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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Language: | English |
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Canadian Science Publishing
1987
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Online Access: | http://dx.doi.org/10.1139/e87-220 http://www.nrcresearchpress.com/doi/pdf/10.1139/e87-220 |
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crcansciencepubl:10.1139/e87-220 2024-09-15T18:20:06+00:00 Fossil evidence for fault-derived stratigraphic repetition in the northeastern Newfoundland Appalachians Pluijm, Ben A. van der Karlstrom, Karl E. Williams, Paul F. 1987 http://dx.doi.org/10.1139/e87-220 http://www.nrcresearchpress.com/doi/pdf/10.1139/e87-220 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 24, issue 12, page 2337-2350 ISSN 0008-4077 1480-3313 journal-article 1987 crcansciencepubl https://doi.org/10.1139/e87-220 2024-07-25T04:10:08Z 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 to repetitions in the stratigraphic sequence.A compilation of the ages of various rock types based on fossil evidence indicates a relatively simple stratigraphy for the Dunnage Zone. This interpretation appears to be at variance with many reported stratigraphic successions, until repetitions by bedding-parallel faulting are taken into account.Examples are given of sequences in which the repetition of various rock types, dated by means of fossils, is due to bedding-parallel faulting. We believe that the simple lithostratigraphy is a reliable aid for structural interpretations in areas where fossils are scarce or absent. Article in Journal/Newspaper Newfoundland Canadian Science Publishing Canadian Journal of Earth Sciences 24 12 2337 2350 |
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Open Polar |
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Canadian Science Publishing |
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crcansciencepubl |
language |
English |
description |
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 to repetitions in the stratigraphic sequence.A compilation of the ages of various rock types based on fossil evidence indicates a relatively simple stratigraphy for the Dunnage Zone. This interpretation appears to be at variance with many reported stratigraphic successions, until repetitions by bedding-parallel faulting are taken into account.Examples are given of sequences in which the repetition of various rock types, dated by means of fossils, is due to bedding-parallel faulting. We believe that the simple lithostratigraphy is a reliable aid for structural interpretations in areas where fossils are scarce or absent. |
format |
Article in Journal/Newspaper |
author |
Pluijm, Ben A. van der Karlstrom, Karl E. Williams, Paul F. |
spellingShingle |
Pluijm, Ben A. van der Karlstrom, Karl E. Williams, Paul F. Fossil evidence for fault-derived stratigraphic repetition in the northeastern Newfoundland Appalachians |
author_facet |
Pluijm, Ben A. van der Karlstrom, Karl E. Williams, Paul F. |
author_sort |
Pluijm, Ben A. van der |
title |
Fossil evidence for fault-derived stratigraphic repetition in the northeastern Newfoundland Appalachians |
title_short |
Fossil evidence for fault-derived stratigraphic repetition in the northeastern Newfoundland Appalachians |
title_full |
Fossil evidence for fault-derived stratigraphic repetition in the northeastern Newfoundland Appalachians |
title_fullStr |
Fossil evidence for fault-derived stratigraphic repetition in the northeastern Newfoundland Appalachians |
title_full_unstemmed |
Fossil evidence for fault-derived stratigraphic repetition in the northeastern Newfoundland Appalachians |
title_sort |
fossil evidence for fault-derived stratigraphic repetition in the northeastern newfoundland appalachians |
publisher |
Canadian Science Publishing |
publishDate |
1987 |
url |
http://dx.doi.org/10.1139/e87-220 http://www.nrcresearchpress.com/doi/pdf/10.1139/e87-220 |
genre |
Newfoundland |
genre_facet |
Newfoundland |
op_source |
Canadian Journal of Earth Sciences volume 24, issue 12, page 2337-2350 ISSN 0008-4077 1480-3313 |
op_rights |
http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining |
op_doi |
https://doi.org/10.1139/e87-220 |
container_title |
Canadian Journal of Earth Sciences |
container_volume |
24 |
container_issue |
12 |
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2337 |
op_container_end_page |
2350 |
_version_ |
1810458466289975296 |