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Ontario Geological Survey
Permanent Link to this Record:
MDI41P12SW00040
Record Name(s) | Shannon Island 2 - 1984, Our Island - 1933, Young Island - 1934, Siragusa #54 - 1993 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 1993-Aug-06 |
Date Last Modified | 2022-Sep-23 |
Created By | |
Revised By |
Primary Commodities: Gold
Township or Area: Chester
Latitude: 47° 32' 44.83" Longitude: -81° 57' 20.25"
UTM Zone: 17 Easting: 428091.57 Northing: 5266260.69 UTM Datum: NAD83
Resident Geologist District: Timmins
NTS Grid: 41P12SW
Point Location Description: Flooded pit measuring 2x2x2m on a small island in Clam Lake
Location Method: Field Visit with GPS
Access Description: Access is possible via boat from a landing at the north end of the lake on the Chester Shannon mine access road from Highway 144.
1933: The occurrence was found by the Chester Shannon Group - Young Shannon GML. Reported gold values ranged between 15 and 19 g/t gold ($8.80 to 0.56opt) in a quartz vein. 1934: Young Shannon GML started shaft sinking on the adjacent Shannon Island. During this period the vein on Our Island (Young Island) was resampled and reported values ranged between 7.8 and 22 g/t gold (0.23, to 0.64opt). 1965: Chester Minerals Ltd acquired the property and carried out a program of geological mapping, magnetic and HLEM electromagnetic surveying. Based on this work 5 holes were drilled to test targets east of Our Island. 1973: Park Precious Metals optioned the property but no work was directed towards the gold occurrence on Our Island. Results of a nearby diamond drill hole cored at this time were reported as 'of no economic value'. 1980: Hargor Resources together with Canadian Gold and Metal Inc carried out a regional airborne magnetic and VLF electromagnetic survey which covered the area. 1984: Chester Minerals carried out a geological evaluation of the occurrence in combination with other known occurrences on Clam Lake and resampled the mineralization with the following result 0.29 g/t Au 46ppm Cu. Chester Minerals Limited – EM, Mag. 1987: Young Shannon Gold Partnership carried out a 7 holes diamond drill program to test the mineralization in the area. No holes intersected the known vein. 2010: Robert, P. – EM, Mag. Trelawney Mining and Exploration Inc. – AEM, AMag.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
---|---|---|
T-2023 / 63A.470 | 41P12SW8459 | 41P12SW8459 |
T-2023 / 63.1866 | 41P12SW0117 | 41P12SW0117 |
T-2034 / 63.1866 | 41P12SW0117 | 41P12SW0117 |
T-6043 / 2.44000 | 20000004358 | 20000004358 |
T-6382 / 2.50730 | 20000007118 | 20000007118 |
T-2023 / 63.4435 | 41P12SW0999 | 41P12SW0999 |
T-2034 / 63A.470 | 41P12SW8459 | 41P12SW8459 |
T-3201 / 63.4941 | 41P12SW0052 | 41P12SW0052 |
T-2357 / 2.3559 | 41O09NW9161 | 41O09NW9161 |
Province: Superior
Subprovince: Abitibi
Terrane: Wawa-Abitibi
Belt: Swayze
Geological Age: Neoarchean Geochronological Age: 2740 MA Geochron. Age Ref.: GSC OF 3384A
Dec 07, 2005 (S Fumerton) - The mineralization is located in a narrow shear zone that transects the host granodiorite. This shear is up to 2m thick. There are abundant fractures near to the main shear zone. These are both subparallel with, and discordant to the shear zone. The vein on the mainland strikes 236 deg.
Rock Type | Rank | Composition | Texture | Relationship | Granodiorite | 1 | Host |
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Schist-Unsubdivided | 2 | Sericite | Schist | Near |
Vein | 3 | Quartz-Sulphide | Vein | Host |
Vein | 4 | Quartz-Sulphide | Host |
Dec 07, 2005 (S Fumerton) - Medium grained granodiorite with an off white to pink weathered surface and a pale green fresh surface. Quartz forms 20 - 30% of the rock and fine grained amphibole forms 10 - 15%. Local sericitic alteration occurs in the shear zone. Just north of the shear zone that has been pitted, and mostly under water, there is a banded and locally brecciated intensely silicified and carbonated material. This alteration may be centred on a shear. On the mainland near Our Island is a shear zone with strong chlorite alteration and a pinkish tint to the quartz diorite. This alteration emphasises the original blue quartz grains.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
---|---|---|---|---|---|---|---|
1 | Pyrite | Economic | Ore | ||||
1 | Pyrrhotite | Economic | Gangue | ||||
2 | Specularite | Economic | Gangue | ||||
Chlorite | Alteration | Chloritic | 1 | Strong | Replacement |
Dec 07, 2005 (S Fumerton) - Medium grained semi massive pyrite veins occur in a silicified shear zone. The individual veins are attenuated and range between 3 and 5cm. The shear zone is also cut by a network of thin quartz stringers (<<10cm) containing sparse disseminated pyrite in very fine grained milky quartz. One quartz pod measuring 0.3 x 2m also occurs in the shear zone. Sulphides are concentrated in the western part of the exposed shear zone. On the mainland the extensive trenching is centred on a quartz - carbonate - sulphide - specularite vein. Pyrite and specularite each make up about 20% of the vein and pyrite also occurs along fractures in the vein.
Dec 07, 2005 (A Wilson) - At the time of discovery reported gold values from grab samples averaged between 15-19 g/t Au. The vein was resampled in 1934 and returned values of between 7.8 and 22 g/t Au. Diamond drilling has returned poor gold values. Grab samples collected by the OGS in 1980 returned values of 3.8 g/t Au. Grab samples collected by the OGS in 1993 returned values of: 1.05 g/t Au, 0.3 g/t Ag; 3.6 g/t Au, 0.7 g/t Ag; 1.22 g/t Au, 1.6 g/t Ag; 2.35 g/t Au, 1.1 g/t Ag; 0.0g g/t Au, 0.1 g/t Ag.
Commodity | Analytical Method | Digestion Method | Result | Unit | Limit | Qualifier |
---|---|---|---|---|---|---|
Copper | Unknown | .0033 | % | |||
Copper | Unknown | .0043 | % | |||
Copper | Unknown | .76 | % | |||
Copper | Unknown | .0031 | % | |||
Copper | Unknown | .0096 | % | |||
Gold | Unknown | 3.8 | g/t | |||
Gold | Unknown | .06 | g/t | |||
Gold | Unknown | 3.61 | g/t | |||
Gold | Unknown | 1.22 | g/t | |||
Gold | Unknown | 2.35 | g/t | |||
Gold | Unknown | 1.05 | g/t | |||
Lead | Unknown | .0008 | % | |||
Lead | Unknown | .001 | % | |||
Lead | Unknown | .0021 | % | |||
Lead | Unknown | .0012 | % | |||
Lead | Unknown | .0013 | % | |||
Molybdenum | Unknown | .0002 | % | |||
Molybdenum | Unknown | .0022 | % | |||
Molybdenum | Unknown | .0006 | % | |||
Molybdenum | Unknown | .0009 | % | |||
Molybdenum | Unknown | .0006 | % | |||
Silver | Unknown | .1 | g/t | |||
Silver | Unknown | 1.1 | g/t | |||
Silver | Unknown | 1.6 | g/t | |||
Silver | Unknown | .7 | g/t | |||
Silver | Unknown | .3 | g/t | |||
Zinc | Unknown | .0028 | % | |||
Zinc | Unknown | .0058 | % | |||
Zinc | Unknown | .0027 | % | |||
Zinc | Unknown | .0059 | % | |||
Zinc | Unknown | .0085 | % |
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 | 20 | 2 | 255 | 60 | N/A | N/A |
Date: Jul 28, 1954
Geologist: W Savage
Notes: On the west side of the island there is a 'blowout' of quartz and sulphides in a weakly sheared breccia. The shearing strikes N75E and dips 60N. Sulphides observed were pyrite and pyrrhotite. [ PRECIS ]
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: 41P-64 Date: 1985
Author: Rose, D. G.
Publisher Name: Geological Survey of Canada
Location: https://doi.org/10.4095/129999
File - Resident Geologist files T-6349
Publication Number: Date:
Author:
Publisher Name:
Location: Timmins RGP office
Map - Three Duck Lakes area, District of Sudbury, Ontario
Publication Number: ARM41D Scale: 1:47,520 Date: 1997
Author: Laird H.C.
Publisher Name: Ontario Dept. of Mines
Location:
Map - Geological series, Precambrian geology of Chester and Yeo townships, and parts of Neville and Potier townships, Jerome area, Sudbury District
Publication Number: P2449 Scale: 1:15,840 Date: 1981
Author: Siragusa G.M.
Publisher Name: Ontario Geological Survey
Location:
Map - Precambrian Geology, Parts of Chester, Neville, Potier and Yeo Townships
Publication Number: OFM0214 Scale: 1:15,840 Date: 1993
Author: Siragusa G.M.
Publisher Name: Ontario Geological Survey
Location:
Map - Geology, Swayze greenstone belt, Gogama, Ontario
Publication Number: OF3384G Scale: 1:50,000 Date: 1999
Author: Heather, K B; Shore, G T
Publisher Name: Geological Survey of Canada
Location: https://doi.org/10.4095/210455
MonoMap - Geology, Geochemistry and Mineralization of the Southern Margin of the Swayze Belt
Publication Number: OFR5844 Page: 88 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: 409-411 Date: 1995
Author: Fumerton S.L., Houle K.A.
Publisher Name: Ontario Geological Survey
Location:
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