Purcell supergroup, Fernie west-half, southeastern British Columbia
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Purcell supergroup, Fernie west-half, southeastern British Columbia by Trygve Höy

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Published by Ministry of Energy, Mines and Petroleum Resources in Victoria, B.C .
Written in English

Subjects:

  • Geology -- British Columbia -- Fernie Region,
  • Mines and mineral resources -- British Columbia -- Fernie Region,
  • Geology -- British Columbia -- Purcell supergroup

Book details:

Edition Notes

Statementby Trygve Höy.
SeriesBulletin (British Columbia. Ministry of Energy, Mines and Petroleum Resources) -- 76.
Classifications
LC ClassificationsBRITCBULL#76 1985
The Physical Object
Pagination79 p. :
Number of Pages79
ID Numbers
Open LibraryOL22073390M
ISBN 100771884761
LC Control Number85-222082

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Klippen of Purcell Supergroup rocks are as much as km from the mountain front northeast of Mokowan Butte area (Fig. 2; Douglas, ). Assuming a minimum age for the Flaxville-Blackfoot surface of ca. Ma and that the mountain front was continuous with the easternmost klippen when the Interior Plains was at the level of the Flaxville. Early Precambrian greenstone belts (Chapter 10) are relatively uniform and lithologically “simple”, with a limited selection of rock types. This is the consequence of less diversified early crustal Author: Peter Laznicka. The southern Canadian Foreland Fold and Thrust Belt forms a north-eastward tapering contractional belt comprising Mesoproterozoic intracontinental, Palaeozoic continental margin and Mesozoic to lower Cited by: 8. The lower Rocky Mountain Supergroup of Pennsylvanian age contains five formations which in ascending order are: Todhunter, Tyrwhitt, Storelk, Tobermory and Kananaskis. All except the Kananaskis are new formations that are equivalent to the Tunnel Mountain Formation. The Todhunter, Tyrwhitt and Tobermory consist mainly of brown weathering, dolomitic and .