Q 34 1 <2 .â3 1

4 <2 .3-7 <1 2. Q .42 1 43. <2 44 1 53: <2 .43 <1 21' Q .41i 2

<.2 ;2!D' <2 .:46 <1 :84 44 <:2 <5 <5 ..

<.2 35: <2 45 1 74 59 <:2. <5 <5.

< 2 91.: <2 45; 2 67 31 <:2 â <5 <.2 100' <2 61: <1 116 61 <.2 <5 <5 x.2 207 <2 51: 1 109 24 4. <5 45

<5 6:.20<: 640 <t(1::.. 72 <5 547 <10 : 48 _..

<5 4;8ri ; 490 <10- 34 <5 6:57 < 655 51 <5 6<46 713 <10:' 66

<.2 <2 <.2 <.2 <.2

24 <2 2 <2 19. <2 9 <2 5 <2



CLIENT: CAMECO GOLD INC. PROJECT: CEDAR RAPIDS REPORT: 099-62785.0 ( COMPLETE )



, ca PCT

Mn Ts' Ba Cr V Sn PPM PPM.PPM PPM:': PPM PPM

W La'; Al PPM PPM s PCT

K Sr Y Ga Li Nb: Sc Ta: Ti PCT PPM PPM PPM PPM PPM PPM PPM:: PCT PPM

SAMPLE NUMBER

CDR 9934-1551 COR 9934-1552 CDR 9934-1553 CDR 9934-1554 CDR 9934-1555

<5 6.00! 406 <10. 12 <5 4:.90 283 <10<; 28 <5 44,8<' 257 <10: i 28 <5 445 348 <10 29 <5 3;1.2:!; 316 <10 21

157 58 <20: <20 19 :3 .16 3,014 <:1 88 0.07 :0.07 : .89: . 3 <2 14 :'4 <5 <10 0.14 108 28 40'. <20 72.24 1.91::1.60 0.08:0 20 51 2 <2. 9 €:1 <5 x10::0.13 97 26 52.0.' <20 5:;2.02 1.65 1 89 0.09 0.19 53. 2 <2 9 '1 <5 <10':i0.11 99 36 <20: <20 4 2.36 1.95'<:i2.55 0.09 0.15 76. 3 <2 11 <:2 <5 <10::0.14 10 40 <20: <20 9 2.15 2.09 2.55 0.10 0.08 100 3 <2 12 :;3 <5 <10:!0.14 15

304:: 50 <20::<20 13`2.76 3.103.09 0..060.09 103 4 I<2:; 21 3 <5 <10 0.15 ::13; 2791.: : 43 <20:<20 .16 i2.40 2 67>'2.14 0:0.0.12 . 91 4 <2 18 3 <5 <10 0.15 :16; 239 45 <20<20 15;:1.71 1.713;2 35 (69f.-0 28 85 4 <2i 12 3 <5 <10 0.16 <i 19 92;: 64 <20,:<20 3;2.56 2 29<;1.55 0 10 0 43 i!.100:42: 131 4 <2 14 5 <5 <10 0.22

110 :' 58 <20'::<20 4 :2.05 .1.87.3.73 , 09: 0 28 ..99 5 :<2:. 13 4 <5 <10 0.14 •

106': 63 <20::<20 3:::2.T1 2«52 4.04 0;09 0.09 ::94 5 >3 18 4 <5 <10 0.12 109;: 56 Q0::<20 62.14 1.90 6.53 0.05: 0.66 176 5 . <2 14 3 6 <10 0.13 78 47 s20:<20 6 1.83 .1.70 3.44 0 09:0 40 108 5 <~ 12 3 <5 <10 0.12

: 92'; 28 <20::<20 6:;1.70 1.63::2.90 0. D7 0 25 : ë3 . 4 x2 11 1 <5 <10 0.10 : 95 : 26 <20;:<20 5 1.69 1.703.3_0 0,06'0.20 51. 5 i2. 12 1. <5 <10 0.11

_.. . 108:: 25 <20:<20 1.89 1 $(1 ;2.82 0. 06: 0.24 46 4 <2: 13 <5 <10 0.11 ' 72:: 17 <20<20 3:1.33 1.05 3.78 0 06 0 29 54 3 <2> 7 <5 <10 0 12 '. 97 '; 29 <20.<20 4 :1.65 1.51.;3.61 0 ~; 0 21 5.,1 3 <2 < 10 <5 <10 0.14 .: :126' 39 40`.:<20 32.59 2.35 3.58 0.06: 0.22 67. 3 :<2.:: 15 <5 <10 0.13 111 40 <20:<20 5 2.40 x.ü$.3 .35 0.07 0.25 d3 2 <2:: 13 <5 <100 15

132 41 <20 ;<20 5;2.77 442 0;070.21 '$;2 3 15 <5 s:#0:0.16 .174;s. 53 40:<20 4 2.82 2.66.:3.75 _... .:..... 0.07.: 0 13 .94 4<2`>. 16 <5 <10 0.17: _. ... 211 < 72 <20><20 3:3.18 2.88 ;3.86 0.07 0.44 105. 3 <2 19 <5 <10 0.17 ><i. 170 77 <20<20 4.3.09 2.94 3.34 0.08 0 66 :85. 3 <2 19 5 <I0::0.20 161J: 82 <20<20 5 3.19 2.94 3.34 0,06 0.72 91 4 <2 20 6 <!0 0.21 ;;<1;:

154". 67 3:;3.62 3.072.53 845 0. ." <2 22 :::4: <5 <10 0.21 119;> 57 <2p.><20 __._. 4.:3.11 2.69:2.50 0.06'::0 59 67 3 <2 19 :4 <5 <10<0.20 128 : 47 x20 ,;<20 2:2.89 2,43`2.52 0.07'0 35 77 2 42 16 3 <5 <10 0.18 216 : 63 <20~20;` 4:3.69 3.25:2.69 (0,0 60 76 2 <2 24 4 <5 t1(#';0.16 203': 73 <20<20 2:3.57 4;81":3.07 0 05: 1 00 :$3 3 <2 22 5 <5 610`:0.21

CDR 9934-1556 CDR 9934-1557 CDR 9934-1558 CDR 9934-1559 CDR 9934-1560

CDR 9934-1561 CDR 9934-1562 (DR 9934-1563 CDR 9934-1564 CDR 9934-1565


174 281 55 195 70

85 <5 <5 10 95

42 74 61 44 35

16 30 51 176

6588

CUR 9934-1571 16 (DR 9934-1572 <5 (DR 9934-1573 <5 CDR 9934-1574 38 CDR 9934-1575 <5

CDR 9934-1576

<5 CDR 9934-1577

27 CDR 9934-1578

17 CDR 9934-1579

33 CDR 9934-1580

16


Rapport Lab Geochimie Geochemical Lab Report Mige Intertek Testing Services

Chimitec Bondar Clegg CLIENT: CAMEO GOLD INC. REPORT: C99-62785.0 ( COMPLETE )


SAMPLE NUMBER

Ca PCT PCT

Ti :;73"'. PCT PPM

K Sr Y G6 Li Nb Sc 40 PCT PCT PPM PPM PPM PPM PPM PPM PPM

ELEMENT Au30 Au rej` Ag Cli Pb Zn Mo N,i Co . Gti Bi As Sb::fa: Mn':Te; Ba Et' V S`n: W La UNITS PPB G/T PPM PPM:PPM PPM PPM PPM PPM PPM PPM PPM. PPM PCT;: PPM PPM PPM PPM;PPM PPM'PPN PPM:

48: <1 112 27 <;Z <5 .<5 <5 6:.62: 686 <10 ; 57 :157:: 71 <20 .<20 2; 3.39 2 ai ..2.91 0:450.89 3 20 :5; <5 +t10;0.21 55; 2<5 <10: 32 60 6.35: 700 151 .*?0<20 23.18 2 57:2.78 0 Oâ' 0.41 80 2 <2 18 ;:4.. <5 <10:0.18 7A 1 72. 21 <.2 ~ .a <5 4 .;98 : 637 <10s: 17 123' 48 ;20.<20 ; 3 ;2.94 x 7,4 ;3.05 0. 07.: 0.11 81.1 4 16 ::3 <5 si010.16

1 .60. 26 ~.Z <5 <5 d 4:1T< 414 a10 : 26 i111; 37 ~.<ZO 3;.:2.61 2.052.59 0 07:;0.16 73 3 <Z 13 .:'2 <5 <100.15 50: 1 6d 25 < x <5 <5 <5 4:64 424 <10 27 ; 90 ; 36 00::.<20 5;2.75 2 ü9::2.69 0 .06':0 17 77 3 <2 14 <5 <10,0.13

_... 3~ 1 14 26 2 <5 :<S <5 2';88 264 :<10'` 35 ::::.W 12 <20;i<20 8 1.57 0.92 1.47 006:;:0.20 2 <2 ' 6 <:1 <5 <10 0.07 45: 1 15. 24 <.Z <5 <5 <5 3.i1T: 305 <10' 40 ::::6:::: 12 ::<20;:<20 8 1.81 1.02 1.45 0 08.:;0.21 2 <2 7 <1 <5 K:10 0.08 47: 1 ,26i 17 <~2 <5 <5 <5 3:36 . 329 <10 34 i 81:: 18 <20;<20 8 2.17 1.31 1.88 0.08 0.17 3 <2 10 <1 <5 +J0 0.08 . <> 47 2 .24. 19 %.2. <5 45 . <5 3.:30 : 322 4Cr 31 >.78;: 18 ~0':i<20 8 2.14 1.36 1.67 0.08 0.14 3 <2 11 <1 <5 x10 0.08 50.; 2 .13: 9 <..2 <5 <5 : 14 <20 <5 2;07: 427s10:: 51 7'4 <.W%200'> 7 1.96 1.14 1.77 0.11 0.11 2 4 12 <1 <5 <10 <.01

. 0» 1 14 9 <5 : <5

21 0: 378 <10 > 14 40. <20 $ 2.06 1.19'' 0.10;;0.11 96> 2 5: 12 <t <5 <10`< 01

41:: 4 14 13 <2 <5 <5 <5 ?"7°-: .70 420 <10': 61 >: 78:; 14 ;±~0:{<20 6E';1.93 1 26 ;2.01 0 A0::0.13 2 4 12 <:1 <5 <i0 < 01

.55 2 65: 21 <.2 <5 45 <5 447'704 <10 38 117 45 :*<20 3 3.20 2 45;3.59 0 06`:0 O8 67: 2 7 24 ;:2; <5 <1,0. < 01

.53: 2 58: 24 <;2 ô <5 <5 4-:54 676 ::<10 40 126; 40 :<20':QO 2:3.17 2 38'3.17 0.06:0.08 53: 2 6 22 : 2 <5 00.< 01

ITS - Chimitec - Bondar Clegg, 1322-B Harricana, Val-d'Or, P.Quebec,19P 3X6, (819) 825-0178


78 <-2 231;: <2 32 <.2 118:; <2 12 < 2 66:: <2 <5 18 < 2 94`. Q

CDR 9934-1591 CDR 9934-1592 CDR 9934-1593 CDR 9934-1594

<5 <5 <5 <5

<,2 <.2 <.2 (.2

<2 <2

<2 <2

CDR 9934-1586 CDR 9934-1587 CDR 9934-1588 COR 9934-1589 CDR 9934-1590

59 . <.2 93 <-2 121 <2 <5 <.2 19 <2 9 <.2 46I: <2 <5 <.2 .7 <2





DATE RECEIVED: 24-SEP-99 DATE PRINTED: 1-OCT-99 PAGE 3 OF 4

Accepted Value 5 0.2

00! 0 7 W.::: 1.1

STANDARD ELEMENT Au30 Au Mel Ag Cu Pb Zn Mo Ni Co Cd Bi As Sb Fe Mn Te Ba Cr; V Sn W #.a;; Al NAME UNITS PPB 0/T PPM PPM: PPM PPM PPM PPM PPM PPM PPM PPM PPM PCT; PPM PPM: PPM PPM PPM PPM'PPM PPM PCT

Ca NA K Sr Y Ga Li Nb Sc Tit Ti . Zr PCT PCT: PCT PPMI PPM PPM PPM PPS PPM PPM PCT PM<

ANALYTICAL BLANK <5 <.2 <1 <2 1! <1 <1 <1 <2: <5

ANALYTICAL BLANK <5 <.2 <1:. <2 <1 <1 <1 <1 <.2 <5 Number of Analyses 2 2 2 2 2 2 2 2 2: 2 Mean Value 3 -. <0.1 <1 1 <1' <1 <1: <1 01 3

Standard Deviation - - <1, -

_. _ . __. <1 <20.<20 <1;<.01 <41 <.01 e 01:< 01 <1 < <1 s1 <5 x10<.01

<1 <20 ':<20 <1 ;<.01 ‹pi ;<.01 < 01;: < 01 r1 <1 <Z <1 r1 <5 <10 <.01 2. 2'!; 2 2' 2 2:: 2 2> 2 2 2 2! 2: 2

<1 10 : 10 <1 >'<.01 < 01 > <.01 <01 % <.01 t1 . <1 ..1 . <1 <1 3 ;'i5;:<.01

<5 <:01;: <1 <10:;: <1

<5 <.01 ! <1 <10.:i: <1

2 2 i 2: 2':!: 2

3 <:01 ! <1 : 5:: <1


Nudfer of Analyses 1

Mean Value 462

Standard Deviation

Accepted Value 465

BCC GEOCHEM STD 5

Nunter of Analyses

Mean Value

Standard Deviation

Accepted Value

0.4 91< 8 73 1

1 1 1 1 1

.04 91; 8 73; 1

Oxide (feldspar E. 965 Nuiber of Analyses 1

Mean Value 965

Standard Deviation - Accepted Value 968

CANMET LAKE-SED 2

Nuiber of Analyses

Mean Value

Standard Deviation

Accepted Value

0 3 36>: 37 195: 1

1 1:',i 1

0.3 36:' 37 195;; 1

0.8 :36< 40 200: 2

24; 17 049!:

17 0.9<: 3

1708::

<5 387 1947 :00 229 ; 28 44 :~ <:<20 1 1 1: 7 _ 1: 1;,: 1

<5 C91: 728 10 208 .; 48122 <20 $;3.41 1 73;::1.18 040).35 4a: 8

3 4".1, 728 ;; 5;:208

3.87 1947 .! 5 229 ;28 ; 44 > 10:; 10

720 ; 4!].200 :: 54 :133 ' 4 ;' 1 53.091.831.08 0.060.32

1 :.:1:: 1 ..:.7I 1

10 8 3.41 173 .18 040; 0.35 46' 8 1=

1.83 0.72 0.72 0 04"0 26 32. 29 <,2 17 ;~ 5 <1:tï;0.08 1 1>: 1 1 1 1 1 1 1 1 1 1;!; 1

17 : $ 5 5 0.08 1.83 0,72 0.72 0.04;0 26 32 29


:24 <2 36 2 111 30 c2: <5 <5 3:;781 488 <1:0 23 304 50 <20:<20 2.76 3.10!:3 09 0;06 0.09 103 4 <<2;: 21 <5 10 0.15 23 <2 36 2 114 31 <2 <5 <5 31:77:: 4% <16 23 317; 49 <20 <20 2.82 3.13 3.10 0.45 0.08 101. 4<Z;: 21 <5 <10 ;0.15 .;

<2 <2 42 1 74 17 <5 <5 <5 444:;:; 565 <10'> 18 174:: 53 <20.':<20 ... 4 2.82 2 6ft;3 75 0;07'0 13 ;:94 4 16 <5 x10':'0.17 .2 <2 42 2 74 17 <5 <5 <5 4:04;; 559 <10::: 19 17Q'.; 51 <20<20 M42.87 M73.61 0.07 0 13 :11 3 16 <5 <10';0.17

4$ <2 !6 45 20 <2 <5 <5 <5 4.74 6% <1. 0.1. 35 211 : 72 <20 <20 3.18 2 3.86 0,07 0.44 105 34; 19 <5 0Q:0.17 : 44 <2 46.. 97. 21 <2 <5 <5 <5 4J0'' 702 <10; 35 214'> 72 <20;;<20 3.19 2.90 3.84 0.06 0.43 103 3 <2 19 <5 <10::0.17

<2 2 31 K:.2;:; <5 <5 4. 85 490 <10 '. 34 128 : 47 <20L<20 2.89 2.43<2.52 0.07 0.35 :77 2 <2<: 16 <5<10'::0.18 :

<2 41` 4 14 . 13 <:2 <5 <5 2.70 420 ‹..1qH 61 14 1.93 1.26 :2 01 0.10 0.13 :!5Q 2 ;; 4 12 <5 <10:<.01 2 40: 3 14 13 <:2 <5 <5 2:60. 405 <10 56 74 13 Q1) ::<20 1.83 1.22::1.94 0.09 0.12 ;.46 2 ::4: 12 <5 <10i:<.01 .:

CDR 9934-1556 85 <.2 Duplicate 97 <.2

CDR 9934-1572 <5 <.2 Prep Duplicate 6 < 2

CDR 9934-1573

<.2 Duplicate <.2

CDR 9934-1578 17 .2 Duplicate 18

CDR 9934-1592 <5 <.2 Duplicate <.2





DATE RECEIVED: 24-SEP-99 DATE PRINTED: l-OCT-99 PAGE 4 OF 4

SAMPLE ELEMENT Au30 Au raj Ag :i4.4. Pb . 1.n. ..Mo Ai: Co Ccl Bi :1. Sb :fe: Mn .Te Ba Cr V Srn:: WAft: Al

Ca Na; K Sr Y Ga Li ' Nb!. Sc ;TA; Ti ..` NUMBER UNITS PPB G/T.PPM PPM PPM PPl1 PPM PPM PPM PPM PPM PPM PPM <PCT PPM PPM PPM PPM :PPM PPM;PPM PPM: PCT

PCT PCT PCT PPM PPM PPM'PPM PPM .PPM PPM PCT PPM::


Intertek Testing Services Chimitec Bondar Clegg Rapport Lab Geochimie

Geochemical Lab Report







INVOICE TO: MIKE KOZIOL REPORT COPIES TO: MIKE KOZIOL


NUMBER OF ANALYSES


991004 1 Au30 Gold 50 5 PPB Fire Assay of 30g 30g Fire Assay - AA 991004 2 Ag Silver 50 0.2 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991004 3 Cu Capper 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991004 4 Pb Lead 50 2 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991004 5 Zn Zinc 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991004 6 Mo Molybdenum 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

991004 7 Ni Nickel 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991004 8 Co Cobalt 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991004 9 Cd Cadmium 50 0.2 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991004 10 Bi Bismuth 50 5 PPM HCL:HNO3 (3:1) IMXJC. COUP. PLASMA 991004 11 As Arsenic 50 5 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991004 12 Sb Antimony 50 5 PPM HCL:HNO3 (3:1) IMDUC. COUP. PLASMA

991004 13 Fe Iron 50 0.01 PCT HCL:HNO3 (3:1) INDUE. COUP. PLASMA 991004 14 Mn Manganese 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991004 15 Te Telluriun 50 10 PPM HCL:HNO3 (3:1) INDUC. COW. PLASMA 991004 16 Ba Barium 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991004 17 Cr Chromium 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991004 18 V Vanadium 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

991004 19 Sn Tin 50 20 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991004 20 W Tungsten 50 20 PPM HCL:HNO3 (3:1) INDUC. COLA. PLASMA 991004 21 La Lanthanum 50 1 PPM HCL:HNO3 (3:1) INDUIC. COUP. PLASMA 991004 22 Al Alunirun 50 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991004 23 Mg Magnesium 50 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991004 24 Ca Calcium 50 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA

991004 25 Na Sodium 50 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991004 26 K Potassium 50 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991004 27 Sr Strontium 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991004 28 Y Yttrium 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991004 29 Ga Gallien 50 2 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991004 30 Li Lithium 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA


This report rust not be reproduced except in full. The data presented in this report is specific to those samples identified under "Sample Number" and is applicable only to the semples as received expressed on a dry basis unless otherwise indicated



REFERENCE: 170412


IDEU Intertek Testing Services Chimitec Bondar Clegg

DATE RECEIVED: 29-SEP-99 CLIENT: CAMECO GOLD INC. REPORT: 099-62832.0 ( COMPLETE )

PROJECT: CEDAR RAPIDS DATE PRINTED: 12-OCT-99 PAGE 1 OF 5

<5

<5

<5

<5 4.27 300:: <10 106 194 . 54 <20 i20: 32 2.53 2.46 1.91 0.05 0.76 105 <5 7.77 235 <10 39 115 43 <20 <20 16 2.08 1.46 0.47.!0.04 1.06 96 <5 2.81 180 <10 35 134 23;<20 <20 11 1.78 1.36 1.60 0.06 029:'; 91 <5 2.57 206 <10 41!< 121 . 21 <20 <20 10 1.86 1.43 2.14 0.06 0.24:!. 94 <5 ::4.17 432 <10 15 131 43 <20 <20 9 2.34 :1 95 2.43 0.05 0..15::106

<10 .41123 ;59:

<10 ..:10:103 :lS1::

<10 '.251 18 34;

<10 18.:171 :b5;

<10 17102 43

<5 <5::5.10 ;759 6 4:5.72 .718 8 ô;8.71 394 <5 +5:;7.49 562 <5 . s5 5.36 417

30:

~<5 :;5.70 540:;<10 <5 5.60 450:: <10 `..

<5:6.64 355 <10 45::6.36 653 <10 <5 6.02 873:: <10

3 <5: 5

~

5 14:: 2 : 5 17:: 2 6 3. 4 20; 1 3 19 <1

<70 0-14-< 2 <10 Fî.15:: <1

<1 <10 0 41; <1 <10 0.11`: <1

5 2;57:2.15 448:0.04 0:13 ; 54 4 2:j0.1.863.030.04 0.07:: 97 4 2.95 2.40 63 . 4 271 2.13 2.97:0.04 013; 55 3 244-1.99 2 71:0.04 0 12.i 49 : .._. _. ..

<5::: <5 K5 :'.:4.86 0400 44171 4420 K20 . <5 :: <5 . <5:4.86 623<10 ..28:191 43:<20 K20 •,(5: : <5 <5:4.60 ..7221<10 25:.214

. a:: <5 <54.06 . .647<10 . 39:.158 .30 <20 <20 <S;i 4 4>3.73 588><10 .4046 .2$<20 <26

ELEMENT Au30 Ag: Cu Pb Zn Mo Ni Co

UNITS PPB PPM PPM PPM, PPM PPM :PPM PPM Cd 8f:.: As :so:

PPM PPM :;PPM PPM: Fe Mn<. Te .86; Cr V! Sn :W: La

PCT PPMI::PPN PPMPPM PPMPPM PPM:PPM

Al Mg PCT':: PCT

Ca` Na

PCT:: PCT SAMPLE NUMBER

Zr

PPM

CDR9935-1595 41 <,2 20 52 136 23:i <.2 CDR9935-1596 565 1.84644 Q'. 51 75 287: 0.3 CDR9935-1597 1003::' 6 10 27 49 34: <.2 COR9935-1598 <5 0 4! 6 4 26 51 16; <.2 CDR9935-1599 11 <,2: 27 x2: 38 3 104 22: <.2

CDR9935-1600 7 0;3: 88 2:: 46 83 L2T <.2 CDR9935-1601 39 0.5; 241 2: 51 60 23'. <.2 CDR9935-1602 141 141392 <2: 73 85 125; 0.2 CDR9935-1603 2205;249 , x2: 68 3; 92 27: <.2 CDR9935-1604 1402:: 78 2: 50 74 <.2

CDR9935-1605 24 0 3;: 64 61 3:: 78 . 31.:<.2 CDR9935-1606 5703; 147 ¢ 60 4;: 76 55.:<.2 (DR9935-1607 189 0.*: 317 4 61 4:: 86 CDR9935-1608 16 0.2< 51 <2 50 3;; 84 26:<.2 CDR9935-1609 146 0.3::: 4 38 2: 97 66::<.2

œR9935-1610 19 0.3:: 47 44 3:;154 34<.2 œR9935-1611 20 0 3:< 24 <2 45 2; 99 316<.2 œR9935-1612 13 < 2 24 <2: 47 •.L: 81 65 ;<.2 œR9935-1613 172 0.3:: 20 <Z: 57 .. 3> 93 œR9935-1614 18 0.4;; 171 <2: 53 3';: 90 31.:<.2

œR9935-1615 <5 (43. % 50 ~ 50 2;: 83 25 ;:0.2 œR9935-1616 26 K2;; 58 <2 50 3 86 25;:<.2 œR9935-1617 12 0 4;; 20 4 56 . 3 :105 . 42 ; <.2 __.. œR9935-1618 <5 0.4:< 12 <2' 58 3>;: 99 39 :; <.2 œR9935-1619 58 0,4:> 8 <2' 52 3 93 70::10.2

œR9935-1620 72 0.3:: 6 Q:: 49 5;;; 79 28!<<.2 œR9935-1621 10 0.3:: 77 _.... 44 3': 70 24i<.2 œR9935-1622 7 0,3< 77 <2: 50 2::; 82 18.:<.2 œR9935-1623 <5 0.3; 59 <2:<: 49 2:i 67 *<.2 œR9935-1624 7 <,2:; 43 Q:' 47 :4, 59 19;;<.2

<10 0.18:: 10 <10 0.15; 1 <10 0.12: 8

<5 <10 0 12 8 6;<10 0.161 2

<20 <20:: 5 2:871.13 4.35:0.04 0,27::124 <20 K20: 8 248.2.01 4.16:0.04 0.23104 <20 x2Q 8 2.94.2.01 1.94:0.02 0.3'4 50 <20 <20'1 9 3.272.32 244 :.:10.05 0.22: 82 <20 <2Q: 7 2:35.1.64 2.26>:0.05 0.23: 62

:<10 020::: <1 <10 0.17.:: <1 <10 0.10::: 5

::<10 0.1!€>: 3

<5 ;6.34 ~r40> <10 21 129 32 <20 +t20: 10 2.78:;1.92 2.890.03 0,26: <5 7.20 . 457:<10 23 177 36 <20 <20:. 8 2.97 2.09 1.50 0.03 0.27.: 3 <,S 7.60 433 <10 31 189 : 47 <20 <20 16 3:t1T 2.19 1.86 0.03 0.~

<5 7.08 385;<10 52 207 92 <20 <20 12 3.05 2.37 1.81 0.07 0.99 <5::6.69 258 <10 91 206 90 <20 +t20 8 2.75 2.22 1.49 0.08 1 44

386 ::'7â <20 <20: 12 3;63>3.63 2.97':0.04 0.97 282 77 <20 rt20: 6 3.12 2.85 2.02 0.04 1.03:: 184 63:<20 <20 7 2.63:2.25 1.50::0.06 0.47:: 5 182 . 44 <20 <20:. 10 2.85 2.34 3.63 0.04 0..19 : 62 146 50 <20 <20 6 3,08 2.47 4.760.03 0.15;105

131 4T.<20 20:::: 4 2 84: 2.36 4410.03 o02:]68 $: 5 8:<10 h15:;': 2 157 . 48 <20 41: 4 2.71.2.18 3.56:0.04 0.10>: 77 b<: 4 19; 2.5::<10 0.1~`>: <1 267 63:.< . 20 <20: .18: :2 4 3.69 5.26: ,06 0.02 0 >103 , 6: 4 23:: 4: 8:<10 0,14:> <1

271 .62: <20 <21.7::::: 4 346:2.74 5..04::0.03 0.Ab:: 96 4: 4 24i 3 : 7:;<10 0.14: <1 223 66:<20 <20' 4 2;752.26 441::.0.04 0,05:; a8 7;: 4 2i3:: 3 8:<10 0.15: <1


<5:4.95 069;:<10 +5 5.03 877:':<10 <,5 5.77 1081;: <10 _.. _ . <5 6.37 1003 <10 <5 7.81 731 <10

K5 : a <5>: <5 <5: . <5 <5 ; <5 <5 <5

4 18:: <1 7:<10 0. QB:: 7 ..... ,: <10 t)13:; 8

8 23> 6 15:<10 0.21,: 3 7 24:: 6 . 1:1::<10 022;: <1

7 3x' : 5 18 <<10 0414 5 .25.: 5 ..10:<10 (.04. 5 14: 3 7.<10 O.1T 4 14;: 2 ....8><10 0.:13: 3 ;<10

: <1 : 2 : 2 <1

ELEMENT Au30 Ag

UNITS PPB PPM

__._. Cu Pb : Zn WI ;: Ni Co :: Cd Bi.::

PPM PPM PPM PPM>PPM PR' PPM PPM:

As Sb Fe PPM PPM;; PCT

I Te Ba' Cr V Sn (!

PPM PPM PPM, PPM PPM PPM PPM;

Na [(: Sr . .Y: Ga ii;: Nb 8C<: Ta Ti.::: Zr

PCT PCT:.:PPM PPN::PPM PPM;:PPM PPMI;PPM PC1`;PPM

La

M9

PPM

PCT

5 0.3;: 8 32 6 0 3<: 35 <2'; 60 <5 <:2 7 <2; 50 <5 0.2:: 15 <2:!: 76 <5 < 2: 12 55 _..

36 19<.2 2. 75 23<.2 2 50 21. <.2 2':i 63 30:<.2 2 55

2.75 656;.<10 46 139 4.86 802 <10 27 167 4.82 697 <10 5$.122 6.59 810 <10 44 149 5.52 764 <10 32 126

16<2° <20 41<20 <2Q 34<20 <â0 03]<20 <20. 46<20 42p

1.20 4.600.03 0.16: 86 2;; 2 12 <1 2.50 5.060.03 0.09€ 58 2:: 4 26 2 1.74 2$0,0.0L3 0.12 55 2 4 21 1 2.26274<0.030.10: 42 ..3;: 6 .30. 2 2.13 2.980.04 o,09; 48 3: 6 .29.'

:<10 0 - 07,> <1

<10 0.12: <1

<10 0:0i 2

;<10 2

s<10 e.01;: 2

4 1':75 5 40. 4 2.80 4 359 4 3.25

InjIntertek Testing Services Chimitec Bondar Clegg Rapport Lab Geochimie

Geochemical Lab Report CLIENT: CAMECO GOLD INC. PROJECT: CEDAR RAPIDS REPORT: 099-62832.0 ( COMPLETE ) DATE RECEIVED: 29-SEP-99


SAMPLE NUMBER

cDR9935-1625 COR9935-1626 0DR9935-1627 (DR9935-1628 0DR9935-1629

(DR9935-1630 0)R9935-1631 CDR9935-1632 œR9935-1633 CDR9935-1634

13 04':: 50 <2" 56 5 <.2.: 17 51 <5 < 2: 56 <2:< 73 <5 .!4 : 13 <Z: 95 _ .. <5 <2; 14 !2.;51

59 30.:<.2 4 60 21::<.2 .<5>

14 i25<.2 31 ...24:.;<.2 . 4:

13 .15>:<.2

764i,410 11159 ::2¢..<20 <20 w5 4.79 732:: <10 . 421.4

<5 +4';3.26 5.11<:<10 45i 90 12 <20 <2Q

<5 43J<20~;:4.50 .657::<10 33:.110 +20 _ _..

<5 <5 3.29 48/610 3$; ffi .13<20 420:

5 2401.80 3.99;0.02 Q* 54 .. 73;142.12347.0.04Q09; 59

18 1.99 1.00 2 155:;0.04 0.18:: 50

9 40-39 3.06:0.03 0.14:: 14 1..929.95 2 67:.0.05

3 <1 <5 6 .:31.; 2 <5r

4 157: 4 22:: <1 4: 3 15':: <1 15

CDR9935-1635 CDR9935-1636 CDR9935-1637 œR9935-1638 (DR9935-1639

8<2: 4..4';52 <5 <4:: <1 <'L; 55 <5 <.2 1 <2';: 56 <5 <.2 20 ~¢. 57 6 0.3;I <1 42;: 58

15 10 <.2 +4 > <5 <5; 2.59 499:; <10 15 10 <.2 <5 :; a 45 :2.28 52Q; <10

2'< 20 11:: <.2 ô: <5 <5 2.47 442 <10 3 20 13 <.2 <5;: <5 <5 2.75 . 532::<10 2': 68 18;;<.2 <5 <5 <5::;3.80 $25!:<10

.46A06 11:

45:109 .1Z.

36: 120 .1~.

92 78 20.166 33

520 14 1:96::1.07 2.82.0.06 0.16:: 69 . ,;3; 3 17;' <1 <20 +20 12 1..89::1.04 2.82:8.06 0.13.: 93 2: 3 .f6i <1 <20 <20 14 1790.10 1.0.07 0.10:: 90 3:: 4 17;: <1 <20 *,:.1 13 2:15:1.28 2:26.0.06 0 10<: 78 4>: 4 20:: <1 <20 <20. 5 2.89 2.09 A:00).04 0.04 0,10::: 58 3:: 4 32:: 1

<10 !q! 8

s<10 < 01:: 8

:<10 <.01,:: 10

;<10 < 01;; 8

<10 < 01' ; 3

CDR9935-1640 œR9935-1641 œR9935-1642 CDR9935-1643 œR9935-1644

<5 0.3 31 <5 0 3;;: 28 <5 < 2 48 <5 D 2!; 53 <5 0.3: 13

64 x5;:<.2 15;; <5 <5 4.32 787.<10 26 18;:<.2 <5 ; <5 <5 ;4.22 687><10 60 .19 <.2 .6.: <5 ;4 4.05 862 <10 58 18 <.2 . 4':: <5 <5:3.73 819 <10 37 11 <.2 <5.: <5 +6 2.43 500> <10

57 144 13:.<20 53'. 95 21: <20 <20 55:.139 35: <20 i24.

20165 .41:i!!<20 <2Q

49169 2020 ~2v

4 2:70 1.81 2.67 0.04 0.1:2;: 63 5 2.49- 1.39 1.770.04 0.11 95 6 2.84;2.11 2,500.04 011: 65 5 2.72 2.08 2.17 0.06 0 05.; 76

3 2:05.;1.12 2.56.:0.04 0,10s153

ei.;<10 0.14s <1 zij<10 0* <1 .... ..

<10 0 i~:;: <1 <10 o-14> 1

ITS - Chimitec - Bonder Clegg, 1322-B Harricana, Val-d'Or, P.Quebec, 3X6, (819) 825-0178

STANDARD

ELEMENT Au30 AN Cu Pb Zn MO Ni Co Cd Bi As Sb Fe

NAME

UNITS PPB PPM PPM PM PPM PPM PPM PPM PPM PPM PPM PPP( PCT

ANALYTICAL BLANK

ANALYTICAL BLANK

ANALYTICAL BLANK

of Analyses

Mean Value

Standard Deviation

Accepted Value

Oxide (Feldspar &

tiuther of Analyses

Mean Value

Standard Deviation

Accepted Value

CANMET LAKE-SED 2

of Analyses

Mean Value

Standard Deviation

Accepted Value

Oxide (Feldspar &

Nuther of Analyses

Mean Value

Standard Deviation

Accepted Value

Oxide (Feldspar &

Nuer of Analyses

Mean Value

Standard Deviation

Accepted Value

<5 <1 <2 <1 <4.<,.2 <5 <5'<-01

<5 <1 4 <1 <1 <1 46.2 <5 <5 i5<.01 <5

3 2 2 4 2:2 2 pg 2 2 2 2 2

3 <1 Ni <1 <1 <1 40.1 4 3 .1.01 „-,

' - ' . ' . . ' ' ' ' ' . - . ' ' . ' : ' . • ' - ' • ' - ' - . . . • . . , . , , .

50.2 1 M2:!::! 1 ..!:.•J.:: ,,,... ......,... ,...........

........... „..,„ .... ........... „,...

.....„ ..::': -.A mg MgN . .... ........ ..*

....„.

- i::::•,:7.......]: : 462

-.. „:. --------------------------------------- ----------------------.

- 7'

'..iv .ghil ..••-. - ' i. -g.g

465 Ut!--! - .:.f. :!:•:: • •- •• -.•-• :::::*:::::,

- 04_

--• 35•41 .188 1;i:! ':':)J!:4.8 00•. 12 i:I*53.60 ::::::::

-1

1 :::.118 18 4. 1 :::: :::: 1 61' 1 -0.4 . -i-,

35,_,

i 114.8 ,::* 12 gX3.60

36 40200,2* 23 I70.8 i',,.:0t

0 2 5 50.05

462

- 0.8 9 43.50

-

2884 NN.

1 „ -

2884

2940

176

1

176 !EN

186

•

• - • •....

•••• :"•:••-• •-

. •

End Intertek Testing Services Chimitec Bondar Clegg Rapport Lab Geochimie

Geochemical Lab Report CLIENT: CMECO GOLD INC.

REPORT: C99-62832.O ( COMPLETE ) DATE RECEIVED: 29-SEP-99



;::•::: Al ti;ii Na ;:iiii Sr :::.,,:,,:!:: ,...,,,..,,,,‘„,

..Y: Ga ••_.•,.. ____ „......„..

,, .••••..• ..•,..... i

Cr i :ii Sn :..RO:,.: La '',:::Ak6 Mg .k..:'..z.... :.i4pm 0,iippm Otkmni!r1"m

:::.tt Nb ,::,:.,!0, Ta

Te ]::-.7 -- !!!::::L,,,,, PPM :ilPCT PCT •:::::K.0 PCT ATA ..,.,....,„:„...,„„ $•41PPM P*PPM !

...rr...]iPPM

<1 <5 <10

::::::::::::!:,.,•]: ,:?:!::::,!' •::::i:, 'M ::::::M.!: ''M',;]q: :.:.:::.!:. n1 i1J.i: <1 ]..,.:*I <2 :!. .:i ::< <1 . i-. <20 :to;:i.. <1 7..„... ,...-?.:.,,i, ::..-iii::i <1 '..:,....51* <2 ''.

-......:01..c.01 ..514-1-::.<-- ...4.„.......::„ :......ii :.:.4i:..: <1 !:::::<7<10

"<1 <10 '':<1',:i '..:.! i-.: ‹20 ..;i6 <1 !k-40<.01 <.01-:.1!...!z

1.,.<10 ':::.''. <1 ''1.-g

.i.: ::0i-ii 2 i.:'...2::::: 2

]',..:.1..N: . ..,...:,,:::::::: _ ::::.,..:,..,:.. ...,..?..„,..7.... R•0:.,,.., i::: 2 :.iM2]::: 2 k4..: 2 .':.-i.:::,:: 5

.1 2 .-::.i.2!::! 2 .''ng' 2 '.,,..,f ::.i 1 .,.<t <1 kl

"....2- 2 2, ,,•.-.... ,.........--- -•,--- al -4-0I: <1 ..5....„.

o,.

2.::: 2 '..;at:',. -.,.:i.,.,..,,,....: ,...;... 1 <.01 <.01 .., A!.;It.:<-- ii„..,.7 i::........,i.:... i...iiQ :.]:.i :

..„:, 5 .....!.1,i, , ,...,...::„...,

..::,.: <1 cl 10 ::::::1M < !::,::::,•,..-, ...•:=::::: R::::::?,M .:':::.i.::,...:'.. .......,:..,i: i]..:..i.::::.....*

.- - - • - - • • •

.,....-:... ''•:.,'

. . -. ••. . . .

.. _. ......-

__,

.,',,,i 4 i..,ii <1 <.01 <.01 Zi$i <1 i11

<1 11 <I 'i"

.:;.qP :::Q.:......:....- 01 •

............

. • ' - - - .

._.„: :,..]:•,...m

i: <1 '-'...41....::: 1 ::::Pt:::: <1 ........

..........,.,.,...... ... ..

.1.<-3' <1 K41:::<' :-••••••

•••:.!.:i::...:!-.!

.........

....

...........

.. ....

!:!:i:.M:.!

• "•••••••

. ::::•::,..::.: 'n.::!7:..:! ......._. ...........

........

........... _ ... _

-,_..._

..... . . ..... •• •

.....

. ........

- ,..:.!:.:!:,,.i:i.: :.:,,,•

;i!ii•!•;.,•!!

'.:!:!:!!::::::,!:!:. •---

.

!:'•e:,.:..0 ::•ii.':!!..:!i.!

-„,-

. . . ._

----

-,''''.0.i:i: • :,'-'lii: • :....1..]::1'.

HO i

.. -."--•••.....

'•:•::,:::,:,::::::

...... -....:::::::::.....:.....;

.•

.,•:,..:.,.: .::]::&.&:-.,:, 207

45<20 021.72 ..•.

29 48

•

1884<10 .• -

• ••

_ .

• • „

0.62 0.59 0.04 0.25 . 29 52 4 1; i I 1 • I 1

0.62 0.59:0.04 4,25 29 52 4 17 -

- -



Geochemical Lab Report CLIENT: CAMECO GOLD INC. PROJECT: CEDAR RAPIDS

REPORT: C99-62832.O ( COMPLETE )


STANDARD ELEMENT Au30 .Ag

NAME UNITS PPB PPM

Cu Pb Zn Mo Ni Co'; Cd Bi, ? As Sb

PPM PPM PPM PPR PPM PPM PPM PPM PPM PPM

Fe

PCT

Mn;; Te w Cr V Sn u La

PPNPPM PPM PPM PPM PPM PPM PPM

Al Mg

PCT PCT

Ca ; Na IC Sr Y,: Ga L#;: Nb Ta Ti; Zr

PCT PCT Pçr.. PPM PPN!I:PPM PPN;;PPM 004 13P14 PÇT;PPM

STD GEOCHEM STD 6 - 0:4': 150 137 3';'144 36;;0.4 +SS 151 7.70 1549 <10 6>235 46<20 <40'; 6 2.05 2.56 3,54 0.02 0 05I:: 77 ~',; <2 23!>: 2 8'><10 <.01i; 6

Nimber of Analyses 1'

1 1 1€i 1. îli: 1 1 1 1;, 1 1;; 1 1' 1 1; 1 1

1 1.!i 1 1 1 1! 11:; 1 1;' 1

Mean Value - 0.4.4: 150 137 3'> 144 36'x::0.4 151 7.70 1549 5 bi 235 46 10 10'. 6 2,05.:2.56 3.54 0.02 0.05 77 4_: 1 23?; 2 8:? 5 <.01'; 6

Standard Deviation

Accepted Value - 0;2. 148 148 .4::135 35..0. 7.20 145O < :â:;251 5I. 5 2.70 4r00::0.01 0.04: 1 < 4t:: 5


œR9935-1595 41 i.2:: 20 52 136 23<.2 <5>:: <5 <5€4.27 388 4><10 106;194 54:<20 <20:> 32 2.53246 1.91`:0.05 Prep Duplicate 62 { 2 17 ~; 52 122 22<.2 <5'.; <5 <5:14.42 .352<10 104::209 52 <20 <20 30 2.51 2.31 11.76:0.07

__ _... œR9935-1597 10 03<<; 6 :10 27 49 34:<.2 6': <5 <5 2.81 180 <10 35 134 23 <20 <20 11 1:78 1.36 1.60 0.06 Duplicate 10 0.3;: 4 10 27 43 32;:<.2 <5; <5 <5 2.91 179 <10 34 143 23';<20 <20 11 1.81 1 35 1:63:40.06

œR9935-1614 18 0.4 171 90 31 <.2 s5'; <5 <5 6.02 873<<10 3it;146 50{<20 <20 6 3;08 2.47 4;7.6.:0.03 Duplicate 0.4 168 52 78 29 <.2 <5?: <5 <5;6.09 848;<10 29 154 50:<20 <20 6 3.06 2 41 4:76::0.03

œR9935-1619 58 D 4:: 8 52 : 3: 93 70:::0.2 â:: â 7.81 731 <10 66::<20 +20;: 4 2.75 2.26 4.310.04 Duplicate 52

Prep Duplicate 62<2;; 17 52 3:;122 22:<.2 <5:4.42 352.:<10 1041209 52:;<ZO e20; 30 ;.51'...2.31 1:7â;0.07 Duplicate 17 513111 22:4<.2 ;ü <54.36 356. '<10 105::204 54.;<20 <20 30 2.31:::2.27 147,0.07

œR9935-1640 <5 0.3 31 98 . Z;: 64 25:<.2 <5 cS;4.32 767 <10 57 144 33 <20 <20 4 2.70 1.81 Z;67:;0.04 Duplicate <5 ! ..

45:f<10 0.18 10

3 <5<10 0 18 9

0.12:: 8

0.1x.: 8

:<10 Ü.1S .: <1

<10 0.16: <1

~?<70 0:15: <1

<10 0.18: 9 ~;<70

0.38:-. 10

<5':: <10 0.14î: <1

6 0,76:105

0.80x4 93 4 6

0.29:; 91

0,30::

0.05

0 84

0.80; 9

0.12 63





PPMPPM PPM ;PPM PPMPPM PPMt:PPM PC3 PCT PCT; PCT

SAMPLE ELEMENT Au30 :Ag: Cu Pb;: Zn Ma4: Ni Co;: Cd 11U: .; As Sb; Fe iMn : Te BB:: Cr V:; Sn {~14: La .Ai Mg NUMBER UNITS PPB PPM:: PPM PPM;PPM PPM:;PPM PPPPM PPM(:PPM PPId; PCT

a Sr r.: Ga Li : Nb Sc: Ta :; Tfi.: Zr

PCT:PPM PPFI:PPM PPK;PPM PPIOPM :PPM

ITS - Chimitec - Bondar Clegg, 1322-B Hacricana, Val-d'Or, P.Quebec, J9P 3X6, (819) 825-0178

REPORT: C99-62833.O ( COMPLETE )




NLMBER OF ANALYSES


REFERENCE: 170412

SUJBMITTED BY: D. BASIN


SAMPLE TYPES NIMBER SIZE FRACTIONS NUMBER SAMPLE PREPARATIONS HUMBER

DRILL CORE 44 -150 44 CRUSH/SPLIT & PULV. 44 991004 1 Au30 Gold 44 5 PPB Fire Assay of 30g 30g Fire Assay - AA 991004 2 Ag Silver 44 0.2 PPM HCL:HNO3 (3:1) IMDUC. COUP. PLASMA 991004 3 Cu Copper 44 1 PPM HCL:HNO3 (3:1) IMDUC. COUP. PLASMA REPORT COPIES TO: MIKE KOZIOL INVOICE TO: MIKE KOZIOL 991004 4 Pb Lead 44 2 PPM HCL:HNO3 (3:1) IMDUC. COUP. PLASMA 991004 5 Zn Zinc 44 1 PPM HCL:HNO3 (3:1) IMDUC. COUP. PLASMA 991004 6 Mo Molybdenum 44 1 PPM HCL:HNO3 (3:1) IHDUIC. COUP. PLASMA This report must not be reproduced except in full. The data presented in this

report is specific to those samples identified under "Sample Number" and is 991004 7 Ni Nickel 44 1 PPM HCL:HNO3 (3:1) IHDUC. COUP. PLASMA applicable only to the samples as received expressed on a dry basis unless 991004 8 Co Cobalt 44 1 PPM HCL:HNO3 (3:1) INDUIC. COUP. PLASMA otherwise indicated 991004 9 Cd Cadmiun 44 0.2 PPM HCL:HNO3 (3:1) INOUC. COUP. PLASMA 991004 10 Bi Bismuth 44 5 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991004 11 As Arsenic 44 5 PPM HCL:HNO3 (3:1) IMDUIC. COMP. PLASMA 991004 12 Sb Antimony 44 5 PPM HCL:HNO3 (3:1) INDUIC. COUP. PLASMA

991004 13 Fe Iron 44 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991004 14 Mn Manganese 44 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991004 15 Te Tel 44 10 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991004 16 Ba Barium 44 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991004 17 Cr Chromium 44 1 PPM HCL:HNO3 (3:1) IMDUC. COUP. PLASMA 991004 18 V Vanadium 44 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

991004 19 Sn Tin 20 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991004 20 W Tungsten 20 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991004 21 La Lanthanum 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991004 22 Al Alunirun 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991004 23 Mg Magnesium 0.01 PCT HCL:HNO3 (3:1) IMDUIC. COUP. PLASMA 991004 24 Ca Calcium 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA

991004 25 Na Sodium 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991004 26 K Potassium 0.01 PCT HCL:HNO3 (3:1) IMDUC. COUP. PLASMA 991004 27 Sr Strontium 1 PPM HCL:HNO3 (3:1) INDl1C. COUP. PLASMA 991004 28 Y Yttrium 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991004 29 Ga Galliun 2 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991004 30 Li Lithium 1 PPM HCL:HNO3 (3:1) IMDUC. COUP. PLASMA

991004 31 Nb Niobium 44 1 PPM HCL:HNO3 (3:1) IMDUC. COUP. PLASMA 991004 32 Sc Scandium 44 5 PPM HCL:HNO3 (3:1) IMDUC. COUP. PLASMA 991004 33 Ta Tantalum 44 10 PPM HCL:HNO3 (3:1) IMDUC. COUP. PLASMA 991004 34 Ti Titanium 44 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991004 35 Zr Zirconium 44 1 PPM HCL:HNO3 (3:1) IMDUC. COUP. PLASMA

tPtP

tV

tVg

ttt

Intertek Testing Services Rapport Lab Geochimie Chimitec Bondar Clegg



6 2.92 2 05 .;2343.02 0.12:: 75

7 24t2-17 2.17 3:54 0.03 0.07` 75 69 .:::4:0.35 0.02;0.04 011051 6 2.68:1.92 5.190.04 0109:: 98 _.. 7 3.12'.2.68 12:0.04 0.02. 38

9 2.48: 1.82 5.34 0.06 0,07:: 20 0.67 0.33 2.22 0.08 0.13:: 7 7 2.57 1 95 5,20 0.06 0 04;; 93 7 2.53 2 20 5.60 0.07 0.04 55 7 2.62:2 37 4.78:ü.05 0.,05:: 37

15 : 1 35.< 2 . :8 ><10 <.01

1 :.-6;<10 4i <1 <52.<10 41 3 10'.<10 <.Ul


Geochemical Lab Report CLIENT: CAMECO GOLD INC. PROJECT: CEDAR RAPIDS REPORT: C99-62833.O ( COMPLETE )



SAMPLE

AMER

Na PCT

ELEMENT Au30 i Al: Cu : Pb;: Zn No Ni Co>: Cd Si::

UNITS PPB PPi1PPM PPM PPM PPF4PPM PPb1::PPM PPM As Sb> Fe Mn; Te 88. Cr Y Sn W.> La Al; Mg

PPM PPM PCT '4144 PPM PPM.: PPM PPM PPM PPM PPM PCT> PCT Ga lfi;: Nb 8C; Ta 1 i; Zr

PPM PPMF:PPM PPM::PPM PPM:PPM PçT.:PPM

COR9935-1645 <5 < 2: 69 :«2103 66 25<.2 6 <5;:3.97 809 <10 23;:;176 43;:<20 <20:

CDR9935-1646 <5 24 - X008 61 26<.2 <5 <5::4.31 825 <10 36:134 42::<20 <20`: CDR9935-1647 <5 74 ; <2:::116 73 <5 <5 4.67 893 <10 18::176 53:<20 Q0 CDR9935-1648 <5 <4 47 : <2.::102 71 <5 <5::4.23 861'::<10 __.. 22::182 51:<<20 QO:

CDR9935-1649 <5 0.2: 56 : (2:; 31 28 13<.2 <5 <5 2.04 533 <10 68155 .27k20

_.. _ _..... CUR9935-1650 9 «" 2: 14 '<k: 61 5 13::<.2 :<5: <5 <5 2.08 388;<10 113 68 13><20 <20 CDR9935-1651 <5 < Z;: 51 : <2;: 80 63 ,22.;<.2 <5 <5 <5:3.28 792 <10 ...:8:'165 46::Q0 .00:: CDR9935-1652 8 <.x: 59 WI 86 64 23 <.2 , <5<: <5 <5 3.37 727':<10 8 157 44::Q0 +t20î: CDR9935-1653 <5x2:58;<2::100 .. 71 28::<.2 _ ... <5 < <5 <5:3.64 1`74;:<10 __. .... 13::179 _..... 47.:<20 <20;: CDR9935-1654 <5 ~ Z 11 c2;;116 <1 : 67 26;:<.2 <5; <5 15 3.92 . 8Q1;<10 34 130 .37:<20 420;

ŒR9935-1655 <5 <.2;; 29 4::104 56 ,:23<.2 <5 : < X5 3.49 j40C<10 '27116 37::<20 <2.0 ;; CDR9935-1656 <5 i 2:; 2 60 1.; 20 11::0.2 <5...: <5 <5:2.27 170A0 38105 15:4:20 44:<

CDR9935-1657 <5 39 <2 :137 x: 41 20:0.4 . <5:: <5 ï5..4.34 . 4W<10 31;106 :.15;420 ~20:; CDR9935-1658 <5 <..2 55 <2;' 88 3s: 99 25<.2 <5: <5 <5>:2.90 609::<10 6:211 34<20 00:: CDR9935-1659 <5 <.2> 71 3>:135 <1136 .27<<.2 <5'!: <5 ::X51.79. 945► <10 24:::287 42<20 .<'20:

ŒR9935-1660 <5 <,Z 28 <2::117 1 106 24::<.2 . <5 : < 3.74 1071 <10 28;;187 .: ~;20<: CDR9935-1661 20 <.083 K2` 80 <t: 59 21 <.2 <5:: .. <5 .<5:5.22 ....... 1417><10 .......... 134 0 ~c20: CDR9935-1662 <5 <.2:: 5 <2::131 <1 :100 24 :<.2 <5: <5 <5::4.24 1n7: <10 1$;198 0 <20;: CDR9935-1663 <5 K.2:: 18 <2l` 65 <1:: 59 19 <.2 <5 <5 . <5;:3.48 . 561::<10 27;:108 7<20 <20'.: CDR9935-1664 7 2..Z: 7 23 .3: 24 8 <.2 <5 <5 <5 ::1.42 353:i<10 26::218 9:fQ0 <20:

CDR9935-1665 <5 < 2!;. 10 <2 78 1 69 24 <.2 <5;: <5 <5:4.14 é48;<10 '25;117 <20 +20;; CDR9935-1666 12 r.2 <.: 47 <2 67 <1 70 21:<.2 <5 <5 <5:3.85 723>: <10 24153 <20 <201 CDR9935-1667 9 <.2;171 76 5; 31 0.3 <5 <5 K5;5.81 1.250;;<10 36; 65 <20 +20> CDR9935-1668 <5 35 66 2> 72 20<.2 . 45 < <5 K5 3.55 . 74.2<10 31 :;143 <20 <20; CDR9935-1669 <5 < 2> 42 71 <l ` 67 21;;<.2 <5; <5 <5';;3.99 697';<10 10:;164 <20 <20:::

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II 113 Intertek Testing Services

Chimitec Bondar Clegg Rapport Lab Geochimie Geochemical Lab Report





SAMPLE ELEMENT Au30 Ag Cu Pb Zn •Mo ,] Ni Co CdBi •••• Te Cr Sn La Mg Na Sr Ga Nb Ta Zr As Fe ' WISER UNITS PPS PPM PPM PPM PPM PPM PPM PPM PPM PPM PPM PPM PCT PPM PPM PPM PPM PPM PPM PPM PPM PCI PCT PCI PCT J.04pri PPM PPM PPM PPM PPM PPMPCT PPM

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........ ........ .......... .......... .......,.. ........ ........

........

........ ........

., ._.

........ ........ ---

........

........ • • • • • • • • .,........ ........ ,....... ........ ::....:::..,.....,::::':

........ ........ .„. .. ..........

.... ..

- - • • • • • ........

.,.,.... ........ ....„.... - - - - - .......• ....,... ...,..,.. ....,...,.......... ...• .. ........ .. ..,..

-"" • " - -

.,...... "" - -

.,...... ......,. .....„.

,.. ....... .......• ......... ........ ,......... • - -•

..,.,..,.. • • • •-• • • • • - -• •


::::5-.::.3.77

•!*3.64

.i,;<5]:.0.49

:.::<5.:::.:3.81 .;i,.....::.47

i::442<10

..:::;717':::<10

161 <10

.:--.981 <10

1342 <10

.-A5180

':',22-.128

;:.4i.-121

i.:::19::!]135

:::,44110 ..............%

:..26...,.,<20 !!iab.'..

:-: 0

'- 12:2280 ....716

:i.4$.:..-.<20 i2-8..

]:::::.1ii<21) 4.0 -,:.:.,..,,:.::. --...'...:-.,....... 177°7 .1

.B7 2.30

?I?......:...°°°676 .;--,- ;;J::: ;1: i;:.,,.i - ;222 ....1-.:;;:-..:: <11 :•::::::E:::::11: :::.111)::-:11i. 3

05 0.10 41 41 2:: <2 ::: ., i14 <1 'ii::,*::-.:.<lo ;ioii- 3

<1 <5 <10 ;;O g. 3 .....--':::::..]:--...:::-.:...:

1 18.<10 ''.. .-'iiii.. 3 6 i.......ii.92 -. ..$0.05 0'..]..*$ 70 0.,.* <2 i-.t:;ii.::

........:,.....?.........)...:-..,........ :...,,......i.:::...:::....i'...., :: .:..m..... .. -....,.........x: ..........:::,,., ....,..... • -........i •







5 02:. Accepted Value 1.0 5::>:::5::;0.

STANDARD ELEMENT Au30 YAT. Cu Pb;.. Zn Mo.; Ni ; ;Co Cd :BI As lb: Fe NAME UNITS PPB PPM.PPM PPM PPM PPM PPM PP14:PPM PPM PPM PPM PCT

ANALYTICAL BLANK <5 <.2 <1 :i<2 <1<1 <1 <1 :<.2 <5': <5 <5';<.01

ANALYTICAL BLANK <5 <.2.: <1 <2. <11;:'. <1 <1;;<.2 . <5: <5 <5'`<.01

Number of Analyses 2 2 2 2 2 2:' 22 2 2',: 2 2;;; 2

Mean Value 3 0.1 <1 1. <1 : <1. <1 X1.0.1 3:i 3 .3: <.01

Standard Deviation - - ..... -



Mean Value 2788


Accepted Value 2940



Mean Value 191


Accepted Value 186

c1:;-<10 <1>; <1 <1;~0 +dOs: <1 r.01':< 01 <;:01 <.01 <:01: ... ... ..... .. _..

<1:.<1,<20 +~0; <1 K 01':>< 01 <.0 1 < 01 ;< i1t;

2:: 2 2:: 2 ~:: 2. 2:> 2 2; 2..:~. 2

<1 . <7.: 10 .10:: <1 t.0# :<.01 E.:01:. <.01 <:1)1 _. ... _. _.. .... ........ .......

51 <20 <20<: 20 1.30 0 75 1:34:0.04 0r09";; 59

1:< 1 ::;.1 ; 1 ,....

0i:: 20 1.30:0 75 134:0.04 0c1

3 2.03:22 39 3:55:<.01 603;;

Ga . Li :: Nb SG:<: Ta . .:TiÈ:: Zr

PCT :: PC1'';PPM PPM:;PPM PPM-:PPM pPF1. PPM ;;PPM

<1 .<1;: <2 <1.:: <1 d:><10 <,01;: <1

<1 <1,> <2 <1.:: <1 <.01.> <1

2 .2:,< 2 2 .2::: 2

12 <5:::2.99 1273>:<10 874 _.

1 1< 1 1:

12 3:::2.99 1273: 5 874

4::2.60 1200:::

7.42 1595<

7.42 1595:

7.20 1450 <


<2 9':: 4 '5<10 047;: <1

1

4 5:; 5 0.07:: <1

Q ;21::: 2 : #:0:<10

_._._

_.... . _...

... .

Te .Oa:: Cr ..: VJ Sn :. :N:: La

PPM PPM:;:PPM PPM::PPM PPM:PPM

Mg

PCT

GANNET STREAM-SED 4

Number of Analyses

Mean Value

Standard Deviation

Accepted Value

<.2 70 ;:12: 81 ::,1':: 25 12 0.3

1:

1 1<#: 1: #:> 1

- 0.1 70 _:12:: 81 ; 1: 25 : 1Z0.3

- 0 3 66 :::13 . 82 ; 2: : 23 1 T:':0.6 __ _._..

147 19: - e4!:157

:3156 -01157;19 147 ; 148:39:::0.4

148 4;:135 35'<IO. - 0;2.148 _._.

148 ':39 :0.4 <5 156 .:< STD GEOCNEM STD 6

Number of Analyses

Mean Value

Standard Deviation

Accepted Value

Rapport Lab Geochimie Geochemical Lab Report Effla





M4ti:; Te 8$ PPM;PPM PPF4

SAMPLE ELEMENT Au30 :Ag Cu :Pb; Zn Nb:: Ni Co:: Cd 8i:: As Sb: Fe NUMBER UNITS PPB Pint PPM PPM PPit;PPM PP.M, :PPM PPM ::PPM PPM:: PCT

Ca Mg

PCT

Na 1C;: Sr Y PCT POT, >PPM pRF1

Cr v:. Sn W : La

PPM PPM.,PPM PPM:;PPM

11 13

4.23 861 <10 4.10 893'::<10

<5 3.64 7T4::<10

<5:3.87 771'<10

<5,;!4.14

668<10 2S 24

22 21:

<5 <..;2. 47 :<2102 7: 71 ?7,/<.2 <5 <5

<5 <.2 46 <2101 <} 73 27:<.2 <5 <5

<5 <*? 58 <2;100 71 28 <.2 <5

<5 <.2: 58 <2 97 71 xr i<.2 <5

<5 <.2 10 2;' 78 1<:: 69 24 <.2 <5 2' 9 Z. 78 <t; 70

<5 < 2:; 50 68 :: 5 18:::<.2 <5 <5

<5 54 95 8 12::<.2 <5<: <5 <.2 0 <2 93 3 17 ..1Z.:<.2 <5:: <5


<10 22:;129 26 <20 <20; 9 2.48 1.82 5.34 0.06 0 <5 3.56

48

48

67

68

15:3.06 1314 <10 <5:;3.00 1299 <10

Q0 40 41 0 7Cl 0.95 4.42405 0.24 <: <20 <ZO:: 40 00:0.94 4.42:0.05 0.24;:


œR9935-1653 Prep Dtplicate

œR9935-1665

Duplicate

œR9935-1670 Duplicate

œR9935-1684

Duplicate

Ga Ei ; Nb St :'. Ta

PPM PPM;PPM PPFI:;PPM

182 51''<20 <20::I 3 2:90.2 08 2:17>0.04 0.04 67 175 49;<20 <20 3 2.80 2.19 2.25 0.03 0.04 63

179 47::<20 <20 2 2 83 2.14 2:.060.04 0.03: 66 3 :: <2 27::

158 §7`:<20 <20 2 2.94 2.14 2:070.04 0.03 65

117 32;:<20 <20 6 2.92 2.05 3:23>0.02 0„12::: 75 : 4:; <2 â5:: 1~;<10 <.i,.., 115 31 <20 <20 : 6 2.87 2.10 3.33 0.02 0.11 : 73 <1 <5 :<10 <.01:

<10 012i <1

2 5 :;<10 0 11;: <1

::<10 ~oyy.1z; <1 1:<10 V.r.1:2 [ <1

REFERENCE: 170414 REPORT: 099-62834.0 ( COMPLETE )

SUBMITTED BY: D. BASIN CLIENT: CAMECO GOLD INC.

NUMBER SIZE FRACTIONS NUMBER SAMPLE PREPARATIONS NLFIBER SAMPLE TYPES


REPORT COPIES TO: MIKE KOZIOL

*w**********k******* ***********

This report must not be reproduced except in full. The data presented in this report is specific to those samples identified under "Sample Number" and is applicable only to the samples as received expressed on a dry basis unless. otherwise indicated


NUMBER OF ANALYSES

LOLER DETECTION EXTRACTION NETNOD

991005 1 Au30 Gold 70 5 PPS Fire Assay of 30g 30g Fire Assay - M 991005 2 Ag Silver 70 0.2 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991005 3 Cu Copper 70 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991005 4 Pb Lead 70 2 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991005 5 Zn Zinc 70 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991005 6 Mo Molybderxm 70 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

991005 7 Ni Nickel 70 1 PPM HCL:HNO3 (3:1) IMDUC. COUP. PLASMA 991005 8 Co Cobalt 70 1 PPM HCL:HNO3 (3:1) INDUC. COMP. PLASMA 991005 9 Cd Cadmium 70 0.2 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991005 10 Bi Bismuth 70 5 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991005 11 As Arsenic 70 5 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991005 12 Sb Antimony 70 5 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

991005 13 Fe Iron 70 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991005 14 Mn Manganese 70 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991005 15 Te Tellurium 70 10 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991005 16 Ba Barium 70 1 PPM HCL:HNO3 (3:1) IMDUC. COUP. PLASMA 991005 17 Cr Chromium 70 1 PPM HCL:HNO3 (3:1) IMDUC. COUP. PLASMA 991005 18 V Vanadium 70 1 PPM HCL:HNO3 (3:1) IMDUC. COUP. PLASMA

991005 19 Sn Tin 70 20 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991005 20 W Tungsten 70 20 PPM HCL:HNO3 (3:1) INDUC. COIF. PLASMA 991005 21 La Lanthanum 70 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991005 22 Al Alunirun 70 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991005 23 Mg Magnesium 70 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991005 24 Ca Calcium 70 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA

991005 25 Na Sodiun 70 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991005 26 K Potassium 70 0.01 PCT HCL:HNO3 (3:1) INDIC. COUP. PLASMA 991005 27 Sr Strontium 70 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991005 28 Y Yttrium 70 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991005 29 Ga Gallium 70 2 PPM HCL:HNO3 (3:1) INDUC. COMP. PLASMA 991005 30 Li Lithium 70 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA


INVOICE T0: MIKE KOZIOL

PROJECT: CEDAR RAPIDS DATE RECEIVED: 29-SEP-99 DATE PRINTED: 12-OCT-99




49! 91 58!::108 65;'110 53 98 45::118

22;<20 <20 8 1:78 r1 22 1K70:'0.05 0.15 107 23ü<20 <20:: 8 1.75 1.34 1:670.05 0.15 80 25 <20 <20 9 1,.89. 1 44 1.49 0.06 0.16 96 22 <20 <20 8 1.72 1.44 1.15 0.05 0.13 71 24 <20 40:: 11 1.75; 1.28 1,60:0.07 0.15 108

9 1: 84 20::20 <20:: 10 24<Q0 <24; 11 1,77 21:::Q0 <ZQ; 10 1 45

5340 <20;: 43 245

52 62 57 78 48

99 91

'113 85 246

<20 <20,;. 10 1,68 1 31 1:52::0.05 0:19r 80 <20 <20'> 11 1..62:.1 32 1:54:>0.06 0,17: 72 <20 <20,. 10 1..52:1 16 1;40'.;0.05 0.18:: 71 <20 <20 8 1.76 1.51 1:18'0.05 0.09€ 76 <20 <20 9 1.56 1.35 1:34:;0.06 0.13;> 63

90 71 80 78 93

71:i 22 20

32

21

67; 32:

• 45:





SAMPLE NUMBER

ELEMENT Au30 Ag. Cu Pb Zn :Ms Ni UNITS PPB PPM:":PPM PPM:,PPM PPM:;PPM

_ _._. Co Cd 8i=: As Sb; Fe

PPM 6PM::PPM PP11;: PCT Te Ba;! Cr V:: Sn Olk La

PPM PPMÉPPM Ga . Li:i: Nb . SC:: Ta

PPM PPM::.PPM PPM:;PPM Mg Ca: Na

PCT PC1': PCT PPM: PPM PPM.PPM PPM: Zr

PPM

CDR9936-1689 CDR9936-1690 CDR9936-1691 œR9936-1692 œR9936-1693

<5 <4 43 <$

11 <.2': 95 <2

46 0.3' 67 <2

890 1 3:::998 <2:

16i.2::94

35 42 44 50 31

28 33 32 34

1; 28

11%

70i0.2 10:<.2

•<5i:,:

<5<: <5

<5 <5 <5 6 <5

2.53 2.70 2.77 3.41 2.25

329;:<10 369><10 374:<10 361<10 305;.:<10

œR9936-1694 72 <.2:: 91 ,a;: 34 1<~ 37 19<.2 <5 ;: <5 <5.2.56 324<10 œR9936-1695 151 <.2:153 <2> 30 1;: 28 15': <.2 . <5': <5 <5 >2.28 261<10 œR9936-1696 <5 <,2 22 <2.; 33 1: 34 12::<.2 <5;: <5 <5;2.34 320:<10 œR9936-1697 19 <.2:: 13 : <2: 25 . ..1: 31 11;<.2 4;; <5 <5>1.77 252:;<10 œR9936-1698 <5 X:2: 20 ::xi: 42 <1:>192 24<.2 <Si2.61 474::<10

_..... œR9936-1699 12 21 : <2>; 30 28 11<.2 <5:: <5 234;:<10 œR9936-1700 56 <4 44 : <r : 25 32 .15 :<.2 . <5 : <5 <5 ::2.16 218 :<10 œR9936-1701 105 0.3 ;675 ; <2; 20 55 11i<.2 <5; <5 <5:1.58 242<<10 œR9936-1702 116 <.2>;425 ; <21: 20 52 11:':<.2 <5:: <5 <5>'1.61 273::<10

œR9936-1703 108 0,3::689<2;: 19 61 10:i<.2 <5:; <5 ~5;!1.60 .223;:<10

œR9936-1704 113 253 04253 <2 22 2 . 42 10 ::<.2 <5 ; <5 s5 ;1.92 œR9936-1705 25 <2::25 <2:: 20 1[ ': 35 14 <.2 <5 <5 %.-7,01) œR9936-1706 11 c 2;: € 16 26 i ; 34 11 `<.2 <5 < <5

<5 : 2. 01 <5::2.29 251'.;<10

œR9936-1707 12<2::32 <2; 33 33 12::<.2 <~ <5 <5:2.41 296:.<10 œR9936-1708 <5 10 <2 ;; 30 8: 34 1#;<.2 <5 <5 <5 2.21 274'<10

œR9936-1709 20 < 2<: 45 <2:: 24 : 2 `: 28 10::<.2 e5:; <5 ~5. 2.02 205;:<10 œR9936-1710 126 <.2:: 43 <2> 27 : 1>: 27 10;<.2 <5:: <5 <5;. 2.27 218<10 œR9936-1711 251 < 2<: 90 <2; 48 :<1;: 38 18;.;<.2 <5 ; <5 3.62 441<10 œR9936-1712 60 <.2'1 18 <2< 36 : 2: i 25 <5 <5:; 2.46 291 :<10 œR9936-1713 210 <.2 33 <2' 34 %:4, 23 16:: ;<.2 <5;' <5 <5> 2.48 244:1<10

œR9936-1714 54 <.2 63 : <2 32 : 1;! 26 16'i;<.2 <5 <5 2.58 275 <10 œR9936-1715 69 <.2 40 ::<2; 37 <1 22 . 12 <.2 <5 <5 2.48 255 <10 œR9936-1716 108 <.2 : 84 ' <2 34 ' 2 23 13 <.2 <5:: <5 <5 2.23 276:s<10 œR9936-1717 22 <.2 35 : 5 44 <1 30 12 0.4 <5 <5 2.54 347:<10 œR9936-1718 26 <4 , 67 :..<2 : 34 : 1 29 13 <.2 <5 <5 5 2.32 290<10

<1 <5:::<10 0.08:i 8 <1 . ' ,6.:X10 0.091:: 9 <1 <5;;<10 0.09'; 10 <1 <5 :<10 0.07 : 11 <1 ~5':<10 0.08'; 11

1.65 1.64 0.05 0.1 1.35 1:36:0.06 0.1 1.40 1:76 0.06 015.;1 1.14 2:07:.:0.04 0.19 2.91 2.71 0.05 0.15::1

1 6;<<10 049.: 8 7 > <1 . <5:<10 0.08:: 9 ;<1 a <10008; 9 <1 ad.':<10 0.07 < 8 2 .<10 0.11.; 14

226 <10

:1°7 11

97 31; <20 <20 ; 12 1 59,:1 49 1 t;78 0.07 40 : 90 30 ;<20 12 56;: 92 32;<20 <20:: 12 1.0Q;1 ▪ 52 1:5$;0.06 Q 1 43 98 30,:<20 <20:: 10 1 6d;1 ▪ 43 1;25 0.06 O. 1

50;::81 53:: 85 45;: 92 88:; 88 67 67

70:: 81 22::<20 <20 94 22<20 <20:

1$: 80 37<20 <20; 20:105 .35::<20 <20: 16130

24 <20 <20 11 1 51: 1 25 1,400.06 0:1 24 <20 <20 11 1.63 1.33 1:35;0.06 0.13 88 4 ::

72;40 <20: 8 ma 85 1.72>0.04 0,14 : 82 5 <2 21,'<20 <20: 11 1.67:.1 28 1.71 0.05 0.21 79 5 <2 21 <20 <20 11 1.66 1.30 1:05::0.06 0.15 78 .5 < <2

12 U$761.38 1,39<0.06 0,13:111 11 1J2).48 t::T►5 :0.06 0 12;105 14 1.30.55 2;54;0.06 0.08> 55 : 13 1.44:.1.54 2:90;0.07 0.09> 66 12 1.42:1.47 2,40<0.07 0.05': 76

<10 0.08:: 9

2 . <?,;<10

1 <5', <10 0 09; 9 2 <5:<:<10 0 09:: 9

9 0.k ; 9

• 0. osR; 10 8

<5:<10 Q,Q9' 8

04w 9 <1 . Y5;<10 000:: 8 3

5 <<10 OW 4 <1

0:0. 9 <1 <SI<10 0,08<: 9

<1 <10 0.07; 9 <1 <5:;<10 Oil 9 <1 • 0.07:: 9 1 <5<10 0.09 8 <1 <5<10 0 07: 9

Y.

~ ITS - Chimitec - Bondar Clegg, 1322-B Harricana, Val-d'Or, P.Quebec, J9P 3X6, (819) 825-0178

4:1.59 180;<10 <51.39 17.4::<10 <5.1.34 Y.18610

::5.!1.93 339. ::<10 <5>1.58 315I:<10

<5<1.21 217::<10 <5:1.74 34010 ..<5,1.47 290<10 6; <5 .:2.56 .476::<10 <t i: ::<51.64 209:<10 33:

83 17;<20 <20:; 12 1.23.; 1 00 248;0.06 86 .21: <20 <20:: 12 1;24).01 1:63:0.06 O.l._..

135 4620 <20:: 14 1;200.97 1:.79,.0.08 006; -- 103 35<20 r20`:: 8 1.671.66 200>0.07 0.01:: 70 102 44.<20 +400: 3 140.53 140).05 <.01.:: 5

30-';'<20 <20;: 5 1.021.05 1::72;;0.06 003:;; 46 41<20 <20:: 5 f.:40.56 2:00:0.05 0.02 :: 53 321:<20 +t20:: 3 1:41.23 1.57::0.07 0,02: 62 ::

3 140!I.95 1.55 0.04 ;< 01; 62 22:<20 <2Q;: 3 1 30;.1 17 1.:00;0.06 :0 11;: 61

9 <10 0.07:: 10

10 0.07:: 9

;<10 0,06:: 7

<5:::<10 0.07<: 8 *<10

<5:<10 0 14: 5

5

<10 0.13;: 6

<10 0.14> <5<10 004: 4

2 :1:1100 ~::<10 0 15.; 1

1 <5 :<10 0. i0> 7

14

7

104 145 131 159 105

<5;2.00 229 <10 24; 86 18:Q0 <20:: 14 1.45: 1.08 .1::62;0.06 0,47;: .K5:1.94 239::<10 22: 85 19::<20 <20:; 14 1:37:].:1.05 1:36 0.06 (105:: .:::45ï..2.06 222 ><10 .311 92 19::<20 <20:; 14 1.47:1 01 1,19::0.07 0 07`<

...<.5,1.93 :...265..... ::<10 . 26;109 19::Q0 <20: 14 1.39.: 1.01 1:.54 U.07 0.07i: <5:1.92 191;'<10 22.112 19;Q0 <20:: 14 1.39: 1 04 1':460.06 0.06: :

EGO Intertek Testing Services Chimitec Bondar Clegg


CLIENT: CAMECO GOLD INC. PROJECT: CEDAR RAPIDS REPORT: C99-62834.0 ( COMPLETE ) DATE RECEIVED: 29-SEP-99 DATE PRINTED: 12-OCT-99 PAGE 2 OF 6

_._ __ . ......., _..

SAMPLE ELEMENT Au30 ;Ag; Cu :Pb: Zn Ma:; Ni Cd:: Cd Bi;; As Sb;: Fe Mrt>: Te Bb': Cr V;; Sn {t; La NUMBER UNITS PPB PPMIPPM PPM :PPM PP11;PPM PPM..PPM PPFIPPM pP(4:: PCT PPMI;PPM pPM:PPM PPM PPM pPMt:.PPM

Mg PCT

Cë

Pç1

Na : K;;: Sr :Y;: Ga IC Nb Sc.:: Ta T#; Zr PCT : Pi;T;:PPM 1?PM >PPM PPN ;PPM ~1;PPM PCT;PPM

_.. _ _ . __ __... _._.. CDR9936-1719 31 <:,2::: 73 .;<2;; 37 30 17::<.2 <5;: <5 CDR9936-1720 9 <.2 30 :<2:: 32 2>: 30 <5 14 { <.2 <5'; CDR9936-1721 <5 :(„z 28 ::<2 28 1: 26 13<.2 <5_ <5 mR9936-1722 7 <4. 32 ::<2' 28 1:i 25 12;<.2 <51<; <5 CDR9936-1723 <5 < 2 27 < 3: 32 2> 25 13':;<.2 <S'':: <5

CDR9936-1724 <5 ~ Z 29 :;<2 29 ;;~;: 29 141<.2 <5

CDR9936-1725 <5 ; ....2::: 30 ;' 3: 29 : 1:> 37 15<.2 <5 CDR9936-1726 <5 <4 27 ;: <Z .; 30 ; 1::; 21 12;0.3 <5; <5 CDR9936-1727 <5 r 2 52 ;.<2 24 :<1:; 20 12<.2 __. <5 LUR9936-1728 <5 <..2 32 ::<2!: 28 : 1; 15 12 :i<.2 4 <5

ŒR9936-1729 <5 < 2 9 ; 31 15 10<.2 <5 ŒR9936-1730 15 <.2 51 :.< 25 16 11;:<.2 <5 ŒR9936-1731 116 t14. 590 <2: 24 25 12<.2 <5 ŒR9936-1732 <5 <.2 40 <2 25 17 11<.2 <5 ŒR9936-1733 35 <.2180 e2:: 23 19 .18ü'<.2 <5

ŒR9936-1734 <5 <.2:: 15 <2 24 14 <.2 <5 ŒR9936-1735 <5 2. 65 <2: 22 15 16 <.2 <5: <5 ŒR9936-1736 <5 <4i 61 6 32 14 13 <.2 <5: <5 ŒR9936-1737 6 <,2; 71 .4 32 14 16 0.2 <5: <5

ŒR9936-1738 24 4.2:263 3 24 17 26 <.2 <5

ŒR9936-1739 66 0.2 534 :: <2' 18 17 <.2 <5 ŒR9936-1740 183 0.2 430 <2: 18 17 13: <.2 <5;; <5 ŒR9936-1741 58 < 2 337 < <2 17 19 11 <.2 <5: <5 ŒR9936-1742 125 < 2 380 <2 27 35 11; <.2 <5 :: <5 ŒR9936-1743 26 <.2 325 <2:: 24 51 11 <.2 <5;; <5

1DR9936-1744 17 44032 <2: 20 44 10:<.2 . <5:; <5 ŒR9936-1745 33 <.2:i231 4 26 52 13 <.2 <5::; <5 ŒR9936-1746 6 <.2: 53 24 i:1 36 11:<.2 ::.<5:. <5 ŒR9936-1747 20 <.2 184 <2: 36 2 82 .25<.2 <5:: <5 ŒR9936-1748 6 4.2 33 <2> 23 40 .14.><.2 <5 ; <5

_.. _.. .... <20 <20 10 1.59 1 39 1.47 0.05 0.11 67 <20 <20 11 1 68;1 44 1.13 0.05 0.08 75 <20 <20 10 1.57 1.32 1.33 0.06 0.09 77 <20 <20 10 1.54 1.35 1.98 0.07 0.11 72 <20 <20 9 1.41 1.25 2.:77>0.06 0.09: 6

<5 ;:2.20 266 <10 31::: 96 23 <20 <20 : 10 1.64 1.34 1.49 0.06 0.09 . <5 2.30 . 287 <10 ..29' 116 25 :: <20 <20:: 10 1.67: . 1.52 1:50::0.05 0.08:. _..._.._,....__.....

22 <20 <20 : 11 1,54 1.27 1:32:10.06 O. .<5'<2.08 239<:<10 30::95 <5 2.11 214 ; <10 33 :: 98 22 <20 <20 12 1.60 1 22 1.34 0.06 0.49

19 <20 <20 < 9 1.52 1 04 1.22 0.06 0.10'.> <5 <1.95 262::<10 49 < 78

<5 2.05 287 <10 53 92 17:;<20 <20:; 9 1.52 1 00 1.30 0.06 0.11 <5 2.00 206 <10 34 93 18 <20 <20 11 1.57 1 06 1:13:0.06:0.08;: 95 . <5 2.01 210 <10 33: 89 .19::Q0 <20. 12 1.49:1 10 1.63 0.05 0.09 86 <5 2.06 208 <10 .28> 91 20 <20 <20 12 1.62 1.10 1.18 0.06 0.07 102 <5 2.27 230 <10 29 78 18::<20 <20!; 13 1.35 1 03 1.83 0.06 0.119;: 70

4: <2 <1 <5<;<10 006:; 10 4:

<2 <1

<2 7:.: 1 ~Si <10 11..:09:, 9

<27; <1 ~'::<10 0.07:: 8

<1 <8;:<10 041, , 8 1 <5<10 <1 .<5::<10 <1 <5<10 p 08: 8 <1

:;<10 047; 10 9

'10;i <1 8 <2 10:<: <t <5::<10 0.08:: 8 <2 ..9.> <1 <5i<10 0.06:: 8

2.41 315 <10 40 83 21:: 2.32 298 <10 33< 88 24::

<5 2.08 272 <10 37 96 24;: <5 1.98 266 <10 4) 100 28:'

1.93 276:;<10 2.100 24:


SAMPLE

NUMBER

ELEMENT Au30 ]Ai ;; Cu Pb. Zn .Mo. Ni Co Cd .B

UNITS PPB PPMi:PPM PPMPPM PPM:PPM PPM PPM

As Fe

PPM P44C PCT

Mn Te Ba! PPM; PPM PPM

1.25 1 09 i;1$,<fl.06 67 4?:

1.41 1.32 1':20:>0.06 0.U8 :: 77

1.36 1.37 1.70'0.06 0.12':: 63

1.14 1.02 T:47;0.06 0.13:i 59 4::

1..74.1 91 1:33::0.03 O.Qi.;: 51

118 2.13 2.05 0.03 Il 06 :: 2.05 2.47 1.91 0.02 0.06 2.21 2.36 2.60 0.02 0.01 1.41 1.04 1.59 0.07 0.07; 1.33 1.10 2.09 0.06 0.06::

36::108 23::<20 <20; 4

24 €107 25::<20 <20 : 4

30 11125i;<20 <20; 6

36:105 23<QO 4

4137 37::<20 ~t0; 1

16 119 37 <20 <20<; 2 13 204 57 <20 <20 2 2.::136 54 <20 <20 3 20€ 80 22::<20 <20:: 10 19:: 59 19;:<20 <20 11

a Tt.: Zr PPM . PCT:;PPM

<10 041 1 :: 7 <10 p 11: 7

<10 0.11:: 8 <10 0.113:: 8 <10 0.14: <1

°<10 0.12:: 1

.<10 0.t3:: <1

<10 0. 12; <1 <10 0.07:: 7

<10

œR9936-1749 7 40 <2_ 27 n..2;; 36 13::<.2 <5: <5 1.45 227;<10 œR9936-1750 11 <2;; 24 <z: 31 <1;; 41 12<.2 <5: <5 <5 :1.58 283> <10

• œR9936-1751 12 <-,2190 28 2::42 liv.4.2 <5: <5 <5 i:1.82 263 <10 œR9936-1752 42 < Z;: 99 23 1>: 39 <51 <5 <5 s:1.9i 200:<10 œR9936-1753 8 <,,2s 47 43 <1:: 74 <5: <5 5 <2.36 466::<10

œR9936-1754 8 t234 <2< 44 e1;: 64 21;:<.2 <5 . c5 2.56 508;:<10 œR9936-1755 <5 <2; 2 40 1;; 98 22.;<.2 <5: <5 c5 2.95 660;<10 œR9936-1756 82 4124 42 2;115 <5; <5 <5 3.81 1445H0 œR9936-1757 91 c 2; 36 22 <t:: 27 10<.2 : <5 ~ 1.94 231<10 œR9936-1758 <5 <4; 2 <2s: 18 <t:;: 17 <5 ~ 1.49 ..1761<10

11010 Intertek Testing Services

Chimitec B ondar Clegg Rapport Lab Geochimie Geochemical Lab Report




Rapport Lab Geochimie Geochemical Lab Report ffis Intertek Testing Services

Chimitec Bondar Clegg CLIENT: CAMECO GOLD INC.




<1. <.2 <5':: <5 <5:<.01

<.2 <5> <5 <5;<.01

2 2'> 2

Te 88: Cr V':' Sn il; La

PPM PPMPPM PPM': PPM PPM<:PPM

r :;Y;: Ga AV Nb : SÇ: Ta Ti; Zr

PPM PPM ::PPM PPM>3PPM PPM :PPM pGTPPM

78

466

465

Oxide (Feldspar &

Nuiber of Analyses

Mean Value

Standard Deviation

Accepted Value

30 51 - 2.60 1200:::

CANMET STREAM-SED 4 - <,2>: 61

Number of Analyses Mean Value - 0 1<i 61

Standard Deviation -Accepted Value

<20 <20 2.76 1296:::<10 765:: 30 55':

3 2.76 1296 5 765 30 55<: 10

;0.04 0,

1

18 103j1.77 1::510.04

<10 0.07: <1

5 0,117; <1


As Sb Fe

PPM PPM?: PCT NAME

STANDARD ELEMENT Au30 Ag Cu Pb: Zn No: Ni CO Cd

UNITS PPB PPM1<PPM PI5I;PPM PPMI::PPM PPM ::PPM PPM

ANALYTICAL BLANK

ANALYTICAL BLANK

ANALYTICAL BLANK

ANALYTICAL BLANK

Number of Analyses

Mean Value

Standard Deviation

Accepted Value

Oxide (Feldspar &

Oxide (Feldspar &

Hunker of Analyses

Mean Value

Standard Deviation

<5 <.2;; <1 <1 i1!;: <1

<5 i.2>; <1 : <2>:: <1 <1F: <1

<5 -

<5

4 2

179

180

2

180

<1

O. :; 3' 3 :;:::;3;:<.01

1.0 2'i: 5 5::0.

Accepted Value 186

<10 e1';;; <1 p9. <20 <20:

<10 <1';: <1 '<Y<20 <20:

<1 <,01: <1 <. )1': < 01 <.01.: <.01

<1 <1;;: <2 <1,

<1 ~5::<10 <.01;: <1

<1 <2 <1 : <1 <5 ><10 <.0. <1

25 10 0.4 <5 12

1 1;> 1 1';! 1

25 10:0.4 3 12

82 2€ 23 11;:0.6 1

<1 <.01 <:ï11::>:<.01 <;SI'

<.01 <:01:::<.01 1.01::

2 ;~::: 2 :::~>; 2 2 2::: 2

<1 <.A1:: <1

<1

1

7

8 AO10

8 VIC 5 0'1

38 22;;0.3 <5

38 2Z:;10.3

7 <5 :4.21 758';<10

1

3::4.21 788::: 5


Geochemical Lab Report CLIENT: CAMECO GOLD INC.

REPORT: C99-62834.0 ( COMPLETE ) DATE RECEIVED: 29-SEP-99


STANDARD

NAME

ELEMENT Au30 Ag<: Cu Pb: Zn Ma;; Ni Co.:

UNITS PPB PPM PPM PPM<PPM PPMi:PPM PPM Cd .1u, As Sb.< Fe

PPM PPMI::PPM PPM: PCT

Te Be; Cr V:: Sn Y::: La

PPM PPM::PPM PPM::PPM PPF(PPM

Mg s; Ca' Na

PCT iPCT PCT

Sr Y::; Ga 'OW Nb SC;: Ta

PPM PPM::PPM PPM:<PPM PPM:: PPM .. Zr PPM

164 46 127 <20 8 2.71 1 65 1.06 0.05 0.30; 32 <20:. 0 5': 88 7: 70

- 0 7:> 90 11::: 80 Z`.: 40 18:0.

Oxide (feldspar &

952

Number of Analyses

1

Mean Value

952

Standard Deviation

Accepted Value 968

BCC GEOCNEM STD 5

Nurber of Analyses

Mean Value

Standard Deviation

Accepted Value

164 : 46 127:; 10 10:: 8 2.71 1.65 1.0b:0.05

4.74 720 <1 200 54 133 41':; 5 3-09 te-a, 1:08;0.06

0.30 32 11:;: 2

0.32 : 39 9

-

2 15~


DATE RECEIVED: 29-SEP-99 CLIENT: CAMECO GOLD INC. REPORT: C99-62834.0 ( COMPLETE )



<2:: 31 <2: 33

_ _.. 10 1.64 1.34 1.49 0.06 0.09;: 10 1.64 1.36 1.48 .0.06 0, 571! .:

<20 <20 9 1.52 1.00 1,30;:0.06 0:11 <20 <20 10 1.58 1.03 1.41 0.06 0.11

15 10 <.2 <5 <5 K5;'2.05 287 <10 53 92 15 10::<.2 . <5 <5 <5':2.13 . 289::<10 55; 97

12 1.23 1.00 2:08:0.06 0,0:: 61 .. 13 1.32 1.07 2.43 0.06 0.11:: 68

3 1.40 1.23 1:57:0.07 0.02 4 1.49 1.28 :.1.72::0.07 0 02:: _..

11 1.33 1.10 2.09 0.06 0.06

C8. Ti

Sn W La PPM PPMIPPM

Na

PCT Al: Mg

PCT PCT

14. <.2

11<.2 31 28

29 <V31

43 <2 27 <,2 CDR9936-1710 126 <.2. 43 c2 27 Duplicate

53 85 218:<10 218<10 53 86

29 <5:: <5 1>!2.20 28 14::<.2 <5.i <5 <5 2.32

<20 <20 14 1.47 1.01 1.19 0.07 0.07 32 92 14 13:::<.2 :<5 <5 <5:>2.06 222:f<10

17 .21<.2 ~5 19 25::<.2 <5

<5 i5::1.59 180<10 6 <5:':1.72 205_:<10

<5 <7.2 9 <.2<! 10


66 0;.2534 84 0.3;657

œR9936-1739 Prep Duplicate

4 <10 0:16: 4 <10 Or1..7

6 <.2 53 <2 : 24 <2.: [ 36 <;:.2.:: 54 <2 : 25 1.: 36

1.47 290:<10 1.56 2$l7i<10


11 ><.2 <5;:; <5

11::< 2 <5 <5 . <

<5 1.49 <.2 <10 17 18 76 21

ELEMENT Au30 Ag UNITS PPB PPM

. _.... __.... _ ... . _... Cu Pb;: Zn Ma:: Ni S:a.: Cd 8i=: As 8b; Fe Mn; Te

PPM PPK::PPM PPM`PPM PPM PPM PPM:PPM PPM:: PCT 4014-PPM

Cr 1f:

PPM PPM PPM

Ta T#.: Zr

PPM::PPM PPM:;PPM :PPM SAMPLE NUMBER


16 <,,L 9 <5 <.2:: 8

<5 . <5 > 2.25 . 305! : <10 . 65 > 118 <5 <5 2.29 306 <10 64 126

<20 <20 11 1.75 1 28 1.60 0.07 0.15 <20 <20 11 1.74 1.30 1.61 0.06 0.16

<1 <5 <10 0.08 11 <1 :-,55::.<10 0.08; 11

27 10:i<.2 <5; <5 <52.27 28 10<.2 <5 <5 <52.27

11 1.63 1.33 11 1.64 1 32 1.37

0.06 0.13 0.06 0 13

<1 '<5 <10 0:08.; 8 1 ~5':<10 0.08;: 8

CDR9936-1715 69 < 2:; 40 r2 37 <1 22 Duplicate 57

5 <5:2.48 10 55A 71 11 14.1.32 1.54; 0.06 0.17 72 <10 0 07< 9 .2

24 25 '.

24 25

<20 K20 <20 40

<20 <20

œR9936-1724 <5 <.2 29 Prep Dtplicate 8 4.2 30

266::<10 31:: 96 254<10 31' 99

<20 <20 QO op

<10 0.07: 8 <10 047; 8

<10 0 07. 10 <10 0.08; 10

<10 13;o7 10 CDR9936-1736 <5 <2 61 Duplicate <5

<10 0 <10 0

<10 œR9936-1758 Duplicate

_. 25:: 83 17:;<20 40

84 .19::<20 <20

131 32<20 <20. 140 *<20 <20

59 19<20 <20

1

<2 29 <2 3







REFERENCE: 170416

CLIENT: CAMECO GOLD INC. SUBMITTED BY: D. BASIN PROJECT: CEDAR RAPIDS

DATE RECEIVED: 07-OCT-99 DATE PRINTED: 21-OCT-99


NUMBER OF ANALYSES

LOWER DETECTION

991012 1 Au30 Gold 51 5 PPB 991012 2 Ag Silver 51 0.2 PPM 991012 3 Cu Copper 51 1 PPM 991012 4 Pb Lead 51 2 PPM 991012 5 Zn Zinc 51 1 PPM 991012 6 Mo Molybdenum 51 1 PPM


991012 13 Fe Iron 51 0.01 PCT 991012 14 Mn Manganese 51 1 PPM 991012 15 Te Telluriun 51 10 PPM 991012 16 Ba Barium 51 1 PPM 991012 17 Cr Chromium 51 1 PPM 991012 18 V Vanadium 51 1 PPM

991012 19 Sn Tin 51 20 PPM 991012 20 W Tungsten 51 20 PPM 991012 21 La Lanthanum 51 1 PPM 991012 22 Al Alumirnm 51 0.01 PCT 991012 23 Mg Magnesium 51 0.01 PCT 991012 24 Ca Calcium 51' 0.01 PCT

991012 25 Na Sodium 51 0.01 PCT 991012 26 K Potassium 51 0.01 PCT 991012 27 Sr Strontium 51 1 PPM 991012 28 Y Yttrium 51 1 PPM 991012 29 Ga Gallium 51 2 PPM 991012 30 Li Lithium 51 1 PPM

991012 31 Nb Niobium 51 1 PPM 991012 32 Sc Scandium 51 5 PPM 991012 33 Ta Tantalum 51 10 PPM 991012 34 Ti Titanium 51 0.01 PCT 991012 35 Zr Zirconium 51 1 PPM

SAMPLE TYPES NUMBER SIZE FRACTIONS NUMBER SAMPLE PREPARATIONS NUMBER EXTRACTION METHOD

DRILL CORE

51 -150 51 CRUSH/SPLIT & PULV. 51 Fire Assay of 30g 30g Fire Assay - AA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA REPORT COPIES TO: fl6-1349, KELLY LAKE RD. INVOICE TO: AU6-1349, KELLY LAKE RD. HCL:HNO3 (3:1) IMDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA

********************w***********,t***w************,t***w**********w******LA******* HCL:HNO3 (3:1) INDUC. COUP. PLASMA

This report must not be reproduced except in full. The data presented in this report is specific to those samples identified under "Sample Number" and is

HCL:HNO3 (3:1) INDUC. COUP. PLASMA

applicable only to the samples as received expressed on a dry basis unless HCL:HNO3 (3:1) INDUC. COUP. PLASMA

otherwise indicated

HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) IMm1C. Coup. PLASMA

HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) IMDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA

HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) 1MDUC. COUP. PLASMA

HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA



InjIntertek Testing Services Chimitec Bondar Clegg

CLIENT: CAMECO GOLD INC. REPORT: 099-62921.0 ( COMPLETE )

PROJECT: CEDAR RAPIDS DATE RECEIVED: 07-OCT-99 DATE PRINTED: 21-OCT-99 PAGE 1 OF 5

UNITS PPB PPM PPM PPN SAMPLE ELEMENT Au30 Ag` Cu Pf

NUMBER

<5: <5:

<5

<5:

2.05 200i;<10 4.71 641.'s<10 4.29 539<10 4.12 575<10 6.34 396:i <10

<5.: <5 <5:: <5 <5:;: <5 ~<5: <5 <5:: 15

~

~b e5

~

<,5

<5 2.90 <5:':2.98 <5 3.36 <5 3.05 <5 4.75

Zn Mo;; Ni Co: Cd Bi;; As Sb:

PPM VPM::PPM PP4:::PPM PPAt`:PPM PRM

Fe Mnj Te Ba Cr V Sn f1 La At qWi Mg PCT PPM: PPM PPM PPM PPM PPM PPM PPM PCT.;:: PCT

Na . M:: Sr . Y:: Ga L(::

PCT PGT::PPM PPik:,:PPM PPIi: Ta Ti Zr

PPM PCI PPM Nb Sb:

PPM PP'F1:

CDR 9936-1759 22 0;2!: 15 '52 27 23 6. <.2 CDR 9936-1760 197 <2: 7 4 22 24 9<.2

CDR 9936-1761 179 <,2 ' 48 <2: 31 21 8.<.2 (DR 9936-1762 5 <.2,> 22 29 3> 24 9-4.2 CDR 9936-1763 <5 <.2:: 13 <2 25 11 27 9: <.2

CDR 9936-1764 47 < 2>: 68 <2;: 25 <1 26 1Dî <.2 (DR 9936-1765 18 <.2: 37 <2 29 ti 33 10 <.2 CDR 9936-1766 47 <.2:: 44 <2 26 29 9 <.2 CDR 9936-1767 96 <.2i: 54 <2:1 26 25 8 <.2 CDR 9936-1768 <5 <„ 2 ; 4 <2 27 25 <.2

CDR 9936-1769 135 0.3:: 860 <2>; 30 6: 25 I9<<.2 CDR 9936-1770 20 K.2 5 <2 26 . 1::: 24 81:i<.2 CDR 9936-1771 994 <,2:; 120 <2: 27 <1:> 24 12:<.2 CDR 9936-1772 <5 <.2> 4 <21: 25 <1: 23 10i:'<.2 CDR 9936-1773 6 <,2: 10 <2 20 <#;< 15 14!.:<.2

CDR 9936-1774 56 < 2: 123 <2.: 23 1:: 15 20:<.2 CDR 9936-1775 301 0.3' 319 <2;:: 50 6;: 79 37:<.2 CDR 9936-1776 950 0.5: 669 . 52;: 47 4: 88 27:<.2 CDR 9936-1777 127 0.i: 318 . <2: 4s .. 6 82 3i1<.::<.2 CDR 9936-1778 1062 24:5265 54 36:138 389.2

(DR 9936-1779 88 1.2: 185 44 35 55 33'. <.2 CDR 9936-1780 86 <.2!' 201 <2>: 40 65 22. <.2 CDR 9936-1781 173 <,2: 268 <2s 41 69 34; <.2 (DR 9936-1782 55 0.2:: 86 <2 38 61 34: <.2 CDR 9936-1783 96 0.3 < 105 <2:I: 50 81 102'. <.2

CDR 9936-1784 53 <,2i:: 3 <2<; 38 6 54 41 <.2 CDR 9936-1785 <5 <.2 ':: 2 <2>: 29 4 45 27 <.2 (DR 9936-1786 <5 0.2!: 3 <2's 37 20 51 31 <.2 CDR 9936-1787 196 0.3: 400 <2 41 28 58 53 <.2 (DR 9936-1788 35 <.2s 13 <2 34 18 60 106 <.2

14: 77 15: <20 <20 9 1.53 1.07 2.47 0.05 0,06::: 58 <2 12: <1 <10 4.41:. 5

16: 88 14. <20 <20. 8 1.45 0.95 3.30 0.04 0.10,: 59 3; <2 11:; <1 <10 < 01;! 5 13. 89 16 <20 <20 7 1.54 1.05 3,45;0.05 0,08;: 56 2':;I <2 12 <1 <10 < 01: 4 15:.. 88 21 <20 <20 8 1.73 1.24 2.60 0.05 0.06 55 3;:: <2 13. <1 <5 <10 0.02'< 5 18; 88 24 <20 <20 10 1.99 1.31 1.56 0.05 0.06; 70 <2 13:i <1 As <10 4f 7

.,,..,.. _ _.. :19: 89 :22 .:<20 <20 8 1:76::1.26 1.65:::0.05 0.06: 59 3:< <2 1 21! < <10001< 6 11014 28 <20 <20: 8 2.041.53 1.73<0.04 0.06:: 58 <2 13:! 1 <5: <10 0,01':: 6 18 93 ,24 <20 9 1.93:1.37 1:, 24!0-04 0.06 56 3 <2 12:: <1 <5: <10 0,04 7 161 78 ..22 <20 <20 9 4:.83:1.28 1,15:0.05 0.05: 63 3< <2 1 1:. <1 <5 <10 0.03> 7

..16. 97 22 <20 <20'.. 8 1.80.11.25 1.34<:0.05 0,05.: 65 3; <2 1: <1 445; <10 0.04 7

24..85 :41<20 <û . 9 1:78 1.28 1.95 0.04 0 08<' 47 <2 1 1::: <1 <5I':<10 0.02 6 16. 98 '20<20 <20: 10 1:66 1.19 1.52 0.05 0.05 64 3 <2 1 Q;; <1 <5;<10 0.04< 7 21:: 80 .24.<20 <24 9 1085 1.31 1.40 0.04 0,07: 56 3 i <2 1 <1 <<10 063: 7 16 92 ..:20:<20 <20 9 1.72 1.23 1.09 <0.05 0.05 61 : <2 1 1: <1 <5;<10 6* 7 18; 86 13.<20 <20 7 1.53 0.91 1.08 0.05 0.07 66 <2 9: <1 <5 <10 (64Y. 9

86 14 <20 <20 08 1,51 1. 04 1.39 0.04 OM 51 <2 9':: <1 <5:<10 C 03. 7 186 .5b <20 120: 2 3.39 2.84 3.34 0.02 .4.01 57 2.I <2 26:: 2 <5:<10 0.05 : <1

3; 175 51 <20 <20 3 2.93 2.44 2.97 0.03 0.01 51 <2 2 <5::<10 0.06: <1 4;196 56 <20 <20 4 3.29 2.82 3.21 0.03 0.01 52 3: <2 25:: 2<S;<10 0.06. <1 13:152 411 <20 <20 6 a.74 2.35 ;1 63 0.03 0.04': 28 2:;I <2 21;: <1 <5;:<10 0.06. <1

5 129 43 <20 <20: 3 2.38 2.17 2.71 0.04 0,01;: 50 2 <2 17 2 <5.><10 00: 1 <1::150 56 <20 <20 3 2.63 2.57 2.93 0.03 <.01:,; 50 2 <2 18 3 '.<5<.10 0. 07 `: 1 1:145 .50 <20 528 3 2.55 2.48 2.51 0.03 <,01: 50 2 <2 17 2 <5<10 0,07:: <1 1;:143 49: <20 <20 3 2.29 2.25 2.60 0.04 <.01:: 47 . 2 <2 16 2 <.5i„i<10 0.07: 2 3 164 52 <20 <20 3 2.79 2.52 $ 04 0.03 <.01:: 54 2 <2 18 2 <5i'::<10 0,06< <1

131 45 <20 <20 4 2.29 2.14 2,48 -0.04 < fl1:;; 48 <2 1b 2 <5;:<10 007:: 1 3 131 36 <20 <20. 3 1.80 1.71 3.66::0.03 <,01; 65 2 <2 13 2 .<5<<10 00 1 4 132 .42.<20 <20 3 2.36 2.31 4.91 0.04 0 01; 46 3i <2 18`:' 2 <5> <10 0.08ü <1

16 121 38 <20 <20 3 2.48. 2.24 3.08>0.03 0.04>: 50 2I <2 18 1 45::<10 0.07:: <1 17 123 33 <20 <20 3 1.82 1.76 2.670.04 0.03> 48 <2 12 1 <5:;<10 0 07: <1


Ça

PCT

<5 <5< <5

<5.:: <5 45: <5 <5:: <5

<5: <5 45.:: <5 <5:: <5 b < <5 <5' <5

<5;; <5 <5:2.62 237:<10 <5 : <5 <5 1.98 222 <10 <5;: <5 55;2.34 .210;<10 <5: <5 <5;12.05 206t<10 <5:> <5 <5::11.80 167.<10

<5 <5 <5 3.16 412 <10 <5 : <5 <5 1.77 423 <10 <5 <5 <5;:2.49 425 <10 <5 <5 <5:>3.51 457 <10 <5 <5 <5 3.10 371 <10

1.79 2.05 2.19 2.07 2.34

234 285; 297 266 221i'.

<10 <10 <10 <10 <10

<5>; 2.02 <52.49 <5'2.35 <52.15 445:2.16

_.....,. 410<10 243 <10 196<10 215<10 223:<10

422 506 481 421 534

<10 <10 <10 <10 <10





Mg Ca: Na PCT PCT:: PCT

Fe Mlti Te 8a Cr :;V Sn La PCT PPM PPM PPM PPM PPMI PPM PPM PPM

K. Sr HC. Ga L#,;: Nb SC,: Ta Tf i Zr PCi:.>:PPM Pp1#:; PPM PPl1`PPM PPM1>:PPM PCi;:',PPM

SAMPLE ELEMENT Au30 Ag Cu Pb Zn 110:' Ni Co Cd Bi As Sb

NUMBER UNITS PPB PPM}: PPM PPM PPM PPM: PPM PPM:: PPM 141 PPM PPM:

2 :a

<2 1t. <2 13.. <2 11; <2 10 <2 .16

33 1$ d 14 7:

138 25.::<20 <20 104 30i<20 <20. 138 3.9.. <20 <20 114 ::.:33<20 <2Q. 116 40 <20 <20

2 2>

<2 14 <1 <5;.<10 0.04;i <1 <2 11:; 1 <5, <10 0 06;; <1 <2 12<; 2 <5<10 0.08:: <1 <2 11;: 1 <5;<10 0 Q8:: <1 <2 1fJ:: 2 <5:<10 0.09i: <1

<5 <5 <5 <.5

<5 <5 2.75 407 <10 : 9 126 36 <20 <20 <5 <5 2.59 379 <10 15 106 29 <20 <20 <5 <5 2.59 423 <10 10 144 27 <20 <20 <5 <5:2.81 405 <10 10 119 .33 <20 <20 <5 <5 3.20 594 <10 7 145 46 <20 <20.

2:; <2 3;: <2

3> <2

13:. 14<:

7.; 7>

<5 <5

2 3 <1 <1

3 27 26

<5

<10 0 07:: <1

<10 0.10:'. <1

<10 0,05 : 3

<10 0,04. 5

<10 0.05: i <1

.. _. . _.__.. 159 48 <20 <20 183 102 21' <20 90 :15: <20 <20 184 '60<20 <Zfj

<5 <5;::4.32 662;:i<10 <5 <5 3.86 589 <10 <5 <5.? 2.53 330 <10 <5 <5 2.58 291 <10 <5 <5.; 4.44 577 <10

1 2.80 2.51 2.56 0.03 0,04:: 49 2 3:04.'2.64 2.24 >0.03 0.02 64 6 1.82 1.24 1.% :' 0.04 0,14 :: 67 7 1.67 1. 06 2.26 0.04 0.16 : 67 4 2.95 2.47 2.52 0.03 0.04> 74

<5 é5 3.87 161 .32: <20 <20 <1 2.93::;2.42 2.50;0.02 0.04 <2 .869:-.<10 <10 0.09 <1

CDR 9936-1792 5 < 2: 70 <2 45 <1 84 CDR 9936-1793 <5 < 2:; 7 4 55 1': 85

CDR 9936-1794 297 0.5:;i 810 <2 52 2 84 86 <.2 CDR 9936-1795 40 0.3 171 <2 32 <1 : 53 32 <.2 CDR 9936-1796 <5 <.2 24 <2;! 32 <1 55 13 <.2 CDR 9936-1797 15 <,2 68 <2 31 .<1:> 56 28 <.2 CDR 9936-1798 <5 e,2s: 2 <2 32 <1 56 11;<.2

CDR 9936-1799 <5 c 2.:: 4 35 54 I1:<.2 CDR 9936-1800 <5 <.2<: 4 37 . 1: 56 17;:<.2 CDR 9936-1801 36 (43: 277 <2> 36 <1<i 52 16<.2 CDR 9936-1802 7 <.2 11 <2 37 2': 60 23<.2 CDR 9936-1803 <5 <:2' 3 ~ 52 1 : 71 25;<.2

CDR 9936-1804 17 <.2:: 6 <2 60 <1`; 68 51:;<.2 CDR 9936-1805 16 < 2> 35 <2: 55 <1> 68 26'><.2 CDR 9936-1806 71 <.2;. 83 +2>: 39 ::',.<.0 > 42 17.:<.2 CDR 9936-1807 5 <.2< 35 <2`: 33 <1; 36 13 :<.2 CDR 9936-1808 <5 <, 2 : 53 <2 ; 5.8,:!& 73 49!:<.2

CDR 9936-1809 17 <.2< 361 <2> 94 79 ;25;:<.2


CDR 9936-1789 CDR 9936-1790 CDR 9936-1791

15 <,2_ 120 14 <.2!: 55 15 0.31; 92

<2 37 <1: 60 <2; 51 .<1 91 <2; 44 <1 78

<5 <5;2.01 412 <10 ;6 130 <5 <5 2.98 505 <10 2 215 <5 <5 2.46 580 <10 : 7 195 <5 <5 2.54 517 <10 . ..2 204 <5 <5::3.38 522 <10 ..2 185

_... __. 41:<20 <20 4 2 :06;:2.08 2 77:0.04 0 01; 63 351 <20 <20 6 2.b7 2.62 1.%:0.03 <,01 65 42 <20 <20 7 2:34 2.31 3t51'.0.03 6.41' 84 41 <20 <20 6 2:46 2.41 2.32;0.03 71 43 <20 <20 6 3..24 3.28 1.95;;0.02 ~.01:: 52

2 <5<10 1 5'..<10 046:: 1 2 <5<10 0 05:; <1 2 <5<10 0 06'; 1 1 <5;:<10 0.05 <1

<5 <5 <5 5.49 416 <10 <5! <5 .<5>2.95 321 <10 <5:i! <5 .<5:i2.77 298:<10 <5 <5 .<5<2.99 247 <10 <5 <5 <5::2.68 345!<10

2 2.74 2.42 2.01 0.01 011:: 38 1 2.16 1.83 1.99 0.03 0.07> 51 1 2.38..1.97 1.80:::0.04 0,03:: 67 1 2.29 1.83 1.40 0.03 0.08`: 64 1 2.26 1.96 ;1 95 0.04 0,04<: 53

1 2:27>1.96 a44 0.04 0 06.:: 51 3;< <2 10:: 2.<5:<10 0,08s:: <1 1 2.a7 1.86 1.70 0.04 0,08!< 42 2< <2 10 : 1<5<10 0,0i:: <1 1 2.101.79 a.40 :0.03 0* 53 2:: <2 9:: <1 <5.<10 0 06: <1 1 60.95 :69::0.04 0.A6:: 59 . 2< <2 . 10> 1<5<10 0.08<: <1 1 2.542.22 2 30;0.03 0.04 59 4: <2 11< 2 <5<10 0.095 <1





DATE RECEIVED: 07-OCT-99 DATE PRINTED: 21-OCT-99 PAGE 3 OF 5

STANDARD ELEMENT Au30 Ag Cu Pb, Zn I Ni Co; Cd B : As Sb

NAME UNITS PPB PPM:: PPM PPM: PPM PPii:PPM PPMPPM PPM PPM PPM

Fe Mtti; Te .Ba Cr V Sn . u La Mg ! Ca- Na 1(; Sr Y Ga LI Nb Sc T

PCT PPM PPM PPM PPM PPM PPM PPM. PPM PGT PCT >'CT PCT PCT ::PPM OS. :sPPM PPM PPM PPM; PPM

ANALYTICAL BLANK <5 <.2`; <1 <2€ <1 <l <1 <1'';<.2

ANALYTICAL BLANK <5 <.2 <1 <2 <1 <1<. <1 <1:';<.2

ANALYTICAL BLANK <5 - - -

Number of Analyses 3 . 2'I 2 2. 2 2; 2 2i 2

Mean Value 3 0.1 ! <1 1 <1<'. <1 <1: 0.1

Standard Deviation

Accepted Value 5 0.2 1.



Mean Value 179


Accepted Value 186

BCC GEOCHEM STD 5 - 0.6ii 100 7 88 <1!i 39 21>:0.3 Number of Analyses - 1: 1 1 1 1 1 ';

Mean Value - 0,6,' 100 7 88 39 21'::0.

Standard Deviation

Accepted Value - 0.. 90 80 2::: 40 1g:0.1



Mean Value 462


Accepted Value 465


Number of Analyses 1 Mean Value 2958


Accepted Value 2940

<5:,

<5

<5

<.01

<.01

2

<.01

0.05

41<10

<T:<10

2; 2

<11: 5

..1> <1

<1 <1'

2

+t1:

<1

<1

2

<1

1

<.1

Z <.1

<20 ~2Q

<20 <20

2 2

10 10

<1 <1

2

<1

<1

<1 <.c01: < 01 <.OY;<.01 <,p1,!; <1 <1 01

<01<.01 <.01 <.01 > <1 <1 : <

<2 <1 <5<10 <4t: <1

<2 <7,<; <1 <5<:<10 <.01; <1

2 '2;; 2 Z; 2 . 2ç< 2

1 <1 !: <1 3';: 5 ,41:: <1


<2 25:>: 7 10<10 0:1

1 25,:: 7 11): 441 6

1 18; 1 9

2: 2 :; 2;: 2 2; 2

<;.01 < 01 <.01':<.01 <1

<1 <.0'1:

7 <5 '.4.77 ?:40 :,<10 11x3> 57 121<20 ~2i1 6 3.48 1 1 1 7

3 7 3 ::4.77 5 163. 57 125 10 10 6 3:48

1;: 8 4.74 720;: <1 200: 54 13$:: 5 3:09

1.70 0.93 0.05 0.30;: 31 1 1::

1 1; 1

1.70 0.93 0.05 0.30 31

:1.83 1.08 0.06 0 32 39

REPORT: C99-62921.0 ( COMPLETE ) DATE RECEIVED: 07-OCT-99 DATE PRINTED: 21-OCT-99 PAGE 4 OF 5

STANDARD ELEMENT Au30 :Ag. Cu Pb Zn Mb Ni CO Cd Bi As Sb Fe

NAME UNITS PPB PPM' PPM PPMI<:PPM PPM PPM PM PPM PPMsPPM PPM PCT

M1n:; Te 8a: Cr tit; Sn La

PPM.::PPMPPM4` PPMI PPM' PPM PP~F: PPM

Mg Ca;' Na

PCT :PCT: PCT

Sr Y; Ga Lï : Nb SC:' Ta

PPM PPM PPM :PPM 1lN;PPM 1.f.% Zr

KT :PPM

CANMET LAKE-SED 2

Nu ter of Analyses

Mean Value

Standard Deviation

Accepted Value

23 16;;0.9 <5, 10

1 .1> 1 1 1

23 16:;0.9 3' 10

23 17::0.8 9

3.34 1752 <10 213 29

1 1<; 1 1:; 1

3.34 1752 5 21$1 29

3.50 1840::r;

<20 <20 54 1.650.59 Q 5.530.03 0.2a 27 28;:: <2 16i: 4 5 <10 0.05 2

1 1: 1 1 1 1:: 1 1 1 i:; 1 1:; 1 i; 1 1: 1

10 54 1.63 0.59 0.55 0.03 0,22 27 x0; 1 16 4 5 5 0.05 : 2

44 204

44 204

29 200

- 0 3;:: 36

1; 1

- 4 36

- 0.8:: 36


10M Intertek Testing Services Chimitec Bondar Clegg Rapport Lab Geochimie






_._ . .. SAMPLE ELEMENT Au30 Ag::: Cu Pb::: Zn 14o::; Ni Co Cd BI As 'Sb Fe NUMBER UNITS PPB PP)#:: PPM PI* PPM PPMI::PPM PPMI:' PPM PPM PPM PPM PCT

DATE RECEIVED: 07-OCT-99

Mrti Te :B$. Cr V Sn Tlir La Al< Mg

PPM PPM PPM PPM PPM PPMPPM PCT. PCT


Sr . ;Y.;: Ga Ci ;: Nb §t ; Ta TI Zr PCT PET >PPM PPM PPM PPtt>:PPM PPit:>PPM PC': PPM

CDR 9936-1760 197 <.2 7 <2 22 <1:' 24 9 <.2 <5 <5 <5':2.05 :285',<10 18 88 14 <20 <20 8 1.45 0.95 3.30 0.04 0 10 59 <10 4 0t :: 5 Duplicate 217 0.4 7 <2 22 <1.!; 24 9:<.2 <5 <5 <5 2.00 283; <10 17. 86 '14:::<20 <20 8 1....8-93 3. 27 0.04 0.10 59 <2 <10 < OI; 4

CDR 9936-1778 1062 2.3 5265 <2 5436!:138 389 <.2 <5 : 15 <5! 6.34 396':<10 13 152 41 <20 <20 6 2.74 2.35 1.63 0.03 0.04;: 28 <2 2:1 <1 <5,;<10 p:06:: <1 Duplicate 2 3.;5211 <2;; 55 36 138 388:;<.2 <5? 17 <5 6.17 388 <10 14 155 41 <20 <20 6 2.71 2.29 1.59 0.03 (1 04; 28 2 21 <1 <5;<10 0 05; <1

CDR 9936-1782 55 0 2: > 86 <2 38 2;:; 61 34 <.2 <5 <5 <5:'3.05 421;<<10 143 <20 <20 3 2.292.25 24,0 0.04 <,01:: 47 <2 2 <5.<10 041T 2 Duplicate 64

CDR 9936-1791 15 0.3 92 <2 < 44 <1 78 13'<.2 <5 <5 <5: 2.46 580 <10 T.195 >42 <20 <20. 7 2.34 2.31 3.51:0.03 0.01 84 2 <2 2 K5;;<10 (405. <1 Prep Duplicate 11 0.2 97 <2 47 <1 82 15,<.2 <5, <5 <5 2.65 623 <10 7219 47' <20 <20 8 2.54 2.47 3.78 0.03 0 02.: 97 3; <2 2 <5>:<10 0;* <1

CDR 9936-1797 15 <,2« 68 <2' 31 <1< 56 28•<.2 <5 <5 <5 2.99 247 <10 14. 114 33. <20 <20 1 2.291.83 1 40>0.03 008 64 2 <2 <10 04k <1 Duplicate 0.2 70 <2 32 <1 ; 57 285;0.2 <5 <5 <5 ::3.03 251 <10 14 116 33 <20 <20 1 2..331.89 144`;0.04 008: 64 <2 <10 0* <1

CDR 9936-1803 <5 < 2:; 3 <2;i 52 1 71 25<.2 <5 <5 <53.20 .5942<10 7;145 <20 2.54 :2.22 2.30:0.O3 0045: 59 <2 2 <5 <10 0 09,: <1 Duplicate <5


SAMPLE TYPES NUMBER SIZE FRACTIONS NUMBER SAMPLE PREPARATIONS NIMBER

Fire Assay of 30g 30g Fire Assay - M HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) IMDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASM HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA

HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) IM)UC. COP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA

EXTRACTION METHOD DRILL CORE


REPORT COPIES TO: )16-1349, KELLY LAKE RD. INVOICE TO: MI6-1349, KELLY LAKE RD.

*,tie*,eira**** **,nlr*** trt********* rrt*,k rirye **** *,rieir,irkVn nk** rwrt,t rintinr *** This report must not be reproduced except in full. The data presented in this report is specific to those sanples identified under "Sample Number" and is applicable only to the samples as received expressed on a dry basis unless otherwise indicated

HCL:HNO3 (3:1) IMDUC. COUP. PLASMA HCL:HNO3 (3:1) IMDUC. COUP. PLASMA HCL:HNO3 (3:1) IMDUC. COUP. PLASMA HCL:HNO3 (3:1) IMDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) IMDUC. COUP. PLASMA

HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) IMDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA

HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASM HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA

HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA HCL:HNO3 (3:1) INDUC. COUP. PLASMA




CLIENT: CAMECO GOLD INC. SUBMITTED BY: D. BASIN




NUMBER OF ANALYSES

LOWER DETECTICN

991018 1 Au30 Gold 50 5 PPB 991018 2 Ag Silver 50 0.2 PPM 991018 3 Cu Copper 50 1 PPM 991018 4 Pb Lead 50 2 PPM 991018 5 Zn Zinc 50 1 PPM 991018 6 Mo Molybdenun 50 1 PPM


991018 13 Fe Iron 50 0.01 PCT 991018 14 Mn Manganese 50 1 PPM 991018 15 Te Telluriun 50 10 PPM 991018 16 Ba Barium 50 1 PPM 991018 17 Cr Chramiun 50 1 PPM 991018 18 V Vanadium 50 1 PPM

991018 19 Sn Tin 50 20 PPM 991018 20 W Tungsten 50 20 PPM 991018 21 La Lanthanum 50 1 PPM 991018 22 Al Aluminum 50 0.01 PCT 991018 23 Mg Magnesiun 50 0.01 PCT 991018 24 Ca Calcium 50 0.01 PCT

991018 25 Na Sodiun 50 0.01 PCT 991018 26 K Potassiun 50 0.01 PCT 991018 27 Sr Strontiun 50 1 PPM 991018 28 Y Yttrium 50 1 PPM 991018 29 Ga Galliun 50 2 PPM 991018 30 Li Lithium 50 1 PPM

991018 31 Nb Niobium 50 1 PPM 991018 32 Sc Scardiun 50 5 PPM 991018 33 Ta Tantalun 50 10 PPM 991018 34 Ti Titanium 50 0.01 PCT 991018 35 Zr Zirconiun 50 1 PPM



Or Intertek Testing Services Chimitec Bondar Clegg

SAMPLE NUMBER

ELEMENT Au30 Ag Cu Pb Zn I4D Ni COl:: Cd Bi As SID Fe UNITS PPB PPM PPM PPM:' PPM PPM:: PPM PPM>PPM PPM PPM PPM PCT

45 6

<.2 <5;i: <5 la. <.2 <5:: <5 15 <.2 <5;; <5 27 <.2 . <5:: <5

26 <.2 <5: <5

309 o 7;: 225 250 2: 6 0,2 99 0.9

462 <2 60 90 54 12 <2 50 11 <2 56

505 <2: 64

93 18:0.2 81 24 <.2 43 17'j<.2 64 16 <.2 82 41<.2

1;

<11'

2

<.2 <5: <5 <5 3.61 <.2 <5: <5 ..<5>:4.07 <.2 <5 5 îS::4.30 <.2 <5 <5 K5::4.11 <.2 <5: <5 4::5.01

<5!> <5 .+5)6.54 <5!:: <5 <5<.:5.01 r,5:::; <5]-.:]'<5]:,.3.57 4] ~<5]::4.23 *8: <5 <54.89

PROJECT: CEDAR RAPIDS DATE RECEIVED: 07-OCT-99 DATE PRINTED: 29-OCT-99

Mr Te 8â Cr ;;V Sn 1. La 'AL ' : Mg C8:> Na

PPM PPM PPM PPM PPM PPM PPM PPM ?qv:, PCT PCT;: PCT

PAGE 1 OF 5

Zr

PPM

: 723 <10 17 151 36 <20 <20 3 2:85;<2.36 4.14 0.02 0.12>; 96 5 .18; 1 _... <10 0..11;: 1 728 <10 15 190 47.<20 <20 3 3.10 2.58 4.03 0.02 0.10 108 6 19' 2 <1 669 <10 14 163 47 <20 <20 3 3.01 2.48 3.56 0.03 0.10> 96 6 19 3 e5

<10 013:; 1 593 <10 18 117 39 <20 <20 3 2.68 2.08 3.51 0.03 0.17 95 5 17. 2 <5}<10 0* 1 439 <10 11 99 40 <20 <20 3 2.20 1.69 2.64 0.05 0.10 83 614';; 2 <$:<10 0.15:`; 1

452 <10 19 90 28 <20 <20 3 2:30 1.74 2.87 0.03 0.19 77 3: 5 141> <1 <5:><10 O' 12:: 2 426 <10 17 68 30 <20 <20 3 2:32:1.72 2.63::;0.03 0.20:: 47 4 1 <5:<10 3 380 <10 10 79 34 <20 <20 4 2.32 1.68 2,21:0.04 0.15:: 51 3:< 5 15; <1 <5;;<10 2

366 <10 1$ 74 33 <20 <20 4 2.31 1.62 2.51 0.04 0.23 67 3< 5 14!:: 2 . <5:::<10 3 436 <10 1S. 104 38 <20 <20 4 2.42 :1.72 278):0.03 0.27 67 3' 5 2 <5:;:<10 0.171: 3

:467 <10 13: 88 34 <20 <20 3 2.29 1.67 2.49>0.04 0.21 52 4 14 2 <5<<10 04 2 .564::<10 13:103 45::;<20 <20 3 2.54.:1.90 2.95 0.03 0.24 53 5 .16 2 <5'::<10 0.14< 2 57?;<10 13 95 35 .<20 <20 4 2,44.:1.83 3.16:::0.03 0.23 54 4 16: 2 <5::<10 0,12: 3 5731<10 16;,108 .3.8»:<20 <20 3 2:77.. 2.12 2.93 0.03 0.30 61 5 18: 1 2 bb0'<10 40 185 4.8.<20 <20 4 3.37 2.58 2.96 0.03 0 81: 66 5 21 4i5::<10 0.23:: <1

827<10 24144 67 <20 2 3:492.63 4,08`0.02 0,52: 63 4 22';< 3 <5:;<10 0,17; <1 T20 <10 17:160 44 <20 <21 4 3.15 2.37 4 55:::0.02 0.30':' 80 5 AP:, 2 <5<10 0.17:! <1

:449. 10 15101 30 <20 +t2Q 3 230:1 65 2;73,0.03 0.:$6: 65 : 4 12:; <1 K5::<10 0.12:: 2 :553.<10 16134 54 <20 <20: 5 2.85 >2.17 2.560.04 0:36:: 76 6 16: 3<5;::<10 0 2Q:: 2

.590' <10 .4071 52 <20 <2p 4 3.132.41 2.44'0.02 0,77:': 56 5 18:: 2 0:07. 1

__...

.. .... _.. _ ... 684: <10 31232 61f <20 <20 3 326: 6 14 3 :<5:::<10 0.17<: <1 0.9.,..i<10 16:.191 38<20 _._ .. 4 2.66 2.05 4.73;:0.02 _... 0.28 z 73 3 5 15 : 2 <5 <10 0.13 <1 417 <10 86 .4.0..<20 4 04 1.54 2.22:; 0.04 01$: 60 ~!.; 4 :Î: 2 <5 <10 0.17.; 3 411:::<10 81 J6'..<20 0 5 I:95 1.37 2.52 0.04 0.16; 58 4;; 47:: 2<5:<10 016:: 4 4042:700 15' 85 4c4 <20 11 2:09 1.42 288::0.04 0.20:: 69 5::: 5 8::: 2 <5 <10 0.16 5

__.. _..... _. _....... 497:i<10 25::. 85 19 <20 '420 9 1.82 1.17 3.94 0.02 _:... 0.25:: 87 5;: 3 =r <1 {5:::<10 O.iQ:: 6 519.<10 16 105 39 <20 <20 7 2:39;:1.63 3.17 0.03 0.2'f:: 63 . 4: 5 10]> 2 0.14< 3 630<10 27 155 67 <20 <20 3 3.24 2.63 2.72: 0.03 0.38:: 64 3":: 5 1.6; 5 0.23:< <1 533:<10 34:.165 57 <20 <20. __._. 5 2.99 2.32 2.38: 0.03 _....... ?0.46> 70 3<; 4.13:€ 3 ..<5><10 0.22:!: <1 52dî:<10 14 145 .49:<20 <20 4 2.72 2.25 2.58 0.03 0.16" 60 3:. 4 12:: 3<5;:<10 0.19'; <1




15 0,4:! 86 18 0.3:'. 10 8 03:: 6 <5 0.3 13 <5 0 2:: 6

<5 <,2 4 9 0.3>I 113 13 0 3 112 <5 0.2` 20 <5 0.3 13

70 .2: 82 81 2<:104 79 1<: 94 74 1; 73 62 1 51

59 <1:; 49 49 1,!; 47 48 1;: 42 42 .' 1 : 42 46 2: 48

28<.2

16;<.2 15::<.2



<5 0 2f: 18 <2;: 44 18 0.2 54 <2::: 54

395 2.0:2605 <2::: 69 <5 0.3>: 37 2:: 57 30 0.4`< 134 3:! 49

46 55 58 63 88


CDR 9937-1835 (DR 9937-1836 CDR 9937-1837 CDR 9937-1838 CDR 9937-1839

15 0,2. 20 8 D.5> 35 35 0.3: 88 88 0.5 119 118 0;2; 34

240 44:: 33 12 0.2' 9 <5 0,2' 29 <5 0.2 25 <5 0.2 2

<î:4 <2 ~

<z <2i <2 <2: <2

4.43 4.78 4.47 4.09 3.28

3.27 3.69 3.96 3.57 3.79

15 25 71 26 20

<2i: 61 2':: 86 .16: :<.2 '.<5;> <5 <5::5.12

73 75 18::0.2 <5 > <5 <5 ::4.31 _ ... _. _

43 2;:' 40 34::<.2 <5: <5 :4(3-50 4: 39 3:: 53 114<.2 <5: <5 ..-<5]3.76 <2. 42 3!: 38 70:<.2 <5;: <5 <53.59

7'

44 5::: 45 152.;<.2 6 __.. 49 2;: 49 14:;<.2 <5; <5 55 1:: 86 20<.2 <5;: <5 49 1:: 88 18:::<.2 <5;; <5 45 1: 77 16><.2 <5

<5;'3.52 <5 64.06 <5 4.76 <5j:3.96 <5;;3.61


Na Sr T:; Ga LfiC; Nb Sc : Ta T# ;: Zr

PCT PGT;:PPM pPFI.:PPM P'PMi:.PPM FpFE:PPM PCi PPM

5 15'>: 3 <5<10 041;Y:; <1 2 lrj <1 <5<10 0.* 6 3 6> <1 <5<10 0.09:: 6 3 . 5 : <1 <5: <10 O.OSI:: 6 3 b:i <1 <5':<10 0.:08:_ 8

2 2

2

2 1 4 ..13:: 2 6 14;.: 3 4 9: 1

5 13;: 3

4 11.!; 2 3 10:: 2

2 3 2. 2 1U:; 2

2 10 1

2`; 3 ..3 3

3' ! <2

2'! <2

1 2 2 12 2

.......... __.... _ ... <5;:<10 4 <5<10 0.15 : <1 <5<10 0.17:: <1 <5:<:<10 0.12;: <1

<1

<5<10 0.14;: 1 K5:::<10 0.14; <1 <5<10 0.15: <1

0..45:: <1 <5:<10 0.14<: <1

<10 0.14 <1

<10 0.16 : 1 <10 0.14:< <1 .<10 0.1g:< <1 <10 9.18:': <1

<5 <5:

<5:

IOW Intertek Testing Services Chimitec Bondar Clegg Rapport Lab Geochimie


CLIENT: CAMECO GOLD INC. REPORT: C99-62922.0 ( COMPLETE ) DATE RECEIVED: 07-OCT-99



SAMPLE NUMBER

ELEMENT Au30 Ag;; Cu Pb; Zn 0b Ni Co' Cd 11 UNITS PPB PP$ PPM PF4 PPM PPM: PPM PPMPPM PPM

As Sb: Fe PPM PPM: PCT

Te Ba Cr.;V Sn W La Al Mg PPM PPMMPPM PPM PPM PPM PPM PCT';' PCT

CDR 9937-1840 <5 0.3 30 <2 ,' 60 92 20,<.2 sS:> <5 <5 4.87 651 <10 164 .55<20 ë20. 6 3.44;2.84 2;72 0.02 0.11

CDR 9937-1841 <5 02' 43 35 39 12'<.2 <5:; <5 <5 2.32 315 <10 79 '..10:<2o <20 7 1.65 1.01 2.20 0.03 0.24 ;:

CUR 9937-1842 <5 0.3 43 3. ' 45 1€: 34 11><.2 <5>: <5 <5 2.24 250 <10 83 13 <20 <20 7 1,70 1.00 1.03 0.03 0.21 60

CDR 9937-1843 <5 0.2' 11 28 ts: 29 <5(s<5 <5 1.75 232! <10 134 12.:<20 <20 5 1:42:0.78 1.72 0.03 0.16 61

CDR 9937-1844 <5 <.2:; 5 44 1: 34 <51!: <5 2.29 334 <10 107 !14':. <20 <20 6 1.73 1.09 2,50> 0.03 0,18: 55

CDR 9937-1845 156 0.7 261 66 x: 50 11;:10.3 <5 ; <5 2.76 431 <10 33 107 18 <20 <20 7 1.;62 ;1.00 3.43 0.03 0,23 53

CDR 9937-1846 <5 4.2 2 3 101 1;`: 81 14;:;<.2 <5 <5 3.97 631 <10 7187 42 <20 <20 5 2.79 2.21 3.27 0.03 0 06'. 59

CDR 9937-1847 <5 <.2.. 1 <ï 92 2 <: 93 17 <.2 :<$: <5 <5 4.89 680; <10 3 223 60 <20 <20 . 3 3.34 2.72 2.69 0.03 0.07 51

CDR 9937-1848 CDR 9937-1849

<5 <5

< 2;: <2.

2 1

~

a

50 97

2; 58 2 : 85

9:<.2

:i:<.2 <5::

<5 : <5 <5

<5 <5

2.96 4.72

572; <10 4 199 775 <10 11 212

34 <20 52 <20

<20 <20

6 3

2:24 1.53

3.17.2.55 4.27.

3.00

0.01 0.03

0.05 0,19

127 56

CDR 9937-1850 188 OA. 293 3 :120 98 5550.2 <5>; 12 <5 4.84 635 <10 15:165 40:<20 <20 5 2.75 2.16 2.7$ 0.03 p.23;: 41

CDR 9937-1851 <5 <.2;: 6 38 3:112 21 ><-2 <5: 15 <5 3.58 583 <10 14:189 37 <20 <20 5 2.48 1.93 2.66 0.03 0.12 : 42

CDR 9937-1852 <5 <.2? 10 <2: 33 73 10 :<.2 <5: <5 <5 2.88 491 <10 1.3.126 .35 <20 <20 3 2:02 1.56 2.40 0.04 0,07> 30

CDR 9937-1853 100 0 5<: 255 46 2: 95 24 <.2 <5>:: <5 <5 5.47 763 <10 18 259 47 <20 <20 4 2.76 2.10 3.76 0.03 0.14 44

CDR 9937-1854 60 0.5!:i 310 47 1 : 99 32:<.2 <5;> <5 6.04 757 <10 29.334 .46 <20 <20 4 2.84. 2.12 3.69 0.02 0.22 45

CDR 9937-1855 89 0:5 336 43 2 124 <5 <5 5.22 659 <10 26]-:307 46:<20 <20: 3 243 1.95 3.14 0.02 0 14;; 35

CDR 9937-1856 <5 < 2: 9 40 2<;: 80 <5 .r5 4.00 612 <10 24.152 . 34..<20 <20 4 2.74 2.18 3.00 0.03 0.13:: 41

CDR 9937-1857 14 0,2: 278 44 3,;107 34:<.2 .<5> 7 <5 4.76 612 <10 36~ 133 31.<20 <20 4 2;72 2.06 1.84 ;:0.02 0.16 24

CDR 9937-1858 <5 0.4" 231 •1t 54 24141 .<5;: <5 .<5 5.94 857 <10 25,V1208 40<20 <20 5 3.14 2.44 3.60!::0.02 0.24 50

CDR 9937-1859 <5 <.2: 21 ~ 45 2>i 90 4C <5 <5 4.34 708 <10 2082 34:<20 <20 4 2.89 2.31 3.00;:0.02 0.171: 41

t › ITS - Chimitec - Bondar Clegg, 1322-B Harricana, Val-d'Or, P.Quebec, 19P 3X6, (819) 825-0178

2

<10 :+t1> <1 <10 x1: <1

2 Z: 2 <1; <1

STANDARD ELEMENT Au30 Ag Cu Pb Zn Mlo:; Ni C0', Cd Bi : As lb: Fe Mn; Te Ba Cr I. Sn Y: La NAME UNITS PPB PPM;: PPM PPM: PPM 00)T PPM PPMPPM PPFI. PPM PPM : PCT PPM: PPM PPM: PPM PPM PPM PPMPPM

ANALYTICAL BLANK <5 < 2 <1 < <1 <1 <1z<.2 ANALYTICAL BLANK <5 <.2:> <1 x2 <1 <1.:<t‹.2 ANALYTICAL BLANK <5 -

Nunber of Analyses 3 2 2 2 2:; 2 Mean Value 3 OS <1 1; <1 <1 <1::0.1

Standard Deviation

Accepted Value 5 0:2:: 1.0



Mean Value 494


CANMET LAKE-SED 2 - 0,4: 36 40194 25 16:0.8

Hunter of Analyses - 1 > 1 EiP 1 1 1:: 1 Mean Value - 0.4: 36 40:194 25 1.6. 0.8 Standard Deviation

Accepted Value 23 ::!17::0.8

Oxide (Feldspar 8 2900 !!'

Nurber of Analyses 1

Mean Value 2900

Standard Deviation

Accepted Value 2940



Mean Value 183


e5.;: 10 :.<5. 3.53 1880;:<10 205::: 31 ::46:.<20 <20. 1;' 1 1:: 11: 1 fi: 1 1< 11i.

~; 10 3 :3.53 1880:: 5 20$ i: 31 46: 10 1Q

Mg

PCT ;: PçT :: PCT PPM PPr+~

Nb SC; Ta Tfi : Zr PPM P~T;PPM

<.01:: <1

<.01 .<Y01.:<.01 <Ai:: <1

z 2; <1 3:> 5 4,0;

<1 <5:<10 <1 <5::<10 4,411<

30 4 17 <10 OE OB 4 1 4 5 0 0$

<1 <'0.

x20 <1 <01

. _..

59 i;73 0.59; ~ 62:::0.04 0,23 30 1 . ><:1 . 1 ::; .1 .: 1 . 1:> 1

59 1.73 0.59 0,62 0.04 0,x3.: 30 3()<. 4

<5;,<.01 <5

Z': 2 2: 2 3:': 3 3::i<.01

<S: <5 <5:< <5 _,..

<1 <1

2 <1

EOM Intertek Testing Services Chimitec Bondar Clegg Rapport Lab Geochimie


REPORT: 099-62922.0 ( COMPLETE ) DATE RECEIVED: 07-OCT-99 DATE PRINTED: 29-OCT-99 PAGE 3 OF 5


STD GEOCHEM STD 6 - 0.4 151 17:1149 . 3:144 38;!0.5 <5<146 <5;i7.52 1538<10 234 W<20 #20. 2 .08 2.32 Number of Analyses 1 1 1 1 1',> 1 1 1 1 Mean Value - 0.4I 151 17:;149 3.:144 .38 ;!0.5 3>!146 3'>7 52 1538' 5 44 10 10 2 $$. 2.32 Standard Deviation

Accepted Value - 0.2-: 148 20.,148 4:135 35 0.2 1> 7.20 1450,' < :251 50. 5 :80 2.70

3,54

3.54 _...

4.00

<:0.01 1

0.01

0.01

0.03 ; ~

0,03<:

0.04;

72

72

70

<2 21





STANDARD ELEMENT Au30 Ag Cu Ypot> Zn Mb Ni o Cd Bi Aslib: Fe ;l Te ;BB

NAME UNITS PPB PPM PPM PPM: PPM PPM PPM PPM:.PPM PPM PPM PPM; PCT PPM PPM PPM

Cr ;;Y : Sn .; 41; La

PPM PPM.PPM PPM PPM PCT

M9 PCT

Ga Lfi:: Nb Sc.' Ta PCT .PCT>PPM PPM PPM;:PPM PP1ii;:PPM

Zr

PPM


SAMPLE ELEMENT Au30 Ag Cu Pb Zn 14v: Ni Ca: Cd Bi As Sb; Fe NUMBER UNITS PPS PPM PPM PPM. PPM PPM PPM PPM PPM PPM PPM PPM PCT

Ga L1;# Nb BC^ Ta

PG

Tf.; Zr PP!!. PPM pPli:.:PPM PPM :PPM l` :PPM

I* . Te Ha Cr . :V Sn G La Al PPM PPM PPM PPM PPM PPM PPM. PPM Pct:.

Mg Ce PCT i?CT PCT

r

mal Intertek Testing Services Chimitec Bondar Clegg Rapport Lab Geochimie




8 0,3 6 <2< 79 1: 94 . 15:<.2 <5 <5 <5I;4.47 669 <10 1C163 z7 <20 ë2Q. 3 3:.01 2.48 3 56<:0.03 0 1Di 96 <10 0;0.:, 1 8 0.2. 6 <2 80 11 97 15;i<.2 <5 <5 <5:4.63 691: <10 .15. 198 50 <20 <20. 3 3.12 2.55 3.63 0.03 0.11 109 <10 0:4S. 1

99 0 9 505 <2 64 82 41::<.2 x5:; <5 <5.;4.89 L590.!<10 38 171 :52,<20 KZO 4 3.13 2.41 2.44 0.02 0 77::. 5 <5 <10 (4: 511 <2 63 80 41:<.2 <5; <5 <5 :4.98 602.<10 39 199 i5C<20 e20 4 3.24 2.45 2.48 0.03 0.77 6 +5 <10 O:24 1

_... _ 118 Q.2::; 34 42 38 70; <.2 <5'': <5 <5 <!3.59 442;;<10 85 3s:<20 e.20 11 2.09 1.42 2,138;0.04 0.20:: 69 5::: 5 2 !$; <10 0ab ; 5 108

7C ,Z. 25 62 85 20 <.2 ,éy:; <5 <5 5.13 679 <10 32 262 82 20 3 2.64 3.17;0.03 0.64': 58 6 20;: 3<5'><10 0.17; <1

89 0.5;I 336 43 124 34<.2 <5;: <5 <55.22 :659:;<10 $0:307 :46:: <20 3 2.53< 1.95 3 14;<0.02 0.14;: 35 3 1 .c5;;:<10 0.14 <1 90

CDR 9937-1812 Duplicate



Prep Duplicate

Duplicate


ITS - Chimitec - Bondar Clegg, 1322-B Harricana, Val-d'Or, P.Quebec, 3X6, (819) 825-0178





PROJECT: CEDAR RAPIDS SUBMITTED BY: D. BASIN


DRILL CORE 53 -150 53 CRUSH/SPLIT & PULV. 53 TRANS FROM POLY BAG

51 PULVERIZATION

1

DATE APPROVED

NUMBER OF ELEMENT ANALYSES

LOWER DETECTION EXTRACTION

991018 1 Au30 Gold 53 5 PPB Fire Assay of 30g 991018 2 Au rej Gold assay on rejet 1 0.03 G/T FIRE ASSAY 991018 3 Ag Silver 53 0.2 PPM HCL:HNO3 (3:1) 991018 4 Cu Copper 53 1 PPM HCL:HNO3 (3:1) 991018 5 Pb Lead 53 2 PPM HCL:HNO3 (3:1) 991018 6 Zn Zinc 53 1 PPM HCL:HNO3 (3:1)

991018 7 Mo Molybdenum 53 1 PPM HCL:HNO3 (3:1) 991018 8 Ni Nickel 53 1 PPM HCL:HNO3 (3:1) 991018 9 Co Cobalt 53 1 PPM HCL:HNO3 (3:1) 991018 10 Cd Cadmium 53 0.2 PPM HCL:HNO3 (3:1) 991018 11 Bi Bismuth 53 5 PPM HCL:HNO3 (3:1) 991018 12 As Arsenic 53 5 PPM HCL:HNO3 (3:1)

991018 13 Sb Antimony 53 5 PPM HCL:HNO3 (3:1) 991018 14 Fe Iron 53 0.01 PCT HCL:HNO3 (3:1) 991018 15 Mn Manganese 53 1 PPM HCL:HNO3 (3:1) 991018 16 Te Tellurium 53 10 PPM HCL:HNO3 (3:1) 991018 17 Ba Barium 53 1 PPM HCL:HNO3 (3:1) 991018 18 Cr Chromium 53 1 PPM HCL:HNO3 (3:1)

991018 19 V Vanadium 53 1 PPM HCL:HNO3 (3:1) 991018 20 Sn Tin 53 20 PPM HCL:HNO3 (3:1) 991018 21 W Tungsten 53 20 PPM HCL:HNO3 (3:1) 991018 22 La Lanthanum 53 1 PPM HCL:HNO3 (3:1) 991018 23 Al Aluminum 53 0.01 PCT HCL:HNO3 (3:1) 991018 24 Mg Magnesium 53 0.01 PCT HCL:HNO3 (3:1)

991018 25 Ca Calciun 53 0.01 PCT HCL:HNO3 (3:1) 991018 26 Na Sodiun 53 0.01 PCT HCL:HNO3 (3:1) 991018 27 K Potassium 53 0.01 PCT HCL:HNO3 (3:1) 991018 28 Sr Strontium 53 1 PPM HCL:HNO3 (3:1) 991018 29 Y Yttrium 53 1 PPM HCL:HNO3 (3:1) 991018 30 Ga Gallium 53 2 PPM HCL:HNO3 (3:1)

991018 31 Li Lithiun 53 1 PPM HCL:HNO3 (3:1) 991018 32 Nb Niobium 53 1 PPM HCL:HNO3 (3:1) 991018 33 Sc Scandiun 53 5 PPM HCL:HNO3 (3:1) 991018 34 Ta Tantalum 53 10 PPM HCL:HNO3 (3:1) 991018 35 Ti Titaniun 53 0.01 PCT HCL:HNO3 (3:1) 991018 36 Zr Zirconium 53 1 PPM HCL:HNO3 (3:1)



30g Fire Assay - M FIRE ASSAY 1NDUC. COUP. PLASMA INDUC. COUP. PLASMA INDUC. P. PLASMA INDUC. COUP. PLASMA

INDUC. COUP. PLASMA INDUC. COUP. PLASMA INDUC. COUP. PLASMA INDUC. COUP. PLASMA 1NDUC. COUP. PLASMA INDUC. COUP. PLASMA

METHOD

INDUC. COUP. PLASMA INDUC. COUP. PLASMA IMUC. COUP. PLASMA INDUC. COUP. PLASMA IMUC. COUP. PLASMA INDUC. COUP. PLASMA

IKOUC. COUP. PLASMA INDUC. COUP. PLASMA INDUC. COUP. PLASMA INDUC. COUP. PLASMA INDUC. CM'. PLASMA INDUC. COUP. PLASMA

INDUC. COUP. PLASMA INDUC. CUP. PLASMA INDUC. COUP. PLASMA INDUC. COUP. PLASMA INDUC. COUP. PLASMA INDUC. COUP. PLASMA

INDUC. COUP. PLASMA INDUC. COUP. PLASMA INDUC. COUP. PLASMA IPOUC. COUP. PLASMA INDUC. COUP. PLASMA INDUC. COUP. PLASMA


********************************************************************************

This report must not be reproduced except in full. The data presented in this report is specific to those samples identified under "Sample Ntmber" and is applicable only to the samples as received expressed on a dry basis unless otherwise indicated

338 ;2.5 2857 .3.06.15.5

96 0-5

7 03

112 1.5

115

1).2

17

1).4

35

1).4

15

0.4

118 .0

<5 <:< 2

152 ?:1.6

382 4.3

221 2.3

21 0.3

138 <5 <5 73 208

8 18 <5 9

112

1038 <5 <5 <5 70

0.9 <.2 <.2 0.2 0.6

0.5 0.4 <.2 0.4 0.5

0.5 0.2 0.4 <.2 0.6

0.02 0.31 0.02:0.23 0,02 : 0.22 0.02 0.23 0.03:0 21

4i3' 3 42 2

Oi 2 $6: 2 59 3

4 10 <2 10 Q:: 9 QI 8

8

<5 <10::0.11 <5 <10::0.08 6 <10€:0.10 6 <10:0.11 <5 <10'::0.13

0,0$ 0.21 0.02 0.18 0.03:;0.18 0.02 0.21 0,01:;0 24

56 3 fib 3 54! 3

42 3 36 2

<2 9 <2 9

9

<2 10

1 <1

<5 <10::0.13 6 <10>:0.11 <5 <10;:0.12 <5 K.10::0.11 <5 <10`:;0.10

0.01 0.21 0.02 0.16 0.02 0.14 0.02 0.12 0.02 0.09

44. 3 9 <1. 46 3 <2 9 <1

44 3 4 8 60. 4 t2:< 7

46 3 s2<: 11

6 <10 0.10 <5 <10 0.10 <5 <10 0.10 6 <10 0.11 <5 <10 0.10

_...

0.43 0.01: 0.03 0.04 0,03

0.p4<0 06 0 0 16

0.02::0 10 002! ; 0 07 0.03 0 06

42 3 <2 10 ;::2 <5 <10 0.11 633 .~2. 10 ..:>2 <5 ~10 0.11 .;<1: __. __.

49 3 <2 11 3 a <10013 .:<1:

44 3 <2 9::'2a K10 0.12 <i 1

....... ........

50 3 <2 8 <1 <5 <10 0.09

45 3 ;<2 7 ';2 ô <10 !0 10 31 3 <2 9 <1. <5 <10;0 09 << 40 3 <2.. 9 ;2 <5 <10 0 10 < 34 2 <2 9 <1 <5 <10 0.11 '<

42 3 <2 9 <1 <5 <10 0.11 :+~

0.14 0.05 0.18 0.04

°-18


Geochemical Lab Report CLIENT: CAMECO GOLD INC. REPORT: C99-62923.0 ( COMPLETE )



SAMPLE NUMBER







;Fe:

PCT-

369 <2 :54. 4 • 106 21 0:3 <5 <5 <5 440 > 683 <10!; 26 156 31 <20020 3 2.57 2.28 3.96 3; <2 4F 2 T8. 18 <;2 <5 <5 4.01 552 <10 : 30 125. 30 <40:<.:<20 4 <!2.74 2.231;1.61 19 <2 46: 1 84. 19 c,2: <5 <5 $;84 i 578 <10 : 25 ;150 : 33 ;Q0:<20 4 2.60 203;; 2.41 85; <2 6S: 2 120. 25 <:2. <5 <5. <5 5..41 ; 700 <10 37 162: 42 :<20<20 5 3.37 2892.00

539! <2 66 5 114 35 0,2. <5 <5 <5 5:52 . i 661 <10 ;: 26 183 :: 41 ;Q0):<20 3 3.21 2.79::2.00

66.:• <2 '85 18 <:.2. <5 IKS <5 4::15 i 577 <10 30 131 32 ;<20;::<20 3 2.65 2.18:2.92 64 <2 . 47 3 64 13 <.2 <5 <5 <5 3.97 578 :<10 23 '133:: 26 :<20 :<20 2: 2.50 2.1C1 4.06 40' <2 43 2 68 24 <,2 <5 12 <5 3:67 552 <10 27 28 40:<20 2 2.39 1.98 2.90 174 <2 45 3 91 102 0.2 <5 60 <5 5;34. 679 <10s 20 1161' 36 Q0:><20 3. 2.48 2.00'3.33 403 <2 65. 5 92 45<:2.;<5 <5 6;03 ' 730 <10: 14 201; 51 <20Q0 2.66 2.22 3.32

205! <2 49 2 85 25 <42. <5 <5 <5 4:65';I 682 <10 14 177:: 53 Q0<20 2 2.75 2,30 3. 27 104: <2 48 2 83 19 <.2 __. <5 : <5 <5 4.07: __... 542 40:<20 <10.: 23 134 __. 33 2 2.60 2.13.:2.13 53 <2 73 1 5$ 15 <.2 <5 <5 <5 3;46 : 494 <10.' 18 :121: 30 <2040 2 ;2.42 1.417`;2.42 45 <2 41! 1 60 14 <,2 . <5 Y5 . <5 3:54: 436 <10 ; 27 .10s : 26 :+•20::Q0 4 2.54 2.05 ::1.52

343 <2 .99 2 148; 37 0.4 <5 <5 <5 4.93 ; 510 <10 : 23 149': 29 _...... _.. <20 <20< 6>2.69 2.32<2.17

_.... 1735: <2 :71; 2 210: 62 0:4 <5 ;:12 <5 6:02 ; 543 .0.c .K 22 134;; 30 <20 <20 6::2.76 2;32 2.53 3133: <2 82 3 250:103 0.7 6 <5 <5 5L81 : 560 :<1Q!: 16 :118:< 33 s20 <20 $'> 2.63 2.15: 2.90 376: <2 ;48 2 80: 44 s.2, <5 <5 <5 4;:42 : 602 :<10'> 16 .122 : 33 <20 <20 4;2.55 2,18 2.99

:43- <2 : 43 <1 â6: _.... 19 <.2 _.... <5 : s5. <5 3.:82 : _ 593 :<1D , 10 1121' < 35 :~10 <20: __.. 2::2.53 2.09 3.41 :161 <2 78'. 1 115: 47 0.5 <5 Pij . i <5 4;74. 546 {10': 9 1146; 41 <20 <20 : 42.53 2.22 2.77

115; <2 44 2 53; 17 <42 <5 :<5 <5 4.03 553 <10 14 135 ": 37 <20 <20 ; 3 2.50 2,13':;2.35 2091: <2 58 2 100: 39 E.2 <5 c► <5 6.31: 855 <10; _..._.. 5 234;: 50 <20 <20 :.. 3 3.27 2.~73.81 290! <2 60: 1 114: 37 <,2 <5 aT. <5 644 667 <10 15 179 66 40: <20 : 4 3.30 2.66 1.74 H24.4.:: <2 45' 2 .50a 20 <.2 <5 <5. <5 3.62 468 <10 : 4 136 46 <0 <20 : 3 2.38 1.99 1.93 1384: <2 45.; 3 .98: 16 442 <5 12 <5 4.01. 312 <10 : 28 ;! 86 21 <20 <20 : 5 2.25 1,63 0.97

40: <2 44; 3 5ÿ 17 ~`2< <5 <5 3,47. 501 <10 7131 35 <20':;Q0 2.17 1.65:2.17 2054 <2 74:: 6 229 60 0 4, <5 23 483 <10 24 127 30 i<20<Q0 2.66 1 .8.6;i0.65 6090 <2 136 5 249 61 1:.3, <5 <5• <5 6473 :: 518 <10 < 16 128,; 32 <20;<20 2.76 1.93;:.79 2752( <2 92i 3 105' 33 0.6 <5 ~ <5 4.97. 529 <10. 10 137 31 !,q6.40 2.56 v

1'33 1.97

241:.: <2 62:: 2 55: 23 <.2. <5 <5 <5 4;38 526 <10: 8 148 31 <20':<20 2.57 240 1.77

V G a Li ;Mb Sc Ta Ti s'Zr

PPM PPM PPM PPM PPM RPM PCT PPM

2

11 .: ;:1 <5 <10;:0.08

3

11 . <16 <10::0.13 3

10 1 <5 <10:0.13 3

14 1 6K10:;0.12 3

13 <1 <5 <10:0.11

ELEMENT Au30 Au rej Ag . pÙ. Pb Z11 Mo N.i; Co : Cd. Bi 40' Sb

UNITS PPB G/T.PPM PPM PPM PPM PPM PPM PPM PPM PPM PPM PPM Mn ;! Te.

PPM PPM

Ba : CP<! V ; 5n;:; W #:A;

PPM PPM:PPM PPM:PPM PPM

0.01;;0.20 32 0.02 0.20 46 0.02 0.24 59• 0.01 0.44 37 0.02;;0.26 24:

Al Mg Ca Na K PCT PC1 PCT PCT :i PCT PPM


14 0.4 198: 11 <.2 .97 32 0.3 104 18 <.2 113 25 <.2 137

19 25 12 5 <5

<.2 0.4 .3 02 <.2

192: 169: ' 91

<5 0.3 181<

6 <.2 .130i <.2 205

5 349 6

218 13

8 11 75 8

<.2 0.4 <.2 z2 <.2

<.2 <.2 0.2 <.2 <2

37

723 97 76i . 49.

4:11

9 2.4

10 ___ 69

0.04::: 0.14

3 0.04 0.12 54. 3 0.03 0.09 67. 3 0.04 0.11 62 3 0.04 0.14 32 3

<2 12 ; <1: <5 <10 2 15 <1 <5 <10 <2 14 <1 b <10 4. 13 ::<1 <5 <10 4 10 <1 b <10

<.U1

<.01 < 01 <.01 <.01

0.03;:0.14 0.03 0.19 0.01 0 04 0.0410 17 0.04 0.16

0.04::0.14 0.04 0.12 0,0510 11 0.04:i'.0.13 0.0(+:.0.11

3 :Q 7 <:<1 : <5 <10 <.01 22 4 <L 6 :<1 <5 4<-01 ;124<1

.36

4 3 29 :; 6 17 00.01

51

6 : z1, <5 <10 < 01 55 4 '<I 8 <1 6 <10J<.01

42 3 8 <5 <10, <.01

it`r 5 <2: 14 <1 <5 <10.01 5:1 4 ~ . 11 <1 a <1ll;:<.01 33 3 d:: 11

a {10:<.01 26 3 .<2: 12

<5 00.01

K Sr Y:Ge Li Nb Sc 1a Ti ;Zr; PPM P ; PCT PPN:s

78 4 0.07

69. 5 0.07 69 5 0.05

61. 3 <.0

55 3 . <.01

Q 8 <1 <5 <10 Q. 12 <1 <5 <10 ., <2 10 <1 <5 <10 12 14 :<1::<5 <10 Q 14 <1 b <10 _....

0.04 0.18 0.03 0.15 Q.04 0.15 0.033 0.14 0,03:0.12

0.02..: 0 02 ;56: 3 0.05 0.12 29 . 3 0.05 0.12 30 3

40 ;7" 19 <:10< 01 12 ~1 ô ::10.1<.01 9 6 '.1-i6.01

~.,

~




SAMPLE NUMBER


ELEMENT Au30 Au réj Ag Cl. Pb Zn Mo . tit. Co Cd: • Bi ::.P4 : Sb

UNITS PPS Alf.tPPM PPM.PPM PPM PPM PPM PPM PPM. PPM PPM PPM

<2 <:24 2 . i21 20 <:2 <5 <5 : <5 3.07 297 <10i11 18 19 <20 <20 8:'11.69 0,91::2.57 <2 10:0: 1:..39 20 0:4 <5 :+5 <5 4.21 345 <101 15 73. 25 <ZD'91<20 _._ 9:I2.10 1.40 2.41 ...,.. ....

<2 :2$ 1 27 17 <.2 <5 . <5 <5 3:52 294 <10 17 711 23 <20 <20 10 1.76 1.14 2.20; 2 26 7 37 17 < :42.: <5 '...4:'. <5 3.61; 276 <10:1 20 841 23 <20 ;<20 ..12> 1.91 1.28 2.09 <2 27 3 51 15 <.2 <5 ::<5:. <5 3.68 255 <10 16 gz 22 Q0;<<20 15;;2.02 1.35 1.96

<2 :1:26 4 >44: 16 <.2 <5 ::<5.. <5 3;13: 192 <10>: 15 77; 16 Q020 13;;:1.75 1.10 1.80 <2 32 <1 .40: 10 <5 <5 . <5 3;24'1 254 <10i:: 11 75:1 21 <20<20 13 2.10 1.39 2.30 <2 ;30. _._ <1 40 _._ .. 10 <;2 _. .. <5 <5 _..... <5 3:27:: _ 268 <10<;i 9 90:; 22 <20;<20 11 °.I 1.92 1.25::2.45 <2 .28 _. . <1 28 _ .. 9 <.2 <5 <5 <5 2.86 212 <10! : 10 66;: 20 <2(620 12 1.82 1.16 2.09 4 5.7' 2 4!v 21 0.:5: <5 <5. _.. <5 2:93:1 _.. ... 1974. 97<14; 21 .69:; ... 18 <2.0<20_ 15'1.63 1.01 2.21

12 193 2 ;41 43 2;1 <5 <5 <5 3.70 166 <10:1 29 79; 12 <20<i1<20 12 1.26 0.78 1.46 2 .65 1 28 24 0.5 <5 <5 <5 2.70 125 <10 39 55 11 <20 <20 16 1.31 0.66 1.32 <2 119 <1 89 42 0.5 <5 <5 <5 9:57: 571 <10 7 203 128 Q0:1<20 614.70 3.10 3.56 6 455 2 . 21 26 0;4 <5 <5 . <5 2.40 f 164 :<14:< 39 : 55 9 <20 <20 12 ':1.04 0.51 2.50 <2 72 2 .3$ 33 0.3 <5 10. <5 3.03 :; 134 <10.1 37 ; 49 11 <20 <20 11, ::1.22 0,64;;2.18

<2 2 28 0:2 <5 <5 <5 3.28 108 <10 32 64 12 <20`:1<20 8>1.10 0.57':1.83 3 991: 3 35 04 <5 23 . <5 3.97 221;<141 20 91 14 <20 <20 9<:1.47 0.87:<3.51 <2 50 3 46 30 <5 9. <5 3.31 291 <10:: 17:87!? 15 <,20::<20 12:>:1.38 1433.68 <2 26. 1 26 23 <:2 <5 <5 <5 2.83 ? 137 <10 16 : 79 13 Q0 :1<20 9:I1.34 0.74 2.08

411 2 25 15 <. .g <5 <5 <5 2.57 160 <10 15 : 87 28 <20;<20 1.1:1'1.43 0.83:1.78

<2 65 <1 70 49 <12 <5 <5 705 t10:11 3 232', 136 40 <20 4 4.23 2.86 4.20 <2 23 <1 24 32 <.2 <5 166 '09:g 17 20 .201<20 13'>1.47 0,844:2.02 <2 29 2 2:7 42 <5 <5 <5 288: 144 04: 17 ' 66. 16 <20 <20 13 1.24 0.71 1.94

_.... ___. _..

fé ;: Mn ; Te.'; Ba Cr:

pCT,:1 PPM PPM::<PPM PPM. V

• :Stü

PPM PPMt:! W t.é. j At

PPM PPM::.. PCT PCT:

Ca PCT



COR 9937-1905 CDR 9937-1906 CDR 9937-1907 CDR 9937-1908 CDR 9937-1909

COR 9937-1910 CDR 9937-1911 CDR 9937-1912


<5 t10:::<.01

<5 <10:<.01

2

<.01

2

<.01

20 ;;Z 8

1 4 1

20

I33 35 A';2<;;

0.2 <155; 16 159 , 3 146

1 1: 1 11> 1

0.2 155: 16 159 3 146

0.2 148:.,20 148: 4

<5 7:74;;1503

1 MI 1

3 7;74 }1503

7..24g1450

4 2Z8;; 48 <20 <20 3:'2.04 Z.61 3.55 001::<0.04

1 1: 1 1 1 1 .. 1 1

4 228`: 48

12 1.80 2.7¢4.00 0.01 0.04 ::78.

10 3 2.04 2,61 3.55 0,01 0.04 .....:..:.

36 04. <5 154

1 1 1 36 0.4 3 159


Geochemical Lab Report CLIENT: CAME00 GOLD INC. PROJECT: CEDAR RAPIDS



STANDARD ELEMENT Au30 AU rej Ag Cu Pb Zn Mo NiCo Cd Bi As Sb

NAME UNITS PPB G/T PPM PPM PPM PPM PPM PPM PPM PPM: PPM PPM PPM

ANALYTICAL BLANK <5 <.2 . t1 <2 <1. <1 . <1 <1 <,2 <5 <5 <5 c.01 >

ANALYTICAL BLANK <5 <.2 . <1 <2 <1 <1 <1 <1 <.2 <5 <5 <5 <.01

ANALYTICAL BLANK <5

Nutter of Anales 3.', 2 2. 2 2 ys 2 2 2 2 2 2 2 I!2:i 2

Mean Value 3 0.1 cis. 1 1 <1 <1 <1 0.1 3 ;3 3 <:01'i <1

Mn je,:; Ba Cr, van, W AA, Al Mg?; Ca Na K .:St' Y Gs' Li ::II Sc LTa

PPM PPM PPM PPM :PPM PPM. PPM PPM::: PCT PCT:: PCT PCT PCT PPM. PPM PPM .PPM PPM PPM PPM'. PCT PPM::

<1 <10> <1 ~1::; <1 -Q0 <<20 ~~ :::<.01 <.~1:1.::< 01 ~.01' < 01 s:1 <7 Q::; <1

<1 <10 > <1 <1;: <1 Q6>>.<20 . <.1 i <.01 <.fl1 s<.01 s.01 < 01 <1 <1 : ¢ü <1 _

2 2l> 2 2::: 2 22:;: 2 2 2

<1 S1;!:i <1 1<' 10 ~1'>:<-01 <,01'::< 01 5.01 0 : < 01 ;5,1 <1 :':!1':: <

Standard Deviation

Accepted Value 5 .14)411)3.2 . , T. 2 .,1 1 1 1 TO 2


Nuiber of Analyses

Mean Value 2876

Standard Deviation

Accepted Value 2940

<1::j<.01 < fl1;:',< 01 4:01 <.01 <1 <1 <1 <1

STD GEOCHEM STD 6

Number of Analyses

Mean Value

Standard Deviation

Accepted Value



Mean Value 177

Standard Deviation

Accepted Value 186 <I;<019



Mean Value 467

Standard Deviation

Accepted Value 465

ITS - Chimitec - Bondar Clegg, 1322-B Hamcana, Val-d'Or, P.Quebec, J9P 3X6, (819) 825-0178

GANNET STREAM-SED 4

Number of Analyses - 1 Mean Value

Standard Deviation

Accepted Value 0.3

IEGU Intertek Testing Services Chimitec Bondar Clegg Rapport Lab Geochimie





t•e) : Ag

G/T;PPM

Na.

PCT: STANDARD

NAME

ELEMENT Au30 Au UNITS PPB

Cu Pb Zn ma NI Co Cd B1 As Sb fr

PPM PPM PPM PPM PPM PPM PPM PPM PPM PPM ;PCT; Mn gw Ba Cr :`: V 1;-n:; W

Al Mg:: Ca PPM PPM: PPM PPM: PPM PPM ::PPM PPM PCT P'GT< PCT

Sc .:Ta Ti Zr

PCT PPM: PPM PPM.PPM PPM PPM PPM PCT PPM

K St`. Y ..Ga. Li

61: 11 ;:84:"s; 1 11 <5 ~ 1 1: 1

69 11 $4 1 24. 11 P*1 3

:6d 13 ::8x 2 :23 11 0:6<!

<10:;:766 50 Q0<20 1.12 0.60<1.05 0.05- 0.11 11 :;Q: ; 8 <5 O0 0.06

1 1<! 1 1 1 1 1; 1 1

; 5:>766 50 00., 10 1.12 0.60 1.05 005,.:0.11 11 1 8; 0.06

30 51

<5 2:66!:1183 1

3 ~:6G 1183

4 2:60 1200

ITS - Chimitec - Bondar Clegg, 1322-B Hamcana, Val-d'Or, P.Quebec, J9P 3X6, (819) 825-0178

• •••

2 49 21 0.5 <5 <5 <5 2.93 197 <1

2 48 21 0.5 <5 <5 <5 2.96 201

3 52 35 0.4 <5 a. <5 3,97.! 221 Al ... .. -..- •• • .., . . ........... ..... .. •••••:.-..::...-. ........ ........... . ..

• • :::•:.:::::::::::::::::::

•.'...":"..::::'..•:'..:::. •••••••••••••••••.: ...„.... ...........

..,. ........ ....

'""'"" •••• ........ ......... .... ........... .„ ...... ........... ::: :•:.-.

•- '.'.'.'.'.•.',','.'.' ......... ... ........ •:::::•:::: - • •• ' ' " " .'.. "" ""' • •• .......... --- •• ....... :.':'.':'•.:-.-',..".

„.. "" '"" ••• .... •••••• '• ::::.:•::: .... ....... .....• .• --• •• ........ "'"' - ••••••••••• .,....... ••••••.••• •.:....:,..J...:,..:.• ••••••••• ........ .......... ........ ......... ••:::•••••.• .............. ......... ........ "• " "

.....::::::.•:::•: :::':::•':'::::::: " .......... ... ......... ........ .... ......... .......... ......... ' ' '"" •.. .......... :-.::.•::: ........ •"•••••• ...... .... .... ...... ......... .. .... ........ ...... .......•.:.•.... - " • '' --"."

.......... .... .••• ...... ......,... ........ ..„.... ....... ,.......... ' • " • '

.... •••,........:;....• ::::-..: .......... ..„..... .-• ........... ......... .... '.. •.• .• "'"' ' ' ...... ....,...:.: ........ .......... ........... .. ........ .. ,.... • " - .. - ...... .... ......... ....... .......... .....,. ......... :.:::.•::.: ' • . ' ....... ... • • ... ... .... . ........... ......... ''''''''''''' :i•.:,•••••••••••,.:.•••..:••••• '''''•'' ...-..::.:.::: ........

•,:i::::::: •••::::::: ........ ........ " '"'

.......... ......... .......... ...... ........ :i..:::•.:,..?.....,;.•.:...• ....... ......... ..-.... ........ ......... ......... ........ ---- .......... .......... .......... ,... ... .......... .i:':'..::::::':....'',:....:..: .......... .......... ..........

... .... .... ........ .... ... ... ... . ...... ......... '.'. ...... . ... ... ..........,.... .......... :.:::::•: ......... ... .'. .......... ........ ... ........... ... ...............,.... '::::.•:::: ........

•••...:-:::::•:.•..f...,.: ........... .......... ..:•'.•.•.•.••.•.•.

..'. .... ... i',...•::::.i:•••,.......•.:,'::.: ].......•:-.f.:.'...:-.•-..-.•:::: ."' ....

.'.' "•"'"' .... •.'....•'.....'::::.:.•,..',..:.::, .... ..._ ......... .... _....... .......... ........... ........ .......... .......... ....,::.

.•'• f.',••••••.'...::::',.. .... -....::::',...:',.'::::'.....-. .... ...... ""„." .... ........ '." ......... .......... ......... ....- ........• .... .... ........ • .. ......... ---- ........ • -- •• . ......... .... "•"'.' ----• • . . ••••••••••••'••• ,.........i.•:•....i•...•......, "" ....

. • ..,. - • .." --.•:::•::: ,... .... •,,,:.•••••:•••• ..........

' •

• • • • • • • • • •

• .• • • • • . • • • •

0 14 135 37<20 <20 32.50 2.13 2.35 0.03 0.14 0 14 135 37 <20 <20 32.51 2.15 2.32 0.03 0.14

0 7 131 35 <20 <20 3 2.17 1.65 2.17 0.04 0.06

021 69- 18 <20<20 15 1.63 1,01 2.21 0.04 0.14

0 20 68 19 <20 <20 16 1.65 1.03 2.24 0.04 0.14

0 20 91 14 <20 <20 91.470.87 3.51 0.04 0.12

......... ........ ........ .........

....... ........ ........

........

......... ........ •'"'"'

........

.........

""-• .........

........ .........

........

........ ........ ••••••••'•••••'.' ••••••••• ........ ••••••••• ........ ......... ........ .........

........

........ ......... ........ .......

1111 Intertek Testing Services Chimitec Bondar Clegg Rapport Lab Geochimie


REPORT: C99-62923.0 ( COMPLETE ) DATE RECEIVED: 07-OCT-99 PROJECT: CEDAR RAPIDS


SAMPLE ELEMENT Au30 Au rai Ag Cu Pb 7n Mo Ni co !:(* Bi A Sb Fa Mn I. Ba Cr V Sn 1.4 ta Al Ma C.a NKr Y :!P!',.( Li t& Sc Ti NIER UNITS PPB 0/I PPM PPM PPM PPM PM PPM PPM PPM PPM PPM PPM 4Cij PPM PPM PPM PPM PPM PPM PPM PPM: PCT PCT PCT PC1 PCT PPM PPM PPM PPM PPM PPM PPM PCT PPM


CDR 9937-1877 Prep Duplicate


(DR 9937-1885 Duplicate



730.2 85 <2 65 2 120 25 <5 <5 <5 5.41 700 <10.: 37162 42 20<20 M53.37 71 :.:::OMMA.2 80 <2 63 1 24 <5 ;.;: :A.5! <5 5.03g 657 <10 35 153 39 <20 <20 4 3.17 2.69 L84 0410.41

INFN 1g4: 96 :1•:0.5 376 <2 43 2 80 44 ç2 <5 <5 <5 4.42, 602 <10 16 122 33 A0.<20:a*'.:2.55 4.1.8 2.99 0.0.20.14

175 • :190 <2 47 2 80 44 <5 <5 <5 4.40] 601 <104 16 10T,. 32 - 41,,,,(20 -V42.55 2.12 306 . . 0.14

115MENF:60.2 4. <2 44g1 2 17 <5 <5 553 <1 0.3

. _ .._....

116 <2 44 2 54 17 554 <1

<5 PgJ8M.2 Lg401 <2 r:441 3 53 17 <5 <5 <5 3.47 501 <5

..•.•.•..•.•.•..•...•••••..•.:... ••.•.:•...•:.......-.. .....•••••••_••....

6 .2 ..,.-.0 4 57i ..„....-....---.... .......-.......„. .................

<.2 -.. ,..--.69......::: 5 :-.':::::57:::•:

........................... .................... ................. .............. ........_ ........ ............... .......... .........

25 •.....,!...:......§:::•. :1- y..0./. ..,.-..::::,Ip.. .:-..:, 3 ''.....-:-,99::.;:...i 24 ::::".::::::::::::::::•::: .,g: .....:::.•::::.:',::•::::....: '....:::::::::,:::•,]...::::::"..•::: ..„....... ........... ........... ........... ..........

.......... ....... ...........

.......... ......... ....... ...........

........... ........

.......... ......... ......... ........... .........

........... ........ ..........

::.:?.......:::.::::::::•:::: ::::.:::: ........ ........ ......... ...............•. ........ ........

.......--.E..:.........::::::::., ......... •••••••• .........•::::

........... ....,........:

„:„..... ..............,,

......... ......... ....... •-•••••-• :::::::: ...........

.......... ..,....,........ ........... .......... .........

........... ........ :•::::::::: .......... .......... ........... .......... ........... ........... ........... ..........., ••••••••••• ••••••••••

........... ,.....•:-:•.-....•:. "••••••,•••• .......... ...........

.......... :•::::::: ...,,..... ........... ........ ...........

----• :•.,•.....•...: ....„....

........... ...........,.... ........

.......... ......... .....„...

........... ........

.......... ........

........... ....,,......,

:,,,...„.., ......... •••••••••••

........... ....,„..:..

•••••••••• ........ ..........

.......... ...::::.,:::::::......• ........... ..........

........... ........

.......... ........ .......„. ........... •-• •••••• :,:::::.•: .......... ...........

•••••••••• •••••••••••'•••••••.••:: ...........

........... ........,.....,..............,... ......... ........

:••.:.:••.::•••••;••••••••••••••••:. ......... ::.•:::::: •-:.....-...-:::::•••••••••,••••••• :::::::::

•••••:::::::J::•,•::::::::::•••••• •:::::::: .....-........: ........ .........

::.:::::::::::::::::::: ....:•:•'••••,.::::•:!::.....:-...:!;•:::::.: ..........

::::::::::: -....i-•::::•:]:::i'••! .....]'::::::, .......... •.::::::::: ........... .......... ........... .......... ........... ........... ........... .......... .......... .......... ........... ..........

::::::::::: :.:...:.-.-.•...• .......... „........ „......... ........... .......... .......... .......... .......... „........ .......... ........... ..........

.......... :...,:.......:•:....,:.,- ..... .... .........

:,::_••:.•_•:•. :::::::: .......... .......... .......... .......... ........... ::.•::::::: ........... ........... ..„....... ......... ........... .......... ........... .......... .......... ........... .......... ...........

.......... ......,....„.

34

43.

3

3 <2

3

14 1 <5 14 1 <5 <10 011

8 'E:1:i <5 <100.10<1 2 8 ::,1• <5<100.09 <1

42 3 10 :2<5 41 3 11 2.11:: <5 <10 13.11

45 3 <2 7 2 <5<10010

. . .

32 3 <2 10 .".<1.• <5 <10-:<.01 15 33 3<2 10 <1 <5 A.10..<.01 14

• • 56 5 ••••••'......4; 14 ti <5 <1%......<.01 23

........

........ ........

........

.....,.. ........ ........

ITS - Chimitec - Bondar Clegg, 1322-B Harricana, Val-d'Or, P.Quebec, l9P 3X6, (819) 825-0178

53 52 1

53 -150 53 CRUSH/SPLIT 8 PULV. TRANS FROM POLY BAG PULVERIZATION






DRILL CORE



991018 1 Au30 Gold 53 5 PP8 Fire Assay of 30g 30g Fire Assay - M 991018 2 Au rej Gold assay an rejet 1 0.03 G/T FIRE ASSAY FIRE ASSAY 991018 3 Ag Silver 53 0.2 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991018 4 Cu Copper 53 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991018 5 Pb Lead 53 2 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991018 6 Zn Zinc 53 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

991018 7 Mo Molybdenum 53 1 PPM HCL:HNO3 (3:1) IMDUC. COUP. PLASMA 991018 8 Ni Nickel 53 1 PPM HCL:HNO3 (3:1) INDUE. COUP. PLASMA 991018 9 Co Cobalt 53 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991018 10 Cd Cadmium 53 0.2 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991018 11 Bi Bismuth 53 5 PPM HCL:HNO3 (3:1) IM)UC. COU'. PLASMA 991018 12 As Arsenic 53 5 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

991018 13 Sb Antimony 53 5 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991018 14 Fe Iron 53 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991018 15 Mn Manganese 53 1 PPM HCL:HNO3 (3:1) INDUC. COL'. PLASMA 991018 16 Te Tellurium 53 10 PPM HCL:HNO3 (3:1) 1MDUC. COUP. PLASMA 991018 17 Ba Bariun 53 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991018 18 Cr Chromiun 53 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

991018 19 V Vanadium 53 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991018 20 Sn Tin 53 20 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991018 21 W Tuigsten 53 20 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991018 22 La Lanthanum 53 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991018 23 Al Aluninxm 53 0.01 PCT HCL:HNO3 (3:1) IMDUC. COUP. PLASMA 991018 24 Mg Magnesium 53' 0.01 PCT HCL:HNO3 (3:1) IM)UC. COUP. PLASMA

991018 25 Ca Calciun 53 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991018 26 Na Sodium 53 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991018 27 K Potassium 53 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991018 28 Sr Strontiun 53 1 PPM HCL:HNO3 (3:1) INDUC. COUS. PLASMA 991018 29 Y Yttriun 53 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991018 30 Ga Gallium 53 2 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

991018 31 Li Lithiun 53 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991018 32 Nb Niobiun 53 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991018 33 Sc Scandium 53 5 PPM HCL:HNO3 (3:1) IMDUC. COUP. PLASMA 991018 34 Ta Tantalun 53 10 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991018 35 Ti Titaniun 53 0.01 PCT HCL:HNO3 (3:1) IM)UC. COUP. PLASMA 991018 36 Zr Zirconiun 53 1 PPM HCL:HNO3 (3:1) IMDUC. COUP. PLASMA


REPORT COPIES TO: #6-1349, KELLY LAKE RD. INVOICE TO: fl6-1349, KELLY LAKE RD.

****** **** ta*,n*,t****,w,trt****x** ******ir****,r************,k t *********,we+r***

This report must not be reproduced except in full. The data presented in this report is specific to those samples identified under "Sample Nteber" and is applicable only to the samples as received expressed on a dry basis unless otherwise indicated

************************************************************************w*******







Mo :Iii. Co Cd Bi :As PPM PPMPPM PPM PPM PPM

ELEMENT Au30 Au t•e) Ag Ct1 Pb 2r UNITS PPB Oft PPM PPM: PPM PPM

SAMPLE

MARGER

65; 21: 22 32 32:

<5 <5

<5.

38 <5

<5 <5 <5

21 25 2

2 2 2

2 58 68

52 O. MR <5 76 <.2 <5 48 <.2 <5 65 <,2 <5 67 <.2 <5

<.2 565.! 2 <.2 319> <2 <.2 270: <2 0.3 336 <2 0.3 394 <2

CDR 9937-1913 CDR 9937-1914 CDR 9937-1915 CDR 9937-1916 (DR 9937-1917

46'. 98 97 103 98

9 <:1.1 1770 <2 82 .. 1.4 2.192 <2 20 0.9 1413 <2 <5 0.6 300' <2 21 ;08610. <2

<5 <5 T7.

<5 15

9 541:329 ,<:;2 . <5 12 593.310 <.2.. <5 16365217<.2.<5 2 354 87 <,2 <5 3 309,106 s.Z: <5

0:: 0:: 0::

<5 A0.00::: 317 <1 <5 s10.00i> 693 <1 <5 >1i1.#IO> 912 <1 <5 .:9 T7>1182 <1 <5 >10.00:1152 <1

K Sr!: Y .Ge: Li .Nb:: Sc 2a< Ti Zr

PCT PPM PPM PPM PPM PPM PPM pP1M PCT PPN::: 1.4t > Ca CT PCT

0. 0>: 0:

4

<5 <5 >:10 00;; 921 <1 5 <5 '10.00:1028 <1 9 <5>10.004:1100 <1 48 <5 *10j..101007 <1 ¢ <5 ::9:28- 10851

15 37:; 12 <20 <.<20 18:41 03 0 56 1.66 0.05 0.08 27 3 <2;j: 6 <1;f <5 <10;<.01 17 46; 12 <20<20 18::1.05 0.59 1.78 0.04 0.09 31! 4 <2:: 6 <1

: <5 <10;<.01 13:4' 22 73: 12 <20:<20 16 1 14 0.67 1.73 0;04 0.09 28 5<2::i 6 <1: <5 <10<.01 21 85:> 24 <20<20 10 1.33 0.86 1.43 0.04 0.08 26 4 <2:: 8 <1: <5 <10:<.01 10:: 29 70 18 <20?:<20 14 1 28 0.0.0 2.06 0.04 0.11 40 4 1!4:!. <1: <5 <10<.01 11:

30250;i. 24 <24,<20 5 1.21 0.73 3.21 0.03 0.11 57 4 <x;1; 5 <5 <10 0.03 14 780100 <20';<20 4 3.11 2.15 4.09 0.02 0.04 72' 4 <2'': 14 4 15 <10;0.04 11 970:> 98 <20<20 1;3942.62:469<.01 0.04 84 3 <2 :: 14 4 14 <10 0.04 6 1151:.130 <20:<20 1?4 91 3.61 6.01 <.01 0.02 105. 4 <2';'. 18 6; 20 <10 0.05 5 1011:128 <20<20 5.21 3,63 5.85 <.01. 0.02 93 4 e2';17 6 21 <10 0.05

6 1226126 <20:<20 <1 4 93 2.89 4.19 <.01 0.02 69_:: 3 <2; 13 6; 19 <100.04 4 1203147 <2[620 4.78 3.39 4.98 <.01': <.01 3 <2;:: 15 It 25 <100.05 3 1207151 <201<20 1 4 74 3,50.5 17 041; <.01 80:I 3 <2;:: 12 8 27 <10.05 5 1063::136 <20::<20 4.79 3.37 3.91 <;01; <.01 56: 3<2i; 10 04 23 <10 0.04 3 1320::168 <20: : <20 4.49 3.32'S 43 0.02 <.01 85;i 5 .<2:; 9 4 29 <10::0.08

5 1083:144 <20 <20 <1::4 87 3;21 3.78 0.01„i<.01 3 7 16 <100.06 4 995 133 <20 <20 <1;5 09 3 91 0.51 <'.01 , <.01 103 4 <2: 9 22 <100.07 3 1031111 <20 <20 <1::4 88 441 $95 <.01<.01 104':i 4 .4' 8 13 <10.04 3 1141.131 120 <20 <1 4 52 3 58. 5.10 0ŸO1':;<.01 84: 4 <2: 10 17 <10.07 3 1066119 <20 <20 <1.4 04 3.36 4760.01:'<.01 4 <2: 10 13 110.06

4 1130::146 <20:', <20 A4.55 3.26 5.05 0;01;<.01 4 <2': 10 7 23 <10 0.06 5 121Q>:146 00<20 5.34 0.01 ;<.01 83 4 <2,.. 11 ?: 28 <10 0.06 3 117046 <20;<20 44.4o 3.70 6.91 0:01::<.01 113 5 12 7 27 <10 0.06 3 1086:::138 <20::<20 3<:4.78 4.15 6.23 <:01 <.01 95 3 42: 15 7: 25 <10 0.04 5 1099;151 <20;<20 1:4 56 3.69 5.04 0',020.01 79i 4 <2> 13 28 <10 0.06

6 11149. 144 7 .720 144

<20;4<20 <2(}:;<20 __..

. 1:;5 02

. 1;:4.95 k;.31:5 40 <;01.;0.02 5«00..6.84 1:01 0.05:

-82;:

045 4 42i 5 <Z

15 19

7 4: 7::

26 26 <10

<10;:40.06 0.07

4 :412 167 <20 <20 1 4 45 3;77 6.41 0.02 <.01 98:< 4 <2: 14 9 30 <10 0.07 14 2iZ 173 <20 <20 1<:4.37 3.91 6.42 0.02 0.13 105:! 7 Q 15 9 ;: 29 <10 <40.09 74 734 156 <20 <20 2 4 75 4.53 6.65 0.01 0.91 111:: 7 <2 19 8 27 <10 0.11

Sb

PPM

<5 . 3 49; 115 <10:: <5 ..;3 b4;: 121 <10:; <5 4;79i:. 149 <10:; <5 ..5.00: 152 <10:: <5 .4 21;; 168 <10

Mn 7e;:; Ba V Sn:; W Le;: Al PCT:: PPM PPMb?PPM PPM::PPM PPMI;::PPM PPM; PCT

ITS - Chimitec - Bondar Clegg, 1322-B Harricana, Val-d'Or, P.Quebec, )9P 3X6, (819) 825-0178

(DR 9937-1918 CDR 9937-1919 CDR 9937-1920 (DR 9937-1921 (DR 9937-1922

CDR 9937-1923 (DR 9937-1924 CDR 9937-1925 (DR 9937-1926 CDR 9937-1927

23 0-6 642i <2 84 7 422.187 <:.2: <5

61 1-1 1172: <2 8.6 3 401 159 <:2 <5

21 >0 6 286. <2 83: 4 314 139 <.2 <5

122 . 2.3 1805:. <2 ..88i 5 65:7.365 0.4 <5

5 0.4 189 <2 78! 2 299102 0;2 <5


2.5 522:4i 1.1 823

1.3 1183: 1.1 938: 1.5 1423

<2 103:: 5 555 361 0.5: <5 <2 :78: 2 347 124 <2. <5 <2 75 <1 390'100 <2 <5 <2 87. 1 329 89 <2. <5 <2 844 <1 282 98 <'2 <5

<5 >10; 00 6 . <5 40 ,5. <5 y.10.00 +~. <5 '.1:0.00

.*54 <5

1017 <10:: 1154 <10: 993 <10: 1045 <10:: 1077 <10;:

430 43 75 55 96


CDR 9937-1938 CDR 9937-1939 (DR 9937-1940 (DR 9937-1941 CDR 9937-1942

55 0.8 558 <2 53 1.1 967 <2 <5 0.4 59 <2 10 0.5 173 <2 16 0.8 522 <2

43 1.3 1155':; <2 <5 0.5 102 <2 9 0.4 105: <2 10 0.6 216: <2 8 .0 .6 79 <2

74 1 374. 74r 1 422 71<. 1 271 _._. 68: <1 367 74 . 1 359

82::: <1 372 58 . <1 1811 61!:. <1 100 Oti <1 119 64: <1 215

111 <;2 <5 7 : <5 04(1. <10:i 136 fi.2 <5 .11 <5 >10.00'.:1048 <10>: 52 <.2 <5 45 <5 8,53>.:1196 <1Ef:; 77 <.2 <5 * <5 g9.80129 <10: 95 <.2 <5 . :5 <5 }10.001030 <10:

138 <:.2 <5 .414. <5 r10 00:i:1125 <10:4 43 <.2 <5 <5 <5 8.31::>1192 <10:: 48 <.2 <5 <5 <5 9.7b:;1355 <10: 56 < 2 <5 tS <5 9 20::1390 51 <.2 <5 <5 <5 .I9.31:4:1241 <10`

507 :.40 ,..1_5.05 . . -2:5.30 5.05:6.37 0.01,1.13 .2 5.21 5.83.6.18 <.01.-:0.55 25• 35 6 19-5.75 <01 0.32 .

. . . :15.26 6.865.52 <.01.0.68

1 5.00 .<1 4.74 7.84:5.38 :<1 4.42 7. 774.98

<.61.01

▪ 463:4.93 <,011<.01

1

'<1, 3.78 749:5.21 <.06.01 7.164.96 4..66.01

;:<1:4.40 737.4.07<:01 <.01

40 4.88 46.01 . . ▪ , . .

7.44:4.67 <;01!<.01 7.45:.4.19

7.313:5.89 <L01:0.31

....1:5.23 6,0t..5.21 0.0.1.32

<;,01- 0.14 2 5.36 6:43.41

(401:1.88


Geochemical Lab Report CLIENT: CAMECO GOLD INC. PROJECT: CEDAR RAPIDS REPORT: C99-62924.0 ( COMPLETE )


ELEMENT Au30 AUtej:: Ag Cu Pb Zn Mo Ni Co Cd Bi As Sb Fa:: Mn Te Ba Cr V Sn W La Al Mg Ca Na K Sr Y Ga Li Nb Sc Ta Ti Zr UNITS PPB G;t.PPM PPM PPM PPMPPMPPM PPM PPM PPMPPM- :PCT PPM !MPH PPM F1144 PPM !PH. PPM !,114 PCT PCI PCT PCy PCT PPM PPM PRI. PPM PPM -PPM PPM PCI PPM

SAMPLE NUMBER

CDR 9937-1943 <5 0.6 112 <2 61 <1 2B2 44 <5 <5 <5 65 ....627.149 <20. 1<20 CDR 9937-1944 52 <1 200 ' 47 <2 <5 .<5 <5 7 fv.1182 <10: 44 .635150 <20.<20 CDR 9937-1945 10 0.5 79 <2 .Y.: 2 <5 <5 <5 8.50 .1249 <10 73 -642.161 <20.<20 CDR 9937-1946 81 <2 . 57 <1 195 48 <.2 <5 <5.] <5 8.24 1181 <10- 34 627 147 <20:<20 CDR 9937-1947 6 . 0.4 . 84.: <2 . 61. <1 193 . . 48 <5 <5. i <5 . 0*,0 116° 21 . 150 : h1q!.: 20:420

. . . .

CDR 9937-1948 106: <2 71 <1 254 56 <,21: <5 :•6. <5 .4,651240 <10: 40 787 146 <20<20 CDR 9937-1949 <2 66 <1 283 52 <5 <5 <5 :::6.00316 <10: 4 499.f. 126 <20 <20 CDR 9937-1950 343 57 <.2 <5 <5 <5 7.961307 <10 2 1620'113 <20 <20 CDR 9937-1951 <5 <5: <5 :1.51:1294 <10: 2 1261:107 <20 <20 (DR 9937-1952 8 <2 61 <1 363:: 54 <4; <5 c5 <5 -..7.13:1357 <10 2 1517: 99<20<20

. . . CDR 9937-1953 <5 0.2: 37 <2 62 <1 352:: 52 <.2 . <5 <5 <5 . 1 ...7.20. 1295 <10:. 2 1607101 CDR 9937-1954 10 0.2 . TO <2 58: <1 333 51 <5 <5 <5 .::03..1365 <10 2 .1651 92 <20<20 CDR 9937-1955 <5 0.3 26 <2 .59: <1 354: 48 <:;2:: <5 <5 <5 ..„:6.40327 <10 2 1635:: 90 <20.....<20 CDR 9937-1956 20 1.0 90::' <2 68 <1 483 138 <5 AZ% <5 .. :9.961252 <10J 3 190007 <20:<20 CDR 9937-1957 <5 00. <2 :00: <1 392: 45 <5 :15:: <5 ::6.82 1304 <10:. 2 97 2P-:.<20

CDR 9937-1958 <5 I 0.2 4 <2 48 <1 338: 47 <5 <5 <5 . ..42:1216 <10: 2 1$01 99 <20-k20 CDR 9937-1959 9 :::0.2 67 <2 .49. <1 327 50 <4:: <5 :<5. <5 -:717.1176 <10 2 1377103<20<20 CDR 9937-1960 <5 <2 :53- <1 354: 51 <5 <5 <5 ;:.7...4.1248 <10 2 1259)04 <26.:<20 CDR 9937-1961 48 0.5 ...490 <2 60 <1 296 50 04; <5 <5: <5 8.18 1198 <10 15 *5'125 CDR 9937-1962 56 0.6.:391 <2 63 <1 22556 <;2! <5 ;."6 <5 ..'8.81:1010 <10:. 64 .694154 20.20

CDR 9937-1963 9 0.5 97 <2 54 <1 310 44 <5 <5 <5 ::61:94)090 8 CDR 9937-1964 38 !:6.4 238 <2 61 <1 227. 42 <.2 <5 <5. <5 i 8.61: 987 <10 46 685 143 <20:<20 CDR 9937-1965 2867 ; .:3.28 1.5 31 <2 55 <1 196 34 <4:: <5 <5 <5 ::43;401018 44, 97 :635.)44 <20:<20

161:2.

. 120 :913:

6

6 <2 5(2

237 23 25 24

8 8 7

26 <100.11 27<100.09 28 *:0.10 26 <10.0.05

92 5<2 28 7 26<100.03 <1 .

_ 3 12 26 7 25 <10 0.06 <1

3 <2 24 6 23 <10H<.01 . 49 2 A2 20 5 21 <16:k.01 cl

1 <2 17 4 20 <10-.!<.01 42 2 <2 16 4 19 F4i1

:38: 1 <2 16 4 19 36 1 <2 15 4 17 -!<10<.01 44:: 1 .12 15 4 17 1(1...,<.01 32 <1 <2 17 4 20 <10::<.01

10.: 1 <2 16 5 18 10::<.01

28 1 <2 17 5 18 <:10:;:<.01 2 <2 17 5 20(10 412 . _ 2 !2; 19 21 <I6k.01

54...j 3 <2 23 6 23 <10 0.03 <1

'71::; 4 .42 28 13 27 <10 0.10 <1

. . . 53 4 <2 21 5 22 40.02

5 29 7 25 *10::0.08 63 5 : 4:: 26 7 26 <10::.0.14






STANDARD

NAME

Bi As Sb PPM PPM. PPM

Mn )e; Ba Cr; V Stt: W LB; Al Mg Ca .;

PPM PPFI:PPM 1P01l;PPM PPMPPM PPM PCT PCT PCT

ELEMENT Au30 A.4.1..„ Ag Cu Pb Zn Mo Ni Co Cd

UNITS PPB 41T'PPM PPM:, PPM PPM PPM 00 00 PPM

<1 <20;<20

<1 420<20

2.2: <1 10'i; 10 44:

2 . ::2 2 :: 2:: 2 <.01 4.01 < 01

<1:< 01 <:0.1 < 01 <;0i1<:<.01 <1:: 41;<.01 <.01 <.01 <.01:<.01 <1:

<1 <1 : <1 <1 <1>< 01 4,0E4.01 01 <01<.01

6S.

4 1 19 0; 1.11 0.04 0.10 65> 12

1

k:;1 19 0.66 1.11 0;04;0.10 12

2 2

1

8 51 4243;<20

1 1; 1

51 10.: 10

51 -

ANALYTICAL BLANK

ANALYTICAL BLANK

ANALYTICAL BLANK

Number of Analyses

Mean Value

Standard Deviation

Accepted Value

Oxide (Feldspar &

Number of Analyses

Mean Value

Standard Deviation

Accepted Value

GANNET STREAM-SED 4

Nuiber of Analyses

Mean Value

Standard Deviation

Accepted Value

Oxide (Feldspar &

Nunber of Analyses

Mean Value

Standard Deviation

Accepted Value

Oxide (feldspar &


Mean Value 969

Standard Deviation

Accepted Value 968

<1 <1(~'; <1

<1 4 <1

2 <1 5>: <

11 0:.3 <5 ';1:1 <5 ;;?2x99:1:1275 410>:763

1 1 1.::1. 1 1:: 1 11 0.3 3 1i1 3 2.991275 5::763

2 :'23 11 O;i

<1 ~~ <1 <:2;' <5 <1 :<1 . <1 <.C:i <5

2 2 2 <1 t1; <1 0.:1:1

tiU Intertek Testing Services Chimitec Bondar Clegg Rapport Lab Geochimie







Mg Ca

PCT PCT

STANDARD ELEMENT Au30 Au Pei Ag Cu> Pb Zti; Mo N.i Co:CO:Bi AS Sb NAME UNITS PPB G/T PPMPPM; PPM PPM: PPM PPM PPM 'TON PPM PPM

Cr< V Sn W Le Al

PPM. PPM PPM PPM PPIR PCT

K Sr;: Y ;.GA;: Li :Nil; Sc tS:; Ti

PCT PPM:PPM PPM:;PPM PPM;.PPM PFM:; PCT

18

102: 7 181<: 1

102: 7 .81 1 3.6

11 1$0.; 2 40!;'

756 <10170 55:117 < : <20 333 14 ,0-98 114:0.31 35:: 8 24 :' 7>: 10 <10 0.15

1 1 1> 1 1,:1 1

756 5';:170 55017 10 10 3.33 1.63!0.98 0:050.31 35:: 8 0.15

720 <1>200 54133 3.09 1:8.3:1.08 0R06:;0.32 ; 39;: 9

BCC GEOCHEM STD 5

Number of Analyses

Mean Value

Standard Deviation

Accepted Value

0 9

0.9

.7 'I




REPORT: C99-62924.0 ( COMPLETE ) DATE RECEIVED: 07-0CT-99 DATE PRINTED: 21-OCT-99 PAGE 5 OF 5

14 14

18 <2();<20 18 <20::<20

7 <1 :; <5 '10.01 <5 <105<.01

4 7 4Q

1.28 0:8.0 2.06 0.04 0.11 1.29 0.81 2.12 0 04>:;0.12

19 <10 ::0.04 20 S10 0.05

4.93 2.89 4.19 <.01 0.02 69:: 3 <2 13 5.23 3.11 4.48 <:01 0.02 72; 4 <2 : 14

V

$0 PPM PP1

W A..k Al Mg`; Ca PPM PMI{.: PCT POj PCT

CDR 9937-1934 53 zh.1 :967 <2 74 1 422 136 .5.g. <5 11 <5 >10.00 Duplicate 0.9 992 <2 75 1 427.137 <.2 <5 10 <5 >10.00

1048 <10: 5 121111146 <20:<20 A>:4.61 3.:525.34 0;A1'';:<.01 1059 <10;: 5 124043 <20::<20 4.65 338 5.51 0.01<.01

28 <100.06 27 <10 0.07

83 4 11 83>: 5 <2 11

21 <10;<.01 2 125 104 <20k20 4.66 7::78 4.76 <.01:;<.01 42:<: 2

SAMPLE ELEMENT Au30 AU re] Ag CU Pb Zn Mo Ni Co Cd Bi As S NUMBER

CDR 9937-1917 <5 0 3 394 <2 32 2 <58 67 <.2 <5 :<5i! <5 Duplicate 6 0 3 406 <2 33 2 69. 68 <.2 <5 <5;! <5

CDR 9937-1923 23 0.6 642 <2 84 7 422 187 <.2. <5 ::<5 <5 >10.00 Prep Duplicate 18 0.8 705 <2 87 8 441 191 <.2 <5 <5 <5 >10.00

Mn Te Ba

PPM PPM>PPM

168 <10; 29 169 <10> 31

921 <10>: 6 1225>126 <20:€<20 968 <10: 6 1301 126 41:<20

K r SrLi NIS: Sc Ti : PCT PCT PPM>PPM PPM;PPM PPM;PPM PPI!4': PCT PPM UNITS PPB O/T:PPM PPM PPM PPM PPM PPM PPM PPM PPM PPM

CDR 9937-1960 <5 < 2 34 <2 153< <1 353. 51 i<2 <5 <;<5. <5 .1:7.42:1248 <10;


Duplicate <5

19 0: <20 7 720::144 <20

0: 2 1507101 <20<20 0: 2 1572. : 97 <20<20

38:> *1-

16 16 ~

CDR 9937-1939 <5 0.5 :102 <2 :58 <1 181 . 43 <2 <5 !'<5;;' <5 Duplicate 5

CDR 9937-1953 <5 0 2 37 <2 :62; <1 352 . 52 <.2 <5 <5 <5 Duplicate 0.3 34 <2 <1 340. 50 4.2 <5 <5 <5

4.95 5.006.84 ::<-01.:0.05 .111:

4.24 7.63 4.93 <.01 <.01 <1 4 09 7.29 4.83 <.01 <.01

1192 <1

720';;1295 <1

6 94:1253 <1

26 <10'.0.07

19 <W<.01 19 <10: 1<.01


REPORT: C99-62925.0 ( COMPLETE ) REFERENCE:


PROJECT: CEDAR RAPIDS SUBMITTED BY: D. BABIN



50 -150 50 CRUSH/SPLIT & PULV. 50 PULVERIZATION 34

DRILL CORE



991018 1 Au30 Gold 50 5 PPB Fire Assay of 30g 30g Fire Assay - M 991018 2 Au rej Gold assay an rejet 33 0.03 G/T FIRE ASSAY FIRE ASSAY 991018 3 Ag Silver 50 0.2 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991018 4 Cu Copper 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991018 5 Pb Lead 50 2 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991018 6 Zn Zinc 50 1 PPM HCL:HNO3 (3:1) INDUC. COU1P. PLASMA

991018 7 Mo Molybdenum 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991018 8 Ni Nickel 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991018 9 Co Cobalt 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991018 10 Cd Cadmium 50 0.2 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASM 991018 11 Bi Bismuth 50 5 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991018 12 As Arsenic 50 5 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

991018 13 Sb Antimony 50 5 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991018 14 Fe Iron 50 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991018 15 Mn Manganese 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991018 16 Te Tellurium 50 10 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991018 17 Ba Barium 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991018 18 Cr Chraniun 50 1 PPM HCL:HNO3 (3:1) INDUC. COLA. PLASMA

991018 19 V Vanadium 50 1 PPM HCL:HNO3 (3:1) IMDUC. COUP. PLASMA 991018 20 Sn Tin 50 20 PPM HCL:HNO3 (3:1) INDUC. COLA. PLASMA 991018 21 N Tungsten 50 20 PPM HCL:HNO3 (3:1) IMDUC. COLA. PLASMA 991018 22 La Lanthanum 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991018 23 Al Alunir= 50 0.01 PCT HCL:HNO3 (3:1) IMDUC. COUP. PLASMA 991018 24 Mg Magnesiun 50• 0.01 PCT HCL:HNO3 (3:1) IMDUC. COUP. PLASMA

991018 25 Ca Calcium 50 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991018 26 Na Sodium 50 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991018 27 K Potassium 50 0.01 PCT HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991018 28 Sr Strontium 50 1 PPM HCL:HNO3 (3:1) IMDUC. COUP. PLASM 991018 29 Y Yttrium 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991018 30 Ga Gallium 50 2 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

991018 31 Li Lithium 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991018 32 Nb Niobium 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991018 33 Sc Scandium 50 5 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991018 34 Ta Tantalum 50 10 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA 991018 35 Ti Titanium 50 0.01 PCT HCL:HNO3 (3:1) IMDUC. COUP. PLASMA 991018 36 Zr Zirconium 50 1 PPM HCL:HNO3 (3:1) INDUC. COUP. PLASMA

REMARKS: IS indicates Insufficient Sample

REPORT COPIES TO: i16-1349, KELLY LAKE RD. INVOICE TO: 86-1349, KELLY LAKE RD.

**************************************** tut**********k********* *****************

This report mist not be reproduced except in full. The data presented in this report is specific to those samples identified under "Sample Number" and is applicable only to the samples as received expressed on a dry basis unless otherwise indicated

********************************************************************************

ing6jIntertek Testing Services Chimitec Bondar Clegg Rapport Lab Geochimie




Feu Intertek Testing Services Chimitec Bondar Clegg


PROJECT: CEDAR RAPIDS DATE PRINTED: 26-OCT-99 PAGE 1 OF 5 DATE RECEIVED: 07-OCT-99

62 79 63 75'. 78

<1 2801: 49 <;2:.: <5 <1 190:: 65 <.2::: <5 1 342::: 52 < 2:: <5

<1 253„, 42 0.2: <5 1 232: 56 0.2> <5

1 1

4.63 6.333, 5.71 7.12 4.69 i6.24: 5.36 5.63: 5.53

53 67 44 77

4.05 <.01 0 07 4.62 0.01 2 76 3.05 0.01 1 19 5.74 0.01 1.86 5.35 0.01 1.88

<1

14 <10:0.08 27 410::0.14 6 <14:;0 11 <1!> 25 <10::0.14 26 <10:! 0.15 <'f

3741 1448 1937 1230 3065

18 69

<5 b: 10:

3.03 4.7

1.64 0.9 1.86 0.9 2.58 0.8 4.14 1.6

œR9937-1968 œR9937-1969 œR9937-1970 œR9937-1971 œR9937-1972

<5 >10.003:1046 <10 <5 *10 00<:1098 x10 <5 >10.00::1071 <1.0 <5 >10.00::1017 <10 <5 >100:1007 <10

62 588A28 <2020 88 731 158 <2020 81 .723. .160 <2020 81 .764:157 <2020 50 692 146 Q0,:<20

1.4.33 4.22 6.26 0.01 1.20 1 5.73 5.54 5.38 0.01 1.71

<1 5.50 5.38 5.23 Q 01::1.56 <1 5.58 5.50 4.82 0 01':1.54 1,4.67 4.61 5.41 0.02;:0.97

<2 93 1 348118 O..âl<: <5 <2 .87> 1 225: 54 <.2:: <5 <2 79.; 1 203 51 0.x;' <5 <2 77<? 2 221 58 <.2 :': <5 <2 71 2 246:: 90 0.2: <5

20 g> 21 <10 0.12 <1 7 .<2:< 26 .. . 7 26 <10:;0.15 . 4:1::

8 <2 :: 24 7:: 26 <10': 0 15 <1 _.. _. . 7 <2 24 8 27 <10:0 15 <1 7 <2 21 6: 23 <10:0.12

78 79

113;', 90:!

86

2937 <2 1772!: <2

6771 <2 2098 > <2 3411:; <2

œR98330-2013 CDR9830-2014 CDR9830-2015 œR9937-1966 œR9937-1967

_.. _._. .._

<5 0.2 ::1QQ<;; <2

871 0.5 140:> <2

<5 0.2 39 i <2

1114 1.09 1.7 1611 <2

454 . 0.40 0.8 812 ' <2

941021 ~0: 1947 123 ~20:;<20 9.14.`: 1231 <:1()11: 1129189

6` <5 b.57: 972 <10 49 1>rN 129 •2Q::20

<51 <5 9.32:1054 <10 90 ..727 157 ~LQ>: <20

<5,< <5 .>.10.04`1048 <1t$ 96 .75Q:164 QQ:<20

6 18 4 <Z:: 23 7 19

6 1411 26 6 <2; 26

œR9937-1973 œR9937-1974 œR9937-1975 œR9937-1976 œR9937-1977

877 0:88: 0.9 ^217: <2 78 <1 197 6159 6.30 4.0 4364' <2 108::' 1 198!

1388 M4,0.7 7 ...:.839< <2 90i <1 186

2116 2.16i 1.3 .. 1870 : <2' 91::: 1 147 2012 2.58 1.6 2069 : <2 ; :12. <1 131:

55 <.2: <5 <5:;: <5 >10.00:: 995 <10 35 :790'169 <20 133 6:3.: <5 14`: <5 >10.00:1150 K10 46 .760166 <20 56 <.2 ;: <5 a > <5 ;',10:00.: 955 <10 44 ::130-'159 QQ 52 <.2<: <5 â> <5 ..9.03: 844 40 36 711149 <20 47 < 2:: <5<.5;> <5 .. 8.02;: 731 410. 38 650 143 s20

5.21 5.184.59 0,02 1.5.995.71::423001: 1 5.23 5.05.3.73 0,02 1 4.40 4.173.48 0.02 1 3.81 3.50 2.80 0.03

0.67 E1;;

092 55 088.43> 0.71 . 44 :: 0.72 3H:

9 r2'; 23 6 <2:' 26 7 ~; 23 7 ..<Z:: 20 7 <2 :: 18

21 .10 21 <10

43f: 17 410 7' : 15 410

11 <1Q

0.15 <1 0.13 . <1 0.14 0.14 0.14

<20 <20 <20 <20 <20

œR9937-1978 œR9937-1979 œR9937-1980 œR9937-1981 œR9937-1982

4273 3.12 2.4 812 0.48 1.3 7154 4.23 4 2 1215 1.36 2.4 3953 3.85 9.4

<1 185:109 0 3;: <5 15:; ô <1 147:: 59 <,2< <5 g* <5 i. .0*: 1 165:: 980.6:; 8 5iR <5 1410 1 142': 55 0.2<: <5 IC <5 Mt* 1 276':'161 0.2< <5 iViiA a >10.Q01

715 <10 33 725 110.. 41 693 <10:. 29 663 <10. 38 716 <10. 46

615116 +281<20

632119 <2020 $85106 0020 584 111 574 110 <20;<20

1 3.78 3,40 2.45 0 03;;0 63 3'.... 1 3.81 3.27 2.46 0.03;0 78 36 5 1 3.62 3,11';;2.13 Q02;0 55 32; 4 1:3.59 3.10:;1.94 0.03:!0.73 . 30:: 4 1 3.89 3,44<:'2.16 0,02.:0.94 .31 4

<2 : 18 . 5 > 7 <10:::0.13 <2 19 5 7 i10:0.14 <2 :: 19 6'<i 6 <10;0.13 .42> 19 . 5:: 6 <1(!<:0.13 <2 21 4:> 7 410::0.13

œR9937-1983 œR9937-1984 œR9937-1985 œR9937-1986 œR9937-1987

Q40;;04 1.47:1.0

.4

! .26.2.8

36ô'< 2 : 73'< 1 .189. 44 < x;: <5 i130,51 <2 b3 2 160:: 47 < 2 : <5 837 <2 69 <1:183: 89 <.2:: <5 470. <2 52;: 1 :190:; 92 <.2:: <5

2287 <2 :: 82 ; <1 284304 0 5; <5

a 7 41:; 777 ~10: 19 :t47T' 118 <20 QO ~; b 7 14; 758 ci:0. 26 âtl6 110 <20. <20

9.45> 806 <10 42 . 620 123 <20 <20 15:;: <5 7 87; 738 c10i.. 22 593. 108 +20, 20

53;: <5 y4 887 <~0: 18 bQ1 129 ~0 <20

2 4.18 3.80 2.39 0 03;:0.32 2.3.42 3.073.47 0.02 0.47 1 4.03 3,583.23 0.02 0.77 1 3 38 3:15.3.15 0,05 0.36 36

<1 4.67 4 21 3.26 0 01 1.15 40

6 <10:0.17 5 <10::0.12 ;.

7 «0;0.13 <5 <10:0.12 16 <10:0.13

1052 1069 1040 4190 2270

œR9937-1988 œR9937-1989 œR9937-1990 œR9937-1991 œR9937-1992

2834 3.26!I 0.9 571 < <2 :' 69 1 1$4 1070 0.88 0.8 249 Q. 65 <1 215

484 4.11 0 6 ;306. <2 58 <1 212

92 0.08::0 9 720 <2 >82:: <1 255 2411 0.74 3 5 .:2889 <2 ::95:: 1 690

51 Q,2;; <5 <5;i ~ 9 56;:1053 <10 61 66 < 2:: <5 ..7;: <5 8 73;: 962 <10, 51 678.143 +20.<20 41 <,2; <5 <5 14,1:k 860 c10 27 .679:138 <20 <20 57 0 2; <5 <5;: <5 >10 001106 AX . T29 165 <20 <20

225 0 7:;: <5 36;;: ~ >10 00<:1306 <10: 67 b4S 136 4C<20

x 4.78 4,$3 5.35 0.02: 1 4.72 4.67 4.32 0.0Z 1 4.26 4.403.670_02 1:;5.73569:4.640f11::

2 6.01 5,71 <;6.32 4.01:

1.13 :61; 7 +~:: 23 7 16 410.i0 13 <1:::

0.86 53 7 <2 21 7'• : 12 <10 0.13 <1.:

0.45 47:; 8 <2 19 7:: 7 <10 0.14 ..?t1.

1.40 59 8 <2 26 8 17 <10:0 15 0: 1.29 80:: 8 <2 28 5;: 22 <10::0 12 <1:


SAMPLE ELEMENT Au30 Au réj AEI NUMBER UNITS PPS O/T

Pb .*: Mo Ni:

PPM PPMPPM PPM Coi".d; Bi

M:::PAS:;

PPM PPPM PPMP Mn .Te.. Ba

PPM PPM PPM Ca Na: K Sr :::: Y Ga< Li Nb

PCT PCT: PCT PCT PCT PPM PPM PPM PPM FPO Sc Ta Ti PPM PPR PCT PPM

Gr . V >Sn W La;: Al 10'

144. 6" PPM PPM PPM'.


IOW Intertek Testing Services Chimitec Bondar Clegg

DATE RECEIVED: 07-OCT-99 CLIENT: CAMECO GOLD INC. REPORT: C99-62925.0 ( COMPLETE )


Ma

PCT::

SAMPLE NUMBER

Al Mg';; Ca PCT :PCT PCT

K Sr Y ;G8. PCT PPM:.PPM PPR

Mn Te Ba

PCT:: PPM PPMPPM Cc V 'Sri W .<La '

PPM PPM PPM PPM PPM,

Li Nh;: Sc .T Ti :Zr PPM PPlS;PPM PPMI:: PCT PPM::

ELEMENT Au30 Au rel:: Ag Cti : Pb : 2ti : Mo : lli ;: Co td;: Bi :<7 UNITS PPB Gl1:PPM PPM:PPM PPMPPM PPM`PPM PPN;PPM PPM,`.PPM _

<5

<5

<5

<5

<5

0.9 1138;:! <2 : 67 <1 463 41 <2:; 0.3 . ':582 > <2 : 81>: <1 448 > 37 <.2

209; <2 : 70; <7 433: 59 <.2 0.2 167 <2 60 <1 336 39 <.2 .4 ...>187. <2 :;79:: <1 446 52 <.2

<5; <5::

<5

<5

<5 <5

<5

<5:

<5:

<5

<5

<5

<5

<5

15

6,20;i 883 <10 .

7.16:: 967 <10:.

7.35:1162 <1B:

S 08: 769 <10:

8051222 410

3.93 873 <10.

6.68 939 <10.:

9.10: 998 <10: 7.40 1055 <10. 7.50 1000 <10.

.,..... _.. 102 745158 <20: <20 2 5.84 5.74 4.91 0 01:;1.83 69. ! 8 A2'. 28 7; 24 <10 0.15 78 . .736154 40; <20 2.5.73 5.88:4.83 0..01::1-53 70r 8 ,<2: 26 T: 20 <10 0 14 ~1'z

93

.719149 40; <20 3.5.69 55$':5.44c01.;!:1.94 81» 7 ,42 28 6 24 <14'i0 15 <1;

82 583 130 <¢0: <20 14.31 4.18 `{5.60 0.01 !:1.77 93I 6 <2. 23 5 20 <10:0 13 <1;

71 .11055 <20: <20 3 5.65 5,974.21 0,01:;1.52 6$:: 7 28 6:: 25 <10.>0 14 <1;;

27 442 : 45 ~0 <20 ;:23 1.43 :1 52 1.64 0,02 0.19 39;:i 14 8 2:: 7 <100.12 : '::8:: 58 648 128 QO <20 >1 4.76 5.12 8.99 0 01;:1.37 151 10 25 6`: 22 <10 :0 13 73 *048 <20 <20 :> 1 5.46 5,684.94 0.01 1.90 84 5 52 27 6:: 23 <10 0 14 <1

28 20k 95 Q0::<1:4.06 40 _.. 5.31:2.85 _.... <.01>0.80 _.__.... 47>: 4 17 35 211.6 97 40 40 <1 3.90 5,21 2.28 < 01 0.99 39 3 ~ 17 4 :: <5 <10:0.08

28 1901 95 <20;Q0 <1 3.66 4.84 3.58 <-0 0.84 56 3 K2 15 4:: ô <10:0 08 s1::

22 2278 110 <20:.Q0 4.33 5.70 3.56 <.01; 0.65 57: 5 17 4: 7 <10:0 08 .<1" 22 2215 112 +?20 QO 4.12 5.485.15 <41i 0.62 82' 3 ~ 17 5 > 11 <10;:0 06 7 1335 64 fZ0 QO 11 2.95 4.41 3.25 0.01:: 0.06 71 8 <2:: 12 3 8 <10;:0.05 ...;2'.:

13 2371:116 Q4.<20 t1 4.53 5.84::5.13 <.01:0.41 83' 3 17 5% 14 :A10:1 0.06

_ .. 16 .75:1 37 <20: <20 12 ::1.99 3 14.s5.74 0..02i 0.08 139 10 <2 8 1:< 6 <10:i0 04 9 2354 123 <28 :..420 .<1.4 13 5:49.3.85 <41, 0.24 65 3 <2 17 5>; 22 <10 <0.04 .<

5 2179113 <20.<20 :<1 4.00 0.13 78:; 3 <2' 17 21 <10;:0 02 ........ ; <

8 232020 <2.0i:::.<20 0.19 74:: 4 <2 19 ;5 20<10003:< 14 5 62,4.14 0.36 63;: 4 4 18 $::: 20 <10;0 04 <


CDR9937-1993 62 CDR9937-1994 319 CDR9937-1995 270 CDR9937-1996 39004 CDR9937-1997 436

CDR9937-1998 123 CDR9937-1999 144 CDR9937-2000 3243 CDR9937-2001 86 CDR9937-2002 <5

CDR9937-2003 49 CDR9937-2004 12 CDR9937-2005 101 CDR9937-2006 171 CDR9937-2007 21

CDR9937-2008 32 CDR9937-2009 19

CDR9937-2010 183 CDR9937-2011 24 CDR9937-2012 33

0.16 0.7 163:; <2 0.26 0.5 94;; <2 0.24 0.7 542 <2

IS 2.5 . 3164 <2

83 > <1 232; 54 0 2::: <5 76,' 1 249;: 53 < 2;:: <5 87 <1 208;: 61 <.2« <5 112:: <1 :146; 62 0.4:: <5 741. 1 238' 54 0.2:!s <5

380-: <2: 30I:: 1 : 77<'. 19 <.21i: <5 2~ <2 : 64 ; 1 2101: 41 < 2'<: <5

1856 : <2 : 93 <1 :409' 57 0,3 !: <5 --:1-

52.. <2 48.. <1 510:I 33 <.2.; <5 <2 66; <1 538';; 34 <.2: <5

<2 : 38:: 2 210; <2 :5ô; <1 $66s

<2 ; 59:: <1 442> ...

<2 ::59; <1 397:

<2 :: b1 > <1 377,

32 <.2::: <5 38<.2:<<5 1074 <5 45 <.2: <5 47<2s: <5

<5 . 1.0.00: 1123 <10 <5 <5 9..85:1104 <10 <5;;: <5 >10.00:1185 <10 <5 <5 9.34:' 1051 <10 <5.!: a 9.91:1080 <10

<5':; <5 3.07 339 <10 <5 <5 .8.221405 <10 <5; <5 ?i0.00: 1147 <10 <5;< <5 6.23: 800 <1b

<5 <5 ô.16: 725 <10

STANDARD ELEMENT Au30 AwreLi Ag

NAME UNITS PPS G/T PPM

ANALYTICAL BLANK

ANALYTICAL BLANK

ANALYTICAL BLANK

Number of Analyses

Mean Value

Standard Deviation

Accepted Value

Oxide (Feldspar &

Number of Analyses

Mean Value

Standard Deviation

Accepted Value

BCC Au Std.12

Number of Analyses

Mean Value

Standard Deviation

Accepted Value

< 01

<.01






Pb 7)t;: Mo Ni::; Co Câ< Bi AB;;

Mn Tés Ba

PPM PAP PPM I PFFPPM PPK;:PPM PPII ;PPM

PGT: PPM PPM::PPM

_._.. _... _.. __....

Q ::

<1 <1::' <1 <,x;; <5 r5:: <5 <0.41:; <1 <10: <1

<2 <1 c1.: <1 < 2: <5 <5; <5 <0 01: 2 K10>: <1

2

2. 2<!: 2:..2< 2. 2: 2 2i:: 2 ::2s: 2

<1'< <1 A:;: <1 0.1 ':' 3 3 3<0.01

W :18 Al ►~: Ca

K f Y Aff Li 41 Sc >Te

PPMPPM PPM':PPM PPM:;: PCT

PCT

PCT Pp![ PPM PPM PPM PPM' PPM PPR

<1 40:<20 '<1 <.01 <41;<.01 <,0i. <.01

<1 <20 :<20 ::<1;<.01 <.01><.01

2 2. 2 2' 2 2':: 2 2: 2

<1 ;:10 10 !;<1;;<.01 c.01;i<.01 AA '<Al

<.01

b <10

<5 <10.

2: 2: 2.2 2 Z 2 :::Z>:

<1 1: <1 3 5i :<.01

BCC GEOCHEM STD 5 8

Nunber of Analyses

Mean Value 8 8b> 1

Standard Deviation

Accepted Value 11

Oxide (feldspar &

Number of Analyses

Mean Value

Standard Deviation

Accepted Value

3: 22

. . ... .... ....

_.. _..... 748 <10 160 ::57:127

1 . ;1 1 :.T 1

748 5 160 5:7127

720 <1 200

;3.59

10 10 : 73.59

4. 1 3.09

1 M::1.05 0,05::0.31

1..43.:1.08 0.06>:0.

1..75;:1.05 Q1,44 .>0.31 40.

1 1:


W !La Al PPM PPM PCT PC1;'

Mn . Te; Ba : <:Cr V <:Sn PPM PPM PPM PPMPPM PPM

...............

STANDARD ELEMENT Au30 Au.#'è]: Ag NAME UNITS PPB G,fT .PPM

Oxide (Feldspar & 178 Nuiber of Analyses 1 Mean Value 178 Standard Deviation Accepted Value 186

CARNET LAKE-SED 2 Number of Analyses Mean Value Standard Deviation Accepted Value

0.3

0.8

1 0.3

Ca K ::5r Y .GB: Lt Nb.i Sc Ta' Ti PCT PCT; PCT PPM PPM PP1l PPM PPM PPM PPM;: PCT

<20 1

10

;.S8;;1.73 . > 1,: 1 €58 1.73; _..

0,64 ;; 1 0.64 _._.... _..

0.61

0.61: 1 0.04;:0.25

..1:: 1 0. 04 :0 25 .:. 32; 29

1829 #10 191 32 : 47 <20 1 1 1 1 1 1

1829 5 191 32 47 :1i1 _... ...._. ...

1840

_.... CtS:; Pb Mo 4t

':PPM!:IPPM PPM::PPM PPM

Co id>: Bi AS;: Sb PPM PPMPPM PPM;PPM

38 199;>i 1 25;i; 17 0.9'<> <5 11:; 1 11' 1 1:: 1 1;: 1 1;':

38 .199;' 1 25: 17 0.9:; 3 11:

40 200::: 2 23 i:; 17 0$:; - 9>

<5 1

mou Intertek Testing Services Chimitec Bondar Clegg Rapport Lab Geochimie

Geochemical Lab Report CLIENT: CANECO GOLD INC. PROJECT: CEDAR RAPIDS REPORT: C99-62925.0 ( COMPLETE )






PROJECT: CEDAR RAPIDS DATE PRINTED: 26-OCT-99 PAGE 5 OF 5 DATE RECEIVED: 07-OCT-99

ô ~.40`:1055 <10. 8 234,020 +QO€:I

81 78

<1 448:< 37 (.2. <5 <1 432> 36 < 2:: <5

;QO <20

<5 7.16 967 t10'; 22 2278 110 <20 <5 6.89>! 934 <10 21 2214 109 S20

4.33 5.70 3.56 <:11: 0.65 57 5 <2 17 4.17 5.283.48 <.01 0 64 54€ 5 17

82:: $1>:

:601 .:

600

__ . _. <1 284:304 9.A:! <5 <1 285'327 (1.5:: <5

<5 )10.00: 887 <10: 18 <5 r10 00;i: 865 <10 11

860 s10: 27 <1 212.; 41 <2 : 6

W La Al < M9: Ca :Ma K sr; T Ga> Li'NO; sc :Ta PPM PPM PCT POT; PCT . PCT. PCT PPM. PPM PPM. PPM PPM PPM PPM

v :sn PPM PPM

Ti PCT PPM

SAMPLE NUMBER

...............

ELEMENT Au30 AU reji : Ag

UNITS PPB G/F PPM

œR9937-1968 3741 3.03 4.7 Duplicate 2545 4.7

CDR9937-1978 4273 3,12 2.4 Duplicate


_.... ~► 7 c10€:0.08

7 <10;A.08

<10:0.03

K1

œR9937-1987 Prep Duplicate




PPM

Mn Te> Ba PPM PPN'PPM

Pb Zn Mo Ni": Co DJ < Bi PPM PPM (;FN ;:PPM PPM PPM PPM : iPPM PPM

183 195

620 653

89 < 2; <5 95 <.2> <5

837 <2 69`: cl 881 <2 73 : <1

11 <5 945 806 <10 : 42 11 <5 9.93 849 <10. 42

9710 <2 93:: 1 34$:::118 0.3 <5 18 <5 >11).00 1046 <10 62 )10000 2 100 2 375 126 0.4 <5 20 <5 )10.00 1137 <10 66

2937:: ; 33 <2 78:; <1 185:::109 0 3.~: <5 15:' <5 9.34:: 715 10 ...:. . ., __:,......::

58$ 631

613

1 399. 45 4.28 5.70::4.56


019 . 79 4

128 <.20<20 132

4.33 4.22 6.26 0.01 4.76461;6.660.01

1.20 ;$0:: 7 1.24 81':: 8

21 <10 0.12 : <1 22 <10:0 13 <7;!

116 Q.020

123 420; <20 127 4,20:40

3.78 3.4 2.45 005:':0 63 31.; 5

4.03 3,44:3.23 04)k0.77 45:: .25 .0Z::0.79 .47;

7 <10:40.13

7 <10:: 0.13 <1:> 7 <10<0 13

129 420:: 20 128 Q0 ::Q0

4.67 4.21:3.26 0.01

4.55 4.10 3.15 0,01

1.15 40i: 4 1.11 39!:: 4

:< 25 5<: 16 <100.13 +~ 24 5 16<100.12

:138 IQ 4.26 4.40 3.67 0.45 8 <2: 19 0.14 20 7

DRILL CORE 1 +150/-150 1 SPECIAL METAL. PREP 1

SAMP.LE..T.YP.ES NUMBER SIZE..F.RACT.IOWS NUMBER SAMP.LE..P.REPARATIOMS....NUMBER

REPORT COPIES TO: #6-1349, KELLY LAKE RD. INVOICE TO: #6-1349, KELLY LAKE RD. **********************************************rt,r**1 ******4***4.***fir*************

This report must not be reproduced except in full. The data presented in this

report is specific to those samples identified under "Sample Number" and is

applicable only to the samples as received expressed on a dry basis unless

otherwise indicated ********************************************************************************

Intertek Testing Services Certificat D'Analyse Chimitec Bondar Clegg Assay Lab Report




DATE

APPROVED ORDER ELEMENT

NUMBER OF

ANALYSES


LOWER

DETECTION LIMIT EXTRACTION

REFERENCE:


DATE PRINTED: 15-OCT-99

METHOD

991015 1 AU Avg Gold Average 1 0.03 G/T FIRE ASSAY

991015 2 WT+150 +150 Pulp Weight 1 0.01 Gr.

991015 3 Au+150 Gold +150 mesh 1 0.03 G/T FIRE ASSAY

991015 4 Au-150 Gold. Minus Fraction 1 0.03 G/T FIRE ASSAY

991015 5 Wt-150 Pulp Weight -150 1 0.1 Gr.

ITS - Chimitec - Bondir Clegg

1322-B rue Harricana, Val d'Or, Québec, I9P 3X6

Tél: (819) 825-0178, Fax: (819) 825-0256

Intertek Testing Services Certificat D'Analyse Assay Lab Report Chimitec Bondar Clegg

REPORT: C99-62925.1 ( COMPLETE ) DATE RECEIVED: 07-OCT-99 DATE PRINTED: 15-OCT-99 PAGE 1 DE 2


CDR9937-1996 12.75 31.93 203.97 2.98 625.0

SAMPLE ELEMENT AU Avg WT+150 Au+150 Au-150 Wt-150

NUMBER UNITS G/T Gr. G/T G/T Gr.

ITS - Chimitec - Bondar Clegg 1322-B rue Harricana, Val d'Or, Québec, J9P 3X6

TéI: (819) 825-0178, Fax: (819) 825-0256

REPORT: C99-62925.1 ( COMPLETE ) DATE RECEIVED: 07-OCT-99 DATE PRINTED: 15-OCT-99 PAGE 2 DE 2

BCC Au Std.11

Number of Analyses

Mean Value

Standard Deviation

Accepted Value

9.50

9.497

9.90 9.90

Oxide (Feldspar &

Number of Analyses

Mean Value

Standard Deviation

Accepted Value

2.91

1

2.914

•


STANDARD ELEMENT AU Avg WT+150 Au+150 Au-150 Wt-150

NAME UNITS G/T Gr. G/T G/T Gr.

EMI Intertek Testing Services Certificat D'Analyse Chimitec Bondar Clegg Assay Lab Report

ITS - Chimitec - Bondar Clegg

1322-B rue Harricana, Val d'Or, Québec, J9P 3X6 Tél: (819) 825-0178, Fax: (819) 825-0256

APPENDIX 3

WHOLE ROCK ANALYSIS CERTIFICATES FOR DRILL CORE



Val d'Or, PQ, Canada

"URGENT & CONFIDENTIAL"

To: CAMECO GOLD INC. Our Fax No: (819) 825-0256 Attention : MR. MIKE KOZIOL Your Fax No: 1-705-523-4571 Reference : 170418 Number of Pages : 3 including this page. Submitter : D. BASIN

Report : C99-62926,0 statue : COMPLETE Total number of samples: 32

Element Method Totl Element Method

Totl Element Method Totl

Si02 INDUC. COUP. PLASMA 32 TiO2 INDUC. COUP. PLASMA 32 A1203 INDUC. COUP PLASMA 32 Fe203* INDUC. COUP. PLASMA 32 Mno INDUC. COUP. PLASMA 32 Nq0 INDUC. COUP. PLASMA 32

Cao INDUC. COUP. PLASMA 32 Na20 INDUC. COUP, PLASMA 32 K20 INDUC. COUP, PLASMA 32 P205 INDUC. COUP. PLASMA 32 LOI GRAVIMETRIC 32 Total 32 8a INDUC. COUP. PLASMA 32 Cr INDUC, COUP. PLASMA 32 Sr INDUC. COUP. PLASMA 32 8r XRAY FLUORESCENCE 32 Y XRAY FLUORESCENCE 32

Sample Preparations Totl sample Type Totl Size Fraction Totl I Remarks

CRUS!/SPLIT & PU/V. 32 DRILL CORE

32 -150 32

Notes:

If you do not receive the entire transmission in legible form, please call us at (819} 825-0178.

FAXSR: ITS VAL D'OR At 3-NOV-1999 09:53 Pacte 2



SAMPLE ELEMENT Si02

NUMBER UNITS PCT T102 PCT

A1203 PCT


Fa203* Mn0 Mg0

PCT PCT PCT Ca0 PCT


DATE PRINTED: 3-NOV-99

Na20 F20 P205

PCT PCT PCT

PAGE

LOI

PCT

lA( 1/ 2)

Total PCT

CDR 9906-A 42.82 0.45 9.40 11.25 0.14 18.79 6.03 <0.01 0.74 0.04 10.23 100.06 CDR 9906-13 47.30 0.65 12.67 11.98 0.14 11.37 10.60 1.71 0.29 0.05 2.88 99.75 CDR 9906-C 46.02 0.68 13.26 15.87 0.16 6.79 8.64 1.58 0.41 0.06 6.42 99.98 CDR 9906-D 49,25 0.65 14.25 10,69 0.16 7.16 9.28 3,30 0.07 0.05 4.20 99.23 CDR 9932-G 63,62 0.37 16,86 4.15 0.03 2,27 4.79 4.74 0.90 0,07 2.32 100.22

CDR 9932-5 64.06 0.39 17.42 3.09 0.02 2.45 3.01 5.60 1.22 0.10 2.33 99.78 CDR 9932-I 62.24 0.39 17.01 3.68 0.03 2.15 4.86 5.34 0.73 0,09 2.88 99.47 CDR 9932-J 64.05 0.32 16.97 3.79 0.05 1.85 4.77 4.85 1.13 0.10 2.43 100.41 CDR 9933-A 66.65 0.47 15.80 1.78 0.03 0.46 4.90 2,07 1.40 0.11 6.08 99.84 CDR 9933-5 64.03 0.48 17,12 1.38 0,04 0,66 4.53 3.83 1.49 0.10 5.99 99.72

CDR 9933-C 68.02 0.44 15.66 1.88 0.03 0.61 3.90 3.93 1.32 0.09 4.38 100.33 CDR 9933-D 70.38 0.39 14.63 2.69 0.04 0.58 2.75 4.36 1.16 0.13 2.65 99.82 CDR 9933-E 67.07 0.53 15.93 2.05 0.06 0.67 3.64 3.89 1.56 0.13 4.46 100.07 CDR 9933-F 52.78 0.55 16.22 5.98 0.09 3.27 7.53 4.45 1.23 0.08 8.14 100,39 CDR 9933-0 40.49 0.44 8.37 9.44 0.12 15.69 8.46 0.21 0.05 0.04 17.00 100.53

CDR 9934-A 64.01 0.30 16.55 4.31 0.03 2.00 4.67 4.09 1.49 0.10 2,69 100.32 CDR 9934-8 62.18 0.37 16.87 5.27 0.05 2.16 5.34 4.44 0.84 0.13 2.53 100.27 CDR 9934-0 63.51 0.34 17.25 4.04 0.07 2.03 4.49 4.83 0.83 0.14 2.87 100.50 CDR 9936-A 62.15 0.37 16.84 5.53 0.06 2.39 4.58 4.21 1.35 0.13 2.54 100.27 CDR 9936-B 61.31 0.39 16.75 2.81 0.03 2.40 5.46 5.94 0.83 0.13 3.67 99.80

CDR 9936-C 62,06 0.37 17.41 5.24 0,05 2.32 4.70 4.42 1.36 0.13 2.30 100,47 CDR 9936-D 61.73 0.34 17.39 3.91 0.04 1.79 5.66 5.35 0.73 0.12 2.60 99.74 CDR 9936-E 63.19 0.41 16,70 4.15 0.05 2,73 5.24 4,64 0.80 0.09 2.06 100,14 CDR 9936-F 63,90 0.35 17.53 3.85 0.02 1.80 4.63 5.15 0.92 0,12 1.88 100,25 CDR 9936-G 63.28 0.33 17.06 4.02 0.03 1.71 5.13 4.87 0.84 0.13 2.33 99.83

CDR 9937-A 45,18 0.54 11.26 16.03 0.13 5.48 9.45 0.85 0.22 0.04 8.48 97,84 CDR 9937-B 42.35 0.60 11.66 10.97 0.15 10.28 9.16 1.14 1.47 0.04 11.09 99.01 CDR 9937-C 66.98 0.40 13.78 4.31 0.02 1.53 2.54 3,82 1.62 0,13 3.05 98,25 CDR 9937-D 43.28 0.57 10.86 12.02 0.14 8.50 9.13 1.23 2.34 0.05 9.52 97.74 CDR 9937-E 46.28 0.63 12.03 13.76 0.15 9.51 9.29 2.49 0.62 0.06 4.73 99.64

CDR 9937-F 41.65 0.62 11.22 12.90 0.15 9.33 9.18 1.04 2.14 0.05 10.27 98.66 CDR 9937-G 46.07 0.39 7.28 11.88 0.15 18.00 7.31 0.12 1.24 <0.03 6.93 99.61

Igo Intertek Testing Services Chimitec



DATE RECEIVED: 07-OCT-99 DATE PRINTED: 3-NOV-99 PAGE 18( 2/ 2)

SAMPLE NUMBER

ELEMENT Ba

UNITS PPM Cr

PPM Sr PPM

Zr PPM

Y PPM

CDR 9906-A 35 •1750 56 26 10

CDR 9906-8 18 899 166 38 15 CDR 9906-C 50 648 116 40 17 CDR 9906-D 11 1787 107 38 17

CDR 9932-G 296 159 499 95 10

CDR 9932-8 394 137 317 101 10 CDR 9932-I 212 152 415 97 11 CDR 9932-J 383 116 559 104 10 CDR 9933-A 451 105 312 163 11

CDR 9933-B 419 109 249 162 11

CDR 9933-C 437 89 270 164 11 CDR 9933-D 296 108 238 156 13 CDR 9933-E 380 161 228 176 14 CDR 9933-F 262 193 209 78 13 CDR 9933-0 <10 2067 160 26 11

CDR 9934-A 233 139 415 105 10 CDR 9934-B 187 137 641 104 10 CDR 9934-C 364 122 489 105 11 CDR 9936-A 505 129 528 105 10 CDR 9936-B 232 113 420 102 10

CDR 9936-C 591 93 519 105 10 CDR 9936-D 235 128 542 104 10 CDR 9936-E 236 165 493 95 10 CDR 9936-F 272 110 499 110 10 CDR 9936-0 220 131 550 107 11

CDR 9937-A 44 1472 170 30 13 CDR 9937-B 111 821 122 35 14 CDR 9937-C 354 119 166 156 18 CDR 9937-D 155 803 85 33 13 CDR 9937-E 45 874 115 37 15

CDR 9937-F 136 729 95 35 12 CDR 9937-0 53 2320 44 19 9






SAMPLE TYPES NUMBER SIZE FRACTIONS NUMBER SAMPLE PREPARATIONS NIMBER

DRILL CORE 6 -150 6 CRUSH/SPLIT & PULV. 6


LOWER DETECTION

991028 1 Si02 Silica (S102) 6 0.01 PCT 991028 2 Ti02 Titanium (Ti02) 6 0.01 PCT 991028 3 Aî203 Alumina (Aî203) 6 0.01 PCT 991028 4 Fe203* Total Iron (Fe203) 6 0.01 PCT 991028 5 Mn0 Manganese (Mn0) 6 0.01 PCT 991028 6 Mg0 Magnesium (Mg0) 6 0.01 PCT

991028 7 CaO Calcium (Ca0) 6 0.01 PCT 991028 8 Na20 Sodium (Na20) 6 0.01 PCT 991028 9 K20 Potassium (K20) 6 0.05 PCT 991028 10 P205 Phosphorous (P205) 6 0.03 PCT 991028 11 LOI Loss on Ignition 6 0.05 PCT 991028 12 Total Whole Rock Total 6 0.01 PCT

991028 13 Ba Barium 6 10 PPM 991028 14 Cr Chromium 6 10 PPM 991028 15 Sr Strontium 6 5 PPM 991028 16 Zr Zirconium 6 1 PPM 991028 17 Y Yttrium 6 1 PPM


**********,r,Mr ******** wee***** rnr******** r*,r,w****,r r****** r********** e+►**** This report must not be reproduced except in full. The data presented in this report is specific to those samples identified under "Sample Number" and is applicable only to the samples as received expressed on a dry basis unless otherwise indicated

~

EXTRACTION

BORATE FUSION BORATE FUSION BORATE FUSION BORATE FUSION BORATE FUSION BORATE FUSION

BORATE FUSION BORATE FUSION BORATE FUSION BORATE FUSION Ignition 1000 Deg.

BORATE FUSION BORATE FUSION BORATE FUSION Pressed Pellet Pressed Pellet

METHm

INDUC. COUP. PLASMA INDUC. COUP. PLASMA INDUC. COUP. PLASMA INDUC. COUP. PLASM INDUC. COUP. PLASMA INDUC. COUP. PLASMA

IMDUC. COUP. PLASMA IMDUC. COUP. PLASMA INDUC. COUP. PLASM IMDUC. COUP. PLASM GRAVIMETRIC

INDUC. COUP. PLASMA INDUC. COUP. PLASMA IMDUC. COUP. PLASM XRAY FLUORESCENCE XRAY FLUORESCENCE





IDEU Intertek Testing Services Chimitec Bondar Clegg



1 00.13:;208

SAMPLE ELEMENT S102 1102A(203 NUMBER UNITS PCT PCT:; PCT

feâ06* :: Nn0 MgO CaO wa?pi K20 P205 :: LOI Total ; Ba C1~; Sr Zr : Y PCT :: PPM PP11:. : PPM PPM :: PPM PCT < PCT PCT::: PCT P : PCT PCT ` PCT

0.04 0.05 0.09 0.03 0.08

0.03

2.56 4.04 3.30 6.56 4,94 6.95 2.00 4.49 5.04 7.42

2. 27;'4.87

4.g9':1 43 OAT;: 2.96 3.92!:1 14 0.13 4.57 3,79'::0 45 0.15 3.78 4 71:1 21 0.09" 2.23 _.._

4.28 0 15 0.22 3.69 ...........

5 0.80 0.10 2.68

182 629 115;: 10 240. 421 89:: 11 259 530 Wi:: 18 157 466 101:: 10 234 572 95:: 14

134 478 961: 10


CDR9932-F 63.38 0.37 16.48

rv>

100.15 386 100.00 235 99.77 134 99.93>281 _.. .....

99,19> 69

CDR9932-A CDR9932-B CDR9932-C CDR9932-D CDR9932-E

62.78 0:35;:16.69 58.65 0.52 15.48 54.95 0,64 15.98 64.73 0.35 16.52 54.61 0.49 16.54

IgHW Intertek Testing Services Chimitec Bondar Clegg Rapport Lab Geochimie




STANDARD ELEMENT Si02 Ti02'.AL203 F:e203* WO MgO CaO Na2O; K20 P205 LOI TotaL Ba Cr NAME UNITS PCT PCT:: PCT pCT PCT PCT: PCT PCT:; PCT PCT, PCT PGTPPM PPM

Granite - Cert.Ref.M

Number of Analyses

Mean Value

Standard Deviation

Accepted Value

CANMET SO-2 REF STD

Number of Analyses

Mean Value

Standard Deviation

Accepted Value 53.46 :..:: 15.24

59.82 0 11 83 ::6:43:;0.32 2.60 !:;8.30 4.15 1>4.20 0.53 -....... ... 1 1 1!< 1 1:: 1

_... ___._.. _._.... _.... _.... _. _...... . __. _._..-..

_.. ....... .... 59.82 0.15 11 83 ::6 43 0.32 2.60 8.30 4.15 4.20

6.42 0.32 2 67:8.26 4.15'':4 20 0.54 1.

<0.01 <,01 <0 01 .<0,01::.<.01 <,01<<.01 <.01 < 05 s303>::

1 1 1 1:;;:1!::: .1: __....

<0.01 <.01 <0 01 <0.01 <.01 4,01 <.01 < fî1;'0 03 0;:02 '<:

<0.01 <,01 <0.01

10.30

-:::37.60

37.60

37.30


GANNET STD SY-3

Number of Analyses

Mean Value

Standard Deviation

Accepted Value

ANALYTICAL BLANK

Number of Analyses

Mean Value

Standard Deviation

Accepted Value

CANMET STREAM-SED 2

Number of Analyses

Mean Value

Standard Deviation

Accepted Value

Loss On Ignition

Number of Analyses

Mean Value

Standard Deviation

Accepted Value

59.68 0.15;:11.80

0.04 2.56 4.04 4$4;1 43 4;17::; 2.96

2.98

0.03 2.00 4.49 4.71 1 21 0.09 __.. 2.23

0.03 401 4.50 4.77 1 22 0.08

62.78 0,35 16.69

64.73 0.35 16.52 64.89 035 16.60

100.15::386 182`:629 115': 10 :..

281 157 466 101:::: 10

281 165:466 97 9

EOM Intertek Testing Services Chimitec Bondar Clegg Rapport Lab Geochimie




SAMPLE

NUMBER

CDR9932-A

Duplicate

CDR9932-D

Duplicate

ELEMENT Si02 T102 A1203 Fe203*; Mn0 MgO CaO N820> K20 P206:: LOI Total` Ba C1`: Sr ZP Y

UNITS PCT PCT::: PCT ..PCT: PCT PCT: PCT PCT; PCT PCT; PCT MPCT4PM PPM PPM PPM PPM


APPENDIX 4

DIAMOND DRILL HOLE SECTIONS


REPORT ON THE FALL, 1999 DRILLING PROGRAM, CEDAR ...

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