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The geochronology and geochemistry of Karoo volcanics in the Lebombo and adjacent areas

Includes bibliographical references.

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Bibliographic Details
Main Author: Bristow, John William
Other Authors: Erlank, A J
Format: Thesis
Language:English
Published: Department of Geological Sciences 2015
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access_status_str Open Access
author Bristow, John William
author2 Erlank, A J
author_browse Bristow, John William
Erlank, A J
author_facet Erlank, A J
Bristow, John William
author_sort Bristow, John William
collection Thesis
description Includes bibliographical references.
format Thesis
id oai:open.uct.ac.za:11427/12534
institution University of Cape Town (South Africa)
language eng
last_indexed 2026-06-10T12:33:17.409Z
license_str Not specified — see source repository
provenance_str_mv Harvested via OAI-PMH from UCTD — University of Cape Town Open Access Repository
publishDate 2015
publishDateRange 2015
publishDateSort 2015
publisher Department of Geological Sciences
publisherStr Department of Geological Sciences
record_format dspace
source_str UCTD — University of Cape Town Open Access Repository
spelling oai:open.uct.ac.za:11427/12534 The geochronology and geochemistry of Karoo volcanics in the Lebombo and adjacent areas Bristow, John William Erlank, A J Duncan, A R Geochemistry Includes bibliographical references. Karoo volcanics of Jurassic to Cretaceous age crop out in the eastern areas of southern Africa. These volcanics are well preserved in the Lebombo monocline which straddles the borders of South Africa, Swaziland and Mozambique, and in the Nuanetsi and Tuli synclines and Sabi monocline of south-east Zimbabwe. Geochronological and geochemical data have been used to evaluate the geochemistry of the rock types found in the above areas, particularly with respect to the mafic volcanics of the Lebombo. In the eastwardly dipping Lebombo monocline, nephelinites overlain by picrite basalts occur in the northern part of the volcanic succession whereas over the remaining area olivine-poor basalts are dominant. Rhyolitic volcanics in the form of massive flows overlie the basaltic rocks and attain their maximum thickness in Swaziland and the southern Lebombo. The rhyolites are notably thinner to the north of Swaziland and are overlain by an upper sequence of olivine-poor lavas with interdigitated rhyolite flows. Basic dykes are ubiquitous in the Lebombo whereas acid dykes, though present, tend to be localised. In Nuanetsi, picrite basalts, olivine-poor basalts and rhyolite flows with interbedded basic lavas crop out ina major synclinal structure. Dyke rocks are common and late Karoo intrusive complexes cut the lavas. Volcanic rocks in the Tuli syncline consist predominantly of picrite basalts and olivine poor lavas, whereas nephelinites, picrite basalts and olivine-poor lavas crop out in the Sabi Monocline. 2015-02-24T04:12:40Z 2015-02-24T04:12:40Z 1980 Doctoral Thesis Doctoral PhD http://hdl.handle.net/11427/12534 eng application/pdf Department of Geological Sciences Faculty of Science University of Cape Town
spellingShingle Geochemistry
Bristow, John William
The geochronology and geochemistry of Karoo volcanics in the Lebombo and adjacent areas
thesis_degree_str Doctoral
title The geochronology and geochemistry of Karoo volcanics in the Lebombo and adjacent areas
title_full The geochronology and geochemistry of Karoo volcanics in the Lebombo and adjacent areas
title_fullStr The geochronology and geochemistry of Karoo volcanics in the Lebombo and adjacent areas
title_full_unstemmed The geochronology and geochemistry of Karoo volcanics in the Lebombo and adjacent areas
title_short The geochronology and geochemistry of Karoo volcanics in the Lebombo and adjacent areas
title_sort geochronology and geochemistry of karoo volcanics in the lebombo and adjacent areas
topic Geochemistry
url http://hdl.handle.net/11427/12534
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