Ontario Geological Survey
Permanent Link to this Record:
MDI41P12SW00082
Record Name(s) | Walker - 1966, Darwin DDH 1-71 - 1971, Occurrence #43 - 1981, Siragusa #55 - 1993 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Discretionary Occurrence |
Date Created | 1993-Nov-05 |
Date Last Modified | 2022-Jul-15 |
Created By | |
Revised By |
Primary Commodities: Gold, Copper
Secondary Commodities: Silver
Township or Area: Chester
Latitude: 47° 33' 38.17" Longitude: -81° 56' 26.13"
UTM Zone: 17 Easting: 429242.58 Northing: 5267893.7 UTM Datum: NAD83
Resident Geologist District: Timmins
NTS Grid: 41P12SW
Point Location Description: A washed outcrop in which a number of small trenches have been excavated.
Location Method: Field Visit with GPS
Access Description: Easy access is possible as the prospect is adjacent to an old logging road that extends north of the Chester Shannon mine access road. The Chester Shannon road connects to Highway 144 via Mesomikenda Lake. Alternatively the southern extension of the logging road connects with the Sultan access road some 10km to the south.
1966: Shannon Minerals covered the prospect with a horizontal loop electromagnetic survey and geologically mapped the area as part of a program to trace possible extensions to the Young Shannon mineralization. During this program a series of pits and trenches were excavated at the prospect but there is no record of any results. 1970: Darwin Mines acquired an area covering the prospect and carried out a geological evaluation together with a VLF electromagnetic and induced polarization surveys. One diamond drill was cored to test a northeast trending IP anomaly. 1979: Canadian Crest GML flew a magnetic and radiometric survey over the claims to locate a potential source for some radioactive boulders found along the Mollie River and help define the bedrock geology. 1985: Emerald Isle Resources remapped the area and carried out another VLF electromagnetic survey which covered the prospect. No mention of this particular prospect was made in any of the reports but in 1987 three short holes were drilled on a 'Au Zone'. These holes intersected a number pyritic patches and pyrite-quartz fractures and veins but no assays are given. 2007: Augen Gold Corp. – AEM, AMag, ARAD. 2010: Trelawney Mining Augen Acquisition Corp. – GC. Augen Gold Corp. – EM, IP, Mag.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
---|---|---|
T-1751 / 2.2731 | 41P12SW0089 | 41P12SW0089 |
T-2013 / 2.319 | 41P12SW0120 | 41P12SW0120 |
T-2034 / 63A.470 | 41P12SW8459 | 41P12SW8459 |
T-2994 / | 41P12SW0041 | 41P12SW0041 |
T-2994 / | 41P12SW0048 | 41P12SW0048 |
T-5671 / 2.37373 | 20000002805 | 20000002805 |
T-6067 / 2.48167 | 20000006558 | 20000006558 |
T-6453 / 2.52492 | 20000007362 | 20000007362 |
T-1751 / 2.3181 | 41P12SW0083 | 41P12SW0083 |
T-2013 / | 41P12SW0101 | 41P12SW0101 |
T-2034 / 63.1866 | 41P12SW0117 | 41P12SW0117 |
T-2994 / 2.8372 | 41P12SW0064 | 41P12SW0064 |
Province: Superior
Subprovince: Abitibi
Terrane: Wawa-Abitibi
Belt: Swayze
Geological Age: Neoarchean Geochronological Age: 2740 MA Geochron. Age Ref.: GSC OF 3384 G
Dec 07, 2005 (S Fumerton) - The dominant fabric in the area is the occurrence of southeast trending shear zones. These are locally curvy-linear and form a stockwork. Between the shears that are closely spaced there are abundant splay faults which results in a shattered / fragmented appearance. Away from the northern contact a strong foliation / flaser texture is locally present in the outcrops. At the showing these shears take on a slightly different form occurring as en-echelon 'Black Line' faults. These faults are less than 10cm thick and material within the faults are locally brecciated and voids are filled with fine grained tourmaline. At varying intervals within the 'Black Line' faults there are small quartz veins up to 20cm thick.
Rock Type | Rank | Composition | Texture | Relationship | Quartz-Feldspar Porphyry | 1 | Host |
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Schist-Unsubdivided | 2 | Host | ||
Vein | 3 | Quartz-Tourmaline | Host |
Dec 07, 2005 (S Fumerton) - The general host rock to the mineralization is a very fine grained intermediate and felsic contact phase of the Chester Granitoid Complex. This material contains small (<1x4mm) subhedral to anhedral feldspar phenocrysts which form up to 50% of the rock but the typical amount is less than 20%. To the south the matrix of the granitic rocks becomes slightly coarser. A number of diabase dykes occur in the area but are not apparently associated with the mineralization. Chlorite alteration is associated with some of the curvy-linear shear zones that transect the outcrops in the area. The boundaries to the alteration are sharp and the alteration does not extend more than 10cm from the shear zones.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Pyrite | Economic | Gangue | ||||
2 | Hematite | Economic | Gangue | ||||
3 | Tourmaline | Economic | Gangue | ||||
Chlorite | Alteration | Chloritic | 1 | Strong | Replacement | ||
Tourmaline | Alteration | Tourmalinization | 2 | Strong | Veins |
Dec 07, 2005 (S Fumerton) - The mineralization is associated with a series of en-echelon 'Black Line' faults and associated shears. The whole collective mineralized zone is about 10m wide but individual zones are less than a metre thick. Adjacent to the shear zones, splay faults and some of the 'Black Line' faults, fine pyrite is disseminated. Within the quartz veins and to a lessor extent in the 'Black Line' faults there are discontinuous trails of coarse semi-massive pyrite which are up to a centimetre thick.
Dec 07, 2005 (A Wilson) - Grab samples collected from the muck pile by the OGS in 1993 returned assays of 0.02 g/t Au, 0.1 g/t Au; 0.1 g/t Au and 0.3 g/t Ag.
Commodity | Analytical Method | Digestion Method | Result | Unit | Limit | Qualifier |
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Arsenic | Unknown | % | BDL | |||
Arsenic | Unknown | % | BDL | |||
Copper | Unknown | .0058 | % | |||
Copper | Unknown | .0067 | % | |||
Gold | Unknown | .021 | ppm | |||
Gold | Unknown | .103 | ppm | |||
Lead | Unknown | .0004 | % | |||
Lead | Unknown | .0002 | % | |||
Molybdenum | Unknown | .0053 | % | |||
Molybdenum | Unknown | .0016 | % | |||
Silver | Unknown | .1 | ppm | |||
Silver | Unknown | .3 | ppm | |||
Zinc | Unknown | .0005 | % | |||
Zinc | Unknown | .0025 | % |
Rank | Classification |
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1 | Mesothermal |
Rank | Characteristic |
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1 | Sheared |
2 | Vein |
Shape | Length | Thickness | Depth | Strike | Dip | Plunge | Trend | Age | Reference |
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Tabular | 130 | 90 | N/A | N/A |
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-45 Date: 1985
Author: Rose, D. G.
Publisher Name: Geological Survey of Canada
Location: https://doi.org/10.4095/129999
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
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:
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: 457-458 Date: 1995
Author: Fumerton S.L., Houle K.A.
Publisher Name: Ontario Geological Survey
Location:
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