Ontario Geological Survey
Permanent Link to this Record:
MDI52F09SE00015
| Record Name(s) | Glatz Occurrence - Dumond Property - 1900, Lady Marion Prospect - 1900 |
|---|---|
| Related Record Type | Simple |
| Related Record(s) | |
| Record Status | Occurrence |
| Date Created | 1991-Feb-27 |
| Date Last Modified | 2022-Jul-06 |
| Created By | |
| Revised By |
Primary Commodities: Gold
Township or Area: Hyndman
Latitude: 49° 33' 44.84" Longitude: -92° 6' 34.98"
UTM Zone: 15 Easting: 564380.673 Northing: 5490364.962 UTM Datum: NAD83
Resident Geologist District: Kenora
NTS Grid: 52F09SE
Point Location Description: Transfer
Location Method: Conversion from MDI
Access Description: The Lady Marion Prospect is located on mining location H.W. 525 in lot 6, Concession IV of Revell Township. The property can be found by walking 1.37 km west from Tache along the C.P.R. Railroad track. The prospect is 152 metres due north of the railroad track.
1900: Shaft reported to be sunk on the claim.
| Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
|---|---|---|
| 2.5679 / 52F09SE I-3 | 52F09SE0025 | 52F09SE0025 |
Province: Superior
Subprovince: Wabigoon
Terrane: Western Wabigoon
Belt: Eagle-Wabigoon-Manitou
Geological Age: Precambrian
| Rock Type | Rank | Composition | Texture | Relationship | Mafic lava flow-unsubdivided | 1 | Amphibolitized | Contains |
|---|---|---|---|---|
| Diorite | 2 | |||
| Vein | 3 | quartz |
| Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
|---|---|---|---|---|---|---|---|
| 5 | Pyrite | Economic | Ore |
Jul 06, 2022 (Q Unknown) - Best assay: 0.132 opt Au. The occurrence is situated at the contact between dioritic rocks of the Revell Batholith and amphibolitized mafic metavolcanic flows. Two shafts have been sunk on a 0.9 m to 1.2 m wide shear zone striking 310°/ 60° -70° SW within medium-grained, biotite-hornblende diorite. The shear zone controls a stock work of milk-white quartz veins and stringers with rusty brown and red hematite staining. The wall rocks are intensely sheared, iron carbonatized, and chloritic. The quartz veins and wall rocks contain < 1% pyrite. Wall rocks in the dumps at the two shafts consists of biotite-hornblende diorite containing small [<1.0 mm], blue, quartz "eyes" and amphibolitized, porphyritic, mafic metavolcanic flows containing large [<1.5 cm], white feldspar phenocrysts. A 0.45 m chip sample, taken by the author, across a quartz vein in a trench 4.6 m west of the south shaft assayed <2 ppb gold. A grab sample of quartz vein material from the dump at the north shaft assayed <2 ppb gold. (OFR 5723, p.225)
Article - Kenora Resident Geologist's area, Northwestern Region
Publication Number: MP134.001 Page: 19 Date: 1997
Author: Blackburn C.E., Hailstone M.H., Parker J.R., Storey C.C.
Publisher Name: Ontario Geological Survey
Location:
Mono - Geology, gold mineralization and property visits in the area investigated by the Dryden-Ignace economic geologist, 1984-1987
Publication Number: OFR5723 Page: 225 Date: 1989
Author: Parker J.R.
Publisher Name: Ontario Geological Survey
Location:
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