Ontario Geological Survey
Permanent Link to this Record:
MDI52F05SE00027
Record Name(s) | Del Norte Southwest - 1983 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 1991-Mar-02 |
Date Last Modified | 2022-Sep-16 |
Created By | |
Revised By |
Primary Commodities: Gold
Township or Area: Rowan Lake Area
Latitude: 49° 18' 13.52" Longitude: -93° 36' 52.11"
UTM Zone: 15 Easting: 455329.88 Northing: 5461405.3 UTM Datum: NAD83
Resident Geologist District: Kenora
NTS Grid: 52F05SE
Point Location Description: Map in AFRI 52F05SE0036
Location Method: Conversion from MDI
Access Description: Floatplane from Nestor Falls; winter ice road maintained to Nuinsco's Cameron Lake and Monte Cristo camps and area tourist camps on Rowan Lake. A private all-weather road to the Cameron Lake camp also exists.
1983: Del Norte Chrome Corp. commissioned airborne magnetometer and VLFEM surveys. 1984: Silver Lake Resources optioned a 50% interest in the property and conducted ground VLFEM, magnetometer, and IP surveys, geological mapping, and soil sampling. Silver Lake Resources and Nuinsco Resources drilled a JV hole on their common boundary. 1985: Silver Lake drilled 4 DDH totalling 240 m in Sullivan Bay, and conducted soil sampling, rock sampling, and geological mapping. 1986: A 57 hole, 2668.8 m reverse circulation basal till sampling program was conducted across the ice of Sullivan Bay. An additional 4 DDH were drilled. Platinum Exploration Canada Inc. acquired a 50% interest in the property from Del Norte.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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52F/05SE, RRR-2, International Platinum Corp. | 52F05SE0036 | 52F05SE0036 |
63.4431 | 52F05SE0045 | 52F05SE0045 |
2.7280 | 52F05SE0083 | 52F05SE0083 |
2.7813 | 52F05SE0076 | 52F05SE0076 |
63.4787 | 52F05SE0036 | 52F05SE0036 |
Province: Superior
Geological Age: Precambrian
Mar 10, 2011 (J Bongfelt) - 'Drill holes RL-86-7A, RL-86-08, and RL-86-09 were all collared at 14+45W, 7+50N. These three holes were drilled at -45 degrees bearing S50 E, S25 E, and due south respectively. All holes were positioned to test the geometry and downward extension of a mineralized outcrop that consists of intermediate lapilli tuff located in close proximity to a gabbroic intrusion. Neither hole intersected mineralization equivalent to that observed on surface although a strongly silicified lapilli tuff similar to that hosting the gold mineralization on surface was encountered in RL-86-08 and RL-86-09. However, several geochemically anomalous zones were intersected within the gabbro. It has been determined that the intersected anomalous zones are attributable to very narrow mineralized quartz-feldspar veinlets.' (Kenora AF 52F/05SE, RRR-2, International Platinum Corp.)
Mar 10, 2011 (J Bongfelt) - Drill Hole RL-86-04: best assay result 1703 ppb/Au (0.049 oz./ton Au) (Kenora AF 52F/05SE, RRR-2, International Platinum Corp. - Diamond Drilling Log)
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