A Mid-Mesozoic Breccia from the Coast of Labrador

A unique occurrence of Mesozoic breccia cut by lamprophyric-carbonatite dikelets, near Makkovik, Labrador is interpreted to relate to the opening of the Labrador Sea. The breccia has been dated by nannofossils; vitrinite reflectance studies show that some time during or after deposition the rock was...

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Published in:Canadian Journal of Earth Sciences
Main Authors: King, A. F., McMillan, N. J.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1975
Subjects:
Online Access:http://dx.doi.org/10.1139/e75-005
http://www.nrcresearchpress.com/doi/pdf/10.1139/e75-005
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spelling crcansciencepubl:10.1139/e75-005 2024-09-15T18:09:30+00:00 A Mid-Mesozoic Breccia from the Coast of Labrador King, A. F. McMillan, N. J. 1975 http://dx.doi.org/10.1139/e75-005 http://www.nrcresearchpress.com/doi/pdf/10.1139/e75-005 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 12, issue 1, page 44-51 ISSN 0008-4077 1480-3313 journal-article 1975 crcansciencepubl https://doi.org/10.1139/e75-005 2024-07-25T04:10:05Z A unique occurrence of Mesozoic breccia cut by lamprophyric-carbonatite dikelets, near Makkovik, Labrador is interpreted to relate to the opening of the Labrador Sea. The breccia has been dated by nannofossils; vitrinite reflectance studies show that some time during or after deposition the rock was heated to at least 170 °C. It is suggested that shallow seas extended westward beyond the present Labrador Marginal Trough during early Jurassic time and that the period of late alkaline igneous activity is related to the rifting between Greenland and Labrador that commenced about the middle of the Mesozoic Era. Article in Journal/Newspaper Greenland Labrador Sea Makkovik Canadian Science Publishing Canadian Journal of Earth Sciences 12 1 44 51
institution Open Polar
collection Canadian Science Publishing
op_collection_id crcansciencepubl
language English
description A unique occurrence of Mesozoic breccia cut by lamprophyric-carbonatite dikelets, near Makkovik, Labrador is interpreted to relate to the opening of the Labrador Sea. The breccia has been dated by nannofossils; vitrinite reflectance studies show that some time during or after deposition the rock was heated to at least 170 °C. It is suggested that shallow seas extended westward beyond the present Labrador Marginal Trough during early Jurassic time and that the period of late alkaline igneous activity is related to the rifting between Greenland and Labrador that commenced about the middle of the Mesozoic Era.
format Article in Journal/Newspaper
author King, A. F.
McMillan, N. J.
spellingShingle King, A. F.
McMillan, N. J.
A Mid-Mesozoic Breccia from the Coast of Labrador
author_facet King, A. F.
McMillan, N. J.
author_sort King, A. F.
title A Mid-Mesozoic Breccia from the Coast of Labrador
title_short A Mid-Mesozoic Breccia from the Coast of Labrador
title_full A Mid-Mesozoic Breccia from the Coast of Labrador
title_fullStr A Mid-Mesozoic Breccia from the Coast of Labrador
title_full_unstemmed A Mid-Mesozoic Breccia from the Coast of Labrador
title_sort mid-mesozoic breccia from the coast of labrador
publisher Canadian Science Publishing
publishDate 1975
url http://dx.doi.org/10.1139/e75-005
http://www.nrcresearchpress.com/doi/pdf/10.1139/e75-005
genre Greenland
Labrador Sea
Makkovik
genre_facet Greenland
Labrador Sea
Makkovik
op_source Canadian Journal of Earth Sciences
volume 12, issue 1, page 44-51
ISSN 0008-4077 1480-3313
op_rights http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining
op_doi https://doi.org/10.1139/e75-005
container_title Canadian Journal of Earth Sciences
container_volume 12
container_issue 1
container_start_page 44
op_container_end_page 51
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