Fossil evidence for fault-derived stratigraphic repetition in the northeastern Newfoundland Appalachians
Two types of bedding-parallel faults are common in the Dunnage Zone of eastern Notre Dame Bay. They are (i) early thrusts, which together with bedding were rotated by later folding into steep attitudes; and (ii) postfolding transcurrent faults. Both types of faults occur at all scales and give rise...
Published in: | Canadian Journal of Earth Sciences |
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Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Canadian Science Publishing
1987
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Subjects: | |
Online Access: | http://dx.doi.org/10.1139/e87-220 http://www.nrcresearchpress.com/doi/pdf/10.1139/e87-220 |