Ontario Geological Survey
Permanent Link to this Record:
MDI000000000162
| Record Name(s) | M-6 - 1984 |
|---|---|
| Related Record Type | |
| Related Record(s) | |
| Record Status | Occurrence |
| Date Created | 2006-Oct-12 |
| Date Last Modified | 2022-Jul-14 |
| Created By | |
| Revised By |
Primary Commodities: Gold
Township or Area: Miminiska Lake Area
Latitude: 51° 34' 24.63" Longitude: -88° 39' 13.35"
UTM Zone: 16 Easting: 385400.003 Northing: 5714900.001 UTM Datum: NAD83
Resident Geologist District: Thunder Bay North
NTS Grid: 52P10SE
Point Location Description: Location obtained from assessment file map.
Location Method: Data Compilation
1983-1987: An exploration program consisting of geophysical surveys, geological mapping, humus geochemical sampling and diamond drilling was carried out by BP-Selco on a property that included the M-6 occurrence. 2003-2006: Candor Ventures has carried out an exploration program consisting of geochemical and geophysical surveys, diamond drilling and assaying on claims that include the M-6 occurrence.
| Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
|---|---|---|
| 2.30150 | 20000000511 | 20000000511 |
| 2.28483 | 52P10NE2001 | 52P10NE2001 |
| 2.27142 | 52P10SE2002 | 52P10SE2002 |
Province: Superior
Subprovince: Uchi
Terrane: North Caribou
Domain: Uchi
Belt: Miminiska-Fort Hope
Geological Age: Neoarchean
Oct 12, 2006 (Mark Puumala) - The geology of the Miminiska Peninsula area was mapped by Wallace (1981), who identified three major supracrustal rock sequences. These include two mafic metavolcanic-dominated sequences and one metasedimentary rock-dominated sequence. The oldest of these units is interpreted to be a thick, predominantly mafic metavolcanic sequence that is found in the southern portion of the Miminiska Peninsula and the area immediately south of Miminiska Lake. These mafic metavolcanic rocks have in turn been interpreted to be overlain by a metasedimentary rock sequence that is dominated by wacke and mudstone, but also contains significant thicknesses of banded iron formation. The metasedimentary sequence is overlain to the north by a second mafic-metavolcanic rock-dominated sequence. A significant unit of felsic to intermediate pyroclastic rocks has also been mapped in the western portion of this area (southeast of Howells Lake). This unit is located immediately south of the metasedimentary sequence west of Miminiska Lake, but is enclosed within the metasedimentary rocks further to the east. This area is bounded to the northwest by felsic intrusive rocks of the Troutfly Lake Batholith. Stratigraphic units in the vicinity of Howells Lake generally strike approximately northeast, with steep, near-vertical dip. Further to the northeast, towards Keezhik Creek, stratigraphy strikes in a more easterly orientation. Wallace (1981) indicates that foliation is generally oriented sub-parallel to the primary sedimentary bedding and igneous flow contact features. Foliation and shearing are noted by Clark (2005) to be most prominent in tuffaceous mafic metavolcanic layers. Wallace (1981b) mapped a number of northeast-trending faults and lineaments in this area. More recent maps (e.g., McKay 2004) illustrate a northeast-striking fault that parallels the metavolcanic/metasedimentary rock contact in the vicinity of Howells Lake. This structure appears to be related to many of the gold and antimony/gold occurrences in this area.
| Rock Type | Rank | Composition | Texture | Relationship | Terrigenous-Clastic-Unsubdivided | 1 | Interbedded Wacke, Siltstone, Mudstone, Phllite | Near |
|---|---|---|---|---|
| Ironstone-unsubdivided | 2 | Near | ||
| Schist-Unsubdivided | 3 | Garnetiferous Quartz-Chlorite Schist | Contains |
| Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
|---|---|---|---|---|---|---|---|
| 1 | Pyrrhotite | Economic | Ore | ||||
| 2 | Arsenopyrite | Economic | Ore | ||||
| 3 | Gold | Economic | Ore | ||||
| Chlorite | Alteration | Chloritic | 1 | ||||
| Garnet | Alteration | Garnetization | 2 |
Oct 12, 2006 (Mark Puumala) - Waldie (2004) reports that BP-Selco encountered gold mineralization at this location from diamond drill hole M-6 during a 1984 exploration program. The mineralized interval is described as locally-garnetiferous chlorite-quartz schist. The host rock is reported to be metasedimentary rock consisting of interbedded phyllite and quartz wacke. Mineralization includes up to 30 % pyrrhotite with disseminated pyrite (1-2 %) and arsenopyrite (1-2 %). Trace chalcopyrite and visible gold were also reported. The most significant assay was 33.5 g/t over 0.26 m.
| Rank | Classification |
|---|---|
| 2 | Lode (Gold) |
| 1 | Replacement |
| Rank | Characteristic |
|---|---|
| 1 | Sheared |
Map - Miminiska Peninsula, Kenora and Thunder Bay districts
Publication Number: M2416 Scale: 1:31,680 Date: 1979
Author: Wallace H.
Publisher Name: Ontario Geological Survey
Location:
MonoMap - Geology of the Miminiska Lake area, districts of Kenora (Patricia Portion) and Thunder Bay
Publication Number: R214 Date: 1981
Author: Wallace H.
Publisher Name: Ontario Geological Survey
Location:
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