Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI000000002313

Record: MDI000000002313

General

Mineral Record Identification
Record Name(s) Snowbank Pegmatite - 2018
Related Record Type
Record Status Occurrence
Date Created 2019-Jul-29
Date Last Modified 2021-Nov-30
Created By Therese Pettigrew
Revised By Therese Pettigrew

Commodities

Primary Commodities: Lithium



Location

Township or Area: Paterson Lake Area

Latitude: 50° 16' 52.71"    Longitude: -94° 32' 41.2"

UTM Zone: 15    Easting: 389940   Northing: 5571050    UTM Datum: NAD83

Resident Geologist District: Kenora

NTS Grid: 52L07SE

Point Location Description: OGS staff field visit

Location Method: Field Visit with GPS



Exploration History

2018: Avalon Advanced Materials Inc. carried out prospecting, mapping, sampling, and channel sampling.


Geology

Province: Superior

Subprovince: English River

Belt: Separation Lake

Geological Age: Archean  



Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Pegmatite 1 Is

Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
1PetaliteEconomicOre
1FeldsparEconomicGangue
2AlbiteEconomicGangue
3QuartzEconomicGangue

Mineralization Comments

Jul 29, 2019 (Therese Pettigrew) - The Snowbank Pegmatite was discovered in a large outcrop area traceable for 127 m along strike (open under overburden at both ends) averaging 6 m wide. The lithium occurs primarily in the ore mineral petalite, which occurs as large crystals up to 15 cm in diameter. Individual channel samples have yielded assays of up to 2.51% Li2O over 1.1 m, indicating that petalite comprises approximately 50% of the mineral content in the rock sampled. The main Snowbank Pegmatite zone is up to 9 m wide, but pinches and swells with some sections bifurcating into two to three smaller parallel dykes from 1 to 3 m in width, for a combined average width of 6 m, over the 100 m exposure. Individual dykes exhibit classic pegmatite zoning features, with an internal assemblage of coarse petalite, potassium feldspar, albite and quartz, flanked by narrow albitic border and wall zones. Three channel samples collected from the petalite mineralized sections of the main Snowbank Pegmatite zone average 1.40% Li2O, while three other parallel dykes, also sampled, locally host similar mineralization over narrower widths. Highlights include lithium values of 1.53% Li2O over 2.6 m in channel 1A; 1.61% Li2O over 2.3 m in channel 2B; and 1.07% Li2O over 2.9 m in channel 4A - comprising six out of 11 analyzed samples (Avalon Advanced Materials Sept 4, 2018 and Nov 30, 2021 news releases).



Mineral Record Details

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For detailed information regarding this mineral record please contact the Kenora Resident Geologist District Office