Age, palaeomagnetism and chemistry of melilite basalts in the Southern Cape, South Africa

Summary Post-Karroo melilite basalts intrude Cretaceous and older sedimentary units in the Cape Province, South Africa. K-Ar ages determined from 4 occurrences range from 63–75 Ma b.p. (Late Cretaceous to earliest Tertiary) and are significantly older than alkaline intrusions to the 5, on the Alphar...

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Published in:Geological Magazine
Main Authors: Duncan, R. A., Hargraves, R. B., Brey, G. P.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1978
Subjects:
Online Access:http://dx.doi.org/10.1017/s001675680003733x
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S001675680003733X
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spelling crcambridgeupr:10.1017/s001675680003733x 2024-06-16T07:39:11+00:00 Age, palaeomagnetism and chemistry of melilite basalts in the Southern Cape, South Africa Duncan, R. A. Hargraves, R. B. Brey, G. P. 1978 http://dx.doi.org/10.1017/s001675680003733x https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S001675680003733X en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Geological Magazine volume 115, issue 5, page 317-327 ISSN 0016-7568 1469-5081 journal-article 1978 crcambridgeupr https://doi.org/10.1017/s001675680003733x 2024-05-22T12:55:56Z Summary Post-Karroo melilite basalts intrude Cretaceous and older sedimentary units in the Cape Province, South Africa. K-Ar ages determined from 4 occurrences range from 63–75 Ma b.p. (Late Cretaceous to earliest Tertiary) and are significantly older than alkaline intrusions to the 5, on the Alphard Bank. These igneous intrusions may be part of a linear trend that connects young oceanic volcanism at Bouvet Island with Cretaceous kimberlitic activity in southern Africa. This lineament nearly parallels the Walvis Ridge and a hot spot model for its origin is examined. Article in Journal/Newspaper Bouvet Island Cambridge University Press Bouvet ENVELOPE(3.358,3.358,-54.422,-54.422) Bouvet Island ENVELOPE(3.358,3.358,-54.422,-54.422) Geological Magazine 115 5 317 327
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collection Cambridge University Press
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language English
description Summary Post-Karroo melilite basalts intrude Cretaceous and older sedimentary units in the Cape Province, South Africa. K-Ar ages determined from 4 occurrences range from 63–75 Ma b.p. (Late Cretaceous to earliest Tertiary) and are significantly older than alkaline intrusions to the 5, on the Alphard Bank. These igneous intrusions may be part of a linear trend that connects young oceanic volcanism at Bouvet Island with Cretaceous kimberlitic activity in southern Africa. This lineament nearly parallels the Walvis Ridge and a hot spot model for its origin is examined.
format Article in Journal/Newspaper
author Duncan, R. A.
Hargraves, R. B.
Brey, G. P.
spellingShingle Duncan, R. A.
Hargraves, R. B.
Brey, G. P.
Age, palaeomagnetism and chemistry of melilite basalts in the Southern Cape, South Africa
author_facet Duncan, R. A.
Hargraves, R. B.
Brey, G. P.
author_sort Duncan, R. A.
title Age, palaeomagnetism and chemistry of melilite basalts in the Southern Cape, South Africa
title_short Age, palaeomagnetism and chemistry of melilite basalts in the Southern Cape, South Africa
title_full Age, palaeomagnetism and chemistry of melilite basalts in the Southern Cape, South Africa
title_fullStr Age, palaeomagnetism and chemistry of melilite basalts in the Southern Cape, South Africa
title_full_unstemmed Age, palaeomagnetism and chemistry of melilite basalts in the Southern Cape, South Africa
title_sort age, palaeomagnetism and chemistry of melilite basalts in the southern cape, south africa
publisher Cambridge University Press (CUP)
publishDate 1978
url http://dx.doi.org/10.1017/s001675680003733x
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S001675680003733X
long_lat ENVELOPE(3.358,3.358,-54.422,-54.422)
ENVELOPE(3.358,3.358,-54.422,-54.422)
geographic Bouvet
Bouvet Island
geographic_facet Bouvet
Bouvet Island
genre Bouvet Island
genre_facet Bouvet Island
op_source Geological Magazine
volume 115, issue 5, page 317-327
ISSN 0016-7568 1469-5081
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/s001675680003733x
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