ODLUM 010
SUMMARY REPORT ON THE EXPLORATION OFTHE WHITE RIVER Au PROPERTY
WHITE RIVER, ONTARIO
FOR
AKIKO GOLD RESOURCES LIMITED
NTS 42C 110, 11, 14, 15
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A.C.A. HOWE INTERNATIONAL LIMITED Daniel Leroux, BSc. Report # 692 November 15, 1993
SAULT 9F E. UAflE MINING DIVISION RECEIVED
AM17 NOV1993 PM
7,8,9,10,11112,11213,4,516
l^^ 42C10NW89e0 2.15248 ODLUM 010C
l TABLE OF CONTENTS PAGE
B SUMMARY l
I.0 INTRODUCTION 2
l 2.0 LOCATION, ACCESS AND PROPERTY DESCRIPTION 2
1 2.1 Location 22.2 Access 22.3 Property Description 2
" 3.0 PERSONNEL 4
l 4.0 PREVIOUS WORK 4
5.0 LAND STATUS 5
" 6.0 PROJECT DESCRIPTION 5
l 7.0 GEOLOGY 7
7.1 Regional Geology 7g 7.2 Property Geology 7
7.21 Table of Lithological Units 8
1 7.22 Structure 117.23 Mineralization 12
7.3 Geochemical Humus Survey 13m 7.4 Geophysical Survey 13
8.0 DISCUSSION OF RESULTS 13
l 9.0 CONCLUSIONS AND RECOMMENDATIONS 14
B 10.0 REFERENCES
II.0 STATEMENT OF QUALD7ICATIONS
l FIGURES1. Location Map
1 2. Claim Map 3. Geology Map at 1:5000 ( North and South sheets ) 4. Reconnaissance Road Map at 1:20000
1 5. Geochemical Humus Sampling Survey at 1:5000 ( North and South sheets) 6. Geophysical Interpreted Geology at 1:5000
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l l APPENDICES
I A. Geochemical Rock Sampling Results ( certificates ) B. Rock Sample Descriptions C. Geochemical Humus Sampling Results ( certificates )
I D. Claim Information E. Geophysical Report
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SUMMARY
A.C.A. Howe International Limited ("Howe") has been retained by Akiko Gold Resources Limited ("Akiko Gold") to conduct a grass-roots exploration program consisting of geological mapping, prospecting and sampling, geochemical humus sampling and a ground MAG-VLF survey of Akiko Gold's claim block situated approximately 40 kilometres northeast of White River Ontario. This assessment report summarizes the geological, geochemical and geophysical work performed on the property from September l to 30, 1993.
The Dayohessarah Lake Greenstone Belt is a 30 km by 6 km arcuate shaped belt that trends in a north-northwest direction. The greenstone belt is composed of Archean metavolcanic and metasedimentary rocks that have been intruded by felsic and mafic-ultramafic dykes, sills and stocks and is surrounded by granitic to intermediate stocks and batholiths. The belt is located approximately 40 kms northeast of White River Ontario and is situated between the gold producing Hemlo greenstone belt to the west and the Kabinakagami greenstone belt to the northeast.
A 66.0 line km grid was cut in order for Howe's personnel to carry out the various geotechnical surveys and sampling programs. Geochemical humus sampling, ground MAG- VLF EM surveying and geological mapping and sampling was completed on the property. The geological mapping and sampling program has outlined a 500 metre wide, moderately to strongly foliated "deformation zone" with a strike length of approximately 5.0km. Within this zone a well foliated and/or sheared debris flow-agglomerate unit, trending, 160 degrees can be traced for approximately 4.5 km. This weakly magnetic unit is dextrally offset (NE- SW) near L 18S and locally contains sporadic quartz veins/veinlets. Also within this zone, intrusions of quartz-feldspar porphyries, granites, gabbros and felsic pegmatites occur throughout this zone and are generally parallel to the foliation. Ninety-eight rock samples were taken on the property and 15 samples assayed > 10 ppb Au. The highest gold assay was 35 ppb Au and was obtained from a well foliated and/or sheared porphyry. Two thousand and three (2003) humus samples were collected on the property, with 25 samples assaying > 10 ppb Au. The highest value obtained was 25 ppb Au which is located at L 30 S/ 550 W.
A two phase exploration program, consisting of a first phase horizontal loop EM or induced polarization (IP) survey over the deformation zone is recommended. Follow-up stripping, geological mapping and sampling program should focus on any geophysical anomalies. Reconnaissance geological mapping along the northeastern portion of the claim boundary is recommended in order to determine whether Noranda's "Sugar Vein" gold occurrence strikes onto Akiko's claim block. Based on the results obtained from the phase I program, phase II would consist of a diamond drill program to evaluate any geophysical targets.
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1.0 INTRODUCTION
At the request of Akiko Gold Resources Limited ("Akiko"), A.CA. Howe International Limited ("Howe") has undertaken to prepare a report summarizing the exploration work recently completed on Akiko's White River property. The main focus of the exploration program was to determine if the deformation zone hosting the "Sugar Vein" Au occurrence located within Noranda Exploration's claim block, 5.6 km north of Akiko's claim boundary, was present on Akiko's property. Preliminary geological reconnaissance work was conducted by R. Irwin, on behalf of Akiko Gold. Geochemical rock samples representative of the various lithologies found on the property were taken in order to locate zones of possible mineralization. More extensive exploration work was conducted during September l to 30, 1993 and included a 66.0 line km grid where a detailed geophysical survey (ie: MAG and VLF ) and a geochemical humus survey were conducted to determine possible Au anomalies. Detailed geological mapping and sampling at a scale of l: 5000 was conducted within the grid area and a 1:15000 reconnaissance road mapping program was completed to establish the location and trend of the contact between the mafic volcanic - metasedimentary rocks on the eastern section of the greenstone belt. With the permission of Noranda Exploration, geochemical, geophysical and geological orientation surveys were conducted on the "Sugar Vein" Au occurrence. Results of these surveys are not included in this report.
2.0 LOCATION, ACCESS AND PROPERTY DESCRIPTION
2.1 Location
Akiko Gold's White River property is located approximately 40 km northeast of the town of White River, Ontario ( figure l ) between Dayohessarah Lake to the north and Hwy. 631 to the south. The claim block is located within Odlum, Tedder, Strickland and Cooper townships.
2.2 Access
The property is easily accessible from White River, Ontario via Domtar gravel logging roads ( road 100 and 200 ). Numerous secondary logging roads (ie: roads 206, 213, 207 D and B ) extend within the property and grid area provide further local access.
23 Property Description
The White River property is dominated by a number of N-S trending lakes and ponds with numerous alder, cedar swamps and wetlands also present. The area is considered
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AKIKO GOLD RESOURCES LIMITED WHITE RIVER GOLD PROJECT
LOCATION MAP
FIGURE 1.
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somewhat rugged with numerous hills and cliffs 10-15m in height. Wind and/or deadfall is widespread throughout the grid area making traversing locally difficult. The area has been logged by Domtar during the late 1980's and large cut-over areas now exist along the secondary logging roads.
3.0 PERSONNEL
The following personnel were involved in the geological mapping and sampling, and the geophysical and geochemical surveys performed on the property.
Dr. Wayne D. Ewert GeologistDaniel C. Leroux GeologistMichael C. Wilson Geophysical OperatorHarry Claridge Geochemical TechnicianChristopher Keith Geochemical TechnicianRay Irwin Geologist
4.0 PREVIOUS WORK
Since 1958, the Dayohessarah Greenstone Belt has seen numerous exploration companies conduct work in the area. Various companies such as Canadian Pacific Railway (1958), Canex Aerial Exploration Limited (1969), and Shell Canada (1975) conducted various geotechnical surveys on portions of the greenstone belt.
Between 1983 -1986, Pezamerica Resources Corporation subcontracted Dighem Surveys and Processing Ltd. to conduct airborne EM and MAG surveys over the entire Dayohessarah Greenstone Belt. The airborne surveys outlined thirty-one airborne anomalies. A follow up two phase work program conducted at the request of Teck Exploration Ltd. consisted of regional mapping, soil sampling, and detailed airborne anomaly follow-up. The geochemical survey obtained 35 anomalous samples that were > 26ppb Au and outlined a large soil gold geochem anomaly on the west side of Dayohessarah Lake. This exploration work was followed up by a diamond drill program which tested nine of the airborne geophysical anomalies. Drilling indicated that these anomalies were related to substantial amounts of pyrite and pyrrhotite within a sequence of felsic volcanic rocks. None of the drill holes intercepted any gold anomalies. Hole PZ-6 intersected a zone of stratiform pyrite and pyrrhotite with minor amounts of sphalerite. This intersection returned an assay of Q.47% Zn over 2.8 feet.
In 1988, United Reef Petroleums Ltd. subcontracted Stratigraphic Research toconduct a total field magnetic survey of the greenstone belt. The survey outlined linear NW-
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trending magnetic highs on the western shore of Dayohessarah Lake. No further follow-up work was reported.
In 1989, Terraquest Ltd. at the request of Broad Horizons conducted an airborne MAG and VLF-EM geophysical survey over the central and southern portion of the greenstone belt. This airborne survey duplicated the geophysical anomalies detected by the Pezamerica Dighem surveys of 1983.
In 1990, Hemlo Gold Mines Inc. in conjunction with Noranda Exploration Company Ltd. conducted a reconnaissance geological mapping and prospecting program along the eastern shore of Dayohessarah Lake which outlined sulphide-rich quartz veins within a deformation zone approximately 200m wide and trending 320 to 335 degrees along a strike length of 600m. This work program was successful in outlining the "Sugar Vein" which is a 25-30m wide zone of quartz veining containing polymetallic sulphide and gold mineralization occuring within this deformation zone. Visible gold has been noted in some samples.
Between 1990 and 1993, a legal dispute took place between Broad Horizons and the claim holders. During this period, all work was suspended pending a settlement of the case.
In 1992, at the request of Gold Giant Limited, Orequest Consultants Ltd. conducted a regional geological appraisal of Gold Giant's claims in the White River area. It was recommended that a two phase exploration program be recommended to further evaluate the property.
5.0 LAND STATUS
Appendix D is a list of claim holdings ( 256 contiguous claims ) defining Akiko Gold Resources Limited White River property upon which the exploration work was performed. These claims are located within Odlum, Tedder, Strickland and Cooper Townships ( figure 2 ). All of the claims lie within the Sault-Ste-Marie mining division. The claim block was staked by a prospecting syndicate (ie: J. Ternowesky and P. Nabigon) in 1987-88. An option agreement covering these claims exists between the staking syndicate and Akiko Gold and Gold Giant Minerals Ltd..
6.0 PROGRAM DESCRIPTION
A line cutting company was subcontracted by Howe to cut a 66.0 line km, non-surveyed, grid on the claim group. The 0+00 base station was established 25 m east of a N-S linear lake situated 1.0 km east of Dayohessarah Lake ( Figure 4 ). A 5.6 km non-transited baseline
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AKIKO GOLD RESOURCES LIMITED IffllTE RIVER COLD PROJECT
CLAIM MAP
prcpof*J tl A.CA Mi-* FIGURE 2.
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at an azimuth of 160 degrees was established with 29 cross-lines trending at 250 degrees cut every 200 metres. West of the baseline, cross-lines were cut to 800 metres whereas cross- lines east of the baseline were cut to 1200 metres. Two tie lines at 160 degrees were cut for grid control purposes. Picket spacing was established at 25 metre intervals on all of the cut lines.
Detailed and reconnaissance geological mapping, prospecting and sampling at 1:5000 and 1:15000 scale was conducted on and off of the grid area. The reconnaissance road mapping program was concentrated towards the western portion of the property. Geochemical humus sampling was conducted at 25 metre sampling interval east of the baseline and at a 50 metre sampling interval west of the baseline. A ground MAG-VLF survey, utilizing an EDA OMNI PLUS magnetometer/VLF-EM receiver and base station system, was completed on the grid.
7.0 GEOLOGY
7.1 REGIONAL GEOLOGY
The rocks located around Dayohessarah Lake are part of the Dayohessarah Lake greenstone belt an arcuate shaped, north-northwest trending belt of rocks that is approximately 32 km long by 6 km wide. The belt is situated between the gold producing Hemlo greenstone belt to the southwest and the Kabinakagami greenstone belt to the northeast and consists of a central zone of metasedimentary rocks which is flanked and underlain to the east and west by mafic volcanic flows and tuffs. The Dayohessarah greenstone belt is flanked and intruded by a series of felsic igneous intrusions and/or batholiths (ie: granites, granodiorites, etc.). Minor mafic to ultramafic stocks occur along the north shore of Dayohessarah Lake and in the southern portion of the belt. Diabase dykes cross-cut the belt along NE-SW and NW-SE directions.
7.2 PROPERTY GEOLOGY
Geological mapping and regional road mapping and prospecting was conducted on Akiko Gold's claim block situated approximately 2 km south of Dayohessarah Lake (figure 3 ). A cut grid was established southeast of Dayohessarah Lake and is oriented at an azimuth of 160 degrees ( figure 4 ). The rocks underlying the grid are predominantly foliated and/or massive mafic volcanics (amphibolite - Ib) with metasediments identified to the west and granitic rocks to the east. These rocks have subsequently been locally intruded by a series of dioritic-gabbroic and hornblendite stocks, quartz-feldspar porphyries, granites, pegmatites and diabase dykes. Within the mafic volcanic sequence, a unit of moderate to strongly foliated and/or stretched, multi-lithic debris flow l agglomerate has been identified
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and can be traced for a strike length of approximately 6 kms. This unit is generally in contact with the fragmental amphibolite ( Ib - frgm) or with the foliated amphibolite (Ib). Occassionally quartz veins, veinlets, and sweats are present in the mafic volcanics. Structurally, the debris flow l agglomerate unit has been extremely sheared and contains numerous micro structures such as flexure slip folding and brittle/ductile fracturing. Local oxidized/limonitic patches occur but no visible sulphide mineralization was noted.
The metavolcanic rocks represent a mix of massive and pillowed mafic flows which have been metamorphosed to upper greenschist - lower amphibolite facies. Locally, mid- to upper amphibolite facies occur with most of these rocks converted to moderately to well foliated amphibolite rich equivalents.
The metasedimentary rocks within the property were probably derived from the local meta volcanic suite of rocks. At the contact between the central metasediments and metavolcanics to the east, the metasediments grade from a narrow garnet-rich schistose biotite metasediment to an interbedded siliceous wacke/greywacke to the west. These rocks have been metamorphosed to lower amphibolite facies.
The intrusive rocks on the property are predominantly medium to coarse grained granites and granodiorites with pegmatitic dykes and sills intruding the sequence locally. To the east, granitic rocks of various compositions intrude the metavolcanics stoping out portions of these mafic volcanics as xenoliths of amphibolite which often retain their original orientations ( foliation at 160 deg. ). Northeast - southwest trending diabase dykes cross-cut the metavolcanic/metasedimentary package. These dykes are off-set in a NW-SE direction ( dextral ).
The following section is a summary of lithological units observed on the property with a general description of each unit.
7.21 Table 1: Table of Lithological Units
1. MAFIC METAVOLCANIC ROCKS
la) Massive amphibolite (mafic flows)
Green to dark green-black, massive, very fine to fine grained, weakly to moderately foliated, with approximately 4596 hornblende, 2596 quartz, 1096 plagioclase, 10*8* biotite, and 1096 accessory minerals (ie: epidote, apatite, etc. ). Biotite books and trace sulphides occur locally.
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Ib) Foliated amphibolite
Green to dark green-black, fine to medium grained, moderately to well foliated, weakly to moderately sheared locally, with approximately 35-4096 hornblende, 20-2596 quartz, 1596 plagioclase, 15-2096 biotite, and < 2-596 accessory minerals present in unit. The fragmental variety of the foliated amphibolite (ie: Ib-frgm ) contains wisps of stretched and/or boudinaged felsic veinlets which are parallel to the foliation of the unit.
le) Pillowed amphibolite ( pillowed mafic flows )
Dark green to black, fine to medium grained, homogeneous, weakly chloritic, with remnant amygdules and pillow selvages structurally elongated and distorted at 160 degrees. Local elongated epidote blebs/clots trend at 160 degrees.
ld,e) Debris flow/agglomerate and/or an epiclastic interflow metasediment/tuff
Multi-lithic debris flow/agglomerate with well foliated and elongated fragments of felsic and mafic material. This unit has same foliation as the mafic volcanics. Locally, the unit is either mafic or felsic rich in fragments. Overall, the mafic fragments have a maximum stretch ratio of 50:1 whereas the felsic fragments have a maximum ratio of 25:1. Few random oxidized-limonitic spots present but no visible sulphide mineralization noted.
2. METASEDIMENTARY ROCKS
2a,b,c) Siliceous wackes/greywackes (2a), sandstone/siltstones (2b) and rusty siltstone/wackes (2c)
These rocks are light grey to grey in colour, very fine to fine grained, moderately to well bedded quartz-rich wackes/greywackes/siltstones which are moderately to strongly foliated at @ 160 deg.. Locally, the matrix can be moderately to strongly siliceous.
2d) Amphibolite metasediment with garnets
Light brown to moderately limonitic, very fine to fine grained, moderately to strongly foliated and/or schistose, biotite-rich ( 35-4096 ) metasediment with clots of disseminated, anhedral to subhedral garnets ranging in size from 1mm to 5 mm in diameter.
3. MAFIC INTRUSIVE ROCKS
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3a) Gabbro l gabbro porphyry
Green to dark green, medium to coarse grained, massive, homogeneous, anhedral hornblende-rich gabbro with fine to medium grained Ca-plagioclase present. These rocks occur either as plugs or stocks and have locally intruded the mafic volcanics.
3b) Hornblendite
Green to dark green, medium to very coarse grained, massive, homogeneous, anhedral to subhedral hornblende - rich ( 70*26 ) hornblendite with 2096 Ca-plagioclase and trace sulphides (ie: pyrrhotite, pyrite, magnetite ) present. Generally, unit is slightly magnetic.
3c) Diorite
Green to dark green, medium to coarse grained, massive, hornblende - rich (5096) diorite with 3096 plagioclase and 2096 quartz present. Locally, the diorite appears to become porphyritic as the hornblende becomes coarser grained ( type of enrichment ? ). Diorite dykes and plugs seem to intrude only the pillowed flows (le).
4. GRANITIC INTRUSIVE ROCKS
4a) Granite
Light to moderately pinkish in color, massive, heterogeneous, equigranular and moderately to strongly foliated locally. Mineralogically, the unit is generally composed of quartz (4096), K-feldspar (2096), biotite (2096), plagioclase (1596) and accessory minerals (596). These rocks occur as stocks, and/or dykes within the mafic volcanic - metasediment package. A large intrusive body is also in contact with the mafic volcanics to the east.
4b) Granodiorite
Light grey to moderately grey/black ( color index - 25 ), medium to coarse grained, equigranular, massive granodiorite and is moderately to strongly foliated locally. Mineralogically, the unit is composed of biotite (3096), quartz (2596), plagioclase (2096), hornblende (1596), and accessory minerals ^596). These rocks occur as dykes, sills or stocks and occur with or in contact with the granitic phases throughout the property.
4c) Pegmatite
Pinkish white, very coarse grained, massive, heterogeneous, quartz-rich (4096) pegmatite with anhedral to subhedral K-feldspar (3596), and fine to medium grained plagioclase (2596) present. This unit occurs as dykes, sills and/or stocks and intrude both the metavolcanics
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5. LATE FELSIC INTRUSIVE ROCKS
5a) Quartz-feldspar porphyry
Light grey to dark grey, slightly pinkish locally and porphyritic where the phenocrysts are moderately to strongty foliated and/or stretched locally. Phenocrysts are dominantly composed of quartz that are elongated locally to form quartz - eyes and K-feldspar crystals being less competent than quartz, are extremely elongated ( up to 50:1). In some areas, the K-feldspar are so stretched that they can be mistaken for layering or banding. The matrix is aphanitic and is composed of quartz, plagioclase and occassionally biotite. Trace to < 296 disseminated pyrite and chalcopyrite occurs locally in these rocks.
6. PROTEROZOIC INTRUSIVE ROCKS
6a,b) Diabase l porphyritic diabase
Green to dark green, light brown on weathered surface, fine to medium grained, slightly to moderately magnetic, massive, equigranular diabase with 'felty* feldspar laths present. The porphyritic equivalent has the same mineralogy except for very coarse grained anhedral phenocrysts of plagioclase ( from lcm to 5cm in diameter ). Visible fine grained anhedral magnetite crystals ( < l%) are present locally.
7.22 STRUCTURE
The Dayohessarah Lake greenstone belt is arcuate in shape and is approximately 32 km long by 6 km wide. The belt is clearly defined as a symmetrical syncline which appears to plunge southward and the fold hinge trends approximately 335 - 340 degrees. The hinge is located within the metasediments which are positioned centrally to Dayohessarah Lake. Regional foliations and bedding trend at 320 to 340 degrees but dip steeply to the west along the eastern limb and steeply to the east on the western limb of the syncline.
Within the property, foliation measurements within the mafic volcanics and bedding features in the metasediments are generally 160 degrees and steeply dip to the west from 70 to 90 degrees. A deformation zone, approximately 300m wide and in excess of 4.5 km
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long occurs near the metavolcanic-metasedimentary contact. This deformation zone is characterized by moderately to strongly foliated and/or sheared amphibolites, extremely stretched debris flows and major intrusive activity. The multi-lithic debris flow/agglomerate unit contains mafic and/or felsic rich fragments that has been stretched in accordance with their respective competencies in a south-east direction. Numerous generations of intrusive activity occur within this deformation zone. Quartz-feldspar porphyries, granites, pegmatites, gabbro-hornblendite, diorites and diabase all occur within the property. The porphyries show evidence of stretching and shearing within the bodies and along contact margins. Very few wide quartz veins were noted within the mafic volcanics or quartz-feldspar porphyries.
The metasediments are characterized as being well bedded units where local micro- structures such as S and Z folding, kink banding and stretching have occurred. Tension gashes and ptygmatic veinlets infilled with quartz (ie: quartz sweats ) do occur but no visible mineralization has been found.
7.23 MINERALIZATION
Geological mapping of the grid area has resulted in the discovery of a 20cm wide oxidized- limonitic band trending at 160-165 degrees which can be traced for over 700m between lines 6+00 S and L 14+OOS. This band contains trace to < 196 anhedral disseminated pyrite and chalcopyrite and is hosted by a foliated amphibolite unit (Ib ) that is weakly to moderately sheared. This shear cross-cuts the foliation and dips 50 degrees to the east. Within this horizon, a series of discontinuous quartz veins occur within a quartz-feldspar porphyry which intrudes the foliated amphibolite. These quartz veins vary in thickness and are generally oriented parallel to the porphyry. No visible mineralization was found.
Pyrite mineralization was found mostly in the foliated amphibolites and in the quartz- feldspar porphyries. The pyrite occurs along foliation planes or within micro-fracture patterns in the amphibolites whereas in the porphyries, it was mainly disseminated and fine grained.
A small, narrow altered felsic intrusive containing molybdenite rosettes up to lcm in diameter was discovered between line 2+00 S and line 4+OOS at 4+OOE. The intrusive was adjacent to a quartz-feldspar porphyry which intruded the surrounding mafic volcanic package.
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7 J GEOCHEMICAL SURVEY
A total of 2003 humus samples were taken on the grid in order to aid in defining anomalous Au zones that could be investigated later by rock sampling or stripping. The sample site was prepared by utilizing a shovel to expose the humus/soil profile. The samples were then collected by hand and all roots or non-decomposed material discarded so that only a fresh, black, organic-rich material was placed into humus sample bags individually labeled with the grid coordinates of the sample site. These samples were then sent to XRAL Labs in Don Mills, Ontario for Au assay where they were oven dried ( 70 degrees C ), blended and pressed to form a 4mm diameter by 4mm thick briquette (disc). Briquettes were bundled in lots of 38-40 in polyethylene wrap for irradiation. Irradiation is accomplished by placing the bundle into an irradiation cylinder which is lowered into a preselected site at the edge of the reactor core. After a one hour exposure the samples are removed and placed in storage for 8 to 9 days to allow undesirable background radiation to decay. After this cooling off period, the samples are analysed for the elements requested. The analytical instrument is a multi channel analyser connected to a pacified hyperpure germanium detector. Results of the geochemical survey are pending and will be submitted in its entirety in a follow-up report.
All geochemical rock samples were sent to XRAL Labs in Don Mills, Ontario for Au assay utilizing the fire assay method with direct current plasma finish after dissolution of the fire assay bead. The samples were assayed at l assay ton with detection limits of l ppb Au. Of the 147 rock samples, only 15 samples returned values > lOppb Au. The highest value obtained was from sample 2329 which assayed at 35 ppb Au. This sample was obtained from a fine to medium grained, moderately to strongly foliated porphyry with numerous qtz veinlets present (see Appendix C ). This sample is located at L 33+00 S, 8+05 W.
7.4 GEOPHYSICAL SURVEY
A 66.0 km ground MAG-VLF survey was conducted in order to define zones of possible deformation with mineralization that resembles the 'Sugar Vein' deformation zone located on Noranda's claim block to the north of Akiko Gold's claims. The results and interpretations of the geophysical survey are documented in Appendix D.
8.0 DISCUSSION OF RESULTS
The geological mapping and sampling program has been successful in outlining areas of interest within the property. Firstly, a debris-flow/agglomerate unit (ld,e) has been identified along a strike length of 5.0kms. This unit contains numerous mafic and/or felsic clasts which have been elongated or stretched at a ratio of 50:1. The rocks are strongly sheared locally and evidence of micro-folds and kink banding are present. This stratigraphic package is
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considered similar to that hosting the "Sugar Vein" on Noranda's property along trend to the north. The highest Au assay obtained from this unit is 15 ppb Au. The geological contacts between the metasediments-metavolcanics and the metavolcanics-granitic rocks have been located on the property and are depicted on the geological map at 1:5000. Establishing the limits of the major lithologic units is considered important in outlining horizons similar to those hosting known mineralization on adjoining properties.
The highest gold rock assay on the property was obtained from sample 2329 which assayed at 35 ppb Au. It was sampled from a porphyritic unit located at L 33+OOS; 8+25W. The MAG-VLF geophysical survey helped in delineating the geological units on the property. Numerous NW-SE and NE-SW diabase dykes have been identified via geophysics and correspond with the mapping of the property. The geochemical humus sampling program was successful in determining 50 anomalous Au targets. These anomalies are significant as they are oriented parallel (NW-SE) to the foliation of the regional geology of the area.
9.0 CONCLUSIONS AND RECOMMENDATIONS
The exploration program has identified a major deformation zone of approximately 4.5-5.0 km long by 500 metres wide where the mafic volcanics are moderately to strongly foliated and/or sheared at 160 degrees. The deformation zone is characterized by a well foliated and/or elongated debris-flow/agglomerate that trends at 160 degrees and can be traced for approximately 4.5 kms. Within this deformation zone, felsic and mafic intrusive activity occurred and is comprised of quartz-feldspar porphyries, gabbros and granites. To date, only sporadic narrow quartz veins have been observed.
In order to explore this zone more thoroughly, a two phase program is recommended to further evaluate the White River property. Phase I will consist of either a horizontal loop EM or induced polarization survey in order to locate any conductive sulphide horizons within the deformation zone. If anomalous targets are located, a follow-up detailed stripping, mapping and sampling program is recommended in order to determine the source and type of mineralization. Further reconnaissance geological mapping and sampling along the northeastern portion of the claim boundary is recommended in order to determine if the "Sugar Vein" gold bearing deformation zone can be traced into Akiko's claim block. Based on the results of the above program, phase II would consist of a diamond drill program to evaluate any significant anomalies.
lI 10.0 REFERENCES
" Fenwick, K.G., 1967 Geology of the Dayohessarah Lake Area; ODM Report 49; 16 pp.
* Londry, J., 1990. Geology Report - Dayo Project; Noranda Exploration Company Ltd.;Assessment Report; API # 2.14806
Londry, J., 1990. Geochem Report - Dayo Project; Noranda Exploration Company Ltd.; Assessment Report; API # 2.14740
Petersen, D., 1988 Assessment Report on Reconnaissance Soil and Rock Geochemistry;
I Dayohessarah - 1138; Noranda Exploration Company Ltd.; API # 2.11785.
I Scott, G., 1993 Report on the White River Project, Northwestern Ontario for Gold Giant Minerals Ltd.; Orequest Consultants Ltd.
I Tindall, M., 1985 Geological and Geochemical Report on the 1985 Summer Exploration Program - Operation Pezamerica; Mascot Gold Mines Ltd.; Piche # Hambleton - 0021.
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ll 11.0 STATEMENT OF QUALIFICATIONS
l I, Daniel Leroux, HEREBY CERTIFY THAT:
l 1.1 am a practising geologist with A.C.A. Howe International Limited in Toronto, Ontario and reside at 326 Major MacKenzie Drive East, Unit # 122, Richmond Hill, Ontario.
l 2.1 am a graduate of Laurentian University, June 1993 with a degree of Bachelor of Science in Geology.
B 3.1 have practiced my profession for approximately l year since graduation and have been employed in the mineral exploration industry since 1988.
' 4.1 hereby certify that I have personal and intimate knowledge of the facts set forth in this report, having performed the work or witnessed same during and/or after its completion and
l report it is true.
5. I have based conclusions and recommendations contained in this report on knowledge l obtained from work conducted on the property between September l, 1993 and September U 30, 1993.
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I dated at Toronto, Ontario November 15, 1993
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l l l l l ll APPENDIX A - GEOCHEMICAL ROCK SAMPLING RESULTS
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1 TO: A. C. A.
A i X-RAY ASSAY LABORATORIESf^L ^^ A DIVISION OF SGS CANADA INC.
m '^ 1 885 LESLIE STREET - DON MILLS. ONTARIO MSB 3J4 - CANADATEL: (416)445-5755 TELEX: 06-986947 FAX: (416)445-4152
CERTIFICATE OF AJNTAIL, Y S I S
REPORT 24422 '0CT - 5 1993
HOWE INTERNATIONAL LTD1 ATTN: DINO TITARO CUSTOMER No. 1943" 22 FRONT STREET WEST, SUITE 1400
TORONTOm M5J 1C4
1 REF
, ONTARIO DATE SUBMITTED20-Sep-93
. FILE 16172-U6 Total Pages 1
B 13 ROCKS Pro j . WHITE RIVER
1
1
METHOD DETECTION LIMITAU-1AT PPB FADCP 1.
1 *** UNLESS INSTRUCTED OTHERWISE WE WILL DISCARD PULPS IN 90 DAYS ***
1
1
1
1
1
1
1
AND REJECTS IN 30 DAYS FROM THE DATE OF THIS REPORT
/i HA
I HATF m Oft-— en PFPTTFTFD RV j^^C^iAi?C*-^ut*^--^\Jean H. L. Opdefeeck, General Manager \
1t ' -*
Member of the SGS Group (SociEtE GEnErale de Surveillance) ~"
fXRAL01-Oct-93
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SAMPLE AU-1AT PPB
2301 42302 22303 32304 32305 4
23062307230823092310
231123122313
273
•d42
912
REPORT 24422 REF.FILE 16172-U6 PAGE 1 OF 1
AU-1AT PPB - ASSAY PERFORMED ON 30 GRAM ALIQUOT
X-RAY ASSAY LABORATORIES 1885 Leslie Street Don Mills Ontario M36 3J4 (416)445-5755 Fax (416)445-4152 Tlx 06-986947Member of the SGS Group (Societe Centrale de Surveillance)
1 XR| *
l
* i X-RAY ASSAY LABORATORIESAV 1^- A DIVISION OF SGS CANADA INC. * * * 1885 LESLIE STREET * DON MILLS. ONTARIO MSB 3J4 * CANADA
TEL: (416)445-5755 TELEX: 06-986947 FAX: (416)445-4152
CERTIFICATE OF AJSTAILYSIES
REPORT 24469
TO: A. C. A. HOWE INTERNATIONAL LTD
I ATTN: DINO TITARO CUSTOMER No. 1943 22 FRONT STREET WEST, SUITE 1400TORONTO
- M5J 1C4
1
B REF
, ONTARIO DATE SUBMITTED24-Sep-93
. FILE 16198-RO Total Pages 1
g 22 ROCKS
1
1
METHOD DETECTION LIMITAU PPB FAAA 5.
1 *** UNLESS INSTRUCTED OTHERWISE WE WILL DISCARD PULPS IN 90 DAYS ***
1
1
1
1
1
1
1
AND REJECTS IN 30 DAYS FROM THE DATE OF THIS REPORT
l//*
I DATE 39-flr!*--Q7 CKPTTFTEH R V ST^^-Q^^vV^TV . A. . . .
1
Jean H. L. Opdeoeeck. /General Manager }' J.—. — - ——— —
Member of the SGS Group (SoclEtE GEnErate de Surveillance)
12-Oet-93 REPORT 24469 REF.FILE 16198-RO PAGE 1 OF 1
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SAMPLE AU PPB
002314002315002316002317002318
002319002320002321002322002323
002324002325002326002327002328
002329002330002331002332002333
002334002335
D 002314 O 002326
565
7513
35815
16
QUALITY CONTROL DUPLICATE
X-RAY ASSAY LABORATORIES 1885 Leslie Street Don Mis Ontario M3B 3J4 (416)445-5755 Fax (416)445-4152 Tlx 06-986947Member of the SGS Group ( Societ* Centrale de Surveillance)
1111111111111111111
I-RAT ASSAT U
SAMPLE
2336 P 2337^ 2338233923402341 2342 2343234423452346 2347 2348234923602351 2352 2353 2354235623662357 2358 2359236023612362 2363 2364236523662367 2368 23692370237123722373 2374. 2375237623772378 2379 2380238123822383 2384 2385238623872388 2389 2390 2391239223932394 2395 239623972398
D 2336 D 2348 D 2360D 2372D 2384D 2396
BORATORIES 25-Qct-93 REPORT — —— REF. 16283 PAGE 1
AU- UT PPB CTT y, Zl X MO X FAAA XRF XRF XRF
20 18 16156
14
(510rt13
rt1729
rtrt7
rtrtrtrt106
rtrt
rtrt ~ - .56rtrtrtrtrt <.Ql ^ 01 .15
rtrtrt rtrtrt
rt
rtrtrt
30rtrt
2470 12 22rt
MOOOO16rt rtrtrt18
Chemex Labs Inc.Analytical Chemisis ' Geochemlsis' Registered Assayers994 West Glendale Ave.. Suite 7. Sparks. Nevada, U.S.A. 89431 PHONE :702-356-5395
To: AKIKO GOLD RESOURCES LTD.
709 - 700 W. FENDER ST. VANCOUVER, BC V6C 108
Project: Comments:
Page Number : lTotal Pages Certificate Di Invoice No. P.O. Number Account
: 1JUN-93
a 15751
:KXQ
ATTN: CHRISTINE REYNOLDS CC: RAYMOND IRWIN
SAMPLE
RB-lRB-2RB-3RB-4RB-5
RB-6RD-1RD-3RD-3RD-4
RD-S ^RD-6 S*RD-7RF- 01RF- 02
RF- 03RF-04RF-OSRF- 06RF- 07
RF- 08RF- 09RF- 10DU 1lul- 1 RH-2
RH-3RH-1RS-1
PREPCODE
205205205205205
205205205205205
205205205205205
205205205205205
205205205205205
205205205
274274274274274
274274274274274
274274274274274
274274274274274
274274274274274
274274274
AU PAoi /T
< 0 .002< 0 .002< 0 .002* 0.002* 0.002
< 0.002< 0 .002* 0 .002
0.006< 0.002
1.2741.1030.1010.05S0.016
0.1640.044
< 0 .002< 0 .002< 0.002
0.006< 0 .002< 0.002< 0 .002< 0.002
f 0 .0020.1590.027
Ag ppiAqua R
* 0.2< 0 .2
0.3< 0 .2
0.3
0.20.31.01.20.6
18.09.50.58.1
c 0.3
16.04.60.3
c 0.2< 0 .2
0.3< 0 .2< 0.2
1.52.8
0.722.0
5.5
AsPPI
22222
22222
1662
902
89074
222
22222
324
160
Cuppi
111765058
395
85115
3699
135
345130
4580
S
340135
531
* 1
< 13
< l350
1360
7667
1710
Pa\
0.603.403.603.407.10
5.802.905.504.503.30
1.600.903.502.801.60
12.602.503.501.300.65
1.701.800.90
13.803.60
6.103.40
16.60
CERTIFICATE OF ANALYSIS A931 5751
Happb
1010101010
, l o1 10
101010
101010so10
3070301010
1010101010
101010
PbPP"
< 1< 1< 1< 1
8
< 1< 1< 1147
11
2050800
231550
46
24002000
613
< 1< 1< 1
SO6
3680< 1
SbPPI
< 0 .3•c 0 .3< 0.3< 0 .3< 0 .3
< 0 .3< 0.3< 0 .3K 0.3< 0 .3
1.00.4
* 0.30.3
< 0.3
1.40.3
< 0 .3K 0.3< 0.3
< 0 .3< 0 .2< 0 .3< 0 .2< 0.3
< 0 .30.6
< 0.2
ZnPP"
9105SI33
112
305245
41200
31
7502450
66340245
2004250
171215
425
5108
44
40180
40
MOPPI
-.-~-..-..
-----
~.-..2
1511
111
-,---
.,----.~--
...-.-...~.....
~.--~.....
T*ppi
~...~................-...
-.-.-0.3
< 0.10.30.4
19.03.40.5
....~-----
---,---.......-~----
--.--..........
.....
.-...
i
-
CERTIFICATION:
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03 -' 2 1-' 9 3 12:04 887 379 GOLDEN SHEAF MGT 12)002/002
ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORY
AKIKO GOLD RESOURCES LTD. '709-700 West Ponder Street Vancouver, British Columbia V6C 1G8
Sample Accurassay
1 '234567a9
10 ' 10
11' : 12.
131414
CustomerRF-11 'RF-12 .RF-13RF-14RF-1SR?-16RP-17RD-6RD-9RD-10RD-10RD-11RD-12'RD-13RD-14RD-14
QCS(MA-3)
Check
Check
7570
1070 LITHIUM DRIVE. UNIT 2THUNDER BAY, ONTARIO P78 *G3
PHONE (B07) 623^*48FAX ^07) 423-6820
Page l
August 24, 1993
Job #934346
Goldppb
^66.
67396^18<58
19241783
124550109
GoldOz/t
^.001< 0.001<0.0010.0200.003
<0.001<0.001<0.001KO.OOl0.0560.052
<0.0010.0010.001
•CO. 001<0.001
0.221
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a-::u-ao -* i O
ACCURASSAY LABORATORIESJL A DIVISION OF ASSAY LABORATORY SERVICES INC.
AKIKO GOLD RESOURCES LTD. 709-700 West Fender Street Vancouver, British Columbia V6C 1G8
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P78 603
PHONE (807) 6234448FAX (807) 623-4820
Page l
September 20, 1993
Job 1934346
Sample Accurassay
1234567
. 8 9
1011121314
Certified By:,
Customer
RF-11RF-12RF-13RF-14RF-15RP-16RF-17RD-8RD-9RD-10RD-11RD-12RD-13RD-14
Molybdenum
l l l l l l l
x c" *Zt o 2. •1.
Lead ppm
3135207151412 12 90l
20l3
10l
Jftl
Zinc ppra
485456
76876361633189627323617
Silver
a<l3
<i <l <l <la u a a<l a
Copper ppm
73
127216
. 54
37301386
1939
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ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORY SERVICES INC.
MR. RAY IRWINAKIKO GOLD RESOURCES LTD.P.O. Box 5472Sparks, NV89432
Sample t Accurassay Customer
1070 LITHIUM DRIVE, UNIT 2THUNDER BAY, ONTARIO P7B 6G3
PHONE (807) 623-6443FAX (SOT) 623-6820
Page l
September 23, 1993
Job #934408
1234567899
RD-15RD-16RD-17RD-18RD-19RD-20RD-21RD-22RD-23RD-23 CheckQCS (Actual)QCS (Expected)Blank
Gold Goldppb Oz/t
<5 ^ .001<5 0 .000<5 0 .000<5 0 .000<5 0 .000<5 0 .000<5 0 .000<5 0.000<5 0 .000<5 0.000
616 0.018618 0.018
Certified By:
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ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORY SERVICES INC.
AKIKO GOLD RESOURCES LTD
P.O. Box 5472
Sparks, NV
89432
1070 LITHIUM DRIVE. UNIT 2THUNDER BAY, ONTARIO P7B 6G3
PHONE (807) 623-6448FAX (807) 623-6820
Page 1
September 23, 1993
Job #934346
Sample tt
RD-10 RO-11 RD-12 RD-13 RO-U
5102
X
68.46
70.32
71.39
71.57
48.46
A 1203
X
13.47
13.71
14.15
13.83
14.03
Fe203
X
3.16
2.36
2.94
2.74
12.80
MgO
X
1.27
0.79
0.98
0.89
4.65
CaO
X
3.57
3.08
3.193.54
13.68
Na20
X
1.85
4.55
3.07
2.89
1.41
K20
X
3.47
1.25
2.18
2.30
0.15
P205
X
0.053
0.060
0.063
0.085
0.084
T102
X
JUP2-6.247
0.293
0.270
0.976
MnO
X
0.069
0.042
0.052
0.053
0.258
BaO
X
0.045
0.063
0.048
0.048
0.003
Cr203
X
0.011
0.008
0.007
0.009
0.038
SrO
X
0.013
0.020
0.024
0.017
0.022
LOI
X
1.7
1.0
1.0
0.6
1.1
Total
X
97.4
97.5
99.4
98.8
97.6
Certified
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APPENDIX B - ROCK SAMPLE DESCRIPTIONS WHITE RIVER PROJECT
Note: sample numbers in parentheses refer to XRAL Lab sample number booklets. AG, CK, HRC, and WDE prefixes refer to the field numbers used.
AG-1 (002301) - dark green to black, f.g.,foliated and/or sheared mafic volcanic ( Ib - amphibolite ), visible oxidation is present ( suphides ? ). 351 hbl, 30% bio, 20% plag, 15% qtz. No visible mineralization. (4 ppb)
AG-2 (002302) - same as above (2 ppb)
AG-3 (2303) - v.c.g. qtz-felds porphyry; 30t qtz phenocrysts, 3^ f elds phenocrysts, 35% bio and 15% plag matrix. 0/C has a rusty appearance. No vis min. (3 ppb)
AG-4 (2304) - dark green to black, f.g., well foliated amphibolite ( Ib ); same mineralogy as 2301. 0/C has a zoned rusty appearance. Few epidote-rich qtz veinlets present and trend //to foliation. No vis. sulphide min. (3 ppb)
AG-5 (2305) - dark green to black, f.g., well foliated to sheared amphibolite; same mineralogy as sample 2304. (4 ppb)
AG-6 (2306) - same as 2304 (27 ppb)
AG-7 (2307) - same as 2304; old sample site for former company (#88-02301). No vis. sul. min. (3 ppb)
AG-8 (2308) - med. to e.g., massive, well fol. qtz-felds porphyry. Elongated felds phenocrysts and qtz eyes are present. Bio. is present in matrix. Trace py. ^ l ppb)
AG-9 (2309) - v.c.g. biotite-rich felsic intrusive. Sample has an almost 'porphyritic 1 appearance. 50t qtz, 35% bio, 15% plag. No vis. sulphide min. (4 ppb)
AG-10 (2310) - dark green to black, f.g. well foliated amphibolite ( Ib ). Similar to 2304. No vis. sulphide min. (2 ppb)
AG-ll (2311) - brownish to grey, f.g., well fol. siliceous meta-sed with numerous diss. rusty spots ( py ? ). 55% qtz, 30% bio, 15% plag. Sample has 'sugary' texture. (9 ppb)
AG-12 (2312) - dark green to black, f.g. well fol., amphibolite ( Ib ) which has an odidized zone //to foliation; @ 1.5 ft. wide and strikes for @ 15 ft. Trace to < l% py., trace cpy. (l ppb)
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AG-13 (2313) - brownish to rusty, well fol. fine to med grained porphyry with < 3* py, po, trace cpy and galena. Sample is weakly to mod. magnetic. (2 ppb)
AG-14 (2314) - well fol. and/or sheared Ib. similar to 2312. tr. to < l* py. 0/C has an oxidized zone. (5 ppb)
AG-15 (2315) - same as above; some thin gtz veinlets. Shearing on the o/c seems to plunge at @ 50 deg. east. ^5 ppb)
AG-16 (2316) - F. g., well fol., 2a (siliceous meta-sediment) with a qtz rich (7(^) sugary texture with 3 (tt bio. present. Few bands of m. g. qtz grains, and fine laminae features present. No vis. min. .
AG-17 (2317) - F. g., well fol. /sheared, 2a (meta-sediment). o/c has few rusty spots scattered about. Possible slickensides present at the same fol. as shear ( strike-slip movement ?) . Weakly schistose. Trace py. (5ppb)
AG-18 (2318) - fine to m. g., massive, mod. to strongly fol/elongated, mod. to srongly silicified porphyry? Surface is bleached, grey in fresh sample. Numerous thin, discontinuous, greyish fracture filling veinlets (possibly v.f.g. moly.) which are randomly oriented. Trace to < l* py,po. (5ppb)
AG-19 (2319) - f. g., well fol/sheared, 2a; rusty appearance. 35% bio, 45% qtz, 15% plag, 5% accessory min. Unit is thinly laminated. No vis min. .
AG-20 (2320) - e.g. qtz vein/ sweat with conchoidal fracturing. Vein cross-cuts o/c (2319) and is discontinuous. No vis. min..
AG-21 (2321) - qtz veinlet or sweat, i 0.5 ft wide, in Ib o/c. No vis. min.. (5ppb)
AG-22 (2322) - f. g., well fol/sheared, Ib (fol. amphibolite) with @ 30% hbl. 25% qtz, 20* bio, 15* plag, 10% muse. No vis. min.. (6ppb)
AG-23 (2323) - f. g , well sheared, l d, e with 50% elongated felsic fragments trending at 162 deg. and dips at 90 deg. Matrix mineralogy consists of 60* hbl, 20* bio, and 201 qtz. (5ppb)
AG-24 (2324) - f. g., weakly to mod. sheared Ib in contact with 4a dyke. Shear strikes at 162 deg and plunges at 85 deg E. (7ppb)
AG-25 (2325) - fine to m. g., mod to well fol., qtz-felds. porphyry (5a) . o/c/ is massive, qtz eyes and fol. lenticular bands of bio. are present and trend at 169 deg.. Tr. py. . (5ppb)
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AG-26 (2326) - qtz sweat within 5a. No vis. rain.. (13ppb) repeat (16ppb)
AG-27 (2327) - Massive, mod to well fol. bio crystals, f. g., gtz augen rich porphyry, o/c does have rusty blotches scattered about. No vis. min. .
AG-28 (2328) - Well f ol 7 sheared l d, e with elongated felsic and mafic fragments oriented at 162 deg. dip; vertical. Chip sample @ 3ft. . (8ppb)
AG-29 (2329) - fine to m. g., greyish, mod to strongly fol. crystals porphyry with numerous qtz vnlts and tension cracks which are cut by the fol. also. Few qtz sweats present. Trace to < l* cpy. (35ppb)
AG-30 (2330) - well fol/elongated l d, e on o/c in island. Mafic clasts 45%, felsic frag. 30t, matrix 25% (felsic rich) . chip sample @ 2ft. (8ppb)
AG-31 (2331) - extremely fol-schistose, bio rich alteredporphyry with < 5% garnet present occuring either in disseminatedor clustered, o/c is rusty. No vis. min.. (15ppb)
AG-32 (2332) - dark green to black, mod. fol., massive la. hbl 60t, bio lot, qtz 20t, plag 101. No vis. min..
AG-33 (2333) - o/c of massive la with few rusty discontinuous micro-fractures with odd subhedral py ^ It) . (9ppb)
AG-34 (2334) - o/c of massive to weakly fol. la, with few felsic bands. No vis. min..
AG-35 (2335) - o/c of weak to mod fol. with 0.5 ft. qtz-carb vein (@ 5ft. long) , slightly rusted, no vis. min. o/c also has epidote sweats present.
AG-36 (2336) - f .g. f massive to weakly fol. l a, b with v. thin qtz vnlts. Fractures are oxidized. No vis. min..
AG-37 (2337) - Massive to weakly fol., f. g., la with numerous rusty (limonite) stains throughout o/c.. Very small, thin, discontinuous qtz vnlts occur and are //to fol.. Epidote clusters also occur but are minor ( < 5t of o/c) .
AG-38 (2338) - massive, f. g., poorly to mod. fol., la with qtz sweat. < It py present.
AG-39 (2339) - mod to well sheared/fol. la in contact with 4b with few qtz-rich vnlts //to fol. Limonite staining throughout. < or * 5t py, < or = It cpy.
AG-40 (2340) - f .g. , mod. fol. Ib. No vis. min..
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AG-41 (2341) - pinkish, slightly to mod. fol., 4a or 5a. Strained qtz eyes present. Tr. py..
AG-42 (2342) - qtz vein in qtz-felds porphyry. Vein is @ 8-10 ft. long, 0.8 ft. wide. No vis. min..
AG-43 (2343) - qtz vein in 5a. in an o/c of l a,b
AG-44 (2344) - Well fol./elongated and/or sheared Id,e with 70* felsic frgms and 30% mafic frgms present and fol. at 170 deg. dipping at 67-70 deg.. Felsic frgms stretched up to 30:1 and 50:1 for mafic frgms. No vis min..
AG-45 (2345) - f.g., massive, mod. to strongly fol. porphyry?, fol. at 162 deg., dip 85-90 deg. W.. Visible elongated qtz. eyes present. No vis. qtz veins and min.
AG-46 (2346) - o/c of lb frgm or Id,e with mafic-rich matrix and @ 40% each of felsic and mafic frgms present. No vis. min..
AG-47 (2347) - o/c of lb with qtz sweats present. No vis. min. in qtz sweats.
AG-48 (2348) - o/c of massive, well fol/elongated porphyry with stretched qtz eyes present. Fol.is 150 deg, dip 65 deg. E.. No vis. min..
AG-49 (2349) - fine to med. grained, mod. to well fol. porphyry with slightly elongated qtz-eyes present. < or = l* py. present.
AG-50 (2350) - well f ol/sheared to schistose, bio-rich altered 5 (prph) with muse, and qtz present. No vis. min..
AG-51 (2351) - sample of Id,e (debris flow) with qtz sweat. Sample similar to one on L 22S 500W ( 2330).
AG-52 (2352) - qtz vein, e 12-15" wide, strike length not determined. No vis. min.
AG-53 (2353) - o/c of lb to Id with numerous elongated felsic fragments (60%) and mafic fragments (40%) present and trending at 166 deg. St dipping 85 deg. W.
AG-54 (2354) - o/c of well fol./sheared, sil. qtz-feld. porphyry (5a) with visible qtz-eyes present. No vis min or qtz veining. Pegmatite (4c) dyke cuts o/c parallel to foliation.
AG-55 (2355) - med. to c.g., qtz phenocryst-rich porphyry (5a) with small, narrow, discontinuous qtz vein cross-cutting porphyry. No vis sulphide min..
l l AG-56 (2356) - o/c of well fol/elongated qtz-felds porphyry
with qtz vein (@ 0.3 ft. wide). Vein is discontinuous (4 ft long). M No vis min in 5a or qtz vein.
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AG-57 (2357) - fine to med. grained, mod to strongly fol. Ib (frgm) with gtz sweats parallel to foliation of 170 deg. No vis min..
AG-58 (2358) - f.g., massive to mod. fol., homogeneous Ib with *c or *" ^ banded py present. No vis qtz veining present.
AG-59 (2359) - well sheared and/or fol. Ib with rusty (limonitic) zone present, trace to < l* py present. Same o/c whrer samples 2314 and 2315 were taken. Channel sample - 0.50m.
AG-60 (2360) - same as 2359
AG-61 (2361) - sheared, silicified, epidotitized, slightly chloritic Ib (frgm). No vis sulphide min.. Channel sample - 0.50m.
0.50m.
AG-63 (2363) - fine to med. grained, mod to strongly foliated, mod. to strongly silicified porphyry with 25 - 30% bio present. Foliation is 165 deg. No vis sulphide mineralization.
AG-64 (2364) - weakly to mod. oxidised, gtz vei of 0.5m in width, strike length traceable to 6 ft.. No vis sulphide min..
l AG-66 (2366) - qtz vein in sheared Ib; same Ib as 2359.
AG-67 (2367) - qtz vein in sheared Ib; same as 2361
AG-68 (2368) - qtz vein in 5a; same as 2363
AG-65 (2365) - qtz vein in well deformed "pillowed" amphibolite (possible flow-top breccia). No vis. sulphide min.. sample located at L 4S/ 2+50 E.
I AG-69 (2366) - altered felsic intrusive with < 5% Mo rosettes. Assayed for Au, Mo.
AG-70 (2370) - qtz vein (0.2 ft wide) in foliated amphibolite Ib. No vis. min.
AG-71 (2371) - discontinuous qtz vein in foliated amphibolite (Ib). No vis. min.
AG-72 (2372) - 1.5 to 2 ft. wide, discontinuous qtz vein m intruding into Ib. Tr.py..
l l ll 13; Mo, < l% sph present. Vein is @ 4m long, 0.3m wide and is
AG-73 (2373) - qtz vein in a well foliated felsic intrusive, found @ 300m north of L OS.
AG-74 (2374) - qtz vein within 5a that intrudes into la,c. < l% Mo, < l% sph prt trending at 270 deg.
l HRC-1 (2375) - qtz vein, no vis. min. Located at @ 1700S, 375W.
l HRC-2 (2376) - qtz vein or sweat, no vis. min., no location.
HRC-4 (2377) - qtz vein or sweat, no vis. min; located at H 900S, 100E
CK-2 (2378) - qtz vein sampled from o/c., no vis. min.; . located @ at 1710S, 450W
CK-4 (2379) - qtz vein from boulder, no vis. min., located @ at 1375S, 400W
l CK-6 (2380) - qtz vein from boulder, no vis. min., located @ at 1160S, 350W
l CK-7 (2381) - qtz vein float, no vis. min., located @ at 675S, 100E
I CK-8 (2382) - qtz vein sampled from o/c., no vis. min., located @ at 525S, 100E
I WDE-2 (2383) - 2 cm wide qtz vein from edge of o/c of e.g. gabbro, no visible sulphides.
I WDE-3 (2384) - 40 cm wide qtz vein in large o/c of sheared mafic volcanic, no vis. sulphide min.
WDE-4 (2385) - 6 cm wide qtz vein in qtz monzonite, minor M pyrite < 13;.
WDE-5 (2386) - 6 to 8 cm wide qtz vein in qtz monzonite, no m vis. sulphides min..
WDE-6 (2387) - 10 cm wide qtz vein in pegmatite within qtz — monzonite o/c.
™ WDE-7 (2388) - 5 cm wide qtz vein a;ong edge of amphibolite boulder, minor pyrite.
l WDE-8 (2389) - 4 to 6 cm wide qtz vein hosted within a 10 cm wide feldspar porphyry dyke.
l
l
l8
l
l
WDE-9 (2390) - >30cm wide qtz vein along edge of pegmatite intrusive into amphibolite boulder.
WDE-10 (2391) - qtz vein in amphibolite
CK-1 (2392) - qtz vein, no vis. min., located @ at 1650S, M 450W
CK-5 (2393) - qtz vein, no vis. min., located @ at 1350S, 425W
— SV-1 (2394) - well folXsheared,metased or sheared intrusivel with qtz stringers ( max 40-60 cm wide) trending at 140 deg. Sample™ is from the Sugar Vein.
SV-2 (2395) - quartzo-feldspathic dyke (sheared porphyry).
SV-3 (2396) - pinch and swell qtz vein found in well foliated m mafic volcanic ( 150 deg j dipping at 85 deg W ). No vis. min..
SV-4 (2397) - qtz vein in contact with qtz-felds porphyry (Sugar Vein).
™ SV-5 (2398) - qtz vein cutting qtz-felds porphyry (Sugar Vein)
l
l l l
l l l l l l
l l l l l ll APPENDIX C - GEOCHEMICAL HUMUS SAMPLING RESULTS
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l XRAL X-RAY ASSAY LABORATORIESA DIVISION OF SGS CANADA INC.
1885 LESLIE STREET - DON NILLS, ONTARIO (OB 3J4 * CANADA TEL: (416)445-5755 TELEX: 06-986947 FAX: (416)445-4152
CERTIFICATE OF ANALYSIS
REPORT 2 4 6 4 O
TO: A.C.A. HOWE INTERNATIONAL LTD ATTN: DINO TITARO22 FRONT STREET WEST, SUITE 1400 TORONTO, ONTARIO M5J 1C4
CUSTOMER NO.
DATE SUBMITTED 14-Sep-93
1943
l l l l l l l l l l l l l
REF. FILE 16106-
93 HUMUS Proj. WHITE RIVER
Total Pages 3
AU PPBMETHOD NA
DETECTION LIMIT 1.
*** UNLESS INSTRUCTED OTHERWISE WE WILL DISCARD PULPS IN 90 DAYS *** AND REJECTS IN 30 DAYS FROM THE DATE OF THIS REPORT
DATE 19-Oct-93 CERTIFIED BYJean H.L. Opdei
Member of the SGS Group ( SociEtE GEnErale de Surveillance)
p111111111111111111
:RAL9
SAMPLE
L128N-99+OOE L128N-99+25EL128N-99+50EL128N-99+75EL128N-99+87.5E
L128N-BL100EL128N- 100+12. 5EL128N-100+25E L128N-100+50EL128N-100+75E
L128N-101+OOE L127N-99+OOEL127N-99+25EU27N-99+50EL127N-99+75E
L127N-99+87.5EL127N-BL-100EL127N-100+12.5E L127N-100+25EL127N-100+50E
L127N-100+75E L127H-101+OOEL126N-98+50EL126N-98+75EL126N-99+OOE
L126N-99+25EL126N-99*50EL126N-99+75E L126N-100+OOEL126N-10012.5E
L126N-100+25E L126N-100+37.5EL126N-100+50EL126N-100+75EL126N-101+OOE
L126N-101+25EL126N-101+50EL125N-98+50E L125N-98*75EL125N-99*OOE
L125N-99*25E L125N-99*50EL125N-99*75EL125N-100+OOEL125N-100+12.SE
ct-93
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REPORT 24640 ftEF.FILE 16106- PAGE 1 OF 3
ifie Street Don Mills Ontario M3B 3J4 (416)445-5755 Fax (416)445-4152 Tlx 06-986947 Member of the SGS Group (Societe Generate de Surveillance)
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L125N-100+25E L125N-100+37.5EL125N-100+50EL125N-100+75EL125N-10UOOE
L125N-101+25EU25N-101+50EL1200S-500W L1200S-400WL1200S-350W
L1200S-300W L1200S-250WL1200S-200UL1200S-150UL1200S-100U
L1200S-50WL1200S-BLL1200S-475E L1200S-500EL1200S-525E
L1200S-550E L1200S-575EL1200S-600EL1200S-625EL1200S-650E
L1200S-675EL1200S-700EL1200S-725E L1200S-750EL1200S-775E
L1200S-800E L1200S-825EL1200S-850EL1200S-875EL1200S-900E
L1200S-925EL1200S-950EL1200S-975E L1200S-1000EL1200S-1025E
L1200S-1050E L1200S-1075EL1200S-1100EL1200S-1125EL1200S-1150E
AU PPB
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X-RAY ASSAY LABORATORIES 1885 Leslie Street Don Mils Ontario M3B 3J4 (416)445-5755 Fax (416)445-4152 Tlx 06-986947Member of the SGS Group (Soci6te Centrale de Surveillance)
IXRALi i i i i i i i i i i i i i i i i i
19-Oct-93 REPORT 24640 REF.F1LE 16106- PAGE 3 OF 3
SAMPLE AU PPB
L1200S-1175E 6L1200S-1200E 6L1200S-450W 7
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O - QUALITY CONTROL DUPLICATE
X-RAY ASSAY LABORATORIES 1885 Leslie Street Don Mills Ontario MSB 3J4 {416)445-5755 Fax (416)445-4152 Tlx 06-986947Member of the SGS Group ( Societe Generate de Surveillance)
l
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l
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XRAL X-RAY ASSAY LABORATORIESA DIVISION OF SGS CANADA INC.
1885 LESLIE STREET ' DON MILLS, ONTARIO M3B 3J4 - CANADA TEL: (416)445-5755 TELEX: 06-986947 FAX: (416)445-4152
CERTIFICATE OF ANALYSIS
REPORT 2493V
TO: A.C.A. HOWE INTERNATIONAL LTD ATTN: DINO TITARO22 FRONT STREET WEST, SUITE 1400 TORONTO, ONTARIO M5J 1C4
REF. FILE 16295-
589 HUMUS Proj. WHITE RIVER
AU PPBMETHOD
NA
CUSTOMER NO.
DATE SUBMITTED 29-Sep-93
Total Pages 14
1943
DETECTION LIMIT 1.
l l l l l l l
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*** UNLESS INSTRUCTED OTHERWISE WE WILL DISCARD PULPS IN 90 DAYS *** AND REJECTS IN 30 DAYS FROM THE DATE OF THIS REPORT
DATE 10- j CERTIFIED BYJean H.L. Opdeb^feck, Gegferal Manager
Member of the SGS Group (SoclEtE GEnErale de Surveillance)
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TL800U-4650S TL800W-4700STL800W-4750STL800U-4850STL800W-4900S
TL800U-4950STL800U-5050STL800W-5100STL800U-5150STL800W-5200S
TL800W-5250S TL800U-S300STL800W-5350STL800W-5450STL800W-5500S
TL800W-5550STL800W-5600STL775W-4500S TL775W-4550STL8U-3050S
TL8U-3100S TL8W-3200STL8U-3250STL8U-3300STL8W-3350S
TL8W-3400STL8W-3450STL8W-3500S TL8U-3550STL8U-3600S
TL8U-3650STL8U-3700STL8W-3800STL8W-3850STL8W-3900S
TL8U-3950STL8U-4000S TL8U-W5QSTL8W-4100STL8U-4150S
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Mov-95 REPORT 24937 REF.FILE 16295-
AU PPB
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PAGE 1 OF 14
Fax (416)445-4152 Tlx 08-986947
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*SAMPLE
BL200U-45+25S BL200U-45+75SBL200W-3550SBL200W-4675SBL200W-4725S
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BL200W-S575SBLX2+50W-3450SBLXS+50U-3500SBLX2+50W-3550SBL2U-3650S
BL2W-3700SBL2W-3750SL34S-8SOWL34S-800WL34S-750W
L34S-700WL34S-650WL34S-600W L34S-550WL34S-500W
L34S-4SOWL34S-400UL34S-350WL36S-750W L36S-700W
L36S-650WL36S-600W 1365-550WU36S-500WL36S-450W
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PAGE 2 OF 14
Fax (416)445-4152 Tlx 06-986947
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L46S-750WL46S-700W L46S-650WL46S-600WL46S-550W
L46S-500WL46S-450UL46S-400UU6S-350W L46S-300W
L46S-250WL46S-200U U6S-150W
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Nov-93 REPORT 24937 REF.FILE 16295-
AU PPB
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X-RAY ASSAY LABORATORIES 1885 Leslie Street Don Mils Ontario MSB 3J4 (416)445-5755Member of the SGS Group (Societe Generate de Surveillance)
PAGE 3 OF U
Fax (416)445-4152 Tlx 06-986947
IXRAL1 11111111111111111
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L46S-825EL46S-850E L46S-875EL46S-900EL46S-925E
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L46S-1075EL46S-1100E L46S-1125EL46S-1150EL48S-550E
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REPORT 24937 REF.FILE 16295- PAGE 4 OF 14
5slie Street Don Mills Ontario M3B 3J4 (416)445-5755 Fax (416)445-4152 Tlx 06-986947Member of the SGS Group ( Socitte' G6n4rale de Surveillance)
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L48S-9SOE L48S-975EL48S-1000EL48S-1025E L48S-1050E
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L50S-350SL50S-375E L50S-400E L50S-425EL50S-450E
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L50S-600EL50S-625E L50S-750EL50S-775ELSOS-800E
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-Nov-93 REPORT 24937 REF.FILE 16295- PAGE 5 OF 14
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Nov-93
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REPORT 24937 REF.FILE 16295- PAGE 6 OF 14
die Street Don Mils Ontario M3B 3J4 (416)445-5755 Fax (416)445-4152 Tlx 06-986947Member of the SGS Group ( Societe Generate de Surveillance)
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L3600S-525E L3600S-550EL3600S-575EL3600S-600EL3600S-625E
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X-RAY ASSAY LABORATORIES 1885 Leslie Street Don Mills Ontario M3B 3J4 (416)445-5755Member of the SGS Group (Soci6t6 Generate de Surveillance)
PAGE 7 OF 14
Fax (4161445-4152 Tlx 06-986947
IO-Nov-93 REPORT 24937 REF.FILE 16E95- PAGE 8 OF 14
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L4825S-750WL4825S-700WL4825S-600UL4825S-550UL4825S-500U
L4825S-450WL4825S-400WL4825S-350UL4825S-300WL4825S-250W
L4825S-200WL4825S-150WL4825S-100UL4825S-50WL4825S-0+00
L4825S-2SEL4825S-50EL4825S-75EL4825S-100EL4825S-125E
L4825S-150EU825S-175EU825S-200EL4825S-22SEL4825S-250E
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X-RAY ASSAY LABORATORIES 1885 Leslie Street Don Mis Ontario MOB 3J4 (416)445-5755 Fax (418)445-4152 Tlx 06-986947Member of the SGS Group ( Soeiete Generate de Surveillance)
IXRAL111111111111111111
*SAMPLE
L4825S-400E L4825S-425EL4825S-450EU825S-475EL4825S-500E
L5025S-700WL5025S-650ULS02SS-600W L5025S-550WL5025S-450U
L5025S-400W L5025S-350UL5025S-300WL5025S-250WL5025S-200W
L5025S-150UL5025S-100UL5025S-50U L5025S-0+00L5025S-25E
L5025S-50E L5025S-75EL5025S-100EL5025S-125EL5025S-150E
L5025S-175EL5025S-200EL5025S-225E L5025S-250EL5025S-275E
L5225S-900U L5225S-800WL5225S-750UC522SS-700WL5225S-650U
LS225S-600WL5225S-550UL5225S-500WL5225S-500UAL5225S-450U
LS225S-400WL5225S-350UL5225S-300WL5225S-250U L5225S-8L200W
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X-RAY ASSAY LABORATORIES 1885 Leslie Street Don Mills Ontario M3B 3J4 (416)445-5755Member of the SGS Group (Soci6t6 GeYteYale de Surveillance)
PAGE 5 OF 14
Fax (416)445-4152 Tlx 06-986947
V111111111111111111
(RALSAMPLE
L5225S-150U L5225S-100WL5225S-50WL5225S-0+00 L5225S-25E
L5225S-50EL5225S-75E LS225S-100E L5225S-125EL5225S-150E
L5225S-175E LS225S-200EL5225S-225EL5225S-250E L5225S-275E
L5225S-300EL5225S-325E L5225S-350E L5225S-375EL5225S-400E
L522SS-425E L5225S-4SOEL5225S-475EL5225S-500E L5225S-525E
L5225S-550EL5225S-575E L5225S-600E L5225S-625EL5225S-650E
L5225S-675E L5225S-700EL5225S-725EL5225S-750E L5225S-825E
L5225S-850EL5225S-875E L5225S-900EL5225S-925EL5225S-950E
L5225S-975EL5225S-1000EL5225S-1025EL5225S-1050E L5225S-1075E
-Nov-93 REPORT 24937 REF.FILE 16295-
AU PPB
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X-RAY ASSAY LABORATORIES 1885 Leslie Street Don Mis Ontario M3B 3J4 (416)445-5755Member of the SGS Group (Socfit* GineYale de Surveillance)
PAGE 10 OF 14
Fax (416)445-4152 Tlx 06-986947
IXRALiiiiiiiiiiiiiiiiii
*SAMPLE
L5225S-1100E L5225S-1125EL5225S-1150EL5225S-1175ELS22SS-1200E
LS425S-900UL5425S-850WL5425S-800U L5425S-750UL5425S-700W
L5425S-650U L5425S-600WL5425S-550UL5425S-505WL5425S-380U
L5425S-350WL5425S-300WL5425S-250W L5425S-150WL5425S-100W
L5425S-50W L5425S-0+00L5425S-25EL5425S-50EL542SS-75E
L5425S-100EL5425S-125EL5425S-150E L5425S-175EL5425S-200E
L5425S-22SE LS425S-250EL542SS-275EL542SS-300EL542SS-325E
L5425S-350EL5425S-375EU5425S-400EL5425S-425EL5425S-450E
L5425S-475EL5425S-500ELS425S-525EL5425S-550E L5425S-575E
AU PPB
•el^t]
1
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3 22
2 2356
225 33
4 3232
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X-RAY ASSAY LABORATORIES 1885 Leslie Street Don Mills Ontario M3B 3J4 (416)445-5755Member of the SGS Group (Societe Generate de Surveillance)
PAGE 11 OF 14
Fax (416)445-4152 Tlx 06-986947
IXRALiiiiiiiiiiiiiiiiii
9SAMPLE
L5425S-600E L5425S-625EL5425S-650EL5425S-675EL5425S-700E
L5425S-725EL5425S-750EL5425S-775E L5425S-800EL5425S-825E
L5625S-900U L5625S-850WLS625S-750UL5625S-700UL5625S-650U
L5625S-600WL5625S-550WL5625S-400W L5625S-350WL5625S-300U
L5625S-250W L5625S-BL200UL5625S-150UL5625S-100UL5625S-50W
L5625S-0+00L5625S-25EL5625S-50E L5625S-75EL5625S-100E
L5625S-125E L5625S-150EL5625S-175EL5625S-200EL5625S-225E
L5625S-250EL5625S-275E1,56255-3005L5625S-325EL5625S-350E
L5625S-375EL5625S-400EL5625S-425EL5625S-450E L5625S-475E
AU PPB
2121
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X-RAY ASSAY LABORATORIES 1885 Leslie Street Don Mills Ontario MSB 3J4 (416)445-5755Member of the SGS Group (Societe Generate de Surveillance)
PAGE 12 OF 14
Fax (416)445-4152 Tlx 06-986947
IXRALiiiiiiiiiiiiiiiiii
9SAMPLE
L5625S-500E L5625S-525EL5625S-550EL5625S-S75EL5625S-600E
L5625S-625EL5625S-650EL5625S-675E LS625S-700EL562SS-725E
L5625S-750E TL12E-3650STL12E-3700STL12E-3750STL12E-3800S
TL12E-3900STL12E-3950STL12E-4000S TL12E-4050STL12E-4100S
TL12E-4150S TL12E-4200STL12E-4250STL12E-4300STL12E-4350S
TL12E-4400STL12E-4450STL12E-4500S TL12E-4550STL12E-4650S
TL12E-4700S TL12E-4750STL12E-4800STL12E-4850STL12E-4900S
TL12E-4950STL12E-5050STL12E-5100STL12E-5150STL12E-5250S
TL12E-5300STL12E-5350STL12E-5450STL12E-5500S TL12E-5550S
AU PPB
1 <1<13
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Tlx 06-986947
IXRALiiiiiiiiiiiiiiiiii
*SAMPLE AU PPB
TL12E-5600STL1200E-3450STL1200E-3500STL1200E-3550S
D TL800U-4650S
0 TL8W-3350SD BL200U-4675SD L34S-600W D L38S-400WD L46S-500W
D L46S-350E D L46S-1025E0 L48S-1000E0 L50S-625E0 L54S-1100E
D L3200S-1200ED L3600S-475ED L3600S-1075E D L4825S-400UD L4825S-400E
D L5025S-150E D L5225S-0+00D LS225S-600ED L5425S-850U0 LS425S-22SE
D L5425S-825ED LS625S-200E0 TL12E-3700S D TL12E-5050S
D - QUALITY
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CONTROL DUPLICATE
X-RAY ASSAY LABORATORIES 1885 Leslie Street Don MMs Ontario M3B 3J4 (416)445-5755 Fax (416)445-4152 Tlx 06-986947Member of the SGS Group (Societe Centrale de Surveillance)
l XR. | 01
l
A i X-RAY ASSAY LABORATORIESf^ ^ A DIVISION OF SGS CANADA INC.
^™" 1885 LESLIE STREET ' DON MILLS. ONTARIO M3B 3J4 * CANADATEL: (416)445-5755 TELEX: 06-986947 FAX: (416)445-4153
CERTIFICATE OF AJSTAJL.'Sr S I S
REPORT 24826
I TO: A. C. A. HOWE INTERNATIONAL LTD ATTN: DINO TITARO CUSTOMER No. 194322 FRONT STREET WEST, SUITE 1400
m TORONTO1 M5J 1C4
| REF
". 1 2 87
1
1
, ONTARIO DATE SUBMITTED24-Sep-93
. FILE 16232- Total Pages 7
PULPS Proj . WHITE RIVER
METHOD DETECTION LIMITAU PPB NA 1.
1 *** UNLESS INSTRUCTED OTHERWISE WE WILL DISCARD PULPS IN 90 DAYS ***
1
1
1
1
1
1
1
HATP lLJf\ X J-* '
1
AND REJECTS IN 30 DAYS FROM THE DATE OF THIS REPORT
^ft*Jl J A^8~Nov~Q3 CERTIFIED BY l/ v-^x^j *fu^c^^Qx** * ^ \
Jean H. L. Opdebleck, Geneoal Manager \I ' —s
Membe^ of the SGS Group (SociEtE GEnErale de Surveillance) ' ————— ' ————————
f frR AL
1111l-t.
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VSAMPLE AU
BL200U-3850S BL200W-3900SBL200W-3950SBL200U-4050SBL200W-4100S
BL200W-4150SBL200W-4250SBL200W-4300S BL200V-4350SBL2+50W-33+50S
3L2U-32SOS SL2W-3300SBL2W-3350SL34S-250WL34S-125W
L34S-75W1.34-0L34S-25E L34S-50EL34S-100E
L34S-125E L34S-150EC34S-175EL34S-200EL34S-225E
L34S-250EL34S-275EL34S-300E L34S-325EL34S-350E
L34S-375E L34S-400E134S-425EL34S-450EL34S-525E
L34S-550EL34S-575EL34S-600E L34S-62SEL34S-650E
L34S-67SEL34S-700EL34S-725EL34S-750EL34S-775E
V3 REPORT Z4K6 REF.FILE 1623Z- PAGE 1 OF 7
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X-RAY ASSAY LABORATORIES 1885 Leslie Street Don Mills Ontario M3B 3J4 (416)445-5755 Fax (416)445-4152 Tlx 06-986947Member of t ne SGS Group (Societi Centrale de Surveillance)
IXRAL1.,,. na.U~.,.07 DCOnBT t l.
11
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SAMPLE AU PPB
L34S-800E L34S-825EL34S-850E SMPL34S-875EL34S-900E
L34S-925EL34S-950EL34S-975EL34S-1000EL34S-1025E
L34S-1050E L34S-1075EL34S-1100EAL34S-1000EBL34S-1125E
L34S-1150EL38S-200WL38S-150W L38S-100WL38S-50W
L38S-0 L38S-25EL38S-50EL38S-75EL38S-100E
L38S-125EL38S-150EL38S-175E L38S-200EL38S-225E
L38S-250E L38S-275EL38S-300EL38S-325EL38S-350E
L38S-375EL.38S-400EL38S-425E L38S-450EL38S-475E
L38S-500E L.38S-525EL38S-S50EL38S-575EL38S-600E
SMP. MISS. - SAMPLE
1 2
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1 221
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31
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321
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WAS NOT RECEIVED AT XRAL
X-RAY ASSAY LABORATORIES 1885 Leslie Street DeMembe" of the SGS Gro
REF.FRE 1 6232- PAGE 2 OF 7
Don Mills Ontario MOB 3J4 (416)445-5755 the SGS Group (Societe Generate de Surveillance)
Fax (416)445-4152 Tlx 06-986947
IXRALiiiiiiiiiiiiiiiiii
9SAMPLE
L38S-62SE L38S-650EL38S-675EL38S-700EL38S-725E
L38S-750EL38S-775EL38S-800E L38S-825EL38S-850E
L38S-875E L38S-900EU38S-925EL38S-950EL38S-975E
L38S-1000EL38S-1025EL38S-1050E L38S-1075EL38S-1100E
L38S-1125E L38S-1150E144S-600WL44S-550UL44S-500U
L44S-450WL44S-400UL44S-350W L44S-300WL44S-250W
L44S-200U L44S-1SOUL44S-100UL44S-50UL44S-0
I.44S-25EL44S-50EL44S-75E
L44S-100EL44S-125E
L44S-150E U4S-175EL44S-200EL44S-225EL44S-250E
Nov-93 REPORT 24826 REF.FILE 16232- PAGE 3 OF 7
AU PPB
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X-RAY ASSAY LABORATORIES 1885 Leslie Street Don Mifls Ontario M3B 3J4 {416)445-6755 Fax (416)445-4152 Tlx 06-986947 Member rr r he SGS Grouc (Societe Genera l e de Surveillance)
IXRALiiiiiiiiiiiiiiiiii
9SAMPLE
L44S-275E L44S-300EL44S-325EL44S-350EL44S-375E
L44S-450EL44S-475EL44S-500E L44S-525EL44S-550E
L44S-575E L44S-600EL44S-625EL44S-650EL44S-675E
L44S-700EL44S-725EL44S-750E L44S-775EL44S-800E
L44S-825E L44S-850EL44S-875EL44S-900EL44S-925E
L44S-950EL44S-975EL44S-1000E L44S-1025EL44S-1050E
L44S-1075E L44S-1100EL44S-1125EL4000S-9L200UL4000S-150U
L4000S-100WL4000S-50W[.'•OQOS-0+00 L4060S-25EL4000S-50E
L4000S-75EL4000S-100EL4000S-125EL4000S-150E L4000S-175E
Mov-93 REPORT 24826 REF.FILE 16232- PACE 4 OF 7
AU PPB
^1
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X-RAY ASSAY LABORATORIES 1885 Leslie Street Don Mis Ontario M3B 3J4 (416)445-5755 Fax (416)445-4152 Tlx 06-986947Member of the SGS Grouo (Societi Centrale de Surveillance)
IXRALiiiiiiiiiiiiiiiiii
9SAMPLE
L4000S-200E L4000S-225EL4000S-250EL4000S-275EL4000S-300E
UOOOS-325EL4000S-350EL4000S-37SE L4000S-400EL4000S-425E
L4000S-450E L4000S-475EL4000S-500EL4000S-525EL4000S-550E
L4000S-575EL4000S-600EUOOOS-625E L4000S-650EUOOOS-675E
L4000S-700E L4000S-725EL4000S-750EL4000S-775EL4000S-800E
L4000S-82SEL4000S-850EL4000S-875E L4000S-900EL4000S-925E
L4000S-950E L4000S-975EL4000S-1000EL4000S-1025EL4000S-1050E
L4000S-1075EL4000S-1100EL4000S-1125E L4bOflS-1150EL4000S-1175E
UOOOS-1200E L4200S-SL200UL4200S-150WL4200S-100WL4200S-50W
Nov-93
AU PPB
33
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2 3
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41142
X-RAY ASSAY LABORATORIES 186Memt
REPORT 24826 REF.FILE 16232- PAGE 5 OF 7
islie Street Don Mils Ontario M3B 3J4 (416)445-5755 Fax (416)445-4152 Tlx 06-986947Membe^ of the SGS Group ( Sociite G*nerale de Surveillance)
IXRAL1 , no.ii~..-OT BCB/uiT 1 1. at L r, f r r, ir ttit-\
1
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9SAMPLE
L4200S-0+00 L4200S-25EL4200S-50EL4200S-75EL4200S-100E
L4200S-125EL4200S-150EL4200S-175E L4200S-200EL4200S-225E
L4200S-250E L4200S-275EL4200S-300EL4200S-325EL4200S-350E
L4200S-375EL4200S-400EL4200S-425E L4200S-450EL4200S-475E
L4200S-500E L4200S-525EL4200S-550EL4200S-575EL4200S-600E
L4200S-625EL4200S-650EL4200S-675E L4200S-725EL4200S-750E
U200S-775E L4200S-800EL4200S-825EL4200S-850EL4200S-875E
L4200S-900EL4200S-925EL4200S-950E L4200S-975EL4200S-1000E
L4200S-1025E L4200S-1050EL4200S-1075EL4200S-1100EL4200S-112SE
AU PPB
3 •O
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X-RAY ASSAY LABORATORIES 1885 Leslie Street Don Mite Ontario MSB 3J4 (416)445-5755Member of the SGS Group (Societ* G^nsrale de Surveillance)
PAGE 6 OF 7
Fax (418)445-4152 Tlx 06-986947
(KRAIiiiiiiiiiiiiii
SAMPLE
L4200S-11SOE L4200S-1175EL4200S-1200EL4400S-850UL4400S-800U
L4400S-750WL4400S-700UL4400S-650U TL800W-4400STL12E-3050S
TL12E-3100S TL12E-3150STL12E-3200STL12E-3250STL12E-3300S
TL12E-3350STL12E-3400S
D SL200W-3850S D L34S-225E0 L34S-875E
D L38S-175E D L38S-775ED L44S-200UD L44S-550E0 L4000S-BL200W
D L4000S-500E0 L4000S-1100E0 L4200S-375E D L4200S-1000E
Mov -93
AU PPS
2 3
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1
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1X-RAY ASSAY LABORATORIES 186
Memt
REPORT 24826 REF.MLE 16232- PAGE 7 Of T
islie Street Don Mills Ontario M3B 3J4 (416)445-5755 Fax (416)445-4152 Tlx 06-986947Member of the SGS Group (Societ* Generate de Surveillance)
l IXRAL
l l l l l l l l l l l l l l l
l
X-RAY ASSAY LABORATORIESA DIVISION OF SCS CANADA INC.
1885 LESLIE STREET - DON MILLS, ONTARIO M38 3J4 - CANADA TEL: (416)445-5755 TELEX: 06-986947 FAX: (416)445-4153
CERTIFICATE OF AJSTAJL, Y SI S
REPORT 24839
TO: A.C.A. HOWE INTERNATIONAL LTDATTN: DINO TITARO22 FRONT STREET WEST, SUITE 1400TORONTO, ONTARIOM5J 1C4
REF. FILE 16199-
CUSTOMER NO.
DATE SUBMITTED 24-Sep-93
Total Pages 10
1943
427 HUMUS
AU PPBMETHOD NA
DETECTION LIMIT 1.
*** UNLESS INSTRUCTED OTHERWISE WE WILL DISCARD PULPS IN 90 DAYS *** AND REJECTS IN 30 DAYS FROM THE DATE OF THIS REPORT
DATE OS-Hov-93 CERTIFIED BY .Jean H.L. Opde
Member of the SGS Group (SociEtE GEnErale de Surveillance)
IXRALiiiiiiiiiiiiiiiiii
9SAMPLE
TL800U-1850S TL800U-1900STL800U- 1950STL800W-2050STL800W-2100S
TL800W-2150STL800W-2250STL800W-2300S TL800U-2350STL800U-2450S
TL800W-2500S TL800W-2550STL800W-2650STL800W-2700STL800W-2750S
TL800U-2800STL800U-2850STL800W-2900U TL800W-2950SBL200U- 1950S
BL200U-2050S BL200W-2100SBL200W-2150SSL200W-2250SSL200U-2300S
BL2W-2350SBL2W-24+50SBL2U-2500S BL2U-25SOSBL2W-2650S
BL2W-2700S BL2W-2750SBL2U-28+OOSBL2U-2850SBL2W-2900S
8L2W-2950SBL2W-3050S3L2W-3100SBL2U-3150SL22S-800W
L22S-750UL22S-700WL22S-650WL22S-600W L22S-550W
-Nov-93
AU PPB
5 2744
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REPORT 24839 REF.FILE 16199- PAGE 1 OF 10
.eslie Street Don Mills Ontario M3B 3J4 (416)445-5755 Fax (416)445-4152 Tlx 06-986947Member of the SGS Group ( Soci6te Centrale de Surveillance)
IXRAL111111111111111111
0SAMPLE
L22S-500U L22S-450UL22S-400WL22S-3SOUL22S-300W
L22S-250UL22S-200UL22S-150W L22S-100UL22S-50W
L22S-0+00 L22S-25EL22S-50EL22S-75EL22S-100E
L22S-125EL22S-150EI22S-175E L22S-200EL22S-225E
L22S-250E L22S-275EL22S-300EL22S-325EL22S-350E
L22S-375EL22S-400EL22S-425E L22S-450EL22S-475E
L22S-500E L22S-525EL22S-550EL22S-575EL22S-600E
L22S-625EL22S-650EL22S-675EL22S-700EL22S-72SE
L22S-750EL22S-775EL22S-300EL22S-825E L22S-850E
AU PPB
<1 *1<1<1
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X-RAY ASSAY LABORATORIES 1885 Leslie Street Don Mils Ontario M3B 3J4 (416)445-5755 Fax (416)445-4152 Tlx 06-986947Member of the SGS Group (Sociit6 G6n6rale de Surveillance)
KRALiiiiiiiiiiiiiiiiii
0SAMPLE
L22S-87SE L22S-900EL22S-925EL26S-800WL26S-750W
L26S-700WL26S-650UL26S-600U L26S-350UL26S-300W
L26S-250W L26S-200WL26S-150UL26S-100WL26S-50W
L26S-0L26S-25EL26S-50E L26S-75EL26S-100E
L26S-125E L26S-150EL26S-175EL26S-200EL26S-225E
L26S-250EL26S-275EL26S-300E L26S-325EL26S-350E
L26S-375E L26S-400E126S-425EL26S-450EU26S-475E
L26S-500EL26S-525E126S-550EL26S-575EL26S-600E
L26S-62SEL26S-650EL26S-675EL26S-700E L26S-725E
AU PPB
2 3221
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PXRALiiiiiiiiiiiiiiiiii
*SAMPLE
L26S-750E L26S-775EL26S-800EL26S-825EL26S-850E
L26S-875EL26S-900EL26S-925E L26S-950EL26S-975E
L26S-1000E L26S-1025EL26S-1050EL26S-1075EL26S-1100E
L26S-1125EL26S-1150EL26S-116SE L28S-450WL28S-400U
L28S-350W L28S-300WL28S-250WL28S-150WL28S-100W
L28S-50UL28S-0L28S-25E L28S-50EL28S-75E
L28S-100E L28S-125EL28S-150EL28S-175EL28S-200E
L28S-225EL28S-250EL28S-275EL28S-300EL28S-325E
L28S-350EL28S-375EL28S-400EL28S-425E L28S-450E
AU PPB
•O 2
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X-RAY ASSAY LABORATORIES 1885 Leslie Street Don Mills Ontario MSB 3J4 (416)445-5755 Fax (416)445-4152 Tlx 06-986947Member of the SGS Group (Soci6t6 Centrale de Surveillance)
IXRALiiiiiiiiiiiiiiiiii
*SAMPLE
L28S-475E L28S-500EL28S-525EL28S-S50EL28S-575E
L28S-600EL28S-62SEL28S-650E L28S-675EL28S-700E
L28S-725E L28S-750EL28S-775EL28S-800EL28S-825E
L28S-850EL28S-875EL28S-900E L28S-92SEL28S-950E
L28S-975E L28S-1000EL28S-1025EL28S-1050EL28S-1075E
L28S-1100EL28S-1125EL28S-1150E L28S-1175EL32S-150W
L32S-100W L32S-50WL32S-0L32S-25EL32S-50E
L32S-75EL32S-100EL32S-125EL32S-150EL32S-175E
L32S-200EL32S-225EL32S-250EL32S-275E L32S-300E
-Nov-93 REPORT 24839 REF.FILE 16199- PAGE 5 OF 10
AU PPB
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REPORT 24839 REF.F1LE 16199- PAGE 6 OF 10
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Fax (416)445-4152 Tlx 06-986947
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REPORT 24839 REF.FILE 16199- PAGE 7 OF 10
.eslie Street Don Ms Ontario M3B 3J4 (416)445-5755 Fax (416)445-4152 Tlx 06-986947Member of the SGS Group (Societ* Generate de Surveillance)
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REPORT 24839 REF.FILE 16199- PAGE 8 OF 10
.eslie Street Don Mils Ontario M3B 3J4 (416)445-5755 Fax (416)445-4152 Tlx 06-986947Member of the SGS Group ( Societe Centrale de Surveillance)
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1885 LESLIE STREET - DON HILLS, ONTARIO H3B 3J4 - CANADA TEL: (416)4A5-5755 TELEX: 06-986947 FAX: (416)445-4153
CERTIFICATE OF ANA.3L.Y S X S
REPORT 2 493V
TO: A.C.A. HOWE INTERNATIONAL LTD ATTN: DINO TITARO22 FRONT STREET WEST, SUITE 1400 TORONTO, ONTARIO M5J 1C4
REF. FILE 16295-
589 HUMUS Proj. WHITE RIVER
NOV f 5 1993CUSTOMER No.
DATE SUBMITTED 29-Sep-93
Total Pages 14
1943
AU PPBMETHOD NA
DETECTION LIMIT 1.
*** UNLESS INSTRUCTED OTHERWISE WE WILL DISCARD PULPS IN 90 DAYS *** AND REJECTS IN 30 DAYS FROM THE DATE OF THIS REPORT
DATE 10-NOV-93 CERTIFIED BYJean H. L. Opdebej&k, Gene/a l Manager
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PAGE 2 OF 14
Fax (416)445-4152 Tlx 06-986947
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L46S-750WL46S-700WL46S-650UL46S-600WL46S-550U
L46S-500UL46S-450WL46S-400WL46S-350W L46S-300W
L46S-250WL46S-200W L4W150WL46S-100WL46S-50U
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PAGE 3 OF 14
Fax (416)445-4152 Tlx 06-986947
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L46S-125E L46S-150EL46S-175EL46S-200EU6S-225E
L46S-250EL46S-275EL46S-300E L46S-325EL46S-350E
L46S-375E L46S-400EL46S-425EL46S-4SOEL46S-550E
U46S-575EL46S-600EL46S-625E L46S-650EL46S-675E
L46S-700E L46S-725EL46S-750EL46S-775EL46S-800E
L46S-825EL46S-850EL46S-875E L46S-900EU6S-925E
146S-950E L46S-975EL46S-1000EL46S-1025EL46S-1050E
L46S-1075EL46S-1100EL46S-1125EL46S-1150EL48S-550E
L48S-575EL48S-600EL48S-625EL48S-650E L48S-675E
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IXRALiiiiiiiiiiiiiiiiii
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L48S-700E U8S-725EL48S-750EL48S-775EL48S-800E
L48S-825EL48S-850EL48S-875E L48S-900EL48S-925E
L48S-950E L48S-975EU8S-1000EL48S-102SEL48S-1050E
L48S-1075EL48S-1100EL50S-900U L50S-850WL50S-800U
L50S-750W L50S-725EL50S-700ELSOS-300EL50S-325E
L50S-350SL50S-375ELSOS-400E L50S-425EL50S-450E
L50S-475E L50S-500EL50S-525EL50S-550EL50S-575E
L50S-600EL50S-625E
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REPORT 24937 REF.FILE 16295- PAGE 5 OF 14
islie Street Don Mifls Ontario M3B 3J4 (416)445-5755 Fax (416)445-4152 Tlx 06-986947 Member of the SGS Group (Societe Generate de Surveillance)
IXRALi ——————————————— 1 10-Nov
SAMPLE AU
I L50S-950E L50S-975EL50S-1000E
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I L54S-975E L54S-1000EL54S-1025E
I L54S-1050E L54S-1075E
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I L54S-1125E L54S-1150E L54S-1175EL54S-1200E
I L56S-1150E L56S-1175EL56S-1200E
I L3200S-800E L3200S-825E
L3200S-850E
I L3200S-875E L3200S-900E L3200S-925EL3200S-950E
I L3200S-975E L3200S-1000EL3200S-1025E
I L3200S-10SOE L3200S-1075E
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PAGE 6 OF 14
Fax (416)445-4152 Tlx 06-986947
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L3600S-150EL3600S-175EL3600S-200E L3600S-225EL3600S-250E
L3600S-275E L3600S-300EL3600S-325EL3600S-350EL3600S-375E
L3600S-400E13600S-425EL3600S-450E L3600S-475EL3600S-500E
L3600S-52SE L3600S-550EL3600S-575EL3600S-600EL3600S-625E
L3600S-650EL3600S-675EL3600S-700EL3600S-725EL3600S-750E
L3600S-77SEL3600S-800EL3600S-825EL3600S-850EL3600S-875E
L3600S-900EL3600S-925EI.3600S-950E13600S-975EL3600S-1000E
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X-RAY ASSAY LABORATORIES 1885 Leslie Street Don Mills Ontario MSB 3J4 (416)445-5755Member of the SGS Group (Societe Generate de Surveillance)
PAGE 7 OF 14
Fax (416)445-4152 Tlx 06-986947
IXRALL in.
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L4825S-750WL4825S-700WL4825S-600U L4825S-550UL4825S-500U
L4825S-450U L4825S-400WL4825S-350UU825S-300UL4825S-250U
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L4825S-25EU825S-50EU825S-75EL4825S-100EL4825S-125E
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L4825S-275EL4825S-300EL4825S-325EL4825S-350E L4825S-375E
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PAGE 8 OF 14
Fax (416)445-4152 Tlx 06-986947
IXRAL111111111111111111
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L4825S-400EL4825S-425EL4825S-450EL4825S-475EL4825S-500E
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L502SS-400WLS025S-350UL5025S-300WL5025S-250UL5025S-200U
L5025S-150WL5025S-100WL5025S-50UL5025S-0+00L5025S-25E
L5025S-50EL5025S-75EL5025S-100EL5025S-125EL5025S-150E
L5025S-175EL5025S-200E L5025S-225EL5025S-250EL5025S-275E
U5225S-900WL5225S-800WL5225S-750UL5225S-700W L5225S-650U
L5225S-600WL5225S-550W L52.25S-500HL5225S-500WAL5225S-450W
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X-RAY ASSAY LABORATORIES 1885 Leslie Street Don Mills Ontario M3B 3J4 (416)445-5755Member of the SGS Grouo (Soci^t* Genirale de Surveillance)
PAGE 9 OF 14
Fax (416)445-4152 Tlx 06-986947
IXRAL111111111111111111
*SAMPLE
LS225S-150UL5225S-100UL5225S-50WL5225S-0+00LS225S-25E
L5225S-50EL5225S-75EL5225S-100EL5225S-125EL5225S-150E
L5225S-175EL5225S-200EL5225S-225EL5225S-250EL5225S-275E
L5225S-300EL5225S-325EL5225S-350E15225S-375EL5225S-400E
L5225S-42SEL5225S-450EL5225S-475EL5225S-500EL5225S-525E
L5225S-550EL5225S-575EL5225S-600EL5225S-625EL5225S-650E
L5225S-675EL5225S-700EL5225S-725EL5225S-750E L5225S-825E
L5225S-850EL5225S-875E I.5225S-9Q06L5225S-925EL5225S-950E
L5225S-975EL5225S-1000EL5225S-102SEL5225S-1050E L5225S-1075E
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X-RAY ASSAY LABORATORIES 1885 Leslie Street Don Mills Ontario MSB 3J4 (4161445-5755Member of the SGS Group (Sociite Generate de Surveillance)
PAGE 10 OF 14
Fax (416)445-4152 Tlx 06-986947
IXRALiiiiiiiiiiiiiiiiii
*SAMPLE
L5225S-1100EL5225S-112SEL5225S-1150EI5225S-1175EL5225S-1200E
LS425S-900U15425S-850ULS425S-800UL5425S-750WL5425S-700U
L5425S-650UL5425S-600UL5425S-550UL5425S-505WL5425S-380U
L542SS-350WL5425S-300WL5425S-250WL5425S-150WL5425S-100W
L5425S-50UL5425S-0+00L5425S-25EL5425S-50EL5425S-75E
L5425S-100EL5425S-125EL5425S-150EL5425S-175EL5425S-200E
L5425S-225EL5425S-250EL5425S-275EL5425S-300EL5425S-325E
L5425S-350EL5425S-375E 154255-4001L5425S-425EL5425S-450E
L5425S-475EL542SS-SOOEL5425S-525EL5425S-550E L5425S-575E
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X-RAY ASSAY LABORATORIES 1885 Leslie Street Don His Ontario MSB 3J4 (416)445-5755Member of the SGS Group (Soci6te Ge'ne'rale de Surveillance)
PAGE 11 OF 14
Fax (416)445-4152 Tlx 06-986947
1 l 111i1111111111111
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SAMPLE
L5425S-600E L5425S-625EL5425S-650EL5425S-675E L5425S-700E
L5425S-725EL5425S-750E L5425S-775E L5425S-800EL5425S-825E
L5625S-900U L5625S-850WL5625S-750WLS625S-700WL5625S-650U
L5625S-600UL5625S-550W L5625S-400U L5625S-350WL5625S-300U
L5625S-250U L5625S-BL200UL5625S-150UL562SS-100UL5625S-50U
L5625S-0+00L5625S-25E L5625S-50E L5625S-75EL5625S-100E
L5625S-125E L5625S-150EL5625S-175EL5625S-200E L5625S-225E
L5625S-250EL5625S-275E L5625S-300EL5625S-325EL5625S-350E
L5625S-375EL5625S-400EL5625S-425EL5625S-450E L5625S-475E
•Nov-93
AU PPB
2121
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X-RAY ASSAY LABORATORIES 18*Meml
REPORT 24937 REF.FILE 16295- PAGE 12 OF 14
jslie Street Don Mis Ontario MSB 3J4 (416)445-5755 Fax (416)445-4152 Tlx 06-986947Member of the SGS G roup ( Societe Centrale de Surveillance)
IXRALiiiiiiiiiiiiiiiiii
*SAMPLE
L5625S-500EL5625S-525EL5625S-550EL5625S-575EL5625S-600E
L5625S-625EL5625S-650EL562SS-675E L5625S-700EL5625S-725E
L5625S-750E TL12E-3650STL12E-3700STL12E-3750STL12E-3800S
TL12E-3900STU2E-3950STL12E-4000S TL12E-4050STL12E-4100S
TL12E-4150STL12E-4200STL12E-4250STL12E-4300STL12E-4350S
TL12E-4400STL12E-4450STL12E-4500STU2E-4550STL12E-4650S
TL12E-4700STU2E-4750STL12E-4800STL12E-4850STL12E-4900S
TL12E-4950STL12E-5050S TL12E-5100STL12E-5150STL12E-5250S
TL12E-5300STL12E-5350STL12E-5450STL12E-5500S TL12E-5550S
Nov-93 REPORT 24937 REF.FILE 16295-
AU PPB
1^<1
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X-RAY ASSAY LABORATORIES 1885 Leslie Street Don Mills Ontario M3B 3J4 (416)445-5765Member of the SGS Group (Soci6te GeYie'rale de Surveillance)
PAGE 1 3 OF 14
Fax (416)445-4152 Tlx 06-986947
JXRAL111111111111111111
9SAMPLE
TL12E-5600STL1200E-3450STL1200E-3500STL1200E-3550S
0 TL800U-4650S
0 TL8U-3350S0 BL200U-4675S D L34S-600W0 L38S-400U0 U6S-SOOU
D L46S-350ED L46S-1025ED L48S-1000ED L50S-625E D L54S-1100E
D L3200S-1200ED L3600S-475E D L3600S-1075ED L4825S-400WD L4825S-400E
D L5025S-150ED L5225S-0+00D L5225S-600ED L5425S-850U D L5425S-225E
D L5425S-825ED LS625S-200E D TL12E-3700SD TL12E-5050S
Nov-93 REPORT 24937 REF.FILE 16295-
AU PPB
2O
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X-RAY ASSAY LABORATORIES 1885 Leslie Street Don Mills Ontario M3B 3J4 (416)445-5755Member of the SGS Group (Soci*te Centrale de Surveillance)
PAGE 14 OF 14
Fax (416)445-4152 Tlx 06-986947
l l l l l l l l l
XR X-RAY ASSAY LABORATORIESA DIVISION OF SGS CANADA INC.
1885 LESLIE STREET - DON MILLS, ONTARIO M38 3J4 * CANADA TEL: (416)445-5755 TELEX: 06-986947 FAX: (416)445-4152
CERTIFICATE OF AJST AJL, Y SI S
REPORT 24839
TO: A.C.A. HOWE INTERNATIONAL LTD ATTN: DINO TITARO22 FRONT STREET WEST, SUITE 1400 TORONTO, ONTARIO M5J 1C4
REF. FILE 16199-
427 HUMUS
AU PPBMETHOD NA
^A*NOV 1 5 W95
CUSTOMER NO.
DATE SUBMITTED 24-Sep-93
Total Pages 10
1943
DETECTION LIMIT 1.
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*** UNLESS INSTRUCTED OTHERWISE WE WILL DISCARD PULPS IN 90 DAYS *** AND REJECTS IN 30 DAYS FROM THE DATE OF THIS REPORT
DATE 08-NOV-93 CERTIFIED BYJean H.L. Opde
Member of the SGS Group (SociEtE GEnErale de Surveillance)
PXRAL111111111111111111
*SAMPLE
TL800U-1850STL800U-1900STL800U- 1950STL800W-2050S TL800W-2100S
TL800W-2150STL800W-2250S TL800W-2300STL800W-2350STL800U-2450S
TL800U-2500STL800U-2550STL800U-2650STL800U-2700S TL800W-2750S
TL800W-2800STL800W-2850S TL800U-2900WTL800W-2950SBL200W- 1950S
BL200U-2050SBL200U-2100SBL200U-2150SBL200W-2250S BL200U-2300S
BL2W-2350S8L2U-24+50S BL2W-2500SBL2W-2550SBL2W-2650S
BL2W-2700SBL2W-2750SBL2W-28+OOSBL2U-2850S BL2U-2900S
BL2W-2950SBL2W-3050S BL2U-3100SBL2U-3150SL22S-800U
L22S-750WL22S-700WL22S-650WL22S-600U L22S-550U
-Nov-93 REPORT 24839 REF.FILE 16199-
AU PPB
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X-RAY ASSAY LABORATORIES 1885 Leslie Street Don Mis Ontario MSB 3J4 (416)445-6755Member of the SGS Group (Soctete* Genera l e de Surveillance)
PAGE 1 OF 10
Fax (416)445-4152 Tlx 06-986947
IXRALiiiiiiiiiiiiiiiiii
9SAMPLE
L22S-500W L22S-450WL22S-400UL22S-350UL22S-300U
L22S-250UL22S-200UL22S-150W L22S-100WL22S-50W
L22S-0+00 L22S-25EL22S-50EL22S-75EL22S-100E
L22S-125EL22S-150EL22S-175E L22S-200EL22S-225E
L22S-250E L22S-275EL22S-300EL22S-325EL22S-350E
L22S-375EL22S-400EL22S-425E L22S-450EL22S-475E
L22S-500E L22S-525EU22S-550EL22S-575EL22S-600E
L22S-625EL22S-650E1.22S-675E L22S-700EL22S-725E
L22S-750EL22S-775EL22S-800EL22S-825E L22S-850E
AU PPB
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X-RAY ASSAY LABORATORIES 1885 Leslie Street Don Mffls Ontario M3B 3J4 (416)445-5765 Fax (416)445-4152 Tlx 06-986947Member of the SGS Group (Socilte Centrale de Surveillance)
fXRAL111111111111111111
*SAMPLE
L22S-875EL22S-900EL22S-925EL26S-800W L26S-750W
L26S-700UL26S-6SOU L26S-600UL26S-350WL26S-300U
L26S-250WL26S-200WL26S-150WL26S-100U L26S-SOU
L26S-0L26S-25E L26S-50EL26S-75EL26S-100E
L26S-125EL26S-150EL26S-175EL26S-200EL26S-225E
L26S-250EL26S-275E L26S-300EL26S-325EL26S-350E
L26S-375EL26S-400EL26S-425EL26S-450E L26S-475E
L26S-500EL26S-S2SE L26S-550EL26S-575EL26S-600E
L26S-625EL26S-650EL26S-675EL26S-700E L26S-725E
•Nov-93 REPORT 24839 REF.F1LE 16199-
AU PPB
23221
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X-RAY ASSAY LABORATORIES 1885 Leslie Street Don Miis Ontario M3B 3J4 (416H45-5755Member of the SGS Group (Societe Centrale de Surveillance)
PAGE 3 OF 10
Fax (416)445-4152 Tlx 06-988947
IXRALiiiiiiiiiiiiiiiiii
9SAMPLE
L26S-750E L26S-775EL26S-800EL26S-82SEL26S-850E
L26S-875EL26S-900EL26S-925E L26S-950EL26S-975E
L26S-1000E L26S-1025EL26S-1050EL26S-1075EL26S-1100E
L26S-1125EL26S-1150EL26S-1165E L28S-450UL28S-400U
L28S-350W L28S-300WL28S-250UL28S-150UL28S-100U
L28S-50WL28S-0L28S-25E L28S-50EL28S-75E
L28S-100EL28S-125EL28S-150EL28S-175EL28S-200E
L28S-225EL28S-250E L28S-275EL28S-300EL28S-325E
L28S-350EL28S-375EL28S-400EL28S-425E L28S-450E
-Mov -93 REPORT 24839 REF.FILE 16199- PAGE 4 OF 10
AU PPB
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X-RAY ASSAY LABORATORIES 1885 Leslie Street Don MiHs Ontario M3B 3J4 (416)445-5755 Fax (418)446-4152 Tlx 06-988947 Member of the SGS Group (Societe Centrale de Surveillance)
IKRAL1 11111111111111111
9SAMPLE
L28S-475EL28S-500EL28S-525EL28S-550E L28S-575E
L28S-600EL28S-625E L28S-6SOEL28S-67SEL28S-700E
L28S-725EL28S-750EL28S-775EL28S-800E L28S-825E
L28S-850EL28S-875E L28S-900EL28S-925EL28S-950E
L28S-975EL28S-1000EL28S-1025EL28S-1050E L28S-1075E
L28S-1100EL28S-1125E L28S-1150EL28S-1175EL32S-150W
L32S-100UL32S-50WL32S-0L32S-25E L32S-50E
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PAGE 6 OF 10
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L2000S-675EL2000S-700EL2000S-725EL2000S-750EL2000S-775E
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L2000S-925EL2000S-950E12000S-975EL2000S-1000EL2000S-1025E
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PAGE 7 OF 10
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X-RAY ASSAY LABORATORIES 1885 Leslie Street Don Mills Ontario M3B 3J4 (416)445-5755Member of the SGS Group (Soci6te Generate de Surveillance)
PAGE 8 OF 10
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X-RAY ASSAY LABORATORIES 1885 Leslie Street Don Mills Ontario M3B 3J4 (416)445-6755Member of the SGS Group (Soci^t* Generate de Surveillance)
PACE 9 OF 10
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REF.FILE 16199- PAGE 10 OF 10
Don Mis Ontario M3B 3J4 {416)445-5755 Fax (416)445-4152 Tlx 06-986947Member of the SGS Group ( Soc1*t* Generale de Surveillance)
TO: A.C.A. HOWE INTERNATIONAL LTD ATTN: DINO TITARO22 FRONT STREET WEST, SUITE 1400 TORONTO, ONTARIO M5J 1C4
REF. FILE 16232-
287 PULPS Proj. WHITE RIVER
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1885 LESLIE STREET - DON MILLS, ONTARIO M3B 3J4 ' CANADA TEL: (416)445-5755 TELEX: 06-986947 FAX: (416)445-4152
CERTIFICATE OF AJST AJL Y SI S
REPORT 24826
CUSTOMER NO.
DATE SUBMITTED 24-Sep-93
Total Pages 7
5 19931943
METHOD NA
DETECTION LIMIT 1.
*** UNLESS INSTRUCTED OTHERWISE WE WILL DISCARD PULPS IN 90 DAYS *** AND REJECTS IN 30 DAYS FROM THE DATE OF THIS REPORT
DATE 08-NOV-93 CERTIFIED BYJean H.L. Opdejfeeck,
Member of the SGS Group ( SociEtE GEnErale de Surveillance)
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PAGE 2 OF 7
Fax (416)445-4152 Tlx 06-986947
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Nov-93 REPORT 24826 REF.FILE 16232- PAGE 4 OF 7
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PAGE 5 OF 7
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PAGE 6 OF 7
Fax (416)445-4152 Tlx 06-986947
IXRALiiiiiiiiiiiiii
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1X-RAY ASSAY LABORATORIES 1885 Leslie Street Don Mills Ontario M3B 3J4 (416)445-5755
Member of the SGS Group (Soci*te Centrale de Supveiltance)
PAGE 7 OF 7
Fax (416)445-4152 Tlx 06-986947
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APPENDIX D - CLAIM INFORMATION
CLAIM NUMBERS10437311043789-7911043774-7761043743-7711043718-7211043724-727
1043779-7861043994-9951044084-086
1043799-8021024801-808
1024809-8371044389-3921044393-4011044402-403
1069122-1851069107-119
1069101-1061044378-3791044359-361
10443721044374-377
1044380-38710443881044362-371
NUMBER OF CLAIMS1332944
8234829
4926413
62314
8110
TOWNSHIP
OdlumOdlumOdlumOdlumOdlumOdlumOdlumOdlumOdlumOdlumOdlumTedderOdlumTedderStricklandStricklandStricklandCooperTedderTedder
StricklandStrickland
StricklandTedderStrickland
OWNER
J. TernoweskyJ. TernoweskyJ. TernoweskyJ. TernoweskyJ. TernoweskyJ. TernoweskyJ. TernoweskyJ. TernoweskyJ. TernoweskyJ. TernoweskyP. NabigonJ. TernoweskyJ. TernoweskyJ. TernoweskyJ. TernoweskyP. NabigonP. NabigonP. NabigonJ. TernoweskyJ. TernoweskyJ. TernoweskyJ. Ternowesky
J. TernoweskyJ. TernoweskyJ. Ternowesky
EXPIRY DATEDec. 7/93Dec. 7/93Dec. 7/93Dec. 7/93Dec. 7/93Dec. 7/93Dec. 7/93Dec. 7/93Dec. 7/93
Dec. 7/93Nov. 23/93Nov. 23/93
Dec. 15/93Dec. 15/93Dec. 15/93May 2/94May 2/94
May 16/94Dec. 15/93Dec. 15/93Dec. 15/93Dec. 15/93
Dec. 15/93Dec. 15/93Dec. 15/93
l l l l l l l l l l l l l l l l l l l
1078215-219
1078220-2351078236-237107823810782391078240-2421078305-3061078307TOTAL
516
211321256 claims
OdlumStricklandOdlumStricklandOdlumStricklandStricklandOdlum
P. NabigonP. NabigonP. NabigonP. NabigonP. NabigonP. NabigonJ. TeraoweskyJ. Teraowesky
Mar. 10/94Mar. 10/94Mar. 10/94Mar. 10/94Mar. 10/94Mar. 10/94Mar. 10/94Mar. 10/94
l l l l l ll APPENDIX E - GEOPHYSICAL REPORT
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l TECHTERREX INCORPORATEDOakville, Ontario
m October 22, 1993
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REPORT ON A GROUND MAGNETIC/VLF-EM SURVEY
STRICKLAND t ODLUM TOWNSHIPS
SAULT STE. MARIE MINING DIVISION
ONTARIO
FOR
AKIKO GOLD RESOURCES LTD.
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TABLE OF CONTENTS
Page
l1.0 Introduction l
2.0 Property Location and Access 2
l 3.0 Grid Description 3
g 4.0 Geological Setting 3
l 5.0 Previous Work 4
U 6 .0 Ground Magnetic/VLF-EM Survey
6.1 Survey Instrumentation And Description 5
l 6.2 Data Presentation 7
6.3 Discussion of Results 7
7.O Summary S Recommendations 8
l— Figures
1. Property Location
2. Claim Block
Tables
I. Odlum S Strickland Mining Claims
ll W TABLE OF CONTENTS (Cont'd)
l Maps
m NORTH MAP SHEETS
WRP-01 Total Field Magnetic Postings St Profiles
l WRP-03 Total Field Magnetic Contours
—
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WRP-05 VLF-EM Postings 6 Profiles
WRP-07 VLF-EM Fraser Filter Contours
WRP-09 Plan of Interpretation
SOUTH MAP SHEETS
WRP-02 Total Field Magnetic Postings 6 Profiles
l WRP-04 Total Field Magnetic Contours
WRP-06 VLF-EM Postings d Profiles
WRP-08 VLF-EM Fraser Filter Contours
WRP-10 Plan of Interpretation
Selected References
Appendix
A Survey Personnel
B Survey Instrument Specification
l
- l -
1.0 Introduction
l l l
During the period of September 2, 1993 through to September 29,
l 1993 TechTerrex Inc. performed a ground magnetometer and VLF-EM
survey over a portion of the mining claims held by Akiko Gold
f Resources Ltd. It was anticipated that these surveys would assist
— the geological mapping program that was being conducted
™ concurrently in order to define lithological boundries as well as
fl structural settings of the area under investigation. Exploration
efforts were concentrated towards tracing the possible extention of
l a gold bearing deformation zone reported by Hemlo Gold Mines on the
mining claims immediately to the north of the report area.
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l l -B 2.0 Property Location and Access
The mining claims reported herein are located in Strickland and
l Odlum townships in the Sault Ste. Marie Mining Division of Ontario.
Refer to Table I for a listing of the claim numbers. Figure l
l illustrates the location of the property. Figure 2 shows the claim
— block covered by this report.
H The property is accessible by either two or four-wheel drive
vehicle from the village of White River located on the Trans Canada
J Highway (#17) approximately 315 kilometers northwest of Sault ste.
Marie, Ontario. A travel permit is required from the White River
B office of Domtar Ltd. in order to travel the logging roads that
m lead to the centre of the property; specifically, logging roads
#200, 206 and 216. The exploration area is approximately 40
l kilometers northeast of White River.
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11 '1 1111111111111111
tTABLE Z
The following claims are located in Odlum and Strickland Townships:
1042761
1043718
1043768
1043782
1043783
1043800
1043801
1043802
1043994
1043995
1044080
1044085
1044394
1044396
1044804
1068159
1069154
1069155
1069156
1069157
1069160
1069161
1069162
1069163
1069164
1069165
1069166
1069167
1069168
1069169
1069170
1069171
1069172
1069173
1069174
1069175
1069176
1069177
1069178
1069179
1069180
1069181
1069182
1069183
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AKIKO GOLD RESOURCES LIMITED ffHITE RIVER GOLD PROJECT
LOCATION MAP
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l l -l 3.0 Grid Description
The Strickland Lake grid was prepared by Norman McBride Linecutting
l Services between August 23, 1993 and September 23, 1993. The grid
consists of a series of baselines oriented at a 340 degree azimuth
f using a magnetic declination of 7 degrees west. Baseline O extends
from O to 1625S while baseline 200W runs from 1600S to 5625S. Two
B tielines oriented parallel to the baselines were established at
•j 800W and 1200E and stretch from O to 5600S. Perpendicular to the
baseline, crosslines have been established at 200 metre intervals
l along the base line from OS to 5625S. Station intervals along all
cross, base and tie lines are at a nominal 25 metre separation. A
l total of approximately 66 line kilometres were cut out.
4.0 Geological Setting
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The report area lies within the Dayohessarah Lake greenstone belt
which is composed primarily of a metavolcanic and metasedimentary
rock package surrounded by granitic rocks.
l The metavolcanic rocks are primarily massive and schistose type
amphibolites, basic to intermediate lava flows and volcanic
fragmental rocks such as tuff and agglomerate.
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The metasedimentary rocks consist of quartz-plagioclase-biotite
schists and gneisses, garnetiferous biotite schists and
conglomerate.
Basic intrusive rock types, such as gabbro and metagabbro are found
l within both the metavolcanics and metasediments and occur as dikes
M and small stocks. In some instances, the metavolcanics and
" metasediments have been intruded by sills, dikes and small stocks
of granitic material.
jj Numerous diabase dikes intrude the other rock types and are
— oriented in either a northwest or northeast direction and can range
" in width from a few inches to hundreds of feet.
5.0 Previous Work
lThe Oayohessarah Lake metavolcanic-metasedimentaary belt has been
l subjected to numerous mineral exploration programs. Some of the
m more recent work includes:
-In 1975 Shell Canada Ltd. mapped the central part of the
l greenstone belt at a scale of I llssl74 mile.
l -In 1983 Pezamerica Resources Corporation commissioned an
electromagnetic/magnetic airborne survey over parts of
ll -l Hambleton Township. Pezamerica investigated the
•j anomolous responses with limited geochemical, geological, and
geophysical surveys. Geochemical results indicated that the
l eastern edge of the metasedimentary belt contained highly
anomolous gold values.
M -In 1985 the Pezim group conducted geological reconnaisance
™ and geochemical ("B" horizon) surveys over 24 small grids in
l Odlum Township. The most promising geochemical result was a
690ppb gold anomoly on the northeast corner of claim #665317,
J located west of the southern part of Dayohessarah Lake.
" -In 1990 Broad Horizons Inc. commissioned an airborne
B magnetic/VLF-EM survey over portions of Odlum, Strikland,
Tedder and Hambleton Townships.
l lm 6 .0 Ground Magnetio/VLF-EM Survey
l 6.1 Survey Instrumentation and Description
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The total field magnetic and VLF-EM measurements made over the
Strickland Lake grid were recorded at 12.5 metre intervals along
l l -l all base, tie and crosslines. In each instance, both the VLF-EM
m and total field magnetic measurements were collected simultaneously
using the EDA Omni Plus magnetometer/VLF-EM receiver system
l manufactured by Scintrex Ltd. of Concord, Ontario.
l The magnetic survey also used an EDA Omni IV base station
^ magnetometer to monitor and record the diurnal fluctuations to the
* earth's magnetic field. These measurements, using a base station
l value of 58,750 nanoteslas were used to correct the field
measurements for diurnal magnetic drift.
lThe VLF-EM survey conducted on all crosslines made use of the
B transmiter facility at Annapolis, Maryland which transmits at 21.4
B kHz. For the base and tielines, measurements were taken using the
Cutler, Maine transmitter station which operates at 24.0 kHz. In
l each instance, both the in-phase and quadrature components of the
electromagnetic wave were recorded.
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6.2 Data Presentation
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The results of the survey are divided into North and South map
l sheets at a scale of 1:5000.
l The total field magnetic data is presented in plan as postings and
g profiles (maps WRP-01 and WRP-02) and as contours (maps WRP-03 and
" WRP-04).
lThe VLF-EM measurements, i.e., in-phase and quadrature, are
l presented as postings and profiles on maps WRP-05 and WRP-06. A
Fraser filter was applied to the in-phase data in order to
™ transform the cross-overs over possible conductors into positive
peak anomalies. These are presented in contour form on maps WRP-07
and WRP-08.
l5.4 Discussion of Results
m An interpretation of the lithological units and the underlying
structure has been presented in plan on maps WRP-09 and WRP-10.
l The total field magnetic survey has outlined six possible
geological units as follows:
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l Unit 1: broad, moderately magnetic high, dipping near
•j vertical which correlates with possible mafic
metavolcanic rocks such as amphibolites.
lUnit 2: broad, weak magnetically, near vertical dip
g which corresponds to typical metasedimentary rocks such
— as siliceous wacke and sandstone.
l Unit 3: broad, strong magnetic high which corresponds to
mafic intrusive rocks such as gabbro.
lUnit 4: broad, erratic magnetic high which corresponds
l to granitic rocks.
Unit 5: very weak magnetically, difficult to
l differentiate from Unit l other than by shape, possibly
late felsic intrusive rocks.
lm Unit 6: outlines the strongest, positive magnetic
anomalies ranging in widths from 20 metres to 100 metres
l correlating with diabase dikes. These dikes trend
predominately northwest although others trend north-
l northeast.
l l -l Structurally, two systems of fault planes have been outlined from
•| both the magnetic and VLF-EM data. The first set strikes
™ predominately northwest while the second set strike north to
l northeast. These faults may contain conductive material.
J 6.0 Summary fi Recommendations
™ The ground geophysical surveys have assisted in mapping the main
•j geological units of the area. This first phase of geophysics
should be followed with a second phase of exploration in order to
l pinpoint any possible extention to the mineralization found on the
claims north of the property. Prior to undertaking any drilling
l program, the following is recommended:
1) obtain the airborne electromagnetic results of the 1983 Dighem
l survey in order to assess whether or not concentrations of
sulphides exit which may be associated with possible gold
l mineralization.
2) undertake either a horizontal loop EM or induced polarization
l survey after considering the results from item l and bearing
in mind that the interpreted faults may contain conductive
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sulphides. A diamond drill program would then test any
favourable anomalies encountered.
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3) complete magnetic and VLF-EM coverage over the various lakes
and swamps prior to performing additional surveys.
Respectfully submitted, TechTerrex Inc.
Michael C. Wilson, President.
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STATEMENT OF QUALIFICATIONS
m The author of the report is Mr. Michael C. Wilson who resides at
199 Sheraton Court, Oakville, Ontario L6L 5N3. Mr. Wilson is a
l graduate of the Geology Technology Program, Cambrian College of
Applied Arts S Technology, having graduated in 1974. Since that
l time he has been steadily employed as a geophysical consultant,
— namely as president of TechTerrex Inc. The report is based upon
™ the survey results which were acquired by Mr. Wilson between
H September 2, 1993 and September 29, 1993.
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TechTerrex Inc.
Michael C. Wilson President
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SELECTED REFERENCES
Fenwick, K.G., Geology of the Dayohessarah Lake Area, Ontario.
Geological Report 49, Scale: l inch to 2 miles,
Accompanyed by Map 2129, 1967
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APPENDIX A
SURVEY PERSONNEL
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The following personnel provided data acquisition services for the
duration of the surveys:
Michael C. Wilson
199 Sheraton Court
Oakville, Ontario
L6L 5N3
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APPENDIX B
SURVEY INSTRUMENT SPECIFICATION
EDA Omni Geophysical System
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Brief Description
When you require more flexible geo physical techniques in order to find the increasingly more elusive anoma lous targets, Scintrex offers you the EDA Omni System. This system enables you to design your own unique instrument whether it is for complete Magnetic surveys, VLF Electromagnetic surveys or a combi nation of these techniques.
At the heart of the Omni System is the Omni System Control Console which is common to all Omni System appli cations. This customized approach gives you the ability to select the fol lowing options for your instrument:
* Portable Field and Base Station Magnetometer
* True Simultaneous Gradiometer* Portable Field and Base Station VLF
Electromagnetic Receiver* Two Probe, VLF Resistivity* Non-Orientation, VLF Resistivity
Applications
Since the Omni System capabilities are so versatile, the data collected and recorded by the instrument can be applied to a variety of earth sciences including:
- mineral exploration- geological mapping- groundwater exploration- groundwater contamination- civil engineering- geotechnical studies- archaeology
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Features
Omni System Features
Each Omni System incorporates the fol lowing features:
Flexibility of the Omni System
You can select your own options to cus tomize your unit to suit your specific geo physical needs.
Microprocessor Controlled
Gives you a choice of three fully protected data storage modes:
- spot record, for readings without grid co ordinates (random samples)
- multi-record, for multiple readings at one station
- auto-record, for automatic update of sta tion position
Complete Data Protection
The internal lithium battery assures you of complete data protection for up to 5 years.
Measures and Records In Memory
Measurement and recording in memory of the following magnetic field data for each reading:
- total field magnitude- true gradient of the total field- applied base station value- statistical error- signal strength . decay rate
Measurement and recording in memory of the following VLF data for each field read ing:
- vertical in-phase- vertical quadrature (out-of-phase)- total field strength- total dip angle- primary field direction- apparent resistivity- phase angle- signal-to-noise ratio- operator quality
The OMNI system configured as a MAG/VLF simplifies geophysical surveys by combining Magnetic and VLF EM techniques.
Records Survey Data
Records the following survey data for each magnetic and/or VLF reading:
- time of measurement and date- grid co-ordinates- direction of travel along grid lines- natural and cultural features
Measures up to 3 VLF Transmitting Stations
The Omni System can measure up to 3 VLF transmitting stations and provides more complete coverage of an anomaly regardless of the orientation of the trans mitter with respect to the survey grid or the anomaly itself.
Electronic Notebook
The internal Electronic Notebook enables you to record natural and cultural features that are unique to each grid location. This feature eliminates the need for a field notebook and provides additional informa tion that can assist in interpreting record ed data.
Automatic Correction Using The Omni System's Unique "Tie-Line" Technique
The Tie-Line" algorithm used exclusively by the Omni System allows for the self cor rection of atmospheric magnetic variations and variations in the primary field from the VLF transmitter(s). The instrument is able to store 'looping' or tie line' data in a sepa rate memory at the beginning of each sur vey and then subsequently stores total field readings in a second memory along with the field readings of the tie point(s). At the end of each survey day the Omni System will then merge these two memo ries to automatically correct the total field data for diurnal variations.
The Omni System in the "Tie-Line" mode can:
- Store looping or tie line data, 3 ways:
1. Using one looping base point2. Using one "Tie-Line" comprising a
number of tie points, or3. Using multiple tie lines.
- Store up to 100 tie points in one survey area or divide these points into exten sions of survey areas as needed.
- Store tie points or tie lines for the dura tion of the survey.
- Calculate the drift between established tie points, to readily see variations in the Earth's magnetic field.
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Features
"Looping" Method
1 +OON j-
0 + 50N !-:|- - ———— *
LO+00•^ —— .
0 + 50S
1+OOS
(^) Base Point^. Tielng back to base point-* Direction of Travel
"Tie-Line" Method
c1+OON i-
0 + 50N j-
-^y —————
- - — i
- ^ — *
LO+00 0 + 50S
1+OOS
^) Base Point
(x) Tie-Point ^
f"
ft~
7^L L
^ 4—
^~~~~~
. *-
,— —-•*-
:i^— Base Line
"}
L1+OOE L2+OOE
^ -
^(,\.
^
P 3 "j"i i "
""i —
— ^ —j
-]
:j"^e- Tie-Line•0 *J J J J
L1+OOE L2+OOE
Setting up Tie-Line and tieing back to base point Direction of travel
The "Tie-Line" feature available in all OMNI configurations provides a significant cost savings by allowing diurnal corrections to be made internally by one instrument without the need of a dedi cated base station instrument
Rapid Data Recall
With a few keystrokes, you can instantly recall data from memory to the digital dis play by record number or in sequence. Scanning through the memory of a partic ular parameter is also possible.
Wide Range of Data Output Capabilities
The ability to efficiently transfer and pre sent data in an interpretable format is important to the success of any survey or project.
The Omni System accomodates a wide selection of data output options, from sim ple listings of data and profile plots on a printer, to integrated software programs for computer plotting and modelling. The Omni System can transfer uncorrected, corrected or filtered magnetic and VLF data to most computers and printers with a RS-232C serial port.
Two Types of Formats available - data can be output from the Omni System in two format types. For ready to use data, the columnarized data dump format is the most suitable for direct hard copy printer
outputs. For data which is to be further used with computer plotting or analysis software packages, you can select the fixed ASCII CPU dump format.
Profile Plot Outputs - Since VLF as well as magnetic data is often easier to inter pret as a profile plot, data that the Omni System collects, can be presented in this analog format at a vertical scale best suit ed for data presentation. You can selec tively output in analog and/or digital for mat the following:
- the magnetic total field strength- the magnetic vertical gradient- the VLF in-phase- the VLF out-of-phase (quadrature)- the VLF total field strength
Data Presentation - The grid co-ordi nates under which the Omni System col lects the data can be output in the stan dard Cartesian format (using positive and negative signs) or with the more familiar N,S,E,W compass descriptors.
Editing Capabilities - Prior to data trans fer, you can program your Omni System to transfer a designated block of data, denoted by start and end points. Data can be separated into files that are best suited for survey or plotting conditions.
Pause Feature - You may stop the trans fer of data at any time and resume where it left off, when it is more convenient. The Omni System will continue to pause until you press any one of keys on the keypad.
Choice of Data Outputs - The Omni System outputs data in a choice of for mats, depending on the operating mode:
- corrected magnetic total field data- uncorrected magnetic total field data- magnetic base station data- magnetic gradient field data- corrected VLF field strength data- uncorrected VLF field strength data- VLF base station data- corrected "Tie-Line" data- uncorrected "Tie-Line" data
The Omni System can also transfer VLF data from all 3 VLF frequencies simulta neously or sequentially.
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Features
ami-tint Tie-iim MAG/VLF RHK tut 1 421150TOTAL FICLO DATA (uncorrected) ( GRADIENT
Reference field: 5(000.0 Datum subtracted: O.ODate 13 DEC S t Operator: 5000 Reeorda: 10 Bat: 17. S Volt lithium: 3.41 Volt tait time update: 12/13 9:50:00 Start of print: 12/13 14:34:01
Lin* 0400 E Data 13 DEC t t 1 2 POSITION r J ELD ERR DRIFT TIKE DS CULT
0410 N 56779. .04 0.0 11:38:55 IB 0490 N 5(7(9. .04 0.0 11:39:33 VI1+001*10142014JO1440145014(0 N1470 H
5(747.S((27.5*418.5((1(.5(733.5(7(5.5(7(4.5(7(7,
.05
.05
.01
.07
.05
.04
.05
.04
0.0 11:40:10 M0,0 11:41:47 (B0.0 11:42:30 tiPIPE0.0 Il:43l3( II0.0 11144:28 II0.0 11:45:01 II0.0 11:45:47 II0.0 11:46:26 II
GRADIENT 1.1 1.22.11.7
-13.1-41.0
(.2I.I1.10.7
CMNI-PLUS Tl.-lln. MAG/VLF R22K Sar 1421150 VLF TOTAL FIELD DATA {uncorreeted)
Data 13 DEC IIOperator: 5000 Raeordal 10 Batt 17.5 Volt Llthlun: 3.41 Volt
Laat tlna update: 12/13 1:50:00 Start or print: 12/13 14:35:51
Line 0400 E Date 13 DEC II 24.0 12 POSITION I/P QUAD T.FLD TILT TIME CULT S DIR 4-FRA S-FRA 0410 N 20. -5.4 71.14 (1.0 11:31:55 55 7.0 0490 N 21. -7.6 73.45 (7. 11:39:33 44 11.71400 N1410 N1420 N1430 D1440 N1450 N14(0 N1470 N
41.(1.K.
-101.-11.1-53.6-40.7-34.6
-10.2 71.12-13.7 91. (1-t. t 202.412.2 202.021.7 95.1715.1 77.0313.4 (1.0711.7 (3.02
79.15.14.14.11.76.74.71.
11:40110 4311:41:47 43ll:42i30PIPE 5211:43:36 5911:44:21 5911:45:01 5911:45:47 4911:46:26 49
0.6-K. 4 -36.0-14.4 -22.7-9.5 -4.0
-14.2 3.6-22.2 10.0-24.3 14.4-K. 9 12.5
-29.4-13.4-0.2(.1
12.213.4
Typical sample of data output from the OMNI system
Sealed, User Friendly Keypad
Protects your Omni System from water and dust and allows for easy operation and reliability.
Digital Display
Distinctly shows data which can some* times be unclear with analog or audio- nulled systems.
Display Descriptors
Monitor the signal strength and decay rate of the magnetic total field and/or the quality of all three VLF transmitter signals being measured.
Power Supply Options
You can choose from the following power supply options:
1 Non-magnetic rechargeable sealed leadacid battery
' Non-magnetic rechargeable sealed leadacid battery belt
' Alkaline battery belt 1 12V DC power source for base stationoperation
TIEBASE SPECIAL] SPOT
RECORD
MCALLI M*T IftEF.FtD
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Imni System Benefits
Only One Instrument Needed (or Magnetometer, Gradiometer, VLF and VLF Resistivity Surveying
The Omni incorporates the capabilities of a "Tie-Line" magnetometer and simulta neous Gradiometer system with the ability to measure VLF magnetic and electric Melds.
Only one complete Omni System is need ed to record all of the following geophysi cal parameters:
1. The total magnetic field2. The simultaneous gradient of the total
magnetic field.3. The VLF magnetic field including:
- the vertical in-phase- the vertical quadrature- the total field strength- the total dip
4. The VLF electric field, Including:- the phase angle- apparent resistivity
A complete Omni System can, at each location, calculate and record in less than 8 seconds, four VLF magnetic field parameters from three different transmit ters, a magnetic total field reading and a simultaneous magnetic gradient reading. In addition, it can also measure and record two VLF electric field parameters from three different transmitters.
Upgrade your Unit at any Time
Since the Omni System is based on a modular design, you can upgrade your system at any time. This built-in flexibility allows you to purchase an Omni System with only the surveying equipment that you need for now but does not limit you to one application. When your surveying needs grow, so can your Omni System.
Saves you Time
The Omni System with the unique 3-coil VLF Sensor does not require orientation of the VLF Sensor head toward the trans mitter station. This simplifies VLF field procedures and saves considerable sur vey time. The operator does not need to orient the sensor head toward the first, selected transmitting station and then re
orient towards the second or third trans mitting station.
The non-orientation technique Is the first of its kind, and this provides the Omni System with many additional benefits. These benefits include:
- When you use the Omni System as both a magnetometer and VLF base station, you only need one instrument instead of three,, to record data auto matically from 3 VLF transmitting sta tions.
- When you use the Omni System with the Non-orientation VLF-Resistivity option, you can record automatically from 3 different stations the phase angle and apparent resistivity without having to re-orient any of the three electrodes. You can also use the Omni System with the conventional, two electrode method.
The Omni System quickly responds with a one-key operation. For example, if you must complete a magnetometer/gra- diometer and three frequency VLF survey using the Omni System, you automatically measure the magnetometer, simultane ous gradiometer and three VLF frequency data by pressing only one key. Using another combined system, up to 5 differ ent steps may be required. Such as, the operator would have to take one magnetic reading; then another sequential magnet ic reading to calculate the gradient; orient the VLF sensor to the first VLF transmitter and then take a reading; orient the VLF sensor to the second transmitter, take a new reading and then repeat the same procedure for the third frequency. The Omni System one-key operation takes less than 8 seconds; a significantly short er time period than the 5 step operation of other combined systems.
Since the Omni System saves all of the field data in memory and has many output capabilities, the elimination of the field notebook and also the transciption errors that can occur saves you a considerable amount of lime.
Diurnal corrections, using the time saving lie-line" method, can be done automati
cally by the Omni System eliminating hours of manual and tedious calculations. You can then directly transfer the correct ed data to a computer for further data pro cessing.
Higher Productivity System
Combined Magnetomeler/VLF systems are inherently faster than conventional methods whereby two different operators collected magnetometer and VLF data from separate instruments.
Because of its unique user-friendly design, the Omni System provides higher field productivity for the user. The increased productivity originates from its two-micro processor approach which significantly reduces calculation time and also from the non-orientation VLF technique.
Sensitive to Weak VLF Signals
The Omni System's ability to obtain repeatable readings from weak signals offers a number of benefits:
- It extends the use of VLF on to coun tries where its use was previously marginal.
- It enables you to increase the number of frequencies with which you can operate.
- It reduces your need for portable VLF transmitters
- It improves the quality of your read ings in rugged terrains, such as the deep valleys of the North American Rockies.
The Omni System's digital signal process ing removes the modulation in the received signals. This technique helps stabilize too weak signals much greater than the conventional phase-locked loop method.
Ability to receive weaker signals (20nA7m) and a background noise reduction algo rithm are among the reasons why the Omni System can obtain repealable read ings from signals which had previously been too weak to record.
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Omni System Benefits
Excellent Data Quality and Repeatability
The Omni System provides users with unparalleled data quality and repeatability. The 3-orthogonal coil sensor that the Omni System uses improves the data reli ability over the conventional two-coil method as it provides a more complete calculation of both the in-phase and out- of-phase parameters. This difference becomes even more important in measur ing large anomalies.
The 3-coil sensor method provides con sistently high data quality unrelated to the operator's ability to orient the sensor for optimum coupling with the transmitting station. The higher data quality that the Omni System obtains with weak signals is enhanced even further when signals are stronger. Additional features, such as greater channel selectivity, atmospheric noise reduction and better immunity to spikes, Improve even more the Omni System's capability to obtain repeatable data.
No Need lo Take Multiple Readings
The Omni System's magnetic component uses four leading-edge design features to eliminate the need to take multiple read- Ings, these are:
- Signal Processing Technique- Constant Energy Polarization that
maintains equal energy to the sensor- Processing Sensitivity to ± 0.02
gamma- Automatic Fine Tuning which uses the
previous reading as the base for the next reading.
The "Tie-Line" Advantage
Not only does the Omni System eliminate hours of manual correction of data, it also gives you the flexibility of choosing the most appropriate tie-line method best suited for the survey, depending on the size and character of the grid. You can choose from:
- a single base point,- a single tie-line,- multiple tie-lines, or- a random scattering of tie-points.
The self-correcting Tie-Line" feature can remove base station requirements from some surveys. The "Tie-Line" data can be recalled even if it was stored on differ ent days.
You can program the Omni System to automatically remove a designated datum from field data and by removing this coarse, background value, plotting and interpreting the magnetic field data is made easier. The Omni System can also automatically calculate the desired diurnal drift measured between consecutive tie- point readings.
-\, 4' V: ,* \ -i .Environmentally sealed design ol the OMNI permits use in all weather conditions
Operate Your Omni System in any Environment
The Omni System is completely water proof and dust proof. The fully sealed housing console ensures that you can perform your surveying needs during adverse weather conditions.
A Variety of Software Programs Available
Although the Omni System can transfer data directly to a serial printer, most com puters require some initial handshaking prior to actual data transfer. Scintrex pro
vides such handshaking programs for many computers including IBM PS-2/ IBM PC (AT and XT), Compaq, Macintosh and compatible systems.
In addition to handshaking software, we can provide you with plotting, profiling, contouring and modelling programs avail able from certain software houses. Packages for use with the Omni System include:
- Mapping systems that allow you to post and plot many of the geophysical parameters available, in a plan-profile or contoured format.
- Cartographic quality large-scale and real-location plan maps, complete with custom map surrounds, legends, scale bars, etc., that can be produced in a matter of minutes on most dot- matrix printers or small and larger- scale plotters. Standard graphics screen previewing is available prior to plotting.
- Software that allows you to present the data in 2 or 3-D perspective plots, through a full menu and/or command driven system interface in which you can select different colours, sizes, scales, angles etc. For example, you can create shaded relief maps and colour image plotting on common high resolution printers, including grey- scale support on laser printers.
- Interactive filtering and modelling pro grams that are used to determine the possible geometry and physical char acteristics of the sources of magnetic anomalies, such as the MAGMOD program.
- Autocad and image-processing capa bilities.
Through new software interface programs, you can use the Omni System as a field unit together with other integrated magne- tometer/VLF systems (such as the Scintrex IGS-2) or with other microproces sor based base station magnetometers.
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Omni System Benefits
More System Benefits
- Display descriptors monitor the status of the primary battery source used.
- Output of grid co-ordinates with the des ignated compass bearing, using N, S, E, W descriptors.
- Audio feedback to confirm every keystroke- Decimal spacing of 12.5 (metres or feet)
for intermediate station intervals- The ability to clear an unwanted last
reading- Two keystrokes to record data in memory
- the first verifies the grid co-ordinate; the second puts it into memory.
The Omni Magnetometer unit measures and stores in memory the Earth's magnet ic field at the touch of a key. This precise instrument is able to do the following:
- identify and store the location and the time of each measurement
- compute the statistical error of the reading- store the decay and strength of the sig
nal that you are measuring
Provides Data-Protected Readings
The Omni Magnetometer is packaged in a compact, lightweight and rugged hous ing and is able to measure and store the following set of information:
- total field magnitude- time of measurement- grid co-ordinates- direction of travel- statistical error of readings- signal strength and rate of decay
.Increases Productivity
The Omni Magnetometer significantly increases survey productivity as:
- it can read and store a measurement in only 3 seconds.
- data is highly repeatable so a second measurement is usually not required.
- it calculates statistical error for each measurement which indicates whether an additional reading is required.
All of these benefits permit you to cover more ground and gather more data than would be otherwise possible. OMNI MAG configuration used for measurement of total field magnetics
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The Omni System as a Portable Field IVIagnetometer
Simplifies Fleldwork
The Omni makes surveys easier to con duct because:
- the electronic notepad eliminates the need to write down field data. The Omni simultaneously stores time, field measurements, grid co-ordinates when you press any one of the three record keys.
- you are able to clear the unwanted last reading.
- the Omni automatically calculates the difference between the current reading and previous one.
- you can remove the coarse magnetic field value or data from the field data to simplify plotting of the field results.
- the Omni automatically calculates diurnal corrections.
The flexibility of the Omni System offers the following choices:
- If you use the Omni as a field magne tometer or as a gradiometer, the total field data can be corrected using the unique Tie-Line" or "Looping" method.
- if you use one Omni as a base station, it will correct the total field magnetic data in:
1 an Omni set-up as a field magnetometer
- an Omni set-up as a gradiometer
Unparalled Repeatability of Data
The Omni provides you with unparallelled data repeatability. This is a result of four leading edge design features that elimi nates the need for taking multiple read ings:
- Signal Processing Technique- Constant Energy Polarization that
maintains equal energy to the sensor- Processing sensitivity to ± 0.02 gamma- Automatic Fine Tuning which uses the
previous reading as the base for the next
Saves You Time
The error analysis feature is a great time saver as the calculation of the statistical error of each reading lets you make an on-the-spot decision whether or not you should store the reading.
The Omni System also saves you time- consuming steps as tt can:
- automatically assign a record number which you can also use to identify read ings measured off of the grid.
- take more than one reading at one point without updating the current sta tion number.
- according to the programmed station interval, automatically update your sta tion position without having to program
OMNI MAG electronics console with total field magnetic sensor
each station coordinate. The Omni magnetometer also provides a decimal digit for intermediate station intervals of 12.5 metres.
- rapidly recall readings either by record number or in sequence.
Tolerates Higher Gradients
The ability to tolerate local higher gradi ents of up to 6000 gammas per metre (field proven), is possible due to a sophis ticated signal processing method and to a miniature sensor design using a highly optimized sensor geometry.
A Variety of Power Supply Options
You can choose from the following power supply options:
- non-magnetic rechargeable sealed lead-acid battery or belt
- heavy duty rechargeable battery- alkaline battery belt- 12V DC power source
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The Omni System as a Base Station IVIagnetometer
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The Omni Base Station Magnetometer effectively measures and stores in its memory the daily fluctuations of the Earth's magnetic field. The Omni can automatically correct total field data of other Omni units in just a few minutes.
Records Magnetic Field Activity
The magnetic field activity is recorded in the following format:
- time of measurement- magnitude of total field- difference from the reference field value- difference from the previous reading- sequential record number
Automatically Corrects Data
The Omni in the base station mode can automatically correct magnetic field data for both diurnal variations and reference field values. It can also correct total field data stored in:
- another Omni System used as a field magnetometer
- another Omni System used as a field gradiometer
This fs ideal when you want to remove diurnal errors sufficiently to make use of the full 0.1 gamma resolution of the Omni System.
Automatic Drift Calculations
The Omni automatically calculates the dif ference between each reading and its programmed reference field. If at the end of the survey day you find that the refer ence field is incorrect, you can re-select a new one and the Omni System can Instantly re-calculate the drift. The drift calculation can be presented in either dig ital and/or profile plot format. It can also be simultaneously output to a compatible printer so you can visually verify the activ ity of the field.
Calculates Differential Field Variations
The Omni calculates the difference between the current reading and the previ ous one to a resolution of 0.1 gamma. This features assists you in ascertaining the
degree of activity that is occurring such as a magnetic storm or active conditions.
Stores Approximately 55 Hours Of Continuous Unattended Monitoring
The Base Station mode enables you to store up to 20,000 sets of readings which is the equivalent to approximately 55 hours of unattended monitoring at a 10 second sampling interval. You can pro gram the cycling time at any interval between 5 seconds and 60 minutes in 1 second increments.
Outputs and Stores Data At the Same Time
The Omni can simultaneously output data in digital or ASCII format to your choice of data collection units at the same time it stores the data in memory.
Synchronize Real Time Clocks
The Omni System real time clocks can be synchronized to the nearest second.
Magnetic Base Station Accessories Kit
Sensor Extension Cable - This 30 metre cable enables you to place the Omni in a sheltered environment such as a tent, and position the magnetic sensor up to 30 meters away. This capability aids in elimi nating possible cultural interference.
Rope Joiner - The rope joiner enables the sensor staff to be supported by ropes when it is being used as a base station sensor.
•-••SftMagnetic diurnal corrections are automatically made by using an OMNI MAG as a base station magnetometer
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Omni System as a True Gradiometer
The Omni System provides you with an accurate means of measuring both the total field and the gradient of the total field. It reads and stores the measure ments of both sensors simultaneously to calculate the true gradient measurement.
Displays and Stores Fully Protected Data
The Omni System provides the following Information on screen and in memory:
- the gradient of the total magnetic field- the total magnetic field magnitude of the
upper sensor- the time of measurement- the grid co-ordinates where the
measurement is taken- the statistical error of total field reading of lower gradient sensor
- the signal strength and decay rate mea surement of lower gradient sensor
No Lost Survey Time
The Omni enables you to conduct gradi ent surveys during magnetic storms resulting in no lost survey time. This is another benefit of the simultaneous mea surement of both sensors.
Cancels the Effects ot Diurnal Magnetic Variations
The technique of simultaneously measur ing the two sensors cancels the effects of diurnal magnetic variations. The total field measurement of the top sensor can be self-corrected by the Omni when you use the Tie-Line" feature or with another Omni System in the base station mode.
Increases Resolution of Total Field Anomalies
The Omni in the gradient mode more sharply defines the magnetic responses determined by total field data. It individu ally delineates closely spaced anomalies rather than collectively identifying them under one broad magnetic response.
Directly Delineates Vertical Contacts
The Omni is an ideal contact mapping tool especially in vertical to near-vertical contact or fault zones. These vertical
Simultaneous vertical magnetic gradient mea surements using the OMNI GRAD configura tion
contacts are expressed at the zero line of gradient contour or profile values. Vertical dyke-like bodies can also be mapped effectively.
Provides On-The-Spot Approximate Depth of Anomalies
Shallow, near-surface sources (higher fre quency anomalies) are emphasized rela tive to deeper responses (lower frequency anomalies). This can provide an on-the- spot approximation of the depth of the anomalous source.
Automatically Removes Regional Gradient
The gradient measurements ability to dif ferentiate between higher and lower fre quency responses effectively removes background regional gradients from anomalous residual responses.
Offers a Unique Alternative in the Interpretation of Magnetic Field Data
The Omni enhances data by simultane ously recording in memory both the gradi ent and total field measurements as well as the statistical error. Both types of data offer a unique alternative in interpreting the magnetic field data such as gradient vector diagrams, dip and strike length of body, etc.
Gradient-Base Station Operation
The Gradient Mode of the Omni System can cycle automatically every 5 seconds. This option can be used in stationary or mobile applications.
Emphasizes or Diminishes Near Surface Effects
The gradient sensor of the Omni is mounted onto a sectional aluminum staff in which you can add or subtract sections to achieve the desired height of sensors from the ground. This enables you to adapt the Omni to local ground noise con ditions, terrain effects and survey logis tics. In doing so, you can selectively emphasize or diminish near surface effects depending upon the survey target.
Choice of Sensor Separation
The choice of sensor separation provides unique interpretative information especial ly useful in near surface anomalous con ditions such as determining if the field has curvature or if it is linear. You can choose the following sensor lengths and configu rations:
- standard 0.5 metre sensor separation mounted on staff
- optional one metre sensor separation mounted on staff
The Omni System as a Portable VLF Unit
The Omni VLF unit allows you to do all of your surveying completely hands free and provides you with the ability to measure and record in a fully protected memory for each field reading the following informa tion:
- vertical in-phase- vertical quadrature (out-of-phase)- total field strength- dip angle- primary field direction- apparent resistivity- phase angle-time- grid co-ordinates- direction of travel along grid lines- natural and cultural features
The field data is compensated for 180 degree difference in direction of travel up and down survey lines.
Requires No Orientation
The Omni does not require you to orient the VLF sensor head toward the VLF transmitter station. This simplifies field procedures as well as saves you consid erable survey time. When you measure three VLF transmitters, the benefits of this time-saving feature automatically triple. You do not have to orient yourself and the sensor head toward the first selected transmitting station and then re-orient towards the second or third transmitting station.
The ability to obtain data from as many as three VLF transmitting stations provides complete coverage of an anomaly regard less of the orientation of the survey grid or of the anomaly itself.
Saves You Time
The Omni can measure up to three VLF frequencies (transmitter stations) simulta neously, in as little as 8 seconds, or one VLF frequency in only 3 seconds, depending on the transmitter strength.
The Omni automatically tunes to the pre programmed frequency(s) for each read ing. Display descriptors indicating signal- to-noise ratio provide you with an immedi ate indication of how usable a frequency
The unique 3 coil design of the OMNI VLF allows reading of up to 3 separate frequencies with out having to orient to each of the transmitting VLF stations
is. Using up to three frequencies opti mizes conductor coupling, even in the most complex geologic environments.
Receives Very Weak or Too Strong Signals
Being able to select a transmitter station(s) best suited for the survey target and orientation is not always possible with conventional VLF systems. The ideal sta- tion(s) may be too weak or overwhelmed
by the signal strength of a transmitter that is close in frequency proximity. Through digital signal processing, the Omni can receive signals as low as 20 nA/m from very weak stations, by remov ing the modulation in the received signal. Analog filtering of the Omni System offers an unparalleled 80 dB for a 600 Hz chan nel separation. In other words, the Omni can isolate and measure a 1000 times weaker signal from a distant station in lieu
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The Omni System as a Portable VLF Unit
of the closer and subsequently more stronger station that is only 600 Hz apart in frequency.
Reduced Atmospheric Noise
Atmospherics such as thunderstorm activ ity, as well as the resultant interaction between the sun's rays and the iono sphere can drastically alter the wave guide in which the VLF wave travels from the transmitter station.
Through signal enhancement, the Omni is able to suppress the effects of these atmospheric and ionospheric phenomena, which are more predominant in the sum mer months, in order to pick up the weak est of transmitter stations. For example, Omni Systems used in Southern Africa have demonstrated the unparalleled abili ty to pick up 7 transmitter stations.
Provides More Complete, 3-Dimenslonal Description of Survey Area
The Omni can measure the total tilt or dip of the polarization ellipse from the vertical axis. Unlike conventional systems, where only the tilt of the major axis of the polar ization ellipse is measured, the Omni is most sensitive to the horizontal compo nents perpendicular to the primary field which can detect anomalies off to the side. This provides a more complete, three dimensional description of the sur vey area that can lead to the detection of anomalies between grid lines. The Omni's tilt transducers compensate for both tilt and roll position of the VLF sensors.
Scan For The Most Usable Station
The Omni enables you to automatically scan the entire VLF spectrum for the most usable stations between 15.0 kHz to 30.0 kHz in Increments of 100 Hz. This is most desirable if you do not know first hand what stations are readable or what stations are available from your location. Unpublished or unknown stations now become accessible. You can then deter mine if a known station has changed fre quency simply by the direction of trans mission.
50 -i
O)
30H
fc 20H0)
5cd•S 10H
-XV. .A15.0 20.0 25.0
Frequency (kHz)VLF frequency Spectrum - Toronto, Canada
30.0
By completing a VLF Spectrum the operator can determine which VLF stations are useable in the survey areaAutomatically Calculates the Fraser Filter
The Omni automatically calculates the Fraser Filter from the dip angle data, regardless of the interval between the stations along the grid lines. You no longer have to manually perform this mathematical calculation thereby reduc ing the possibility of human error. The Fraser Filter algorithm follows established conventions.
The Fraser filtered data is output using both the 4 point and 5 point filter method.
The latter method allows filtered data to be plotted easier, such as at the station interval instead of in-between stations.
Calculation of Ellipticity
As an option, the Omni can calculate the true ellipticity of the VLF magnetic field from the measurement of the in-phase and quadrature of all three components. The ellipticity provides more interpretive information about the anomaly than the dip angle and is less influenced by over burden shielding.
OMNI VLF electronics console with the VLF backpack assembly utilizing the unique 3 coil VLF sensor
ITCe Omni System as a VLF Base Station
The Omni VLF Base Station monitors and records in protected memory, variations in the primary field strengths that can origi nate from the VLF transmitter itself or from atmospheric/ionospheric changes.
You Only Need One Omni System VLF Base Station for 3 Simultaneous Measurements
Like the Omni VLF Field unit, you only need one Omni VLF Base Station to simultaneously monitor up to 3 VLF transmitter stations, regardless of their field direction.
Conventional, "oriented" systems may require as many as 3 separate base stations for the same cover age offered by one Omni VLF Base Station.
In addition, the Omni Mag/VLF Base Station also monitors the Earth's mag netic field for diurnal varia tions, eliminating the need for a separate base station magnetometer.
The simultaneous measuring capability reduces the length of time the Omni System needs to be turned on. This, in turn, reduces the power consumption needed by the Omni System and lengthens the battery life. By being able to take three measure ments in approximately the same amount of time as conventional sequential sys tems take one measurement, you can shorten the programmable sampling inter val to attain better monitoring coverage of the field strengths from each of the VLF transmitters.
Both VLF and Magnetometer Base Stations in One Instrument
The Omni System eliminates the need to have two separate instruments to monitor the primary field strength of selected VLF transmitter(s) and the variations in magni tude of the Earth's magnetic field — one Omni Base Station does both. By com
bining both of these capabilities into one unit, it significantly reduces the cost of the survey. The Omni measures and stores these variations in protected memory.
Automatically Corrects VLF and Magnetic Field Data
The Omni base station can automatically correct the Omni System field units for the measured field strength variations from the VLF transmitter(s) and the Earth's magnetic field. Through linear interpola-
station. The field unit then displays and decrements the remaining time, in sec onds, until the base station is scheduled to take a measurement. You can obtain a field reading at exactly the same time as the base station. The simultaneous field and base station measurements sig nificantly improves the accuracy of the automatic correction.
Synchronize the Real Time Clocks
Real time clocks among any number of Omni units can be synchro nized to the second unit when using the Omni Base Station with another Omni portable field unit.
Monitor Rapid Variations of Primary Field
You can program your Omni base station to cycle at any interval, in one second incre ments, from 5 seconds to 60 minutes, to montior rapid vari ations of the primary field. The minimum cycling time for VLF Base Station use depends on the VLF Transmitter strength that the Omni receives.
Compatibility with Airborne Systems
Diurnal corrections for fluxuations of the VLF primary field are possible by using an OMNI VLF as a VLF base station
The Omni is compatible with airborne VLF systems which also use 3 component sensors.
tion, these corrections are applied at the time of data transfer. Unlike other inte grated systems, the Omni does not alter the original field data during the correction process. The Omni base station correc tion and Tie-Line" correction capabilities are applied at the time of each data trans fer, therefore securing the integrity of the data collected during the survey.
Obtain a Reading at the same lime as the Base Station
The Omni has a unique countdown fea ture which can be activated in the field unit upon synchronization with the base
VLF Base Station Accessories Kit
VLF Sensor Extension Cable - This is a 10 metre cable which allows you to put the Omni console in a sheltered environ ment while placing the VLF sensor up to 10 meters away.
Rope Joiner - The rope joiner enables the sensor staff to be supported by ropes when it is being used as a base station sensor.
Mounting Bracket - This bracket is for mounting the VLF sensor to the staff.
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The Omni System as a Portable VLF Resistivity System
The Omni VLF Resistivity unit can calcu late and record the apparent resistivity and phase angle from the measurement of the VLF electric and magnetic fields.
Non-Orientation Resistivity Option
In addition to the standard resistivity option that uses 2 electrodes, the Omni also offers a non-orientation VLF resistivi ty option which includes a third electrode. This third electrode, with the standard resistivity unit, eliminates the need for you to orient toward the selected transmitter station(s).
This significantly improves survey produc tion and reduces the time consuming Jogistics often associated with resistivity surveys.
Calculates the Vector Resistivity
The optional third electode in the Omni VLF Resistivity unit offers not only a non- orientation capability of the VLF electric field, but also measures the elements of tensor impedance necessary for the Omni to compute the two components of the apparent resistivity, or the vector resistivity.
This provides you with additional interpre tive information of the survey target.
Select Your Own Type of Electrode
Survey conditions largely dictate the type of electrode you should use. The stan dard Omni resistivity electrode includes both capacitive plates and resistive probes so you can select the type of elec trode that offers the best coupling capabil ity for the survey conditions.
The unique threaded design permits you to easily exchange the choice of elec trode In the field.
Flexible Probe Spacing
The Omni resistivity options offer a stan dard 10m cable assembly. However, you can program the console for a 5 or 10 metre separation.
The acquisition of VLF resistivity data using the 2 probe or the unique 3 Probe VLF resistivity option allows the operator to collect valuable additional information from the VLF method
Possible Configurations of the Omni Geophysical System
Mag
System Control Console *
Total Field and Base Station Mag Option *
Magnetic Gradiometer Option
Magnetic Total Field Sensor ; * ; :1
0.5m Magnetic Gradient Sensor : l i: i
1 .Om Magnetic Gradient Sensor ^ ; : i !f i
128K RAM extended Memory Option 0 :
VLF Electromagnetic Sensor Option -. ; . ;.- '-^'Wf ••••''v
2 Probe VLF Resistivity Option ; ; :
"Non-Orientation" VLF Resistivity Option : : : : ^
Non-Rechargeable Battery Belt : ? i
Rechargeable Battery Belt f B i i
Standard Rechargeable Battery Cartridge ;: B |
Heavy Duty Rechargeable Batt. Cartridge : :; B i ::; ;i
Battery Charger ylf ;C?v::Mi.lf J-i
RS-232CKit ^Ip^S
Mag Base Station Accessories Option 0
VLF Base Station Accessories Option
Transit Case (#1) 0
Transit Case (#2) ] - 'V* ^jti^jff^
Transit Case (#3) 0
Magnetics Spare Parts Kit 0
VLF Spare Parts Kit
Magnetics/VLF Spare Parts Kit
Data Transfer Program 0
Grad**
*
0
A
A
0
N/A
B
B
B
C
0
0
0
0
0
0
0
VLF Mag/VLF Grad/VLF
. - ' - * • '••" * -,, ';: .' *
•' ' : '- ::: ' : --::'- '.' : -:,-:. : *
(included in VLF configurations)
: : ; ;-*.' .'•••. '.'.' *
: . : Q - :. '-: ''. 0
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' . ^.^••'•••^ B - -B '--'-. '" - : ... ' D '
- 1 : ':. '- - ' D
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::' ^; :?p?|(*V :-|f;f 'f ^ - :
: ':- -: :^:A:: : '6' ;i ':S"--': 0 :"'
:.;,..-j,'-'. : : v: :: : 0
;e.-^p;-v^- o•••- v : -:i'.:;0,,:::..i' 0
f : -^| ?ijMi^r- N/A - : ' .Q 0
0
0
•: ;^ --.o.'-" 1 --: o
• ;:* -
*
•*
0
A
A
*
0
0
N/A
B
B
B
C
0
0
0
0
N/A
0
0
0
Required in the configuration A Selection of one o/the A options required to complete configuration
B Selection of one of the B options required to complete configuration
C If a rechargeable battery option is required then the charger must also be included in the configuration
O Optional for configuration, see a sales representative for more details
N/A Not available for this configuration
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Specifications
OMNI System Specifications
Operating Environment -400 to +55C; D-100% relative humidity; weatherproof
Power Supply Non-magnetic recharge able sealed lead-acid battery or belt; alka line battery belt; or 12V DC power source option for base station operation.
Battery Life 1.700 to 5,000 readings, for sealed lead acid power supply, depending upon ambient temperature and rate of readings.
Weights and Dimensions
Instrument Console 3.8kg, 122 x 246 x 210 mm
VLF Sensor Head0.9 kg, 140 dia. x 130 mm
VLF Electronics Module1.7 kg, 280 x 190 x 75 mm
Standard Rechargeable Battery 1.8kg, 138 x 95 x 75 mm
Standard Rechargeable Battery Belt1.8 kg, 540 x 100 x 40 mm
Heavy Duty Rechargeable Battery 2.0kg, 138 x 115 x 75 mm
Alkaline Battery Belt1.2 kg, 540 x 100 x 40 mm
Magnetometer Sensor 1.2 kg, 56mm dia. x 200mm
Gradient Sensor(0.5m separation - standard)2.1 kg, 56mm dia. x 790mm
Gradient Sensor(1.0m separation - optional)2.2 kg, 56mm dia. x 1300mm
DisplayCustom designed, rugged liquid crystal display with an operating temperature range from -40C to +55C. The display contains six numeric digits, decimal point, battery status monitor, signal decay rate and signal amplitude monitor and function descriptors.
Magnetometer Component Specifications
Dynamic Range 18,000 to 110,000 gam mas. Roll-over display feature suppresses first significant digit upon exceeding 100,000 gammas.
Tuning Method Tuning value is calculat ed accurately using a specially developed tuning algorithm.
Automatic Fine Tuning ±150Xo relative to ambient field strength of last stored value
Display Resolution 0.1 gamma
Statistical Error Resolution0.01 gamma
Absolute Accuracy ± 1 gamma at 50,000 gammas at 23C* ±2 gamma over total temperature range
Memory Capacity
Standard Memory Capacity 1 300 data blocks (48K) or 5200 data blocks (128K)
Total Field or Gradient 1 00 data blocks
Base Station 4000 data blocks (48K) or 16,000 data blocks (128K)
RS-232C Serial I/O Interface Variable baud rate from 300 to 9600 baud, 8 data bits, 2 stop bits, no parity
Gradient Tolerance 6,000 gammas per metre (field proven)
Test Mode A. Diagnostic testing (data and programmable memory) B. Self Test (hardware)
Sensor Optimized miniature design. Magnetic cleanliness is consistent with the specified absolute accuracy.
Gradient Sensors 0.5 metre sensor sep aration (standard) normalized to gam mas/metre. Optional 1.0 metre sensor separation available.
Sensor Cable Remains flexible in tem perature range specified including strain relief connector
Cycling Time (Base Station) Programmable from 5 seconds up to 60 minutes in 1 second increments.
VLF Component Specifications
Frequency Tuning Range 15 to 30 kHzin 100 Hz increments with bandwidth of 150 Hz; tuning range accommodates new Puerto Rico station at 28.5 kHz.
Transmitting Stations Up to 3 stations can be automatically measured at any given grid location within frequency tuning range.
Recorded VLF Magnetic Parameters Vertical In-phase, vertical quadrature (out- of-phase), total field strength (or optional horizontal amplitude), dip angle
Channel Separation 80 dB at 600 Hz frequency separation
Standard Memory Capacity 1300 com bined VLF magnetic and VLF electric measurements as well as gradiometer and magnetometer readings
SCIIMTP^X
222 Snidercroft RoadConcord.Ontario.CanadaL4K1B5
Telephone: (416)669-2280 Telex: 06-964570 Telefax: (416)669-6403
(416)669-5132
42C18NW8988 2.1524B ODLUM
ntario 300
Ministry of Ministere du Geoscience Approvals OfficeNorthern Development Developpement du Nord "J Ramsey Lake Road
. ... K A j 11- 6th Floorand Mines et des Mines sudbury, OntarioP3E 6B5
Telephone: Fax:
(705) 670-5853 (705) 670-5863
March 22, 1994
Mining RecorderMinistry of Northern Development our File: 2.15240and Mines Transaction #: W.9350.0005260 Church StreetSault Ste. Marie, OntarioP6A 3H3
Dear Sir/Madam:
SUBJECT: APPROVAL OF ASSESSMENT WORK CREDITS ON MINING CLAIMS1078220 ET AL IN STRICKLAND, ODLUM AND TEDDER TOWNSHIPS.
The assessment work credits for Assays filed under Section 17 of the Mining Act Regulations have been approved as amended in the original submission.
The approval date is February 2, 1994.
If you have any questions regarding this correspondence, please contact Lucille Jerome at (705) 670-5855.
Yours sincerely,
Ron C. GashinskiSenior Manager, Mining Lands Section Mining and Land Management Branch Mines and Minerals Division
O LJ/jlEnclosures:
cc: Resident GeologistSault Ste. Marie, Ontario
Assessment Files Library Toronto, Ontario
Northern Development and Mines
Ontario
nepuu 01 wont wonauctea After Recording Claim
Mining Act
transaction Number -,- v...i l .. s v -. ...\: i ,\0.
sonal l^^atlon coflecled on this form Is obtained under the authority ol the Mining Act. This Information will be used for correspondence. Questions about coflecnw s
PersonaH^^this coOectW should be directed to the Provincial Manager, Mining Lands, Ministry ol Northern Development and Mines, Fourth Floor, 159 Cedar StreetSudbury, Ontario, P3E 6A6, telephone (705) 670-7264.
Instructions: - Please type or print and submit in duplicate.- Refer to the Mining Act and Regulations for requirements of filing assessment work or consult the Mining
Recorder.- A separate copy of this form must be completed for each Work Group.- Technical reports and maps must accompany this form in duplicate.- A sketch, showing the claims the work Is assigned to, must accompany this form.
Recorded HoMerfs) John E. Ternowsky /Peter Nabigon c/o Akiko Gold Resources Ltd.Address709 - 700 Vest Fender Street. Vancouver, B.C. V6C 1G8
Mining Division Sault Ste. MarieOates Perform* fn™ July 15, 1993
Township/AreaStrickland. Odlum, Tedder, Coopei
Client No. lfi MO bit n^3(UiipSSSlio. - ' J~ *J 604-689-0988
M or Q Plan No.
To: September 30, 1993Work Performed One Work Group Only)
x
Work Group
Geotechnical Survey
Physical Work, Including Drilling
Rehabilitation
Other AuthorizedWork
Assays
Assignment from Reserve
Humus and rock
' L'H^\/'*' '
RFCIrVv^Q
DEC 0 2 1993
MINING LANiia r)HANCH
samples (Au. Cu. Zn
lype
. Mo)
. RECORDED. ^
NOV 1 7 1993
R^Alpf
lTotal Assessment Work Claimed on the Attached Statement of Costs f 27.988.^gTNote: The Minister may reject for assessment work credit all or part of the assessment work submitted If the recorded
holder cannot verify expenditures claimed In the statement of costs within 30 days of a request for verification.
Persons and Survey Company Who Performed the Work (Give Name and Address of Author of Report)Name
A. C. A. Howe International Ltd.
t
Address
22 Front Street West, Suite 1400, Toronto, Ontario M5J 1CA
(attach a schedule If necessary)
Certification of Beneficial Interest * See Note No. 1 on reverse sidel certHy that at the time the work was performed, the claims covered In this work report were recorded In the current holder's name or held under a benefldal Interest by Ilw current recorded holder. ___ ^^^^^^^^
Date
Nov. 15, 199:
Holder or Agent (Signature)
Certification of Work Reportl certify that t have a personal knowledge ol the (acts set lorth In this Work report, having performed the work or witnessed same during and/or after Ra eomplellon and annexed report Is true.
of Penon C*rUrytng Leroux, 326 Major MacKenzie Dr. East, 1122, Richmond Hill, Ontario L4C8T4
Jto.
905-770-0293
Date
Nov. 15. 1993
For Office Use OnlyTotal Value Cr. Recorded
1 01 9
Dale Recorded
A/GO niDeemed
OP nApproval Dale
Dale Notice lor Amendments Sent r
ONISON RECEIVED
2 9 NOV 1993 rM
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ou w
ish lo
prio
rite
the
delet
ion
ol cr
edits
. Plea
se m
ark
(s)
one
of th
e fo
llowi
ng:
1. K)
Cre
dits
are
lo b
e cu
t bac
k st
arlin
g wi
th th
e cla
im li
sted
last,
work
ing b
ackw
ards
.2.
O C
redi
ts a
re lo
be
cut b
ack
equa
lly o
ver a
lt cla
ims
cont
ained
in th
is re
port
ol w
ork.
3. D
Cre
dits
are
lo be
cut
bac
k as
prio
rlzed
on
the
atta
ched
app
endix
.
In th
e ev
ent t
hat y
ou h
ave
not s
pecif
ied y
our c
hoice
of p
riorit
y, op
tion
one
will
be Im
plem
ente
d.
Note
1:
Exam
ples
ol b
enef
icia
l Int
eres
t are
unr
ecor
ded
trans
fers
, opt
ion
agre
emen
ts, m
emor
andu
m o
l agr
eem
ents
, etc
., wi
th re
spec
t to
the
min
ing
clai
ms.
Mot
t 2:
If wo
rk h
is b
een
perfo
rmed
on
pate
nted
or l
ease
d la
nd, p
lease
com
plet
e th
e fo
llowi
ng:
l cer
tify
thai
Ih*
reco
rded
hol
der
had
a be
nefic
ial I
nter
est
In (h
e pa
tent
ed
or le
esed
land
al t
he (t
one
the
work
was
per
form
ed.
Sign
atur
eDa
le
V
l o\
OB 50 v^
X*
50. Jo X
CK4
Ob
CD
O-C
i
l
VC
K
\
irte
S? *te
tefe
c*S* o^
fete
Vmhtt
ssess Work
D
ri
, this
PX
te?ON
Oo
*fe
C*
ON o*S*
fill i
UN
) rc; c
Cred
its y
ou a
re c
laim
ing
In th
is re
port
may
be
cut b
ack.
In or
der l
o m
inim
ize (h
e ad
vers
e ef
tocls
ol s
uch
delet
ions
, plea
se In
dica
te fr
om
which
clai
ms
you
wish
lo p
rlorlz
e th
e de
letio
n ol
cre
dits
. Ple
ase
mar
k (^
) one
ol t
he fo
llowi
ng:
1. (JJ
Cre
dits
are
to b
e cu
t bac
k st
artin
g wi
th th
e cla
im li
sted
last
, wor
king
back
ward
s.2.
O
Cre
dits
are
to b
e cu
t bac
k eq
ually
ove
r all
claim
s co
ntai
ned
in th
is re
port
of w
ork.
3.
O C
redi
ts a
re lo
be
cut b
ack
as p
riorlz
ed o
n th
e at
tach
ed a
ppen
dix.
In th
e ev
ent t
hat y
ou h
ave
not s
pecif
ied y
our c
hoice
ol p
riorit
y, op
tion
one
will
be Im
plem
ente
d.
Note
1:
Exam
ples
of b
enef
icia
l Int
eres
t are
unr
ecor
ded
trans
fers
, opt
ion
agre
emen
ts, m
emor
andu
m o
f agr
eem
ents
, etc
., w
ith re
spec
t to
the
min
ing
clai
ms.
Note
2:
If wo
rk h
aa b
een
perfo
rmed
on
pate
nted
or l
ease
d la
nd, p
leas
e co
mpl
ete
the
follo
wing
:
l cer
tify
thai
the
reco
rded
hol
der h
ad a
ben
efici
al In
tere
st In
the
pate
nted
or
leas
ed la
nd e
i Hie
time
the
work
was
per
form
ed.
Sign
atur
eDa
le
.
Ox
Ox
Ox :x
oxO
xO
x
x^
-O
vK
-O
o-- a
l rfete
C*
b*i
kSt?
seC
*
s
U)
u* 1
Cred
its y
ou a
re c
laim
ing
In th
is re
port
may
be
cut b
ack.
In o
rder
lo m
inim
ize (h
e ad
vers
e ef
fect
s ol
suc
h de
letio
ns, p
leas
e in
dica
te fr
om
which
cla
ims
you
wis
h lo
prlo
rlze
the
dele
tion
of c
redi
ts.
Plea
se m
ark
(f)
one
of th
e fo
llowi
ng:
1. (S
) Cr
edits
are
to b
e cu
t bac
k st
arlin
g wi
th th
e cla
im li
sted
last
, wor
king
back
ward
s.2.
D
Cre
dits
are
lo b
e cu
t bac
k eq
ually
ove
r all
claim
s co
ntai
ned
In th
is re
port
of w
ork.
3.
O C
redi
ts a
re to
be
cut b
ack
as p
rioriz
ed o
n th
e at
tach
ed a
ppen
dix.
In th
e ev
ent t
hat y
ou h
ave
not s
pecif
ied
your
cho
ice o
f prio
rity,
opt
ion
one
will
be Im
plem
ente
d.
Note
1:
Exam
ples
of b
enef
icia
l Int
eres
t are
unr
ecor
ded
trans
fers
, opt
ion
agre
emen
ts, m
emor
andu
m o
f agr
eem
ents
, etc
., w
ith re
spec
t to
the
min
ing
clai
ms.
Note
2:
If w
ork
has
been
per
form
ed o
n pa
tent
ed o
r le
ased
land
, pl
ease
com
plet
e th
e fo
llow
ing:
l cer
tify
lhal
In*
reco
rded
hol
der h
ad a
ben
efici
al In
tere
st In
(he
pate
nted
or
leas
ed la
nd a
t the
tim
e th
e wo
rk w
as p
erfo
rmed
.Si
gnat
ure
Dal
e
u
StI s
o 30s
-Ci
O
U
00
VXA
"Vt
CN
1^
r y f lGo
:to
*
tel
tefe
sti!
bo VQ
00X
s:-•c;
s:u
Ofi
S?
Cred
its y
ou a
re c
laim
ing
In th
is re
port
may
be
cut b
ack.
In o
rder
to m
inim
ise th
e ad
vers
e ef
fect
s of
suc
h de
letio
ns, p
leas
e In
dica
te fr
om
which
cla
ims
you
wish
lo p
rlorlz
e th
e de
letio
n of
cre
dits
. Pl
ease
mar
k (*
-) on
e of
(he
follo
wing
:
1. JS
Cre
dits
are
to b
e cu
t bac
k st
artin
g wi
th th
e cla
im li
sted
last,
wor
king
back
ward
s.2.
D
Cre
dits
are
to b
e cu
t bac
k eq
ually
ove
r all
claim
s co
ntai
ned
In th
is re
port
of w
ork.
3.
O C
redi
ts a
re to
be
cut b
ack
as p
rioriz
ed o
n th
e at
tach
ed a
ppen
dix.
In th
e ev
ent t
hat y
ou h
ave
not s
pecif
ied
your
cho
ice o
f prio
rity,
opt
ion
one
will
be Im
plem
ente
d.
Note
1:
Exam
ples
of b
enef
icia
l Int
eres
t are
unr
ecor
ded
trans
fers
, opt
ion
agre
emen
ts, m
emor
andu
m o
f agr
eem
ents
, etc
., w
ith re
spec
t to
the
min
ing
clai
ms.
Not
t 2:
II
wor
k ha
t be
en p
erfo
rmed
on
pate
nted
or
leas
ed la
nd, p
leat
e co
mpl
ete
the
follo
win
g:
l cer
tify th
at Ih
s re
cord
ed h
older
had
a b
enef
icial
Inter
est I
n the
psle
nlsd
or le
ased
land
at t
he ti
me
the
work
was
per
forme
d.Sl
gniitu
rtDa
l*
ffl If
e*. s
S il
Cred
its y
ou a
re c
laim
ing
In th
is re
port
may
be
cut b
ack.
In or
der l
o m
inim
ize (h
e ad
vers
e ef
fect
s ol
suc
h de
letio
ns, p
lease
Indi
cate
Irom
wh
ich c
laim
s yo
u wi
sh lo
prio
rite
the
dele
tion
of c
redi
ts. P
lease
mar
k (x
) on
e ol
the
follo
wing
:1.
CJ C
redi
ts a
re to
be
cut b
ack
star
ting
with
the
claim
liste
d las
t, wo
rkin
g ba
ckwa
rds.
2.
O C
redi
ts a
re lo
be
cut b
ack
equa
lly o
ver a
ll cla
ims
cont
ained
In th
is re
port
ol w
ork,
3. O
Cre
dits
are
lo b
e cu
t bac
k as
prio
rlzed
on
the
atta
ched
app
endi
x.
In th
e ev
ent t
hat y
ou h
ave
not s
pecif
ied y
our c
hoic
e ol
prio
rity,
optio
n on
e wi
ll be
impl
emen
ted.
Note
1:
Exam
ples
of b
enef
icial
Inte
rest
are u
nrec
orde
d tra
nsfer
s, op
tion
agre
emen
ts, m
emor
andu
m o
l agr
eem
ents
, etc
., wi
th re
spec
t to
the
minin
g cla
ims.
Note
2:
If wo
rk h
as b
een
perfo
rmed
on
pate
nted
or l
ease
d lan
d, p
lease
com
plet
e th
e fo
llowi
ng:
l cert
ify th
ai th
e re
cord
ed h
older
had
a b
enefi
cial I
nteres
t In
the p
atente
d or
leas
ed la
nd a
t the
lim
e th
e wo
rk wa
s pe
rform
ed.
Sign
ature
Dale
Ontario
Northern Development and Mlnet
Mlnlslftfo du Dtvetoppement du Nord at des mines
oicuumern 01 costs for Assessment Credit
Etat des coQts aux fins du credit devaluation
Mining Act/Lol sur les mines
WS350 . 00052
Personal Inlormatlon collected on Ihls lorm Is obtained under the mrlboflly Of the Mining Act. This Inlormatlon wilt be used lo maintain a record and ongoing slelus ol the mining elalm(s). Questions aboul Ihls collection should be directed lo the Provincial Manager, Minings Lands, Ministry ol Northern Development and Mines, 4lh Floor, t SB Cedar Street, Sudbury, Ontario P3E 6AS. telephone (705) 070-7264.
Les ronsolgnomonls personnels conlenus dans In prosonle formula son recuelllls en vsrtu de le Lol sur Iss mlnss el servlronl e tsnlr A lour un rtoiiirc des concessions mlnleree. Adresssr (oule qussMon sur la.eolleee de eo- fonsolgnomenls au chel provincial des terrains mlnlers, mlnJstoro di Dovoloppemonl du Nord el des Mines. 159, rue Cedar, 4* itage. Sudbur, (Onlerto) P3E 6A5. Itlephone (70S) 670-7264.
1. Direct Costs/CoOls directs
Type
Wage*Selalres
Contractor's and Consullsnl's FeesDrolls de I'antreprsneur at da I'expert- consell
Supplies Used Fournllures utnialaa
Equipment Rantal Location da materiel
Description
Labour Maln-d'oeuvreField Supervision Supervision sur la terrain
Type Research and
feport Writing
Type
Analytical Assays
Lone Cutting
Helicopter
Type
Amount Montan!
113,332,00
9,400.00
9,095.00
24,176.75 '
17,432.97^
3.852.77
Tola) Dlract Coata Total des coOta directs
Totals Total global
••f ' t .., 57,732;6C
W
^m
t#:-#afr
iIMi
2. Indirect Costs/CoOls Indlrecls*' Note: When claiming Rehabilitation work Indirect costs are not
allowable as assessment work.Pour le remboursemont des Iravaux do rehnbllllallon, los coOls Indlrecls ne sonl pas admlsslbles en lanl que Iravaux devaluation.
Type
Transporlatlon Transport
Food and Lodging Nourrllurt el hlbergsmenlMobllliatlon end Demobltliallon Mobtllsstlon el demobilisation
Description
Typ. Airfare-Vehicle
Field Supplies, Food, AoccnnodatAonsRentals, csnp, •"fsppT lonpous
Amount Monlanl
5,133.32
1&22JQL
6,027.30
Sub Total of Indirect Costs Total partial des coOls Indlrects
Amount Allowable (not gristsr than 20U of Direct Costs) Montan! admissible (n'sxcldsnl pas 20 H des eoOls directsTotal Value ol Assessment CredH Vsltur lot lit du crldll (Teisl el Olrtcl tmJ ANewable d'tvalustlon Indirect costs) fTolil ett noil Silttil
Totals Tolol globnl
- I'M,', -li.'- 5.138.32
•i-*. ' '• -- • •'•'. -. i
loilLQLip-t i"i*(. v* * ;* * ;t'Hvf-'.:-ityfVjRfiT^;! ::'v-73 Att GO
fctt Mlrtctl trfmliilMll
Note: The recorded holder will be required lo verily expenditures claimed In Ihls statement of costs within 30 days ol a request lor verification. II verification Is not made, the Minister may reject lor assessment work at) or part ol the assessment work submitted.
Note : Le tilulalra enregislre sera lenu de v6rlfler (os doponsos demandoos dans lo present eta l des coOls dans les 30 fours sutvanl uno demando a col ellel. SI la verification n'est pas efleclue'e, le mlnlstre pout re|oler tout ou une perite des travaux devaluation presents.
Filing Discounts
1. Work Illed within two years of completion Is claimed el 100W ol the above Total Value of Assessment Credit.
Remises pour dep6l
1. Les Iravaux deposes dans les deux ans sulvanl leur achavemonl sont rembourtes a 100 tt de la valeur lolale susmenltonneo du credH devaluation.
2. Work filed three, lour or live years alter completion Is claimed at SOW of the above Total Value of Assessment Credit. See calculations below:
Total Value ol Assessment CredH x 0.50 -
Total Assessment Claimed
2. Les Iravaux deposAs trots, quatre ou cinq ana apras leur achevemeni sonl rembourses i SO H de la valour lolale du credit devaluation susmentlonne. Vdr les calculs cl-dessous.
Valeur lotsle du credit devaluationx 0,50
Evaluation totals domandAe
Certification Verifying Statement of Costs
F hereby certify:that the amounts shown are as accurate as possible and these costs were Incurred while conducting assessment work on (he lands shown on the accompanying Report ol Work form.
that as ir. Agent, Position In Company)
lo make Ihls certification
Attestation da I'etat des coOls
J'alloslo par la prdsonlo :que les montants Indlques sont le plus exact possible el que ces depenses onl ate engagees pot/r effectuer lea Iravaux devaluation •ur les terrains Indlques dans la lormulede rapport de travail cl-|olnl.
l em authorized Et oxTa litre de . ____________ . (IHulalrs enregltlri, reprisenlant, posit occup* dans la compagnlt)
elleVleslalion.
]e suls autorisd
isMIS (04ftl) Nola : Dans cslle form dlslgne des personnes, le masculln est utllli* au st,ns nsulre.
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•2a deadfall 4 bush
7X 2313(2). 3b4c "
'tt'!'' *-*.Jj*-* .1 i, i '.* f '
60 y," ;
.-.- -4o deadfall tt bushL l 4-t-t l-1 *-4—U-t. 4-t-^
5a?,4a,4b
10782382a,5a dyke',"/ ^
'.2359-64.66-68^ -
Strickland Lake
1194198(4)o2a,2b/
W7a?j5 . 1o.1 b r- sheared
:. : : 4c boulds
Strickland Lake
xenos in 4a bould- r~\ / n
^ '7 2321(5) \Alder
•' boulds A o/c/ , /lb xenos-, \ - ":
7 c- ;-il :^
4a75a 1a,1b.5a-- -
L 14+OOS
Road 206
— L 16+QOS
L 18+005
— L 20+OOS
— L 22+OOS
— L 24+OOS
— L 26-VOOS
— L 28-t-OOS
\
oo
ooO
hom
Declination: T W
LEGEND
1. MAFIC METAVOLCANIC ROCKSa) Massive Amphibolite (mafic flows)b) Foliated Amphibolite and/or fragmental (frg)c) Pillowed Amphibolited) Debris Flow/ Agglomeratee) Epiclastic Interflow Metasediment/ Tuff
2. METASEDIMENTARY ROCKSa) Siliceous Wacke/ Greywackeb) Sandstone/ Siltstone (Arenites)c) Rusty Siltstone/ Wackesd) Amphibolitic Metasediments 4/- garnetse) Conglomeratef) Argiilites
3. MAFIC INTRUSIVE ROCKSGabbro/ Gabbro PorphyryHornblenditeDiorite/ Porphyritic Diorite
4. GRANITIC INTRUSIVE ROCKSGraniteGranodioritePegmatiteApliteMigmatite
5. LATE FELSIC INTRUSIVE ROCKS Quartz Feldspar PorphyryQl
b Felsite
6. PROTEROZOIC INTRUSIVE ROCKSQ] D iabaseb) Porphyritic Diabase
Inferred outcrop
'/': Defined geological contact
Assumed geological contact
2357(10).x"- Geochemical rock sample location,
sample number and Au ppb
Foliation with dip. Shearing with dip
Claim post(located, approximate location)
——— Claim line
T
Swamp
Road 207D Domtar logging roads
— Old logging roads
> Gentle slope^ Moderate slope>>> Steep slope
Cliff
Stream (intermittent)
Cut over area
Scale ^ 1:5000 100 200 300
-*Metres
400
AKIKO GOLD RESOURCES LTDWhite River Gold Project
Strickland Lake Grid (North Sheet) GEOLOGICAL PLAN
Strickland fc Odlum TownshipsSault Ste. Marie Mining District
OntarioNTS: 42C/11.14 Map No. TOP-10
A.C.A. HOTTE INTERNATIONAL LIMITED
42C10NW8900 2,15240 ODLUM 250
CO
ea j—
oro rn
oo
L 30+OOS -
L 32+OOS — — L 32+OOS
L 34+OOS — — L 34-f-OOS
L 36-rOOS
L 38-vQQS — L 38-fOOS
Road 207D--—
L 40-fOOS — — L 40+OOS
L 42+OOS
L 44+OOS —
L 46+OOS
L 4B+OOS —
L 50+OOS
L 52+OOS
L 54+OOS —
L 56+OOS —
l 2343'^ a' b
Id or 5a (fol)
ia,b 1a,4a
\'// \ 1069175
lb(frg)D//
f i* */' ' * ".t..* * ' * i fi 4
•' 3a ; f
'f. . ' 4Mij/ y
-J4b'-. /-.
\ : \'
L 30-rOOS
L 36+OOS
L 42+OOS
L 44+OOS
— L 46+OOS
— L 48+OOS
L 50+OOS
— L 52+OOS
— L 54+OOS
— L 56+OOS
oo
CO
ODf-
o
Declination: T W
LEGEND
1. MAFIC MtTAVOLCANIC ROCKSa) Massive Amphibolite (mafic flows)b) Foliated Amphibolite and/or fragmental (frg)c) Pillowed Amphibolited) Debris Flow/ Agglomeratee) Epiclastic Interflow Metasediment/ Tuff
2. METASEDIMENTARY ROCKSa) Siliceous Wacke/ Greywackeb) Sandstone/ Siltstone (Arenites)c) Rusty Siltstone/ Wackesd) Amphibotitic Metasediments -f/- garnetse) Conglomeratef) Argillites
3. MAFIC INTRUSIVE ROCKSa) Gabbro/ Gabbro Porphyryb) Hornblenditec) Diorite/ Porphyritic Diorite
4. GRANITIC INTRUSIVE ROCKS
bGranite Granodiorite
c) Pegmatited) Aplitee) Migmatite
5. UTE FELSIC INTRUSIVE ROCKSa) Quartz Feldspar Porphyryb) Felsite
6. PROTEROZOIC INTRUSIVE ROCKSal Diabaseb) Porphyritic Diabase
Road 207D
Inferred outcrop
(/: Defined geological contact
Assumed geological contact
2357(10).x"; Geochemical rock sample location,
sample number and Au ppb
80;/ Foliation with dip f Shearing with dip
Claim post(located, approximate location)Claim line
Swamp
Domtar logging roads
Old logging roads
Gentle slope Moderate slope Steep slope
Cliff
Stream (intermittent)
Cut over area
Scale ^ 1:5000 100 200 300
-^-Metres
400
AKIKO GOLD RESOURCES LTDWhite River Gold Project
Strickland Lake Grid (South Sheet) GEOLOGICAL PLAN
Strickland ft Odlum TownshipsSault Ste. Marie Mining District
OntarioNTS: 42C/11.14 Map No. ffRP-10
A.C.A. HOWE INTERNATIONAL LIMITED
42C10NW8900 a.15240 ODLUM 260
x LAST KNOWN OUTCROP f)F SUGAR VON EXTENSION
tricklandLakeX ! /U.4c \
Wowsgami Lake
INTERNATIONAL LIMITEDprepared by A.C.A HOWE
LEGEND
MAFIC METAVOLCANIC ROCKSo) Massive Amphibolite (mafic flows)b) Foliated Arnphibolitc and/or fragmental (frg)c) Kllov/ed Amphibolited) Hebris Flow/ Agglomeratee) Epiclastic Interflow Metasediment/ Cuff
2. METASEDIMENFARY ROCKSa) Siliceous Wacke/ Greywackeb) Sandstone/ Siltstone (Arunitcs)c) Rusty Siltstone/ Wackcsd) Amphibolitic MetasecJiments f/- garnetse) Conglomeratef)
3. MAFIC INTRUSIVE ROCKSa) Gabbro/ Gabbro Porphyryb) Hornblenditec) Oioritc/ Porphyritic Diorite
4. GRANITIC INTRUSIVE ROCKSa) Oraniteb) Granodioritec) Pegmatited) Aplite c] M igmatite
5. UTE FELSIC INTRUSIVE ROCKSa) Quartz Feldspar Porphyryb) Felsite
6. PROTEROZOIC INTRUSIVE ROCKSDiabase Porphyritic Diabase
Outcrop
Assumed geological contact
Geochemical rock sample location
Foliation with dip
Claim post
Claim line
Logging roads
Streon
**** /9 ^9 s / e ' ;.
Scale - 1:20,000
400 800
Metres
AKIKO GOLD RESOURCES LTD.White River Gold Project
Strickland Lake Grid
RECONNAISSANCE GEOLOGICAL ROAD MAP
Strickland, Odlum, Tedder TownshipsSault Ste, Marie Mining District
OntarioNTS: 42C/1V4 Mop No. WKH-10
42C10NW8900 2.15240 ODLUM 270
L 0+00 —
L 2+OOS
L 4+OOS —
L 6+OOS —
L 8+OOS
L 10+OOS —
L 12+OOS —
L 14+OOS —
L 16+OOS
L 18+OOS —
L 20+OOS —
L 22+OOS
L 24+OOS —
ooO
en m
NJm
oo
L 0+00
— L 2+OOS
— L 4+OOS
L 6+OOS
L 26+OOS
L 28+OOS —
Strickland Lake
1W!9B(4)
l t t l 1'4-t—t l t t t l lilt l l l l'"* t ' * ' t t f-l l" t t t t l l l l JA M C i* A i w iUll A ^ W i i A^-A
t i t t t l /l i/i i i i t t .(..(-r i * t i t .1 i i t i t t t i i i t i t ^ l -t-1 t i i t t i Ki r, ^ "* t ,-t /** ^ -* -t -C*" </.tlJ k'l*J l^--*: tV-t^N-ft l C
l ll l
t l__l l l l l l t i l l t t l t t l l J^ l l l l l l l t t tl"" |-j l t l l t -t [ l l t * l l l l t t l l l l l l l l
Rood 206 c-
L 18+OOS
-- L 20+OOS
- L 22+OOS
L 24+OOS
— L 26+OOS
— L 28+OOS
rCO m
ea
oorUlm
om
Deciination: 7 W
LEGEND
Road 207D
>
Claim post(located, approximate location)
Claim line
Swamp
Domtar logging roads
Old logging roads
Gentle slope Moderate slope Steep slope
|V\NV Cliff
Stream (intermittent)
Cut over area
Scale = 1 :5000 100 200 300 400
Metres
t
AKIKO GOLD RESOURCES LTDWhite River Gold Project
Strickland Lake Grid (North Sheet)
GEOCHEMICAL HUMUS CONTOUR MAPCONTOUR INTERVAL - 2 PPB
Strickland ft Odlum TownshipsSault Ste. Marie Mining District
OntarioNTS: 42C/11.14 Map No. WRP-10
A.C.A. HOWE I NTERNATIONAL LIMITED
42C10Nfffl9ei0 2.15240 ODLUM
roo
Oen m
o m
m
i
30+OOS -
L 32+OOS —
L 34+OOS —
L 36+OOS —
L 38+OOS —
Rood 207D —:
L 40-hOOS —
L 42+OOS
L 44fOOS —
L 46+OOS —
L 48+OOS -
L 30+OOS
— L 32+OOS
— L 34+OOS
— L 38+OOS
— L 40iOOS
L 50+OOS
L 52+OOS
L 54-HOOS —
L 56+OOS
---V- \\ f^ — , x- H t-1 t i \\i/1 rxt ' ' * ' ' ) ' ' ' i *M *l *) ' if * 11 ^-\p. \ " . *- -l - s -j }r^ v * ^
f•g"*^L"M * *-*- ' ' ' 'l 1 ' i -' ' i ' * l * *~*-'
^ * . Jl t -4- l t ^t-* t 4—t -l l .-l t t 4—t 't l l. J
•| t ^~*"t *' -t-"* 'I'gl- l l *-*' t ( j 'i l l i 't -It t ( t l l f '
< ^ X /^l i i * t t i-* l t-t—t i t i t l i i ' j j t-f-j i .t-1 t f-f i l ~i~]~~) i i t t f i j i 1 1^ ^ A A A u -,^.~ A ~ — X" *- i i i -N~^-' ** f~ y. rf'- ~ ~ - cc - v " ^-^
^ Nl 'X' l ' ' ' l ' *- ll ' t l~t * ' \"' t -*- ' t i i I i i -*-*--t i i I i i i |X' ' l
xT - - C.H " p, ± ^ ^ A i; - A i ^ f7^ .^ *~ -f .
f/ l J-l" t t t-1/l t f t l t-J t i—l ( l l l l l l l l l f H ^ ' r ^i*1 ^J•-^/
/
L 36+OOS
— L 42+OOS
— L 44+OOS
— L 46+005
— L 4S+OOS
— L 50+OOS
— L 52+OOS
1044398
Road 207B^~
— L 54+OOS
L 56-hOOS
oo
pa CDf— r~
o o
rro rn
oo
ri
en
UJ
oen m
o m
Declination; 7' W
LEGEND
Claim post(located, approximate location)
——— Claim line
Road 207D
Swamp
Domtar logging roads
Old logging roads
Gentle slope Moderate slope Steep slope
Cliff
Stream (intermittent)
Cut over area
Scale ^ 1:5000 100 200 300
——-Metres
400
AKIKO GOLD RESOURCES LTDWhite River Gold Project
Strickland Lake Grid (South Sheet)
GEOCHEMICAL HUMUS CONTOUR MAPCONTOUR INTERVAL -
Strickland k Odlum TownshipsSault Ste. Marie Mining District
OntarioNTS: 42C/11.14 Map No. WRP-10
A.C.A. ROUTE INTERNATIONAL LIMITED
42C10NWS900 2.15240 ODLUM SS0
L 0+00 —
L 2+OOS —
L 4+OOS —
L 6+OOS
L 8+OOS —
L 10+OOS —
L 12+005
L 14+OOS
L 16+OOS
L 18+OOS
L 20+OOS -
L 22+OOS
L 24+005 —
L 26+005
L 28+005 —
oo
CDf—
o
CO
— L 0+00
— L 2+OOS
L 4+005
— L 6+OOS
L 8+OOS
— L 10+OOS
— L 12+OOS
\ t \ t l l [ Jftl 1.1 t l t j) l- t It l l t j t t t tt-) t j i ( t l l t l j ) 4 t 4
y t i t i i j t i * t t i
** vy*/,/
Strickland Lake
If If l t t * l l l l l l l l j 11 il l l l t * l l l l t Iff l
Strickland Lake
f * l\-\ \ i ' t t l t t l l ft l -l l l t l l l t l ( l l t l l* l l \ * t .*-4-'4-l t l l l t
L H+OOS
Road 206 ,x•
— L 16+OOS
— L 18+OOS
L 20+005
— L 22+OOS
L 24+OOS
— L 26+005
L 28+005
oo
CO
CDr~O
fsj
Declination: 7 W
LEGEND
Road 207D
Claim post(located, approximate location)
Claim line
Swamp
Domtar logging roods
Old logging roads
Gentle slope Moderate slope Steep slope
Cliff
Stream (intermittent)
Cut over area
l
Z
3
H
RotKs
ite. Intrusirusve
i.a+4. FilsiC.In'V'-uii
R-oTftrozoic. Ir.TrM.-Swe KOC.KS-
SUear
fr W. F -JET-1
Lifkol
Scale = 1:5000 100 200 300
•^^Metres
400
AKIKO GOLD RESOURCES LTDWhite River Gold Project
Strickland Lake Grid (North Sheet)
GEOPHYSICAL INTERPRETED GEOLOGY
Strickland k O dlum TownshipsSault Ste. Marie Mining District
OntarioNTS: 42C/11.U Map No. WRP-10
A.C.A. HOffE INTERNATIONAL LIMITED
42C10NW8900 2 .15240 ODLUM 300
COO
POm
L 30+OQS —
L 32+005 —
L 34+OOS —
L 36+OOS
L 38+OOS
Road 207D==::
L 40+OOS —
L 42+005 ~
L 44+005 —
L 464-OOS —
L 48+005 —
L 32+OOS
L 34+OOS
— L 36+OOS
— L 38+005
— L 40+OOS
L 50+005 —
L 52+OOS -
L 54+OOS
L 56+QOS —
\ \..,,.. .Vi..
. .i t t * t l i i i-* t i y l i—h
yi i i i i l i i i X t i ill i^ i i i\i Wi i i""
L 30+OOS
— L 42+005
— L 44+OOS
— L 46+OOS
— L 48fOOS
— L 50+OOS
— L 52+OOS
— L 54+OOS
— L 56+005
CO
CO COr~ r—
o oNJ
CO
CO 01 m
horn
Declination; T W
LEGEND
Claim post(located, approximate location)
—— Claim line
Swamp
Road 207D Domtar logging roads
~ Old togging roads
> Gentle slope^ Moderate slope^ S teep slope
.\\^' Cliff
Stream (intermittent)
Cut over area
3 Mafic. InTYusive, ROC
LaVe Ftlsic Xn't'ruSlve
flnsl/or SKear
(V)
R-ojetTecl LiVKoloqi4f
Scale s 1:5000 100 200 300
——-Metres
400
AKIKO GOLD RESOURCES LTDWhite River Gold Project
Strickland Lake Grid (South Sheet)
GEOPHYSICAL INTERPRETED GEOLOGY
Strickland ft Odlum TownshipsSault Ste. Marie Mining District
OntarioNTS: 42C/11.14 Map No. WRP-10
A.C.A. HOWE INTERNATIONAL LIMITED
42CiaNW89a0 a.15240 ODLUM 310
L O
L 200 S
L 400 S
L 600 S
L 800 S
L 1000 S
L 1200 S
L 1400 S
L 1600 S_
L 1800 S
L 2000 S
L 2200 S
L 2400 S
L 2600 S
L 2800 S
CD CD OO
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CO LOCDCD -si-
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- 58938.1 58927.7 58959.4
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58873.558919.158907.7
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— L O
L 200 S
L 400 S
L 600 S
L 800 S
— L 1000 S
L 1200 S
L 1400 S
L 1600 S
L 1800 S
L 2000 S
L 2200 S
L 2400 S
L 2600 S
L 2800 S
Declination: T W.
LEGEND
Scale: 1:5000
Profile Scale: 200 nT/cm.
Profile Base Level: 58.700 nT
SURVEY SPECIFICATIONS
Instruments: EDA Omni IV Base Magnetometer EDA Omni Plus Field Magnetometer
Base Station Location: Latitude 48-44-00Longitude 85-10-00
Base Station Value: 58,975 nT.
Base Station Sample Interval: 15 sec.
100Scale 1:5000
O 100 200 300
(meters)
O
AKIKO GOLD RESOURCES LTD.White River Gold Project
Strikland Lake Grid (North Sheet)GROUND MAGNETOMETER SURVEYTotal Field Postings 4 ProfilesStrikland ft Odlum Townships
Sault Ste. Marie Mining DivisionOntario
NTS: 420/11,14 Map No. WRP-01Survey 4 Presentation:
TecriTerrex Inc. Oakvie, Ontario September 1993
42C10NWH9B0 2 .15240 ODLUM 320
L 3000 S
L 3200 S
L 3400 S
L 3600 S
L 3800 S
L 4000 S
L 4200 S
L 4425 S
t m
L
tlw
L 5408 S
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LEGEND
Scale: 1:5000
Profile Scale: 200 nT/cm.
Profile Base Level: 58,700 nT
SURVEY SPECIFICATIONS
Instruments: EDA Omni IV Base Magnetometer EDA Omni Plus Field Magnetometer
Base Station Location: Latitude 48-44-00Longitude 85-10-00
Base Station Value: 58,975 nT.
Base Station Sample Interval: 15 sec.
100Scale 1:5000
O 100 200
(meters)
AKIKO GOLD RESOURCES LTD.White River Gold Project
Strikland Lake Grid (South Sheet)GROUND MAGNETOMETER SURVEYTotal Field Postings 4 ProfilesStrikland A Odlum Townships
Sault Ste. Marie Mining DivisionOntario
NTS: 42C/1U4 Map No. WRP-02Sufvej 4 Presentation:
TectiTenex Inc. Ockville, Ontario September 1993
42C18NW8980 2.1524® ODLUM 330
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Declination: 7* W.
LEGEND
Scale: 1:5000
Contour Interval: 20 nT. 100 nT. 500 nT.
SURVEY SPECIFICATIONS
Instruments: EDA Omni IV Base Magnetometer EDA Omni Plus Field Magnetometer
Base Station Location: Latitude 48-U-OO Longitude 85-10-00
Base Station Value: 58.975 nT.
Base Station Sample Interval: 15 sec.
100Scale 1:5000
O 100 200 300
(meters)
2
AKIKO GOLD RESOURCES LTD.White River Gold Project
Strikland Lake Grid (North Sheet)GROUND MAGNETOMETER SURVEY
Total Field ContoursStrikland A Odlum Townships
Sault Ste. Marie Mining DivisionOntario
NTS: 42C/11.14 Map No. WRP-03Survey S Presentation:
TechTera k. OokviHe, Ontario September 1993
42C10NW8900 a.l 5240 ODLUM340
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Scale: 1:5000
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SURVEY SPECIFICATIONS
Instruments; EDA Omni IV Base Magnetometer EDA Omni Plus Field Magnetometer
Base Station Location: Latitude 43-44-00Longitude 85-10-00
Base Station Value: 58,975 nT.
Base Station Sample Interval: 15 sec.
100Scale 1:5000
O 100 200 300
(meters)
AKIKO GOLD RESOURCES LTD.White River Gold Project
Strikland Lake Grid (South Sheet)GROUND MAGNETOMETER SURVEY
Total Field ContoursStrikland A Odlum Townships
Sault Ste. Marie Mining DivisionOntario
NTS: 42C/11.H Map No. WRP-04Survey 4 Presentation:
TediTara Inc. Ookville, Ontario September 1993
42C10NWB90a 2,15240 ODLUM 3B0
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In-Phcse Profiles:
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SURVEY SPECIFICATIONS
Instrument: EDA Instruments Omni Plus Mag/VLF receiver
Transmitter Station: Annapolis, Maryland
Transmitter Frequency: 21.4 kHz.
Transmitter Azimuth: Approx. 145 degrees
Initialization Direction: N-S Lines; Facing North E-ff Lines; Facing East
NOTE: Base A Tie lines surveyed with Cutler, Maine
Transmitter Frequency: 24.0 kHz.
Transmitter Azimuth: Approx. 95 degrees
100Scale 1:5000
O 100 200 300
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2.15 O
AKIKO GOLD RESOURCES LTD.White River Gold Project
Strikland Lake Grid (North Sheet)GROUND VLF-EM SURVEY NSS Postings A Profiles
Strikland A Odlum TownshipsSault Ste. Marie Mining Division
OntarioNTS: 420/11,14 Mop No. WRP-Q5
Survey 4 Presentob'on: lectilerrex k Oakville, Ontario September 1993
42CI0NW89B0 2 ,15240 ODLUM 360
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Declination: T W.
LEGEND
Scale: 1:5000
Contour Interval: 1 nl5nT.
20 nT.
SURVEY SPECIFICATIONS
Instrument: EDA Instruments Omni Plus Mag/VLF receiver
Transmitter Station: Annapolis, Maryland
Transmitter Frequency: 21.4 kHz.
Transmitter Azimuth: Approx. 145 degrees
Initialization Direction: N-S Lines; Facing North E-W Lines; Facing East
NOTE: Base A Tie lines surveyed with Cutler, Maine
Transmitter Frequency: 24.0 kHz.
Transmitter Azimuth: Approx. 95 degrees
100Scale 1:5000
O 100 200 300
(meters)
2.152
AKIKO GOLD RESOURCES LTD.White River Gold Project
Strikland Lake Grid (North Sheet)GROUND VLF-EM SURVEY
NSS Fraser Rlter ContoursStrikland A Odlum Townships
Sault Ste. Marie Mining DivisionOntario
NTS: 420/11.14 Mao No. WRP-07Survey ft Presentation:
Odkvile, Ontario September 1993
42C10NW8900 2 .15240 ODLUM 380
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LEGEND
Scale: 1:5000
Contour Interval; 1 nT.5nT.
20 nT.
SURVEY SPECIFICATIONS
Instrument: EDA Instruments Omni Plus Mag/VlF receiver
Transmitter Station: Annapolis, Maryland
Transmitter Frequency: 21.4 kHz.
Transmitter Azimuth: Approx. 145 degrees
Initialization Direction: N-S Lines; Facing North E-W Lines; Facing East
NOTE: Base ft Tie lines surveyed with Cutler, Maine
Transmitter Frequency: 24.0 kHz.
Transmitter Azimuth: Approx. 95 degrees
100Scale 1:5000
O 100 200 300
(meters)
2.152
AKIKO GOLD RESOURCES LTD.White River Gold Project
Strikland Lake Grid (South Sheet)GROUND VLF-EM SURVEY
NSS Fraser niter ContoursStrikland ft Odlum Townships
Sault Ste. Marie Mining DivisionOntario
NTS: 42 C/H.U Map No. WRP-08Survey 4 Presentation:
Techlero Inc. Oak*, Ontario September 1993
42CI0NW6980 2.15248 ODLUM 330