Marginal Basins of the Labrador Sea and the Davis Strait Hot Spot
There are deep marginal sedimentary basins in the Labrador Sea extending to the region of Davis Strait. In contrast, the central part of the Sea shoals toward Davis Strait. The difference is explained by the central part of the Sea being formed while the Davis Strait hot spot was active, producing i...
Published in: | Canadian Journal of Earth Sciences |
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Language: | English |
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Canadian Science Publishing
1975
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Online Access: | http://dx.doi.org/10.1139/e75-095 http://www.nrcresearchpress.com/doi/pdf/10.1139/e75-095 |
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crcansciencepubl:10.1139/e75-095 2024-09-15T18:03:31+00:00 Marginal Basins of the Labrador Sea and the Davis Strait Hot Spot Hyndman, R. D. 1975 http://dx.doi.org/10.1139/e75-095 http://www.nrcresearchpress.com/doi/pdf/10.1139/e75-095 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 12, issue 6, page 1041-1045 ISSN 0008-4077 1480-3313 journal-article 1975 crcansciencepubl https://doi.org/10.1139/e75-095 2024-07-25T04:10:08Z There are deep marginal sedimentary basins in the Labrador Sea extending to the region of Davis Strait. In contrast, the central part of the Sea shoals toward Davis Strait. The difference is explained by the central part of the Sea being formed while the Davis Strait hot spot was active, producing increased vulcanism and crustal thickness. The sea floor along the margins was produced before the hot spot became active about 60 m.y. ago, so has normal crustal thickness and thus normal basement depth. Article in Journal/Newspaper Davis Strait Labrador Sea Canadian Science Publishing Canadian Journal of Earth Sciences 12 6 1041 1045 |
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Open Polar |
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Canadian Science Publishing |
op_collection_id |
crcansciencepubl |
language |
English |
description |
There are deep marginal sedimentary basins in the Labrador Sea extending to the region of Davis Strait. In contrast, the central part of the Sea shoals toward Davis Strait. The difference is explained by the central part of the Sea being formed while the Davis Strait hot spot was active, producing increased vulcanism and crustal thickness. The sea floor along the margins was produced before the hot spot became active about 60 m.y. ago, so has normal crustal thickness and thus normal basement depth. |
format |
Article in Journal/Newspaper |
author |
Hyndman, R. D. |
spellingShingle |
Hyndman, R. D. Marginal Basins of the Labrador Sea and the Davis Strait Hot Spot |
author_facet |
Hyndman, R. D. |
author_sort |
Hyndman, R. D. |
title |
Marginal Basins of the Labrador Sea and the Davis Strait Hot Spot |
title_short |
Marginal Basins of the Labrador Sea and the Davis Strait Hot Spot |
title_full |
Marginal Basins of the Labrador Sea and the Davis Strait Hot Spot |
title_fullStr |
Marginal Basins of the Labrador Sea and the Davis Strait Hot Spot |
title_full_unstemmed |
Marginal Basins of the Labrador Sea and the Davis Strait Hot Spot |
title_sort |
marginal basins of the labrador sea and the davis strait hot spot |
publisher |
Canadian Science Publishing |
publishDate |
1975 |
url |
http://dx.doi.org/10.1139/e75-095 http://www.nrcresearchpress.com/doi/pdf/10.1139/e75-095 |
genre |
Davis Strait Labrador Sea |
genre_facet |
Davis Strait Labrador Sea |
op_source |
Canadian Journal of Earth Sciences volume 12, issue 6, page 1041-1045 ISSN 0008-4077 1480-3313 |
op_rights |
http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining |
op_doi |
https://doi.org/10.1139/e75-095 |
container_title |
Canadian Journal of Earth Sciences |
container_volume |
12 |
container_issue |
6 |
container_start_page |
1041 |
op_container_end_page |
1045 |
_version_ |
1810440998892863488 |