Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI31C15SE00112

Record: MDI31C15SE00112

General

Mineral Record Identification
Record Name(s) Deer Lake Inlet - 1989
Related Record Type Simple
Record Status Occurrence
Date Created 1991-Jun-25
Date Last Modified 2022-Jan-05
Created By Q Unknown
Revised By A Wilson

Commodities

Primary Commodities: Anorthosite, Garnet (Gemstones)



Location

Township or Area: South Sherbrooke, South Sherbrooke

Latitude: 44° 46' 50.71"    Longitude: -76° 33' 43.01"

UTM Zone: 18    Easting: 376426   Northing: 4959782    UTM Datum: NAD83

Resident Geologist District: Southern Ontario

NTS Grid: 31C15SE

Point Location Description: General

Location Method: Data Compilation

Access Description: Inlet of Deer Lake from Rock Lake.



Geology

Province: Grenville

Subprovince: Central Metasedimentary Belt

Terrane: Frontenac

Geological Age: Mesoproterozoic  



Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Gabbro 1 Anorthositic Gabbro Host
Anorthosite 2 Contains

Lithology Comments

Sep 19, 2015 (A Wilson) - The rock type Is composed primarily of anorthosite and anorthositic gabbro. Large areas contain >90% feldspar with minor amounts of pyroxene. This body is very massive, especially in its interior. The anorthositic gabbro is interlayered with varied amounts of medium to fine-grained, dark weathering horneblende gabbro. This is a dark bluish-grey anorthosite of the Lanark-Oso mafic intrusion. It is medium-grained, generally massive and contains mafic inclusions which appear to have parallel alignment.




Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
1AnorthiteEconomicOre
2CorundumEconomicOre

Mineralization Comments

Sep 19, 2015 (A Wilson) - Chemical analysis of eight samples of anorthosite show the purest phases to contain 30-33% Al2O3. Corundum is limited to discrete zones. In outcrop, the corundum is excellently formed, coarse-grained, and euhedral.



Mineral Record Details

Characteristics
Rank Characteristic            
1 Disseminated

References

Mono - Building stone potential in eastern Ontario

Publication Number: OFR5706 Scale:     Date: 1989

Author: LeBaron P.S., Verschuren C.P., Papertzian V.C., Kingston P.W., Chevrier R.L.

Publisher Name: Ontario Geological Survey


Map - Sharbot Lake, southern Ontario

Publication Number: M2471 Scale: 1:31,680    Date: 1985

Author: Wolff J.M.

Publisher Name: Ontario Geological Survey


Map - Precambrian Geology, Sharbot Lake Area

Publication Number: P3440 Scale: 1:50,000    Date: 2001

Author: Easton R.M.

Publisher Name: Ontario Geological Survey


MonoMap - Geology of the Sharbot Lake area, Frontenac and Lanark counties, southeastern Ontario

Publication Number: R228 Scale:     Date: 1985

Author: Wolff J.M.

Publisher Name: Ontario Geological Survey


Report an Error

We are continuously updating our assessment file / technical report information. If you notice errors in the data, please contact us.


Terms of Use

Please review our Terms of Use agreement for this data product.


Ministry Contact Information

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