A 1950 ± 60 Ma Rb–Sr whole-rock isochron age from two Kangâmiut dykes and the timing of the Nagssugtoqidian (Hudsonian) orogeny in West Greenland

Thirteen samples from two Kangâmiut dykes give a Rb–Sr whole-rock isochron age of 1950 ± 60 Ma. This age is interpreted as the age of intrusion of the dykes. The post-dyke Nagssugtoqidian orogeny took place between ca. 2000 and ca. 1800 Ma and can be correlated with the Hudsonian in Canada and the L...

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Published in:Canadian Journal of Earth Sciences
Main Authors: Kalsbeek, F., Bridgwater, D., Zeck, H. P.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1978
Subjects:
Online Access:http://dx.doi.org/10.1139/e78-118
http://www.nrcresearchpress.com/doi/pdf/10.1139/e78-118
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spelling crcansciencepubl:10.1139/e78-118 2024-09-15T18:09:21+00:00 A 1950 ± 60 Ma Rb–Sr whole-rock isochron age from two Kangâmiut dykes and the timing of the Nagssugtoqidian (Hudsonian) orogeny in West Greenland Kalsbeek, F. Bridgwater, D. Zeck, H. P. 1978 http://dx.doi.org/10.1139/e78-118 http://www.nrcresearchpress.com/doi/pdf/10.1139/e78-118 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 15, issue 7, page 1122-1128 ISSN 0008-4077 1480-3313 journal-article 1978 crcansciencepubl https://doi.org/10.1139/e78-118 2024-07-25T04:10:07Z Thirteen samples from two Kangâmiut dykes give a Rb–Sr whole-rock isochron age of 1950 ± 60 Ma. This age is interpreted as the age of intrusion of the dykes. The post-dyke Nagssugtoqidian orogeny took place between ca. 2000 and ca. 1800 Ma and can be correlated with the Hudsonian in Canada and the Laxfordian in Scotland. Article in Journal/Newspaper Greenland Canadian Science Publishing Canadian Journal of Earth Sciences 15 7 1122 1128
institution Open Polar
collection Canadian Science Publishing
op_collection_id crcansciencepubl
language English
description Thirteen samples from two Kangâmiut dykes give a Rb–Sr whole-rock isochron age of 1950 ± 60 Ma. This age is interpreted as the age of intrusion of the dykes. The post-dyke Nagssugtoqidian orogeny took place between ca. 2000 and ca. 1800 Ma and can be correlated with the Hudsonian in Canada and the Laxfordian in Scotland.
format Article in Journal/Newspaper
author Kalsbeek, F.
Bridgwater, D.
Zeck, H. P.
spellingShingle Kalsbeek, F.
Bridgwater, D.
Zeck, H. P.
A 1950 ± 60 Ma Rb–Sr whole-rock isochron age from two Kangâmiut dykes and the timing of the Nagssugtoqidian (Hudsonian) orogeny in West Greenland
author_facet Kalsbeek, F.
Bridgwater, D.
Zeck, H. P.
author_sort Kalsbeek, F.
title A 1950 ± 60 Ma Rb–Sr whole-rock isochron age from two Kangâmiut dykes and the timing of the Nagssugtoqidian (Hudsonian) orogeny in West Greenland
title_short A 1950 ± 60 Ma Rb–Sr whole-rock isochron age from two Kangâmiut dykes and the timing of the Nagssugtoqidian (Hudsonian) orogeny in West Greenland
title_full A 1950 ± 60 Ma Rb–Sr whole-rock isochron age from two Kangâmiut dykes and the timing of the Nagssugtoqidian (Hudsonian) orogeny in West Greenland
title_fullStr A 1950 ± 60 Ma Rb–Sr whole-rock isochron age from two Kangâmiut dykes and the timing of the Nagssugtoqidian (Hudsonian) orogeny in West Greenland
title_full_unstemmed A 1950 ± 60 Ma Rb–Sr whole-rock isochron age from two Kangâmiut dykes and the timing of the Nagssugtoqidian (Hudsonian) orogeny in West Greenland
title_sort 1950 ± 60 ma rb–sr whole-rock isochron age from two kangâmiut dykes and the timing of the nagssugtoqidian (hudsonian) orogeny in west greenland
publisher Canadian Science Publishing
publishDate 1978
url http://dx.doi.org/10.1139/e78-118
http://www.nrcresearchpress.com/doi/pdf/10.1139/e78-118
genre Greenland
genre_facet Greenland
op_source Canadian Journal of Earth Sciences
volume 15, issue 7, page 1122-1128
ISSN 0008-4077 1480-3313
op_rights http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining
op_doi https://doi.org/10.1139/e78-118
container_title Canadian Journal of Earth Sciences
container_volume 15
container_issue 7
container_start_page 1122
op_container_end_page 1128
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