Ontario Geological Survey
Permanent Link to this Record:
MDI42A02SW00067
| Record Name(s) | Oliver-East - 1991, E-Zone - 1991, Oliver Syndicate - 1935 |
|---|---|
| Related Record Type | Simple |
| Related Record(s) | |
| Record Status | Occurrence |
| Date Created | 1991-Mar-16 |
| Date Last Modified | 2023-Mar-08 |
| Created By | |
| Revised By |
Primary Commodities: Gold
Secondary Commodities: Copper
Township or Area: McNeil
Latitude: 48° 7' 26.21" Longitude: -80° 49' 39.53"
UTM Zone: 17 Easting: 512825.974 Northing: 5330091.043 UTM Datum: NAD83
Resident Geologist District: Kirkland Lake
NTS Grid: 42A02SW
Point Location Description: Approximate
Location Method: Conversion from MDI
Access Description: Access is provided by a bush road which branches off to the north from Highway 568, at a distance of 14 miles west of Matachewan. The bush road is usable by truck for a distance of four miles from the highway; beyond this point access is by foot trail along an old tractor road for an additional six miles.
1996: Oliver Group/Canadian Zeolite Project- line cutting, ground geophysical (electromagnetic) survey, and drilling of three diamond drill holes. 1983-1985: Manville Canada Inc.- outcrop stripping, prospecting, geological mapping 1983: Manville Canada Inc.- electromagnetic surveying 1981: Manville Canada Inc.- staking, cutting and chaining of grid lines, magnetometer survey Prior to 1981: Oliver Gold Syndicate- pitting and trenching
| Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
|---|---|---|
| KL4175 | 42A02NW0014 | 42A02NW0014 |
Province: Superior
Subprovince: Abitibi
Terrane: Wawa-Abitibi
Belt: Abitibi
Geological Age: Archean
| Rock Type | Rank | Composition | Texture | Relationship | Intermediate lava flow-unsubdivided | 1 | Andesites | Host |
|---|---|---|---|---|
| Quartz-Feldspar Porphyry | 2 | Quarzt-Feldspar Porphyry Dykes And 'Felsite' Dykes | Contains |
Mar 22, 2010 (J Suma-Momoh) - The property is underlain mainly by Keewatin greenstones grading from pillow-lavas in the north to dioritic types towards the south. The formations have been intruded by felsitic and quartz-porphyry dykes. Diamond drill hole data (hole 96-3) shows mainly fine-grained, medium gray to green meta-andesites and quartz-porphyry dykes.
| Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
|---|---|---|---|---|---|---|---|
| 2 | Gold | Economic | Ore | ||||
| 1 | Pyrite | Economic | Gangue | Disseminated | |||
| 3 | Chalcopyrite | Economic | Gangue |
Mar 22, 2010 (J Suma-Momoh) - The best intersection of the diamond drill hole (Hole 96-3) was a 27-foot wide 'felsite' dyke cut by narrow quartz and quartz-carbonate veins carrying anomalous gold (up to 626 ppb/0.02 oz/t). REF: KL 4175, page 7, A12.
File - Resident Geologist files KL1016, KL1729
Publication Number: Date:
Author:
Publisher Name:
Location: Kirkland Lake RGP office
Mono - Gold deposits of Ontario, part 2, part of District of Cochrane, districts of Muskoka, Nipissing, Parry Sound, Sudbury, Timiskaming, and counties of southern Ontario
Publication Number: MDC018 Page: 213 Date: 1979
Author: Gordon J.B., Lovell H.L., de Grijs J.W., Davie R.F.
Publisher Name: Ontario Geological Survey
Location:
Part - Geology and ore deposits of the Matachewan-Kenogami area
Publication Number: ARV44-02.001 Page: 48-49 Date: 1998
Author: Dyer W.S.
Publisher Name: Ontario Dept. of Mines
Location:
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