Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI42D09NW00006

Record: MDI42D09NW00006

General

Mineral Record Identification
Record Name(s) Kadrey Energy Corp. - 1983, Cal Dynamics Energy Corp. - 1984
Related Record Type Partial
Related Record(s)
Record Status Occurrence
Date Created 1991-Mar-26
Date Last Modified 2022-Mar-02
Created By
Revised By

Commodities

Primary Commodities: Barite



Location

Township or Area: Pic

Latitude: 48° 41' 56.18"    Longitude: -86° 16' 15.83"

UTM Zone: 16    Easting: 553636.56   Northing: 5394245.46    UTM Datum: NAD83

Resident Geologist District: Thunder Bay South

NTS Grid: 42D09NW

Point Location Description: Precise

Location Method: Conversion from MDI



Exploration History

1983: Kadrey Energy Corp. carried out an IP survey and drilled 7 DDH totaling 123.19 m.


Assessment Work on File

Assessment Work on File
Office File Number Online Assessment File Identifier Online Assessment File Directory
2.6808 42D09NE8287 42D09NE8287
28 42D09NE0192 42D09NE0192
2.6998 42D09NE0180 42D09NE0180



Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Schist-Unsubdivided 1 Graphitic
Terrigenous-Clastic-Unsubdivided 2 Pyrite-Carbonate

Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
1BariteEconomicOre
2PyriteEconomicOre

Mineralization Comments

Dec 17, 2018 (Therese Pettigrew) - The barite-rich unit, 2.8 m wide, striking 85 degrees and dipping 80 degrees S, is associated with graphitic schists and pyrite-carbonate metasediments. The barite unit is light grey-white in colour with minor beds of pyrite-chert-carbonate. In drill core, the massive barite gradually grades into pyrite-rich chert-carbonate. Drilling on a series of Induced Polarization anomalies has intersected 3 parallel barite units, up to 3 m wide, associated with sericite-green mica schists on the footwall. To the north of the stripped barite occurrences are siltstone units, with graded bedding indicating tops to the north. In drill core, rip-up clasts rich in green mica occur within some of the siltstone units. The rocks are cut by numerous lamprophyre dykes. The drill holes cut a number of cataclastic breccias. An assay of the baritic sediment returned 45.9% BaO with a specific gravity of 3.8 (Patterson, 1984).



Mineral Record Details

References

Mono - Field trip guidebook to the Hemlo area

Publication Number: MP118 Scale:     Date: 1984

Author: Patterson G.C.

Publisher Name: Ontario Geological Survey

Location:


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For detailed information regarding this mineral record please contact the Thunder Bay South Resident Geologist District Office