Ontario Geological Survey
Permanent Link to this Record:
MDI000000002238
| Record Name(s) | Western Kidd Resources Inc. DDH W09-20 - 2009 |
|---|---|
| Related Record Type | |
| Related Record(s) | |
| Record Status | Discretionary Occurrence |
| Date Created | 2018-Dec-04 |
| Date Last Modified | 2022-Sep-26 |
| Created By | |
| Revised By |
Primary Commodities: Copper
Secondary Commodities: Zinc
Township or Area: Loveland
Latitude: 48° 37' 59.12" Longitude: -81° 41' 50.54"
UTM Zone: 17 Easting: 448619 Northing: 5386904 UTM Datum: NAD83
Resident Geologist District: Timmins
NTS Grid: 42A12NE
Point Location Description: Approximate
Location Method: Based on Assessment
1999: Prospectors Alliance – Compilation. 2004: Woodruff Capital – Ground geophysics. 2007: Western Kidd Resources Inc. DD – 1 – 618 m, Assays. 2009: Western Kidd Resources Inc. – DD – 1 – 800 m, Assays.
| Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
|---|---|---|
| T-5596 / 2.36541 | 20000002859 | 20000002859 |
| T-6155 / 2.45020 | 20000006084 | 20000006084 |
Province: Superior
Subprovince: Abitibi
Terrane: Wawa-Abitibi
Belt: Abitibi
Geological Age: Archean
| Rock Type | Rank | Composition | Texture | Relationship | Felsic Tuff | 1 | Rhyolite | Tuff | Host |
|---|---|---|---|---|
| Intermediate lava flow-unsubdivided | 2 | Andesite | Hanging Wall | |
| Mafic lava flow-unsubdivided | 3 | Basalt | Footwall |
Dec 04, 2018 (P Bousquet) - T-6155 states: “In the upper part of the hole, above about 300m, bedding angles (to core axis) in tuffs are consistent with about a 60. east dip. From Hathway's work and detailed mapping to the east (Beecham 2005), it is assumed that facings are to the east. In this portion of the hole, a potentially important VMS horizon is recognized at 254.1m where dominantly quartz-phyric,felsic volcanics overlie mafic flows including feldspar-phyric types. Anomalous concentrations of sulphides and base metal are present and the contact is marked by minor chert-like beds". (T-6155)
| Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
|---|---|---|---|---|---|---|---|
| 1 | Pyrrhotite | Economic | Gangue | ||||
| 2 | Pyrite | Economic | Gangue | ||||
| 3 | Sphalerite | Economic | Gangue | ||||
| 4 | Graphite | Economic | Gangue |
Dec 04, 2018 (P Bousquet) - A one metre intersection near the contact between the felsic and mafic units returned an assay of 8251 ppm Cu. It is noted in the report that no sulphides were seen in the core half left in the core box. It is assumed that the anomaly is coming from a laboratory or sampling error (T-6155).
File - Resident Geologist file T-4516
Publication Number: Date:
Author:
Publisher Name:
Location: Timmins Resident Geologist office
Map - Loveland and Macdiarmid townships, Cochrane District
Publication Number: M2288 Scale: 1:31,680 Date: 1974
Author: Middleton R.S.
Publisher Name: Ontario Division of Mines
Location:
MonoMap - Magnetic survey of Loveland and Macdiarmid townships, District of Cochrane
Publication Number: GPR02 Date: 1998
Author: Middleton R.S.
Publisher Name: Ontario Division of Mines
Location:
Map - Timmins data series, Loveland Township, District of Cochrane
Publication Number: P0839-REV Scale: 1:15,840 Date: 1980
Author: Hunt D.S., Richard J.A.
Publisher Name: Ontario Geological Survey
Location:
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: 42A-322 Date: 1985
Author: Rose, D. G.
Publisher Name: Geological Survey of Canada
Location: https://doi.org/10.4095/129999
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