Ontario Geological Survey
Permanent Link to this Record:
MDI000000000258
Record Name(s) | McFauld's #5 - 2004, Spider DDH MCF-04-37 - 2004 |
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Related Record Type | |
Record Status | Occurrence |
Date Created | 2007-Mar-19 |
Date Last Modified | 2022-Jan-05 |
Created By | A Wilson |
Revised By | A Wilson |
Primary Commodities: Copper
Township or Area: BMA 527 861
Latitude: 52° 47' 58.59" Longitude: -86° 3' 48.32"
UTM Zone: 16 Easting: 563144 Northing: 5850390 UTM Datum: NAD83
Resident Geologist District: Thunder Bay North
NTS Grid: 43D16SE
Point Location Description: Drill collar for MCF-04-37
Location Method: Field Visit with GPS
Access Description: The site is accessible by air from Nakina
2003-10: Spider Resources Ltd. - MAG, EM, DD-2-461 m, AEM, AMAG gravity survey. 2010-11: Cliffs Chromite Far North – name change, DD-1-177m
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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2.38108 | 20000002923 | 20000002923 |
2.28659 | 43C13NW2001 | 43C13NW2001 |
2.43405 | 20000005401 | 20000005401 |
2.48617 | 20000006568 | 20000006568 |
2.50059 | 20000007685 | 20000007685 |
2.36240 | 20000002823 | 20000002823 |
Province: Superior
Subprovince: Sachigo
Terrane: North Caribou
Geological Age: Archean
Mar 19, 2007 (A Wilson) - The stratigraphic section consists of Archean-aged, steeply dipping, mafic to felsic volcanic rocks with minor amounts of interflow sediments intruded by sills and small stocks of gabbro and granits. The volcanic units have been isoclinally folded to produce a weak to very strong foliation.
Rock Type | Rank | Composition | Texture | Relationship | Intermediate Tuff | 1 | Tuff | Host |
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Mar 19, 2007 (A Wilson) - The drill hole intersected a sequence of intermediate to felsic tuffs, crystal tuffs and agglomerates. A mylonite has been interpreted between 180.61 m and 181.56 m.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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3 | Chalcopyrite | Economic | Ore | ||||
1 | Magnetite | Economic | Gangue | ||||
2 | Pyrite | Economic | Gangue | ||||
Chlorite | Alteration | Chloritic | 1 | Unknown | Replacement | ||
Talc | Alteration | Phyllic | 2 | Unknown | Disseminated |
Aug 01, 2014 (A Wilson) - The drill hole tested a large, strong bull's-eye magnetic anomaly unexplained by two previous drill holes. Mineralization consists of a 4.9 m thick zone of massive magnetite within chlorite-talc altered felsic tuffs. Sparse sulphides are present. The best intersection returned 0.86% Cu over 1.07 m. DDH MCF-10-80 intercepted a massive magnetite + sulphide zone from 165.50-171.80m or a length of 6.3m. The mineralized zone is composed of an upper and lower layer of mostly magnetite (165.50-167.00m and 169.45-171.80m) and a center layer of sulphides (167.00-168.83m). The portion 168.83-169.45m is a non-magnetic country rock with 10cm quartz vein. The magnetite and sulphides occur as fine grained minerals. Pyrites generally comprise the sulphide zones. 8 samples marked 235226 to 235233 were collected from this hole. Of the 8 samples collected for laboratory analysis, 1 sample returned a value of 1.5% Cu
Publication - Preliminary review of a VMS occurrence, McFauld's Lake area, NW Ontario for Spider Resources Inc.
Publication Number: Scale: Date: 2003
Author: Franklin, J. M.
Publisher Name:
Publication - News Releases
Publication Number: Scale: Date:
Author: Spider Resources Ltd.
Publisher Name:
Map - Precambrian Geology of the Hudson Bay and James Bay Lowlands Region Interpreted from Aeromagnetic Data-East Sheet
Publication Number: P3598-REV Scale: 1:500,000 Date: 2008
Author: Stott G.M.
Publisher Name: Ontario Geological Survey
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For detailed information regarding this mineral record please contact the Thunder Bay North Resident Geologist District Office