Sedimentology of the Dezadeash flysch and its implications for strike-slip faulting along the Denali Fault, Yukon Territory and Alaska
The Dezadeash Formation of Late Jurassic – Early Cretaceous age is a flysch sequence with a thickness of about 3000 m. It consists of turbidites, mass-flow deposits, and argillite. Most of the formation was deposited on a deep-sea fan system fed by an uplifted volcanogenic terrane to the west. Along...
| 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
1976
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| Online Access: | https://doi.org/10.1139/e76-157 http://www.nrcresearchpress.com/doi/pdf/10.1139/e76-157 |