Ordovician to Devonian sea-level changes in western and northern Canada
Lower Paleozoic sediments of central, Cordilleran, and arctic Canada are dominated by two megafacies: supratidal to shallow subtidal carbonates and minor evaporites of the platformal (cratonic) areas, and deeper water dark shales and dark limestones of the slope and basinal areas. Large areas of the...
Published in: | Canadian Journal of Earth Sciences |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Canadian Science Publishing
1982
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Online Access: | http://dx.doi.org/10.1139/e82-170 http://www.nrcresearchpress.com/doi/pdf/10.1139/e82-170 |