15095 l reconnaissance surveys vlf-em surveys l · map b92-1d : magnetometer and max-min recce....

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42A08SE9907 2.15095 BISLEY 010SUMMARY R.

ON

. 15095RECONNAISSANCE SURVEYS

( 1992 Field Season )

VLF-EM Surveys

Magnetic Surveying

Max-Min Surveying

Geological Reconnaissance

Sampling

BISLEY S MELBA TOWNSHIPS PROJECTS

( OPAP Initiatives )

by . 15095

fc

Frank P. Tagliaroonte , P.Eng.

( Frank H. Toews )

May

1993

JUL 4 19933 l

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42Ae8SE9907 2.15095 BISLEY 010G

CONTE- --

INTRODUCTION 6 SUMMARY.... . . . . . . . . . . . . . . . . . . . . . . l

PROPERTY. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2

LOCATION........................................ 2

ACCESS.......................................... 2

DATA ATTACHED............ . . . . . . . . . . . . . . . . . . . . . . . 3Report Pockets

F.P.Tagliamonte Project Area F.H.Toews Project Area

Appendix. . . . .. .. . . ....... ..... .. . . ... . .. .. . . . . . . 3a.

GEOLOGY......................................... 3GeneralTable of FormationsLocal

WORK DONE................................ . . . . . . . 4 Referencel ,-- Claim Staking Personnel

Proj ect Area ............................. 5

I Work Period Grid Control Geological Observations

IVLF-EM Surveying Max-Min Surveying ........................ 6 Magnetometer Surveying ................... lSampling

RESULTS OBTAINED........ . . . . . . . . . . . . . . . . . . . . . . . . 8Geological Reconnaissance fi ProspectingGeophysical SurveyingFPT Proj ect Area ......................... 9VLF-EM SurveyingMagnetometer ft Max-Min Recce. SurveysVLF-EM amd Max-Min EM Survey ............. 10FHT Project AreaVLF-EM SurveysMagnetometer St Max-Min Recce. Surveys .... 11

CONCLUSIONS AND RECOMMENDATIONS................. 12FPT Project Area FHT Project Area

.........cont'd

CONTENTS

APPENDIX

l l l ll I Table of Lithologic Units , Melba ft Bisley townships

l II F.P.Tagliamonte OPAP Project Area

III F. H. Toews OPAP Project Area

MAP DATA

l F.P.Taaliamonte Project Area - Bisley twp.

Maps: B92-A ; B92-1 ; B92-1A ; B92-1B ; B92-1C ; m B92-1D ; B92-1E

B F.H.Toews Project Area - Melba S Bisley twps.

" Maps: MB92-1 ; MB92-2 ; MB92-1A ; MB92-1C ; MB92-1B

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SUMMARY REPORT

on

VLF-EM SURVEYReconnaissance Geological Surveying

Prospecting S Sampling

BISLEY 6 MELBA TOWNSHIP PROJECT( OPAP Initiatives )

by

Frank P. Tagliamonte , P.Eng.

Frank H. Toews , Geologist

January

1993

INTRODUCTION S SUMMARY

Colour coded portions of Map B 92-A locate the areas of a larger property package in the NWest quadrant of Bisley township where exploration work was carried out during the 1992 field season. The exploration program was funded by OPAP and involved two applicants , one of whom is a joint partner in a portions of the property package. The applicants are also authors of this report.

Exploration work completed during the 1992 field season was a follow up on anomalous responses obtained during reconnaissance geological and geophysical surveys completed during 1991.

The 1992 exploration program involved grid line surveying , VLF- EM and geological surveying as well as prospecting and local sampling.

Conventional magnetic and Max-Min EM profile surveys were completed on cut grid lines over peak portions of previously detected ( 1991 ) VLF-EM anomalies and over portions of mineralized units located during the 1992 season.

Two copies of a report complete with maps and sketches on the 1992 exploration program has been submitted to OPAP. This report is a slightly revised version of the reports sent to OPAP.


Additional VLF-EM anomalies , one coincident with a magnetic closure , and mineralized formations (peperite) were located during the 1992 exploration work.

There are also a series of discreet airborne magnetic closures within the claim group that have not been investigated on the ground. Current interest in Kimberlite structures with diamond potential imply that these anomalies represent target areas for follow up exploration.

Continuing exploration is recommended.

PROPERTY

The property package is located in the NWest quadrant of Bisley amd the NEast quadrant of Melba townships as shown on Map B 92-A. It is registered in the name of Frank P. Tagliamonte but portions of the property are jointly owned. One portion of the package is owned by an associate applicant.

Those portions of the property package where 1992 exploration work has been done is shown in colour coded outlines on the map.

Specifically, the following claims were covered or partially covered by exploration work:

Melba townshipt

Claim L 1186760

Bisley township

Claims: L 1186160 ; L 1186150 ; L 980240 ; L 1186151 , 6152 , 6153 ; L 1045478 , 5479.

LOCATION

Kirkland Lake Resident Geologists DistrictBisley S Melb townshipsLarder Lake Mining DivisionClaim map #G3191NTS 32 D 5Lat: 48 degrees 20 min. +- ; Dep: 80 degrees 00 min. +-NWest quadrant of Bisley twp. 6 NEast quadrant of Melba twp.

ACCESS

The central part of the project area is accessible by motor vehicle approximately 36 road miles (58km) from Kirkland Lake.

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*Road

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access is provided by travelling East of Kirkland Lake onHighway No 66 to the Esker Park road (Hwy # 672) then North forabout 18 miles (28.5km) to a gravel logging road which trendsWesterly , then Northerly to the Project Area , a distance ofapproximately 10 miles (15.7km).

DATA ATTACHED

Report Pockets

1) Map B 92-A: Claim Location St 1992 O. P. A. P. ProjectArea Locations

F.P.Taaliamonte ( FPT ) 0 P A P Project Area

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Map B92-1 : Recce. VLF-EM Surveys , Composite Data Plan

Map B92-1A : Magnetometer and Max-Min Recce. Surveys

Max-Min profiles (4) : Lines 61W ; 67W ; 'A 1 ; 'B'

Map B92-2 : Geological Reconnaissance Map

Inset Sketches

Map B92-1B : VLF-EM Surveys (Fraser Filter Contours) SW

Map B92-1C : VLF-EM Surveys (Fraser Filter Contours) AM

Map B92-1D : Magnetometer and Max-Min Recce. Surveys ,Profiles - Lines 61 S 67 W

Map B92-1E : VLF-EM Max-Min Surveys , East Claim Line ,Claim : (L-980240)

Toews ( FHT ) 0 P A P Project Area

Map MB92-1 : Recce. VLF-EM Surveys , Composite Data Plan

Map MB92-1A : Magnetometer and Max-Min Recce. Surveys

Max-Min Profiles (4) : Lines 98W ; 106W ; part of 108W and 'C 1

Map MB92-2 : Geological Reconnaissance Map

Inset Sketches

Map MB92-1C : VLF-EM Surveys (Fraser Filter Contours) SW

Map MB92-1B : VLF-EM Surveys (Fraser Filter Contours) CM


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Appendix

I) Table of Lithologic Units , Melba Se Bisley townships

II) F.P. Tagliamonte OPAP Project Area

1) Sample and Assay Data sheet

2) Photo Folios (2)

III) F. H. Toews OPAP Project Area

1) Geology supplements ( GI S Gil ; GSI - GSVI )

2) Sampling and Assayinng ( SI - Sil and Certificates of Analysis )

3) Photo Folio (1)

GEOLOGY

General

The project area lies within a package of Blake River Group volcanic stratigraphy. The package includes mafic , intermediate and felsic volcanics with some associated tuffs and sediments as well as basic intrusives.

Table of Formations

A photo copy of the Table of Lithologic Units from page 4 , ODM Geological Report 103 is inserted in the appendix.

Local

Geological reconnaissance observations and prospecting indicated that the predominant rock types within the project area are intermediated volcanics which are amygdaloidal and pillowed.

The North portion of the Project Area hosts broad bands of lapilli tuff and tuff breccia more popularly identified as hyaloclastite. Some portions of the hyaloclastite appear to be rhyolitic in composition. The central portion of the area appears to be mainly intermediate volcanics. Mafic volcanic predominate in the Southern portion of the area.

Breccias of various types are common. Most are flow breccias but some may be pyroclastic.


Two diorite occurrences have been noted. One near anomaly 'L 1 (1991 survey area) , and another adjacent to the road in the NEast corner of Map B92-1. A photo ( B-2 ) showing the mineralized breccia contact of the diorite and host volcanics is in the appendix.

A mineralized unit identified by Dr. L. S. Jensen , OGS , as peperite was observed in outcrops along the North boundaries of claims L 980240 and 842945 as shown on Map B92-1E. Surface exposures of this unit are usually variably gossaned and contain patchy areas of pyrite and minor pyrrhotite mineralization up to a maximum of 5%. This unit is also exposed in outcrop in Melba township associated with VLF-EM anomaly 'MB92-C' as shown on Maps MB92-1 and MB92-1B b 1C.

Geological observations by F. H. Toews , geologist , are documented on pages G I , G II and GS1 - GSVI in the appendix.

WORK DONE

Reference; Summary Report on VLF-EM Survey, ReconnaissanceGeological surveying, Prospecting b Sampling , Bisley Township Project (OPAP Initiatives) by Frank P. Tagliamonte , P.Eng. St Frank H. Toews , Geologist , January 1992.

Claim Staking; Map B92-A shows the claims that have beenindependently staked during 1992 by the applicants (FPT S FHT) following the 1991 exploration program. The staking was designed to enclose both VLF-EM anomalies located on the ground during the 1991 exploration program and extensions of the anomalies into adjacent unexplored ground.

The staking was also designed to enclose airborne magnetic closures that may be reflecting kimberlite structures.

Personnel; Frank P.Tagliamonte Project Area BisleyTownship

Frank P. Tagliamonte , P.Eng. - Frank H. Toews , Geologist

Frank H. Toews Project Area Townships

Applicant assistant

Bisley S Melba

Frank H. Toews , Geologist - Applicant Frank P. Tagliamonte , P.Eng. - assistant


Project Area; The respective Project Areas are as outlined on

the following maps:

MAP B 92 - A and MAP B 92 - A and

MAPS B92-1 St B92-2 : FPT MAPS MB92-1 Se MB92-2 : FHT

Work Period;

Grid Control:

Work began during the month of June and was carried out in approximate l week segments (weather permitting) at intervals during the period June - October 1992.

North-South blazed and chained compass control grid lines with 100' interval flagged stations were established by extending East-West base lines used during the 1991 exploration program. Grid line intervals varied from 100'(locally) to generally 400 and 600' within most of the Project Area.

The grid was established simultaneously with VLF- EM surveying and geological reconnaissance observations. Follow-up prospecting and sampling was done in areas of particular interest.

Conventional cut picket lines were used to accommodate Max-Min EM and Magnetic surveying in both project areas. These lines are shown on the Magnetometer and Max-Min Recce. Survey plans.

Total miles surveyed:

FPT Project Area:

FHT Project Area:

11.0 miles +-

5.8 +- miles( 2.0 +- miles picket lines )5.3 +- miles( 1.5 +- miles picket lines )

Geological Observations; Supplementary geological reconnaissance

observations and preliminary prospecting were performed simultaneously with grid development and geophysical surveying.

Geological reconnaissance data prepared by F. H. Toews is included in an appendix to this report.

VLF-EM Surveying; Instrument:

Parameters:Crone Radem VLF-EM Dip Angle - degrees


Out of Phase - t of normal fieldTransmitters: SW , Seattle , Washington 24.8 KHz

CM , Culter , Maine 17.8 KHz AM , Annapolis , Maryland 21.4 KHz

ReadingInterval: 100'Operator: F. P. TagliamonteAssistant: F. H. ToewsTotal ReadingsRecorded: 976 4 ( check and repeat readings

not recorded ) 515 *- FPT Project area 416 4 FHT Project area

Processing: Fraser Filter

A Crone Radem VLF-EM unit was used utilizing three (3) transmitter stations as indicated on the VLF- EM Survey Plans. Three stations were used for two specific reasons. One was to achieve optimum coupling and the second was to use whatever station was transmitting at the time survey operations were in progress so that there would be no delay in the survey program.

Two transmitter stations were read routinely at each grid point. A total of three stations were read when all three transmitters were operating.

Dip angle and Out of Phase readings were taken at each 100* interval station along grid lines. Dip angle readings have been processed by the Fraser Filter method to produce Filter Numbers which are recorded on the plans and used to produce contoured closures.

Out of Phase readings were booked but do not appear on the maps.Grid control operations were carried out simultaneous with the VLF-EM surveying.

Max-MinSurvey:

Operator: G. Couture , Val d'Or Assistant: Frank P. Tagliamonte Instrument: Apex Max-Min II ; # 555 Frequencies used: 444 , 1777 , 3555 KHz Coil Separation: 300' Reading Interval: 100' Total Readings Recorded: 1206 +-

750 FPT Project area 456 FHT Project area


Magnetometer Survey:

Sampling:

Documentation: Shown on Plans S profiles The Max-Min survey was essentially a profile type coverage over peak portions of what was deduced to be the best VLF-EM anomalies obtained during the 1991 exploration program, (see Map B91-1)

Max-Min profiles were run on the following lines:

FPT Project Area : Lines 'A 1 'B 1 61W 67Wand part of 52W ( East claim line - L 980240 )

FHT Pro j ect Area : Lines 94W , 106W , 'C' and part of 108W.Readings taken are documented on plans and sections included with this report.

Instrument: Parameters:

Base Station:Operator:Assistant:Stations:Total ReadingsRecorded:

Sharpe MF1 , # 601182Vertical component of earth'smagnetic fieldL-43+00 W ; 3+00 N ( 1100 g )F. H. ToewsF. P. Tagliamonte50 ' and 100' interval

527 *-262 FPT Project Area{ includes base line from 44Wto 102+25W )

265 FHT Project Area

Magnetometer readings were corrected for diurnal variation. Corrected readings are plotted on the plans and are shown as either unprocessed readings readings and contours or readings and profiles.

Four (4) samples were taken for analysis during work on the project. Details are documented in the appendix. Sample locations are shown on MAP B92-1A and Map B92-1E.

Broad areas of mineralization were noted on outcrop exposures within the North boundary of claims L-980240 and 842945 indicated by gossan patches . The South flank of the outcrop is strewn with mineralized float. Selected portions of some mineralized area were sampled in both the 1991 and 1992 programs.


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A gossan at the brecciated contact between diorite and volcanics adjacent to the road on claim L 1186153 contained pyrite in the matrix material which is prominently oxidized. Sample B92-4 was taken at this location.

Several samples were collected for possible rock geochemistry analysis. These samples are in storage for possible future use or geological observation.

Rock type samples have been collected from most of the specialty rock types encountered during prospecting and geological reconnaissance activities. These samples are stored for reference.

Sampling and assaying by F. H. Toews , FHT project area , are documented on sheet SI 6 S II and attached analysis data in the Appendix.

RESULTS OBTAINED

Geological Reconnaissance S Prospecting

Reconnaissance geological observations are recorded on Map B92-2 and MB92-2.

A description of geological observations is provided by geologist F.H.Toews in the Appendix on sheets GS I S GS II and GS I - GS VI for both the FPT and FHT project areas.

Geophysical Surveying

Most of the geophysical data collected is recorded on geophysical survey maps included with this report and cover both FPT and FHT project areas. These maps record individual readings some of which are Fraser Filter processed , are contoured or are profiled.

Three transmitter stations were utilized for VLF-EM surveying. The specific station used is indicated on the map. Two transmitter stations were routinely used and occasionally three stations were read.

Magnetic profiles were read to determine the magnetic characteristics over peak portions of VLF-EM anomalies obtained during both the 1991 and 1992 exploration programs. Similarly , Max-Min profiles were run over peak portions of VLF-EM anomalies to determine their conductive characteristics. Results are shown on the maps and summarized in this report.

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A brief resume of geophysical investigations and results obtained on both the FPT and FHT project areas follows. FPT Project Area

VLF-EM Survey : Maps B92-1 . B92-1B S C

Anomaly 'A 1 (1991) and '92A 1 appear to be the same anomaly. There is a gap in the Seattle (SW) and Annapolis (AN) Fraser Filter contours because one or other of the transmitter stations was shut down during portions of the survey procedure. A break or offset in the Northwest trend of the anomaly appears to occur about L 12W. Some detailing may ultimately be required here. The anomaly may be traversed by an East-West or NNortheast fault in this locale. These probable interpretations are shown on the maps.

The anomaly lies in a shallow depression which is in part swamp , but is flanked in places by exposures of pillowed volcanics , volcanics that are locally foliated and sheared and by volcanics that appear to have some felsic affinities.

Fraser Filter processing of the Seattle (SW) and Cutler (CM) VLF-EM readings suggest that anomaly 'A 1 (1991) may be open to the Southeast. The anomaly here lies within a cedar swamp adjacent to Intermediate volcanics.

Anomaly '92B' has been located by extending the 1991 VLF-EM survey. It has not been closed to the West.

This anomaly lies in a localized wet swamp basin. The extreme East end of the anomaly lies adjacent to volcanics which are intruded by diorite.

Anomaly '92C' is only partly defined and will require detailing to close it off. It lies in flat swampy terrain. It may be an offset of the '92B 1 anomaly.

A few satellite anomalies are partly contoured but are undefined.

Magnetometer and Max-Min Recce. Surveys ; Maps B92-1A St ID

Grid lines 'A 1 S 'B 1 ( Map B92-1A ) have been traversed with Max- Min EM without significant results. Profiles for these lines are in the pocket of the report.

A very restricted partially defined magnetic closure with an average relief of about 1200 gammas + is associated with VLF-EM anomaly '92B 1 . Though there is no Max-Min EM response over this anomaly , it is of interest as a magnetic feature. Local definition magnetic surveying supplemented by VLF-EM surveying will be required to define this anomaly.


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Magnetic and Max-Min profiles along lines 61W and 67W ( Map B92- 1E ) did not produce significant anomalous responses.

Modestly elevated magnetic values are associated with VLF-EM anomaly 'E 1 . This anomaly lies within an area where hyaloclastite ( felsic tuff breccia ) is exposed.

VLF and Max-Min EM Survey ; Map B92-1E

A VLF and Max-Min EM survey was conducted along line 52W ( West boundary of claim L-980240 ) mainly to test the response of this EM equipment over areas of known mineralization. Peperite exposures in the outcrop area are prominently gossaned and contain patchy sulphide mineralization , mainly pyrite with minor pyrrhotite in amounts up to about 5%.

Two VLF-EM conductors were located during this survey. Both Annapolis (AM) and Cutler (CM) transmitters were used and EM conductors were located with each.

A 1988 drill hole at about 31+00 +- South appears to have intersected part of the southernmost VLF-EM anomaly. Bands of sulphide mineralization were intersected in the hole but no significant values in precious or base metals were obtained. Selected sampling of some drill core did detect local sodium depletion.

No significant Max-Min response was obtained over the mineralized peperite unit or over the VLF-EM anomalies.

The line was not profiled with the magnetometer.

FHT Project Area

VLF-EM Surveys : Map MB92-1 ; MB92-1B S 1C

Extended VLF-EM surveying detected extensions of anomaly 'P 1 (1991) and defined and partially defined new anomalies 'MB92-A' , 'MB92-B 1 , "MB92-C 1 , and 'MB92-D 1 . These anomalies have been Fraser Filter processed to produce contours that better define them.

Three transmitter stations were read when available and at least two were routinely employed. It was not possible to utilize the same transmitter for the whole coverage area since different stations transmit at different time and work periods were not compatible with these variants. Both Cutler (CM) and Seattle (SW) , though on different frequencies are oriented approximately in the same field and were used to produce Fraser Filter contours on


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some maps.

Max-Min EM and Magnetic profiles have been run over portions of all the anomalies except 'MB92-B 1 .

A brief review of the VLF-EM anomalies follows:

Anomaly 'MB92-A' lies in a trough area between outcrop ridges and appears to lie along the North edge of it's Southern outcrop ridge. The anomaly extends Easterly off the property. There are no significant magnetic or Max-Min responses on this anomaly. A structural feature is indicated. The West end of the anomaly may abut a postulated NNEast fault structure.

Anomaly 'MB92B 1 is partially defined and is situated on the West boundary of the property. It may extend to the West. No magnetic or Max-Min profiles have been run over this anomaly.

The East end of anomaly 'MB92-C 1 overlies peperite formation which is variably mineralized with patchy sulphides , mainly pyrite and minor associated pyrrhotite. The outcrop exposure is variably gossaned. A diabase dike trends NEasterly through the East end of the anomaly.

There are some local , relative magnetic high and low readings within the South flank of the anomaly which may be due to the diabase dike or to pyrrhotite in the peperite. Pyrrhotite is present in minor amounts within sulphide patches in the peperite.

Max-Min EM did not respond over this anomaly or the weakly mineralized peperite formation associated with it.

Anomaly 'MB92-D 1 may be the NWesterly extension of anomaly 'P 1 (1991) . It appears to terminate West of line 106W but some detail work will be required to completely define the anomaly. The anomaly may be offset slightly by a postulated NNEast fault. The East end of the anomaly lies between two outcrop ridges and extends beyond the claim. A structural feature is implied.

A modest relief of about 150 gammas is indicated from the magnetic profile over a portion of the anomaly. A very weak Max- Min response is indicated on the line 'C 1 profiles from the 3555 KHz frequency.

Magnetometer S Max-Min Recce. Surveys ; Map MB92-1A

Magnetic profiles over most of the VLF-EM anomalies suggest that there is no direct correlation with local magnetic relief and the VLF-EM anomalies , except for anomaly 'MB92-C 1 . Elevated readings adjacent to the 'MB92-C 1 anomaly are likely caused by local pyrrhotite mineralization in peperite formation or by magnetite in a diabase dike that cut through the anomaly.


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Weak Max-Min responses are indicated on the profiles of line 'C 1 , line 106W and line 108W. These responses are more clearly shown on the 3555 KHz frequency and are confirmed on the 1777 KHz frequency which may suggest a possible weak bedrock response. The line 106W profile 'Max-Min anomaly 1 overlies VLF-EM anomaly 1 MB92-D 1 which may be the possible Westerly extension of VLF-EM anomaly 'P 1 (1991) . A possible bedrock influence is conjectured.

The line 108W profile 'Max-Min anomaly 1 lies adjacent to VLF-EM anomaly 'MB92-C'. This was a reconnaissance profile but nevertheless is associated with the mineralized peperite formation and may be significant as a possible bedrock response.

Max-Min responses at the top end of line C are generally co incident with VLF-EM anomalies obtained during the 1991 program. These Fraser Filter anomalies are designated 'M 1 S 'N 1 on Map B91-1. Max-Min responses probably overlie or are adjacent to VLF- EM anomaly 'N 1 . A bedrock source is conjectured.

VLF-EM anomaly locations are indicated on the Max-Min profiles.

CONCLUSIONS AND RECOMMENDATIONS

FPT Project Area

VLF-EM anomalies shown on Maps B92-1B St 1C and Map B92-1E are deduced to reflect bedrock structures , possibly faults , fractures or shear zones. Max-Min results imply that there are no massive sulphides associated with those anomalies that have been profiled.

A magnetic closure associated with VLF-EM anomaly '92B 1 will require follow-up VLF-EM and Magnetic surveying on 100' interval grid lines to define and evaluate it. A Pulse EM or IP profile test may ultimately be necessary to further investigate the anomaly. A kimberlite source is a remote possibility.

The Max-Min profile over the mineralized peperite unit documented on Map B92-1E confirms that Max-Min does not respond to disseminated type mineralization.

Magnetic closures indicated on government maps occur within and NEast of Maps B91-1 and B92-1. They may represent targets for ground magnetic surveying to search for kimberlite structures.

Follow up exploration , both geological and geophysical is recommended for those anomalies that have not been adequately explained by the work completed to date.

A ground magnetic survey investigation of airborne magnetic


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closures is also recommended to search for currently popular kimberlite structures.Airborne magnetic maps indicate that there are magnetic closures on the FPT Project Area property immediately NEast of Map92-l. A ground magnetic survey to define these features is recommended. Kimberlite host structures are a possibility.

FHT Project Area

VLF-EM anomalies shown on Maps MB92-1 and MB92-1B St 1C are deduced to reflect bedrock structures such as faults, fractures or shear zones.

Some Max-Min responses on or in the vicinity of VLF-EM anomalies 'MB92-C' , 'MB92-D 1 and 'M' b 'N' (1991) may reflect mineralized bedrock sources that should perhaps be investigated by more specialized techniques such as Pulse or IP profiles. Patchy mineralization , mainly pyrite , is associated with VLF-EM anomaly 'MB92-C 1 though assays obtained from samples taken are marginally anomalous in copper and zinc.

The VLF-EM anomaly identified as 'P 1 (1991) and 'MB92-A 1 extends Easterly off the property. It is of special interest since there is a circular airborne magnetic closure on the adjacent claim group that is to be investigated as a kimberlite structure.

Respectfully submitted,

5 F. P. 1AGL1AMQKTEtol SI

lamonte , P.Eng

Frank H. Toews , Geologist

20 January 1993

Revised 25 May 1992

APPENDIX

Table of Lithologic Units

Melba 8. Bisley Twps*

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Photo Copy Excerpt:

Melbo-Bisley Townships

ODM Geological Report 103Geology of Melba and Bisley Townships ,Distrit of Timiskamingby: L. S. Jensen1972page 4

Toble 2 TABLE OF LITHOLOGIC UNITS MELBA AND BISLEY TOWNSHIPS

CENOZOIC

RECENT

Peat, alluvium

PLEISTOCENE

Gravel, sand, silt, varved clay

Unconformity

PRECAMBRIAN

ARCHEAN

LATE MAFIC INTRUSIVE ROCKS

Quartz diabase (dikes)

Intrusive Contact

FELSIC INTRUSIVE ROCKS

Hornblende diorite, monzonite porphyry

Intrusive Contact

EARLY MAFIC INTRUSIVE ROCKS

Gabbro, quartz gabbro, hornblende gabbro

Intrusive Contact

FELSIC VOLCANIC ROCKS

Pillow lava, flow breccia, pyroclastic rocks u

INTERMEDIATE VOLCANIC AND SEDIMENTARY ROCKS*/

Massive lava, pillow lava, flow breccia, pyroclastic rocks, argillite *

MAFIC VOLCANIC ROCKS

Basalt, andesite, massive lava, pillow lava, flow breccia

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APPENDIX

OPAP INITIATIVES Bisley Township Project Area

F.P.Tagliaroonte Project Area Data

1) Sample S Assay sheets (5)

2) Photo Folios (2)

IfillTMTl

M

Au .Mn RgCec.51..:"

Swastika LaboratoriesA Division of Assayers Corporation Ltd.

l EM** 1928 Assaying -Consulting -Representation

Geochemical Analysis Certificate 2W-0687-RG1Company: F. TAGLIAMONTE Date: JUL-13-92

l Project: Copy 1. 29 BEAVER CRES, N.B. ONTARIO P1A 3N1Ann:

I We hereby certify the following Geochemical Analysis of 2 ROCK samples submitted JUL-08-92 by .

Sample Au Ag Cu Zn Number PPB PIM PIM PIM

lB92-1 10 0.2 139 158 B92-2 Nil 0.1 51 122

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.LP.O. Box 10, Swastika, Ontario POK1TO

Telephone (705) 642-3244. FAX. (705)642-3300

BELL-WHITE ANALYTICAL LABORATORIES LTD.P.O. BOX 1 87, POJ 1KO

HAILEYBURY, ONTARIO TEL: 672-31O7FAX: (7O5) 672-5843

QJrrttfirat? of Analysis180

feAMPLE(S) OF: Rock(l)

SAMPLE(S) FROM: Mr - Frank P. Tagliamonte

DATE: August 05, 1992

RECEIVED: August 1992

Ample

J2-3

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Au ppb

Cu pprn

Zn ppm

Ag ppm

237 32 196 14

ICCORDANCE WITH LON&-ESTABLISHEO NORTH CUSTOM. UNLESS IT IS SPECIFICALLY STATED

E COLD AND HLVER VALUES MEPORTED ON TMtW SMETTS HAVE NOT VEEN ADJUSTED TO COMPEN- ATC rOR LOCSES AND CAINS INHERENT IN THE riRE

ASSAY PMOCCSS.

l

BELL-WHITE ANALYTICAL LABORATORIES LTD.

Pot

ACCURASSAY LABORATORIESA DIVISION OF BARRINGER LABORATORIES LIMITED, REXDALE, ONTARIO

BOX 426KIRKLAND LAKE, ONTARIO, CANADA P2N 3J1

TEL.: (705) 567-3361

President: Dr. GEORGE DUNCAN, M Se, Ph D . c. Chem lom.i. c Chem iu K.i. M etc, M.R.S.C., A R.c.s.T.

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45982 Certificate of AnalysisFrank TagliamonteGeological Engineering Service29 Beaver CrescentNorth Bay, Ontariop'lA 3N1

Page": 1

September 21 92

SAMPLE NUMBERS

tccurassay Customer

5965959659

B92-4 B92-4

LMO

1

Work Order * Project

Gold Gold ppb Oz/T

<5 ^.001<5 <0.001 Check

920324

Per: ^ Jufaj^

ORIGINAL



TEL.: (705) 567-3361

President: Dr. GEORGE DUNCAN, M.SC.. Ph D . c Chem iOm i, c Chem IU.K.I. M c i c , M R se. A R c s T

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45921 Certificate of Rnolysis

Frank TagliamonteGeological Engineering Service29 Beaver CrescentNorth Bay, OntarioP1A 3N1

Page :

September 23

SAMPLE NUMBERS Accurassay Customer

Silver ppm

259659 B92-4

Work Order Project

Copper ppm

76

920324

Zinc ppm

37

Per:

92

ORIGINAL


OPAP Initiatives F- H, Toews Project Area

PEPERITE EXPOSURES Patchy gossan g dissem. sulphides

Photos: MB-5 , -6 , -7Anomaly MB92-C

(see Map u1B92-1B for location)

OPAP Initiatives Tagliamonte Project Area

PEPERITE EXPOSURE Patchy gossan 8, dissem^ sulphides

Photo: B-1Adjacent VLF-EM anomalies

(undefined)

(see Map B92-1E for Location)

fpt

li ,-,"-V.'- \

OPAP Initiatives F 0 H 0 Toews Project Area

INTERMEDIATE VOLCANICS EXPOSURE

Photo: B-3 Faint gossan sparse pyrite

Adjacent to Anomaly P(1991)

see Map MB92-1B for location) fpt

APPENDIX

OPAP INITIATIVES

l l l l l l ll Bisley S Melba Townships Project Area

F. H. Toews Project Area Data

Is

(F.P.Tagliamonte project Area)

l 1) Geology Supplements ( GI &GII ; GSI - GSVI )

2) Sampling S Assaying ( SI - Sil and Certificates of m Analysis )

3) Photo Folio (1)

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BISLEY E, MELEA TOWNSHIP PROJECTS

COPAP Initiatives:'

EEDLDEY E l

Eeneral

Bisley Township was previously mapped by L.S. Jensen (197E, D.D,11. Report ER 103 with accompanying Hap EE5EJ along with the adjoining township of Delba to the west. Both townships are underlain mainly by Archean age volcanic rocks of the Blake River Group consisting of mafic to Felsic lavas, pyroclastics and minor associated sedimentary rocks. These are intruded by gabbroic bodies and by dikes of diorite and monzonite porphyry. Younger dikes of Matachewan Diabase are also present, as are bodies of kimberlitic rocks.

Unconsolidated deposits of sand, gravel and clayCPleistocene age) as well as alluvium and peat (Recent) mantle the bedrock.

The bedrock lies within a synclinorium which opens to the east and is cut mainly by northwesterly- and northeasterly- trending faults. Uery low-grade regional metamorphism has been imposed upon the bedrock.

In Melba Township, approximately l km. southwesterly of the Bisley project areas, a sulfide prospect at the contact of felsic pyroclastics and intermediate lavas contains pyrite and some chalcopyrite mineralization. Another copper bearing prospect also occurs l.E km. west-southwesterly of the project areas. The Melba Gold Hine, in the northwest quadrant of Melba Township, has been the subject of surface and underground exploration in the past.

Local(See MAPS B9E-E E, MB9E-E)

Bedrock outcrops as low knolls and as exposures on low hills, the highest point occurring near the north end of L-5BU. Maximum relief in the project area is estimated to be about 150 feet C50 metres?. The area has been recently logged, mainly for spruce and some poplar. Uegetation is indicated on the map, as are the areas of cutting. Overburden consists of forest soil, swamp deposits and local exposures of gravel and sand. A gravel pit is located to the east of the southern part of L-5EU). An intermittent stream, up to B feet C3 metres) wide, drains the low swampy area found south of the main baseline.

In order to provide continuity, some of the 1931 geology

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B IIwith revisions is plotted on the 199E? maps.

Geclcgical reconnaissance observations and prospecting indicated that the predominant rock types underlying the project area are intermediate volcanics Candesitic-dacitic) consisting oF massive, amygduloidal and pillowed lavas, Flow breccias and some pyroclastics. Dacitic, and possibly" more Felsic rock types, appear to be more prevalent in-the outcrops Found in the southwest part oF the project area. Lapilli tuFF is exposed south oF ULF Anomaly 'I'C 1991 Survey."), L-"B'V7N, north oF L-40U fi -46UJ, between the south ends oF L-BEUJ S -BBU1, BL-14S/107U end L-110LU/17 . 5S . TuFF breccia outcrops near the northwest end oF ULF Anomaly 'ISTC1991 Survey). A sulFide-mineral ized, gosssaned unit, a sample oF which was identiFied as "Peperite" by Dr. L.S. Jensen oF the O.B.S., occurs in the vicinity oF L-106W/17S and L-5EW/17S, associated with ULF Anomaly 'ME9E-C' C199E Survey.") in the First case. The extent oF this unit in the project area could not be determined due to overburden and vegetation.

Possible Felsic volcanics occur near the north end oF L-18U). Lapilli in some oF the tuFFs appear to represent more Felsic types and are indicated on the maps. Boulders oF sulFide-mineralized rhyoliteC?) were Found west oF L-9BU/30S. Locally, east oF L-98UJ/E1S, possible Felsic dike(s) trends ENE and appears to biFircate within the maFic volcanics.

MaFic volcanic Cbasaltic) rocks are massive, amygduloidal and pillowed lavas and Flow breccias which can be interbedded with the intermediate varieties, However, isolated exposures were observed, and in the southern portion oF the project area a zone oF predominately maFic volcanics occurs.

The volcanic rocks host exposures oF east-west to northeasterly-trending diorite bodies and diabase dikes in the project areas. One diorite body is associated with ULF Anomaly 'L' C1991 Survey."*, and another occurs on L-5E, north oF the road. Outcrops oF diabase dike trend NNE From Helba into Bisley Township. A body oF gabbro occurs on the southwest Flank oF ULF Anomaly 'B'C1991 Survey), at the south end oF L-3EUI. Contacts oF the intrusive rocks are mainly obscured by overburden, brush, trees or tree stumps in logged areas.

Additional notes on the local geology are Found below under Results Obtained.


BS I RESULTS DETAINED

Geological Surveying C Reconnaissance)

(See mPS BSE-E B MBSE-E)

Rock Descriptions

nafic volcanic weathering surfaces are grey to rusty in appearance while the fresh rock is a der): grey to greenish-grey in color. These often massive rocks are aphanitic to fine grained, ftmygdules are rounded to ovoid in shape, 1-5 mm in size, and contain carbonate and/or quartz. Pillow selvages are up to E inches (5 cm) in thickness, surrounding elliptical pillows up to 4 feet C l.E m) in size. The mafic volcanics are non-magnetic where tested.

The intermediate volcanic flows and pillow lavas weather grey, are medium to light grey to greenish-grey in color, and are aphanitic to fine grained. Rounded to ovoid amygdules, 1-5 mm in size, are filled with carbonate and/or quartz mineralization. Pillows vary from 0.5-5 feet CO.15-1.5 m) in size, are generally elliptical in shape, and have chlorite +/- carbonate -t-/- epidote in selvages O.E5-E inches (0.6-5 cm) thick. Some brecciation of pillow margins can be seen, and some brecciated pillows were noted. Quartz- carbonate veinlets are sometimes visible in coolingC?) fractures in pillows. Possible pillow fragments occur in outcrop with flow breccia. Photo E shows flow breccia from the west side of the hill near Baseline IMS/ 107 + 50U).

Pyroclastic lithologies are classified according to the following fragment size ranges : breccia OE4 mm) , lapilli tuff C64-E mm) and tuff (XE mm), Most appear to be intermediate volcanics Candesitic-dacitic) although more felsic rock types Chard, siliceous) appear to be present in some outcrops. Fragments are angular to sub-rounded, aphanitic to fine grained, and light to medium grey to pale greenish in color. The matrix consists of the smaller size fraction of lithic material, crystal fragments, sometimes chlorite and/or carbonate, and occasionally pisoliths and chloritized shards are recognized. Matrix and fragment supported varieties can be seen. Outcrops weather grey to beige to rusty brown.

The gossaned unit, or 'PEPERITE', is an heterogenous unit which is rusty to brownish-grey weathering (Photo 1.) The matrix is medium to light grey, fine grained, tuffaceousC?), moderately to fairly hard (partly silicified?), and is amygdaloidal in part. Possible pumice


GS II

Fragments can be observed. Distinctive, very Fine grained to aphanitic, black, rounded to irregular clots and patches end irregular to ragged veinlets cF metasedimentary C?} material can occur in the matrix. Disseminations and blebs oF pyrite, pyrrhotite and occasional chalcopyrite are present in the matrix in amounts of 1/2 to locally 5";. Minor quartz veinlets also can be found in the 'Peperite'. Geochemistry indicates that copper and zinc values are present, and that the unit appears to be andesitic. CSee be l oiu. J

Felsic dikeCs.i weather beige to tan, are fine grained and light grey in colour. Some quartz veinlets are present in the dikes as well.

The diorite is grey weathering, Fine to medium grained, light to medium greenish-grey with 10-20"; amphibole. Traces of pyrite may be observed. Epidotisation is sometimes present.

Outcrops of diabase weather to a rusty brown. The diabase is fine grained and dark grey to medium grained and medium grey in color. The rocks are generally magnetic and become finer grained (chilled) as the contacts are approached.

The gabbro is grey weathering, dark to medium greenish grey, medium grained, with black hornblende and saussuritic feldspar.

Mineralization

Generally, traces to l"; fine disseminated pyrite can be observed in the volcanics and the intrusive bodies.

Three areas of more prominent sulfide mineralization were encountered during the 1992 reconnaissance survey. In the eastern part of the FPT project area between L.-5E and L-9E north of the road, disseminated pyrite occurs in the matrix of brecciated, gossaned contact of volcanics and diorite. Low values of copper and zinc were obtained in the sample CB92-4}. The second area of interest occurs near L-5EW where rusty outcrops of 'Peperite' are found along uiith brecciated, pillowed, amygduloidal volcanics. The outcrops are pyritic and mineralized float also occurs on a talus slope below the outcrops. A sample CB92-13 of 'Peperite' contained up to 139 ppm copper and 158 ppm zinc. To the west, in Melba Township, the third area of sulfide mineralization was observed in the FHT project area. Outcrops and float of the gossaned unit contain 'Peperite' with <1^i to Ssi disseminations, blebs and streaks of pyrrhotite and pyrite (minor rare chalcopyrite^. The


BS III

pyrrhotite can be megnetic. The unit is associated with the 1392 ULF Anomaly f1E9E-C . Samples taken from outcrop and From float contained up to 160 ppm copper, 190 ppm zinc end minor gold values C eg. sample nEL9E-QE:t .

In addition, boulders of siliceous, felsic Crhyolitic ?) volcanics with <Es'i veinlets and disseminations of pyrite ujere noted and sampled from a location at about 30S, between L-9BW and the Bisley-flelba Township boundary (semple EIS9E-01-FJ . The source of the boulders is not known and low base metal contents are present.

Alteration

Uisible alteration in the volcanics includes epidotization, saussuritization, chloritization, carbonatization and silicification, as indicated on the MAP B9E-E and HB9E-E .

Structure

Structural measurements obtained are plotted on MAP E9E-E and MB9E-E.

Pleasured foliations are generaly steeply dipping and mainly trend from ENE to ESE .

Postulated faults may be reflected by topography and/or by geophysics, as indicated on both the geological and the geophysical maps. Postulated structures are shown to trend northwesterly to northeasterly. The one defined fault, west of L-110W/EES appears to offset the northern contact of the northeasterly trending diabase dike along a north-south depression on HAP MB3E-E .

Possible southerly facing pillow directions were observed on L-4EUJ, north of the main baseline.

Geochemistry

Four samples were obtained in the FHT project area for preliminary whole rock analysis. The sample locations are plotted on MAP MB9E-E; two are from Melba and two samples come from Bisley Township, and all sample numbers have the prefix 'WR' . The oxide and trace element data are tabulated on the attached sheet CES

One of the samples CWR-MELSE-OE) is from the gossaned unit C 'Peperite '5 in Helba Township; the other three straddle the 199E ULF Anomaly "P", near the Bisley-flelba Township boundary, and appeared to be intermediate-f elsic volcanics in the field.


GS IU

GEDCHEMICAL ANALYSESEISLEY-MELEA TOWNSHIP WHOLE ROCK CWR - PREFIX'' SAMPLES

Frank H. TDBUJS Project Area COPAP. 199E!'

Major Element Oxides

EIS9E-01 EIS9E-OE MEL9E-01 riEL9E-OE

SIDETIDEA1E03FeEOSCT)MnOHgDCaONaEOKEOPE05CrED3BaOSrDLOI

53.890.9E

15.955. 750.151 .91

11 .965. BE0.110.09O.EBO.E30.01E. 50

59.11O.BB

13.345.980.09E. 81

11 .103.5E0.010.130.37O.OE0.01E. 10

55. 3B1 .05

15. S37.E50.134 .898.514.E30.400.130.2E0.03O.OEE. 40

53. 4EO.BB

1B.E4B.OB0.114.34B. 984.E50.37o.ieO.E3O.EBO.OEE. 40

Total 99.34 99.46 100.45 99.64

Trace Elements

ppm Ba Sr UCr CD Ni Cu Zn Pb Ag Au O O O O

<l3

117341El14343131

O.E

1IE74464EE9150903

0.3

153178EB91867397E4

O.B

135

1E1347El31639315

0.7


BS U

Geochemistry, ctd.

A Jensen Cation Plot of the oxides cf total iron * titanium aluminum and magnesium appears to indicate that rocks have a tholeitic affinity and are geochemically classified as follows: U.'R-EIS9E-01 Dacite

UR-EI99E-OE AndesiteLi'R-nELSE-Ql AndesiteUJR-hELSE-OE Andesite

The samples obtained were cleaned cf the weathering rind and contained as little sulfide Ctrace to l".; and oxidized fracturing as possible. The samples were generally fine grained and differences are noted as Follows:

WR-EISSB-01 - darker to medium grey with light grey hard bands, minor epidote?

WR-EIS9B-OE - light grey, fairly hard, few felsic lapilli visible, occasional quartz amygdule

UR-nEL9E-01 - medium-light grey with slightly greenish cast, few quartz-chlorite fracture fills medium hardness

WR-MEL9E-OE - medium grey with light grey, siliceous patches, E', white-grey quartz amygdules ~5". very fine grained, hard black blebs, rags 8, veinlet-like material

Uolcanic Rocks: Jensen Cation PlotBislev-Helba Tups.-ftw Data (QPflP.1992)

Fe203(T) 4 JiQS

LEGEND

Bl : Whole Rock Sample tt UR BI59E-01BE : " " " tt UR BIS3E-OEMl : " " " tt UIR MEL9E-01NE : " " " tt WR HEL3E-OE

m in


Sampling and Assays

In the FHT project area Five rock samples were submitted for geochemical analysis for copper, zinc, silver and gold content, cf which something has been mentioned under "!1i neral izetion" .

One sample is from boulders of B siliceous felsic volcanic west of L-9BUJ 7 305 in Bisley Twp., and four were collected from outcrops and boulders of the gossaned unit ('Peperite') in tlelba Twp.

Sample numbers and locations are plotted on fi A P MB9S-E .

The following table lists the semple data.


C-.-"- ,--.*.--- -i . fc. . - ~ - M^C p lpl - 2 ~,.

rey.pstc":-, ::i:c;'::;t::- r ,EC!re blebs l ve:r!ets o* blacf chsrtv" JJtErial, 1-2/; blebs t- :iEr?r:r,-ctEC Fyrr*-Ct;tE 4 F\'r;tf| SeUctEC ESffflE

^ F'yrite; ccfpCEite f! flost ssrplEE

F-yrrhctite S- ^'^te; curt: \E:^et; fcojlder

cCEEa^s: L-.it rFEpr'itr 1.; 3art t: light grey Nit 1- E l 1AO 74 EDte tit.; i e CLiert: erycc^les i sere tlacl- tlefcs li veinlfitE; 1-21 rscs ! :iESBir.:pstB: Pyrrhotite J- Pyrite */- Chclcop^itE! Selertec: ssirple

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ACCURASSAY LABORATORIESA DIVISION OF BARRINGER LABORATORIES LIMITED. REXDALE. ONTARIO


TEL.: (705) 567-3361

President: Dr. GEORGE DUNCAN, M.SC . Ph D . c. cnem (Om i. c Chem ;U.K.I. M c i.c . M.R s c.. A.R c ST.

Certificate of AnalysisFrank H. Toews HWY. 537, RR #3 Sudbury, Ontario P3E 4N1

Page #3


258960 WR-BIS 92-01258961 WR-BIS 92-02258962 WR-MEL 92-01258963 WR-MEL 92-02




258960 WR-BIS 92-01258961 WR-BIS 92-02258962 WR-MEL 92-01258963 WR-MEL 92-02.

SiO2

Ha2O

5. 623. 524. 234. 25

BaO

0.227 0.018 0.034 O. 277

A1203

K20

0.110.010.400.37

Cr2O3

0.284 0.374 0-.220 0.232

August 26, 1992

Work Order # : 920272

Fe203 MgO CaO

5.725.987.258.02

P205*

0.0900. 1330. 1290.117

SrO

0.0080.0060.0220.017

'er:

1 .912.814.894.34

Ti02Sfe

0.9210.8611 .0490. 860

LOI

2.52. 12.42.4

Sv' Av, s

/#Xi r^ ' 'v

•~~ l'}'-

Y&Xw

y

11 .9611 . 108.518.98

MnO*

0. 1500.0930. 1270. 113

TOTAL

99.399.5

100.599.6

^!C -'^;x^ "N-::-\-ioPTFriCrJ V''~\-l,^! li L 'J^^J. \'.\

'O . L .- ' i 1--;- 1' . ~-';

CHEMIST""/^/ v^IIx^ ^~ -^"^

'/fJfA/JU^OCtAA.

ORIGINAL

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ACCURASSAY LABORATORIESA DIVISION OF BARRINGER LABORATORIES LIMITED. REXDALE, ONTARIO


TEL.: (705) 567-3361

President: Dr. GEORGE DUNCAN, M.SC . PH D . c. Chem iom i. c. Chem IU.K i. M c.i c . M.R.s c A.R.c.s.T.

Certificate of AnalysisFrank H. Toews HWY. 537, RR #3 Sudbury, Ontario P3E 4N1

Page #1




258960258961258962258963

WR-BIS 92-01 WR-BIS 92-02WK-MEL 92-01 WR-MEL 92-02


258960258961258962258963

WR-BIS 92-01 WR-BIS 92-02 WR-MEL 92-01 WR-MEL 92-02


Mo ppm

122l

Ni ppm

143916791

Au ppm

O O O O

Bi ppm

258960258.961258962258963

WR-BIS WR-BIS WR-MEL WR-MEL

IF-30

Cu ppm

43503963

Co ppm

21221821

Hg ppm

o o^3 O

V ppm

1177478

121

August 26, 1992

Work Order # : 920272

Pbppm

<234

15

Mnppm

448363544653

Srppm

31231

5

CaSfe

3.602.37I.. 56 '2.22

Znppm

13907293

Fe*

2.343. 113. 324. 32

Cdppm

1111

P*

0.060.040.060.05

Agppm

0.20.30.80.7

Asppm

29

1514

Sbppm

223

<2

Lappm

3344

X//*er: -X^* /jfjLJLn^ C Gr^tA.

SORIGINAL



TEL.: (705) 567-3361

President: Dr. GEORGE DUNCAN, M.SC.. Ph. o., c Chem lOmj, c. cnem iu K.I, M c i c , M.R.s.c., A R.c s.T.

l Certificate of Analysis Frank H. Toews Page #2

HWY. 537, RR #3 August 26, 1992 Sudbury, Ontario P3E 4N1 Work Order # : 920272

I Cr Mg Ba Ti AlSAMPLE NUMBERS ppm * ppm * *

Accurassay Customer

1 258960 WR-BIS 92-01 341 0.36 <l 0.26 2.51258961 WR-BIS 92-02 464 0.81 l 0.15 2.11258962 WR-MEL 92-01 289 1.65 15 0.24 2.66258963 WR-MEL 92-02 347 1.70 13 0.24 3.47

Na Si W BeSAMPLE NUMBERS Sfe Sfe ppm ppm

Accurassay Customer258960 WR-BIS 92-01 0.12 0.01 2 3

B 258961 WR-BIS 92-02 0.08 0.01 10 2l 258962 WR-MEL 92-01 0.23 0.01 5 2 258963 WR-MEL 92-02 0.27 0.02 3 3

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ORIGINAL

Swastika LaboratoriesA Division of Assayers Corporation Ltd.

Assaying - Consulting - Representation

l Geochemical Analysis Certificate 2W-0689-RG1

Company: FRANK H. TOEWS Date: JUL-13-92

I Project: Attn:

I We hereby certify the following Geochemical Analysis of l ROCK samples submitted JUL-08-92 by .

Sample Au Cu Zn

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l Certified by jL jGYUy^q CgSO^

P.O. Box 10, Swastika, Ontario POK 1TO j B . Telephone (705) 642-3244. FAX (705)642-3300

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TEL.: (705) 567-3361

President: Dr. GEORGE DUNCAN, M.SC., Ph. o., c. cnem ou, c. cnem IU.K.I, M.C.I c . M.R.s.c., A R c.s.T.

Certificate of Analysis

Toews, Mr. Frank HWY.537, RR# 3 Sudbury, Ontario P3E 4N1

;

SAMPLE NUMBERS curassay Customer

158956 58957 58958 ^58959 58959

MEL 92-02MEL 92-02-CMEL 92-03-F

MEL 92-04MEL 92-04

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lLF-30

Gold ppb

34 169

<58

Page :

August 5 92

Work Order # Project

Gold O?, X T

0.001

Check

920271

<0.001 <0.001

Per: s? /Oju^

ORIGINAL

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ACCURASSAY LABORATORIESA DIVISION OF BARRINGER LABORATORIES LIMITED. REXDALE. ONTARIO


TEL.: (705) 567-3361

President: Dr. GEORGE DUNCAN, M.SC , PH. D., c. Chem .O.H.I. c. cue tu K i. M.c.i.c .MRS c.. A R c s T.

Certificate of Analysis

Toews, Mr. Frank HWY.537, RR# 3 Sudbury, Ontario P3E 4N1


K8956 258957

P 8958 8959

MEL 92-02 MEL 92-02-C MEL 92-03-F

MEL 92-04

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Silver ppm

2221

Page

August 5 92

Work Order Project

Copper ppm

16012054

140

: 920271

Per:

Zinc ppm

190170

6674

Q Dr. G. Duncan S]

ORIGINAL

SCALE: 1 INCH ' 40 CHAINS

utr3000 4000

O 2OO MITNES

1000 11 KM)

1000(a KM)

HAP^ B 92TOCATION————

- A

PROECT AREA

•— F.P, Tagliamonte Project Area *~--' - * .. , ,.J f

BARNET TWP. THACKERAY TVVP.

1166335 XT

JI86165

! \ i i*- — •'•i—T" — —— •••"••"y! u IT 1- 'i. 7 i \j i-

^________J. w-r

—-/.v/ J t.

TOWNSHIPPART'OF8M

VBISLEY G-3I9I

M.N.R. ADMINISTRATIVE DISTRICT

KIRKLAND LAKEMINING DIVISION

LARDER LAKELAND TITLES/ REGISTRY DIVISION

COCHRANE _~m

TO ACCOMPANY MAPS AND 'MB

LEGENDIntrusive RocKs

.2. I 5095D i Q b ase

Diorite

Ga b b ro

Vol can t c Rocks

Felsic01 - U f\ d i f f erent i ated b - Rhyolite ( Boulders)

Intermediate 'a- Uvia/ffe b - Tuff c- Lap.' Hi Tuff .4- Pill

(Andesite -Dacite)

•f -Flow 0recc\Cvg -Tuff Breccia. ;h -Gossanec\ Ur."t

M a-f (ca- IMdi f ferenti a ted C Basa l fie)b - TuffC- Lapllli Tuffd - P; (lo \veol . ,6,- Amyo duloid a l ^•p - Flow Breccia

fc.o

co

Q UP -

S.U8.

SYMBOLSj

Small ou4trop ; area, of outcrop ' Sccirp (^acKures down slope) Contact w i -VV\ dip direction ; ajpptroximate assumed cov\tact"; pos&ible. contact StirlKe w(-Hr\ dip of fractures - Vert i cal , dip KKOWA ; direction

Probable-FauU-, possibles-fault Pillow iqva. with 4-0p

o-p g labial p j Becks/er Daw\,

Ba.se o^ slope, or hill

U

li

M II

trees

Uir\e-

Line. Po si"

ip Line ^- Survey Bar Hax-MinU Survey i

0IS R2.-OI A?,say sample, rv uVVR, MEL C?2.-0'5 WUole Rock Av\a.lysis Sample number

; Carbo^at i

Ffipd -Epidote, Fe

C 'p P o Py

co py r i~- Py rv Notite.-. Pyrite

8/2.^-14,-

'^ 4*.

IR SETP, P,TA6MAM0NTfc OPAP PfcTCeCT

VLF-EN\

'* rlfl f'j

MAP MB92

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33S-S141 METRIC

Ontario 42A08SE9907 2.15095 BISLEY 900

Ministry ofNorthern Developmentand Mines

Ministere duD6veloppement du Nord et des Mines

Geoscience Approvals Section 933 Ramsey Lake Road 6th Floor Sudbury, Ontario P3E 6B5

September 14, 1993Telephone: Fax:

(705) 670-5853 (705) 670-5863

Our File: 2.15095 Transaction #: W9380.00173

Mining Recorder Ministry of Northern Development and Mines 4 Goverment Road East Kirkland Lake, Ontario P2N 1A2

Dear Sir/Madam:

Subject: APPROVAL OF ASSESSMENT WORK CREDITS ON MINING CLAIMS L1185337 ET AL IN BISLEY AND MELBA TOWNSHIPS

The assessment work credits for Geology, Section 12, Geophysics, Section 14 and Assays, Section 17 of the Mining Act Regulations, have been approved as originally filed.

The approval date is September 8, 1993.

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

J^ LJ/dm

cc: Resident GeologistKirkland Lake, Ontario

Assessment Files Library //' Toronto, Ontario

Ministry ofNorthern Developmentend Mines

Report of Work Conducted After Recording Claim

Mining Act

Transaction Number

UQOntario ( ,

Sk _Personal Information collected on this form It obtained under the authority of the Mining Ad. Tnl* Information will be ueed for correspondence. Question* about thie Collection should be directed to the Provincial Manager, Mining Lands, Ministry of Northern Development and Mines, Fourth Floor, 159 Cedaj Stre Sudbury, Ontario, P3E 6A6, telephone (705) 870-7204. - ~ /\

l 5 GInstructions: - 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.

Work Performed (Check One Work Group Only)Work Group Type

Geotechnical SurveyPhysical Work, Including Drilling

Rehabilitation RECEIVED"Other Authorized Work JUL 1 4 1993Assays

MIAssignment from Reserve

Total Assessment Work Claimed on the Attached Statement of Costs 3Note: 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)

(attach a schedule If neceseary)

Certification of Beneficial Interest * See Note No. 1 on reverse side

Certification of Work Reportl certify that l have a personal knowledge of the facts set forth in this Work report, having performed the work or witnessed same during and/or after He completion end annexed report Is true.

Name and Address of Pereon Certifying

IVEDLARDER LAKEFor Office Use Only_^_^__

Total Value Cr. Recorded l Date Recorded

JUN l 4 W93Deemed Approval Date

DatrNottde for Amendments Sent

l certify 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 beneficial Interest by the current recorded holder.

0841(0*81)

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Ontario

Ministry ofNorthern Developmentand Mines

dudu Nord

et des mines

Statement of Costs for Assessment Creditfetat des coOts aux fins du credit d'evaluatlon

Mining Act/Lol sur les mines

Transaction No./N 0 de transaction

2. 15095Personal information collected on this form is obtained under the authority of the Mining Act. This information will be used to maintain a record and ongoing status of the mining claim(s). Questions about this collection should be directed to the Provincial Manager, Minings Lands, Ministry of Northern Development and Mines, 4th Floor, 159 Cedar Street, Sudbury, Ontario P3E 6A5. telephone (705) 670-7264.

Les renseignements personnels contenus dans la presents formule sont recueillis en vertu de la Lol sur le* mines et serviront a tenir b jour un registre des concessions minieres. Adresser toute quesiton sur la collece de ces renseignements au chef provincial des terrains miniers, ministers du Developpement du Nord et des Mines, 159, rue Cedar, 4e etage, Sudbury (Ontario) P3E 6A5, telephone (705) 670-7264.

1. Direct Costs/CoQts directs

Type

Wages Salalres

Contractor's snd Consultant's Fees Droltsde ('entrepreneur et d* ('expert-COO90I1

Supplies UsedFoumrturesutlllse+s

Equipment Rental Location d* materiel

Description

Labour Main-d'oeuvreField SupervisionKPT Supervision sur le tffj^r

Type

Type

JUL

ivlNING i.KiNDv/

Amount Montant

572Y&totas*

993

Total Direct Costs Total des coOts directs

Totals Total global

flKI*

Note: The recorded holder will be required to verify expenditures claimed in this statement of costs within 30 days of a request for verification. If verification is not made, the Minister may reject for assessment work all or part of the assessment work submitted.

2. Indirect Costs/Couts Indlrects* * Note: When claiming Rehabilitation work Indirect costs are not

allowable as assessment work. Pour le remboursement des travaux de rehabilitation, les couts indirects ne sont pas admisslbles en tant que travaux d'evaluation.

Type

Transportation Transport

Food and Lodging Nourrlture et hebergementMobilization snd Demobilization Mobilisation et demobilisation

Description Amount Montant

Totals Total global

Sub Total of Indirect Costs Total partlel des coOts Indirect!

Amount Allowable (not greater than 20H of Direct Costs) ( Montant admissible (n'excedsnt pas 20 H des coOts direct!)Total Value of Assessment Credit (Total of Direct and Allowable Indirect cottt)

Vsleur totale du creditdevaluation(Total d** coott dlrtctstt Indlrtctt tdmlttlbltt

Note : Le titulaire enregistre sera tenu de verifier les depenses demandees dans le present etat des couts dans les 30 jours suivant une demande a cet effet. Si la verification n'est pas effectuee, le ministre peut rejeter tout ou une partie des travaux d'evaluatlon presentes.

Filing Discounts

1. Work filed within two years of completion is claimed at tOO'to of the above Total Value of Assessment Credit.

Remises pour depot

1. Les travaux deposes dans les deux ans suivant leur achievement sont rembourses a 100 "ft de la valeur totale susmenttonnee du credit d'evaluatkxi.

2. Work filed three, four or five years after completion is claimed at 500/fo of the above Total Value of Assessment Credit. See calculations below:

Total Value of Assessment Credit Total Assessment Claimedx 0.50

2. Les travaux deposes trois, quatre ou cinq ans apres leur achevement sont rembourses a 50 •to de la valeur totale du credit devaluation susmentionne. Voir les calculs ci-dessous.

Valeur totale du credit devaluation Evaluation totale demandeex 0,50 -

Certification Verifying Statement of Costs Attestation de I'itat des couts

l hereby certify:that the amounts shown are as accurate as possible and these costs were incurred while conducting assessment work on the lands shown on the accompanying Report of Work form.

that as(Recorded Holder, Agent, Position in Company)

to make this certification

J'atteste par la presente :que les montants indiques sont le plus exact possible et que ces depenses ont ete engagees pour effectuer les travaux devaluation sur les terrains indiques dans la formule de rapport de travail ci-joint.

l am authorized Et qu'a litre de je suis autorise(titulaire enregistre, representant, poste occup* dans la compagnie)

a faire cette attestation.

0212 (04/91) Nota : Dans cette formule

Date

f y- (mines, le masculln est i i au sens neutre.

TRIM LINE

REFERENCESAREAS WITHDRAWN FHOM DISPOSITION

KLItO. - MWING RK2HTVONLY

4.R.O. - SURFACE RIGHTS ONLYM.+ S. -MINING AND SURFACE RIGHTS

Order No. DM* D Milton PH*

THE INFORMATION TKAT APPEARS ON THIS MAP HAS BEEN COMPILED FROM VARIOUS SOURCES AND ACCURACY IS NO" GUARANTEED THOSE WISHING TO STAKE WIN ING CLAIMS SHOULD CON SUIT WITH THE MINING RECORDER, MINISTRY OF NORTHERN DEVELOP MENT AND MINES, FOR AD DITIONAL INFORMATION ON THE STATUS OF THE LANDS SHOWN HEREON

NOTICE OF FORESTRY ACTIVITYTHIS TOWNSHIP ; AREA r ALLS WITHIN THE ———

^AND MAY BE SUBJECT TO FORESTRY OPERATIONS. THE MNR UNIT FORESTER FOR THIS AREA CAN BECONTACTED At: P.O. BOX 129

SWASTIKA, ONT.POK ITO 705-642-3222

BARNET TWP. THACKERAY TWP.

OD-l UJ

IHGG48 l—————— \ 861651(06192 -IIBSISB j 1186337

I0454T5 l 1045478 l K)4S479

118673^ .l^-L^r^^^.'

^X^-Cd. ---l !86257 i.L 115io7 Q I.JI8665I l xx.^ j

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86436 tr----:7--T-

M86258

COPY OF THIS MYLAR ARCH'VED NOV 26/91

MORRISETTE TWP. CO 'V OF THIS MYl.Ar ARC H.Vf ON JULY 17/92

LEGENDHIGHWAY AND ROUTE No. OTHER ROADSTRAILSSURVEYED LINES:

TOWNSHIPS, BASE LINES, ETC.LOTS, MINING CLAIMS, PAR&LS, ETC

UNSURVEYEO LINES:LOT LINESPARCEL BOUNDARYMINING CLAIMS ETC.

RAILWAY AND RIGHT OF WAY UTILITY LINES NON-PERENNIAL STREAM FLOODING OR FLOODING RIGHTS SUBDIVISION OR COMPOSITE PLAN RESERVATIONS ORIGINAL SHORELINE MARSH OR MUSKEG MINES TRAVERSE MONUMENT

DISPOSITION OF CROWN LANDS

TYPE OF DOCUMENT SYMBOLPATENT, SURFACE ft MINING RIGHTS —................ 0

" , SURFACE RIGHTS ONLY........................ C" , MINING RIGHTSONUY ___.......,........... Q

LEASE, SURFACE ft MINING RIGHTS....-..-.........™ H" .SURFACE RIGHTS ONLY.......................... B" . MINING RIGHTS ONLY.:.........,.,.............. O

LICENCE OF OCCUPATION ,._........,................. TOWOER-IN-COUNCIL .....—...,.......................... OCRISERVATION .—..............,.^..^......,....,..... ©CANCELLED ——....................................... 9

SAND A GRAVEL ._.....___.......................,.. ©

MOTE: MINING RIGHTS IN PARCf LS PATENTED PRIOR TO MAV C. 1913. VESTED IN ORIGINAL PATENTEE gY THE PU1LIC LANDS ACT, fl.S.O 1970. CHAP 1M, tiC *3, SUBSEC 1.

SCALE: 1 INCH = 40 CHAINS

FEETO 10OO 20OO 4000 6OOO •000

O 200 METRES

10OO(1 KM)

20OO(2 KM!

TOWNSHIP

BISLEYM.N.R. ADMINISTRATIVE l

KIRKLAND LAKEMINING DIVISION

LARDER LAKELAND TITLES/ REGISTRY

COCHRANE

JUL l 4 1993

MINING

DATE OF ISSUE

JUL 12 1993

LARDER LAKE

Ministry of LandNatural Management

Resources BranchOntario

••t* JANUARY 1985Nimbtf

G-3I9I

42A08SE9907 2.15095 BISLEY

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