mackelcan and rathbun townships properties sudbury area o ...€¦ · summary report on extended...

SUMMARY REPORT

ON

EXTENDED DIAMOND DRILL PROGRAM

(Wolf Lake Sector)

Mackelcan and Rathbun Townships Properties

Sudbury Area

Ontario

O 0

for

FLAG RESOURCES LIMITED

(Wolf Lake Joint Venture)

by

Frank P. Tagliamonte, P. Eng. GEOLOGICAL ENGINEERING SERVICES

NORTH BAY Ontario

February

1984

*----

41MSSE0ei5 MACKELCAN27 MACKELCAN 010C

CONTENTS

page

INTRODUCTION AND SUMMARY . . , . . . . . . . . . . . . . . . . . . . . . . . . . l.

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

COMP?*NIES ......... .... . . .. .... .. . . .. ... ... . . . . . . .. .. 3 .

LOCATION ......... .. ... . . ... . ..... . .. . .. ..... .. . .. .. .. 3.

ACCESS ...... . ... .... . . .. . . . . . . .. ... .. . .. . . . . .. ...... 3.

TOPOGRAPHY .......................................... 6.

HISTORY AND DEVELOPMENT ..................... . . . . . . . . 6.

Early li.

Recent 6.

GEOLOGY . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . T.

General 7.

Local 7.

Showings 10.

DIAMOND DRILL PROGRAM . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 11.

SHOWING DESCRIPTION AND COMMENTARY ............ . . . . . . 12.

No. l Zone 12.

Camp Zone 13.

Shaft Zone 14.

No. 2 Zone 14.SUMMARY AND CONCLUSIONS ..................... . . . . . . . . 15 .

CONTENTS ( continued)

page

RECOMMENDATIONS

REFERENCES

16.

i.

Table No. l

Tables

Huronian Formations 8.

Figure No. l

Figure No. 2

Figure No. 3

Figure No. 4

Figure No. 6

Figure No. 7

Figure No. 8

Figure No. 9

Figures

Index Map

Claim Group Location Map

- Claim Location Map

Local Geology Map

Regional Geology Map

- Composite DDH Plan

DDH Plan1 No. l Zone

- Diamond Drill Hole Plan

4.

5.

in pocket

in pocket

in pocket

in pocket

in pocket

in pocket

Diamond Drill Hole Sections (3) in pocket

SUMMARY REPORT

ON

EXTENDED DIAMOND DRILL PROGRAM

(Wolf Lake Sector)Mackelcan and Rathbun Townships Properties

Sudbury Area Ontario

for


Wolf Lake Joint Venture

INTRODUCTIONANDSUMMARY This report has been prepared at the

request of Murdo C. McLeod, President, FLAG RESOURCES LIMITED, Calgary, Alberta.

The report summarizes a series of short drill holes which probed the vicinity of the No. l and Camp Zones as well as the deepening of one hole and a probe of the West edge of the No. 2 Zone.

A brief gross resume of the regional and local geology is made as well as descriptions of the showings and showing structures on the point at Wolf lake.

This report is an adjunct to a report dated January 1984 which summarized all the drilling done on the Mackelcan township property by FLAG RESOURCES LIMITED during 1983 except for the extended drilling done between November and December 1983 on the point at Wolf

,-fl*- 2.

lake. Some of the material used in the January 1984 report has been revised and used in parts of this report. Several of the maps have also been used.

A total of 1,745' of drilling was completed in 7 short holes plus the deepening of another hole. Direct field costs for the extended drilling portion of t'ne program amounted to $40 / 144.45.

DDH IWL83-41 intersected a long section of mineralization in the Camp Zone structure. The best gold intersection was:

.42 02 Au/9'

The best gold and copper intersection was:

.04 oz Au, Cu/9.5 1

To date, mineralization encountered on parts of the No. 1-Camp-Shaft-No. 2 Zone'structure is rich but local and restricted in extent. Mineralized intersections obtained nevertheless demonstrated that areas of en- ichment are present in this particular structure and are likely to occur in other mineralized structures on the property.

Some selective I.P. surveying and cross- trenching is recommended prior to proceeding with further drill probes on the structure.

PROPERTY 568 Unpatented Mining Claims 22,720 acres - approximately Sudbury Mining Division Ontario

30 optioned claims - Mackelcan township 367 staked claims - Mackelcan township 171 staked claims - Rathbun township

See Figures No. 2 and No. 3.

COMPANIES

3.


Wolf Lake Joint VentureMackelcan and Rathbun townshipspropertiesSudbury Mining DivisionOntario

Flag Resources Limited Golden Briar Mines Ltd.

- 60i

LOCATION

ACCESS

Wolf Lake

Approximate centre of Mackelcan township, Approximate centre of North quadrant of claim group. 30 miles NEast of Sudbury, Ontario

See Figures No. l, No. 2, and No. 3.

Aircraft i

Float plane from Ramsey Lake - Sudbury.

Roads

No direct road links.

Nearest road on South terminates at Rathbun lake about 7 miles South of the camps on Wolf lake.

Nearest access on North are bush roads that terminate on Dewdney lake about 3 miles North of the camp on Wolf lake.

Nearest road on West about 5 miles West of camp on Wolf lake.

Snow track vehicle access possible a distance of about 7 miles up the North arm of Matagamasi lake into Jones and Wolf lakes from road end at Rathbun lake.

Boat and Canoe

From Dewdney lake on North to Wolf lake.

From Matagamasi lake on South to Wolf lake.

4.

LOCATION MAP Scale: l: 1 584 000 or 1 inch to 25 miles


Wolf Lake Joint VentureMackelcan S Rathbun Townships Properties

Sudbury AreaOntario

INDEX MAP

DATE: February FIGURE NO


*

Uolf Lake Joint VentureMackelcan S Rathbun Townships Properties

Sudbury AreaOntario

CLAIM GROUP LOCATION MAP

DATE: February 19BI*

If!

MACKELCAN TWP.

FIGURE NO 2

568 MINING CLAIM GROUP

WOLF LAKE PROJECT AREA

MACKELCAN — RATHBUN TWPS.

234

KILOMETRES ^ .

From FLAG RESOURCES LIMITED Annual Report ( 30 April 1981

6.

TOPOGRAPHY Rugged in the general area.

Low ridges on point and West side of Wolf lake with the most pronounced elevation at about 150'.

The point and West side of Wolf lake wooded with stately red pine in a park-like setting.

Labrador tee, spruce, cedar and mixed birch and poplar make up the vegetation cover in the valleys and flats between the hills and ridges.

HISTORY AND DEVELOPMENT

Recent

1973

1979

1980

1981

Wolf Lake Sector - Mackelcan township

Shallow inclined shaft near point. Adjacent stripping and hand trenching.

Wolf Lake Sector - Mackelcan township

Four (4) shallow packsack holes on No. lZone.Intersections with gold and coppervalues in all but l hole.Some rock trenching.

Local geochemical surveying and sampling by P.A.R. Brown over peninsula on West side of Wolf lake.

Modest trenching on No; l, No. 2 and No. 3 Zones.

Property Examination report by Frederick C. Charlton, M.Se., F.G.A.C. for A.E. Jerome.

Property Examination report by C.T. Bischoff, P. Eng. for M.C. McLeod.

Ground I.P., magnetic and VLF electromagnetic surveying totalling 33.5 miles covering gold-bearing structures on Wolf, Jess and Jones lakes.

7.

Diamond1 drilling - 11,364' in 31 holes.

Most drilling done on No. l, No. 2 and No. 3 showings on Wolf Lake.

GEOLOGY

General

Local

Mackelcan township gold occurrences held by FLAG RESOURCES LIMITED are hosted by Lorrain quartzite formation, a member of the Cobalt Group (Lorrain and Gowganda formations), part of a larger sedimentary package of rocks classified as the Huronian Supergroup.

Huronian Supergroup sediments extend from Sault Ste. Marie Easterly through Elliot Lake and Sudbury then arch Northerly along the flank of the Grenville front through Mackelcan township fanning out to include parts of the Temagami, Cobalt, Elk lake, Englehart, Gowganda, Matachewan and Kirkland lake areas.

Some of the principal lithological units in the Huronian sequence are: quartzite, siltstone, arkose, argellite, greywacke, conglomerate, dolomite and limestone. Table No. l on page 8 lists the Huronian formations. It is taken from Energy Mines and Resources paper 68-40, by S.M. Roscoe.

Lorrain quartzite in the immediate showing areas in Mackelcan township, particularly at Wolf lake, are prominently bedded grey-green generally uniformly fine granular quartzites.

Local thin conglomeritic beds with rounded quartz pebbles up to about l" or less are common.

Fine hairlike alternating beds of black magnetite have been observed in the quartzite in some drill core and on an island in Wolf lake.

The gold occurrences at Wolf, Jess and Jones lakes are situated with .n the

8.

TABLE I

HURONIAN FORMATIONSGroup

sum

Quirke Lake

Hough1 it UM

ElliotLake

Formation

Bar River

Cordon Lake

UorraVr*

^^1^19d ow^ ot** AaSerpent

Espanola

Bruce

Mississagi

Pecors

Ramsay Lake

McKim

Mstinenda

Copper Cliff

Thessalon Pater StobieLivingstone

Creek

Composite lithoiogical sequence

juartcite, red siltstone juartxite *

varicoloured siltstone

quartzite

arkose

reddish argilliteargilliteconglomeratic greywacke, orev and oink arkose.arkose -subgreywacke

dolomite, siltstone siltstone, greywacke limestone

conglomeratic greywacke

coarse subarkose

argillite, siltstone

conglomeratic greywackesubgreywacke, argillite

gritty subarkose

acid volcanic*

basic volcanics

subarkose

From pas* B , by S. M. Roscoe.

Survey of Can Bda Paper 6fl-*0

9.

SEast sector of a large eliptical shaped basin of Lorrain quartzite measuring approximately 8 miles East-West by 14 miles North-South. Underlying the Lorrain quartzite are wackes of the Gowganda formation.

A maximum thickness in excess of 11,000' of Lorrain quartzite lies within the basin located in Mackelcan, Aylmer, Tefler and Mcconnell townships.

Numerous lineaments and fault structures bisect the basin. The lineaments are sometimes prominently evident in topography appearing as scarps and linear depressions that extend for considerable distance.

Bedded Lorrain quartzite segments have been tilted and rotated at various angles on either side of the lineaments and regional fault structures.

The tilting of quartzite beds is prominently displayed at Wolf lake where visual apparent rotation can be observed. For example, the beds on the point near the No. l Zone are inclined 56 0 Northerly. The beds on the East side of Wolf lake are inclined 09 0 Northerly and the beds on the West side of Wolf lake are inclined between 20 and 25 0 Northerly.

Sudbury type breccias appear to be localized along and adjacent to some of the lineaments, faults, and fracture zones. They are prominently exposed adjacent to some of the gold showings on Wolf, Jess and Jones lakes.

Pink arkosic quartzite and mineralized pink quartzite breccia are localized within and along some of the lineaments. They appear as rounded, oblong or tabular bodies.

Diabase dykes are associated with at least one lineament that trends NEasterly through Wolf lake. It is exposed in outcrop and has been noted in drill core.

10.

Showings

Approximately 3 0* of the terrain adjacent and surrounding Wolf, Jess and Jones lakes is outcrop. The predominant rock type is bedded grey-green granular Lorrain quartzite.

Figure No. 5 portrays some of the geological features alluded to here. They are illustrated in cartoon-like fashion on the geological map. Figure No. 6 illustrates the regional geology.

Gold mineralization appears to be localized within mineralized pink quartzite breccia zones and in hematized limonitic and kaolinitic fracture zones assobiated with the pink quartzite breccia.

Milk white quartz-carbonate veins and fragments comprise the matrix of the breccia.

Pyrite ,{non cubic) or marcasite ? is erratically disseminated in portions of the pink quartzite breccia. Occasionally, massive patches, lenses, or fragments of sulphides, mainly pyrite, over core lengths of 4 feet, have been intersected in drill holes.

Chalcopyrite is a common sulphide consistent in the No. l Zone, Camp Zone and parts of the No. 3 Zone. It appears to be a minor constituent in the No. 2 Zone and is virtually absent at Jess and Jones lakes.

Some carbonate minerals identified are calcite, ankerite and an apple green unidentified variety.

The No. l Zone and Camp Zone contain a deep blue mineral coating chalcopyrite which i-s tentatively identified as covellite.

Geothite occurs at the No. l Zone surface showing and has also been observed in drill core from the No. l and Camp Zones.

Native gold is common at the No. l Zone both in surface samples, pannings and drill core. Native gold has been observed in surface samples and drill core from

the No. 2 Zone. Gold can be panned and has been observed in drill core from the No. 3 Zone.

Variations are common and pervasive in the pink quartzite breccia zones. Some sections intersected in drill core contain generally narrow, but sometimes up to 2' widths of thinly bedded, fine grey-green granular quartzite beds and occasionally, fragments.

Chlorite is a frequent constituent in portions of the breccia zones. It occurs as chloritized quartz fragments , and as massive clots of dark green chlorite. The chlorite is both barren and pyfitic.

Textural and mineral content variations occur within the breccia zones over very short distances laterally and vertically.

Native gold, where observed, is associated with pyrite and/or chalcopyrite but appears to occur in the free state.

There appears to be no unfailing corellation between the amount of pyrite or chalcopyrite and gold values. Some sulphides must nevertheless be present in any section that yields gold.

DIAMOND DRILLPROGRAM An extended drill program was carried out

on the Camp Zone, Shaft Zone and No. 2 Zone during the period 9 November - 2 December 1983.

This extended drill program entailed drilling 7 short holes (WL83-39 - WL83-45) and deepening of l hole (WL81-17).

A total of 1,745' were drilled during the extended drilling program.

The holes are listed below:

DDHIWL83-39

DDH#WL83-40 207'

DDH#WL83-40 100' (deepened)

12.

DDH|\ . 83-41

DDH#WL83-42

DDH#WL83-43

DDH#WL81-83-17

DDH#WL83-44

DDHIWL8-3-45

Total

(deepened from 517-54?-')

V'*7 1.745'-

Direct on-site field drilling costs of $40,144.45 were incurred to complete the 1,745' of extended drilling. These costs do not include air transportation, assaying, engineering or overhead.

The extended drill program was directed and supervised by Murdo C. McLeod, President, FLAG RESOURCES LIMITED, assisted by A.E. Jerome, vendor-prospector.

Drill hole locations are shown on Figure No. 7 and No. 8.

Appendix A abstracts the intersections and geology as well as generally classify the drill holes.

SHOWINGDESCRIPTION AND COMMENTARY

No. l Zone The No. l Zone is a generally typical mineralized pink quartzite breccia comparable to the No. 3 Zone, Jess lake Zone and Jones lake Zones.

It is the best exposure on the property since it has attracted most of the attention of prospectors. Considerable local surface blasting has been done.

Angular, unsorted pink quartzite breccia liberally mineralized with pyrite (non cubic) chalcopyrite, and covellite? are exposed here. Matrix material comprises milk white quartz-carbonate fragments and gash veinlets, Minor amounts of geothite have been observed at surface and in drill core.

v^^vw-'^v?'^v--;tf ;;^;

13.

Camp Zone

Native gold is pervasive in the mineralized breccia. It can be panned with ease from fines and shoreline sediments. It is visible in hand specimens and drill core.

Some visual examples of large eliptical- form breccia fragments are observable where the breccia is in contact with Sudbury Brecciated host Lorrain Quartzite. There are also visual examples of pink quartzite permeating the host Lorrain quartzite somewhat like a metasomatic type alteration feature.

Assays from hand samples, composite samples and drill core have returned some high values up to 1.00 oz in gold and 2%-f in copper.

Se -eral random holes have been drilled on and in the vicinity of the No. l Zone. None of the drilling provides definitive data on which to interpret the configuration or tenor of the zone. It is nevertheless conjectured that the No. l Zone is a local lense lying along a branch or subsidiary "break" to the lineament projected through the Southwest structure, Lake Structure and No. 3 Zone. The same break or system of tight fractures are postulated to trend through the shaft area and the No. 2 Zone.

The No. l Zone provides an example of the type of high grade gold and copper likely to be. present in portions of, or directly in, mineralized pink quartzite breccias at Wolf lake and vicinity.

This is an atypical zone. Massive patches of chalcopyrite with associated pyrite occur with irregular quartz- carbonate veins and fragments in kaolinitic and hematitic stained Lorrain quartzite and Sudbury breccia. There appears to be considerable fracturing associated with the mineralization. Chalcopyrite is the predominant sulphide mineral.Quartz and carbonate gangue make up the largest percentage of host rock in the mineralized zone.

Camp Zone mineralization intersected in vertical discovery hole WLI 83-28 has been intersected in a series of sectional and vertical holes drilled on East-West and North-South sections. These are shown on the cross-sections in the pocket of this report.

The zone appears as a shallow 'octopus- like 1 blob of essentially mixed chalcopyrite and quartz-carbonate in a cross-fracture zone adjacent to the No. 1- No. 2 Zone lineament or fracture system.

An alternate possibility to explain the attitude of the mineralization is a NEasterly plunging, fracture controlled, cigar-shaped lense.

Figure No. 9 and the 3 DDK sections in the pocket of this report provide basic data on which to support alternate interpretations on the attitude and control, of the mineralization in the Camp Zone structure.

Shaft Zone The Shaft Zone appears in outcrop asa narrow silicified hematite stained, pyritic, quartz vein zone in a NEast striking Easterly dipping fracture cutting Sudbury brecciated Lorrain quartzite.

Gold values up to .50 oz Au have been obtained from chip and grab samples taken from surface exposures on the North edge of the shaft. Visible gold has been observed in excavated picked samples from dump material.

Hole WL# 81-83-17 drilled under the Shaft Zone did not intersect vein material or mineralization. Patchy areas of weakly kaolinitic and hematitic stained, quartzite appear at intervals throughout the length of the hole however.

No. 2 Zone A vertical hole drilled on the West edgeof the No. 2 Zone lineament sectioned Sudbury Breccia and bedded Lorrain quartzite.

15.

This zone appears to be localized along a subsidiary lineament or localized fracture zone that trends NEasterly through the Ne. l Zone, Camp Zone and Shaft Zone.

A small' pop blast location on one part of the No. 2 Zone exposes mineralized, kaolinitic, and hematitic stained quartzite. Fine visible gold has been observed in rock samples from the showing and in drill core from the vertical hole. Some hand samples contair glassy quartz in association with sulphides (non cubic pyrite).

Surface 'showings' are localized along a short section of outcrop on the East edge of a scarp that is the topographic expresssion of the No. 2 Zone lineament or fracture zone.

Sudbury breccia exposures flank the No. 2 Zone.

There are several areas along the No. 2 Zone that could easily be cross- trenched.

The No. 2 Zone has not been adequately investigated by drilling but cross- trenching and/or orientation drilling will be required to sort out structural control and the geological setting before a meaningful program of exploration drilling can be initiated.

SUMMARY AND CONCLUSIONS The extension drilling program was

essentially a series of random prospect drill hole probes in the vicinity of the No. l and Camp Zones to test the underlying rocks for extensions of the Camp Zone mineralization that may have been present.

The deepening of hole WL# 81-83-17 served to show that hematitic staining is pervasive over a long East-West section of the point on Wolf lake.

The significance of this is not certain. Drill results on other parts of the property suggest that hematitic staining, limonitic staining and kaolinitic alteration are proximal to mineralized pink quartzite breccias.

Hole WLi 83-45 drilled on the West flank of the No. 2 Zone lineament produced inconclusive results. It may support the hypothesis that No. 2 Zone fractures are inclined Easterly.

Apart from the No. l Zone, which appears to be a typical mineralized pink quartzite breccia, the remaining gold-bearing structures along the No. l-No. 2 Zone lineament are local fracture controlled structures impregnated with quartz, carbonate, and sulphides mainly chalcopyrite and pyrite with accessory covellite, geothite and occasionally native gold.

The Camp Zone appears to be localized in cross-fractures adjacent to the main NEast trending fracture system. A steep NEasterly plunging small irregular diameter cigar-shaped body may be present.

Results obtained from both surface trenching and in some drill holes suggest that significant values in gold and copper are present in local portions of the No. l -Camp-Shaft-No. 2 Zone structure.

A selected program of cross-trenching in readily accessible portions of the structure will help in interpreting the structural and geological setting as well as provide sample access points.

RECOMMENDATIONS A program of selected cross-trenching mapping and sampling is recommended for the No. 1-Camp-Shaft-No. 2 Zone structure prior to attempting either orientation or prospect drilling.

Selective, specialized I. P. surveying over the point, which will include the No. 3 Zone, may isolate target areas for either trenching or drilling,

lRespectively submitted,

17,

/" ^ ^\Frank P. Tagliamonte, P. Eng,

GEOLOGICAL ENGINEERING SERVICES

NORTH BAY Ontario

'S&i't'^i - . •.•Z'!.:'.:.- •••: ,'.-i•••1X:*--1- - - ' - '-:: - -: i

Tagliamonte, F.P. 1984

i.

REFERENCE

Summary Report on 1983 Diamond Drill Program, Mackelcan and Rathbun Townships Properties, Sudbury Area, Ontario, FLAG RESOURCES LIMITED, Wolf Lake Joint Venture.

APPENDIXFLAG RESOURCES LIMITED

Mackelcan Township Gold Prospect Sudbury Area

Ontario

WOLF LAKE EXTENDED DDH PROGRAM

1983

Resume of DDH IntersectionsWL83 Series t

(see DDH Tlans for Locations)

DDH No. INCLINATION DEPTH

Camp Zone - Prospecting

WL83-39 -90" 207'

WL83-40 -90 0 307'

WL83-41 -70 0 267'

(includes

(includes( includes

WL83-42 -90 0 207'

AVERAGES FOOTAGE02 Au/Ft

(or core length sampled) From To

.078 oz

.079 oz

.138 oz

.208 oz

.42 oz

.040 oz

.081 oz

.119 oz

.042 oz

.002 oz

.004 oz

0 0

0 0

Au/102.5' 145.0 - 247.5 Au/100.5' 147.0 - 247.5Au/ 42.5' 205.0 - 247.5Au/ 23.5' 224.0 - 247.5Au/ 9.0* 224.0 - 233.0 )

Au, 1.52% Cu/77' 147.0 - 224.0 Au, 2.34% Cu/19' 166.5 - 185.5Au, 1.95* Cu/9.5 1 166.5 - 176.0 )Au, 4.40% Cu/9.5 1 176.0 - 185.6 )

Au, .01* Cu/10' 0.0 - 10.0 Au, .07* Cu/10' 10.0 - 20.0

REMARKS

Sectioned: Lorrain quartzite Sudbury Breccia

Sectioned: Lorrain quartzite Sudbury Breccia Hematitic L. Q. L. Q.

Gold values over sections sampled

Copper values over sections sampled

Sectioned: weakly mineralize' .Sudbury breccia

WL83-43 -90' 227'Lorrain quartzite

^Sectioned: Bedded Lorrain "quartzite with Sudbury Breccia fragments

A 2

AVERAGES FOOTAGE

DDH No. INCLINATION DEPTHoz Au/Ft

(or core length sampled) From To REMARKS

Camp Zone - Prospectiny (continued)

WL83-44 -90'

No. 2 Zone -Prospecting

102' Sectioned: Bedded Lorrain quartzite

WL83-45 -90' 200' Sectioned Sudbury breccia bedded Lorrain quartzite

Shaft Zone - Prospecting

WL81-83-17 -50' 230'

[hole deepened from 517* (19oi) to 747' (1983)1

Sectioned: Bedded hematitic Lorrain quartzite Random breccia fragments

p|r^?^p3-^*vjA"-*---v-ipti'-T;'-IcSw^i^^

NOTE: FOR DUPLICATE DETERMINATIONS

BY DIFFERENT METHOOSt VALUES

APPEAR IN ORDER OF LISTING

ON HEADER PAGE.

X-RAY ASSAY LABORATORIES LIMITED

LESLIE STREETt DON MILLSt ONTARIO M3B 3J4

PHONE 416-445-5755 TELEX 06-986947

CERTIFICATE OF ANALYSIS

TO: COOKSVILLE STEEL LTDATTN: SIDNEY MISZCZUK, PRESIDENT 510 HENSALL CIRCLE ^ ^ MISSISSAUGAt ONTARIO " *L5A 1Y1

REPORT 19988

CUSTOMER NO.

DATE SUBMITTED 8-DEC-83

755

REF. FILE 15655-K1

2 ROCKS

WERE ANALYSED AS FOLLOWS:

AU PP3AU 02/TONCO XNl tPT PPB30 ELEMENT

METHOD FADCP FA XRF XRF FADCP EMS

DETECTION LIMIT 2.000 0.001 0.010 0.010

10.000

DATE 21-D6C-83

X-RAY ASSAY LABORATORIES LIMITED*"W.''"^

CERTIFIED BY ..1

UNLESS INSTRUCTED OTHERWISE WE WILL DISCARD PULPS 180 DAYS AND REJECTS 90 DAYS FROM DATE OF THIS REPORT

X-RAY ASSAY LABORATORIES LIMITED

ESLIE STREETt DON MILLS* ONTARIO M38 3J4

PHONE 416-445-5755 TELEX 06-986947

CERTIFICATE OF ANALYSIS

\

REPORT 19988 REF. FILE 15655-K1

TO: COOKSVILLE STEEL LTDATTN: SIDNEY MiszczuKt PRESIDENT510 HENSALL CIRCLE MISSISSAUGA, ONTARIO L5A 1Y1 f , * AS?/?*? 2 R OCKS ' T SVt^-^JjMiHf'^j)/^,

^ ELEMENT SENS* fitTMEN

Zl-OEC-83

CUSTOMER NO. 755

DATE SUBMITTED 8-OEC-83

tt 2ANTIMONYARSENICBERYLLIUMBISMUTHCADMIUMCERIUMNIOBIUMCHROMIUMCOBALTCOPPERGALLIUMGERMANIUMIRONLEADLITHIUM

(41(4)(2](2 l(4J(5)(4](41(3(1(2(1(2(2(4

NDNDNONDNDNDNDTTtHFTNDHFTND

NDNONDNDNONDNOTLMFTFTNDHFTND

MANGANESEMERCURYMOLYBDENUMNICKELSILVERTANTALUMTHORIUMTINTITANIUMTUNGSTENURANIUMVANADIUMYTTRIUMZINCZIRCONIUM

(1)(4)(3)(1)(1)15)(3)(2)(2)(4)(3)(2)(3)(4)(4)

FTNDFTTFTNDNDFTFTNDNDFTNDNDND

FTNDFTTLNDNONDFTTNONDFTNDNDND

LEGEND

KEY TO SYMBOLS

H - 10* PLUS MH - 5-15*

M - i -lQ'4 LM - 0.5-5*

LTL

T FT

0.1-1* 0.04-0.5* 0.01-0. IX 0.01* OP. LESS

ND - NOT DETECTED

•^SENSITIVITY (LIMIT OF DETECTION)

1 - 0.0005-0.001*2 *- 0.001-0.005*3 - 0.005-0.01*4 - 0.01-0.05*5 - 0.05-0.1*

NOTE: SETTER SENSITIVITIES CAN BE OBTAINED WITH SPECIAL TECHNIQUES* IF AND WHEN REQUIRED.

.•Jk-'i y "-:'. - . •'-- ••.' '- ••- ' '" - -" ' '- "" ' •'-

ATORieS 21-OEC-83 REPtJRT 19988 REF.FILE; 15655-Kl PAGE l OF l

AU PPB AU OZ/TON CO * Nl't PT PPB

>10000 1500

0.660 0.070.37

0.010.04 OO

- CONCENTRATION TOO HIGH FOR TREATMENT BY GEOCHEMICAL METHOD

NO. 40363

SAMPLE (S) OF:

.SAMPLE(S) FROM:

-WHITE ANALYTICAL LABORATORIES LTD.O. BOX 187. HAILEYBURY. ONTARIO

of Analgma

TEL: 672-31O7

DATE: D ecember 5, 1983

Core(5) RECEIVED: December, 1983

Mr. F. Tagliamonte, Flag Resources Ltd.

Sample No.

WL-8341-10

WL-8341-11

WL-8341-12

WL-8342-1

WL-8342-2

Oz. Gold

0.420

0.056

0.123

0.002*

0.004

1 C opper

0.1

0.14

0.28

0.01

0.07

* Estimated

ACCORDANCC WITH LONO.tfTAlLISHCO NORTH CaiCAN CUtTOK, UNLCft IT II *PCCiriCALLY 1TATCO HCHWI*C GOLD AND IILVfH VALUE* StPORTCD ON CtC *HfITS HAVI NOT tltN ADJU5TID TO C OHflH. It fOH LO*ftl AND BAIN* 1NHCHCNT IN THC HBC

A**AV PMOCCM.

BELL-WHITE ANALYTICAL LABORATORIES LTD.

HITE ANALYTICAL LABORATORIES LTD.BOX 187. HA1LEYBURY. ONTARIO TEL: 672-3107

Qkrttftrat? of AtmlptsNO. 38946 DATE: November 23, 1983

SAMPLE(S) OF: Core(9) RECEIVED: November, 1983

SAMPLE(S) FROM: Mr. F. Tag 1 iamonte, Flag Resources Ltd.

Sample No.

WL 8341-1

2

3

4

5

6

7

8

9

f;-.; f' IN' ACCOHOANCl WITH CONO.ESTABLISHED NORTH

- AMIftlCAN CUSTOM, UNLESS IT It SPECIFICALLY STATED

, OTHCHWIlf OOID AND VILVtH VALUCt MEPORTEO OH ' THltl IHCtTI HAVC NOT CtCN ADJUtTCD TO COMPCN-

l AT f f OH kOlttt AND OAIN* INNCHtNT IN THC FIHC AflAV PMOCCft.

Oz. Gold

0.006

0.016

0.032

0.119

0.042

0.006

0.010

0.058

0.046

Copper

0.070

1.80

1.38

l .95

4.40

0.280

0.195

1.80

0.420

BEU..WHITE ANALYTICAL LABORATORIES LTD.

38

,O-f 5Oe 164-

A/6 l ZANZ y\*E,

36 29BEAVEP NORTH BAY. Or

—— .1. a?

30

33^54 !M 33

aa

36

FLAG RESOURCES LTD.

GeouecAi Encjxramw SomcoORESCENT TAMO PI A INI

Wolf Lake projectMackelcan township - Sudbury Area

OntarioDIAMOND DRILL HOLE PLAN

SCALE: 1:500 DATE: October 1983

FPT

Figure No 9

DRILL RECORD LOGGED BY Frank P. Tagliamonte, P. Eng.

PROPERTY Flag Resources Ltd. , Mackelcan, Ontario________________^_^_^___^

LATITUDE O * 22.35____ BEARING OF HOLE____^__________ STARTED 12 Nov. 1983

DEPARTURE. O -t- 6 6. 5E DIP OF HOLE -90' COMPLETED 13 Nov. 1983

DEPTH 207' (63.09m)

D.D.H. N0. WL83-39 PAGE l

f CLAIM No. S472927______

FI FVAT1QN20'± above Wolf LakeDIP TESTS ________fi————————^

CORE SI7F BQ___________DIAMOND DRILL CONTRACTOR Philippon Diamond Drilling Inc., Rouyn, Quebec

-DIRECTION AND DISTANCE FROM

NE. CLAIM POST

FOOTAGEFROM

0

2

117 +

TO

2

117 +

207

207

(63.09

*, , . ,; . DESCRI PTION *loaoed in feet

CASING

QUARTZITE Lorrain

Grey-green alternating" beds of fine, medium andgranular quartzite. Beddino @ 40 0 ±.Predominantly coarse grained granular quartzite occasional small conglomeratic pebbles.Numerous bedding plain fractures. Numerous low angle fractures from 15-35 0 .

QUARTZITE Lorrain Sudbury Breccia

Quartzite as above but with series of Sudbury Btype fragments distributed throughout. Beddino features absent.Sudbury Breccia fragments very fine grained to ; with, disseminated beads or "eyes" of fine silic*Locally micro fractures. Threadlike networks cuttinct the quartzite.Multiple fractures. Random 1/8" quartz stringers - some with finedisseminated pyrite. Ouartzite weaklv kaolinitic.

194 - 197 Multiple series of fractures @ 75 0 .

END OF HOLE

Casing in hole.

SAMPLE No.

coars

with

"eccia

imorph i .

FOOTAGEFROM

e

DUS

TOSAMPLE LENGTH

ASSAY

\l

/9//A

If*Ho F. P\*'r\--\\^

pFESs/s" ™ **i

MININ(

TAGltA.y

^-- —— 'c* o' 0

VV

).vrE 5 1"7 7

^

L'DIAl ' • -:-.-~f. :

PROPERTY

LATITUDE.

D DRILL RECORD LOGGED BY Frank P. Tagliamonte, P. Eng Resources Ltd., Mackelcan, Ontario

525

DEPARTVRE O * 54±E

BEARING OF HOLE

DIP OF HOLE

ELEVATION 1Q'

CORE SI7E BO

above level DIP TESTS of Wolf Lake

STARTED 14 Nov. 1983

COMPLETED 16 Nov. 1983

DEPTH 207'

D.D.H. No. WL33-40 PAGE

T C LAIM No. S472927


NE. CLAIM POST

DIAMOND DRILL CONTRACTOR Philippon Diamond Drilling ^J[iuebecFOOTAGE

FROM

0

10

64

105

TO

10

64

105

207

207-

*, , . f . D ESCRIPTION ipaaea^jLli-JLGjsi

CASING

QUARTZITE Lorrain

Alternating bed of coarse grained somewhat conaquartzite and fine grained quartzite. Vagup. bedding @ 20 0 .Fractures from 15-50 0 .

31.5 i" quartz stringer @ 70 0 ±.


Predominantly medium to coarse grained grey-gre Quartzite intermixed with swirly fragments of SQUARTZITE Bedded Hematitic

Vaguely bedded fine to medium grained predominagranular quartzite. Bedding @ 60 0±.25!i± random patchy areas of pale and deep hemat Pitted core surface in the hematitic zones andQuartzite weakly kaolinitic. Numerous beddino pi ain and low angle slips.Random thin black magnetite threads generally c t-hp bedding at intervals through the zone.

END OF HOLE

Hole deepened. 20 Nov. 1983 - 21 Nov. 1983

SAMPLE No.

lojaerj

;n grz isLbjir^

itly g

FOOTAGEFROM

tic

nular Erect

rey-g:

Ltic sjtainii matches.

xnformable i

TO

•een

ig.

:O

SAMPLE LENGTH

ASSAY

i

——

ISv\*'s

^^." M INI

P. TAGLI,

v^e* of

^\^\MOM? |~~2jJ

^GeoLOG.c*L ENCINCCRING SERVICES. 2 9 B EAVER CRESCENT. NOTTH BAY. CNTABIO

Frank P. Tagliamonte.

D.O.H.

FOOTAGEFMOM

207

290

TO '

290±

307

307

DESCRIPTION

QUARTZITE Bedded Hematitic

as per paqe 1 105'- 207'.

207 Series of limonitic stained slips from 35-45 0 .

2Q7 - 217 + Ash grey siliceous amorphous zone with streaksof charcoal grey - possibly fine magnetite.

254.5 2' band of finely bedded quartzite @ 60 0 .

QUARTZITE Bedded

Finely' bedded fine grained grey-green granular

Bedding @ 55 0 ±.

END OF HOLE

Casing in hole.

-

V

-

SAMP16 NO.

md pa

juartz

,

FOOTACE

FHOM

tches

ite.

TOSAMPLE LENGTH

ASSar

———

fi(s ila

-^

•^ctOFfO ' -^ —

XM .'rv

P. MCr1 ——— -* —— •"•^^

—— — - \

^'^^ ^ C* ^-

SffT^-V

•S*vN?,vr*\ *-~^J'••••Oiii*

i—~~J -a-^

! i-*r-.-:-^ --, :v ,.-Y' V '-"' 'V 1 ' ' '" '.

IlwPROPERT

LATITUDE

DEPARTU

ELEYATK

CORE SI2

r;--?.: , '...:--. - - :

VKIIV fiDII 1 Dt/T^DrV LOGGED BY Frank P. Taqliamonte, P. Ena.r Flag Resources Ltd. , Mackelcan . Ontario

- 0 * 22.3S BEARING OF HOLE Az 360 0 STARTED 16 Nov. 1983RF 0 * 66. 5E DIP OF HOLE -70 0 COMPLETED18 Nov. 19835 M 10'± above level of DIP TESTS ^ DEPTH 81.38 (267')

D. D. H. No. WL83-41 PAGE 1

T C LAIM No

-* ? ————— DIRECTIO

NE. CLAI

S472927

N AND DISTANCE FROM

M POST

-

Wolf Lake rf BQ DIAMOND DRILL CONTRACTOR Philippon Diamond Drillina Inc., Rouyn, Quebec

FOOTAGEFROM

0.00

1.22

24.38

40.54

TO

1.22

24.38

40.54t

±44.81±

.

DESCRIPTION

CASING

QUARTZITE Lorrain

Alternating beds of fine and foArê grînerigranular grey-green quartzite. Coarser beds appear somewhat- rongT omeri f-i f -random pearly semi-rounded 1/2-3/4" fragments. Beddina vaciue and not distinct.Occasional Sudbury Breccia fragments. Numerous low angle fractures.

9.75 Series of low anqle slips @ 25 0 with qouqe.11.43 12" limonitic stained zone.17.07 2.5' Sudbury Breccia fragment.


Somewhat aranular quartzite intermixed with fraof Sudbury Breccia.

24.38 - 28.96 Series of limonitic stained fractures - some at37.19 14" Sudbury Breccia fragment with limonitic and

Fractures generally from 35-65 0 .QUARTZITE Sudbury Breccia Hematitic Staining

Predominantly vesicular-like grey Sudbury Brecc intermixed with aranular quartzite .

SAMPLENo.

jmenii

lOW e

nema t

La f re

FOOTAGEFROM

ngles

itic

gment

TO

to co

;taini

;

SAMPLELENGTH

re.

:g.

ASSAY

i

/o

|5 T.

\ \

\,

r W |N"p. Mtim

V,2f* or

^v\•^ \ *\

~ÔNfe J

^/2^

P. Tagliamonte. P e*

D.D.H. NO. WL8 3 ~ 4 IpAGE_7

FOOTAGE^^BiFROM

40.54

44.81

TO -

t44.81*

±75.29

•^ DESCRIPTION

QUARTZITE Sudburv Breccia Hematitic Stainincr (continued)

Pronounced patchy areas of deeo hematltic stainPrincipal fractures @ 60 0 ±.

MINERALIZED ZONE

Intermixed zone of granular, occasionally finel conolomeritic quartzite and- irregular patchy a r*milk white quartz-carbonate containing small an of pink quartzite and irregular massive blebs crimmed with peacock blue covellite. Minor pyrite.3C^± patchy milk white quartz-carbonate. 101 h chalcopyrite in milk wh i tp quartsr-Mrhnnatwhich is locally vuggy. Granular quartzite portions of zone variably ka

Numerous low angle slips with slickensides @ 25

50.60 20 cm zone with vuggy quartz-carbonate.

53.95 - 50.44 40%± milk white quartz-carbonate.30%± massive chalcopyrite in quartz-carbonate.

- 56.54 - 64.31 Predominantly pale, weakly hematitic and limoni kaolinitic quartzite.Random irregular thin quartz veinlets with diss chalcopvrite and pyrite.Less than 2** sulphide.

60.81 Series of low angle slips with hematitic gouge

64.31 - 66.75 Random patches of very vuggy milk white quartz- intermixed with hematitic stained kaolinitic quVuggs coated with bright green malachite.

68.28 - 71.02 Visible Gold coated on pyrite at one location.

68.58 Possible fault or fracture zone. Crumbled and lost core.

64.31 15 cm zone with massive blebs of granular pyrit

SAMPLEMO.

inc.

yasgular f chai

p

olinit

0 ± .

tic st

eminat

e 35^1carbon artzit

(69.19

A

FOOTAGE

f BOM

f ragm copvr

ic.

ained

ed

-

ate e.

)

TO

;rits .te

SAMPLE LENGTH

ASS*/

/#l' L

Tt-frfi w\tC f-

\

^pf C33|i^*"^

MINIM

L TAGIIA;.

^^^**-t 0* l•*- — —

E?KfVA* i*\li'ONTc ffj

_ t 5)M

Frank P. Tagliainonte.

D.O.H. NO. WL-8.3-4.JpAG6__3-

FOOTAGEFMOM

44.81

75.29

TO

±75.29

81.38

-

81.38 (267 1 )

DESCRIPTION

MINERALIZED ZONE (continued)

67.97 - 69^80 Random sprier of slips wi t-h hpmAt-iM,- gonn^ ,

69.80 -71.63 8 0* vuqay micro fractured milk white quartz witfractures appearing as intersecting hair-like h Occasional patch of granular pyrite.

71.63 - 75.29 Kaolinitic quartzite with irregular small patchpyritic quarr zose fragments. Disseminated beads, streaks and patches of hemaRandom seams and fine patches of pyrite. 21± pyrite.

QUARTZITE Grey-Green Sudbury Breccia

Somewhat amorphous micro fractured quartzite wismall fragments of Sudbury Breccia. Random vaaue patrh^s and r-1 nst-^rc; of pearly whiconglomeritic quartz pebbles.

END OF HOLE

Casing in hole.

.

)

SAMPLE NO.

*

h mict;ematit

es of

tite.

th rar

te

FOOTAGE

FMOU

oe thr

qrev

dom

TO

;ads.

SAMPLE LENGTH

ASSAY

-

X*^

//ft~f-n — v- f ** 15 F.~T9 ———

Y S^

**~ —— *"JxO*""^/^* ""

MINIX

PL TAGUA:

V^"C* or

Qj^^

^Y\^ONTg Sj—— — IT!-''h^A

FLAG RESOURCES LTD.LJolf L ake P roject

Mackelcan township - Sudbury AreaOntario

DDH CROSS-SECTIONS

....3.pSCALE: 1:500

DATE: December 1983FPT /A

Ofo*;

__________Frank P. Tagliamonte.

O.O.M. NO. ^83-41 pACg 4

FROM TO

fly

DESCRIPTION

SAMPLING AND ASSAYING HLg

-

AVER

Samp

- —————————————— Safflf

Samp

Samp '

&LL . . . ,, .. . Samp It-^-tfW*''

SAMPLE NO.

-41- 1

- 2

- T

- A

- 5

- 6

- 7

- 8

- 9

-10

"11

~12

GES

es 2-5

.052lea 6 9

.03 oes 2-9

.041

Les 2-1J2-7D8-OZ

es 9-1 '

.208 )

FOCr BOM

44.20

44.81

visible Gold

incluj

)2 AU,

TTir-1i,JLLK. LU ;

z. Au,

incluj)z Au,

inchAu/ 1H

inrli .

z AU/::

HAGC TOi- "'

44.81

47, 8S

50.75

53.64

56.54

59.44

62.48

65.38

68.28

71.02

74.07

75.44

i ve

2.32J Ci

661^Cu

i ve

1.477. i

s i veny—fiiivf" 1

L5 f fl(

l s*Mn.E•JltMCTMj ~

.62

3.04

2.90

2.89

2.90

2.90

3.04

2.90

2.90

2.70

3.05

1.37

/38.5 1

38.5'f

A. f; --i—- -j- - ' --

.006

.016n-io

.119

.042

.006

.010

.058

.046

42

.056

^12JL.

rom 14

"Od 1 8 5

u/77* From 14

3m 224

~ ^4 1 .

- 9A7

-" _

' —— ~ —— .^^

- 18!

S -?-— * — r

1 - 22i

i

' — - — —

ASSAY

ZCu '

rt "7*^

i . on

—— L .Jo

1.95

4.40

9O- ^Co

_ .m1.80

4 n2

?u

—— — ——^ —

—— -

———

———

-

Ft.

. 2.,,,9.'

9.-

9..

d"

10.*

9.:9.J

9. C

10. v

4.5

DI/^^HND DRILL RECORD LOGGED BY Frank p. Tagnamonte, p. r.ng .PROPERTY Fla'o^Resources Ltd.. Mackelcan, Ontario .^^^^^——.^——^^l ATITlinF O * 315________ BEARING OF HOLE_____fi_________ STARTED 21 Nov. 1983DEPARTURE. 40. 5E

ELEVATION 20*± above WolfLake

CORE SIZE BQ________

DIP OF HOLE.

DIP TESTS —

-90 COMPLETED22 Nov. 1983

DEPTH 707'

D.D.H. No. WT.RT-A? PAGE i

CLAIM No. S472927^^^t-DIRECTION AND DISTANCE FROM

NE. CLAIM POST

.DIAMOND DRILL CONTRACTOR Philippon Diamond Drilling Inc., Rouyn, Quebec

FOOTAGEFROM

0

0

110

TO

0

110

207

*logged in feet DESCRIPTION

CASING

QUARTZITE Sudbury Breccia

Grey-green somewhat amorphous,, micro fracturedSudbury Breccia. Random series of swirly vesicular-likp fraamenjtSudbury Breccia mixed with congealed, granular, fractured quartzite.Vague series of fine pearly white conglomeritic granular quartzite sections.

0-17 Limonitic stained f rarturo^ .Series of random small faint hematitic patches. Soarse. fine Granular patch of pyrite and chair1Fractures generally from 60-90 0 . Local vuqcrv zones.Fracturing from 55-90". T.ooal areas of weaklv kaolinitic alteration.Occasional fine 1/8-1/4" quartz stringer at upp

QUARTZITE Bedded Hematitic

Alternating narrow beds of granular and fine grBedding from 55-80".

Random patchy areas of hematitic staining. 15%± hematitic stainina.

Local zones of kaolinitic alteration confined tquartzite beds.

SAMPLE No.

s ofmicr(

pebb]

opyril

er poj

lined

D the

FOOTAGEFROM

1

es j.n

** n

tion

grey-

gjcami

TO

)f zon

freen

ar

SAMPLE LENGTH

-

S .

juart2

ASSAY

————

ite.

i t

#

\r'V *'M

5 F.1* rV^ \^.\

^^ff P-Cc-iv0fFS.,

M:;J^

'. TAtillA

v^*'*. 0^

-^ —— -

" .

N'NX A\^ v^\. —— * o

WNFt mnr __ ^

W

Frank P. Tagitamont*.

NO.F001

FHOM

110

•Ac^^mTO -

207

207'

f , DESCRIPTION

QUARTZITE Bedded Hematitxc (continued)

146 - 148 ' Random series of 1/4" quartz stringprs^150 - 170 Series of limonitic coated slips from 25-35 0 .

END OF HOLE

Casing in hole.

SAMPLING AND ASSAYING

WL8

SAMOLENO.

J-42-1

-2

FOOT

FROM

From

. 0

10

AGE

TO

To

.

10

20

SAMPLELENGTH

Au

•dot..004

ASSAY

&C.

•d-07

-rfi*'

fv (^

lo F. P

V ^v^v.

off lt c. ^ —— M.NlfK

hdil,-,

^^__"~~" .. i -"

**w

EvXL-J o \]NT5 g)

XI

^*S•S

l PIAJPROPERTY

LATITUDE .

ID DRILL RECORD LOGGED BY Frank P. Tagliamonte, P. Eng.

Resources Ltd., Mackelcan. Ontario--.—-^^—

O -t- 0 4N

DEPARTURE O * 98. 5E

ELEVATION 20 '± above WolfLake

CORE SIZE BQ -——^

BEARING OF HOLE

DIP OF HOLE -90"

DIP TESTS ________O

STARTED23 Nov. 1983

COMPLETED25 Nov. 1983

DEPTH _____227'_____

D.D.H. No. WL83-43 PAGE l

T CLAIM No. S472926_____


NE. CLAIM POST

.DIAMOND DRILL rONJTPACTng Philippon Diamond Drilling Inc., Rouyn, Quebec

FOOTAGEFROM

0

2

TO

2

148.5

227


CASING

QUARTZITE Bedded Sudbury Breccia

Grey-green alternating beds of granular and firquartzite with random small fragments of Sudbur!

Bedding features confined to the fine grained b

SAMPLE No.

e gra:

FOOTAGEFROM

.nedy Breccia.

j '

TO

i

eds. :i

Granular quartzite zone very weakly kaolinitic,) grains Rom^whaf concealedj. and vaguely micro fractured!. l

Fracturing throughout.Most common fracturing with thin gouge and slic

Bedding features vague @ 60 0 .

148. 5± Slip contact @ SO 0 .

Alternating beds of granular and fine grained g T.oT-T-Ain quartzite. -Random patches of faint hematitic staining.3% hematitic staining.

Bedding from 45-60 0 .

Random low angle fractures. Fracturing generally from 45-60 0 .

END OF HOLE

Casing in hole.

t

kensic

rey-gj

es e

een

50 0 ±.

~

SAMPLE LENGTH

ASSAY

i

i '4

1 ! ' - i; ! i i Si - .i i | -ii

/Jtt

f M

f 5 F.—li*\ 1~x

-

b,-/•^ ' -MIN^

P. TAGUA

s^'^C* or

——————

^x*-^ x X\ A,G\^\ ,,.—J O

WJSIE Jft

Mu* So*\S

D DRILL RECORD . LOGGED BY-V

U3 YAft\'\.\ . H ^

;.- ^1 x l \J ,, l *\

y LATITUDE I?.V)\

WO -v* g

BEARING OF HOLE.

DIP OF HOLE ———

. 09tf STARTED

ELEVATION IS'"ciboOrU)flVr VoVeDIP TESTS -4r~~_____™ l

CORE SIZE r^y.^_______DIAMOND DRILL CONTRACTOR.

COMPLETED.

DEPTH

l 7

CLAIM No.

M Mo -MD


NE. CLAIM POST

tFOOTAGE

FROM TODESCRI PTION

SAMPLE No.

FOOTAGEFROM TO

SAMPLE LENGTH

ASSAY

OJL& 6*ct. cooftrnuir -

\fari1ST ri f 1 0 r

Wurovx)\ \ i * Li OCCA\ 0 pr^vî c'hv^ fvr i.\rr ritj P s.

Cu .SJJ-OJL -ffi0 ~ •sir!- at/lv ci CV-xyrr ro t//t- r-. CC

O•Ko*4-

f .C

Inanrln^. a A C -s T t1 C C

JRJ Ai-trr-Otrr IT ftYp C

* l

fpjfvfr^ ^TTHiêr- r*\lttti (V^rA? ."S

/trrti r*ni****i tr*jr;iPê-e-otKJrt SffWICF*? 9O NORTM BAY

'•CCTHSBfc^Sfti-PNOlidlfcDSaO

PACE 3 l

HOM TODESCRIPTION

SAMPLE FOOT ACEP WOM TO

SAMPLE LENGTH

ASSAY

&L 3iC-

TrTr

l-e. f

.-/r*

\ WA|DOnDCDTV

LATITUDE

DEPARTURE

ELEVATION .

10 t0 -f

12'±

llD DRILL RECORD1 Resources Ltd.. Mackelcan. Onti

UP BEARING OF HOLE A;

30E DIP OF not p -50 0

above Wolf — DIP TESTS _____ 3QQ*.

LOGGED BY

ario

E 090*

- 48-

Frank P. TagliaasonteLP. Eng. **D**pening of Hple IMLflLL-R^rll

STARTED 26

COMPLETED

DEPTH

Nov. 1983

28

747

Nov. 1983t

•^

0.0

.1.H.No.|S*L8J

CLAIM No.

-DIRECTION

NE. CUAIM

-83-17 PAGE

S472926

AND DISTANCEPOST

1

FROM

Lake CORE SIZEjffl_____________DIAMOND DRILL CONTPACTOft Philippon Diamond Drilling Inc., Rouyn, Quebec

FOOT ACEPftOM

517

TO

737

747

•loooed in f~t DESCR.PT.ON

QUARTZITE Bedded Heroatitic .... . ———————— —

Alternating beds of fine grained and coarser gil— Lorrain quartzite.

Random patches of heroatitic staininq. ————— ' Hematitic stained areas have pitted core surfac;

Approximately 20* hematitic staining, . ...i

SAMPLEN*.

ainedjii

rOOTAClPKOM

es. ti J

! 1

. —- ^ .--JteddinAJWrJjes.JLr-ORi.30-42.!..^ — ... — .^..—— ——— i —— -J

Numerous fractures ganerally 9.. 50.*.... ... , . —. __ i

variations as notedi ——

Sil Sil T,|nK*nitie .atalnlna- —————— ——————————— - ————

55d[L^^339 ____ Random series of Sudbury Breccia fragments.

588 - 590 2-1/2-3/4" vuggy auartz stringers f 50 0 ±.

511 - 617 Area of multiple fracturing.

617 - 737 Generally massive quartzite, random fractures.

675 - 679.5 Patchy deep hematitic staining.

— 716.5 1" laminated quartz stringer f 32 e ± along a sli

END OF HOLE

Casing in hole.

i—.-.

———— 1

j.

( .- ————

*

TO1AMPLC

LENGTH

l

——— il

ASSAY

l1

•~ l! :

1

r ' - l

———1

' l ,^L J .J

' l

x-ft— nr 1^* V*

iii Ji

i

s^T +V?v-/xtl

[•fc-frf*

^•sS?*^-^yIU4C-^-

UlAMWtE

-^

i-Ta'xm *

V

PROPERTY

L ATITUOE

ID DRILL RECORD LOGGED BY Frank P. Taqliaroonte. P. Eng.

'Resources Ltd., Mackelcan, Ontario___.—————.-^—..————,..—.™.-..-

UN

30E

BEARING OF HOLE Az

DIP OF MOLE -90*

STARTED 29 Nov. 1983

COHPLETED 30 NOV . 1903

DEPTH 102ELEVATION 12't above Wolf LakcQip TESTS _______S________

CORE Si7P BQ__________DIAMOND DRM CQMTttACTQP Philiopon Diamond Drilling

PACE

CLAIM Mo. S472926

•DIRECTION AND DISTANCE FROM

NE CUAIM POST

Rouyn, Quebec

FOOT ACEPROM

0

6

TO

6

101

—————————————— i ii

.

102

nocoed in feet DESCRIPTION

CASING

QUARTZITE (Lorrain) Bedded

Grev-qreen alternating fine and coarser graineequartzite. liVjn^rous f-raeturea froi^ 30—58*^ .

SAMPLEM*.

beds '-MC"ai

roOTACErMOM

.Of-i

TO

'

SAMPLELEMCTH

ASSAY

1 ;

Most fractures in 55* range. ; ; j . - . 5 ;i ' " i

More obvious bedding features confined to fine grained beds. i - i Bedding P 25*±. . .. i l j i i i . :

33 - 35 Series of 3-1/8-1/4" quartz stringers 3 70*i. !12*" zone of vuggy quartz fragments.

60 1/4" quartz stringer 9 65 0 .

END OF HOLE

Casing in hole.

.

1 . -

1 - 't i',i

r if

\XjJoM'

/MIN

:, t, l\f;.

^

**ON-V

NG^S*

f

*— - N —— -rf

CtOLOO'CAL ENClNCtHING SCNVlCt*. S* *t*VtW T MOUTH *A*. ONTARIO

PROPERTY .

LATITUDE xJL

DRILL RECORD LOGGED BYResources Ltd., Mackelcan, Ontario

.Frank ?^ .JTaglJjMnonte. P. Eng,

11M

DEPARTURE JULJLPJ5

BEARING OF HOLE

DIP OF HOLE ——

STARTED 1 Dec. 1983

COMPLETED 2 Dec. 1983

DEPTH 200*

•^

P.O.H.H.. WL83-45

CLAIM Ho. S472926

ELEVATION 30'i above level DIP TESTS 3_____of Wolf Lake

CORE SITE BQ___________DIAMOND DRIU rOMTBACTQB Philippon Diamond Drilling Inc., Rouyn, Quebec


HC. CIAIM POST

rooTAccfKOM

0

0

TO

0

200

* ^

C-


CASING

QUARTZITE Sudbury Breccia

Mixed of vesicular like elongated, bulbous andBreccia fragments in 'welded" granular and loo conqlomeritic qrey-green Lorrain quartzite.Some local elipsoidal conglomeratic fragments v maximum dimension. iFine micro fracturing (fine, intersecting milk, threads) permeating the granular quartzite zoniNumerous fractures, several with limonitic and Most of the fractures at about 48*1.Random fractures 9 about 20" some with sericit

25.5 1/8" vuggy quartz thread S 87".

37* 1/4" quartz stringer 3 48* with limonitic and :

44 l" quartz stringer 9 55* with limonitic staine*

110 1/8" quartz thread 9 4 5*.

120 1/8" quartz thread * 50*.

128.5 1/4" quartz stringer in a 15" Sudbury Breccia rare beads of granular pyrite.Minute vuggs in quartz stringer. (V**Jning Post Dates Sudbury Breccia)

145,5 4" zones of limonitic stained solution cavatie3"± Sudbury Breccia fragment.

SAUPltM*.

strea!

FOOTAGEPROM

Icy Sueilly fJLnely

t

ip to 1" inf iwhit J hair- s * i- ^

TO

bury

SAMPICLENGTH

ASSAY

:

i ilike

rusty; staining., L 'c lam.

usty

i ma r g

ragme

s in i

inatK

dip c

Lns.

it, wJ

smal

ns.

on t ac

th

. *

*

r i —— i

5

i

,; it j1 i* i

;

|

-/Q[St

s*****^~"MIN^

i* Llo F.f. TACLW |M 1"V-T —— \\ X

'^c* o'^"'i i. i '

, v^JQ \vi — * ^1XONTE J—r^^A0*^X

O.O.H, HO.

fOOTMMnKHt

0

TO

200

-

200

DESCRIPTION

QUARTZITE Sudbury Breccia (continued)

147 2" grey quartz stringer S 35 0 .1/16"! pale yellow sericitic laminations on eac

Patchy areas of very weak kaolinitic alteration Characterized by match head vuqqs on core surf a

176 - 200 Vague bedding features in fine quartzite beds.Alternating beds of fine and coarser grained gr Lorrain quartzite.Bedding from 55-65*.

END OF HOLE

Casing in hole.

Uu**vtM

i side

throi res.

cy-grt

•OOTMMMOO

*

ghout

en

TOSMM\tUNO**

ASM*

fif^f*15 r.\ -

VN

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, MIMU

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*. ^*" '

————

vS\.-X ^' *- Y- 1*' ——— ) Q

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x*

/Od

FLAG RESOURCES LTD.Wolf Lake project.

Mackelcan township - Sudbury Oiiiario

'O

II

.•O* -/7ft /•f7 J'-'*

•05* -0?4*M /-it•AM-•Z40

35 CROSS-SECTION

SCALE: 1:500 .DATE: October

VfT

0444*

SO : ttO.

'

01*0———

\L

t

67

2-0

7*'

7-0'1C-*6o'

HO* - wtu (

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ioii^ifiofty s * i v.*

4*J

72

PUG RESOURCES LTD.Wolf L*ke proJtot

Mackelcan township - Sudbury Are*Ontario

' WL83-35 CROSS-SECTIONse;

DVTB:3j 1:500 Holier 1963

FI'T

/'

FOR

N FORM/^TI ONt'M-APS :

• no aT 41- l- 5

i L

.NISTRY OF NATURAL' RESOURCES

" SURVt f S AND MAPPING


•t -1 , '.1 . ' .' " ' J

f v ' - . -^ ' ,'•l i " 'i

Idol f Lake Joint VentureMackelcan S Rathbun Townships Properties

Sudbury AreaOntario

CLAIM PLAN

rin/u.r.: 3. t f -?fi'tnD A T b: February l

FPT

BU &Y M /V/3 FIGURE I\ID 3 h

r/?/ c T" s UP B c//? xD' Surface Rights Reservation

und all Lakes and R ivers. (

l

77364 I577S69 t 595886 I s

|60606(^ i~~~ T i ~ s .____ __^."^ ~

S , s \ c ^vi i g j S

391577346 ^77563^577370

577361 57737Z 1593883

T — —— —— — —. — — — -j —

• tOQ8* •t9Q69i8lg|Q70

T ~ — T ~ 'r.-r ~ ~'~ - * - — —j ' g,Dationed Claims

57T2BI— — _ — L- — ™.J.

• s -" s- s . .

3*5722 ! 563783 |583724 l 565725-——|-^-

8

. * 077493 J"'~"~ ~ — — -^

385069 l 585680 '885681 l 89574?

t fi ws Is.

585179 586767.1586766 '

If'tj^.JMW/-]

^p^fga||pp-Y, ^ *VÂ*ry^/-! infill II lî*Wll(ll |ll III Jl^l.ll.%'

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FLAG RESOURCES LIMITED -

EAST BOUNDARY -

Mackelcan Tounship

,

V* v\ Vv

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LEGEND

PHANEROZOIC

CENOZOIC"QUATERNARY

PLEISTOCENE AND RECENT

~I tt Sin*, flint, tilt, tauOtl tiH, Knunf Otparii.

PALEOZOICOHDOVICi AN-SILUHIAN

~ l Ji Iimtuone, flWgi/ww, itiilr, ana-

CAMBRIAN

SUPEHIOfl. SOUTHERN AND GHENVILLE PROVINCES

PRECAMBRIAN

LATE PRECAMBRIANMAFIC INIRUSIVl ROCKS*

( —— -^i ii c/nwotfirrew.\ f*-" tJ* Onflisr. WKll an ft tt flJlIl.l — : —— l wo oiiriiH a.ibiu aii.it.

lit Gtbbio, wilt, pfHrttnitt, pfliOo-lilt ilKH,

(Jd drily itiaenliniiHl (w/.'ooMi in*mine; ofi./iw B*BWO trgrtl,

ALKALIC aOCX-CARBONATITt COMPLEXES'

mf?o Ntiintlint

GRENVILLE PROVINCE

METAMORPHOSED MAFICINTRUSIVE ROCKS

7~] t t UniulioniatfIII Mfltm&phtiira Oiitatt tut CIO'

METAMORPHOSED ALKALIC INIRU5IVE ROCKS

ffi t in C r*,iKc illiln Htnilt, ^J too G fltrtiic mgnttinr i,tni\i

FELSIC INTRUSIVE ROCKS

ANORTHOSITE SUITE INTRUSIVE

MD (iiOBiwc inoilftimlf, i .-KB mwl*

umtltlM roclt i/tf tfriirrd pilil'

Me T oniliH, fliOJi'lf, lid (or, rf

JM fii* I 'M B 'trn monMnfl* 'tt 1 1,

MIDDLE AND LATE PRECAMBRIAN

l! UniitltJi'iilrl. )!l GiMilt* ytiibra,

of -taliU.3H MfflrWf-AOUd

3ft Gnti*sft mtlti mwiittrtl la Hw in t Sovlttitn f in,

MIDDLE P RECAMBRIAN rcLSic if.T*u!ivE ROCKS'

—————— l M Uni\itxh,ia*l. in pvl p * iQvi.iltnl tt unil M.

—~— —— —J Mi Cnt/ttrc qvt'tl fnoffwit mirtot QtitHHJiottlt tfxt srtnii

JOB G nc'isic itondbjtt\rtt ind

D:H(TAStDIMEfir)'

—l IJ Ualili (wil

fJJO) 1^0 inmiluii t,'It ctltltc mrlllta,- tff finn pttt'i l o

EARLY PRECAMBRIANFELSIC INTRUSIVE ROCKS

METASEDIMENTS

SUPERIOR AMD SOUTHERN PROVINCES

MIDDLE PRECAMBRIANLATE MAFIC INTRUSIVE ROCKS

. LATE FELSIC INTRUSIVE HOCKS 1'

SUDBURY NICKEL IRRUPTIVE

WHITEWATER GROUP CHELMSFORD FORMA1ION

lH C 'fr"K"p ™™ i''"sto"(.

ONWATIN FORMATION

FJ6 C xoonicwui ii*l*.

ONAPING FORMATION

——l inrfche'/ifKii. MPIISINO DIABASE

FELSIC INTRUSIVE ROCKS

COIAIT t nou PBAR RIVER FORMAllON

~i f! Quitti untuoni. (Irmii - J IfBof . J ^tf Idicrifoif

CORDON IAKC IOHMATION

' J t l S'Htlfr.tisM.'r. Mi-gu

LORRAIN fOftMAItON

GOWGANDA f OHM* I ion

OUIKKt LAKE GROUP SF.RPINT FOHMA1ION

-.l II Ouiil c If lo lil, ti-4 jrrnw i iiitiaof, c-ii Uonr, t"} c on gram

ESfANOLA rOHMAHO

BRUCL (OHMATtON

tj| UO'H-irnJ KIISICDf.

HOUGH LAHC GROUP MISS1SSAGI tORMAIION

——l l) Qvlitl-trttw nnttllont i

PECOflS FORMATION—i H Sitiaant. tif.iMi, val ve,**

wait minis' tuini Hieuai n—l tier*.

HAMSAI LAKE FORMATtON

PI \3 Cwehmriilt —m maar fa u iignr t na U ,'IIIWM

ELLIOT LAKi GROUP MCKIM FORMATION

Q "l" nnoi a uittt-lcutpt' H

MAriNENOA FORMATION

9 II Q ulltl-llianill lirteiltnt . CB mtnv nnykwt'tlw tna utttlo

VOLCANIC ROCK*/ SALMAf LAUE FORMATON

Mi/t AMUiHcinJci -.I" m

COPPER CLIFF FORMATIONl l *f'HT inil inltrfnrG'tlt irnr*

STOBIE FORMATION

ILSIF stOIJNIAIN 10" M J Mif,c m.J..Lilfi

MAFIC INTRUSIVE "OCBS

Z.—.—J BIDIC *ntriroi[(r mtf mwiiris.

ft Mr(i(jCO-o inff pu'^n,/!!.; nwli

EARLV PRECAMBRIAN • MD

10CHSl B'l^'l1 * n^ ^I'fl.'n.

SD

ID r*(vi(. aui'ii fm Itnttiai frfifr. fiemtfitrWr. ynnttdK

UK J'l J B l/H'tt, iarill, 5 JO Or c

—\ 3 GttjnK**, Si'll/oni, i fittl. J 1***lffi* "'I'l fl'ric^ milifOJcni"

.J IKl(, J *nJ tfdikKl m'flrcul'lft.

METAVOLCANICS FELSIC TO INTLHMEOIATE

MElAVOlCANlCS

t yniuhJi.rorfllKn,H'lt, tlK'tt IK-1 *'"- m ifim

/e/sic iniiuirOiii *na ft/i.t flyo

^ /vliic lo ,fnrt'o*litlt p^pcUhiici-ii/li, uittu ma lae 1""1''*"-

UAFiC 'O INTEHWtOIATE MEIAVOLCAMCS

whffi lnO'oc' i-n i t cp0r0.

*Jwnt mi/ H a l Ftimt'vtw tye.'MMipti tyrt I fpirwnln). M-"H tnavMI li l o Ifwiili tuiftiDcii KCUI in df inuWwn ft wine*

*iBm*eflfln*'Klirw*rniGr(riririrl;'on(flouiW fiu/l n HufBti/8'*, KMimrr. Ci' (i*. GOKWH. 3 tn^ Bnin fo.nin,pii'iBMi"Pf*cimt'iiii(*

'fleeter Mpfireiontutt wwitfntr m t(* 'oHvtofiitA Suena""'f-r?ntxtlr ttvlrUtil 'in let la Nipiiunt Dili*!*.

*Ciii'jfl(eo lid M mn f s'u/ont.

*Jnf Hutonan locH I'l -ti"/ lo nxn)ci*leli m jnajVHiHil eu( iiwvi'/ii/JiOMovici/crii'KWiii 1/lJfWiny B*N WIM'-K, M*m*ntti*'i**** /Itlwil l'( u lM.

/Fn* njfc*nK fwmwwn i'* fin* irnfi'j'io'iK (ViflVl/rnl le PJ'/I O/ "H Ml('orn*l l"* Mc fw/TMlibni md in ffi lo UT" OCwc.

*fw imf'riiiu inmi ii mig tc lit.

Legend for FIGUHt; ND b

\\

4III5SE001S MACKELCAN27 MACKELCAN

lYliN l N


Uolf Lake Joint l/entureMackelcan S Rathbun Toujnships Properties

Sudbury AreaOntario

REGIONAL GEOLOGY MAP

SCALE: l" - ^ miles

DATE: February 1984

FPT

'X?

FIGURE ND 6

5 + OOW 4fOOW

N

LEGEND

VERTICAL HOLE

•l ANGLE HOLE

5 (

16 1983 SERIES DIAMOND DRILL HOLES

1981 SERIES DIAMOND DRILL HOLES

NOTE: Ex ac t l ocations art not certified and a r-* only accurate within the i nherent discrepancies of the grid ,

CLAIM CORNER AND LINE

FLAG RESOURCES LTD.

WOLF LAKE AREA PROPERTYMACKELCAN TOWNSHIP

SUDBURY AREA. ONTARIO

DDK LOCATION PLAN

SCALE: 1/2500 DATE: MAR 1983/

SERVICES FIGURE NO 7

3-t-00W 2+OOW 2 + OOE 3tOOE 4fOOE 5+OOE 6+OOE 7+00 E

L-9+OON i

L-8+OON

L-7+OON

L-6+OON

L-5+OON

L-4+OON

L-3+OON

L-240ON

L-I + OON

B.L.-O400

L-I + OOS

L-2+OOS

L-3 + OOS

L-4+OOS

L-5+OOS

L-6+OOS

L-7 + OOS

L-8+OOS

L-9+OOS

L-KHOOS

L-llfOOS

L-I2 + OOS

L-I3 + OOS

L-I4+OOS

L-I5400S

L-I6+OOS

LAKE

WL81 8WL83 SERIES DRILL HOLES

NO 3 ZONE

24 2524 A24B

l CAMPS

NO. l ZONE

9 ABCD

LAKE STRUCTURE

WOLF LAKE

S .WEST STRUCTURE .

A8I - 83 SERIES DRILLfNG

JESS LAKE ZONEA8SSERteS PfftU. HOLES

SHAf!T A83-22OPEN CUT

-9 A83-2IASt-9

A 83-9A83-23.23A

JESS

JONES LAKE

8f GOE

5-1-OOW 4 100 W 3* OOW 2+OOW I+OOW Of 00 f GOE 2tOOE 3 + OOE 4tOOE 5 + OOE 7tOOE 8+OOE

41M5SE001S MACKELCAN27 MACKELCAN 230

L-O+50N

B.L-O-t-OO

N

L-H-OOS

LEGEMD

ANGLE HOLE

VERTICAL M C

983

O

O

ANGLE P ~n r-M8"

VERTICAL, MO' r- 1981

FLAG RESOURCES LTD.

WOLF L AKE A* E. A

M AC K E L C AKI TONf,'V4SW\r SUDBURY AREA J O VI A Ri O

DDH LOCATION PLAN

WOLF LAKE-

SCALE: i /500

D t\/ t c i rv w r- y)DATE . 17/84

4II155EWI15 HACKELCAN27 MACKELCAN 240

L-2.+ OOS

APPROXIMATE

CLAIM l i NE

BASE

LINE

NO i ZON

W27

cO

ui

LAKE STRUCTURE

y

-t-OOW o+ooFIGURE HO.8

2-i-OOE

mackelcan and rathbun townships properties sudbury area o ...€¦ · summary report on extended...

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