Ontario Geological Survey
Permanent Link to this Record:
MDI52F04NE00006
Record Name(s) | Aremis Lake - 1984 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Discretionary Occurrence |
Date Created | 1991-Mar-02 |
Date Last Modified | 2022-Sep-09 |
Created By | |
Revised By |
Primary Commodities: Gold
Township or Area: Brooks Lake Area
Latitude: 49° 12' 49.54" Longitude: -93° 33' 29.22"
UTM Zone: 15 Easting: 459353 Northing: 5451369 UTM Datum: NAD83
Resident Geologist District: Kenora
NTS Grid: 52F04NE
Point Location Description: Location of trenches in AFRI 52F04NE0022
Location Method: Conversion from MDI
Pre-1934: early exploration and trenching was conducted. 1984: Noranda Exploration Company Ltd. conducted geological mapping, trenching and sampling.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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2.7489 | 52F04NE0022 | 52F04NE0022 |
2.7490 | 52F04NE0020 | 52F04NE0020 |
2.7500 | 52F04NE0019 | 52F04NE0019 |
Province: Superior
Subprovince: Wabigoon
Geological Age: Archean
Oct 27, 2017 (Therese Pettigrew) - The property is approximately 3 km northeast of the Pipestone-Cameron Lake Fault (AFRI 52F04NE0022).
Rock Type | Rank | Composition | Texture | Relationship | Mafic pillowed flow | 1 | Tholeiitic | Pillowed |
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Quartz Porphyry | 2 | Quartz |
Oct 27, 2017 (Therese Pettigrew) - Detailed mapping by Noranda in the area of the trenches on the shore of Brooks Lake indicate a mafic metavolcanic sequence intruded by a felsite or quartz porphyry sill no greater than 15 m in thickness. A unit of intensely altered rock (approximately 10 m wide) lies on the north flank of the felsic sill (AFRI 52F04NE0022). South of Brooks Lake, some pillow interstices are abnormally wide especially where pillow selvages are well developed. Calcite is a common filling of the interstices and where weathered out, has left individual pillows with high relief (Edwards, 1980).
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Chalcopyrite | Economic | Ore | ||||
2 | Pyrite | Economic | Ore |
Oct 27, 2017 (C Ravnaas) - Best assay: 4960 ppb Au from surface 0.157 oz/t Au.
Oct 27, 2017 (Therese Pettigrew) - Visible mineralization consists of up to 4% pyrite and trace chalcopyrite. Gold assays rarely exceeded 0.01 opt Au although 0.054 opt Au was recovered from one trench (AFRI 52F04NE0022).
File - Resident Geologist files 52F04NE O-3
Publication Number: Date:
Author:
Publisher Name:
Location: Kenora RGP office
MonoMap - Geology of the Schistose Lake area, District of Kenora
Publication Number: R194 Date: 1980
Author: Edwards G.R.
Publisher Name: Ontario Geological Survey
Location:
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