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Ontario Geological Survey
Permanent Link to this Record:
MDI000000000266
Record Name(s) | Probe DDH M6 - 2005, Probe A-Zone - 2005, Tamarack Property - 2005 |
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Related Record Type | |
Record Status | Prospect |
Date Created | 2007-Mar-21 |
Date Last Modified | 2022-Jan-05 |
Created By | A Wilson |
Revised By | A Wilson |
Primary Commodities: Copper, Zinc
Secondary Commodities: Gold, Silver
Township or Area: BMA 528 861
Latitude: 52° 52' 33.33" Longitude: -86° 1' 1.07"
UTM Zone: 16 Easting: 566159.999 Northing: 5858921.004 UTM Datum: NAD83
Resident Geologist District: Thunder Bay North
NTS Grid: 43D16NE
Point Location Description: Drill collar for Probe DDH M6
Location Method: Based on Assessment
Access Description: The site is accessible by air from Nakina
2004-07: Probe Mines Limited - AEM, AM, EM, MAG, DD-8-77.1 m, DD-8. 2007-2009: Mantis Mineral Corp. – optioned property, airborne geophysics
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
---|---|---|
T-5303/ 2.30967 | 20000001195 | 20000001195 |
2.36449 | 20000002885 | 20000002885 |
Province: Superior
Subprovince: Sachigo
Terrane: North Caribou
Geological Age: Archean
Rock Type | Rank | Composition | Texture | Relationship | Felsic Crystal Tuff | 1 | Siliceous | Crystal Tuff | Host |
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Felsic Lapilli-Tuff | 2 | Lapilli Tuff | Footwall |
Aug 01, 2014 (A Wilson) - The host lithology is a dark grey, highly siliceous felsic fragmental compised of fine-graned siliceous matrix, fine-grained magnetite and quartrz-feldspar phenocrysts/crystal fragments. The footwall rocks are siliceous, coarse-grained lapilli tuffs. The drill hole terminated in the same felsic tuff as the host to the mineralization. The sulphide mineralized horizon is hosted by coarse felsic volcanic fragmental units comprised of large (up to 8cm) volcanic clasts in a siliceous, variably chloritized quartzsericite matrix. Hangingwall fragmentals are devoid of sulphide and non-magnetic while the footwall fragmental horizon is strongly magnetic, and typically more chloritized.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Chalcopyrite | Economic | Ore | ||||
1 | Pyrite | Economic | Gangue |
Aug 01, 2014 (A Wilson) - A 0.5 m section of drill core returned assays up to 5.16% Cu, 238 ppm Zn and 33 ppb Au. Mineralization consists of 2.4 m of massive to weakly bedded fine-to coarse-grained pyrite and chalcopyrite that appears as thin bands and disseminations interstitial to the pyrite. Chalcopyrote forms up to 10% of the sulphides. Drill hole M6 intersected a 7.8 m section of core that graded 3.1% Cu and drill hole M7 returned 2.4% Cu over 6 m including 3.4% Cu over 5 m. Drill holes M9, M10, M14 and M15 drilled in 2006 tested continuation of A-Zone. Drill holes M9-10 encountered 7 m of Cu-bearing massive sulphides with Cu values ranging from 0.3% to 0.7%. Drill holes M16 and M17 were designed to test a deep (>100m) ground geophysical anomaly along the same horizon as the A-Zone mineralization, approximately 800m to the south. Drill hole M17 intersected a thick zone (35m) of continuous massive and semi-massive sulphides between 129 and 164m depth which returned anomalous values of copper, zinc, gold and silver, and showed a distinct zonation between the base metals.
Publication - News Release
Publication Number: Scale: Date: 2005
Author: Probe Mines Limited
Publisher Name:
Publication - News Release
Publication Number: Scale: Date: 2006
Author: Probe Mines Limited
Publisher Name:
Publication - News Releases
Publication Number: Scale: Date: 2006
Author: Probe Mines Limited
Publisher Name:
Map - Precambrian Geology of the Hudson Bay and James Bay Lowlands Region Interpreted from Aeromagnetic Data-East Sheet
Publication Number: P3598-REV Scale: 1:500,000 Date: 2008
Author: Stott G.M.
Publisher Name: Ontario Geological Survey
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For detailed information regarding this mineral record please contact the Thunder Bay North Resident Geologist District Office