Ontario Geological Survey
Permanent Link to this Record:
MDI41P12SW00033
Record Name(s) | Claim S19970 - 1984, #19 Vein - 1935, The Ditch - 1980, Occurrence #28 - 1981, Young Shannon B Zone - 1987, Siragusa #56 - 1993 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Developed Prospect Without Reported Reserves or Resources |
Date Created | 1993-Jul-30 |
Date Last Modified | 2022-Sep-23 |
Created By | |
Revised By |
Primary Commodities: Gold, Copper
Township or Area: Chester
Latitude: 47° 33' 39.47" Longitude: -81° 55' 29.92"
UTM Zone: 17 Easting: 430417.58 Northing: 5267919.7 UTM Datum: NAD83
Resident Geologist District: Timmins
NTS Grid: 41P12SW
Point Location Description: North side of an open cut adjacent to a mine access road
Location Method: Field Visit with GPS
Access Description: Access from Highway 144 is easy. This can be done by taking the Mesomikenda Lake road to the lake of the same name. Then the Young Shannon mine access road crosses some narrows and eventually passes right by the open cut.
1931: Three Ducks Syndicate - prospecting. 1934: Martin Syndicate - prospecting. 1935: Young Shannon Gold Mines Ltd. - exploration program. 1946: Young Shannon Gold Mines Ltd. - diamond drilling. 1965: Gogama Gold Mines Ltd. - geological reconnaissance, ground VLF-EM and magnetic survey. 1973: Park Precious Metals Inc. - IP survey, diamond drilling. 1975-79: Canadian Crest Gold Mines Ltd. - underground rehabilitation, mining. 1980: Hargor Resources - Canadian Gold and Metals Inc. - airborne magnetic and VLE-EM survey. 1984-90: Young Shannon Gold Mines Ltd. - ground VLF-EM survey, IP survey, diamond drilling (45 ddh - 7020 m). 1986: Wesport Resources Inc. – DD, GL, IP, Samp. 2010: Trelawney Mining and Exploration Inc. – AEM, AMag.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
---|---|---|
T-2020 / 63A.470 | 41P12SW8459 | 41P12SW8459 |
T-3201 / 63.5079 | 41P12SW0035 | 41P12SW0035 |
T-6382 / 2.50730 | 20000007118 | 20000007118 |
T-3201 / 63.4941 | 41P12SW0052 | 41P12SW0052 |
T-2357 / 2.3559 | 41O09NW9161 | 41O09NW9161 |
T-2020 / 63.1866 | 41P12SW0117 | 41P12SW0117 |
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) - There are numerous subparallel joints and slicken sided surfaces are present along the walls of the vein. A shear foliation is also present locally. There is also a rhombohedral fracture pattern present in the rocks which locally has acted as a conduit for chlorite alteration.
Rock Type | Rank | Composition | Texture | Relationship | Granodiorite | 1 | Host |
---|---|---|---|---|
Vein | 2 | Quartz-Sulphide | Vein | Host |
Dec 07, 2005 (S Fumerton) - The host rock is a medium grained, weakly foliated granodiorite with 20 - 30% quartz, 2 - 5 % mafic minerals. The quartz typically has a blue - grey opalescent appearance. Near the vein the granodiorite has a darker colour which may be due to fine grained chlorite alteration. Also there are local patches where the host rock has a pink/ purple tint which may be indicative of hematite alteration. Locally massive, dark green chlorite and pink calcite occur as fracture fillings. Malachite commonly occurs as a wide spread, thin film along joint surfaces. In contrast recent white sulphate alteration is restricted to the vein with some malachite streaks.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
---|---|---|---|---|---|---|---|
1 | Pyrite | Economic | Ore | ||||
2 | Chalcopyrite | Economic | Ore | ||||
3 | Bornite | Economic | Ore | ||||
4 | Gold | Economic | Ore | ||||
Chlorite | Alteration | Chloritic | 1 | Weak | Replacement | ||
Malachite | Alteration | Supergene | 2 | Weak | Disseminated | ||
Azurite | Alteration | Supergene | 3 | Weak | Disseminated |
Dec 07, 2005 (S Fumerton) - Mineralization is centred on a quartz/sulphide vein that pinches and swells between 10cm and 40cm in thickness. Adjacent to this main vein there are a number of small subparallel carbonate veins, quartz veins with wall rock fragments, and coarse grained, quartz - iron carbonate veins. The mineralization occurs as fine disseminated sulphide grains in the matrix of the adjacent granodiorite and in a semi massive portion of the vein structure varying between 4 and 10cm thick. The vein itself is a composite vein consisting of very fine grained quartz, a quartz breccia set in a chloritic/sulphide matrix, and massive sulphides.
Dec 07, 2005 (A Wilson) - Assay results obtained from diamond drilling on the B Zone ranged up to 41 g/t Au. Grab samples collected by the OGS in 1979 returned values of 16.1 g/t Au; 19.88 g/t Au and 32.91 g/t Ag; 1.37 g/t Au. Samples collected by the OGS in 1980 returned values of 6.5 g/t Au; 2.4 g/t Au, 8.2 g/t Au, 6.2 g/t Au and 9.9 g/t Au.
Commodity | Analytical Method | Digestion Method | Result | Unit | Limit | Qualifier |
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Copper | Unknown | .56 | % | |||
Copper | Unknown | .175 | % | |||
Copper | Unknown | .338 | % | |||
Copper | Unknown | .165 | % | |||
Copper | Unknown | .538 | % | |||
Copper | Unknown | 1.45 | % | |||
Copper | Unknown | .72 | % | |||
Copper | Unknown | .14 | % | |||
Gold | Unknown | 19.88 | g/t | |||
Gold | Unknown | 8.2 | g/t | |||
Gold | Unknown | 1.37 | g/t | |||
Gold | Unknown | 9.9 | g/t | |||
Gold | Unknown | 16.1 | g/t | |||
Gold | Unknown | 2.4 | g/t | |||
Gold | Unknown | 6.2 | g/t | |||
Gold | Unknown | 6.5 | g/t | |||
Silver | Unknown | 32.91 | g/t |
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 |
---|---|---|---|---|---|---|---|---|---|
Tabular | 150 | 284 | 60 | N/A | N/A |
Date: Jul 27, 1993
Geologist: S Fumerton
Notes: In the company of Bill Yee this mineral occurrence was visited. The site consists of a 75-100m long open cut that is between 2 and 4m deep. This cut dips to the north and the hanging wall overhangs the workings. The footwall is generally more gradational. To the east a series of overgrown trenches and pits extend the workings another 75m. These pits and trenches are up to 2m deep with gradual walls and locally filled with water. Gangue has been dumped to the southwest of the workings. The Young Shannon mine access road makes a short detour around the west end of the open cut. There is no fence or signs marking the open cut. The lack of notices was brought to the attention of an affiliate of the property owner and it was stated that such notices would be installed. To the south there are additional trenches which have been put down to test a parallel vein structure.
Year | Tonnes | Commodities | Reference | Comment |
---|---|---|---|---|
1979 | 3265 |
Gold 2575 Grams |
Production was carried out for a two month period and the ore was processed at t |
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-38 Date: 1985
Author: Rose, D. G.
Publisher Name: Geological Survey of Canada
Location: https://doi.org/10.4095/129999
File - Resident Geologist files T-6350
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:
Mono - Preliminary report on the Timmins-Kirkland Lake area, gold deposits file
Publication Number: OFR5467 Date: 1983
Author: Hodgson C.J.
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
Article - 1979 report of Northern Regional Geologist and Timmins Resident Geologist
Publication Number: MP091.005 Date: 1997
Author: Luhta L.E.
Publisher Name: Ontario Geological Survey
Location:
MonoMap - Geology, Geochemistry and Mineralization of the Southern Margin of the Swayze Belt
Publication Number: OFR5844 Page: 88-89 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: 401-403 Date: 1995
Author: Fumerton S.L., Houle K.A.
Publisher Name: Ontario Geological Survey
Location:
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