jan 1 $ 2q07 on the gold commissioner's office vancouver, b.c

REPORT

JAN 1 $ 2Q07 Gold Commissioner's Office

VANCOUVER, B.C.

on the

CHU AND PORPHYRY PROJECTS

Omineca Mining Region, British Columbia Latitude 53° 21' N., Longitude 124° 37' W.

NTS map sheet 93F/7E

by

James W. McLeod, P.Geo.

on behalf of A

v *

Omega Exploration Services Inc.

"V'- j i 'Sj

January 2,2007 Delta, British Columbia

I

TABLE OF CONTENTS

Page

SUMMARY 3 INTRODUCTION 4 LOCATION AND ACCESS 4 TOPOGRAPHICAL AND PHYSICAL ENVIRONMENT 4 PROPERTY AND OWNERSHIP 5 HISTORY 6 REGIONAL GEOLOGY 6 LOCAL GEOLOGY 7 PRESENT WORK PROGRAM 8 CONCLUSIONS 9 RECOMMENDATIONS 13 COST ESTIMATE 13 STATEMENT OF COSTS 17 CERTIFICATE 18 REFERENCES 19

APPENDICES After Page

1. SAMPLE ANALYSES - MMI-M 20 2. IP FIELD DATA 21

FIGURES After Page

1. LOCATION MAP 3 2. CLAIM MAP 4 3. REGIONAL GEOLOGY MAP 6 4. SAMPLE GRID LOCATION MAP 8 5. GEOCHEMISTRY AND GEOPHYSICAL MAP

CHU AND PG GRIDS 9 6. GEOCHEMISTRY

PORPHYRY GRID 10

2

SUMMARY

During the period August 16 - September 3, 2006 a fieldwork program was conducted over several areas of the adjacent Chu molybdenum (copper, tungsten) and the Porphyry (copper-gold) properties situated in the Omineca Mining Region in central British Columbia, Canada. The project area occurs about 125 km. by road south of the Town of Vanderhoof, B.C. The program included rock exposure mapping, mobile metal ion (MMI) soil sampling and proprietary digestion over three separate areas and a single line induced polarization (IP) survey over a coincident MMI soil sample line. The fieldwork was conducted over separate portions of the two properties that may tie-in with a quartz stockwork system or the same one underlying both properties. To date the emphasis of exploration work has been on the large zone of molybdenum mineralization that appears to be mainly contained within a hornfelsed, fine grain sized meta-siltstone unit. This unit is in places found to be highly fractured and welded with quartz stringers that are part of a large, well developed quartz stockwork which hosts the major molybdenum (Chu) and less well documented copper-gold (Porphyry) zone. This hornfels stockwork zone strikes NW-SE and dips toward the NE. The Porphyry zone is also hosted in a metamorphosed sediment that has been hornfelsed.

The current recognized size of the zone of molybdenum mineralization, while not satisfying the requirement of the technical standards required by NI 43-101 reveals certain approximate dimensions of a zone of possible mineralization of the size of 800 m. X 200 m. X 200 m., (apparent strike length X apparent width X apparent depth), respectively. The results obtained to date from all of the fieldwork conducted are encouraging and the writer recognizes that further exploration work should be carried-out on the property. The hornfels quartz stockwork molybdenite and copper-gold zones are open in a number of directions, along the strike toward both the NW and SE, downdip and across the apparent width particularly toward the SW. The recommended separate two phase work programs are mainly as diamond core drilling and related analytical studies.

3

* u K 0 i\, T c R R T C R Y

PROPERTY LOCATION

,Zo^S\

yCpLDMO

OMEGA EXPLORATION SERVICES INC.

CHU MOLYBDENUM PROJECT

LOCATION MAP N.T.S. 9 3 F - 7 E OMINECA M.D.,B.C

•50 3 0 0 450 KM. 1

SCALE: 1 = 7,500,000 DRAWN BY: J . M .

DATE: DEC. 2 0 0 6 FIGURE N9. |

C M O N G

INTRODUCTION

The current fieldwork programs were conducted by the author and consists of three separate areas all undergoing initial mobile metal ion (MMI) sampling and proprietary digestion prior to ICP (MMI-M) analyses. In addition one area underwent a single line IP survey coincident with a portion of the MMI sampling.

The work program was conducted on behalf of Omega Exploration Services Inc. of Delta, British Columbia, Canada.

LOCATION AND ACCESS

The property areas may be located on NTS map sheet, 93F/7E at latitude 53° 21' north and longitude 124° 37' west. They are situated approximately 80 air-kilometres south of the Town of Vanderhoof, B.C., at the southeast end of the Nechako Range. The properties lie within the Omineca Mining Region, British Columbia, Canada.

Access to the property is gained by traveling 26.5 km. southwest of the Town of Vanderhoof, B.C. on the Kenney Dam road and then southerly for about 100 km. on the Kluskus-Ootsa road. This major logging haul-road can be described as a wide, good all weather, gravel surfaced logging road.

Just north of the cutoff to Chutanli Lake at 98.5 km., the Kluskus-Ootsa road branches off to the west from the south trending Blue road. At 106 km. on the Kluskus-Ootsa, the main Chu property road to the north is accessed. A number of other gravel roads traverse much of the claim area.

TOPOGRAPHICAL AND PHYSICAL ENVIRONMENT

The property lies within the intermontane (physiographic) belt of the Interior Plateau. This regional area lies between the Coast mountains on the west and the Columbia mountains on the east. More particularly the Chu property is found to occur in the transition zone on the south end of what is called the Nechako range between the northwesterly trending Nechako and Fraser plateaux. The claim area generally is

4

r

~\

L E G E N D

Logging rood

Creek , lake

/ S ESS 10..' ■■ « ° / \ V ^ 'PR0WNC8 V

OF

OMEGA EXPLORATION SERVICES iNC.

CHU MOLYBDENUM PROJECT

CLAIM MAP NTS. 93F-7E

O 2

OMINECA M.D.,B.C. 6 KM.

SCALE : I--100,000 DRAWN BY: J.M.

DATE: DEC. 2006 FIGURE N?. 2

CHONG

fluvial-glacial covered, rounded mountainous terrain and the general area reflects many glacial effects, in particular extensive drumlin (moraine) features. The claim area ranges in elevation from approximately 1,150 metres (3,450') to 1,430 metres (4,700') mean sea level. The area is conifer covered with lodgepole pine and spruce. Much of the claim and general area has undergone extensive clearcut logging of the coniferous forest cover to try and salvage some goodness from the widespread and massive insect, pine beetle infestation. The general area lies within the sub-alpine biotic zone and experiences greater than 100 cm. of precipitation annually, of which 15%-25% may occur as a snow equivalent i.e. about 20 cm. The summers are generally mild with moderate precipitation and the winters can be very cold, but usually not for extended periods. The area historically reveals a cyclic repetition of hot and cold periods.

PROPERTY AND OWNERSHIP

The property summarized in this report is comprised of 11 contiguous lode mineral claims. The claim particulars are listed as follows:

Name Tenure No.

390574

Hectares

500

Anniversarv Date

Chu

Tenure No.

390574

Hectares

500 October 15 Chul 390575 400 October 15 Chu 2 390576 400 October 15 N/N 507782 695 October 15 N/N 507793 193 February 24 Porphyry#l 527382 482 February 10 Au#l 533567 483 May 4 N/N 533568 482 May 4 N/N 533569 193 May 4 N/N 533570 77 May 4 ChuFr 537381 77 July 18

Total 3,982 *N/N - No claim name

The claim area totals approximately 3,982 hectares or 9,840 acres.

5

The above listed lode mineral claims are owned by Omega Exploration Services Inc. of Delta, Guy Delorme of Vernon and Jacqueline McLeod of Delta, British Columbia, Canada.

HISTORY

The recorded mining exploration history of the property area dates from 1969 when a helicopter supported prospecting and regional reconnaissance geochemical silt survey program indicated the anomalous copper, molybdenum and tungsten values in the area.

Apparently, coincident reconnaissance silt surveys were conducted by Rio Tinto Canadian Explorations Ltd. and Asarco (American Smelting and Refining Company) during 1969-70 led to a joint discovery of what is now known as the Chu molybdenum property.

During this early period, both companies undertook some shallow diamond core drilling. The author, during a fleldwork program he was conducting in 2003 located the remains of some of the drill core from Rio Tinto's 1969-70 diamond drilling program.

The construction of the Kluskus-Ootsa logging road in the 1970's saw Asarco consolidate the project areas and carry-out a number of geological, geochemical, geophysical surveys and some shallow diamond core drilling. They were joined by Armco Mineral Exploration Ltd. in a joint venture in 1979 which Armco managed. They conducted core drilling programs in 1980: DDH 1-3,1981: DDH 1-7 and 1982: DDH 1-2. This rather extensive fleldwork has partially outlined a large northwest-southeast trending zone of strong molybdenum-bearing mineralization in a hornfels quartz stockwork.

REGIONAL GEOLOGY

The oldest rocks in the general area are volcanics and sediments which have been assigned to the Hazelton Group of Jurassic age. These rocks in places have been intruded by late Jurassic and early Cretaceous aged Coast Range plutonic rocks of granitic to dioritic composition, which are referred to in the property area as the Nechako intrusions. More than one period of intrusive activity appears to have affected the area.

6

1—I Pcieocene. Eocene, Oligoc / / j Rhyolite, dccite, tuffs, br

Upper Jurassic qoti/frr/Cre?oceous Grani te, quartz diorite f/granodior{

1 Middle Jurassic Greywocke, argitiite,conglomerpitfjtuff, et-ol- - _

Andesite, tuffs,breccias, cahglomerotes' shale, sondsfone «

^ ^ 5 ' d i r e c t i o n of g lac ia l transport

"iHe? GSC »--ehr-M^cTf Mop 5'


CHU MOLYBDENUM PROJECT REGIONAL GBOLDGY

NTS. 93F-7E*. OM1NECA M.D..B.C. s5 KM

- - ; ; ■ ; ■ ■ — ; - l

SCALE 1-250.000 DRAWN 8Y J. M.

DATE DEC,. 200 6 FIGURE N? 3

Some intrusive rocks observed in the general area appear to be younger than the Nechako intrusions and may be more alkalic in composition. These rock units appear to have in some places a close proximity to the stronger MoS2 mineralized zones. The youngest rocks observed in the area are the andesite to basalt flow volcanics which are thought to be of Oligocene age. The host rocks of the mineral zone which is the focus of historical attention, the hornfelsed quartz stockwork is considered to be mainly contained within Hazelton Group rocks although this does not preclude a younger age of mineralization.

LOCAL GEOLOGY

The different rock units are found to occur as northwesterly striking and northeasterly dipping sediments and volcanics. The oldest underlying bedded rocks are found to occur in the central area of the property as hornfelsed siltstone, mudstone and quartzite and (conformably?) overlain on the northeast side by dipping clastic andesitic tuffs. These units appear to trend through the property in a northwest-southeast direction. The bedded sediments and volcanics are intrusive contacted with granitic rocks thought to be Coast Range intrusions of Jurassic age. The mineral host units appear to occur as a large package of older rocks that may represent a roof pendant lying on the intruding granodiorite and being cut in places by the still younger alkalic (dyke) rocks.

The molybdenum mineralization is related to a quartz vein stockwork that is best developed in the hornfelsed (siltstones) that have undergone varying degrees of biotitization following structural preparation (brittle fracturing) and subsequent quartz-welding. Pyrite and pyrrhotite are found widespread throughout the molybdenite (MoS2) mineralized zones and the core in general. The iron minerals on contacts of the hornfels unit appear to have undergone moderately strong oxidation. Local concentrations of minor chalcopyrite and scheelite appear to offer the copper and tungsten values observed. The overall trend of the molybdenum mineralized zone appears to dip toward the northeast. The contact on the northeast side of the hornfels host appears to be with the northwest trending Hazelton Group andesites. The contact of the same zone of mineralization on the southwest side of the hornfels is with Coast range intrusive units, i.e. granodiorite.

7

The copper-gold (Porphyry) zone appears to have undergone some silicification and a stronger contact metamorphic effect than the molybdenum zone that may be explained by its closer proximity to the igneous contact.

PRESENT WORK PROGRAM

The present fieldwork program was undertaken during the period August 16 - September 3, 2006. Rehabilitating 1.1 km. of the original baseline (reference line) on the eastside of the L0+00 gridline to allow orientation of the new MMI sample line along L7+75S from 8+50E -13+50E, samples C1-C18. The second MMI sampling line was conducted within the area currently occupied by the Porphyry #1 mineral claim, samples P1-P17. This was formerly a Granges Exploration project, April mineral claim in 1981 and later a Placer Development project on the former CH mineral claim in 1992 and by Orvana Resources Corp. in 1995-98 on the CH mineral claims. The third area to undergo exploration during the current program was on the southside of the Porphyry #1 mineral claim and on the southside of the Kluskus-Ootsa road where a single-line IP line was conducted. A coincident MMI soil sample line was undertaken in this area, samples PG1-PG7. For MMI sample results see Appendix 1. A total of 3,400 m. of MMI sampling line was installed with a total of 42 samples taken. 210 m. of IP surveying was completed over the PG sample grid that was a total of 650 m. in length using a Hewitt 200, time domain pulse system, serial no. 250.

The IP survey was conducted as a pole-dipole array with the Cl, current electrode considered to be at infinity (oo) and the C2, moving current electrode was at (n x "a" where "a" = 30 m) and (n x "a" where "a" = 60 m.) station interval. A symmetric array where n is a whole number of from 1-6 and "a" = the station interval between PI and P2. The IP survey was conducted using a pulse-type Hewitt, HEW Prospector 200 model, serial no. 250.

Forty-two MMI soil samples were taken from the 20 cm. - 25 cm. depth horizon, that is measured from the bottom of organic layer (ground cover, humus and the bottom of the organic matter layer. An area

8

roughly 0.5 metre2 is cleaned off and a vertical face is dug through the surface cover of, moss, needles, lichen, and organic matter of any significance. The type and thickness of this zone is recorded. The vertical face is deepened through the soil zone below the organic layer. The author tries to achieve an approximately 30 cm. vertical soil horizon. The soils in the property area can generally be described as podzols which have developed under coniferous cover. The soil texture and type of horizon, i.e. "A" (often a greyish, bleached) horizon, sometimes followed by a "B" (often a rusty, oxidized and sometimes enriched) horizon. The interval to be sampled in this soil section ranging from 20 cm. - 25 cm. in vertical depth is sampled with a plastic scoop and the soil is put through a plastic sieve with openings of 0.635 cm (1/4") and the undersized is caught in a plastic (gold) pan. Note the use of plastic tools because they are thought to be essentially chemically benign and of course the need of thorough cleaning of the collection tools between each sample. The 0.84 - 1.84 kilogram samples were bagged in marked 30 cm. x 50 cm. polyethylene sample bag. The samples were taken to ALS Chemex laboratory in North Vancouver, B.C. where they are registered using our project name and sample numbers and then sent by air to Australia for proprietary digestion and subsequent induction coupled plasma (ICP) analyses. The author chose the MMI-M (multi-element + gold) package. These samples were taken, where possible, over the surface projection of the IP zone of high chargeability.

CONCLUSIONS

The results from the MMI soil sampling surveys exhibit some apparently anomalous features keeping in mind the small sample populations, for example if sample results from all three grids are used it totals 42 samples whose results seem to generally fit, i.e. standard deviation and frequency distribution curves. There appears to be two different populations, i.e. Cl-18 and P 1-17 with the PG 1-7 sort of crossing the larger populations. The Chu project is generally known as a base metal property, i.e. molybdenum, copper and tungsten. The current MMI sampling program conducted along the Chu Grid, samples C-l through C-18 (see Figure 4 and Appendix 1) return values that may be anomalous in the following:

9

PG GRID NIP Reodings

30m. interval 60m interval

35 -■40

--60

Sample locations

^ Silver ) l8ppb

& Arsenic >75ppb

0 Cobalt )84 ppb

(& Zinc >525ppb

Scale 1=2500 SO Metres

y ^ E S S I O ^

CHU GRID Sample ocations

e Cobalt > 225 ppb

e Copper >625 ppb

$ Zinc >525 ppb

$ Molybdenum > 120 ppb

Scale 1=5000 0 50 100 Metres

^ Y ^ *


CHU PROJECT GEOCHEMISTRY a GEOPHYSIC

CHU a PG GRIDS N.T.S. 9 3 F / 7 KLUSKUS-CXDTSA AREA, B.C.

SCALE : AS SHOWN DATE' DEC. 2006 DRAWN BY-" J .M. FIGURE' 5

Note: the MMI-M sample data has in a large part been treated with conventional statistical techniques for determining standard deviation and frequency distribution. These suites are: Gold Exploration (GES) composed of Gold (Au), Silver (Ag), Palladium (Pd), Cobalt (Co) and Nickel (Ni); Base Metal (BMS) composed of Copper (Cu), Cadmium (Cd), Lead (Pb) and Zinc (Zn); Porphyry Pathfinder (PPS) composed of Arsenic (As), Mercury (Hg)*, Antimony (Sb), Molybdenum (Mo), Selenium (Se) * and Iron (Fe) and the Granophiles, Pegmatite (GPS) composed of Uranium (U), Thorium (Th), Lead (Pb), Tantalum (Ta)*, Tin (Sn) and Tungsten (W). The * denotes elements not reported in our MMI-M analyses package.

The elements used in some of this testing are not normally available using conventional digestion and detection methods. It has been found that certain other elements group together and may have usefulness as pathfinder components. These elements normally reported by MMI digestion and induction coupled plasma (ICP) detection are at times observed to share a similar position in the periodic table and some appear to fit well with respective pathfinder element suites. An example might be the GES and the minor and even still rarer elements Cesium (Cs), Lanthanum (La), Lithium (Li), Niobium (Nb), Neodynium (Nd), Praseodymium (Pr), Scandium (Sc), Samarium (Sm), Terbium (Tb), Tellurium (Te), Yttrium (Y), Yetterbium (Yb) and Zirconium (Zr) (see Appendix 1).

It remains to be determined what the significance is, if any is revealed in this data. On the main MoS2 zone to the northwest of the Chu Grid occurrences of an alkalic dyke trending northeast and cutting the main northwest mineralization trend is observed in a number of places that appear to be related to occurrences of stronger MoS2 mineralization. These dykes may have considerable impact on the location of the main zone of mineralization. At the Chu Grid (C-l to C-18) the indicated zone of MMI anomalies could well be surface features reflecting underlying NE-SW dykes possibly responsible for the mineralizing fluids. These zones need further testing. On this property the author has observed northeast trending dyke-like features in close proximity to zones of known Mos2 mineralized drill intersections. These features appear from hand specimen examination to be a medium grained, grayish coloured crystalline alkalic rock. These features may be

10

Sample locations

$ Gold >l.8 ppb

( £ Copper ) 625 ppb

0 Zinc )525 ppb

0 Arsenic >7.5ppb


CHU PROJECT GEOCHEMISTRY

PORPHYRY GRID N.T.S.93F/7 KLUSKUS-OOTSA AREA,B.C.

200 400 i—

600 Metres

SCALE1 1:10,000 DRAWN 8Y= J . M .

DATE: DEC. 2006 FIGURE

offering or intimately associated with the mineralized zones and may be detected in covered areas by using the MMI method of sampling, digestion and detection. All three sampled areas contain anomalous appearing zones with some differences. One zone, the PG Grid area also underwent a partially coincident, single line induced polarization survey over 210 metres of line that may cross the southern extension of the Porphyry Gold if it exists.

The thresholds for the various elements are listed as follows where it seemed meaningful to calculate them:

Chu Grid

Element Background Anomalous Highly Anomalous

Silver (Ag) 0 - 18 ppb >18 - 21 >21 - 30+

Gold (Au) 0 - 0.3 ppb >0.3 - 0.4 >0.4 - 0.7+

Palladium (Pd) 0 - 4.5 ppb >4.5 - 6.0 >6,0 - 10.5+

Cobalt (Co) 0 - 225 ppb >225 - 375 >375 - 600+

Nickel (Ni) 0 - 150 ppb >150 - 200 >200 - 300+

Copper (Cu) 0 - 625 ppb >625 - 1000 >1000 - 2250+

Cadmium (Cd) 0 - 30 ppb >30 - 40 >40 - 60+

Lead (Pb) 0 - 45 ppb >45 - 150 >150 - 300+

Zinc (Zn) 0 - 525 ppb >525 - 875

Arsenic (As) 0 - 7.5 ppb >7.5 - 12.5

Iron (Fe) 0 - 120 ppm >120 - 180 Molybdenum (Mo) 0 - 120 ppb >120 - 240

>875 -1390+

>12.5 - 22.5+

>180 - 240+

>240 - 480+

n

PorDhvrv Grid

Element Background Anomalous Highly Anomalous

Silver 0 -150 ppb >150 - 300 >300 - 527+

Gold 0 -1.8 ppb >1.8 - 4.2 >4.2 - 9.1+

Palladium 0 -15 ppb >15 - 25 >25 - 32.9+

Cobalt 0 - 84 ppb > 84 -144 > 144 - 217+

Nickel 0 - 150 ppb > 150 - 250 >250 - 550+

Copper 0 - 625 ppb >625 - 1000 >1000 - 8240+

Cadmium 0 - 30 ppb >30 - 40 >40 - 60+

Lead 0 - 45 ppb >45 - 150 >150-7110+

Zinc 0 - 525 ppb >525 - 875 >875 - 2580+

Arsenic 0 - 7.5 ppb >7.5 - 12.5 >12.5 - 54+

Molybdenum 0-20 ppb >20 - 27 >27 - 131+

Antimony (Sb) 0 - 12 ppb >12 - 20 >20 - 48+

Examination of the geochemical data from the three grid areas suggests the possibility of a number of other potential pathfinder elements, but since the data set is so small it precludes making conclusions until a larger population of MMI analyses from the immediate area are available.

The IP survey results when considered alone are apparently high chargeabilities and low to moderate resistivities. When the one line results of IP and coincident MMI are examined some coincident features are displayed. This possible copper-gold southern extension

12

zone may exhibit coincident IP and GES - BMS geochemical values. Only further work in these areas will validate this exploration method. Ultimately only drilling will able to thoroughly check these anomalies.

RECOMMENDATIONS

Further diamond core drilling and analytical work is recommended to be undertaken on both the Chu and the Porphyry projects. The project area should undergo additional MMI testing and some coincident IP reconnaissance lines.

COST ESTIMATE

The writer has developed the following two program, i.e. Chu and Porphyry as two phase work programs are displayed separately and each is provided a separate two phase cost estimate:

Chu Project Cost Estimate

Phase 1

Diamond core drilling 1,525 metres, all inclusive i.e. core boxes, bulldozer, etc. @ $85/metre, except for mob. and demob.

Geology, supervision, core logging, sample preparation, transport to the assayers

Assistant

Transportation

Camp and board

Assaying and analyses

Reclamation bond

$ 129,625

10,000

5,000

5,000

51,500

15,000

10,000

13

Reports, maps and filings 4,500

Contingency 18,000

Sub-total $ 248,625

Phase 2

Diamond core drilling, 4,500 metres, all inclusive

@ $85/metre $ 382,500

Geology and supervision 15,000

Assistant 8,000

Transportation 15,000

Camp and Board 125,000

Assaying and Analyses 30,000


Contingency 47,000

Sub-total $642,500

Total $891,125

Porphyry Project Cost Estimate

Phase 1

Diamond core drilling 750 metres, all inclusive i.e. core boxes, bulldozer, etc. @ $85/metre, except for mob. and demob. $ 67,750

14

Geology, supervision, core logging, sample

preparation, transport to the assayers 5,000

Assistant 2,500


Camp and board 24,500

Assaying and analyses 7,000

Reclamation bond 10,000


Contingency 11,000

Sub-total $ 133,250

Phase 2

Diamond core drilling, 4,500 metres, all inclusive

@ $85/metre $ 382,500

Geology and supervision 8,000

Assistant 4,000


Camp and Board 52,000

15

Assaying and Analyses 15,000


Contingency 20,000

Sub-total $498,500

Total $631,750

16

STATEMENT OF COSTS

Grid line installation, mapping, MMI sampling and

IP survey: J. W. McLeod, P. Geo. $ 8,350

Assistants, J.A. McLeod and S.C. McLeod 4,500

Camp and board, 60 mandays 2,100

Transportation, 4x4 rental and mileage 2,100

Equipment rental: 4 Trac, IP unit, MMI sampling

supplies, chainsaws and tools 800

MMI analyses 1,560

Report, maps and filing 1,200

Total $ 20,610

17

CERTIFICATE

I, James Wayne McLeod, of the Municipality of Delta, Province of British Columbia, hereby certify as follows:

I am a Consulting Geologist with an office at 5382 Aspen Way, Delta, B.C.,V4K3S3.

I am a Professional Geoscientist registered in the Province of British Columbia and a Fellow of the Geological Association of Canada.

I graduated with a degree of Bachelor of Science, Major Geology from the University of British Columbia in 1969.

I have practiced my profession since 1969.

I have a direct interest in the Chu molybdenum property and I have an indirect interest in the Porphyry copper-gold property because of the ownership of the Porphyry #1 mineral claim by my wife, Jacqueline A. McLeod.

The above report is based on personal field experience gained by the writer during the period 2001-06.1 have also conducted considerable research, both private and public on the Chu and Porphyry properties and discussed these properties in detail with knowledgeable parties.

DATED at Delta, Province of British Columbia this 2nd day of January, 2007.

18

REFERENCES

British Columbia Ministry of Energy, Mines and Petroleum Resources Assessment Reports - 8476 and 9691.

McLeod, J.W., January 7,2002-03. Magnetometer Survey Reports on the Chua Chua Claim for Chris Delorme.

Milsom, John, 1989. Field Geophysics. Geological Society of London Handbook. Open University Press, Halsted Press (a division of John Wiley Inc.)

Ostensoe, E.A., 1980-82. Private Chu Project, Progress Reports to Armco Mineral Exploration Ltd.

Ostensoe, E.A., February 15,2002. Private Chu Property Report for Javelin Capital Corp.

Vinogradov, A.P., 1959. The Geochemistry of Rare and Dispersed Chemical Elements in Soils. Consultants Bureau, Inc., New York, 2nd Edition.

19

Appendix 1

Sample Analyses MMI-M

20

To: MCLEOD, JIM ) Page: 2 - A 5382 ASPEN WAY Tota... r»ages: 2 (A - C) DELTA BC V4K 3S3 Finalized Date: 8-NOV-2006

Account: MCLJIM

Project: CHU ' I

CERTIFICATE OF ANALYSIS VA06092687

M»thod Analyte

Units Sample Descr ip t ion LOR

WEI-21 ME-MS18 ME-MS18 ME-MS18 ME-MS18 ME-MS18 ME-MS18 ME-MS18 ME-MS1B ME-MS18 ME-MS18 ME-MS18 ME-MS18 ME-MS18 ME-MS18 RecvdWt. Ag As Au Ba Bi Ca Cd Ce Co Cr Cu Er Fe Gd

kg ppb ppb ppb ppb ppb ppm ppb ppb ppb ppb ppb ppb ppm ppb 0.02 0.1 1 0.1 10 3 0.2 1 0.1 0.3 1 10 0.1 0.1 0.1

C-1 C-2 C-3 C-4 C-5

1.22 9.5 4 <0.1 990 3 22.2 4 99.2 172.5 25 280 4.2 112.0 7.9 1.02 18.5 3 0.2 490 <3 5.6 7 36.4 197.5 14 340 4.8 99.1 5.0 1.32 12.4 5 0.1 780 <3 31.1 10 71.0 107.0 29 440 6.2 96.0 10.0 1.58 16.3 5 0.1 530 3 26.8 8 91.7 148.5 34 480 4.4 118.5 8.1 1.62 6.9 3 0.1 630 <3 267 19 68.6 138.5 32 610 17.9 92.9 23.9

C-6 C-7 C-8 C-9 C-10

2.90 14.1 18 0.7 1240 7 257 13 165.0 111.5 125 1080 16.5 220 34.1 1.40 22.6 3 0.1 720 <3 657 29 7.4 35.3 2 630 11.7 15.3 18.3 1.26 26.8 5 0.1 1030 <3 506 17 26.1 32.3 . 16 290 3.3 39.2 7.8 1.02 17.8 4 0.2 280 <3 821 60 <0.1 559 <1 2040 7.1 8.2 11.0 1.16 11.2 6 0.1 1020 <3 22.8 4 79.7 139.5 42 220 5.3 113.5 9.3

C-11 C-12 C-13 C-14 C-15

1.10 3.7 11 <0.1 740 <3 96.1 3 55.5 251 37 320 5.0 181.0 7.0 0.92 6.2 7 0.1 390 <3 30.2 19 12.7 350 4 250 3.8 114.0 1.9 0.96 2.7 4 <0.1 620 <3 52.7 10 34.5 148.0 9 350 4.8 68.4 5.2 1.02 2.1 3 <0.1 410 <3 28.6 28 0.9 236 <1 410 3.8 55.5 0.4 0.98 5.0 4 0.6 3200 <3 29.0 46 4.7 199.0 <1 840 8.0 50.0 1.3

C-16 C-17 C-18

1.00 1.0 4 0.3 450 <3 10.9 1 3.4 56.6 <1 610 2.9 126.5 2.9 0.90 0.9 4 <0.1 740 <3 24.8 1 5.1 75.6 4 110 1.8 167.0 0.7 0.94 9.1 11 0.1 710 <3 24.0 2 41.4 107.5 12 330 3.1 100.5 5.1

( A L S )

ALS Chemex EXCELLENCE IN ANALYTICAL CHEMISTRY ALS Canada Ltd.

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212 Brooksbank Avenue North Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 WWW.alschemex.com

"o: MCLEOD, JIM

5382 ASPEN WAY

DELTA BC V4K 3S3

Project: CHU

Page: 2 - B

Total rr r»ages: 2 (A - C)

Finalized Date: 8-NOV-2006

Account: MCLJIM

f CERTIFICATE OF ANALYSIS VA06092687

Method Analyta

Units Sample Description LOR

ME-MS18 ME-MS18 ME-MS18 ME-MS18 ME-MS18 ME-MS18 ME-MS18 ME-MS18 ME-MS18 ME-MS18 ME-MS18 ME-MS18 ME-MS18 ME-MS18 ME-MS18 La Li Mg Mn Mo Nb Nd Ni Pb Pd Pr Rb Sb Sc Sm ppb ppb ppm ppm ppb ppb ppb ppb ppb ppb ppb ppb ppb ppb ppb 0.1 0.2 0.01 0.01 5 0.1 0.1 3 10 0.1 0.1 5 1 3 0.1

C-1 C-2 C-3 C-4 C-5

54.7 1.8 4.86 2.49 12 1.7 37.2 80 30 4.2 11.1 264 <1 29 6.5 18.5 0.7 1.27 1.90 9 0.9 17.3 50 30 2.8 5.1 274 <1 22 3.5 36.0 0.5 1.81 2.42 15 0.7 35.0 56 30 4.4 9.3 216 <1 33 7.8 49.8 0.9 <0.01 0.95 26 1.1 37.6 75 30 4.5 11.2 192 <1 27 6.8 37.1 7.5 48.0 3.40 146 0.4 62.3 158 30 4.7 13.8 47 <1 25 16.7

C-6 C-7 C-8 C-9 C-10

81.6 13.7 19.75 4.05 462 3.2 107.0 276 20 10.3 24.4 37 1 34 25.8 8.3 5.3 19.75 6.51 22 <0.1 24.5 200 10 5.2 4.6 37 <1 8 9.9 15.2 18.7 13.35 0.44 6 1.3 20.9 107 20 5.8 5.0 63 <1 14 5.3 <0.1 4.9 18.30 2.06 19 <0.1 5.7 200 10 5.5 1.1 23 <1 6 3.9 40.1 3.4 2.40 0.97 10 1.7 39.9 154 50 4.8 10.5 211 <1 19 8.3

C-11 C-12 C-13 C-14 C-15

23.4 12.4 12.70 1.13 17 2.8 23.9 81 50 4.7 6.6 118 <1 37 5.0 6.1 1.8 5.59 0.30 <5 0.4 6.0 68 70 2.7 2.1 108 <1 18 0.9 17.4 0.8 7.74 1.18 7 0.1 18.0 82 80 3.4 5.0 136 <1 14 3.9 0.4 0.5 2.87 0.33 <5 <0.1 *0.1 11 60 1.2 0.5 156 <1 10 <0.1 2.4 0.3 4.16 0.84 <5 <0.1 2.0 74 300 1.5 1.1 185 <1 18 <0.1

C-16 C-17 C-18

0.7 0.7 0.91 0.41 <5 <0.1 4.5 8 <10 1.7 1.3 127 <1 31 1.9 2.6 2.6 3.46 0.14 <5 0.3 1.6 20 10 2.1 1.1 177 <1 12 <0.1 22.0 1.5 <0.01 0.43 12 0.5 18.4 51 50 3.9 5.3 69 <1 15 3.6

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A ALS Chemex EXCELLENCE IN ANALYTICAL CHEMISTRY ALS Canada Ltd. 212 Brooksbank Avenue North Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 WWW.alschemex.com

ro: MCLEOD, JIM 5382 ASPEN WAY DELTA BC V4K 3S3

Project: CHU

) Page: 2 - C Totai.. r»ages: 2 (A - C)

Finalized Date: 8-NOV-2006 Account: MCLJIM

1 CERTIFICATE OF ANALYSIS VA06092687 Method Analyta Units

Sample Descr ip t ion LOR

ME-MS18 ME-MS18 ME-MS18 ME-MS 18 ME-MS18 ME-MS18 ME-MS18 ME-MS18 ME-MS18 ME-MS18 ME-MS18 ME-MS18 ME-MS18 Sn Sr Tb Te Th Ti Tl U W Y Yb Zn Zr ppb ppb ppb ppb ppb ppb ppb ppb ppb ppb ppb ppb ppb 0.2 10 0.1 1 1 10 10 1 0.2 0.1 0.1 20 1

C-1 C-2 C-3 C-4 C-5

0.5 280 1.1 <1 13 1180 <10 6 11.6 35.8 3.6 190 21 0.2 90 0.8 <1 6 560 <10 4 5.7 33.7 4.5 330 13 0.2 230 1.7 <1 17 410 <10 9 15.1 47.1 4.9 320 30 0.4 250 1.2 <1 13 830 <10 5 17.3 32.6 3.6 230 26 0.2 1730 4.3 <1 12 500 <10 30 2.6 143.0 13.7 100 15

C-6 C-7 C-8 C-9 C-10

0.9 1050 5.2 1 38 2590 <10 35 26.6 151.5 12.9 230 64 <0.2 1220 3.1 <1 3 150 <10 13 0.6 87.5 8.9 50 5 0.3 910 1.1 <1 6 1000 <10 6 1.4 29.3 2.4 90 15 <0.2 1790 1.8 <1 2 20 <10 5 0.2 67.3 4.8 780 1 0.2 310 1.4 <1 10 710 <10 4 1.6 40.1 4.5 30 37

C-11 C-12 C-13 C-14 C-15

0.8 610 1.1 <1 10 2110 <10 6 3.5 33.2 4.1 170 38 0.2 320 0.3 <1 4 600 <10 2 0.5 21.8 3.3 1060 20 <0.2 450 0.9 <1 6 230 <10 3 0.7 34.0 3.6 310 19 <0.2 380 <0.1 <1 <1 140 <10 <1 <0.2 17.9 3.4 500 3 <0.2 470 0.3 <1 2 90 <10 2 0.4 37.2 7.1 1390 8

C-16 C-17 C-18

<0.2 120 0.5 <1 3 60 <10 3 0.2 14.5 4.6 20 17 0.2 400 <0.1 <1 1 500 <10 1 1.2 7.8 2.5 20 18 0.2 300 0.8 <1 6 560 <10 2 3.0 30.8 2.2 40 28


^ L S )



"o: MCLEOD, JIM 5382 ASPEN WAY DELTA BC V4K 3S3

^ Page: 2 - A Total tt Pages: 2 (A-C)


CERTIFICATE OF ANALYSIS VA06092686 3 Method Analyta


WEI-21 Recvd Wt.

kg 0.02

ME-MS18 Ag ppb 0.1

ME-MS18 As PPb

1

MEMS 18 Au ppb 0.1

ME-MS18 Ba ppb 10

ME-MS18 Bi

ppb 3

ME-MS18 Ca

ppm 0.2

ME-MS18 Cd ppb

1

ME-MS18 Co PPb 0.1

ME-MS1E Co ppb 0.3

ME-MS18 Cr

ppb 1

ME-MS18 Cu ppb 10

ME-MS18 Er

ppb 0.1

ME-MS18 Fe

ppm 0.1

ME-MS18 Gd PPb 0.1

P#1 P#2 P#3 P#4 P#5

1.28 1.42 1.32 1.26 1.58

332 292

169.5 527 478

10 26 12 54 21

9.1 3.2 1.0 2.4 3.4

5980 3700 5520 4100 3860

<3 3 <3 <3 <3

421 281 219 101.5 108.0

25 61 12 20 15

97.3 31.4 84.7 274 203

30.1 60.0 56.0 180.5 54.9

51 40 36 89 28

1300 2390 1540 8240 4390

60.1 4.8 5.2 12.9 11.1

22.1 39.7 39.2 84.9 29.3

75.6 8.7 13.1 31.3 26.9

P#6 P#7 P#8 P#9 P#10

1.52 1.70 1.50 1.84 1.32

73.8 21.9 42.0 32.4 15.6

0,9 0.4 1.4 0.5 0.9

2450 1570 1070 1210 3240

<3 <3 6 5 3

637 509 96.3 234 206

11 4 4 14 2

13.3 13.1 89.7 83.8 68.8

62.8 94.7 73.1 59.8 44.7

4 7 35 27 31

2330 690 350 290 740

5.4 2.6 10.6 18.1 7.2

6.3 13.3 41.9 52.7 25.8

10.8 4.9 18.3 28.0 14.4

P#11 P#12 P#13 P#14 P#15

1.48 1.82 1.20 1.44 1.86

21.9 39.7 19.2 22.6 40.1

1.1 0.4 0.2 0.3 0.6

770 3180 1160 1760 920

3 3 <3 <3 <3

77.5 196.0 121.0 250 228

12 5 23 13 15

121.0 66.6 84.6 85.4 70.1

145.5 47.9 217 60.8 41.0

5 21 43 30 13

500 480 280 290 250

19.5 6.2 10.2 15.5 5.7

51.6 42.9 131.5 64.5 50.9

31.0 13.4 14.8 26.5 12.3

P#16 P#17

1.58 1.46

32.7 20.9

0.8 0.3

940 900

<3 <3

246 205

13 5

29.5 101.5

89.0 26.8

27 31

170 130

3.8 6.1

47.2 26.5

6.9 13.0


(TKISS)


212 Brooksbank Avenue North Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 WWW.a lschemex.com

o: MCLEOD, JIM 5382 ASPEN WAY DELTA BC V4K 3S3

Page: 2 - B Total » Pages: 2 (A-C)



Sample Description

Method Analyt*

Units LOR

ME-MS18 La

ppb 0.1

ME-MS18 Li

ppb 0.2

ME-MS1B Mg

ppm 0.01

ME-MS18 Mn

ppm 0.01

ME-MS18 Mo ppb

5

ME-MS18 Nb ppb 0.1

ME-MS18 Nd ppb 0.1

ME-MS18 Ni

ppb 3

ME-MS18 Pb ppb 10

ME-MS18 Pd ppb 0.1

ME-MS18 Pr

ppb 0.1

ME-MS18 Rb ppb

5

ME-MS18 Sb ppb

1

ME-MS18 Sc ppb

3

ME-MS18 Sm ppb 0.1

P#1 P#2 P#3 P#4 P#5

58.1 21.1 49.0 107.0 89.6

0.6 5.0 1.3 4.2 1.0

35.4 24.9 31.3 11.55 4.24

6.67 3.38 0.70 5.54 1.99

<5 36 13 65 66

1.8 2.3 2.5 3.8 2.2

113.0 22.6 47.9 103.5 88.4

294 295 148 528 178

430 3700 1930 7110 3320

8.6 9.4 13.3 32.9 32.9

22.5 6.8 13.5 27.4 22.8

81 255 164 154 179

1 48 4 29 10

90 19 15 46 38

44.0 5.9 10.9 25.3 22.6

P#6 P#7 P#8 P#9 P#10

5.4 5.6 30.5 43.5 30.6

2.2 1.9 0.5 0.8 0.3

61.7 73.8 7.38 17.35 27.3

2.21 5.38 0.84 2.74 1.01

131 28 7 <5 <5

0.7 0.6 1.8 1.4 0.9

16.6 9.9 51.3 70.9 41.1

202 152 36 108 43

20 10 60 210 30

22.5 13.0 9.5 6.4 7.3

3.5 2.8 12.8 16.2 10.0

31 19 71 125 106

1 <1 <1 <1 <1

8 6 30 29 21

6.4 2.9 14.8 19.7 11.0

P#11 P#12 P#13 P#14 P#15

51.7 31.6 33.7 41.7 31.9

<0.2 1.0 1.0 0.7 0.5

10.25 42.9 26.7 42.6 42.3

2.54 0.43 3.03 1.88 1.06

<5 <5 <5 <5 <5

0.4 1.0 0.3 0.5 0.4

86.6 39.1 48.4 74.4 38.0

59 52 146 135 52

50 60 120 60 60

5.4 6.1 3.5 5.7 4.8

19.5 9.7 11.8 16.5 10.0

214 94 68 76 128

<1 <1 <1 <1 <1

49 23 15 21 18

22.9 9.7 10.9 19.2 8.7

P#16 P#17

16.8 37.6

<0.2 <0.2

31.3 13.80

2.97 0.89

<5 <5

0.4 0.2

17.8 43.4

67 61

100 150

5.0 6.7

5.1 11.0

174 97

<1 <1

11 18

4.3 10.1


A ALS Chemex EXCELLENCE IN ANALYTICAL CHEMISTRY ALS Canada Ltd. 212 Brooksbank Avenue North Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 WWW.alschemex.com

To: MCLEOD, JIM 5382 ASPEN WAY DELTA BC V4K 3S3

Page: 2 - C Total »■ Pages: 2 (A - C)


CERTIFICATE OF ANALYSIS VA06092686 |

Method Analyt*


ME-MS18 ME-MS18 MEMS 18 ME-MS18 ME-MS18 ME-MS18 ME-MS18 ME-MS18 ME-MS18 ME-MS18 ME-MS18 ME-MS1B ME-MS18 Sn Sr Tb Te Th Ti Tl U W Y Yb Zn Zr ppb ppb ppb ppb ppb ppb ppb ppb ppb ppb ppb ppb ppb 0.2 10 0.1 1 1 10 10 1 0.2 0.1 0.1 20 1

P#1 P#2 P#3 P#4 P#5

0.6 2460 14.8 1 6 10 <10 10 0.6 431 46.6 510 7 0.9 4090 1.7 1 5 500 <10 6 0.2 41.2 3.6 1180 12 0.6 2780 2.4 <1 9 560 <10 6 0.2 40.1 3.8 270 23 1.0 990 5.6 1 26 1850 <10 17 0.5 98.7 9.0 940 83 0.6 960 4.8 <1 17 640 <10 14 0.3 84.5 7.5 210 64

P#6 P#7 P#8 P#9 P#10

0.2 3150 1.8 <1 3 20 <10 32 <0.2 49.6 3.9 <20 7 0.2 5840 0.8 <1 3 80 <10 21 <0.2 21.6 1.9 <20 5 0.5 1100 3.5 <1 11 550 <10 8 0.3 72.6 8.0 2330 49 0.3 1590 5.2 <1 7 470 <10 5 0.2 144.5 12.7 350 24 0.7 2510 2.5 <1 6 300 <10 5 <0.2 54.8 5.2 70 24

P#11 P#12 P#13 P#14 P#15

0.3 480 5.5 <1 3 200 <10 3 0.2 167.5 13.5 370 12 0.2 1820 2.2 <1 5 550 <10 4 0.2 52.3 4.3 280 23 <0.2 1180 2.6 <1 7 520 <10 3 <0.2 80.1 7.1 2580 9 <0.2 2120 4.6 <1 5 260 <10 5 0.2 132.5 10.8 740 24 <0.2 1550 2.0 <1 5 290 <10 4 <0.2 54.8 3.9 360 18

P#16 P#17

<0.2 1360 1.2 <1 5 210 <10 5 <0.2 31.7 2.6 710 18 <0.2 1620 2.0 <1 10 150 <10 7 0.2 49.9 4.5 40 44


(A.ISS)



"o: MCLEOD, JIM 5382 ASPEN WAY DELTA BC V4K 3S3

Project: PG

Page: 2 - A Total tr images: 2 (A - C)



Method Analyt*


WEI-21 Recvd Wt.

kg 0.02

ME-MS18 Ag ppb 0.1

ME-MS18 As ppb

1

ME-MS18 Au ppb 0.1

ME-MS18 Ba ppb 10

ME-MS18 Bi

ppb 3

ME-MS18 Ca

ppm 0.2

ME-MS18 Cd ppb

1

ME-MS18 Ce ppb 0.1

ME-MS18 Co ppb 0.3

ME-MS18 Cr

ppb 1

ME-MS18 Cu ppb 10

ME-MS18 Er

ppb 0.1

ME-MS18 Fo

ppm 0.1

ME-MS18 Gd ppb 0.1

PG#1 PG#2 PG#3 PG#4 PG#5

1.72 1.12 1.52 1.40 1.46

30.2 26.3 8.8 24.5 15.3

8 6 7 17 9

<0.1 <0.1 0.2 0.3 0.2

890 590 2090 1070 760

<3 <3 <3 <3 <3

113.5 48.3 213 210 108.0

236 50.1 102.0 147.0 167.0

65.4 133.0 39.8 28.3 27.8

37 30 33 45 38

520 390 430 200 200

16.7 10.2 7.8 11.1 9.5

66.9 116.5 21.6 53.7 44.1

30.2 9.8 14.6 23.6 21.7

PG#6 PG#7

1.58 1.18

27.5 54.4

60 15

0.2 0.2

750 1100

<3 <3

181.0 188.5

8 17

89.1 45.2

66.6 27.3

40 22

360 390

7.5 4.6

50.2 42.8

16.8 9.2


A ( A L S )


212 Brooksbank Avenue North Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 W W W . a l s c h e m e x . c o m

r o: MCLEOD, JIM 5382 ASPEN WAY DELTA BC V4K 3S3

Project: PG

Page: 2 - B Totai ,r Pages: 2 (A - C)



S a m p l e D e s c r i p t i o n

Method Analyt*

Units LOR

ME-MS18 ME-MS18 ME-MS18 ME-MS18 ME-MS18 ME-MS18 ME-MS18 ME-MS18 ME-MS18 ME-MS18 ME-MS18 ME-MS18 ME-MS18 ME-MS18 ME-MS18 La Li Mg Mn Mo Nb Nd Ni Pb Pd Pr Rb Sb Sc Sm ppb ppb ppm ppm ppb ppb ppb ppb ppb ppb ppb ppb ppb ppb ppb 0.1 0.2 0.01 0.01 5 0.1 0.1 3 10 0.1 0.1 5 1 3 0.1


94.4 23.1 38.4 53.2 66.8

<0.2 0.4 0.5 2.0 0.2

14.10 10.35 23.8 18.55 5.63

2.05 3.00 0.81 1.58 2.20

<5 <5 5 <5 <5

0.2 0.2 0.1 2.5 1.3

107.0 28.6 45.6 67.4 76.7

133 216 58 55 33

80 70 80 80 100

7.0 4.2 7.9 3.3 3.4

25.9 7.1 11.2 13.6 16.7

102 87 130 104 130

<1 <1 <1 <1 <1

37 23 29 28 27

23.9 6.9 11.8 16.0 17.8

PG#6 PG#7

51.5 29.7

0.6 0.2

15.90 5.87

2.01 0.71

<5 <5

1.4 1.0

59.3 31.0

87 72

140 120

1.8 0.6

12.3 5.7

150 157

<1 <1

17 12

13.4 7.1


A ( A L S )


212 Brooksbank Avenue North Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 W W W . a l s c h e m e x . c o m

To: MCLEOD, JIM 5382 ASPEN WAY DELTA BC V4K 3S3

Project: PG

Page: 2 - C Total ff Pages: 2 (A - C)



Sample Descr ip t ion

Method Analyte

Units LOR

ME-MS18 Sn ppb 0.2

ME-MS18 Sr

ppb 10

ME-MS18 Tb ppb 0.1

ME-MS16 Te ppb

1

ME-MS18 Th ppb

1

ME-MS18 Ti

ppb 10

ME-MS18 TI

ppb 10

ME-MS18 U

ppb 1

ME-MS18 W

ppb 0.2

ME-MS18 Y

ppb 0.1

ME-MS18 Yb ppb 0.1

ME-MS18 Zn ppb 20

ME-MS18 2r

ppb 1


PG#6 PG#7

<0.2 <0.2 <0.2 0.3 0.2

0.2 <0.2

880 460 2340 2240 970

1620 2020

5.0 2.0 2.6 3.9 3.5 TF

1.5

<1 <1 <1 <1 <1

<1 <1

14 6 14 12 12

"i~ 5

230 250 250 580 250

380 130

<10 <10 <10 <10 <10 <10 <10

0.2 0.2 0.2 0.4 0.3 UT 0.2

141.0 75.9 53.9 75.8 77.3 59.2 38.3

12.4 7.4 5.7 7.9 6.7 5.3 3.3

30 590 20 150 50 50 40

52 32 58 52 50

~ 17


Appendix 2

IP Data Field Data

21

IP Data

PG Grid - Porphyry Gold Project

MP = D»xlO APP. Res. = 2n n (n+l) a V AV I

LO

Station I(ma) dV(mv) IP(mv) Res NIP SP V RSS

P1=210W P2=150W 4 -0.02 0.07 6.33 35 +0.5 6* 1000

Pl=210 P2=180 3.45 -0.3 2.2 688 73 -1.2 6 1000

Pl=240 P2=180 3.4 -0.2 -1.3 665 65 -0.4 5* 1000

Pl=240 P2=210 3.4 -0.2 -.55 1662 27.5 -0.2 5 1000

Pl=270 P2=210 3.4 -0.2 -0.8 443 40 0 4* 1000

Pl=270 P2=240 3.4 -0.2 -0.7 222 35 -0.6 4 1000

Pl=300 P2=240 3.4 -0.2 -1.2 266 60 -0.6 3*

Pl=300 P2= 270 3.4 -0.2 -0.55 133 27.5 -0.7 3 1000

Pl=330 P2= 270 3.4 -0.2 -1.6 266 80 +0.4 2* 1000

Pl=330 P2= 300 3.4 -0.2 -1.2 66 60 +0.9 2 1000

Pl=360 P2= 300 3.4 -0.6 -1.2 133 20 +0.2 1* 1000

Pl=360 P2= 330 3.4 -0.4 -1.6 44 40 -1.2 1 1000

jan 1 $ 2q07 on the gold commissioner's office vancouver, b.c

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