Ontario Geological Survey
Permanent Link to this Record:
MDI41P12SE00019
Record Name(s) | Mcauley Vein B - 1922, Siragusa #97 - 1993 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Discretionary Occurrence |
Date Created | 2000-Mar-01 |
Date Last Modified | 2022-Jul-15 |
Created By | |
Revised By |
Primary Commodities: Gold
Township or Area: Champagne
Latitude: 47° 32' 50.89" Longitude: -81° 40' 18.47"
UTM Zone: 17 Easting: 449450.45 Northing: 5266223.9 UTM Datum: NAD83
Resident Geologist District: Timmins
NTS Grid: 41P12SE
Point Location Description: McAuley B vein transcribed from sketch map
Location Method: Data Compilation
Access Description: Presently, the access into the area is difficult. The road from Highway 144 which is about 20 km long, has been washed out 8 km from the highway and the bridge across the Mollie River is no longer safe for large vehicles. Therefore it is best to take all terrain vehicles to the general area of the prospect near the power line.
1922: McAuley and Thompson - prospecting, stripping, trenching. 1971: Molly River Mines - ground magnetometer and EM survey, diamond drilling. 1984: Hargor Resources - airborne magnetometer and Em survey. 1985: Blue Falcon Mines: airborne magnetic and VLF survey. 1990: Blue Falcon Mines: airborne magnetic and EM survey. 2010 – 2011: 1571925 Ontario Ltd.- EM, Mag.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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T-2012 / 2.600 | 41P12SE0523 | 41P12SE0523 |
T-3020 / W8906-00006 | 41P12SE5008 | 41P12SE5008 |
T-6381 / 2.50897 | 20000007088 | 20000007088 |
T-3020 / 2.13771 | 41P12SE0520 | 41P12SE0520 |
T-2357 / 2.3559 | 41O09NW9161 | 41O09NW9161 |
T-2012 / | 41P12SE0524 | 41P12SE0524 |
Province: Superior
Subprovince: Abitibi
Terrane: Wawa-Abitibi
Belt: Swayze
Geological Age: Neoarchean
Rock Type | Rank | Composition | Texture | Relationship | Granodiorite | 1 | Near |
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Vein | 2 | Quartz | Host |
Jun 14, 2013 (A Wilson) - The mineralized vein is hosted in a chloritic schist which is a xenolith in a granodiorite which is part of the Chester Granitoid Complex.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Gold | Economic | Ore | ||||
1 | Chalcopyrite | Economic | Gangue |
Dec 07, 2005 (A Wilson) - The quartz vein is white with locally abundant chalcopyrite.
Rank | Classification |
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1 | Mesothermal |
Rank | Characteristic |
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1 | Vein |
Shape | Length | Thickness | Depth | Strike | Dip | Plunge | Trend | Age | Reference |
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Tabular | 5 | 30 |
Map - Precambrian Geology, Parts of Champagne, Groves, St. Louis and Benneweis Townships
Publication Number: OFM0209 Scale: 1:15,840 Date: 1993
Author: Siragusa G.M.
Publisher Name: Ontario Geological Survey
Location:
MonoMap - Geology, Geochemistry and Mineralization of the Southern Margin of the Swayze Belt
Publication Number: OFR5844 Page: 121 Date: 1993
Author: Siragusa G.M.
Publisher Name: Ontario Geological Survey
Location:
MonoMap - Mineral Prospects of the Swayze Greenstone Belt (Volume 1, Parts of NTS 41 O and Volume 2, Parts of NTS 41 P, 42 A and 42 B)
Publication Number: OFR5912 Page: 385-386 Date: 1995
Author: Fumerton S.L., Houle K.A.
Publisher Name: Ontario Geological Survey
Location:
Publication - Gold Occurrence At Makwa, Sudbury District, Ontario; Geological Survey of Canada, Summary Report 1922, part D
Publication Number: GSC SR 1922D Date: 1924
Author: Tanton, T L
Publisher Name: Geological Survey of Canada
Location: https://doi.org/10.4095/100570
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For detailed information regarding this mineral record please contact the Timmins Resident Geologist District Office