A note on post-Mississippian thrust faulting in northwestern Cape Breton Island
Thrust faulting, apparently of major proportions, has been observed at five localities in northwestern Cape Breton Island and inferred at several more. The thrust blocks of Precambrian crystalline rocks and Horton Group clastic sedimentary rocks have over-ridden Windsor Group (Viséan–Namurian) rocks...
Published in: | Canadian Journal of Earth Sciences |
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Language: | English |
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Canadian Science Publishing
1977
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Online Access: | http://dx.doi.org/10.1139/e77-254 http://www.nrcresearchpress.com/doi/pdf/10.1139/e77-254 |
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crcansciencepubl:10.1139/e77-254 2024-09-15T18:00:23+00:00 A note on post-Mississippian thrust faulting in northwestern Cape Breton Island Currie, K. L. 1977 http://dx.doi.org/10.1139/e77-254 http://www.nrcresearchpress.com/doi/pdf/10.1139/e77-254 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 14, issue 12, page 2937-2941 ISSN 0008-4077 1480-3313 journal-article 1977 crcansciencepubl https://doi.org/10.1139/e77-254 2024-07-25T04:10:06Z Thrust faulting, apparently of major proportions, has been observed at five localities in northwestern Cape Breton Island and inferred at several more. The thrust blocks of Precambrian crystalline rocks and Horton Group clastic sedimentary rocks have over-ridden Windsor Group (Viséan–Namurian) rocks but not Riversdale Group rocks (Westphalian). Thrusting can be explained by sliding of material from an elongate horst extending from northern Cape Breton Island to southwestern Newfoundland which rose throughout Tournaisian and Viséan time. Article in Journal/Newspaper Breton Island Newfoundland Canadian Science Publishing Canadian Journal of Earth Sciences 14 12 2937 2941 |
institution |
Open Polar |
collection |
Canadian Science Publishing |
op_collection_id |
crcansciencepubl |
language |
English |
description |
Thrust faulting, apparently of major proportions, has been observed at five localities in northwestern Cape Breton Island and inferred at several more. The thrust blocks of Precambrian crystalline rocks and Horton Group clastic sedimentary rocks have over-ridden Windsor Group (Viséan–Namurian) rocks but not Riversdale Group rocks (Westphalian). Thrusting can be explained by sliding of material from an elongate horst extending from northern Cape Breton Island to southwestern Newfoundland which rose throughout Tournaisian and Viséan time. |
format |
Article in Journal/Newspaper |
author |
Currie, K. L. |
spellingShingle |
Currie, K. L. A note on post-Mississippian thrust faulting in northwestern Cape Breton Island |
author_facet |
Currie, K. L. |
author_sort |
Currie, K. L. |
title |
A note on post-Mississippian thrust faulting in northwestern Cape Breton Island |
title_short |
A note on post-Mississippian thrust faulting in northwestern Cape Breton Island |
title_full |
A note on post-Mississippian thrust faulting in northwestern Cape Breton Island |
title_fullStr |
A note on post-Mississippian thrust faulting in northwestern Cape Breton Island |
title_full_unstemmed |
A note on post-Mississippian thrust faulting in northwestern Cape Breton Island |
title_sort |
note on post-mississippian thrust faulting in northwestern cape breton island |
publisher |
Canadian Science Publishing |
publishDate |
1977 |
url |
http://dx.doi.org/10.1139/e77-254 http://www.nrcresearchpress.com/doi/pdf/10.1139/e77-254 |
genre |
Breton Island Newfoundland |
genre_facet |
Breton Island Newfoundland |
op_source |
Canadian Journal of Earth Sciences volume 14, issue 12, page 2937-2941 ISSN 0008-4077 1480-3313 |
op_rights |
http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining |
op_doi |
https://doi.org/10.1139/e77-254 |
container_title |
Canadian Journal of Earth Sciences |
container_volume |
14 |
container_issue |
12 |
container_start_page |
2937 |
op_container_end_page |
2941 |
_version_ |
1810437553163075584 |