Ontario Geological Survey
Permanent Link to this Record:
MDI41K16SW00030
Record Name(s) | Lucinda Mine - 1904 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Discretionary Occurrence |
Date Created | 1991-Sep-01 |
Date Last Modified | 2022-Apr-26 |
Created By | |
Revised By |
Primary Commodities: Lead, Zinc
Secondary Commodities: Gold
Township or Area: Fenwick
Latitude: 46° 46' 16.34" Longitude: -84° 23' 37.72"
UTM Zone: 16 Easting: 698976.998 Northing: 5183038.002 UTM Datum: NAD83
Resident Geologist District: Sault Ste. Marie
NTS Grid: 41K16SW
Point Location Description: Shaft
Location Method: AMIS Site Visit
Access Description: Drive along Anderson Road from highway 17 west for 1.45 km to end of road and north on ATV trail for 1.7km north to northwest to site.
1904: Lucinda Gold Mining Company - shaft sinking, stripping. 1970: W. Doughty - stripping, trenching 1971-83: Ontario Geological Survey - sampling, site visit
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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FENWICK 0010-B1 | 41K16SW0020 | 41K16SW0020 |
Province: Superior
Subprovince: Abitibi
Terrane: Wawa-Abitibi
Geological Age: Neoarchean
Dec 07, 2005 (P Beach) - Sulphides in chert in greywacke.
Rock Type | Rank | Composition | Texture | Relationship | Terrigenous-Clastic-Unsubdivided | 1 | Tuffaceous | Hanging Wall |
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Mafic lava flow-unsubdivided | 2 | Footwall |
May 04, 2011 (A Wilson) - The shaft is inclined at about 70° north. The hanging wall of the shaft is a dark grey tuff or greywacke with fragments to 3/8". The footwall appears to be a basaltic or andesitic rock with pale creamy, green selvages. The rock in which the shaft was sunk is mainly dark greywacke with two 1-foot bands of chert, and minor siliceous laminae in the greywacke.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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3 | Sphalerite | Economic | Ore | ||||
4 | Galena | Economic | Ore | ||||
5 | Chalcopyrite | Economic | Ore | ||||
1 | Pyrrhotite | Economic | Gangue | ||||
2 | Pyrite | Economic | Gangue |
May 04, 2011 (A Wilson) - The cherty beds contain about 10% pyrrhotite, 3% pyrite, about 1% of sphalerite and galena and a trace of chalcopyrite. Spectacular splashes of chalcopyrite, galena and sphalerite, as well as pyrite and pyrrhotite are present on a few fractures in the greywacke. Analysis of a chip sample from the two chert beds gave negative results, as follows: Au and Ag, trace only; Pb, 0.03%; Zn, 0.03%. W. Doughty reported that he obtained negative results when he burned and panned specimens for gold. The beds of chert strike 098° and dip 72° north. A grab sample of the sulphide-bearing chert, collected by P. Born in 1985 returned 120 ppb Au.
Map - Geological series, Precambrian geology, Havilland-Goulais Bay area, Algoma District
Publication Number: P2959 Scale: 1:15,840 Date: 1986
Author: Born P., Worona R., Stephenson C.D.
Publisher Name: Ontario Geological Survey
Location:
Mono - Geology of the Havilland-Goulais Bay area, District of Algoma
Publication Number: OFR5602 Page: 65-66 Date: 1987
Author: Born P.
Publisher Name: Ontario Geological Survey
Location:
Part - Sault Ste. Marie area, District of Algoma
Publication Number: ARV35-02.001 Page: 46 Date: 1998
Author: McConnell R.G.
Publisher Name: Ontario Dept. of Mines
Location:
Part - Mines of western Ontario
Publication Number: ARV14-01.003 Page: 59 Date: 1998
Author: Carter W.E.H.
Publisher Name: Ontario Bureau of Mines
Location:
Book - Sudbury Timmins Algoma Mineral Program, Project 1: mineral inventory of the Sudbury-Timmins-Sault Ste. Marie region, Ontario
Publication Number: GSC OF 1087 Page: 132 Date: 1985
Author: Rose, D. G.
Publisher Name: Geological Survey of Canada
Location: https://doi.org/10.4095/129999
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