Ontario Geological Survey
Permanent Link to this Record:
MDI52H09NE00015
Record Name(s) | Wilport - 1982, East Leitch - 1960, Cryderman - 1930 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 1982-Aug-31 |
Date Last Modified | 2022-May-09 |
Created By | |
Revised By |
Primary Commodities: Gold
Secondary Commodities: Silver
Township or Area: Summers
Latitude: 49° 37' 47.13" Longitude: -88° 0' 37.62"
UTM Zone: 16 Easting: 427030 Northing: 5497957 UTM Datum: NAD83
Resident Geologist District: Thunder Bay North
NTS Grid: 42E12NW, 42E12SW, 52H09NE, 52H09SE
Point Location Description: AMIS location
Location Method: Data Compilation
1929-1930: Mining Corporation of Canada Limited prospected the area and carried out an electromagnetic survey. 1961: Ventures Limited carried out geologic mapping of the Cryderman claim group which consisted of 20 claims adjoining the east boundary of the Leitch Gold Mine property. In conjunction with this mapping, a study of the Leitch Gold Mine vein controls was carried out. 1994: J. McMahon completed a program of prospecting, sampling, geology and VLF-EM. 1994: Morning Dew Exploration carried out a program of prospecting, mechanical stripping and sampling for J. McMahon and M. Rentz on the latter two's claim group. 2008: Kodiak Exploration Ltd. drilled 2 DDH totalling 314 m.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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OP93-689 | 42E12NW0123 | 42E12NW0123 |
63.4129 | 42E12SW0098 | 42E12SW0098 |
63A.377 | 42E12SW0094 | 42E12SW0094 |
2.41729 | 20000004212 | 20000004212 |
Province: Superior
Subprovince: Wabigoon
Belt: Beardmore-Geraldton
Geological Age: Archean
Nov 04, 2019 (Therese Pettigrew) - The East Leitch Project property is situated on the contact between a finger of the central volcanic panel and the overlying southern sedimentary panel within the Beardmore Geraldton belt (Assessment report 20000004212).
Rock Type | Rank | Composition | Texture | Relationship | Mafic lava flow-unsubdivided | 1 | Contains |
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Terrigenous-Clastic-Unsubdivided | 2 | Near | ||
Vein | 3 | Quartz | Host |
Nov 04, 2019 (Therese Pettigrew) - The property is underlain by predominantly mafic to intermediate volcanics. Clastic sediments dominated by feldspathic wacke occur along the northern boundary of the property. The volcanics occupy the nose of a westerly plunging anticline. The dominant rocks are massive, dark green, fine grained to aphanitic, mafic to intermediate flows. Within the flows are thin lapilli tuff units with fragments more felsic than the groundmass, capped with thin pillow tops. Occasional amygdaloidal intercalations of similar composition to the massive flows, contain up to 30% amygdules 2-4 cm in size and composed commonly of quartz, carbonate and chlorite. Both clastic and chemical sediments underlay the northwest portion of the property as well as the immediate surrounding area. The clastic sediments are dominated by feldspathic wackes with lesser thin argillite and polymictic conglomerate interbeds. The conglomerate consists of sub-pebble to cobble sized clasts in a fine to very coarse sand groundmass. Clast compositions include unfoliated granite, fine-grained felsic volcanic, quartz porphyry, fine-grained mafic volcanic, vesicular buff-white volcanic, jasper pebbles and quartz. The chemical sediments in the southern sedimentary panel consist of oxide facies (hematite and/or magnetite±jasper) banded iron formation. The width of the formation is variable up to the approximate 15 metre width south of the East Leitch Project property. Late stage dikes include synvolcanic feldspar and quartz feldspar porphyry dykes as well as diabase dykes. The porphyritic dykes are narrow «4 metres) and contain rounded, 3 to 5 mm. quartz eyes and 1 to 3 mm anhedral feldspar phenocrysts. The diabase occurs on the property as a northerly trending dyke which transects the property. This diabase is texturally and compositionally similar to diabase sheets intersected at both the Northern Empire Mine and the Leitch Gold Mine (Assessment report 20000004212).
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Pyrite | Economic | Ore | ||||
2 | Arsenopyrite | Economic | Ore | ||||
3 | Chalcopyrite | Economic | Ore | ||||
4 | Gold | Economic | Ore | ||||
5 | Tetrahedrite | Economic | Ore |
Nov 04, 2019 (Therese Pettigrew) - The No. 1 Vein has been exposed by trenching for 152 m in an E-W direction. The quartz varies between 30 cm to 2 m in width and is accompanied by a pronounced wall rock alteration (Assessment report 42E12SW0094). DDH EL08-01 returned up to 9.92 g/t Au over 1.6 m from quartz veining in a sheared mafic metavolcanic (Assessment report 20000004212).
Part - The western part of the Sturgeon River area (Sturgeon R.-Beardmore section)
Publication Number: ARV45-02.002 Date: 1998
Author: Laird H.C.
Publisher Name: Ontario Dept. of Mines
Location:
File - Resident Geologist Mineral Deposit Files
Publication Number: Min Dep Date: 1996
Author:
Publisher Name:
Location: Thunder Bay RGP
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