GOODWIN MINERAL EXPLORATIONS

GOODWIN MINERAL EXPLORATIONSJohn R. Goodwin, MSc Consulting Geologist

52F16SW8832 2.8249 LAVAL010

REPORT ON THE PROPERTY

OF

A. GLATZ

IN THE

TOWNSHIP OF LAVAL

DISTRICT OF KENORA, ONTARIO

BIU1BG L

June 25/84 NTS 52F/16 SW

R. R. 1, Pine Creek Road • Callander, Ontario POH 1 HO - 705-752-1204

52F16SW8a32 2.8249 LAVAL

TABLE OF CONTENTS

PAGE NO

INTRODUCTION.......................................... 1

LOCATION AND ACCESS ................................... 1

CLAIM STATUS .......................................... 1

EXPLORATION HISTORY................................... 1

REGIONAL GEOLOGY...................................... 6

METAMORPHIC GRADE..................................... 7

STRUCTURE............................................. 7

ECONOMIC GEOLOGY...................................... 7

CONCLUSIONS........................................... 10

RECOMMENDATIONS....................................... 11

CERTIFICATE........................................... 12

REFERENCES............................................ 13

ILLUSTRATIONS

Location iriap GME4-1............................. 2Claim map GME4-2............................. 3Regional geophysics GME4-3...................... 4Regional geology GME4-4......................... 5Detailed geology GME4-5......................... 8

APPENDIX ASummary Log DDK LBl-3-78 Summary Log DDK LEl-4-78 Summary Log DDH LBl-5-78

APPENDIX BGeophysical profiles/drill section DDHLBl-3-78

DDHLB1-4-78 DDHLBl-5-78

John R. Goodwin, MSc Consulting Geologist

GOODWIN MINERAL EXPLORATIONSJohn R. Goodwin, MSc Consulting Geologist

INTRODUCTION

Goodwin Mineral Explorations was commissioned by Mr. A. Glatz

to report on 4 mineral claims. This report is based on data

available relating to the regional geology and previous

exploration:history of the area, discussions with Mr. M.

Hailstone, resource geologist and examination of the assess

ment files in the district MNR office in Kenora.

LOCATION AND ACCESS

The subject claims consist of 4 unpatented mining claims

situated in the southwest quarter of Laval Township approx

imately midway between Rafter and Diamond Lake as shown in

Figure GME4-1. Access to the area is via a gravelled timber

road starting at a point 11.5 miles north of the junction of

Highway 72 and 17 at Dinorwic.

CLAIM STATUS

x

The claim group was staked on April 23, 1983 and all rights

transferred to Mr. A. Glatz, Dryden. No assessment work was

submitted by April, 1984 however an extension was granted until

December 23, 1984. (GME4-2).

EXPLORATION HISTORY

In the vicinity of Laval Township, the exploration emphasis has

traditionally been for gold. The area was investigated in 1965

by Penarroya Canada Limited by means of an airborne magnetic

and electromagnetic survey. The survey revealed several linear

R.R. 1, Pine Creek Road Callander, Ontario POH 1 HO 705-752-1204

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Source: MNR Map 24-6 GOODWIN MINERAL EXPLORATIONS

GLATZ CLAIMS

PROPERTY LOCATION Laval Twp. Dist. of Kenora

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GLATZ CLAIMS

CLAIM LOCATION

Laval Twp. Dist. of Kenora

Scale 2"=1 m. Figure GME4-2


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LEGEND\ \\\VS -Spartan Aero System

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VEM -Vertical loop HEM -Horizontal loop -M- -Ground magnetic anomaly A s -Mineral occurrence

GOODWIN MINERAL EXPLORATIONS

GLATZ CLAIMS REGIONAL GEOPHYSICS


l-"-)£ mile Figure GME4-3

John R. Goodwln, MSc Consulting Geologist

.a

Source: ODM Geological Series Map P1204

LEGENDla-Mafic flows, Ic-Pillow flows 2b-Felsic to Intermed. volcanic^ 3 -Metasediments, migmatites

a-greywackec-siltstone,quartzite,chert j-biotite-quartz-plagioclase

9 -Biotite trondhjemite A -Mineral occurrence_________

GOODWIN MINERAL EXPLORATIONSGLATZ CLAIMS

REGIONAL GEOLOGY


. „ Figure GME4-4 1 =lmile

John R. Go'odwin, MSc Consulting Geologist

anomalies straddling the main volcanic-sedimentary contact to the south of the subject claims. The type and extent of ground follow-up carried out is not known, however the results apparently justified a drill program as a drill hole setup and core was located just east of the main showing. (GME4-3).

In 1976, Hollinger Mines Limited conducted ground magnetometer, HEM and geological surveys over a large claim group including the main showing. As a result of these surveys, two drill holes were contracted to test the main showing and one drill hole near the southwest corner of the Glatz claims tested a moderate HEM anomaly with weak magnetic correlation. "•"";"."

REGIONAL GEOLOGY

The oldest rocks exposed on the property are a layered sequence of mafic to intermediate volcanic lavas. Flow units are continuous and vary from 80 to 500 feet in thickness. Meta- morphic equivalents such as amphibolite, hornblende schist and biotite-chlorite schist are also present. A distinct marker unit of porphyritic basalt crosses the property 600 feet north of the main showing. Another distinct unit about 300 feet north of the main showing consists of an aquagene tuff breccia up to 5 feet wide. The felsic volcanic units are principally frag- mental although a section of massive,very fine-grained, dark grey to black cherty rhyolite comprises part of the felsic unit in the area of the main showing. (GME4-4).

The main showing is situated in a narrow sequence of inter calated felsic flow units and volcanogenic sediments or tuffs. The sediments consist of alternate black and buff-white bands

John R. Good win, MSc Consulting Geologist

up to 2.5 inches. Within the banded sequence is a 12 inch bed of fine grained, dark grey rhyolite. There is a hint of graphite or black carbonaceous material in some of the dark bands. Many of the rocks within the sequence are magnetic due to dissemin ated magnetite. Two roughly linear and parallel bodies of meta- diorite cut the layered volcanic assemblage. They are of irregular shape, trend north-northeast, and vary from 60 to 1200 feet in width. (GME4-5).

METAMORPHIC GRADE

Many of the mafic volcanic rocks have been metamorphosed to horn blende and biotite-chlorite schist, or black, amphibole rich, strongly foliated rocks. This assemblage, combined with the association of almandine, hornblende, albite, and quartz suggests that the rocks are in the high temperature quartz-albite-epidote- almandine subfacies of the greenschist facies.

STRUCTURE

The regional components and observed structural elements suggests that the layered metavolcanic assemblage is synclinally folded around younger metasediments to the south. Late stage faulting is represented by north-northeast fractures parallel to the main synclinal axis and along which the diorite bodies were intruded. These rocks were later cut by a series of north trending faults.

ECONOMIC GEOLOGY

The mineral showing situated at the centre of the subject claims consist of up to 10% fine-grained sulphides within volcanogenic tuffs or sediments near the contact with fine felsic fragmentals. A trench 15 feet by 5 feet exposed pyrite, galena, minor sphalerite and chalcopyrite with traces of pyrrhotite. Some


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good assay values in lead, zinc and silver were obtained, however the distribution seemed to be localized. Other sulphide occurences containing galena, sphalerite and chalcopyrite are present in the area. These sulphides are often associated with quartz veins as rims in internal fractures and/or on the contact with the host rocks.

Several pyritic deposits are situated along or near the volcanic/ sedimentary contact and interest has been sparked by drilling on the Goldlund property. One drill hole, 3000 feet east of the old shaft passed through the target granodiorite dyke into a 74 foot section of andesitic tuff mineralized with sphalerite and pyrrhotite. Subsequent drilling failed to uphold such significant widths but did lead to the development of a gold producer.

In 1978, Hollinger Mines Limited drilled the westerly extension of the mineralization exposed in the main showing, a flanking geophysical target, and a moderate HEM anomaly with weak magnetic associations near the southwest corner of the subject claims. Summary logs and geophysical profiles with drill sections are included in Appendix A and B. The anomalies were explained as graphitic tuff and 5% to 15% sulphides consisting of pyrrhotite, pyrite and chalcopyrite and minor galena over 10 to 11 feet. Assays from these holes returned trace values in Cu and Zn but it is not specified if these samples were run for gold.


10

CONCLUSIONS

The property is underlain by a layered volcanic sequence that has been synclinally folded around a north-northeast axis. The principal felsic volcanic unit occurs on the northwest limb of this fold and is host to the main lead-zinc-silver occurence. Some significant assays have been obtained to date from the sulphide horizon exposed in the trench. Significantly, recently exposed sulphides exposed in the trench extension appear bedded and would suggest a possible sulphide source not too far distant. The geological environment appears favourable for a distal volcanogenic sulphide deposit. The known mineralization has not been tested at depth or on strike to the east which may contain higher grade ore than that encountered in DDH LB1-4--78.


11

RECOMMENDATIONS

1) Prospect and sample all sulphide showings for gold potential

2) Establish a grid on the property at 300 footline spacing with 100 foot stations.

3) Max Min II and proton magnetometer surveys to trace the conductive zone away from the main showing

4) Trenching and/or diamond drilling to test anomalous zones.


12

CERTIFICATE

I, John R. Goodwin of RR # 1, Callander, District of Parry Sound in the Province of Ontario.

DO HEREBY CERTIFY THAT:

1. I am a Consulting Geologist.

2. I have practiced my profession since 1969

3. I am a graduate of Laurentian University inSudbury, Ontario where I obtained a MSc degree in Geological Sciences in 1981.

4. I am a Fellow of the Geological Association of Canada.

5. I am a member of the Prospectors and Developers Association.

6. I have no interest in the properties or securities of A. Glatz, nor do I expect to receive or acquire any.

DATED THIS 25th DAY OF JUNE 1984.

,/JOHN R. GOGDVJIN. MSc


REFERENCES

13

Bateman, P.J.

Breaks, F.W. et at.,

Hailstone, M.

Ministry of Natural Resources,

1977. Geology of Laval-Brownridge Group #1 (Kozowy Option), assess ment report for Hollinger Mines Limited, Timmins,, Ontario.

1976. Operation Kenora-Ear Falls, Sandybeach-Route Lakes Sheet; District of Kenora, Ontario Division of Mines Preliminary Map P 1204, Geological Series, Scale 1:63,360

Resource Geologist, Ontario Division of Mines, Kenora District.

Ontario Division of Mines, Resident geologissts office in Kenora - assessment files.


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Day | Mo. | Yr. j D.ny | Mo i v,

/,Credits Requested per Each Claim m Columns at righr

C*LC-£K fa-.r>oH iHQ

Special Provisions

For first survey

Enter 40 days. (This includes (me cutting)

For each additional survey: using the same grid

Enter 20 days (for each)

Geophysical

- Electromagnetic;

- Magnetometer

- Rfldtometric

- Otnei

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Days perClm m

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Complete reverse side and enter total(s) here

Geophysical Davs perClaim

- Electromagnetic '

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Note: S pecial provisions i Electromagneticcredits do not apply ;to Airborne Surveys. | Magnetometer

Radiometric

Days perClaim

Mining Claims Traversed (List in numri ic^ sequence!

Expenditures (excludes power stripping)Type of Work Performed

Performed on Claim(s)

Calculation of Expenditure Days Credits

Total ExpendituresTotal

Days Credits

InstructionsTotal Days Credits may be apportioned at the claim holder's choice. Enter number of days credits per claim selected in columns at right. _ _

Mining ClaimNumhpt

RECEW

Expcncj. Days Cr.

Tota number of mining claims covered bvthls report of w

Certification Verifying Report of Work t/1 hereby certify that 1 have a personal and intimate knowledge of the facts set forth in the Report of Work annexed heroSwr-rfaving performed the work or witnessed same during and/or after its completion and the annexed report is true. ^_^

Name arid Postal Address of Person Certifying

.^//

cjpate Certified

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Mining Lands Section

Control Sheet

File No

TYPE OF SURVEY

MINING LANDS COMMENTS:

GEOPHYSICAL

GEOLOGICAL

GEOCHEMICAL

EXPENDITURE

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NOTES

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Documents

GOODWIN MINERAL EXPLORATIONS