GEOCHEMICAL, GEOPHYSICAL & PROSPECTING REPORT ON … · 2004. 5. 3. · GEOCHEMICAL, GEOPHYSICAL & PROSPECTING REPORT ON THE KECHIKA PROPERTY A - CLAIM BLOCK Al to A24 Claims Dease

GEOCHEMICAL, GEOPHYSICAL & PROSPECTING

REPORT ON THE KECHIKA PROPERTY

A - CLAIM BLOCK

Al to A24 Claims

Dease River Area, British Columbia Liard Mining Division

NTS 104P115E,16W 5950’ N latitude, 128’28’ W longitude

for

Tizard Explorations Inc. (owner & operator)

LIST OF ILLUSTRATIONS

Figure 1: Location Map 2 Figure 2: Claim Map 5 Figure 3: Tectonic Setting 7 Figure 4: Regional Geology 9 Figure 5: Property Geology. 14 Figures 6A - 6D: MagneticNLF-EM Geophysical Data pocket Figures 7A - 7D: MagneticNLF-EM Geophysical Profiles pocket Figures 8A - 6D: Soil Geochemical Survey Data and Profiles pocket Figure 9: Compilation Map pocket

TABLES Table 1: A Block Claims 3 Table 2: Soil Statistics Summary 17

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SUMMARY

In 1996 an aerial magnetic survey over the northern Kechika Trough was carried out on behalf of Tizard Explorations Inc. Encouraged by the results of the survey, the company staked 1,637 claim units in eight blocks. Block A contains 24 claims with 472 claim units and is located about 30 km southeast of Watson Lake. Access is via helicopter from Watson Lake. The claims lie within the Liard Plains and overburden up to 60 m in depth may occur, in consequence few outcrops can be found. Due to the difficult access and extensive overburden, very little exploration has been carried out in this area in the past.

Tizard Exploration’s work on the A-Block consisted of lake sediment sampling (46 samples), four grid systems comprising 45.9 km, 45.9 km of soil sampling with 914 samples, and 44 km of magnetometerA/LF-EM surveying, as well as minor prospecting.

The Kechika Trough is the southern extension of the Selwyn Basin and as such, is highly prospective for lead-zinc-silver sedex deposits. Numerous sedex deposits have been located in the Selwyn Basin in the Yukon and several deposits are known in the Trough. These deposits are generally found in Upper Devonian to Missisissippian Earn Group carbonaceous argillites, cherty argillite and slate, and in Upper Ordovician to Middle Devonian Road River Group black shales, limestone and chert.

Other types of mineralization have also been located in the area, ex. lead, zinc, copper in quartz veins (Kitza Showing) and tungsten-copper skarns (Boya Showing). The interpretation of the 1996 aerial magnetic survey also suggests that volcanic associated mineralization may be present.

Very little geology has been mapped on the A-Block due to the extent of the overburden. Tertiary basalt and Mississippian-Permian chert have been identified.

A lake sediment survey of the claims and the surrounding area was carried out with 46 samples collected. Ten to twelve samples gave values from threshold to highly anomalous, mostly in copper but also in arsenic and occasional lead, zinc, silver and bismuth. The Liard Tom Creek drainage in the northwest claim area contains several anomalous lake sediment samples including highly anomalous copper (650 ppm) in sample A-2. A single sample (A- 44) in the Trepanier Creek drainage was highly anomalous in copper, zinc, silver and nickel. Several scattered samples from the southeast area were also anomalous,

The soil survey shows some minor scattered anomalies on the AB grid. The geophysical survey indicated a number of small VLF-EM anomalies, including a coincident VLF conductor and irregular magnetic low anomaly on the AD grid.

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DISCUSSION I CONCLUSIONS

The preliminary exploration program on the A-Block claims gave some encouraging results

which warrant follow-up investigation, The Liard Tom Creek drainage in the northwest claim

area and the upper Trepanier Creek drainage near the AD grid in the southwestern part of

the claims contain several anomalies of interest.

The Liard Tom Creek contains four consecutive lake sediment samples (A-2 to A-5) with

multi-element anomalies over a length of 4.5 km. At the downstream end is the highly

anomalous A-2 sample with 850.8 ppm copper. Element concentrations do not necessarily

decrease downstream and the individual elements vary. Bismuth is elevated in three

samples, arsenic, copper and barium in two samples, and antimony and mercury in one

sample. This area is considered to be of primary interest and should be followed up with

stream silt and soil surveying to narrow down the target area.

In the Trepanier Creek area, lake sample A-44 in the upper tributary is anomalous in

copper, zinc, silver, nickel, bismuth and molybdenum. About 1 km to the southeast on the

AD grid, a broad irregular magnetic low from 1200-1900 E coincides with a zone of VLF-EM

conductors. The conductors appear to strike northwest in the direction of the A-44 lake

sample, and it is possible that these anomalies are related. Soil samples from the grid

returned a single sample at line 2N. 700E with highly anomalous molybdenum (78.4 ppm)

and elevated uranium (19 ppb), as well as some other scattered anomalous samples.

Follow-up work in this area should consist of extending the first 2,000 m of Grid AD with

parallel lines to the northwest to cover the lake area.

Several lake sediment anomalies also occur in central Trepanier Creek and in branches of

Black Angus Creek in the southeast corner of the claim block. This area should be further

investigated by more lake bottom sampling and soil surveying to narrow down a target area.

TABLE OF CONTENTS

SUMMARY

DISCUSSION I CONCLUSIONS

INTRODUCTION Location and Access Physiography and Climate Claim Status. Property History Summary of Work.

REGIONAL GEOLOGY

REGIONAL METALLOGENY

PROPERTY GEOLOGY

1997 EXPLORATION PROGRAM Grid System Ground Geophysical Survey. Soil Geochemical Survey Lake Bottom Sediment Survey. Prospecting / Rock Sampling

REFERENCES

COST STATEMENT

STATEMENT OF QUALIFICATIONS

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25

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27

APPENDICES Appendix A: Lake Sediment Geochemistry Element Maps Appendix B: Geochemistry Analysis ( by R.R. Walker) Appendix C: Rock Sample Descriptions Appendix D: Certificates of Analyses

INTRODUCTION

During the period of July 6 - August 8th. 1997, a program of soil and lake sediment

geochemistry, ground geophysics and minor prospecting was carried out on the Kechika

Property in north central British Columbia. The property comprises 9 claim blocks, of which the

A - claim block is discussed in this report. The work was conducted by Donegal Developments

Ltd. on behalf of Tizard Explorations Inc.

The focus of the exploration program was to investigate anomalies delineated from an earlier

reconnaissance airborne geophysical survey. The property is located within the Kechika

Trough, a region which is prospective for sediment hosted zinc-lead-silver deposits.

Location and Access

The Kechika A-Block is located near the British Columbia-Yukon border, approximately 30 km

southeast of the town of Watson Lake, Yukon [Figure I]. The centre of the property lies at

5950’ N. latitude, 128”28’ W. longitude on NTS mapsheets 104Pll5E & 104P/16W within the

Liard Mining Division.

Access to the claims is available by helicopter out of Watson Lake, which is about a 20 minute

trip. The Alaska Highway passes about 3 km north of the property boundary. No road access

is present, but a cat trail crosses just outside the north and eastern boundaries of the claims

which allows good foot access.

Physioaraphy and Climate

The claims are situated within the Liard Lowlands physiographic division (Liard Plains), a low

lying, drift-covered region with subdued topography adjacent to the Liard River. Elevations

range from about 2050 ft. (625 m) at the northern end to 2864 ft. (873 m) above sea level in the

central part of the claim block. The claims lie just south of the junction of the Dease and Liard

Rivers. The property is drained by four main creeks (Liard Tom, Trepanier, Kloye and Black

Angus) flowing northeasterly across the claims into the Liard River. Outcrops are scarce in this

claim block, with perhaps 1% bedrock exposure.

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“ANCO”“ER ISLAND !

j- YUKON 1 TERRITORY

/IKA RTIES

Fort Neko”

7 4

ALBERTA

” -.._ \\ ( ‘..\

*I TIZARD EXPLORATIONS INC.

125-

KECHIKA PROJECT

LOCATION MAP

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Irr The claims are predominantly covered by a blanket of morainal till on the order of 5-30 m thick

(Klassen, 1978). The material is classified as lodgement and ablation till, which is generally

sandy and stony. On the north end of the claims towards the river, glaciofluvial and

glaciolacustrine terraces composed of silt, sand, and some gravel are present. These terraces

are thought to be in the range of 20-60 m thick. Several drumlinoids in the area indicate glacial

movement was in a northeasterly direction as shown in Klassen’s surficial geology map.

Vegetation consists of mostly lodgepole pine and spruce, with a greater abundance of aspen

towards the river terraces and surrounding major drainages. Forest cover is roughly 30%.

The climate is typical of northern continental regions, with temperatures ranging from about

-25” C in January to 15” C in July. Much of the precipitation falls as snow, with annual snowfall

averaging 219 cm. Field work can be carried out from about May to October.

Claim Stat-

The A - Claim Block comprises 24 individual claims totaling 472 claim units, covering an area of

w about 11,800 hectares (29,158 acres). The owner on record of these claims is Tizard

Explorations Inc. The claims are listed in Table 1 below and illustrated in Figure 2.

Table 1: A-Claim List

Claim Tl?lllWe Record Units Expiry Claim Name Number Date Date Owner

Al 350020 A2 350021 A3 350022 A4 350023 A5 350024 A6 350025 A7 350026 A0 350027 A9 350026 A 10 350029 All 350030 A 12 350031 A 13 350032 A 14 350033 A 15 350034 A 16 350035

96 Aug 14 96 Aug 15 96 Aug 15 96 Aug 16

96 Aug 14 96 Aug 15 96 Aug 13 96 Aug 14 96 Aug 12 96 Aug 16 96 Aug 17 96 Aug 15 96 Aug 16 96 Aug 13 96 Aug 14 96 Aug 14

20 98 Aug 14 20 98 Aug 15 20 98 Aug 15 20 98 Aug 16 20 98 Aug 14 20 98 Aug 15 20 98 Aug 13 20 98 Aug 14 20 98 Aug 12 20 98 Aug 16 20 98 Aug 17 20 98 Aug 15 20 98 Aug 16 20 98 Aug 13 20 98 Aug 14 7.0 98 Aug 14

Tizard Explorations Inc. Tizard Explorations Inc. Tizard Explorations Inc. Tizard Explorations Inc. Tizard Explorations Inc. Tizard Explorations Inc. Tizard Explorations Inc. Tizard Explorations Inc. Tizard Explorations Inc. Tizard Explorations Inc. Tizard Explorations Inc. Tizard Explorations Inc. Tizard Explorations Inc. Tizard Explorations Inc. Tizard Explorations Inc. Tizard Explorations Inc.

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A 17 350036 96Aug13 20 98 Aug 13 Tizard Explorations Inc. A 18 350037 96Aug11 20 98 Aug 11 Tizard Explorations Inc. A 19 350038 96Augll 20 98 Aug 11 Tizard Explorations Inc. A 20 350039 96 Aug 11 16 98 Aug 11 Tizard Explorations Inc. A 21 350040 96 Aug 11 16 98 Aug 11 Tizard Explorations Inc. A 22 350041 96 Aug 13 20 98 Aug 13 Tizard Explorations Inc. A 23 350042 96Aug13 20 98 Aug 13 Tizard Explorations Inc. A 24 350043 96Augll 20 98 Aug 11 Tizard Explorations Inc.

Total: 472

Proper&Hi&iy

No previous work had been recorded on the ground covered by these claims prior to 1996. The

brief history of this property is as follows:

1996: An airborne magnetic survey, covering a 100 km by 20 km area is flown over the northern Kechika Trough area by Questor Surveys for Donegal Developments Ltd. Eight claim blocks, including the A-Block are staked for Tizard Explorations Inc. during the summer to cover the most favorable anomalies.

Summarv of Work

Work performed on the Kechika A-Block in 1997 included lake sediment sampling on all claims

totaling 48 samples. Grid establishment, soil sampling and ground geophysics was conducted

on the A5,6,8,9,12,13,17-19 claims consisting of 45.9 line km of flagged gridlines, 45.9 line km

of soil sampling (914 samples), and 44.0 line km of magnetometer/VLF-EM surveying. Minor

prospecting on the A 1,2,7,8,15.17,23 claims covering a cumulative area of about 100 hectares

was also completed.

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N

I

REGIONAL GEOLOGY

The area of interest lies within the Kechika Trough, a sedimentary basin developed off the

western shelf of Ancestral North America during early Paleozoic time [Figure 31. The trough is

bound to the west by the Northern Rocky Mountain Trench and is considered to be the southern

extension of the larger Selwyn Basin in the Yukon. Recent mapping of the Northern Kechika

Trough by the B.C. Geological Survey has identified strata of predominantly Proterozoic to

Mississippian age with lesser Permian to Quaternary units [Figure 41.

Stratigraphic units are summarized below from Ferri et. al. (1997):

&per Proterozoic Hvland Gro!,@

Grey to brown weathering sandstone and slate with distinctive sequences of fine to coarse, gritty feldspathic quartz-rich sandstones and conglomerates.

(Upoer Proterozoic and/or Lower Paleozoic ?) ‘Aeroplane I ake Panel”

Low grade metamorphic rocks in the Aeroplane Lake area, subdivided into 3 packages? a calcareous phyllite and schist, siliceous schist and quartz sandstone, and a limestone, phyllite, sandstone.

I, !&per Proterozoic and Cambrian

Undivided Hyland Group and Cambrian rocks

Cambrian Siliciclastics

Slate, siltstone, quartz sandstone to quartzite, conglomerate and minor limestone are grouped into an unnamed sequence of probable Cambrian age.

U. Camb. - I Ord. Kechika Grouo

Slate, calcareous slate, limestone, siltstone, and sandstone. This unit is extensive in the map area but poorly exposed and displays variations in thickness and lithology. In the Kechika River area, the unit is more siliceous and dolomitic.

U. Ord. - Mid. Devonian Road River Grout

Divided into 2 informal subunits (although not recognizable in this map area). A lower sequence known as the Duo Lake Formation is composed of black shale, siliceous shale, chert and minor limestone. The overlying “Silurian Siltstone” is distinguished by distinctive buff- orange weathering, bioturbated dolomitic siltstone. Road River exposures are dominated by‘ the Silurian Siltstone unit due to its relatively resistant nature.

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TIZARD EXPLORATIONS INC. DONEGAL DEVELOPMENT3 LTD.

KECH I KA PROPERTY

TECTONIC SETTING N.i.S. 94M,104P LIAR0 M.D..B.C

Ordovrc an - Miss. “Kitza Creek Facies” i

An informal unit in the Kitza Creek area consisting of calcareous dark grey to black, carbonaceous siltstone to silty argillite, shaly slate. May be older, younger than or equal to the Road River Group.

Upper Devonian to Mississipgian Farn Group

Thin to thickly bedded, carbonaceous blue-grey to dark grey or black argillite, cherty argillite, siltstone and slate. These rocks have a characteristic yellowish stain on weathered surfaces. Upper Devonian rocks of the Earn Group host many of the Cordillera’s most important sedex deposits.

.- mi ount Christie Formation r?)

Grey to buff-weathering, pale to dark grey chert. Locally pale salmon pink or green. Thinly to thickly bedded. Minor argillite. Locally found stratigraphically above Earn Group.

Tertiary - Quaternarv Tuva Formation

Fresh, massive to fragmental basalt. Dark grey-brown to dark green, plagioclase-olivine-phyric. Locally vesicular or glassy. Minor basaltic tuff, with angular basalt fragments.

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-,-“* - XMBRIAN -

m ‘c:,:-i-l__.:_- _: _____..___._ \

Structure

The regional structural style in the Kechika Trough is dominated by northwest trending folds

and thrusts. Folding is open to moderate and upright to northeast verging. The dominant

cleavage is generally parallel or subparallel to bedding. A major thrust is located on the east

side of Chee Mountain, where Cambrian quartzites and slates overlie Earn Group rocks. West

of Chee Mountain, the Hyland Group is separated from the Cambrian rocks by another

northeast-verging thrust fault. Another significant thrust carrying Proterozoic rock passes

through Aeroplane Lake in the Rocky Mountain Trench. The Northern Rocky Mountain Trench

on the western boundary of the trough is a broad, well defined valley along with right-lateral

fault displacement in the range of 450 - 700 km. Several steep, northeast trending dip-slip or

oblique slip faults are also present in the map area.

Intrusive Rocks

In the northern Kechika Trough map area, intrusive rocks consist of mainly gabbro and smaller

stocks or dikes, Several elongate gabbro bodies are found in Kechika Group rocks northeast of

Gemini Lakes of possible early Paleozoic age. At Boya Hill, 10 km southeast of Graveyard w Lake, skarn mineralization is related to quartz-biotite-feldspar porphyry and quartz porphyry

dikes, sills and small stocks of early Cretaceous age. Several feldspar and quartz-feldspar

porphyry dikes also occur within the Aeroplane Lake panel. At Mount Monckton. strongly

hornfelsed rocks indicate the proximity of a large intrusive body.

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REGIONAL METALLOGENY

The most economically important mineral deposits in the Kechika Trough, and the primary

exploration target of this program are zinc-lead-silver sedimentary exhalative (sedex) deposits.

These deposits are characterized by thin laminations to massive beds of pyrite, pyrrhotite,

sphalerite and galena within host rocks of shale, chert. and carbonates. Barite is also a major

component of many sedex deposits.

Some of the world’s largest sedex deposits are found within the Selwyn and Purcell basins of

the Canadian Cordillera, including Howard’s Pass in the Yukon (125 million tonnes of 5.4% Zn

and 2.1% Pb) and the Sullivan deposit in southeastern B.C. (155 million tonnes of 5.7% Zn.

6.6% Pb, 68 g/t Ag). The Selwyn Basin is host to over 20 sedex deposits, and has been

estimated to contain a total tonnage potential of 900 million tonnes (Carne 8 Cathro, 1981).

The Kechika Trough, which is the southern extension of the Selwyn Basin, hosts 12

documented sedex occurrences. Among these are the Cirque (32.2 million tonnes of 10.0%

combined Zn-Pb, 48g/T Ag) Driftpile, and Akie deposits. These deposits are found in Road

River Group and Lower Earn Group strata.

A secondary exploration target is poly-metallic volcanogenic massive sulphide deposits (VMS).

These are syngenetic stratiform deposits of copper, zinc, lead, silver and gold occurring in

marine volcanic rocks or associated marine sedimentary rocks. VMS deposits share similarities

to sedex deposits as they are both formed by discharge of hydrothermal fluids onto the

seafloor. The VMS deposits often contain 5 to 20 million tonnes and can attain high grades (ex.

Wolverine, $2701tonne).

Mineral Occurrences in the Northern Kechika Trough Area

K&a Showing On Kitza Creek, about 3 km east of Kitza Lake, low grade sulphide vein

mineralization occurs in “Kitza Creek facies” siltstone-limestone. Several dozen veins contain

one or more of tetrahedrite, sphalerite, barite. and rare galena. An aerial electromagnetic

survey consisting of over 600 line km was flown over the Kitza area in 1981. The 3 main

anomalous areas were thought to be graphitic shears, but ground soil surveying and geological

mapping located a large number of scattered low-grade showings. Small and patchy soil

anomalies are associated with these mineral showings. w

Red Showing: This showing occurs on the banks of the Red River, 5 km upstream from the

junction with the Kechika River. Low grade vein mineralization occurs at 3 localities within a

kilometre. A quartz breccia zone and quartz veins carry sphalerlte, galena. pyrite, smithsonite

and minor chalcopyrlte.

m: The Roman zinc-lead-silver showing is hosted in Earn Group rocks just south of the

Yukon-B.C. border. Several concordant to discordant sphalerite and galena bands up to 20 cm

thick are hosted by graphitic slate and silty limestone. These bands can be traced for 10

metres before they disappear under the Liard River. A silicified zone at the contact contains

quartz veins with patches of sulphide mineralization. The mineralization has been suggested to

be part of a sedex feeder system or related to regional folding. Assays from the mineralized

lenses have returned values of 22.6% Zn, 46.3% Pb and 23 g/tonne Ag. The property has

been extensively explored by geological mapping, geophysical surveys and some diamond

drilling. The presence of bedded barite, pyrite and stratabound lenses of sphalerite and galena

suggest that the right conditions have existed to form sedex deposits in the northern Kechika

Trough.

u The Boya porphyry/skarn prospect is located on Boya Hill, 10 km southwest of

Graveyard Lake. Low grade tungsten and chalcopyrite and molybdenum occurs at the Main

Face and West Hill showing areas. At the Main Face, quartz-biotite-feldspar porphyries intrude

Proterozoic host rocks forming a talc-silicate rock locally mineralized with pyrrhotite,

chalcopyrite and scheelite. The most significant mineralization occurs in quartz stockworks and

fracture-filling veins in the intrusion and altered metasediments which contain molybdenite and

minor scheelite. At the West Hill showing, 3.5 km to the northeast, skarn mineralization

consists of massive pyrrhotite with minor chalcopyrite, arsenopyrite, sphalerite, galena.

bismuthinite and variable molybdenite.

Kechika River Bade: This barite-pyrite stratiform deposit occurs along a creek valley g km

NW of Gemini Lakes and 1 km upstream from the creeks junction with the Kechika River. The

barite is at least 4 m thick with local finely disseminated pyrite and is overlain by a sequence of

slate with pyrite concretions, barite nodules, and finely laminated pyrite. The occurrence is

hosted in Earn Group rocks.

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PROPERTY GEOLOGY

W

A small part of the A-Claim Block has been mapped as Tertiary to Quatemary Tuya Formation

[Figure 51. This unit consists of massive to fragmental, fresh-looking basalt occurring on

several hill tops between Black Angus and Kloye creeks (Fern et. at.. 1997). These rocks are

described as grey weathering, dark grey-brown to dark green, aphanitic or plagioclase-olivine

phyric basalt. The fragments can be vesicular, angular to sub-rounded and up to 30 cm in size.

Alteration appears as yellow to tan colour in the tuffaceous matrix. It is not clear whether these

volcanics are sub-aerial or sub-marine.

Observations of our field crew this year have confirmed the presence of this basalt in several

other outcrops over the claims, as well as minor chert. Outcrops of chert at Trepanier Creek,

on the eastern edge of the claims and on the southeastern boundary of the property may be

part of the Mississippian - Permian Mount Christie Formation. Government mapping has

identified sporadically exposed pale coloured cherts in the northern Kechika Trough which are

similar to descriptions of cherts encountered during this season’s prospecting.

w

w

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A CLAIM BLOCK

I 1 N.T.S. 94M,104P LlARDM.D.,B.C

I N.T.S. 94M,104P LIARD M.D.,B.C

1997 EXPLORATION PROGRAM

GRID SYSTEM

Four separate grids totaling 45.9 line km were established on the A Block [Figure 91 across

anomalous aerial magnetic responses as advised by Mr. Ron Sheldrake, geophysicist with

Questor Surveys. The grids were put in using compass and hip chain. Lines were spaced 200

m apart and stations marked at 50 m intervals along the lines with red flagging. Most of the

lines extended northeasterly crossing the predominant bedding direction and the corresponding

direction of the magnetic response. A few lines extend easterly to cross north striking magnetic

responses. Minor adjustments to the position of the lines was subsequently made by the

writers to avoid lakes, rivers or other serious obstacles.

GROUND GEOPHYSICAL SURVEY

w Introduction

Very low frequency electromagnetic (VLF-EM) and magnetic geophysical surveys were carried

over areas of the claim blocks selected on the basis of an aeromagnetic survey. The surveys

were done simultaneously with two EDA OMNI PLUS instruments equipped for both VLF-EM

and magnetic surveys. Diurnal variations in the geomagnetic field were recorded and removed

from the magnetic results using a third EDA OMNI PLUS magnetometer operated in the base

station mode. Two VLF-EM stations were utilized, namely, Seattle (Jim Creek), WA. (NLK)

transmitting at 24.8 kHz and Hawaii (NPM) transmitting at 21.4 kHz. The Seattle station,

located to the southeast of the project area, was the primary station providing ideal coupling

with the anticipated northwest/southeast geological trends. Although not so favourably located,

the Hawaii transmitter, acted as both a backup station, when the Seattle transmitter was off the

air for repairs and/or scheduled maintenance, and an alternate station for more easterly

trending features. Readings were taken at 25 m intervals.

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Results and Discussion

The data has been plotted and interpreted by J.L. LeBel, Geophysicist. The results of the

survey are posted and profiled separately on the accompanying maps [Figures 6A-D, 7A-D] at a

scale of 15,000. For the VLF-EM survey, the in-phase and the quadrature components of the

vertical magnetic field are in per cent (%) of the horizontal primary field (i.e. the tangent and

ellipticity) are presented. The magnetic results show the total magnetic field in nano Teslas

(nT). For VLF-EM survey the horizontal field strength is also profiled although the data is not

posted due to space limitations.

As most of the grids consist of 3 lines or less, the three individual sets of results are stacked on

one plan map. For the grids with more than 4 lines the results are presented on individual

maps.

Valid VLF-EM anomalies, as marked on the maps, are indicated by positive to negative sense

inflections or cross-overs in the in-phase component considered from west to east for east/west

lines and south to north for north/south lines. Quadrature phase anomalies may have any

sense. Field strength over anomalies always increases thereby provides a secondary

confirmation that an anomaly is valid. Anomaly locations are not routinely provided for the

Hawaii station because the results tend to be redundant.

Grid AA

The magnetic survey on grid AA outlined two areas of irregular highs and lows with peak to

trough amplitudes up to 500 nT where no particular feature stands out. A variable magnetic

signature like this is typical of volcanic rocks. Several VLF-EM anomalies were recorded in two

groups which coincide with the bands of magnetic anomalies. Several of the VLF-EM

anomalies have quadrature-phase anomalies which have the opposite sense as the in-phase

anomalies which indicates a good conductor. Selected examples occur at line IN, 525E, where

the asymmetry of the anomaly suggests the conductor has a shallow dip to the west and LIN,

2300E where the anomaly is close to an isolated? 500 nT magnetic low.

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The magnetic survey on grid AB outlined three magnetic lows up to 700 nT, a wide one at the

east ends of the lines, a moderately wide one in the middle of the lines and a narrow one at the

west ends of the lines. The wide lows reflect wide shallow bodies with uniform negative

magnetic susceptibility contrast compared to the surroundings. Felsic intrusions are possible

causes. The narrow magnetic low is caused by a shallow, thin body which strikes north/south

based on the alignment of the (negative) peaks. The VLF-EM survey outlined a few poor

anomalies. Features located between 1400E and 1500E on line 3N may be related to a

magnetic low. However, on line 2N an adjacent VLF-EM anomaly is displaced from the

magnetic low.

The magnetic survey on grid AC outlined a broad 500 nT high at the west ends of the lines and

a compound, two (negative) peak 200 to 500 nT low at the east ends of the lines. Depths to the

sources are qualitatively estimated at 100 m. A few VLF-EM anomalies are present.

Anomalies at about 550E on lines 2N and 3N outline a conductor along the flank of the

magnetic high.

Grid AD

The magnetic survey on grid AD outlined two, 1 km wide lows. The lows differ in character, in

that, the feature to the west of the centre of the lines is composed of a number of irregular lows

while the other low at the east ends of the lines has two main components. The 1500 nT

negative spike at L2N, 1550E is a bad reading. The VLF-EM survey outlined two belts of

multiple anomalies, one of which correlates with the first magnetic low discussed above. Areas

exhibiting conductors and variable magnetic signature are often favourable exploration targets.

The other, series on anomalies in the vicinity of 2400E to 2800E occurs in an area of bland

magnetic response.

SOIL GEOCHEMICAL SURVEY

A soil survey was conducted over each of the 4 grids, with a total of 910 samples collected.

The soil horizon generally consisted of a IO-30 cm deep A-horizon and a mostly well developed

B-horizon at about 5-15 cm depth. On north facing slopes, the soil horizons were less well

developed. Samples were collected from the B-horizon in kraft paper bags and partially dried

before shipping to Acme Analytical Labs in Vancouver. A 32-element ultratrace ICP and

geochemical gold analysis was conducted on the samples. Refer to Figures 8A - 8D for

element plots and profiles and Appendix D for complete analytical results.

Table 2: Soil Statistics Summaty

ELEMENT MIN MAX MEAN MEDIAN THRESHOLD*

MO @pm) 0.1 78.4 1.1 0.9 7.0 Cu (pm 1 47.4 0.8 a.0 17.1 Pb Wm) 0.7 14.1 7.2 7.4 11.7 Zn (wm) 1 208.1 46.8 45.0 86.9 Ag NW <30 700 62 52 175 Ni kwn) 1 57 20 21 35 Mn (Pm'0 17 55809 425 212 4521 Fe (%) 0.07 5.55 1.93 2.04 3.26 As @pm) < 0.5 12.0 2.5 2.2 5.4 U mm) <5 86 3 3 13 Cd (w-4 0.02 2.91 0.26 0.19 0.76 Sb kvm) < 0.2 6 0.3 0.3 1.1 Bi @Pm) < 0.1 7 0.6 0.1 3.4 Ca (%) 0.11 12.41 1.02 0.28 4.56 P (%) 0.010 0.443 0.057 0.049 0.123 Ba km) 68 4246 309 215 884 Hg kvb) < 10 107 20 15 54 Se (fwm) < 0.3 6.6 0.3 0.2 1.4 Au (fwb) Cl 77 2 1 10 Note: Sa not total * = mean + Z(std dev)

Results

AA Grid:

This grid is located on the north end of the claim block with three lines extending east-west for

4300 m [Figure 91. Analytical results from 255 soil samples show mostly values within

background range. A few erratic high manganese values were obtained. The grid is about 4-5

bf

-19.

km south of the Dease and Liard Rivers and the overburden may be deep enough to mask any

geochemical anomalies.

A0 Grid;

This grid extends northeasterly from the south boundary of the A23 claim the south end of the

A19 claim. The grid covers about 2.0 km of part of the upper drainage basin of Liard Tom

Creek and some tributaries of this creek from the east. Three small anomalies are noted.

Anomaly AB 500 (around 500E) consists of two anomalous molybdenum values and three very

high manganese values. Anomaly AB 1500 (around 1500 E) consists of minor anomalous

manganese and weakly anomalous bismuth and molybdenum. Anomaly AB 3600 (around

3600 E) contains a few very high manganese values and minor anomalous zinc and

molybdenum, as well as one high gold value (19 ppb).

AC Grid:

The three lines of this grid extend northeasterly for 3,000 m from the central part of claim A5 to

the bottom central part of claim A8, and north of the central part of Trepanier Creek. The lines

cross a magnetic high response, the rim of a large ellipsoid high and a magnetic low lense

outside the ellipsoid. No anomalous soil values were obtained from the 161 samples collected.

AD Grid;

This grid consists of three 4,000 m long lines extending northeasterly (N50”E) from the south

central border of claim Al3 to the southeast corner of A14. It more or less follows the divide

between the two main branches of Trepanier Creek. A few isolated weak anomalous values

were obtained from the 235 samples collected. Sample AD2N,700E returned a highly

anomalous molybdenum value of 78.4 ppm (A block average = 1 .l ppm MO) and anomalous

uranium of 19 ppm, while values for zinc (3.6 ppm), manganese (17 ppm) and iron (0.16%)

were extremely low.

A lake (A-44) lies about I km northwest of the grid. This sediment sample gave anomalous

values in copper (203.7 ppm). zinc (165.2 ppm). silver (354 ppb) and nickel (42 ppm). The grid

samples gave no indications of mineralization which might be the source of the anomalous lake

sediment. The main drainage into the lake appears to come from the northwest.

-2o-

LAKE BOTTOM SEDIMENT SURVEY

A total of 162 lake sediment samples were collected from lakes and ponds on the Kechika

Property, of which 48 are from the A claim block [Figure 91. Samples were collected using a

dart collector from a Bell 2068 (jet ranger) helicopter on pontoons. The samples were placed in

a cloth bag and hung to dry in camp before being shipped to Acme Analytical Labs in

Vancouver. A 32-element ultratrace ICP and geochemical gold analysis was performed on all

the samples. See Appendix D for complete analytical results.

Analysis of the lake sediment data by Richard R. Walker has concluded that samples high in

calcium are consistently low in metals as the presence of marl acts as a dilutant in the samples

(refer to Appendix B for discussion). The sediments probably range from organic-rich and

calcite-free to essentially pure marl (eg. sample D-15, 40% Ca). Anomalous metal values may

not be recognized due to high Ca contents, so metals of interest have been recalculated on a

calcite-free basis according to the formula: calcite free metal = (ppm metal)(lOO) I [lo0 - (2.5)(%Ca)

w Plots of individual elements are found in Appendix A, with the recalculated values in brackets

beside the actual obtained values for comparison,

Liard Tom Drainaae. . On claim A21 at the north end of the claim block, sample A-2 returned

highly anomalous values of 850 ppm copper and 22.7 ppm bismuth, as well as elevated silver

(272 ppb) and gold (5 ppb). Sample A-l at the northwest corner of the claims gave a value of

4.5 ppm copper, but contains 38% calcium. When recalculated with out the calcite, the copper

content increases from 4.5 to 107 ppm Cu. Another sample (A-3) from a small lake in the Liard

Tom drainage, about 2.5 km south-southwest of sample A-2, gave values of 100.2 ppm copper,

2.3 ppm bismuth and 570 ppm barium. Small lakes 1-2 km further southwest (A-4 to A-7)

returned anomalous values in arsenic, barium, and mercury.

The Liard Tom Creek drainage system flows north and north-northeast, covering the far

northwest corner of the claim block. It follows a segment of the elliptical aeromagnetic high.

The catchment basin extends south for about 8 km from the A-2 lake sample, with a maximum

width of 2.5 km and minimum width of less than 1 .O km, for a total area of roughly 14 km*. Grid

w AA lies a short distance northeast of Liard Tom Creek and did not return any anomalous values.

-21-

Grid AB intersects 1.0 km of the drainage with no significant values. A tive km stretch of the

Liard Tom drainage thus gives anomalous lake sediments, with the highest being furthest down

stream. The area is considered to be a very high priority exploration target.

Klove Creek Drain= Kloye Creek cuts diagonally across the central part of the claim block.

Twelve lake sediment samples were taken along this drainage, with no significant values from

samples on the east and west sides. Five lakes on the west half of the claims were slightly

anomalous in selenium (6.6 to 12.6 ppm). The creek cuts across the whole elliptical magnetic

high. No grid soil sampling was done in this drainage basin.

Trewanier Creek Drainaae: Trepanier Creek flows northeasterly across the claim ground, with a

north branch joining the main creek on the A6 claim. Lake sample A-44 in the north branch

near its headwaters was highly anomalous in copper (203.7 ppm), zinc (165.2 ppm), silver (364

ppb), nickel (42 ppm), bismuth (3.3 ppm) and slightly anomalous in molybdenum (6.1 ppm). No

other samples were taken in the drainage for 5.5 km downstream where two samples returned

low values (except for one 0.6 ppm Bi). The south branch did not give anomalous values in

four samples at the southwest corner. Three samples from the Al2 and A3 claims contained

anomalous values as follows: A-26 with 15.9 ppm Pb and 150 ppb Hg; A-30 with 83.1 ppm Cu;

and A-31 with 1267 ppm Mn. The next 7.5 km of the creek downstream on the claims had no

further lake/pond suitable for sediment sampling.

The highly anomalous lake sediment (A-44) in the north creek branch may have its source to

the northwest while anomalous values in the south branch may be derived from a southeasterly

source, where other anomalous values are found in the Black Angus Creek drainage.

Black Angus Creek Drainaae: Black Angus Creek drains the southeast corner of the claims.

The creek branches out and drains the Al, A2, A3 and A4 claims. A swamp and numerous

ponds occupy the extensive southwest corner. Six lake sediments were collected in the area.

Sample A-36 on the A4 claim on a northern branch was not anomalous. Sample A-45 on the

Al claim was taken at the headwaters of a branch flowing east across the Al and A2 claims

into Black Angus Creek. This was the only sample taken on this 3.5 km long branch and gave

anomalous (>95th percentile) values of 199.5 ppm copper, 4.9 ppm bismuth, 0.204%

phosphorus, and 3 ppb gold and weakly anomalous (>90th percentile) values of 285 ppb silver,

5.6 ppm molybdenum and 116 ppb mercury. On the A2 claim, a central creek branch 2.5 km

-22-

long, gave anomalous lake sediment values of 120.6 ppm copper, 3.2 ppm bismuth and weakly

anomalous molybdenum of 5.7 ppm.

Sample A-40 just south of the A2 claim, returned anomalous values in zinc, silver, manganese,

cadmium and mercury, and weakly anomalous values in nickel. Sample A-38 is anomalous in

arsenic (12.9 ppm). A-39 is anomalous in copper (49.4 ppm), zinc (219.3 ppm), silver (330

ppb), nickel (50 ppm), antimony (1.3 ppm), bismuth (0.5 ppm), selenium (9.3 ppm) and elevated

in gold (4 ppb). These four anomalous samples may have a common source near the

boundary between the Al and A2 claims.

PROSPECTING I ROCK SAMPLING

Minor prospecting was conducted on the claims covering roughly 100 hectares, The scarce

outcrops on this claim block are mainly limited to drainages. The predominant rock type

w encountered was basalt and minor chert. A total of 22 rock samples were collected for

analysis. See Figure 9 for sample locations and Appendix C for sample descriptions.

Outcrops along Trepanier Creek at the east end of the AC grid consist of bedded chert, ranging

from green to grey to dark grey and black in colour. Thin bedding is oriented at 095”/60” N in

the middle of the outcrop, and more flat dipping to the west and east. The outcrop is strongly

and closely fractured through brittle shearing. Numerous light grey to white clay seams along

bedding planes appear to be clay altered gouge seams.

On the Al claim, a large outcrop of basalt occurs consisting of massive and vesicular basalt.

Many tube vesicles have a preferred orientation with a trend of 355” and a plunge of 35” N, and

also weak banding or layering at 305”/35” N. A basalt breccia outcrop is also present with an

exposed height of about 200 ft. and contains very angular clasts (2-l 0 cm) with 15-35% matrix

of coarse sand to granule size. The breccia is recognizable from the air and is probably a

blocky aa flow lacking apparent internal bedding. No carbonate, sulphide or rust was noted in

these oucrops.

W

-23-

An orange rusty weathering chert was found just south of the southern boundary of the A2

1clr claim. The chert is thin-bedded (2-10 cm) at 340”/75” W. Outcrops are intermittent along a

northwest trending steep slope over an area of 200 m by 70 m. A small outcrop of light grey,

medium-grained quartz sandstone is also present and a unit of very fine, compact limestone

with about 30% recrystallized sparry calcite is exposed over 300 ft.

On the Al5 claim, just north of lake sample A-18, an outcrop of massive basalt was examined.

Some specks of specular hematite were noted. The basalt is not vesicular and has no

noticeable pull on a magnet.

Mineralization consisting of fine pyrite was noted in several samples from Trepanier Creek.

Some samples of interest include a fractured and in part brecciated and limonite-cemented

chert sample (AREL3) with 163 ppm copper and 163 ppm zinc. Samples ARSY-3 & 4 also

returned anomalous zinc values of 165 ppm and 182 ppm Zn respectively.

Panning was attempted at several locations including Trepanier Creek near the AC grid, where

one gold flake was recovered from moss. A pan of bank gravel from bedrock surface did not

w produce any gold. At the confluence of Trepanier Creek with the Liard River, a 0.5 mm flake of

gold was recovered from gravel. No gold was recovered at the mouth of the second tributary

into Dease River above its confluence with the Liard.

R. Chow, B.Sc,

-24-

REFERENCES

CARNE. R.C, and CATHRO, R.J. (1982): Sedimentary Exhalative (Sedex) Zinc-Lead-Silver Deposits, Northern Canadian Cordillera; in CIM Bulletin, Volume 75, No.840, pp.66-78.

COOK, S.J., JACKAMAN. W., FRISKE, P.W., DAY, S.J., CONEYS, A.M., and FERRI, F. (1997): Regional Lake Sediment Geochemistry of the Northern Kechika Trough, British Columbia (94M12.3,4.5.6. 12; 104P/8,9,10.15,16); B.C. Ministry of Employment and lnvesfmenr, Open File 1997-15.

CORDILLERAN ROUNDUP PROGRAM ABSTRACTS (1996): Geological Survey of Canada and B.C. Geological Survey, Vancouver, British Columbia; Jan 30 - Feb 2, 1997.

a) The Northern Kechika Trough: Insights and Indications of Sedex Potential; F. Fern, C. Rees and J. Nelson, B.C. Geological Survey.

b) Age Constraints on Ba-Zn-Pb Sedex Deposits, Gataga District, Northeastern B.C.; S. Paradis. J. Nelson and S. Irwin. Gelogical Survey of Canada and B.C. Geological Survey.

c) Devono-Mississippian Tectonics and Mineral Deposits of the Cordilleran Margin; S. Gordey, Geological Survey of Canada.

d) Wolverine Deposit, Yukon T. Tucker, Westmin Resources Ltd.

e) The Yukon-Tanana Terrane: The Devono-Mississippian Story; S.T. Johnston, CanadaiYukon Geoscience Office.

FERRI, F., REES. C., NELSON, J. AND LEGUN, A. (1997): Geology of the Northern Kechika Trough (NTS 94U14,i5; 94M/3,4,5,6,12,13; 164P/8,9,15,16); in Geological Fieldwork 1996; B.C. Ministry of Employment and Investment, Paper 1997-1, pp.125144.

FERRI, F.. REES. C.. NELSON, J. and LEGUN, A. (1997): Preliminary Geology of the Northern Kechika Trough, British Columbia; B.C. Ministry of Employment and Investment, Open File 1997-14.

GABRIELSE. H. (1962): Geology: Rabbit River, British Columbia (94M); Geological Survey of Canada; Map 46-1962.

GABRIELSE, H. (1963): McDame Map-Area (104P), Cassiar District, British Columbia; Geological Survey of Canada, Memoir 319 and accompanying Map 11 IOA.

MACINTYRE, D.G. (1991): Sedex-Sedimentary Exhalative Deposits; in Ore Deposits, Tectonics and Metallogeny in the Canadian Cordillera; B.C. Ministry of Energy, Mines and Petroleum Resources, Paper 19914; pp.25-70.

MINFILE REPORTS: 094M 020 (Red), 094M 016 (Boya West Hill), 094M 021 (Boya Main Face); Ministry of Energy, Mines and Petroleum Resources.

RAINSFORD, D.R.B. (1984): Geophysical Report on Val, Roman 50, Rom 1, Rom 2 and Vent 19 Claims; 6. C. Ministry of Energy, Mines and Petroleum Resources, Assessment Report No. 12731.

SHELDRAKE, R. and PEZZOT, T. (1996): Questor Surveys Limited, High Resolution Aeromagnetic Survey in the Dease River Area, British Columbia, Interpretation and Technical Report for Donegal Developments Ltd.

-25-

STATEMENT OF COSTS

Seamus Young, Supervision, Lake Sed. Sampling July 13-19; 7.5 days @ $330/day

Jim Donaldson, Supervision July 10-14; 5.5 days @$275/day

Richard Walker, Geologist July 25-27; 3.8 days @$440/day

Egil Livgard. Geologist July 18,20-21; 3.3 days @$385/day

Paul MacDonald, Soil Sampler July 12-20; 9.3 days @ $220/day

Timothy Young, Soil Sampler July 12-20; 9.6 days @ $192/day

Graeme Zucko, Soil Sampler July 11-20: 10.6 days @$llO/day

Sam Skiber, Soil Sampler July 12-20; 9 days @ $1 IO/day

Andrew Robinson, MaglEM Surveying July 25-27; 22.95 km @$38.5/km

Shawn Ryan, MaglEM Surveying July 25-27; 22.95 km @$38.5/km

2,475

1,513

1,672

1,271

2,046

1,843

1,166

990

884

884

Food 8 Accommodation

Meals - 67 mandays @ $30/day

Motel - 6.5 nights @ $159/night (double) x 5 rooms

2,010

5,188

Tranwortatipn

Airfare - 4 round trips, Vancouver to Watson Lake (apportioned cost)

Vehicle rental - 2 4x4 trucks, 32 days @ $4Olday (apportioned cost)

Gas (apportioned cost)

Helicopter - 14.4 hours @ $EOO/hr.

1,233

657

257

11,520

Analvses and Shiopinq

914 soil samples @$16.75/sample (ultratrace ICP + geochem gold) 15,310

50 lake sediment samples @ $17,47/sample 874

Eaubment/Su~

MaglEM rental - 3 days @ $6001day (2 instruments + base station recorder)

Supplies/field gear (apportioned cost)

ReDorI PreDarationlDraftinq

Total:

1,800

3,859

2&9!

$59,432

-26-

CERTIFICATE

I. EGIL LIVGARD, of 1990 King Albert Avenue, Coquitlam, B.C., do hereby certify:

Dated at Vancouver. British

1.

2.

3.

4.

5.

6.

I am a Consulting Geological Engineer, practising from #436 - 470 Granville Street, Vancouver, B.C.

I am a graduate of the University of British Columbia, with a B.Sc., 1960 in Geological Sciences and have regularly updated and expanded my geological knowledge through nwerous short courses given by MDRU, GAC, the Chamber of Mines, and B.C.G.S.

I am a registered member in good stanclmg of the Association of Professional Engineers of the Province of British Columbia, Registration No. 7236.

I have practised my profession for over 30 years.

This report is based on the writer’s property examinations during the period of July 17th - 22nd, 1997 and on references as listed.

I co&m that I have not, directly or indirectly, received or expect to receive any interest, direct or indirect, in the properties of Tizard Explorations Inc. or any affiliate, or beneficially own, directly or indirectly, any securities of Tizard Explorations Inc. or any affiliate.

Col~biathi~~;- ( ~ ,

Egil Livgard, BSc ng.

-27-

STATEMENT OF QUALIFICATIONS

I, Rita Chow of 5615 Dumfries Street, Vancouver, British Colombia, do hereby declare that:

1. I graduated from the University of British Columbia with a BSc. Degree (first class standing) in Geological Sciences in June, 1995.

2.

3.

I have been employed with Donegal Developments Ltd. since June of 1995.

This report is based on work done on the property during the period of July 6th to Aug. Sth, 1997 and on references as listed.

4. I have no interest, direct or indirect, in the Kechika Property or in the securities of Tizard Explorations Inc. nor do I expect to receive any.

Rita Chow, BSc. November 7, 1997

-2a-

STATEMENT OF OUALIFICATIONS

I, J. L. LeBel, of 2684 Violet Street, North Vancouver, British Cohmbia hereby cerQ:

1. I am a graduate of the Queens Univemity and the Univemity of Manitoba and I hold a BSc. degree in geological engineering and a MSc. degree in geophysics.

2. I am a Professional Engineer rcgjstered with the AwGation of Professional Engiom and Geoscientists of British Cohn&k

J.L. LeBel, P.Eng.

DATED at Vancouver, British Columbia, this 10th day of October, 1997.

APPENDIX A

Lake Sediment GeochemistryFement Maps

APPENDIX 6

Geochemistry Analysis by R.R. Walker

TO: S. Young 6r. E. Livegard fax: (604) 689-0288 Doncgat Dcvclopments Ltd. Ph.: (604) 689-0299

From: RR Walker Date: Sept., 19!+7 Subject: KechikaProject Geochemistry

A) Lake & Pond Samples

fax@h: (250) 287-3891

L e. , . J :i .7 1

The lake sediment samples are variable with respect to acid soluble wt % Ca and data inspection suggests a bJmod.sJ calcium distribution with samples tending to group into those with less than a few % Ca and those with more than several % Ca. This together with the observation that some samples were white indicates that many samples contain substantial calcite (marl) which has precipitated in some lakes and ponds but not others. As the sampling program targets metals trapped in organic oarbon compounds we view the presence of significant marl as a dihrtsnt in the samples. This appears supported by inspection of results from which we conclude that samples h!& in Ca are consistently low in metals. In contrast Sr shows a strong positive correlation with Ca reflecting the expected trapping of Sr in calcite.

We expect that the samples could be divided into two groups, those which are essentially calcite free but which may release a smalJ amount of Ca (up to .- 3%?) from silicates such as clays or from organ& during digestion in HCI - HNO3 and those with calcite present in variable amounts. This implies that some lakes have aJkaJine pJ?I capable of precipitating calcite while others are more acid, leading to sediment dominated by organics. The government tie sediment survey measured pH of surface waters and documented a pH range from 5.2 to 8.6 although most were alkaline. This variabihfy of pH wiJJ substantiahy effect the mobility of metals such as tic and copper in the hydromorphic envirotnmzrd. High Ph ponds indicated by high Ca sediments can act as baniera to transport of metals if pH is high enough to inorganically precipitate the metal. Copper wih precipitate from water at a lower pH than Zn so that some ponds could precipitate copper but let zinc pass downstream in solution. Copper normaby begins to precipitate as insoluble basic salts at a pH between 5.0 and 5.5 whereas Zn does not begin to precipitate until pH exceeds 7.0 and at a pH of 8.2 we should expect GrtualJy all zinc will be precipitated inorganica&. Adsorption of metals by organ& and clays is also affected by pH.

The presence of sediments which probably range from organic-rich and calcite-free thou& to essentiahy pure marl (e.g. sample D-15, 40% Ca) wiU complicate interpretation of the data but will also provide clues regarding potential metal sources. For example, we do not expect copper to move far in the general hydromorphic environment of the Kechika Project and any ma@ pond should by viewed as a geochemical barrier. Ziic wilJ be more mobile however ponds with strongJy mariy sediment are Likely barriers to zinc mobility. AS an example we expect that the strongly anomalous copper (850 ppm) m low c&ium sample A-Z is probably de&fed from a proximal source. J do not have the sample locations however I recall sample A-2 ia one of a set of ponds along Liard Tom Creek in NW Mock A. Samp1.e A-J is about 96% marl. Jf it lies upstream from A-2 then the melal

w source enters the drainage between tie two ponds for more directly at A-Z site. If A-l lies downstream then rbis metal barrier pond with low metals in sediment will bl0ck passage of copper and probably tic. from any further downstream dispersion. If we remove the marl component from sediment A-l then the residual copper content is increased from 4.5 ppin to 107 ppm which is anomalous comparcd to the norm for low cakium samples. If A-l is downstream from A-2 then we could conclude that most of the copper WBS trapped in site A-2, however some has reached A-l where the anomaly can only be detected by recalculation of the analyses on a calcite free basis.

v

V

I think the basic metals should be plotted as raw data on one set of maps due to the d&ability of presenting unmanipulatecl data; however a plot of Ca values should also be made for comparison.

A second set of maps should plot the metals of interest recalculated on a calcite-tie bask. To de&z these values each metal should be recalculated by the following formula:

calcite free metal r (ppm metal)(lOO) I [lo0 - (2.5)(Ca)]

This formula assumes all acid soluble calcium is in calcite. In low Ca samples which may be calcite free but which may report 1 or 2% Ca the metal value will be essentially unchanged. High Ca samples which are clearly marly will produce a significant increase in metal values with the calculated values being more comparable to the low Ca samples than are the raw data. In samples approaching pure marl (40% Ca) the recalculated metal values will become relatively inaccurate due sensitivity to accuracy of both metal and ti values. For example sample A-l (38.31% Ca) requires multiplying the Cu value by a factor of 23.7. Ifthe raw copper value of 4.5 were to have an analytical error of = 1 ppm, the recalculated copper value of 107 ppm would have an error of = 24 ppm. Sample D-15 has a Ca content of 40.22% which is higher than pure stoichiometxic calcite (40.0%) however the difference is within analytical error. The recalculation formula implies that recalculated metal values ti approach infinity as Ca approaches 40% and samples with more than 40% Ca cannot be recalculated at face value. I recommend using a maximum value 0f 38% Ca for the three samples reporting >38% Ca to avoid the problem of creating artificial extremes due to amplification on analytic error.

Samples with less than 35% Ca will have metal values multiplied by less than 8 which should cause little problem with taking the recalculated metals at face value. Samples with 35 to 38% Ca will have a metal multiplier of 8 to 20 and should be viewed cautiously and in context.

If the copper anomaly at site A-l indicat,ed only by the “lime-free” Cu value lies downsticam adjacent to obviously anomalous A-2 then it is likely a valid an0maly mak a suing of 3 anomalous ponds instead of the two ponds evident in the raw data, quite a coflclnsion from a sample value of only 4.5 ppm Cu. Unfortunately WC can’t compare associated elements Ag & Bi due to inadequate det.ccrion limits on the sample strongly diluted v&h marl. The only other over high Ca sample which indicated a Cu anomaly on

Kechika Project Page-2 R. R. Walker

recalculation is A-35 indicating UK recalculation of Cu does not generate copper anomalies in most samples and we should also examine site A-35. Samples with 335% Ca represent poor quality sample medium and follow-up should focus on o~anic-s around the mar& of these swampy pond3

The government lake sediment samples should be plotted along with Done&l’s samples but distlngghed by some symbol. This should by done within and between the areas of Donegal’s survey but there is no need to represent government samples at Kitza Creek east of F-block which are centred on competitor’s claims in an area of different relict drainage and overburden conditions than DOnegab data and which would distract from the @&%ance of Donegal’s zinc anomalies.

The government data records total Ca content rather than the acid soluble Ca reported for Donegal’s data. The range of values and their distribution seems similar by inspection. At least for the axa of L&d plain (low gradient, elastic starved drainage) we should assume that total calcium is carried in marl and apply the same correction to metaL to derive marl- free equivalent values. Those with l-&h calcium are almost certainly marl and those with low calcium, which may have a silicate component will by little affected by the caktdafion.

Elements of interest include MO, Cy Pb, Zn, Ag, Ni, As, Cd, Sb. Bi, U, I&, Se Mn, Ca, P, Ba.

-Phosphorous is relevant to Nick Type Mineralization which is enriched in Nii MO, U, Zn, PT-group, An, As, Se & Ba and is overlain by a phosphatic black sediment bed. It is of interest the two highest P values are in A-44 & A-45 associated with high or anomalous MO, Cu, Ag, Bi, Ni, Cd & Zn (high for A Block).

-Ba in Donegal’s data is not total Ba in contrast to government survey data. l’he two sets of data do not look comparable and should not be plotted together. Government Ba is higher.

-Se in lake S&S does not correlate with Ca whereas in soils Se correlates with Ca very strongly. Take the pond sediments at f&e value but question v.alidity of Se in soils, (plot an X-Y graph of Se vs Ca in soils and ask Acme why the unbelievable correlation - interference with Ca or Sr? Then why not in the lake s&j?)

-One could use spot plots of various s&s following the pattern OF the government SIUVZ~ with groupings at the approximate SO, 70, 90 & 95th percentile. Labelling the value on the top 5 percentile samples would b$;useful.

b) soils:

The soil data will he influenwd by the type of soil sampled. Ca (acid soluble) looks importarIt to distin,tiSh area? of carbonate bearing soil which is probably alkal&e from low Ca soils which are probably more acid and more leached. Most soils have low Ca less than 0.5% and ate probably essentially carbonate free. High calcium soils run ~JJ strings of

K&ii Project PAge - 3 R. R. Walker

.)

w

w

adjacent samples with more than 106 Ca and are probably ca&oiUte bearing. Calcite rich samples contain up t,o about 9% Ca imlicarhlg up ro 23% calcite and would undoubtedly be pH buffered and moderately alkaline. It is hard to imagine calcite rich soils developing on the dominant sand and gravel seen in the area. They may be indicative of soil affected by seeps or else developed on sub-crop or close to bedrock on lower slopes of meltwater channels or higher elevations poking above the gravel plain. A sample from a dry marly pond would also contain high Ca. One may tind that hlgb Ca samples have different metal contents.

Met& of interest are the same as for lake sediments except add iron. Iron doesnt look too interesting in general but it is standard for soils and there are places where it looks useful. For example, sample CB 1N 1900E looks anomalous in MO, Zn, As, P, Hg Sr Se. It is also very enriched in Mn & Fe suggesting the soil may he afkted by a seep carrying water from an oxidizing &tide source. The soil is Ca-rich and precipitation of Fe and Mn should be expected in a calcite rich alkaline soil. Although the metal anomaly is not outstanding, and is likely scavanged by Fe & Mn hydroxides & oxides, the site warrants follow-up to Iook for a potential site of strong metal emichment nearby, at the point of emergence of a groundwater seep, Zn would show detectable dispersion further from the discharge than Cu and Pb would likely stay behind in the source rock as sulfate.

Regards

Richard R. Walker

W

Keohka Project page - 4 R. R. W&ker

APPENDIX C

Rock Sample Descriptions

SAMP #

- I LOCATION

AREL- 1 Trepanier Creek

AREL-2 Trepanier Creek

AREL-3 Trepanier Creek

AREL-4

AREL-5

AREL-7

AWL-8

ARELZl- 1

ARRWl

Trepanier Creek

Trepanier Creek

Trepanier Creek

Trepanier Creek

Trepanier Creek

Trepanier Creek

ARRW2

ARRW3

Al Claim

Al Claim

ARSY 1 Trepanier Creek

ARSY2 Trepanier Creek

ARSY3 Trepanier Creek

- I DESCRIPTION

Green-grey fractured chat.

Green-grey fractured chat. Some beds are strongly fractured, while others show little fracturing.

Yellow, brecciated chert; brown hard (limonite-goethite?) iron oxide cements the fragments (homolithic).

Yellow, fractured chat.

Shattered yellow chat from fault zone.

Grey clay layer (1-3 cm) between yellow chat beds (IO-30 cm).

Yellow-grey shattered chert and limonite coating.

Grey chat with much limonite and black manganese oxide.

Sample of white clay seam in chert. Seams oriented at 18OV35” E. From large scarp wall of bedrock on east side of creek. [Whole rock analysis].

Massive basalt from large fragment in breccia.

Matrix-rich basalt breccia. Appears moderately clay altered; pale yellowish “sandy” matrix and fresh black basalt fragments. Sample is about 60% matrix. The breccia is unsorted with very angular equant clast from few mm to 1 m; mostly 2-10 cm. Matrix comprises 15-35%, and very locally up to 60% ranging from coarse sand to grit (granules). Clasts are very dark grey aphanitic groundmass in frag cores with 30% fluidal oriented plag microlites, perhaps 0.1 by 1 mm with polysynthetic twinning and look fresh. Also -10% honey coloured olivine up to 0.5 mm. Rims on fmgs -304 cm wide, grade to jet black and glassy gwmdmass with plagioclase microlites. No fabric, cleavage or joints; non-magnetic.

Quart&e with fme-grained pyrite. Located on north side of creek (flow 260’).

Weathered, rust stained chat(?). Outcrop here dips 30” westerly. Located 2 m east of ARSY I.

Z* Q-w) T=

35

163 f

19

13

10

40

101

24

81

74

17

103

165

5 co.3 28

12 0.4 163

15 0.4 21

67 0.3 65

26 co.3 13

14 ~0.3 81

8 co.3 30

15 co.3 13

3 co.3 12

4 0.3 13

Cl

1

I

<l

1

-i-

<l

<l

<l

<l

2

I

I

SAMP #

ARSY4

c

ARSYS

ARSY6

ARSYX F ARSY9

LOCATION -

T Trepanier Creek Chert, rust stained and with botlyoidal hematite alteration. Located 10 m east of 182

Trepanier Creek

Trepanier Creek

Trepanier Creek

Trepanier Creek

- ZII

(pwl

ARSY3.

Rust stained outcrop (chat?), 25 m downstream from ARSY4. 11

Grey and black chei-t; unaltered. Located 20 m downstream from ARSYS. 4

Rust stained (chat?) with minor amounts of silver coloured mineral. First outcop 4 on west side of creek, downstream from other samples.

Dark to light grey and greenish grey chat which weathers rusty orange. Thin 12 bedded (2-10 cm) at 34OV75”W. Exposed thickness -100 A.

I Pb

(ppm) 10

17

& (ppb) co.3

co.3

co.3

co.3

co.3

Cu Au @pm) (ppb)

71 1

26 <l

7 2

9 2

5 2

APPENDIX D

Certificates of Analyses

SOIL SAMPLES

ACME AN 4f”

ICAL LABORATORIES LTD. 852 E.~XASTINGS ST. V w

OUVRR BC VkA ~lR6 PiiONE(604)25~3-3158 ~FAX(604Q53-1716 j

\ GEOCHEMICAL ~XW.%IS CERTIFICATE m

Tizard Exolorations Inc. PROJECTS KETCHIKA File # 97-3740 Page 1 1022 - 470 Crsnville ~St..~~~Yan~~uver~ BC~V6C~lV3

:e

SAHPLE# no C" Pb zn AS Ni co nn Fe x ,A; $ & ,T; $ 2 ,; $ ,; Ca P La Ci- MS Ba Ti 8 Al Na K u AU'

wPwppnppnppnppnmPpn x XPpmPpn xppn xppn x x xppnppb

RAlW OOOE RE AAlN 1OOE ,,A," 050E ,%A," 1OOE MlN 150E

AAlN 2OOE AAIN 250E AAlN 300E AAlN 350E AA," 400E

AAlN 450E AAlN 550E AAlN 600E AAIN 650E AA,N 700E

AAlN 750E AAlN 800E AA," 950E MlN 1OOOE AAlN 1050E

AAlN 1lOOE AAIN 1150E AAlN IZOOE MIN 1250E AAlN 1350E

AAlN 1400E AAIN 1450E AAlN 1500E AAlN 1550E AAlN 1600E

AAlN 165Oi AAlN 1700E MlN 175OE AAlN 1800E AAlN 1850E

6 12

3 10 10

12 33 c.3 5 ‘9 <US 9 i6 .:i 6 51 c.3 5 43 c.3

20 9 505 2.69 2 27 9 568 2.24 3 14 5 249 1.56 <2 26 9 586 2.39 4 25 7 299 2.02 4

7 7 44 <.3 22 3 6 54 c.3 19 5 7 36 c.3 16 7 9 51 q.3 24 4 5 39 c.3 17

11 8 9 9 5

28 13 27

5 4

12 8

12 13

5

26 6 9

30 6

7 9 5

15 13

9 37 c.3 5 25 c.3 4 35 q.3

<3 7 <.3 c3 4 c.3

7 41 c.3 <3 2 c.3 <3 8 c.3

8 42 c.3 <3 16 c.3

s3 7 c.3 <3 iI s.3 <3 1 c.3

5 36 c.3 <3 6 c.3

8 P 4

29 6

14 14 12

5 6

c3 2 c.3 3 38 c.3 9 37 q.3 4 25 c.3 9 39 c.3

9 19 29 18 26

4 4 4

11 5

5 30 c.3 4 29 s.3 ; 35 c.3

42 c.3 7 43 c.3

13 14 22 29 19

7 374 1.88 7 36J. I.68 6 229 1.69 9 310 2.12 3 149 1.49

7 154 2.14 8 828 2.39 7 213 2.32

~1 309 .23 1 22, .25

8 286 2.12 ci 199 .31

4 652 .48 10 293 2.17

4 3724 .27

2 452 .28 4 2951 .36 1 198 .28 9 319 2.17 1 a5 .49

4 433 .64 5 146 1.34 8 267 2.29 5 115 1.69 8 223 2.29

5 99 1.58 5 112 1.60 7 145 2.12 5 143 2.02 7 187 1.88

4 ‘2 ‘2

2 2

6 5 4

<2 2

7 2

<2 3

‘2

‘2 <2 c2

6 <2

3 2 5 2 2

<2 2

<2 ‘2 <2

<2 <2 <2 c2 c2

c2 <2 <2 <2 <2

c2 <2 <2 <2 <2

c2 <2 c2 <2 <2

c2 <2 ‘2 <2 <2

<2 <2 <2 <2 <2

<2 <2 <2 <2 ‘2

3 33

i 52 20 3 55 3 58

3 34 2 55 3 20 3 26 3 20

.7

.9

.4

.5

.a

.8

.9

.5 .7 .2

4 34 ‘2 122

5 25 s2 154 ‘2 201

.4

.9

.4

.4

.3

3 71 .2 ~2 204 .7 <2 174 .4

4 59 .9 ‘2 157 .3

~2 158 ~2 161 <2 139

4 48 <2 153

<2 153 c2 78

6 26 5 18 4 27

.3

.7

.3

.7

.6

1.3 .6 .3 .2 .6

4 12 c.2 4 12 .3 5 13 c.2 5 18 .2 4 13 c.2

<3 <3 <3 <3 <3

<3 <3 <3 <3 <3

<3 <3 <3 <3 <3

<3 <3 <3 <3 <3

*3 <3 <3 <3 <3

<3 <3

3 <3 <3

<3 <3 <3 c3 <3

<3 50 .64 .w9 15 c3 38 1.17 .073 15 <3 39 .4l .o42 12

5 40 1.26 .076 16 4 37 1.48 ,076 16

<3 34 1.38 .073 14 <3 29 I.16 .076 13 <3 39 .35 .033 13

3 43 .49 .040 14 3 35 .38 .040 13

<3 42 1.10 .031 18 7 34 4.39 ,085 12

<3 44 .51 ,055 20 5 4 5.00 .078 1 6 3 5.01 ,054 2

<3 <3

3 <3 <3

<3 <3

3 <3

4

5 <3 <3 <3 <3

<3 <3 c3 <3 c3

40 3.67 .061 15 5 5.05 .063 2 7 5.14 .OPl 2

36 1.55 ,094 16 4 4.65 ,093 1

4 4.71 .089 1 6 4.71 .078 1 3 4.13 ,067 ~1

34 1.24 ,083 15 6 4.32 .133 2

5 4.33 .078 2 28 2.36 .069 10 43 .49 .063 20 37 .30 ,036 16 47 .54 ,031 16

4, .17 .029 14 41 .I8 ,036 14 44 .20 .033 15 41 .32 .048 18 43 .21 ,031 14

28 .30 354 .06 30 .53 490 .06 23 .27 242 .06 33 .57 528 .06 32 .57 453 .Ob

29 .47 478 .05 29 .48 368 .05 26 .31 196 .07 33 .42 241 .07 26 .38 179 .06

34 .48 411 .07 18 .92 705 .03 37 .57 275 .oa

3 .35 347 .01 3 .29 637 .01

30 .63 489 .06 2 .27 596 .Ol 4 .30 675 .Ol

30 .59 407 .06 3 .32 778 c.0,

2 .29 541 s.01 3 .23 940 c.01 1 .25 466 c.01

29 .47 452 .05 6 .29 649 .01

3 .22 585 .Ol 2, .47 718 .03 36 .53 318 .08 30 .42 201 .08 37 .44 411 .07

25 .30 126 .07 25 .32 112 .08 32 .42 154 .08 35 .43 235 .08 29 .36 179 .08

<3 1.33 .Ol .05 c2 3 1.06 .Ol .05 ~2 3 1.09 .Ol .03 <2 6 1.14 .Ol .05 s2 4 1.06 .Ol .04 ~2

<3 1.02 .Ol .05 <2 <3 1.02 .Ol .04 ‘2 <3 .96 c.01 .06 ~2 <3 1.31 .Ol .05 <2 <3 1.04 .Ol .05 c2

~3 1.29 .02 .05 <2 7 .86 .Ol .04 <2

~3 1.26 .Ol .04 ‘2 7 .I9 .Ol .04 <2 3 .42 .02 .Ol ~2

3 1.10 .02 .05 <2 5 .39 .02 .Ol c2

11 .34 .Ol .02 <2 4 1.04 c.01 .05 <2 3 .20 .Ol .03 <2

7 .13 .Ol .02 <2 <3 .21 .o, .Ol x2

7 .07 .02 .02 q2 3 .88 .Ol .04 <2 7 .38 .02 .02 <2

4 .22 .01 .02 c2 ‘ -93 .02 .04 <2 4 1.19 .Ol .05 <2

<3 1.11 .Ol .03 c2 ~3 1.60 .Ol .04 ~2

<3 1.07 .Ol .04 <2 <3 1.10 s.01 .04 <2 <3 1.30 c.01 .04 <2 ~3 1.26 .Ol .05 ‘2 <3 1.32 s.01 .04 <2

STANDARD C3/AU-S 25 59 30 154 5.3 35 11 717 3.42 57 18 3 22 28 24.2 11 23 75 .57 .087 18 167 .63 152 .09 22 1.81 .03 .I6 14 48

ICP - ,500 CRAM SAMPLE 15 DiGESTED WTH 3ML 3-1-2 HCL-HYO3-"20 AT 95 DEG. t FOR ONE "CUR AN0 IS DILUTED TO 10 ML UITH WATER. THlS LEACH 15 PARTlAL FOR "N FE SR CA P LA CR MG BA TI S V AN0 LIMITED FOR NA K AND AL. - SAMPLE TYPE: SOIL A"' - AQUA-REG,A,M,BK EXTRACT, W/AA FINISHEO.(lO GM) Samles besinninq 'RE' are Reruns and 'WE' are Reiect Reruns.

DATE RECEIVED: JUL 21 1997 DATE REPORT MAILED:

+tf i 'I 47

c

b SIGNED BY...:...... .O.TOYE, C.LEONt, JMNC; CERTlFlEO B.C. ASSAYERS

ALL results are considered the confidential property of the client. km assmes the liabiliries for actual cost of the adysis only. Data- FA _

/

c Tizard Explorations Inc. PROJECT KETCHIKA FILE # 97-3740

HO C" Pb 2n AL2 Ni co nn Fe AS ” AU Ti a AL Na K u A". FvFmFP %F?mppn xppn xppn % % XmPFJJ -

4 1.51 .01 .04 <2 9 48 s.3 b 41 <.3 7 33 q.3

10 35 C.3 9 40 C.3

20 7 168 2.36 23 b 171 2.01 I6 6 159 1.90 18 7 157 2.06 I7 7 175 2.15

9 u c-3 i ii c:i 10 36 c.3

9 37 s.3 9 39 <.3

25 la 15 lb 24

a 228 2.44 6 lb8 1.99 b 145 1.86 5 I43 2.13 7 142 2.19

a 33 c.3 5 33 C.3 9 36 c.3 a 36 C.3 b 51 C.3

22 24 20 11 13

7 255 2.16 8 258 2.16 7 156 2.27

1 13

4 6 6

5 35 s.3 <3 a c.3

a 31 c.3 a 43 c.3

7 172 1.30 6 144 2.04

9 47 C.3

10 7

18 24 24

4 138 1.42 1 132 .I8 6 206 1.78 9 200 2.34 7 179 2.65

9 5 48 c.3 14 7 3552 1.16 20 14 b8 c.3 32 9 386 2.52

5 6 60 C.3 13 6 I2a 1.67 5 7 61 C.3 I4 5 lb5 I.50 6 a 57 C.3 I7 7 lb2 1.86

I9 IO Ia9 1.95 2, 8 233 2.30 15 5 256 1.35 24 7 163 2.27 22 9 I79 2.27

9 79 c.3 9 64 C.3 8 38 c.3 a 40 C.3 6 40 <.3

7 39 C.3 11 39 C.3

9 50 C.3 9 37 C.3 5 32 c.3

17 6 159 1.90 I7 6 135 2.07 18 7 181 2.14 23 6 I76 2.07 16 5 113 1.82

C2 <2 <2 <2 <2

<2 <2 <2 <2 <2

<2 ‘2 <2 <2 <2

x2 <2 <2 ‘2 <2

<2 <2 <2 <2 <2

C2 C2 <2 <2 <2

<2 ‘2 <2 <2 <2

6 14 .b ~3 6 15 .9 -3 4 14 .5 a 4 lb q.2 G 4 15 .2 <3

4 15 T.2 4 4 14 T.2 4 4 13 q.2 4 3 13 .3 <3 3 13 .4 <3

3 <3 <3

3 <3

<3 4

a c3 <3

q3 3

C3 <3 C3

‘3 <3 <3 <3

3

0 <3

3 <3 <3

3 <3 <3 C3 <3

<3 C3 <3 <3

3

51 .20 .036 I4 43 .23 .033 15 43 .21 .029 14 44 .25 .032 14 45 .22 .oza I4

36 .45 138 .08 33 .47 173 .09 30 .41 173 .07 32 .48 145 .09 33 .49 159 .OP

37 .49 159 .09 32 .43 154 .08 28 .37 154 .oa 31 .3b 154 .08 33 .L4 I46 .07

8 1.24 .Ol .04 <2 3 1.25 .Ol .04 <2

<3 1.27 .OI .04 ~2 <3 1.33 .Ol .04 <2

3 3

<I 6

<I

51 .22 .032 14 44 .22 .030 13 43 .19 .027 12 49 .18 .028 12 52 .I9 .021 12

3 1.57 .01 .05 <2 1 ~3 1.28 .oI .o4 ~2 <I

7 1.16 .Ol .05 C2 <l <3 1.34 .Ol .03 <2 4 ‘3 1.31 .01 .04 <2 4

4, .54 .032 14 42 .54 ,034 15 46 .25 .019 13 36 .25 .025 10 49 .21 .096 13

33 .45 338 .07 33 .45 333 .07 36 .48 202 .lO 20 .24 170 .Ob 26 .27 143 .Ob

4 1.28 .ol .05 ~2 ~3 1.27 .02 .05 <2 <3 1.30 .OI .05 C2

4 .98 .01 .03 ~2 C3 1.14 c.01 .03 C2

39 .23 .030 11 22 .2b 174 .Ob ~3 .Pb c.01 .O4 ~2 77 10 4.18 .113 2 3 .22 684 c.01 I3 .13 ‘.Ol .01 C2 5 44 .25 .027 11 27 .32 187 .07 3 I.23 .Ol .04 ~2 1 49 .I8 ,032 I2 35 .46 214 .Oa <3 1.49 c.01 .04 ‘2 8 5, .I9 ,067 12 37 .44 136 .08 C3 I.47 c.01 .05 <2 1

I3 5.07 .12I 4 I3 .44 858 .02 33 2.06 .049 I7 29 .78 341 .04 42 .30 .033 I3 28 .39 210 .07 36 .24 ,045 12 23 .34 170 .Ob 41 .28 ,059 13 26 .37 204 .05

9 .54 .02 .04 <2 3 I.27 c.01 .Ob ~2 3 I.18 .oI .04 ~2

-z3 1.06 .01 .05 x2 <3 I.,2 ~.Ol .05 C2

1 1 1

<l 2

AAlN IPOOE AAlN 1950E WIN ZOOOE AAlN 2050E AAIR ZIOOE

AAlN 2150E AAlN 22OOE AAlN 2250E AAIN 2300E Ml" 2350E

AAlN 2400E RE AAIN 2400E AAlN 2450E AAIN 2500E AAlN 2550E

4 27 .5 ~3 4 26 .2 <3 5 16 T.2 C3 2 15 C.2 <3 * 12 .5 C3

AAlN 2bOOE AAlN 2650E AAIN 2700E RAlN 2750E AAIY 2800E

3 14 .3 <3 <2 133 1.4 <3

3 15 C.2 <3 4 13 q.2 <3 3 13 .3 <3

~2 lb9 .b <3 3 50 .b C3 3 I7 C.2 <3 2 I5 .2 <3 2 17 C.2 <3

AAlN 285OE AAlN 2900E AAlN 2950E ARlN 3000E k&IN 3050E

AAlN 3100E AAlN 3150E AA,N 3200E AAIN 3250E AAlN 3300E

42 .25 .087 13 28 .37 194 .ob ~3 I.42 c.01 .04 ~2 ~1 43 .29 .068 15 31 .53 184 .oa 3 I.33 .o, .Ob <2 2 39 .23 .062 12 24 .32 717 .05 4 .70 .01 .04 C2 2 45 .20 .037 14 36 .47 lb9 .09 C3 1.41 .Ol .04 <2 1 4a .la .037 I5 35 .46 lb3 .08 <3 1.50 .Ol .03 C2 1

3 14 .3 C3 4 I7 .4 C3 2 14 .3 <3 4 14 C.2 C3 5 I3 C.2 C3

PIAIN 3350E 4 13 .4 <3 4 13 c.2 <3 4 I3 .5 <3 5 la .2 ~3 3 13 .2 <3

41 .19 ,034 13 30 .40 139 .oa 4 1.28 <.Ol .03 ‘2 47 .19 .032 13 31 .40 130 .oa C3 1.40 c.0, .03 C2 47 .I9 ,029 13 33 .43 162 .09 3 1.40 .01 .03 <2 40 .30 ,053 I5 33 .53 lb7 .09 3 1.20 .Ol .04 <2 44 .19 .047 I2 27 .35 131 .07 C3 1.27 C.01 .03 C2

1 AAIN 3400E AAlN 345OE AAlN 3500E

Cl / 1 2 /

<I I AAlH 3550E

!L 25 62 40 159 5.5 32 11 744 3.60 52 19 ‘2 17 30 22.5 15 24 76 .59 .090 17 159 .bb 153 .09 19 1.9, .04 .I6 lb 46 :

SawLe type: SOIL. SmvLes beqinniw 'RE' are Reruns and 'ME' are Reiect Rewns.

All resulrs are considered the confidenfial pmperfy of the client. Acme assums the Liabiliries for actual cost of the analysis Only. oata- FA _

Tizard Explorations Inc. PROJECT KETCHIKA FILE # 97-3740 Page 3 13E UullllW

AAIN 3600E AAlN 3650~ AAlN 3700E AAlN 3750E AAlN 38OOE

AAlN 3850E AAlN 3900E AAlN 3950E AAlN 4000E AAlN 4050E

AAlN 4100E AAlN 4150E AAlN 42OOE AAlN 4250E AAlN 430OE

AAZN OE AAZN 50E RE AAZN 50E AAZN lOOE AAZN 150E

AAZN 2OOE AAZN 250E AAZN 300E AAZN 350E AAZN 400E

AAZN 450E AAZN 50OE AA2N 550E AAZN 600E AAZN 65OE

AA2N 700E AAZN 750E ARZN 800E AAZN 850E AAZN 9OOE

7 7 42 c.3 5 I 38 s.3 4 6 34 c.3

10 4 32 c.3 6 7 44 <.3

4 11 8 10 5 7 5 7 3 7

11 6 6 c3 7 <3

12 5 8 5

5 6 6 6 3 6 6 6 5 9

11 7

15 8 8

5 11 10 7

6 8 17 9

9 8

16 10 4 <3 4 3

16 3 12 8

44 c.3 43 c.3 39 c.3 35 c.3 32 c.3

33 c.3 7 c.3 2 c.3

45 q.3 37 c.3

31 c.3 35 c.3 32 c.3 46 c.3 38 c.3

38 c.3 34 c.3 41 s.3 39 .7 38 c.3

89 c.3 37 ‘.3 47 c.3 52 c.3 64 c.3

53 c.3 3 c.3

25 c.3 36 c.3 41 c.3

22 15 22

:;

7 161 2.43 <2 5 127 1.72 ~2 7 171 2.08 3 6 118 1.99 4 7 183 2.24 5

19 8 184 2.40 3 26 8 262 2.22 3 18 6 146 2.48 5 16 5 145 2.15 4 15 5 114 1.66 3

24 10

2: 23

72621.75 3 2 637 .47 ~2 1 216 .,5 ~2 83961.94 2 8 171 2.27 2

14 21 16 24 24

29 23 34 30 23

6 198 1.68 ~2 6 144 2.07 ~2 6 138 1.97 2

11 38L 2.41 ~2 7 165 2.32 2

10 348 2.50 ~2 7 442 1.53 ~2

Ii 581 2.91 5 12 278 2.49 5

7 165 2.45 2

:'; 22 36 28

Ii 233 3.02 <2 9 183 2.47 4 7 163 2.18 ~2

28 5 7

12 28

10 298 2.65 5 10 200 3.22 5

8 183 2.30 5 1 433 .24 ~2 2 1057 .96 ~2 3 865 1.64 3

10 200 2.36 2

<2 <2 <2 <2 <2

<2 <2 c2 <2 c2

<2 x2 <2 ‘2 <2

c2 ‘2 ‘2 ‘2 <2

<2 <2 <2 ‘2 <2

c2 c2 <2 <2 ‘2

<2 <2 <2 <2 <2

5 16 .5 4 15 .2 5 17 c.2 2 18 .3 5 17 c.2

5 18 .4 5 2L .2 4 14 .5 3 16 .2 3 18 <.2

3 36 .2 ~2 296 .2 c2 413 .2

3 134 .3 3 38 .4

4 19 c.2 4 18 <.2 4 18 <.2 4 36 .3 3 23 .3

4 43 .3 <2 101 .3

4 48 .7

: 29 17 .3 .2

4 19 .5 5 26 .3 5 20 c.2 3 31 c.2 4 14 .3

4 37 .4 <2 185 .4 ~2 192 .3 <2 173 1.1

3 35 .2

<3 <3

4 6

<3 7 3

4 4

4 <3

<3 <3 <3 <3 <3

<3 <3 <3 <3 <3

c3 <3 <3 <3 <3

<3 c3 <3

4 <3

54 .22 .044 17 37 .43 148 .09 <3 1.64 .Ol .03 42 .20 .027 15 28 .33 148 .08 c3 1.24 c.01 .04 42 .26 .041 17 34 .48 139 .09 5 1.30 .Ol .06 44 .27 .061 14 31 .31 128 .06 <3 1.18 .Ol .04 46 .27 .036 17 36 .53 146 .I1 4 1.40 .Ol .06

51 .26 .050 44 .39 .OM 52 .21 .085 47 .21 .0&c 43 .26 .034

17 37 .47 144 .lO ~3 1.46 .Ol .05 18 34 .51 201 .09 ~3 1.36 .Ol .06 13 35 .39 83 .09 <3 1.35 .Ol .07 17 32 .35 113 .08 ~3 1.14 .Ol .06 14 26 .28 117 .08 <3 1.00 .Ol .04

37 .79 .040 14 28 .31 266 .06 3 .98 .02 .03 8 5.26 .073 4 6 .52 475 .Ol 8 .31 .02 .03

11 3.87 .089 1 3 .67 331 c.01 18 .12 .02 .Ol 30 3.70 .094 15 24 .59 349 .05 3 .90 .03 .OL 45 .59 .030 15 33 .52 233 .08 c3 1.33 .Ol .05

44 .28 .026 52 .28 .025 30 .26 ,024 31 .57 .026 32 .38 .026

52 .63 .053 26 2.71 ,114 31 .98 ,077 33 .3l .046 57 .29 .045

64 .24 ,039 49 .48 .031 52 .33 .045 49 .60 .074 68 .,9 .043

52 1.30 ,067 5 5.99 ,114 4 5.59 .097 0 5.63 .232

48 .96 .059 18 36 .32 470 .08

14 27 .33 184 .08 <3 1.21 .Ol .04 14 35 .41 194 .09 <3 1.44 .o, .04 14 33 .38 184 .09 ~3 1.36 c.01 .04 14 37 .45 368 .08 <3 1.70 .02 .05 17 38 .55 236 .I0 <3 1.48 .Ol .04

18 41 .60 392 .09 <3 1.53 .Ol .03 10 25 .31 493 .04 <3 .94 .02 .OL 19 42 .66 532 .08 <3 1.56 .02 .OL 18 40 .55 298 .OP <3 1.60 .02 .03 15 37 .47 I60 .09 <3 1.55 .Ol .05

16 41 .43 201 .,I 19 41 .55 296 .OP 17 36 .52 236 .lO 21 41 .64 409 .08 16 43 .34 196 .ll

17 38 .95 477 .07 1 3 .30 566 c.01 1 3 .32 731 c.01 2 5 .29 ,151 .Oi

<3 1.93 .Ol .05 <3 1.43 .02 .05 x3 1.49 c.01 .05 <3 1.54 .02 .05 ~3 1.83 .Ol .06

<3 1.41 .02 .06 10 .ll .Ol .02

3 .13 .Ol .02 17 .21 .Ol .03 ~3 1.28 .02 .07

<2 <2 ‘2 <2 <2

<2 ‘2 <2 <2 <2

‘2 <2 <2 c2 s2

<2 ‘2 <2 <2 <2

<2 ‘2 <2 ‘2 <2

<2 <2 c2 <2 <2

<2 <2 ‘2 <2 <2

1 2 5 1 1

2 <I

3 <I

2

1 <I 4

2 1

2 1 1 1 1

1' 1 3 1 i

1 2 1 1 3

7 4

3 1 2

STANDARD CJ,A"-S 25 62 33 158 5.7 36 il 733 3.53 54 23 2 18 34 23.5 16 19 79 .64 ,090 18 167 .66 153 .lO 17 1.95 .03 .18 20 48

All results are considered the confidential property of the client. Acme assmm the liabilities for actual cost of the analysis only. oara- FA _

Tizard Explorations Inc. PROJECT KETCHIKA FILE # 97-3740 Page 4 '

t

M2N 950E AA2N 1OOOE AAZN 1050E M2N 1lOOE AA2N 1150E

AAZN 12OOE AAZW 1250E AAZN 1300E AA2N 1350E AA211 1400E

M2N 1450E M2N 1500E AA2N 1550E M2N 16OOE kA2N 1650E

RA2N 170OE AA2N 1750E M2N 16OOE AA2N 1850E AAZN 1900E

10 4 36 c.3 30 3 11 50 c.3 21 5 6 5, ‘.3 20 9 14 50 c.3 22 6 9 42 c.3 24

8 183 2.56 7 309 2.01 7 181 2.24 8 141 2.21 9 173 2.56

6 7 4 7 5 a 4 7 6 6

54 c.3 39 q.3 69 c.3 58 c.3 34 c.3

7 c.3 4 c.3 3 c.3

20 c.3 43 c.3

26 15 26 20 21

8 177 2.96 5 149 2.16 9 201 2.61 7 185 2.16 6 169 2.00

7 3 13 <3 13 <3 28 4 14 6

4 5 8

:;

2 730 .20 1 128 .24 2 210 .39 7 538 1.47 9 395 2.22

9 8 5 6 4 4 6 5 6 6

24 17 16 16 18

10 283 2.47 9 303 2.19 6 224 1.92 7 184 1.96 7 204 1.96

7 b 5 7 5 7 7 8 4 8

45 c.3 46 s.3 38 <.3 38 c.3 48 c.3

37 c.3 46 c.3 44 c.3 34 c.3 28 c.3

24 7 186 2.26 25 8 171 2.23 26 8 lb6 2.19 20 8 154 2.12 17 6 132 1.81

7 5 29 c.3 18 7 160 1.77 5 6 33 q.3 20 7 144 1.08

10 8 40 c.3 23 8 191 2.22 b 7 45 c.3 19 7 270 2.02 9 7 45 c.3 27 10 332 2.24

7 3 38 c.3 20 7 5 41 c.3 22 3 6 39 c.3 14 8 3 45 c.3 29 8 4 46 c.3 29

7 220 2.02 7 215 2.17 5 133 1.98

10 218 2.85 10 196 2.94

7 ‘2

2 12 c2

<2 <2 c2

2 2

‘2 <2 ‘2 ‘2

2

<2 <2 <2

2 <2

<2 <2 <2

2 <2

<2 <2

3 <2

2

2 2 3 2 3

<2 ‘2 ‘2 x2 <2

‘2 <2 <2 <2 <2

<2 <2 ‘2 <2 <2

‘2 <2 <2 <2 <2

<2 <2 <2 <2 <2

<2 <2 <2 <2 <2

<2 <2 <2 <2 <2

5 27 .3 3 26 .3 4 15 c.2

<3 <3 <3 <3 c3

49 .47 ,027 20 44 .45 ,028 15 48 .25 .059 17

41 .53 405 .lO 32 .41 310 .08 35 .47 166 .lO 34 .34 205 .07 38 .47 160 .lO

~3 1.42 .02 .05 <3 1.50 .02 .05

47 .25 .071 15 54 .21 .042 16

~3 1.52 .01 .06 ~3 1.24 .O, .06 c3 1.59 .Ol .Ob

<3 62 .18 ,067 16 <3 52 .23 .074 lb <3 54 .20 .055 16 <3 46 .24 .051 16 <3 43 .31 ,034 20

42 .45 132 .lO 32 .34 121 .09 39 .47 179 .lO 36 .46 140 .I0 34 .48 210 .10

3 .33 551 .Ol 4 .34 598 c.01 5 .34 867 .Ol

20 .49 1510 .03 32 .62 663 .06

<3 1.90 .Ol .05 <3 1.40 .Ol .04 <3 1.74 c.01 .05 <3 1.41 .Ol .05

3 1.24 .Ol .04

<3 3 5.25 .090 1 c3 3 4.83 .092 1 <3 9 5.60 .076 3 <3 27 4.18 .0@6 11 c3 42 1.07 ,059 16

10 .I5 .02 .04 9 .17 .02 .03 7 .38 .02 .02 3 1.04 .02 .03 3 1.32 .02 .04

<3 50 .57 ,024 18 38 .55 434 .lO <3 52 .46 .018 14 33 .39 396 .OP <3 47 .28 .039 15 28 .40 194 .lO <3 47 .27 .027 15 31 .41 232 .09 <3 45 .31 ,024 16 32 .47 269 .09

<3 1.54 .03 .06 <3 1.57 .Ol .05

<3 46 .38 .040 17 36 .55 235 .I0 <3 47 .33 .020 16 36 .50 269 .ll <3 46 .32 .019 15 36 .49 260 .I, <3 47 .38 ,023 16 34 .47 321 .08 <3 43 .29 ,029 lb 31 .45 188 .09

~3 1.16 .Ol .05 ‘2 <3 1.29 .Ol .04 <2 <3 1.43 .02 .04 <2

<3 1.39 .02 .05 <3 1.37 .02 .05 <3 1.37 .02 .05 <3 1.50 .02 .04 <3 1.23 .O, .04

<3 39 .37 .035 15 <3 45 .30 .035 16 <3 46 .40 .041 20 <3 43 .42 ,036 15 <3 45 .48 ,036 18

31 .43 212 .08 32 .51 196 .09 37 .53 272 .I0 32 .48 284 .09 36 .46 346 .09

<3 1.21 .Ol .04 <3 1.25 .Ol .04 <3 1.41 .02 .05 <3 1.41 .02 .05 <3 1.53 .02 .06

<3 46 .32 .025 17 33 .47 231 .OP <3 1.44 .02 .04 3 44 .34 .044 17 36 .54 197 .OP <3 1.35 .02 .06

<3 51 .26 .079 14 29 .30 128 .08 *3 1.05 .Ol .05 <3 57 .I9 .061 16 43 .54 159 .lO ~3 1.80 .Ol .06

6 60 .22 ,100 18 40 .53 171 .09 4 1.85 c.01 .06

<2 <2 <2

2 15 .2 4 16 .3

4 15 .5 2 15 <.2 4 16 .3 5 16 .3 5 19 ‘.2

<2 184 .7 q2 194 .4

<2 <2

<2 c2 c2 <2 <2

<2 ‘2 <2 <2 ‘2

x2 <2

c2 222 c.2 <2 180 q.2

3 52 .2

32 .5 26 .2 18 c.2 16 c.2 19 .2

22 .2 21 c.2 20 c.2 23 .3 18 c.2

21 .3 17 c.2 23 c.2 24 <.2 28 c.2

20 c.2 19 c.2 17 .3 14 c.2 14 .2

AAZN 1950E AAZW ZOOOE RE AAZN 2000: AAZN 2050E AAZN 2100:

RA2N 2150: I\AZN 22ooi M2N 2250E IU\ZN 23OOE kA2N 2350E

<3 <2 <2 <2 <2 <2

<2 <2 <2 <2 <2

<2 <2 ‘2 c2 <2

c3 s3 <3 <3

<3 c3

3 <3 <3 <1

18 i 2 2 7

<3 c3

k&2" 2400: W.2" 2450: b.A2N 2500E I\AZN 2550E 9A2N 2600:

<3 3

c3

jTANOAR0 C3/AU-S / 24 61 31 156 5.7 35 11 727 3.40 53 21 2 17 31 23.2 17 28 78 .61 ,088 18 163 .6b 160 .lO 19 2.00 .04 .18 20 48

SamLe twe: SOIL. Sawles kginninq 'RE' are Reruns and 'ME' are Reject Reruns.

ALL results are considered the confidential property of the client. Acme assws the Liabilities for actual cost of the analysis only. oata- F/L _ !

Tizard Explorations Inc. PROJECT KETCHIKA FILE # 97-3740

SAHPLE# i no tu Pb 2n Ag Ni Co Nn Fe Y A"* 'FvPFmmFwwpp"Pp"w xppnw xppn xppn x x XPPppb

AAZN 265OE AAZN 2700E AAZN 2750E &AZ" 28OOE M2W 2850E

9 9 8 5 7 4 7 8 6 9

46 <.3 I9 53 <.3 11

7 201 1.97 2 7 311 1.89 6 6 090 2.70 9 7 198 2.09 4 9 202 2.88 7

a 2351.95 3 7 185 2.18 4 8 I@5 2.27 ~2 7 168 2.14 3 8 193 2.00 4

<2 <2 <2 <2 <2

<2 ‘2 <2 ‘2 c2

<2 <2 ‘2 c2 <2

14 1.7 29 .9

193 .9 15 .6 16 .5

15 c.2 17 c.2 16 s.2 14 .2 15 .2

3 50 .22 .039 <3 46 .60 .041

7 10 5.55 .09a 7 45 .26 .061 4 60 .26 ,062

14 3, .33 147 .07 10 26 .27 302 .06

3 7 .44 647 .Ol 16 34 .46 138 .07 15 40 .52 138 .lO

14 29 .34 131 .07 16 36 .54 151 .09 15 37 .49 165 .lO 15 34 .48 122 .lO 14 3, .39 206 .07

3 1.23 .Ol .04 <3 1.10 c.01 .04

14 q.3 7 42 <.3 22 50 c.3 27

55 c.3 12 46 c.3 23 64 <.3 22 45 c.3 20 44 <.3 18

10 .23 .02 .01 3 1.27 .01 .05 5 1.58 .Ol .07

AA2N 2WOE AAZN 2950E AAZN 3000E Apl2N 3050E .UZN 3100E

4 5 8 7 4 8 6 7 5 7

3 44 .26 [email protected] <3 46 .30 .061

3 51 .24 .029

<3 1.13 .01 .06 <3 1.39 .Ol .05 c3 1.5a .01 .04

3 1.39 .Ol .05 <3 1.38 .Ol .04

AAZN 3150E AA2N 3200E AAZN 3250E PAZ" 3300E RE AAZW 3300E

7 6 4 5 6 5 6 6 6 5

41 c.3 20 43 c.3 22 42 c.3 20 41 c.3 22

41 c.3 22 8 184 2.14 ~2 8 205 2.07 3 7 178 2.10 <2 7 172 2.10 3

a 2201.86 2 28 c.2 19 <.2 20 .2 18 c.2 18 c.2

c3 46 .25 .050 c3 47 .24 .036

<3 38 .49 ma 4 46 .31 .036

c3 45 .33 .039 c3 45 .27 .041 c3 45 .27 .042

15 32 .47 283 .07 15 34 .46 225 .08 15 33 .46 206 .08 16 36 .46 199 .09 16 35 .46 205 .09

kk2N 3350E AAZN 3400E M2N 3450E AAZN 3500E AAZN 3550E

12 7 42 c.3 27 5 6 37 c.3 20

12 4 52 c.3 32 13 7 32 <.3 31

7 6 37 c.3 24

8 207 2.40 6 7 133 1.90 2

1, 294 2.31 3 9 193 2.21 6 9 221 2.13 4

6 27 .4 4 19 .3 4 30 .2 6 24 .2 5 18 c.2

c3 44 .51 .074 c3 40 .32 .040 <3 44 .57 .063 c3 40 .46 .089

3 47 .29 .04a

22 40 .58 284 .09 14 32 .45 215 .08 18 37 .54 384 .oa

<3 1.33 .02 .05 <3 1.35 .02 .04

3 1.33 .Ol .05 5 1.45 .Ol .05

~3 1.42 .Ol .05

<3 1.37 .02 .07 <3 1.23 .oi .04 <3 1.50 .02 .05 <3 1.17 .02 .05 ~3 1.38 .ol .05

AA2N 360DE AA2N 3650E AAZN 3700E M2N 3750E AAZN 3800E

2a c.3 17 7 110 2.08 <2 38 c.3 15 6 152 1.70 ~2 40 c.3 22 7 171 2.37 5 59 c.3 27 10 232 2.82 4

12 483 1.79 ~2

2 341 .47 c2 1 99 .I7 2

12 945 1.81 2

43 <.3 21

10 c.3 25 4 c.3 10

a6 c.3 23 40 c.3 24 41 c.3 17

34 c.3 26 38 c.3 23 43 c.3 27 44 c.3 14 36 c.3 29

13 .2 14 .2 17 c.2 17 c.2 36 .3

5 49 .,a ,050 c3 42 .23 ,044 c3 52 .27 ,064

6 58 .27 ,093 c3 41 .65 .056

M2Il 3850E M2Il 3900E M2N 3950E AAZM 4000E AAZN 4050E

13 4 9 7 4

8 7 8 2 8

<3 <3 c3

a 5

<3 8 6.29 .094

20 36 .62 237 .08 16 34 .49 193 .09

9 27 .23 154 .07 13 28 .36 130 .08 15 35 .45 128 .09 16 41 .54 166 .09 15 2a .37 419 .07

5 6 .35 920 .Ol

~3 1.52 .Ol .04 <3 1.21 .01 .05

3 1.35 .Ol .06 <3 1.62 .Ol .07 c3 1.31 .02 .06

6 .54 .Ol .02 14 .14 .Ol .03

AAZN 41DOE kA2N 4150E AAZN 4200E AAZN 4250E AA2N 4300i

8 187 2.17 2 6 140 1.63 2

8 161 1.95 3 8 192 2.04 ~2 8 212 2.37 6 5 124 1.71 ~2 9 190 2.57 4

<2 <2 <2 <2 <2

c2 <2 c2 c2 <2

<2 <2 <2 <2 <2

<2 c2 ‘2 c2 <2

2 3 4 5 2

<2 <2 c2

4 4

5 5 5 3 5

248 .5 222 .2 271 1.4

22 c.2 16 c.2

<3 c3 <3 <3 <3

<3 <3 c3 c3 <3

<3 -c3 <3 c3 <3

<3 <3 <3 <3 <3

<3 <3 <3 <3 <3

<3 c3 s3 c3 c3

c3 <3 <3 <3 <3

4 6 5.63 .096 <3 17 4.19 .I65 c3 45 .35 ,036 c3 37 .26 ,043

3 39 .26 .043 <3 41 .2E .037 <3 46 .28 .053

5 44 .19 .02a

1 2 .27 642 c.01 7 12 .49 550 .02

16 37 .46 262 .09 13 26 .37 152 .OB

8 .59 .02 .OL <3 1.40 .02 .05 c3 1.18 .Ol .04

17 c.2 17 q.2 17 s.2 14 c.2 17 c.2 5 46 .28 .060

16 32 .47 182 .08 14 35 .4a 170 .09 15 38 .56 164 .09 14 27 .33 138 .oa 16 40 .55 146 .lO

<3 1.37 .Ol .05 ~3 1.29 .01 .05 c3 1.45 .O, .06 <3 1.22 .Ol .05 <3 1.58 .oi .07

c2 c2 c2 c2 c2

<2 <2 <2 <2 <2

<2 <2 c2 <2 <2

<2 <2 ‘2 <2 <2

<2 <2 <2 c2 <2

<2 c2 ‘2 <2 c2

‘2 <2 *2 ‘2 <2

3 1 1

4 1

4 2

<l 1 1

<I <I Cl <I

2

<I 1 2 1 2

<I 1

Cl 4

3

<I <i <l

2 <I

4 <I <I

1 1

STANDARD CS,AU-S i 25 64 35 165 5.7 37 12 780 3.63 55 13 2 19 30 23.8 14 23 81 .61 .095 18 168 .67 148 .I0 22 2.00 .05 .I7 19 54


MO tu Pb zn Ag Ni Co Nn Fe As U Au Th ST Cd Sb Bi V Ca P La CT Hg Ba Ti 8 AL "3 K v Air w x Y. xppnppb

AA3N OE AA3N 30E kk3N IOOE RE AA3Y 1OOE

8 II 13 14 10

10 3 8 b 6

9 9

11 7 7

10 3 9 9 9

IO 10

8 7 5

27 16 24 21 lb

7 58 c.3 7 42 c.3 6 35 s.3 6 52 c.3 5 70 c.3

6 34 c.3 8 39 <.3 8 62 <.3 7 39 c.3 8 36 c.3

8 36 c.3 b 56 c.3 6 43 c.3 8 47 c.3 8 43 c.3

b 33 c.3 3 39 c.3 7 37 c.3 3 47 c.3 9 34 c.3

7 42 c.3 7 64 c.3 6 39 c.3 6 31 c.3

IT 30 q.3

25 10 276 2.60 2 13 6 3731.64 <2 15 9 261 1.92 ‘2 14 9 260 1.87 2 25 8 301 2.39 <2

24 30 44 41 33

8 218 2.14 9 321 2.48

11 287 2.91 9 353 2.30

10 261 2.59

‘2 2 2 8 2

28 9 203 2.36 ‘2 14 6 166 1.94 ‘2 27 9 216 2.66 3 24 8 192 2.43 c2 22 7 176 2.12 3

21 6 i49 2.02 3 30 9 198 2.46 3 27 7 1&i 2.40 3 28 9 203 2.55 3 23 7 156 2.08 <2

25 7 200 2.33 2 13 6 281 1.37 <2 26 7 162 2.29 4 28 10 234 2.68 2 28 9 778 2.49 4

25 8 228 3.28 <2 29 9 18, 2.94 b 24 8 138 2.18 <2 22 8 194 2.35 4 23 7 185 2.17 5

41 11 382 3.21 4 34 9 398 2.68 2 38 10 1060 2.47 2 30 6 2417 1.14 ‘2 23 7 637 1.50 <2

19 c.2 21 .4 17 c.2 17 c.2 23 .b

37 .3 32 c.2 37 ‘.2 32 c.2 30 c.2

17 .2 13 c.2 18 .4 18 .3 17 .2

lb .2 16 c.2 15 ‘.2 16 .4 17 c.2

18 .4 20 .2 16 .2 17 .2 26 .2

20 .3 13 c.2 22 .2 18 c.2 19 .5

<3 37 .30 .031 7~ 43 .34 .032

<3 31 .27 .027 <3 30 .27 ,026 <3 35 .31 ,040

16 39 .50 *OS .ll <3 1.31 .02 .07 13 28 .30 263 .07 <3 1.19 .Ol .o4 14 31 .33 194 .09 ~3 1.32 .02 .04 14 30 .32 191 .09 <3 1.28 .Ol .04 18 39 .44 277 .I0 ~3 1.87 .Ol .Ob

c.3 <3 c3 <3 <3

<3 c3 <3 <3

3 3 6 5 5

5 5 5 3 3

3 3 4 5 3

4 4 4 5 4

z" <2 <2 <2

19

G

<3 <3 <3 <3 <3

<3 c3 <3 <3 <3

<3 <3 <3 <3

4 48 .b3 .042 13 37 .31 285 .08 <3 47 .b2 ,099 22 43 .b4 237 .I0

5 35 .73 .07b 21 45 .b5 433 .lO 3 49 .63 .093 21 43 .68 290 .lO 3 52 .53 .Ob7 21 45 .60 277 .lO

<2 <2 <2 ‘2 <2

<2 <2 <2 q2

<3 31 .27 ,037 17 39 .50 174 .lO <3 30 .22 ,036 14 32 .3b 176 .09 <3 56 .27 .033 17 43 .37 213 .I1 <3 33 .29 .039 17 38 .44 207 .lO

6 48 .27 ,059 lb 34 .40 210 .09

c3 1.54 .02 .05 ~3 1.26 .03 .08 <3 1.56 .03 .Ob

3 1.24 .03 .Ob <3 1.54 .03 .05

<3 1.30 .Ol .05 c3 1.38 .01 .03 ~3 1.69 .02 .05 ~3 1.69 .Ol .04 c3 1.44 .01 .05

46 .2b .049 lb 33 .42 173 .OP ~3 1.36 .01 .04 30 .2b ,057 20 42 .52 176 .,O ~3 1.37 .Ol .Ob 33 .22 .071 17 40 .42 127 .OP <3 1.31 .Ol .Ob 53 .23 ,043 18 41 .32 167 .11 ~3 1.60 .Ol .Ob 30 .27 .038 19 33 .42 216 .OP <3 1.49 .Ol .04

3 43 c.3 4 35 c.3 3 40 c.3 9 41 c.3 7 56 c.3

7 60 c.3 9 79 c.3 6 69 ‘.3 5 69 c.3 4 41 c.3

<3

<3 <3

49 .31 .Ob9 17 40 .31 139 .lO 33 .33 .049 14 25 .33 198 .09 52 .23 .042 20 37 .42 159 .09 57 .29 ,080 17 42 .30 185 .lO 51 .45 ,052 2, 40 .52 275 .o9

<I <l <l <l

1

3 4

1 5 1

Cl 3

Cl Cl 4

<I ‘1

: 1

3 <1

2 3

32 .3 43 .3 74 .8

159 1.3 114 .b

<3 <3 <3

<3 <3

<3 <3

3 7

<3

<3 <3 c3

3 4

3 <3 c3 <3 <3

<3 <3 <3 <3 <3

67 .30 .088 57 .18 ,101 48 .39 .058 51 .29 .076 49 .28 ,030

14 44 .35 212 .09 13 38 .28 159 .08 18 38 .45 241 .09 16 36 .46 135 .09 14 34 .46 178 .lO

4 1.47 .02 .05 <3 1.20 .Ol .05 <3 1.54 .02 .06 <3 1.73 .ll2 .07 <3 1.33 .02 .05

c3 1.79 .Ol .03 c3 1.74 .Ol .04 <3 1.56 .02 .OS <3 1.57 .Ol .05 <3 1.41 .Ol .05

<3 <3 c3

13

33 .b4 ,062 23 43 .68 337 .08 47 .89 ,081 22 38 .60 439 .05 43 2.16 .095 17 33 .46 847 .05 21 4.79 .125 11 18 .35 1029 .02 28 3.24 .099 11 24 .46 369 .04

<3 1.74 .oz .oa ~3 1.76 .02 .07

4 1.48 .Ol .03 6 1.08 .03 .03

<3 .95 .02 .04

c2

<2 <2 <2 <2 c2

<2 <2 <2 <2 <2

‘2 <2 <2 ‘2 <2

<2 <2 <2 <2 <2

<2 <2 <2 <2 <2

23 62 37 163 5.8 34 12 767 3.63 3, 21 <2 32 23.7 25 82 .63 ,092 19 170 .67 156 .ll 19 2.07 ,115 .18 19 44

AlUN 130E

M3N 2OOE eA3" 230E M3N 300E AA3N 330E AA3N CODE

AA3N 430E bA3N 500E Lb2.N 550E AluN b00E .U3N b30E

AA3N 700E kA3N 730E AA3N 800E W.3N 830E kA3N 900E

M3N 950E M3N 1OOOE AA3N 1050E AA3N 1lOOE AA3N 1130E

L43N 12OOE AA3H 1230E AA3N 1300E MN 1430E AMN 1300E

AGN 1330E AA3N 160OE AA3N 1630E A/UN 1700E MN 1750E

STANDARD C3/AU-S

Tizard Explorations Inc. PROJECT KETCHIKA FILE # 97-3740 Page 7 rnuIII,IN i

MO C" Pb 2n AS Ni Co Mn Fe As " Au Th Sr Cd Sb 8i wwFwwPmPp"P Fv ~FmWxnPwmFmFPFw ppn

1 1

<I 1 1

1 <I <I <I

1

1 1

<I 1 1

Cl <I

1 <I <I

1 1

<I 1

<I

1 <I

1 <I Cl

<I Cl <I <I <I

11 4 14 ‘.3 4 11 7 40 c.3 30

7 8 45 c.3 23 8 7 44 c.3 18 b 10 65 c.3 23

2 li71 .29 ~2 11 650 2.46 10

8 187 2.45 2 5 144 1.79 2

10 218 2.68 4

C8 <8 <8 C8 <8

<2 <2 c2 <2 ‘2

c2 247 .5 4 46 .3 5 24 c.2 4 18 c.2 5 17 .2

8 13 67 c.3 22 9 220 2.74 ~2 <a 8 9 46 c.3 25 8 186 2.44 4 <8 a 6 45 c.3 22 8 169 2.51 6 <a 8 7 46 c.3 23 8 199 2.55 <8

10 10 43 c.3 26 10 239 2.70 : <8

5 17 .2 4 19 c.2 4 19 .3 5 17 .3 5 17 .2

11 b 5 9

11

6 b

10 14 15

4 6 9 7

10

7 7

17 13

9

8 7

10 12 13

6 44 c.3 b 57 c.3

10 88 c.3

24 24 15

3 34 c.3 7 48 ‘.3

15 27

3 32 c.3 7 57 c.3

12 65 c.3 7 39 c.3

9 227 2.35 3 9 235 2.44 4 6 200 1.94 2 6 161 1.51 ~2 8 325 2.14 2

-c8 <8 <8 <8

8

6 40 c.3 <3 15 c.3

3 12 .3 7 35 c.3

6 213 2.13 4 10 261 2.48 ~2 12 259 2.82 9

9 286 2.27 5 11 399 2.80 5

5 144 1.63 3 3 12244 .28 ~2 2 436 .I9 c2 7 222 2.35 ~2 7 165 1.87 4

6 18 c.2

: 26 17 .4 .4 3 17 .3 2 31 .4

10 45 c.3

20 21 31 33 32

4 26 .3 4 27 .3 5 17 c.2 6 28 c.2 6 33 .4

7 33 c.3

14 4 5

24 22

<8 <a C8 <8 <8

3 19 .5

7 179 2.36 ~2 8 163 2.21 3

11 259 2.81 6 11 337 2.74 4

8 216 2.61 6

c2 <2 <2 <2 <2

<2 <2 <2 <2 <2

<2 <2 ‘2 <2 <2

<2 s2 x2 <2 <2

c2 <2 c2 <2 <2

<2 ‘2 <2 <2 <2

.; 14; :i <2 307 .7

5 26 .3 5 18 c.2

10 40 q.3 22 9 38 c.3 19 9 45 c.3 35 7 39 c.3 35 9 48 c.3 27

<8 <8 C8 <8 <8

6 16 <.2 5 17 c.2 6 41 .3 7 32 c.2 6 27 c.2

10 54 c.3 27 8 60 c.3 30 9 50 c.3 31

<3 15 c.3 17 5 29 c.3 24

9 219 2.61 4 9 266 2.40 4

12 595 2.42 4 4 229 .89 <2 6 508 1.65 <2

C8 <8 <8 <8 <8

5 21 c.2 6 21 .3 6 34 c.2

<2 222 .5 <2 141 .5

4 <3 <3 c3 <3

<3 4 <3 <3 c3

<3 <3 <3 c3 <3

<3 <3 <3 <3 <3

<3 <3 <3 <3 <3

<3 <3 c3 c3 <3

c3 <3 <3 <3 <3

<3 q3 <3

4 <3

<3 <3 <3 <3 <3

x3 <3 <3 <3 <3

5

i <3 c3

<3 <3 c3 <3 <3

<3 <3 <3 <3

4

<3 <3

4 4

<3

8 5.64 .089

” ca P La cr !4g *a Ti 8 AL Ila K u A"' i w x ~ppnppn XFP xppn 7. x %ppnppb ~

2 3 .39 731 .Ol 17 .25 .Ol .03 <I 19 36 .62 499 .00 ~3 1.24 .03 .05 1 16 39 .52 235 .ll <I 16 30 .40 242 .09 1 lb 39 .47 194 .I1

44 1.11 .077 50 .38 .024 44 .28 .022 59 .27 .062

<3 1.48 .02 .05 ~3 1.32 .02 .05 <3 1.58 .02 .Ob

59 .28 .061 52 .31 .047 52 .28 .054 53 .2b .042 56 .26 .041

16 17 15 16 17

3 1.62 .02 .06 <3 1.50 .02 .05 <3 1.60 .Ol .06 ~3 1.62 .Ol .05 <3 I.66 .Ol .05

47 .3l .056 49 .2b .039 41 .49 ,034 39 .29 .048 47 .b5 ,050

43 .53 .042 50 .48 .035 57 .30 .085 41 .53 .O?b 52 .b4 .069

47 .37 ,039 3 6.67 ,091 8 6.66 .I17

46 .47 ,056 39 .29 ,061

54 .22 .034 53 .23 .018 53 .92 .078 50 .bO .085 51 .4b .047

19 16 14 17 17

39 .48 208 .ll 39 .57 187 .12 39 .51 177 .lO 41 .52 187 .I0 42 .57 230 .ll

38 .52 243 .lO 38 .51 195 .,I 34 .4b 314 .OP 25 .37 208 .07 35 .48 469 .07

3 1.40 .02 .05

33 .38 311 .07 38 .54 332 .I0 36 .48 218 .08 37 .67 256 .09 42 .62 484 .I0

3 1.47 .02 .Ob 3 1.28 .02 .06

~3 1.06 .Ol .06 3 1.55 .02 .05

18 lb 16 21 23

4 1.21 .Ol .05 <3 1.59 .03 .05

6 1.52 .02 .07 <3 1.10 .03 .07

5 1.43 .03 .06

11 1 1

18 18

27 .23 230 .06 3 .41 1840 c.01 2 .43 449 c.01

38 .5b 246 .I0 33 .48 170 .09

38 .45 163 .I0 35 .42 202 .lO 42 .80 434 .09 43 .68 349 .lO 42 .55 308 .lO

4 1.17 .Ol .05 20 .20 .02 .Ob 21 .I5 .02 .03 <3 1.40 .02 .05 <3 1.27 .Ol .04

20 18 23 25 20

6 1.60 .Ol .04 <3 1.55 .02 .03

3 1.49 .03 .06 7 1.45 .03 .05 5 1.58 .03 .05

51 .33 .040 47 .3b .060 46 .53 .066 16 4.02 .082 30 3.13 .074

18 40 .55 270 .I0 19 39 .57 269 .lO 21 39 .51 332 .09

7 14 .44 629 .02 12 22 .60 417 .05

<3 1.54 .02 .05 <3 1.49 .02 .06

3 1.40 .02 .Ob 9 .59 .02 .03 9 .81 .04 .06

‘2 <2 <2 <2 <2

‘2 <2 c2 <2 ‘2

<2 <2 <2 <2 <2

<2 <2 <2 <2 <2

c2 <2 <2 ‘2 <2

<2 <2 <2 c2 <2

<2 <2 <2 <2 c2

Kzw 1800E ,A3N 1850E LA3W 1900E WW 1950E V\3N ZOOOE

LE AA3Y ZOOOE WN 2050E LA3N ZIOOE LA3N 2150E tA3N 22OOE

U3N 2250E @.3N 23OOE VUN 2350E LA3N 2400E @.3N 2450E

IA3N 2500E WN 2550E kA3N 2600E VUN 2650E bA3N 2700E

@.3N 275OE @.3N 2800E MN 2850E ti3N 29OOE IA3N 2950E

IA3N 3000E tiN 3050E A3N 3100E d3N 3150E IA3N 3200E

A3N 3250E A3N 3300E A3N 3350E A3N 3400E ilUN 3450E

;TANDARD C3/AU-S 25 64 40 lb5 5.8 38 ii 772 3.66 60 - - 21 c2 19 32 23.4 lb 22 82 .b2 ,094 19 172 .68 159 .lO 24 2.02 .04 .I7 18 46

Sample type: SOIL. Samles beqinnins 'RE' are Reruns and 'RRE' are Reject Reruns.

All results are considered the confidential property of the client. Acme assms the Liabilities for actual cost of the analysis only. Data- FA _

Tizard Explorations Inc. PROJEC KETCHIKA FILE # 97-3740 f Page 8 m!l uumii mf lluLlT,w

SAMPLE# no C" Pb 2n Ag Ni co nn Fe x & $ 2 $ ,; $ g &i ,; Ca P La CT Mg 88 Ti B AL *a Y v ALP FwwPPPFP!mppnwpnppn % xppnw %fw ZPpn x x x ppn Ppb

AA3N 3500E ~1 11 ~3 2 .3 16 2 375 .21 c2 e c2 <2 375 .9 s3 6 9 7.18 .065 2 3 .53 362 s.01 17 .la .03 .02 <2 1 AluN 3550E <l 9 c3 2 c.3 15 3 543 .63 ~2 4 <2 ~2 435 .6 ~3 6 9 6.74 .Oa2 1 3 .59 684 <.Ol 22 .17 .03 .02 <2 1 AA3N 3600E <l 12 7 39 .3 28 10 367 2.25 3 4 ~2 5 76 .3 ~3 c3 39 1.63 .Oa5 19 32 .77 412 .07 9 1.06 .02 .07 ~2 1 .WN 3650E <l 19 <3 6 c.3 22 5 1212 .6a <2 <a c2 <2 319 .5 c3 5 10 5.80 .oa2 5 9 .59 1360 .Ol 12 .54 .Ol .02 <2 1 AA3N 3700E <l 19 3 18 .3 25 7 ,883 1.61 3 <a ~2 ~2 265 .7 <3 4 20 5.83 .lOl 7 16 .55 1360 .02 12 .61 .02 .04 ~2 ~1

Au" 375OE ~1 16 ~3 23 c.3 11 3 1329 .32 ~2 4 ~2 ~2 251 .8 ~3 5 8 6.55 ,108 2 5 .35 1236 .Ol 11 .40 .02 .02 <2 <l AA3N 3aOOE 4 17 3 40 c.3 30 7 286 1.69 4 4 ~2 5 176 .4 <3 3 31 7.44 .092 14 27 .&5 320 .06 5 .80 AA3N 3850E 1 15 3 37 .3 29

.02 .09 c2 2 7 297 2.03 5 8 ~2 4 88 .5 s3 <3 35 2.07 .096 17 32 .57 471 .06 3 .99 .02 .05 2 2

kA3N 3900E -cl 11 5 45 c.3 29 10 346 2.34 4 ~0 ~2 5 57 .2 <3 ~3 41 1.26 .Oa2 20 35 .65 435 .07 3 1.20 .02 .05 <2 1 AAX" 3950E Cl 13 6 46 c.3 27 8 841 1.83 3 -3 <2 4 137 .5 c3 5 34 4.21 .086 14 27 .93 464 .05 6 .&5 .03 .08 ~2 ~1

M.3" 4000E <I 12 3 43 c.3 26 11 814 2.57 4 4 ~2 3 206 .3 ~3 <3 28 4.72 .099 11 23 .R 655 .04 10 .02 .02 .07 <2 1 RE .U3N 4000E <I 13 5 43 c.3 22 10 a32 2.62 4 4 ~2 2 210 .6 ~3 ~3 AA3N 4050E

28 4.79 ,101 11 24 .72 659 .04 9 .@4 .Ol .07 c2 <l 1 10 4 36 c.3 25 12 374 2.04 2 9 c2 2 141 c.2 <3 <3 37 2.94 .I04 15 23 .67 436 .04 7 .07 .03 .04 <2 1

kA3N 4100E 4 17 3 12 c.3 19 5 1454 .82 <2 a c2 ‘2 380 .6 ~3 6 13 6.64 .Oa7 5 11 .54 1641 .Ol 8 .49 .02 .03 <2 4 MN 4150E ~1 10 7 48 c.3 27 7 277 2.10 4 4 ~2 6 28 .2 ~3 ~3 37 .47 .083 20 34 .57 la4 .07 s3 1.12 .O, .06 ~2 1

M3N 4200E ,ci 5 6 42 <.3 17 5 158 1.75 2 ~8 ~2 6 17 .2 ~3 ~3 36 .30 .062 18 31 .45 158 .08 <3 1.11 .Ol .o4 <2 1 AA3N 4250E ~ 1 11 8 41 c.3 25 8 216 2.24 4 4 ~2 8 19 .4 c3 c3 42 .29 .048 24 AA311 4300E 19

38 .46 204 .OP <3 1.24 .01 .05 ~2 4 5 37 c.3 30 9 229 2.54 4 ~8 ‘2 8 15 .3 ~3 c3 46 .23 .039

Aa3N OE 22 41 .50 201 .OP 3 1.48 .Ol .06 ~2 1

1 10 a 30 c.3 27 7 188 2.05 ‘2 4 ~2 6 18 <.2 <3 c3 43 .31 .03a AB3N 50E

19 40 .43 221 .OP 4 1.17 .02 .05 <2 5 1 11 8 37 c.3 23 6 159 1.91 2 4 ~2 6 14 c.2 <3 <3 45 .20 .032 16 34 .44 186 .oa <3 1.35 .Ol .04 <2 1

AB3N lOOE 1 6 4 48 c.3 21 7 265 1.86 ~2 ~8 ~2 3 15 <.2 s3 3 44 .22 ,037 17 32 .40 193 .09 <3 1.31 .oi .04 c2 I AB3N 150E ~1 6 6 45 c.3 23 8 217 2.07 ‘2 4 ‘2 5 14 c.2 <3 <3 48 .19 ,031 17 35 .43 199 .09 <3 1.45 .02 .03 c2 Cl AB3N 2OOE 17 3 29 c.3 ~18 5 169 1.43 3 <8 ~2 5 15 c.2 s3 <3 37 .31 .027 18 24 .25 170 .06 3 .a0 .01 .05 <2 <l AB3N 250E 15 4 38 c.3 16 7 145 1.91 <2 <a s2 5 15 c.2 <3 <3 50 .22 .033 AB3N 300E 1 5

17 3, .32 209 .08 <3 1.27 .Ol .OL ~2 1 8 62 c.3 20 9 140 2.57 <2 4 ~2 5 15 c.2 <3 3 59 .20 .152 16 35 .40 301 .oa *3 1.59 .Ol .05 <2 <l

AB3N 350E C! 8 7 46 c.3 27 10 155 2.63 4 <8 ~2 7 13 .3 <3 <3 56 .,5 .064 17 AB3N 400E 19

43 .47 209 .08 6 1.87 .02 .04 ~2 2 8 34 c.3 23 8 118 2.03 4 ~8 ~2 6 11 .2 <3 <3 46 .I3 .031 17 37 .37 163 .07 <3 1.41 .01 .04 2 4

Aa3N 450E 2 9 13 6i c.3 29 9 181 3.29 2 ~8 ~2 4 14 .3 <3 c3 72 .25 ,080 14 40 .45 305 .09 4 2.06 .Ol .04 ~2 1 AE3N 600E 1 8 <3 30 c.3 13 7 709 1.11 <2 4 <2 c2 71 .5 <3 c3 22 1.89 ,089 a AB3N 650E 1

16 .3, 324 .04 <3 .80 .02 .06 ~2 <1 I, 10 46 c.3 28 8 276 2.65 4 c8 ~2 6 25 c.2 q3 <3 52 .47 ,051 17 44 .63 240 .lO <3 1.64 .02 .06 ~2 3

AB3N 700E 2 2 c3 25 c.3 2 3 ,984 .71 <2 4 c2 c2 133 .2 c3 <3 43.88.099 1 5 .35 550 .Ol AB3N 750E 2 2 s3

10 .I4 .03 .07 <2 4 30 ‘.3 Cl ~1 489 .I6 ~2 ~8 ~2 ~2 a5 c.2 <3 <3 2 2.41 .092 ~1 3 .26 273 c.01

AB3N BOOE 2 4 <3 8 .05 .03 .,l c2 2

17 c.3 1 4 2130 1.35 4 <B ~2 ‘2 176 .2 ~3 c3 3 5.06 ,089 ~1 2 .27 ,129 ‘.Ol 8 .I0 .02 .03 <2 1 AB3N 850E ~1 9 6 34 c.3 16 6 290 1.56 2 4 ‘2 3 49 .4 ~3 c3 35 1.28 .037 12 AB3N 900E

24 .46 360 .06 ~3 .92 .02 .04 ~2 cl 1 9 s3 19 c.3 12 4 225 .98 3 <a ~2 ~2 59 .2 ~3 <3 23 1.83 .057 9 15 .26 35, .04 ~3 .58 .02 .04 ~2 2

STANDARD C3/AU-5 25 63 32 164 5.8 36 11 765 3.64 58 31 3 22 30 24.4 12 22 80 .61 ,092 20 179 .67 163 .lO 25 1.99 .04 .18 16 46

SamLe type: SOIL. Samples beginning 'RE' are Reruns and 'RRE' are Reject Reruns.

ALI results are considered the confidential property of the client. Acme assms the liabilities for actual cost of the analysis only. oata- FA _

i

AB3N 950E AB3W 1OOOE AB3W 1050E AB3W 1lOOE AE3N 1150E

AB3N 12OOE AB3R 1250E AB3N 1300E AB3M 1350E AE3N 1400E

AE3N 1450E AB3N 1500E AE3N 1550E AB3N 1bOOE AE3N lb50E

AE3N 1700E AE3N 1750E AB3N 1800E RE AB3N 1800E AB3N 1850E

AB3N 1900E AE3N 1950E AB3W ZOOOE STANDARD C3/AU-S -

Tizard Explorations Inc. PROJECT KETCHIKA FILE # 97-3740 Page 9

no C" Pb 2n Ag Ni co nn Fe Ti B Al "a K U A"* ppnWppnWFFPpmWpnppn

x & 2 & $ & $ $ & ,; Ca P La Cr Mg Ba x IPPnppn %m %ppn x x xppnppb

14 4 26 c.3 22 7 791 2.03 <2 3 82 c.2 <3 <3 36 3.65 .043 12 27 .5E 603 .06 <3 1.16 .03 .04 4 4 24 c.3 10 3 05 1.14 c2 2 13 .3 <3 3 33 .28 .017 8 15 .20 116 .06 G .70 .Ol .02 4 4 65 c.3 13 7 390 1.60 <2 2 20 .4 <3 <3 38 .38 ,050 11 24 .26 204 .07 ~3 .98 .Ol .05 7 5 29 c.3 lb 5 104 1.24 <2 4 ,I .3 <3 <3 28 .19 .027 13 21 .33 123 .05 <3 .89 .Ol .03

10 5 79 c.3 32 14 282 3.39 <2 4 17 c.2 <3 <3 64 .22 .042 I2 48 .43 264 .12 *3 2.31 .02 .07

lb x3 18 c.3 11 3 341 .bb <2 <2 158 .8 <3 6 14 4.46 .108 6 8 .34 764 .Ol 7 .47 .Ol .03 1 <3 23 c.3 1 ~1 1274 .50 <2 ‘2 166 .3 <3 4 3 4.49 .116 Cl 2 .31 639 c.01 22 .05 .02 .04

13 8 44 c.3 20 6 270 1.b4 c2 2 21 .b ~3 4 45 .47 .024 12 22 .26 281 .06 4 .9b .Ol .lO 4 7 53 c.3 17 7 396 2.10 ‘2 3 18 .5 <3 4 51 .30 .034 12 29 .35 224 .10 ~3 1.24 .Ol .07 8 7 45 c.3 24 6 224 2.27 <2 4 ,* .3 <3 -c3 50 .32 .032 14 35 .51 211 .lO <3 ,.34 .01 .07

7 8 34 c.3 lb 6 ,45 1.76 <2 4 lb c.2 ~3 <3 41 .29 .032 13 28 .40 168 .07 c3 1.10 .Ol .05 10 9 47 c.3 26 9 206 2.34 <2 3 17 .2 <3 <3 45 .30 .052 14 36 .53 172 .09 <3 1.39 .O, .06

7 a 51 c.3 24 7 197 2.48 c2 4 16 .3 <3 <3 51 .26 ,032 13 37 .48 168 .ll <3 1.38 .o, .OB 7 8 54 c.3 14 6 177 2.09 <2 3 16 .5 ~3 <3 50 .27 .027 12 27 .37 149 .10 <3 .99 .Ol .07 8 8 52 c.3 24 8 208 2.55 ‘2 4 13 .b ~3 <3 50 .22 .047 14 36 .47 149 .09 ~3 1.52 .02 .07

7 a 40 c.3 24 8 198 2.39 ‘2 4 18 .5 <3 <3 48 .33 .069 14 39 .56 149 .lO <3 1.35 .02 .08 5 7 40 c.3 12 5 145 1.68 <2 3 lb .2 4 3 40 .29 .047 13 28 .43 142 .09 x3 1.14 .01 .05 7 5 35 c.3 20 6 lb, 2.04 <2 5 20 .2 <3 <3 43 .39 .046 15 36 .48 182 .lO <3 1.20 .02 .05 7 8 35 x.3 20 7 160 2.03 ‘2 4 20 .2 *3 <3 43 .38 .044 15 35 .48 166 .lO <3 1.18 .Ol .05 6 12 &c <.3 lb B 206 2.69 ‘2 4 15 .4 c3 4 57 .24 ,127 16 35 .39 222 .OP c3 1.43 .o, .05

4 6 94 q.3 19 9 553 2.34 ‘2 2 19 .b q3 <3 49 .35 .107 12 32 .40 281 .09 c3 1.38 .02 .07 5 7 101 c.3 18 6 396 1.67 2 4 c2 2 15 .b ~3 <3 39 .26 .08b 13 25 .31 281 .Ob -z3 1.06 .Ol .Ob <2 Cl

6: b 53 c.3 18 5 134 1.71 c2 -3 2 12 .2 <3 6 41 .20 .074 11 27 .29 117 .07 ~3 .96 .01 .05 <2 2

25 38 lb2 5.7 34 12 746 3.62 56 22 18 30 24.5 lb 22 80 .60 .093 18 165 .67 159 .ll 16 1.99 .05 .17 19 45

<2 Cl c2 4 <2 1 -c2 1 <2 <l

-c2 <l <2 <I <2 1 ‘2 I c2 <1

*2 <I c2 Cl <2 2 ‘2 2 <2 1

<2 Cl ‘2 e <2 1 <2 2 c2 1

c2 Cl

‘2 <2

ICAL LABORATORIES LTD. 85XR. BASTINGS ST. V COWER BC V6A ~lR6

A?

PHONR(604)253-3158

GEOCHEMICAL EXTRACT1 ANALYSIS CERTIFICATE Tizard Bmlorations Inc. PROJECT KETkHIKA :Eile~,# 97~-~3778 Page ,1

1022 - 470 Orwwilte St., Vancower BC V6C 1V5 Suhitted by: Seems Ymg

SAMPLEIl

ABIN OE ABIN 50E ABIN IOOE ABIN 15OE ABlN 2OOE

ABIN 250E ABIN 300E ABIN 350E ABIN LOOE ABIN 450E

.4 5.1 6.7 31.9 80 13 5

.4 4.0 6.3 31.6 67 13 6

.7 6.2 5.7 20.0 127 16 5

.5 4.2 7.3 29.7 42 9 5

.6 8.6 7.7 61.4 76 27 11

.B 5.7 7.3 53.3 68 16 6 1.0 8.3 7.2 58.1 54 15 8

.5 7.7 7.5 44.4 120 24 7

.6 8.9 8.2 55.5 84 22 9 1.3 12.7 9.3 69.2 86 27 8

130 1.88 2.4 ~5 2 ,I .08 .2 .l 45 .I4 .059 11 26 .30 140 .08 120 1.46 1.3 <5 1 16 .I0 .2 .I 45 .28 .032 11 21 .25 214 .06 141 1.18 2.6 *5 1 10 .I0 .5 i.l 30 .20 .066 10 18 .22 148 .04

99 1.05 1.3 <5 Cl 7 .ll .3 c.1 26 .I3 .I12 ,I 15 .I4 74 .03 142 2.36 3.3 ~5 2 11 .20 .4 .I 49 .I6 .I32 15 32 .43 175 .06

.39

<3 1.23 .Ol .03 c3 .94 .Ol .04 <3 .66 .Ol .03 <3 .59‘.01 .03

4 1.61 .Ol .04

128 .I0 <3 1.33 .Ol .04 255 .06 <3 .94 .Ol .04 180 .08 <3 1.30 .Ol .05 208 .OP 4 1.59 .Ol .05 195 .09 <3 1.55 .Ol .06

136 .04 205 .09

<3 .61<.01 .03 3 1.68 .Ol .04 3 1.70 .Ol .OL

<2 <.2 40 <.3 c.2 5.1 ~2 c.2 16 s.3 c.2 4.2 ~2 s.2 13 c.3 .2 2.4 <2 c.2 15 c.3 c.2 3.4 <2 <.2 24 <.3 s.2 5.1

~2 <.2 40 c.3 c.2 5.6 ~2 <.2 26 c.3 c.2 4.5 <2 <.2 23 <.3 c.2 4.6 ~2 c.2 25 s.3 c.2 5.5 <2 <.2 21 c.3 c.2 6.0

150 2.52 1.7 ~5 1 13 .21 .4 .2 61 .21 .030 13 33 212 1.73 2.1 <5 1 17 .65 .3 .I 41 .27 .055 12 23 159 1.84 1.8 <5 1 16 .I0 .3 .l 40 .28 .065 14 31 166 2.53 3.0 7 2 13 .13 .4 .I 56 .20 .046 14 37 240 2.57 3.0 <5 2 16 .I8 .5 .3 55 .25 ,058 13 36

75 .a2 1.2 -z5 1 11 .Ob .2 .I 23 .20 ,020 8 15 191 3.10 3.1 <5 1 12 .32 .5 .I 67 .I9 .I30 13 34 201 2.46 1.5 ~5 1 15 .15 .3 <.I 54 .22 .080 13 36 212 2.43 2.1 6 1 16 .I8 .3 .l 53 .25 .069 12 34 49, 1.93 1.4 <5 1 17 .25 .2 <.I 42 .27 .074 10 30

.29

.49

.47

.50

.20

.35 .40 .44 .34

<2 <.2 12 c.3 c.2 2.2 <2 *.2 29 c.3 s.2 8.0 ~2 c.2 25 c.3 q.2 6.5 ~2 .2 26 c.3 c.2 5.9 ‘2 c.2 15 c.3 c.2 4.8

4 1

ABIN 500E ABIN 550E ABIN 6OOE ABIN 650E

.4 5.4 3.9 19.7 46 14 4 1.1 9.2 11.6 76.0 95 23 8

.8 7.2 8.6 64.2 81 25 9 .8 8.0 7.3 66.5 57 27 9 .8 6.8 6.4 63.0 86 21 8

.6 6.9 6.8 61.0 111 18 8

.8 5.7 6.9 51.6 ~30 13 7

.8 4.5 4.6 35.6 32 12 4

.8 18.7 9.8 54.7 171 32 7

.8 a.1 6.4 37.5 97 14 5

193 .09 224 .OP 319 .08

331 .08 251 .05

1 <I <I

~3 1.56 .Ol .06 <3 1.25 .Ol .07 ABIN 700E

496 1.95 1.4 q5 1 16 .28 .2 .I 41 876 1.51 c.5 5 cl 12 .19 .2 c.1 36 102 1.05 1.6 <5 ql 12 .09 .2 <.I 27 388 2.13 3.4 ~5 ~1 37 .25 .5 .2 43 149 1.11 1.3 <5 1 23 .25 .3 .2 29

.25 ,074 9 28 .33 10 22 .26 11 16 .23 18 35 .59 11 25 .28

10 21 11 21 12 30 11 31 12 29

.23

.27

.33

.32

.43

142 .04 365 .08 202 .06

‘3 1.19 .Ol .07 <2 c.2 13 c.3 c.2 4.7 <3 1.04 .Ol .05 ~2 c.2 12 <.3 c.2 4.6 <3 .69 .Ol .04 <2 c.2 12 c.3 q.2 2.7 <3 1.20 .02 .05 <2 q.2 40 .4 c.2 4.3

3 .74 .Ol .04 <2 c.2 10 c.3 c.2 3.0

133 .06 ‘3 .lm.Ol .03 108 .06 3 .90 .01 .03

‘2 .2 12 c.3 c.2 3.4 <2 c.2 13 c.3 <.2 3.7 ‘2 <.2 14 s.3 c.2 5.8 <2 .2 22 <.3 c.2 5.1 <2 .2 Cl0 c.3 c.2 5.3

‘2 c.2 13 c.3 c.2 4.4 <2 .2 18 c.3 q.2 6.3

5 <I

1 3

RE ABlN 700E ABIN EOE ABIN 800E ABIN 850E

.21 .043

.22 ,025

.89 ,084

.4a ,037 77

4 1

<l Cl *i

ABIN 900E

ABlN 950E ABlN lODOE ABIN 1050E ABlN 1lOOE ABIN 1150E

80 1.46 2.0 ~5 1 11 .06 .3 .I 37 86 1.54 1.5 ~5 i 13 .14 .3 .I 41

146 2.10 1.9 7 2 14 .08 .2 .I 50 236 2.38 2.3 ~5 1 18 .37 .3 .2 51 170 1.99 1.3 6 2 19 .34 .2 .I 41

.16 ,017 .9 5.5 4.9 23.4 ~30 15 4 .9 6.8 5.4 37.3 ~30 11 4 .5 5.9 7.3 38.0 ~30 15 6 .7 9.5 8.5 43.7 <30 28 11 .7 6.2 8.7 84.5 ~30 18 6

.I8 .080

.20 ,086

.32 .0&c

.34 ,037

137 .o* <3 1.34 .Ol .03 283 .Ob ~3 1.43 .Ol .04 236 .lO 3 I.28 .Ol .04

270 .09 ~3 1.25 .01 .05 394 .08 <3 1.16 .Ol .03 276 .07 <3 1.15~.01 .03 654 .04 4 .86 .Ol .02 646 .04 3 .75<.01 .03

<l 1

ABIN i2OOE AEIN 1250E ABlN 1300E ABIN 1350E ABIN 1400E

.7 7.3 7.3 132.4 <30 20 9 1.3 8.9 10.2 43.8 ~30 17 6

.6 8.5 7.2 39.5 q30 19 7 1.3 13.1 7.9 29.0 98 17 7 1.2 0.0 7.6 45.7 65 10 5

676 2.03 .9 <5 <I 22 .77 .2 .I 40 178 2.11 2.7 ~5 1 31 .27 .4 .2 51 324 1.90 2.1 6 1 22 .23 .4 c.1 46 552 1.29 1.5 ~5 ~1 66 .34 .3 .l 29

-40 .071 12 30 .67 ,036 .44 ,039

I.84 .049

.4l 13 26 11 33

9 22 a 18 352 1.43 1.9 <5 cl 67 .35 .2 .I 32 1.56 ,028

<2 c.2 14 c.3 c.2 4.0 <I ~2 c.2 32 .7 c.2 3.2 <l ~2 c.2 25 .B c.2 3.2 Cl

4.7 9.8 1.7 48.5 39 9 7 10861 2.74 2.6 <5 <, 165 .58 c.2 c.1 3 5.61 ,106 1 2 .32 1953<.01 11 .lO .Ol .03 ~2 q.2 28 1.1 q.2 1.0 <l .6 16.4 1.5 27.1 95 14 2 307 .21 .7 <5 1 172 .69 .9 .I 4 12.41 .063 1 7 .31 1035<.01 12 .ll<.Ol .02 <2 q.2 37 3.1 <.2 .B <I .8 8.3 7.9 47.2 40 21 7 216 1.98 3.0 5 2 16 .13 .3 .I 44 .40 ,032 12 31 .43 193 .08 ~3 1.33 .Ol .04 ~2 c.2 14 .3 q.2 4.9 4 .5 9.8 7.4 54.0 50 28 9 409 2.3, 3.2 4 1 26 .I3 .3 .2 44 .52 ,065 16 36 .55 286 .09 3 1.28 .02 .04 <2 c.2 21 .3 <.2 4.3 1 .8 12.1 7.7 46.0 110 26 8 303 2.24 2.5 ~5 <, 39 .17 .2 .2 42 .88 .088 15 38 .56 511 .07 ~3 1.46 .Ol .06 ~2 c.2 30 .5 c.2 4.2 1

ABIN 1450E ABIN 1500E ABIN 1550E ABIN 1600E ABIN 1650E

STANOARO 021 i23.4 117.9 97.7 257.5 1914 30 16 985 4.47 75.1 21 15 60 2.02 0.7 21.8 70 .69 ,108 17 55 1.18 266 .I4 25 2.24 .06 .69 17 2.2 453 1.0 2.1 7.2 51

Standard is STANDARD OZ/HG-SOOIAU-2. ICP 15 GRAM SAMPLE IS DIGESTED UliH 90 ML 3-l-2 "CL-HN03-H20 AT 95 DEG. C FOR ONE "@JR AN0 IS OlLUTEO TO 300 ML WTH WATER. THIS LEACH IS PARTIAL FOR MN FE SR CA P LA CR MC BA T, B W AND LlMlTEO FOR NA K GA AND AL. SOL",,ON ANALYSEO DIRECTLY B" ICP. MO CU PB 2N AS AS A" CO 58 BI TL HO SE TE AN0 GA ARE EXTRACTED U,TH MIBK-ALIPUAT 336 AN0 ANALYSEO BY ICP. ELEVATED OETECTlON LlMlTS FOR SAMPLES CONTAIN CU,PB,ZN,AS>lSOO PPM,F-20%.

SAMPLE TYPE: Pl TO PI8 SOlL PI9 TO P23 LAKE SEO. Samples besinnins 'RE' are Reruns and 'RRE' are Reiecf Reruns.

DATR RECEIVED: JUL 23 1997 DATE REPORT MAILED: ALL results we considered the confidential property of the client. A

..O.TOYE, C.LEONO, J.VANG; CERTIFIED B.C. ASSAYERS

of the analysis only. Data- FA _

c Tizard Explorations Inc. PROJECT KETCHIKA FILE # 97-3778 Page 2 '#

ABIM 1700E ABIN 175OE ABlll 1800E ABlN 1850E ABIN 19OOE

ABlY 1950E ABlW 2OOOE ABIW 2050E ABlY 2100E ABIM 2150E

ABlW 22OOE ABlN 2250E RE ABIN 2250E ABIN 2300E ABlN 2350E

ABIN 2400E ABlN 2450E ABIN 2500E AElN 2550E ABIN 2600E

AB~N 2650E ABlW 2700E ABIN 2750E ABIN 2800E ABlH 2850E

.0 12.5 8.5 44.4 50 29 1.3 18.9 9.6 57.4 131 36

IO 548 2.60 3.8 ~5 2 36 II 391 2.67 3.9 7 2 46

7 165 2.14 1.3 ~5 2 17 B 231 2.39 3.1 5 3 15 7 207 1.76 2.1 4 1 15

.I3

.35 .3 .2 47 .82 ,049 17 38 .56 591 .07 4 1.44 .02 .04 <2 C.2 17 .3 q.2 4.5 4 .3 .3 46 2.12 ,069 17 40 .61 767 .07 4 1.37 .02 .05 <2 C.2 21 .4 C.2 4.3 Sl .2 .l 45 .32 ,021 11 32 .42 240 .OB ~3 1.20 .Ol .06 <2 c.2 16 c.3 c.2 3.0 2 .2 .2 49 .28 ,034 12 36 .52 175 .09 ~3 1.42 .Ol .06 <2 <.2 40 c.3 c.2 5.0 1 .3 .4 40 .27 ,050 ,2 23 .40 151 .06 <3 ,.OL<.Ol .06 ~2 <.2 40 <.3 c.2 4.3 cl

.2 .3 43 .22 .023 ,2 26 .36 186 .07 ~3 1.19c.01 .04 <2 <.2 16 c.3 c.2 5.3 1

.2 .2 42 .I5 ,034 13 24 .27 101 .06 <3 .93 .Ol .04 <2 .2 <IO <.3 c.2 4.5 ~1

.2 .2 57 .I6 .081 13 35 .32 105 .08 3 1.37 .Ol .04 C2 C.2 12 C.3 C.2 7.1 -Cl

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.I6

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ABIN 2900E AEIN 2950E ABlN 3000E ABlN 305OE ABlN 3lOOE

ABlN 3150E ABlN 3200E ABlW 3250E ABlN 3300E ABlN 3400E

.7 21.9 8.3 43.9 162 34 8 231 2.11 4.0 ~5 2 29 .12 1.1 7.1 7.3 37.6 51 16 7 170 2.04 2.1 ~5 2 15 .13 1.0 4.1 6.8 35.2 52 9 b 342 1.45 .a C5 i 15 .17

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1.3 9.9 8.0 42.8 95 20 9 248 2.38 3.6 ~5 2 17 .14 1.0 11.0 7.8 41.7 69 23 8 364 1.72 2.6 ~5 ~1 44 .23

.6 12.5 7.1 47.7 115 24 7 390 1.77 1.8 <5 1 5B .43 1.3 9.4 8.0 54.2 60 26 8 206 2.76 3.5 ~5 2 15 .25 1.2 10.1 5.4 31.6 112 13 4 182 1.13 2.8 <5 2 93 .23

i 4.3 121.4 94.7 259.0 1951 30 16 970 4.51 77.3 28 17 6, 2.05 10.4 21.4 69 .71 ,109 17 54 1.14 254 .I4 29 2.27 .06 .71 18 2.3 454 .7 2.1 6.7 54 STANDARD D2/H

Standard is STANDARD DZ/HG-SOO/AU-S. Samies b-ginning IRE' are Reruns and 'RRE' are Reiecr Reruns.

All results are considered the confidential property of the client. Acme BSSUWS the liabilities for actual cost of the analysis only. Data- FA _ !

Tizard Explorations Inc. FILE # 97-3778 Page 3 .- ."", -,-., I_ “-.,,-

no C” Pb 2n Ag Ni Co IW Fe As " Th ST Cd Sb Bi V Ca P La tr ng Ba Ti B Al NB K U Tk "9 Se Te ta A,,+ am DDnm mn!mbmn!mn am Y. mmuxllDm mm mm x xcmmn xm xmn x % %mnmnwbmnmnDmnmb

ABIN U50E ABlN 3500E ABlN 3550E ABlN 3700E ABI" 3750E

ABlN 3800E ABIN 3850E ABlN 3900E ABlN 3950E ASIN 4000E

ABZN OE ABZN 5OE ABZN 1OOE RE ABZW IOOE ABZN 15OE

ABZW 2OOE ABZN 250E ABZW 300E AEZW 350E ABZN 400E

ABZN 450E ABZN 500E ABZN 550E ABZN 600E ABZN 650E

ABZN 700E ABZN 750E ABZN 800E ABZN 850E ABZN 900E

I,:

AB2N 950E ABZN IOOOE ABZN 1050E ABZN 1lOOE ABZN 1150E

STANDARD D2, z -

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.7 8.0 7.4 58.1 63 21 8 149 2.64 2.8 ‘5 3 12 .16 .3 .I 58 .17 ,060 13 38 .39 157 .09 -C3 1.69 .O, .04 <2 c.2 12 c.3 c.2 5.7 ~1

3.6 118.7 95.5 258.5 1862 27 15 961 4.39 67.3 16 16 60 2.20 8.5 19.6 69 .70 ,106 17 54 1.13 247 .I4 26 2.23 .06 .69 16 2.0 451 .5 1.8 7.1 53

Standard is STANDARD OZIHG-500/AU-S. Samoles beginning 'RE' are Reruns and 'RRE' are Reiecr Reruns.

ALI results are considered the confidential property of the client. Acme assms the liabilities for actual cost of the analysis only. Data- FA _

AEZN 12OOE ABZN 1250E ABZN 13OOE ABZN 1350E ABZN 1400E

ABZN 1450E ABZN 1500E ABZN IWOE ABZW 1650E ABZN 1700E

ABZN 175OE RE ABZW 1750E AEZW 18OOE ABZN 1850E AEZN 1900E

ABZN 1950E ABZN ZOOOE ABZN 2050E ABZN ZIOOE ABZN 2150E

ABZN 22OOE ABZN 2250E ABZN 23OOE ABZN 2350E ABZN 2400E

ABZN 2450E ABZN 2500E ABZN 2550E ABZN 2600E ABZN 2650:

ABZN 2700E ABZN 2750E ABZN 2800E ABZN 2850E AEZN 29OOE

Tizard Explorations Inc. TCHIKA FILE # 9-J-3778 Page 4 '49

1.2 9.5 6.7 37.3 ~30 21 8 151 2.17 1.4 ~5 1.2 11.1 8.0 65.3 76 20 6 239 1.84 1.9 ~5 1.9 5.8 4.8 34.2 36 9 5 2087 5.55 3.6 ~5 I.7 6.0 7.9 40.9 39 I3 5 160 I.64 1.7 ~5 1.3 8.9 10.2 60.7 117 18 7 388 I.95 2.0 ~5

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.8 7.9 8.0 31.7 ~30 17 6 162 I.67 2.9 ~5 2 I4 .09 .2 ., 39 .27 ,028 11 27 .42 180 .07 ~3 1.12 .01 .03 ~2 c.2 10 c.3 q.2 4.0 4

.8 6.9 8.4 61.2 62 17 7 162 2.08 2.0 ~5

.6 6.7 8.1 57.8 63 17 7 161 2.08 2.0 4

.9 9.0 7.4 35.6 30 I7 5 143 1.77 3.4 ~5

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.9 7.4 7.6 69.6 <30 17 7 I80 2.25 1.6 ~5

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.9 9.6 7.6 36.9 <30 2, 8 168 2.10 2.6 ~5

.8 7.0 7.2 52.0 41 I8 9 398 2.58 2.4 ~5

3 22 .06 .2 .2 48 .41 .013 11 36 .52 274 .09 <3 I.47 .01 .05 ~2 c.2 12 c.3 <.2 4.6 <I 2 I3 .06 c.2 ., 47 .21 .019 li 26 .36 154 .08 ~3 1.12 .O, .03 ~2 c.2 10 c.3 c.2 4.4 <1 3 11 .04 .L .I 54 .18 .028 11 34 .47 198 .06 ~3 1.46 .Ol .04 ~2 c.2 11 c.3 c.2 4.0 2 3 I2 .07 .2 .I 46 .20 ,033 13 32 .44 173 .07 <3 1.30 .01 .04 C2 <.2 <,o C.3 C.2 4.7 3 3 15 .09 .2 .2 54 .30 .I26 12 32 .47 194 .07 ~3 I.41 .O, .07 ~2 <.2 40 c.3 c.2 5.0 2

STANDARD 02/H i23.5 117.1 89.6 253.4 1827 31 14 968 4.4, 65.3 I6 I7 60 2.17 9.8 22.4 68 .69 ,105 I7 53 1.15 256 .I4 33 2.27 .06 .70 I6 2.3 464 .6 1.9 6.8 46

Standard is STANDARD 02/K-500/A&S. Samoles beginning 'RE' are Reruns and 'WE' are Reject Reruns.

ALL results are considered the confidential property of the client. Acme assmes the liabilities for actual cost of the analysis only. Data- FA _


ABZN 2950E ABZN 30OOE AEZN 3050E ABZN 3lOOE ABZN 3150E

ABZN 3200E ABZN 3250E ABZN 3300E AB2N 3350E ABZN 3400E

ABZN 3450E ABZN 3500E ABZN 3550E ABZN 3600E AEZN 3650E

ABZN 3700E AB2N 3750E AB2N 3800E ABZN 3850E RE AB2N 3850E

ABZN 3900E ABZN 3950E AB2N 4000E AE3N 2050E AB3N 2lOOE

AB3N 2150E AB3N 2200E AB3N 2250E AB3N 2300E AE3N 2350E

AB3N 2400E AS3N 2450E AB3N 2500E AB3N 2550E AB3N 26OOE

STANDARD 02/H

!

P -

=

I -

.9 8.5 9.9 54.3 57 25 10 203 2.83 4.1 ~5 2 15 .lO .3 .1 58 .24 ,160 11 35 .49 232 .08 c3 1.59 .Ol .04 <2 s.2 11 C.3 C.2 5.3 <l

.9 6.2 8.6 38.6 43 14 6 119 1.64 3.1 ~5 1 11 .12 .3 c.1 41 .17 .054 10 22 .24 138 .06 ~3 .90<.01 .04 -z2 s.2 40 s.3 q.2 3.4 4 1.4 8.6 9.4 44.6 34 19 6 157 2.29 5.1 ~5 2 14 .I4 .4 <.I 55 .23 ,037 13 3, .38 126 .09 <3 1.07 .O, .06 ~2 s.2 <IO q.3 C.2 4.0 ql 1.2 30.4 10.5 45.2 150 27 10 988 1.59 3.4 <5 ~1 60 .58 .4 <.I 32 1.52 ,062 10 24 .32 766 .04 3 .9, .Ol .04 c2 C.2 38 1.2 C.2 3.0 <l

.8 9.5 8.5 42.3 6.5 13 4 161 1.45 2.8 ~5 4 24 .22 .3 c.1 37 .50 ,017 12 2, .19 379 .05 ‘3 .78 .Ol .03 <2 C.2 21 C.3 C.2 3.1 8

l.2 21.8 4.9 33.8 113 18 6 629 .69 .6 3 1 191 .94 .7 c.1 9 5.82 ,073 4 10 .44 ,201 .o, 9 .49 .01 .02 C2 C.2 48 6.6 C.2 1.7 4 I.1 16.8 5.3 60.8 207 5 3 637 .36 2.2 ~5 1 235 .58 .4 s.1 8 6.60 .076 2 5 .36 645 .Ol 10 .31 .Ol .03 ~2 s.2 41 .5 C.2 2.0 <l

.8 7.9 8.9 42.2 <30 17 6 129 1.92 2.5 <5 1 11 .I1 .3 s.1 43 .I7 .098 12 26 .27 154 .06 G 1.17c.01 .04 <2 s.2 10 C.3 s.2 4.0 4

.8 10.6 11.6 55.1 66 26 10 203 2.91 3.7 ~5 3 13 .I1 .4 ., 60 .21 .087 14 42 .47 154 .09 6 1.94 .01 .06 ~2 s.2 15 c.3 s.2 5.6 1

.6 14.5 7.8 52.3 121 11 4 73 .PO 1.2 <5 4 57 .I2 .3 <.I 22 1.51 .047 7 17 .2, 473 .02 ~3 .92 .Ol .02 ‘2 c.2 37 .9 c.2 2.5 1

1.4 12.7 11.8 63.4 88 35 12 231 2.91 6.3 5 2 14 .I4 .6 .I 60 .24 .I29 16 4, .53 208 .OP 3 1.92 .Ol .06 ‘2 s.2 17 c.3 q.2 5.7 1 1.0 8.3 10.7 57.2 48 24 9 185 2.67 2.8 <5 2 13 .09 .3 .I 59 .17 .087 14 39 .42 190 .OP 4 1.83C.0, .04 C2 ‘.2 13 <.3 c.2 5.7 1

.9 8.8 12.3 66.7 87 22 9 199 2.74 4.0 5 2 13 .18 .3 c.1 58 .16 .080 14 39 .45 162 .I0 5 1.92s.01 .05 ~2 c.2 16 c.3 c.2 5.5 4 1.2 10.8 12.9 47.8 54 30 8 175 2.91 6.5 ~5 3 13 .I0 .5 s.1 60 .20 .,35 16 40 .46 149 .09 <3 ,.77<.01 .06 ~2 s.2 16 c.3 c.2 5.1 4 1.3 8.9 12.3 69.0 ~30 22 10 209 3.03 3.1 <5 3 15 .21 .4 .2 70 .23 .I43 15 40 .47 199 .,O ~3 1.8, .O, .05 ~2 c.2 16 <.3 c.2 6.6 2

.6 9.2 6.6 31.7 74 17 6 216 1.25 2.1 ~5 2 4, .14 .4 <.I 27 2.50 ,041 13 22 .43 262 .05 <3 .76 .O, .06 ~2 c.2 43 c.3 c.2 2.1 2

.6 5.3 6.1 27.6 39 15 5 94 1.16 1.5 ~5 1 10 .06 .3 c.1 29 .I9 .030 11 17 .23 122 .04 <3 .77<.01 .03 ~2 s.2 13 c.3 c.2 2.4 19 1.4 9.4 10.5 63.5 88 25 8 167 2.53 3.6 ~5 2 13 .I7 .4 <.I 56 .20 ,127 13 34 .35 164 .08 <3 ,.61<.0, .05 ~2 c.2 13 s.3 c.2 5.3 2

.5 9.9 9.2 51.8 53 29 9 223 2.44 3.6 ~5 3 16 .06 .3 ., 5, .24 ,059 15 40 .5, 194 .,O ~3 1.66 .O, .06 ~2 c.2 40 c.3 <.2 4.5 2

.B il.1 9.4 51.5 83 27 9 218 2.40 4.4 ~5 4 16 .08 .3 .I 50 .24 ,059 16 40 .51 189 .I0 ~3 1.6b.01 .06 ~2 s.2 12 c.3 c.2 4.8 2

.9 10.6 9.0 39.0 45 25 8 240 2.24 4.1 ~5 4 15 .06 .5 .I 46 .24 ,039 15 37 .46 174 .OP <3 1.31 .Ol .06 ‘2 <.2 14 c.3 c.2 3.8 1

.3 7.7 8.5 37.2 69 19 6 137 1.71 1.1 ~5 3 14 .04 .2 .I 39 .22 ,039 13 29 .38 144 .08 3 1.23 .Ol .04 ~2 q.2 16 ~3 ~2 3.9 8 1.0 9.6 10.1 53.3 82 31 11 238 2.78 3.6 ~5 3 14 .07 .3 .I 57 .21 .095 15 41 .53 147 .lO 3 1.77 .O, .07 ~2 c.2 14 q.3 c.2 5.2 2

.8 7.6 8.9 51.2 77 18 7 181 2.02 2.5 <5 ~1 13 .I4 .4 c.1 46 .2, ,086 14 27 .35 139 .06 <3 1.24<.01 .05 <2 <.2 16 <.3 c.2 3.8 ~1

.9 10.5 10.6 74.6 127 20 7 196 2.35 2.7 5 2 14 .I4 .4 .I 56 .21 ,081 14 34 .4, 199 .09 ~3 1.63 .Ol .04 ~2 c.2 14 c.3 c.2 5.7 Cl

.3 7.0 10.4 37.0 168 14 4 101 1.36 .9 <5 2 13 .05 .2 .I 37 .20 ,054 12 25 .29 142 .07 <3 1.26 .Ol .05 <2 c.2 1, c.3 c.2 4.6 4

.6 8.5 10.0 40.4 95 21 9 159 2.38 2.8 ~5 2 14 .06 .3 .1 51 .25 ,072 14 34 .L7 145 .09 <3 1.54 .Ol .05 ~2 c.2 19 c.3 c.2 5.0 2 !.3 10.1 8.2 44.0 38 20 5 128 I.66 3.7 6 1 14 .09 .6 <.I 43 .20 ,081 13 23 .3l 159 .05 ~3 .97 .O, .06 ~2 s.2 1, <.3 c.2 2.7 ~1

.8 4.7 9.3 49.7 62 10 5 150 1.54 1.0 <5 1 16 .22 .3 .A 41 .29 ,096 12 22 .23 179 .07 <3 .93 .01 .06 ~2 c.2 40 c.3 c.2 4.0 1 1.0 9.2 9.0 56.3 98 22 9 181 2.44 2.5 c5 2 13 .I3 .4 .I 58 .I9 ,065 14 33 .4, 147 .OP ~3 1.6, .O, .04 <2 c.2 10 <.3 q.2 5.6 <I

.8 10.3 9.8 40.8 123 30 7 153 2.40 3.7 ~5 3 13 .04 .3 .I 50 .22 ,087 13 39 .47 143 .08 <3 1.66 .Ol .06 ‘2 ‘.2 18 C.3 C.2 4.8 1 1.3 10.0 8.6 42.4 60 31 8 187 2.36 3.9 5 3 15 .04 .5 .I 51 .24 ,033 15 37 .53 206 .08 ~3 1.66 .01 .05 <2 .2 ~10 c.3 <.2 4.2 <l I.2 a.2 8.5 35.8 48 20 6 137 1.84 3.1 ~5 1 14 .07 .4 .I 47 .23 ,026 14 28 .37 172 .07 4 1.18 .Ol .03 ~2 c.2 <IO c.3 c.2 4.0 1 I.2 13.9 10.4 54.2 86 31 10 411 2.00 2.3 ~5 ~1 41 .25 .5 .2 5, 1.08 ,030 17 29 .37 679 .04 4 1.68 .O, .04 ~2 s.2 32 .3 s.2 4.0 Cl

.6 17.8 10.0 55.5 102 33 9 147 1.89 2.3 5 4 37 .27 .3 .I 44 .89 ,041 15 3, .44 630 .05 ~3 1.53 .02 .03 <2 <.2 27 c.3 c.2 3.7 4

1.7 119.5 95.1 256.2 2125 30 15 974 4.27 66.4 2, 16 6, 2.1, 9.8 20.7 68 .72 ,105 17 54 1.14 260 .,4 26 2.20 .05 .69 17 1.2 422 .4 2.0 6.7 54

Standard is STANDARD 02/H&SOD/AU-S. Samples besinnins 'RE' are Reruns ard 'WE' are Reiect Reruns.

ALI results are considered the confidential property of the client. Acme ~fsmes the Liabilities for actual cost of the analysis only. Data- FA _

LABORATORIES LTD. 852 E. ~RASTINGS ST. ‘V

r

UVRR BC V6A ,‘lRS 3-1716 ~' PIiONR(604)253-3158 ~~ZAX(604)@

GEOCREMICAL EXTRACT10 ANALYSIS CERTIFICATE

Tizard ?&mlorations 'Inc. PROJECT'KETCHIKA File # 97-3917 Page ~1 1022 - 470 Granville St.. ~"mcower EC Y6C ,,vs

:#

-' SAMPLE#

ACIN GE KIN 50E KIN IOOE ACIN 15OE KIN 2OOE

&CIN 250E KIN 300E KIN 350E KIN 400E AClN 450E

KIN SOOE KIN 55OE KIN 600E ACIN 650E KIN 700E

KIN 73OE !BAL.

BAZN 50E RE ACIN OE BAZN IOOE

BAZN 150E EAZN 2OOE EAZN 250E BA2N 300E BAZN 350E

BA2N 400E 8A2N 450E BAZN 500E BAZN 550E BAZN 600E

EAZN 650E BAZN 7OOE EAZN 750E EAZN 800E BAZN 850E

Ma CU Pb 2n l\g Ni Co Nn Fe As " Th sr Cd Sb Bi V Ca P La cr Ng Ba Ti B AL Ha K U TL Hg se Te Ga Au+ w Ppn Fw Fwppbwppnw % Fwwwm PpnPpn FFW 2 XPpnPm XFW %ppn % Y. ~Pmmppbwppnmppb

.7 10.5 9.4 52.8 55 26 7 258 2.11 3.9 ~5 6 28 .I7 .3 .I 42 .64 .036 18 32 .47 L9E .06 5 1.35 .02 .OL <2 .2 18 .3 c.2 4.1 <I 1.0 10.1 2.3 92.8 71 10 2 561 .18 .8 6 5 219 1.27 .4 <.I 5 5.34 ,102 4 4 .33 955c.01 I4 .I5 .OI .04 2 c.2 48 1.0 c.2 .9 I ,.I 5.7 8.7 45.5 43 I2 6 195 I.69 1.2 <5 3 37 .34 .2 ‘.I 42 .72 ,018 I, 21 .34 460 .09 ~3 1.20 .OI .04 <2 c.2 16 <.3 c.2 4.2 I 1.0 8.1 11.2 96.2 72 27 9 715 2.69 2.4 ~5 3 I4 .31 .2 .I 50 .22 ,102 I3 31 .38 244 .08 3 1.70 .Ol .06 <2 c.2 13 s.3 c.2 6.4 <I

.B 6.6 11.7 89.1 49 31 9 262 2.76 2.6 ~5 3 I4 .21 .3 .2 56 .24 .081 I3 34 .38 262 .09 3 I.92 .OI .05 *2 c.2 12 c.3 c.2 6.7 5

.B 7.7 9.8 74.9 42 26 9 282 2.63 2.7 ~5 4 13 .I5 .2 .I 53 .20 .077 13 35 .40 229 .09 ~3 1.73 .OI .06 ~2 c.2 I6 c.3 c.2 5.8 4

.5 7.5 9.7 34.9 42 30 8 163 2.38 3.3 7 9 I2 .20 .3 .I 55 .17 .066 15 34 .39 187 .I0 7 1.58 .02 .05 ‘2 <.2 18 c.3 c.2 5.9 1

.6 5.7 9.5 75.2 36 21 7 185 2.56 1.8 4 6 II .24 .2 .I 55 .I6 .I25 I5 33 .35 158 .09 ~3 1.60 .Ol .05 <2 <.2 I4 c.3 c.2 6.0 <I 1.0 7.6 10.9 67.9 <30 31 8 310 2.51 3.2 5 9 14 .26 .3 .l 59 .20 ,078 16 34 .38 240 .lI 8 1.69 .02 .08 ~2 c.2 16 c.3 c.2 7.4 28 1.2 7.8 11.5 101.3 69 29 10 306 3.52 3.3 ~5 3 12 .33 .3 .2 68 .18 .I30 13 35 .40 233 .I1 3 2.06 .Ol .06 2 c.2 23 c.3 ‘.2 8.2 ~1

.7 8.3 10.1 116.0 88 32 11 271 3.13 3.2 ~5 5 14 .30 .2 .1 62 .20 .I70 I3 37 .39 309 .I0 ~3 2.09 .02 .06 ~2 c.2 15 *.3 c.2 6.9 ~1

.6 4.9 9.4 82.1 37 20 8 144 2.53 I.6 ~5 4 I2 .I8 .2 .1 56 .16 .045 I2 31 .32 1% .I0 q3 1.61 .Ol .05 ~2 c.2 I2 c.3 c.2 6.4 <I

.9 8.7 9.4 61.4 ‘30 25 7 152 2.67 3.9 ~5 6 12 .19 .3 .I 56 .I6 .044 14 37 .44 173 .08 ~3 I.72 .OI .06 ~2 c.2 ‘IO s.3 q.2 5.6 <I

.9 6.0 9.7 93.9 57 I9 7 182 2.51 2.0 ~5 5 13 .21 .2 .I 56 .I8 ,097 12 29 .33 207 .08 ~3 1.66 .OI .05 ~2 c.2 16 x.3 c.2 6.1 <I 1.L a.9 10.8 43.5 37 28 6 219 2.24 3.4 q5 3 19 .02 .5 <.I 55 .29 ,040 I3 32 .36 315 .09 ~3 1.69 .OI .08 2 c.2 48 c.3 c.2 5.7 2

1.0 6.1 9.6 70.6 44 23 8 I34 2.78 2.3 ~5 4 I4 .25 .2 .I 61 .20 .057 14 34 .40 231 .I0 ~3 I.81 .O, .O4 ~2 c.2 <IO c.3 c.2 6.2 1

8 215 2.80 3.3 ~5 6 ~2 c.2 38 c.3 c.2 5.6 I 73 23 7 247 2.01 2.5 ~5 4 ~2 c.2 16 c.3 s.2 4.1 1

307 17 7 214 2.62 3.6 ~5 .I 71 .19 ,095 30 .39 244 .06 ~3 1.35 .OI <2 c.2 55 c.3 c.2 5.9 <I

8 310 2.63 3.2 ~5 .1 64 .30 .089 7 194 2.67 13.8 ~5 3 27 .18 593 .OI .2 479 2.6 c.2 3.4 3

9 II .I7 78, .OI <3 .53 .02 7 <2 c.2 335 3.5 c.2 2.0 7 9 .13 519 .Ol c3

5.1 37.5 14.1 7 379 1.59 21.5 <5

1.3 41.5 212 55 10 485 2.25 31.3 ~5 29 1.35 7.5 .I 41 .60 .I28 23 <2 c.2 121 16.3 c.2 I.6 6 3.2 23.9 9.8 169 8 I 530 .25 .5 6 83 I.65 2.4 c.1 10 3.66 ,113 4 ~2 c.2 80 4.9 c.2 1.6 2 5.8 26.3 7 313 1.69 7.8 ~5 58 .80 2.8 .2 I4 2.40 .I25 6 9 .36 6IB.0, ~2 s.2 70 2.0 <.2 2.3 5 !.7 34.6 79.1 300 30 6 746 1.05 4.5 ~5 81 .76 2.4 <.I 16 3.16 ,105 6 7 .35 6b2c.01 ~2 <.2 IO8 I.6 .2 2.2 2 1.3 13.1 3 ~1 229 .I4 c.5 ~5 137 2.40 .5 <.I 2 3.67 .090 2 2 .46 I95<.Ol ~3 ~2 c.2 65 1.3 <.2 1.1 <I

!.I 23.7 2. 80.0 138 10 I 209 .21 c.5 ~5 104 1.27 1.2 <.I 3 .44 255<.01 .03 ~2 c.2 43 1.1 <.2 I.6 <I 121.3 458 40 15 441 3.1, 9.6 ~5 5

I ‘2 57 .9B 2.5 7 I5 .60 327s.01 .05 ~2 c.2 116 2.2 c.2 3.0 4

123.2 474 40 13 298 2.93 14.6 ~5 3 55 .51 3.9 I4 17 .42 37Os.01 .08 ~2 q.2 110 2.0 c.2 2.9 7 165.6 I78 13 2 850 .38 .7 7 ‘2 160 2.01 2.0 <.I .37 317<.01 14 .18 .06 ~2 c.2 46 5.1 c.2 I.4 2 144.4 656 34 i, 246 2.49 18.5 a 5 77 1.03 3.9 .I 36 1.29 .I I6 I4 .31 424 .OI .I0 ~2 c.2 130 2.4 c.2 2.3 3

STANDARD 0 :25.0 125.1 105.6 263.7 1893 31 16 984 4.57 70.2 24 20 59 2.10 7.1 22.2 72 .68 .llI I8 55 1.20 256 .I4 25 2.31 .07 .71 20 2.1 432 .5 1.8 7.0 45

Standard is STANDARD DZ/HG-SOO/AU-S. ICP - 15 GRAM SAMPLE IS DIGESTED "lTH 90 ML 3-1-2 "CL-HNO3-"20 AT 95 DEG. C FOR ONE HOUR AND IS DILUTED TO 300 ML VlTH UATER. THIS LEACH IS PARTlAL FOR MN FE SR CA P LA CR MS BA TI B V AHD LlHlTEO FOR NA Y GA AN0 A,.. SOLUTlON ANALYSEO OlRECTLY BY ICP. MO C" PB 2N At AS A" CO SB BI TL HG SE TE AN0 GA ARE EXTRACTED VlTH HIBK-ALIPUAT 336 AND ANALYSEO BY ICP. ELE AMPLES CONTAIN CU,PB,2N,AS~1500 PPM,Fe>ZOX. - SAMPLE TYPE: SOlL AU+ - AQUA-RECIA/HIBK EXTRACT, GF/AA FINISHED.

DATE RECEIVED: JUL 28 1997 DATE REPORT MAILED: 4 i

Samples beginnins l&B' Reruns and 'RRE' are Reject Reruns.

77 Il 97 ..D.TO"E, C.LEONt, J.UANt; CERTlFlED B.C. ASSAYERS

All results am considered the confidential property of the client. Acme ~ssmes the of the malysis only. P Data- FA _

AB3Y 2650E AB3N 2700E AB3N 2750E AB3N 2800E AB3N 2B50E

AB3N 2900E AB3N 2950E AB3N 3000E AB3N 3050E AB3N 3lOOE

AB3N 3150E RE AB3N 3150E AB3N 3200E AB3N 3250E AB3N 3300E

AB3N 335OE AB3N 3400E AB3N 3450E AB3N 3500E AB3N 3550E

AB3N 3600E AB3N 3650E AB3N 3700E AB3N 3750E AB3N 3800E

AB3N 3650E AB3N 3900E AB3N 3950E AB3N 4000E AClN 950E

AClN lOOOE AClN 105OE AClN 1lOOE AClN 1150E AClN 1200E

STANDARD DZIH 12

t Tizard Explorations Inc. PROJECT KETCHIKA FILE # 97-3778 Page 6 v

no C" Pb zn Ag Ni Co H" Fe As " Th ST Cd Sb Bi V ta P La tr llg Be Ti B Al 118 Y ,, T, Hg Se Te Ga A"+

P ppnppn FPppbmw Fw % ppnppnppnppn PPppn Fwppn x xppnppn %ppn%ppn %% ~ppnwppbppnppnwP

.9 9.7 B.0 41.3 42 27 9 197 2.46 5.9 5 6 22 .07 .3 <., 46 .40 .025 15 38 .5, 292 .09 <3 1.34 .02 .05 <2 c.2 12 .3 S.2 4.9 4 1.3 6.5 0.2 53.5 95 20 a 186 2.47 3.1 ~5 4 14 .17 .3 ., 56 .22 .021 13 34 .4B 156 .lO ~3 1.37 .Ol .04 ~2 c.2 14 q.3 c.2 6.0 3 1.3 7.3 8.6 46.3 65 20 8 219 2.16 3.2 ~5 4 17 .I, .2 <.I 50 .30 .0,5 13 3, .43 233 .09 <3 1.40 .Ol .ffi <2 s.2 12 s.3 c.2 5.7 Cl 1.4 6.9 8.1 50.3 72 21 8 211 2.19 5.1 <5 3 16 .,7 .3 <., 49 .29 .027 12 30 .40 235 .07 ~3 1.27s.01 .05 <2 c.2 13 c.3 S.2 4.9

.9 6.6 7.7 37.2 5B 21 8 181 2.39 5.2 6 4 I6 .06 .3 .I 53 .27 ,019 13 34 .50 18, .09 <3 1.45 .Ol .04 <2 s.2 <IO c.3 c.2 5.0 ;

1.3 0.6 9.9 68.6 58 25 9 239 2.94 5.7 ~5 4 14 .31 .4 ., 64 .20 ,067 14 36 .43 189 .lO <3 1.49 .Ol .05 <2 S.2 40 q.3 c.2 6.8 cl 1.6 9.8 9.3 66.9 70 25 9 22B 2.81 5.3 7 3 15 .24 .4 .I 62 .25 ,033 13 37 .46 206 .I0 3 1.58 .Ol .05 s2 c.2 17 c.3 c.2 7.1 <l

1.5 7.6 9.6 50.9 63 19 8 244 2.49 4.5 <5 3 13 .22 .4 .I 57 .21 .033 12 31 .3B 181 .G9 ~3 1.21 .Ol .05 <2 c.2 12 c.3 c.2 6.5 ~1 .9 11.7 8.2 39.1 83 25 6 293 1.65 4.8 ~5 4 22 .27 .5 <., 34 .43 .048 15 27 .43 241 .06 ~3 .90 .Ol .05 S2 c.2 24 c.3 c.2 3.1 3 .8 9.7 8.6 41.8 39 25 9 189 2.37 4.0 5 5 21 .I1 .3 ., 49 .39 ,030 16 36 .47 272 .09 ~3 1.53 .O, .O5 ~2 q.2 19 c.3 c.2 5.2 2

1.1 11.5 6.9 33.0 99 15 4 175 1.15 5.0 <5 3 83 .22 .9 <.I 33 3.57 ,056 1, 16 .69 345 .04 ~3 .60 .Ol .03 ~2 ‘.2 79 .3 q.2 2.7 2 ,.I 11.5 6.3 33.6 98 15 4 173 1.16 4.3 ~5 3 76 .20 .9 <., 33 3.18 ,053 11 17 .64 344 .04 ~3 .61 .Ol .04 <2 s.2 65 .3 c.2 2.2 4

.B 14.6 2.6 13.3 175 7 4 314 .40 c.5 ~5 4 166 .75 .4 c.1 10 5.80 .063 3 5 .23 1141 .Ol 6 .36 .02 .Ol ~2 c.2 42 3.7 <.2 1.9 ~1 1.5 4.0 1.1 13.6 ~30 3 2 257 .89 .6 ~5 4 138 .I1 .2 c.1 3 4.57 .lOE 1 2 .3O 225<.01 13 .06 .01 .03 ‘2 c.2 44 1.3 s.2 I.1 <l

.7 9.5 2.0 9.4 92 7 4 452 .34 .5 <5 1 221 .36 .2 c.1 6 6.91 ,074 2 3 .40 ,,,1<.01 10 .20 .O, .Ol ~2 c.2 62 1.0 c.2 1.3 ~1

1.0 7.7 1.3 13.6 ~30 4 2 531 .15 c.5 <5 <, 185 .45 .2 <.I 4 6.M .07-l 1 2 .39 ,0,7<.01 10 .I4 .01 .02 <2 <.2 46 1.1 c.2 1.1 <l .B 9.7 1.4 5.8 85 3 3 311 .19 c.5 9 1 193 .53 .6 c.1 5 6.53 ,069 1 2 .30 913c.01 10 .27 .02 .O, <2 <.2 46 2.9 c.2 1.1 ~1

2.9 8.3 1.4 7.6 34 4 4 3026 .32 .5 6 <I 171 .23 .2 c.1 5 4.92 ,083 2 3 .22 1365 .Ol 7 .35 .02 .Ol <2 s.2 31 1.0 c.2 1.4 <l 1.3 10.5 3.1 32.2 59 9 3 410 .53 s.5 <5 1 182 .58 .5 <.I 12 6.08 .OB2 3 7 .33 1154 .Ol 9 .30 .Ol .03 <2 s.2 64 .9 <.2 1.9 2 1.9 7.1 .9 12.6 92 5 6 2052 1.17 2.0 5 Cl 210 .54 .2 <.I 3 7.65 .098 1 2 .34 ,187<.01 14 .OP .Ol .03 ‘2 q.2 57 1.2 c.2 1.4 1

3.0 5.3 1.0 179.8 <30 10 37 55809 1.44 1.7 c5 4 193 .77 c.2 c.1 2 4.T7 ,093 <I 1 .30 4246c.01 6 .06 .Ol .04 <2 <.2 50 <.3 c.2 1.0 1 3.2 12.7 1.6 34.0 152 IO 4 2275 .70 2.4 ~5 4 146 .94 .3 s.1 7 5.06 ,159 1 4 .30 949c.01 11 .I7 .02 .02 <2 c.2 53 2.1 c.2 1.7 4 1.6 1.4 c.3 21.0 <30 2 2 191 .58 3.2 ~5 ~1 103 .04 c.2 <.I 2 3.22 ,076 1 2 .19 606<.0, 13 .05 .Ol .Ol <2 c.2 59 .7 q.2 c.5 <I 4.2 5.1 1.1 14.3 <30 4 1 175 1.24 3.0 ~5 ~1 122 .37 c.2 c.1 2 3.06 ,089 1 2 .17 742c.01 7 .07 .Ol .Ol <2 c.2 68 <.3 c.2 1.4 1

.6 7.8 5.3 42.5 83 18 5 185 1.14 1.9 <5 1 24 .20 .3 <., 27 .LB ,058 12 ,9 .24 244 .04 ~3 .92 .Ol .03 ~2 s.2 23 c.3 c.2 3.0 1

.5 6.6 7.6 38.0 43 15 7 290 1.69 2.2 ~5 3 13 .11 .2 ., 38 .20 .050 13 25 .32 169 .07 ~3 1.09 .Ol .05 <2 q.2 22 c.3 c.2 5.4 1

.B 7.0 8.6 40.9 37 22 6 146 2.22 2.8 ~5 5 14 .OB .2 ., 53 .22 ,061 16 34 .37 160 .09 ~3 1.50 .O, .04 ~2 c.2 12 ‘.3 c.2 6.6 1 1.0 10.1 7.9 54.9 ~30 27 9 180 2.31 3.8 5 6 14 .15 .2 c.1 50 .21 .086 16 35 .42 185 .09 ~3 1.53 .Ol .05 ‘2 c.2 <,O c.3 <.2 5.6 2 1.1 7.0 6.0 47.4 ~30 31 9 341 2.45 2.9 7 5 13 .07 .2 <.I 51 .2l ,062 16 38 .4B 175 .lO 3 1.62 .Ol .06 ~2 c.2 19 c.3 c.2 4.6 ~1

.E 6.3 7.5 52.2 ~30 15 6 175 2.19 2.3 ~5 3 9 .22 .2 ., 49 .12 ,064 1, 27 .27 113 .07 ~3 ,.2B .O, .03 ~2 c.2 ~10 c.3 c.2 5.2 1

.3 12.3 1.1 42.4 113 7 3 662 .20 .7 <5 1 224 .63 .2 .I 5 6.47 ,084 2 3 .37 7t!a<.Ol 10 .,7 .o, .02 ‘2 c.2 78 .9 ‘.2 c.5 1 1.1 9.5 9.6 64.0 45 22 a 291 2.32 2.8 <5 3 18 .21 .3 .2 47 .32 ,102 13 30 .3B 24, .OB ~3 1.40 .O, .05 ~2 .2 <IO c.3 s.2 6.5 2

.6 0.5 6.5 48.0 106 21 7 273 2.10 2.2 <5 4 15 .ll .3 .2 42 .23 ,062 13 30 .35 214 .08 <3 1.26 .O, .06 <2 c.2 10 c.3 c.2 4.4 1 ~ 1.0 14.9 9.1 67.7 125 30 9 269 2.31 4.5 ~5 4 29 .17 .4 .2 44 .Y, ,051 18 36 .50 233 .08 ~3 1.36 .02 .07 ~2 c.2 23 c.3 c.2 5.3 1

1.3 6.9 .B 45.6 ~30 2 2 480 .47 .6 ~5 ~1 212 .30 c.2 <.I 2 5.63 ,107 1 2 .41 742<.01 12 .05 .Ol .03 ‘2 s.2 54 1.3 c.2 .6 1

,3.7 116.3 97.1 253.7 ,888 29 14 996 4.36 69.6 10 19 59 2.17 9.5 22.1 69 .69 ,108 17 53 1.15 250 .l4 24 2.17 .05 .70 16 2.1 443 .6 2.0 7.2 51

Standard is STANDARD D2fHG-500/AUS. Samples beginninq 'RE' are Rerms and 'ME' are Reiect Reruns.

ALL rerulrs are considered the confidential property of the client. Acme BSSUWE the Liabilities for~,actual cost of the analysis only. Data- FA _

a Tizard Explorations Inc. PROJECT KETCHIKA FILE # 97-3778 Page 7 ~ IDEhwm(*. ‘44 m uwmcu I SAHPLE# No Cu Pb 2n Ag Ni Co Hn Fe As u Th sr Cd Sb Bi v ca P Le Cr Ng Ba Ti B Ail Na I: N TL Hg Se Te Ca A"+

,ppn ppnw FvmPwppnppn ~PpnFmwppnppnFwlmw x XPWnm xppn xlm % % ~wppnppbppnFwwmP - i AClY 1250E AClY 130OE

.6 1.0

.8

.7

.9

11.7 1.5 19.8 105 IO 3 484 .40 c.5 IO.6 7.6 65.4 50 25 0 267 2.11 2.7

<5 <5 <5 4 <5

1264 123 I 20 1 I8

4 13

1 27

.66

.19 .3 .3

c.1 .l .2 .l .I

7 a.91 .063 3 6 .40 974 .Ol 42 .40 .070 I4 32 .36 249 .09 47 .32 .042 15 37 .47 233 .ll 47 .31 .030 15 36 .50 258 .I0 37 .22 .045 11 23 .28 215 .06

8 .2a .Ol .02 7 1.31 .Ol .oa 3 1.46 .02 .07

<3 1.50 .Ol .06 6 1.21 .02 .04

<2 <.2 17 1.4 <.2 1.3 <2 .2 40 .3 c.2 4.9 <2 <.2 40 c.3 <.2 4.7 <2 c.2 la c.3 c.2 4.8 <2 c.2 17 c.3 c.2 4.8

49 .50 .031 17 38 .47 314 .lO 4 1.58 .02 .06 <2 c.2 31 c.3 <.2 4.7 47 .29 .069 15 26 .30 123 .oa 7 1.07 .Ol .04 <2 .2 11 c.3 c.2 5.9 53 .47 .022 15 38 .47 321 .ll <3 1.68 .02 .05 ~2 s.2 36 s.3 ‘.2 6.0

2 6.37 .066 12 .36 732c.01 12 .ll .Ol .Ol <2 c.2 37 c.3 c.2 s.5 3 5.65 .072 12 .63 527<.01 15 .lO .Ol .Ol ~2 q.2 51 .4 c.2 .a

43 .58 .026 48 .28 .024 46 .30 .051 33 .33 .054 43 .28 .072

21 33 14 37 I4 33 I1 23 12 30

12 31 11 20 13 21

.46 245 .OE

.4a 183 .I2

44 .29 ,072 30 .23 .057 32 .51 .059

.3a 275 .I0

.27 256 .Ob

.38 265 .09

5 1.18 .02 .lD <2 .2 24 .4 s.2 4.0 5 1.25 .02 .I1 ~2 .2 14 c.3 c.2 4.6 7 1.43 .02 .lO <2 .2 I2 c.3 ‘.2 5.1

<3 I.D5 .02 .lO <2 .2 20 c.3 <.2 4.0 ~3 I.23 .02 .ll ~2 c.2 13 c.3 c.2 4.2

.38 274 .09 <3 1.28 .Ol .ll <2 .2 I2 c.3 <.2 4.9

.2‘ 219 .06 4 .7B .Ol .07 ~2 c.2 40 c.3 c.2 2.8

.31 239 .06 4 .76 .Ol .lD ~2 c.2 20 .3 <.2 2.7

1 1

<I 1

<I

AClN 1350E AClN 1400E AClY 1450E

9.6 9.2 59.5 0.8 7.9 59.5 6.9 8.0 65.0

11.5 a.3 60.5

105 25 9 275 2.34 2.3 84 24 9 327 2.20 2.5 67 16 9 554 1.63 .a

.I5

.13

.25

.I1

.2

.3 s.2

AClN 1500E AClN 1550E AClN 1600E AClN 1650E AClN 1700E

.6 I.1

:t .9

6.9 9.0 47.2 11.7 10.3 58.7

5.4 1.0 24.7 6.0 .9 13.5

118 28 52 I5 55 26 43 4

<30 5

9 341 2.44 I.9 5 212 1.85 1.7 9 341 2.64 2.5 I 206 .ll c.5 1 721 .25 .5

<l 15 .18 <I 26 .I8

1 226 .19 <l 312 .25

.2 .l

.2

.2 c.2

.2

.2 .I

‘.l c.1

AClN 175OE 1.6 ACIN 18OOE 1.3 AclN 1850E .9 AClN 1900E 1.1 AClN 1950E .7

13.1 9.8 52.6 8.9 7.4 47.9 8.0 8.6 56.1 6.6 7.4 46.3 5.9 6.9 64.0

73 44 a2 aa 55

23 20 24 16 22

7 261 2.24 3.4

<5 <5 <5 IO

5

<5 <5 <5 ‘5 <5

8 233 2.35 2.9 8 327 2.19 2.0 65181.44 .a 8 412 2.06 1.0

Cl 40 .l4 I 19 .07

<I 20 .13 4 19 .lL 4 19 .16

.2 .5 .4 .3 .2 .2

.2 .2 .l .l

1 1 1 1

<l

2 I I

<l 4

RE AClN 1950E AClN ZOODE ACIN 2050E AClN ZIOOE AClN 2150E

.9 6.1 7.4 64.8 58 23 .9 6.1 6.2 31.5 83 ID

1.3 12.8 7.1 37.7 90 19

8 419 2.09 1.1 5 4 20 .17 ‘.2 5 421 1.32 .5 <5 ~1 16 .I0 .2 6 724 1.41 2.0 <5 <I 27 .17 .L

c.1 .I

<.I

<l I

1.3 11.3 7.9 40.8 245 22 7 257 1.90 2.0 5 Sl 34 .21 .4 ‘.I 41 .61 .030 15 29 .38 277 .08 4 1.07 .Ol .ll ‘2 .2 26 .3 c.2 3.3 2 1.5 18.0 9.8 36.3 147 26 9 370 2.25 2.2 <5 I 40 .3a .4 .l 48 .62 ,021 16 32 .41 385 .08 5 1.38 .02 .11 ‘2 .3 31 1.0 <.2 4.7 1

AClN 22OOE AClN 2250E AClN 2300E AClN 2350E AClN 2400E

AClN 2450E AClN 2500E AClN 255OE AClN 2600E AClN 2650E

I.2 13.4 7.6 41.8 67 22 8 312 2.08 2.6 ~5 1 33 .12 .4 .I 41 .47 .035 17 30 .36 248 .07 5 1.13 .02 .07 ~2 c.2 41 .4 c.2 3.3 1 2.1 17.3 12.3 51.5 94 33 10 323 2.41 3.9 5 Cl 30 .09 .7 .I 50 .50 .022 20 36 .45 286 .07 4 1.48 .02 .I4 ~2 .2 50 .5 c.2 4.3 2 1.2 11.6 6.8 33.8 <30 Ia 7 177 1.72 3.3 ~5 ~1 21 .05 .4 <.I 38 .33 .037 15 28 .34 166 .08 4 1.03 .oi .08 <2 .2 28 c.3 c.2 3.0 2

.7 6.7 8.0 79.1 54 19 8 228 2.29 1.7 6 ~1 17 .19 .2 .l 51 .28 ,056 14 34 .42 241 .09 ~3 1.55 .Ol .05 ~2 c.2 ~10 c.3 c.2 5.3 1 1.2 11.4 8.4 43.5 33 19 7 339 I.78 1.8 c5 <I 25 .3a .5 c.1 40 .52 ,037 15 26 .36 307 .07 5 1.02 .oi .oa ~2 .2 43 c.3 c.2 3.4 <I

.7 21.2 II.8 88.8 68 24 II 380 2.62 I.8 ~5 ? 30 .34 q.2 c.1 59 .48 .061 I6 40 .59 433 .07 ~3 2.10 .Ol .OB ~2 .2 29 .L c.2 5.3 <I

.6 15.2 12.5 83.3 63 22 9 248 2.26 2.1 ~5 1 41 .54 .3 c.1 45 .78 ,063 16 32 .49 417 .08 5 I.35 .Ol .ll ~2 .2 52 .3 <.2 3.8 2

.9 15.8 9.4 55.6 56 24 9 383 2.02 2.5 <5 ~1 44 .67 .3 <.I L3 .a6 ,063 14 28 .46 370 .07 5 1.10 .02 .06 ~2 .2 64 .B c.2 3.4 2

.7 19.2 12.1 91.9 113 20 10 444 2.23 2.0 <5 1 32 .A .2 .l 47 .50 ,111 I5 32 .46 478 .07 5 1.38 .Ol .lO <2 .3 34 .7 c.2 4.2 2

.9 II.5 a.0 69.7 ~30 24 ID 276 2.42 2.0 <5 2 I7 .14 .3 .l 48 .25 .060 16 38 .47 215 .09 ~3 1.59 .Ol .06 ‘2 c.2 17 <.3 c.2 4.8 1

AClN 2700E 1.1 9.8 9.2 106.2 31 28 9 576 2.70 3.1 <5 2 13 .45 .2 .l 53 .20 ,064 I2 38 .46 253 .,O <3 1.76 .Ol .06 ‘2 .3 15 <.3 <.2 6.2 ~1 AClN 2750E 1.0 7.9 9.0 83.4 ~30 22 7 390 2.28 1.0 7 <l 14 .30 .2 q.1 50 .22 .056 12 30 .34 290 .06 <3 1.53 .O, .05 ~2 .2 11 <.3 <.2 5.3 1 AClN 28OOE 1.0 9.3 8.6 79.6 ~30 24 9 280 2.64 1.3 <5 2 15 .17 .2 .l 54 .23 ,055 13 38 .47 274 .08 <3 1.81 .Ol .05 <2 .2 15 <.3 <.2 5.5 4 AC~N 2a50E 1.1 11.8 8.3 68.4 ~30 28 10 329 2.79 2.0 <5 2 Ia .12 .3 c.1 54 .27 .063 15 42 .54 224 .09 <3 1.78 .O, .06 <2 .3 15 <.3 <.2 5.2 1 AClN 2900E .8 9.5 8.3 78.8 33 28 10 261 2.73 2.0 c5 I 16 .l7 .3 1 56 .24 .074 I3 39 .48 236 .O9 <3 1.84 .O, .06 <2 c.2 22 <.3 <.2 5.3 1

STANDARD DZ/H '23.8 118.6 96.8 258.5 1839 3, 15 994 4.50 74.9 15 15 64 2.22 10.3 23.2 70 .76 ,104 17 55 1.18 26, .14 25 2.29 .05 .70 17 2.2 487 .7 1.9 6.7 54 ~

Standard is STANDARD DZ/HG-SOO/AU-S. Samples bwinning 'RE' are Rewm and 'ME' are Reject Reruns.

All results are considered the confidential property of the client. Acme ~ssms the liabilities for actual cost of the analysis only. Data- fA _

# c Tizard Explorations Inc. PROJECT KETCHIKA FILE # 97-3770 Page 8

UN Mu"7101 Y SAMPLE11 I

8 254 2.57 2.5 q5 2 13 7 149 2.05 1.6 7 2 14

1.0 9.3 9.0 75.4 50 25 .8 6.8 7.8 54.9 45 15 .8 10.2 8.9 27.9 65 15 .7 10.9 8.3 32.6 58 20 .7 13.1 8.9 99.8 90 29

4 152 1.52 2.2 <5 1 15 7 140 1.98 2.5 ~5 1 19

11 405 2.79 1.9 ~5 2 13

.22 .3 .2 48 .22 -059 11 34 .44 249 .08 -z3 1.52 .Ol .05 <2 <.2 12 c.3 c.2 5.9 cl

.12 .2 .2 43 .23 ,031 11 30 .38 172 .07 <3 1.23 .Ol .03 <2 <.2 12 <.3 <.2 5.0 5

.lO .3 .2 33 .34 ,028 9 24 .2L 205 .04 <3 .70 .Ol .02 <2 c.2 14 <.3 c.2 2.5 4

.lO .3 .2 39 .34 ,026 14 31 3 233 .08 5 1.14 .Ol .05 ~2 c.2 18 q.3 c.2 4.2 1

.27 .2 .2 51 .20 .085 11 38 .42 314 .lO 3 1.75 .Ol .07 ‘2 c.2 29 c.3 c.2 5.6 <I

.7 8.4 8.0 47.6 35 18 7 221 2.19 2.3 ~5 2 13 .I0 .2 .2

.7 7.0 10.5 66.4 43 20 7 181 2.43 2.0 ~5 4 11 .20 .2 .I

.9 10.4 8.8 61.1 54 25 9 269 2.75 3.3 ~5 1 14 .I9 .3 .2

.9 6.2 7.2 34.1 36 13 5 119 1.74 2.3 ~5 cl 20 .08 .2 .2

.8 10.7 7.6 37.1 <30 17 5 240 1.62 2.2 ~5 ~1 22 .24 .3 .2

44 .I8 ,065 44 .18 ,166 52 .21 ,099 40 .36 ,013 33 .53 ,037

10 30 .38 210 .07 <3 1.35 .Ol 11 29 .33 178 .06 ~3 1.35X.01 12 37 .50 302 .09 3 1.59 .Ol

9 26 .33 252 .07 <3 1.09 .Ol 10 23 .27 266 .05 ~3 .99 .Ol

<2 c.2 23 c.3 c.2 4.9 1 <2 <.2 27 c.3 g.2 5.2 1 <2 <.2 17 c.3 c.2 5.6 1 <2 <.2 Cl0 c.3 q.2 4.1 1 ‘2 s.2 31 c.3 c.2 3.2 4

.6 10.3 7.5 62.2 71 21

.8 12.4 8.8 56.8 52 31 I.2 10.6 9.9 55.7 41 29 1.1 12.6 9.5 43.2 56 29 1.2 10.5 8.3 40.4 60 20

1.1 9.7 4.3 28.9 49 11 2.8 18.8 6.2 45.1 127 18 1.3 7.6 a.7 41.8 38 18 1.3 5.2 1.6 18.3 ~30 3 1.0 6.5 7.4 43.2 55 18

8 242 2.07 1.8 c5 2 14 10 294 2.63 3.9 ~5 4 12

9 183 2.68 3.4 <5 3 12 8 2.36 2.31 4.7 S5 3 13 6 291 1.73 3.4 ~5 ~1 24

2 250 1.10 .7 <5 Cl 106 5 458 1.67 3.5 ~5 ~1 143 5 153 2.06 2.7 ~5 1 18

.12 .2 .2

.I9 .4 .2

.16 .3 .3

.13 .5 .2

.31 .3 .2

39 .20 .070 49 .21 .126 52 .I8 ,085 47 .21 .059 34 .59 ,048

11 31 13 37 12 38 15 37

9 25

.03 .04 .05 .05 .04

.04

.06

.I%

.41 224 .07 3 1.42 .Ol

.48 212 .07 <3 1.68 .Ol

.45 234 .08 c3 1.75 .Ol

.43 196 .07 <3 1.47c.01

.32 368 .04 3 1.04 .Ol

.35 356 .02 4 .43 .03

<2 s.2 40 c.3 s.2 4.5 3 <2 q.2 20 <.3 c.2 4.8 2 ‘2 <.2 10 c.3 c.2 6.0 1 ‘2 <.2 20 c.3 c.2 5.0 1 ~2 c.2 16 .3 c.2 3.4 1

.04

.03

13 2.48 ,089 24 3.94 ,089 44 .32 .049

3 4.16 .059 44 .38 ,049

.05 <2 c.2 51 1.4 c.2 2.2 1 <2 <.2 58 1.7 c.2 2.9 3 <2 c.2 40 c.3 c.2 4.9 2 ~2 c.2 48 .6 q.2 .6 1 <2 c.2 <IO c.3 c.2 4.2 ~1

.8 6.1 7.7 36.4 76 1L

.9 8.3 6.2 24.9 ~30 13

.8 10.2 8.1 63.2 122 24

1 288 .15 c.5 5 ‘1 171 5 159 2.04 2.5 9 2 20

.8 10.9 7.6 44.2 67 19 .9 9.8 6.4 52.6 4 26

.7 11.9 8.6 63.8 117 26 .8 7.2 7.4 52.2 98 19

1.2 8.4 6.6 43.3 92 16

4 166 1.42 1.5 ~5 1 Id L 107 1.21 1.9 <5 1 11 7 322 2.46 2.1 ~5 3 18 6 200 2.05 2.6 ~5 3 15

5 13 ~~~ 5 16 .50 520 .04 16 .57 .03 .07 9 28 .30 304 .06 4 1.31q.01 .06 1 2 .52 367c.01 11 .07 .02 .02

10 30 .32 314 .06 3 1.34 .Ol .07

8 219 2.42 2.8 c5 2 16

32 .23 ,104 923 31 .20 .023 9 20 43 .33 ,054 15 36 37 .26 .051 14 32 49 .25 ,069 13 34

.22 260 .04 ~3 .97 .Ol .06

.23 156 .05 ~3 .74 .Ol .05

.4, 265 .09 ~3 1.48 .Ol .W

.43 178 .08 ~3 1.12 .Ol .07

.49 221 .OP 4 1.41 .Ol .07

.43 286 .09 ~3 1.56 .Ol .06

.6 a.2 6.6 48.1 46 21

.8 10.9 6.7 38.9 30 23

47 .30 ,046 17 37 43 .30 .026 12 33 .43 276 .09 3 1.35 .Ol .06 40 .23 ,052 11 25 .33 230 .05 ~3 1.14<.01 .04 47 .23 ,042 12 34 .49 215 .09 3 1.44<.01 .Ob 43 .21 ,047 13 33 .46 199 .07 ~3 1.23c.01 .05

ACZN 1400E .7 13.2 7.2 40.3 38 31 ACZN 1450E 1.0 7.7 2.7 48.1 88 8 ACZN 1500E .9 11.1 6.2 29.2 62 17 ACZN 1550E .8 8.9 5.2 32.5 65 17 AC2N 1600E .8 8.2 6.3 76.2 113 22

9 372 2.60 2.8 c5 3 18 7 240 2.13 1.8 ~5 2 18 6 758 1.76 2.1 ~5 1 14 8 261 2.36 2.1 C5 2 14 7 183 2.22 3.2 7 3 12

9 234 2.47 4.5 ~5 4 16 3 490 .48 c.5 c5 2 172 5 134 1.40 2.3 ~5 2 17 6 138 1.57 2.2 <5 2 14 7 624 1.96 1.3 c5 2 15

.25 .2 c.1

.6.5 .4 .l

.12 .3 .I

.29 c.2 .I

.I0 .2 .2

.I5 .2 .I

.07 .3 <.I

.I4 .3 .2

.08 .3 .l .08 .3 .l

.12 .3 .l

.09 .2 .I

.08 .3 .2

.05 .3 .I

.05 .3 .l

.02 .4 .I

.51 c.2 <.I

.05 .4 .I

.05 .2 .l

.16 c.2 .I

44 .29 ,039 26 40 .53 246 .08 ~3 1.40 .Ol .05 9 7.54 ,065 2 7 ~37 .-. 95‘ -01 ..~ 7 .37 .o, ~~~ ~~~ .04

33 .35 .014 11 22 .26 199 .07 ~3 .83 .Ol .I1 34 .24 ,030 11 24 .30 165 .07 *3 .89 .Ol .05 39 .24 ,064 11 29 .35 428 .07 ~3 1.41 .Ol .06

<2 .3 13 c.3 c.2 4.2 ~1 c2 .2 17 c.3 c.2 3.0 2 <2 .2 25 c.3 c.2 4.8 <l <2 .2 14 c.3 c.2 4.3 4 <2 .3 16 c.3 c.2 4.4 cl

<2 c.2 28 c.3 <.2 5.3 <1 <2 .3 13 c.3 <.2 5.3 1 <2 .3 20 <.3 c.2 4.2 <I <2 c.2 22 q.3 c.2 4.8 1 <2 c.2 14 s.3 c.2 4.1 <l

<2 c.2 20 c.3 ‘.2 4.1 1 <2 <.2 30 .3 c.2 1.8 2 <2 .3 24 c.3 c.2 2.9 1 <2 .2 21 c.3 c.2 3.3 -4 <2 .2 11 c.3 c.2 4.8 1

ACIN 295OE AClN 3000E ACZW OE ACZW 50E ACZW 1OOE

ACZN 150E ACZW 2OOE ACZN 250E ACZN 300E ACZN 350E

ACZN 400E ACZN 450E ACZN 500E ACZN 550E ACZN 600E

AC2N 650E ACZN 750E RE ACZW 850E ACZN 8OOE ACZN 850E

ACZN 900E ACZN 950E ACZN 1OOOE ACZN IOSOE ACZN 1lOOE

ACZN 1150E ACZN 12OOE

I ;

ACZN 1250E ACZN 1300E ACZN 1350E

STANDARD D2, 4.0 120.0 96.2 257.8 1723 29 ,L 98, 4.45 69.8 20 16 60 2.,6 9.5 22.0 69 .68 ,107 17 54 1.16 258 .,4 25 2.28 .06 .69 17 2.4 439 .5 2.0 6.6 44

Standard is STANDARD 02/K-SOO/AU-S. Samples binning 'RE' are Reruns and 'ME' are Reiect Reruns. I

AlI results are considered the confidential proprty of the client. Acme assures the Liabilities for actual cosf of the analysis only. Oata- FA _

Tizard Explorations Inc. FILE # 9-7-3778

ACZN 1650E ACZW 1700E ACZN 1750E ACZN 18OOE ACZN 1850E

ACZN 19OOE ACZN 1950E ACZN ZOOOE ACZN 2050E ACZN 2lOOE

ACZN 2150E ACZN 22OOE ACZN 2250E ACZN 2300E AC2N 2350E

ACZN 2400E ACZN 2450E ACZN 2500E ACZN 2550E RE ACZN 2550E

AC2N 2600E AC2N 2650E ACZN 2700E ACZN 2750E ACZN 2aOOE

ACZN 2850E ACZN 29OOE ACZN 2950E ACZN 3000E ABN OE

AC3N SOE AC3N IOOE AC3N 150E AC3N 2OOE ADN 250E

STANDARD DZ/H

I :

.9 0.6 7.2 57.6 79 26 I.0 11.1 7.7 57.8 35 28 I.0 7.9 9.4 109.3 97 27 1.5 9.3 7.9 60.6 34 29

.3 8.3 8.5 58.8 a2 27

.9 11.1 9.0 40.5 ~30 32

.4 10.7 8.0 52.1 129 29

.5 13.5 a.6 56.8 108 30

.5 7.4 7.6 45.7 ~30 23

.8 11.0 1.2 6.5 55 14

.5 10.0 a.4 47.0 41 28

.8 6.9 6.6 44.6 42 18

.4 7.5 7.2 39.4 ~30 23

.6 10.7 7.4 34.6 ~30 25

.7 9.7 10.2 46.2 53 29

.a 11.1 a.3 36.9 50 25

.7 11.4 9.9 52.2 66 27

.8 8.5 9.2 60.0 44 23

.7 9.4 6.8 35.2 67 24

.b 10.0 7.1 36.9 51 24

I.0 7.9 9.6 125.6 67 22 I.1 8.5 14.1 77.3 63 21

.7 10.6 7.7 53.9 105 21

.8 14.4 a.4 77.5 100 24

.6 12.7 7.6 53.9 112 21

1.1 8.8 9.8 81.6 42 27 .7 10.6 7.5 61.9 41 34 .b 10.6 8.7 54.6 69 34 .7 47.4 9.6 67.6 55 43 .7 a.0 b.B 56.0 51 26

.8 10.1 7.1 50.4 95 23

.P 9.3 7.3 42.2 60 23

.9 b.8 7.1 90.6 96 21

.0 8.1 7.2 63.6 58 24

.8 a.2 7.2 69.7 70 26

7 214 2.29 1.6 ~5 2 15 .12 .3 9 207 2.63 2.1 7 2 14 .,o .3

10 437 2.58 2.7 ~5 1 15 .23 .3 8 244 2.40 2.7 5 2 17 .16 .4 9 214 2.58 2.8 <5 3 23 .lO .3

9 197 2.78 4.0 ~5 3 ia .09 .4 a 239 1.99 2.1 <5 1 26 .15 .2 8 465 2.39 2.5 ~5 1 29 .22 .2 7 la2 2.34 2.0 ~5 2 la .06 .3 3 210 .21 c.5 6 <l 178 .47 .2

7 198 2.59 3.3 ~5 2 33 .Ob .3 6 744 1.93 1.3 ~5 1 16 .09 .3 7 154 2.05 2.5 ~5 2 13 .05 .3 7 164 2.06 1.9 ~5 3 17 .04 .2 7 208 2.14 2.0 ~5 3 20 .ll .3

7 166 1.96 2.5 10 3 17 .oa .5 8 194 2.47 1.7 ~5 3 17 .lO .4 9 212 2.43 1.4 ~5 2 19 .lD .3 6 202 1.65 1.5 ~5 1 18 .09 .4 5 213 1.69 1.4 ~5 2 la .09 .3

8 775 2.lb .5 5 1 22 .61 .3 8 497 2.91 1.2 ~5 ~1 33 .74 .4 b 250 l.aD ,.I ~5 ~1 60 .31 .4 8 359 1.65 .7 ~5 ~1 55 .5b .4 6 262 1.59 .6 ~5 ~1 52 .27 .4

9 227 2.53 c.5 <5 2 17 .24 .3 10 413 2.70 1.0 ~5 4 2D .I7 .3

8 259 2.51 1.7 ~5 4 19 .16 .4 6 149 2.18 c.5 a 1 22 .I5 .2 7 233 1.97 c.5 ~5 2 19 .I2 .3

8 183 1.85 c.5 q5 cl 23 .19 .4 a 263 1.97 .5 <5 2 18 .13 .4 7 220 1.75 c.5 <5 1 18 .25 .2 8 201 2.26 1.0 5 2 17 .lD .3 9 2L7 2.62 .6 ~5 2 17 .ll .2

.2 51 .25 .031 15 35 .5D 245 .lO ~3 1.54 .O, .05 <2 <.2 <,D <.3 c.2 4.6 1

.2 62 .22 .039 14 SD .63 196 .ll ~3 1.68 .O, .06 <2 c.2 10 c.3 c.2 5.4 4

.2 56 .27 .086 13 34 .39 245 .08 5 1.58 .O, .07 ‘2 c.2 12 c.3 c.2 5.7 <l

.I 54 .29 .074 13 32 .42 192 .08 d 1.43 .Ol .07 ~2 c.2 40 s.3 s.2 4.7 ~1

.I 49 .44 ,033 18 39 .53 2336 .ll 3 1.50 .02 .07 2 S.2 19 <.3 <.2 4.5 1

.2 53 .32 .059 16 39 .54 155 .I0 ~3 1.51 .Ol .07 ~2 s.2 40 c.3 c.2 4.5 ~1

.2 37 .57 .Ob8 14 31 .52 232 .07 3 1.10 .02 .07 ~2 .2 16 q.3 q.2 3.8 ~1

.2 45 .64 .Ob4 18 37 .54 313 .08 ~3 1.34 .02 .07 ~2 c.2 ~10 c.3 c.2 4.3 ~1 .2 48 .32 .025 13 35 .51 1% .10 G 1.38 .Ol .05 ~2 c.2 cl0 s.3 c.2 4.4 ~1 .l 6 5.51 ,078 1 4 .37 840<.01 13 .15 .Ol .02 <2 c.2 56 1.6 c.2 .8 ~1

.2 SD .60 .035 18 39 .57 260 .ll 4 1.47 .03 .06 ~2 c.2 24 .3 s.2 4.7 1

.l 45 .27 ,031 13 29 .39 198 .OB 3 1.23 .Ol .04 <2 c.2 00 s.3 s.2 4.0 ~1

.l 45 .20 .027 13 33 .45 la9 .08 <3 1.34 .O, .D4 <2 c.2 12 c.3 c.2 4.1 cl

.I 43 .29 .039 18 34 .50 164 .09 <3 1.38 .oi .05 ~2 c.2 15 c.3 q.2 3.8 <I

.2 44 .3b .060 17 34 .52 204 .08 ~3 1.42 .Ol .07 ‘2 c.2 14 q.3 <.2 4.2 <l

.3 43 .28 .027 17 33 .44 204 .08 3 1.32 .Ol .06 <2 .2 ~10 c.3 c.2 3.7 1

.2 52 .2b .036 18 37 .51 186 .09 <3 1.62 .Ol .07 ‘2 .2 ~10 c.3 <.2 4.8 1

.2 57 .2a ,034 lb 38 .50 231 .ll ~3 1.75 .Ol .05 ~2 c.2 ~10 <.3 c.2 6.7 cl

.l 41 .30 .050 13 26 .32 213 .07 3 1.18 .Ol .,O ~2 .2 19 <.3 <.2 3.2 ~1

.l 41 .32 ,052 13 27 33 213 .07 <3 1.22 .O, .,l ~2 .2 19 c.3 q.2 3.6 ~1

.I 48 .3b .D58 12 29 .37 339 .07 4 1.44 .Ol .07 <2 .2 <lo c.3 <.2 5.0 3

.I 63 .78 ,098 14 29 .75 637 .Ob 5 1.85 .Ol .07 ‘2 .3 27 c.3 c.2 5.5 cl

.2 43 2.02 .Db5 13 28 .80 330 .07 5 .96 .Ol .06 ~2 c.2 SD .3 q.2 2.7 ~1

.I 38 l.4b ,074 12 26 .54 305 .Ob 5 .91 .oi .oa ‘2 c.2 62 .4 c.2 2.8 ~1

.I 37 1.29 ,083 12 26 .49 306 .Ob 6 .83 .Ol .07 ~2 c.2 53 .4 c.2 2.6 cl

.I 58 .2b ,065 16 35 .4b 240 .08 ~3 1.74 .Ot .05 ‘2 .3 24 <.3 <.2 5.8 cl

.I 57 .31 ,070 16 44 .57 201 .ll ~3 1.70 .02 .OP ~2 .2 12 s.3 c.2 4.7 ~1

.2 51 .32 ,064 18 39 .51 la9 .09 ~3 1.62 .Ol .08 ‘2 .2 ~10 c.3 <.2 4.6 ~1

.I 43 .3b ,040 17 38 .57 247 .09 3 1.63 .02 .oa <2 .3 59 c.3 c.2 4.9 <I

.I 46 .34 ,050 14 31 .38 280 .OP ~3 1.39 .Ol .Ob ~2 .2 16 c.3 s.2 4.5 1

.I 40 .44 ,073 13 28 .3a 235 .07 ~3 1.26 .Ol .07 ~2 .2 13 c.3 c.2 4.1 22

.2 48 .31 ,033 14 30 .32 280 .08 3 1.37 .Ol .Ob <2 .3 ~10 c.3 c.2 4.5 1

.2 41 .32 ,083 11 26 .28 270 .07 ~3 1.40 .Ol .Ob ~2 .2 12 c.3 c.2 4.7 ~1

.2 49 .29 ,098 15 33 .46 234 .08 4 1.58 .O, .05 ‘2 .2 ~10 c.3 c.2 5.1 1

., 57 .33 ,084 14 39 .54 222 .lO <3 1.68 .o, .07 <2 .2 12 c.3 ‘.2 5.4 Cl

i.4 114.2 94.5 249.9 1846 30 14 957 4.30 68.7 25 15 59 1.99 8.5 22.3 70 .70 ,104 16 52 7.14 244 .14 26 2.24 .05 .b7 lb 2.2 453 .5 1.9 6.7 51

Standard is STANDARD DZ/HG-SOO/AU-S. Sawles kinning 'RE' are Reruns and 'RRE' are Rejecr Reruns.

ALI results are considered the confidential properry of the client. Acme .~smes the Liabilities for actual cost of the analysis only. Data- FA _

-

1

Tizard Explorations Inc. TCHIKA FILE # 97-3778 Page 10 .K ."", "Tll.

AC3N 300E AC3N 350E AC3N 400E ADN 450E AC3N 500E

AC3N 600E ADN 650E AC3N 700E AC3N 750E AC3N 800E

AC3N 850E AC311 POOE AC3" 950E AC3" TOOOE ADW 105OE

AC3N 1lOOE RE AC3W 1lOOE AC3N 1150E AC3N 12OOE AC3N 1250E

AC3N 1300E AC3N 1350E AC3N 1400E AC3N 1450E AC3N 15OOE

AC3N 1550E AC3N 1600E AC3N 1650E AC3N 1700E AC3N 1750E

no C" Pb 2n Ag Ni Co Nn Fe AS U Th ST Cd Sb Bi V Ca P LS cr Ng Ba Ti B Al Na K ,, TL "9 Se Te Oa AW

pn mw wmF+wmppn ~mppnFwppnFFppnwFF % %ppnppn %ppn %m % % ~FvFmppbFPppnmP

.O 9.7 8.0 59.4 40 28 9 181 2.60 3.7 ~5 4 14 .09 .2 .1 51 .21 .069 12 39 .53 207 .OP <3 1.64s.01 .05 ~2 q.2 40 c.3 c.2 5.1 4

.9 6.5 8.8 49.0 43 18 6 131 1.76 2.3 ~5 3 14 .,1 .2 .I 42 .26 .065 12 26 .36 188 .06 ~3 1.28S.01 .03 -~2 c.2 40 S.3 c.2 5.0 2

.O 10.9 9.1 81.7 6, 29 11 251 2.8, 4.1 ~5 5 12 .23 .4 ., 55 .20 .I28 13 38 .49 161 .08 ~3 1.75s.01 .05 ~2 c.2 40 c.3 <.2 5.7 6

.5 8.2 1.5 10.8 35 9 3 4324 .22 c.5 ~5 1 207 .47 .4 c.1 5 6.71 ,095 1 4 .37 9&C .Ol 6 .26<.0, .O, <2 c.2 58 .6 c.2 1.2 Cl

.7 8.8 2.4 21.5 38 13 7 2188 .93 1.0 ~5 ~1 182 .33 .3 c.1 16 4.34 ,105 4 10 .44 663 .Ol 6 .45 .02 .03 ~2 c.2 41 .L c.2 1.8 1

.2 6.1 .7 13.4 ~30 6 1 152 .ll c.5 ~5 I 219 .34 c.2 c.1 4 9.30 .067 1 2 .36 715c.0, 14 .09 .O, .02 <2 c.2 35 .9 c.2 c.5 1

.5 5.8 7.5 54.5 ‘3 19 5 209 1.52 1.4 ~5 2 20 .I6 .2 ., 35 .43 .042 1, 25 .36 203 .07 <3 1.12 .Ol .05 ~2 c.2 13 c.3 c.2 4.4 1 .9 7.3 8.8 43.3 73 19 6 140 1.83 1.9 ~5 3 15 .I2 .3 .3 44 .26 ,028 1, 28 .40 166 .08 G 1.25s.01 .05 ~2 .2 40 c.3 c.2 4.7 <I .8 7.3 8.5 62.7 ~30 20 7 172 2.15 2.0 ~5 3 15 .,I .2 .1 46 .26 .044 14 32 .44 191 .09 ~3 1.38q.01 .05 ~2 .2 40 c.3 c.2 5.6 2 .9 9.8 8.3 57.0 35 26 7 204 2.08 2.2 ~5 4 18 .09 .3 .I 45 .32 .037 15 31 .48 247 .08 ‘3 1.54 .Ol .06 ~2 c.2 14 q.3 <.2 4.9 1

.6 8.2 8.6 59.1 54 26 8 284 2.15 2.0 ~5 3 17 .,o .2 .l 46 .29 .032 14 32 .47 219 .09 ~3 1.47c.01 .06 ~2 c.2 11 c.3 <.2 4.9 1

.5 6.3 8.2 44.8 <30 18 6 148 1.75 l.2 ~5 3 15 .06 <.2 .2 4, .24 .027 13 27 .39 187 .OP <3 1.22c.01 .03 ~2 .2 10 c.3 c.2 5.1 <I

.5 7.1 8.2 43.1 ~30 20 7 149 1.86 1.7 c5 3 15 .03 c.2 .2 46 .24 ,018 14 30 .45 193 .09 <3 1.39c.0, .03 ~2 <.2 40 c.3 <.2 5.0 -4

.5 8.4 9.8 51.9 76 19 8 171 2.04 2.4 -c5 3 16 .08 .2 .2 48 .25 ,021 14 32 .46 199 .,O ~3 1.47 .Ol .04 ~2 .2 <lo c.3 c.2 5.9 1

.6 10.8 8.8 47.7 36 22 6 164 1.94 2.6 ~5 4 17 .04 .2 .2 43 .30 .037 15 32 .49 172 .OP <3 1.30 .O, .05 <2 .2 <lo c.3 c.2 5.1 1

.8 12.3 8.0 33.8 ~30 17 6 161 1.72 1.4 ~5 2 23 .05 .2 .I 40 .33 .036 12 27 .35 236 .05 ~3 1.21 .Ol .05 ~2 c.2 16 c.3 c.2 4.2 1

.7 11.4 7.7 33.1 46 20 6 161 1.71 2.2 ~5 3 25 .06 .4 ., 41 .34 ,036 13 28 .35 237 .06 <3 1.27 .Ol .05 <2 c.2 40 c.3 <.2 4.4 4

.3 7.6 8.0 45.3 49 18 6 168 1.85 1.5 ~5 2 16 .05 c.2 ., 43 .28 .043 12 30 -32 240 .O, x3 1.54 .O, .04 ~2 c.2 17 c.3 c.2 5.9 <I .4 16.L 9.7 57.5 72 32 9 266 2.76 2.5 ~5 4 30 .06 .2 .2 50 .58 .038 19 36 .58 369 .09 ~3 1.70 .02 .06 ~2 .2 19 c.3 c.2 6.1 1 .6 10.6 9.1 57.2 39 34 9 256 2.52 2.7 ~5 4 16 .,l .2 .2 49 .29 .,35 13 37 .47 278 .08 <3 1.73 .Ol .08 ~2 c.2 14 c.3 c.2 6.3 4

.8 8.5 8.2 53.1 ~30 30 8 289 2.54 3.1 ~5 3 17 .I0 .2 .I 51 .33 ,100 13 35 .51 178 .08 ~3 1.52 .Ol .08 ~2 .2 cl0 c.3 <.2 5.3 1

.7 9.8 7.8 59.3 ~30 35 10 208 2.88 3.8 ~5 5 17 .I0 .3 ., 58 .33 ,084 16 40 .58 172 .,O ~3 1.69 .Ol .07 ~2 .2 1L c.3 c.2 5.8 <l

.6 8.3 6.3 36.6 ~30 22 6 188 1.83 1.9 7 3 14 .07 .2 <.I 4, .22 ,031 12 30 .35 146 .08 ‘3 ,.I,~.01 .09 ~2 .2 15 s.3 c.2 3.8 <l

.6 8.0 6.1 47.0 59 25 7 197 1.98 2.0 ~5 4 16 .07 .2 ., 45 .26 .03, 14 3, .4‘ 197 .09 <3 1.32 .Ol .07 ~2 .2 <IO c.3 c.2 4.5 4

.9 9.2 6.2 38.2 40 19 5 196 1.45 1.9 <5 3 17 .05 .3 ., 35 .26 .036 14 24 .33 187 .08 <3 .92 .Ol .05 ~2 .3 14 s.3 c.2 3.7 3

i .4 5.8 6.5 65.7 63 21 7 262 1.69 1.0 ~5 3 14 .09 <.2 .l 40 .22 ,030 12 27 .37 243 .08 <3 1.38 .01 .03 ‘2 .2 ~10 q.3 c.2 4.7 1 _ .6 7.6 7.0 93.6 40 25 8 235 2.14 1.1 <5 3 15 .,3 c.2 .I 46 .25 .055 ,2 32 .42 299 .08 ~3 1.50 .Ol .04 ‘2 c.2 12 c.3 c.2 5.2 1

.4 7.8 7.7 62.4 52 24 8 201 2.19 2.1 ~5 4 15 .07 c.2 ., 48 .27 .033 14 34 .48 205 .,O ~3 1.47 .01 .05 ~2 .2 10 c.3 c.2 5.4 <I ~ : .4 7.1 7.0 38.9 ~30 18 5 159 1.53 l.L <5 3 15 .06 c.2 ., 37 .25 ,030 13 25 .36 202 .07 ~3 1.19c.01 .03 ~2 .2 40 c.3 c.2 4.2 1

.2 8.6 7.0 54.7 97 22 6 200 2.04 1.8 <5 4 17 .06 q.2 .1 43 .30 .043 14 32 .50 174 .09 ~3 1.27 .O, .06 ~2 .2 14 c.3 c.2 4.6 1

AC3N 1800E .4 10.8 7.9 51.2 55 24 7 228 2.13 2.2 ~5 4 16 ,119 .2 .2 43 .28 ,032 13 32 .47 183 .09 <3 1.33 .O, .05 ~2 .3 13 c.3 <.2 5.1 AC3N 1850i ~ .3 8.6 6.5 47.0 42 23 7 183 1.76 1.8 <5 3 15 .07 .2 .l 36 .27 .049 12 27 .43 152 .07 3 1.03 .o, .05 <2 .2 11 s.3 c.2 3.8 AC3N 1900i i .6 8.2 7.0 L6.1 ~30 23 9 208 2.34 2.1 6 4 16 .08 .2 ., 49 .25 ,035 14 33 .47 196 .09 <3 1.46 .O, .05 ~2 c.2 cl0 c.3 c.2 4.8 AC3N 1950E ~ .6 7.6 6.5 34.3 ~30 16 6 252 1.49 .7 6 2 12 .lO .2 .I 32 .20 .048 11 2, .30 186 .04 <3 1.03 .Ol .05 ~2 .2 17 c.3 x.2 3.8 AC3N ZOOOE .4 8.5 7.2 42.4 ~30 22 8 196 2.30 2.6 6 4 17 .05 .2 .2 47 .29 .025 14 35 .47 187 .lO 4 1.34 .Ol .07 <2 <.2 10 c.3 c.2 4.4

STANDARD 02," i23.2 114.3 94.4 247.9 1867 30 14 945 4.30 65.5 23 17 58 2.03 10.2 22.0 70 .68 .101 17 52 1.12 242 .14 26 2.26 .04 .68 17 2.5 446 .6 2.3 7.7 47

Standard is STANDARD OZ/HG-500/AU-5. Samples beqinninq 'RE' are Reruns and 'ME' are Reiecr Reruns.

All resulrs are considered the confidential property of the client. Acme assumes the liabilities for actual cost of the analysis only. Data- FA _


AWN 2050E AC3N 2lOOE AC3W 2150E AC3Y 2200E ADN 2250E

AWN 23OOE AWN 2350E ADN 2400E AC3N 2450E AUN 2500E

AC3N 2550E NE At3W 2550E ADN 26OOE ADN 2650E AC3N 2700E

ADN 2750E AUN 28OOE AC3N 2900E AC3N 2950E AC3N 300DE

AOlN DE AOlN 50E AOlN 1OOE ADIN 150E AOlN 200E

ADlN 250E AOlN 3OOE AOlN 350E AOlN 400E AOlN 450E

AOlN 500E kOlN 60OE AOlN 650E AOIN 700E ROIN 750E

Page 11 '49

STANDARD 02/H

.B 0.7 7.5 51.3 <30 24 9 221 2.63 3.6 5 4 15 .lO .3 .l 54 .25 .058 14 36 .50 181 .09 3 1.47 .O, .OS ~2 c.2 11 c.3 c.2 5.7 ~1

.B 9.3 10.2 121.4 64 32 11 237 3.39 2.2 <5 3 14 .33 .4 .l 64 .22 .073 12 41 .47 239 .,O 4 1.93 .O, .06 ~2 c.2 40 c.3 c.2 7.9 I .a 6.5 8.0 39.1 30 15 5 206 1.80 1.9 ~5 3 16 .12 .2 .l 44 .2b .017 13 26 .32 217 .07 ~3 1.18 .Ol .04 <2 c.2 ~10 c.3 s.2 5.1 1 .E 9.5 10.7 90.8 39 29 1, 241 2.93 3.5 ~5 3 15 .32 .4 .l 57 .23 .06-S 14 37 .49 231 .I0 ~3 1.78 .O, .06 ~2 c.2 40 s.3 c.2 7.0 1 .7 7.7 9.9 76.1 41 26 IO 174 2.51 2.5 ~5 3 14 .28 .3 .1 52 .25 .I09 14 33 .39 193 .08 5 1.64s.01 .O4 ~2 c.2 ~10 q.3 c.2 6.2 2

1.0 10.3 8.5 49.7 51 30 9 194 2.45 4.0 <5 4 I4 .ll .4 ., 48 .22 ,078 14 36 .46 153 .OB <3 1.55 .Ol .05 s2 c.2 <,o s.3 c.2 4.9 2 .b 6.4 8.0 62.1 46 22 7 173 2.16 1.6 5 3 15 .I0 .3 .I 46 .25 .O54 14 32 .39 190 .09 <3 1.44 .Ol .05 <2 c.2 18 c.3 c.2 5.4 4 .b 7.4 7.4 45.1 59 21 7 159 1.96 2.1 ~5 3 14 .Ob .2 .I 41 .20 .036 13 31 .39 155 .09 ~3 1.24 .Ol .05 <2 c.2 40 c.3 c.2 4.0 1 .5 a.5 a.4 61.3 86 24 7 307 2.29 1.9 ~5 3 20 .OP .2 .l 43 .34 .024 13 33 .40 288 .OP <3 1.40 .Ol .OB ~2 c.2 24 c.3 c.2 4.7 1 .6 9.1 0.0 39.2 <30 19 7 170 1.93 3.2 ~5 3 18 .06 .3 c.1 43 .28 .032 14 32 .41 185 .08 <3 1.34 .Ol .05 ‘2 s.2 <,o c.3 c.2 4.8 3

.b 9.0 8.5 45.8 53 26 9 245 2.50 4.1 ~5 4 15 .Ob .3 <.l 52 .23 ,042 16 38 .47 182 .lO 3 1.G .Ol .Ob ~2 q.2 10 c.3 c.2 5.1 2 .7 9.5 9.1 46.6 58 29 9 244 2.51 3.9 <5 4 16 .07 .3 .l 52 .24 ,043 16 38 .47 187 .lO ~3 1.65 .Ol .06 ~2 c.2 15 c.3 c.2 5.6 1 .9 7.1 7.4 39.3 68 21 8 2M 2.03 2.7 ~5 3 lb .ll .3 ., 39 .31 .031 12 29 .35 150 .08 <3 1.15<.01 .09 ‘2 c.2 40 c.3 c.2 4.1 Cl

1.1 14.5 a.2 44.4 141 24 8 807 1.73 2.4 ~5 ~2 50 .30 .3 .l 35 1.14 .D42 10 24 .32 552 .05 6 1.08 .Ol .06 ~2 c.2 40 .8 c.2 3.8 ~1 1.0 5.6 7.4 64.1 63 21 6 248 1.69 .9 <5 2 lb .18 .2 c.1 37 .29 .059 10 24 .26 226 .07 3 1.13‘.01 .Ob <2 q.2 20 c.3 c.2 4.3 ~1

1.0 12.0 9.7 72.8 58 25 8 385 2.10 1.9 ~5 ‘2 29 .23 .3 .l 39 .60 ,046 15 29 .47 269 .06 <3 1.3, .Ol .OP ~2 c.2 15 .3 c.2 4.3 1 1.1 20.9 9.4 58.9 178 32 9 895 2.06 4.5 ~5 ~2 67 .39 .5 .l 41 2.17 ,081 14 29 .74 4,b .Ob 4 1.01 -01 .07 <2 ~2 60 1.0 c.2 3.5 1

:; 8.6 8.5 11.5 10.2 88.8 99.0 45 52 19 11 6 8 276 249 2.21 1.87 1.6 1.3 <5 6 ~2 ~2 23 19 .61 .38 .2 .2 c.1 c.1 52 48 .37 .28 ,078 ,093 13 11 31 26 .42 .3l 405 244 .06 .05 ~3 ~3 1.60 1.33 .Ol .Ol .Ob .05 ~2 ~2 q.2 q.2 18 10 q.3 c.3 c.2 C.2 4.8 4.4 2 1 1.1 9.0 9.6 132.5 57 30 9 442 2.66 2.8 <5 3 20 .34 .3 <.I 56 .34 .Oi'5 13 37 .44 275 .,O ~3 1.86 .Ol .Ob ~2 q.2 18 c.3 c.2 6.3 ~1

.5 10.7 a.2 33.6 56 23 7 132 2.02 2.3 ~5 4 19 .04 .2 .l 43 .37 ,045 16 35 .47 216 .OP <3 1.30 .Ol .04 C2 C.2 15 c.3 c.2 4.3 <l 1.1 10.0 8.2 83.7 42 25 11 344 2.58 2.6 <5 3 13 .19 .3 c.1 50 .22 ,094 12 35 .43 162 .08 ~3 1.52 .Ol .05 ~2 q.2 ~10 s.3 c.2 5.3 1

.9 10.0 5.6 26.7 120 13 3 151 1.13 2.1 <5 <2 37 .23 .3 .l 26 1.05 ,035 8 18 .2, 260 .04 3 .b8 .D, .03 ~2 q.2 23 .3 c.2 2.7 1

.9 10.4 5.7 26.9 59 17 4 153 1.20 3.3 <5 <2 39 .I1 .4 c.1 29 1.74 ,044 11 21 .41 423 .04 3 .b4 .Ol .03 ~2 c.2 25 .4 c.2 2.1 1 .9 9.3 I., 22.1 51 5 3 357 .24 .5 ~5 ~2 183 .60 .4 c.1 5 5.76 ,076 1 2 .3, 1063<.Dl 12 .14 .Ol .04 <2 c.2 40 2.4 C.2 1.1 1

1.1 13.5 4.9 30.9 146 18 4 176 1.05 3.3 ~5 <2 i-7 .33 .5 <.I 27 4.63 .054 9 20 .54 211 .04 4 .49 .Ol .05 ~2 q.2 52 c.3 c.2 1.8 3 .8 6.4 6.9 38.6 ~30 lb b 113 1.91 1.5 ~5 2 12 .14 .2 c.1 44 .25 .082 IO 27 .26 126 .Ob ~3 1.12<.01 .04 <2 s.2 13 q.3 <.2 4.4 1

1.3 10.3 8.6 45.1 81 25 7 311 1.73 2.9 <5 2 21 .29 .4 c.1 37 .47 .053 13 26 .32 275 .Ob ~3 1.02 .Ol .05 <2 c.2 21 c.3 <.2 3.6 1 .7 10.7 2.8 24.4 106 9 3 310 .61 1.6 ~5 ~2 135 .39 .5 s.1 11 4.53 ,064 4 8 .2b 904 .02 7 .35<.0, .03 s2 c.2 47 1.5 c.2 1.7 4 .8 9.1 1.1 13.6 59 7 5 321 1.79 8.8 <5 ‘2 208 .41 .4 c.1 7 5.27 .071 2 3 .28 1328 .Ol 5 .3D .02 .Ol <2 c.2 22 3.9 c.2 1.2 Cl

.5 7.7 1.3 4.7 45 5 1 17 .21 .5 8 ~2 126 .2b .4 c.1 6 3.22 ,045 2 2 .21 633 .Ol 5 .27 .02 .Ol ~2 c.2 22 1.0 c.2 1.2 2 I.8 13.8 1.0 7.6 111 9 2 136 .48 2.0 ~5 ~2 190 .43 .3 c.1 6 4.32 ,138 2 4 .20 720 .o, 11 .23 .Ol .Ol s2 c.2 44 1.0 c.2 2.0 <l 1.7 25.7 11.4 71.9 133 37 11 330 2.73 b.1 ~5 2 81 .2a .7 .I 44 3.27 ,040 18 34 .77 397 .04 3 1.55 .Ol .08 ~2 s.2 32 .7 c.2 4.5 2

.9 9.0 6.2 51.0 52 23 8 289 2.02 2.4 ~5 3 18 .lO .3 .I 48 .32 .D34 14 32 .4, 196 .09 ~3 1.37 .Ol .06 C2 c.2 13 c.3 c.2 4.7 1

.a 4.9 6.4 63.3 65 16 7 273 1.92 1.0 ~5 2 15 .I5 .2 .l 46 .26 .037 12 28 .32 205 .09 ~3 1.28 .Ol .05 <2 c.2 14 c.3 c.2 4.6 cl

3.3 116.3 92.9 255.3 1936 29 Ib 957 4.35 66.1 21 17 58 2.07 8.9 22.0 68 .69 .,04 17 53 1.13 245 .14 24 2.20 .05 .68 16 2.3 446 .5 2.0 7.3 54 ~

Srandard is STANDARD DZ/XG-SOO/AU-S. Samples beqinning 'RF' are Reruns and 'RRE' we Reject Remms.

ALL results we considered the confidential property of the client. Acme ~SSMS the liabilities for actual cost of the analysis only. Data- FA _

c Tizard Explorations Inc. PROJECT KETCHIKA FILE # 97-3770

ADIN BODE ADlN a5DE ADIN 9DDE

.? 8.3 7.8 60.7 51 27

.9 7.5 7.2 40.3 <30 24 !.2 20.7 10.8 64.3 232 47

.a 9.2 a.0 76.5 78 27

7 335 2.20 1.0 6 4 17

.6 8.1 7.8 56.4 37 24

.B 9.4 8.7 56.6 ~30 27

.a 5.9 7.7 45.2 ~30 17

.6 9.1 a.7 54.9 52 25

.5 8.6 7.9 60.8 ~30 23 .7 7.1 7.2 40.0 ~30 22

7 225 2.27 1.8 4 2 ia 10 2a2 2.79 4.7 ~5 4 19

8 427 2.43 1.9 ~5 2 15

.13

.ll

.lD

.16

.12

C.2 .2 47 .30 .02a

a 202 2.18 1.3 ~5 2 15

.2 .I 50 .33 .031

.? .1 54 .33 .039

.2 .2 50 .25 .029 <.2 .2 48 .25 .021

14 34 .48 285 .I0 4 1.61 .02 .05 ‘2 <.2 13 <.3 c.2 4.6 ~1 12 33 .4a 265 .Da <3 1.40 .Dl .04 e2 .2 ID c.3 <.2 4.8 2 28 41 .44 221 .05 C3 1.39 .Dl .13 <2 .2 99 .4 C.2 3.5 3 13 37 .43 224 .lD <3 1.64 .Dl .05 ~2 s.2 24 c.3 c.2 5.2 1 13 33 .46 243 .Da <3 1.45 .02 .04 ~2 .2 17 c.3 s.2 4.2 1

7 263 2.32 2.0 ~5 3 16 .11 C.2 .2 48 .29 .027 13 34 6 199 1.70 1.1 5 1 14 .ll C.2 .1 41 .25 .023 11 25 9 288 2.36 1.9 ~5 1 24 .12 .2 .I 47 .48 .040 16 36 7 254 1.97 1.0 ~5 1 19 .15 q.2 .I 42 .33 ,039 12 31 6 145 2.14 1.5 ~5 3 14 .D? .2 .I 50 .22 ,026 13 33

.9 30.5 9.5 106.5 391 57 12 1421 2.71 1.3 ~5 <l 53 1.48 .3 .2 46 1.18 .212

.? 7.0 6.9 46.3 34 23 7 260 2.07 .a ~5 1 19 .I? .2 .l 45 .35 .036

.? 7.4 7.4 56.6 51 25 8 273 2.29 1.1 ~5 2 16 .15 .2 .I 49 .26 .045

.? a.9 a.4 47.9 C3D 25 a 181 2.27 1.9 ~5 3 15 .D9 .2 .2 50 .24 .029

.6 7.3 a.3 53.4 63 17 5 165 1.82 .9 <5 1 22 .07 C.2 .I 44 .37 .D23

35 40 12 32 12 34 14 35

I.3 7.4 7.6 43.9 54 14 .a 7.3 7.3 43.5 a2 16

1.3 7.9 6.1 30.6 ~30 13 I.3 10.9 9.7 67.7 134 21 1.4 8.4 6.8 42.2 49 18

13 29

4 108 2.00 2.3 <5 1 12 5 loa 1.94 1.3 ~5 1 11 3 a2 1.59 1.6 <5 1 12 6 425 2.01 1.9 5 1 26 5 134 1.98 1.7 ~5 1 12

.I6

.16

.14

.31

.23

.3 .2 53 .I? ,042

.4 .2 52 .lb .042 11 27 11 26

9 25 13 30

4 226 1.01 7.2 ~5 4 16 .38 B 339 1.95 2.9 ~5 ~1 61 .48 6 391 1.27 .a e5 ~1 18 .23 6 374 1.70 1.6 c5 Cl ia .,I 7 238 1.93 1.4 ~5 2 17 .I0

.4 <.I 45 .ia .043

.4 .2 45 .52 .046

.3 <.I 51 .22 .041 9 28

1.4 7.4 6.1 60.3 101 14 I.1 8.8 6.9 48.7 101 24

.a a.9 6.4 48.1 93 24

.7 10.4 8.4 72.9 168 26

.? 9.7 5.1 43.1 46 24

.6 a.0 7.1 57.9 90 25

.6 5.7 5.7 44.3 67 17

.5 6.6 7.0 57.9 110 17

7 291 2.10 1.3 ~5 2 19 5 279 1.74 1.1 ~5 1 17 7 225 1.95 1.6 ~5 2 lb 5 19a 1.39 .9 C5 2 15 7 184 1.72 1.1 9 2 16

6 155 1.87 1.0 es 2 14 7 15a 1.86 1.0 a 2 14 5 226 1.68 .a ~5 2 14 5 230 1.57 1.1 7 2 13 7 243 1.99 1.2 C5 2 13

.23

.oa

.I0 .D6 .D6

.3 .I 28 .31 ,029 9 17 .24 149 .D4

.? .2 42 2.91 ,063 13 30 .a2 271 .D5

.3 .I 33 .30 ,034 9 21 .25 199 .05

.3 ., 45 .3, ,031 14 29 .30 313 .D6 .3 ., 42 .3D ,036 14 31 .43 199 .Da

.4 .2 43 .32 .D63 14 34 .46 214 .D9

.3 c.1 43 .3D .038 11 32 .Ll 149 .D7

.2 ., 43 .2E ,027 14 33 .46 189 .I0

.2 .I 37 .24 ,025 13 25 .35 182 .oa

.2 .I 41 .25 ,021 13 28 .44 182 .DP

.6 9.4 a.5 46.3 97 20

.a 6.1 7.6 52.9 88 18

.6 6.6 6.2 39.3 69 18

.4 6.2 6.0 43.2 60 17

.? 8.3 8.4 62.4 93 23

.DE

.06

.D4

.06

.DE

.3 ., 42 .23 ,025

.2 .I 46 .23 .022

.2 <.i 40 .23 .023 C.2 ., 37 .21 .021

.2 .I 45 .20 .028

12 30 .44 iao .oa 13 30 .42 195 .Da 12 28 .39 161 .D? 12 26 .38 163 .oa 12 30 .4D 179 .oa

ADIN 95DE ADIN 1DDDE

ADlW 105DE ADlN 1lDDE ADIN 115DE ADlN 12DDE ADlN 125DE

ADlN 13DDE

a 1.54 .Dl .05 <2 <.2 19 q.3 C.2 4.4 <l <2 s.2 I2 C.3 s.2 3.9 1 <2 <.2 33 C.3 C.2 4.5 4 ‘2 C.2 19 C.3 C.2 4.3 1 <2 .2 18 c.3 c.2 4.2 2

~2 <.2 48 .9 c.2 5.6 1 <2 <.2 CID s.3 C.2 3.9 <1 <2 s.2 12 C.3 C.2 4.7 Cl ~2 c.2 14 c.3 <.2 4.8 1 <2 C.2 21 C.3 C.2 4.9 2

<2 c.2 24 C.3 s.2 4.5 4

.51 254 .oa

.39 217 .D?

.45 364 .a7

.47 236 .oa

.42 164 .09

<3 1.19 .Dl .04 ~3 1.58 .DI .05 <3 1.41 .Dl .a5 <3 1.43 .Dl .04

5 2.63 .02 .09 .5D 935 .06 .39 219 .DP .42 214 .09 .47 207 .D9 .42 281 .oa

.27 124 .D?

.27 125 .07

.22 100 .Db

.36 359 .D?

.25 165 .06

~3 1.29 .Dl .07 3 1.48 .Dl .06

<3 1.51 .Dl .05 C3 1.59 .02 .04

ADlN 135DE ADIN 14DDE ADIN 145DE ADlN 15DDE

ADlN 155DE RE ADlN 155DE ADIN 16DDE ADlN 165DE ADlN 17DDE

ADlN 175DE ADIN la5DE ADlN 19DDE ADIN 195DE ADIN ZDDDE

ADIN 2D5DE ADtN 2lDDE ADIN 215DE ADIN 22DDE ADIN 225DE

~3 1.06 .Dl .04 <3 .a9 .oi .03 C3 1.36 .Dl .05

<2 c.2 24 c.3 c.2 4.1 2 <2 C.2 22 C.3 ‘.2 3.0 1 <2 s.2 27 <.3 C.2 4.3 3 ~2 c.2 26 c.3 ‘.2 3.8 5 <3 1.04 .Dl .04

~2 <.2 13 c.3 c.2 2.3 1 <2 .2 43 .3 C.2 3.3 1 <2 x.2 23 s.3 C.2 3.0 1 <2 C.2 17 C.3 C.2 3.4 3 ~2 c.2 10 4 c.2 3.8 2

C3 .67 .Dl .05 <3 1.07 .Dl .I4 <3 .a6 .Dl .D?

3 1.33 .Dl .07 <3 1.24 .Dl .D6

<3 1.34 .D, .D7 ‘2 C.2 20 C.3 C.2 4.9 1 C3 1.02 .Dl .05 ‘2 C.2 17 C.3 C.2 3.1 1 ~3 1.29 .Dl .D6 <2 C.2 15 C.3 C.2 4.1 4 ~3 1.08 .DI .D3 ‘2 C.2 40 C.3 C.2 3.7 15 ~3 1.23 .Dl .04 C2 C.2 40 C.3 <.2 3.9 1

~3 1.24 .Dl .D3 3 1.39 .Dl .03

<3 1.16 .Dl .04

<2 <.2 <ID C.3 C.2 4.4 <1 <2 C.2 14 C.3 C.2 5.1 3 ‘2 C.2 12 C.3 C.2 3.5 2 <2 C.2 12 C.3 C.2 3.7 1 ~2 c.2 18 c.3 c.2 5.3 i

ADIN 23DDE ADIN 235DE ADlN 24DDE ADlN 245DE ADlN 25DDE

~3 1.18 .DI .03 ~3 1.48<.01 .03

1.3 121.0 96.4 258.4 ,864 3, 15 ,DDD 4.5, 71.1 23 16 6, 2.05 1D.D 22.8 70 .?D .,D? 17 56 1.2, 253 .,4 23 2.31 .D6 .?D 17 2.3 516 .5 l.a 6.3 47 ~ !21 STANDARD 02/H

Standard is STANDARD DZ/HG-SOD/AU-S. Samples besinning 'RE' are Reruns and 'RRE' are Reiect Reruns.

ALI results are considered the confidential prqsrty of the client. Acme 8swmes the Liabilities for actual cost of the analysis only. oata- FA _

Tizard Explorations Inc. PROJECT TCHIKA FILE # 97-3778 Page 13 8.x UalmDI

AOIN 255OE .6 6.0 6.8 46.2 LO 21 7 173 1.96 1.8 ~5 1 15 .ll .2 ., 45 .22 .052 13 30 .40 171 .08 ~3 1.39 .Ol .05 <2 s.2 40 c.3 <.2 4.4 <I ADIN 2600E .7 6.4 7.4 40.3 71 17 7 288 1.84 1.8 s5 2 16 .I5 .3 .2 42 .27 .029 12 27 .38 193 .08 <3 1.24 .02 .06 <2 .2 <IO C.3 C.2 4.7 4 AOIN 2650E .9 8.1 9.5 64.1 41 21 0 236 2.64 2.5 ~5 3 16 .17 .2 .2 58 .24 .037 14 36 .47 18, .I0 <3 1.67 .O, .06 ~2 .2 <IO c.3 c.2 6.0 <I ADIN 2700E .7 5.3 7.7 45.0 32 13 6 370 1.60 1.1 ~5 1 14 .16 c.2 .2 43 .22 .026 12 23 .26 190 .07 ~3 1.29 .O, .03 ~2 c.2 Cl0 c.3 c.2 4.9 Cl AOIN 2750E .7 7.0 7.2 42.7 ~30 25 7 191 2.42 1.8 ~5 2 14 .07 .2 .I 53 .20 .033 14 35 .U 160 .I0 <3 1.86 .02 .03 ~2 .2 40 <.3 c.2 5.2 4

AOIN 2800E AOIW 2850E AOIN 2900E AOlN 295OE AOIN 3000E

NE AOIW 3300E AOIN 3050E AOIN 3100E ADlN 3150E AOIN 3200E

AOIN 3250E AOIN 3300E AOIN 3350E AOIN 3400E ADIN 3450E

AOIN 3500E AOlN 3550E AOIN 3600E AOIN 3650E AOIN 3700:

AOIN 3750E AOIN 3800E AOIN 38506 ADIN 3900E AOIN 3950E

AOIN 4000E AOZN OE AOZN 50E AOZN 1OOE AOZN 15OE

1.1 10.1 9.1 79.2 30 22 17 401 2.42 1.4 ~5 1 23 .30 .2 .3 55 .39 .034 .7 6.3 6.2 47.5 81 18 7 144 1.76 1.2 ~5 1 17 .14 .2 .2 43 .26 .037 .7 6.6 7.1 49.4 35 22 7 161 2.27 1.7 ~5 2 12 .I0 .2 .2 51 .17 .030 .7 6.4 7.4 65.8 <30 22 9 216 2.49 1.5 ~5 1 16 .26 .2 .2 53 .24 .081

1.1 9.1 6.6 46.0 <30 21 7 154 1.90 2.5 s5 1 13 .14 .3 .1 45 .I9 .038

.7 7.7 7.4 38.5 ~30 21 6 15a 1.76 1.6 c5 1 15 .oa .2 .2 u .23 ,034

.7 23.4 6.6 57.7 ~30 19 10 515 1.56 .7 6 Cl a-3 1.15 .3 .2 28 2.28 ,079

.8 5.4 .8 10.1 38 4 2 404 .64 .5 <5 4 186 .29 .3 .l 4 3.01 .I10

.9 15.3 4.8 32.5 ~30 16 6 531 1.34 2.7 ~5 ~1 119 .36 .2 <.I 16 3.06 ,070

.8 10.3 7.3 37.0 68 20 7 226 1.93 1.7 <3 2 20 .I1 .3 .2 44 .42 ,036

.34 475C.01

.36 410 .OB

15 34 .40 352 .08 13 29 .36 211 .08 12 34 .43 200 .09 13 33 .41 249 .09 12 28 .35 157 .07

15 30 .42 197 .oa 16 19 .23 786 .02

13 .34 77ac.01 6 18 .42 902 .02

12 29 .35 207 .07

<3 1.45 .Ol .04 <2 .3 40 C.3 C.2 4.7 1 3 1.19 .02 .03 ‘2 c.2 58 .6 q.2 3.0 Cl

10 .I0 .02 .03 <2 c.2 69 .6 c.2 .a 4 <3 .86 .Ol .02 ~2 c.2 33 1.0 c.2 3.4 <I <3 1.3, .O, .06 ~2 .2 24 c.3 c.2 3.9 cl

.5 6.8 7.5 62.0 57 23 8 217 2.16 1.2 q5 2 IL .14 .2 .2 48 .23 .063 13 32 .39 226 .08 ~3 1.53 .Ol .04 ~2 .2 cl0 c.3 c.2 5.0 Cl 1 17 .22 .2 .2 43 .28 .062 12 29 .40 259 .09 <3 1.44 .Ol .05 ~2 .3 <IO ‘.3 c.2 4.8 <l .6 5.8 7.3 83.2 52 22 a 414 2.05 .5 C5

.9 9.2 7.6 63.6 68 27 9 283 2.18 1.8 ~5 I 18 .22 .3 .2 46 .33 ,042 15 33 .48 269 .09 4 1.42 .02 .05 <2 .2 cl0 c.3 c.2 4.4 <I I 1.6 16.8 7.7 69.6 a9 38 9 735 2.33 3.1 C5 <I 28 .41 .4 .2 47 .49 .080 22 35 .48 352 .06 ~3 1.53 .02 .09 ~2 .2 34 c.3 c.2 4.0 1

~1 .a 8.7 7.2 56.7 a3 22 9 330 2.20 1.7 ~5 2 21 .I8 .3 .2 48 .34 .044 15 32 .42 257 .OP ~3 I.44 .Ol .07 ~2 .3 18 c.3 c.2 4.7

.3 6.8 7.7 51.7 79 19 7 192 2.11 1.2 ~5 2 15 .I5 .2 .2 46 .24 ,057 13 29 .41 197 .OP 3 1.34 .Ol .05 <2 C.2 Cl0 C.3 C.2 4.7 Cl

.6 9.1 6.8 38.1 71 20 6 157 1.95 1.9 ~5 1 22 .I1 .3 .2 41 .48 ,021 13 31 .43 276 .Oa 3 1.25 .O, .05 ~2 .2 14 c.3 c.2 4.1 2

.6 10.3 6.8 44.3 34 25 7 225 2.24 1.7 ~5 2 ia .oa .3 .2 47 .30 ,024 16 38 .48 256 .I0 4 1.50 .02 .05 <2 .3 10 C.3 C.2 4.4 <I

.8 10.1 7.3 56.4 30 28 9 312 2.29 1.8 ~5 3 17 .,I .3 .2 51 .29 ,031 14 36 .50 215 .,O <3 1.69 .Ol .05 <2 .3 <IO c.3 c.2 5.1 9

I 1.0 9.3 6.8 55.8 ~30 27 7 189 2.39 1.7 ~5 1 16 .I4 .3 .2 54 .24 ,034 13 36 .47 240 .lO <3 1.65 .Ol .05 ‘2 .2 14 c.3 c.2 5.3 cl

!2 !4.0 119.1 93.4 254.4 1767 31 16 962 4.35 70.7 18 16 59 2.12 9.1 23.9 69 .69 ,101 17 54 1.14 242 .I4 25 2.33 .06 .68 16 2.1 432 .5 1.8 6.3 44 STANDARD 02,"

.4 6.7 6.9 53.1 43 17 8 367 2.01 1.6 ~5 2 19 .,I 1.0 7.4 0.4 50.5 42 16 7 156 2.37 2.0 <5 1 17 .I5 1.2 11.9 10.1 43.0 80 13 6 161 1.86 1.4 ~5 Cl 12 .37

.9 6.0 7.4 43.2 70 13 5 116 1.99 1.4 ~5 1 13 .15 1.2 18.5 8.9 53.3 157 39 15 1517 2.38 1.9 ~5 ~1 62 .52

.9 6.8 7.6 44.1 68 14 7 146 1.68 1.3 ~5 1 16 .17 l:i 10.6 2.0 10.0 110 10 7 1674 .42 .7 C5 1 211 .46 1.8 5.8 .8 20.9 <30 a 2 898 .OB C.5 c5 4 137 1.02

.7 9.4 1.1 68.3 110 10 1 214 .23 c.5 ~5 -4 204 .90 1.0 8.7 8.2 62.2 67 23 11 767 2.14 .7 q5 1 28 .49

.2 .2 47 .27 ,041

.2 .2 54 .28 ,058

.3 .4 42 .I5 .I25

.3 .2 49 .20 .057

.L .2 48 1.40 .052

.2 .2 40 .25 ,037 .8 .I 16 6.27 ,113 .3 .l 7 4.37 .073 .2 C.1 4 5.49 .07a .2 .3 38 .50 ,122

14 30 .34 203 .OP 12 32 .38 195 .lO 12 23 .22 189 .08 12 28 .27 127 .Oa 25 33 .34 8.34 .07

12 26 2 11 12 2 4

11 28

.34 204 .07

.39 937C.01 .30 532c.01

<3 1.49 .o, .04 <2 .2 <IO C.3 C.2 4.7 4 ~3 1.60 .O, .05 <2 .2 <IO c.3 c.2 6.0 1 <3 1.15 .o, .05 <2 C.2 10 C.3 <.2 5.5 Sl <3 1.16 .Ol .04 ~2 .2 12 c.3 *.2 5.0 3 <3 2.08 .02 .06 C2 C.2 50 .7 C.2 4.8 2

<3 1.22 .Ol .04 C2 C.2 40 C.3 C.2 4.5 2 9 .24 .02 .03 ~2 .2 47 3.4 c.2 1.1 <I

1, .06 .Ol .05 ~2 <.2 74 .6 c.2 c.5 <I 12 .22 .Ol .02 ~2 s.2 32 .6 c.2 .B ~1

5 1.31 .OI .09 ~2 .2 15 c.3 q.2 4.8 1

<3 1.93 .Ol .05 <2 .2 28 .3 C.2 5.7 1 <3 1.29 .O, .05 <2 .3 40 c.3 c.2 L.0 1 <3 1.67 .O, .04 <2 .2 40 c.3 c.2 4.9 4 <3 1.62 .02 .05 ~2 .3 13 c.3 c.2 5.6 4 <3 1.33 .Ol .04 <2 .2 40 C.3 C.2 4.4 <I

Standard is STANDARD 02/WSOO/Au-S. Samles kginninq 'RE' are Reruns and 'ME' are Reiect Reruns.

ALI results are considered the confidential proprty of the client. Acme assums the Liabiliries for actual COST of the analysis only. Data- FA _

ADZN 2OOE AOZN 25OE AO2W 300E ADZ,, 350E ADZN 4oOE

ADZN 450E ADZN 500E AD2N 550E ADZN 600E ADZN 650E

AOZN 7OOE i78.4 14.3 S3.3 3.6 ~330 1 1 17 .lb <5.5 19 ~2 138 c.llc2.2 cl.1 2 3.75 .081 1 2 .15 23m.01 6 .08 .Ol .02 ~2q2.2 3bc3.3c2.2s5.5 1 AO2N 750E I 2.2 8.0 .9 32.3 44 3 2 230 .07 c.5 ~5 <2 197 .67 c.2 c.1 2 3.47 .107 1 2 .41 411s.0, 14 .05 .Ol .D4 ~2 c.2 62 .7 s.2 c.5 ~1 ADZN BOOE 1.7 10.3 6.8 41.1 65 18 6 172 1.40 4.4 ~5 2 19 .22 .5 .l 34 .36 .030 10 23 .29 148 .Ob ~3 .77 .O, .07 <2 <.2 29 .5 c.2 2.2 1 ADZN a50E 1.1 8.3 7.8 36.9 <30 la 6 197 1.82 4.0 ~5 2 16 .I5 .4 .I 43 .29 .027 11 28 .34 161 .08 <3 1.09 .Ol .05 ~2 C.2 14 .3 C.2 4.0 2 ADZN 900E ~ .9 9.7 a.7 40.1 36 22 7 187 1.83 4.3 ~5 3 lb .ll .4 .l 42 .29 ,022 15 30 .42 191 .08 ~3 1.23 .Ol .05 ~2 c.2 11 c.3 c.2 4.0 1

ADZN 95OE ADZN lOODE NE ADZN IOOOE ADZN 1050E AD2N 1lOOE

.7 10.0 a.7 41.1 ~30 23 8 205 2.20 4.7 5 4 16 .lO .3 .l 47 .30 .029 15 36 .49 218 .09 ~3 1.41 .O, .05 <2 <.2 17 <.3 c.2 3.8

.8 7.2 8.0 41.4 37 19 7 158 2.28 3.0 ~5 2 12 .13 .3 .l 49 .19 .053 13 33 .37 174 .09 <3 1.44 .Ol .05 ‘2 C.2 12 C.3 C.2 5.1

.9 7.8 a.6 42.9 51 20 7 159 2.31 3.0 6 2 13 .15 .3 .l 51 .20 .054 14 33 .37 176 .lO ~3 1.47 .Ol .05 ~2 c.2 lb c.3 c.2 5.8

.7 7.1 8.2 51.5 53 21 8 195 2.18 3.3 c5 3 15 .I1 .2 .l 49 .26 ,023 12 34 .42 191 .09 3 1.53 .Ol .03 <2 c.2 15 c.3 c.2 4.5

.b 8.3 a.5 43.7 C30 20 7 159 1.93 3.5 <5 3 15 .06 .2 .l 44 .26 ,022 15 32 .45 la4 .09 ~3 1.38 .Ol .04 ~2 c.2 26 c.3 c.2 4.5

.8 7.1 8.8 73.3 58 23 9 197 2.64 3.0 <5 3 17 .14 .2 .l 57 .26 .034 14 37 .4a 224 .12 ~3 1.73 .Ol .06 ~2 s.2 19 <.3 c.2 5.9 1.0 10.7 8.3 39.2 44 21 7 157 2.27 4.1 ~5 3 13 .lO .4 .2 49 .22 .040 13 32 .44 172 .08 ~3 1.39c.01 .05 ~2 c.2 15 s.3 c.2 4.8

.9 7.0 8.5 64.5 56 20 8 186 2.67 3.9 ~5 3 15 .lB .3 .2 55 .24 .025 11 35 .46 181 .lO <3 1.60 .Ol .06 <2 c.2 ~10 <.3 c.2 5.4

.8 7.5 8.4 55.9 ~30 20 10 196 2.58 2.6 6 3 13 .I7 .3 .l 57 .I9 ,028 13 34 .43 171 .lO 3 1.49 .Ol .05 <2 C.2 40 c.3 C.2 5.9

1 1

4 1 1

Tizard Explorations Inc. PROJECT TCHIIZA FILE # 97-3'778

.8 5.2 6.6 52.2 ~30 lb 7 354 1.80 1.1 <5 2 12 .09 C.2 .l 44 .21 ,031 1, 26 .29 174 .08 ~3 1.22c.01 .03 ‘2 .2 Cl0 c.3 q.2 4.4 ~1 1.1 10.0 7.0 42.8 <30 20 7 172 1.85 4.1 ~5 2 14 .lO .4 c.1 45 .24 .020 12 30 .36 174 .07 G 1.25 .Ol .04 ~2 c.2 40 s.3 C.2 3.8 1 1.4 9.9 6.6 38.1 ~30 17 6 258 1.39 3.9 5 2 12 .23 .4 .2 36 .21 .029 10 22 .25 151 .04 ~3 28 .Ol .04 <2 <.2 28 c.3 c.2 2.4 1 1.2 11.7 5.7 41.3 61 17 4 185 1.20 4.5 ~5 <2 38 .25 .4 c.1 30 1.35 .05a 11 20 .50 152 .04 4 .6.6 .Ol .06 ‘2 c.2 53 <.3 q.2 1.7 3 1.5 5.8 2.1 25.9 ~30 4 1 1389 .27 .a <5 ~2 121 .47 c.2 g.1 5 4.47 ,081 1 3 .25 431c.01 6 .I3 .Ol .04 <2 C.2 79 C.3 C.2 1.5 1

.8 5.1 1.1 32.7 ~30 2 1 395 .08 c.5 ~5 ~2 215 .22 c.2 s.1 2 5.25 .084 ~1 2 .39 657c.01 16 .Ob<.Ol .03 ~2 c.2 46 .7 c.2 .6 1

.9 9.6 6.3 19.0 ~30 15 4 160 1.20 4.3 5 2 21 .08 .3 c.1 31 .66 .015 13 20 .22 216 .06 ~3 .75 .Ol .05 ‘2 c.2 15 s.3 c.2 2.2 4

.9 6.0 7.2 24.1 ~30 16 5 125 1.45 3.4 ~5 ~2 14 .06 .3 .l 41 .27 .O,l 10 24 .26 208 .05 ~3 l.llc.01 .02 ~2 c.2 12 s.3 c.2 3.5 9 1.1 10.1 6.3 30.3 49 14 3 122 1.10 3.8 ~5 <2 28 .lb .4 <.I 29 .91 .042 12 20 .32 260 .04 ~3 .61 .Ol .03 ~2 c.2 28 c.3 c.2 1.6 1 1.6 3.8 .a a.2 ~30 2 I 206 .OP .5 ~5 ~2 171 .42 c.2 c.1 2 4.47 ,071 1 2 .27 671c.01 8 .07 .Ol .03 <2 C.2 47 2.0 C.2 C.5 Cl

AOZN 1lSOE 1 AOZN 12OOE 1 ADZN 12SOE <l ADZN 130OE Cl ADZN 1350E ~ 1.2 11.6 7.5 45.7 30 27 8 145 2.44 4.4 6 2 10 .13 .4 .l 53 .16 ,057 11 35 .37 100 .07 ~3 1.50 .Ol .04 <2 c.2 26 c.3 c.2 4.7 2

ADZN 1400E .E 10.3 7.1 45.6 39 24 8 155 2.29 4.3 <5 2 12 .I6 .3 .l 49 .23 ,094 11 30 .43 151 .Ob ~3 1.4Oc.01 .05 <2 <.2 15 c.3 c.2 4.7 1 AOZN 1450E .9 7.6 6.6 36.8 ~30 15 5 126 2.22 2.4 ~5 ‘2 1, .17 .3 .l 5a .15 .090 10 31 .25 100 .07 ~3 .99 .Ol .04 ~2 c.2 15 <.3 q.2 5.2 2 ADZN 1500E 1.0 a.6 9.3 36.4 56 21 8 248 2.65 2.9 ~5 2 15 .15 .3 .2 56 .25 ,059 12 36 .48 159 .lO 3 1.68 .Ol .05 ~2 .2 10 c.3 c.2 6.9 1 AOZN 1550E .9 10.5 6.8 37.5 154 15 7 408 1.43 2.3 C5 <2 58 .21 .3 .l 31 1.40 .051 10 2, .27 4-G' .04 ~3 1.22 .02 .03 <2 c.2 32 .7 c.2 3.9 2 AD2N 16OOi 1.0 6.8 9.4 75.9 37 22 9 312 2.65 2.6 ~5 2 14 .29 .3 .l 54 .26 ,060 11 34 .42 300 .OB ~3 1.75 .Oi .05 ~2 .2 ~10 c.3 c.2 6.4 2

AOZN 1650E 1.1 10.5 a.8 53.4 65 29 10 297 2.30 6.5 5 2 12 .24 .5 .2 46 .22 .105 12 33 .41 179 .05 ~3 1.55 .Ol .06 <2 c.2 71 c.3 <.2 4.1 1 AOZN 1700E 1.1 12.6 2.7 50.7 96 12 6 1812 .96 1.8 <5 2 337 .61 .2 c.1 24 11.85 .195 7 16 .56 786 .02 19 .72 .02 .06 <2 c.2 33 2.5 c.2 2.6 ~1 AOZN 1750E .7 10.0 6.6 43.2 ~30 14 10 239 2.95 1.8 10 <2 52 .09 .2 c.1 53 .90 ,047 15 41 .71 267 .13 q3 1.58 .02 .oa <2 ~2 22 c.3 c.2 3.9 ~1 AOZN 1aOOE 1.1 7.9 6.2 37.8 ~30 22 8 la3 2.29 3.0 ~5 3 15 .oa .3 .2 47 .25 ,047 12 35 .46 135 .lO ~3 1.31 .Ol .09 ~2 .2 14 s.3 c.2 4.0 1 AOZN la50E .7 6.6 5.8 41.1 a2 16 6 253 1.71 1.7 ~5 2 17 .ll .3 .l 39 .29 ,039 11 28 .33 193 .Oa ~3 1.21 .O, .06 <2 .2 12 <.3 c.2 4.2 ~1

STANDARD DZIH :23.9 117.6 90.1 259.4 2004 28 15 969 4.37 68.4 24 16 59 2.08 8.7 21.6 69 .71 ,106 17 54 1.14 243 .14 18 2.23 .05 .69 18 2.2 478 .7 2.0 7.0 50

Standard is STANDARD DZ/HG-500/A"-5. SamLes bwinninq 'RE' are Reruns and 'WE' are Reiect Reruns.

< Tizard Explorations Inc. PROJECT KETCHIKA FILE # 9-l-3778 Page 15 'I+ M MuvTlOl

AOZN 19OOE t ADZW WOE AOZY ZOOOE AOZN 2050E ADZN 2lOOE

ADZN 2150E ADZW 22OOE llD2N 2250E AOZN 2300E AD2N 2350E

RE ADZN 2350E AOZN 2400E ADZN 2450E ADZN 2500E ADZN 2550E

ADZN 2600E M2N 2650E ADZN 2700E AOZN 2750E ADZN 2800E

AD2N 2850E AI,ZN 29OOE AOZN 2950E AOZN 3000E AO2N 3050E

ADZN 3100: ADZN 3150E ADZN 3200E ADZN 3250E ADZN 3300E

ADZN 3350E ADZN JLOOE AOZN 3450E AD2N 3500E AOZN 3550E

STANDARD 02/H

no C” Pb 2n As Ni Co Nn Fe As ” Th sr Cd Sb Bi V CB P La CT ng 8a Ti 8 Ail Na I: V Tl Ng Se Te Ga Au+ p(m pp"m wppbpFmmFw % ppnFwFwm !=mppn Fwppo % XFPFW XFpn %PP % x ~wFmppbwmwlw

.6 7.5 6.7 50.2 79 24 7 312 2.03 1.9 5 3 16 .I4 .3 .l 36 .30 .065 1, 29 .40 178 .08 G 1.14 .Ol .06 ~2 c.2 13 c.3 c.2 4.2 1

.5 6.5 6.1 39.7 50 22 6 210 1.88 1.9 5 3 16 .07 .2 q.1 37 .27 .043 10 28 .40 200 .07 <3 1.15 .Ol .05 ~2 s.2 18 c.3 s.2 4.2 4

.4 5.6 6.7 51.2 30 20 7 149 1.82 1.4 <5 3 14 .07 .2 .l 39 .24 .041 10 27 .36 181 .07 ~3 1.21 .Ol .03 ~2 .2 21 s.3 s.2 4.5 2

.6 9.3 8.3 37.6 ~30 30 7 163 2.05 3.0 ~5 5 14 .03 .2 ., 41 .25 .035 12 33 .48 172 .08 <3 1.31c.01 .05 ~2 c.2 19 <.3 c.2 4.5 4

.5 6.4 6.6 48.1 33 22 7 191 1.98 l.8 8 3 12 .04 .2 .I 42 .23 .041 10 28 .40 172 .07 ~3 1.35 .Ol .07 ~2 s.2 12 c.3 s.2 4.8 <l

.7 5.9 7.0 50.6 e30 18 7 143 1.87 2.0 ~5 3 11 .07 .2 .2 41 .,8 .046 10 27 .38 138 .07 ~3 1.20 .Ol .04 c2 c.2 Cl0 c.3 s.2 4.6 4

.7 7.5 7.9 38.8 32 23 6 168 2.12 3.4 ~5 3 12 .04 .2 .2 43 .I9 ,029 12 30 .46 157 .07 4 1.30 .Ol .04 <2 .2 16 c.3 c.2 4.9 cl .5 6.7 6.5 37.6 ~30 21 6 154 1.96 2.4 ~5 4 13 .03 c.2 .I 39 .2, .025 1, 30 .45 154 .08 <3 1.19 .O, .04 ~2 c.2 21 <.3 c.2 3.6 ~1 .6 7.5 7.7 41.9 32 22 7 178 2.15 2.7 ~5 4 13 .06 .2 .I 43 .22 .041 11 32 .47 176 .08 3 1.3ls.01 .05 <2 c.2 15 c.3 c.2 4.7 2 .6 6.2 7.2 47.6 41 17 5 142 1.81 2.4 ~5 4 13 .05 .2 ., 42 .2, .028 1, 26 .38 166 .07 <3 1.2, .O, .04 <2 <.2 ~10 s.3 <.2 4.4 ~1

.6 6.6 7.6 43.4 ~30 17 6 133 1.71 2.2 ~5 3 11 .05 .2 .1 38 .,9 ,029 10 24 .36 157 .06 <3 1.10 .O, .03 ~2 q.2 <lo c.3 c.2 4.5 ~1

.4 10.4 7.0 36.7 ~30 27 6 145 2.19 3.3 ~5 4 15 .03 .2 c.1 41 .27 .038 13 35 .48 184 .08 ~3 1.24 .01 .03 ~2 c.2 17 c.3 c.2 4.0 Cl

.4 6.8 7.1 52.2 ~30 20 7 169 1.86 2.0 <5 4 13 .05 .2 .I 39 .2, .032 1, 28 .39 170 .07 ~3 1.23 .Ol .03 ~2 .2 18 c.3 c.2 4.5 4

.8 7.6 6.0 45.4 ~30 20 5 126 1.46 2.0 ~5 2 15 .06 .2 c.1 34 .25 ,022 11 22 34 207 .05 ~3 1.01 .Ol .04 ~2 c.2 13 s.3 c.2 3.4 cl 1.2 5.7 7.7 47.9 46 19 6 287 1.59 1.6 <5 3 13 .08 .3 .I 41 .22 .021 10 24 .28 228 .06 <3 1.23 .Ol .04 ~2 s.2 16 <.3 c.2 5.3 1

1.2 5.5 5.7 34.2 <30 17 5 242 1.39 1.9 <5 2 11 .07 .2 c.1 33 .I9 .033 9 19 .23 167 .04 <3 .87 .Ol .05 <2 <.2 29 c.3 c.2 3.5 7 .7 6.0 6.8 42.3 ~30 19 7 296 1.84 2.2 8 3 11 .12 .2 c.1 40 .I8 .055 10 25 .32 203 .06 ‘3 1.08 .Ol .04 ~2 c.2 28 c.3 c.2 4.9 <l .8 6.5 7.1 41.2 48 16 7 247 2.02 2.5 ~5 3 12 .08 .2 .I 43 .I9 .04l 1, 28 .42 227 .07 ~3 1.26 .Ol .04 ~2 <.2 28 c.3 c.2 5.0 <l .7 5.4 7.2 53.8 89 19 6 284 1.63 1.4 ~5 2 13 .19 .2 <., 3.4 .21 ,079 9 24 .28 270 .06 ~3 1.08 .Ol .04 ~2 ‘.2 30 x.3 c.2 4.9 4 .5 5.4 6.3 61.9 39 19 7 230 1.78 1.5 <5 3 13 .09 .2 s.1 40 .2, ,036 1, 26 .37 212 .07 ~3 1.22 .Ol .04 ~2 .2 16 *.3 c.2 4.4 cl

.6 5.8 7.2 60.5 52 21 8 416 2.21 1.8 <5 2 14 .I0 .2 .I 45 .24 .029 10 32 .39 314 .07 ~3 1.38 .Ol .04 <2 .2 23 c.3 c.2 4.9 -cl

.9 8.7 9.5 48.7 46 24 6 170 2.07 2.9 ~5 4 14 .09 .3 c.1 4, .23 .021 12 30 .4l 228 .07 ~3 1.24 .Ol .04 ~2 .2 30 c.3 c.2 6.0 <l

.a 7.0 7.0 61.3 114 16 7 419 2.01 1.2 5 3 14 .32 .2 .1 38 .25 ,133 10 26 .33 282 .07 <3 1.07 .O, .05 -c2 c.2 24 <.3 c.2 5.1 4

.8 10.1 7.5 37.1 50 24 6 140 2.00 2.9 -c5 4 14 .04 .3 .A 37 .23 ,040 13 31 .U 191 .07 <3 1.07 .Ol .05 <2 c.2 27 <.3 c.2 3.9 4

.7 8.8 8.1 37.5 49 21 6 207 1.86 2.2 8 4 12 .04 .2 <., 37 .20 ,035 10 29 .43 172 .07 ~3 1.14 .O, .04 ‘2 .2 36 c.3 c.2 4.9 4

1.1 6.8 7.5 58.2 ~30 19 7 249 2.13 2.2 ~5 3 13 .I6 .3 .i 43 .23 ,046 10 28 .36 223 .07 5 1.21 .o, .05 x2 c.2 54 c.3 c.2 5.7 -cl .a 7.2 7.1 56.7 ~30 27 8 263 2.31 2.2 ~5 3 15 .,2 .2 <., 46 .27 ,057 11 32 .42 195 .08 ~3 1.47 .Ol .05 ‘2 .2 74 c.3 c.2 5.5 <1

1.1 9.3 7.8 55.7 91 26 9 315 2.31 3.0 <5 4 14 .,5 .3 c.1 46 .26 .Oa7 13 35 .45 243 .08 ~3 1.48 .Ol .06 ‘2 .3 62 c.3 c.2 5.9 <l .7 5.9 6.9 51.2 62 22 7 317 1.70 1.3 5 3 11 .17 .2 .1 37 .20 .034 9 25 .30 267 .05 <3 1.15 .Ol .04 ~2 c.2 51 c.3 c.2 4.7 4 .9 7.4 7.4 45.2 47 22 7 275 1.87 2.3 ~5 3 11 .12 .2 ., 42 .20 ,054 10 26 .U 280 .06 <3 1.20 .Ol .04 ~2 <.2 55 <.3 c.2 5.0 ~1

1.1 a.2 8.8 52.8 47 20 8 172 2.15 2.7 <5 3 12 .22 .3 ., 44 .,9 ,095 10 28 .34 217 .06 <3 1.30 .01 .05 ~2 c.2 45 c.3 c.2 6.1 <l .a 5.6 8.6 37.3 59 16 6 155 1.65 1.2 ~5 3 12 .I4 c.2 ., 36 .2, ,048 10 24 .25 222 .06 ~3 1.14 .Ol .04 ~2 .2 36 c.3 c.2 6.1 <l .9 7.0 9.9 34.0 68 12 5 130 1.44 1.7 c5 3 9 .14 .2 .I 36 .14 ,056 10 21 .27 119 .06 <3 1.00 .O, .03 ~2 c.2 31 c.3 c.2 7.6 <l .8 12.5 1.7 17.8 115 12 3 611 .23 s.5 ~5 4 127 1.41 c.2 c.1 6 4.46 ,108 2 4 .I8 921c.01 3 .26 .Ol .02 ~2 <.2 27 .6 c.2 1.2 <l .a 8.3 2.4 13.6 99 6 3 151 .32 c.5 ~5 4 56 1.12 c.2 <.I 4 1.48 ,142 3 3 .09 261c.01 ~3 .22 .02 .03 ‘2 <.2 96 c.3 c.2 1.3 1

3.3 114.7 95.0 251.3 ,864 3, 15 95, 4.44 69.4 28 18 60 2.0, 8.6 21.6 68 .70 ,106 17 52 1.12 255 .,4 26 2.25 .06 .68 15 2.6 444 .6 2.2 7.5 54

Standard is STANDARD 02/HG-SOO/AU-S. SampLes beqinning 'RE' are Reruns and 'RRE' are Reiecr Reruns.

AI1 results we considered the confidential property of the client. Acme assures the Liabilities for actual cost of the analysis only. Data- FA _

Tizard Explorations Inc. PROJECT KETCHIKA FILE # 97-3776 Page 16

Ao2N 36OOE AO2N 3650E ADZN 3700E AOZN 3750E ADZN 3800E

kO2N 3850E AD2N 3900E ADZ" 3950E RDZN 4000E AD3N OE

AO3N 50E AD3N 1OOE AD3N 150E AD3N 2OOE AD3N 250E

RE AD3N 250E AD3N 300E AD3N 350E AD3N 400E AD3N 450E

AD311 500E P93N 550E AD3N 600E AD3N 650E AD3N 700E

AO3N 750E AO3N 8OOE AO3N 850E AO3N 9OOE AD3N 950E

A03N 1OOOE AD3N 1050E AO3N 1lOOE AD3N 1150E AD3N 12OOE

STANOARO 021

.3 5.5 9.0 66.7 59 14 5 199 1.42 .9 c5 2 18 .I4 c.2 .I 29 .37 ,056 13 29 .43 194 .08 c3 1.21c.01 .06 ‘2 <.2 18 c.3 s.2 4.2 1 1.0 9.7 7.2 49.2 32 18 6 128 1.54 1.8 ~5 1 11 .24 .3 .1 35 .21 ,079 9 23 .29 175 .05 <3 l.Ol<.Ol .OL ‘2 <.2 21 c.3 c.2 3.7 1

.? 6.5 7.4 104.1 49 20 8 522 2.05 1.7 ~5 1 16 .30 .2 .2 40 .33 .084 9 29 .36 242 .O? <3 1.38c.01 .05 ~2 c.2 22 s.3 c.2 4.8 2

.? 4.0 6.0 53.7 <30 9 4 165 1.30 .9 <5 1 11 .25 q.2 .I 34 .I8 .060 9 19 .l? 174 .06 3 .86 .Ol .03 ~2 .2 cl0 <.3 c.2 3.4 1 1.1 9.4 7.2 79.8 115 19 7 753 1.86 2.2 <5 1 19 .50 .3 .l 37 .34 .125 10 27 .33 366 .06 ~3 l.ll~.Ol .08 ~2 s.2 10 c.3 q.2 3.9 <l

.? 7.9 8.1 55.5 48 21 7 214 2.12 1.4 <5 2 16 .21 .2 .2 38 .30 .114 10 31 .4O 194 .O? ~3 1.22c.01 .09 ~2 .2 12 c.3 c.2 4.5 ~1

:; 6.2 8.4 6.2 7.7 60.7 52.0 190 66 21 23 6 7 410 299 1.78 1.82 1.8 1.1 ~5 5 1 1 13 13 .22 .16 c.2 .2 c.1 .2 37 37 .24 .24 .075 .048 11 11 28 28 .33 .38 233 221 .06 .O? <3 c3 1.22c.01 1.17 .Ol .O? .06 ~2 ~2 c.2 s.2 29 10 s.3 c.3 c.2 c.2 3.5 3.9 1 1 .3 .2 37 .26 .091 9 29 .32 317 .05 c3 1.38 .Ol .O? <2 .2 17 s.3 c.2 4.8 1 .8 .2 52 .65 .036 16 34 .48 313 .04 6 1.34c.01 .15 <2 .3 62 .4 c.2 4.1 2

.8 10.8 8.9 86.6 188 26 7 379 1.99 1.4 <5 1 14 .36 2.8 24.6 12.2 66.6 192 37 9 322 2.39 4.8 ~5 2 24 .44

.3 .I 30 .27 .035 8 19 .22 322 .04 5 .84 .Ol .12 ~2 c.2 40 c.3 c.2 2.4 1

.3 .I 33 .24 .O41 9 23 .24 189 .05 ~3 .85 .Ol .05 ~2 c.2 14 s.3 s.2 2.8 3

.5 c.1 34 .24 .026 ,I 27 .3L 143 .06 <3 .82<.01 .05 ~2 c.2 18 c.3 s.2 2.9 2

.2 .l 40 .22 .031 9 26 .38 186 .O? ~3 1.15 .Ol .05 ‘2 c.2 13 c.3 c.2 4.3 1

.4 .I 39 .19 .037 10 24 .33 173 .05 ~3 1.02 .O, .03 ~2 c.2 17 c.3 c.2 3.7 1

.4 .I 40 .20 .036 10 25 .3L 182 .06 ~3 1.05c.0, .03 ‘2 c.2 17 c.3 c.2 3.7 1 .2 .I L3 .21 ,033 11 27 .38 176 .08 <3 1.3Oc.01 .04 ‘2 q.2 40 c.3 c.2 4.8 4 .3 .I 32 .13 ,022 9 18 .22 114 .05 3 .73<.01 .02 ~2 <.2 1, c.3 c.2 3.6 1 .3 .I 50 .21 ,029 10 32 .42 179 .O? ~3 1.35 .Ol .03 ~2 s.2 17 c.3 s.2 5.1 3 .5 .l 42 .19 .077 10 23 .30 120 .04 3 .96 .Ol .03 ~2 <.2 20 c.3 c.2 3.5 1

.3 .2 57 .16 .055 11 30 .35 179 .08 ~3 1.34 .Ol .03 ~2 c.2 <lo c.3 s.2 6.8 1

.3 c.1 30 .I1 .044 8 15 .lO 107 .03 ~3 .59 .Ol .02 ~2 c.2 <IO c.3 q.2 2.8 1

.4 .I 39 .I8 ,056 9 26 .30 203 .06 ~3 1.16 .O, .05 <2 c.2 i, <.3 c.2 4.0 1

.4 .l 47 .24 ,099 11 35 .4l 240 .O? ~3 ,.LO .Ol .06 <2 c.2 19 c.3 q.2 5.1 3

.4 .2 49 .23 .075 10 34 .43 175 .08 ~3 ,.44<.01 .05 ~2 <.2 40 c.3 c.2 4.9 2

.4 .I 37 .28 .029 8 24 .31 227 .05 <3 ,.O,<.Ol .05 c2 s.2 19 c.3 c.2 3.4 2

.3 <.I 29 .33 ,016 8 15 .l? 25, .03 ~3 .63 .O, .04 ‘2 <.2 12 c.3 c.2 2.2 1

.3 c.1 35 .I? .Oll 9 21 .22 155 .05 ~3 .87 .O, .02 ~2 c.2 <,O <.3 c.2 2.9 4

.4 .2 47 .20 .053 9 29 .35 205 .08 ~3 1.36 .Ol .03 ~2 ‘.2 <,O s.3 c.2 4.6 1

.5 c.1 35 .33 ,028 9 24 .24 177 .04 <3 .87 .01 .03 ~2 c.2 17 c.3 c.2 2.4 3

.4 .I 34 .37 ,022 8 21 .25 257 .05 ~3 .92 .Ol .03 <2 ‘.2 19 s.3 c.2 3.9 1

.3 .l 30 .20 ,024 8 21 .27 217 .06 ~3 .92<.01 .05 <2 ‘.2 40 s.3 c.2 3.6 1

.4 .2 37 .15 ,036 9 21 .31 161 .O? 3 .85 .Ol .03 c2 c.2 cl0 <.3 c.2 4.2 1

.3 .I 45 .22 ,029 10 31 .4L 273 .08 ~3 1.28 .O, .04 ~2 s.2 <IO <.3 c.2 4.6 2

.4 .I 31 .67 ,012 8 20 .27 334 .04 ~3 .92 .Ol .03 ~2 c.2 cl0 c.3 c.2 2.9 2

1.0 7.8 6.4 50.5 46 17 6 233 1.26 1.4 ~5 4 14 .28 .? 8.3 6.2 28.9 111 16 4 107 1.36 1.5 ~5 1 14 .ll

1.3 14.1 6.7 34.7 ~30 21 6 184 1.57 3.7 -c5 2 13 .08 .8 7.3 7.2 49.8 38 19 6 393 1.83 1.2 ~5 1 12 .13

1.1 8.1 7.0 53.6 49 16 5 393 1.62 1.7 ‘5 4 12 .O?

1.2 8.3 7.1 54.4 31 17 6 395 1.65 2.0 ~5 2 13 .O? .8 6.7 8.0 50.8 5, 17 6 180 1.85 2.3 ~5 1 13 .09 .8 6.3 5.9 26.8 ~30 9 4 96 1.13 1.3 <5 1 8 .05

,.O 8.1 7.8 45.8 34 18 7 179 2.26 2.5 q5 2 12 .12 1.8 9.0 6.7 40.0 32 16 5 135 1.74 2.4 ~5 1 10 .13

1.1 8.4 9.9 62.8 63 16 8 235 2.53 1.5 5 1 ,I .32 .8 6.0 5.7 30.4 36 7 2 55 1.05 1.3 4 ~1 7 .l? .5 6.8 6.8 46.6 93 21 6 209 1.78 1.9 <5 1 10 .I4 .9 10.3 8.3 60.5 59 27 8 208 2.34 2.7 <5 2 13 .21 .6 9.2 7.0 50.9 105 25 8 201 2.36 2.1 ~5 2 14 .18

1.0 8.2 6.3 36.0 72 18 5 289 1.67 2.3 ~5 1 14 .I1 1.2 7.8 5.0 32.7 44 12 4 316 .96 1.7 ~5 1 17 .28 1.1 6.1 4.9 19.7 ~30 13 4 85 1.32 2.4 ~5 1 10 .04

.? 7.6 6.8 39.1 72 21 6 159 2.17 2.1 ~5 1 12 .15 1.2 10.9 5.7 29.2 36 21 5 155 1.43 2.2 c5 1 15 .I4

1.1 9.0 7.0 35.4 94 14 4 26.6 1.44 1.6 5 1 17 .45 .8 5.6 6.3 38.2 69 16 4 232 1.32 1.0 ~5 ~1 12 .13 .8 5.9 6.6 36.4 62 14 5 260 1.56 1.1 ~5 1 9 .19

:; 8.7 7.5 6.5 7.7 52.1 24.8 2; :: 4 8 253 101 2.13 1.27 1.8 1.7 ~5 ~5 ~1 2 30 14 .49 .13

r3.4 119.0 92.8 256.9 1856 30 15 972 4.44 67.5 25 16 60 2.22 10.4 23.6 69 .?, ,106 17 53 1.17 254 .I4 26 2.26 .05 .69 15 2.2 424 .6 1.8 6.2 52

Standard is STANDARD 02/W-SOO/AU-S. Samples kqinnins IRE' are Reruns and 'ME' are Reiect Reruns.

Data- FA _

- BQ Tizard Explorations Inc. PROJECT c, TCHIKA FILE # 97-3778 Page 17 '44 af muniw m ~rmN.

SAMPLE# Ho C" Pb 2n Ag Ni Co nn Fe x puhs& g s $2 ca P La cr Mg 8a Ti B Al 118 K Y ,l Hg se Te oa Au+

wmFvppnppnppbmPpnw % %Fwppn xppn xppn x Y. ~wFvppbppnFFFmP

AD3N 1250E 1.3 6.6 8.7 51.4 ~30 lb 5 145 2.17 1.7 <5 2 10 .27 .2 AD3N 1300E 1.3

., 48 .I4 .076 10 28 .33 118 .07 ~3 1.14 .O, .03 <2 s.2 ~10 c.3 c.2 5.5 Cl 9.1 10.2 66.8 ~30 30 10 204 2.93 2.4 <5 3 15 .20 .2

AD3Y 1350E ., 58 .25 ,073 12 38 .49 192 .,O ~3 1.85 .O, .05 ~2 .2 21 c.3 c.2 6.9 1

.9 7.5 2.4 2b.7 9, 7 2 202 .40 C.5 <5 Cl 158 .83 .3 c.1 8 7.18 ,070 2 6 34 981 .Ol AO3N 1400E 4.6 8.2 1.6 8.2 44

8 .2b .Ol .03 <2 c.2 37 1.3 c.2 .7 1 9 4 1269 2.0, 2.1 6 ~1 200 .4, <.2 c.1 6 4.82 .08D

AO3N 1450E I.2 9.9 7.4 36.6 ~30 24 2 4 .38 932 .O, <3 .27 .02 .O, ~2 c.2 49 1.3 c.2 1.3 1

6 195 1.9b 1.9 ~5 1 24 .15 .3 .I 44 .42 .035 9 30 .39 223 .Ob <3 1.2, .O, .03 ~2 c.2 15 c.3 c.2 4.2 1

AD3N 15OOE 1.0 8.9 8.0 Si.9 32 30 9 183 2.71 3.2 <5 3 11 .15 .2 ., 56 .,8 .Db2 12 39 .48 177 .08 <3 1.83 .O, .04 ~2 c.2 17 c.3 <.2 5.6 Cl AD3N 155OE 1.1 9.1 7.8 53.2 34 23 8 lb6 2.57 3.1 ~5 2 10 .2D .3 ., 54 .15 .Ob4 12 39 .4b 140 .08 G 1.72 .Ol .04 <2 .2 29 c.3 <.2 5.3 1 AD3N 1bOOE .7 9.6 1.2 9.5 <30 b 2 954 .29 c.5 ~5 ~1 191 .53 .3 <.I 6 6.06 .082 1 2 .28 653c.01 9 .14 .Ol .Ol ~2 c.2 45 .4 c.2 .b 1 AD3N 1650E .8 13.9 3.1 12.1 70 18 7 17, 1.22 .9 ~5 ~1 156 .59 .5 .l 2L 4.37 .071 4 15 .33 731 .02 ADJN 1700E .8 6.2 6.9 66.8 32 20

3 .b3 .02 .Ol ~2 q.2 30 2.8 q.2 2.1 2 8 527 2.32 .9 <5 1 24 .20 .2 .I 46 .52 .044 ID 33 .37 305 .D8 ~3 1.75 .02 .Ob <2 q.2 26 c.3 c.2 4.7 3

AD3N 1750E .8 5.6 7., 48.8 43 18 7 279 1.98 .9 <5 1 15 .12 s.2 .2 40 .2b .048 10 30 .34 197 .09 ~3 1.37 .Ol .07 ~2 c.2 10 c.3 s.2 4.6 : AD3N 1800E .8 1O.L 8.6 46.1 ~30 25 8 218 2.18 2.4 ~5 3 lb .15 .2 AD3N 1850E .b

.I 45 .27 .DbO 13 34 .42 198 .09 ~3 1.38 .02 .07 <2 .2 ~10 c.3 c.2 5.4 5.7 6.2 55.1 62 20 b 356 1.97 1.1 <5 2 lb .,4 c.2 ., 40 .30 .05, 1, 29 .3b 274 .07 <3 1.34 .Ol .Ob ~2 c.2 cl0 c.3 q.2 4.0 ;

AD3N 1900E .7 7.9 6.8 50.6 ~30 19 b 277 1.89 1.5 c5 2 15 .I, .2 AD3N 1950E .4 6.7 7.9 74.0

.I 38 .27 ,033 13 29 .40 215 .08 c3 1.25 .02 .05 ~2 ‘.2 16 c.3 q.2 3.9 46 23 7 566 1.90 .5 <5 1 15 .28 C.2 .I 40 .28 ,046 13 30 .3b 26, .08 ~3 1.42 .Ol .05 ~2 c.2 14 x.3 c.2 5.0 <l

AD3N ZOOOE .7 9.7 7.8 57.5 98 22 8 282 2.21 1.6 ‘5 3 16 .13 .2 ., 48 .2b .044 14 35 .43 237 .08 ~3 1.54 .O, .05 ~2 c.2 17 c.3 <.2 5.D 1 AD3N ZOSOE .8 9.4 7.4 38.5 55 18 6 206 1.69 1.6 ~5 2 20 .I0 .3 .2 42 .32 .046 10 24 .29 239 .Ob ~3 1.30 .02 .04 ~2 c.2 12 c.3 c.2 3.0 '; AD3N 2lOOE 7.4 8.8 36.2 69 18 6 152 1.81 2.3 ~5 2 13 .I0 .3 .I 4 .20 .03, 1, 27 .3b 145 .07 ~3 1.25 .02 .04 <2 s.2 15 c.3 C.2 4.5 AD3N 2150E :; 7.5 8.3 67.6 34 24 7 192 2.14 I.? ~5 3 14 .D8 .2 <.I 48 .25 .D32 13 3, .45 203 .07 <3 1.60 .Ol .OC ~2 c.2 1D c.3 c.2 4.9 1 RE AD3N 2150E .8 7.5 8.3 70.1 <30 24 7 194 2.13 2.0 ~5 3 lb .08 .2 ., 49 .2b .D32 14 3, .45 2OD .08 ~3 1.63 .Ol .04 ~2 c.2 ~10 <.3 c.2 5.2 2

AD3N 22DDE .8 7.6 8.1 59.6 57 21 8 254 2.18 2.3 ~5 3 15 .08 .2 AD3N 225DE .7

., 5, .23 ,044 14 33 .44 200 .09 ~3 1.64 .02 .04 ‘2 ‘.2 14 c.3 q.2 5.4 <l 9.2 8.2 52.6 37 25 7 186 2.48 2.7 ~5 3 15 .06 c.2

AD3N 23OOE .7 7.8 7.4 50.8 ., 53 .25 .02D 13 37 .54 176 .,D ~3 1.75 .02 .04 ~2 c.2 ~10 c.3 c.2 5.6 1

43 2, 7 197 2.08 2.3 ~5 3 14 .06 AD3N 2350E

.2 ‘.I 47 .23 .023 14 32 .48 l&c .09 <3 1.53 .Ol .04 <2 c.2 19 c.3 <.2 4.8 1 .6 6.5 7.8 44.9 ~30 I9 6 159 1.91 1.8 ~5 2 15 .D5

AD3N 2400E .6 7.3 9.2 44.7 38 20 8 215 1.94 1.7 ~5 .2 <., 47 .24 ,022 14 30 .45 172 .09 <3 1.43 .O, .03 ~2 <.2 18 c.3 c.2 5.0 3

2 13 .07 .2 ., 46 .23 .D28 13 30 .45 175 .08 ~3 1.40 .O, .D4 ~2 .2 1, c.3 ‘.2 4.9 ~1

it; gz: / ';; 'it; Ly ii; ; 5; a {;; 5:; ifi I; f ip ;;; <;I ‘.I ., 5, .40 ,041 16 36 .42 343 .06 ~3 1.82 .02 .05 ~2 ‘.2 18 c.3 c.2 5.6 ~1

45 .,9 .065 11 26 .28 195 .07 ~3 1.45 .Ol .D4 ~2 c.2 15 c.3 c.2 6.2 5 .l 47 .22 .D56 12 32 .35 217 .09

AO3N 2bOOE ; .5 5.5 6.6 63.1 3 1.64 .Ol .05 ~2 s.2 26 <.3 c.2 5.8 1

45 19 8 356 2.06 1.5 ~5 AO3N 265DE

1 11 .lD <.2 <., 48 .,8 ,038 12 29 .37 159 .08 ~3 1.46 .Ol .04 ~2 c.2 20 c.3 c.2 4.6 <l ! .a 5.5 7.7 57.5 79 16 6 232 1.59 1.1 ~5 2 14 .ll <.2 ., 42 .22 ,034 12 25 .34 262 .07 ~3 1.37 .O, .D3 <2 c.2 17 <.3 c.2 5.4 2 I

AD3N 2700E / .7 6.2 7.8 61.2 45 20 7 194 2.25 1.8 ~5 2 12 .I2 .2 <.l 51 .2D .032 1, 3, .4, lb9 .D8 ~3 1.54 .Ol .04 ~2 c.2 26 c.3 c.2 5.4 1 AD3N 2750E .9 6.4 8.0 69.0 66 19 7 202 2.02 2.0 ~5 1 12 .ll .2 AD3N 28OOE /

., 49 .2D ,040 12 28 .37 168 .07 ~3 1.49 .O, .04 ~2 q.2 12 c.3 <.2 5.4 <l .7 7.0 7.9 51.8 60 23 7 216 2.15 3.6 ~5 2 14 .07 .2 <., 50 .22 .028 13 33 .45 214 .09 <3 1.66 .Ol .04 ~2 C.2 19 c.3 c.2 5.6 3

AD3N 2850E ! .5 5.3 6.5 37.5 ~30 17 5 164 1.62 1.5 ~5 2 13 .04 <.2 <., 42 .21 .02b 12 27 .39 lb2 .07 3 1.36 .OI .03 ~2 q.2 12 c.3 q.2 4.3 2 AD3N 2900E / .9 8.4 6.4 31.2 ~30 15 5 I74 1.39 2.1 <5 2 I4 .08 .2 ., 40 .24 .024 12 23 .33 173 .Ob ~3 1.11 .O, .03 ~2 c.2 16 c.3 c.2 4.1 1

STANDARD D2," /24.2 118.2 96.8 256.5 ,875 29 16 980 4.39 70.4 14 16 60 2.0, 10.0 21.0 69 .7, .104 17 54 1.17 25, .,4 26 2.30 .06 .bP 16 2.4 462 .6 2.0 7.3 55

Standard is STANDARD D2IHC.500,AWS. Samies besinninq IRE' are Reruns and 'ME' are Reiect Reruns.

ALI results are considered the confidential property of the client. Acme ~ssmes the liabilities for actual cost of the analysis only. Data- FA _

AD3N 2950E AD3N 3000E AD3N 3050E AD3W 3100E AO3N 3150E

AO3N 32OOE AD3N 3250E AD3N 33OOE AD3N 3350E AD3N 34OOE

AD3N 3450E AD3N 3500E AD3N 3550E AD3N 3600E RE AD3N 3600E

AD3N 3650E AD3" 3700E AD3N 3750E AD3N 3800E m3w 3850E

AD3N 39OOE An3N 3950E AD3N 4000E STANoARD 02/H

.5 5.6 7.3 46.7 ~30 19 .5 8.0 8.1 62.4 35 20 .7 7.1 a.3 47.0 <30 17 .7 6.4 7.0 43.9 40 I6 .7 6.8 8.2 41.2 71 I7

.5 3.6 6.1 33.6 34 7

.7 5.0 8.3 37.5 c30 10

.7 4.9 6.6 25.0 <30 8

.5 6.2 7.9 L7.7 ~30 19

.6 6.3 7.6 35.6 ~30 17

.6 6.3 8.9 120.0 111 16

.6 6.3 8.4 60.1 <30 I5

.7 5.6 7.7 59.6 56 I6

.8 8.7 7.3 41.7 34 15

.9 9.2 7.4 41.7 43 17

.7 6.4 7.9 64.5 35 18

.6 7.8 7.4 40.5 <30 18

.6 7.2 8.5 53.9 31 19 .7 6.8 8.7 48.5 31 14 .7 9.3 7.7 46.7 55 24

.6 7.4 8.4 54.3 70 19

.5 6.2 6.1 34.7 ~30 12

6 157 1.79 2.5 ~5 2 13 .08 c.2 .l 43 .2l .036 12 28 .38 161 .08 <3 1.35<.01 .04 ~2 c.2 ~10 c.3 c.2 4.5 ~1 7 176 2.03 2.8 ~5 2 14 .14 .2 .I 47 .22 .037 13 3, .39 196 .08 <3 1.53 .Ol .04 ~2 c.2 ~10 c.3 c.2 5.5 ~1 6 175 I.&c 3.4 <5 2 12 .12 c.2 <., 44 .20 .0X 10 27 .33 188 .O, <3 1.36 .Ol .04 ~2 c.2 31 c.3 c.2 5.1 1

6 223 1.75 2.L ~5 2 12 .lO .2 <.l 42 .22 .028 12 28 .39 176 .07 <3 1.25 .Ol .03 ~2 s.2 ~10 <.3 c.2 4.4 1 6 161 1.62 3.0 ~5 2 11 .lO .2 .l 38 .21 .036 12 27 .39 156 .07 G 1.22 .Ol .04 ~2 q.2 12 c.3 c.2 4.5 1

3 88 1.26 l.2 ~5 ‘2 1, .I1 <.2 <., 37 .,6 .023 10 19 .21 A8 .06 3 .91 .O, .03 ~2 c.2 10 c.3 c.2 4.0 1 4 104 1.49 1.3 c5 <2 9 .17 .2 <.I 40 .,3 .042 10 2, .20 96 .07 <3 .98<.01 .04 ‘2 c.2 10 c.3 c.2 5.7 1 3 79 1.14 1.9 -c5 s2 9 .17 .2 .l 35 .12 .027 10 18 .I8 68 .06 <3 .74 .O, .03 ~2 q.2 11 c.3 C.2 4.1 -4 6 153 2.12 2.5 ~5 2 10 .08 .2 .1 49 .18 .030 12 33 .42 154 .08 3 1.47 .Ol .04 c2 s.2 11 c.3 c.2 5.1 1 5 150 1.R 2.4 ~5 2 12 .07 .2 .I 41 .20 ,023 12 27 .35 181 .OB 3 1.24 .Ol .04 ~2 s.2 10 c.3 c.2 5.0 7

8 265 1.99 .7 <5 2 15 .46 .2 .2 42 .24 .114 12 28 .30 268 .08 3 1.41 .Ol .05 <2 c.2 12 c.3 c.2 5.5 <l 6 356 1.74 2.2 ~5 2 13 .19 c.2 c.1 42 .19 .035 1, 25 .3, 185 .08 <3 1.33 ,O, .04 ~2 .2 15 c.3 <.2 5.6 3 6 168 1.88 2.9 ~5 2 13 .16 .3 .1 45 .20 .033 12 27 .33 192 .08 <3 1.27 .Ol .04 ~2 c.2 11 ‘.3 c.2 4.9 1

5 155 l.R 3.9 ~5 2 12 .07 .3 <.l 42 .20 ,050 12 27 .Y 132 .07 <3 1.15 .Ol .05 ~2 c.2 13 c.3 q.2 4.2 1 6 155 1.72 4.6 <5 2 13 .OB .3 .I 43 .21 ,050 13 27 .34 130 .07 ~3 1.17<.01 .05 ~2 c.2 13 c.3 c.2 4.5 2

6 209 2.09 3.2 ~5 2 13 .ll .2 .l 47 .2, ,052 11 30 .34 182 .08 <3 1.44 .Ol .04 ~2 s.2 ~10 c.3 c.2 5.7 3 6 235 1.86 2.9 ~5 3 13 .07 .2 ., 41 .2X ,034 14 3, .42 155 .08 ~3 1.25c.01 .05 ‘2 c.2 40 c.3 c.2 4.3 2

7 225 1.94 2.2 5 2 16 .12 .2 .l 45 .27 .033 13 29 .41 218 .08 ~3 1.43 .Ol .O& ~2 c.2 11 <.3 x.2 5.6 2 6 216 1.93 2.2 ~5 ‘2 14 .I4 .2 .I 46 .23 .03, 13 29 .39 178 .08 <3 1.32 .Ol .03 ~2 c.2 12 c.3 c.2 5.9 2 8 206 2.25 5.7 <5 2 13 .13 .3 .I 46 .24 .144 13 33 .U 169 .07 3 1.40 .Ol .05 <2 c.2 15 <.3 c.2 5.0 2

7 285 1.89 2.4 5 2 11 .,, c.2 c.1 44 .,7 ,030 1, 28 .32 180 .08 <3 1.5, .O, .03 ~2 .2 17 c.3 c.2 5.9 1 5 169 1.32 1.6 ~5 2 11 .05 c.2 c.1 35 .18 ,019 1, 22 .29 136 .06 ~3 1.06 .Ol .03 ~2 c.2 ~10 c.3 x.2 4.2 7

.6 5.7 6.5 38.5 ~30 15 5 153 1.60 1.6 ~5 ~2 12 .06 c.2 .l 39 .20 ,026 1, 25 .33 143 .07 <3 1.2, .Ol .03 <2 s.2 18 c.3 c.2 4.5 2

1.1 116.8 92.6 253.7 ,895 28 15 955 4.28 69.5 27 16 58 2.10 8.7 25.3 68 .70 .,03 17 53 1.12 242 .I4 26 2.20 .06 .68 17 2.5 440 .6 2.0 7.0 45 i2 -

Srandard is STANDARD DZ/HG-500/W-S. Samples beqinnino 'RE' are Reruns and 'ME are Rejecf Reruns.

ROCK SAMPLES

AREL-1 AREL-2 AREL-3 AREL-4 AREL-5

AREL-7 AREL-a AREL-21-l ARSY-1 ARSY-2

ARSY-3 ARSY-4 ARSY-5 ARSY-6 ARSY-7

ARSY-a ARSY-9 ARSY-10 RE ARSY-10 BREL-1

c BREL-2 ,%+'I

BRSY-1 BRSY-2 BRSY-3 BRSY-4 BRSY-5

BRSY-6 BRSY-7 BRSY-a BRSY-10 BRSY-10 dup.

STANDARD C3,A"-R

t-

~PPFvPPFvpFmw Ppn XPpnPpnWPpn Ppn mPwmPpn x ~ppnppn

2 17 8 41 .6 12 4 76 2.17 <2 4 <2 <2 22 .a <3 <3 IO .07 .OlO 1 16 .06 271s.01 3 .17 .Ol .09 5 <5 -4 2 2 28 5 35 s.3 9 4 71 1.35 3 a ~2 ~2 33 .7 s3 <3 11 .09 .ola 1 17 .04 407c.01 3 .20 .oi .oa 3 ~5 ~1 i 3 163 12 163 .4 62 50 1078 8.28 5 e3 ~2 <2 112 <.2 ~3 ~3 19 .27 .127 1 18 .04 2154q.01 ~3 .42<.01 .09 2 <5 4 <I 1 21 15 19 .4 4 1 37 .77 ~2 <a <2 ~2 45 .4 ,<3 <3 10 .04 .015 2 26 .02 3abs.01 5 .26<.01 .08 3 <5 <I 1 1 65 67 13 .3 5 4 102 2.48 ~2 <a ~2 4 535 s.2 ~3 <3 60 .I3 .160 13 64 .09 304ag.01 11 1.03 .o, .2a <2 ‘5 1 1

1 13 26 IO <.3 6 3 27 .53 ~2 <a ~2 3 464 s.2 <3 3 15 .06 .194 14 26 .07 3433c.01 7 .77 .Ol .20 <2 s5 Cl s1 I a1 14 40 <.3 7 2 33 1.38 2 <a ~2 2 40 .3 <3 3 20 .04 .017 2 25 .03 390<.01 5 .35<.01 .12 2 <5 4 1 1 30 L3 101 c.3 80 38 1630 5.77 3 4 ~2 ~2 159 c.2 ~3 ~3 74 2.10 .266 27 111 .67 297 .I9 ~3 2.14 .43 .09 <2 <5 1 1 1 21 5 17 c.3 7 6 111 1.75 2 4 ~2 ~2 36 .4 <3 s3 a .ll .022 1 16 .03 522s.01 3 .ia .Ol .06 4 <5 <I <I 4 91 14 103 .5 24 8 130 4.62 ~2 4 ‘2 ~2 114 .7 <3 ~3 16 .13 .oai 3 15 .oa 1373s.01 4 .37 .oi .oa 2 ~5 4 2

5 75 44 165 .5 54 85 3695 4.95 5 4 ~2 ~2 aa s.2 <3 G 12 .29 .092 1 30 c.01 1544<.01 4 .30<.01 .oa 6 <5 4 1 1 71 IO 182 s.3 55 10 208 6.19 4 4 <2 <2 40 .7 <3 <3 19 .ia .031 1 13 .06 661~.01 3 .29<.01 .I1 ~2 ~5 ~1 1 1 26 a 11 <.3 5 2 61 2.30 <2 a ~2 e2 43 <.2 ~3 <3 16 .lO .017 2 21 .04 413c.01 4 .34 .Ol .I1 s2 c5 s1 4 1 7 7 4 s.3 4 1 3, .40 2 <a ~2 <2 103 c.2 ~3 ~3 4 .02 .04a 3 20 .OI 1012~.01 q3 .14<.01 .04 5 e5 <I 2 2 17 5 15 s.3 a I 37 .51 c2 9 c2 K2 38 s.2 c3 s3 6 .02 .018 2 30 .01 386s.01 ~3 .20<.01 .06 5 ~5 ~1 6

1 9 4 4 c.3 4 1 26 .90 6 8 ~2 2 6 s.2 c3 s3 9 .06 .003 2 16 .Ol a9s.01 4 .14<.01 .08 2 <5 Cl 2 1 5 17 12 s.3 6 3 393 .71 19 9 ~2 16 174 s.2 83 ~3 4 1.80 .015 21 16 .ll 56s.01 3 .37 .02 .ia 3 ~5 ~1 2

:1 25 16 79 c.3 3 4 384 2.92 3 4 <2 5 26 s.2 ~3 ~3 16 A4 .094 17 5 .67 659 .28 4 1.42 .03 .I9 2 <5 1 2

.84 .lll 5 2 5 7.69 .014 1 3 19.93 .003 4

c.2 <3 <3 34 1.62 .023 1

:1 4 5 12 q.3 4 1 286 .91 .lO<.Ol .02 <2 c5 4 <I 1 8 3 45 e.3 0 2 <5 Cl 1

:1 1 ~3 16 e.3 a 2 1185 3.47 3 <a .13<.01 .Ol <2 <1 :1 6 9 27 s.3 5 3 306 1.23 3 4 ~2 s 1 6 3 6 s.3 5 1 97 .57 <2 <a ~2 ( 32ls.01 ~3 .09<.01 .06 4 <5 s1 1

3 246 11 118 .6 41 2 22 3.47 55 .25 .163 10 i ~3 .a9<.01 .IO ~2 ~5 ~1 17 2 3 3 5 c.3 5 ~1 126 . 22 c.2 <3 <3 4 2.65 .Ol5 6 ~5 <I 1

3 <3 12 c.3 a ~2 ~2 20 .5 ~3 <3 6 4.20 .027 1 10 .22 274s. 3 <5 <I 1 6 691 468 639 4.3 148 ~8 ~2 4 14 3.6 ~3 G 245 .43 .061 19 72 1.35 220 .ll ~3 1 46 256 55 60 4.19 217 <a <2 6 17 3.6 4 3 198 .46 .068 20 79 .97 234 .I1 ~3 1.76c.O

36 164 5.7 35 12 724 3.39 56 22 2 17 29 25.0 14 23 76 .57 .Oa5 16 154 .66 145 .09 20 1.89 .04 .I6 20 ~5

ICP - .500 GRAM SAMPLE IS DIGESTED WITH 3ML 3-l-2 HCL-HN03-HZ0 AT 95 DEG. C FOR ONE HWR AND IS DILUTED TO IO HL WTN UAYER. THIS LEACH IS PARTIAL FOR MN FE SR CA P tA CR MC BA TI B U AND LlHITEO FOR NA K AN0 At. ASSAY RECDMMENOEO FOR ROCK AND CORE SAMPLES IF C" pa 2N AS > 1X, AG > 30 PP,, 8 A" > 1000 PPB . SAWLE TYPE: ROCK AU' - IGNITED, AQUA-REGIAIWIBK EXTRACT, GF,AA FINISHEO.(lO GW Samles beginning 'RE' we Reruns end 'RRE' we Reiect Reruns.

DATE RECEIVED: AU0 5 1997 DATE REPORT MAILED: @I d+

SIGNED BY . . ..O.TOYE, C.LEONG, J.UANC; CERTIFIED B.C. ASSAYERS

All results are considered the confidential property of the client. BSOM~S the Liabilities for actual cost of the analysis only. O&A _

IS”-9 :RW-1 SW-2 :RW-3 RN-4

RN-5 W-6

RW-7 RW-B-A

RRRW-&A

1 3 71.3 3.2 10.7 63 5 1 81 1.33 4.9 c5 c2 10 .06 .6 c.1 16 .02 .018 1 19 .01 157c.01 c3 .16<.01 .04 5c.2 155 c.3c.2 .5 81 6.5 233.9 9.4 212.3 699 33 6 49 6.38 28.9 7 3 104 .79 1.7 Cl 58 53 ,463 15 17 .06 166c.01 4 .58 .Ol .lB 4 c.2 194 5.6 .2 2.3 1

65.3 53.7 7.3 56.6 432 19 7 112 11.59 54.4 5 2 94 .29 2.0 <.I 17 9.09 ,026 3 2 .49 5c.01 ~3 .49 .Ol .14 ~2 .2 786 10.4 .3 2.1 66.1 77.5 5.5 73.9 190 10 4 54 15.27 52.1 8 ~2 50 .51 2.2 c.1 7 4.18 ,006 ~1 5 .13 8c.01

<I! ~3 .4lcOl .07 ~2 .5 601 4.3 .31.6 cl,

4.2 58.8 6.6 167.1 503 15 18 266 .88 5.0 4 ~2 543 3.87 1.7 <.I 58 16.70 ,279 18 8 .61 29lc.01 5 .38<.01 .12 ~2 c.2 91 .6 c.2 1.3 Cl

2.2 9.6 19.9 20.5 61 4 3 369 1.58 1.6 ~5 11 28 .06 .2 .3 3 .86 ,021 8 12 21 16kOl ~3 ,18<.01 .06 3 c.2 51 <,3 <,2 .8 .9 34.6 29.2 115.1 91 29 14 190 5.33 2.7 c5 18 20 .03 1.0 .5 10 .23 ,042 22 9 ,86 64c.01 ~3 .30<.01 .13 ~2 c.2 Cl! 47 c.3 c.2 1.0 <l

13.9 150.1 13.8 200.9 1712 31 7 48 2.90 30.0 ~5 2 77 1.30 6.3 e.1 108 .40 ,228 14 13 .06 398<.01 7 .59<.01 .21 ~2 c.2 337 7.8s.22.3 3 3~5 38~3 6.0 28547.9 804 5 2 666 1.83 e4.5 <5 2 525 291.01 Cl.8 c.9 27 15.89 ,021 19 4 4.91 23c.01 ~3 .06<.01 .02 2~1.8 10735 8.3~1.8 5.9 ~1; 5.0 39.6 <3 29521.9 726 5 2 689 1.88 4 <5 c2 545 300.30 ~2 ~1 28 16.33 ,022 20 3 5.04 2b.01 ~3 ,06<.01 .02 ~2 c2 11500 9.3 c2 7.0 4

RN-8-E 3,7 59.1 c3 50453.9 905 6 3 725 2.00 ~5 ~5 ~2 363 463.16 ~2 4 26 14.38 ,013 17 3 5.09 17c.01 ~3 .06<.01 .03 ~2 ~2 15068 8.2 c2 9.0 cl RW-B-C L5 10.5 e2.4 8455.2 <240 2 1 760 2.06 ‘4 ~5 r2 464 71.03 cl.6 c.8 11 18.61 ,005 24 1 5.74 129c.01 s3 .03~.Oic.O, ~2~1.6 2811 ~2.4~1.6 <4 I XI-1 cl.8 8399.4 15854.2 3675.3 99999 4 1 48 .16 385.4 23 3 32 36.69 5236.6 cl.8 1 .05 ,001 1 2 .OZ 11c.01 4 .05<.01 .02 6~3.6 1628 ~5.4~3.6 4 lf Y1~2 2.9 8214.2 17552.7 46186.6 99999 ~1 2 54 .34 283.1 286 2 30 192.92 3441.0 cl.3 4 .06 ,001 1 6 .03 12<.Oi ~3 .09<.01 .01 71 3.5 1836 <3.9<2.6<6.5 1B: &WARD DZiHG-500,A".R 26.7 132.5 104.6 285.7 1937 34 18 1033 4.29 70.4 21 19 56 2.03 10.7 22.7 76 .6? ,103 17 58 1.16 249 .15 22 2.29 .04 .69 23 2.4 479 .4 1.8 7.1 44i

ICP - 15 GRAM SAMPLE IS DIGESTED !A,,” 90 ML 3-l-2 HCL-HNOJ-HZ0 AT 95 DEG. C FOR ONE HWR AND IS DILUTED TO 300 ML VITH VATER. THIS LEACH IS PARTlAL FOR MN FE SR CA P LA CR MG BA T, B U AND LIMITED FOR NA K GA AND AL. SOLUTION ANALYSED DIRECTLY BY ICP. MO C" PB 2N AG AS AU CD SB B, TL HG SE TE AND GA ARE EXTRACTED UITH MIBK-ALIQUAT 336 AND ANALYSED BY ICP. ELEVATED DETECTION LIMITS FOR SAMPLES CONTAlN CU,PB,ZN,AiS>1500 PPM,Fe>ZOX. - SAMPLE TYPE: ROCK A"+ AQUA-REGIA,MIBK EXTRACT, W/AA FINISHED. Sawles beginning 'RE' are.Reruns and 'RRE' are Reject Reruns.

DATE RECEIVED: AUG 8 1997 DATE REPORT MAILED:,&,t&~ SIGNED BY.yy . . . . . . ..D.TOYE. C.LEONG, .,.VANG; CERTIFIED B.C. ASSAYERS

All results are considered the confidential property of the client. Acme assmes the liabilities for actual cost of the analysis only.

THlS LEACH IS PARTlAL FOR MN FE SR CA P LA CR MG BA 7, B w AN0 LlHlTEO FOR NA K AN0 AL. ASSAY RECDMMENOEO FOR ROCK AN0 CORE SANPLES IF C" PB ZN AS > 1%. AG > 30 PPH is A" > ,000 PPB - SAMPLE TYPE: ROCK AU* IGNITED, AQUA-REGlA/HIBK EXTRACT, GF,AA FINISNED.(lO GM),

DATE RECEIVED:

ALL results are considered the confidential property of the client. Acme as~mes the liabilities for actual cost of the analysis only. Data FA _

ARR!J- 1 73.98 14.51 .78 .a5 .26 .30 2.01 .68 .09 s.01 .016 1969 25 92 213 20 12 10 5.9 .02 x.01 51.99

99.64 ARRU-2 16.14 9.54 3.85 7.66 2.99 1.96 1.90 A.5 .I6 .Oll 1236 ~20 544 251 32 16 16 2.4 .02 ARRU-3

c.01 99.51 49.90 14.92 10.19 3.90 6.88 2.25 1.33 1.78 .68 .I5 .008 1113 22 491 239 30 15 15 7.3 .03 .03 99.51

RE ARRU-3 49.69 14.83 10.20 3.88 6.87 2.31 1.46 1.76 .69 .I5 .012 1095 22 535 242 30 19 15 7.4 .02 q.01 99.48

.200 GRAM SAMPLES ARE FUSED WITH 1.5 GRAM OF LIE02 AND ARE DISSOLVED IN 100 MLS 5X HN03. OTHER HETALS ARE SUM AS OXIDES. TOTAL C & S BY LECO (NOT lNCL"OE0 IN THE WN). - SAMPLE TYPE: ROCK Samples bwinnins 'RE' are Reruns and 'RRE' are Reiect Reruns.

DATE RECEIVED: AUG 5 1997 DATE REPORT MAILED: a IGB Ql c SIGNED BY.. .: C.LEONG, J.UANG; CERTIFIED B.C. ASSAYERS

ALL results are considered the confidential property of the client. Acme asswes the Liabilities for actual cost of the analysis only.

LAKE SEDIMENT SAMPLES

A-l 3.0 4.3 A-2 2.2 850.8 A-3 3.1 100.2 A-4 3.1 26.2 A-5 2.4 30.8

A-b 2.7 15.1 A-7 1.9 12.5 A-8 5.4 10.6 A-9 3.9 12.0 A-10 2.4 30.5

A-l, A-12 A-13 A-14 R-15

Tizard Explorations Inc. PROJECT KETCHIKA FILE # 9-l-3-778 Page 19 ‘tQ

2.0 12.0 7.2 23.4 2.0 23.7 2.7 15.4 2.3 13.6

A-16 ‘.I 19.7 RE A-16 ~ 3.6 18.2 A-17 2.1 14.7 A-18 2.8 14.6 A-19 2.2 19.9

A-20 1.8 21.6 A-21 1.7 23.7 A-22 ~ 3.1 21.5 A-23 4.8 67.0 A-24 6.0 40.0

A-25 2.9 lb.5 A-26 2.1 11.2 A-27 2.6 26.4 A-28 2.3 33.8 A-29 2.0 28.6

4.9 55.7 69 17 5 200 1.21 2.8 C5 <2 80 .56 .4 .2 25 2.30 .074 9 21 .32 406 .04 6 .71 .O, .04 ~2 c.2 58 1.9 c.2 2.8 1 8.i 61.1 196 18 8 166 1.71 3.7 C5 2 74 .48 .6 .1 45 2.04 .I20 16 31 .28 453 .04 3 1.14 .03 .05 C2 .2 71 5.1 C.2 4.4 Cl 4.1 98.6 102 26 8 185 1.04 3.8 ~5 ~2 84 .b3 .7 .9 23 2.43 ,087 8 22 .45 315 .03 7 .79 .02 .09 ~2 c.2 67 2.0 c.2 3.4 3 2.4 66.0 92 30 4 60 .$3 3.5 7 ~2 62 .43 .8 .3 16 1.73 ,053 3 15 .29 139 .O, 11 .33 .Ol .04 <2 c.2 47 3.0 c.2 2.5 2

3.4 44.0 64 20 4 170 1.05 2.2 <5 ~2 64 .37 .3 c.1 17 2.34 ,054 6 18 .45 318 .03 7 .65 .O, .05 ~2 c.2 43 2.4 c.2 3.0 1 1.6 17.3 57 4 2 191 .28 1.8 <5 <2 334 .I7 .3 c.1 6 22.99 .028 2 6 .37 732 .Ol 4 .I7 .Ol .02 <2 c.2 21 2.4 c.2 1.6 2

11.9 65.3 145 22 5 122 1.14 2.4 ~5 ~2 72 .b4 .5 1 :l

27 2.21 ,071 9 28 .50 372 .04 10 .73 .O, .07 ~2 c.2 77 4.2 <.2 2.6 1 15.9 96.3 197 28 8 291 1.51 3.1 5 2 78 .Pl .7 3, 2.55 .085 12 29 .56 415 .03 10 1.02 .Ol .09 <2 c.2 150 5.5 c.2 3.7 <l 10.3 81.5 183 25 8 335 1.80 5.2 ~5 ~2 65 .78 .5 .l 3, 7.77 ,082 10 27 .54 391 .04 4 .BBc.O, .08 ~2 c.2 89 4.0 c.2 3.5 <l

A-30 A-31 A-32 A-33 A-34

2.7 83.1 12.3 86.2 178 25 8 370 1.39 3.1 <5 2 109 .68 .5 1.1 30 5.02 ,088 9 28 .51 450 .03 12 .88 .Ol .12 ~2 C.2 123 3.6 c.2 2.9 1 1.7 29.9 12.4 78.3 167 24 8 1220 1.75 5.1 7 2 59 .b6 .4 .1 32 1.48 ,082 11 26 .41 467 .04 5 .85 .O, .08 ~2 .2 115 4.0 C.2 3.1 2 1.4 24.6 11.8 75.8 133 17 7 360 1.64 2.1 <5 2 74 .60 .S x.t 35 2.29 .071 12 27 .54 452 .06 5 1.02<.01 .07 <2 c.2 92 2.8 <.2 3.9 ~1 3.1 40.1 3.4 56.9 63 16 3 189 .89 1.9 ~5 ~2 82 .49 .2 .6 16 2.16 .105 5 16 .32 294 .02 9 .57 .02 .06 <2 C.2 55 2.2 C.2 3.0 5 3.3 24.5 3.0 93.4 67 11 1 76 .36 l.0 ~5 ~2 156 .%3 .4 .1 10 10.11 .070 3 8 .24 229 .Ol 9 .30 .O, .03 ~2 c.2 63 3.2 c.2 2.1 2

.9 5.0 <30 Cl 2 309 .38 1.9 <5 <2 407 .05 C.2 C.1 1 38.31 ,003 1 4 .b2 779<.01 ~3 .Ol .Olc.Ol <2 .2 <lO .3 C.2 .5 Cl 4.2 81.3 272 22 3 74 .97 1.5 ~3 <2 61 1.02 .3 22.7 21 2.21 ,091 7 21 .33 346 .03 6 .70 .01 .05 12 C.2 115 2.0 .4 2.8 5 8.0 60.9 120 18 6 251 1.53 5.0 ~5 2 95 .55 .5 2.3 28 3.17 ,107 7 22 .39 570 .02 7 ..31 .02 .07 2 c.2 77 2.0 c.2 4.2 2

10.1 58.3 175 24 7 507 2.71 21.2 ~5 2 78 .64 1.5 .2 48 1.83 .lOl 9 25 .32 846 .02 6 .80 .O, .Ob ~2 s.2 144 6.1 s.2 3.4 4 9.5 80.3 167 21 8 505 2.83 17.0 ~5 3 @a .75 1.0 .5 47 3.02 .103 10 25 .33 760 .02 6 1.03 .Ol .Ob ~2 c.2 115 4.9 c.2 3.7 ~1

7.6 64.3 78 20 6 314 1.50 10.4 ~5 2 90 .54 .6 .l 22 3.36 .OR 7 20 .32 524 .02 9 .81 .Ol .05 ‘2 s.2 55 5.3 c.2 3.1 1 9.6 57.7 72 17 7 230 1.51 12.2 ~5 3 45 .44 .5 c.1 20 1.16 .050 10 21 .27 428 .02 6 .91<.01 .05 ~2 c.2 43 5.1 C.2 3.1 Cl 1.3 56.6 46 12 5 86 .39 2.0 ~5 ~2 65 .25 .2 c.1 5 1.92 .084 7 8 .18 302 .O, 11 .24 .Ol .02 <2 ~2 39 .7 C.2 1.7 Cl

.5 25.5 ~30 1 1 308 .24 1.4 ~5 ~2 236 .ll c.2 .l 1 20.00 .ou 1 2 .23 767s.01 7 .07 .o, .Ol c2 s.2 15 .5 C.2 .a 4 3.8 75.8 134 24 4 145 .79 7.9 ~5 <2 61 .97 .5 .1 18 1.76 .113 6 19 .32 288 .02 14 .70 .03 .Ob <2 q.2 77 2.2 C.2 2.6 1

5.3 45.4 89 17 3 232 .83 3.0 ~5 2 172 .44 .4 c.1 20 7.80 .047 6 16 .b8 352 .03 3 .49 .02 .06 ~2 c.2 49 2.0 c.2 2.1 3 2.3 38.1 53 9 2 344 .63 3.4 C5 C2 646 .33 .5 .5 13 19.54 .029 2 7 .60 305 .02 4 .22 .02 .05 ~2 .2 20 2.9 c.2 1.7 4 6.7 63.1 119 16 3 127 1.05 1.8 ~5 <2 96 .79 .5 .2 19 2.34 .ow 7 18 .32 484 .02 8 .58 .O, .04 ~2 q.2 67 2.0 c.2 2.8 1 5.0 49.6 118 13 3 107 .b4 7.9 ~5 <2 59 .68 .5 .1 20 1.44 ,067 6 lb .27 320 .02 5 .59<.0, .05 ~2 c.2 44 1.0 c.2 2.5 ~1 3.1 42.9 52 9 4 206 1.37 5.2 4 ~2 133 .74 .4 .2 15 3.84 .082 4 31 .2b 530 .02 11 .30 .Ol .03 <2 ~2 52 10.4 c-2 1.7 <1

7.3 54.7 125 19 9 172 1.85 3.7 ~5 ~2 113 .b4 .5 c.1 33 3.10 .I05 10 47 .58 se4 .05 8 1.32 .O, .Ob ‘2 c.2 37 12.8 c.2 4.9 6.6 53.7 99 21 10 lb4 1.85 3.5 ~5 ~2 115 .39 .4 c.1 33 3.18 .103 10 47 .59 611 .05 12 1.31 .02 .05 ~2 <.2 39 12.1 c.2 4.7 5.5 46.4 78 12 5 288 1.22 3.0 <5 <2 93 .77 .3 c.1 22 2.02 .085 7 39 .32 h78 .03 6 .b2 .O, .04 ~2 c.2 47 11.7 <.2 2.9 5.7 66.6 106 16 7 415 1.64 2.6 ~5 ~2 97 .63 .4 c.1 32 2.16 ,098 10 42 .43 532 .04 8 .83 .02 .05 ~2 c.2 32 7.1 <.2 3.2 6.1 60.3 82 19 7 147 1.38 2.0 7 2 71 .54 .3 .I 32 1.56 ,087 12 36 .37 409 .05 <3 1.00 .Ol .05 ~2 c.2 45 6.6 <.2 3.5

3 1 1 2

-Cl

5.7 57.8 97 17 6 235 1.67 3.1 ~3 r2 8.8 .58 .3 <., 26 2.66 .091 10 28 .34 452 .04 3 .77 .02 .05 <2 c.2 51 6.1 C.2 3.5 1

STAWOARO z24.0 114.6 100.9 248.8 1923 29 15 947 4.24 70.7 21 18 59 1.96 8.7 22.5 68 .77 ,098 17 53 1.13 240 .I4 25 2.18 .05 .b4 17 2.9 440 .9 2.4 7.3 49

Standard is STANOARO DZIHC-5001AU-5. Samples beginnins 'RE' are Reruns and 'ME are Reject Reruns.

ALI results are considered the confidential property of the client. Acme assmes the Liabilities for actual cost of the enalysis Only. Data- FA _

SAMPLE11 / "o C" Pb 2n Ag Ni Co Hn Fe P LB CT Hg Ba Ti 8 AL Wa K U Tl "9 Se Te ta Au+

/Fw ppn FW ppn ppbwppn pp" XPppnppn xrm xppn % % 'IppnPp"mppnFvwppb

A-35 A-36 ~ ;:; ,;:; 2.0 .6 24.6 6.9 ~30 41 12 2 ~1 2 178 4, .03 .55 <.5 1.0 ~5 ~5 ~2 ~2

A-37 4.6 5.7 120.6 19.3 4.4 1.1 139.9 60.6 70 80 16 5 3 1 215 119 1.52 .50 12.9 c.5 <5 6 ~2 ~2

274 193 141 .,5 .29 .39 :; .5 3.2 :: 7 5 1 39.18 8.68 6.64 .007 .051 .059 2 1 1 6 3 , .38 .29 .18 473c.01 369 151 .Ol .Ol 23 5 7 .03 .24 .18 .Ol<.Ol .02 .02 .03 .03 ~2 ~2 2 c.2 c.2 <.2 cl0 4, 14 1.6 1.6 .5 c.2 c.2 c.2 c.5 1.6 1.3 Cl 4 1 I /

A-38 ~ 181 .TI .4 <., 2, 8.72 .078 4 10 .36 142 .Ol 11 .38 .02 .08 <2 S.2 57 3.7 c.2 1.1 -d / i

A-39 i 1.8 49.9 13.6 219.3 330 50 10 415 2.04 9.3 ~5 3 127 1.59 1.3 .5 4, 4.33 .090 11 26 .74 404 .03 9 .94 .02 .,2 ~2 <.2 114 9.3 c.2 2.6 4

I

A-40 A-41 A-42 A-43 A-44

A-45 A-46 A-47 A-48 A-49

2.0 32.3 13.5 226.3 364 37 9 547 2.55 6.8 ~5 2 133 1.66 1.2 ., 45 4.12 .125 10 24 .90 441 .Ol 7 .78 .02 .12 <2 c.2 162 5.1 c.2 2.2 2 2.3 38.0 6.0 85.5 106 27 4 79 1.09 1.4 5 <2 68 1.04 .6 ., 27 2.00 .097 9 25 .38 414 .04 9 .85 .02 .06 ~2 c.2 163 2.6 c.2 3.1 1 2.9 9.6 1.8 78.8 <30 7 2 395 .77 1.9 ~5 ~2 76 .33 .3 <.I 6 2.39 .087 2 5 .22 328 .Ol 12 .31 .02 .04 <2 C.2 15 .7 C.2 1.3 <l 1.9 14.8 8.1 63.7 76 20 8 410 2.28 8.7 6 2 73 .50 .6 .2 26 2.62 .079 11 23 .30 653 .02 6 .93 .Ol .05 ~2 c.2 47 4.5 s.2 2.7 <l 5.9 203.7 6.5 165.2 354 42 9 146 1.17 4.3 7 C2 41 1.17 .6 3.3 44 1.05 ,170 11 35 .41 363 .03 5 1.46 .03 .I1 3 .7 88 1.0 C.2 5.1 3

5.6 199.5 6.5 114.5 285 26 5 207 .70 .5 7 C2 45 .99 .6 4.9 29 .99 .204 8 24 .27 373 .02 16 1.09 .04 .13 3 c.2 116 1.2 c.2 3.0 3 2.4 65.1 5.6 58.6 126 16 10 536 2.23 1.8 10 <2 94 .52 .3 1.4 35 2.28 .108 14 25 .31 685 .03 8 .93 .02 .06 ~2 c.2 53 2.8 c.2 2.9 4 1.9 24.7 7.2 73.5 133 18 10 466 2.29 1.6 6 ~2 84 .49 .4 .2 44 1.72 .137 20 31 .33 538 .05 4 1.15 .03 .06 <2 c.2 77 2.7 c.2 3.4 4

15.4 17.9 4.1 88.4 <30 20 3 82 .81 4.8 12 ~2 67 .50 .5 .I 21 1.42 .059 5 19 .32 167 .03 13 .59 .02 .06 ~2 .8 24 1.6 .2 3.4 <1 15.8 28.9 4.2 106.4 126 25 5 62 1.28 1.7 19 <2 54 1.01 2.0 .I 23 1.38 ,073 4 22 .28 72 .02 17 .48 .02 .05 C2 C.2 45 12.1 C.2 1.9 <l

A-50

B-2 NE B-4 8-3

B-4

9 1.45 .054 3 11 .I8 133 .02 5 .37 .02 .04 ~2 c.2 17 <.3 c.2 1.6 ~1

.03 ,081 10 19 .27 2 .02 11 .77 .02 .09 <2 C.2 .9 C.2 3.0 2 3.01 ,090 13 23 .50 7 1.29 .02 .17 ~2 c.2 0 2.3 c.2 3.6 3

<2 40 .39 .4 7 12 .20 2 .4 .2 2.4 i

1.0 24.9 2.6 57.2 4.1 32.4 2.0 22.5 1.7 24.5

7 5 102 .44 15 4 97 2.10 20 4 8.6 1.31

8 2 72 .54 11 3 82 .67

3.13 .092 15 25 1.53 .093 13 25 1.62 ,091 22 23 1.52 .087 13 20 1.54 .086 18 23

3 33.06 .OOP I 10

6 1.38 .02 .20 <2 c.2 7 7 1.51 .02 .18 <2 c.2 0 5 1.40 .03 .13 ~2 c.2 56 4 .80 .02 .09 <2 C.2 78 7 1.03 .02 .ll <2 C.2 87

<3 .07 .02 .02 <2 C.2 -30 7 1.06 .02 .12 <2 c.2 150

3 .02 12 .51 .02 .04 ~2 9 .88 .03 .16 ~2 c. 87 8 1.20 .03 .I5 <2

. J 76

<. 105

9 .71 .03 .12 4 .06 .03 .02

10 .87 .02 .08 5 .81 .02 .lO

322 .02 6 .73 .02 .08

2.4 c.2 4.0 2 8.0 q.2 4.6 3 5.9 C.2 4.9 1 2.0 C.2 2.4 2 2.6 c.2 3.7 2

Tizard Explorations Inc. PROJECT KETCHIKA FILE # 97-3778 Page 20 us UlllnilDI

B-5 B-6 B-7 B-8

B-9 1.7 4.2 E-10 1.3 29.9 8-17 1.9 20.8 B-12 4.1 26.1 B-13 1.7 38.3

B-14 6.9 40.2 B-15 2.5 3.3 B-16 2.2 21.8 B-17 5.9 21.0 8-18 2.7 17.5 .6 82.6 157 14 5 231

9 ~2 329 .15 10 3 94 .65

8 C2 85 .58 14 3 191 1.09 17 5 97 .w+

20 2 160 .90 9 <2 507 .10

11 2 111 1.27 16 2 128 .98 18 3 87 .79

30 2.25 ,084 9 24 29 2.91 ,092 9 22 27 2.32 .077 12 22

-zz C. 82 <2< 18 <2 < 88

f

<2 < 2 83 C2 2 64

.8 <.2 c.5 6 2.6 c.2 3.3 4

.3 .2 1.5 1 4.4 C.2 2.4 Cl 5.3 C.2 4.0 3

6.0 c.2 2.6 2 1.6 c.2 c.5 1 5.0 C.2 3.0 4 3.5 c.2 2.7 ~1 3.1 c.2 2.7 4

STANDARD 124.9 123.6 101.7 264.9 2088 30 17 ,025 4.48 78.9 25 19 59 2.11 10.1 22.7 70 .80 .,08 17 53 1.18 259 .I4 23 2.22 .06 .71 17 2.5 447 .6 2.2 7.4 43

Standard is STAHOARO OZ/HG-500/A@5. SanvLes beqinning IRE' are Reruns and 'ME' are Reiect Reruns..

Documents

GEOCHEMICAL, GEOPHYSICAL & PROSPECTING REPORT ON … · 2004. 5. 3. · GEOCHEMICAL, GEOPHYSICAL & PROSPECTING REPORT ON THE KECHIKA PROPERTY A - CLAIM BLOCK Al to A24 Claims Dease