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Friday, July 17, 2020 | History

1 edition of Precambrian geology and mineral deposits of the Cobalt-Kirkland Lake-Timmins area of Ontario found in the catalog.

Precambrian geology and mineral deposits of the Cobalt-Kirkland Lake-Timmins area of Ontario

Precambrian geology and mineral deposits of the Cobalt-Kirkland Lake-Timmins area of Ontario

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Published by International Geological Congress in Montreal .
Written in English


Edition Notes

11

ID Numbers
Open LibraryOL22013733M


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Precambrian geology and mineral deposits of the Cobalt-Kirkland Lake-Timmins area of Ontario Download PDF EPUB FB2

Precambrian geology and mineral deposits of the Timagami, Cobalt, Kirkland Lake and Timmins Region, Ontario (Field excursion guidebook / International Geological Congress) [E. G Pye] on *FREE* shipping on qualifying offers.

Buy Precambrian geology and mineral deposits of the Timagami, Cobalt, Kirkland Lake and Timmins Region, Ontario (Field excursion guidebook / International Geological Congress) by E. G Pye (ISBN:) from Amazon's Book Store. Everyday low prices and free delivery on eligible orders/5(2).

1] Structural style of the southern Canadian cordillera --[v. 2] Quaternary geology of the southern Canadian Cordillera --[v. 3] Geology of the southern Canadian Cordillera --[v. 4] Plutonic and associated rocks of the coast mountains of British Columbia --[v.

5] Geology of Vancouver area of British Columbia --[v. 6] Mineral deposits along. Pye, E. et al. Precambrian Geology and Mineral Deposits of the Timagami, Cobalt, Kirkland Lake and Timmins Region, Ontario.

International Geological Congress,International Geological Congress, Twenty-Fourth Session, Canada, Field Excursion, Ab-C 96 pages with illustrations. Softbound, very good condition. Guidebook. $ Early Precambrian (Archean) metavolcanic-metasedimentary northeast trending rocks are the principal geological feature of the Northeast Temagami area in which the Niemetz property is located.

This belt averages about 13 kilometers wide and 29 kilometers long with the dominant structure being a northeast trending syncline called the Tetapaga.