l G H A m

. 53 77

LEGENDLITHOLOGYINTERPRETATION

cor'^osi T;: AIR PHOTP MAPshowing AIRBORMR 5 GROUND GEOPHYSICAL ANOMALIES, their

INTERPRETATION

MIDDLE TO LATE PRECAMBRIAN

[Qj O livine Diabase Dykoc

EARLY PRECAMBRIAN

6 ) Granite

Migmatitic Rocks

4) Metagabbro

Magnetic Unit Within (T)

contact

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VLF-EM CONDUCTOR AXES

normal quadrature

1087-8 DIAMOND DRILL HOLE LOCATIONS, the Proposed new "OUTCROP GP.IC"

h P roposed nPH Boreholes.Claims TWP ' " r K )( K reverse quadrature

in phase only

zone of conductivity

SUAY2T COLD BELT

OntarioVLF TRANSMITTER

Cutler, 24.0 kHz

azimuth 101.9

Mafic to intermediate Vole

DRAWING NO. A- 6 O 1 . 4H.T.S. NO: 4 1 O l 1 6

1:10,000 April 1986

Toronto. Canada*

5 June 198PTERRAQUEST LTD. 1 by A. Hopkins.

4IC16NW005I 63.5277 SILK TORONTO, CANADA

7 x. SUMMARY

00 41016NIM51 63.5277 SILK 010

HIAWVD

andGROUND GEOPHYSICAL SVPVEYS

on the property of

652422 Ontario inc.

during the winter of 1987-1988

byALBERT HOPKINS

Consulting Geologist

INTRODUCTION;-In 1985 Mr. J.F. Gravely arranged for Terraquest Ltd. of Toronto to

perform airborne geophysical surveys over parts of Silk and Horwood twps. These Magnetometer and VLF-EN surveys were completed early in 1986, and they indicated several very interesting conductor anomalies on the underlying 49-claim property of 652422 Ont. Inc., adjoining the Orofino Resources Ltd. property in Silk twp. and Placer Dome's 25-square mile property in Newton twp.

In 1987 a very limited grid of picket lines was cut over the main conductive area as well as over several other detached conductor anomalies on the large property of 652422 Ont. Inc.. Mr. John Ward, consulting geophysicist, was commissioned by 652422 Ont. Inc. to carry out very limited Mag., EM. and S.P. (Self Potential) geophysical surveys on parts of this limited P.L. Grid to pin point the airborne anomalies, which he did in mid 1986.

John Ward's report on his surveys dated Nov. 1986 recommended 3 drill holrt to intersect these indicated conductor anomalies. This year's (1987-88) small drilling program was the result of Mr. Hard's recommendations.

PROPERTYThis consists of 49 contiguous unpatented mining claims, numbered:-

P.757522 * l claim P.755481 - 502 inclusive = 22 " P.808194 - 212 " "19 " P.924115 - 120 6 "

P. 1026201 ________^ l "

Total s 49 claims.These claims expire on various dates, but are believed to be all presently in good standing.

LOCATION:-The property lies in the S. section of Silk twp., adjoining that of Orofino

Resources Ltd., to the latter's W., NW.and N. The 652422 property is also immediately N. of Placer Dome's 25 square-mile property in Newton twp., and is 5.5 a irm iles NNW. of Breakwater's Rundle 11 gold mine, and 9 a i miles (14 kms.) NE. of the former Kenty small gold producer, now owned by Emerald Isle Resources Ltd.

The property is 63 airmiles (100 kms.) WSW. of Timmins; 21 airmiles (34 kms.) due S. of Foleyet; 44 airmiles (70 kms.) ENE. of Chapleau, and 38 air miles (60 kms.) NW. of Gogama, Ont.

ACCESS:-By car from Toronto one drives N. on Hwys. Nos. 400 and 69 by Parry Sound

and Estaire, then on Hwy. 144 by Lively and Chelmsford, and N. on 144 to the "Watershed crossroad intersection. Then drive W. on Eddy Forest Products' private gravel highway (the Sultan-Chapleau road) to the Dore road (Hwy 616) about 50 miles W., and thence N. about 50 miles or 80 kms. to the Orofino turn-off road junction.

If from Timmins, drive WSW. about 60 miles (90 kms.) on Hwy. #101 to the new gravel Hwy.#616 (1 mile W. of Mooseland motel), and thence S. about 31 miles (50 kms.) to the same Orofino turnoff road junction.

From this Orofino junction, it is about 5 miles SE. on Orofino's new road to the 652422 Ont. Inc. property, and a mile further to the Orofino camp.

GENERAL GEOLOGY-The northern limb of the Swayze Gold Belt is underlain by Archaean

metavolcanics and metasediments, which connect ENE-erly along the Destor- Porcupine fault with the Porcupine Gold Camp surrounding Timmins, Pnt.

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These Archaean (Keewatin) rocks are flanked and underlain by the ancient basement granite of the pre-Cambrian shield. The Keewatin metavolcanics and metasediments are also intruded by Algoman-age granite plutons and porphyry dykes, and by Keweenawan diabase dykes.

LOCAL GEOLOGY;-Little is known of the rocks underlying the "652422" property, due

to the paucity of outcroppings. However, from the few rock outcrops known, and from aerial geophysics, it is believed that the SE. portion of the property is underlain by mafic to intermediate metavolcanics (Keewatin greenstone), intruded in the NW. section of the property by the E. part of a batholith of Algoman granite. This is sometimes called the Whigham batholith, which is about 6 miles (10 kms.) in diameter.

Cutting across the 652422 property in a USU-ENE direction, just SE. of the Whigham granite batholith is the famed Destor-Porcupine fault. This regional feature is partially filled by olivine diabase or dolerite dykes, which, with the secondary magnetite developed by such powerful tectonic forces, makes it a magnetic high anomaly, all the way to Timmins and Destor, Quebec.

All of the above older rocks are intruded and displaced horizontally by N-S and NNU-SSE faults, which are often filled by Keweenawan diabase, dolerite, and gabbro dykes.

ECONOMIC GEOLOGY:-Although there are no large precious or base metal producers in

the Swayze Gold Belt at present, it has a rich mineral endowment typical of the Abitibi orogenic belt. There are well in excess of 100 known deposits, prospects, showings and occurrences of gold in the Swayze district.lt has long geen recognized that the rocks in the North Swayze limb or belt represent the first major reappearance of greenstones U. of the Timmins or Porcupine gold camp, the latter notable for its production of some 58 million ounces of gold to date. The relationship of gold deposits close to the Destor-Porcupine fault is well known.

Gold mineralization in Swayze is typical of the quartz vein variety, generally accompanied by shearing, fracturing, and associated sulphides and carbon atization. Gold is present in a large variety of lithological and structural settings. Two prominent examples are:-(a) Gold in quartz veins and replacements in diorite-porphyry and metagabbro, such as toe Orofino deposit (about two miles SE. of the 652422 surveyed area). Here, geologically indicated reserves of 1,651,591 tons grading 0.14 oz. Au per ton are published, with the deposit open in two directions. Underground work is proceeding there at present, to prove and increase these indicated reserves.

(b) Gold in siliceous zones associated with felsic diorite-porphyry, such .as at theRundle 11 gold mine of Breakwater Resources in Newton twp., about 6 miles SSE.

of the 652422 surveyed area. Here ore reserves are conservatively estimated at about 360,900 tonnes grading 8.55 grams per ton (9.25 oz. Au/ton.).

Dome Exploration (now Placer Come) has spent over 2 1/2 million dollars to date in Newton and COppell twps., where they now hold 25 square miles of patented mineral rights.One of their mineralized zones,about 3 miles S. of the 652422 property, in Newton twp., consists of altered diorite-porphyry and felsic volcanics, where DDH.I23 cut 6.3 meters grading 5.67 g. Au per tonne. Placer DOme is continu ing work in this area.

Emerald Isle Resources reports the discovery of a new wide stratbound carbonatized lava auriferous zone N. of their No. l shaft. Exploration work is reported to be about to resume on this property very shortly. This is 9 airmiles (14 kms.) SU. of the 6E2422 property.

Until now there has been practically no exploration performed on the 652422 claims, and, as noted above, the property is about 99? covered by overburden. However one of its few outcrops, a small one on the N. side of the original Orofino- Dome- Run di e access road, close to 652422's E. boundary with Orofino, is composed of fine-grained altered silicified, slightly pyritized metadiorite-or gabbro-porphyry, carrying some low but anomalous gold values. This rock-type is believed to be similar to those auriferous rocks drilled by Crofino and Placer Dome, and should be investigated further.

1987-88 DIAMOND DRILLING PROGRAM:-Due to the popularity and increased use of "C.E.E.-

Flow-Through Share" financing in 1987, gold exploration in Ontario and all of Canada expanded, and diamond drill rigs and crews became scarce last autumn. 652422 called for tenders to drill, and belatedly was lucky to find a contractor willing to take a small contract to drill John Ward's conductor anomalies.

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This small contract was awarded to Triangle Drilling Co. Ltd. of Lively, Ont. in December 1987.Triangle bored 3 holes of "BQ" wireline drilling totalling 930' (283 ) for 652422 Ont. Inc. Each hole strikes O0 and dips -450N. The core is stored at Ont. Ministry of Mines' Core Library, Timmins. There now follows a tabulation description of the drill ing:-

Drill Hole

No.

S-87-1

Collar Co-ordinates Slope Depth

N-SE-Hfeet meters Claim l

. 50mE.

S.87-2 B.L.(0,0) 0-0

S.87-3 10mS. of 5V of C.L. of N-s P.L. road.

320

310

30091

Remarks

In massive granite, the drill cut a sand and water seam from 186.5' to 188.7', which probably caused the conductor anomaly.In massive granite, the drill cut crushed and oxidized core and water (probably an open fault seam), from 244.O1-246.O', which probably caused the conductor anomaly.

P.808206 Basaltic lava. The drill cut a mudand water seam from 151.6' to 152.4', which probably caused the conductor.

98 P.75548D

94 P.755489

3 Holes Total 930 283 The drillers averaged only 33' pershift - very slow, and thus expensive for overhead costs, but easy on the resident geologist.

The Triangle drilling started on 13 Jan.'88 and finished on 26 Jan.'88. Thus 930' of drilling took 14 days, or only 66' per day (2 shifts) or 33' per shift, on average.

SAMPLE AND ASSAY RESULTS:-During the logging of the drill core, none of the split

(sawn) core appeared to be mineralized or altered enough to be auriferous. However, to make sure, 12 of the best-looking sections of the core were sampled, and assayed at Timmins Analytical Services lab. (Pamour) at the Mcintyre mill assay office, Schumacher. This lab. gives fast, reliable, inexpensive service. Assay speed counts when drilling, in case unusual assay results would cause an immediate change in the drilling program.

All our assays were nil or trace, with the highest being 0.01 oz. .*u per ton. Thus the drilling results were very disappointing, and John Ward's drill targets proved to be of no interest. f!o further drilling should be done in the main granite area of holes S-87-1 and S-87-2, in my opinion.

EXSICS GROUND GEOPHYSICS:-A contract was awarded to this Timmins company fo perform!-

(a) an I.P. survey on a newP.L. grid S. and E. of the 2 drill holes just finished,to ascertain if there were any sulphide targets worth drilling in that area

between the 2 drill holes just finished and the Whigham granite pluton contact with the Destor-Porcupine fault and lavas to the SE., and(b) E.M. and Mag. surveys over the new P.L. grid that we recently had cut in the

Testicle Lakes area, to pinpoint Terraquest's aerial conductor anomalies on the ground.

Exsics* report and maps, only just received from Timmins this week, conclude:-

(a) that there is no drill target (i.e. no sulphides detected) SE. of drill holes l and 2 in the area covered by the survey, and

(b) there are two conductors, "A" and "B", worth testing by drilling, one just NT.of W. Testicle lake, and the other NE. of E. Testicle lake. These conductors

are 3543' and 3280* long respectively, i.e. of excellent lengths. These drill holes should each be lOOr deep, 9 -45 dips to the NNW. Exsics also recommends further geophysical work.

MINERALIZED eUTCRO?:-During the staking of this property in April of 1983, the

staker, Chas. Mortimer, noted sulphid and quartz mineralization on an outcrop on the N. side of the old Crofino access road, just W. of the common 652422-Orofino boundary, some 10(T N. of 12 Post of claim #P.757522.

A bulldozer was contracted to strip the overburden adjacent to this outcrop, but it soon brokedown in deepening overburden, and very little new rock was exposed. Mortimer was engaged to drill, blast and bulk-sample the silicified, pyriti zed section of this rock exposure, which he did, taking out about 1000 Ibs. , bagged in 10 samples. Fire-assaying of most of these samples assayed trace in gold, but selected grab samples ranged from 0.03 to 0.07 oz. Au per ton.

-4--i..

*

This bedrock may be described as a felspathic metavolcanic or felsic basalt, having or/ "nally been slightly porphyritic, now altered. It is said to resemble Orofino's go lv-ore hostrock, also that of Placer Dome's "West Zone" near their DDH.*23.

The writer believes that this small outcrop could be near better mineralized sections that might constitute oreshoots, and that this area warrants further investigation. This could best be done by cutting a limited Picket Line Grid over about one mining claim in size (about 40 acres) around the outcrop on the 652422 property. This would comprise an fc-W Baseline, with crosslines at 100-meter spacing* and labelled pickets chained in at 25-meter intervals. A contractor like Exsics would be engaged to perform Kag., EH.- VLF and IP. over this approximately l mile grid of lines. Total cost would be about (5000. Most likely at least one 100 borehole would be warranted to test the most interesting anomaly indicated by these geophysical surveys.

CONCLUSIONS:-

1. The 1987-8 winter season short drilling program was unsuccessful in intersecting any thing of interest in its three holes totalling 930 feet. The two northern holes that were recommended by geophysicist John Ward cut only massive granite, and the one S. hole cut non-mineralized basaltic lava. The highest gold assay was 0.01 oz. Au per ton.

Instead of sulphide bands or zones, all three holes intersected water-, sand-, or mud-seams, which probably account for the conductor anomalies. No further drilling is recommended by this writer in these two immediate areas.

2. The mineralized outcrop on claim IP.757522 just north of the old Orofino access road does contain some fractured, pyritized and silicified sections which carry low but anomalous gold values. They appear somewhat similar to the hostrock of Orofino's ore body and the hostrock of Placer DOme's DDH.I23 area. A small geophysical survey and one drill hole are warranted here. Total cost about (15,000.

3. Two ground geophysical surveys were performed by Exsics Exploration Ltd. of Timmins, Ont. in NE. sections of the property. One, an "I.P." survey on the Grid extended ST. from J. Ward's grid to the Whigham granite pluton contact with the Destor-Porcupine fault, showed no indication of sulphides, nor any drill targets. The other, fag. and VLF-EN. ground surveys over the Testicle lakes grid area, indicated several conductor anomalies, A, B, C, D, and E. Of these, A and B are strong and long enough to be tested by drilling, altho Exsics recommended more geophysics. Two drill holes, one to cut each anomaly, totalling 600 feet are warranted.

The recent 1987-? winter program mentioned in paras, l and 3 above cost about J53.010, of which *50,000 was covered by ntfEP. and CEE.-flow-through share financing.

RECOMMENDATIONS:-It is therefor recommended by the writer that:-

(a) Applications be made as soon as possible for:- . . .(i) A work permit to perform the a/m recommended work program from Chapleau Forestry,

(ii) An OMEP. designation (Form l for a contract.)

(iii) "C.E.E.-"Flow-through11 C.E.I.P." financing. (Cdn Exploration Incentive Program.) (iv) Call for tenders for Line-Cutting, Geophysics i Diamond Drilling contracts.

(b) A small grid of Picket Lines (P.L.'s) be cut for about 500' aroun-1 the a/m mineral ized outcrop, and three geophysical surveys be performed on this small Grid. Total cost would be about *5000.

(c) The following three AQ or BQ-size drill holes are recommended,to be drilled thus:-

Hole Collar Co-ordinates Strike Dip Slope Depth To cut Anomaly imeters E. meters N. _______1000 E. 1050 N. 3400 -45O?!W. 300' "A"

2100 E. 1225 N. 336O -450NW. 300' "B"

P.3 These depend on new SgQJ&Xf- -450_____300* Mineralized outcrop area.

Total:- 900' in three holes.

The above recommended exploration work program would cost from S35,000 to *40,000. Subsequent future work would depend on the results of the above program.

All of which is respectfully submitted,

Toronto, Canada. ^*55*-^5®V Albert Hopkins. 6 June 1988. t^fs ^wl\ Consulting Geologist.

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