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The geochemistry of the Olivine Melilitetes and related rocks of Namaqualand Bushmanland, South Africa

Includes bibliographical references.

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Bibliographic Details
Main Author: Moore, Andrew Edward
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 Moore, Andrew Edward
author2 Erlank, A J
author_browse Erlank, A J
Moore, Andrew Edward
author_facet Erlank, A J
Moore, Andrew Edward
author_sort Moore, Andrew Edward
collection Thesis
description Includes bibliographical references.
format Thesis
id oai:open.uct.ac.za:11427/12595
institution University of Cape Town (South Africa)
language eng
last_indexed 2026-06-10T12:33:48.261Z
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:11427/12595 The geochemistry of the Olivine Melilitetes and related rocks of Namaqualand Bushmanland, South Africa Moore, Andrew Edward Erlank, A J Includes bibliographical references. Early Tertiary olivine melilitites and associated non-diamondiferous kimberlites occur in two pipe clusters in the Namaqualand and Bushmanland regions of South Africa. The more northerly cluster is centred about the town of Gamoep and the second is located south of Garies. The olivine melilitites are characterized by olivine phenocrysts which exhibit a broad range in composition on the scale of individual hand specimens. It is possible to distinguish four petrographically and chemically distinct olivine populations in both the northern and southern pipes studied: (a) Rare anhedral or subhedral olivines that display marked disequilibrium features with the surrounding matrix and which are characterized by having high iron and extremely low nickel contents (referred to as HILN olivines) relative to the remaining olivines in the same rock; (b) euhedral and often skeletal (hopper) olivines that are richer in Mg and Ni than HILN olivines in the same rock. Some of the euhedral olivines show abnormal zonation patterns ("unusual" hoppers). Hopper and HILN olivines contain fluid and carbonate inclusions which apparently record the separation of a vapour phase and an immiscible carbonate liquid during magma ascent: (c) large rounded olivines (megacrysts) up to 40 mm across. Individuals are chemically homogeneous, but megacrysts from the same pipe collectively define a trend of decreasing Mg with Ni (F092, 0.36% Ni to F075, 0.17% Ni). The most fayalitic megacrysts are depleted in Mg and Ni relative to the hopper olivines in the same rock. [d] In addition to these main populations, there also occur rare magnesium-rich (F091) anhedral olivines which show strained extinction and are believed to be xenocrysts. 2015-03-13T14:06:03Z 2015-03-13T14:06:03Z 1979 Doctoral Thesis Doctoral PhD http://hdl.handle.net/11427/12595 eng application/pdf Department of Geological Sciences Faculty of Science University of Cape Town
spellingShingle Moore, Andrew Edward
The geochemistry of the Olivine Melilitetes and related rocks of Namaqualand Bushmanland, South Africa
thesis_degree_str Doctoral
title The geochemistry of the Olivine Melilitetes and related rocks of Namaqualand Bushmanland, South Africa
title_full The geochemistry of the Olivine Melilitetes and related rocks of Namaqualand Bushmanland, South Africa
title_fullStr The geochemistry of the Olivine Melilitetes and related rocks of Namaqualand Bushmanland, South Africa
title_full_unstemmed The geochemistry of the Olivine Melilitetes and related rocks of Namaqualand Bushmanland, South Africa
title_short The geochemistry of the Olivine Melilitetes and related rocks of Namaqualand Bushmanland, South Africa
title_sort geochemistry of the olivine melilitetes and related rocks of namaqualand bushmanland south africa
url http://hdl.handle.net/11427/12595
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