Ontario Geological Survey
Permanent Link to this Record:
MDI000000000858
Record Name(s) | DDH Gp2-08-01 - 2008, GP Property - 2008 |
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Related Record Type | |
Record Status | Occurrence |
Date Created | 2010-Aug-11 |
Date Last Modified | 2022-Jan-05 |
Created By | N Bennett |
Revised By | A Wilson |
Primary Commodities: Copper, Nickel
Township or Area: BMA 522 871
Latitude: 52° 14' 48.19" Longitude: -87° 4' 15.69"
UTM Zone: 16 Easting: 495151 Northing: 5788482 UTM Datum: NAD83
Resident Geologist District: Thunder Bay North
NTS Grid: 43D03NE
Point Location Description: The property is 90 km northwest of Marten Falls First Nation at Ogoki Post. Fly in access.
Location Method: Based on Assessment
Access Description: The property is 90 km northwest of Marten Falls First Nation at Ogoki Post. Fly in access.
2008: Temex Resources Corp. – airborne geophysics 2008: East West Resources Corp. – DD-1-200 m
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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2.42271 | 20000004366 | 20000004366 |
2.42265 | 20000004130 | 20000004130 |
Province: Superior
Subprovince: Sachigo
Terrane: North Caribou
Geological Age: Archean
Rock Type | Rank | Composition | Texture | Relationship | Vein | 1 | Quartz | Host |
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Quartz Gabbro | 1 | Quartz Gabbro | Host | |
Pyroxenite | 1 | Pyroxenite | Host |
Aug 13, 2014 (N Bennett) - The hole drilled through 39m of overburden until it intersected quartz gabbro up to 85.06m. Mineralization occurs as pyrite and chalcopyrite mineralized quartz veins at 83.49m near the bottom of the unit. Evidence of this being the bottom of the pulse is the sharp contact of the quartz gabbro and chill zone in the quartz gabbro with the bordering amphibole pyroxenite of pulse 3. The third pulse lower down contains mineralized amphibole pyroxenite with basal mineralization from 86.86 to 103.46m. . Below the amphibole pyroxenite is quartz gabbro that represents the crustally contaminated bottom of this pulse from 103.46 to 143.50m. The unit contains brecciated xenoliths of amphibole pyroxenite, from the underlying unit, starting at 105.46m and all the way to the bottom of the pulse at 143.50m. The gabbro is consistently brecciated and xenolith-rich to 143.50m. The second pulse observed in the hole contains amphibole pyroxenite that is brecciated with pyrrhotite-chalcopyrite mineralization starting at 149 to the bottom of the unit/pulse at 168m. At the bottom of the amphibole pyroxenite, the unit contains phenocrysts of feldspar from 168.09 to 168.62m which is interpreted to be assimilation of the underlying unit/first pulse. The hole then intersects a quartz diorite (possible roof unit to first pulse) followed by the main quartz gabbro from 186.83 to the end of the hole at 200m.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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2 | Chalcopyrite | Economic | Ore | ||||
3 | Pyrrhotite | Economic | Ore | ||||
4 | Pentlandite | Economic | Ore | ||||
1 | Pyrite | Economic | Gangue |
Aug 13, 2014 (N Bennett) - Zones and intercepts include an intercept of 0.208% Cu at 89.32m; a zone of average 0.187% Cu and 0.066% Ni over 5.79m from 91.69 to 97.48m, including intercepts of 0.319% Cu and 0.072% Ni at 94.57m and 0.268% Cu and 0.083% Ni at 96.61m; a zone of average 0.317% Cu and 0.092% Ni over 4.02m from 99.54 to 103.56m, including intercepts of 0.354% Cu and 0.169% Ni at 100.71m and 0.452% Cu and 0.073% Ni at 101.8m; an intercept of 0.512% Cu at 108.26m; an intercept of 1.432% Cu and 0.214% Ni at 112.6m; an intercept of 0.412% Cu and 0.260% Ni over 30cm at 115.22m; an intercept of 0.209% Cu and 0.039% Ni at 129m; a zone of average 0.128% Cu and 0.075% Ni over 9.46m from 143.15 to 152.61m including intercepts of 0.473% Cu and 0.088% Ni at 144.1m, 0.239% Cu and 0.081% Ni at 147.05m and 0.472% Cu and 0.137% Ni at 151.68m; an intercept of 0.169% Cu and 0.152% Ni at 161.9m; an intercept 0.606% Cu and 0.070% Ni at 62.88m and a zone of average 0.343% Cu and 0.091% Ni over 2.79m from 166.27 to 169.06m
Rank | Classification |
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1 | Mafic-Ultramafic Intrusion |
Rank | Characteristic |
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1 | Layered |
Map - Precambrian Geology of the Hudson Bay and James Bay Lowlands Region Interpreted from Aeromagnetic Data-South Sheet
Publication Number: P3599-REV Scale: 1:500,000 Date: 2009
Author: Stott G.M.
Publisher Name: Ontario Geological Survey
Mono - Mineral Deposits of Northern Ontario, North of Latitude 49 30'
Publication Number: OFR6242 Scale: Date: 2009
Author: Stott G.M., Josey S.D.
Publisher Name: Ontario Geological Survey
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