Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI31E08SE00008

Record: MDI31E08SE00008

General

Mineral Record Identification
Record Name(s) H. Bolton Property - 1932
Related Record Type Simple
Related Record(s)
Record Status Prospect
Date Created 1999-Dec-09
Date Last Modified 2023-Jun-13
Created By
Revised By

Commodities

Primary Commodities: Feldspar (Nonmetals)

Secondary Commodities: Rare Earth Elements, Uranium, Niobium



Location

Township or Area: Sabine

Latitude: 45° 20' 48.13"    Longitude: -78° 2' 41"

UTM Zone: 17    Easting: 731511.001   Northing: 5025715.003    UTM Datum: NAD83

Resident Geologist District: Southern Ontario

NTS Grid: 31E08SE

Point Location Description: quarry

Location Method: AMIS Site Visit

Access Description: At the point where old highway 127 departs from new highway 127 upon entering Sabine Twp at the south end take a bearing of 063° and proceed for 1.1km to feature.



Exploration History

1924-1925: Mahoney and Morin - in production. 1955-56: ground geophysics, stripping


Geology

Province: Grenville

Subprovince: Central Gneiss Belt

Geological Age: Mesoproterozoic  



Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Pegmatite 1 Host
Gneiss-Unsubdivided 2 Contains

Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
1MicroclineEconomicOre
2EuxeniteEconomicOre
3BiotiteEconomicGangue

Mineralization Comments

Feb 22, 2012 (A Wilson) - The pegmatite consists of a coarse graphic intergrowth of quartz and microcline with occasional patches of microcline crystals up to 3 feet in length. Nodules of martite were common but did not assay greater than 1% TiO2. Euxenite occurs as masses up to 4 inches in diameter and is often associated with biotite, in microcline. The euxenite crystals returned 0.26% BeO, 0.05% ZrO2, 28.62% Cb2O3, 3.94% ThO2 and 24.31% (Yt,Er) 2O3


Feb 22, 2012 (D Laidlaw) - Euxenite occurs in a microcline-quartz dike with abundant biotite. In 1932 several carloads of feldspar bad been produced from the 12- to 20- foot wide dike.



Mineral Record Details

Classification
RankClassification            
1 Pegmatite

Mineral Zones - Size and Shape

Zone Name: Detour Lake - Rank 1
Shape Length Thickness Depth Strike Dip Plunge Trend Age Reference
Tabular 1000 15
Production Data
Year Tonnes Commodities Reference Comment
1925 181 Feldspar 731, p.53 total production 1924-25; 200 tons

References

Mono - Uranium and thorium deposits of southern Ontario

Publication Number: OFR5311 Page: 394  Date: 1981

Author: Gordon J.B., Rybak U.C., Robertson J.A.

Publisher Name: Ontario Geological Survey

Location:


Publication - Rare-element minerals of Canada; Geological Survey of Canada, Economic Geology Series 11

Publication Number: GSC EconGeol 11 Page: 195-196  Date: 1932

Author: Ellsworth, H V

Publisher Name: Geological Survey of Canada

Location: https://doi.org/10.4095/102445


Mono - Pegmatite mineral resources of Ontario

Publication Number: IMR021 Page: 21  Date: 1997

Author: Hewitt D.F.

Publisher Name: Ontario Dept. of Mines

Location:


MonoMap - Columbium (niobium) deposits of Ontario

Publication Number: MDC014 Page: 50  Date: 1971

Author: Ferguson S.A.

Publisher Name: Ontario Dept. of Mines and Northern Affairs

Location:


Map - Haliburton area, Province of Ontario

Publication Number: ARM52A Scale: 1:126,720    Date: 1998

Author: Satterly J.

Publisher Name: Ontario Dept. of Mines

Location:


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