A trondhjemite vein in the Sulitjelma Gabbro, Norway, and its implications for the age of the Sulitjelma Ophiolite

Summary The Sulitjelma Gabbro, occurring as a member of the Sulitjelma Ophiolite Complex, and typical of the ophiolite suite in its petrography and geochemistry, is cut by a vein of trondhjemite (plagiogranite). The previous identification of the vein as an offshoot of a continental potassium-rich g...

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Published in:Geological Magazine
Main Author: Mason, Roger
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1981
Subjects:
Online Access:http://dx.doi.org/10.1017/s001675680003288x
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S001675680003288X
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spelling crcambridgeupr:10.1017/s001675680003288x 2024-03-03T08:49:02+00:00 A trondhjemite vein in the Sulitjelma Gabbro, Norway, and its implications for the age of the Sulitjelma Ophiolite Mason, Roger 1981 http://dx.doi.org/10.1017/s001675680003288x https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S001675680003288X en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Geological Magazine volume 118, issue 5, page 525-531 ISSN 0016-7568 1469-5081 Geology journal-article 1981 crcambridgeupr https://doi.org/10.1017/s001675680003288x 2024-02-08T08:33:28Z Summary The Sulitjelma Gabbro, occurring as a member of the Sulitjelma Ophiolite Complex, and typical of the ophiolite suite in its petrography and geochemistry, is cut by a vein of trondhjemite (plagiogranite). The previous identification of the vein as an offshoot of a continental potassium-rich granite, the Furulund Granite, is wrong. Therefore the Rb-Sr isochron age of 413±34 Ma, obtained from the granite, cannot be taken as the age of intrusion of the Sulitjelma Gabbro. Article in Journal/Newspaper Sulitjelma Cambridge University Press Norway Sulitjelma ENVELOPE(16.077,16.077,67.133,67.133) Furulund ENVELOPE(22.080,22.080,69.727,69.727) Geological Magazine 118 5 525 531
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Geology
spellingShingle Geology
Mason, Roger
A trondhjemite vein in the Sulitjelma Gabbro, Norway, and its implications for the age of the Sulitjelma Ophiolite
topic_facet Geology
description Summary The Sulitjelma Gabbro, occurring as a member of the Sulitjelma Ophiolite Complex, and typical of the ophiolite suite in its petrography and geochemistry, is cut by a vein of trondhjemite (plagiogranite). The previous identification of the vein as an offshoot of a continental potassium-rich granite, the Furulund Granite, is wrong. Therefore the Rb-Sr isochron age of 413±34 Ma, obtained from the granite, cannot be taken as the age of intrusion of the Sulitjelma Gabbro.
format Article in Journal/Newspaper
author Mason, Roger
author_facet Mason, Roger
author_sort Mason, Roger
title A trondhjemite vein in the Sulitjelma Gabbro, Norway, and its implications for the age of the Sulitjelma Ophiolite
title_short A trondhjemite vein in the Sulitjelma Gabbro, Norway, and its implications for the age of the Sulitjelma Ophiolite
title_full A trondhjemite vein in the Sulitjelma Gabbro, Norway, and its implications for the age of the Sulitjelma Ophiolite
title_fullStr A trondhjemite vein in the Sulitjelma Gabbro, Norway, and its implications for the age of the Sulitjelma Ophiolite
title_full_unstemmed A trondhjemite vein in the Sulitjelma Gabbro, Norway, and its implications for the age of the Sulitjelma Ophiolite
title_sort trondhjemite vein in the sulitjelma gabbro, norway, and its implications for the age of the sulitjelma ophiolite
publisher Cambridge University Press (CUP)
publishDate 1981
url http://dx.doi.org/10.1017/s001675680003288x
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S001675680003288X
long_lat ENVELOPE(16.077,16.077,67.133,67.133)
ENVELOPE(22.080,22.080,69.727,69.727)
geographic Norway
Sulitjelma
Furulund
geographic_facet Norway
Sulitjelma
Furulund
genre Sulitjelma
genre_facet Sulitjelma
op_source Geological Magazine
volume 118, issue 5, page 525-531
ISSN 0016-7568 1469-5081
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/s001675680003288x
container_title Geological Magazine
container_volume 118
container_issue 5
container_start_page 525
op_container_end_page 531
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