report oil novj - ontario€¦ · 2 .28404 island copper report on fall drilling program november-...

Amerigo Resources Ltd.

Report oilNovJ

41K09NW2005 2.28404 AWERES 010

2 .28404

Island Copper

Report On Fall Drilling Program

November- December 2002

John Gamier, M.Sc. and Roger Moss Ph.D., P.Geo.

Technical Report prepared for

Amerigo Resources Ltd.

April, 2003

Table of Contents

Title Page.......................................................................................................................j

Table of Contents............................................................................................................H

List of Figures.................................................................................................................Hi

List of Tables...................................................................................................................Hi

List of Photo-plates.........................................................................................................iv

List of Appendices...........................................................................................................iv

Summary .........................................................................................................................l

1. Introduction................................................................................................................^

2. Location and Access ...................................................................................................5

3. Previous Work............................................................................................................. 7

4. Regional Geology........................................................................................................ l O

5. Geology, A Iteration and Mineralization of the Island Copper Property....................13

6. Geology of the Diamond Drill Holes..........................................................................20

6.1 DDHICO2-1.................................................................................................20

6.2DDHICO2-2.................................................................................................31

6.3DDHICO2-3.................................................................................................36

6.4DDHICO2-4.................................................................................................42

7. Sampling and Quality Control....................................................................................45

8. Conclusions and Recommendations ...........................................................................51

9. References...................................................................................................................55

Certificate for J. Cornier ................................................................................................57

Certificate for R. Moss....................................................................................................58

Appendices......................................................................................................................59

List of Figures

Figure I.... Location of Island Copper...........................................................................3

Figure 2.... Claims map..................................................................................................6

Figure 3.... Geology of the Island Copper property .......................................................14

Figure 4.... Location map of drill holes..........................................................................21

Figure 5.... Diagram of Long Section.............................................................................22

Figure 6.... Cross-section ofIC02-l ...............................................................................26

Figure 7.... Cross-section of IC02-2...............................................................................32

Figure 8.... Cross-section ofIC02-3...............................................................................37

Figure 9.... Cross-section of IC02-4...............................................................................43

List of Tables

Table l .....Claims list.....................................................................................................4

Table 2 .....Previous work...............................................................................................8

Table 3 .....List of sample numbers and summary of Au, Cu and Ag for IC02-1............23

Table 4 .....List of sample numbers and summary of A u, Cu and Agfor IC02-2 ............24

Table 5 .....List of sample numbers and summary of A u, Cu and Agfor IC02-3 ............25

Table 6..... List of sample numbers and summary of Au, Cu and Agfor IC02-4 ............25

Table 7 .....List of sample numbers ICO2-1....................................................................46

m

Table 8.....List of'sample numbers ICO2-2....................................................................47

Table 9 .....List of sample numbers ICO2-3....................................................................48

Table 10...List ofsample numbers ICO2-4 and standards............................................49

List of Photo-Plates

Photo-plate 1...................................................................................................................16

Photo-plate 2...................................................................................................................18

Photo-plate 3...................................................................................................................19

Photo-plate 4...................................................................................................................30

Photo-plate 5...................................................................................................................41

List of Appendices

Appendix l: Drill logs

Appendix 2: Assays

Appendix 3: Expenditures

IV

Summary

The Island Copper property is an iron oxide copper gold (IOCG) prospect located

approximately 19 kilometres northeast of Sault Ste Marie, Ontario. The property hosts

significant copper mineralization accompanied by minor gold, hosted in hematite-rich

albite granite breccia at or near the contacts with Gros Cap Batholith granite and

granodiorite gneiss and brecciated gneiss. The mineralized albite granite breccia occurs

at or near the intersection of major structural lineaments. The copper mineralization

occurs as chalcopyrite associated with iron oxides and pyrite.

A four-hole diamond drill program was undertaken by Amerigo Resources Ltd. on the

Island Copper property during November and December of 2002. A total of 992 meters

was drilled in four holes numbered IC02-1, IC02-2, IC02-3 and IC02-4. The drill

program was designed to test the depth extent and continuity of previously outlined

historic copper and gold mineralization, and to test chargeability and residual gravity

anomalies. The anomalies discovered by geophysical surveys, included airborne heli-

mag, ground gravity, and induced polarization conducted by Falconbridge Ltd. in 2000.

The drilling intersected iron sulphide and copper mineralization, and K and Fe-O

alteration in all four holes. Significant intersections Include 4A^o Cu over 2 metres and

l.52^o over 8 metres in drill hole IC02-1. This section also includes gold values of 0.5

g/t over 3 metres.

Amerigo is currently earning a 55/4 interest in the property from Falconbridge Ltd.

1. Introduction

The Island Copper iron oxide copper gold (IOCG) property is located approximately 20

kilometres northeast of Sault Ste. Marie in the province of Ontario (Figure 1). It covers

an area of approximately 705 hectares comprised of four unpatented claims 1239731,

1239732, 1239733 and 1239734 held by Falconbridge Ltd., three freehold patents held by

the YMCA of Sault Ste. Marie, and two leasehold patents held by the Nystedt Family of

Sault Ste Marie.

Under an option-joint venture agreement signed January 21, 2002 with Falconbridge

Ltd., Amerigo Resources Ltd. has the right to earn a 55*^ interest in the Island Copper

property by spending 5250,000 on exploration and issuing 200,000 shares to

Falconbridge over a three year period. As part of Amerigo's first year expenditure

commitment, a 4-hole drill program was completed in December, 2002, to test the

continuity and depth extent of known mineralization as well as chargeability and gravity

anomalies that were recently delineated by Falconbridge. Historic copper and gold

assays up to 6.22Vo Cu and 1.7 g/tonne Au over 3.05 metres within a 9.5 meter

intersection grading 4.02*^ Cu and 1.03g7tonne Au were obtained during a 1965 drilling

program conducted by Kennco Explorations (Canada) Ltd.

The exploration target on the Island Copper property is Olympic dam type

mineralization. Similarities between Island Copper and IOCG deposits elsewhere in the

world were described by Gamier and McLellan (2000).

Figure 1: Location of the Island Copper property near Sault Ste Marie, Ontario, Canada.

Table 1: Claim disposition of Island Copper as of March 22, 2003.

Owner

Falconbridge Limited




Nystedt Family, Sault St Marie

YMCA, Sault Ste Marie

Claim Number

1239731

1239732

1239733

1239734

Leasehold Patent

Freehold Patent

Recording Date

September 01, 1999

September 01, 1999

September 01, 1999

September 01, 1999

N/A

N/A

Due Date

September 01 , 2008

September 01, 2008

December 09, 2008

September 01 , 2008

N/A

N/A

Claim Unit Size

8

3

8

4

2 blocks surface and mining rights

3 blocks surface and mining rights

Standing

Good

Good

Good

Good

Current

Current

2. Location and Access

The Island Copper Property is located approximately 20 kilometres northeast of the port

town of Sault Ste. Marie, Ontario, and north of the cottage community of Island Lake

(Figure 2). It is situated north and northwest of the junction between Highway's 556 and

552, and straddles Highway 552. The Algoma Central Railway line (ACR) passes on the

southern boundary of the property adjacent to Highway 556. A 5-car spur line is located

off a gravel quarry located on the eastern side of the property. This quarry is leased from

the YMCA by DCI Investments of Sault Ste. Marie and is accessed from the east side of

Highway 552 across from the historic adit and main hilltop Cu-showing.

To minimize environmental impact and degradation, the drill holes were accessed by a

drill road cut over an old and overgrown forestry access road built during the late

nineteen seventies for logging purposes. Wherever possible, drill roads to individual drill

sites followed these existing forestry roads. Water lines were laid along the existing grid

lines and along the roads. Water used for drilling was taken from a pond adjacent to the

westernmost drill hole. All trees knocked down during access were bucked into l metre

lengths and left at the side of the roads. No knocked-down or cut trees were left hanging

in the brashes of other trees, and meticulous care was exerted by both the geologists and

St. Lambert Forage drill crew to leave the area as pristine as possible.

Figure 2: Location claims map of the Island Copper property and surrounding area.

TOPOGRAPHICl 1

f" ]

Administrative Boundaries

Township

CoXDauton. Lot

PrtnrtncM Park

Indian Reserve

Contour

Mine Shats

Mkne Headbwie

Railway

Road

Matura! Ga* Pipeline

Land TenureFraehoW Patent

Surface And Mining Right*

Surface Rights Only

Mining RlgMs OnlyL*|

Leasehold Pa lent

j~^l Surface And Mining Rights

n,7| Surface Rjghd Only

r^l Mining Rlgnts Only

Licence ol Occupation

PT] Uses No! Specified

l A l Surface And Mintng Rights

pn Surface Rights Only

|~1 Mining Rtghte Only

L|J Land USB Permll

hy~\ Order In CouncM (Not open lor staJung)

C^T] Water POWB' Lease Agreemert

r ~ ~ ~ ~'l I234ser i

l 1234567 l

Mining Claim

Filed Only Mining Claims

LAND TENURE WITHDRAWALS

'34 l Areas Withdrawn Irom Disposition

Mining AcU Withdrawal Types Wsm Sortaca And Lining Rflhn WarioHm

Wm Mining Kghli On*y WrMFtdfviViiOrdar In Council Withdrawal Types

W* SITl Surt.cn And l In. mg Rjgtils Wiindisv.ilW*S Surfat* Rlghli Only Viindn^m"/m hVloig Kgnit Onl, Wstxlrawn

IMPORTANT NOTICES

rosoooE 71WOOE

B1T5000N

Island CpppSTFropertyV, YMCA Patents , ,;.

TransCanada SasteMaHighway -w Kilometres

UTM zou. IB Map is captured and modified from Ministry of Northern Development and Mines. Mining CLAIMaps III website.sooooigrw http^-Vbrww.mndm govon ca/nnndnVmines/lands/damiapa/

3. Previous work

Although exploration on the property appears to date back for almost one hundred years,

there are no documented reports of work prior to the 1960's. Work performed since the

1960's is summarized in Table 2 and discussed below.

Copper mineralization was discovered in the area over 90 years ago. However, very little

information about early exploration is available. An historic exploratory adit exists on

the property indicating the extent of previous work. Exploration in the 1950's culminated

with some diamond drilling; however, no detailed records can be found. Detailed

assessment research by both Highland-Crow Resources Ltd. in the eighties, and

Falconbridge Limited in 2000 did not find any records of the early drilling.

The Geological Survey of Canada (1964) and the Ontario Geological Survey (1965)

carried out regional reconnaissance mapping over the area. This was coincidental with

prospecting in 1965 by Kennco Explorations (Canada) Ltd. near the old adit, and led to

the discovery of the hilltop showing. The discovery inspired further work including grid

cutting, geochemical surveys, geological mapping, geophysical surveys that included

ground EM, resistivity and IP, and the blasting of numerous trenches in exposed

mineralization. The work concluded with 2,700 feet of diamond drilling in 14 drill holes.

Other than the historic drill logs, no record of the core was found.

Other work includes prospecting and diamond drilling in 1970 by Mr. H. Nystedt of Sault

Ste Marie, who drilled 503 feet in two drill holes southwest of the hilltop showings.

Copperville Mining Corp Ltd. optioned the property in 1970 and 1971, and drilled 10

Table 2. Summary of previous work on the Island Copper Property (Mumin and Gamier,

2002, Gamier and McLellan, 2000).

Year of Work Name of Company Work Carried Out

Pre 1960 Unknown, no records were found of the companies or prospectors who previously worked the area.

Early prospecting led to the drifting of a historic adit. Diamond drilling was reported to have occurred in the 1950's, although no detailed records have been recovered.

1964 to 1965 Geological Survey of Canada; Ontario Geological Survey

Regional geological reconnaissance mapping.

1965 -1966 Kennco Explorations (Canada) Ltd.

Prospecting, geological mapping, geophysics, geological sampling and geochemical assaying, diamond drilling (18 diamond drill holes; 2700 feet {822.96 m})

1970 H. Nystedt Prospecting and diamond drilling (2 diamond drill holes; 503 feet {l53.31 m})

1970-1971 Copperville Mining Corp. Diamond drilling (10 diamond drill holes; 3,558.6 feet {1084.66m})

1981 - 1982 Highland-Crow Resources Ltd.

Geological mapping, geochemical sampling, line cutting,

2000-2001 Falconbridge Limited Airborne magnetic survey, I.P. survey and gravity survey, geological mapping, geochemical sampling, line cutting

2002 Amerigo Resources Ltd. and Falconbridge Limited

Joint venture agreement and diamond drilling.

diamond drill holes for a total of 3,559 feet. Other companies that have worked in the

area include Delta Minerals, Tri-Bridge, and Colleen Copper.

Approximately 10,000 feet of diamond drilling in at least 43 historic drill holes has been

recorded on or adjacent to the property. Unfortunately, the core is not recoverable and

lays scattered amongst the leaf litter covering the property.

As a result of regional reconnaissance program conducted during 1980 and 1981,

Highland-Crow optioned the property from the YMCA of Sault Ste Marie and Mr.

Nystedt in 1981. Highland-Crow's exploration included geological field mapping and

geochemical sampling; however, they did not continue with any additional work on the

property. No further work was carried out until Falconbridge optioned the property in

late 1999, and staked additional contiguous ground to the north and west of the YMCA

and Nystedt properties. In the spring of 2000, Falconbridge flew airborne radiometrics

over the entire property. This was followed in 2000 by gridline cutting, detailed

geological mapping and geochemical sampling (Gamier and McLellan, 2000). The

Nystedt property was optioned by Falconbridge in the fall of 2000, with detailed

geochemical sampling and geological mapping conducted in 2001 (Gamier and

Oosterman,2001).

4. Regional Geology

The geology on the property has been described in detail by Gamier and McLellan, 2000;

Gamier and Oosterman, 2001; and Mumin and Gamier, 2002, and is summarized below.

The Island Copper property is composed of steep hilly terrain in the southern and central

portions of the property, while the northern area drops steeply at first, then gently towards

the Goulais River valley. The region is covered with a mixture of outcrop and

overburden consisting of glacial tills in varying thickness covered by humus. Outcrop

exposure occurs predominantly along rock ridges, hilltops and cliff faces. The area is

overgrown with thick stands of maple alternating with cedar and spruce. Drainage along

the northern portion of the property is towards the Goulais River and forms deep ravines

with fast-flowing creeks. Drainage is relatively poor in the central highland area of the

property, forming occasional swamps and beaver ponds between the hills with surface

water available for diamond drilling (Gamier and McLellan, 2000).

The property occurs in moderately to strongly foliated Archean gneissic-granitoid rocks

of the Gros Cap Batholith, immediately north of the Archean-Proterozoic boundary. The

boundary is delineated by the Highway fault (Proterozoic boundary fault) that parallels

Highway 556 and the ACR rail line. This fault separates Proterozoic aged clastic rocks

of the Aweres Formation in the Upper and Lower Island Lake areas from Archean gneiss.

To the north and northwest of the property, clastic rocks of the Cambrian-aged

Jacobsville Formation unconformably overlie the Archean rocks (Gamier and McLellan,

2000).

Gros Cap Batholith rocks encompass the majority of the outcrop exposures on the

10

property. The gneissic rocks are composed of granite and granodiorite that have been

strongly to moderately foliated, and contain localized migmatitic units. At several

locations, the gneiss appears intensely sheared, altered, and crosscut by east-west

trending chlorite-altered amphibole schist. The gneiss has been further intruded by

numerous gabbroic to fine-grained diabase dikes of at least three different ages. Larger

dikes trend in a west-northwest direction and display a gabbroic texture, moderate to

weak magnetism, and weak chloritization. Finer grained, moderately to strongly

magnetic diabase dikes trend hi a northwest direction. Several, southeast trending and

north-south trending dikes of strongly magnetic biotite-lamprophyre comprise the

youngest mafic intrusive units (Gamier and McLellan, 2000).

The Gros Cap gneiss is locally brecciated in the eastern area of the property adjacent to

the north-northwest trending Island Lake fault. This brecciation covers an extensive area

of the south-west portion of the property (Gamier and McLellan, 2000). Anastomosing

stockworks of quartz veins of varying widths occasionally crosscut and silicify the

breccia. Associated with the quartz veins are infrequent, parallel trending veins and

veinlets of specular and earthy hematite. These occasionally crosscut the quartz veins

and occur as coatings along fracture walls (Gamier and McLellan, 2000).

Fe-oxide and copper mineralization is confined primarily to localized albite-rich granite

bodies that exhibit sharp contacts within the brecciated gneiss. These granite units

display crackle or shatter brecciation, with specular hematite, chalcopyrite and

occasionally chlorite-altered amphibole schist veins forming the matrix. Copper

mineralization within this albite-rich granite does not extend into the Gros Cap breccia

(Gamier and McLellan, 2000).

11

The area is structurally complex and exhibits zones of intense faulting. Bennett and

Innes (1977) state that the Archean-Proterozoic boundary, or Highway Fault, is a thrust

or reverse fault trending northeast along the southern boundary of the property (Innes,

1983). This fault has been interpreted to represent the northern margin of the Lake Huron

Graben Structure. The north-northwest trending Island Lake Fault crosscuts the gneiss

on the eastern side of the property and is visible hi outcrop along Highway 552. The

Island Lake fault appears to be truncated and offset by the Highway Fault. The

brecciated gneiss is primarily concentrated along the Island Lake Fault, and represents

cataclastic brecciation formed in a zone of structural weakness, at the intersection of the

two faults (Gamier and McLellan, 2000).

12

5. Geology, Alteration and Mineralization of the Island Copper Property

Geological mapping of the Island Copper property was completed by Falconbridge

Limited in 2000 and 2001, and is discussed in detail in Falconbridge technical reports by

Gamier and McLellan (2000), Gamier and Oosterman (2001). Further discussion of the

property is presented in an independent geological assessment report by Mumin and

Gamier (2002).

The majority of the rock on the property consists of Gros Cap gneiss (Figure 3). The

gneiss consists of light gray to pink granite and granodiorite, comprised of plagioclase,

quartz, and biotite hornblende. It displays a strong to moderate fabric or gneissic

layering. Localized zones of migmatite consisting of alternating wispy bands of Fe-rich

minerals are set in white quartz and pink feldspar, and in one location the gneiss is

strongly albitized (Gamier and McLellan, 2000).

Gros Cap gneiss is extensively brecciated in the eastern portion of the property straddling

the north-northwest trending Island Lake fault on both sides of Highway 552. The

gneissic breccia is recognized by angular to subrounded and occasionally stretched

fragments, with moderate to well-defined gneissic layering still well-preserved.

Fragments are set in a black to greenish-black matrix of occasionally silicified, chlorite-

altered amphibole schist. The fragments are easily identified by the preserved gneissic

fabric and differential weathering between the gneissic fragments and matrix. Some of

the fragments exhibit intense potassic and/or hematite alteration (Gamier and McLellan,

2000). Silicification is apparent in the breccia fragments and often overprints the matrix.

Quartz also forms anastomosing to fragmental white quartz veins and veinlets between

13

Figure 3: Geology of the Island Copper Property

Legend

Amphibole Schist

Mafic Intrusive Dikes

Alkali Granite

Brecciated Gros Cap Gneiss

Gros Cap Gneiss

Aweres Formation

Thrust Fault

x Fault

4k Inferred Amphibole Schist

Inferred Mafic Dikes

Inferred Alkali Granite

Inferred Brecciated Gneiss

Inferred Gros Cap Gneiss

Lake l River

Contact l Inferred Contact

Road

Railway Line

O v x\\N* ^

the fragments. Larger quartz veins crosscut both the massive and brecciated gneiss,

forming anastomosing veins and stockworks that parallel the Island Lake fault. Some of

these quartz veins are not continuous, but appear to have been fractured and dislocated

(Gamier and McLellan, 2000).

Hematite and chalcopyrite mineralization are confined to outcrops of pink albite-rich

granite that intrudes the brecciated gneiss. This albite-rich granite appears to be a

separate rock unit composed of SO-85% pink to pinkish-white albite crystals intermixed

with K-feldspar and minor quartz, set within a microcrystalline quartzo-feldspathic

groundmass (Camier and McLellan, 2000). The unit has undergone crackle or shatter

brecciation with hematite (specularite) and chalcopyrite mineralization forming the

matrix and alternating with occasional chlorite-altered amphibole schist veins. This

granite does not exhibit gneissic layering or fabric and is interpreted as a separate rock

unit. The contact between the albite-rich granite and brecciated gneiss is sharp, with a

very narrow chill margin extending into the albite-rich granite suggesting the gneissic

breccia was lithified prior to emplacement of the albite-rich granite (Photo-plate 1).

Further evidence for this is suggested by the lack of hematite and chalcopyrite

mineralization extending beyond the albite-rich granite and brecciated gneiss contact.

However, some specular hematite veining associated with late quartz-filled fractures

extends into the brecciated gneiss (Camier and McLellan, 2000).

The albite-rich granite comprises a large portion of the cliff face where the historical adit

is located and outcrops at several locations to the north along Highway 552. However,

the main showing with abundant hematite and chalcopyrite mineralization within the

15

Photo-plate l.

Plate A and B: Photographs of the contact between the Gros Cap brecciated gneiss and

the Fe-oxide rich alkali granite. White dotted line indicates the sharp contact

between the two units. The hematite (specularite) was confined to the alkali

granite and not observed extending across the contact. Photographs taken by J.

Gamier in 2000, during geological mapping of the property for Falconbridge Ltd.

he-Oxide rich Atkali Gfanit

16

albite-rich granite is located between L88+OON and L91+OON on L100+OOE on top of the

hill above the adit (Photo-plate 2). Only one exposure of the albite-rich granite occurs on

the east side of highway 552, located along L91+OON in historical trenches cut into a cliff

face (Photo-plate 3). The trenches provide excellent exposures of hematite and

chalcopyrite mineralization within the matrix of the albite-rich granite (Gamier and

McLellan, 2000). Detailed observation of the outcrop face indicates the unit may have

been faulted and juxtaposed against unbrecciated gneiss (Gamier and McLellan, 2000).

Also observed on the eastern side of Highway 552, the majority of quartz veins appear to

parallel the Highway Fault and trend in a north-northeast direction.

17

Photo-plate 2.

The photographs are from the hilltop showing and were taken by J. Gamier during

geological mapping of the property in 2000 for Falconbridge Ltd.

Plates A and B: Photographs of the contact (dotted white line) between brecciated Gros

Cap gneiss and Fe-oxide rich alkali granite. The supporting matrix of the

brecciated gneiss is weakly chloritized amphibole schist with occasional

anastomosing veins of epidote. Fe-oxide and malachite staining on surfaces of the

brecciated alkali granite are from weathered specular hematite and chalcopyrite,

which form the matrix. No sulphides or hematite were observed in the brecciated

gneiss.

-Malachite '

Fe-0/ich * t - Alkali Granhe

IS

Photo-plate 3

Photographs are of the only albite granite showing that occurs on the east side of

Highway 552, and were taken by J. Gamier during geological mapping of the

property for Falconbridge Ltd.

Plate A: Photograph of the Fe-oxide rich alkali granite intruding into the Gros Cap

brecciated gneiss. Contact is illustrated by the white dotted line. Fe-oxide

alteration of the alkali granite is evident on the weathered surface by the reddish-

brown staining. Chalcopyrite veining occurs near the contact with the brecciated

gneiss, but does not extend into the gneiss.

Plate B: Photograph of Fe-oxide rich alkali granite intruding into the Gros Cap

brecciated gneiss. The reddish brown staining on the surface of the alkali granite

is from weathered anastomosing veins of specular hematite that occur within the

granite. Also visible is a sulphide pod containing pyrite and chalcopyrite

mineralization. No sulphides were observed in the brecciated gneiss.

6. Geology of the Diamond Drill Holes

A four-hole diamond drill program was undertaken by Amerigo Resources Ltd. on the

Island Copper iron-oxide copper-gold (IOCG) property near Sault Ste. Marie, Ontario,

during November and December of 2002. A total of 992 meters were drilled in four

holes numbered IC02-1, IC02-2, IC02-3 and IC02-4. Locations of the drill holes on the

property can be found in Figure 4. The drill program was designed to test the depth

extent and continuity of previously outlined historic copper and gold mineralization, and

to test recent chargeability and residual gravity anomalies. The following subsections

describe in detail the geology and mineralization observed within the drill holes. A wire-

diagram long section with a corresponding cross-section for holes IC02-1, IC02-2 and

IC02-3 are found in Figure 5. Assay summaries of Cu, Ag and Au are listed in Tables 3,

4, 5 and 6 for all four holes. Diamond drill logs are attached in Appendix l and assay

results are in Appendix 2.

6.1 DDHIC02-1

Diamond drill hole IC02-1 is located on L89+OON at L99+80E at the summit of the hill

above the historic adit. Azimuth of the drill hole is 2650 and inclination is -500 from the

horizontal. Total depth of the drill hole is 418 metres. The hole was collared into

brecciated and mineralized alkali granite under 3 metres of glacial and swampy

overburden. A cross-section of the hole is illustrated in Figure 6.

The first unit encountered within the drill hole consists of brecciated albite-rich granite

with a veined matrix of specular hematite and chalcopyrite pyrite, alternating with

20

Legend* 2002 Drill Hole

Historical Drill Hole

1.5/8.0 Cu (070 yintersection (m)

500

Meters

ISLAND COPPER PROJECTAmerigo Resources Ltd^^^

Island Copper Project Drill Hole Location Plan

Figure 4: Historic and recent drill hole locations.Drawn by. J. Camter/R. Moss Date: 21/02/2003

Figure 5: Plan A and cross-section B of DDK's IC02-1, IC02-2 and IC02-3. Dashed

lines indicate gridline, solid lines represent UTM co-ordinates. Alkali granite

hosted in the Gros Cap breccia is outlined in the dashed pink line.

5172500N 517230QN 5172200N

708600E

7085005

Overburden [J Alkali Granite Brecciated Gneiss | Ultramafic Dyke (Lamprophyre)

Microgabbro Flj Schist j Quartz Stockwork

Heterolithic Fault Breccia M Cu Mineralization

ISLAND COPPER PROJECTAmerigo Resources Ltd

Section: Long SectionJjfawn by: J. Camjet f R. MOM T 0818:21/02/2003 Scale_______ l Long SacOon N-S

Table 3: Summary of Cu, Ag, and Au assay results.DDH IC02-1

Hole ID

IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1

Sample

1408414035140861408714088140891409014091140921409314094140951409614097140981409914100141011410214103141041410514106141071410814109141101411114112141131411414115141161411714118141191412014121141221412314124141251412614127

Depthfrom

345678910111213141518213132394041

52.2253.2254.2255.2256.2257.2258.2259.2160.2261.25

72737475

81.582.583.586.2587.2588.2589.2590.2591.25

93

to4567891011121314151821243233404142

53.2254.2255.2256.2257.2258.2259.2160.2261.2562.59

73747576

82.583.584.587.2588.2589.2590.2591.25

9394

Lengthmetres

11111111111133311111111111

0.991.011.031.34

111111111111

1.751

Cu496943913229598160711447186365373794827131731

210194276

5687

13120533737

21226642917267820401511

149135310912

4132678607569157

23491801554

AssayAu (ppb)

5994694432311

5610*2*253^^^^^^*26^*2^^^^^*2^^^^^^^^^^^*22^^^^

Ag (ppm)1.11.30.52.91.2O.30.40.90.50.51.40.4O.30.4O.3O.3O.3O.30.30.3O.3O.3O.3O.30.30.30.30.50.30.4O.3O.3O.3O.31.10.3O.30.40.40.30.510.50.7O.3

Hole ID

IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1

Sample

1412814129141311413214133141341413514136141371413814139141401414114142141431414414145141461414714148141491415014151141521415314154141551415614157141581415914160141611416214163141641416514166141671416814169141701417114172

Depthfrom9495105106

136.38137.38138.38139.38140.48

159160161162163

163.86165.46166.96

168169170171172173183184185192193194195196197198199200201202203204205206207208209

to9596106107

137.38138.38139.38140.38141.38

160161162163

163.86164.85166.96

168169170171172173174184185186193194195196197198199200201202203204205206207208209210

Lengthmetres

11111111

0.91111

0.860.991.51.04

111111111111111111111111111

Cu2976728913787332344112386445339441133361222485443322 el

2

AssayAu (ppb) Ag (ppm)

^ 2.3*2 0.5^ 0. 3^ 0. 33 0.3^ 0. 3^ 0. 3^ 0. 3^ 0. 3^ 0. 3^ 0. 3^ O.3^ 0. 3^ 0. 3^ 0. 3*2 0. 3^ 0. 3^ O.3^ 0. 3^ 0.3^ 0. 33 O.34 O.3^ 0. 3^ 0.3^ 0. 316 O.3^ 0. 36 O.3^ 0.35 0.3^ O.3^ 0.3^ 0. 3^ O.3^ 0. 3^ 0.5*2 0. 3^ 0. 3^ 0. 3^ 0. 3^ 0. 3^ 0. 3^ 0. 3

Table 4: Summary of Cu, Ag, and Au assay results for DDH IC02-2. DDHIC02-2

Hole ID

IC02-2IC02-2IC02-2IC02-2IC02-2IC02-2IC02-2IC02-2IC02-2IC02-2IC02-2IC02-2IC02-2IC02-2IC02-2IC02-2IC02-2IC02-2IC02-2IC02-2IC02-2IC02-2IC02-2IC02-2IC02-2

Sample

14178141791418014181141821418314184141851418614187141881418914190141911419214193141941419514196141971419814199142001420114202

Depthfrom14151617181920212262636667686970717273747576777879

to15161718192021222363646768697071727374757677787980

Lengthmetres

1111111111111111111111111

Cu642517793335149

781751122588

216

1458633715

AssayAu (ppb)

^^^0^^^2^^^53^10^20^^^^^^^^

Ag (ppm)O.3O.30.30.3O.30.3O.3O.3O.3O.30.3O.3O.30.3O.3O.30.40.3O.30.3O.3O.30.30.32.4

Hole ID

IC02-2IC02-2IC02-2IC02-2IC02-2IC02-2IC02-2IC02-2IC02-2IC02-2IC02-2IC02-2IC02-2IC02-2IC02-2IC02-2IC02-2IC02-2IC02-2IC02-2IC02-2IC02-2IC02-2IC02-2

Sample

142031420414205142061420714208142091421014211142161421714218142191422014221142221422314224142251422614227142281422914230

Depthfrom808182838485868788

208.04209210211212213214215216217218219220242243

to818283848586878889209210211212213214215216217218219220221243244

Lengthmetres

111111111

0.9611111111111111

Cu34711242721032310747

43361339888430637611030183754010

AssayAu (ppb)

^^787^^^^^^^^^^55^^^^^19^

Ag (ppm)0.52.30.4O.3O.30.40.3O.30.30.60.70.81.21.32.20.81.21.52.00.90.70.45.3O.3

(si

Table 5: Summary of Cu, Ag, and Au assay results for DDH IC02-3. DDH IC02-3

K)

Hole ID Sample Depthfrom

IC02-3 14030 6!C02~3 14031 7 5IC02-3 14032 9IC02-3 14033 10.5IC02-3 14034 12IC02-3 14035 15IC02-3 14036 18IC02-3 14037 21IC02-3 14038 24IC02-3 14039 30IC02-3 14040 31.5IC02-3 14041 46.81IC02-3 14044 87IC02-3 14045 105IC02-3 14046 106.5IC02-3 14047 120IC02-3 14048 121IC02-3 14049 122IC02-3 14050 123IC02-3 14051 124IC02-3 14052 125IC02-3 14053 126IC02-3 14054 127IC02-3 14055 128IC02-3 14056 156

to7.5g

10.5121518212427

31.533

47.3188.38106.5107.74

121122123124125126127128129157

Lengthmetres

1.51.51.51.533333

1.51.50.5

1.381.5

1.241111111111

AssayCu Au (ppb)78 ^

5305 *221 ^14 ^14 223 ^1 22 ^3 ^3 ^3 ^

153 ^8 3

75 ^116 ^6 ^4 ^4 74 54 ^4 ^2 *3.1 ^2 43 ^

Ag (ppm)O.3O.30.3O.30.50.30.3O.3O.3O.3O.3O.3O.3O.30.3O.30.3O.3O.30.6O.3O.3O.3O.3O.3

Hole ID Sample

IC02-3 14057IC02-3 14058IC02-3 14059IC02-3 14060IC02-3 14061IC02-3 14062IC02-3 14063IC02-3 14064IC02-3 14065IC02-3 14066IC02-3 14067IC02-3 14068IC02-3 14069IC02-3 14070IC02-3 14071IC02-3 14072IC02-3 14073IC02-3 14074IC02-3 14075IC02-3 14076IC02-3 14077IC02-3 14078IC02-3 14079IC02-3 14080

Depthfrom157158159160161162163164165166170171172173174180181186187188

197.5198.25

199200

to158159160161162163164165166167171172173174175181182187188189

198.25199200201

Lengthmetres

11111111111111111111

0.750.75

11

Cu22813743322247

2631332433

35017278

AssayAu (ppb)

^^*2^^33^^44^^^^^^^34^^^6

Ag (ppm)0.30.30.30.30.40.30.3O.30.3O.3O.3O.3O.3O.3O.3O.3O.3O.3O.3O.3O.30.4O.30.3

Table 6: Summary of Cu, Ag, and Au assay results for DDH IC02-4.DDH IC02-4

Hole ID Samplefrom

IC02-4 14001 12IC02-4 14002 47IC02-4 14003 72IC02-4 14004 81IC02-4 14005 87IC02-4 14006 93IC02-4 14007 99IC02-4 14008 114IC02-4 14009 126IC02-4 14010 138IC02-4 14011 150IC02-4 14012 162IC02-4 14013 189IC02-4 14014 192IC02-4 14015 195

Depthto155075849096102117129141153165192195198

Lengthmetres

333333333333333

AssayCu Au (ppb)3 ^

21 ^4 ^5 ^2 ^97 ^155 ^134 ^155 ^139 ^141 ^139 ^28 ^25 ^15 ^

Ag (ppm)0.50.3O.3O.3O.3O.3O.30.3O.30.3O.3O.30.30.30.3

Hole ID Sample

IC02-4 14016IC02-4 14017IC02-4 14018IC02-4 14019IC02-4 14020IC02-4 14021IC02-4 14022IC02-4 14023IC02-4 14024IC02-4 14025IC02-4 14026IC02-4 14027IC02-4 14028IC02-4 14029

Depthfrom198201204207210213216219222225228231234237

to201204207210213216219222225228231234237

239.5

Lengthmetres

3333333333333

2.5

Cu2931968735504949508269243810

AssayAu (ppb)

^^30^^^^^53^^^2

Ag (ppm)0.3O.30.80.3O.3O.3O.31.50.6

10.4O.3O.3O.3

Figure 6: Cross-section of DDH IC02-1.

DDH IC02-1 Az. 2650 1 -500

Surface

ir

'oS*? "x\O^ ^c

\ \ eg'j*

cf

E.G.H. 252m

Key CA* Core Axis

l Overburden H Alkali Granitel Brecciated Gneiss | Ultramafic Dyke (Lamprophyre)

l Microgabbro | Mineralization


IC02-1 Cross-SectionDrawn by J Carn*w i R Moss^ Scale____' i 'i.roo ' ' .

Dale, j'iffi'atobaLong Secfcn N-S"

amphibole chlorite veins. The unit extends from 3.00 metres to 12.13 metres. The

fracture breccia is comprised of subhedral to euhedral whitish-pink albite plagioclase

phenocrysts set in a pink aphanitic quartzo-feldspathic groundmass. The albite

phenocrysts are randomly oriented, fractured and occasionally corroded on their edges.

They display well-formed polysynthetic twining visible on crystal faces with the unaided

eye. Local weak to moderate hematite K alteration imparts localized reddish-brown

colouration to the granite. This is most prominent along fractures that emanate off the

matrix into the granite.

The matrix consists primarily of metallic, silver-coloured specular hematite that forms

anastomosing veins and veinlets supporting the brecciated fragments of alkali granite.

The predominantly specular hematite occasionally contains reddish-brown earthy

hematite that often rims some fragments and coats late fracture walls. Sulphide minerals

consisting of chalcopyrite and pyrite alternate with hematite in the matrix. Chalcopyrite

locally forms up to 10*M) of the rock, occurring as anhedral blebs, veins and veinlets that

often rim granite fragments. It is intergrown with up to 207o pyrite and trace amounts of

bornite. Pyrite generally occurs as aggregates of subhedral to euhedral grains within the

matrix. Below 4.5 metres up to Wo sulphides occur, but appear to diminish with depth.

It was observed that as pyrite increases in the matrix, chalcopyrite decreases, and as

chalcopyrite increases, pyrite decreases. Both chalcopyrite and pyrite were also observed

as blebs within granite fragments. Occasionally alternating with the hematite and

sulphide matrix, are veins and veinlets of moderately to intensely chloritized amphibole

schist that locally replaces the hematite as the dominant matrix mineral. Pyrite as

euhedral grains and aggregates was the only sulphide observed associated with the

27

amphibole schist.

The section between 3.0 and 10.0 metres contains the bulk of the copper mineralization.

The upper one meter of the unit between 3.0 and 4.0 metres contains 4.9"^o Cu, which

decreases to S.9% Cu between 4.0 and 5.0 metres. From 5.0 to 11.0 metres the Cu grade

drops to an average of Q.5% over the 6 metres. Average grade between 3.0 and 11.0

metres is l .520/^ over 8 metres (Table 3). The section also includes gold values of 0.5 g/t

over 3 metres between 3.0 and 6.0 metres depth.

The lower section of the alkali-granite contains a late fracture that is filled with calcite-

rich fault gouge and finely comminuted Iron-oxide altered reddish-brown alkali granite

fragments supported by the calcite minerals. The fault crosscuts the core between 10.70

and 10.88 metres at 350 to the core axis. This fault marks the lower contact and trends

500 to the core axis. The walls of the fault contain intensely chloritized amphibole schist

and white quartz veining.

Gros Cap granite gneiss breccia occurs between 12.13 and 52.22 metres. It is comprised

of fracture brecciated granite gneiss alternating with crosscutting zones of greenish-black

chloritized amphibole schist. Within the schist are occasional gneissic fragments and

discontinuous vermicular veins of quartz and an unknown mineral that exhibits intense

pink to reddish-pink potassic alteration. The section is further crosscut by numerous

quartz-filled fractures and quartz-vein stockwork containing occasional clots of

specularite and chalcopyrite mineralization. Some veins contain earthy-red hematite

staining along fracture walls. Pyrite mineralization was observed in the schist as

subhedral to euhedral aggregates and individual crystals.

28

Between 52.22 metres and 62.59 metres is a brecciated Fe-O and K altered alkali granite

that has a sharp upper contact with the brecciated gneiss. This contact is marked with

slickensides and weakly chloritized amphibole schist. The alkali granite contains angular

to subrounded fragments composed of subhedral, broken phenocrysts of albite

plagioclase supported in a pink to red hematite and potassium altered quartzo-feldspathic

groundmass. The fragments are matrix to clast supported, with a matrix of fine-grained

amphibole schist and quartz; veining (Photo-plate 4).

Sulphides occur as chalcopyrite and pyrite at trace to Wo locally. Chalcopyrite

mineralization consists of anhedral grains and blebs occurring hi the matrix and

groundmass of the fragments. Pyrite forms crosscutting veins and veinlets of subhedral

to euhedral granular aggregates. Copper mineralization within this section grades G.28%

over 6.37 metres, between 56.22 metres and 62.59 metres (Table 3).

Gros Cap gneissic breccia occurs between 62.59 metres and 94.32 metres, 101.60 metres

and 150.19 metres, and 152.62 metres and 252.00 metres. The gneissic breccia is

described above.

Mineralized gneissic breccia crosscut by high angle (subparallel to core axis) quartz veins

occurs in the lower section from 62.59 to 94.32 metres. The quartz veins are comprised

of white to translucent quartz and contain minor anhedral blebs and veinlets of

chalcopyrite. Copper mineralization grades Q.27% over l metre, between 86.25 metres

and 87.25 metres, and Q.20% over 2.75 metres, between 90.25 metres and 93.00 metres.

Overall, the quartz veined section has elevated copper mineralization of 67 ppm to 2678

ppm between 86.25 metres and 94.32 metres (Table 3).

29

Photo-plate 4: Photograph of drill core in DDK IC02-1 between 52.22 and 62.59

metres depth. The section is near the lower contact and illustrates the Fe-oxide

and K-alteration to the alkali granite breccia. The matrix is composed of weakly

to moderately chloritized amphibole schist.

An Iron-oxide and biotite-rich lamprophyre dike crosscuts the gneissic breccia between

94.32 metres and 101.60 metres. The unit is black, fine to very fine-grained, exhibits

moderate to strong magnetism and is crosscut by numerous earthy-red hematite and white

medium-grained calcite veins that trend at 500 to the core axis. The upper and lower

contacts are marked by calcite alteration extending over l metre into the lamprophyre at

either contact. Copper mineralization grades 297 ppm from 94.00 and 95.00 metres and

67 ppm between 95.00 and 96.00 metres (Table 3).

Between 150.19 metres and 153.62 metres, a fine-grained greenish-black non-magnetic,

weakly to moderately chlorite altered diabase dike crosscuts the gneissic breccia. The

upper contact is sharp, while the lower contact is marked by a friable fault gouge

comprised of sand and gravel fragments including diabase and calcite. Occasional

subangular xenoliths of gneiss are caught within the diabase groundmass. These

xenoliths display alteration rims of up to 5 mm and are intensely iron-oxide altered to a

reddish-brown. Primary gneissic textures in the fragments are well-preserved.

The bottom of the hole at 252.00 metres consists of fracture brecciated gneiss crosscut by

quartz vein stockwork. No sulphide mineralization was observed in the quartz veins.

6.2DDHIC02-2

Diamond drill hole IC02-2 is located at L88+OON and L100+3 OE. The azimuth of the

hole is 0850, inclination is -50" and total depth is 257.0 metres. A cross-section of the

drill hole is illustrated in Figure 7. The drill hole is collared in Gros Cap granite gneiss

breccia under 3 metres of glacial overburden. The gneissic breccia extends from 3.00

31

Figure 7: Cross-section of DDH IC02-2

metres to 65.30 metres. It is comprised of Fe-O and K altered, and silicified fracture

brecciated gneiss with alternating matrix and clast-supported sections. The matrix is

composed of greenish-black moderately chloritized amphibole schist, forming

anastomosing veins and veinlets in the clast-supported sections. Matrix-supported

sections contain angular fragments of gneiss up to 2 cm in diameter that are generally less

poorly sorted and comminuted. Sulphide mineralization occurs as granular aggregates of

subhedral to euhedral grains of pyrite and pyrrhotite supported wholly within the

amphibole matrix.

Iron-oxide rich alkali granite occurs between 65.30 metres and 95.87 metres. The upper

50 em's of the contact is friable and intensely blocky, comprised of sand, mud, gravel and

angular fragments of alkali granite and gneiss surrounded by calcite mineralization. The

alkali granite is comprised of subhedral to euhedral white to pink albite plagioclase

phenocrysts that exhibit well-defined visible albite twinning. The phenocrysts are set

within a fine-grained to aphanitic, quartzo-feldspathic pink to reddish-brown fracture

brecciated groundmass. Hematite alteration within the granite is either pervasive or

occurs as wispy tendrils of reddish-brown alteration fingering into the pink silicified

groundmass. Occasional pink potassium feldspar phenocrysts are intergrown with the

plagioclase. Rounded quartz eyes were observed scattered throughout the groundmass.

The matrix of the fracture brecciated granite is platy metallic-silver specular hematite and

earthy-red hematite, alternating and occasionally intergrown with anastomosing veins and

veinlets of chloritized amphibole schist.

Sulphide mineralization consists of pyrite and chalcopyrite (locally up to 20A) and trace

33

pyrrhotite. Pyrite occurs as subhedral to euhedral grains forming veins, veinlets and

granular aggregates within both the hematite and amphibole schist matrices.

Chalcopyrite occurs as anhedral grains in the groundmass of the granite and as veinlets,

veins and blebs within the matrix. Pyrrhotite occurs as subhedral to euhedral grains

randomly scattered in the amphibole matrix. Copper mineralization within this section

grades at G.35% between 80.0 and 81.0 metres (Table 4).

Heterolithic fault breccia occurs between 95.87 and 117.48 metres, 118.24 and 172.73

metres, 174.40 and 197.30 metres, 199.82 and 208.04 metres, and from 221.40 metres to

the end of the hole at 257.00 metres. The breccia is comprised of comminuted, matrix

supported, rounded to angular, silicified, grayish Gros Cap granite gneiss fragments

intermixed with rounded to angular fragments of pink alkali granite. Variable intensities

of Fe-O and K-alteration affect all the fragments, and the gneiss is identifiable by still

visible gneissic layering. The breccia commonly grades into zones of intensely altered

fragments supported hi chloritized amphibole schist. Fragment outlines are visible

depending on the degree of alteration. Some exhibit pervasive reddish-brown hematite

alteration. Chlorite alteration of the schist varies from weak to intense. No sulphides

were visible in the matrix or fragments. These heterolithic breccias exhibit textures and

alteration features that are remarkably similar to diatreme breccias.

A strongly magnetic, fine-grained, black to dark-gray lamprophyre dike crosscuts the

heterolithic breccia between 117.48 and 118.24 metres. No sulphides are associated with

this unit. Between 172.40 and 174.40 metres a weakly to moderately magnetic, fine

grained greenish-black to dark-gray diabase dike intrudes the breccia. It contains

numerous rounded xenoliths of heterolithic breccia supported within the groundmass.

34

The unit is crosscut by numerous calcite quartz veins and veinlets that plunge 750 to

perpendicular the core axis. A similar unit was noted between 197.30 to 199.82 metres.

A significant discovery in this drill hole was the intersection of Fe- and K-

metasomatized, reddish-brown quartz-feldspar porphyry (QFP) that exhibits comparable

characteristics to the Keweenawan-aged Fe- and K-metasomatized quartz-rich felsic

intrusives observed along the Lake Superior coastline associated with the Mid-

Continental Rift near Mamainse Point. The upper contact is sharp with a 2 cm chill

margin extending into the QFP. The contact is marked with l cm of amphibole

alteration. The reddish-brown QFP is comprised of fine to medium-grained feldspar

phenocrysts alternating with 1-3 mm rounded quartz-eyes set in a fine-grained, sugary-

textured Fe- and K-metasomatized groundmass. Pink to reddish-brown feldspar

phenocrysts comprise lS-20% of the rock and are weakly to moderately Fe- and/or K-

metasomatized. The feldspars alternate with ragged greenish amphibole clots.

Occasional veinlets of chlorite epidote emanate from the amphiboles. Sulphides are

occasionally associated with the amphibole clots. Quartz-eyes comprise 20-3 QVo of the

rock. Very-fine veinlets of reddish-brown hematite surround the quartz grams and

occasionally intrude into the grains along minute fractures or crystal faces. A three metre

section of the unit is intensely bleached and altered by amphibole chlorite and/or

epidote alteration, imparting a pale green to green-black colour to the rock.

Sulphide mineralization consists of pyrite at between l and 5^o locally and trace

chalcopyrite. The pyrite is strongly associated with the amphibole clots hi the

groundmass. Chalcopyrite was observed associated with the pyrite, as occasional

35

anhedral blebs along the edges of amphibole, and as minute anhedral blebs within the

groundmass. The QFP exhibits only background copper levels of between 13 to 110 ppm

(Table 4).

6.3DDHIC02-3

Diamond drill hole IC02-3 is located at L91+OON and L99+35E. The inclination of the

hole is 900 and total depth is 243.0 metres. A cross-section of the drill hole is illustrated

in Figure 8, and assay results are listed in Table 5. The hole was collared in a diabase

dike under 2.10 metres of overburden. The unit is comprised of fine-grained, black to

dark gray, strongly magnetic and weakly chloritized diabase. No visible sulphides were

observed within the unit. The unit has a sharp lower contact at 5.87 metres.

Brecciated Iron-oxide rich alkali granite and granite gneiss were encountered between

5.87 and 46.08 metres. Angular to subangular fragments of breccia and comminuted

materials are clast to matrix supported. The matrix is comprised of weakly to moderately

chloritized amphibole schist forming anatomising veins and veinlets. Quartz forms a

stockwork of veins and veinlets that crosscut the section. Late calcite veins also form a

stockwork that cuts both the breccia and quartz. Calcite veins comprise S-10% of the

section. The walls of both the quartz and calcite veins are coated with earthy red

hematite and occasional specularite. Late anastomosing hematite veins crosscut the

entire section.

Alkali granite fragments contain subhedral to euhedral, fractured and occasionally

ragged, pink to white-pink albite phenocrysts with well-developed twinning set in a pink

to reddish-pink quartzo-feldspathic groundmass. The groundmass is weakly to

36

Figure 8: Cross-section of DDH IC02-3.

Microgabbro (Diabase) Dike

Fe-O rich Alkali Granite 0.53 07oCu over 1.5m from 7.5 to 9.0m

50m X- ^

Microgabbro (Diabase) Dike v '

Gros Cap Granite Gneiss Breccia



Microgabbro (Diabase) Dike100m

350

GA

600 CA

35Q GA

90" GA

DDH IC02-3 Az. O l -90C

or<

o <

150m O 4

Gros Cap Granite /-s Gneiss Breccia /s

200m

Amphibole Schist Gros Cap Granite Gneiss Breccia Quartz Stockwork

O

O <

o <

Q

0

?5To <

KeyB Overburden

l Brecciated Gneiss

| Microgabbro

CAsCoreAn9'e

Alkali Granite

Quartz Stockwork

Schist

Mineralization

500 CA

150 CA E.O.H. 243.0m


1C 02 -3 Cross-SectionDrawn By J Gamier l R. Moss SaS________1.1.000

Data: 21/02/3003Lwo Swakx. N^S

moderately Fe- and K-altered. Occasional specks of sulphide minerals were observed

within the groundmass too small to be identified. The granite gneiss fragments contain

plagioclase, potassium feldspar and quartz, and still exhibit primary gneissic layering. A

well-developed fabric allowed easy identification of the gneiss. Neither the fragments or

matrix display any evidence of gneissic layering. Intense pervasive and turbid Fe-O and

K-alteration was observed in some of the granite gneiss fragments, and well-defined

gneissic layering is still preserved in some reddish-brown clasts.

Sulphide mineralization within the sections consists of pyrite hi trace amounts to S 0/**

locally, chalcopyrite in trace to 407o locally, and trace amounts of pyrrhotite. Pyrite

occurs as subhedral to euhedral grains and aggregate clusters within the matrix.

Chalcopyrite occurs as anhedral blebs and discontinuous veins and veinlets within the

matrix and occasionally in the alkali granite fragments. Some blebs were observed

within the gneiss; however, these were always associated with fractures emanating off the

matrix into the fragment. Copper assayed at Q.53% over 1.5 metres between 7.50 and

9.00 metres (Table 5).

A crosscutting, non-magnetic, weakly-chloritized, fine-grained, greenish-black diabase

dike occurred between 46.08 and 58.98 metres. The unit was crosscut by a sulphide vein

with pyrite and chalcopyrite. Fragments of gneissic breccia are contained within the

lower margin of the dike, and still have a recognizable fabric. Two other diabase dikes

occur between 73.64 and 78.00 metres, and 88.38 and 107.74 metres. Both units exhibit

a weak to moderate magnetism, are greenish-black, fine-grained and weakly to

moderately chloritized. Trace sulphides consisting of euhedral pyrite and pyrrhotite

38

occur as grains within the groundmass.

Brecciated Gros Cap granite gneiss occurs at 58.98 to 73.64 metres, 78.00 to 88.38

metres, 107.74 to 227.90 metres, and 231.98 to 241.19 metres. The breccia consists of

angular to subangular fragments of previously described gneiss with well-developed

gneissic layering in clast and/or matrix-support. The matrix is comprised of fine-grained,

weakly to moderately-chloritized amphibole schist. Breccia fragments display varying

degrees of weak to moderate Fe-O and/or K alteration. A number of fragments exhibit

pervasive and intense Iron-oxide alteration, with very little trace of the original protolith

visible. Discontinuous broken veins of very-fine-grained, iron-oxide altered reddish-

brown unidentified silicified material was observed within the matrix. This material was

also observed periodically in some sections of the clast-supported breccias. Sporadic,

intense sericite alteration is visible as bleached units up to 10 cm wide below 175 metres.

The greenish-black to black matrix forms anastomosing veins and veinlets in the clast

supported sections. In matrix-supported sections, fine-grained matrix minerals comprise

nearly 60*Mi of the rock with narrow sections up to 85*54. These sections contained

comminuted angular fragments of gneiss that average l to 2 mm in diameter with

occasional larger fragments. Careful examination by hand lens reveals a gneissic fabric.

However, some fragments do not exhibit any fabric, are fine-grained and intensely Iron-

oxide altered. These zones are interpreted to be mylonites. Occasional larger breccia

fragments exhibit rotational textures with trains of comminuted material emanating off

the fragments. These breccia fragments do not exhibit any perceptible reaction rims.

Several sections within the breccia appear to be entirely comprised of amphibole schist

and contain no fragments whatsoever. These sections are interpreted as fault gouge, and

39

generally are under a metre wide. However, a 4.08 metre wide section occurs between

227.90 and 231.98 metres (Photo-plate 5). A number of these sections are iron-oxide

altered and silicified.

Quartz veins and veinlets crosscut the breccia and schist at varying degrees of 300 to 500

to the core axis. The veins on occasion form anastomosing stockworks and are generally

between l to 5 mm hi width, although some veins were up to several centimetres wide.

The abundance of quartz veins decreases substantially with depth, and only occur as

infrequent veinlets below 195.00 metres. The quartz veins abruptly appear between

227.90 and 231.98 metres as up to 3 cm veins. Within the veins are numerous angular

fragments of fine-grained amphibole schist. Quartz flooding begins at 241.19 metres and

intensifies to the bottom of the drill hole. Locally the quartz stockwork supports angular

fragments of amphibole schist and Fe-O K-altered fragments. No sulphides were

observed in this unit.

Calcite veins up to 3 cm in width crosscut the breccias, matrix and quartz veins.

However, with increasing depth, the calcite veins trend parallel to the quartz veins.

These veins also decrease in abundance with depth.

Sulphide mineralization occurs only within the matrix, consisting of pyrite, pyrrhotite and

chalcopyrite. Pyrite varies from trace amounts to Wo locally, as subhedral to euhedral

grains, aggregate clusters, and occasional veinlets. Pyrrhotite occurs in trace amounts,

primarily as individual subhedral to euhedral grams and occasional aggregates.

Chalcopyrite occurs only as trace amounts forming sporadic anhedral blebs in the matrix.

Assays for drill hole IC02-3 are listed in Table 6.

40

Photo-plate 5: Photograph of the drill core in DDH IC02-3, showing a pyrite

mineralized quartz-flooded fault zone supporting brecciated fragments of

amphibole schist. The contact at 231.98 metres depth is with weakly to locally

intense Fe-oxide and K-altered Gros Cap brecciated gneiss. The matrix for the

brecciated gneiss is weakly- to moderately-chloritized amphibole schist. The

photograph also shows good examples of both fracture brecciated and matrix

supported Gros Cap brecciated gneiss that resembles a hydrothermal breccia.

6.4DDHIC02-4

Diamond drill hole IC02-4 is located at L88+96N and L94+54E. Inclination of the hole

is 900 and total depth is 239.5 metres. A cross-section of the hole is illustrated in Figure

9, and assay results are listed hi Table 6. The hole was collared in silicified Gros Cap

granite gneiss breccia under 4.0 metres of glacial and muskeg overburden. The gneissic

breccia is comprised of angular to subrounded fragments of granite gneiss with well-

preserved gneissic layering. The mostly gray-white to reddish-brown gneiss fragments

are comprised of plagioclase and potassium feldspar phenocrysts alternating with

rounded quartz grams (20*Xi) set in a quartzo-feldspathic groundmass. Feldspar

phenocrysts exhibit turbid iron-oxide alteration. Fragments are matrix to clast-supported

hi silicified and weakly chloritized, very-fine-grained amphibole schist. The matrix

forms anastomosing veins and veinlets and contains numerous angular clots of calcite

mineralization. Quartz veins crosscut the core at between 3 O0 and 900 to the core axis,

are between l to 5 mm wide, and form a stockwork within the unit. The lower contact at

41.80 metres is marked by an 8 cm wide fault gouge composed of clay, mud and sand.

Between 41.80 and 45.00 metres a brecciated ultramafic intrusion crosscuts the granite

gneiss. It is comprised of angular to subangular black to greenish-black, non-magnetic

soft fragments hosted in a quartz and calcite vein stockwork. Late, earthy hematite filled

fractures up to 3 mm wide crosscut the unit subparallel to the core axis. Some fragments

display a crenulation or schistose cleavage that is suggestive of movement. The lower

contact is undefined and gradational into a diabase dike that extends to 56.93 metres

depth. The greenish-black diabase is weakly chloritized containing greenish-gray clots

supported in the fine-grained groundmass. The lower contact is marked with intense

42

Figure 9: Cross-section of DDK IC02-4.

DDH IC02-4Surface

f^V^*

b ^jP.^'td OO C

^00 CO C*3 (T'OÔô 0(TcQ (T*3 *- O^*O Q OO CQoOV o ô * tko'Vc

o oo c

Q ^^ ^

O GQ <O ^y5 ^

O Oo ^

x x x

x x x

x x x

0 00 Svvo oo ^Q Iî tfo^ôô o-^crW^j

r îrr:''^^ "o Oo ^

x xx

X X

î

-- 500 CA (core axis)


45Q CA Gneissic layering

----19" CA Fault gouge contact


-----28Q CA Brecciated contact


--- - 40" CA Sharp contact





Legend

Microgabbro M Overburden

(Diabase) Dike g Brecciated Gneiss

E.O.H.239.5m H Microgabbro

708000E

U

7081 OOE

L89+OON

708000E

IC02-4o-e

50-

100-

150-

200-

)

(

N

7081 OOE

l i l

Ann Ai

metres

y


Cross-Section of DDH ICO2-4Drawn by: R. Moss ' J. CamierCross-Section Scale: 1:1.000

Date: 21/02/2003Wire Diagram 1:2.500

quartz flooding over 10 em's, supporting angular fragments of mafic material and gneiss.

Silicified Gros Cap gneissic breccia occurs from 56.93 to 92.86 metres, 183.20 to 202.13

metres, and 210.20 to 212.88 metres. The silicified breccia and matrix minerals are as

described above. Similar quartz and calcite veins crosscut the Gros Cap breccia. Up to

y/o sulpliide mineralization within the Gros Cap breccia consists primarily of pyrite and

trace amounts of pyrrhotite and chalcopyrite. Pyrite occurs as euhedral grains forming

granular aggregates, occasional veins, veinlets, and individual crystals within the

amphibole matrix. Pyrrhotite occurs as subhedral to euhedral grains scattered randomly

hi the matrix and as very sporadic anhedral granular clusters. Sulphides occasionally rim

breccia fragments.

Fine to medium-grained diabase dikes crosscut the breccia between 92.86 and 183.20

metres, 202.13 and 210.20 metres, and 212.88 and the end of the hole at 239.50 metres.

The weakly to moderately magnetic, greenish-black diabase is generally massive,

exhibits a "salt and pepper" texture, is weakly chloritized, and contains trace amounts of

pyrite, pyrrhotite and chalcopyrite. Anastomosing quartz and calcite veins and veinlets

crosscut the diabase. Lithologic contacts with the gneissic breccia are marked by a

stockwork of intense quartz and calcite flooding. These veins generally contained

angular fragments of both gneiss and diabase.

44

7. Sampling and Quality Control

Two hundred and twenty-three samples (223) were collected and split from the drill core

by the writers, and include 10 quality control samples added during the packing of the

samples. Sample numbers and interval lengths are presented hi Tables 7, 8, and 9.

Quality control samples are listed hi Table 10. Assays are listed hi Appendix 2.

All samples were marked for splitting and sample numbers attached to the sample

interval. The core was then split hi two by a mechanical splitter, fitted together and

placed back hi the core box with the corresponding sample number for that interval.

Samples that shattered when split were fitted together as best as possible and returned to

the core box for the sampling procedure. The core splitter and the trays that captured the

split core were cleaned and swept after every interval. Samples were collected from the

core boxes after several boxes had been split, and bagged with the corresponding sample

number for that interval. Where possible, the core sampled for assay was removed from

one contiguous side only, with the remainder of the core left hi the core box for future

reference. All samples were put hi individual sample bags with the corresponding sample

number for each sample interval, and taped closed with clear packing tape. Samples were

packed into rice bags, approximately 25 samples per bag, and shipped via Greyhound bus

from Sault Ste Marie to Activation Laboratories, 1336 Sandhill Drive, Ancaster, Ontario,

Canada, L9G 4V5, for analysis. Each core box was fitted with a lid and secured with 6

centimetre wood screws. The core boxes for each drill hole were strapped together onto a

pallet with 3A inch metal strapping for storage.

Quality control standard assay samples were ordered from Natural Resources Canada

45

Table 7: Sample numbers and sample interval lengths for DDH IC02-1.

Hole IDIC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1

Sample No.

1408414085140861408714088140891409014091140921409314094140951409614097140981409914100141011410214103141041410514106141071410814109141101411114112141131411414115141161411714118141191412014121141221412314124141251412614127

Depth from to3.004.005.006.007.008.009.0010.0011.0012.0013.0014.0015.0018.0021.0031.0032.0039.0040.0041.0052.2253.2254.2255.2256.2257.2258.2259.2160.2261.2572.0073.0074.0075.0081.5082.5083.5086.2587.2588.2589.2590.2591.2593.00

4.005.006.007.008.009.0010.0011.0012.0013.0014.0015.0018.0021.0024.0032.0033.0040.0041.0042.0053.2254.2255.2256.2257.2258.2259.2160.2261.2562.5973.0074.0075.0076.0082.5083.5084.5087.2588.2589.2590.2591.2593.0094.00

Length metres

1.001.001.001.001.001.001.001.001.001.001.001.003.003.003.001.001.001.001.001.001.001.001.001.001.001.000.991.011.031.341.001.001.001.001.001.001.001.001.001.001.001.001.751.00

Hole IDIC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1IC02-1

Sample No.

1412814129141311413214133141341413514136141371413814139141401414114142141431414414145141461414714148141491415014151141521415314154141551415614157141581415914160141611416214163141641416514166141671416814169141701417114172

Depth from to

94.0095.00105.00106.00136.38137.38138.38139.38140.48159.00160.00161.00162.00163.00163.86165.46166.96168.00169.00170.00171.00172.00173.00183.00184.00185.00192.00193.00194.00195.00196.00197.00198.00199.00200.00201.00202.00203.00204.00205.00206.00207.00208.00209.00

95.0096.00106.00107.00137.38138.38139.38140.38141.38160.00161.00162.00163.00163.86164.85166.96168.00169.00170.00171.00172.00173.00174.00184.00185.00186.00193.00194.00195.00196.00197.00198.00199.00200.00201.00202.00203.00204.00205.00206.00207.00208.00209.00210.00

Length metres1.001.001.001.001.001.001.001.000.901.001.001.001.000.860.991.501.041.001.001.001.001.001.001.001.001.001.001.001.001.001.001.001.001.001.001.001.001.001.001.001.001.001.001.00

46

Table 8: Sample numbers and sample interval lengths for DDH IC02-2.

Hole ID

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

Sample

No.

14178

14179

14180

14181

14182

14183

14184

14185

14186

14187

14188

14189

14190

14191

14192

14193

14194

14195

14196

14197

14198

14199

14200

14201

14202

from

14.0

15.0

16.0

17.0

18.0

19.0

20.0

21.0

22.0

62.0

63.0

66.0

67.0

68.0

69.0

70.0

71.0

72.0

73.0

74.0

75.0

76.0

77.0

78.0

79.0

Depth

to

15.0

16.0

17.0

18.0

19.0

20.0

21.0

22.0

23.0

63.0

64.0

67.0

68.0

69.0

70.0

71.0

72.0

73.0

74.0

75.0

76.0

77.0

78.0

79.0

80.0

Length

metres

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

Hole ID

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

IC02-2

Sample

No.

14203

14204

14205

14206

14207

14208

14209

14210

14211

14216

14217

14218

14219

14220

14221

14222

14223

14224

14225

14226

14227

14228

14229

14230

Depth

from to

80.0

81.0

82.0

83.0

84.0

85.0

86.0

87.0

88.0

208.0

209.0

210.0

211.0

212.0

213.0

214.0

215.0

216.0

217.0

218.0

219.0

220.0

242.0

243.0

81.0

82.0

83.0

84.0

85.0

86.0

87.0

88.0

89.0

209.0

210.0

211.0

212.0

213.0

214.0

215.0

216.0

217.0

218.0

219.0

220.0

221.0

243.0

244.0

Length

metres

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

47

Table 9: Sample numbers and sample intervals for DDH IC02-3.

Hole ID

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

Sample

No.

14030

14031

14032

14033

14034

14035

14036

14037

14038

14039

14040

14041

14044

14045

14046

14047

14048

14049

14050

14051

14052

14053

14054

14055

14056

from

6.0

7.5

9.0

10.5

12.0

15.0

18.0

21.0

24.0

30.0

31.5

46.8

87.0

105.0

106.5

120.0

121.0

122.0

123.0

124.0

125.0

126.0

127.0

128.0

156.0

Depth

to

7.5

9.0

10.5

12.0

15.0

18.0

21.0

24.0

27.0

31.5

33.0

47.3

88.4

106.5

107.7

121.0

122.0

123.0

124.0

125.0

126.0

127.0

128.0

129.0

157.0

Length

metres

1.5

1.5

1.5

3.0

3.0

3.0

3.0

3.0

1.5

1.5

0.5

1.4

1.5

1.2

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

Hole ID

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

IC02-3

Sample No.

14057

14058

14059

14060

14061

14062

14063

14064

14065

14066

14067

14068

14069

14070

14071

14072

14073

14074

14075

14076

14077

14078

14079

14080

Depth

from to

157.0

158.0

159.0

160.0

161.0

162.0

163.0

164.0

165.0

166.0

170.0

171.0

172.0

173.0

174.0

180.0

181.0

186.0

187.0

188.0

197.5

198.3

199.0

200.0

158.0

159.0

160.0

161.0

162.0

163.0

164.0

165.0

166.0

167.0

171.0

172.0

173.0

174.0

175.0

181.0

182.0

187.0

188.0

189.0

198.3

199.0

200.0

201.0

Length

metres

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

1.0

0.8

0.8

1.0

1.0

48

Table 10: Sample numbers control samples with assay

Sample Hole ID No.

and sample intervals for DDH IC02-4. Quality values are listed in the lower table.

Depth Length from to metres

IC02-4IC02-4IC02-4IC02-4IC02-4IC02^IC02-4IC02-4IC02-4IC02-4IC02-4IC02-4IC02-4IC02-4IC02-4IC02-4IC02-4IC02^*IC02-4IC02-4IC02-4IC02-4IC02-4IC02^*IC02-4IC02-4IC02-4IC02^IC02-4

Quality ControlNumber14212142131421414215142311423214173141741417514176

1400114002140031400414005140061400714008140091401014011140121401314014140151401614017140181401914020140211402214023140241402514026140271402814029

SamplesTypeStd.Std.

DuplicateDuplicateDuplicateDuplicate

Std.Std.

DuplicateDuplicate

12.047.072.081.087.093.099.0114.0126.0138.0150.0162.0189.0192.0195.0198.0201.0204.0207.0210.0213.0216.0219.0222.0225.0228.0231.0234.0237.0

NameCCU-1CKC-1A

IC-DUP-3IC-DUP-4IC-DUP-5IC-DUP-6CCU-1CKC-1A

IC-DUP-1IC-DUP-2

15.050.075.084.090.096.0102.0117.0129.0141.0153.0165.0192.0195.0198.0201.0204.0207.0210.0213.0216.0219.0222.0225.0228.0231.0234.0237.0239.5

Cu999997034

282089

999996550

1016

3333333333333333333333333333

2.5

Assay ValueAu

5560*:10

^^^^

5320^2^^

Ag92.62531.30.4O0

80.32590.3O.3

49

Certified Reference Materials at CANMET Mining and Mineral Sciences Laboratories in

Ottawa, Ontario. Duplicate samples were collected from outcrop on the Island Copper

property.

The writers verify that all drill core samples for assay were marked during core logging,

split, collected, packed and shipped by themselves. The values reported here are from

Activation Laboratories, Ancaster, Ontario.

The drill core is stored on the Island Copper property in a locked quarry enclosure leased

from the YMCA by DCI Investments of Sault Ste Marie, and is located across the

highway from the historic adit.

50

8. Conclusions and Recommendations

Amerigo's 2002 drill program was able to duplicate and confirm historical drill data from

the hill top showing in DDH IC02-1, including several lenses of copper and gold

mineralization hosted within brecciated Fe-rich alkali granite. The depth of the Gros Cap

breccia in this drill hole was not determined as the drilling ended in brecciated gneiss.

However, it appears the brecciated gneiss extends to considerable depths. Copper

mineralization found within brecciated gneiss between 83.5 and 94.0 metres was not

hosted by the gneiss, but was hosted within quartz veins associated with hematite

mineralization. Diamond drill holes IC02-2 and IC02-3, both contained narrow sections

of copper mineralization hosted entirely within alkali granite. No significant copper

mineralization was encountered in DDH IC02-4.

Intersected within DDH IC02-2 were heterolithic breccias below the alkali granite

contact ait 95.87 metres depth. These heterolithic breccias are composed of both alkali

granite and granite gneiss breccias supported within a silicified chlorite-altered

amphibole schist matrix. These heterolithic breccias constituted the majority of the rocks

intersected in this drill hole. Also discovered in IC02-2, was a sulphide-bearing (l -S^/o

locally), Fe-oxide and K altered quartz-feldspar porphyry between 208.0 and 221.4

metres. This unit bears striking resemblance in texture, mineralogy and alteration to

Keweenawan-aged porphyry's exposed at surface near Mamainse Point. The intrusive

unit has sharp upper and lower contacts with chill margins extending into the porphyry.

In all IOCG deposits there is a strong association between mineralized breccias and

intrusive bodies such as quartz and/or feldspar porphyries and/or other felsic to

51

intermediate intrusives (Hitzman, 2000; Porter, 2000; Williams and Skirrow, 2000;

Gamier, 2002).

As previously indicated in historical records and confirmed in Amerigo's drilling, all

copper and gold mineralization seems to be hosted entirely within the alkali granite and is

confined to the upper segment of the brecciated gneiss. This however, does not suggest

that copper mineralization is absent at depth. The alkali granite appears to be segmented

within tlie drill intersections, occurring as lenses or bodies hosted within the Gros Cap

granite gneiss breccia. This may indicate a larger body at depth that has intruded the

Gros Cap breccia and was itself brecciated and faulted into its present location. Also, the

alkali granite observed in core at Island Copper may be finger-like protrusions from a

larger body at depth.

The following recommendations are strongly encouraged in order to better understand the

Island Copper property:

1. Further detailed mapping in zones of copper mineralization and areas known to

contain outcroppings of albite-rich granite based on 50 meter spaced grid lines.

Although the property was mapped by Falconbridge in relative detail, l :5000 and

1:2500, closer spaced gridlines and mapping on a 1:500 scale over these zones

may yield better information on the system hosting the copper and gold

mineralization.

2. Detailed structural mapping to better understand the following relationships:

a. Attitude and movement of faults, both large and small scale, especially the

52

Island Lake Fault,

b. Contact between the Gros Cap breccia and alkali granite.

c. Establish possible tune-lines between the gneiss breccia and fault, alkali

granite and fault, alkali granite and gneiss breccia

d. Although a structural geologist was sent by Falconbridge to visit the

property, there was insufficient time for a detailed assessment of fault

movement and an understanding of the controls governing the

emplacement of the alkali granite intrusion.

3. Further geochemical and petrographic studies of the albite-granite and gneiss to

establish their relationship to each other both geochemically and petrographically,

and to provide data essential in the correlation of lithologic units for development

of cross sectional maps. Are the Gros Cap breccias and heterolithic breccias

hydrothermal diatreme-like, or proto-diatreme features, or intrusion related

hydrothermal breccias?

4. Age dating of the albite-granite and the quartz-feldspar porphyry to indicate tune

of emplacement. Are the alkali granite and porphyry Keweenawan in age, and

therefore, related to the Mid-Continent Rift?

5. Further detailed assessment of historic data combined with data acquired in

recommendation 4, to develop lithologic correlations.

6. Detailed ground exploration and geological mapping over the area to the

53

northwest were gravity and magnetic data was compiled by Falconbridge,

suggesting a possible extension of the system.

7. Physical property measurements on representative rock types to design a

technique specifically targeting mineralized alkali granite.

54

9. References

Gamier, J., 2002. The Sue-Dianne Proterozoic Fe-Oxide Cu-Ag-Au Breccia Complex,

Southern Great Bear Magmatic Zone, Northwest Territories, Canada, University of

Western Ontario, Masters Thesis, London, Ontario.

Gamier, J., and McLellan, D., 2000. Island Copper Project 2000 Report, Island

Copper PN 297. Technical report for Falconbridge Limited, Timmins Exploration

Office, Kidd Creek Minesite, Timmins, Ontario.

Gamier and Oosterman, 2001. Island Copper Project - Nystedt Extension Report,

August, 2001, Addendum to Island Copper Project 2000 Report, Island

Copper PN 297. Technical report for Falconbridge Limited, Timmins Exploration

Office, Kidd Creek Minesite, Tirnmins, Ontario.

Innes, D.G. and Associates Ltd., 1983. Island Lake Property Geological Report.

Technical report for Highland Crow Resources Ltd.

Hitzman, M.W., 2000. Iron Oxide-Cu-Au Deposits: What, Where, When and Why; in

Porter, T.M. (Ed.), Hydrothermal Iron Oxide Copper-Gold 8c Related Deposits: A

Global Perspective, Australian Mineral Foundation, Adelaide, p. 9-25.

Mumin, A.H., and Gamier, J., 2002. Geology and Mineralization of the Island Copper

Property, Sault Ste. Marie, Ontario. Qualifying report for Golden Temple

Mining Corporation (now: Amerigo Resources Limited) Vancouver, BC.

55

Porter, T.M. 2000 - Hydrothermal Iron-Oxide Copper-Gold and Related Ore Deposits; in

Porter, Porter, T.M. (Ed.), Hydrothermal Iron Oxide Copper-Gold & Related

Deposits: A Global Perspective, Australian Mineral Foundation, Adelaide, pp 3-5.

Williams, P. J. 8c Skirrow, R.G., 2000 - Overview of Iron Oxide-Copper-Gold Deposits in

the Curnomona Province and Cloncurry District (Eastern Mount Isa Block),

Australia; in Porter, Porter, T.M. (Ed.), Hydrothermal Iron Oxide Copper-Gold *fc

Related Deposits: A Global Perspective, Australian Mineral Foundation, Adelaide,

pp 105-122

56

CERTIFICATE

I, John Gamier, M.Sc., of Box 51 Campbells Tr. Crt, RR5, Brandon, Manitoba R7A 5Y5, certify as follows concerning the report for Amerigo Resources Limited, "Island Copper Report On Fall Drilling Program November - December 2002", dated April 05,2003:

1. That I have received an M.Sc. in Economic Geology from the University of Western Ontario (2002), and a B.Sc. Specialist Degree in Geology (1996) from Brandon University, Brandon, Manitoba.

2. That I am registered as a Geoscientist in Training in good standing in the Province of Manitoba with the Association of Professional Engineers and Geoscientists of Manitoba.

3. That I have worked as an exploration geologist and consultant for the following companies; INCO Limited, Thompson Exploration Office, Thompson, Manitoba; Phelps Dodge Corporation, Winnipeg, Manitoba; Fortune Minerals Limited, London, Ontario; Falconbridge Limited, Timmins Exploration Office, Timmins, Ontario, Mumin Consulting Mineral Exploration and Development, Alexander, Manitoba; and Rare Earth Metals Corporation, Vancouver, BC.

4. That I have instructed at Brandon University, Brandon, Manitoba as a Sessional Lecturer, course number 42:272 Environmental Geology.

5. That I have carried out and assisted hi resource evaluations and successful exploration projects in Canada, and have supervised exploration camp staff of up to 15 persons including up to 3 geologists.

6. That I first visited the Island Copper property in 1999 while working for Falconbridge Ltd.

7. That I have carried out geological mapping and geochemical sampling on the Island Copper property for Falconbridge Ltd in 2000 and 2001.

8. That this report was prepared as a result of the work that was carried out over a period of four weeks during November and December 2002.

9. That I have no interest, direct or indirect in Amerigo Resources Limited or its affiliated companies and properties, nor do I expect to receive any interest, direct or indirect in Amerigo Resources Limited or the Island Copper property as a result of the work I have carried out.

10. That this report may be used hi good faith for whichever purposes and disclosures are required or deemed necessary by Amerigo Resources Limited.

Dated this 05th day of April, 2003

John Gamier, M.Sc.G.I.T. (APEGM)

57

CERTIFICATE

I Roger Moss, of 326 Rusholme Rd. Toronto, Ontario, M6H 2Z5 Canada, certify as

follows:

1. That I am registered as a Professional Geoscientist in the Province of Ontario

(Registration Number 0192), and am a Member in good standing of the Association of

Professional Geoscientists of Ontario

2. That I graduated with a Ph.D. in Geology from the University of Toronto in 2000.

3. That I graduated with an M. Se. in Geology from the University of Toronto in 1995.

4. That I graduated with a B.Se. in Geology from the University of the Witwatersrand in

1987.

5. That I am a member of the Canadian Institute of Mining, Metallurgy and Petroleum

and the Society of Economic Geologists.

6. That I am currently President and a Director of Amerigo Resources Ltd. and own

shares of the company.

7. That this report may be used in good faith for whichever purposes and disclosures are

required or deemed necessary by Amerigo Resources Ltd.

Dated this 8* day of April 2003

S.-""

Roger Moss, Ph.D., P.Geo.

58

APPENDICES

59

Appendix l - Drill Logs

Diamond Drill Hole IC02-1 Log

i-ITfl^

AMERIGO DIAMOND DRILL Property:RESOURCES LTD LOG ISLAND COPPER

Drilled By: St. Lambert Drilling

Start Date: December 5, 2002

Depth

From

0.00

3.00

10.70

To

3.00

12.13

10.88

UTM X: UTM Y: Elevation: 708500E 1 99+80E 5172385N/ L89+OON 418m

Township: AWERES

Azimuth: 2650

Completed: Date Logged: Logged By: December 8, 2002 December 12, 2002 J. Gamier, M. Se.

Description (colour, grain size, texture, mineralization, minerals, alteration); CA - core axis

OverburdenBRECCIATED AND MINERALIZED ALKALI GRANITEFracture brecciated albite-rich granite with alternating matrix- supported sections of up to 30cm in width.The matrix is composed of hematite (specularite) and sulphide mineralization alternating and locally intermixed with amphibole chlorite schist.The matrix of specular hematite forms anastomosing veins and veinlets throughout the fracture breccia and occasionally forms a supporting matrix in finely comminuted breccia. Moderately to intensely chloritized fine-grained amphibole comprises the matrix where hematite decreases or diminishes.The granite is composed primarily of subhedral to euhedral albite plagioclase phenocrysts set in an aphanitic quartzo-feldspathic groundmass that has weak to locally moderate hematite K alteration overprint, which imparts a pink to pale reddish-brown colouration to the rock.The sulphide mineralization consists of Cpy (trace to 100Xo locally) Py (trace to 207o) Bn (very trace). The sulphides decrease to between trace amounts to 1 0Xo below 4.5 metres. Were Py increases, the Cpy appears to decrease. The sulphides are predominantly contained within the matrix and occur as occasional veins, often rimming the fragments. Trace amounts occur within some of the alkali granite fragments as anhedral blebs and appears to be mostly Cpy.A calcite-rich fault gouge occurs between to metres plunging at:This gouge is composed of finely comminuted fragments of reddish- brown Fe-O altered alkali granite fragments supported in a calcite and amphibole chlorite matrix. The section is crosscut by occasional white quartz veins up to 2 mm wide.

Planar feature

Angle

350 CA

Sample No.

14084

14085

14086

14087

14088

14089

14090

Inclination: -500

TD: 252m

Depth

from

3.00

4.00

5.00

6.00

7.00

8.00

9.00

to

4.00

5.00

6.00

7.00

8.00

9.00

10.00

Claim: YMCA Patent

Hole No.

IC02-1

Dip Test

102m 201m

Length

metres

1

1

1

1

1

1

1

460

Pages

6

Map Ref:

Assay

Cu (ppm)

49694

39132

2959

8160

7114

4718

6365

Au (PPb)

599

469

443

23

1

1

56

Ag (ppm)

1.1

1.3

0.5

2.9

1.2

O.3

0.4

12.13

52.22

52.22

62.59

fhe lower contact is marked by chloritized amphibole schist containing white quartz veins.3ROS CAP GRANITE GNEISS FAULT BRECCIA

Upper contact at:Brecciated and fracture brecciated granite gneiss alternating with ones of comminuted fault gouge supported in amphibole chlorite

schist.Pervasive to turbid hematite K alteration extends to 28.74 metres.

Below this the alteration is weak to sporadic forming occasional discontinuous and wormy veins and intensely altered fragments mixed with weakly altered fragments of granite gneiss.Numerous quartz veins (3 to 5 per metre) crosscuts the section at various angles between 450 and 750 to the GA, with the most prominent at 500 CA.All the quartz veins contain reddish-brown hematite staining along the vein walls extending up to 2-3 mm into the veins.There are occasional clots of specularite and Cpy mineralization (trace o J\Jo locally), and occasional subhedral to euhedral Py aggregates.The gneiss fragments contain a moderate to intense gneissic layering.The matrix forms anastomosing veins and veinlets separating and occasionally supporting the fragments.There are narrow sections up to 30 cm wide of black to green amphibole chlorite schist.Occasional intensely altered reddish-brown to red fragments are supported within the schist.3y mineralization occasionally occurs within the amphibole schist as subhedral to euhedral grains and aggregates.BRECCIATED AND MINERALIZED ALKALI GRANITE

Sharp, brecciated and faulted Upper contactThe contact is well-defined marked by slickenfibres and chloritized amphibole schist supporting Fe-O and K-altered gneissic and alkali granite fragments.The contact zone is gradational into matrix and clast supported alkali granite fragments supported in a matrix of intergrown amphibole chlorite and hematite (specularite).The contact fragments are composed primarily of subhedral to euhedral pink albite plagioclase phenocrysts with well-defined cleavage planes.The phenocrysts are set in a pink to red tinted, hematite and K-altered quartzo-feldspathic groundmass.

500 CA

50" CA

800 CA

14091

14092

14093

14094

14095

14096

14097

14098

14099

14100

14101

14102

14103

14104

14105

14106

14107

10.00

11.00

12.00

13.00

14.00

15.00

18.00

21.00

31.00

32.00

39.00

40.00

41.00

52.22

53.22

54.22

55.22

11.00

12.00

13.00

14.00

15.00

18.00

21.00

24.00

32.00

33.00

40.00

41.00

42.00

53.22

54.22

55.22

56.22

1

1

1

1

1

3

3

3

1

1

1

1

1

1

1

1

1

3737

948

271

317

31

210

194

276

5

6

8

7

131

20

53

37

37

10

^

^

53

^

^

^

^

^

^

^

6

^

^

^

^

^

0.9

0.5

0.5

1.4

0.4

O.3

0.4

O.3

0. 3

O.3

^.3

O.3

O.3

O.3

0. 3

O.3

^.3

62.59

94.32

94.32

101.60

he fragments vary in size from 2-3 cm, are angular to subrounded.Mineralization consists of Cpy and Py from trace to 1 0Xo locally.

py is occurs as blebs within the amphibole matrix and as anhedral ggregates.

Occasional anhedral Cpy blebs were observed within the groundmass f the fragments interstitial to the plagioclase phenocrysts.y occasionally occurs as aggregate veins crosscutting the matrix and s individual euhedral crystals supported in the matrix.

The lower contact is sharp and faulted at:GROS CAP GRANITE GNEISS FAULT BRECCIA

Upper contact is sharp at:The breccia is similar to the section previously described above

etween 12.13 and 52.22 metres.The section consists of alternating breccia fragments in matrix to clast-

upport and amphibole chlorite schist (fault gouge).The amphibole schist contains occasional intensely altered rounded ed breccia fragments of granite gneiss and comminuted fragments of

gneiss.Quartz veins crosscut the section hosting hematite (specularite), Cpy and Py.The Cpy occurs as large anhedral blebs within the white quartz.Cpy also occurs as occasional blebs and crosscutting veins along ractures that emanate off the quartz veins.

Py occurs as large subhedral to euhedral blebs within the quartz veins and amphibole schist.Occasional zones of reddish-brown, variably intense and pervasive hematite alteration occurs within the fragments and throughout the section.

Fe-O AND BIOTITE-RICH ULTRAMAFIC DYKE (LAMPROPHYRE)

Sharp contact at:

Black to dark gray fine-grained ultramafic intrusion marked by quartz

520 CA

520 CA

580 CA

14108

14109

14110

14111

14112

14113

14114

14115

14116

14117

14118

14119

14120

14121

14122

14123

1412414125

14126

14127

14128

14129

56.22

57.22

58.22

59.21

60.22

61.25

72.00

73.00

74.00

75.00

81.50

82.50

83.50

86.25

87.25

88.25

89.2590.25

91.25

93.00

94.00

95.00

57.22

58.22

59.21

60.22

61.25

62.59

73.00

74.00

75.00

76.00

82.50

83.50

84.50

87.25

88.25

89.25

90.25

91.25

93.0094.00

95.00

96.00

1

1

0.99

1.01

1.03

1.34

1

1

1

1

1

1

1

1

1

1

1

1

1.75

1

1

1

2122

664

2917

2678

2040

1511

14

9

13

53

109

12

413

2678

607

569157

23491801

554

297

67

^

^

^

^

^

^

^

^

^

^

^

^

^

^

^

2

^^

^

^

^

^

O.3

O.3

0.3

0.5

O.3

0.4

0. 3

O.3

O.3

O.3

1.1

":0.3

0. 3

0.4

0.4

0.3

0.510.5

0.7

0.3

2.3

0.5

101.60

116.07124.84

150.19

152.60

150.19

116.12

124.90

153.62

153.62

nd calcite veins up to 2 cm wide within a tan coloured and calcite-rich ontact zone that extends 1 metre into the section at either contact.he unit contains fine-grained biotite and magnetite.here is moderate to locally strong magnetism in the central portion of

he section.Hematite and calcite veins crosscut the unit with the majority trending

t:'he lower contact is sharp, irregular shaped with rounded xenoliths of

Fe-O altered granite gneiss supported within the intrusion, and plunges at:QROS CAP GRANITE GNEISS FAULT BRECCIASharp contact at:The unit is similar to the section described in detail above between

2. 13 to 52.22 metres.However, there are veins of specularite between 105.00 and 107.25 metres that form anatomising veins and veinlets similar to those found within the alkali breccia. Some contain trace Cpy mineralization.Quartz veins and veinlets contain trace Cpy and Py.Annealed and silicified fault gouge at:Annealed and silicified fault gouge at:Missing the 126m marker from the core. The hole is 3m short. The 129m marker should have been 126m.Py mineralization occurs below 136.0 metres from trace to 1 0Xo. It occurs adjacent to the quartz veins and interstitial to the breccia within the matrix.

DIABASE DYKE

Sharp upper contact at:Fine-grained, greenish black, moderately to weakly chloritized diabase dyke that is non-magnetic.There are occasional xenoliths caught within the dyke near both contacts that exhibit intense and pervasive Fe-O alteration.Fault gouge, extremely friable core, section is extremely blocky composed of diabase fragments, sands, clays and mud.

50" CA

580 CA

580 CA

64" GA

600 CA

220 CA

14131

14132

14133

14134

1413514136

14137

14138

14139

14140

14141

14142

14143

05.00

106.00

136.38

137.38

138.38

139.38

140.48

159.00

160.00

161.00

162.00

163.00

163.86

106.00

107.00

137.38

138.38

139.38

140.38

141.38

160.00

161.00

162.00

163.00

163.86

164.85

1

1

1

1

1

1

0.90

1

111

0.86

0.99

289

13

7

87

3

3

2

3

4

4

11

23

^

^

3

^

^

^

^

^

^

^

^

^

^

O.3

O.3

O.3

O.3

0.3

O.3

O.3

O.3

0.3

O.3

O.3

O.3

O.3

153.62

249.75

252.00

250.10

ower contact is approximately:3ROS CAP GRANITE GNEISS FRACTURE BRECCIA

'he unit is previously described in detail above in the upper units.he section is primarily fracture brecciated with narrow sections of

matrix supported breccia (~10 cm widths).here is less amphibole chlorite schist matrix as was observed phole.

3y mineralization occurs between 159.0 metres and 175.5 metres at race to 1 0Xo locally, and between 182.0 to 195.0 metres at up to 207o ocally.The amphibole chlorite matrix occurs as anastomosing veins and einlets crosscutting and filling the fractures within the breccia. It also ingers into the breccia as discontinuous and continuous hairline racture filling and veinlets.Matrix supported fragments are generally smaller than in the upper units, with more founding and attrition occurring to the breccias.Annealed and silicified matrix and clast supported breccias in a silicified and quartz flooded amphibole matrix form occasional sections of up to 3 metres that appear to be cataclastic breccias."he cataclastic breccias are generally 1 .5 mm in size and are

occasionally up to 5 centimetres in diameter. They exhibit moderate to intense sericite-alteration, are well rounded to subrounded, and occasionally exhibit intense Fe-O and or K alteration.Calcite and white quartz veins crosscut the unit from parallel to the core axis up to 450 to the CA.Some of the cataclastic breccia consists of brecciated quartz veins intermixed with the gneissic fragments.The section becomes more silicified with depth towards the bottom of the hole.Quartz veins increase towards the bottom of the hole.Fault gouge composed of mud, sand and clays.Unit grades into fracture breccia towards the bottom of the hole.

520 CA

14144

14145

14146

14147

14148

14149

14150

14151

14152

14153

14154

14155

14156

14157

14158

14159

14160

14161

14162

1416314164

65.46

66.96

68.00

69.00

70.00

171.00

172.00

173.00

183.00

184.00

185.00

192.00

193.00

194.00

195.00

196.00197.00

198.00

199.00

200.00201.00

66.96

68.00

169.00

170.00

171.00

172.00

173.00

174.00

184.00

185.00

186.00

193.00

194.00

195.00

196.00

197.00

198.00

199.00

200.00

201.00202.00

1.5

1.04

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

1

11

8

6

4

4

5

3

39

4

4

11

3

3

3

6

1

2

2

24

85

^

^

^

^

^

^

3

4

^

^

^

16

^

6

^

5

^

^^

^^

O.3

O.3

O.3

^.3

0.3

^.3

O.3

O.3

O.3

O.3

O.3

O.3

O.3

^.3

^.3

0. 3

O.3

0.3^.3

^.3 cO.S

252.00 End of Hole.

1416514166

14167

14168

14169

14170

14171

14172

14173

14174

14175

14176

202.00203.00

204.00

205.00

206.00

207.00208.00

209.00

Std.

Std.

Std.

Std.

203.00204.00

205.00206.00

207.00

208.00

209.00

210.00CCU-

1CKC-1A

IC- DUP-1

IC- DUP-2

11

1

1

1

1

1

1

4

4

3

3

2

2*:1

2

^

^

^

^

^

^

^

^

0.5

^.3

^.3

O.3

^.3

^.3

^.3^.3

44Jst.

AMERIGO RESOURCES LTD

Drilled By: Lambert DrillingStart Date:

December 9, 2002

Depth

From

0. 03.00

65.30

To

3.065.30

95.87

UTM X: 708547E/100+30E

Completed: December 14, 2002

DIAMOND DRILL LOG

Property: ISLAND COPPER

UTM Y: 51 72231 N/L88+OON

Date Logged: December 15, 2002

Description (colour, grain size, texture, mineralization, minerals, alteration); GA = core axis

Overburden - casing pulled after drilling.GROS CAP GRANITE GNEISS FRACTURE BRECCIAFracture brecciated Gros Cap granite gneiss breccia composed of moderate Fe-O K altered silicified granite gneiss with narrow sections of clast to locally matrix supported breccia.The matrix is composed of amphibole chlorite schist with localized zones of silicification.The Fe-O K alteration is turbid to pervasive, often rimming and invading fragments.Py ± Po mineralization occurs as subhedral to euhedral grains and occasional aggregates within and associated with the matrix.The matrix generally forms anastomosing veins and veinlets within the fracture breccia and is supporting the fragments in narrow intensely brecciated sections that rarely exceed 1-3 cm in width.

Fe-O RICH ALKALI GRANITE BRECCIAContact is unknown in intensely blocky and friable core containing fault gouge composed of mud and sand.

Planar feature

Angle

Elevation: 405m

Township: Claim: AWERES YMCA Patent

Azimuth: Inclination: 0850 -500

Logged By: TD: 257.0 J. Gamier, M. Se. metres

Sample No.

14178

14179

14180

14181

14182

141831418414185141861418714188

14189

Depth

from

14.0

15.0

16.0

17.0

18.0

19.020.021.022.062.063.0

66.0

to

15.0

16.0

17.0

18.0

19.0

20.021.022.023.063.064.0

67.0

Length

metres

1

1

1

1

1

111111

1

Cu (ppm)

6

4

25

17

7

9333514

9

Hole No. Pages

IC02-2 5

Dip Test

100m 530 200m 44D

Assay

Au (ppb)

,

^

^

O

*

^^2^^^

5

Ag (ppm)

*,

O.3

0. 3

O.3

O.3

O.30.30. 30. 30. 30. 3

0. 3

Ibite-rich granite fracture breccia fragments and matrix upported breccia.

The alkali granite is composed of subhedral to euhedral pink o white-pink plagioclase set in an aphanitic pink quartzo- eldspathic groundmass.There is occasional K-feldspar crystals and rounded quartz yes. The unit may be granite gneiss; however, there is no abric in the breccia fragments,The matrix is composed of primarily platy specular hematite with localized zones of amphibole chlorite forming anastomosing veins and veinlets.The hematite occurs as veins and veinlets supporting the jreccia and occasionally replaces the amphibole matrix. Some sections are in complete matrix support with the hematite supporting finely comminute and brecciated ragments.

Some evidence was observed that may indicate the alkali granite consists of slivers of brecciated rock juxtaposed against matrix supported granite gneiss. However, there are zones of intergrown amphibole and hematite matrix indicating the amphibole may grade into hematite matrix.Sulphide mineralization consists of trace to locally 207o Py and Cpy with trace amounts of Pp.The Py consists of subhedral to euhedral grains and aggregates in the amphibole matrix and occasionally within the hematite matrix.Cpy consist of anhedral grains and aggregates forming veins and blebs within the matrix and occasional as small fragments within the groundmass of the alkali breccia.Po appears associated with the Py as subhedral to euhedra grains in the matrix.The lower contact is sharp along annealed and silicified amphibole obtortte fault gouge at: 44" GA

14191

14192

14193

14194

14195

14196

14197

14198

14199

14200

14201142021420314204142051420614207

68.0

69.0

70.0

71.0

72.0

73.0

74.0

75.0

76.0

77.0

78.079.080.081.082.083.084.0

69.0

70.0

71.0

72.0

73.0

74.0

75.0

76.0

77.0

78,0

79.080.081.082.083.084.085.0

1

1

1

1

1

1

1

1

1

1

1111111

17

51

12

25

8

8

21

6

145

86

33715

347112427210323

^

10

^

20

^

^

^

^

^

^

^^^^787

0.3

O.3

O.3

0.4

O.3

O.3

0.3

O.3

O.3

0.3

O.32.40.52.30.40.3O.3

S.87

117.48

118.24

172.40

17.48

118.24

172.73

174.40

HETEROLITHIC FAULT BRECCIAMatrix supported annealed and silicified fault breccia om posed of finelyomminuted Gros Gap granite gneiss breccia fragments and

alkali jjranite fragments (albite-rich, no fabric)The comminuted breccia fragments are rounded to subrounded and occasional sub-angular, generally between 1rnmto 1cm in size.The fragments are supported in amphibole chlorite matrix comprising 50 to 75 0Xo of the rock.The fragments exhibit variable intensities of Fe-O and K alteration."he breccia commonly grades into zones of amphibole

chlorite schist containing occasional intensely hematite-altered and finely comminuted fragments supported within the schist as individual grains.slo sulphides were observed within the section.ULTRAMAFIC INTRUSIVE DYKESharp upper contact at:Strongly to moderately magnetic, black to dark gray, fine grained biotite-magnetite lamprophyre or ultramafic rock.There are 1 cm chill margins along each contactLower contact is sharp at:HETEROLITHIC FAULT BRECCIAThe unit is similar to the unit described in detail above between 95.87 and 117.48 metres.Foliation within the unit is consistent at tjelweeji 400 to 550 to, the CA.DIABASE INTRUSIVE DYKEUpper contact is sharp and contains re-brecciated fragments from the upper unit supported within the diabase groundmassFine-grained, greenish-black to dark gray, moderate to weakly magnetic diabase dyke with the characteristic "Salt and Pepper" texture.The unit is crosscut by numerous calcite quartz veins that

450 CA

380 CA

500 CA

14208142091421014211

85.086.087.088.0

86.087.088.089-0

1111

10747

^^^^

0.4*:0.3

^.30. 3

174.40

197.30

199.82

208.04

197.30

99.82

208.04

221.40

lupge between perpendicular to 750 CA.he low^r contact is sharp marked by calcite veining and a 1 m wide chill margin. The contact is perpendicular to the CA.

HETEROLITHIC FAULT BRECCIA\s described in detail between 95.87 to 117.48 metres

DIABASE INTRUSIVE DYKEUpper contact is sharp at:The unit is as described in detail between 172.40 to 174.40 metres.The lower contact is sharp at:

HETEROLITHIC FAULT BRECCIAAs described in detail between 95.87 to 117.48 metres.

QUARTZ FELDSPAR PORPHYRYThe upper contact is sharp with a 2 mm chill margin and amphibole alteration that grades into the reddish-brown groundmass over 40 cm. The contact trends at:Reddish-brown Fe-O and K altered quartz-eye porphyry, fine to medium grained with 20 to 3007o rounded quartz eyes that are between T to 3 mm in diameter, set within a fine to medium sugary quartzo-feldspathic groundmass.Phenocrysts of pink coloured subhedral to euhedral plagioclase feldspars at between 15 to 20"Xo.The feldspars alternate with amphibole clots altering to chlorite and containing associated sulphide mineralization.The sulphides are composed of Py and Cpy at 1-50Xo locally. The Cpy occurs as anhedral clots associated with Py, which forms subhedral to euhedral grains within the groundmass and associated with the amphibole clots.The section between 213:0 to 216.0 metres has undergone bleaching and amphibole chlorite alteration turning the rock to a pale greenish to green-black.Amphibole filled fractures run parallel to the CA and contain subhedral to euhedral Py grains.Sharp lower contact at:

900 CA

300 CA

200 CA

480 CA

540 CA

14216

14217

14218

14219

14220

14221

14222

142231422414225

208.04

209.0

210.0

211.0

212.0

213.0

214.0

215.0216.0217.0

209.0

210.0

211.0

212.0

213.0

214.0

215.0

216.0217.0218.0

0.96

1

1

1

1

1

1

111

43

36

13

39

88

84

30

6376110

^

^

^

^

^

^

5

5^^

0.6

0.7

0.8

1.2

1.3

2.2

0.8

1.21.52.0

221,40 257.00

257.00

HETEROLITHIC FAULT BRECCIAThe/ unit is similar to that describee) in detail between 95.87 to 117.48 metres.However; the amphibole matrix contains more intense and pervasive chlorite alteration.

End of Hole.

142261422714228

14229

14230

218.0219.0220.0

242.0

243.0

219.0220.0221.0

243.0

244.0

11

1

1

1

301837

540

10

^^^

19

^

0.90.70.4

5.3

O.3

Diamond Prill Hole ICQ2-3 Log

AP AMERIGO


Start Date: December 3, 2002

Depth

From

0.02.10

5.87

To

2.105.87

46.08

RESOURCES LTD

UTM X: 708445E 7 99+35E

Completed: December 5, 2002

DIAMOND DRILL LOGUTM Y:

5172525N/L91+OONDate Logged:

December 8, 2002


Elevation: 402m

Township: AWERES

Azimuth: 0

Logged By: J. Gamier, M. Se.

Description (colour, grain size, texture, mineralization, minerals, alteration); GA = core axis

Overburden - CasingDIABASE INTRUSIVE DYKEFine-grained, black to dark gray weakly chloritized diabase dyke

, strongly to moderately magnetic and

No visible sulphides were observed in the unit.Lower contact is sharp at:Fe-0 RICH ALKALIC GRANITE AND GRANITE GNEISS BRECCIAThe unit is composed of a Fe-0 rich alkali granite breccia intermixed with granite gneiss (gneissic layering visible) matrix to clast supported in a matrix of amphibole chlorite schist and finely to moderately comminuted fragments of host rock.Quartz veins and veinlets crosscut the unit forming localized anastomosing stockworks. Veins are composed of white quartz with occasional earthy hematite coating fracture walls and occasional specularite books.Calcite veins and veinlets crosscut both the breccia and quartz stockwork indicating late to syn injection. Veins are variable crosscutting at between 200 to 400 to GA.The breccia fragments are composed of alkali granite and granite gneiss fragments. The alkali granite is composed of pink to white plagioclase set in a pink, aphanitic quartzo-feldspathic groundmass with weak Fe-O K alteration.The gneiss fragments are composed of plagioclase, K-feldspar and quartz that exhibit moderate to locally intense Fe-O K alteration that colours the fragments a reddish-brown. Alteration is pervasive to turbid within the breccia.The gneissic breccia displays a very prominent gneissic layering as opposed to the alkali granite fragments which do not display a fabric.Purple-brown anastomosing hematite veins and veinlets crosscut the unit

Planar feature

Angle

470 CA

Sample No.

14030

14031

14032

14033

14034

14035

14036

Claim: YMCA Patent

Inclination: -900

TD: 243.00 m

Depth

from

6.0

7.5

9.0

10.5

12.0

15.0

18.0

to

7.5

9.0

10.5

12.0

15.0

18.0

21.0

Hole No. IC02-3

Dip Test

101m 201m

Length

metres

1.5

1.5

1.5

1.5

3

3

3

880 830

Pages

Map Ref:

Assay

Cu (ppm)

78

5305

21

14

14

3

1

Au (PPb)

*

*

^

,

22

^

2

Ag (ppm)

0.3

0.3

0.3

O.3

0.5

0.3

O.3

46.08

58.98

58.98

73.64

ndicating late injection. The hematite also coats the walls of the calcite eins indicating syn-emplacement.

Sulphide mineralization includes trace to 50Xo Py, trace to 40X0 locally Cpy, nd trace Po.

The Py occurs as subhedral to euhedral grains within the matrix and as ccasionai aggregates or clusters.

The Cpy occurs as anhedral blebs and discontinuous veins within the matrix often associated with the Py and as occasional blebs within some of the alkali fragments. Some blebs were observed within the gneiss; however, hese were generally located along hairline fractures extending to the matrix.Po is generally closely associated with the Py as subhedral to euhedral non-magnetic or very weakly magneticjjrains.Observed supported within the calcite veins are intensely to pervasively Fe- O altered angular breccia. Alteration completely overprints the protolith.DIABASE INTRUSIVE DYKE - NON-MAGNETICUpper contact is gradational marked by annealed breccia fragments of host ock supported with the diabase groundmass. Contact is:

Greenish-black, moderately to weakly chloritized, fine-grained non-magnetic diabase intrusive dyke.A vein of Cpy and Py hosted within calcite occurs at 47.06 m, plunging:The lower contact is gradational marked by annealed breccia fragments of host rock supported within the diabase groundmass. Contact is:GROS CAP GRANITE GNEISS FAULT BRECCIAUpper contact is brecciated with fragments supported in diabase. Contact is gradational over 30 cm at:The breccia is composed of moderately to weakly Fe-O K altered Gros Cap granite gneiss with a well-defined gneissic layering.The fragments are matrix to clast supported within a black top greenish- black matrix composed of amphibole chlorite schist. Chlorite alteration is variable within the schist.Quartz veins trending between 300 and 500 to the core axis crosscut both the matrix and the fragments. Late calcite veins further crosscut the unit subparallel to the CA up to 700 to the CA.The veins occasionally contain angular fragments of the host rock.The matrix is composed primarily of amphibole schist overprinted by chlorite alteration. Minor magnetite grains were observed within the matrix that exhibit a weak magnetism.Calcite blebs and alteration was also observed in the matrix indicated with a weak to violent fizz reaction with 100Xo solution of HCI. This calcite alteration

35" CA

320 CA31 0 CA

31 0 CA

14037

14038

14039

14040

14041

21.0

24.0

30.0

31.5

46.81

24.0

27.0

31.5

33.0

47.31

3

3

1.5

1.5

0.50

2

3

3

3

153

i

^

'~2

^

^

^

0.3

*-n t-w.\^

O.3

O.3

O.3

73.64

78.00

78.00

88.38

ecreases with depth and distance from the contact at ~63 metres.he gneissic breccia is composed of Gros Cap gneiss that is weakly to

moderately Fe-O K-altered."he Fe-O alteration is pervasive to turbid. It was often observed rimming he fragments and progressively invading the interior of the fragments with wispy tendrils following crystal planes and the gneissic fabric.The fragments display a well-defined or visible weak to moderate gneissic ayering. However; some of the fragments may have an overprint fabric due o a build up of strain prior to the faulting event.Composition of the fragments under hand lens examination appears to be plagioclase, K-feldspar, quartz and minor hornblende.The fragments are variable in size from less than 1 mm to greater than 20 centimetres. Comminuted fragments occur surrounding the larger breccia pieces and occur supported within the matrix.Very trace amounts of sulphide mineralization was observed as subhedral o euhedral Py Po grains occurring within the matrix only. Smaller anhedral blebs of what appeared to be Cpy also occurs both scattered within the matrix and associated with the other sulphides.DIABASE INTRUSIVE DYKE - MAGNETICSharp faulted contact marked by calcite veining at:Moderately to weakly magnetic, black to dark gray fine-grained chloritized diabase dyke with subhedral to euhedral magnetite grains supported in the groundmass.The unit has numerous crosscutting calcite veins and veinlets that plunge subparallel up to 650 to the CA.Trace sulphides of Py Po were observed in the groundmass.Lower contact is faulted with intensely blocky core some of which exhibit slicken fibres. No angle was obtained.GROS CAP GRANITE GNEISS FAULT BRECCIA AND ANNEALED AMPHIBOLE SCHIST (FAULT GOUGE)No angle obtained on the upper contact.The unit is composed of granite gneiss breccia supported in amphibole chlorite schist matrix alternating with sections of chloritized amphibole schis containing intensely altered comminuted angular fragments of unknown protolith.The gneiss fragments exhibit localized intense hematite alteration K, colouring the rock a reddish-brown and overprinting the protolith. There are often wormy discontinuous veins.Numerous calcite veins and blebs crosscut and occur within the amphibole chlorite matrix.

600 CA

88.38

107.74

07.74

227.90

1

sericite alteration was observed in localized sections of up to 10 cm in width, bleaching the rock to a pale white to buff colouration.Trace sulphides (Py Po) were observed occurring sporadically throughout he matrix.ower contact is sharp at:

DIABASE INTRUSIVE DYKEChloritized, greenish-black to gray, fine grained diabase dyke with moderate o weakly magnetic sections.Quartz veins crosscut the unit at various angles between 230 and 650 to the GA. The veins contain trace to Q.5%, euhedral to subhedral Py..ower contact is sharp and irregular at:GROS CAP GRANITE GNEISS FAULT BRECCIAContact is irregular and perpendicular to the core axis.Core is very blocky and fracture brecciated.The breccia is as previously described above; consisting of comminuted ragments and fracture to angular breccias alternating with amphibole

chlorite schist."he fragments are composed of granite gneiss with a well-defined fabric gneissic layering) set in matrix to clast supported amphibole chlorite

schist.No visible sulphides observed in the upper portion of the unit.Foliation at 122.08 m within the fracture brecciated sections is:Foliation at 131.66 m within the fracture brecciated sections is:Sulphide mineralization occurs below 123.0 metres at trace to 30Xo locally composed of Py Po forming veins and aggregates within the amphibole matrix.There are zones of weak to moderate conductivity indicating at least some of the veins are interconnected within the core.No magnetism was noted in the Po grains.Quartz veins (white to smoky gray) occur within the amphibole schist (fault gouge) and occasionally crosscut the breccia and on rare occasions rim some fraqments.Occasional calcite veins were observed generally paralleling the quartz veins.Trace Cpy mineralization occurs along some fractures and was observe in the matrix often rimming and occurring interstitial to the fragments.Below 171.00 metres the core exhibits a weak to moderate magnetism. Magnetite grains (euhedral) were observed primarily in the amphibole matrix. Some Mt grains were observed within some fragments that

350 CA

900 CA

460 CA460 CA

14044

14045

14046

1404714048

14049

14050

140511405214053

14054

14055

14056

14057

14058

14059

14060

87.00

05.00

106.5

120.0121.0

122.0

123.0

124.0125.0126.0

127.0

128.0

156.0

157.0

158.0

159.0

160.0

88.38

06.50

07.74

121.0122.0

123.0

124.0

125.0126.0127.0

128.0

129.0

157.0

158.0

159.0

160.0

161.0

1.38

1.50

1.24

11

1

1

111

1

1

1

1

1

1

1

8

75

116

64

4

4

442

1

2

3

22

8

13

7

3

^

^

^^

7

5

^^^

^

4

^

^

^

^

^

0.3

O.3

0.3

O.3O.3

O.3

O.3

0.6O.3O.3

O.3

O.3

O.3

cO.3

O.3

O.3

O.3

201.94

227.90

202.00

231.9

esemble alkali granite fragments, as were anhedral blebs of Cpy.hese possible alkali granite fragments do not display any gneissic layering nd are chiefly composed albite grains with well-defined crystal cleavage lanes set in an aphanitic pink groundmass. Some specular hematite was bserved associated with these fragments and may indicate a mixed reccia zone.e-O alteration is moderate to intense within localized sections of the unit.

The alteration colours the breccia to a reddish-brown with turbid and ervasive alteration..ocalized sericite alteration occurs within the breccia bleaching the rock to a uff and yellow-pink colour.

Quartz veins decrease substantially with depth occurring as wispy veins.The breccia below 180.00 metres is composed of annealed and fracture brecciated gneiss containing alternating sections with sharp contacts of annealed, Fe-O altered and silicified fault gouge.The fault gouge sections are composed of a mixture of moderate to finely comminuted host rock and amphibole chlorite matrix.The fracture breccia is composed do granite gneiss with well-defined gneissic layering set in anastomosing veins and veinlets of amphibole chlorite matrix.Sericite occurs sporadically as bleached sections, which is very evident in the narrow (up to 10 cm wide) sections of matrix supported breccias.In these narrow sections the matrix minerals generally exceed 450Xo.r inely comminuted and annealed fault gouge compose of reddish-brown ragments of Fe-O altered host rock mixed with amphibole matrix minerals plunges at:

ANNEALED AMPHIBOLE SHCIST (FAULT GOUGE)Sharp upper contact at:The unit is composed of chloritized, non-magnetic, green to greenish-black

53" CA

500 CA

i

14061

14062

14063

14064

14065

14066

14067

14068

14069

14070

14071140721407314074140751407614077140781407914080

161.0

162.0

163.0

164.0

165.0

166.0

170.0

171.0

172.0

173.0

174.0180.0

186.0187.0188.0197.50198.25199.0200.0

162.0

163.0

164.0

165.0

166.0

167.0

171.0

172.0

173.0

174.0

175.0181.0

187.0188.0189.0198.25199.00200.0201.0

1

1

1

1

1

1

1

1

1

1

11

111

0.750.75

11

4

3

3

2

2

2

4

7

26

31

332433

35017278

^

3

3

^

^

4

4

^

^

^

^^^^34^^^6

0.4

O.3

O.3

0. 3

O.3

O.3

O.3

O.3

O.3

O.3

0.3O.3O.3O.3O.30.3O.30.40.3O.3

231.98

241.19

241.19

243.00

243.00

ine-grained amphibole schist.The section is crosscut by numerous intrusive white quartz veins up to 3 cm n width that support angular fragments of schist.The quartz veins trend at:Emanating from and associated with the veins are subhedral to euhedral Py aggregates and individual crystals at up to d.5% locally.The schist supports numerous angular intensely Fe-O altered reddish- brown fragments of unknown protolith.The fragments are concentrated at both contacts.Lower contact is sharp at:GROS CAP GRANITE GNEISS FAULT BRECCIAThe unit is composed of fracture brecciated granite gneiss with narrow sections (3 to 5 cm widths) of matrix supported breccia.The matrix is composed of chloritized amphibole schist.The section is crosscut by Py-bearing white quartz veins plunging at:Localized intense Fe-O alteration forms irregular discontinuous wormy veins and patches within the breccia.WHITE QUARTZ VEINSThe contact is sharp at:The section consists of intense quartz flooding and amphibole chlorite schist forming veins containing angular breccia fragments suspended in the quartz matrix.The amphibole appears to be a blue-green in colour and may be actinolite.The reddish-brown and pink breccia is intensely Fe-O and K-altered.There are numerous greenish-black angular fragments alternating with the reddish-brown and pink fragments that appear to be brecciated schist. Some have wispy tendrils emanating from them.No sulphides were observed.

End Of Hole

250 CA

400 CA

150 CA

150 CA

XidK\

c/Tv^SmgW^'

AMERIGO RESOURCES LTD


Start Date: November 28, 2002

Depth

From (m)0.04.0

41.7241.80

To (m)4.0

41.72

41.8045.00

UTM X: 707979E 1 L94+54E

Completed: December 1 , 2002

DIAMOND DRILL LOGUTM Y:

5172295N/L88+96NDate Logged:

Nov. 30 to Dec. 4


Elevation: 395m

Township: AWERES

Azimuth: 0

Logged By: J. Gamier, M. Se.

Description (colour, grain size, texture, mineralization, minerals, alteration)

OverburdenGROS CAP GRANITE GNEISS FAULT BRECCIABrecciated Gros Cap granite gneiss with weak to moderate layering) at 450 to the core axis (CA).

fabric (gneissic

The fragments exhibit varying degrees of weak to intense turbid to pervasive hematite alteration.The breccia is predominantly clast supported to locally matrix supported.The matrix (mtx) is composed primarily of silicified to chlorite-altered amphibole schist that is very fine-grained, black to greenish-black in colour.The amphibole schist also forms anastomosing veins and veinlets that appear to be late annealed fracture breccia matrix.There are numerous anhedral to subhedral calcite clots and blebs that occur within the matrix and as an alteration feature in the fragments.Quartz (Qtz) veins and anhedral rounded to oblong eyes at 20-3007o occur interstitial to the feldspars (plagioclase and K-feldspar) in the quartzo- feldspathic groundmass in the fragments. The veins crosscut the core at various angles from 300 to 900 to the CA.The feldspars are primarily subhedral to euhedral K-feldspars with varying intensities of pervasive and turbid hematite (hem) alteration. The altered pink K-feldspars are reddish-brown.Plagioclase is affected similarly but is generally yellow-white in colour.8 cm fault gouge composed of clay, mud and sand.ULTRAMAFIC INTRUSIONUpper contact is marked by calcite clots and blebs.Brecciated, chloritized ultramafic rock supported in a quartz and calcite vein stockwork.Numerous earthy hematite filled fractures (1-3mm) crosscut the core at

Planar feature

Angle

500 CA

190 CA

19 0 CA

Sample No.

14001

14002

Claim: YMCA Patent

Inclination: 900

TD: 239.5m

Depth

from

12.0

47.0

to

15.0

50.0

Hole No.

IC02-4

Dip Test

102m 201m

Length

metres

3

3

-870 -860

Pages

4

iviap r\er:

Assay

Cu ppm

3

21

Au

(PPb)

^

^

Ag (ppm)

0.5

0.3

45.00

56.93

92.86

56.93

92.86

183.20

arious angles from subparallel to 400 to the CA.he fragments are composed of black to greenish-black, angular to ubangular, that are generally matrix supported."he fragments are non-magnetic, 3-4 hardness on the MOHS scale and ccasionally exhibit a platy to schistose texture.

There is a well-defined crenulation cleavage within the section that suggests movement post brecciation.The breccia grades into competent rock with no discernable contact in very blocky core.DIABASE INTRUSIVE DYKENo discernable upper contact in very blocky fracture brecciated core."he rock is greenish-black to black with greenish-gray clots (chlorite), fine to

very-fine grained."race pyrite (Py) and pyrrhotite (Po) occur within the calcite Qtz filled ractures, which plunge 300 to 75" to the CA.The rock is relatively massive and nondescript resembling the amphibole schist.The lower contact is Qtz-veined and brecciated containing angular to ounded fragments of gneissic breccia.

GROS CAP GRANITE GNEISS FAULT BRECCIACataclastic breccia of Gros Cap granite gneiss.White to Pink feldspars alternating with turbid hematite (pervasive) altered feldspars supported in an amphibole chlorite matrix that forms anatomising veins and veinlets.Trace Py mineralization associated with crosscutting quartz veins that trend at180 to900 totheCA.Quartz veins form an anastomosing stockwork crosscutting the breccia and matrix. Late calcite veins crosscut the core along old fracture planes that predate the quartz veins. Lower contact is sharp.DIABASE INTRUSIVE DYKEFine grained greenish-blapk diabase with trace Py ^nd Po mineralization. The upper 7 metres is crosscut by numerous calcite veins and veintets that crosscut the core at various angles to the core axis from 25" to 750 .There are occasional localized zones of breccia hosted by calcite quartz veins up to 3 cm in width containing angular to rounded fragments of diabase. Occasional veins contain hematite and K-feldspar alteration.Below 100 metres the diabase is massive and exhibits the characteristic "Salt and Pepper" texture. The unit is weakly to moderately pervasively chloritized. Localized Ep stringers crosscut the core at angles between 300

280 CA

400 CA

250 to 75" to

CA

14003

14004

14005

14006

14007

14008

72.0

81.0

87.0

93.0

99.0

114.0

75.0

84.0

90.0

96.0

102.0

117.0

3

3

3

3

3

3

4

5

2

97

155

134

^

^

^

^

^

^

O.3

*0.3

^.3

O.3

cO.3

O.3

183.20

202.13

210.20

212.88

202.13

21Q.20

212.88

239.50

o 500 to the GA.Dccasional sulphide mineralization (Py Po) is associated with the Ep.

ematite veins associated with the calcite and quartz veins occur at erpendicular angles to the CA. The hematite occurs as earthy red rouge.

Calcite quartz veins contain occasional magnetite grains that exhibit a weak magnetism and trace Cpy.

he diabase is weakly to moderately magnetic with localized zones that are on-magnetic.

The lower contact is brecciated over several centimetres.GROS CAP GRANITE GNEISS FAULT BRECCIAntensely fracture brecciated contact resulting in extremely blocky core at'he breccia is hosted within a silicified amphibole chlorite matrix that ontains trace amounts of Py and Po and very trace amounts of Cpy. The

Cpy mineralization occurs as blebs associated with the Py.'he granite breccia is composed of angular to well-rounded fragments that

exhibit varying degrees of Fe-0 alteration K-feldspar, that are matrix to clast supported.Quartz and calcite veins crosscut the core at various degrees to the CA rom perpendicular to 100 to the CA. Occasional angular fragments of

gneiss are supported within the quartz matrix.Sulphide mineralization occurs within the groundmass comprised of Py, Po and Cpy. The sulphides vary from trace to locally 30Xo, with Cpy generally as trace. The sulphides form subhedral to euhedral aggregates and individual grains that often rim some fragments.Sections of the breccia contain turbid to pervasive hematite alteration K- feldspar and form discontinuous wormy veins and veinlets that are reddish- jrown. The hematite also occurs as specular hematite within quartz veins and as earthy red (rouge) that coats some quartz vein walls.DIABASE INTRUSIVE DYKEThe unit is similar to that described between 92.86 to 183.20 metres. The contact is Irregular and brecciated and intensely blocky therefore np angle was obtained between the diabase and upper unit.

GROS CAP GRANITE GNEISS FAULT BRECCIAThe unit is similar to that described between 183.20 to 202.13 metres.However, there are fewer sulphides within this section with sections were no sulphide mineralization was observed.DIABASE INTRUSIVE DYKE

330 CA

100 to 906 to

CA

14009

14010

14011

14012

14013

14014

14015

14016

14017

1401814019

14020

26.0

38.0

50.0

62.0

189.0

192.0

195.0

198.0

201.0

204.0207.0

210.0

129.0

141.0

153.0

165.0

192.0

195.0

198.0

201.0

204.0

207.0210.0

213.0

3

3

3

3

3

3

3

3

3

33

3

155

139

141

139

28

25

15

29

31

9687

35

^

^

*2

^

^

^

^

^

^

30^

^

0.3

O.3

O.3

O.3

O.3

O.3

O.3

O.3

0.3

0.8O.3

O.3

239.50

The unit is a chloritized diabase dyke as previously described above between 92. 86 and 183.20 m.However, there are narrow sections of fault breccia with Fe-O, quartz and K flooding and veining altering and locally brecciating the diabase.The diabase is moderately magnetic from 237.50 m to the end of the hole.Only trace amounts df sulphide (Py Po) mineralization was observed as blebs within the groundmass and within localized zones of brecciation, within zones of alteration and the groundmass.Veinlets of sulphide mineralization (Py ± Po ± Cpy) were observed crosscutting the diabase and within the groundmass. Py is the dominant sulphide mineral, with Po next and very trace amounts of Cpy. The subhedral Po and anhedral Cpy are associated with the Py occurring as nterstitial blebs within the subhedral to euhedral Py aggregates.The unit is carbonate-rich with anastomosing veins crosscutting the core, as well as veins and blebs occurring in zones of local brecciation.

** The 195.00 m, marker is in the wrong location; therefore the hole is one raetre longer than indicated by St Lambert Forage. The end of box 34 is- 194.55m.

End of Hole.

14021

14022

14023

14024

14025

14026

14027

14028

14029

213.0

216.0

219.0

222.0

225.0

228.0

231.0

2S4.&

237.0

216.0

219.0

222.0

225.0

228.0

231.0

234.0

237.0

239.5

3

3

3

3

3

3

3

3

2.5

50

49

49

50

82

69

24

sa

10

^

^

^

5

3

^

^

^

2

0.3

O.3

1.5

0.6

1.0

0.4

^

O

0

Appendix 2 — Assays

Sample ID14084140851408614087140881408914090140911409214093140941409514096140971409814099141001410114102141031410414105141061410714108141091411014111

14111 PULPDUP14112

Au ppb59946944323-2-25610-2-253-2-2-2-2-2-2-26-2-2-2-2-2-2-2-2-2-2-2

Agppm-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5

As ppm3.4-0.5

8.65.81.81.51.211.729.134.81662.3-0.5-0.52

-0.541.31.5-0.51.92.21.92.32.11.8-0.5-0.5-0.52

Bappm100-50-50-50-50-50-5080-50-50-501504404502907104002505109401308174-50200250-50-50-50-50

Br ppm-0.5

2.6-0.5-0.53.14.54.43.72.8-0.5-0.51.9-0.5-0.52.52.3-0.52

-0.51.532.81.22.3-0.52.83.34.43.42.8

Ca "/o oxide

-1-1-1-1-1-1-13-1-1-1-1-1-1-1-1-12-1-1-1-12-1-1-12-1-1-1

Coppm13813144462818142011910167189109141122233224137717

Cr ppm30583921212910133141143-51171225461761619311785242182751781016

Cs ppm-1-1-11-12222-13231222-112-12211-1-1-1-1-1

Fe "/o oxide7.968.34132.584.683.431.094.0714.34.2510.73.314.652.844.872.736.512.793.532.893.912.875.616.347.733.877.482.342.283.48

Hf ppm333323343453355333334433333433

Hg ppm-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1

Assay results for DDH IC02-1. Analyses values presented are from Activation Laboratories, 1336 Sandhill Drive, Ancaster, Ontario, Canada, L9G 4V5

Sample ID141131411414115141161411714118141191412014121141221412314124141251412614127141281412914131141321413314134141351413614137141381413914140141411414214143

Au ppb-2-2-2-2-2-2-2-2-2-22-2-2-2-2-2-2-2-23-2-2-2-2-2-2-2-2-2-2

Ag ppm-5-5-5-5-5-5-5-5-5-5-5-511-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5

As ppm2.4-0.51.7-0.52.11.71.61.72.3-0.52.71.61.67.2-0.57.77.92.11.944.181.64.71.82.6-0.51.9-0.51.6

Ba ppm-50150260507088-50110160220710-50-50-50-50110100-50-503503003203101601701201201306070

Br ppm3.9-0.53.82.7-0.5-0.5-0.52.7-0.53.3-0.5-0.5-0.5-0.53.7-0.52.8-0.5-0.5-0.5-0.55.5-0.52.1-0.5-0.5-0.5-0.5-0.5-0.5

Ga "/o oxide

-1-1-1-1-1-12-1-13-1-1-1-1-1-1-1-1-1-113-1-1-1-1-1-1-1-1

Coppm40710293410203030283432271518221591412111717229138133017

Gr ppm32107111159193375-52619213970164326167-51413108403288151322

Cs ppm-1-1-1-1-1-1-1-1-1-1-112-1-1-11,-|

124322-12-1-1-1-1

Fe 0Xo oxide4.631.743.052.844.464.126.4310.62.424.418

8.264.181.372.332.53.833.192.35.065.976.425.46.33.844.224.155.356.135.8

Hf ppm423333437547534453499988687887

Hg ppm-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1


Sample ID14144141451414614147141481414914150141511415214153141541415514156141571415814159141601416114162

14162 PULP DUP14163141641416514166141671416814169141701417114172

Au ppb-2-2-2-2-2-234-2-2-216-26-25-2-2-2-2-2-2-2-2-2-2-2-2-2-2

Ag ppm-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5

As ppm1.81.81.41.63.81.91.81.51.232.2131.61.71.42.94.52.82.62.91.81.92.81.41.71.4-0.5-0.51.1-0.5

Ba ppm180601101006514021028021020010078250665065757560616060100901006580657580

Br ppm-0.51.7-0.5-0.52.82.3-0.5-0.53.41.91.6-0.5-0.5-0.52.4-0.5-0.5-0.52.82.9-0.5-0.5-0.5-0.5-0.51.81.9-0.52.32.2

Ga 0Xo oxide

-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-12-1

Co ppm8471071212139141821181610181617181819181621171815171013

Cr ppm7-511191417141978756142712162912-52827382119276-56191441

Csppm-1-11-1-1-12-1-1-1-1-1-1-1-1-1-12-1-12211-1-1-1-12-1

Fe "/o oxide3.734.824.223.32.35.045.224.73.215.925.855.035.467.553.917.17.126.236.136.395.066.226.096.585.846.225.345.893.974.3

Hf ppm71087761085699973131310109611111178101054

Hg ppm-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1


Sample ID14084140851408614087140881408914090140911409214093140941409514096140971409814099141001410114102141031410414105141061410714108141091411014111

141 11 PULP DUP14112

Ir ppb-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5

Mo ppm-1-16-1-12-1-1-1-1-1-1-1-1-1-174-1-185-1-13-1-1-15-1

Na 07o oxide6.125.424.525.356.787.838.175.854.726.324.674.193.163.212.812.391.234.062.723.613.093.642.242.613.824.185.576.826.617.01

Ni ppm-20-20-20-20-20-20-2081-20-2035-20-25-2442-20152-21-20-20-20-20356110352-23-20-20-24

Rb ppm-15-15

42-15-1595-15-15-15-15-1543-1534-158970-156339-15-15-15-15-15-15-15-15-1541

Sb ppm-0.1

0.20.60.70.30.30.41.80.91

2.20.30.50.20.20.20.40.20.3-0.1-0.10.2-0.1-0.1-0.1-0.10.30.40.20.4

Se ppm1.42.56.92.42.11.60.865.92.25.82.833.35.72.81154.554.62.97.48.110.36.64.51

1.11.9

Seppm-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

Sn "/o oxide-0.02-0.01-0.02-0.01-0.01-0.02-0.02-0.02-0.01-0.01-0.02-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01

Sr 07o oxide-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05

Ta ppm-0.5-0.5-0.5-0.5-0.5-0.5-0.51.9-0.52.32.3-0.5-0.5-0.5-0.5-0.5-0.51.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.51.6-0.5-0.5

Th ppm5.13.54.245.75.74.89.24.23.79.45.38.610.49.25.48.66.94.69.27.94.35.84.976.23.77.37.64.6


Sample ID141131411414115141161411714118141191412014121141221412314124141251412614127141281412914131141321413314134141351413614137141381413914140141411414214143

Ir ppb-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5

Mo ppm-1-1-1-1-1-1-1-1-14-1-1-1-1-11106-1-155-148-19-17-1-1

Na "/o oxide6.354.444.044.794.874.153.252.626.876.374.114.376.087.066.595.786.655.477.183.11.811.061.43.213.913.854.033.223.493.41

Ni ppm-25-20-21-214091166119-20307812241-20-20-20-20-20-20-20-20-20-2045-20-20-20-20-20-20

Rb ppm-1544-15-15-15-15-15-15-15-15-15-15-15-15-15-15-15-15-15-151197591-15-15-15-15-15-15-15

Sb ppm-0.1-0.1-0.1-0.1-0.1-0.1-0.1-0.1-0.1-0.10.30.2-0.1-0.10.20.50.4-0.1-0.10.40.40.40.3-0.1-0.1-0.1-0.1-0.1-0.1-0.1

Se ppm3.51.72.52.74.25.410.226.12.85.413.6114.91.52.62.53.42.32.312.21513.610.913.88.210.49.211.819.321.4

Se ppm-3-3-3-3-3-3-3-34-3-3-3-3-3-3-3-3-3-3-3-3-3-3-3-3-3-3-3-3-3

Sn "/o oxide-0.01-0.01-0.01-0.01-0.01-0.01-0.02-0.02-0.01-0.01-0.02-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.02-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01

Sr 0Xo oxide-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.050.1-0.05-0.05-0.05-0.05-0.05

Tappm-0.5-0.5-0.5-0.5-0.50.6-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.52.1-0.5-0.53

-0.5-0.5-0.5-0.5-0.5-0.5

Th ppm9.84.34.76.44.46.110.27.513.710.58.86.56.45.26.75.28.62.74.254.73.35.69.12.53.85.23.65.84


Sample ID14144141451414614147141481414914150141511415214153141541415514156141571415814159141601416114162

14162 PULP DUP14163141641416514166141671416814169141701417114172

Ir ppb-5^5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5

Mo ppm-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-12-165-1-1-1-1-1-1-18-1-1

Na "/o oxide3.96A not.UU

3.93.653.173

3.053.553.681.932.873.814.183.014.334.654.644.764.744.795.554.94.12.362.94.384.693.964.934.07

Ni ppm-20-20-20-20-20-20-20-20-20-2031-20-20-20-20-20-20-20-20-207840-2035-20-20-20-28-2030

Rb ppm-15-15-15-15-15-15-15-15-15-15-15-15-15-15-15-15-15101-15-15-15-1556-15-154042-15-15-15

Sb ppm-0.1rt A

-VJ. l

-0.1-0.1-0.1-0.1-0.1-0.1-0.1-0.10.30.3-0.1-0.1-0.1-0.1-0.1-0.1-0.1-0.1-0.1-0.1-0.1-0.1-0.1-0.10.3-0.1-0.1-0.1

Se ppm8.113.911.66.63.99.815.611.34.57.913.311.114.612.35.817.215.611.613.413.99.814.613.813.810.910.410.613.37.28.5

Seppm-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

Sn "/o oxide-0.01-0.02-0.02-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.02-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01

Sr "/o oxide-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05

Ta ppm-0.5-0.5-0.5-0.52.6-0.52.22.4-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5

Th ppm7

5.14.74.52.34.73.45.82.43.69.45.710.46.91.613.48.44.96.776.66.36.33.22.84.15.35.75.65.8


Sample ID1408414085

1408614087140881408914090140911409214093140941409514096140971409814099141001410114102141031410414105141061410714108141091411014111

14111 PULPDUP14112

U ppm-0.5-0.5

2.82.4-0.5-0.5-0.5

2.8-0.5

8.19

-0.5-0.5-0.5

1.81.51.21.3

1-0.5-0.5-0.5-0.5-0.5

2.2-0.5

21.30.91.5

W ppm

-1

510-1

2-1-1

611-1

633-1-1-1-1

2-1-1-1-1-1-1-1-1-1

468

Zn ppm-50-50

-50

226101-50-50

281300261354167164-50

128100242145159127-50-50

8311911812171-50-50-50

La ppm12.927.659.316.521.737.725.726.629.921.931.813.852.751

61.317.779.925.844.818.916.69.18.61.92.45.72.32.82.92.2

Ce Ppm31

58123364478645960476831899812037156457734351817-3

6144775

Nd ppm15225110203332252522239

453840105414271216610-5-5

7-5-5-5-5

Sm ppm1.63.36.22

2.54.33.63.72.42.93.51.74.45.36.22.29.62.34

2.21.8

11.30.60.81.10.91.11.10.9

Eu ppm0.60.81.50.70.61.31.21.60.91.51.40.81.11.21.50.52.40.7

10.70.60.40.3-0.2-0.20.50.40.70.70.4

Tb ppm-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.50.6-0.5

Yb ppm-0.2-0.2

0.50.30.30.30.20.40.30.40.40.30.50.50.70.40.50.60.60.60.40.30.40.60.50.50.61.51.4

1

Lu ppm-0.05-0.050.08-0.05-0.05-0.05-0.050.070.050.060.06-0.05-0.05-0.05

0.10.070.10.090.090.090.060.050.070.080.070.080.10.230.210.15

Mass grams

25.7827.5425.0623.7923.8322.6123.9423.1523.8223.2228.0222.7420.1320.422.4921.6218.7324.1124.8225.5322.5223.0225.2722.44

2624.7126.731.9332.3124.25


Sample ID141131411414115141161411714118141191412014121141221412314124141251412614127141281412914131141321413314134141351413614137141381413914140141411414214143

U ppm1.8-0.5

11.4-0.51.62.92.33.54.83.2-0.51.91.91.88.72.5-0.51.82.92.32.41.43.42

1.6-0.5-0.5-0.5-0.5

W ppm

4-T

-1

-1

-1

-1

-1

-1

-1

-1

-1

-1

-1

-1

-1

-1

-1

7-1-187-1

6-1-1-1-1-1-1

Zn ppm9163-50-50-508767202-5012334016117293-5097

224-50-50264230299256205-50-50-5015561-50

La ppm3.1

20.927.427.36.511.795

19.37.42.34.32.82.61.41.46.11.92.41.4

41.260.746.956.474.753.119.841.825.862.630.9

Ceppm

844585313272073917511854-318767971271021101519344876112070

Nd ppm

-5121818610751513-56-5-5-5-5-5-5-5-53360404670411034276028

Sm ppm1.423

2.80.91.5

12.92.61.7

11.21.3

10.50.31.5

11.50.99119.58.212.45.73.55.85.310.5

6

Eu ppm0.70.70.70.70.40.52.90.80.70.50.60.50.4-0.20.30.70.60.60.32.23.12.92.73.11.90.91.51.81.81.6

Tb ppm0.6-0.5-0.5-0.5-0.5-0.50.7-0.5-0.51.4-0.50.7-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.51.3-0.5-0.5-0.5-0.5-0.5-0.5

10.6-0.5

Yb ppm1.4-0.2

0.30.4

10.5

10.91.10.8

11.50.50.4-0.21.63.80.80.62.83.43.82.12.71.21.10.81.62.11.5

Lu ppm0.2

-0.05-0.050.050.150.070.150.140.170.120.150.230.070.07-0.050.240.560.1

0.080.420.520.550.330.410.180.160.120.240.320.24

Mass grams

22.6923.5723.7425.2824.9524.7326.2126.1524.2324.6624.3526.1124.8822.9624.1223.4724.523.8

23.5924.4519.8823.7222.5921.421.2322.3623.923.0324.9523.33

Assay results for DDH lC02-1. Analyses values presented are from Activation Laboratories, 1336 Sandhill Drive, Ancaster, Ontario, Canada, L9G 4V5

Sample ID14144141451414614147141481414914150141511415214153141541415514156141571415814159141601416114162

14162 PULP DUP

14163141641416514166141671416814169141701417114172

U ppm-0.5-0.5-0.5-0.51.8-0.5-0.51.51.3-0.53.4-0.5

2.8-0.52.2-0.5-0.52.82.32.5-0.52.1-0.5-0.51.3-0.50.91.3-0.5

1.4

W ppm

-1-1-1-1-1-1-1-1-16-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1

Zn ppm-50-50-50-50-50-50-50-501513001711001202101108086589168158243252348210627577-50-50-50

La ppm45.752

45.629.416.86.521.725.615.617.911.443.151.523.49.364.715.116.124.624.19.614.313.855.9307.24.512.48.6

33.2

Ceppm881058963331848583340278598541713935375654233232111671812322068

Nd ppm3540402717-5232610169

3943228

519-52220-514124528108117

30

Sm ppm6.37.85.94.52.91.55.24

2.43

2.76.47.83.81.49.23.82.93.94

2.43.12.86.24.62.22

2.52.24.5

Eu ppm1.71.81.61.41.10.71.51.10.7

10.81.521

0.52.71.3

11.31.30.91.20.91.81.30.90.70.80.71.2

Tb ppm-0.5-0.5-0.5-0.5-0.5-0.50.8-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.51.10.9-0.5-0.5

0.9-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5

Ybppm1.41.50.9

10.7

12.80.8

11.61.51.31.71.50.95.23.32.12.52.62.22.32.11.51.71.92.51.31.31.1

Lu ppm0.230.230.150.130.10.160.40.130.150.240.230.220.280.230.140.790.5

0.310.380.390.320.350.30.230.260.280.370.180.2

0.16

Mass grams25.622.921.4420.5221.1522.1122.5725.3423.5623.4224.5921.322.824.1831.5821.7223.1619.9726.6125.6323.3622.5722.5621.5623.9823.8721.72

2523.6124.55


Sample ID14084140851408614087

14087 IR140881408914090140911409214093140941409514098140991410014101141021410314104141051410614107141081410914110

141 10 IR14111

14111 PULPDUP1411214113

Ag ppm1.11.30.52.92.41.2-0.30.40.90.50.51.40.4-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.30.3-0.30.50.3-0.30.4

IR = pulp rerun

Cd ppm0.60.70.30.30.60.5-0.3-0.30.50.70.4-0.3-0.3-0.3-0.3-0.3-0.30.3-0.3-0.3-0.3-0.3-0.3-0.30.3-0.3-0.3-0.3-0.30.4-0.3

Cu ppm49694r*r\A **f\ O9 IO^

2959816083827114471863653737948271317312765687

13120533737

2122664291730002678257620401511

Mn ppm747221710951118252188237193421113332183610695454501439511732262562256419511508318536542396380509381

Mo ppm-13386-1532-14-1362724485-1-1-1365367-1

Ni ppm99132217548791424301944121522421232516355410353162434524

Pb ppm199430297868616443013737172484215813514148641010-3119

Zn ppm6032581911937639372872552333171721078324969152766237698911466565728272836

Al 0Xo oxide1.791.902.433.343.674.342.653.592.743.032.832.323.153.533.015.343.166.372.893.403.274.413.933.463.382.492.732.902.232.653.36

Be ppm-1-1-1-11-1-1-12-11211322311121-1-1-1-1-1-1-1-1


Sample ID14114141151411614117141181411914120141211412214123

14123 IR141241412514126141271412814129141311413214133141341413514136

141 36 IR1413714138141391414014141141421414314144

Ag ppm-0.3-0.3-0.3-0.31.1-0.3-0.30.40.40.3-0.30.510.50.7-0.32.30.5-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3

IR = pulp rerun

Cd ppm-0.3-0.3-0.3-0.3-0.3-0.30.4-0.3-0.3-0.30.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.31.0-0.30.4-0.3-0.3-0.30.6-0.30.4-0.3-0.3

Cu ppm149135310912413267860756956715723491801554297671372287333234411238

Mn ppm1281992043283113615372523641606159272846322631972710743282152116279168381682172624905046254121393508567369

Mo ppm233-111484263323977-1855-15382916556

Ni ppm12192030861501078307573933781315201082313198124619971215132

Pb ppm-3-3-3611209-38161119910622648-3725934415759-3952017144

Zn ppm213336554845953256208205122823045941144326257228277220224197588857168596139

Al 0Xo oxide3.183.243.452.834.174.576.432.622.914.994.225.013.612.813.582.853.292.633.206.7411.225.8310.2411.8113.104.214.204.106.556.066.034.07

Be ppm

11-1-1111-11111-1-1-1221-13443332212111


Sample ID14145141461414714148141491415014151141521415314154141551415614157

14157 IR1415814159141601416114162

14162 PULP DUP1416314164141651416614167141681416914170

141 70 IR1417114172

Agppm-0.3-0.3-0.30.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.30.3-0.3-0.3-0.3-0.30.5-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3

IR = pulp rerun

Cd ppm0.3-0.30.7-0.3-0.3-0.3-0.3-0.3-0.3-0.30.5-0.3-0.3-0.3-0.3-0.3-0.31.40.5-0.31.00.62.10.50.6-0.3-0.3-0.3-0.3-0.3-0.3

Cu ppm6445339441133365122244854433222-12

Mn ppm2892693192454254563296632398147469793216371642748721739126393688973291111531360712820726606617413519

Mo ppm5623-1-11531-1-15635-1-13-15-143742125-1-1

Ni ppm349111581392231121715181821161723227839233210181526271728

Pb ppm4-3-3912-3896094-37250432710151971099612696172241517646158715

Zn ppm312937274749371063071667712020620810983605491691672762133432109311510287894266

Al "/o oxide3.933.774.544.224.905.424.744.124.128.624.224.647.859.034.537.0912.224.065.985.754.426.3612.646.168.554.565.317.4310.484.354.07

Be ppm

1222111122222222332222322222212


Sample ID14084140851408614087

14087 /R140881408914090140911409214093140941409514098140991410014101141021410314104141051410614107141081410914110

14110/R14111

14111 PULPDUP1411214113

Bi ppm

51610655-22-2-2

7773-2

4-2-2-2

4-2

4288-2-2-2

2-2-2

IR = pulp rerun

Ga "/o oxide

0.110.200.250.890.920.140.300.332.160.831.400.640.320.550.240.920.450.510.410.300.220.270.150.210.180.530.620.790.761.581.25

K 0Xo oxide

0.100.110.130.180.220.190.110.200.300.100.080.541.031.062.801.510.742.171.830.430.530.420.360.130.260.160.160.070.070.130.33

Mg "/o oxide

0.070.030.250.760.820.290.120.161.511.021.431.261.422.601.644.321.642.351.993.002.113.924.404.582.711.331.400.270.250.391.18

P 0Xo oxide0.0250.0420.0700.0430.0450.0260.0270.0330.0700.0280.0390.0950.0360.1450.0230.0690.0250.0260.0560.0350.0480.0460.0270.0590.0420.0210.0220.0250.0260.0240.070

Sr ppm34384587859578120985477511019084501031061509611463639095747861529092

Ti "/o oxide

0.200.220.360.320.290.120.200.180.550.180.280.250.340.410.130.250.230.170.260.200.200.110.130.170.170.140.150.190.190.200.26

V ppm4263167242463375

8513028114396365100528556513870778349818324233048

Yppm

-1-1-1-11

-1-114-131-1227152213313225544

S"/o

6.0424.4690.4880.9010.9390.7160.4340.6220.5110.5710.2582.6320.0180.0530.0670.0220.0100.0050.0460.0170.0170.0060.0160.3660.0960.3090.2920.2700.2750.2890.366


Sample ID14114141151411614117141181411914120141211412214123

14123 /R141241412514126141271412814129141311413214133141341413514136

141 36 IR1413714138141391414014141141421414314144

Bi ppm-2-234-25739654-2-2-237-23-2-2-2-2-2-2-2-2-2-2-2-2-2

/R = pulp rerun

Ga 07o oxide0.360.210.170.150.290.750.430.860.650.620.540.880.540.470.200.780.530.540.410.911.273.390.610.661.430.480.450.541.300.930.920.64

K "/o oxide0.850.530.190.190.470.130.080.160.270.440.440.180.260.240.230.450.480.180.140.762.311.262.392.771.360.600.430.420.380.240.230.24

Mg 07o oxide

1.072.071.682.293.434.936.591.002.064.384.304.442.220.340.990.771.340.750.504.234.575.434.114.535.722.302.011.573.983.954.071.88

P "/o oxide0.0200.0220.0170.0220.0530.1730.0820.0320.0660.0900.0890.1840.1140.0350.0350.0250.0370.0160.0220.1100.1160.1020.1050.1050.1810.0430.0940.0950.1040.2190.1570.097

Sr ppm16013111210212413566871009085707060785672656810570485564126195177204117115120127

Ti"/o

0.140.120.140.090.210.230.160.200.280.270.210.300.230.200.160.190.220.120.150.550.590.490.320.310.280.300.270.280.370.450.510.18

V ppm25333246587616924478584764216282934464665797268717751312349916827

Yppm-11223974254521178311942352730375451712139

So/o

0.0300.0170.0810.1000.0100.0040.0520.4240.1280.0980,0990.0190.0990.3400.0970.1310.1900.0690.0480.3010.3470.4590.1390.1430.3330.0540.5920.1000.1850.9280.2250.184


Sample ID14145141461414714148141491415014151141521415314154141551415614157

141 57 IR1415814159141601416114162

14162 PULP ODP1416314164141651416614167141681416914170

141 70 /R1417114172

Bi ppm-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2-23-2-2-2-2-2-2-2-2-2-2-2

IR = pulp rerun

Ca "/o oxide0.620.540.440.320.330.530.550.210.960.990.580.540.370.400.170.550.570.460.520.500.440.450.611.030.470.650.780.570.630.420.44

K "/o oxide0.210.520.460.350.130.290.220.320.510.720.310.450.280.330.170.200.520.380.120.120.160.191.180.410.920.320.360.290.600.210.28

Mg "/o oxide1.701.501.951.413.263.472.801.742.943.842.132.784.124.112.424.134.662.903.773.562.503.294.363.954.243.933.844.404.742.492.84

P "/o oxide0.1360.1020.1000.0400.0900.1360.1510.0410.0620.1110.0960.0960.0780.0810.0330.1180,1190.0960.1320.1260.0760.1120.1310.1130.0810.0730.0920.1120.1150.0600.086

Srppm12919817697861021251031119611512270727911313193103101100107108688095114101109118119

Ti "/o oxide0.360,320.110.190.150.240.300.180.270.260.290.370.170.200.130.390.330.340.430.380.230.300.380.370.300.380.330.320.100.160.21

V ppm34232720474543254464586869673877706874715571717860766374735159

Yppm53546144412165912143293451212613231415111791455

S"/o

0.0650.0680.1720.2520.1520.1100.1740.0760.2310.1690.3250.1150.1050.1020.0790.2170.2010.4040.2210.2080.1260.0660.1170.1050.0670.0420.0630.0940.1100.0560.112


Sample ID141781417914180141811418214183141841418514186

14186 PREP DUP14187141881418914190141911419214193141941419514196

14196 PULP DUP1419714198141991420014201

Au ppb-2-2-2-3-2-2-22-23-2-253-210-220-2-2-2-2-2-2-2-2

Ag ppm-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5

As ppm

1-0.51.3-0.51.4-0.51.23.4-0.5-0.51.92.11.819.41.35.46.867.24.711.31.21.32.58.6-0.5

Bappm31065897010010065-50-50-503506560-50150-50-50-50280-50-50-50-50-50-50-50

Br ppm1.8-0.5-0.5-0.52.4-0.5-0.5-0.5-0.5-0.51.41.52.11.51.92.1-0.51.91.5-0.5-0.5-0.5-0.5-0.5-0.63.1

Ca"/o oxides

1-1-1-1-1-1-1-1-1-1-12-1-1-1-1-121-1-1-1-1-1-1-1

Co ppm1027321174246274555562215919111827341199815128015

Cr ppm1123129-524-54111129613711111212715141714219614

Csppm-1-122-11-1-1-1-1-13-1-1-1-1-1-13-1-1-1-1-1-1-1

Fe"/o oxides2.252.622.154.944.125.534.466,474.454.525.026.422.565.792.742.655.294.843.986.96.9610.34.173.115

23.1

Hf ppm34343443334334433433333374

Hg ppm-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1


Sample ID142021420314204142051420614207142081420914210142111421614217142181421914220142211422214223142241422514226

14226 PULP DUP14227142281422914230

Au ppb-2-2-2787-2-2-2-2-2-2-2-2-2-255-2-2-2-2-2-219-2

Ag ppm-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-57-5

Asppm-0.54.63.819.42.2-0.51.60.82.81.56.850.138.615.16.84.6118.24.23.43.53.28.18.525.73.4

Bappm-50-50-50-50-50-50-50-50-50-504107306409301000100054010001200150089092065039070100

Br ppm-0.5-0.6-0.65.2-0.52.5-0.5-0.54.1-0.51.92.93.24.13.5-0.5-0.5-0.52.62.53.63.52.2-0.5-0.5-0.5

Ca"/o oxides

-1-14-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1

Co ppm1156392253925107211119322578476332213824

Cr ppm1054152315461014672932-556885-5-5-5-5-5-5323365

Cs ppm-1-1-1-1-1-1-1-1-111233452222322215-11

Fe0Xo oxides4.844.072.081.7215.97.892.191.374.352.844.591.321.21.41.983.984.644.943.72.821.691.721.785.3114.611.5

Hf ppm66644377235677777767777523

Hg ppm-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1


Sample ID141781417914180141811418214183141841418514186

141 86 PREP DUP

14187141881418914190141911419214193141941419514196

14196 PULP DUP

1419714198141991420014201

Ir ppb-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5

Mo ppm

-1-1-1

6-17-1-1-1-1-1

87-1-1-1-1-1-1-1-1-17-13-1

Na 7o oxides

4.146.15.825.4

4.424.365.335.224.894.883.012.223.873.853.445.235.2

4.442.884.584.545.863.3

5.515.215.23

Ni ppm-2041-20554562506860-20-20-20-20-20-20-20-20-20-20-20-20-20-20-2050-20

Rb ppm-15-15-15-15-15-15-15-15-15-15-15-15-15-15-15-15-15-1566-15-15-15-15-15-15-15

Sb ppm0.4-0.1-0.1-0.1-0.1-0.10.30.3-0.1-0.1-0.1-0.1-0.10.4-0.1

0.30.40.50.30.20.2-0.1-0.10.3-0.1-0.1

Seppm2.64.64.37.15.67.15.68.96.86.98.19.85.84.94.12

2.54.46

5.75.75.26.54.212.610

Seppm-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

Sn "/o oxides

-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.02-0.02

Sr "/o oxides

-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05

0.1-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05

Ta ppm-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.6-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.6-0.6

Th ppm3.45.25.16.54.55.24.85.64.24.36.46

6.26.57.98.29.85.53.44.24

3.45.33.814.6

7


Sample ID142021420314204142051420614207142081420914210142111421614217142181421914220142211422214223142241422514226

14226 PULP DUP14227142281422914230

Ir ppb-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5

Mo ppm-1-15-1-1-1-1-1-1-1512152213102918111267102018-1

Na"/o oxides7.066.376.98.085.924.994.544.694.343.990.110.10.080.130.090.060.120.10.10.120.140.140.170.380.181.15

Ni ppm-20-20-2035-2030-20-2033-2069-20-20-20-20-20-20-20-20-20-20-20-20603654

Rb ppm-15-15-15-15-15-15-15-15-15-15222272194274299226231203280280260256263240-1546

Sbppm0.40.4-0.1-0.1-0.1-0.1-0.1-0.1-0.1-0.10.60.50.60.90.60.40.40.30.50.40.40.40.30.51.20.2

Se ppm4.25.52.70.95.34.43.42.47.94.313.21.31.31.31.31.51.81.41.21.41.31.31.415.67.413.3

Seppm-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

Sn "/o oxides-0.02-0.02-0.02-0.02-0.02-0.02-0.02-0.02-0.02-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.03-0.03-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01

Sr "/o oxides-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0,05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05

Tappm-0.6-0.7-0.7-0.7-0.52.5-0.5-0.5-0.6-0.53.74.553.94.44.75.43.94.54.63.84.94.93.2-0.5

1

Th ppm8.88.510.484.77.885.43.74.524.438.437.838.138.8363737.337.638.43839.939.62042.6


Sample ID141781417914180141811418214183141841418514186

141 86 PREP DUP14187141881418914190141911419214193141941419514196

14196 PULP DUP1419714198141991420014201

U ppm-0.5-0.5-0.5-0.51.31.4-0.5

2-0.5-0.5-0.5

1.51.81.31.3-0.51.41.421

1.20.91.8

14.8-0.5

W ppm

-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-111-1-17683-11116

Zn ppm72129-50-50

96-50-50-50-50-50

149234-50

959992861292009689-50110-50

180-50

La ppm3.1

30.167.679.937.277.337.316365.966.123.138.229.521.824.111.312.417.622.59.89.911.619

12.693

87.5

Ce ppm

65812014779150743201221244974584249222432421920203826192171

Nd ppm-5175463276129120565120302010207121613891114117655

Sm ppm0.73.87.29.44.69.14.418.57.47.63.95.43.52.32.91.62.12.22.61.51.41.52.21.89.27.7

Eu ppm0.30.81.6

10.71.40.73.11.31.40.81.20.80.50.40.40.80.91.10.40.4-0.20.60.41.81.5

Tb ppm-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5

Yb ppm0.30.4-0.20.2-0.20.4-0.20.60.50.40.60.60.60.50.50.40.40.60.50.40.3-0.2-0.20.30.50.4

Lu ppm-0.050.06-0.05-0.05-0.050.06-0.050.090.070.070.1

0.090.090.090.10.060.070.090.080.060.05-0.05-0.05-0.050.080.06

Mass grams20

22.3321.8321.220.9721.8223.2722.2329.928.8523.4

29.3923.5126.1222.322.1823.1622.722.628.7229.4225.5625.4

23.2323.7529.56


sample ID142021420314204142051420614207142081420914210142111421614217142181421914220142211422214223142241422514226

14226 PULP DUP

14227142281422914230

U ppm-0.5

1.73.2-0.5

2.5-0.5

1.32.2-0.5-0.510.119.516

23.216.920.819.416.418.519.519.521.117.210.21.81.6

W ppm

-1-1-1-1

147-1-1-1-1-1-13-1-1

44-1-1-1-1-1

257-1

Zn ppm-50-50-50-50-50-50-50-50-50-50

3808010073019401830801111017002210795788236509

12200466

La ppm47.397

95.973.25.7

68.37.97.990

38.545.360.663.665.966.541.655.766.363

64.967

69.563

36.320.743.8

Ce ppm97194193146

91331617172809813914414514099126148143142145150134804689

Nd ppm35766762-5

46-5-5643028514951462845544450445046251540

Sm ppm5.311.410.58.3

16.41.31.69

4.28.111.911.712.412.28.510.412

11.811.712

12.111.7

73.76.3

Eu ppm1.12.41.82

-0.2

1.20.50.52.20.80.4-0.2-0.2-0.20.40.60.70.70.70.60.50.50.40.60.91.3

Tb ppm-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.51.31.81.61.81.81.41.51.61.61.71.51.71.6

1-0.5-0.5

Yb ppm-0.2-0.2-0.2-0.2

0.5-0.2

0.90.70.6-0.24.96.47

6.76.37

6.66.67

6.67.47.47.14.42.52.4

Lu ppm-0.05-0.05-0.05-0.050.07-0.050.140.110.12-0.050.730.961.081.070.981.030.970.991.091.081.141.171.110.690.360.36

Mass grams

26.2323.3624.1423.229.2625.525.3325.7825.3823.0228.6219.9624.3523.7423.6122.6722.8823.7926.2822.6

28.4127.5121.829.5624.4624.38


Samole ID141781417914180141811418214183141841418514186

141 86 PREP DUP1418714188141891419014191141921419314194

141 94 IR1419514196

14196 PULP DUP1419714198141991420014201

Ag ppm-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.30.3-0.3-0.30.40.4-0.3-0.3-0.30.3-0.3-0.30.3-0.3

IR - pulp reruns

Cd ppm-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.30.60.3-0.3-0.3-0.3-0.3-0.3-0.30.6-0.3-0.3

Cu ppm642517793332514978175112252488821614586337

Mn ppm2684588927355054793665113813825952700580342586620754167016913425597595258635331433130

Mo ppm33453-1383-1-1424724847235-1-127

Ni ppm19402152435845645754191881613647891512731204816

Pb ppm11-3152161016281611910325571815141475-3-3-3-398

Znpprn42613865567157836767128199946797731171881861679810148120699627

Al "/o oxides4.133.873.663.804.543.803.824.243.984.424.116.053.743.363.524.013.723.443.437.153.944.093.533.513.623.482.61

Be pprn

111111-11-1-111-1-1-1-1-1-1-11-1-1-1-1-1-1-1


Sample ID142021420314204142051420614207

14207 IR1420814209142101421114212142131421414215142161421714218142191422014221

14221 IR1422214223142241422514226

14226 PULP DUP14227142281422914230

Ag ppm2.40.52.30.4-0.3-0.3-0.30.4-0.3-0.3-0.392.62531.30.40.60.70.81.21.32.22.20.81.21.52.00.90.90.70.45.3-0.3

IR ̂ pulp reruns

Cd ppm0.5-0.30.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.376.312520.7-0.31.0-0.30.82.46.86.36.22.83.85.17.33.62.80.90.933.60.9

Cu Ppm15

3471124272103231610747

9999970342820433613398884873063761103029183754010

Mn ppm192229135791602772611941562741831121202692351043768493326206342340405434328244149135170103129862076

Mo Ppm-1223432437213554310122113108251971067815171

Ni ppm162313311029221072918351195527533111-145544573154

Pb ppm7-39510-35-3-338

2559203257240108270207277451720718151501110315633863661151444564131

Zn ppm3735311213434029255134

2959099999258693766010270619381810181283211071683220083178522942810940401

Al "/o oxides3.663.873.784.313.303.673.293.193.283.644.130.090.083.483.794.894.003.933.974.093.543.363.623.413.514.024.193.913.4710.055.366.70

Beppm-1-1-1-1-1-1-1-1111-1-1-1-1944446677654449245


Sample ID141781417914180141811418214183141841418514186

141 86 PREP DUP1418714188141891419014191141921419314194

141 94 IR1419514196

14196 PULP DUP1419714198141991420014201

Bi pprn-2-2-2-2-2-2-2-2-2-2-2-2

3-2-2-2-2-2-2-2-2-2

43-2-2-2

IR s pulp reruns

CaVo oxides

0.230.310.810.610.280.230.240.540.410.420.322.120.220.200.310.561.222.902.893.020.480.490.260.110.160.400.26

K?'o oxides

0.850.300.480.340.390.280.120.040.050.060.150.530.220.140.110.130.070.100.090.850.090.100.040.130.050.020.02

Mg"/o oxides

1.221.411.092.262.392.762.263.122.442.563.214.521.441.271.640.600.410.870.812.921.051.040.332.511.682.430.43

P"/o oxides0.0260.0300.0440.0900.0280.0410.0470.1040.1000.1070.0860.0920.0240.0100.0200.0200.0560.0230.0230.0110.0340.0350.0260.0180.0330.0390.022

Srpprn1047777667765757780816756875673615355577663784665644339

Ti "o oxides

0.130.160.190.230.060.120.110.250.180.180.200.150.130.060.180.120.220.110.110.060.100.100.110.080.120.090.12

VPprn335543705160537868687476334928172936362952505235288269

YPprn

-11311

-1-1322361122222411-1-1-1-1-1

S70

0.0210.0660.1270.6220.1740.1510.1010.1210.2370.2620.0980.0620.0410.2210.0500.3580.5241.2981.3010.1140.0220.0210.0720.0310.0770.8670.136


Sample ID142021420314204142051420614207

14207 IR1420814209142101421114212142131421414215142161421714218142191422014221

14221 IR1422214223142241422514226

14226 PULP DUP14227142281422914230

Bi ppm

-2-2-23-2-2

2-257-2

86-2-2

33-2

4-2

576-2-24-2

5-2-2796

IR s pulp reruns

Ca0Xo oxides

0.280.360.170.250.230.340.330.200.280.250.180.090.020.170.141.270.510.320.180.080.030.030.020.030.040.040.050.050.181.710.440.71

K"/o oxides

0.020.040.040.050.040.060.060.090.080.050.250.010.021.932.344.776.476.046.166.393.393.272.962.965.165.356.356.426.465.240.410.57

Mg 0Xo oxides

0.991.530.820.130.081.571.531.040.692.902.090.49-0.010.880.782.250.380.370.240.310.400.400.420.580.440.310.300.230.412.963.855.81

P"/o oxides0.0340.0430.0250.0260.0200.0650.0610.0130.0120.0310.022-0.0010.0040.0330.0250.037-0.0010.0020.001-0.001-0.0010.002-0.0010.0020.0020.0010.0020.002-0.0010.0380.0240.035

Sr ppm465354675774667797108114

3-1

108120754747454210108133127433844961436

Ti "/o oxides

0.130.200.160.120.080.130.140.090.110.210.160.01-0.010.130.140.370.070.070.080.060.060.070.070.060.070.060.060.060.070.380.140.17

V ppm402816356454526197250-2-22724116-2-2-2-2-2-2-2-2-2-2-2-2-2

11970121

Yppm

-1-1-1

1-11-11211

-1

311

4278796456232627253638584770611421

S0Xo

0.0040.9660.1491.7350.2510.0810.0760.0050.0050.0070.005

20.06826.3120.0430.0220.1170.3470.2660.4510.7380.7210.6820.5800.6631.0210.6860.3980.3510.1480.1222.2050.055


Sample ID14030

I4030 PULP DUP1403114032140331403414035140361403714038140391404014041140421404314044140451404614047140481404914050

4050 PREP DUP14051140521405314054

Au ppb-2-2-2-2-222-22-2-2-2-2-2-2-23-2-2-2-2755-2-2-2-2

Ag ppm-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5

As ppm3.23.4-0.52.622.2-0.5-0.5-0.51.52.1-0.52.2-0.5-0.58.4-0.53.8-0.5-0.5-0.52.93.125.942.3-0.5

Bappm8285-5062320310310240270260190280-50-5028080-50-50240400240-50-5070220180110

Br ppm-0.5-0.5-0.5-0.5-0.5-0.5-0.51.6-0.5-0.5-0.5-0.5-0.5-0.531.3-0.5-0.5-0.52.42.9-0.5-0.5-0.5-0.52.8-0.5

Ca "/o oxides

-1-1-1-1-1-1223-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1

Coppm10099236648213481481061141494038176714142014116

Cr ppm14714580159104127859610114312511712870123112106100210127951111125869170159

Csppm-1-1-1-1-1-12-12-1-1-1-1-1-1222142223-1-1-1

Fe "fa oxidss4.674.735.387.224.823.863.132.223.632.92.23.0111.88.733.654.291212.37.242.983.474.734.728.817.385.613.49

Hfppm332433322434423334333333343

HgPPm-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1


Sample ID140551405614057140581405914060

I4060 PULP DUP1406114062140631406414065140661406714068140691407014071140721407314074140751407614077140781407914080

Au ppb4-2-2-2-2-2-2-233-2-244-2-2-2-2-2-2-234-2-2-26

Ag ppm-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5

Asppm-0.5-0.5-0.5-0.5-0.51.61.51.21.7-0.5-0.5-0.52.22

-0.52

-0.51.7-0.5-0.52.2-0.51.9-0.5-0.5-0.5-0.5

Ba ppm-5032020061014008508409203401502903102507906804901500670130062051015057047017001000870

Br ppm-0.5-0.51.6-0.5-0.5-0.5-0.5-0.52.42.8-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.51.92.41.5-0.5-0.5-0.51.9-0.51.4

Ca 17o oxides

-123-1-1-1-112-1-1-1-1-1-1-1-1-1-1-1-1-1-11-1-1-1

Coppm8252865653637771389744359815885

GrPpm1201441389513212512615312613487828986899994110141102168108109116102101119

Csppm-1-1-121-1-1-12221-1332321-1221-111-1

Fe "o oxides3.445.865.062.161.051.351.312.022.142.213.012.043.53.993.562.443.311.791.992.072.473.242.883.912.521.951.43

Hf ppm256433368677643333645332232

Hg ppm-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1.-j-1-1-1-1-1-1-1-1-1-1-1


Sample !D14030

I4030 PULP DUP1403114032140331403414035140361403714038140391404014041140421404314044140451404614047140481404914050

4050 PREP DUP14051140521405314054

Ir ppb-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5

MoPpm

-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-13534-1-1-1-1

Na /o oxides

4.484.476.153.333.313.491.842.751.6

3.013.983.681.555.183.673.040.350.442.413.094.043.2

3.212.743.154.074.18

Ni Pprn5452-348450-29-25-25-26-27-28-2763-33-29-25

7381109-26-30-25-26-26-2678-29

Rb ppm-15-15-15-15-15561427512546-15-15-15-15-15-15

24-158157374034-15-15-15-15

Sb ppm-0.1-0.1-0.1-0.1-0.1-0.10.20.2-0.1-0.1-0.1-0.10.4-0.1

0.40.30.61.10.50.3-0.10.30.40.6-0.1-0.1-0.1

Seppm9.69.53.5147.96.79.79

17.16.21.63.9

44.76.98.12.940

43.811.8

23.44.84.93.87.57.84.1

Se ppm-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

Sn '/b oxides

-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01

Sr 7o oxides

-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05

Ta ppm-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.51.31.2-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5

Th ppm3.43.32.37.96.43.23.43.72.87.55.43.32.82.27.73.52.32.76.73.65.15.15.73.44.110.66.7


Sample !D140551405614057140581405914060

I4060 PULP DUP1406114062140631406414065140661406714068140691407014071140721407314074140751407614077140781407914080

Ir ppb-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5

Mo pprn-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-19-1-1-1-1-1-16-1

Na "/s oxides4.163.443.723.884.153.733.693.813.563.745.345.394.623.113.74.483.343.683.584.343.984.022.693.633.384.25.02

Ni pprn-28112100-30-28-26-26-31-30-33-34-29-31-26-27-25-27-20-20-20-20-20-23-25-23-22-24

Rb pprn-15-15-15-1599585044345861-157210475536647-15596659123-15111-1545

Sb pprn-0.10.3-0.10.3-0.1-0.1-0.1-0.1-0.1-0.1-0.10.3-0.1-0.1-0.1-0.10.3-0.1-0.1-0.1-0.1-0.1-0.1-0.1-0.1-0.1-0.1

Se pprn4.911.78.63.311.41.31.41.51.52.22.15.45.19.34.4112.43.64.35.47.15.25.13.11.41.3

Sepprn-33-3-3-3-3-3-3-3-3-3-3-3-3-3-3-3-3-3-3-3-3-3-3-3-3-3

Sn O'o oxides-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01

Sr "/o oxides-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05

Tapprn-0.5-0.51.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5

Th Pprn5.34.368.24.33.93.87.88.710.38.277.64.35.32.93.73

13.92.39.52.93.74.62.12.71.3


Sample ID14030

I4030 PULP DUP1403114032140331403414035140361403714038140391404014041140421404314044140451404614047140481404914050

4050 PREP DUP14051140521405314054

U Dpm2.42.7-0.5

21.5-0.5-0.5-0.51.2-0.5-0.5-0.5-0.5-0.5-0.51.9-0.5-0.5-0.5-0.52.4-0.5-0.5-0.5-0.52.7-0.5

W ppm

-1-1-1-1-1-1-1-1-1-1-1-1-15-1-11211-1-1-1-1-145-1-1

Zn ppm81100-50-508114694-5014567-50110201-50186191357371372126153224245535373224208

La ppm1.31.31.3

64.630.715.432

28.336.339.225.620.414.8

129.916.614.218.456.634.437.56.56.738.44.416.610.3

Ce ppm-3-3-3

114623262546676504237-36031323910565691415718

3122

Nd ppm-5-5-547241025172819161318-5251114124628315630-5129

Sm ppm0.50.40.47.43.61.74

3.55.14.22.52.24.60.43.51.94.44.76.33.64.21.21.24.50.82.71.7

Eu ppm-0.2-0.2-0.21.60.90.41.41.11.4

10.50.61.3-0.2

10.81.51.71.51.31.40.60.61.50.30.90.5

Tb ppm-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.50.7-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5

Ybppm

10.91.31.60.80.51.3

11.90.60.40.64.61.30.80.54.34.80.60.50.30.70.80.50.50.60.4

Lu ppm0.140.140.20.240.130.080.190.160.280.09-0.050.090.680.20.120.080.650.670.10.080.050.120.110.070.080.1

-0.05

Mass grams

21.1423.6723.1822.7921.1719.6220.1422.5721.2921.3720.4621.7924.8121.4121.820.4624.9324.2221.9219.219.8420.3920.2222.7422.1622.0921.25


Sample ID140551405614057140581405914060

I4060 PULP DUP1406114062140631406414065140661406714068140691407014071140721407314074140751407614077140781407914080

Uppm-0.5-0.5-0.5-0.5

1.5-0.5-0.5-0.5-0.5-0.5

2.12.53

-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5

W ppm

-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1

Zn ppm275-50

128-50-50-50-50

56104-50-50

109-50

119-50

80-50-50

991229511653165238225-50

Lappm5.8

48.559.371.117.118.217.874.591.412312087.910239.445.621.841.419.310816.970.421.950.423.225.1

74.7

Ceppm

1211013913737363514518124120614917975904677401973512745924550159

Nd ppm

-5

475339121314486568685468293516351867154324402222-5-5

Smppm0.98.69.35

1.51.71.75.67

8.48.46.18.64.45.92.86.82.48.82.56.23.25.63.22.91.10.7

Eu Ppm0.41.71.81.40.60.60.41.11.32

2.31.32.11.21.30.61.40.61.50.61.10.81.30.80.90.4-0.2

Tb ppm-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5

Yb ppm0.41.31.20.7-0.2-0.2-0.2

0.60.60.60.70.70.80.81.10.71.10.50.2-0.2

0.70.60.60.40.40.3-0.2

Lu ppm-0.050.20.190.12-0.05-0.05-0.050.090.10.090.120.080.170.120.16-0.050.22-0.050.10.070.120.050.090.1

0.07-0.05-0.05

Mass grams

22.4522.5822.9221.8520.0221.8621.1919.4521.220.0817.6521.0220.1419.3920.2720.0420.3720.0120.9620.5219.6820.2121.3720.0920.55

2119.93


Sample ID14030

14030 PULP DUP140311403214033140341403514036140371403814039

14039 IR1404014041140421404314044140451404614047140481404914050

14050 PREP DUP1405114052

14052 /R1405314054

Ag ppm-0.3-0.3-0.3-0.3-0.30.5-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.30.6-0.3-0.3-0.3-0.3

IR = pulp rerun

Cd ppm0.71.01.10.70.90.7-0.3-0.31.20.8-0.30.40.82.11.00.50.52.52.11.3-0.30.60.50.51.11.21.90.71.0

Cu ppm787853052114143123323153393148751166444344321

Mn ppm410423278476373531444306485506331343646109433510471754229825102994117410662060206534453061312514971024

Mo ppm645755-1486245106-161257542726107775

Ni ppm50541478463110192535141722612822156681100152228264143417935

Pb ppm-36-37-33613-3-329141245486106330-36695832433520

Zn ppm444214383565443362664951938618140175273321285129129243246555355361188133

Al "/o oxides

2.612.852.766.013.673.254.795.0210.422.942.272.422.528.743.302.803.305.766.044.562.722.843.083.403.534.844.354.293.03

Beppm22-11113232-1-122111332212222211


Sample ID140551405614057140581405914060

14060 PULP DUP140611406214063140641406514066140671406814069140701407114072

14072 IR1407314074140751407614077140781407914080

Ag ppm-0.3-0.3-0.3-0.30.3-0.3-0.30.4-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.30.4-0.3-0.3

IR = pulp rerun

Cd ppm0.81.00.6-0.3-0.3-0.3-0.3-0.3-0.3-0.30.6-0.3-0.30.5-0.30.6-0.3-0.3-0.3-0.3-0.3-0.30.40.40.30.90.60.4

Cu ppm2322813794332224726313352433

35017278

Mn ppm9617136492751271862062253054108085239261040816584652399229237332380685487673628872402

Mo ppm3964-125343515425624343437-123

Ni ppm2410883102675751081210161012845692114221686

Pb ppm24-35-3-3-3665-35-3121118-34-38-3-3-3811325417752

Zn ppm159586229131719223250100589997755570372122303371549919919081

Al "/o oxides

2.535.468.532.602.282.902.883.023.173.393.463.033.173.543.363.293.033.063.033.363.443.442.953.904.152.962.752.93

Beppm

121211111121222221111113-1221


Sample ID14030

14030 PULP DUP140311403214033140341403514036140371403814039

14039 IR1404014041140421404314044140451404614047140481404914050

14050 PREP DUP1405114052

14052 IR1405314054

Bi ppm

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

IR = pulp rerun

Ca "/o oxides

0.180.190.530.620.360.131.781.512.530.370.160.170.160.700.540.220.450.250.240.880.680.340.950.960.510.350.330.690.48

K 0Xo oxides

0.110.110.010.210.350.602.341.252.660.680.520.550.790.590.070.790.300.370.280.770.620.350.210.230.180.390.390.180.30

Mg "/o oxides

1.901.960.614.943.072.532.732.934.762.871.341.461.936.391.331.761.826.355.493.571.091.231.832.002.753.563.583.281.63

P "/o oxides

0.0280.0290.0250.1280.0580.0190.0300.0320.0410.0430.0280.0290.0360.0510.0160.0310.0200.0480.0550.0690.0190.0430.0340.0360.0330.0250.0260.1610.063

Sr ppm54583581767710511417665626773435790563030721211087980818583161106

Ti "/o oxides

0.290.360.160.370.220.170.320.290.470.240.140.140.140.900.120.190.140.941.050.160.100.150.160.170.180,140.140.200.10

Vppm6570791218079141118178714749633311795332

38138274293243435172746835

Yppm

11310419

11364-1-1-1

53322

40403213323221

S"/o

0.1930.1920.5570.2060.0990.0350.0020.0040.0090.0060.0110.0100.0210.2980.0950.0940.1570.4460.2580.0130.0240.0480.3220.3372.5150.2120.2020.0620.022


Sample ID140551405614057140581405914060

14060 PULP DUP140611406214063140641406514066140671406814069140701407114072

14072 /R1407314074140751407614077140781407914080

Bi ppm-2-22-2-2-2-2-2-24-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2

IR = pulp rerun

Ga "/o oxides

0.251.811.210.500.510.420.380.470.640.980.980.370.910.520.560.570.650.390.380.410.480.420.320.370.420.420.680.31

K "/o oxides

0.180.530.431.061.571.281.301.000.720.500.390.210.451.620.980.761.461.011.341.401.040.720.351.640.441.620.740.93

Mg "/o oxides

1.634.133.790.850.260.470.510.520.800.700.970.571.201.231.460.901.110.760.450.470.660.881.711.672.471.411.050.52

P0Xo oxides0.0230.1760.1610.0250.0050.0100.0110.0210.0240.0100.0170.0100.0150.0290.0440.0250.0340.0280.0120.0130.0240.0210.0270.0290.0500.0150.0210.017

Srppm110273170129137112157165198175164128188941381271591131311591301217860108100110152

Ti 0Xo oxides

0,110.700.460.150.070.100.100.170.140.130.170.200.210.190.250.170.210.160.160.110.130.180.190.180.150.090.110.10

Vppm42103702371111162430533046375127562315132133474347532517

Yppm-114171-1111222-12242411224234-11-1

S"/o

0.0470.0670.1130.1120.0450.0500.0520.0240.0600.0370.0210.0590.0490.2390.0610.1470.1120.1250.0590.0490.0290.0650.0630.0750.1150.0300.0730.021


Sample ID1400114002140031400414005140061400714008140091401014011140121401314014140151401614017140181401914020140211402214023140241402514026140271402814029

Au ppb-2-2-2-2-2-2-2-2-2-2-2-2-2-23-2-230-2-2-2-2-253-2-2-22

Ag ppm-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5

As ppm-0.52.51.72.23.11.913.13.243.43.44.21.6-0.51.64.710.855625.56.310.317.916.19.414.75.81.55

-0.5

Ba ppm1300490037034020070150380450460250350630890880960200320280440330940620480440790880330540

Br Ppm1.6-0.51.52

-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.51.5-0.51.71.6-0.52

-0.52

-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5

Ca "/o oxides

-1-1-1-1-135867754442-1-1-131-1-11-13324

Co ppm232547434947575346452323232327473536273433273130192530

Gr ppm186352195172125272364938383335121172181101230223232270141288281241249280210264450

Csppm-111-1-1-12-1-1-1-12-1-1-1-1-1-1-1-1-1-1-1-12212-1

Fe Vo oxides0.895.371.271.31.656.4710.19.029.839.799.059.744.154.123.813.879.9912.79.837.738.8910.510.710.49.277.464

7.026.73

Hf ppm22223232222223222121332222334

Hg ppm-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1


Sample ID1400114002140031400414005140061400714008140091401014011140121401314014140151401614017140181401914020140211402214023140241402514026140271402814029

Ir ppb-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5

Mo ppm-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1-1511-1-1-1-1-1-1-1-1-1-1-1

Na 070 oxides3.610.024.334.024.52.052.52.181871.812.482.623.633.172.933.763.042.063.252.83.671.150.941.431.592.093.142.832.56

Ni ppm-20160-20-20-201594140414041411031041094211010013516086142120140140186100133200

Rb ppm662450-15-15-1544-1550-15-15-15-156043-1527-152536343467494045-15-1539

Sb ppm-0.1

10.20.3-0.1-0.10.2-0.10.2-0.10.4-0.10.4-0.1-0.1-0.10.3-0.1-0.1-0.10.60.61.11.60.2-0.1-0.1-0.1-0.1

Se ppm

115.62.11.62.32339.14244.545.24244.214.713.1138.115.417.617.221.211.515.514.415.91618.612.417.119.3

Seppm-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

Sn "/o oxides-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.02-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01-0.01

Sr "/o oxides-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05-0.05

Ta ppm-0,5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5

Th ppm1,43.11.622.52.84.32.53.43.53.12.92.55.65.743.74.22.31.44.85.53.41.83.422.96.810


Sample ID1400114002140031400414005140061400714008140091401014011140121401314014140151401614017140181401914020140211402214023140241402514026140271402814029

U ppm-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0,5-0.51.9-0.52.2-0.51.81.41.6-0.5-0.50.71.41.61.1-0.5-0.5-0.52.4-0.51.9

W ppm

-17-1-1-1-1-1-1-1-1-1-1-17-1-1-18-1-1696-16-1-1-1-1

Zn ppm-50154-50-50-5085-50-508313813614110610212415928177702252412005247687111930576121366-50

La ppm5.912.18.710.27.319.315.911.812.612.413.612.911.732.530.323136.24.410.213.237.914.410.717.79.819.243.858.9

Ce ppm

11261221123634282827292821534742201212202975282538233681103

Nd ppm

51087613171318891210171617117-510-5281081815213744

Sm ppm0.72.41.11.31.33.74.33.43.63.63.83.82

2.52.33.32.62.31.72.42.86

2.32.13

2.43.16.38.1

Eu ppm0,30.60.40.4-0.21.11.11.20.91.11.21.20.90.80.6

10.90.70.6

10.81.60.60.70.70.80.81.42.2

Tb ppm-0,5-0.5-0.5-0.5-0.5-0.5

1-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5-0.5

Yb ppm0,31.10.3-0.20.31.33.22.72.82.93

2.80.80.70.70.8

10.80.8

10.91.41.20.91.21.1

11.41.6

Lu ppm-0.050.16-0.05-0.05-0.050.180.470.410.420.440.450.420.120.1

0.110.120.110.120.130.150.140.230.180.160.20.160.160.220.24

Mass grams

22.1921.220.0418.819.5

23.4525.1125.0124.0225.2524.3821.1522.3720.7223.4323.3222.7922.521.8923.1620.522

23.0223.1922.2422.6921.9622.1122.94


Sample ID1400114002140031400414005

14005 /R1400614007140081400914010140111401214013140141401514016140171401814019

1401 9 IR14020140211402214023140241402514026140271402814029

Ag ppm0.50.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.3-0.30.8-0.30.3-0.3-0.3-0.31.50.61.00.4-0.3-0.3-0.3

IR = pulp rerun

Cd ppm0.40.9-0.3-0.30.3-0.30.81.81.31.41.41.71.51.40.80.80.72.225.42.52.22.32.12.24.82.68.12.70.71.11.5

Cu ppm321452297155134155139141139282515293196879035504949508269243810

Mn ppm1616841422341911879551858170616801636170418968877717765991535187816781730120112711896218022582016178983310871198

Mo ppm372-13-19128949937781623131010711161478974

Ni ppm71537109615727393840394098969242989113013815281131113109139170102126193

Pb ppm-395462223-3141011232826913-31448130787922521841711489642152686-3

Zn ppm1213816343331671039811194106127687763751855452250253186157386619482156245292227109

Al 0Xo oxides4.093.422.662.282.682.795.665.556.224.694.424.526.5411.9811.5710.922.8113.7512.454.414.809.8214.2110.9512.2111.537.635.844.2113.265.67

Be ppm

13-111121-1-1-11-1111122112122222122


Sample ID1400114002140031400414005

14005 IR1400614007140081400914010140111401214013140141401514016140171401814019

1401 9 IR14020140211402214023140241402514026140271402814029

Bi ppm-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2-2-28-2-2-2-2184-2-2-2-2-2-2

IR = pulp rerun

Ga 07o oxides0.450.730.230.190.350.362.604.976.725.755.785.815.223.873.403.692.320.910.360.820.813.190.970.940.591.310.693.062.631.904.31

K "/o oxides2.350.190.320.440.300.320.120.400.680.780.790.690.851.802.141.851.131.060.780.170.211.010.741.591.911.440.841.071.151.040.55

Mg 07o oxides0.595.430.950.781.041.077.763.014.103.603.653.633.904.574.144.191.665.665.324.294.465.645.545.265.234.634.585.363.087.056.70

P 7o oxides0.0090.0340.0170.0120.0470.0460.0370.0430.0340.0300.0300.0360.0320.0590.0370.0260.0350.0310.0330.0230.0250.0250.0610.0900.0360.0290.0310.0220.0320.1170.115

Sr ppm20784959112412120021626123122128321025530236424499326570211531006212377215294192246

Ti 07o oxides0.060.440.100.090.130.140.490.880.720.640.640.650.640.410.380.260.290.350.320.330.340.350.300.440.400.300.390.380.330.530.49

V ppm131492120232318142136232433426930910991858085901071101207411010010210211685122150

YPpm-1101-1-1-11534282423262715121232828551519322420111173222

S"/o

0.0070.1830.0030.0610.0130.0140.0330.1330.0830.1120.1130.0910.1010.0250.0720.0560.1870.2610.7870.3810.4040.1910.2040.3100.2380.1400.3310.2450.0620.2920.065


Appendix 3 - Expenditures

Appendix 3. Summary of Expenses.

Summary of Expenses for 2002 Island Copper Drilling Program

Item Amount

Geological Consulting 323,822.91

Drilling 365,502.76

Gas S Propane 5751.18

Sample shipping and analysis 58,822.28

Field supplies 5612.82

Equipment Rental 51,758.90

Accommodation S Meals 32,260.08

Truck Rental 31.047.58

Total 3104,578.51

MINISTRY OF NORTHERN DEVELOPMENT AND MINES

Work ReDort Summary

Transaction No: W0450.01412 Status: APPROVED

Recording Date: 2004-AUG-12 Work Done from: 2002-NOV-04

Approval Date: 2004-SEP-10 to: 2003-MAY-08

Client(s):

130679 FALCONBRIDGE LIMITED

400398 Y M C A

Survey Type(s):

ASSAY PDRILL

Work Report Details:

Claim*

G 5050012

SSM 1239731

SSM 1239732

SSM 1239733

SSM 1239734

External Credits:

Reserve:

Perform Perform Approve

5105,780 5105,780

SO SO

50 SO

so soSO SO

5105,780 5105,780

SO

Applied

SO

56,400

52,400

56,400

53,200

518,400

587,380 Reserve of Work

587,380 Total

Status

Applied Approve

50

56,400

52,400

S6.400

S3.200

518,400

Assign

518,400

50

SO

SO

50

S18.400

Assign Approve Reserve

18,400 S87.380

0 SO

6 SO

0 SO

0 SO

518,400 587,380

Reserve Approve

587,380

SO

SO

SO

SO

587,380

Due Date

2010-SEP-01

2010-SEP-01

2010-DEC-09

2010-SEP-01

Report*: W0450.01412

Remaining

of claim is based on information currently on record.

41K09NW2005 2.28404 AWERES 900

2004-Oct-08 10:45 PRUDHOMMEI Page 1 of 1

Ministry ofNorthern Developmentand Mines

Date:2004-SEP-13

Ministers duDeveloppement du Nord etdes Mines Ontario

GEOSCIENCE ASSESSMENT OFFICE 933 RAMSEY LAKE ROAD, 6th FLOOR SUDBURY, ONTARIO P3E 6B5

FALCONBRIDGE LIMITED 800-207 QUEEN'S QUAY WEST TORONTO, ONTARIO M5J1A7 CANADA

Tel: (888) 415-9845 Fax:(877)670-1555

Dear Sir or Madam

Submission Number: 2.28404 Transaction Number(s): W0450.01412

Subject: Approval of Assessment Work

We have approved your Assessment Work Submission with the above noted Transaction Number(s). The attached Work Report Summary indicates the results of the approval.

At the discretion of the Ministry, the assessment work performed on the mining lands noted in this work report may be subject to inspection and/or investigation at any time.

An excellent report accompanies this submission.

If you have any question regarding this correspondence, please contact BRUCE GATES by email at [email protected] or by phone at (705) 670-5856.

Yours Sincerely,

/fWt ^ cRon C. Gashinski

Senior Manager, Mining Lands Section

Cc: Resident Geologist

Falconbridge Limited (Claim Holder)

YMCA (Claim Holder)

Assessment File Library

Falconbridge Limited (Assessment Office)

Visit our website at http://www.gov.on.ca/MNDM/LANDS/mlsmnpge.htm Page: 1 Correspondence ID:19812

CANADAMining Land Tenure

Map

1003

toOo

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Date l Time of Issue: Fri Sep 10 14:33:44 EOT 2004

TOWNSHIP 7 AREA PLAN AWERES G-3090

ADMINISTRATIVE DISTRICTS l DIVISIONS

Mining DivisionLand Titles/Registry DivisionMinistry of Natural Resources District

Sault Ste. MarieALGOMASAULT STE MARIE

TOPOGRAPHIC Land Tenure

Surtsca And Mining Rlghfc

Concession, tot

Provincial Park

Mln* Headframa

RaHway

Ro*tJcB And Mining Rkjhh

Umd UM Ptrmll

Order In CDuncH (Not oponRx M

[3 CB 5) BB B

LAND TENURE WITHDRAWALS

Suited, warm Onfc WMnnm Wiiiijf R^Wi Or-VWIfMlm

Qrdw m Council WUhdnwal Typos

W'm Mama Kami On

IMPORTANT NOTICES

LAND TENURE WITHDRAWAL DESCRIPTIONS

STB 7 Warn Jan

sew S915 Ed Ed

9I1BS) 32

B133

ats0*G G IS

useP. PLASMCSMC W*mCMC Warn

Warn

2001BOW 20W 2001 soai2001

Oescilrrtlon

tHtB TOWNSHIP IS UNDER ALGOMA CENTRAL AND HUDSON BAY fCOMPANYLANDS UNDER THE CONTROL OF THE PFMVIHCELANDS NAVE BEEN RETURNED TO CRDWW CONTROLLANDS HAVE BEEN RETURNED TO CROWN CONTROLQOLD AND SILVER ONLY CONTROLLED BY THE CNOWNfCAHAOA)GOLD AND etLven DNIY CONTROLLED BY THE CSOWN(CAMADA]LANDS UNDEf THE CONTROL OF THE PROVINCE

V THE CROWN (CANADA}

CROWN TO SERVE CACnVN RE SERVE CHOWN RESERVE CROWN RE SE RV E CROWN RESERVE OllARRr PERMIT CKIBJRZ SERVE

GOLD t SILVER ONLY CONTROLLED BY CROWN (CANADA). OOID S SILVER ONLY CONTROLLED BY CROWN (CANADAX BOLD C SILVER ONLY CONTROLLED BY THE CROWN (CANADA) GOLD AND SILVER ONLY CONTROLLED BY THE CROWN (CANADA) QOLD AND SILVER OM.Y CONTROLLED BY THE CROWN (CANADA1 QOLD AND 6IWER ONIY CONTROLLED BV THE CROWN(C*NAnA)

MMNC RIGHTS COOTROtLED BV THE CROW W (CANADA] MINlNffl RIGHTS CONTROLLED Br THE CROWN (CANADA). ENQUIRES

REGARDING (A). fO.S.) 6 (M) SHOULD 83 DIRECTED TO THE DIRECTOR LANDS,EVENUES AND TRUSTS, ONTARIO REGION DEPARTMENT OF INDIAN ANDORTHCRN AFFAIRS.URfACE AND MfMNO WGHTe CONTROLLED BY THE CROWN - (CANADA},andlnt npplfcatbn ardor tin Pubfc Lands Ad.LWFACE B MIMING RIGHTS CONTROLLED BY THE CROWN (CANADA).URFACE AND MINING R1GKT3 CONTROLLED DY THE CROWN (CANADA)

Ce AND MIHINfl Rti^TS CONTROLLED Bf THE CROWN - (CANADA),EC. 38.i*OW-Bt,'TSa4JS;75S.R.O. SBWSC.35 W-LL-C2B1'B9 QNT MAYISBBMIiS

' 60M-S&-03 Worn

'.12*0 Wsm

C2U1.Q3CWT MIS wHMriwiis.aSMiMng Act Rao 1900,njce/03 Boundary fl*rwr*ilydoptuaiwa vfttnarawn Click to vMw actual a wi *n.'*..Mtnlng and SurlncD Rtaht9 wttrdmwn Doc. IT. 2003CEC.^/BOIB.'lilM S.R-O. 11CB91WHOLE TOWNSHIP WITHDRAWN FROM STAKING (M.R1S.R.) SEC. 31 OF MINI MO ACT

(R.S.O. 1900). OfiDiRNO.W.12,'80, AUGUST 36, 1BUO- FILE 1BD5X.

2.28404 ASSAY PDRILL

report oil novj - ontario€¦ · 2 .28404 island copper report on fall drilling program november-...

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