- Title
- MORB-related dolerites associated with the final phases of Karoo flood basalt volcanism in southern Africa.
- Creator
- Duncan, Andrew R, Armstrong, R A, Erlank, Anthony J, Marsh, Julian S, Watkins, R T
- Date
- 1990
- Type
- text
- Type
- conference paper
- Identifier
- http://hdl.handle.net/10962/143299
- Identifier
- vital:38222
- Identifier
- https://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetailampidt=6938249
- Description
- The Rooi Rand dyke swarm is approximately 200km long and up to 20km wide. It crops out in the southern portion of the Lebombo monocline where the dykes intrude basalts of the Sabie River Basalt Formation which is the major basaltic unit in the eastern portion of the Karoo volcanic succession. The Horingbaai dolerites form thin dykes and sills which intrude the base of the Etendeka lava pile (considered part of the Karoo Volcanics, but correlated with the Serra Geral Formation of Brazil) along the coast of Namibia. Both the Rooi Rand and Horingbaai magma types are similar in composition to enriched MORB and are compositionally distinct from most of the Karoo-basalts they intrude.
- Format
- 11 pages, pdf
- Language
- English
- Relation
- International dyke conference, EDuncan, A.R., Armstrong, R.A., Erlank, A.J., Marsh, J.S. and Watkins, R.T., 1990. MORB-related dolerites associated with the final phases of Karoo flood basalt volcanism in southern Africa. In International dyke conference. 2 (pp. 119-129)., International dyke conference volume 2 119 129 1990 1531-2542
- Rights
- Author
- Rights
- Use of this resource is governed by the terms and conditions of the Author
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Marsh, Julian (Goonie)(Prof)
RU Department of Geology
SDG 13. Climate Action
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