31M03SW2008 2.25722 HEBERT 010 NTS 31 M/4, 31 U13, 31 L/14
GROUND GEOPHYSICAL SURVEYS Magnetometer and VLF-EM Surveys - Phase two Assessment Report
Temagami Diamond Project
TRES-OR RESOURCES LTD. May 25, 2003
RECEIVED MAY 2 7 2003
Meegwich Consultants Inc. P.O. Box 482, Temagami, Ontario POH 2HO TeL (705) 569- 2904 Fax. (705) 569-2817 Temagami Diamond Project - Phase two Tres-Or Resources Ltd. Page 2
TABLE OF CONTENTS
1.0 Overview and Introduction 1.1 Summary of Work Performed 2.0 Property Description 3.0 Location and Access 4.0 Magnetometer Survey 4.1 Instrumentation 4.2 Survey Results and Interpretation 5.0 VLF-EM Survey 5.1 Instrumentation 5.2 Survey Results and Interpretation 6.0 Conclusions and Recommendations
LIST OF FIGURES Figure 1 Grid Location Map
LIST OF MAPS 1:5.000 Map 1 Total Field Magnetics Contours - TEMJM-0203 Grid Map 2 Total Field Magnetics Contours - Grids U73 and 306 Map 3 Total Field Magnetics Contours - Grids 310 and 311 Map 4 Total Field Magnetics Contours - Grid 312 Map 5 Total Field Magnetics Contours - Grid U53 Map 6 VLF-EM Profiles - Grids U73 and 306 Map 7 VLF-EM Profiles - Grids 310 and 311
APPENDIX Instrument specifications
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1.0 OVERVIEW AND INTRODUCTION:
Overview of target selected for ground geophysical surveys during May 2003; to accompany the report prepared by Meegwich Inc.
The targets covered by grids and ground geophysical surveys (total field magnetic and VLF-EM) were selected by A.W. Gourlay, P. Geol., Independent Geologist, using the following criteria: Airborne Geophysical Signature, proximity to till samples containing kimberlite indicator minerals, topography and site visits.
The Airborne Geophysical Signature of each target was derived from a 10,500 line kilometers fixed wing survey flown during 2002. The targets selected are discrete magnetic features, both in Total Magnetic Intensity and Measured Vertical Gradient, which are signatures comparable to known kimberlite pipes. The signatures may be either magnetic highs or magnetic lows. In some cases the target©s signature is seen in either the Total Magnetic Intensity or the Measured Vertical Gradient but not in both data sets. The compiled data from the fixed wing airborne survey has been reported in an assessment work filing.
Tres-Or Resources Ltd. carried out an extensive till sampling program during 2002, and a total of 631 samples were collected. Majority of these samples have been processed and sorted for kimberlite indicator minerals. The majority of the samples have returned anomalous numbers of kimberlite indicator minerals. The targets selected are up-ice from samples that returned kimberlite indicator minerals, and are between 500 meters and 2000 meters north of the anomalous sample sites. Results from over 350 of the till samples collected have been reported in assessment work filings.
The targets were also selected based on the topography of the airborne geophysical signature. Topographic lows, swamps and lakes are preferred based on the assumption that a kimberlite occurrence will be more readily eroded than the country rock and will most likely be manifested as a topographic depression.
The targets and grids were selected and located by A.W. Gourlay, P.Geol. based on his interpretation of the data and application of his extensive experience in the Lac de Gras area of the Northwest Territories. The area around the targets were investigated by A.W. Gourlay while he was on-site supervising a drill program in the Temagami area of Ontario during April 2003.
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In addition, the targets selected for grids were ground checked by P. Brown. P. Geo. and an assistant, in conjunction with the ground geophysical crews, during May 2003. P. Brown conducted geological examinations of each of the targets to determine if there was an obvious source of the airborne magnetic feature.
Ai/target overview for 30 May report by: A.Gourlay
1.1 Summary of Work Performed:
From May 1 to 24, 2003 a program of grid establishment, magnetometer surveying and VLF-EM surveying was carried out on five selected targets which are part of the extensive Temagami Diamond Project. The properties are held by Tres-Or Resources Ltd., of 1934-131 Street White Rock, B.C. V4A 7R7. The objective of the work was to test and ground locate airborne magnetic responses that have potential to be caused by kimberlite pipes or dikes. In addition the magnetic information should assist greatly in distinguishing the underlying geological units and associated structural features.
The grid preparation and surveying was done by Real Gauthier, Pierre Coulombe, Stephane Coulombe, and Tom Von Cardinal on behalf of Meegwich Consultants Inc. P.O. Box 482, Temagami, Ontario POH 2HO. David Laronde was the field supervisor and authored this work report. There was a total of 45.25 km of flagged and machete cut grid lines installed and surveyed with magnetometer on five grids. A total of 18.20 km was surveyed with VLF- EM. The baselines of the grids were located with GPS using the UTM NAD 83 co-ordinate system to ensure precise location. In addition the GPS position was monitored to track the crosslines as they were installed.
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Grid Summary Km Township TEM-N-0203 10.80 Eldridge Twp. U-73/306 15.25 Riddell Twp. 310/311 9.80 Riddell Twp. 312 7.10 Hartle Twp. U-53 2.30 Hebert Twp.
Total...... 45.25 km
2.0 PROPERTY:
The work was done on mining claims that are part of an extensive land holding covering several townships. Only the claims that were worked on are listed below.
GRID TP. CLAIM NO.
TEM-N-0203 Riddell Tp. 1248441 1248997 1243278 1243265
U73and306 Riddell Tp. 1248996 1248993 1248901
310 and 311 Riddell Tp. 1248908 1248909
312 Hartle Tp. 3005173 (newly recorded)
U53 Hebert Tp. 1248917 1248923
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3.0 LOCATION AND ACCESS:
The grids are scattered in an area southeast of Temagami. Grids U73 1 306 and also grid 310 1 311 are in Riddell Tp. are accessible by boat from Rabbit Lake. Grid TEM-N-0203 in Eldridge Tp. is also accessed from Rabbit Lake. Rabbit Lake has a number of public access points to put a boat in the water. The best boat launch is situated at the extreme south end of Rabbit Lake which is at km 7 along the Rabbit Lake Road.
Grid 312 is situated in Hartle Tp. near the west township boundary. The Rabbit Lake road cuts the grid in half near km 12.
Grid U53 in Hebert Tp. is also accessible by the Rabbit Lake Road at km 40.
Sudbury Mining Division NTS: 31 M/4, 31 L/12, 31 L/14
4.0 MAGNETOMETER SURVEY:
4.1 Instrumentation: Gem Systems GSM-19 overhauser magnetometers serial no. 58470 and 712776 were used for the field units in mobile mode. These units have an accuracy of +I- 1/100th of a gamma. An EDA Omni IV base station was used to monitor and correct for the diurnal variation during the course of the survey. This instrument reads to 1710th of a gamma resolution. The base station cycled at 20 second intervals.
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Survey Results and Interpretation: The results are presented in contour format on plans at 1:5000 scale. Quality control was monitored by surveying the baseline and then comparing the readings at the same station when the cross lines were surveyed. This cross-referencing technique confirms good data and checked out on these surveys. A total of 45.25 km of line was surveyed (3450 readings) at 12.5 meter intervals.
The results of the survey are discussed on a grid by grid basis as follows:
TEIYLN-0203 Grid: The readings fall in the 56,500 - 57,500 nT range. The survey picked up a series of isolated highs in the central section of the grid and also along the perimeter. These highs are typically 200-800 nT above a background range of 550 -650 nT. A partially covered high in the northwest corner of the grid appears to be more massive. The topography on the grid is severe since it covers a large, steep hill with several cliffs and ledges which account for several truncated survey lines. This area is underlain by sedimentary rock. The magnetic highs are somewhat interesting considering the shape and close pattern. Furthermore a bull©s eye magnetic high occurring on L 400 and 500 E at 150 N is coincident with a small pond.
Grids U73 and 306: The survey picked up two main features. The first is a large massive high in the northwest section of the grid where values range up to 300 nT above a background of 56,700 nT. It is interesting that this feature covers a topographic low area defined by a north-south trending flooded creek area. The second main feature is centered at 350 E on the baseline. At this point the readings are the highest at 100 nT above background. The shape is
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somewhat circular but narrow highs trending northwest-southeast off the southeast end suggest this is part of a dike. A second dike with the same trend can be seen 200 meters to the southwest. This dike runs off the grid to the south and into the massive high to the northwest. A third narrow dike is noted at the north part of the grid between L 300 and 900 E. The width of these dikes range from 25-35 meters. These dikes conspicuously trend with the regional swarm and are likely diabase.
Grids 310 and 311: The prominent feature on this grid is a semi-massive response located at the south central area of the grid along the south end of L 300 E. The most intense readings are on L 400 E at 750 S. There are several other isolated highs as well but these lack any pattern except for the possibility of dikes. All of these highs are low intensity responses being only 50-75 nT above a background of 650 nT.
Grid 312: A group of highs can be seen in the central portion of the grid. The sum of these highs make an elongated shape from 200 to 500 W and 50 S to 100 N. The highest reading are on L 500 W at 50 N. This response has an interesting shape and requires follow-up testing. Other isolated highs are noted along the north perimeter and also at 200 S on L 400 and 600 W. An intense massive feature is partially covered at the southeast corner of the grid. This is a di-polar response with intense values up to 1550 nT above background. A diabase or an ultramafic intrusive may be the source of this response.
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U-53 Grid: An east-west trending high can be seen at 150 S. This response is 100 meters wide on L 1000 W. Intensity ranges 500-600 nT above background. Another high further south is noted.
5.0 VLF-EM SURVEY: 18.20 km of line was surveyed for a total of 728 readings read at 25 meters intervals with the operator facing north at each station.
5.1 Instrumentation: A Geonics EM-16 VLF receiver was used for the VLF surveys to record in-phase and quadrature components of 1 VLF transmitting station: Cutler, Maine NAA transmitting at 24.0 kHz. The measured quantities are the in-phase and quadrature components of the vertical magnetic field measured as a percentage of horizontal primary field (read to a resolution of +I- 1 0Xo).
5.2 Survey Results: The results of the survey are presented in profile form on plans at 1: 5000 scale.
Grids U-73 and 306: The results of the survey are basically flat with the exception of a weakly conductive horizon at 300 N. The conductive horizon is segmented and off set.
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Grids 310 and 312: This grid has a very flat response with the VLF. The conductive lake bottom is however influencing the data as seen by a decrease in resistivity toward the shore from north to south.
6.0 CONCLUSIONS AND RECOMMENDATIONS:
The survey located and defined a number of the airborne responses accurately on the ground. Some of these need more work prior to drilling. These should be infilled with detailed magnetic coverage working around rugged topography and/or flooded lands. For the most part the targets were overburden covered however there are targets that could be examined in the field as a next logical step. The magnetic high with a coincident topographic low on grid TEMJM-0203 could be followed up in the field with geological mapping and detailed magnetic survey coverage with 50 meter line spacing. Grid U73 could also be covered with 50 meter line spacing during the winter to completely cover the western anomaly prior to drilling. Grid U-53 needs expanded coverage to outline responses encountered thus far.
Further assessment as to viability of a drill target should be based on the geometry of the response, intensity the magnetic response, presence of structure, presence of indicator minerals and topographic association. With these parameters as a guide a selection of recommended drill targets is listed as follows:
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Drill targets recommended
Grid Intensity Shape Topo low Structure
312 400 nT Elliptical possible splay faulting 306 150nT Elliptical beaver pond splay faulting
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References
Ontario Geologic Survey Map 2361 Geological Compilation Series
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CERTIFICATE OF AUTHOR
l, David Laronde of the town of Temagami, Ontario hereby certify:
1. That l am a geology technologist and have been engaged in mineral exploration for the past 23 years.
2. That l am a graduate of Cambrian College in Sudbury with a diploma in Geology Engineering Technology 1979.
3. That my knowledge of the property described herein was acquired by field work and documentation.
Dated at Temagami this 25th day of May 2003.
David Laronde
Meegwich Consultants Inc. P.O. Box 482, Temagami, Ontario POH 2HO TeL (705) 569-2904 Fax. (705) 569-2817 1 HEBERT i
S - U73 S 306^ 3
GRID LOCATION MAP TRES-OR RESOURCES
One cenlimctrc represents one kilometre GEM SYSTEMS GSM-19 OVERHAUSER MEMORY MAGNETOMETER GRADIOMETER
GEM SYSTEMS, INC.
MAOI IN CANADA
O OK 4 -4O'" OVERHAU8ER O O IVl "" IC7 MAGNETOMETER
SPECIFICATIONS
Resolution: ...... 0.01 nT(0.01 gamma). Absolute Accuracy: ...... 0.2nT. Range: ...... 20,000-1 SO.OOOnT,autotuning, manual override Gradient Tolerance: ...... Over lO.OOOnT/m. OPERATING MODES: Manual; ...... Automatic storage of label, time and date, magnetic field, 3 sec. minimum interval. Base Station: ...... 3 to 60 sec. intervals standard, others optional time, date, magnetic field stored. Remote Control: ...... The©same as manual but controlled through RS232C interlace. STORAGE CAPACITY: Manual Operation: ...... 3.800 standard, 30.000 optional; with 3 VLF stations 1,850 standard, 3,700 optional. Base Station: ...... 21,800 standard. 174,000 optional (24hr operation at 0.5 sec. interval). Gradiometer ...... 3.200 standard, 26,000 optional; with 3 VLF stations 1.700 standard, 3,400 optional. Power Consumption: ...... 2 Ws per reading, up to 0.5W standby, less than 0.4mW when off. PowerSource: ...... 12Vi.9Ah sealed lead acid battery standard, others optional. Operating Temperature: ...... -40to*60C Storage Temperahire: ...... ,-70tO*65 C. Input/output: ...... 6 pin weatherproof connector, RS-232C, and (optional) analog output. Dimensions: ...... Console 223 X69X 240mm Sensor staff 4 X 450mm sections Sensor 170 X 71 mm dia Weieht- ...... Console 2.1kg Staff 0.9 Kg Sensor 1.1kg Standard Package: ...... Console with batteries, harness Sensor with cable, connector Staff Standard accessories: Charger, manual,case Page l VLF-EM GEONICS
EM16 SPECIFICATIONS
MEASURED QUANTITY Inphase and quad-phase components of vertical magnetic field as a percentage of horizontal primary field. (i.e. tangent of the tilt angle and ellipticity). SENSITIVITY Inphase: 1501 Quad-phase: 401 RESOLUTION 1* OUTPUT Nulling by audio tone. Inphase in dication from mechanical inclinometer and quadphase from a graduated dial. OPERATING FREQUENCY 15-25 kHz (15-30 kHz optional) VLF Radio Band. Station selection done by means of plug-in units. OPERATOR CONTROLS ON/OFF switch, battery test push button, station selector switch, audio volume control, quadrature dial, inclinometer. POWER SUPPLY 6 disposable ©AA© cells. DIMENSIONS 53 x 21.5 x 28 cm WEIGHT Instrument: 1.8kg Shipping: 8.35 kg
CAUTION:
EMlb inclinometer may be damaged by exposure to temperatures below -30 0 c. Warranty does not cover inclinometers damaged by such exposure. COMPILATION AND REVIEW OF GROUND GEOPHYSICAL DATA AND TILL SAMPLING RESULTS
TRES-OR RESOURCES LTD.
Hartle, Riddell and Eldridge Townships and Herbert Township Temagami Diamond Claim Project Sudbury Mining Division Ontario
CONTIGUOUS CLAIMS S1248996, S1248997, S1248995, S1248994, S1248901, S1248993, S1248908, S1248909, S1248910, S1248992, S1248907, S1248906, S1248905, S1248904, S1248903, S1246394, S1246395, S1246389, S1246390, S1248441, S1243278, S1243265, S3005173, S1248917and S1248923
UTM Zone 17 NAD 83 Projection 5202500N to 5208900N 599000E to 607750E
Prepared by:
Laura Lee Duffett, P. Geo., B.C President, Tres-Or Resources Ltd. Phil Brown, P. Geo., ON Geological Consultant A.W. Gourlay, P. Geol., AB Geological Consultant
For Tres-Or Resources Ltd. RECEIVED May 28, 2003 MAY 2 9 2003
GEOSCIENCE ASSESSMENT OFFICE
31M03SW2008 2.25722 HEBERT 020 Summary
Tres-Or Resources Ltd. is exploring for diamonds in a large block of contiguous claims covering parts of 21 Townships in the Temagami - Marten River area. The claims are located 40 to 90 kilometres south of known diamondiferous kimberlites of the New Liskeard kimberlite field, in an area recently identified by government surveys as favourable for diamond-bearing kimberlites. During May 2002 Tres-Or contracted Goldak Exploration Technology Ltd. to complete a detailed fixed-wing, 3 axis gradient magnetometer survey over the project area. Regional geochemical sampling for kimberlite indicator minerals (KIM) returned anomalous numbers of kimberlitic indicators in Riddell, Eldridge and Askin Townships, and electron microprobe analyses of selected grains has confirmed that the indicator minerals are of kimberlitic origin. A number of kimberlite-like geophysical features were identified by Goldak Exploration Technology Ltd. and Ulrich Zimmer, Ph.D., P.Geoph. of Meridian Geoscience Ltd. in the same area.
Detailed ground magnetic and electromagnetic surveys were completed by Meegwich Consultants Inc. over selected airborne targets in Eldridge/Riddell Townships, Hartle and Hebert Townships during May 2003. The results of the ground geophysical surveys have been reviewed and targets have been identified that have magnetic signatures comparable to known kimberlite pipes. Additional ground surveys are recommended to further define these targets for drill testing. Property Description and Location Tres-Or©s Temagami Diamond Property consists of 435 contiguous mining land claim units in the Temagami area located in the Sudbury and Larder Lake Mining Divisions of northeastern Ontario. The 435 claims comprise 5177 claim units totaling 82,832 hectares, and are located on unpatented ground covered by lakes, swamps, forest and recently forested ground. The claims were staked between October 2001 and December 2001 by Norman Collins and Roland Collins for Leane Jolin and transferred to Tres-Or Resources Ltd. Two claims were re-staked and recorded by Meegwich Consultants Inc. on behalf of Tres-Or Resources Ltd. in Hartle Township in May 2003, prior to any grid work being completed on the property (Figure 1 - Claim Location Map). The work performed and discussed in this report cover parts of claims located in Riddell, Eldridge, Hartle and Hebert Townships (Table 1). Tres-Or is 10007o owner of the claims, except for 2.507o Net Smelter Return (NSR) retained by vendors. Grids U73 and 306 — ELDRIDGE
TEM N-0203 Grid
Grids 310 and 311
Jt ** Grid 312 CLAIM MAP AND GRID LOCATIONS FROM : PGEOPH1L FOX NO. 7057521123 May. 28 2003 04:28PM PI
Application to Record Sump Ontario Staked Mining Ciaim(o) Mining Aet, Subjection 44f!), R.S.0.1980
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77 \ TT TROT://T/co FROM : PGEOPH1L FAX NO. : 7057521123 May. 2B 2003 04:36PM PI
Skerch Please complete sketch In Ink.
f*? applicable, tne items indicated on trs sample sketch on Pert B must be shown Magnetic Declination Used (For current iota, ssk at the G r-oup Sketch of claims iistec on Part A. Sketch or plan of the mining dalmas) must Reoarder©s Office ) shew the c&fner posts, witness posts, and fine posts, sno the distances between the POSIS i" Scale include topographic features Such as lakes, rivers, creeks, ponds, etc. and aeveiop.meits sucn as hydro lines, highways, railways, pipelines, buildings, etc. as © shown on sketch in Part B. f " Refer to sample sketc.T on Part 8. Table 1
Claim List
Township Claim Number Recording Date Claim Due Date
Riddell S1248996 2001-May-30 2003- •May-30 Riddell S1248993 2001-May-30 2003- •May-30 Riddell S1248908 2001-May-30 2003- •May-30 Riddell S1248901 2001-May-30 2003- •May-30 Riddell S1248909 2001-May-30 2003- •May-30 Riddell 51248903 2001-May-30 2003- •May-30 Riddell 51248904 2001-May-30 2003- •May-30 Riddell 51248905 2001-May-30 2003- •May-30 Riddell 51246394 2001-May-30 2003- •May-30 Riddell 51246395 2001-May-30 2003- •May-30 Eldridge S1248997 2001-May-30 2003- May-30 Eldridge 51248994 2001-May-30 2003- •May-30 Eldridge 51248995 2001-May-30 2003- •May-30 Eldridge S1248910 2001-May-30 2003- May-30 Eldridge 51248906 2001-May-30 2003- •May-30 Eldridge 51248907 2001-May-30 2003- May-30 Eldridge S1248992 2001-May-30 2003- •May-30 Eldridge 51246389 2001-May-30 2003- •May-30 Eldridge 51246390 2001-May-30 2003- •May-30 Eldridge S1248441 2001-Sept-07 2003- •Sept-07 Eldridge S1243278 2001-Sept-07 2003- •Sept-07 Eldridge S1243265 2001-Aug-17 2003-•Aug-17 Hartle S3005173 2003-May Hebert S1248917 2001-Dec-04 2003-Dec-04 Hebert S1248923 2001-Dec-04 2003-Dec-04 Fixed-Wing Magnetic Survey
The fixed-wing measured vertical and horizontal magnetic gradient survey was completed under contract by Goldak Exploration Technology Ltd., during May and June of 2002. The survey was flown on north-south flight lines spaced 150 metres apart, at an elevation of 90 metres over the entire Tres-Or Temagami claim area. Details of this survey have been reported in an Assessment Report dated October 10, 2002 (W0270.01595).
A number of magnetic anomalies with signatures comparable to known kimberlite pipes were identified by Goldak Exploration Technology Ltd., and Ulrich Zimmer, P.h.D., P.Geoph. of Meridian Geoscience Ltd. Follow-up ground magnetic surveys were initiated to provide detailed data of specific targets. An electromagnetic survey was recommended to further define structures related to potential kimberlite emplacement.
Ground Magnetic and Electromagnetic Survey
The targets covered by grids and ground geophysical surveys (total field magnetic and VLF-EM) were selected by A.W. Gourlay, P. Geol., Independent Geologist, using the following criteria: Airborne Geophysical Signature, proximity to till samples containing kimberlite indicator minerals, topography and site visits.
The ground magnetic and electromagnetic surveys were completed by Meegwich Consultants Inc. during May 2003. The ground surveys completed include five grids covering seven airborne geophysical targets. Three grids are located in Eldridge/Riddell Townships, the other two grids cover targets in Hartle and Hebert Townships. The data was collected on cut, chained and flagged, north- south lines spaced 100 metres apart. A total of 45.5 line kilometres of survey, including tielines, were completed. Details of the ground surveys have been reported in an accompanying Assessment Report compiled by Meegwich Consultants Inc. and dated May 26, 2003.
Review of Kimberlite Indicator Mineral Sampling
As part of an extensive till sampling program carried out by Tres-Or Resources Ltd. during 2002 over the Temagami Diamond Claim Project, a fence of samples were collected along the shoreline of Rabbit Lake. Details of the till sampling program have been reported in Assessment Reports dated November 7, 2002 (W0270.01774) and February 27, 2003 (W0370.00320).
As part of this extensive till sampling program, a review of the surficial geology applicable to the Temagami area was mapped and reported in the detailed assessment report. A summary of the glacial history is provided as a reference in Appendix l. In summary, most of the glacial striae observed and mapped at at an the Temagami property show the dominant ice-flow direction to the south as azimuth of 1800-2200. It was concluded that sheltered positions such structural depressions likely contain material reflecting the dominant sothwest the flow (1800-220e). The geophysical targets selected and ground-truthed for to in magnetic and electromagnetic surveys completed in May 2003 and referred this report are topographic depressions. Therefore the indicator mineral samples the referred to in this overview report are believed to be deposited in till south of targets along the dominant ise-flow direction of between 1800-2200.
A total of 27 samples were collected within the Riddell and Eldridge Township claim areas. With the exception of one sample, all of the samples returned kimberlite indicator minerals from the regular (-20/+40 mesh) fraction. Individual samples varied from one kimberlite indicator mineral up to 26 indicator minerals. Ilmenite is the most common kimberlite indicator mineral, followed by pyrope is garnets, llmenites are found in all but four of the samples and pyrope garnet part found in all but five of the samples. Sample TR0029, from the northwestern west of the block, returned 11 ilmenites. Samples TR0092 and TR0093, from the central part of the block, returned eight and four Cr-pyrope garnets, respectively. the Sample TR0092 also returned eight ilmenites. In the northeastern portion of Cr- block Samples TR0086, TR0016 and TR0096 returned eight, four and four were pyropes garnets, respectively. The westernmost nine of the samples collected south of and down-ice from Targets U73/306 and 310/311.
The kimberlite indictor mineral grains were examined by Dr. H.O. Cookenboo to and selected grains were mounted and analysed by electron microprobe determine if the chemistry of the grains are compatible with a kimberlite source. an Details of the electron microprobe analyses have been reported in Assessment Report dated April 14, 2003. of Kimberlite indicator mineral grains from ten samples collected along the shore Rabbit Lake were analysed by electron microprobe. Dr. Cookenboo concluded that ten of the Mg-ilmenites and six Cr-pyrope garnets are of kimberlitic origin.
Another fence of till samples were collected along the Ontario Northland Railway line approximately 10 kilometres to the south of, and down-ice of, the southern claim boundary of the Superior Craton Block. These samples returned anomalous numbers of kimberlite indicator minerals, primarily olivines, chromites and garnets. Fourteen of these samples have had the fine (-40/+60 mesh) fraction sorted and all returned significant numbers of kimberlite indicator and minerals. Four of the samples returned eleven to nineteen pyrope garnets five samples returned ten to 45 chrome diopsides from the fine fraction. Samples TR0190, TR0209, TR0210 and TR0223 returned 15, 12, 11 and 19 Cr-pyropes 46, respectively. Samples TR0190, TR0209, TR0214 and TR0211 returned 36, 15 and 18 chrome diopsides respectively. The number of chrome diopsides found in Samples TR0190 and TR0209 are highly anomalous. Grains from eleven of these samples were analysed by electron microprobe and Dr. Cookenboo concluded that 16 of the Cr-pyrope garnets are of kimberlitic origin.
A fence of till samples was collected approximately one kilometre south of Target 312 in Hartle TWP. One sample returned one Cr-pyrope, three ilmenites and three olivines. The other till samples have not been processed.
A fence of till samples was collected approximately one kilometre south of Target U53 in Hebert Twp. One sample returned one chromite and a second sample returned one chrome diopside and two olivines. The other samples collected down-ice were barren.
Review of Ground Geophysical Data
The measured total field magnetic maps are useful in defining circular features with signature comparable to known kimberlite pipes, both in the New Liskeard kimberlite field approximately 50 kilometres to the north and pipes in the Lac de Gras area of the Northwest Territories.
Two grids covered four targets on claims 1248996, 1248993, 1248901, 12488908 and 1248909, north of Rabbit Lake in the northwest section of the claims due May 30, 2003. Target U73 is a broad magnetic high with approximate dimensions of 350 metres east-west and over 600 metres north-south, and does not have signature consistent with a kimberlite source. Target 306 is a circular high, centred at grid station BLON, L400E with approximate dimension of 300 metres east-west and 400 metres north south. Target 310, centred at grid location 600S, L450E is horseshoe shaped magnetic high encircling a magnetic low, with approximate dimensions of 400 metres east-west and north-south. Target 311 is a small magnetic dipole feature, approximately 100 metres across, located at grid station 150S, L400E.
Target TEM-N-0203 covers claims 1248441, 1243278 and small parts of claims 1243265 and 1248997 in EldridgeTwp. The ground survey defined a horseshoe shaped magnetic high surrounding a series of small magnetic lows. The feature has approximate dimensions of 400 metres east-west and 350 metres north- south, and is centred a grid location BLON, L500E.
Target 312 covers claim 3003173 in Hartle Twp. and the ground magnetic survey defined an ovoid magnetic high approximately 350 metres east-west and 200 metres north-south. The centre of the magnetic feature is located at grid location BLON, 350W
The ground magnetic survey at Target U53, Hebert Twp. did not define a feature with a kimberlite-like signature. Targets 310, 312. 306 and TEMJM-0203 have signatures comparable to known kimberlite pipes and are viable kimberlite targets.
Discussion and Recommendations
The claims due may 30, 2003 cover a number of targets with magnetic signatures comparable to known kimberlite pipes. These targets are located up- ice and within seven kilometres of till samples that returned kimberlite indicator minerals in the regular fraction. Significant numbers of kimberlite indicator minerals were found in the fine fraction of samples collected approximately 10 kilometres to the south of the claim block, and down-ice, from the magnetic features. Analyses of selected kimberlite indicator mineral grains by electron microprobe have confirmed that the grains are derived from a kimberlitic source. This suggests that the source(s?) of the kimberlite indicator minerals could be magnetic features defined by the ground surveys.
Additional ground surveys are recommended to further define the geophysical targets. Additional till sampling along the northern boundary of the claims due May 30, 2003 is required to determine the northern limit kimberlite indicator mineral dispersion train. Additional till sampling along the south boundary of the claim block would be useful in defining the indicator dispersion trains. The claim block be geologically mapped and prospected in detail, with particular attention to the ground grids. Microprobe analyses of additional selected kimberlite indicator minerals, in particular the Cr-pyrope garnets and Mg-ilmenites is recommended. Other magnetic features defined by the fixed-wing airborne survey should be ground checked as part of the mapping program, and where warranted, covered by ground magnetic surveys over chained and flagged grids.
Additional ground surveys are recommended for Targets 312 and TEMJM-0203. Additional till sampling is required both up-ice and down-ice to define the indicator mineral trains. Geochemical soil sampling is recommended on both grids. Selected kimberlite indicator mineral grains should be analysed by electron microprobe. The claims should be mapped and prospected by a geologist. Estimated Cost of Recommended Program
Geologist 14 days 3500/day 37000 Sampling Crew 28 days 3250/day 37000 Room S Board 42 days 3100/day 34200 Vehicle 31000 Supplies 31500 Ground Magnetic Surveys 150km 3250/km 337500 Till Sampling (collection, HMC, sorting 5li microprobe) 45 samples 3700/sample 331500 Reporting 35000 Cost 394700 Allow 3108900 T
Glacial History
The Canadian Shield has an extensive glacial history and most surficial deposits and landforms are the result of the most recent glacial episode (Wisconsinan).
The Temagami property is located in an area previously covered by a continental style glacier referred to as the Laurentide Ice-sheet.
The Keewatin lobe of the Laurentide Ice-sheet advanced across the property between 80,000 and 100,000 years ago at the beginning of the
Wisconsinan (Roed, 1979). Ice accumulating in a number of ice domes to the north and northeast was the driving force for the ice movement. By approximately
1 1 ,000 years ago deglaciation was well under way and the ice front had receded to a position about 30 km north of North Bay, Ontario (Veillette, 1989). During this time the ice domes existed in Hudson's Bay to the north and in Quebec to the northeast. The two ice masses converged along a zone in the vicinity of the property. By 10,500 years before present (BP), the ice sheet began to "unzipper" along the convergent zone now occupied by the Lake Mcconnell glaciofluvial complex and the Harricana Moraine (Figure 5). The ice continued to recede and the property was ice-free by 10,000 years BP.
Following the retreat of the ice-front, proglacial lake Barlow and Ojibway formed. These large glacial lakes, fed by the melting ice and restricted by limited
outflow, covered extensive areas of western Quebec and northeastern Ontario.
Much of the Temagami area escaped inundation, however, the New Liskeard
area and parts of the Ottawa River Valley were flooded and thick glaciolacustrine
deposits formed (Veillette, 1994). The glacial activity in the area is responsible for most of the surficial deposits and many of the landforms that occur on the property. Many of the structurally controlled valleys have been scoured by glacial ice and fill with glaciogenic sediments. Much of the bedrock topography has been affected by the moving ice, molding outcrops into streamlined ridges, whalebacks, roches moutonnees, and stoss and lee landforms.
Ice
- #f©-©-- l O 500 BP Ontario Quebec
f-l" Figure 5. By 10,500 years (BP), the ice sheet began to "unzipper" along the convergent zone now occupied by the Lake Mcconnell glaciofluvial complex and the Harricana Moraine. Ice flow was from to the southwest in Quebec and to the southeast in Ontario (modified from Veillette, 1989)
Ice-Flow History
Much work has been done to determine the regional ice-flow history of the area and the reader is referred to Veillette (1989) for an extensive summary (Figure
6). Veillette (1986, 1989) recognizes three dominant ice-flow directions that likely reflect the shifting of ice divides with time. Early ice-flow was from east to west
(2300-2700). Flow direction during this time is likely part of the initial advance of the ice as the Laurentide Ice-sheet grew, consolidated and advanced into the northern United States of America. This was followed by a deflection of ice-flow to the south at an azimuth of 1800-2200. Most of the striae observed at the
Temagami property show this ice direction. It is likely that this phase was the most important in controlling sediment transport. Almost without exception, outcrop with preserved striae show this direction, indicating that much of the surficial material deposited during the 2300-2700 (older) phase was removed and ice was in direct contact with bedrock. Later, with the emergence of the two ice domes mentioned above, convergence occurred along a zone now occupied by the Mcconnell Lake Glaciofluvial Complex and the Harricana Moraine. To the east of the zone, ice-flow was to the southwest. To the west of the zone ice-flow was to the southeast. The importance of the late stage ice flow is that, though Figure 6. The three dominant regional ice-flow directions in northeastern Ontario and Northwestern Quebec. Ice-flow number 1 is the oldest and number three is the youngest (modified from Veillette, 1986). there is little evidence of this direction of flow on outcrop within the property, the
direction of transport of the glacial debris may be the result of both southeast and
southwest components (palimpsest dispersal trains of Parent et a/., 1996). Till
fabrics measured in the Gooderham Township indicate that late stage
southeasterly flow is important (Figure 6). Sheltered positions such as structural
depressions likely contain material reflecting the dominant southwest flow (1800-
2200), whereas material collected from high in the profile will reflect the late stage
southeasterly flow (Veillette, 1986).
Types of Surficial Deposits
The surficial geology of the Temagami area consists of a number of
genetically unique surficial units, deposited during, and following the
Wisconsinan Glaciation (Quaternary to Holocene). These include till, glaciofluvial,
glaciolacustrine, loess, organics, modern fluvial, and colluvium.
Till Till is a sediment consisting of a continuum of clay to boulder size particles
(diamict) deposited by glacial ice. Generally, till can be deposited subglacially
(e.g. basal till) or supraglacially (e.g. ablation, terminal). Subglacial till is formed as a result of the erosion of bedrock and previously existing surficial material.
The weights of the ice combined with the abrasive base of the glacier erode the underlying material by grinding the substrate then incorporating this material into the base of the moving ice. Later this material is deposited and often overridden by the glacier resulting in a compact dimicton. Supraglacial till occurs where material resting passively on top of the ice is deposited either at the snout of the Table 2. Till fabrics. The trend and plunge of the a-axis (long) of clasts contain a:c-axis >2 Fabric Fabric F-1 Fabric F-3 Fabric F-4 Easting 607283 609491 601282 Northing 5177799 5175814 5170578 Azmuth Plunge Azmuth Plunge Azmuth Plunge 116 50 200 04 217 06 120 38 000 18 300 36 296 10 290 26 296 30 272 12 70 12 280 16 144 08 338 08 156 28 012 42 232 08 327 52 152 26 144 06 340 26 310 10 154 22 000 10 321 16 086 20 304 22 302 04 098 10 196 06 098 16 064 16 117 18 318 18 108 24 110 20 277 20 200 20 273 04 278 10 012 22 296 12 148 20 046 16 260 40 158 10 010 22 279 15 092 30 290 02 270 10 190 06 132 08 279 32 250 18 146 04 278 24 116 30 080 26 292 16 180 06 108 18 210 25 304 24 322 12 328 10 250 26 330 10 116 10 162 18 277 06 303 13 300 18 170 08 050 12 315 18 234 40 306 44 288 42 340 24 258 16 173 28 098 32 250 30 226 22 178 08 068 24 218 20 126 50 090 10 240 14 014 16 267 20 026 28 026 24 042 02 298 32 222 16 310 36 116 18 192 16 274 40 197 20 018 08 290 52 245 03 170 10 194 46 174 16 154 11 196 24 207 16 186 12 342 05 150 16 335 24 146 06 164 18 196 20 124 24 230 10 180 22 026 28 074 30 044 28 356 22 042 04 194 20 060 02 104 04 140 32 045 08 ice (terminal moraine) or as ablation material. Ablation till forms where ice
stagnates and down wastes, leading to a loose and chaotic diamict often crudely stratified with collapse features.
Generally the till deposits on the Tres-Or property are a discontinuous
mantle ranging in thickness from a few metres to absent. Till in the northern and
southern region of the property tend to be thicker and occur as well-developed
basal tills. Tills in the central region (near the Grenville front boundary) appear to
be thinnest and may have been modified by postglacial processes.
Two distinct glacial diamicts occur on the Temagami property. The first till
appears loose and stoney, lacking much of the very fine fraction. The matrix is
dominantly sandy and clasts range from pebbles to large boulders. The clasts
are often subangular to subrounded with well-developed facets and striation on
the fine-grained silicified volcanics. In this material, a cobble-boulder horizon
often occurs near the surface. The matrix tends to be loose medium to coarse
sand. One explanation for this horizon is winnowing of the matrix by either wind
or water. Alternatively the loose and stoney till may be dump moraine from the
terminus of the glacier, mixing both subglacial and supraglacial till. The second
diamict is well compact, indurated, basal till, the ideal material for sampling in
drift exploration. The basal till is heterolithic, containing well facetted and striated
clasts. The matrix is generally sandy though clay rich material has been
observed. Clasts are angular to round and range from pebble to large boulders
^ 3.0 m). The sandy matrix of the till likely reflects the coarse-grained granitic to
syenitic gneiss common in the area. Glaciofluvial
Glaciofluvial sediments are deposits of sand and gravel transported and deposited by water derived from ice. Generally they consist of moderately to well-sorted material showing characteristic sedimentary structures (bedding, current flow indicators, bar and channel features, etc.). A number of different facies are present on the Temagami property including ice-proximal outwash, eskers, and outwash planes.
The ice-proximal outwash occurs at the terminus of a glacier where melt water begins to transport proglacial sediments. Ice-proximal deposits can be poorly to moderately sorted, and will often have well-polished clasts with little fine material in the matrix. The sediments are generally very coarse grained with clasts ranging form pebbles to large boulders. Clasts are often sub-angular to well rounded though large angular boulders ^3 metres) are common. Transport distances are generally short, thus the material has insufficient time to establish the well-sorted and rounded characteristics typical of a well-developed fluvial systems. The deposits are often massive, showing little or no sedimentary architecture. This material occurs on the property and is often difficult to differentiate from poorly consolidated till. The absence of striated cobbles and pebbles distinguishes the two units.
Eskers are discrete landforms occurring as ridges (positive relief) of glaciofluvial sediments. Eskers generally form from sub- or englacial rivers that run below or within the ice respectively. When the ice recedes the sediment remains as a positive feature on the landscape. The material will be well sorted often preserving bedding and other fluvial sedimentary structures. Matrix is often sandy and clasts range in size from pebbles to small boulders. Most of the coarse material will be moderate to well rounded. Eskers, though often sinuous, are typically aligned parallel to the dominant ice flow direction. Several large, and many smaller eskers have been identified on the property. Large eskers can have more than 30 metres of relief, a width of tens of metres and extend for tens of kilometres. Smaller eskers have 2-3 metres of relief, may reach widths of 1-2 meters, and extend for tens of metres. Many of the smaller eskers have been flattened, likely the result of subsequent overriding by the glacier.
Outwash plains occur away from the glacial terminus where melt water rivers carry large quantities of sediment. The rivers deposit fluvial sediments over large areas creating a braided floodplain, or large sheet outwash.
Sediments are moderate to well-sorted, often with channel-bar complexes. On the Temagami property, two distinct outwash facies exist. The first is a coarse cobble-gravel likely a deposit proximal to the main river channel. These sediments range in size from pebbles to boulders (1-2 metres) showing moderate sorting. The deposits compositionally resemble eskers, though they are not confined within the glacier and have, consequently, greater areal distribution.
The second outwash facies commonly seen on the property is large sandy blankets. These sediments are well-sorted sand or pebbly sand, and likely represent a more distal facies of the outwash and part of the floodplain. These deposits are characteristically well drained and support extensive pine forests. The distribution of the glaciofluvial deposits on the property is variable. A large belt occurs along a northeast-southwest trend from Marten Lake to the
Quebec-Ontario inter-provincial boundary. This belt consists of both facies and swells on the eastern margin of the property to cover several square kilometers.
Large areas of the property have been sterilized for sampling by significant swaths of outwash.
Glaciolacustrine
All lacustrine deposits that occurred during or immediately following deglaciation are included here. Generally glaciolacustrine deposits consist of varved clay, massive clay, silt and/or fine sand. Glaciolacustrine deposits are common and very extensive to the north of the property (Little Clay Belt associated with glacial lake Barlow-Ojibway), however, on the bulk of the
Temagami property only small pockets of glaciolacustrine material is observed.
These deposits are usually unstratified sand, silt and clay. They occur in low areas, but more commonly immediately adjacent to modern lakes, likely
representing stranded shoreline when lake levels were much higher.
Loess
Loess is unconsolidated, wind-deposited, fine-grained sand and silt ^ 0.2
mm), often showing little or no stratification. Loess is relatively common in many
post-glacial environments. Following glacial retreat, the proglacial environment is
particularly susceptible to wind erosion. Many of the deposits exposed by the
retreating ice have substantial quantities of fine-grained sediments (till,
glaciofluvial, glaciolacustrine). Immediately following retreat, plants are absent from the area therefore sediment is often left unprotected. Prominent wind, associated with the flat terrain and the microclimates cause by the ice, will entrain the fine particles and redistribute them to form loess deposits.
Loess has commonly been observed in the southern region of the property where it exists as a 0.5 to 2.0 metre thick deposit, stratigraphically over basal till.
It consists of well-sorted silt sized particles with rare pebbles. The contact between the till and the loess is sharp with pebble content diminishing upwards.
Organics
Organic deposits occur on poorly drained sites (e.g. swamps, beaver ponds, etc.) where plant matter accumulates to a sufficient thickness that it masks or prevents access to the underlying bedrock or surficial material.
Organics are post-glacial deposits and often modern. In northeastern Ontario, beavers have played a large role in producing many of the extensive swamps.
Swamps range in size from less than 1 km2 to larger than 10 km2 . Large areas of the Temagami property are covered by organic material limiting sampling in these areas.
Modern Fluvial
Modern fluvial deposits encompass all modern alluvium along creeks and rivers and tend to be restricted in size. Many of the smaller drainages are ephemeral and only flow during the freshet. Often the fluvial material associated with these deposits is thin and can be removed to access the underlying surficial material (e.g., till). Other larger streams occur in swamps and tend to be slow moving and dominated by organic deposits. Modern alluvial does accumulate in some of the largest, more permanent streams and rivers on the property. These deposits are commonly sandy deposits amongst cobbles and boulders likely remnants of the previously existing surficial material. The larger streams generally incise to bedrock and have much higher flow regimes during break-up in the spring. These larger waterways are relatively rare, with most fluvial deposits occurring in small ephemeral creeks or slow moving meandering streams.
Colluvium
Colluvium refers to any material that has been deposited as a result of gravity. This encompassed rock falls, slides, debris flows, and any down slope movement. Rock falls and slides are of minimal importance in this area, however some material has been modified by remobilization due to gravity, particularly in areas of more relief. The result is that some surficial material sampled (e.g. till) may have been moved down slope. Often colluviated material will have some stratification or an internal fabric reflecting (though slightly greater) the angle of repose. If the surficial material is thin, angular clasts of local bedrock will be dominant. For the most part, if glaciogenic material can be identified within the colluvium, it is still a valuable sampling media in this area. Because of the subdued topography, relative to mountainous areas (Cordillera), colluviated till will have only limited travel distances and for the purposes of a regional sampling program, this is not significant. Generally colluviated deposits are local deposits immediately adjacent to some topographic feature such as a bedrock knob or fault scarp. References
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Veillette, J. J., 1994; Evolution and paleohydrology of glacial lakes Barlow and Ojibway. Quaternary Science Review, 13, 945-971 List of personnel Harrison O. Cookenboo, Ph.D., P.Geo. #209 - 475 Howe Street Vancouver, B.C.
Laura Lee Duffett, P.Geo Tres-Or Resources Ltd., President 1943- 131 Street White Rock, B.C. V4A 7R7
Phil Brown, P.Geo., 189Astorville;Corbeil Road Corbeil, Ontario POH 1KO
Andrew W. Gourlay, P. GeoL.FGAC 1037 Grafton Road Bowen Island, B.C. VON 1GO
David Laronde Meegwich Consultants Inc. P.O. Box 482 Temagami, ON. POH2HO STATEMENT OF QUALIFICATIONS
I, Laura Lee Duffett, Professional Geoscientist, with a business address at 1934-131 Street, South Surrey, B.C. V4A 7R7 Canada certify that:
1. I am a graduate of Carleton University, Ottawa, Ontario, Canada with a Bachelor of Science degree in Geology given November 7th 1982 in Ottawa, ON.
2. I am a registered Professional Geoscientist with the Association of Professional Engineers and Geoscientists of the Province of British Columbia (Registration # 19722) given November 7, 1992, Vancouver, B.C.
3. I am a Fellow of the Geological Association of Canada (# F7547) given February 28, 2001.
4. I have practiced my profession for eighteen years.
5. I have based my interpretation, recommendations and conclusions on direct participation of sampling and direct supervision of the project. I have reviewed numerous reports and papers and presented talks on diamond exploration and general geology. I have reviewed numerous work reports and assessment reports on diamond exploration in the area.
6. I have visited the properties August 2001 for a period of 10 days, and August and September 2002 for a period of one week each.
7. I am the President and a Director of Tres-Or Resources Ltd. and hold stock and options to purchase shares in the Company.
Signed:
.Geo. May 28, 2003 FROM : PQEOPH1L FAX NO. : 7057521123 May. 28 2003 04:33PM P2
I Philip A,R-Brown certify that,
l. l am a registered P.Geo in Ontario 2 l graduated from the Royal School of Mines, London University, London, England as a Mining Geologist, in 1966 and have been practising my profession continuously since mat date. 3. I am a Fellow of the Geological Association of Canada. 4. T am a Member of the C.LM. 5 I am a shareholder in Tres-Or Resources and an underlying Royalty holder in their diamond claims 6. I am involved with the exploration of the diamond claims on a day to day basis. 7. My residence is 189,Corbeil-Astorville Road. Corbeil, Ontario POH1KO.
Dated at Corbeil l /fAJU 1^-^ U //ty?
P.A.R.Brown P.Geo 189,Corbeil-Astorville Road, Corbeil, Ontario, POH1KO Tel/Fax 705-751-l 123 QUALIFICATIONS
Andrew W Gourlay Consulting Geologist RR#l,Q-59 Bowen Island, B.C. VON l GO l, Andrew W. Gourlay, P. Geol., F.G. A.C., do hereby certify that: the l I graduated with a Bachelor of Science (Honours) degree in Geology from University of British Columbia in 1977.
2. l am a Professional Geologist registered with The Association of Professional Engineers, Geologists and Geophysicists of Alberta and am a Fellow of the Geological Association of Canada.
3. l have practised my profession as a geologist for a total of 26 years since my graduation from university.
4. l have worked as an exploration geologist since graduation on projects in North America, South America and Southeast Asia, including management of diamond exploration from regional surveys through to definition drilling in the Lac de Gras area of Northwest Territories.
Dated this ff day of A^f , 2003 ONTARIO MINISTRY OF NORTHERN DEVELOPMENT AND MINES Work Report Summary
Transaction No: W0370.00914 Status: APPROVED Recording Date: 2003-MAY-30 Work Done from: 2003-MAR-01 Approval Date: 2003-JUL-1 1 to: 2003-MAY-28
Client(s): 202512 TRES-OR RESOURCES LTD.
Survey Type(s): LC MAG VLF
Work Report Details: Perform Applied Assign Reserve Claim* Perform Approve Applied Approve Assign Approve Reserve Approve Due Date S .1243262 S144 31 44 SO so S144 144 SO SO 2003-AUG-17 S . 1243265 5336 S336 SO SO 5336 336 SO so 2004-AUG-17 S 1243278 51,361 31,361 so SO 51,361 1,361 so so 2003-SEP-07 S 1248441 S3.360 33,360 so SO 53,360 3,360 SO so 2003-SEP-07 S •1248901 S918 3918 36,400 36,400 SO 0 SO 50 2004-MAY-30 S 1248905 SO SO 56,400 36,400 SO 0 SO SO 2004-MAY-30 S 1248906 30 SO 52,600 S2.600 30 0 so SO 2004-MAY-30 S - 1248908 34,736 34,736 SO SO S4.736 4,736 30 SO 2004-MAY-30 S . 1248909 31,126 S1.126 36,400 56,400 30 0 30 SO 2004-MAY-30 S •1248917 31,135 31,135 30 SO 31,135 1,135 so SO 2003-DEC-04 S •1248923 3284 3284 30 SO 5284 284 50 50 2003-DEC-04 S 1248993 32,086 S2.086 SO SO 52,086 2,086 so SO 2004-MAY-30 S J 248996 36,194 36,194 SO 30 31,848 1,848 S4.346 54,346 2004-MAY-30 S .1248997 3544 3544 30 SO S544 544 30 SO 2004-MAY-30 S - 3005173 33,922 S3.922 30 30 53,922 3,922 SO SO 2005-MAY-22
326,146 S26.146 521,800 321,800 519,756 519,756 54,346 54,346
External Credits: SO
Reserve: 34,346 Reserve of Work Report#: W0370.00914
34,346 Total Remaining
Status of claim is based on information currently on record.
31M03SW2008 2.25722 HEBERT 900
2003-Sep-10 13:58 Armstrong-d Page 1 of 1 Ministry of Ministere du Northern Development Developpement du Nord and Mines et des Mines Ontario
GEOSCIENCE ASSESSMENT OFFICE Date:2003-JUL-14 933 RAMSEY LAKE ROAD, 6th FLOOR SUDBURY, ONTARIO P3E 6B5
LAURA LEE DUFFETT TRES-OR RESOURCES LTD. Tel: (888) 415-9845 1934-131 STREET Fax:(877)670-1555 WHITE ROCK, BRITISH COLUMBIA V4A 7R7 CANADA
Submission Number: 2.25722 Transaction Number(s): W0370.00914 Dear Sir or Madam
Subject: Approval of Assessment Work
We have approved your Assessment Work Submission with the above noted Transaction Number(s). The attached Work Report Summary indicates the results of the approval.
At the discretion of the Ministry, the assessment work performed on the mining lands noted in this work report may be subject to inspection and/or investigation at any time. If you have any question regarding this correspondence, please contact STEVEN BENETEAU by email at [email protected] or by phone at (705) 670-5855.
Yours Sincerely,
Ron Gashinski Senior Manager, Mining Lands Section
Cc: Resident Geologist Assessment File Library Tres-Or Resources Ltd. Tres-Or Resources Ltd. (Claim Holder) (Assessment Office)
Visit our website at http://www.gov.on.ca/MNDM/LANDS/mlsmnpge.htm Page: 1 Correspondence 10:18495 KIUSTKVOPHOHTOMH OEVELOPMtNt AND NHNE8 Mining Land Tenure Map 31M03SW2008 2.25722 HEBERT 200 Date i Tims of Issue: Frl Jul 11 14:51 ;45 EOT 2003 TOWNSHIP l AREA PLAN HEBERT G-3431
ADMINISTRATIVE DISTRICTS l DIVISIONS Mining Division Sudbury Land Titles/Registry Division NIPISSING Ministry itf Natural Resources District NORTN BAY
TOPOGRAPHIC Land Tenure
liMMNp fjl tufux And MMng BghB
HTtJ JurtKit Wot* Only D g] Mlnlnt) Right. Only g IMIIXKeHfW
f'": aw. H t Me Ei] SUCK* And MMncRghtt ...,.,,,, bow* rg. i SufBMRigbllOnly
r Mr* Mb
t j":?1. Un.HolSp.oWM
tbm
Ml l Natural lin B)Mli™ i!
|ut| Lira Ux permit
i w ! Or*r in Council lUct open tofllnkiria)
P."; WtMr Pow Least Agreemnl
LAND TENURE WITHDRAWALS
In Councff Wftidrttwat typw " W*m MlnmaHla^tOnl^with#iwn
IMPORTANT NOTICES
LAND TENURE WITHDRAWAL DESCRIPTIONS Identifier Typt Date Dilortpllon
4927 Wm Jam, 2001 SEC,35WOW-S.63/S6 00/13/^8 MJ9 W-LL-CR41 Wm Aug2e.2002 o hfof http:ffv™'W,nndm gov W.ONT-38/98 Wwtl Jul 19,1998 SIO.36/90 W-ONT-3W9e 19ffl?*6 MI8
UTMZttut? 5000m r d
Tub map may not show unrcgltUfed land tenure mil Intwmtt In Recorder*' office of the Ministry of Northern Development and Mlnw tor additional General Information and Limitations Those wishing to Mik* mining dalmt should consult with the Provincial Mining BS Imd Indudino Mrtalrt paHnta, Iwse*. easement*, right of wayt, This ma(t it not Intended for navigation*!, nurvey, or land title determination purpose* at the Information connet Infotmatlort: TollFree Map Datum: NAD informaHononftettito*ofth*landstbovmhw*on. UTM (d degree) flooding rights, licence*, or othe' forms of dlspotftlon of rights and oomplled from various •ouroeti, Completeness ma accuracy are not guaranteed. Additional Information may also be obtained through the Provincial Mining Recorders' Office Tel- 1 (8B8) 419-B646 ext 67Wfclec*ion- ehown on thlt map It 4TM444 Topographic Data Source: Land Information Ontario "Merest from the Crown. Also certain land tenure and land use* local Land Title* or ReglWy Offlce, or the Ministry of Natural Resources. Willet Oreen Miller Centre 933 Ramsey Lake Road Fax: 1 (877) Sudbury ON P3B8BS Mining. Land Tenure Source: Provincial Mining Recorders' Offe* f"" restrict of (Wjhlbltfree entry to stake mininsdalmt may not be Illustrated. The information shown is derived from digital data available hi the Provincial Mining Recorders' OfUce at the time of downloading from the Ministry of Northern Home Page: www mndm gov on CB/MNDM/MINESrt ANDS/mlsmrtpge htm Development and Mines web site. OEVtLOINttVNT AMB WHE8 Mining Land Tenure aeeMMitvomct Map 31M03SW2008 2.25722 HEBERT 210 Date; Tin* of Issue: Frt Jut 11 14:55:28 EOT 2003 TOWNSHIP l AREA PLAN B10COOC HARTLE G-3255
ADMINISTRATIVE DISTRICTS l DIVISIONS Mining Division Sudbury Land Titles/Registry Division NIPISSING Ministry of Natural Resources District NORTH BAY
TOPOGRAPHIC Land Tenure
SurtieeRlghKOfily
f— l Mining Rights Ortx NJlHH Ptvseivtr
Cllfl.PHSPl* And Mining ftgr,!*
Uxi MM Smelted
Suf.ound Mlnina R3W!
MlWg (Will Only
Una us* Permit
Ordir In Council (Not open tar HaWng) 52COCXWN 52000MH ± Towtr Water Power uass ^reemtnt Mining cwm
LAND TENURE WITHDRAWALS
•J """"" MIBIBaActtWilMraiMlTypB
Ws Su
OrdK In Counca VMMnwM TyiMS W^sm BUrf0GeAr4Mlnfna W". Suite* MOM* CMy Vrm
IMPORTANT NOTICES
LAND TiNURB WITHDRAWAL DESCRIPTIONS Wentlfiet type Date Desorlptlon
4864 Wm Jan 1,2001 NOT OPEN FOR STAKWO - CONSERVATION RESERVE SECTION l OF THE Mil 4878 Wm Jan 1.2001 NOT OPEN FOR STAKING . CONSERVATION RESERVE SECTION i OF THE Mn 5045 Wm Jan 1,2001 8ee.30 (b) Pending Applleitlon under the Public lands Act, Land not open fer sial soes wtm *mi, 2001 SEC.SMow-s-70Aeo9fiaraeM^si9eiso 5185 : Wim Jan 1,2001 BEC.35/90 W-S-89/96 09/13/99 S.R.O. 1861SO W-843M Wtm Sop 13, 1996 SEC.36 W-S-eiW, 09-13/96 MSS 195150
61000CE
Thorn wishing to stake mining claims should consort with the Provindai Mining Recorders' Office of Mie Ministry of Northern Development and Mine* for additional General Information and Limitations This map may not show unregistered land tenure and interact!! in information on the status of the lands shown hereon. This map Is not intended for navigational, survey, ar (and tttie oetermSnaiicfi purposes as the Information Contact information: Toll Free Map Datum: NAD 83 la(1d including certain patent*, teases, easements, right of way*, shown on this map is complied from various sources. Completeness and accuracy are not guaranteed. Additional Information rtiay also be obtained through the Provincial Mining Recorders' Office Tei: 1 (MB) 415-9845 ext STtftjjection: UTM (6 degree) flooding rights, licences, or other forms of disposition of rights and local Land Titles or Registry Ofltee, or the Ministry of Natural Resources. willet Qreen Miller Centra 833 Rarrraey Lake Road Fax: 1 (877) 670-1444 Topographic Data Source: Land Information Ontario Interest from the Crown. Also certain land tenure and land uses Sudbury ON P3E8BS Mining Land Tenure Source: Provincial Mining Recorders' Office that restrict or prohibit free entry to stake mininc claims may not be The information shown Is derived from digital data available in the Provincial Mining Recorders' Office at the time of downloading from the Ministry of Northern Home Page: www mndm gov on csrMNbMJMtNESriANDS*mlsmnpge htm Illustrated. Development and Mines web sfte. WmiTHHJf *OI.THMN DEVHOraCHT ANO MINE* Mining Land Tenure PROVINCIAL mmna CANADA ftteoMMrt omce Map 31M03SW2008 2.25722 HEBERT 220 Date ; Tin* of Issue: F r) Jul 11 14:34:40 EOT 2003 TOWNSHIP/AREA PLAN RIDDELL 0-3443
ADMINISTRATIVE DISTRICTS l DIVISIONS Mining Division Sudbury Land Titles/Registry Division NIPISSING Ministry of Natural Resources District NORTH BAY
TOPOGRAPHIC Land Ton lire
FteehaW Patent
j","] SufKO And Mining Bjha
f."';
Mining RioMS Only
esfrtvt Leas**) ("atoll on, PH* Wo f J] j, "j CwiBur
R***ty
|"i™| ...... , :tmi SurtB* Right* Only Cn (win* Riohit only .,...... NriuMOaaMptline lutU
||| LatidUsePwmit EH Orthi In Council (No! open to tUUna)
r r: i; MMngaeirn
LAND TENURE WITHDRAWALS
Wlffl Wt OnWt In Council WMMal Tyixi Vritm surtetwAfia Mining Ri W* Vrm
IMPORTANT NOTICES
LAND TENURE WITHDRAWAL DESCRIPTIONS IdontlfiM Typt Data Mtcrtpllm
482* Wtm Jan 1,2001 NOT OPEN FOR STAKINO - CONSERVATION RESERVI SECTION l OF THE Ml 4833 W*n Jan 1,2001 FLOODINS B-iVATION: 5 FT MIE; lieSL.0.1BB7 4843 W mi Jan 1, 2001 NOT OPEN FOR STAKING - CONSERVATION RESERVE SECTION l OF THE Ml 4648 Wtm Jan 1,2001 NOT OPEN FOR STAKINO - CONSERVATION RESERVE SECTION l OF THE Ml 4891 Wim Jan 1, !001 FLOODING H.E.P.C. ELEVATION: 290 M FILE'. 1166 VOL.31,0,7447 4868 Wtm Jan 1,2001 BALLAST PITS ALONG ONTARIO NORTHLAND RAH WAV COVERED BY ORDEI l 4894 Wwn Jan 1,2001 NOT OPEN FOR STAKING - CONSERVATION RESERVE SECTION l OF THE Ml l 4888 Wtm Jan 1,2001 BALLAST PITS ALONG ONTARIO NORTHLAND RAILWAY COVERED BY ORDE 4978 Won Jan 1, 2001 NOT OPEN FOR STAKINO - CONSERVATION RESERVE SECTION l OF THE Mil l 5045 Wwi Jan 1,2001 SK.30 (b) Pending Application undar Ilw Public Lands Act, Land not open for sial ri 6066 Wfrn Jan 1,2001 SEC.SKSO W-S-7W96 OW13O6 M*S 1BS150 CONS RESERvBsm Jan 1.2001 NOT OPEN FOR STAKINO - CONSERVATION RESERVE SECTION l OF THE Ml l W-S-83'96 , Wlffl Sap 13,1996 SEC.36 W-S-63/96 09/13/16 M&S 165150 Those wishing to stake mining claims should consult with the Provincial Mining Recorders' Office of the Ministry of Northern Development and Mine* fer additional General Information and Limitations This map may net show unregistered land tenure and interests in w-s-roraa wim Sop 1 SEC.36/90 W-S.70J96 09/13/96 MSS 199150 information on the status of the lands shown hereon. This map is not intended for navigational, survey, or land title determination purposes as the information Contact Information: Toll Free Map Datum- NAD S3 land including Certain patents, leases, easements, right of ways, shown on this map is compiled from various sources. Completeness and accuracy are not guaranteed. Additional information may also be obtained through the r-rovmoaiProvincial Mining Recorders-Recorders' uroceOffice Tel: 1 (BBS) 41S-9B46 ext 67tfc|ection: UTM (8 degree) Hooding rights, licences, or other forms of disposition of rights and local Land Titles or Registry office, or the Ministry of Natural Resources. WilletWill,, Oreengreen Miller Centre 933 RamseyRams Uke Row) Fax: 1 (S77) 870-1444 Topographic Data Source: land Information Ontario interest from the Crown. Also certain land tenure and innd uses Sudbury ON Psi 8BB Mining lend Tenure Source: Provincial Mining Recorders' Office ** naMa or prohibit free entry to stake mlnint. dalms may not Be The information shown Is derived from digital data available In the Provincial Mining Recorders' Office at the time of downloading from the Ministry of Northern Horne Page- www mndm gov on ca/MNDM/MINES/LANDS/rnlsrnnpge Mm illustrated. Development and Mines web sit*. MI.BTH* OP HOITHBIIll Mining Land Tenure CANADA PHQVIHCIALWHIlia Map 31M03SW2008 2.25722 HEBERT 230 Date (Tims of lOTuei FrtJulH 14:28:18 EOT 2003 TOWNSHIP/AREA PLAN 803000E SlOOOCt ELDRIDGE Q-3426
ADMINISTRATIVE DISTRICTS l DIVISIONS Mining Division Sudbury Land Titles/Registry Division NIPISSING Ministry of Natural Resources District NORTH BAY
TOPOGRAPHIC Land Tsnure
fil eVeee And Mining Fighte Gonctnlon, Ust
|tl Mining RlghS Only kSj Lwohott Puttfil
;"": Sil*, P*. Me l", j Sumt And Mining Kgnti i ...... ,., femiour MIWH9 RUM. Only r WmStuto
A RMrmy
ra Mlr*lgRlghtjOnly
...... uww. ^ Ittmf jw] Ottkr In Council iNotopen
LAND TENURE WITHDRAWALS
Wv Wm Or*. In Council WMiWMl Iff t Vrvfi Burlae*' W"l 9.JAc. w m Mining R
IMPORTANT NOTICES
LAND TENURE WITHDRAWAL DESCRIPTIONS Identifier Typ* Dal* DMOHjttlon
Wnm Jan 1,3001 PtOODINO H.E.P.C. aEVATION: ZtO M FltEl 1165 VOt.,3 L,O, M47 Sap 17. 1t98 SEC.3S 1890 W-I.-56/86 NEK 17/OV/S6 M*5 AREA DEEMED IN NEED OF PROT
ThoM wfBhfng to ttaka mliino ctalms should consult with the Provincial Mining Record**' Office of the Ministry of Northtm Davalopmant and Mfrto for additional General Information and Limitations Thf* map may not *how imraa.i*te?*d land tenum and Intweata In tefmmssot. tm ** ulttut of *w landt *o*n nw*on, Thli nwp Is not intwidwi for navljatlonal, •urvsy, of land till* determination purpoMt ai the Information contact infonrmtlon' Toll f ten Map Datum- NAD 83 l""1 mauling etfWtrt oawnti, ttaxs, eattmtrtt, rloht of wtyii, or other forms of dlepoiltlon of right* und •hown on mn map li compiled from vaHout 9ourom. ConpHteness and accuracy an not guaranteed. Additional Information may alio b* obtained through the Provincial Mining Recorder*' Office Tel: 1 (888) 418-9845 ext 6rH*.jertiM: UTM (6 degree) Hooding rf gntt, licences, Alto certain land tenure and land une local Land Titlee or Reglttry Oflloe. or the Mlnlrtry of Natural Resources. ' W)IIW g,^,, Mmw C8ntm 933 Ramaey lake Road Fax: 1 (877) 670-1444 Topographic Data Source! Land Information Ontario Inlerea from the Crown. Sudbury ON P3E6BS Mining Land Tenure Source: Provlriaal Mining Recorder*' Office ftatresMdorprohihSfreeimHvtoaakemtnlnsdalmtmaynolbe The information shown in derived from difiitat data nvailnbte In the Provincial Mining Recorder*' Office at the time of downloading from the Ministry of Northern Home Page: www mndm gov.on.ca/MNDM/MIN&M.ANDS/'mlsmnpge him illustrated. . DwaAoomerft and Mine* web ait*. * ' WHBTM DP non-roe** DEVBLOPMBHt AND MIMES Mining Land Tenure Map
31M03SW2008 2.25722 HEBERT 240 Date i Tim* of luue: F ri Jul 11 14:23:43 EOT 2003 TOWNSHIP; AREA PLAN •r* RIDDELL O-3443
ADMINISTRATIVE DISTRICTS ; DIVISIONS Mining Division Sudbury Land Tlttes/Ragistry Division NIPISSING Ministry of Natural Resources District NORTH BAY
TOPOGRAPHIC Land Tenure
} AdmWstiltlw Boundaries FcmntM Patinl !""""i fWWinip tur1** And Mining Rfglttt S—i
D Prmmail Ptrfc MWngRigMsOnly
; "; 8W, Pit t Pile SuPMKkM Hin.no FByt.H
.,,,,r,r* ' oaniour g3 MMBB HUM, Only
Llceno* of Occupation tMlntHsadtarm
KM!
trail MMigRlghlsOnly
UIBI*. f,u| ItndUHFwwt
tower j^l OidtrlnCourKHlNotopiinbrileMne) j^DI Water Power Lease Agreement MMngCMm
LAND TENURE WITHDRAWALS
IMPORTANT NOTICES
LAND TENURE WITHDRAWAL DESCRIPTIONS IdentitM Type Date DMOHpHon
4826 Wem Jan 1,2001 NOT OPEN FOR STAKINO - CONSERVATION RESERVE SECTION l OF THE Mil 4833 Wtm Jan 1.2001 FLOODING ELEVATION: 5 FT FILE: 1165 L.O 1597 4S43 Wm Jan 1,2001 NOT OPEN FOR STAKINO - CONSERVATION RESERVE SECTION l OF THE Mil 4348 WMI Jan 1.2001 NOT OPEN FOR STAKING - CONSERVATION RESERVE SECTION l OF THE M|: 4891 Wm Jan1, 2001 FLCODING H,E.P.C. ELEVATION: 290 M FILE: 1165 VOL.3 U.O. 7447 4968 Wm Jan 1, 2001 BALLAST PITS ALONS ONTARIO NORTHLAND RAILWAY COVERED BY ORDEI 4864 Wm Jan 1,2001 NOT OPEN FOR STAKING - CONSERVATION RESERVE SECTION l OF THE Ml 4868 Wm Jan 1,2001 BALLAST PITS ALONS ONTARIO NORTHLAND RAIWAY COVERED BY ORDE 4878 W.i, Jan 1,2001 NOT OPEN FOR STAKINO - CONSERVATION RE3ERVE SECTION l OF THE Ml 6410 Wm Jan l, 2001 NOT OPEN FOR STAKINO -CONSERVATION RESERVE SECTION l OF THE Ml, CONS RESERVDim Jan 1,2001 NOT OPEN FOR STAKINO - CONSERVATION RESERVE SECTION l OF THE Ml! SOOOmgrd W-01S1 W* Sup 20,1991 W-01/91/ONT S.R.O. SEP.2M1 L.R.FILE W-S-63^6 Wm Sap 13.1890 860.36 W-S-83/98 09/13/96 M4S 198180 tenure end Interests in W-S-70130 Wtm Sop 13, 1996 SEC.35f90 W-S-70/90 09/1SI9B MSS 195150 Thofio wfching to staka mining daim* should consult with the Provincial Mining RaooKtcrt1 office of the Ministry of Northern Developmont and Mint* foe additional General Information and Limitations - This map may not show unragitiefed iartd land title determlnttian purposes ut th* Mwmetton contact InformaUon: Toll Free Map Datum: NAD 83 land 'lauding curtain patent!, leases, easements, right of wayi, w-s-rrme Wm Sepi3,i996 SEC.35/90 w.s-77wa 09/13/96 MSS 195150 information on th* tutus of the lands shown horeon. This map Is not Mended for navigational, survey, or of rights and various sources. Completeness and awwracy are not guaranteed. Additional Information may also be obtained thtoofjh the Provincial Mining Recorders* office Tel: 1 (6B8) 4194845 ex* B7HlB^eaion: UTM 16 degree) flooding rights, Heencee, or other forms of disposition shown on this map l* compiled from tenure and land uses local Land Titles or Reejslry Office, or the Ministry of Natural Resources. Willet Green Miller Centre 833 Ramsey Lake Road fax ^ (877)6/0-1444 Topographic Data Source: Land Information Ontario Interest from the Crown. Also certain land Sudbury ON P3E 8B5 Mining Land Tmure Source! Provincial MWnfl Recorders' Office """ ""M" w Prohibit free entry to stake mining claims may not be The information shown Is derived from distal rjeta available !n the provincial Mining Recorders' office at the time of downloading from the Ministry of Northern Home Page: www.mndm.gov.on.ca/MNDMA1IN6S/LANDS/mlBmnpfle.htm illustrated. Development and Mines web site. Mining Land Tenure Map 31M03SW2008 2.25722 HEBERT 250
Date/Time of Issue: FrlJulH 14:17:08 EOT 2003 TOWNSHIP 7 AREA PLAN 610000E ELDRIDGE G-3426
ADMINISTRATIVE DISTRICTS l DIVISIONS Mining Division Sudbury Land Titles/Registry Division NIPISSING Ministry of Natural Resources District NORTH BAY
TOPOGRAPHIC Land Tenure
Surges And Wnlng BJMs
f"""] Ccnt*sst()ri,lDt
ri Provincial tat |H Mining Rights Only
Mton Resarvi Laarahold ft/ml
MM* Me S210000N JJttOOON
T, Hi™ B'IH*. LtaKMOlOeoUDMIttt j, Mltm HewJfrwtw
__ ROM ftvice And Mining RfgMf
,.,.,,,., Trill
...... ,.. ' NMunKUtKpetM
....., bmvas fm LSfO UM Perm,t \±M1 -f- ^omf f^l Ofdsr Ir* Council (Not open far staking)
I,.: j Wiler Power L.aseAjfMmani iiHiii Mining CWIm
IMPORTANT NOTICES
LAND TpNURE WITHDRAWAL DESCRIPTIONS Identifier Type Date Description
4851 Wim Jan 1,2001 FLOODING H.E.P.C. ELEVATION: 2(0 M FILE: 1165 VOL.3 L.O. 7447 W-L-56/S6 Wm Sep17,1W6 3EC.35 1(90 WJ.-5S/46NER 17/09/86 MSS AREA DEEMED IN NEED OF PROT C iSJMOOoN
Those wishing to state* mining claims should consult with the provincial Mining Recorders' Office of tha Ministry of Northern Development and Mine* for additional General Information and Limitations this map may not show unregistered land tenure and Interests In information on the status of the lands shown hereon. Thl* map is not intended tar navigational, survey, or lend title determination purposes as the Information Contact Information: Toll Free shown on thientap is compiled Map Datum: NAD 63 !and including certain patents, leases, easements, right of ways, from various sources. Completeness and accuracy are not guaranteed. Additional Information may also be obtained through the pro^nctol Mining Receivers' Office Tel" 1 (888)41S-984Sext67JWfcjectian' t/TM (6 degree) lean Land TWe* or Rejfsty Ofllce. or the MnMry of Natural Resources. flooding rights, licences, w oth*' forms of ofsposftfon of rights and Willet Oreen Miller Centre 033 Kamsey take Road Fax: 1 (en) 670-1444 Topographic Oaf* Source: Land Infonwrton Ontario interest from the CKWn. Also certain land tenure and l/uid use* Sudbury ON PSE 6BS Mining, land Tenure Source: Provtneisl Minine, Recorders' Office that restrict or prohibit tree entry to stake mining claims may not be The information shown It derived from digital data available In the Provincial Mining Recorders' Office at the time of downloading from th* Ministry of Northern HorM pm(V -w-, mt)Iln, am on ca/MNDM/MINBS/LANDSMtmnoae DevWopmmt*Bd Mm Illustrated. Mine* web site. ' ' '" ' ' " 31M03SW2008 2.25722 HEBERT 260
621200E 621400E 621600E 621800E 620600E 621000E en w o B
56984 56923 56891 56866 56840 56815 56791 56767 1 2489 1 8 56748 56730 56713 56689 56652 7-SV——-- -am-^ \ 56624 tO/-^ -rjgi )) \U 56602 56577 5,i!i, .rTTg^ '^yi^.t.d^t l i..-i 56561 56553 56546 56538 -^^359^^5--^ ~9*f VCxr"?^ 56531 '•- -t1fe^\^ 56525 in^-'-0\\\N\-- 56520 56515 56508 56496 56474 56446
56000 subtracted from all readings
1248923
K ry Q 9 2 Q f 6 d
i 621600E 621800E 620600E 621000E 621200E 621400E Tres-Or Resources Ltd. Grid U53 Hebert Township Scale 1:5000 Sudbury Mining Division, Ontario 50 50 100 150 200 250 300 Instruments: H Ground Geophysical Surveys GEM Systems GSM-f 9 Magnetometer Seriaf #712776 metres Total Field Magnetics NAD83 /UTM zone 1 7N SdntrexEOA OmniIVBase Station Serial#255228 Contours NTS 31 U14 Data Processing and Interpretation by: Scale 1:5000 Meegwich Consultants Inc. May 2003 31M03SW2008 2.25722 HEBERT
605200E 605400E 605600E 605800E 606000E
CTl M O O ro o o
57042 56876 56813 56783 56768 en ro 56755 o o 56742 o o 56729 o z. 56719 56711 56703 56697 '•^627 56691 631 602 56684 638 4-637-- 56679 648 en 56673 ?627 CD ' 654 to 56668 oo o 56663 600 o 56657 .590 •581 56653 •576 56648 574 "572 56641 574 546 56634 PS21 56626 485 56614 en 56584 (OCD 56536 O) o 56476 o-z.
56000 subtracted from all readings
en (D CD -p* O O
606000E
Tres-Or Resources Ltd. Grid 312 Hartle Township Scale 1:5000 Sudbury Mining Division, Ontario 50 O 50 100 150 200
metres Ground Geophysical Surveys Instruments: NAD83/UTM zone 17N Total Field Magnetics GEM Systems GSM-19 Magnetometer Serial #712776 Contours Serial#255228 ScintrexEDA OmnilVBase Station Data Processing and Interpretation by: Scale 1:5000 NTS 31 U13 Nleegwich Consultants Inc. May 2003 31M03SW2008 2.25722 HEBERT 280
601800E 602000E 602200E 602400E 602600E
(Astronomic)
i ''- - iiQ7 - - l ; / /- v "- L~*J?^--,\-:\::* b A,",
3 56706 683 56692 669 670 56687 667 657 56684 667 56681 660- 669 697 670 56678 S88,- 673 56676 6ff 672 67( 672 56675 671 674 56674 674 56672 676 678 56671 676 56670 673 667 56669 660 56668 653 658 56667 659 656 56666 56665 56664 661 56662 666 669 56661 668 669 56660 670 56658 671 672 56657 671 669 56655 667 56653 665 664 56650 662 56645 •A 661 660 56637 660
56000 subtracted from all readings
-W -' X-'""-;" ^Sf^S-fffX s- ^~-—~K-^-L r-i- ' -3513-'".--,//1/ TT-^^3 r.X/ -. '' 'i •-—r*Cr\s*s1?fsSS7W.f:3xS^i's'Xw/i/f' ~ ~—— ~:^--.— .-~ t i \ -~-/ fff/ifit't 'fh
601800E 602000E 602200E 602400E 602600E
Tres-Or Resources Ltd.
Scale 1:5000 Grids 310 and 311 50 50 100 150 200 250 Riddell Township Sudbury Mining Division, Ontario metres Instruments: GEM Systems GSM-19 Magnetometer Serial #712776 Ground Geophysical Surveys ScintrexEDA OmniIVBase Station Serial#255228 Total Field Magnetics Geonics EM-16 VLF Receiver Serial #10585 Contours VLF Station: NAA 24.0 kHz Cutler Maine Data Processing and Interpretation by: Scale 1:5000 NTS 31 M/4 Meegwich Consultants Inc. May 2003 31M03SW2008 2.25722 HEBERT 290
607200E 607400E 607600E 607800E 608000E 608200E
(flstooomej
538 CJl ro '1025 o 1069 ^ 887 M 902 o 1039 o 826 723 ^632 -616 756 538 731 '814 736 553 7J14 581 733; 697 56985 751' 779 746 en 56927 737 ro -811 o 56901 CO o 56873 o o 56844 56822 56804 56790 56777 56766 56755
Ui 56743 ro o 56732 oo oo 56721 o o 56710 56701 oBLO l GJ QJ.C 1,6 tS O) O O 56691 56682 56674 56665 56657 01 56648 ro o 56641 oo o 56632 o o 56624 56611 56591 16/ x /' 56557 732/''Rabbit
56000 subtracted from all readings O! ro o oo 4* o o
ro o OD ro o o w9 607200E 607400E 607600E 607800E 608000E 608200E
Tres-Or Resources Ltd. TEM^N-0203 Grid Eldridge Twp. Sudbury Mining Division, Ontario Scale 1:5000 50 50 100 150 200 250 Ground Geophysical Surveys Instruments: Total Field Magnetics GEM Systems GSM-19 Magnetometer Surial #712776 metres Contours Omni IV Base Station Serial #255228 (UTM NAD 83, Zone 17) Data Processing and Interpretation by: Scale 1:5000 NTS 31 M/4 Meegwich Consultants Inc. May 2003 31M03SW2008 2.25722 HEBERT 300
601200E 601400E 601600E 601800E 602000E 602200E 602400E 602600E en
1 243262
en o 09 O O 1 248996
en N) o w00 o o
T24 4-707;- ' ^723ne -705; 56839 71 699 -71 cr 56812 -70S -703' en 56796 M o 56786 OD 56778 O O 56771 O 56765 56760 56755 56749 56744 56738 56733 56728 os 56724 o 56721 "Z.o 56718 56715 56713 - -BLON 56710 56708 56705 en 56703 ro o 56701 56698 o o 56695 56690 1248993 56683
56000 subtracted from all readings
o .668 o -673- y 6S9-. 666 66? 667 669. -631.- -673.-
en M -•JO Casses Lake ro o o
601200E G01400E 601600E 601800E 602000E 602200E 602400E 602600E
Tres-Or Resources Ltd. Grids U73 and 306 Riddell Township Sudbury Mining Division, Ontario Instruments: GEM Systems GSM-19 Magnetometer Serial #712776 Scale 1:5000 ScintrexEDA Omni IVBase Station Serial#255228 50 50 100 150 200 250 300 350 Ground Geophysical Surveys Geonics EM-76 VLF Receiver Serial #10555 metres Total Field Magnetics VLF Station: NAA 24.0 kHz Cutler Maine NADB3/UTM zone 17N Contours Data Processing and Interpretation by: Scale 1:5000 NTS 31 M/4 Meegwich Consultants Inc. May 2003 31M03SW2008 2.25722 HEBERT 310
601800E 602000E 602200E 602400E 602600E
——— In-Phase
•---•Quadrature
Profile Scale: 1 cm =
rn m
601800E 602000E 602200E 602400E 602600E Ires-Or Resources Ltd, Grids 310 and 311 Scale 1:5000 Riddell Township 50 150 200 250 Sudbury Mining Division, Ontario
Instruments: GEM Systems GSM-19 Magnetometer Serial #712776 Ground Geophysical Swveys Scintrex EDA Omni IV Base Station Serial #255228 VLF - EM Survey Geonics EM-16 VLF Receiver Serial #10585 Profiles of the In-Phase and Quadrature VLF Station: NAA 24.0 kHz Cutler Maine Data Processing and Interpretation by: Scale 1:5000 NTS 31 M/4 Meegwich Consultants Inc. May 2003 31M03SW2008 2.25722 HEBERT 320
601200E 601400E 601600E 601800E 602000E 602200E 602400E 602600E en K) o ea O)o o Z
o co 45. o o Z
OJ 1248996 o o
o CO K) oO Z
O zO
tn ro o CO o o o
ro o o
tn K) -vio oo o o Z
-BLON
ro o
O O Z Conductor Axis, Defined 1248993 ro Conductor Axis, Interpreted o o co 5901 en ro o o o ™—— In-Phase
•---•Quadrature
o o CO
en ro -vio ro o o Profile Scale: 1 cm = 20J0
m
J 601200E 601400E 601600E 601800E 602000E 602200E 602400E 602600E
Ires-Of Resources Ltd. Grids U73 and 306 Riddell Township Sudbury Mining Division, Ontario Instruments: GEM Systems GSM-19 Magnetometer Serial #712776 Scale 1:5000 ScintrexEDA Omni IVBase Station Serial #255228 50 50 100 150 200 250 300 350 Ground Geophysical Surveys Geonics EM-16 VLF Receiver Serial #10585 VLF - EM Survey VLF Station: NAA 24.0 kH2 Cutler Maine Profiles of the In-Phase and Quadrature
Data Processing and Interpretation by: Scale 1:5000 NTS 31 M/4 Meegwich Consultants Inc. May 2003 TRES~QR RESOURCES LTD Superior Crton Block
^ m
"'^'^^^t^^^Si^aii^lP'-
^^v^lip^it^^^SN\^\\\\^^^;'','^'AV'-^-'---' ^i:^|S^^~S^^rr-t-S^3:3 feS;^-:/ 'V^SSS/I "SI 'v^ N^4\\\^S^S'S^ ^6^=5—!™^^ ;:'-- i""?
SPIT
r"^sH"""--.wiijw ~~ '-of-'••:' -' /Yf*ffrM?v~-sTl \ !fj'~~±n"' "insS^i
31M03SW2008 2.25722 HEBERT 330