Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI31C05NE00146

Record: MDI31C05NE00146

General

Mineral Record Identification
Record Name(s) Allan Mills - 1991
Related Record Type Simple
Related Record(s)
Record Status Discretionary Occurrence
Date Created 1991-Jun-20
Date Last Modified 2024-Mar-22
Created By
Revised By

Commodities

Primary Commodities: Magnetite

Secondary Commodities: Silver, Vanadium



Location

Township or Area: Seymour

Latitude: 44° 24' 26.55"    Longitude: -77° 43' 16.33"

UTM Zone: 18    Easting: 283326.55   Northing: 4920722.67    UTM Datum: NAD83

Resident Geologist District: Southern Ontario

NTS Grid: 31C05NE

Point Location Description: General

Location Method: Conversion from MDI

Access Description: SW of Allan Mills.



Exploration History

1951 and 1953 - Magnetometer survey and 16 d.d. holes by Trent River Iron Limited.


Geology

Province: Grenville

Subprovince: Central Metasedimentary Belt

Terrane: Elzevir

Domain: Belmont

Geological Age: Mesoproterozoic  



Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Gabbro 1 From Andesite To Gabbro And Trap Chloritization, Brecciation And Shearing Host
Conglomerate 2 Adjacent

Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
1MagnetiteEconomicOre
1HematiteEconomicGangue
2PyriteEconomicGangue
3PyrrhotiteEconomicGangue
4ChalcopyriteEconomicGangue

Mineralization Comments

Dec 07, 2005 (D Laidlaw) - Magnetite as disseminations or bands in marble, breccia and gabbro-diorite, overlain by 100 to 150 feet of Paleozoic limestone. Some pyrite, pyrrhotite, chalcopyrite, and hematite present (MDC011, p. 282).


Mar 22, 2024 (Therese Pettigrew) - The magnetite occurrence is only known from drill core, with 15 DDH having been drilled. The first hole intersected a magnetite zone at a depth of about 85 feet directly below the basal Paleozoic conglomerate. An assemblage of andesites to gabbro occur with varying degrees of chloritization, brecciation and shearing. Magnetite is disseminated in the gabbro-diorite as well as in disseminations, stringers, and bands in propylite, breccia, and crystalline limestone. The magnetite zone appears to dip very steeply. It contains some brecciated and sheared magnetite, commonly cemented by carbonates with hematite, and seamed with serpentine veinlets locally containing chlorite and hematite. Some of the serpentine is colloform and some is polished and slickensided along shear surfaces. White asbestos fibres (chrysotile) are present in some of the serpentine. Almost all the magnetite is fine grained and contains disseminations and stringers of pyrite, pyrrhotite and chalcopyrite. Some coarse-grained magnetite forms seams in brecciated zones. Magnetite and sulphides are veined and in part replaced by red hematite in the upper part of the magnetite zone. This was noted to a depth of 90 feet in diamond drill hole No. 1, or to a depth of about 5 feet below the lightly hematite-stained Paleozoic conglomerate. A thin section of a grey, altered, igneous-looking rock in the magnetite-bearing zone shows mainly fibres and flakes of grey serpentine with brownish carbonate, much disseminated coarse-grained pyrite, fine-grained pyrrhotite and some magnetite. Ghost crystals and relict structures represented by serpentine, and fractured crystals of quartz, rimmed, cemented, and replaced in part by pyrite and brown carbonate, are recognizable in places. Pyrite is veined and in part replaced by fine-grained pyrrhotite, magnetite, carbonates, serpentine and epidote. In polished sections rare tiny interstitial grains of ilmenite or hematite occur with fine-grained magnetite, pyrite, pyrrhotite, chalcopyrite and gangue. In one section, fine-grained magnetite replaces schist and a band of pyrite-pyrrhotite in it. Pyrrhotite also replaces pyrite to some extent in this band (Rose, 1958).



Mineral Record Details

References

Publication - Geology of Canada - Rreport of progress from its commencement to 1863; Geological Survey of Canada, Report of Progress 1863

Publication Number: Rep Prog 1863 Page: 676  Date: 1863

Author: Logan, W E; Murray, A; Hunt, T S; Billings, E

Publisher Name: Geological Survey of Canada

Location: https://doi.org/10.4095/123563


Mono - Iron deposits of Ontario

Publication Number: MDC011 Page: 282  Date: 1968

Author: Shklanka R.

Publisher Name: Ontario Dept. of Mines

Location:


Publication - Iron deposits of eastern Ontario and adjoining Quebec; Geological Survey of Canada, Bulletin 45

Publication Number: GSC Bulletin 45 Page: 15-16  Date: 1958

Author: Rose, E.R.

Publisher Name: Geological Survey of Canada

Location: https://doi.org/10.4095/100563


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