Ontario Geological Survey
Permanent Link to this Record:
MDI31M03NW00023
| Record Name(s) | H.G. Miller, Maiden's Lake Property - 1949, E.B.E. de Camps Estate - 1952, H.R. 69 - 1909 |
|---|---|
| Related Record Type | Simple |
| Related Record(s) | |
| Record Status | Occurrence |
| Date Created | 1980-Aug-26 |
| Date Last Modified | 2022-Dec-05 |
| Created By | |
| Revised By |
Primary Commodities: Silver, Cobalt
Township or Area: South Lorrain
Latitude: 47° 11' 56.16" Longitude: -79° 28' 30.47"
UTM Zone: 17 Easting: 615497 Northing: 5228399 UTM Datum: NAD83
Resident Geologist District: Kirkland Lake
NTS Grid: 31M03NW
Point Location Description: adit
Location Method: AMIS Site Visit
Access Description: From North Cobalt, highway 567 south to Silver Centre. Drive 32.15km. Stop and traverse by foot along SE side of lakeshore.
1963: E. de Camps – DD-1-200 ft. 1999-2000: J. A. Gore Main Showing - DD-1-147.8 m.; sampling and geological mapping of the main showing, assays. magnetometer, HLEM survey. 2008 – Silver Shield Resources Inc. - geological report. 2011: J Gore – magnetometer survey.
| Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
|---|---|---|
| 2.47340 | 20000006529 | 20000006529 |
| 2.21008 | 31M03NW2010 | 31M03NW2010 |
| 31 | 31M03NW0011 | 31M03NW0011 |
| 2.21065 | 31M03NW2012 | 31M03NW2012 |
| CO-1918/ 2.16886 | 31M03NW0043 | 31M03NW0043 |
| 2.38305 | 20000003007 | 20000003007 |
| 2.20596 | 31M03NW2009 | 31M03NW2009 |
Province: Southern
Subprovince: Cobalt Basin
Supergroup: Huronian Supergroup
Formation Group: Cobalt Group
Geological Age: Paleoproterozoic
| Rock Type | Rank | Composition | Texture | Relationship | Vein | 1 | Calcite | Brecciated | Host |
|---|---|---|---|---|
| Conglomerate | 2 | Greywacke | Adjacent | |
| Intermediate lava flow-unsubdivided | 3 | Contains |
Aug 17, 2017 (A Wilson) - Conglomerate, with minor feldspathic quartzite and arkose, overlies the metavolcanics here. Two calcite veins have been reported in the adit. The adit vein strikes N40E and dips 78N and is reportedly up to 18 inches wide. The property lies immediately adjacent to the Maiden’s Lake Fault. Narrow veins of calcite occupy multiple shear zones within mafic to intermediate metavolcanics. The metavolcanics are described as slightly carbonatized and chloritized. The shear zones and veins range from 0.5 to 1.5 ft. in width. Narrow veins of calcite occupy multiple shear zones within mafic to intermediate metavolcanics. The metavolcanics are described as slightly carbonatized and chloritized. The shear zones and veins range from 0.5 to 1.5 ft. in width.
| Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
|---|---|---|---|---|---|---|---|
| 1 | Silver | Economic | Ore | ||||
| 3 | Chalcopyrite | Economic | Gangue |
Aug 17, 2017 (A Wilson) - It is possible that some cobalt or silver bearing veins could have been obliterated by the large, apparently barren carbonate breccia veins. (The breccia veins did not carry anomalous Co in the surface exposures.) It is also possible that some minor silver or cobalt values could have been missed in the sampling. Sections of lost core totaling 2.2 m are reported between 84m and 96m and additional lost core of l .2m near the bottom of the hole. No sludge samples were taken and some significant vein material could therefore have been lost or ground in these sections. However, as no anomalous Ag or Co, at all, was detected in any of the sampling, it seems likely that nothing significant was actually intersected. Two calcite veins have been reported on the adit. The one along the adit strikes N40ºE and dips 78°N with a reported width of 45 centimeters. According to a personal communication from Mr. de Camps to R. Thomson, it was reported to contain 0.48 and 0.42 % cobalt from a vein material near the end of the adit. A second vein found in the adit strikes across the adit with a bearing of N75CVV. This vein was intersected by one of the drill holes put down by G.W. Miller, who reported that it contains cobalt. The mineralization is finely disseminated within brecciated calcite stringers. Typical assays from the sheared veins include: 0.01% Co, tr. Ag over 1.5 ft., 0.76 oz. Ag over 0.5 ft. and 0.38 oz./t Ag over 2 ft.
| Rank | Classification |
|---|---|
| 1 | Vein (Cobalt-Type) |
| Rank | Characteristic |
|---|---|
| 1 | Vein |
File - Resident Geologist files CO-1833
Publication Number: Date:
Author:
Publisher Name:
Location: Kirkland Lake RGP office
MonoMap - Geology of south Lorrain Township, District of Timiskaming
Publication Number: R083 Page: 49-50 Date: 1970
Author: McIlwaine W.H.
Publisher Name: Ontario Dept. of Mines
Location:
Mono - Silver cobalt calcite vein deposits of Ontario
Publication Number: MDC010 Page: 418-419, 439 Date: 1968
Author: Sergiades A.O.
Publisher Name: Ontario Dept. of Mines
Location:
Map - South Lorrain Township, Timiskaming District
Publication Number: M2194 Scale: 1:31,680 Date: 1970
Author: McIlwaine W.H.
Publisher Name: Ontario Dept. of Mines
Location:
Map - South Lorrain Township (north part), District of Timiskaming
Publication Number: P0289 Scale: 1:15,840 Date: 1997
Author: McIlwaine W.H.
Publisher Name: Ontario Dept. of Mines
Location:
Map - Geological Compilation of the Cobalt-Temagami Area, Abitibi Greenstone Belt
Publication Number: P3581 Scale: 1:100,000 Date: 2006
Author: Ayer J.A., Chartrand J.E., Grabowski G.P.B., Josey S.D., Rainsford D.R.B., Trowell N.F.
Publisher Name: Ontario Geological Survey
Location:
Part - South Lorrain Silver Area
Publication Number: ARV18-02.002 Page: 30 Date: 1998
Author: Burrows A.G.
Publisher Name: Ontario Bureau of Mines
Location:
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