Ministry of Energy, Northern Development and Mines
Permanent Link to this Record: MDI000000002371Deposit Name(s) | Clytie Bay Ni-cu - 1968 |
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Deposit Status | occurrence |
Date Created | 2020-Jan-14 |
Date Last Modified | 2020-Jan-14 |
Created By | T Pettigrew |
Revised By | T Pettigrew |
Primary Commodities: nickel
Secondary Commodities: copper
Township or Area: Glass
Latitude: 49° 36' 47.15" Longitude: -94° 57' 21.59"
UTM Zone: 15 Easting: 358702 Northing: 5497452 UTM Datum: NAD83
Resident Geologist District: Kenora
NTS Grid: 52E10SW
Point Location Description: Location of DDH 3 from Assessment report 52E10SW8582
Location Method: data compilation
1968: Olympia Gold Mines conducted magnetometer and EM surveys, mapping, and drilled 6 DDH. 1980: Sherritt Gordon Mines Ltd. reassayed Olympia’s drill core from 2 holes. 1989: Exploration Brex carried out geological mapping. 1998: Royal Oak Mines Inc. carried out mapping.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
---|---|---|
2.3671 | 52E10SW8582 | Open |
2.14243 | 52E10SW8567 | Open |
63.2287 | 52E10NW8503 | Open |
2.18653 | 52E10SW2002 | Open |
Province: Superior
Subprovince: Wabigoon
Geological Age: Archean
Rock Type | Rank | Composition | Texture | Relationship |
---|---|---|---|---|
mafic metavolcanics | 1 | host | ||
gabbro | 2 | host |
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Habit Description |
---|---|---|---|---|---|---|---|
1 | pyrite | economic | ore | ||||
2 | pyrrhotite | economic | ore | ||||
3 | chalcopyrite | economic | ore |
01/14/2020 (T Pettigrew) - A pyrrhotite-rich layer was located near the basal portion of a pyroxene-rich gabbroic sill (Assessment report 52E10SW8567). A strong ground EM and mag anomaly trends north-northeasterly through claim number K 560559. Seven diamond drill holes are reported from 1968 along this anomaly and core from two of these was found. In the old drill core a nickel value of 0.17% over 1.6 m and a copper value of 0.12% over 1.3 m were observed. The high nickel value is in a section of green banded quartz with 30% pyrite stringers. Most of the sulfides are in quartz-(carbonate)-rich rocks as bands and veinlets in altered mafics. Massive pyrrhotite and minor chalcopyrite are fairly common in the core. Gold values were all trace or nil (Assessment report 52E10SW8582).
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