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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

\

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


U.S.A

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

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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 crosslines 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


11.and metasediments on the property at random orientations.

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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l XRA

1

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


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


. FILE 16198-RO Total Pages 1

g 22 ROCKS

1

1

METHOD DETECTION LIMITAU PPB FAAA 5.


1

1

1

1

1

1

1


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

l

l

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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

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40180

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MOPPI

-.-~-..-..

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CERTIFICATION:


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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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


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:


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

l l l l l l i i i i i i i i i i i i i

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)


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)


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..


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.

l

l

l

l

l

l

l

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.

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l8

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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)

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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

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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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L1200S-50WL1200S-BLL1200S-475E L1200S-500EL1200S-525E

L1200S-550E L1200S-575EL1200S-600EL1200S-625EL1200S-650E

L1200S-675EL1200S-700EL1200S-725E L1200S-750EL1200S-775E




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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

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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)

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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


REF. FILE 16295-


AU PPBMETHOD

NA

CUSTOMER NO.


Total Pages 14

1943

DETECTION LIMIT 1.

l l l l l l l

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DATE 10- j CERTIFIED BYJean H.L. Opdeb^feck, Gegferal Manager

Member of the SGS Group (SoclEtE GEnErale de Surveillance)

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TL800W-5550STL800W-5600STL775W-4500S TL775W-4550STL8U-3050S

TL8U-3100S TL8W-3200STL8U-3250STL8U-3300STL8W-3350S

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PAGE 1 OF 14

Fax (416)445-4152 Tlx 08-986947

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PAGE 2 OF 14

Fax (416)445-4152 Tlx 06-986947


9SAMPLE

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PAGE 3 OF U

Fax (416)445-4152 Tlx 06-986947

IXRAL1 11111111111111111

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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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-Nov-93 REPORT 24937 REF.FILE 16295- PAGE 5 OF 14

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SAMPLE






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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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*SAMPLE

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PAGE 5 OF 14

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-Nov-93 REPORT 24937 REF.FILE 16295-

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PAGE 10 OF 14

Fax (416)445-4152 Tlx 06-986947


*SAMPLE

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PAGE 11 OF 14

Fax (416)445-4152 Tlx 06-986947


9SAMPLE



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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


9SAMPLE

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TL12E-3900STL12E-3950STL12E-4000S TL12E-4050STL12E-4100S

TL12E-4150S TL12E-4200STL12E-4250STL12E-4300STL12E-4350S

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Tlx 06-986947


*SAMPLE AU PPB

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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

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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)

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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


. FILE 16232- Total Pages 7

PULPS Proj . WHITE RIVER

METHOD DETECTION LIMITAU PPB NA 1.


1

1

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1

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HATP lLJf\ X J-* '

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^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

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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-375E L34S-400E134S-425EL34S-450EL34S-525E

L34S-550EL34S-575EL34S-600E L34S-62SEL34S-650E


V3 REPORT Z4K6 REF.FILE 1623Z- PAGE 1 OF 7

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L34S-800E L34S-825EL34S-850E SMPL34S-875EL34S-900E


L34S-1050E L34S-1075EL34S-1100EAL34S-1000EBL34S-1125E

L34S-1150EL38S-200WL38S-150W L38S-100WL38S-50W

L38S-0 L38S-25EL38S-50EL38S-75EL38S-100E



L38S-375EL.38S-400EL38S-425E L38S-450EL38S-475E

L38S-500E L.38S-525EL38S-S50EL38S-575EL38S-600E

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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


9SAMPLE

L38S-62SE L38S-650EL38S-675EL38S-700EL38S-725E


L38S-875E L38S-900EU38S-925EL38S-950EL38S-975E


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

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Nov-93 REPORT 24826 REF.FILE 16232- PAGE 3 OF 7

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9SAMPLE







L44S-1075E L44S-1100EL44S-1125EL4000S-9L200UL4000S-150U

L4000S-100WL4000S-50W[.'•OQOS-0+00 L4060S-25EL4000S-50E


Mov-93 REPORT 24826 REF.FILE 16232- PACE 4 OF 7

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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)


9SAMPLE


UOOOS-325EL4000S-350EL4000S-37SE L4000S-400EL4000S-425E


L4000S-575EL4000S-600EUOOOS-625E L4000S-650EUOOOS-675E


L4000S-82SEL4000S-850EL4000S-875E L4000S-900EL4000S-925E


L4000S-1075EL4000S-1100EL4000S-1125E L4bOflS-1150EL4000S-1175E

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PAGE 6 OF 7

Fax (418)445-4152 Tlx 06-986947

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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)

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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.


Total Pages 10

1943

427 HUMUS

AU PPBMETHOD NA

DETECTION LIMIT 1.


DATE OS-Hov-93 CERTIFIED BY .Jean H.L. Opde

Member of the SGS Group (SociEtE GEnErale de Surveillance)


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TL800W-2500S TL800W-2550STL800W-2650STL800W-2700STL800W-2750S

TL800U-2800STL800U-2850STL800W-2900U TL800W-2950SBL200U- 1950S

BL200U-2050S BL200W-2100SBL200W-2150SSL200W-2250SSL200U-2300S

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BL2W-2700S BL2W-2750SBL2U-28+OOSBL2U-2850SBL2W-2900S

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-Nov-93

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L22S-87SE L22S-900EL22S-925EL26S-800WL26S-750W

L26S-700WL26S-650UL26S-600U L26S-350UL26S-300W

L26S-250W L26S-200WL26S-150UL26S-100WL26S-50W

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L26S-375E L26S-400E126S-425EL26S-450EU26S-475E

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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)


*SAMPLE

L28S-475E L28S-500EL28S-525EL28S-S50EL28S-575E

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-Nov-93 REPORT 24839 REF.FILE 16199- PAGE 5 OF 10

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REPORT 24839 REF.F1LE 16199- PAGE 6 OF 10

.eslie Street Don Mills Ontario M3B 3J4 (416)445-5755Member of the SGS Group ( Societe GeneYale de Surveillance)

Fax (416)445-4152 Tlx 06-986947

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.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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L3000S-700WL3000S-650W L30QQS-6QOWL3000S-SSOUL3000S-500U

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-Nov-93

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PAGE 9 OF 10

Fax (416)445-4152 Tlx 06-986947

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REF.FILE 16199- PAGE 10 OF 10

Don Mills Ontario MSB 3J4 (416)445-5755 Fax (416)445-4152 Tlx 06-986947 Member of the SGS Group (Sociite Generate 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


REF. FILE 16295-


NOV f 5 1993CUSTOMER No.


Total Pages 14

1943

AU PPBMETHOD NA

DETECTION LIMIT 1.


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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PAGE 3 OF 14

Fax (416)445-4152 Tlx 06-986947


9SAMPLE

L46S-125E L46S-150EL46S-175EL46S-200EU6S-225E


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IXRALi ——————————————— 1 10-Nov

SAMPLE AU

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PAGE 6 OF 14

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PAGE 7 OF 14

Fax (416)445-4152 Tlx 06-986947

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PAGE 8 OF 14

Fax (416)445-4152 Tlx 06-986947

IXRAL111111111111111111

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PAGE 9 OF 14

Fax (416)445-4152 Tlx 06-986947

IXRAL111111111111111111

*SAMPLE

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PAGE 10 OF 14

Fax (416)445-4152 Tlx 06-986947


*SAMPLE

L5225S-1100EL5225S-112SEL5225S-1150EI5225S-1175EL5225S-1200E

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L542SS-350WL5425S-300WL5425S-250WL5425S-150WL5425S-100W

L5425S-50UL5425S-0+00L5425S-25EL5425S-50EL5425S-75E



L5425S-350EL5425S-375E 154255-4001L5425S-425EL5425S-450E

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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

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L5625S-250U L5625S-BL200UL5625S-150UL562SS-100UL5625S-50U

L5625S-0+00L5625S-25E L5625S-50E L5625S-75EL5625S-100E




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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)


*SAMPLE


L5625S-625EL5625S-650EL562SS-675E L5625S-700EL5625S-725E

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TL12E-4700STU2E-4750STL12E-4800STL12E-4850STL12E-4900S

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PAGE 1 3 OF 14

Fax (416)445-4152 Tlx 06-986947

JXRAL111111111111111111

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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


REF. FILE 16199-

427 HUMUS

AU PPBMETHOD NA

^A*NOV 1 5 W95

CUSTOMER NO.


Total Pages 10

1943

DETECTION LIMIT 1.

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DATE 08-NOV-93 CERTIFIED BYJean H.L. Opde


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9SAMPLE


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PAGE 6 OF 10

Fax (416)445-4152 Tlx 06-986947


9SAMPLE






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PAGE 7 OF 10

Fax (416)445-4152 Tlx 06-986947

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PAGE 8 OF 10

Fax (416)445-4152 Tlx 06-986947

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PACE 9 OF 10

Fax (418)445-4152 Tlx 06-986947

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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)


REF. FILE 16232-

287 PULPS Proj. WHITE RIVER

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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 AJST AJL Y SI S

REPORT 24826

CUSTOMER NO.


Total Pages 7

5 19931943

METHOD NA

DETECTION LIMIT 1.


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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PAGE 5 OF 7

Fax (416)445-4152 Tlx 06-986947


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PAGE 6 OF 7

Fax (416)445-4152 Tlx 06-986947

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Member of the SGS Group (Soci*te Centrale de Supveiltance)

PAGE 7 OF 7

Fax (416)445-4152 Tlx 06-986947


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


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

l

l

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

1069184

1078185

1078215

1078216

1078217

1078218

1078219

1078220

1078221

1078222

1078223

1078224

1078225

1078226

1078227

1078228

1078229

1078230

1078231

1078232

1078234

1078235

1078236

1078237

1078238

1078239

1078240

1078241

1078242

1078305

1078306

1078307


AKIKO GOLD RESOURCES LIMITED ffHITE RIVER GOLD PROJECT

LOCATION MAP

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o 70

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VSi

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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


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


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


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/gradiometer 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.


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 magnetometer/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


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

l l

jl l l l l l l l l l

The Omni System as a Base Station IVIagnetometer

l l l l

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


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 station(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

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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.


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

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(included in VLF configurations)

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A

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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


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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is re

port

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ork.

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endix

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e ev

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hoice

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riorit

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tion

one

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plem

ente

d.

Note

1:

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ples

ol b

enef

icia

l Int

eres

t are

unr

ecor

ded

trans

fers

, opt

ion

agre

emen

ts, m

emor

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m o

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ents

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min

ing

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ms.

Mot

t 2:

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rk h

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een

perfo

rmed

on

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nted

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ease

d la

nd, p

lease

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plet

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nefic

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nter

est

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work

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port

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inim

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tocls

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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

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Cre

dits

are

to b

e cu

t bac

k st

artin

g wi

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last

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king

back

ward

s.2.

O

Cre

dits

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to b

e cu

t bac

k eq

ually

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r all

claim

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in th

is re

port

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ork.

3.

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redi

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re lo

be

cut b

ack

as p

riorlz

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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

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:

l cer

tify

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reco

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hol

der h

ad a

ben

efici

al In

tere

st In

the

pate

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i Hie

time

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per

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rder

lo m

inim

ize (h

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vers

e ef

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suc

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letio

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leas

e in

dica

te fr

om

which

cla

ims

you

wis

h lo

prlo

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the

dele

tion

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redi

ts.

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se m

ark

(f)

one

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e fo

llowi

ng:

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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

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ease

com

plet

e th

e fo

llow

ing:

l cer

tify

lhal

In*

reco

rded

hol

der h

ad a

ben

efici

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tere

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(he

pate

nted

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tim

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as p

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ack.

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rder

to m

inim

ise th

e ad

vers

e ef

fect

s of

suc

h de

letio

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leas

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dica

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om

which

cla

ims

you

wish

lo p

rlorlz

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e de

letio

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cre

dits

. Pl

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mar

k (*

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e of

(he

follo

wing

:

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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

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Inter

est I

n the

psle

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or le

ased

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at t

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me

the

work

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gniitu

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l*

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its y

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is re

port

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cut b

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der l

o m

inim

ize (h

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vers

e ef

fect

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suc

h de

letio

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lease

Indi

cate

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wh

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laim

s yo

u wi

sh lo

prio

rite

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dele

tion

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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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L 8-fOOS

L 10+OOS

— L 12+OOS

l iiid iI:"'J502(2)

deadfall A bush 2a ,-t i t H t t -t l i t t r t i i -[i i 11. t. t j 4- t l /* V-4

Ik-^'f •f'-.'-^S!2303(3/ JlBo &1

l -t t

1b 1b,4o . - vdeadfall tt bush 4a,5a?.-. i i * i t t t l i i i i * t *~f t -t—* ^ t-H- t (-t t i i it

2382x,,// i 1 b,5a-;

•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


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


Cut over area

Scale ^ 1:5000 100 200 300

-^-Metres

400


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


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 line

Swamp


Old logging roads


|V\NV Cliff


Cut over area

Scale = 1 :5000 100 200 300 400

Metres

t


Strickland Lake Grid (North Sheet)

GEOCHEMICAL HUMUS CONTOUR MAPCONTOUR INTERVAL - 2 PPB


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 line

Road 207D

Swamp


Old logging roads


Cliff


Cut over area

Scale ^ 1:5000 100 200 300

——-Metres

400


Strickland Lake Grid (South Sheet)

GEOCHEMICAL HUMUS CONTOUR MAPCONTOUR INTERVAL -

Strickland k Odlum TownshipsSault Ste. Marie Mining District


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 line

Swamp

Domtar logging roods

Old logging roads


Cliff


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


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 line

Swamp

Road 207D Domtar logging roads

~ Old togging roads

> Gentle slope^ Moderate slope^ S teep slope

.\\^' Cliff


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


Strickland Lake Grid (South Sheet)

GEOPHYSICAL INTERPRETED GEOLOGY



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

CD CDr-- CD

CO LOCDCD -si-

CD CDOJ

CD

CD

CDCD OJ

CD CD CD

LOCD CO

CD CD

CD CD OO

CD CD

LLJ

CDCD CD

CD CD

CD CDCNI

LU CD OCN

58945.2 58924.8 58909.9 58990.0 58934.8 58909.6 5B874.3 50869.8

--55878.5 58870.3 58949.7 58958.2 58991.3 .58908.6

j- 58872.3 i' 58865.0

58911.556691.658876.058844.858904.258859.1

- 58938.1 58927.7 58959.4

- 58902.8 5B927.0

- 58918.0f 58901B4- 58698.7

53875.458867.058838

58697.158715.758722.258687.658695.858711.258693.358700.058696.558711.858694.2

no DO op cc eg tp Ip CD dp S DOin in in 55 L* in ILm in io in

58823.4 58829.8 58867.9 58847.0 58902.0 58934.0 58849.8

4-58768.4 58788.3 58784.4 58801.9

58728.7 58708.6 58715.0 58718.4 58722.4 5B715.5 58725.5 58758.9 58E91.1 58711.1 58722.7 58754.7

58873.558919.158907.7

5BB59.158842,358830.858828.958861J58886.358933.859023.558933.9

58964.158976.858963.258966.558959.459031.459064.459024.359009.359122.959154.659014.0

7.58933.7 58942.9 58875.1 58819.9 58815.5 58801.1 5BB03.4 58796.3 58753.3 58723.6

.2

.8. . . 62.758769.258773.758731.558687.6

74.42.3

S8720.6 *58679J

58771,7 5B774.6 &B859.4 58838.4 58837.1 58722.4 58716.9 58750.3

58700.3 58711.7 58729.1 58706.1 (58675.0

'58685.1 , 58724.3

C -58765.1 y 58719.1 f 58756.2 ( 5B775.4

58772,158776.658774.558750.258736.458813.858756.358733.858777.9

- 58776.4 58816.8 58829.8 58945.8 58897.5 59034.3

--5882

58704.558709.058707.258701.858700.858687.758700.258703,558711.7Hi C0 Irt

SK

- 58777.5-' 58753.1

58729J 587!7J 58720.1 58717.2

--58744.0- 58773.4

58741.8 587+7.0

58736.258753.558798.458801.658814.058797.95B781.858787.658776.558783.4

SSSSSBKKK3K

0.158700.458703.058686.958685.258677.258692.558675.5

78.963.0

.5

58816.0 58774.5 58791.9 58802.7 58792.9 5B78B.2 58859.6 58749.5 58718.9

737.2 E8985.0

58824.6 58797,7 58826.0 5B841.5 58841.5 58894.9 58950.7 58923.4 58931.7 59031.5 58918.3 58882.2 58899.2

21*58887.7 8 8 f 58955.4

' i 1-4-59126.9 59524.9 59604.1 59349.6 59417.7 59000.9 58797.4 58796.4 58801.2 58758.2 58795.2 58741.9

7.558707.0 58776.3 58812.5

59867.4 60665.8 60984.3 60028.9 59926.5 59467.6 59193.7 58985.3 58963.8 58915.5

•58883.8

58893.9 58875.8 58824.5 58778.2 58813.5 58860.5 56895.0 58796.B 58698.1 58903.3

753.3 931.7

9137.1

55.473.4

58684.858712.658732.7

58686.056708.158756.758689.758733.858953.159451.560000.459882.959711.159045.858809.15B9U558823.958907.158854.458725.658781.258835.858814.558916.558951.958726.158913.458839.758781.558796.758830.558836.258847.458739.558822.058878.958851.958818.458816.458794.35886,1.85B854.958932.058844.458828.058884.958983.459009.658999.359025.158947.138806.658811.858869.958796.858760.158757.958814.158930.458944.259038.1

58689.3 58893.7 5B900.3 58885.4

O OOO

LU LO

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CO ^QQ

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LO

CD CD CO

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CD CD CO CT)

CD CDCD

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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


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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58691.2 58716.1

f 58733.3 58753.4

--58737.9 58778.2 58763.9 5B827.2

If&'I'gtfg&gai^^58717.958726.550722.658749.358030.758702.8

- 58818.0--58815.6

50028,9 58861.7 58909.9 58921.5

esBagssrfaSxg^jggiaaajiffs*^^

58831.1 58791.5 58769.2 58801,1 58791.9 58795.7 58761.9

- - 58787.3 58799.1

+ 5BB82.4 59005.7

59X5.1 59328.0 59390.7 59609.3 59584.7 50764.8 50977.7 5B947.0 56869. 58822.

58786.158742.858732.058716.958822.458782.656853.158789.658739,4587 J 3.558738.458826.1

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6••58835.6

50820.8 27.7 124,9

50710.1 58712.0 58702.8 50718.6 58823.5 59070.8 59323.4

-1-58964.9 5B974.7 59274.6 59333.0

121.9

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58929.050884.858833.858902.850929.258870.558866.658836.358868.350903.958966.158868.456046.358917.5

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587B3.9 50849.4 58923,4 58908 58903 5891 5903

4-50921.7

58833.9 1 58870.1 ' 50826.2-58006.51 58037.2

50806.556805.4

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- 58738.0 58736.4

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LEGEND

Scale: 1:5000

Profile Scale: 200 nT/cm.

Profile Base Level: 58,700 nT






100Scale 1:5000

O 100 200

(meters)


Strikland Lake Grid (South Sheet)GROUND MAGNETOMETER SURVEYTotal Field Postings 4 ProfilesStrikland A Odlum Townships


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.



Base Station Location: Latitude 48-U-OO Longitude 85-10-00

Base Station Value: 58.975 nT.


100Scale 1:5000

O 100 200 300

(meters)

2


Strikland Lake Grid (North Sheet)GROUND MAGNETOMETER SURVEY

Total Field ContoursStrikland A Odlum Townships


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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LEGEND

Scale: 1:5000

Contour Interval: 20 nL 100 nT. 500 nT.


Instruments; EDA Omni IV Base Magnetometer EDA Omni Plus Field Magnetometer




100Scale 1:5000

O 100 200 300

(meters)


Strikland Lake Grid (South Sheet)GROUND MAGNETOMETER SURVEY

Total Field ContoursStrikland A Odlum Townships


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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Declination; 7* W.

LEGEND

Scale: 1:5000

Profile Scale: 10 %/cm.

In-Phcse Profiles:

Quadrature Profiles:


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



100Scale 1:5000

O 100 200 300

(meters)

2.15 O


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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LEGEND

Scale: 1:5000

Contour Interval: 1 nl5nT.

20 nT.


Instrument: EDA Instruments Omni Plus Mag/VLF receiver




Initialization Direction: N-S Lines; Facing North E-W Lines; Facing East

NOTE: Base A Tie lines surveyed with Cutler, Maine



100Scale 1:5000

O 100 200 300

(meters)

2.152


Strikland Lake Grid (North Sheet)GROUND VLF-EM SURVEY

NSS Fraser Rlter ContoursStrikland A Odlum Townships


NTS: 420/11.14 Mao No. WRP-07Survey ft Presentation:

Odkvile, Ontario September 1993

42C10NW8900 2 .15240 ODLUM 380

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Declination: 7 W.

LEGEND

Scale: 1:5000

Contour Interval; 1 nT.5nT.

20 nT.


Instrument: EDA Instruments Omni Plus Mag/VlF receiver




Initialization Direction: N-S Lines; Facing North E-W Lines; Facing East

NOTE: Base ft Tie lines surveyed with Cutler, Maine



100Scale 1:5000

O 100 200 300

(meters)

2.152


Strikland Lake Grid (South Sheet)GROUND VLF-EM SURVEY

NSS Fraser niter ContoursStrikland ft Odlum Townships


NTS: 42 C/H.U Map No. WRP-08Survey 4 Presentation:

Techlero Inc. Oak*, Ontario September 1993

42CI0NW6980 2.15248 ODLUM 330

summary report on the exploration of the white river … · summary report on the exploration of...

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