Ontario Geological Survey
Permanent Link to this Record:
MDI000000000747
Record Name(s) | North Glatz Grid - 2008 |
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Record Status | Occurrence |
Date Created | 2010-Mar-03 |
Date Last Modified | 2022-Aug-04 |
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Revised By |
Primary Commodities: Gold
Township or Area: Turtlepond Lake Area
Latitude: 49° 30' .58" Longitude: -92° 42' 23.48"
UTM Zone: 15 Easting: 521249.999 Northing: 5483099.999 UTM Datum: NAD83
Resident Geologist District: Kenora
NTS Grid: 52F10SE
Point Location Description: Claim Map TurtlePond Lake (G-2595), NTS; 52F10SE
Location Method: Field Visit with GPS
Access Description: The property can be reached by driving on Highway 502 for a distance of 40 km south of Dryden. A gravel logging road (Domtar) Desarre road is used to travel south west for 5 km. From this point a new trail going east traverses the western portion of the grid. The eastern portion of the grid crosses Highway 502.
2008: Canadian Arrow Mines Ltd completed line cutting, prospecting, grab sampling, mechanical trenching and ground geophysical surveys over portions of the North Glatz Grid. In August 2008, RJ Meikle & Associates were contracted to perform ground magnetic and inducted polarization surveys over the Prig showings.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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2.40804, 52F/10SE AA-7 | 20000003978 | 20000003978 |
Province: Superior
Geological Age: Precambrian
Mar 03, 2010 (J Bongfelt) - The North Glatz Grid is underlain by north-south striking, intermediate to mafic volcanics, locally intercalated with felsic agglomerates and tuffs. These volcanic rocks are intruded by numerous sills of mafic to ultramafic composition. Canadian Arrow Mines Ltd geologists identify the following rock types as underlying the property: 1) Mafic Volcanics: The volcanic rocks occupy the western and eastern parts of the grid, with contacts trending north-northeast. The mafic volcanics are medium to dark green color. The rocks are fine-grained and non-magnetic. The volcanic rocks are locally highly carbonatized and silicified. 2) Gabbro I Diorite: The gabbro is generally medium to coarse grained, although medium-grained phases with blue quartz eyes are locally developed throughout most of the property. The blue quartz eyes in the gabbroic rock are evidence of an intrusive origin. The unit is medium to dark green in color. Minor suphide mineralization was found associated with this unit. 3) Pyroxenite: Pyroxenite underlies one area located in the western part of the grid. The pyroxenite is medium grained, dark black and weakly foliated. Minor sulphide mineralization was found associated with this unit. 4) Sediments: Mechanical trenching of NG-2 was located on an airborne VTEM anomaly with a coincident IP response. Light grey massive to weekly foliated sedimentary unit was identified in the trench. Due to the length of several km of the anomaly is likely that the sedimentary unit is the cause of the geophysical response. (Kenora AF 52F10SE AA-7, Cnd Arrow Mines Ltd., North Glatz Grid)
Mar 03, 2010 (J Bongfelt) - Prospecting samples from the east end of the grid has retuned anomalous gold assay values in three samples up to 0.99 gm/t Au. The foliation in these rocks and the gold values indicate more work should be completed in this area. Mapping, prospecting, soil surveys may be required to determine if the gold showing has potential for developing into a larger exploration target. (Kenora AF 52F10SE AA-7, Cnd Arrow Mines Ltd., North Glatz Grid)
Map - Dryden-Wabigoon area, District of Kenora, Ontario
Publication Number: ARM50E Scale: 1:63,360 Date: 1997
Author: Satterly J.
Publisher Name: Ontario Dept. of Mines
Location:
Part - Geology of the Dryden-Wabigoon area
Publication Number: ARV50-02 Date: 1997
Author: Satterly J.
Publisher Name: Ontario Dept. of Mines
Location:
Map - Dryden-Wabigoon area, District of Kenora, Ontario
Publication Number: ARM50E Scale: 1:63,360 Date: 1997
Author: Satterly J.
Publisher Name: Ontario Dept. of Mines
Location:
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For detailed information regarding this mineral record please contact the Kenora Resident Geologist District Office