REGIONAL TRIAXIAL AEROMAGNETIC SURVEY ASSESSMENT WORK · PDF fileregional triaxial aeromagnetic survey assessment work report by n. ralph newson, m.sc., p. eng., p.geo. for 101047025

REGIONAL TRIAXIAL AEROMAGNETIC SURVEY

ASSESSMENT WORK REPORT

by

N. Ralph Newson, M.Sc., P. Eng., P.Geo.

for

101047025 SASKATCHEWAN LTDCMKM DIAMONDS.

Saskatoon, Saskatchewan. July 29, 2005

TABLE OF CONTENTS

PAGE1.0 INTRODUCTION…………………………………………………………….................... 12.0 PROPERTY DESCRIPTION AND LOCATION……………………………………........ 13.0 ACCESSIBILITY, CLIMATE, INFRASTRUCTURE, PHYSIOGRAPHY…………....... 14.0 PREVIOUS WORK……………………………................................................................. 15.0 GEOLOGICAL SETTING................................................................................................... 2 5.1 REGIONAL GEOLOGY AND GEOPHYSICS.....………………………………..... 26.0 AIRBORNE MAGNETIC SURVEY.................................................................................. 4 6.1 PURPOSE…………………………………………………………………………… 4 6.2 DETAILS OF SURVEY...................................……………………………………… 4 6.3 RESULTS…………………………………………………………………………… 47.0 CONCLUSIONS AND RECOMMENDATIONS………………………………………... 78.0 REFERENCES AND BIBLIOGRAPHY………………………………………………..... 8

LIST OF TABLES

FOLLOWING PAGETable 1. Anomalies picked from Goldak aeromagnetic survey…………………………… 1

LIST OF APPENDICES

APPENDIX A: TECHNICAL REPORT ON THE SURVEY

APPENDIX B: LIST OF CLAIMS

1.0 INTRODUCTION

This report describes a regional aeromagnetic survey carried out over an area which includesthe Fort à la Corne diamond area and a large area surrounding the known kimberlites.

Flying was was carried out from April 3 to June 16, 2004, by Goldak Airborne Surveys, out oftheir office in Saskatoon (see technical report, Appendix A).

2.0 PROPERTY DESCRIPTION AND LOCATION

The property is contained within the area flown. Appendix B is a list of the claims, and maps ofthe claims are presented as one of the products produced by Goldak, Appendix A.

3.0 ACCESSIBILITY, CLIMATE, INFRASTRUCTURE, PHYSIOGRAPHY

The survey area is well served by provincial highways and grid roads. Paved provincialHighway 55 passes east-west through the southern third of the area. Highways 120 and 106 gonorth from highway 55. South of highway 55, grid roads provide access to the cultivated areas.The Fort à la Corne Forest is served by the Division Road, passing east-west through the entireforest. The Inland Trail, the Torch Trail, and the Shipman Trail go north from the DivisionRoad to the grid road system. Highway 11 passes close to the western boundary of the area.Highway 6 forms the eastern survey boundary south of highway 55. North of the cleared landaccess is poorer, with only occasional bush roads.

The terrain is a fairly flat, with low local relief. Average elevation is 425 metres above sea level.The climate is a typical mid-continental type, dry (averaging 405mm rainfall), with extremeseasonal temperature variations, commonly from -35ºC to +35ºC. Work can be carried out allyear round, although some roads can be in poor driving condition in the spring.

The City of Prince Albert is the largest urban centre in the survey area, and is in thesouthwestern corner of the survey area. Some services and supplies are available there.

4.0. PREVIOUS WORK

Some airborne surveys have been done over parts of the area covered by this survey, but this isthe first time the entire area has been surveyed in one program.

Many other types of work have been carried out in the area surveyed. ground magnetic surveyshave been done to check many airborne anomalies from previous surveys. drilling has beendone by many people to check anomalies found by ground and/or aeromagnetic surveys.

Northern Explorers Ltd. Assessment work report 101047025 Sask Ltd 1

5.0 GEOLOGICAL SETTING

5.1. REGIONAL GEOLOGY and GEOPHYSICS

The Precambrian basement in the Fort à la Corne diamond area consists of Proterozoic rocks ofthe Trans-Hudson orogen. Recent work (Chiarenzelli et al, 1987, Collerson et al, 1989, Greenet al, 1980) has demonstrated that this component sits on an Archean basement, which has beendeformed and thickened by the collision of the crustal blocks. This means that the regionsatisfies Clifford’s Rule, which states that economic kimberlites only occur in cratonic nuclei ofArchean age. This is a statement of empirical fact based on African experience, and appears tobe true of the Siberian diamond fields and others.

Overlying the Precambrian basement are the Phanerozoic rocks of the interior sedimentarybasin. The Phanerozoic section in Saskatchewan is up to 3200 m thick in the southern part ofthe province, but thins northward to the exposed edge of the Shield. Paleozoic rocks fromCambrian to Mississippian age occur, but the section is not everywhere complete. From LateMississippian to Early Jurassic the region experienced a period of uplift, and no sedimentationoccurred. Stratigraphy of the Phanerozoic section is a useful tool in exploration for kimberlites. Up tonow, evidence indicated that all of the known kimberlites are about 95 to 100 million years old,so the most likely rock units are those of that age. Recently (B. Jellicoe, May 2001, pers.comm.), evidence has been accumulating which indicates that the period of kimberlitic intrusionmay have spanned 20 million years.

The country rocks which are the same age as the kimberlites are Cretaceous mudstones, whichare not fully consolidated. They are underlain by Mannville sands which are full of water. In thefew holes the writer has drilled through the Mannville, the underlying rocks are carbonates,which are completely dry. The Fort à la Corne kimberlites apparently owe their shape to thefact that up to the base of the Mannville, the rocks are dry. The hot kimberlitic magma passedthrough the dry rocks, but when they hit the water-filled sands they caused a magmatophreaticexplosion, blowing a bowl-shaped hole in the sands and mudstones, which subsequently filledwith kimberlite. The Saskatchewan kimberlites have large surface areas because of this.

Structures in the basement and in the Phanerozoic rocks are believed to have been important inproviding conduits to surface for the kimberlitic magmas. Gent (1989, 1992) has described anumber of sub-Phanerozoic basement structures, interpreted from regional gravity andmagnetic data produced by the Geological Survey of Canada. These include boundariesbetween crustal blocks, axes of gravity highs and lows, and faults with measurable horizontalseparation. He refers particularly to the change in trends of gravity readings on either side ofan interpreted block centred under Prince Albert and Saskatoon. The eastern boundary passesthrough the Fort à la Corne kimberlites. Any of these structures could provide access todiatreme intrusions.

Collerson et al (1989) suggest that kimberlitic intrusion from the Sturgeon Lake area eastwardsto the Manitoba border may have been controlled by a northeasterly extension of the GreatNorthern Explorers Ltd. Assessment work report 101047025 Sask Ltd 2

Falls Tectonic Zone, which is exposed in Montana.

Major structures have been mapped in the Phanerozoic basin using extensive data accumulatedby Saskatchewan Energy and Mines, including gravity, seismic and well log data. All but one ofthe known structures are thought to be reflections of structures in the Precambrian basement.The interpretations here are by Ghent, 1989.

The longest structure, the Shaunavon linear, is defined by highly fractured calcilutites in theJurassic Shaunavon formation, and a depression in the Lower Cretaceous erosional surface. Italigns with the drainage divide between the South Saskatchewan River system and the OldWives Lake- Qu'Appelle River system. Subsurface correlation of strata indicates thatconsiderable tectonic arching has occurred along this trend. The Punnichy Arch trends east-west, and is known to have been active during Late Albian time,during deposition of uppermost Lower Cretaceous rocks, which is the Mannville Group in thearea of the Saskatchewan diamond play. The topographic high over this structure may indicatethat there has been some tectonic arching since the Albian. Evidence exists that some of thekimberlites in Saskatchewan are of about Albian age, or a bit younger.

The Molanosa Arch is near the northern edge of the Phanerozoic basin, and oil well data arescarce there. Available evidence suggests that it has been active over a long time, particularlyduring the Devonian and Jurassic, but also more recently.

The Val Marie Arch deserves particular mention because there are kimberlitic intrusionsnearby, suggesting a genetic link. It was active during late Cretaceous time. Since there isevidence of Mid-Cretaceous kimberlitic intrusion elsewhere in the province, other archstructures whose active period spans this time may have permitted the intrusion of kimberlite.

The Sweetgrass-North Battleford Arch is a major, complex structure. At times, it appears tohave included the Swift Current Platform (including the Cypress Hills) and had a total verticalrise of about 1200 metres. The region subsided, leaving the Cypress Hills Arch and theSweetgrass-North Battleford Arch.

A number of intrusions are known in the Phanerozoic basin, and all but one are diatremes. Ofthe diatremes, some are kimberlitic, as at Fort à la Corne. The kimberlites best described in thepublic domain are those of the JV.

Jellicoe (2000) states that the kimberlites of Kensington/De Beers et al are crater facies, and arecomposed of mixed olivine and lapilli pyroclastics, with 2 generations of olivine. Thegroundmass consists of monticellite, perovskite, spinel, serpentine and carbonate. Xenocrystsinclude olivine, garnet, ilmenite and spinel. Xenolithic fragments include eclogite, peridotite,basement rocks, Paleozoic carbonates, and Cretaceous clastic rocks.

Drilling results and additional ground magnetic and gravity surveys have shown the best knownkimberlite bodies to be bedded, and to have a very different shape from most known kimberlitebodies. In most of the well-known diamond mines in Africa, for example, and in those in theNorthern Explorers Ltd. Assessment work report 101047025 Sask Ltd 3

NWT in Canada, the upper portions of the kimberlites bodies have been eroded, leaving onlythe feeder pipe, which has a "carrot" shape, getting smaller in diameter with depth. However, inthe Fort à la Corne swarm, the tops of the kimberlitic volcanic edifices are completelypreserved, and they are shaped more or less like a soup bowl, with two larger horizontaldimensions, and one smaller vertical dimension. Several of these have an inferred geologicalresource (based on a few holes and on geophysical modeling) in excess of 100 million tonnes,one has nearly a billion tons, and one group of five which are close together, or perhapscoalescing, contain about 2 billion tons of kimberlite. There are thus huge volumes ofkimberlite within a few hundred metres of the surface.

The Fort à la Corne swarm of kimberlitic bodies is the largest swarm known in the world, andsome of the bodies are the largest known such bodies in the world.

The Fort à la Corne kimberlites are covered with about 100 to 120 metres of unconsolidatedPleistocene glacial deposits.

K/Ar dating of phlogopite in the kimberlite, and dating by microfossils in the enclosing rocksgave an age of 94 to 96 million years, although Leahy (1996) has proposed an age of 100 Ma.The bodies are at or very close to the Pleistocene erosional surface, under about 100 m ofoverburden. The presence of crater facies rocks in the core indicates that erosion is slight.

All of the kimberlites discovered in the survey area to date have been found using magnetics.The kimberlites show up as positive anomalies with respect to the enclosing rocks. Some of theanomalies caused by the known kimberlites are so large that they show up on the governmentaeromagnetic maps, and others have been found by low-level surveys by explorationcompanies.

6.0 AIRBORNE MAGNETIC SURVEY

6.1 PURPOSE

This survey was undertaken to look for smaller bodies than those discovered to date, or thosewith lower magnetic susceptibility, or those composed only partly of kimberlite phases whichshow up magnetically.

6.2 DETAILS OF SURVEY

The technical details of the survey are given in Appendix A

6.3 RESULTS

As expected, the survey clearly showed the known kimberlites in the main Fort à la Corneswarm, the Snowden group, those near Foxford, the Dizzy kimberlite, and those in the generalarea of Candle Lake. Also as expected, it showed many cultural features, since the area of thesurvey includes the city of Prince Albert, many villages, and many farms. A farmstead looks likeNorthern Explorers Ltd. Assessment work report 101047025 Sask Ltd 4

a small kimberlite to this and other airborne systems. Many of the cultural features can beeliminated by comparing the magnetic maps with the topographic data. Villages, power linesand most farm buildings can be eliminated in this way. Features near roads can be investigatedby carrying out a "drive-by" survey. By this method, buildings built since the topographic datawere obtained, and other cultural features can be eliminated. Features with no obvious culturalcause, and which appear to be caused by a source significantly above the Precambrian basementare targets for ground magnetic surveys. Follow-up work by all of these methods was done onanomalies picked from the Goldak data.

Few anomalies likely to be caused by completely unknown kimberlites survived the eliminationslisted above. Further processing, consisting of filtering, was carried out on the raw data. Theresulting targets are listed below in table 1. Some have been investigated, and some have notyet been, as noted in the column headed "results".

Table 1. Anomalies picked from Goldak aeromagnetic survey.

NTSsheet

NAD 83UTM

Easting

NAD 83UTM

Northing

Results

73 H 1 535650 5899150

73 H 3 485850 5898525495850 5884875483625 5883050

73 H 5 463060 5901150

73 H 6 471475 5900100491400 5900650492000 5900650496574 5925164 Buildings beside known kimberlite.481750 5922050491450 5910250486920 5916990 Drilled previously by Uranerz, no kimberlite. Ground

mag to check location. Uranerz hole apparently ontarget.

487100 5914710 Cultural.491700 5900650


NTSsheet

NAD 83UTM

Easting

NAD 83UTM

Northing

Results

494500 5926050 Probable extension of known kimberlite.

73 H 7 532325 5919500 Drilled hole, no kimberlite.520325 5911800506339 5905615523900 5921675532050 5912450 No obvious cultural cause-needs ground mag survey.527820 5922060531780 5921100532260 5919440 Drilled 2 holes, no kimberlite.508330 5919560 Cultural.

73 H 8 546597 5913198533550 5926775 Cultural.

73 H 10 520000 5935537 Drilled one hole, no kimberlite.513075 5930750 Cultural.501800 5935940518280 5934220 Jacquine L. Drilled 2 holes, no kimberlite.530860 5929310 Cultural.

73 H 11 493050 5930425 Drilled 2 holes, no kimberlite.495950 5928850 Probable basement (this writer's opinion).471975 5948100472920 5946140480400 5939990 Ground mag done, no target.486530 5949770

73 H 15 501225 5960850500250 5957700501280 5960970


7.0 CONCLUSIONS AND RECOMMENDATIONS

1. This is a very good data set for a large area including and surrounding the Fort à laCorne diamond area.

2. Some anomalies have been selected from the data for follow-up, and some of thesehave been investigated. The remaining ones should be investigated by groundmagnetic surveys to see if they might be drill targets.

_________________________N. Ralph Newson, M.Sc., P.Eng., P.Geo.


8.0 REFERENCES & BIBLIOGRAPHY Chiarenzelli, J.R., Lewry, J.F., and Landon, M., 1986. Bedrock geology, Istwatikan Lakearea: evidence for Hudsonian juxtaposition of Proterozoic and Archean rocks along aductile detachment surface. IN Summary of investigations, 1987, Sask. Geol. Surv. Specialreport 87-4 Collerson, K.D., Lewry, J.F., Bickford, M.E., and Van Schmus, W .R., 1989. Crustalevolution of the buried Precambrian of southern Saskatchewan: implications for diamondexploration. , IN Modern exploration techniques: proceedings of a symposium held in Regina,Saskatchewan, 20- 21 November, 1989. Sask. Geol. Soc. Special Publication Number 10 Gent, M.R., 1989. Regional Phanerozoic anomalies in Saskatchewan. IN Summary ofinvestigations, 1989, Sask. Geol. Surv., Sask. Energy and Mines, Misc. Rpt. 89-4. __________ 1992. Diamond exploration in Saskatchewan. Bull. Can. Inst. of Min. and Met.Vol.84, No. 956. January, 1992.

Green, A.G., Stephenson, O.G., Mann, G.D., Kanasewich, E.R., Cumming, G.L., Hajnal,Z., Mair, J.A., and West, G.F., 1980. Co-operative seismic surveys across the Superior-Churchill boundary zone in southern Canada. Canadian Journal of Earth Sciences, Vol. 17,no. 5, pp. 617-632. Hoffman, P.F., 1988. United plates of America: the birth of a craton. Annual Review ofEarth and Planetary Sciences. Vol. 16, pp.543-604. Janse, A.J.A., 1992. Clifford's Rule and its application to diamond prospecting in Canada.Talk given at the annual meeting of the Prospectors' and Developers' Association, Toronto,1992. Jellicoe, B., 2001. Diamonds in Saskatchewan, 2001. Talks given to CIM Geology Division,Saskatoon, Nov. 28, 2000 and May 3, 2001.

Jennings, C.M.H., 1989. Exploration for diamondiferous kimberlites & lamproites. INModern exploration techniques: proceedings of a symposium held in Regina,Saskatchewan, 20- 21 November, 1989. Sask., Geol. Soc. Special Publication Number 10. Kirkley, M.B., Gurney, J&J., and Livens, A.A., 1992. Age, origin and emplacement ofdiamonds: a review of scientific advances in the last decade. Bull. Can. Inst. of Min. and Met.,Vol. 84, No. 956. January, 1992.

Leahy, K., 1996. The geology of the kimberlites from the Fort à la Corne area, Saskatchewan,Canada. Ph.D. thesis, U. of Leeds.


Lehnert-Thiel, K., Lower, R., Ro, R., and Robertshaw, P., 1992. Talk given at the annualmeeting of the Prospectors' and Developers' Association, Toronto, 1992. Mitchell, R.H., 1986. Kimberlites, Mineralogy, Geochemistry and Petrology. Plenum Press,New York. 442p.

Ross, G.M., Parrish, R.R., Villeneuve, M.E., and Bowring, S.A., 1991. Geophysics andgeochronology of the crystalline basement of the Alberta Basin, western Canada. CanadianJournal of Earth Sciences, Vol. 28, no. 4, pp. 512-522.


APPENDIX A

TECHNICAL REPORT ON THE SURVEY

TECHNICAL REPORT ON A FIXED WING AEROMAGNETIC SURVEY

Fort à la Corne Forest Area Central Saskatchewan

for

Casavant Mining Limited

By

GOLDAK AIRBORNE SURVEYS

Goldak Airborne Surveys 25 Duncan Cres. Saskatoon, Saskatchewan Canada S7H 4K3 Tel: (306) 249-4474 Fax: (306) 249-4475 Cell: (306) 222-5104 Email: [email protected] URL: www.goldak.ca

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1. INTRODUCTION ....................................................................................................................................4

2. SURVEY AREA LOCATION...................................................................................................................5 Illustration – Location of the Fort à la Corne Survey Area ...................................................................5

3. DATA SPECIFICATION.........................................................................................................................6 Line Spacing.........................................................................................................................................6 Altitude..................................................................................................................................................6 Diurnal ..................................................................................................................................................6 Magnetic Noise.....................................................................................................................................6

4. AIRCRAFT AND EQUIPMENT..............................................................................................................7 4.1 Aircraft................................................................................................................................................7

Illustration – Aircraft C-GJBA ...............................................................................................................7 Illustration – Aircraft C-GJBB ...............................................................................................................8

4.2 Magnetometer and Compensation ....................................................................................................8 4.3 Magnetic Base Stations .....................................................................................................................8

Illustration – Base Magnetometer 1 Setting .........................................................................................9 Illustration – Base Magnetometer 2 Setting .........................................................................................9

4.3 GPS Positioning System..................................................................................................................10 Illustration – GPS Base Antenna Location .........................................................................................11

4.3 Radar Altimeter ................................................................................................................................11 4.5 Barometric Altimeter ........................................................................................................................11 4.6 Flight Path Camera ..........................................................................................................................11 4.7 GEDAS Digital Recorder..................................................................................................................12

5. Data Processing and Presentation ...................................................................................................13 5.1 Total Field Leveling..........................................................................................................................13 5.2 Altitude Data ....................................................................................................................................15 5.3 Digital Data Files..............................................................................................................................15 5.4 Map Products...................................................................................................................................16 5.4 Flight Path Video..............................................................................................................................18

6. DETAILED EQUIPMENT SPECIFICATIONS......................................................................................19 Illustration – Survey Aircraft 3-View ...................................................................................................21

7. STATEMENT OF QUALIFICATIONS..................................................................................................22

APPENDIX A: COMPENSATION FLIGHT...............................................................................................23

3

1. INTRODUCTION This report describes an airborne geophysical survey carried out over the Fort à la Corne Forest area of Central Saskatchewan. The tri-axial magnetic gradiometer survey was carried out by Goldak Airborne Surveys (GOLDAK) on behalf of Casavant Mining Limited (CMKM) between April 3 and June 16, 2004. Aircraft equipment operated included four cesium vapor, digitally compensated magnetometers, a GPS real-time and post-corrected differential positioning system, a flight path recovery camera, VHS titling and recording system, as well as radar and barometric altimeters. All data was recorded digitally in GEDAS binary file format. Reference ground equipment included two GEM Systems GSM-19W Overhauser magnetometers and a Novatel 12 channel GPS base station. The GPS was set up at the base of operations for differential post-flight corrections while the magnetometers were installed in remote locations away from traffic and cultural interference. All equipment installations are covered in more detail in Section 6 of this report. Forty six flights were required to complete the survey block. The traverse lines were flown on a spacing of 200 meters with a control line separation of 1500 meters. Aircraft height was specified at 80 meters above ground. Saskatoon, SK was used as the base of operations for this survey.

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2. SURVEY AREA LOCATION The Fort à la Corne survey area is approximately centered 50 km northeast of the community of Prince Albert, SK; the mid point is roughly at 53° 30’ N, 105° 06’ W. The block consisted of 52,900 line kilometers of traverse lines flown 0° UTM North with Tie lines flown perpendicular to the survey lines. Prior to the survey the CMKM provided GOLDAK with coordinates for flying. They are defined by the following WGS84 UTM Zone 13 coordinates

corner 1 405900 5876000 corner 2 450900 5985500 corner 3 535500 5985500 corner 4 535500 5876000

Illustration – Location of the Fort à la Corne Survey Area

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3. DATA SPECIFICATION Line Spacing Traverse Lines bearing: 0°/180° nominal spacing: 200 m tolerance: 50 m over 1000 m (25%) no lines were to cross Control Lines bearing: 90°/270° nominal spacing: 1500 m Altitude Altitude control was accomplished by using Goldak’s GEDAS auto-drape system. Input topographic data for the GEDAS system was acquired from publicly available data generated by the NASA Radar Topography Shuttle Mission.

nominal altitude: 80 m MTC (mean terrain clearance) tolerance: +- 16 meters from the pre planned drape surface (20%)

Diurnal A maximum diurnal tolerance of 2nT (peak to peak) deviation from a long chord equivalent to a period of 25 seconds was not to be exceeded. This time period represents the time required to fly between two control lines. Magnetic Noise The magnetic noise was not to exceed 0.1 nT in the 4th digital difference over a distance of 1000 m. All data was fully examined in the field and judged to have met the above parameters.

6

4. AIRCRAFT AND EQUIPMENT

4.1 Aircraft The two aircraft used in this survey were Piper PA-31 Navajos, registrations C-GJBA and C-GJBB, owned and operated by Goldak Airborne Surveys. Each aircraft is fitted with a 3-meter stinger attached to the rear fuselage on the centerline of the aircraft. The attitude sensing fluxgate magnetometer is positioned at the midpoint of the stinger. Two sensors separated vertically are mounted in the aft end of the tail stinger. The aircraft also has magnetometers installed in composite pods on each wingtip. The pods mount the sensors 1.2 meters outboard of the aircraft wingtip. The four magnetometers form a three-axis gradiometer with following dimensions: Lateral - 14.865m Longitudinal - 8.560 m Vertical - 2.229 m The aircraft has been extensively modified, both mechanically and electrically, to minimize the effects of maneuvering on the measured magnetic field. The aircraft has demonstrated Figure of Merit of less than 0.6 nT as measured to GSC specification. Typical FOMs under less than ideal calibration environments are 0.8 nT for the tail magnetometers. This low level of magnetic noise is considered to be exceptional by experts at the National Research Council.

Illustration – Aircraft C-GJBA

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Illustration – Aircraft C-GJBB

4.2 Magnetometer and Compensation The airborne magnetometers used are a matched set of Geometrics G-822A optically pumped cesium vapor types with sensitivity of 0.005 nT. The magnetometer’s Larmor signal is decoupled and counted by a RMS Instruments AADCII compensator, and data produced at a rate of 10 Hz with a resolution of 0.001 nT. The data bandwidth is from 0 to 0.9 Hz with an internal noise level of less than 0.002 nT. The AADCII compensates for magnetic noise due to aircraft motion and heading. Prior to the survey, the aircraft is taken to an area of low magnetic gradient at a high altitude (7000’ AGL +) and put through a series of rolls, pitches and yaws on each of the survey’s principle headings. This is done so that the AADCII can form a model of the aircraft’s magnetic characteristics without the near influence of the local geology. The remaining magnetic distortion is quantified by a term known as the Figure of Merit, or FOM. The Geological Survey of Canada uses a figure of merit of 1.5 or less as standard survey criteria. As stated above, this aircraft has an exceptional typical FOM of less than 0.9 nT. C-GJBA flew an FOM flight on April 2, 2004. C-GJBB flew two FOM flights: one May 31 and a second June 4, 2004. The results of these calibration flights are given in Appendix A.

4.3 Magnetic Base Stations Two base magnetometer stations were employed in this survey. Dual stations are useful both as a backup in the case of instrument failure and also to discern any cultural events from either unit. The first base station magnetometer employed was a GEM Systems GSM-19W Overhauser type proton precession magnetometer with GPS time base. This unit logged data to a DAP9800 industrial handheld computer with a compact flash memory card. This battery powered system made use of a solar charger. The system was installed on a private acreage approximately 6 km east of Saskatoon. A radio modem

8

link was connected to this system and the data transmitted to Goldak’s office so that diurnal conditions could be monitored in real time. The WGS84 UTM Zone 13 location of this installation was 398278E 5776310N

Illustration – Base Magnetometer 1 Setting The second base station was also a GEM Systems GSM-19W connected to a DAP9800. This station was set up inside the survey block just off an infrequently used trail approximately 25 km east of the Christopher Lake junction along Highway 263. The WGS84 UTM Zone 13 coordinates for this installation were: 467283 E 5938662 N

Illustration – Base Magnetometer 2 Setting

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4.3 GPS Positioning System The GPS receiver in the survey aircraft is a Novatel 3151R Propak 12 channel dual-frequency differential unit that communicates directly with the GEDAS system. The base station GPS is also a Novatel 3151R dual-frequency Propak whose data is logged by a battery powered industrial portable computer. A survey grade GPS base antenna and choke ring is used to minimize multi-path errors. The system can be used for differential positioning in either real-time or post-corrected mode. The positioning system also incorporates a Racal Landstar real-time DGPS system that receives real-time differential corrections from an orbiting geo-synchronous communications satellite. The corrections from this device allow 2-5 meter positioning accuracy in real-time. A GPS base station is also recorded data during the survey flight to provide a higher level of accuracy and an independent confidence check to the Landstar RT DGPS system. GPS signals are occasionally “dithered” by the US Department of Defense for security reasons. This dithering can cause positioning errors of up to 100 meters. In addition to dithering, atmospheric and ionospheric effects typically reduce the accuracy of the non-differential positioning to approximately 10 meters RMS. If a suitable stationary GPS receiver on a known, or assumed, position is used to record the apparent errors in the satellite range data, those errors can be used to correct the moving receiver in the aircraft to a an accuracy of 2-5 meters RMS. This compensation process is called differential correction and can be either applied to the moving receiver in real time for higher dynamic accuracy, or applied later to find out where the aircraft was with high accuracy. This is called real-time and post-corrected differential positioning respectively. The base antenna was installed at Goldak Exploration’s office in Saskatoon, SK. This site has been employed in the past and has been proven to provide good satellite coverage in all directions. After installation and acquiring data for approximately 24 hours, the base positions were determined by position averaging, the assumption being after a quantity of time the mean value of the errors will be zero. Further to this processing the base GPS positions were differentially corrected using a reference base GPS positon established in Flin Flon Manitoba (approx. 400 km E). The differentially corrected base GPS positions were determined to be:

Latitude: 52° 07’ 9.7919” N Longitude: 106° 35’ 6.3486” W Elevation: 514.56m MSL*

*The Canadian GSD95 geoid model was used to transform Height Above Ellipsoid to Height Above Sea Level The above coordinates were used as the master position for differential corrections for the duration of the project.

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Illustration – GPS Base Antenna Location

4.3 Radar Altimeter Aircraft C-GJBA was equipped with a Thompson CSF ERT-160A altimeter with a range of 0 to 8000 feet and a resolution of 1 meter. A Terra TRA-3000 digital unit with accuracy of ±5 meters in the range of typical survey altitudes was installed as the secondary altimeter. C-GJBB had a Terra TRA-3000 as the primary altimeter with a King KRA-10A installed as a secondary unit.

4.5 Barometric Altimeter Both aircraft were equipped with a Setra model 270 barometric altimeter. This instrument has an accuracy of ±1 meter with a range of -1,000 to 10,000 feet.

4.6 Flight Path Camera The flight path is recorded by a Panasonic GP-KR222 SV hi-resolution colour video camera located in the lower rear fuselage of each aircraft. The video was recorded by a Panasonic AG-1980P SVHS recorder. Data pertaining to position, time, speed, altitude, line number and direction was superimposed in the videotape by a Horita SCT-50 video titler.

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4.7 GEDAS Digital Recorder All data was processed and recorded digitally by our GEDAS system. The GEDAS is an industrial rack-mount Intel Pentium based PC computer operating at 233 MHz with multiple hard-drives, IO ports and ADAC devices. The GEDAS system records time, magnetic, and VLF data at 10 Hz. All positioning data is recorded at 1Hz. Data files are organized on a flight-by-flight basis in a proprietary binary format. The data is then converted post-flight to a Geosoft compatible format. Data can be downloaded from the system by either floppy disk or Iomega ZIP disk. Data can be delivered in the field by floppy, ZIP disk, Iomega JAZ disk or CD-ROM.

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5. DATA PROCESSING AND PRESENTATION All latitude/longitude positions in the databases are represented in the original WGS84 datum. All projected positions are expressed in the NAD83 datum. UTM coordinates are calculated in Zone 13N.

5.1 Total Field Leveling GOLDAK carried out conventional tie line leveling. This processing consists of the following basic streams: Positioning processing Magnetic leveling Altimeter processing Layout and production of maps All data processing and most of the map layout were done in Geosoft Oasis Montaj. Many custom routines have been developed and used to facilitate the process, particularly in map layout. Each can be discussed separately although there are many interdependencies. Positioning Data GOLDAK corrected the positioning data in the field. This data was acquired using Novatel 12 channel GPS receivers. Post-processing using Waypoint Consulting GrafNav software was done to enhance the positioning accuracy. This step, depending on baseline distance and ionospheric activity, brings accuracy to the 1-meter level. Flight path is also verifiable by the times and positions superimposed on the flight-path videotape. The video overlay generated by the GEDAS data system, displays the following data format: HH:MM:SS.S MM-DD-YY LAT TYPE LON UTME UTMN LOCX LOCY LINE# HAGL COG VEL Were HH:MM:SS.S is the data system time in UTC as set from GPS time at the last line start. MM-DD-YY is the UTC date. LAT and LON are the latest position update from the GPS in decimal degrees. TYPE is either ‘A’ for autonomous, or ‘D’ for a real-time differential type position. UTME and UTMN are the UTM coordinates of the last positioning fix. LOCX and LOCY are the local track coordinates relative to the survey grid origin. LINE# is the line number designation and HAGL is the radar altimeter derived height above the terrain. COG is the GPS indicated track over the ground in degrees true, while VEL is the aircraft velocity in meters per second. It should be noted that the 10Hz clock display is asynchronous from GPS time and may be subject to drift while on line. The clock is reset at the beginning of every line. The method for determining precise video time is to observe the 10Hz clock at the GPS position change just prior to the event of interest. Note the time of that GPS fix from the data file. Advance the video to the event and note the 10Hz clock again. Subtract the first 10Hz time from the first and add that time to the GPS fiducial time.

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Magnetic Data The first steps in verifying the magnetic data took place in the field. The base station data was monitored to ensure compliance with the contract specification. The fourth difference was also monitored carefully to find any sudden offsets or other problems in the data. Total Field Levelling The intention of tie line levelling is to apply a smoothly varying function to the measured data which results in the near identical values at the intersections of traverse and control lines. The most significant component of the correction is to accommodate the diurnal variation of the magnetic field and to accommodate altitude errors, GPS positioning errors, and system drift. Levelling of the data consists of the following steps:

1. Iterative application of best fit first and second order linear trends (with outliers removed) on traverse and control lines, successively, until resulting correction approaches zero.

2. Iterative application of long wavelength corrections on traverse and control lines until

correction approaches zero. In this case the correction is determined by applying an Akima spline to intersection mismatches and then filtering the levelling correction using non linear and long wavelength filters to enhance and isolate correction “features” which span several intersections. The lengths of the filters are based on the traverse & control line separations.

3. Force the intersections to match by applying 75% of remaining error to traverse lines and

remainder to the control lines. From this point on all corrections are designed to maintain the equality.

4. Smooth the resulting correction profiles to minimize “excess corrections” (EC). Excess

correction is the high frequency component of the correction profile which corresponds to the intersection interval or less. Two types of corrections are applied, iteratively, until the corrections approach zero:

a. If the sign of the control and traverse EC is the same then both lines are moved to

remove the smaller correction.

b. If an “EC feature” can be found on a line, similar to step 2 above, the feature is removed and the intersecting lines are adjusted to maintain equality.

5. At this point the correction profiles are as smooth as possible, but small corrections to the

network may be necessary to remove along line features which are visible in the second vertical derivative (2VG). These are performed manually on individual intersections, or sets of intersections, with the goal of removing pulls in the 2VG without introducing sharp changes in the leveling network

6. Manual corrections may be necessary between tie lines to remove splining artifacts or

diurnal activity which is too fast to be removed by the tie line network.

Gradient Levelling Tie line leveling doesn’t work as well for gradient data, largely because the sources of error vary at a greater rate than the tie line separation, and there are many more areas where the rate of change is high, magnifying the problem. Instead Goldak Airborne Surveys relies on the fact that the gradients oscillate around zero, and reduces the data to meet that criteria.

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1. Data is normalized by scaling by the sensor separation and “flipping” lines of alternating directions. Gradients output by the compensator are left sensor minus the right sensor for lateral (GX) and the average of left and right minus the tail sensor for longitudinal (GY). The normalized GX is orientated so that a positive gradient is produced when the eastern sensor reads a higher value than the western sensor. Likewise the normalized GY is such that a positive gradient indicates a higher value on the northern sensor. On Tie lines the GX and GY channels are interchanged to maintain the relationship. The vertical gradient requires no normalization.

2. Median filter length is determined by experimentation. The goal is to find a filter which

removes all energy from gradient anomalies. A typical result, which was used on this data, is 30 seconds.

3. A baseline for each line is determined by applying the median filter followed by a low pass

convolution filter of equal length. 4. The baseline is removed from the measured gradient to produce the levelled gradient. 5. Gradient is gridded and examined for pulls which can occur when not enough or too much

baseline is removed. Individual lines may be re-filtered to correct. 6. Gradients calculated from the levelled mag can be used at this stage to “tune” the baselines

of the levelled gradients 7. East and North gradients are calculated by rotating the measured levelled gradients.

5.2 Altitude Data Part of the GPS positioning processing involves calculation of the height above sea level. This component of the position is the least reliable, however with suitable care should be accurate to within 2-3 meters. The barometric altimeter is calibrated for the air pressure at the beginning of each flight and allowed to drift from that point. The drift is very similar to the magnetic diurnal in that it varies both in time and in space. It is quite possible that the air pressure would vary significantly from one end of the survey block to the other on a large area. At this point the derived topography was generated for post-processed GPSZ minus radar altitude, gridded and compared with the known topography.

5.3 Digital Data Files Digital data has been provided on ISO CD-ROM in standard Geosoft .GDB format. The fields included are as follows: Balt BAROMETRIC ALTIMETER (m) BaseMag1 DIURNAL BASE MAGNETIC FIELD STATION 1 (nT) BaseMag2 DIURNAL BASE MAGNETIC FIELD STATION 2 (nT) DEM DIGITAL ELEVATION MODEL USED FOR NAVIGATION (m) DGPSZ DIFFERENTIALLY CORRECTED GPS ALTITUDE (m MSL) DLat DIFFERENTIALLY CORRECTED GPS LATITUDE (degrees) DLon DIFFERENTIALLY CORRECTED GPS LONGITUDE (degrees) GTIME GPS TIME (seconds after midnight) GXc LATERAL GRADIENT, COMPENSATED

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GXc_Lag LATERAL GRADIENT, LAGGED (nT/m) Gx_final LEVELLED LATERAL GRADIENT (nT/m) GXn LATERAL GRADIENT, NORMALIZED (nT/m) GXu LATERAL GRADIENT, UNCOMPENSATED (nT/m) GYc LONGITUDINAL GRADIENT, COMPENSATED (nT/m) GYc_Lag LONGITUDINAL GRADIENT, LAGGED (nT/m) Gy_final LEVELLED LONGITUDINAL GRADIENT (nT/m) GYn LONGITUDINAL GRADIENT, NORMALIZED (nT/m) GYu LONGITUDINAL GRADIENT, UNCOMPENSATED (nT/m) GZc VERTICAL GRADIENT, COMPENSATED (nT/m) GZc_Lag VERTICAL GRADIENT, LAGGED (nT/m) Gz_final LEVELLED VERTICAL GRADIENT (nT/m) GZn VERTICAL GRADIENT, NORMALIZED (nT/m) GZu VERTICAL GRADIENT, UNCOMPENSATED (nT/m) MagFinal TIE LINE LEVELLED TOTAL MAGNETIC FIELD [MBC_Lag] (nT) MBc LOWER TAIL MAG, COMPENSATED (nT) MBc_Lag LOWER TAIL MAG, COMPENSATED, LAGGED (nT) MBu LOWER TAIL MAG, UNCOMPENSATED (nT) MLc LEFT WING MAG, COMPENSATED (nT) MLc_Lag LEFT WING MAG, COMPENSATED, LAGGED (nT) MLu LEFT WING MAG, UNCOMPENSATED (nT) MRc RIGHT WING MAG, COMPENSATED (nT) MRc_Lag RIGHT WING MAG, COMPENSATED, LAGGED (nT) MRu RIGHT WING MAG, UNCOMPENSATED (nT) MTc UPPER TAIL MAG, COMPENSATED (nT) MTc_Lag UPPER TAIL MAG, COMPENSATED, LAGGED (nT) MTu UPPER TAIL MAG, UNCOMPENSATED (nT) Radartopo APPARENT TOPOGRAPHY [DGPSZ-Ralt1_Lag] (m) Ralt1a RADAR ALTITUDE, PRIMARY ALTIMETER (m) Ralt1_Lag LAGGED RADAR ALTITUDE, PRIMARY ALTIMETER (m) Ralt2 RADAR ALTITUDE, SECONDARY ALTIMETER (m) Ralt2_Lag RADAR ALTITUDE (m) VMl RMS AADC VECTOR MAG, LONGITUDINAL (nT) VMt RMS AADC VECTOR MAG, TRANSVERSE (nT) VMtf RMS AADC VECTOR MAG, TOTAL FIELD (nT) VMv RMS AADC VECTOR MAG, VERTICAL (nT) X UTM EASTING [NAD83 ZONE 13 N] (m) Y UTM NORTHING [NAD83 ZONE 13 N] (m) The following grids were delivered: Magfinal.grd – Total Magnetic field (Lower Tail Mag) Gx.grd – Measured Lateral Gradient Gy.grd – Measured Longitudinal Gradient Gz.grd – Measured Vertical Gradient Radartopo.grd – Digital Topography

5.4 Map Products Goldak Airborne Surveys compiled and plotted the final maps in their Saskatoon office. Maps were plotted in the NAD83 datum, UTM Zone 13. A scale of 1:50,000 was used. The survey area was divided into 6 sections for mapping. The map divisions are denoted below. Two copies of the following maps (one per map division) were delivered on paper media, Geosoft MAP and PDF format.

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a_claims.map b_claims.map c_claims.map base map with claim boundaries d_claims.map e_claims.map f_claims.map a_hvg.map b_hvg.map c_hvg.map measured vertical gradient with horizontal gradient vectors d_hvg.map e_hvg.map f_hvg.map a_tf.map b_tf.map c_tf.map total magnetic field colour image with contours d_tf.map e_tf.map f_tf.map a_vg.map b_vg.map c_vg.map measured vertical gradient colour image with contours d_vg.map e_vg.map f_vg.map

Two copies of the following were delivered on film:

a_tf_bw.map b_tf_bw.map c_tf_bw.map total magnetic field contours with flight path d_tf_bw.map e_tf_bw.map f_tf_bw.map

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Illustration – Total Field Image With Map Sheet Divisions

5.4 Flight Path Video Flight path video for this survey is supplied on VHS tapes, one per flight. Times, positions, direction and speed are overlain on the tape for detailed flight path recovery if required. For this survey video was critical for identifying cultural anomalies.

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6. DETAILED EQUIPMENT SPECIFICATIONS Our detailed equipment technical specifications are as follows: Aircraft C-GJBA, C-GJBB Piper PA-31 Navajo

4m composite tail stinger w/ vertical gradiometer Demonstrated Figure of Merit < 0.9nT Sensor Separation

Lateral 584" 14.865m Longitudinal 384" 8.560 m Vertical 88” 2.229 m

Aircraft Magnetometers: Manufacturer: Geometrics Type and Model Number: Cesium G-822A Range in nT: 20,000 to 90,000 Sensitivity in nT: 0.005 Sampling Rate: 20Hz Base Station Magnetometer: Manufacturer: GEM Systems Type and Model Number: Overhauser GSM-19W Range in nT: 20,000 to 120,000 Sensitivity in nT: 0.01 Sampling Rate: 5Hz maximum (0.5Hz typical)

Solar Power Supply: 1 - Solarex MSX50

Base Station Data Loggers: Manufacturer: DAP Technologies Type and Model Number: Microflex PC9800 Media Type: Flash RAM (32 Mb) Real-time Magnetic Compensator: Manufacturer: RMS Instruments Type and Model Number: AADCII Range in nT: 20,000 to 100,000 Resolution in nT: 0.001 Sampling Rate: 20Hz Digital Acquisition System: Manufacturer: Goldak Exploration Technology Type and Model Number: GEDAS Sampling Rate: 20Hz Data Format: GEDAS binary Positioning Cameras:

Manufacturer: Panasonic Model: GPKR402 HRSV Lens: WV-LR4R5 4.5mm

FOV at 1000 feet AGL is 1040 x 1300 feet

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Barometric Altimeter: Manufacturer: Setra Type and Model Number: 270 Range: -1000 to 10,000 feet Resolution: 1 meter

Radar Altimeter 1 (C-GJBA):

Manufacturer Thompson CSF Type and Model Number: ERT-160 Range: 0-8000 feet Resolution: 1 meter Accuracy: 1-2%

Radar Altimeter 2 (C-GJBA): Manufacturer Terra Type and Model Number: TRA300 – TRI40 Range: 40-2500 feet Resolution: 1 meter Accuracy: 5-7%

Radar Altimeter 1 (C-GJBB): Manufacturer Terra Type and Model Number: TRA300 – TRI40

Radar Altimeter 2 (C-GJBB): Manufacturer Terra Type and Model Number: KRA 10a Range: 40-2500 feet Resolution: 1 meter Accuracy: 5-7%

Positioning System:

Manufacturer: Goldak Exploration Technology Ltd. Type and Model Number: GEDAS Displays: 10” color LCD graphical display

Graphic LCD pilot indicator GPS Subsystem:

GPS Receiver: Manufacturer Novatel Type and Model Number: 3151R dual-frequency Propak

GPS Real Time Differential Receiver:

Manufacturer Racal Type and Model Number: Landstar

GPS Base Station:

Manufacturer Novatel Type and Model Number: 3151R dual-frequency Propak

System Resolution: 1 meter Overall accuracy: 3 m in real-time, <1m post-corrected

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Computers: Manufacturer: Sony

Type and Model Number: Pentium 3GHz, desktop PC

Manufacturer: Toshiba Type and Model Number: Pentium 2GHz, laptop PC Software Manufacturer: Geosoft Function: Geophysical data processing Type and Model Number: Oasis Montaj v 5.1.8 Manufacturer: Waypoint Consulting Function: GPS post-processing Type and Model Number: GrafNav

Illustration – Survey Aircraft 3-View

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7. STATEMENT OF QUALIFICATIONS Ben Goldak I reside at 25 Duncan Crescent in Saskatoon, Saskatchewan. I hold a B.Sc. Adv. in Computer Science from the University of Saskatchewan. I have been active in the field of geophysics since 1980. I have examined the data referred to in this report and find it to be of suitable quality for purposes of geological interpretation. I am President of Goldak Exploration Technology Ltd. Ben Goldak August, 2004

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APPENDIX A: COMPENSATION FLIGHT Results of a compensation flight flown with aircraft C-GJBA April 2nd, 2004:

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Results of a compensation flight flown with aircraft C-GJBB May 31st, 2004:

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Results of a compensation flight flown with aircraft C-GJBB June 4th, 2004:

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APPENDIX B

LIST OF CLAIMS

Claim no. Owners Area (hectares) Recording DateS-105626 101047025 SASKATCHEWAN LTD. 100% 125 May 6, 97S-107151 101047025 SASKATCHEWAN LTD. 100% 511 Jan 10, 03S-107152 101047025 SASKATCHEWAN LTD. 100% 483 Jan 10, 03S-107153 101047025 SASKATCHEWAN LTD. 100% 866 Jan 10, 03S-107158 101047025 SASKATCHEWAN LTD. 100% 718 Jul 28, 03S-107159 101047025 SASKATCHEWAN LTD. 100% 512 Jul 28, 03S-107160 101047025 SASKATCHEWAN LTD. 100% 468 Jul 28, 03S-135928 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135929 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135930 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135931 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135932 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135933 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135934 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135935 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135936 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135937 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135938 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135939 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135940 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135941 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135942 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135943 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135944 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135945 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135946 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135947 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135948 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135949 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135950 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135951 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135952 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135953 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135954 101047025 SASKATCHEWAN LTD. 100% 96 Aug 1, 03S-135955 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135956 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135957 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135958 101047025 SASKATCHEWAN LTD. 100% 64 Aug 1, 03S-135959 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135960 101047025 SASKATCHEWAN LTD. 100% 32 Aug 1, 03S-135961 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135962 101047025 SASKATCHEWAN LTD. 100% 32 Aug 1, 03S-135963 101047025 SASKATCHEWAN LTD. 100% 96 Aug 1, 03S-135964 101047025 SASKATCHEWAN LTD. 100% 128 Aug 1, 03S-135965 101047025 SASKATCHEWAN LTD. 100% 192 Aug 1, 03S-135966 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135967 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135968 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135969 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135970 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135971 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03

S-135972 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135973 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135974 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135975 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135976 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135977 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135978 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135979 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135980 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135981 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135982 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135983 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135984 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135985 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135986 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135987 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135988 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135989 101047025 SASKATCHEWAN LTD. 100% 128 Aug 1, 03S-135990 101047025 SASKATCHEWAN LTD. 100% 64 Aug 1, 03S-135991 101047025 SASKATCHEWAN LTD. 100% 64 Aug 1, 03S-135992 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135993 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135994 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135995 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135996 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135997 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135998 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-135999 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-136000 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-136001 101047025 SASKATCHEWAN LTD. 100% 128 Aug 1, 03S-136002 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-136003 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-136004 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-136005 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-136006 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-136007 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-136008 101047025 SASKATCHEWAN LTD. 100% 128 Aug 1, 03S-136009 101047025 SASKATCHEWAN LTD. 100% 32 Aug 1, 03S-136010 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-136011 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-136012 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-136013 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-136014 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-136015 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-136016 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-136017 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-136018 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-136019 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-136020 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-136021 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-136022 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03S-136023 101047025 SASKATCHEWAN LTD. 100% 256 Aug 1, 03







S-136345 101047025 SASKATCHEWAN LTD. 100% 256 Aug 27, 03S-136346 101047025 SASKATCHEWAN LTD. 100% 256 Aug 27, 03S-136347 101047025 SASKATCHEWAN LTD. 100% 256 Aug 27, 03S-136348 101047025 SASKATCHEWAN LTD. 100% 256 Aug 27, 03S-136349 101047025 SASKATCHEWAN LTD. 100% 256 Aug 27, 03S-136350 101047025 SASKATCHEWAN LTD. 100% 256 Aug 27, 03S-136351 101047025 SASKATCHEWAN LTD. 100% 256 Aug 27, 03S-136352 101047025 SASKATCHEWAN LTD. 100% 256 Aug 27, 03S-136353 101047025 SASKATCHEWAN LTD. 100% 256 Aug 27, 03S-136354 101047025 SASKATCHEWAN LTD. 100% 256 Aug 27, 03S-136355 101047025 SASKATCHEWAN LTD. 100% 256 Aug 27, 03S-136356 101047025 SASKATCHEWAN LTD. 100% 256 Aug 27, 03S-136357 101047025 SASKATCHEWAN LTD. 100% 256 Aug 27, 03S-136358 101047025 SASKATCHEWAN LTD. 100% 256 Aug 27, 03S-136359 101047025 SASKATCHEWAN LTD. 100% 256 Aug 27, 03S-136360 101047025 SASKATCHEWAN LTD. 100% 192 Sep 2, 03S-136361 101047025 SASKATCHEWAN LTD. 100% 48 Sep 2, 03S-136362 101047025 SASKATCHEWAN LTD. 100% 64 Sep 2, 03S-136363 101047025 SASKATCHEWAN LTD. 100% 48 Sep 2, 03S-136364 101047025 SASKATCHEWAN LTD. 100% 32 Sep 2, 03S-136365 101047025 SASKATCHEWAN LTD. 100% 96 Sep 2, 03S-136368 101047025 SASKATCHEWAN LTD. 100% 64 Sep 2, 03S-136369 101047025 SASKATCHEWAN LTD. 100% 128 Sep 2, 03S-136371 101047025 SASKATCHEWAN LTD. 100% 192 Sep 2, 03S-136372 101047025 SASKATCHEWAN LTD. 100% 48 Sep 2, 03S-136373 101047025 SASKATCHEWAN LTD. 100% 128 Sep 2, 03S-136374 101047025 SASKATCHEWAN LTD. 100% 128 Sep 2, 03S-136377 101047025 SASKATCHEWAN LTD. 100% 256 Oct 1, 03S-136378 101047025 SASKATCHEWAN LTD. 100% 256 Oct 1, 03S-136379 101047025 SASKATCHEWAN LTD. 100% 256 Oct 1, 03S-136380 101047025 SASKATCHEWAN LTD. 100% 256 Oct 1, 03S-136381 101047025 SASKATCHEWAN LTD. 100% 256 Oct 1, 03S-136382 101047025 SASKATCHEWAN LTD. 100% 256 Oct 1, 03S-136383 101047025 SASKATCHEWAN LTD. 100% 256 Oct 1, 03S-136384 101047025 SASKATCHEWAN LTD. 100% 256 Oct 1, 03S-136385 101047025 SASKATCHEWAN LTD. 100% 241 Oct 1, 03S-136386 101047025 SASKATCHEWAN LTD. 100% 256 Oct 1, 03S-136387 101047025 SASKATCHEWAN LTD. 100% 256 Oct 1, 03S-136388 101047025 SASKATCHEWAN LTD. 100% 256 Oct 1, 03S-136389 101047025 SASKATCHEWAN LTD. 100% 256 Oct 1, 03S-136390 101047025 SASKATCHEWAN LTD. 100% 256 Oct 1, 03S-136391 101047025 SASKATCHEWAN LTD. 100% 1024 Oct 1, 03S-136392 101047025 SASKATCHEWAN LTD. 100% 1024 Oct 1, 03S-136393 101047025 SASKATCHEWAN LTD. 100% 1024 Oct 1, 03S-136394 101047025 SASKATCHEWAN LTD. 100% 1024 Oct 1, 03S-136395 101047025 SASKATCHEWAN LTD. 100% 1024 Oct 1, 03S-136396 101047025 SASKATCHEWAN LTD. 100% 1024 Oct 1, 03S-136397 101047025 SASKATCHEWAN LTD. 100% 1024 Oct 1, 03S-136398 101047025 SASKATCHEWAN LTD. 100% 1024 Oct 1, 03S-136399 101047025 SASKATCHEWAN LTD. 100% 1024 Oct 1, 03S-136400 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136401 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03

S-136402 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136403 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136404 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136405 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136406 101047025 SASKATCHEWAN LTD. 100% 256 Oct 1, 03S-136407 101047025 SASKATCHEWAN LTD. 100% 384 Oct 1, 03S-136408 101047025 SASKATCHEWAN LTD. 100% 256 Oct 1, 03S-136409 101047025 SASKATCHEWAN LTD. 100% 64 Oct 1, 03S-136410 101047025 SASKATCHEWAN LTD. 100% 96 Oct 1, 03S-136411 101047025 SASKATCHEWAN LTD. 100% 160 Oct 1, 03S-136412 101047025 SASKATCHEWAN LTD. 100% 256 Oct 1, 03S-136413 101047025 SASKATCHEWAN LTD. 100% 256 Oct 1, 03S-136414 101047025 SASKATCHEWAN LTD. 100% 256 Oct 1, 03S-136415 101047025 SASKATCHEWAN LTD. 100% 256 Oct 1, 03S-136416 101047025 SASKATCHEWAN LTD. 100% 256 Oct 1, 03S-136417 101047025 SASKATCHEWAN LTD. 100% 640 Oct 1, 03S-136418 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136419 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136420 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136421 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136422 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136423 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136424 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136425 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136426 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136427 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136428 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136429 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136430 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136431 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136432 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136433 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136434 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136435 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136436 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136437 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136438 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136439 101047025 SASKATCHEWAN LTD. 100% 384 Oct 1, 03S-136440 101047025 SASKATCHEWAN LTD. 100% 256 Oct 1, 03S-136441 101047025 SASKATCHEWAN LTD. 100% 384 Oct 1, 03S-136442 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136443 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136444 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136445 101047025 SASKATCHEWAN LTD. 100% 384 Oct 1, 03S-136446 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136447 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136448 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136449 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136450 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136451 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136452 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136453 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03

S-136454 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136455 101047025 SASKATCHEWAN LTD. 100% 192 Oct 1, 03S-136456 101047025 SASKATCHEWAN LTD. 100% 384 Oct 1, 03S-136457 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136458 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136459 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136460 101047025 SASKATCHEWAN LTD. 100% 192 Oct 1, 03S-136461 101047025 SASKATCHEWAN LTD. 100% 384 Oct 1, 03S-136462 101047025 SASKATCHEWAN LTD. 100% 768 Oct 1, 03S-136463 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136464 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136465 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136466 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136467 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136468 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136469 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136470 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136471 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136472 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136473 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136474 101047025 SASKATCHEWAN LTD. 100% 490 Oct 1, 03S-136475 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136476 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136477 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136478 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136479 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136480 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136481 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136482 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136483 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136484 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136485 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136486 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136487 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136488 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136489 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136490 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136491 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136492 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136493 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136494 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136495 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136496 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136497 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136498 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136499 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136500 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136501 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136502 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136503 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136504 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136505 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03

S-136506 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136507 101047025 SASKATCHEWAN LTD. 100% 384 Oct 1, 03S-136508 101047025 SASKATCHEWAN LTD. 100% 192 Oct 1, 03S-136509 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136510 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136511 101047025 SASKATCHEWAN LTD. 100% 256 Oct 1, 03S-136512 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136513 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136514 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136515 101047025 SASKATCHEWAN LTD. 100% 640 Oct 1, 03S-136516 101047025 SASKATCHEWAN LTD. 100% 128 Oct 1, 03S-136517 101047025 SASKATCHEWAN LTD. 100% 128 Oct 1, 03S-136518 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136519 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136520 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136521 101047025 SASKATCHEWAN LTD. 100% 128 Oct 1, 03S-136522 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136523 101047025 SASKATCHEWAN LTD. 100% 256 Oct 1, 03S-136524 101047025 SASKATCHEWAN LTD. 100% 256 Oct 1, 03S-136525 101047025 SASKATCHEWAN LTD. 100% 384 Oct 1, 03S-136526 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136527 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136528 101047025 SASKATCHEWAN LTD. 100% 512 Oct 1, 03S-136529 101047025 SASKATCHEWAN LTD. 100% 768 Oct 1, 03S-136743 101047025 SASKATCHEWAN LTD. 100% 192 Dec 23, 03S-136744 101047025 SASKATCHEWAN LTD. 100% 192 Dec 23, 03S-136745 101047025 SASKATCHEWAN LTD. 100% 128 Dec 23, 03S-136746 101047025 SASKATCHEWAN LTD. 100% 256 Dec 23, 03S-136747 101047025 SASKATCHEWAN LTD. 100% 240 Dec 23, 03S-136748 101047025 SASKATCHEWAN LTD. 100% 192 Dec 23, 03S-136749 101047025 SASKATCHEWAN LTD. 100% 192 Dec 23, 03S-136750 101047025 SASKATCHEWAN LTD. 100% 96 Dec 23, 03S-136751 101047025 SASKATCHEWAN LTD. 100% 96 Dec 23, 03S-136752 101047025 SASKATCHEWAN LTD. 100% 576 Dec 23, 03S-136753 101047025 SASKATCHEWAN LTD. 100% 384 Dec 23, 03S-136754 101047025 SASKATCHEWAN LTD. 100% 64 Dec 23, 03S-136755 101047025 SASKATCHEWAN LTD. 100% 256 Dec 23, 03S-136756 101047025 SASKATCHEWAN LTD. 100% 256 Dec 23, 03S-136757 101047025 SASKATCHEWAN LTD. 100% 256 Dec 23, 03S-136758 101047025 SASKATCHEWAN LTD. 100% 256 Dec 23, 03S-136759 101047025 SASKATCHEWAN LTD. 100% 256 Dec 23, 03S-136760 101047025 SASKATCHEWAN LTD. 100% 256 Dec 23, 03S-136761 101047025 SASKATCHEWAN LTD. 100% 256 Dec 23, 03S-136762 101047025 SASKATCHEWAN LTD. 100% 256 Dec 23, 03S-136763 101047025 SASKATCHEWAN LTD. 100% 256 Dec 23, 03S-136764 101047025 SASKATCHEWAN LTD. 100% 256 Dec 23, 03S-136765 101047025 SASKATCHEWAN LTD. 100% 256 Dec 23, 03S-136766 101047025 SASKATCHEWAN LTD. 100% 64 Dec 23, 03S-136767 101047025 SASKATCHEWAN LTD. 100% 255 Dec 23, 03S-136768 101047025 SASKATCHEWAN LTD. 100% 256 Dec 23, 03S-136769 101047025 SASKATCHEWAN LTD. 100% 256 Dec 23, 03S-136770 101047025 SASKATCHEWAN LTD. 100% 256 Dec 23, 03

S-136771 101047025 SASKATCHEWAN LTD. 100% 256 Dec 23, 03S-136772 101047025 SASKATCHEWAN LTD. 100% 256 Dec 23, 03S-136773 101047025 SASKATCHEWAN LTD. 100% 256 Dec 23, 03S-136774 101047025 SASKATCHEWAN LTD. 100% 256 Dec 23, 03S-136775 101047025 SASKATCHEWAN LTD. 100% 256 Dec 23, 03S-136776 101047025 SASKATCHEWAN LTD. 100% 256 Dec 23, 03S-136777 101047025 SASKATCHEWAN LTD. 100% 256 Dec 23, 03S-136778 101047025 SASKATCHEWAN LTD. 100% 256 Dec 23, 03S-136779 101047025 SASKATCHEWAN LTD. 100% 256 Dec 23, 03S-136782 101047025 SASKATCHEWAN LTD. 100% 64 Jan 2, 04S-136783 101047025 SASKATCHEWAN LTD. 100% 64 Jan 2, 04S-136784 101047025 SASKATCHEWAN LTD. 100% 64 Jan 2, 04S-136785 101047025 SASKATCHEWAN LTD. 100% 64 Jan 2, 04S-136786 101047025 SASKATCHEWAN LTD. 100% 192 Jan 2, 04S-136787 101047025 SASKATCHEWAN LTD. 100% 512 Jan 2, 04S-136788 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136789 101047025 SASKATCHEWAN LTD. 100% 64 Jan 2, 04S-136790 101047025 SASKATCHEWAN LTD. 100% 64 Jan 2, 04S-136791 101047025 SASKATCHEWAN LTD. 100% 64 Jan 2, 04S-136792 101047025 SASKATCHEWAN LTD. 100% 64 Jan 2, 04S-136793 101047025 SASKATCHEWAN LTD. 100% 64 Jan 2, 04S-136794 101047025 SASKATCHEWAN LTD. 100% 48 Jan 2, 04S-136795 101047025 SASKATCHEWAN LTD. 100% 128 Jan 2, 04S-136796 101047025 SASKATCHEWAN LTD. 100% 384 Jan 2, 04S-136797 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136798 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136799 101047025 SASKATCHEWAN LTD. 100% 384 Jan 2, 04S-136800 101047025 SASKATCHEWAN LTD. 100% 512 Jan 2, 04S-136801 101047025 SASKATCHEWAN LTD. 100% 384 Jan 2, 04S-136802 101047025 SASKATCHEWAN LTD. 100% 64 Jan 2, 04S-136803 101047025 SASKATCHEWAN LTD. 100% 512 Jan 2, 04S-136804 101047025 SASKATCHEWAN LTD. 100% 512 Jan 2, 04S-136805 101047025 SASKATCHEWAN LTD. 100% 1022 Jan 2, 04S-136806 101047025 SASKATCHEWAN LTD. 100% 896 Jan 2, 04S-136807 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136808 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136809 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136810 101047025 SASKATCHEWAN LTD. 100% 64 Jan 2, 04S-136811 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136812 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136813 101047025 SASKATCHEWAN LTD. 100% 64 Jan 2, 04S-136814 101047025 SASKATCHEWAN LTD. 100% 52 Jan 2, 04S-136815 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136816 101047025 SASKATCHEWAN LTD. 100% 512 Jan 2, 04S-136817 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136818 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136819 101047025 SASKATCHEWAN LTD. 100% 160 Jan 2, 04S-136820 101047025 SASKATCHEWAN LTD. 100% 496 Jan 2, 04S-136821 101047025 SASKATCHEWAN LTD. 100% 384 Jan 2, 04S-136822 101047025 SASKATCHEWAN LTD. 100% 32 Jan 2, 04S-136823 101047025 SASKATCHEWAN LTD. 100% 96 Jan 2, 04S-136824 101047025 SASKATCHEWAN LTD. 100% 512 Jan 2, 04

S-136825 101047025 SASKATCHEWAN LTD. 100% 128 Jan 2, 04S-136826 101047025 SASKATCHEWAN LTD. 100% 512 Jan 2, 04S-136827 101047025 SASKATCHEWAN LTD. 100% 512 Jan 2, 04S-136828 101047025 SASKATCHEWAN LTD. 100% 512 Jan 2, 04S-136829 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136830 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136831 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136832 101047025 SASKATCHEWAN LTD. 100% 896 Jan 2, 04S-136833 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136834 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136835 101047025 SASKATCHEWAN LTD. 100% 128 Jan 2, 04S-136836 101047025 SASKATCHEWAN LTD. 100% 512 Jan 2, 04S-136837 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136838 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136839 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136840 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136841 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136842 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136843 101047025 SASKATCHEWAN LTD. 100% 64 Jan 2, 04S-136844 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136845 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136846 101047025 SASKATCHEWAN LTD. 100% 192 Jan 2, 04S-136847 101047025 SASKATCHEWAN LTD. 100% 768 Jan 2, 04S-136848 101047025 SASKATCHEWAN LTD. 100% 192 Jan 2, 04S-136849 101047025 SASKATCHEWAN LTD. 100% 192 Jan 2, 04S-136850 101047025 SASKATCHEWAN LTD. 100% 320 Jan 2, 04S-136851 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136852 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136853 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136854 101047025 SASKATCHEWAN LTD. 100% 1008 Jan 2, 04S-136855 101047025 SASKATCHEWAN LTD. 100% 992 Jan 2, 04S-136856 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136857 101047025 SASKATCHEWAN LTD. 100% 992 Jan 2, 04S-136858 101047025 SASKATCHEWAN LTD. 100% 448 Jan 2, 04S-136859 101047025 SASKATCHEWAN LTD. 100% 512 Jan 2, 04S-136860 101047025 SASKATCHEWAN LTD. 100% 128 Jan 2, 04S-136861 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136862 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136863 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136864 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136865 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136866 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136867 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136868 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136869 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136870 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136871 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136872 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136873 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136874 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136875 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136876 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04

S-136877 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136878 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136879 101047025 SASKATCHEWAN LTD. 100% 512 Jan 2, 04S-136880 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136881 101047025 SASKATCHEWAN LTD. 100% 224 Jan 2, 04S-136882 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136883 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136884 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136885 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136886 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136887 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136888 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136889 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136890 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136891 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136892 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136893 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136894 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136895 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136896 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136897 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136898 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136899 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136900 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136901 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136902 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136903 101047025 SASKATCHEWAN LTD. 100% 1280 Jan 2, 04S-136904 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136905 101047025 SASKATCHEWAN LTD. 100% 512 Jan 2, 04S-136906 101047025 SASKATCHEWAN LTD. 100% 384 Jan 2, 04S-136907 101047025 SASKATCHEWAN LTD. 100% 768 Jan 2, 04S-136908 101047025 SASKATCHEWAN LTD. 100% 1024 Jan 2, 04S-136909 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136910 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136911 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136912 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136913 101047025 SASKATCHEWAN LTD. 100% 96 Jan 2, 04S-136914 101047025 SASKATCHEWAN LTD. 100% 96 Jan 2, 04S-136915 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136916 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136917 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136918 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136919 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136920 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136921 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136922 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136923 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136924 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136925 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136926 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136927 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136928 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04

S-136929 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136930 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136931 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136932 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136933 101047025 SASKATCHEWAN LTD. 100% 128 Jan 2, 04S-136934 101047025 SASKATCHEWAN LTD. 100% 128 Jan 2, 04S-136935 101047025 SASKATCHEWAN LTD. 100% 128 Jan 2, 04S-136936 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136937 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136938 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136939 101047025 SASKATCHEWAN LTD. 100% 128 Jan 2, 04S-136940 101047025 SASKATCHEWAN LTD. 100% 64 Jan 2, 04S-136941 101047025 SASKATCHEWAN LTD. 100% 239 Jan 2, 04S-136942 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136943 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136944 101047025 SASKATCHEWAN LTD. 100% 106 Jan 2, 04S-136945 101047025 SASKATCHEWAN LTD. 100% 128 Jan 2, 04S-136946 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136947 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136948 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136949 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136950 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136951 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136952 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136953 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-136954 101047025 SASKATCHEWAN LTD. 100% 256 Jan 2, 04S-137082 101047025 SASKATCHEWAN LTD. 100% 256 Feb 16, 04S-137083 101047025 SASKATCHEWAN LTD. 100% 48 Feb 16, 04S-137084 101047025 SASKATCHEWAN LTD. 100% 256 Feb 16, 04S-137085 101047025 SASKATCHEWAN LTD. 100% 64 Feb 16, 04S-137086 101047025 SASKATCHEWAN LTD. 100% 48 Feb 16, 04S-137250 101047025 SASKATCHEWAN LTD. 100% 512 Mar 1, 04S-137251 101047025 SASKATCHEWAN LTD. 100% 512 Mar 1, 04S-137252 101047025 SASKATCHEWAN LTD. 100% 512 Mar 1, 04S-137253 101047025 SASKATCHEWAN LTD. 100% 72 Mar 1, 04S-137338 101047025 SASKATCHEWAN LTD. 100% 96 Apr 1, 04S-137340 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137341 101047025 SASKATCHEWAN LTD. 100% 64 May 3, 04S-137342 101047025 SASKATCHEWAN LTD. 100% 640 May 3, 04S-137343 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137344 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137345 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137346 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137347 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137348 101047025 SASKATCHEWAN LTD. 100% 256 May 3, 04S-137349 101047025 SASKATCHEWAN LTD. 100% 64 May 3, 04S-137350 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137351 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137352 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137353 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137354 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137355 101047025 SASKATCHEWAN LTD. 100% 320 May 3, 04

S-137356 101047025 SASKATCHEWAN LTD. 100% 320 May 3, 04S-137357 101047025 SASKATCHEWAN LTD. 100% 320 May 3, 04S-137358 101047025 SASKATCHEWAN LTD. 100% 128 May 3, 04S-137359 101047025 SASKATCHEWAN LTD. 100% 320 May 3, 04S-137360 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137361 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137362 101047025 SASKATCHEWAN LTD. 100% 320 May 3, 04S-137363 101047025 SASKATCHEWAN LTD. 100% 320 May 3, 04S-137364 101047025 SASKATCHEWAN LTD. 100% 256 May 3, 04S-137365 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137366 101047025 SASKATCHEWAN LTD. 100% 96 May 3, 04S-137367 101047025 SASKATCHEWAN LTD. 100% 128 May 3, 04S-137368 101047025 SASKATCHEWAN LTD. 100% 384 May 3, 04S-137369 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137370 101047025 SASKATCHEWAN LTD. 100% 400 May 3, 04S-137371 101047025 SASKATCHEWAN LTD. 100% 256 May 3, 04S-137372 101047025 SASKATCHEWAN LTD. 100% 632 May 3, 04S-137373 101047025 SASKATCHEWAN LTD. 100% 128 May 3, 04S-137374 101047025 SASKATCHEWAN LTD. 100% 384 May 3, 04S-137375 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137376 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137377 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137378 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137379 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137380 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137381 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137382 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137383 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137384 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137385 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137386 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137387 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137388 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137389 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137390 101047025 SASKATCHEWAN LTD. 100% 128 May 3, 04S-137391 101047025 SASKATCHEWAN LTD. 100% 256 May 3, 04S-137392 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137393 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137394 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137395 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137396 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137397 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137398 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137399 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137400 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137401 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137402 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137403 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137404 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137405 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137406 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137407 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04

S-137408 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137409 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137410 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137411 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137412 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137413 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137414 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137415 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137416 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137417 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137418 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137419 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137420 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137421 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137422 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137423 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137424 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137425 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137426 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137427 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137428 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137429 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137430 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137431 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137432 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137433 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137434 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137435 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137436 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137437 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137438 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137439 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137440 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04S-137441 101047025 SASKATCHEWAN LTD. 100% 512 May 3, 04

Total Hectares 335083.00

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REGIONAL TRIAXIAL AEROMAGNETIC SURVEY ASSESSMENT WORK · PDF fileregional triaxial aeromagnetic survey assessment work report by n. ralph newson, m.sc., p. eng., p.geo. for 101047025