ANNUAL REPORT OF ACTIVITIES - Ontario...5 J 41018NW9155 63.4904 HALCROW 010 ANNUAL REPORT OF ACTIVITIES 1985 WORK PROGRAM CANICO - GOLDEN HOPE - QUINTERRA AGREEMENT SYLVANITE JOINT

5 J

41018NW9155 63.4904 HALCROW 010

ANNUAL REPORT OF ACTIVITIES1985 WORK PROGRAM

CANICO - GOLDEN HOPE - QUINTERRA AGREEMENTSYLVANITE JOINT VENTURE, ONTARIO

NTS: 41-0-10 ft 15

Canadian Nickel Company Limited Copper Cliff, Ontario August 1986

THIS SUBMITTAL CONSISTED OF VARIOUS REPORTS, SOME

OF WHICH HAVE BEEN CULLED FROM THIS FILE. THE CULLED

MATERIAL HAD BEEN PREVIOUSLY SUBMITTED UNDER THE

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41010NW91SS 63.4904 HALCROW

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SUMMARY

I.0 INTRODUCTION

2.0 LOCATION AND ACCESS

3.0 PROPERTY STATUS

4.0 HISTORY

4.1 Foreign4.2 Canico-Quinterra-Golden Hope

5.0 1985 WORK PROGRAM

5.1 General5.2 Line Cutting5.3 Base Camp

6.0 REVERSE CIRCULATION DRILLING CONTRACT

6.1 Bulldozer6.2 Drill6.3 Water Carrier

7.0 DRILLING

7.1 Bedrock7.2 Overburden7.3 Quinterra Diamond Drilling

8.0 GEOPHYSICAL SURVEYS

8.1 Magnetometer Survey8.2 Horizontal Loop Electromagnetic Survey

9.0 CONCLUSIONS

10.0 RECOMMENDATIONS

II.0 1986 PROPOSED EXPLORATION PROGRAM AND BUDGET

12.0 STATEMENT OF EXPENDITURES

13.0 REFERENCES

l

1

2

3

34

555

566

679

99

10

10

11

12

13

Figures

Figure Number Scale

1 Claim Location Map 1:50,000

2 Reverse Circulation Holes Completed 1:50,000

3 Geology Survey (Quinterra) with RC-HMC assays 1:2400 Sheets 1-10 (in pockets)

4 Mag and VLF Coverage 1:50,000

5 Horizontal Loop Coverage 1:50,000

6 Magnetometer and Horizontal Loop Surveys 1:2400 Sheets 1-12 (in pockets)

Tables

1 Drill Summary

2 Expenditure Summary

Appendices

Appendix l

Reverse Circulation Drill Logs: RC 75801 to 75882

SUMMARY

In November, 1985, Canadian Nickel Company took over as operator of the Sylvanite Joint Venture. A total of 27 miles of baseline and picket line were cut on the western half of the property. A Heath and Sherwood Ltd. skid mounted reverse circulation drill was employed during December 1985 and January 1986 to drill eighty-two (82) holes totalling 3492.94 feet in three tiers across the property. A magnetometer survey was carried out over 57 miles, and 36.85 line miles were covered with a horizontal loop electromagnetic survey.

Eighteen reverse circulation holes contained at least l sample with gold values greater than 1000 ppb. The most potentially significant are 6 holes occurring southeast of the northernmost carbonate-silica alteration zone. Anomalous gold and arsenic values occur over a length of 9000 feet and suggest a large stratabound gold bearing sulfide zone to the north.

1.0 INTRODUCTION

Canadian Nickel Company Limited (Canico) entered into an agreement in 1985 with Quinterra Resources Inc. and Golden Hope Resources Inc. whereby Golden Hope and Canico, by collectively spending a total of Si,000,000 by March 31, 1987, can each earn a 25?^ interest in Quinterra's 261 mining claims and 9 patented claims in Greenlaw, Tooms and Halcrow townships in the Swayze greenstone belt. The claims are 100^ owned by Quinterra Resources Inc. who assembled the property from an original 12 claim block staked in January, 1982.

In late 1982 Quinterra carried out a till sampling program to the south of Sylvanite Creek. Fifty-three holes were dug by backhoe. At the same time a 16,000' baseline with cross lines spaced at 400' intervals was established and mag and VLF EM surveys carried out. The first drill program in late 1982 and early 1983 consisted of 3132' in six (6) holes drilled to the west of surface trenching which had indicated anomalous gold concentrations. Encouraging gold values were intersected in holes SC-1 and SC-3. The grid was extended and additional stripping of surface showings was carried out. In August 1983 an additional 14 holes totalling 5797' were drilled. Results indicated a stratabound zone of low grade mineralization in the vicinity of the SC-3 intersection.

In November, 1983, 20 miles of IP survey was carried out on the north side of the baseline between OE and 96E. A number of high chargeability, high resistivity zones were located. In March, 1984, eight (8) of these anomalies were tested by 93 percussion overburden drill holes.

The 1984 program consisted of geological mapping, trenching plus additional IP surveys and 1384' of diamond drilling in four (4) holes. Anomalous gold values were located in three of the holes. Reconnaissance mapping was carried out over some of the Halcrow patented claims located at the north end of the property. In late 1984 an airborne magnetic and VLF-EM survey was carried out over the claims by Terraquest Limited.

Canico took over as project manager in November, 1985 and subsequently completed the 1985 work program which consisted of line cutting, RC drilling, magnetometer and HLEM surveys. A line cutting program was initiated over the western half of the property and a camp established. A reverse circulation drilling program was laid out to cover claims in Tooms and Greenlaw townships to the east of the Kinogama River (figure 2). A total of 3492.94' in 82 holes was drilled during this operation. The new grid was covered with magnetometer and HL-EM surveys. Mag coverage was completed on the unsurveyed portions of the old grid and HL-EM carried out in selected areas {figures 4 and 5).

2.0 LOCATION AND ACCESS

The property is located in NTS area 41-0-10 and 41-0-15 in the Swayze greenstone belt, predominantly in Tooms township but extending north into

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Halcrow and east into Greenlaw townships. The centre of the block is situated about 25 miles east-southeast of Chapleau and about 8 miles northeast of Kormac, Ontario. Access can be made to Kormac from Highway 667 thence to the property over about 10 miles of good bush roads. The Noranda-Pezim "Hotstone Lake Property" is tied on to the east end of the Sylvanite Lake property.

3.0 PROPERTY STATUS

The property consists of 9 patented and 261 unpatented mining claims located within Halcrow, Tooms and Greenlaw Townships, Porcupine Mining Division. The patented claims with their registered land titles parcel numbers, acreage and current land status and the unpatented mineral claims with their recording dates and next assessment due dates are listed below and are graphically shown on Figure l.

Claim No. Parcel No.

S S S S S S S S S

221472215522169221752217622178221852218622187

85298530853385358538853485258526

W.S. W.S. W.S. W.S. W.S.

o * W * j *s.w.s.o * w * o *

8527 S.W.S.

Claims

P 630745 -P 631303 -P 631316 -P 631322 -P 631333 -P 631353 -P 631359 -P 648051 -P 648664 -P 648672 -P 648674P 648675 -P 648677 -P 681174'P 681177 -P 682151 -P 682156 -P 682160 -P 682164 -P 682167-P 700506 -P 708352P 708353 -

P 630756 incl.P 631315 incl.P 631321 incl.P 631330 incl.P 631352 incl.P 631354 incl.P 631362 incl.P 648054 incl.P 648671 incl.P 648673 incl.

P 648676P 648683 incl.

P 681183 incl.P 682155 incl.P 682159 incl.P 682163 incl.P 682165

P 700525 incl.

P 708354

Acreage

44.6544.8563.4751.6548.8050.1943.2638.9260.04

acres acres acres acres acres acres acres acres acres

Land Status

Mining A Surface Mining S Surface Mining 8. Surface Mining S Surface Mining S Surface Mining 81 Surface Mining S Surface Mining A Surface Mining 81 Surface

Recording Dates Due Dates

FebruaryMayMayMayMayMayDecemberJulyFebruaryFebruaryFebruaryFebruaryFebruaryMarchMarchFebruaryFebruaryFebruaryFebruaryMarchMarchFebruaryFebruary

8, 198226, 198226, 198226, 198226, 198226, 19827, 1982

14, 19829, 1983

21, 198321, 198321, 198321, 198324, 198324, 198321, 198321, 198321, 198321, 198322, 198324, 198321, 198321, 1983

FebruaryMayMayMayMayMayDecemberOulyFebruaryFebruaryFebruaryFebruaryFebruaryMarchMarchFebruaryFebruaryFebruaryFebruaryMarchMarchFebruaryFebruary

8, 198826, 198826, 198726, 198826, 198826, 19877, 1988

14, 19889, 1989

21, 198921, 198821, 198921, 198824, 198824, 198821, 198821, 198921, 198821, 198922, 198924, 198821, 198821, 1987

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Claims

P 708355 -P 708377 -P 708382 -P 708385P 708386P 708387P 708388 -P 708395 -P 708399P 708400P 708801P 709741 -P 733574 -P 735757P 735758 -P 735760 -P 735772P 735804 -P 735806P 735807P 735808 -P 735810 -P 735813 -P 735816 -P 752936 -P 772248 -P 772256P 772269 -P 796582 -P 831988 -

) HISTORY

P 708376 incl.P 708381 incl.P 708384 incl.

P 708394 incl.P 708398 incl.

P 709760 incl.P 733576 incl.

P 735759 incl.P 735771 incl.

P 735805

P 735809P 735812 incl.P 735815 incl.P 735817P 752938 incl.P 772255 incl.

P 772274 incl.P 796583P 831991 incl.

Recording Dates Due Dates

FebruaryMarchFebruaryFebruaryFebruaryFebruaryFebruaryFebruaryFebruaryFebruaryFebruaryMarchSeptemberOctoberOctoberOctoberOctoberOctoberOctoberOctoberOctoberOctoberOctoberOctoberOctoberOctoberOctoberOctoberAprilOctober

21, 198324, 198321, 198321, 198321, 198321, 198321, 198321, 198321, 198321, 198321, 198324, 198314, 19847, 19837, 19837, 19837, 19837, 19837, 19837, 19837, 19837, 19837, 19837, 19837, 19837, 19837, 19837, 1983

25, 198415, 1984

FebruaryMarchFebruaryFebruaryFebruaryFebruaryFebruaryFebruaryFebruaryFebruaryFebruaryMarchSeptemberOctoberOctoberOctoberOctoberOctoberOctoberOctoberOctoberOctoberOctoberOctoberOctoberOctoberOctoberOctoberAprilOctober

21, 198824, 198821, 198721, 198821, 198721, 198821, 198721, 198821, 198721, 198821, 198724, 198814, 19887, 19877, 19887, 19877, 19887, 19877, 19887, 19877, 19887, 19877, 19887, 19877, 19887, 19887, 19877, 1988

25, 198815, 1988

4.1 Foreign

The area was covered during the early I960's by a Canico airborne mag and EM survey as part of a regional exploration program in the Swayze area. One hole was drilled to the west of Betty Lake to test an EM conductor.

In 1960, Anaconda drilled three holes to test an EM conductor located between Upper Sylvanite Lake and the Kinogama River. The Tooms Nickel Syndicate investigated a Cu-Ni-Zn showing located on the property to the east of Upper Sylvanite Lake and south of Camp Lake. Nine diamond drill holes were completed during this exploration program. In 1977 Granges Exploration carried out an intensive regional exploration program in the area. Follow-up diamond drilling was undertaken and about 26 holes were drilled within the property boundaries on EM conductors located by Granges.

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4.2 Canico-Quinterra-Golden Hope

Quinterra Inc. staked twelve (12) claims in 1982 and added to this block until the present total of 261 was acquired. Nine patented claims in Halcrow township were optioned. In October, 1982, access roads were prepared and 53 till pits were dug in an E-W line south of Sylvanite Creek. Some anomalous results were obtained. Surface stripping revealed pyritic exhalative rock interbedded with green carbonates which are cut by quartz carbonate veins. In November 1982, the first part of the grid was cut and five holes were drilled to test for strike extensions of mineralization found in the trenches. Numerous anomalous zones and some economic grades were intersected in these holes including 0.154 opt Au over 3'8" in SC-1; 1.36 opt Au over T6" and 0.178 opt Au over 2'10" in SC-3.

During the summer of 1983 the grid was extended and a mag and VLF-EM survey carried out. Stripping located two areas with erratic gold mineralization; up to several hundred ppb Au in trench 6 and 0.064 opt Au in trench 7. Between August and November, 1983, a further 14 holes were drilled. Eight (8) were located near the previous drilling where anomalous results had been obtained and four (4) were drilled tp test magnetic "breaks". Results showed a stratabound zone of low grade mineralization in the vicinity of hole SC-3.

In late 1983, about 20 miles of IP survey was carried out north of the baseline from 0+OOE to 96+OOE. A number of high chargeability, high resistivity anomalies were located.

During 1984 line cutting, reconnaissance prospecting and detailed geological mapping continued along with magnetic and VLF-EM surveys. Between mid-March and early April, 93 percussion overburden holes were drilled on eight separate IP anomalies. Two stratabound sulphide bearing, carbonatized and silicified zones 500 and 1700 feet long were identified. An additional 22 holes were drilled in August to test another IP anomaly.

Between October 25, 1984 and February 7, 1985, a combined airborne magnetic and VLF-EM survey was carried out over the claim block by Terraquest Surveys Limited. The survey area was covered by a grid of parallel flight lines spaced 100 m apart and oriented north-south. A total of 421 line km of magnetic and VLF-EM surveying was completed.

Four diamond drill holes were completed in December, 1984, to^test IP anomalies and areas where anomalous gold values had been previously identified. Holes SC-84-1 to 3 intersected anomalous gold bearing zones. Hole SC-84-4 was drilled 200' east of SC-3 but failed to locate any significant mineralization.

5.0 1985 WORK PROGRAM

In November, 1985, Canadian Nickel Company Limited took over as operator and started a line cutting program on the western half of the property. About 27 miles of baseline and picket line were cut. A Heath and Sherwood Ltd. skid

Canadian Nickel Company Limited

SYLVANITE JOINT VENTURE, ONT. Claim Location Map

SCALE hSOOOO

Figure l

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mounted reverse circulation drill was employed during December (1985) and January (1986) to test the basal till in three tiers of holes, hole spacing about 800', set out across the property south of Sawbill Lake and east of the Kinogama River. Magnetometer (57 miles) and HL-EM (36.85 miles) surveys were carried out on the newly cut grid and on portions of the old grid.

5.1 General

Following the signing of the agreement between Canico, Golden Hope and Quinterra, contracts were let for line cutting, RC drilling and accommodation trailers. The project area was visited to check the state of the grid, the picket markings and access routes for the RC drill.

5.2 Line Cutting

A line cutting contract for 54 miles of baseline and picket line was awarded to Norm McBride. After completing about 27.1 miles of grid this contractor quit due to extreme topography, thick underbrush and abundant blowdown in the vicinity of the esker. The current grid status is indicated on Figure 2.

5.3 Base Camp

Camp was established from Dec. 4 to 7, 1985. Two Atco industrial trailers were brought in and set up; a 40 foot kitchen/dining trailer and a 55 foot 8 man sleep trailer. A generator shack was built to house a 15 kw Flygt light plant, and a washhouse-dry constructed. A 1000 gallon propane tank was rented from ICG in Wawa, and a 1000 gallon diesel fuel tank rented from Carman Construction of Sudbury. A 14 x 16 foot plywood floor - Jutland frame insulated tent was put up in January in order to accommodate additional personnel.

6.0 REVERSE CIRCULATION DRILLING CONTRACTS

The contract for RC drilling was let to Heath and Sherwood Ltd., however, the only machine available was a skid mounted unit which requires a tractor to move. A Kamatsu D65 tractor was contracted to build access roads and to move the drill.

6.1 Bulldozer

A Kamatsu D-65E was contracted from Carman Construction and mobilized on December 4, 1985. The Kamatsu was used for snow plowing and road construction from December 5-11 inclusive and for moving the drill from December 12-19, 1985 inclusive. On January 6, 1986, a D-7E was contracted from Carman Construction and floated to the property. Both bulldozers were employed in road construction on January 7 and 8, after which the Kamatsu was utilized to move the drill for the duration of the program (January 21, 1986). The D-7E continued making access roads, finishing on January 19.

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6.2 Drill

A skid mounted Acker reverse circulation drill contracted from Heath and Sherwood was mobilized on December 11, 1986. Drilling commenced on the 12th., shut down for Christmas on the 19th., and resumed on January 9, completing the program on January 21, 1986.

6.3 Water Carrier

Heath and Sherwood supplied a skid mounted 350 gallon water sloop and water pump. Canico's diesel muskeg tractor and personnel were utilized to pull the water tank, as well as haul fuel for both the drill and bulldozer.

7.0 DRILLING

A total of 1064.65 m or 3492.94 ft in 82 holes was drilled for an average depth per hole of 12.98 m or 42.60 ft. Sixty-five holes were drilled on the previously gridded section east of the esker and 17 holes west of the esker. No holes were drilled on the esker due to extreme topography, expected depths in excess of 150 feet, and the probable lack of a "basal" till. Holes drilled on the eastern margins of the esker showed sand to be sitting directly on bedrock.

Drilling problems encountered are as follows:

75804: abandoned in bedrock at 3.9 ft, moved 100 ft and redrilled as75805

75835, 75862: abandoned at 86.61 ft and 82.02 ft respectively, due to loss ofreturn and tightening of rods (#62 is a redrill of #35)

75838: lost 3 rods, bit and sub in hole75848: abandoned in bedrock (no overburden) - no samples taken 75855, 75858: bedrock collected but no overburden return (only snow S humus) 75873: lost 4 rods, bit and sub in hole

Figure 2 shows the 82 hole locations and heavy mineral concentrate (HMC) assays for the holes west of the esker. HMC assays for holes east of the esker are indicated on figure 3 (in pockets).

7.1 Bedrock

Bedrock chips were processed in the Copper Cliff exploration assay lab. Thin sections of the bedrock samples were prepared and examined. The claims are underlain predominantly by mafic volcanic rocks which locally exhibit volcaniclastic textures, and by ultramafic rocks. The ultramafic rocks have undergone varying degrees of alteration including serpentinization and carbonate-talc alteration. Some drill sites intersected minor quartz-calcitej^ carbonatej^pyrite veining. Several of the holes intersected feldspar-quartz porphyry "and diabase dykes. The highest bedrock assay, 445 ppb gold, was obtained from a green carbonate rock with pyritic quartz veining. The average bedrock assay for each hole on the gridded portion is plotted on figure 3.

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7.2 Overburden

The majority of the holes intersected a basal clastic material classified as till or gravel. All basal till and basal sand/gravel samples were forwarded to Overburden Drilling Management Ltd. in Ottawa for a heavy mineral separation and visual gold grain count. The visual count indicates that 25 holes intersected at least one sample containing l to 5 grains of gold. The grains are typically abraded; a few are classified as irregular, and three as delicate {holes 75818, 75834 and 75874). There appears to be no direct correlation between visible gold in the heavy mineral concentrate and a high gold assay.

A number of the concentrates are sulfide rich (pyrite * marcasite, and rare galena in 2 holes west of the esker). Anomalous gold values roughly correlate to sulfide content of concentrates from holes drilled east of the esker; sulfide rich concentrates collected west of the esker do not contain anomalous gold values.

The heavy mineral concentrates were sent to Neutron Activation Services in Hamilton for a multi-element analysis. Elements analyzed include Au, Ag, As, Co, Cr, Mo, W, Fe, Ni and Zn. Gold assays2.1000 ppb are considered anomalous. Gold values show a trimodal distribution: "background" values ranging up to 300 ppb, weakly anomalous values from 300 to 1000 ppb and strongly anomalous gold values greater than 1000 ppb.

High concentrate gold values are considered significant only in the bottom 3 samples above bedrock and of high priority if 2 or more consecutive bottom samples are anomalous. West of the esker 4 of the 17 holes contained one sample with anomalous values, none of which are considered significant with the possible exception of 75869. The bottom sample in hole 75869 assayed 2600 ppb gold. The concentrate contained no sulfide and no gold grains were observed. The second sample above bedrock assayed 460 ppb but adjacent holes did not contain anomalous gold values.

The second sample above bedrock in hole 75871 contained 4 abraded gold grains and assayed 3100 ppb gold; the sample on bedrock assayed< 14 ppb gold. In hole 75877, the seventh sample above bedrock assayed 14,000 ppb gold as a result of l large abraded gold grain (550 x 575 microns). The bottom sample of hole 75881 contained 5 abraded gold grains and assayed 1200 ppb gold.

East of the esker, 14 holes contained samples with anomalous gold values. The bottom sample in hole 75863 (40+OOE, 40+OOS) contained l abraded gold grain and assayed 1800 ppb gold. The second sample above bedrock in hole 75857 (88+OOE, 42+OOS) assayed 1000 ppb; the bottom sample assayed 46 ppb gold. The bottom sample of hole 75808 (33+70E, 2+50S) assayed 1000 ppb gold. This hole was drilled south of the series of trenches west of camp testing the southern carbonate-silica alteration zone. The bedrock in 75808 is a green carbonate- quartz-sericite rock which averaged 25 ppb Au with a high of 60 ppb. East of camp 3 holes (75812 - 84+OOE, 1+50S, 75813 - 76+OOE, 2+505, 75823 - 76+OOE, 12+85S) which collared into serpentinized peridotite contain anomalous HMC

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gold values of 1100, 1300 and 1100 ppb respectively. These anomalies may reflect the eastward strike extension of the southern carbonate alteration zone or may be down-ice dispersions of the northern alteration zone (trench 7 area).

East of the above 3 holes 2 anomalies were recorded which are considered of low significance. The eighth sample above bedrock in hole 75828 (92+OOE, 10+OOS) contained l large abraded gold grain and assayed 10,000 ppb gold. The bottom sample in hole 75841 (128+OOE, 6+50S) contained l very large abraded gold grain (600 x 1300 microns) and assayed 37,000 ppb gold.

The remaining 6 anomalies may reflect a mineralized (Au-As) zone with a possible strike length in excess of 9000 feet. The bottom sample in hole 75815 (58+OOE, 22+OON) assayed 2000 ppb gold, and the second sample above bedrock assayed 560 ppm As. The bedrock consists of andesite with quartz veining and averaged 45 ppb gold with one sample running 105 ppb gold. The bottom sample in hole 75816 (66+OOE, 20+OON), 900 feet to the southeast, assayed 3200 ppb. The carbonate-quartz-sericite bedrock averaged 350 ppb Au with a high of 445 ppb gold. Hole 75817 (74+OOE, 20+OON), 800 feet east of 75816 did not intersect anomalous till, however, the carbonate-quartz-chlorite bedrock averaged 88 ppb Au with a high of 150 ppb gold. The bottom sample in hole 75819 (80+OOE, 16+50N), 750 feet southeast of 75817, assayed 540 ppm As. Hole 75818 (88+OOE, 16+50N), 700 feet east of 75819, gave the best results of the drill program. It was drilled north of the stripped area referred to as number 7 trench area. The bottom sample assayed 5800 ppb Au and 920 ppm As and contained l delicate gold grain. The second sample above bedrock contained l irregular and l abraded gold grain and assayed 4700 ppb Au and 800 ppm arsenic.

Hole 75831 (106+OOE, 13+OON) was collared 1900 feet southeast of 75818. The bottom sample assayed 910 ppb Au and 1700 ppm arsenic. The third sample above bedrock in hole 75832 (122+OOE, 11+OON), 1400 feet southeast of 75831, assayed 1900 ppb Au. The second sample above bedrock assayed 780 ppm arsenic. Hole 75833 (132+OOE, 12+OON) was drilled 1000 feet east of 75832 and assayed 3200 ppb Au and 460 ppm As in the second sample above bedrock. Hole 75834 (140+30E, 11+OON) collared 800 feet east of 75833, did not carry anomalous gold, however, l grain of delicate gold was observed in the second sample above bedrock and the third sample above bedrock assayed 570 ppm arsenic.

Hole 75839 {144+OOE, 5+50S) was collared 1700 feet south of hole 75834. The serpentinite bedrock averaged 40 ppb Au with a high of 50 ppb. The last 3 samples above bedrock assayed 780 ppb Au and 530 ppm As, 720 ppb Au and 690 ppm As, and 980 ppb Au and 580 ppm As, respectively.

Hole 75838 (152+OOE, 6+OOS) was drilled 800 feet east of 75839. The last 3 samples above bedrock all assayed 1200 ppb Au, and 870, 1000, and 770 ppm As respectively. Eight hundred feet to the northeast, hole 75837 (160+OOE, 3+OOS) intersected anomalous As but no gold. The bottom sample assayed 1400 ppm arsenic.

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Table 1 is a summary of the drilling. The drill logs are appended.

7.3 Quinterra Diamond Drilling

Quinterra drill core was reviewed and sampled where deemed necessary. A sample taken from 288.0 to 289.4 feet in hole SC-14 assayed 1.95 p p m gold. The remaining 14 samples ranged in value from nil to 45 ppb gold.

8.0 GEOPHYSICAL SURVEYS

The magnetometer survey (57 miles) was performed between lines 44E and 102E to complete the coverage to the claim boundary and west of line 44E to cover the newly cut grid. Difficult terrain and frequent dead falls made working during the winter difficult. The horizontal loop survey (36.85 miles) was carried out over some selected lines of the old grid and west of line 44E on existing lines to 8W.

8.1 Magnetometer Survey

The survey was carried out with the Omni IV microprocessor controlled proton precession total field magnetometers manufactured by EDA Instruments Inc. of Toronto. Two mobile magnetometers and one stationary base station magnetometer were used for this survey. These magnetometers electronically store all data, perform drift corrections on the data and output the results through a printer. Readings were taken in the field at 50 foot station intervals and on lines 400 feet apart. The data was hand contoured because it had to be added to existing maps.

The magnetic contour map shows several clearly defined features that outline the geology. Starting from the south side of the property, there is a zone 2000 feet wide of numerous narrow magnetic highs in the range of 1000 gammas indicating discontinuous magnetite or pyrrhotite concentration in seams extending normally over a distance of less than two lines. They typically represent a volcanic sequence under shallow overburden. A zone of low magnetic relief butts onto the area to the north. Through the central portion of the area, strong magnetic anomalies of 1000 to 2000 gammas up to 1000 feet wide indicate the location of ultramafic rocks. To the north and west these anomalies appear more scattered, broken up and intermixed with smaller anomalies possibly from volcanics or metasedimentary units. A clear contact to a flat magnetic low is obvious to the very north of the area near the boundary. West of a line between 40E/60S and 10E/60N the influence of the thicker overburden from the esker is apparent from the smooth and wider magnetic contours.

8.2 Horizontal Loop Electromagnetic Survey

The MaxMin II horizontal loop electromagnetic survey instrument used was built by Apex Parametrics of Toronto. The instrument measures the in-phase and out- of-phase component for several frequencies. During this survey readings were

Shunsby L

l HeWson';) : L. -t

Bam L

s \ \Halcrow-Swayze j ^ \ \(Shaft \ .v

\ - W,

-Halcrow L

7 "4

yTW-^'

\

;\ x

i f.\

DENYES__TWP GREENLAW TWP

iJJiH:'li:.: ljl Mag and VLF Coverage (Ouinterra)f-.-,. ..., j^. j * "

Mag (1986)

^47-461

[ x j Basic Volcanics

l ^ j Felsic Volcanics

j J j Granife

m Sediments___ ^j 5 [ Ultramafic Carbonate Alteration

Ax

40 S

^fj.:.:.T:t- - - - - - - -^l t -


SYLVANITE JOINT VENTURE, ONT.

MAG and VLF COVERAGE (QUINTERRA)

SCALE l- 50000

Figure 441 0/15 41 0 1 101

DENYES TWPGREENLAW TWP

-JGertruoV fi

Completed Reverse Circulation Drill Holes

Existing Roads

66 RC Hole Number (Prefix 738-^)

doo.3100,14) Heavy Mineral Cone. Assays-Au ppb)

(*l9,IOO,J6)"".-. 76^27,150/9)) -

MINOR OALtN*^ (-.SOX.SSX py) |**.-,


SYLVANITE JOINT VENTURE, ONT

REVERSE CIRCULATION HOLES COMPLETED (Holes 75866-82;Au ppb and Au grain count 8 type)

41 0/15,*o s SCALE I 'SOOOO Figure 2 41 0/10

- 10 -

taken at 888 Hz and 1777 Hz with a coil separation of 400 feet and readings taken at 100 foot station intervals. Where required the slope of the topography was measured to allow correction to the in-phase data. Where anomalies were found, the conductor axis is shown on the magnetic survey maps.

Two groups of 3 lines (76, 80, 84E and 136, 140, 144E) and one group of 4 lines (176, 180, 184, 188E) were surveyed across the property's eastern, previously worked, area to assess the quality of some of the VLF conductors and to cover an area near some weak INPUT responses. In the eastern portion of the property (east of 44E) only one weak horizontal loop conductor was found between lines 178E and 188E that correlates with a previously found VLF conductor.

To the west between 40E and 8W all cut lines were surveyed. In this area several weak one line anomalies were located and one conductor that could be traced from 24E/66N to 36E/60N. This conductor occurs near the contact shown by the magnetics indicating sediments to the north. This conductor may be caused by a shear or schist with graphite as indicated in a nearby old borehole (SW-100).

9.0 CONCLUSIONS

The magnetic survey helped to define some of the geological contacts on the property and was used together with bedrock sample data from the RC program to assist in the geological interpretation of the property. The horizontal loop survey located only one significant conductor which was traced over a strike length of 800 feet across the southern part of Betty Lake. Test surveys which were carried out in three line strips did not commonly confirm those conductors which had previously delineated by VLF-EM surveys.

The reverse circulation drilling program outlined a gold anomaly in the basal till from about 50E to HOE between ION and 22N. An arsenic anomaly was also located which can be correlated with the gold. Additional exploration would be required to further evaluate this area.

The string of holes along the southeastern part of the property was disappointingly dry. Holes drilled on the west side of the north-south striking esker did not locate any anomalous trends, however, 4 of the 17 holes contained one sample with anomalous values. None of these are considered to be significant with the possible exception of a 2600 ppb gold value in hole 75869. These southern and western areas are concluded to have much less potential for an economic gold deposit than the anomalous zone noted above.

10.0 RECOMMENDATIONS

Further exploration is required to test the gold anomaly located by the basaltill survey. Additional stripping should be carried out in the vicinity ofthose areas where gold values have been obtained from surface samples.

\ffolcrow -Swayze Shaft

rfxSxjx-il H orizontal Loop Coverage (1986)

l / j Basic Volcanics

l * j Felsic Volcanics

j J j Granite

l * j Sediments

Ultramafic Carbonate Alteration

—— -f-7 Hof f oneCanadian Nickel Company Limited

SYLVANITE JOINT VENTURE, ONT.20S HORIZONTAL LOOP COVERAGE (1986)

SCALE l 500OO

Figure 541 0/1541 0/10

- n -

11.0 PROPOSED 1986 EXPLORATION PROGRAM AND BUDGET

It is recommended that the 1986 program be carried out in two stages: Stage l will include additional RC drilling, geological mapping and prospecting, geophysics, line cutting and power stripping; Stage 2 will consist of diamond drilling and will commence when results from stage l are available.

PROGRAM

1. line Cutting

This will be carried out over the Halcrow township patented claims. Due to the negative results obtained from the RC drilling on the west side of the esker the line cutting scheduled for this area will not be completed.

2. Geological Mapping

Mapping will be completed over the unmapped portions of the new grid and mapping will be performed over some previously unmapped areas as indicated by Ray Lashbrook. Areas underlain by the RC anomalies will be intensively mapped and prospected. Mapping will also be carried over the 9 patented claims in Halcrow township.

3. Power Stripping

Trenching and stripping will be carried out where overburden depths permit in areas of RC anomalies. Several previously stripped areas will also be enlarged.

4. Geophysics

An IP survey will be completed over several sections of the property in those areas where anomalous results were obtained from the RC drilling. EM coverage will be extended to cover previously untested areas and a magnetometer survey will be carried out over the Halcrow patents.

5. RC Drilling

Additional ( 1000') RC drilling will be undertaken in a number of north-south oriented fences to further test anomalies located during the first phase of this drill program.

6. Diamond Drilling

A second phase of the 1986 exploration program will consist almost entirely of diamond drilling. About 7500' of drilling is planned.

- 12 -

BUDGET

Option Payments S 19,000Prospecting and Geological Mapping 71,880Power Stripping 30,650Line Cutting 8,125Geophysics 40,450RC Drilling 45,800Diamond Drilling 210,000Indirect Charges 32,793 1985 Overexpenditure(Agreed to by Golden Hope and Canico) 41,302

Total S500,000

12.0 STATEMENT OF EXPENDITURES

A summary of expenditures ending April 30, 1986, is attached.

Canico - Golden Hope/Quinterra Joint Venture

Expenditure Summary - April 1986

Geological .SurveysSalaries S Fringes Personnel Expenses Materials fc Supplies Services 4 Rentals Assays

Sub-Total

Geophy si cal Surveys Salaries S Fringes Personnel Expenses Materials fc Supplies Services fc Rentals Line Cutting - Contract

Sub-Total

Geochemical SurveysSalaries S Fringes Personnel Expenses Materials fc Supplies Services A Rentals Drilling - Contract Assays

Sub-Total

Property Materials fc Supplies Services 4 Rentals Option Payments

Sub-Total

-Indirect Charges

Total :

Total To Dec 1985

17,721 4,293

10,054 1,142

1133,211

210

3,811

9,19213,213

25,320 338

19,282 12,037 20,000

76,977

42

19,00019,042

15,343

157,796

April

1,420 2,045

1,328

TT793

1,430 75

242 706

774T3

1,130

480

3,819 F^Z9~

1,521

14,196

1986 Total

7,929 6,137 2,615 7,518

5224,251

12,668 859

(2,731) 4,161

14,957

21,650 1,696

(7,659) 28,724 24,479 12,38781,277

28

78

12,993

133,506

Total Since Inception

25,65010,43012,6698,660

6357,472

12,878859

1,0804,1619.192

28,170

46,9702,03411,62340,76144,47912.387

158,254

4228

19,00019,070

28,336

291,302

- 13 -

13.0 REFERENCES

Donovan, J. F.1968: Geology of Halcrow - Rideout Lakes Area, Geological Report 63;

Ontario Department of Mines.

Karvinen, W. 0.1983: Report on Basal Till Sampling, Sylvanite Creek, Tooms and Greenlaw

Townships.

1984: Quinterra's Sylvanite Creek Property. Summary of Work and Results to December, 1983.

1984: Results of Testing IP Anomalies by Portable Overburden Drilling, Sylvanite Creek, Tooms Township.

Lashbrook, R. 1984: 1984 Final Report of the Sylvanite Creek Property, Tooms Township.

Meikle, R. J. 1983: Geophysical Report on the Tooms Township Property, Sudbury

District for Quinterra Resources Limited, Rayan Exploration Ltd.

Middleton, R. and Durham, B.1985: Report on the Induced Polarization Survey carried out on the

Quinterra Resources Inc. Sylvanite Creek Property in Tooms and Greenlaw Townships. R. S. Middleton Exploration Services Ltd.

Watson, R. K.1985: Report on an Airborne Magnetic and VLF-EM Survey. Halcrow, Tooms

and Greenlaw Townships, Porcupine Mining Division, Ontario. Terraquest Surveys Limited.

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vey

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1984

Dat

e dr

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n 19

85R

evis

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41

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1985

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ED

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ANNUAL REPORT OF ACTIVITIES - Ontario...5 J 41018NW9155 63.4904 HALCROW 010 ANNUAL REPORT OF ACTIVITIES 1985 WORK PROGRAM CANICO - GOLDEN HOPE - QUINTERRA AGREEMENT SYLVANITE JOINT

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