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...

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Published in:Canadian Journal of Earth Sciences
Main Author: Hyndman, R. D.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1975
Subjects:
Online Access:http://dx.doi.org/10.1139/e75-095
http://www.nrcresearchpress.com/doi/pdf/10.1139/e75-095
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spelling 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
institution Open Polar
collection 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
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