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A geochemical study of neoproterozoic palaeo-evaporites and their possible role in metallogenesis in the Damara Belt of Namibia

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Main Author: Pillay, Nevantheran
Format: Thesis
Language:English
Published: Department of Geological Sciences 2014
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access_status_str Open Access
author Pillay, Nevantheran
author_browse Pillay, Nevantheran
author_facet Pillay, Nevantheran
author_sort Pillay, Nevantheran
collection Thesis
description Summary in English.
format Thesis
id oai:open.uct.ac.za:11427/4219
institution University of Cape Town (South Africa)
language eng
last_indexed 2026-06-10T12:31:28.055Z
license_str Not specified — see source repository
provenance_str_mv Harvested via OAI-PMH from UCTD — University of Cape Town Open Access Repository
publishDate 2014
publishDateRange 2014
publishDateSort 2014
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:11427/4219 A geochemical study of neoproterozoic palaeo-evaporites and their possible role in metallogenesis in the Damara Belt of Namibia Pillay, Nevantheran Geological Science Summary in English. Bibliography: leaves 157-163. Former evaporite horizons in metamorphic terrains have frequently been referred to as a source for highly saline fluids associated with base metal ore deposits in various parts of the world. Data on the nature of these former evaporites and their associated connate fluids, however, is frequently quite sparse, and the link between the ore deposits and the source evaporites is usually intuitive, at best. In an attempt to characterise such evaporite-derived fluids and their source evaporites, a study of former evaporites in the Duruchaus Formation in the Southern Marginal Zone (SMZ) of the Damara Belt was carried out. The lithological units that make up the evaporite sequence within the Duruchaus Formation were mapped and sampled, along with discordant quartz-dolomite plugs intruding at various levels in the Duruchaus Formation stratigraphy, and in the overlying Bakos Group. 2014-07-30T17:27:59Z 2014-07-30T17:27:59Z 2000 Master Thesis Masters MSc http://hdl.handle.net/11427/4219 eng application/pdf Department of Geological Sciences Faculty of Science University of Cape Town
spellingShingle Geological Science
Pillay, Nevantheran
A geochemical study of neoproterozoic palaeo-evaporites and their possible role in metallogenesis in the Damara Belt of Namibia
thesis_degree_str Master's
title A geochemical study of neoproterozoic palaeo-evaporites and their possible role in metallogenesis in the Damara Belt of Namibia
title_full A geochemical study of neoproterozoic palaeo-evaporites and their possible role in metallogenesis in the Damara Belt of Namibia
title_fullStr A geochemical study of neoproterozoic palaeo-evaporites and their possible role in metallogenesis in the Damara Belt of Namibia
title_full_unstemmed A geochemical study of neoproterozoic palaeo-evaporites and their possible role in metallogenesis in the Damara Belt of Namibia
title_short A geochemical study of neoproterozoic palaeo-evaporites and their possible role in metallogenesis in the Damara Belt of Namibia
title_sort geochemical study of neoproterozoic palaeo evaporites and their possible role in metallogenesis in the damara belt of namibia
topic Geological Science
url http://hdl.handle.net/11427/4219
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AT pillaynevantheran geochemicalstudyofneoproterozoicpalaeoevaporitesandtheirpossibleroleinmetallogenesisinthedamarabeltofnamibia