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Ontario Geological Survey
Permanent Link to this Record:
MDI000000001934
Record Name(s) | Dwyer Mine - 1898, C.G. Hyatt - 1929, Mustang Minerals Corp. - 2000 |
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Related Record Type | |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 2016-Jun-27 |
Date Last Modified | 2023-Mar-15 |
Created By | |
Revised By |
Primary Commodities: Gold, Platinum Metals, Copper
Secondary Commodities: Silver
Township or Area: Drury
Latitude: 46° 25' 21" Longitude: -81° 30' 5.04"
UTM Zone: 17 Easting: 461472 Northing: 5141114 UTM Datum: NAD83
Resident Geologist District: Sudbury
NTS Grid: 41I05NE
Point Location Description: shaft
Location Method: Data Compilation
Access Description: Proceed north 4.8km on regional road #4 from its intersection with the Spanish River Road. Follow the powerline right-of-way 2.2km west either on foot or by ATV. Bush crash 1.3km south.
1896-98: John Dwyer Gold Mining Co. – shaft sinking, prospecting, sampling. 1950; Acme Oil and Gas Ltd. –mapping, ground geophysics, stripping, diamond drilling. 1955: Garrison Harbour Gold Mines – DD-1 – 649 ft. 1969: Acme Oil and Gas – mapping, ground geophysics. 1999: Wallbridge Mining Company Ltd. – airborne geophysics. 2000-2001: Mustang Minerals Corp. – magnetometer survey, mapping, sampling.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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Drury-0015-B1/13 | 41I05NE0041 | 41I05NE0041 |
Drury-0024 | 41I05NE0024 | 41I05NE0024 |
2.19996 | 41I06NW2002 | 41I06NW2002 |
2.22852 | 41I06NW2006 | 41I06NW2006 |
2.20809 | 41I06NW2003 | 41I06NW2003 |
Province: Southern
Subprovince: Sudbury Structure
Supergroup: Sudbury Igneous Complex, Main Mass
Geological Age: Paleoproterozoic
Rock Type | Rank | Composition | Texture | Relationship | Gabbro | 1 | Gabbro | Host |
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Vein | 2 | Quartz | Host |
Jun 27, 2016 (A Wilson) - Five parallel east-striking quartz veins occur in an area underlain by altered and brecciated gabbro. All but Vein No. 1 contain nil to low gold and silver values. The No 1 Vein is exposed for about 400 ft. and is up to 40 ft. in width. In a 38 ft. shaft, the vein width varies from 15 ft. as surface to 8 ft. at the bottom.
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 |
Jun 27, 2016 (A Wilson) - Assays of up to 1.41 oz/t Au were reported for the No. 1 vein. Quartz taken from 15 ft from surface assayed $4.60 and quartz taken from the bottom of the shaft assayed $24.00. Quartz taken from a shaft near the west boundary of the property assayed $14.00 to $26.00 gold. The lithogeochemical sampling, which was conducted in the fall 2000 and summer 2001, delineated a weakly anomalous PGE zone (46 to 317 ppb Pd+Pt) hosted within the central part of the intrusion. Within this zone, the PGE mineralization, which is associated with nil to trace sulphides (pyrrhotite, pyrite chalcopyrite), occurs in a medium to coarse-grained gabbrolayer. Chloritized and silicified deformation zones in feldspar-porphyritic gabbro along the northeast boundary of the property contain anomalous PGEs (394 ppb over 5 m and a grab sample of 3536 ppb PGMs). In addition, the widespread elevated background values and the presence of an anomalous zone, suggests that other parts of the intrusion have the potential of hosting an economic PGE deposit. Structural discontinuities, such as northeast-trending fault/shear zones are additional favourable sites for remobilized PGE mineralization. A mineralized quartz vein along one shear zone returned 4.3 % Cu, 507 ppb Au and 12 ppb Pd. One of the main objectives of this study was to evaluate the PGE-Ni-Cu potential of the Drury intrusion. To do this, a total of 202 grab samples were collected and analyzed for Pd, Pt, Au, Cu, Ni and Co. The best PGE values, though only weakly anomalous to anomalous (46 to 317 ppb Pd+Pt), indicate PGE enrichment of the fractionated/cumulate gabbro-anorthosite layer. Altered deformation zones, as well, are enriched in PGEs. The Cu and Ni values range from background to weakly anomalous within the intrusion. The highest Cu value (568 ppm) was returned by a sample (DPOO-34513), taken from a gabbro-anorthosite layer (L6+125W/4+50S) occurring within the central part of the intrusion. A highly anomalous copper-gold value (4% Cu, 507 ppb Au) however, was returned from a quartz vein along a fault zone.
Rank | Classification |
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1 | Vein |
Map - Drury Township, District of Sudbury
Publication Number: P0134 Scale: 1:15,840 Date: 1997
Author: Card K.D.
Publisher Name: Ontario Dept. of Mines
Location:
Map - Hyman and Drury townships, Sudbury District
Publication Number: M2055 Scale: 1:31,680 Date: 1997
Author: Card K.D.
Publisher Name: Ontario Dept. of Mines
Location:
Folio - Drury Township, District of Sudbury
Publication Number: GDIF285 Date: 1997
Author: Sudbury RGO
Publisher Name: Ontario Geological Survey
Location:
Part - Ore deposits near the north shore of Lake Huron
Publication Number: ARV38-07.001 Page: 36-37 Date: 1998
Author: Moore E.S.
Publisher Name: Ontario Dept. of Mines
Location:
Part - Mines of eastern Ontario
Publication Number: ARV07-01.004 Page: 87-88 Date: 1998
Author: Slaght A.
Publisher Name: Ontario Bureau of Mines
Location:
Map - Geology, Sudbury bedrock compilation, Ontario
Publication Number: OF 4570 Scale: 1:50,000 Date: 2005
Author: Ames, D E; Davidson, A; Buckle, J L; Card, K D
Publisher Name: Geological Survey of Canada
Location: https://doi.org/10.4095/221501
MonoMap - Geology of Hyman and Drury townships, District of Sudbury
Publication Number: R034 Page: 34 Date: 1997
Author: Card K.D.
Publisher Name: Ontario Dept. of Mines
Location:
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