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Post-depositional alteration of the Ventersdorp Contact Reef at Vaal Reef no. 10 shaft, Klerksdorp Goldfield

Bibliography: pages 157-167.

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Bibliographic Details
Main Author: Gartz, Volker Heinrich
Other Authors: Frimmel, Hartwig
Format: Thesis
Language:English
Published: Department of Geological Sciences 2016
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access_status_str Open Access
author Gartz, Volker Heinrich
author2 Frimmel, Hartwig
author_browse Frimmel, Hartwig
Gartz, Volker Heinrich
author_facet Frimmel, Hartwig
Gartz, Volker Heinrich
author_sort Gartz, Volker Heinrich
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description Bibliography: pages 157-167.
format Thesis
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institution University of Cape Town (South Africa)
language eng
last_indexed 2026-06-10T12:32:36.207Z
license_str Not specified — see source repository
provenance_str_mv Harvested via OAI-PMH from UCTD — University of Cape Town Open Access Repository
publishDate 2016
publishDateRange 2016
publishDateSort 2016
publisher Department of Geological Sciences
publisherStr Department of Geological Sciences
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source_str UCTD — University of Cape Town Open Access Repository
spelling oai:open.uct.ac.za:11427/21406 Post-depositional alteration of the Ventersdorp Contact Reef at Vaal Reef no. 10 shaft, Klerksdorp Goldfield Gartz, Volker Heinrich Frimmel, Hartwig Geological Science Bibliography: pages 157-167. The Ventersdorp Contact Reef (VCR) is an auriferous conglomerate which unconformably overlies the rocks of the Witwatersrand Supergroup. It acted as a palaeo-aquifer and is capped by relatively impermeable metabasalts of the Ventersdorp Supergroup. Three post-depositional alteration events, which form an alteration halo in the footwall and hangjngwall rocks around the VCR, can be recognised. The first of these alteration events is attributed to regional metamorphism and is identified by the formation of pyrophyllite in the footwall quartzites and a lower green schist facies mineral assemblage in the hangingwall metabasalts. The second and third alteration events are interpreted as metasomatic fluid in filtration events which were focused along the VCR horizon. The second alteration event involved K⁺metasomatism which affected the footwall and hanging wall rocks up to a distance of several metres away from the VCR The third alteration event, during which the muscovite was partially replaced, was associated with the formation of chlorite in and immediately around the VCR-Chlorite thermometry suggests a temperature of 307 ± 14°C for this event. The close mineralogical association of gold with chlorite, secondary pyrite and secondary quartz in the VCR is interpreted to indicate that gold remobilisation was associated with the chlorite forming alteration event. The inhomogeneity found in gold particles within a hydrothermal quartz vein indicates a sharp drop in temperature after gold precipitation, suggesting a very short period of hydrothermal fluid infiltration. 2016-08-22T12:21:28Z 2016-08-22T12:21:28Z 1996 Master Thesis Masters MSc http://hdl.handle.net/11427/21406 eng application/pdf Department of Geological Sciences Faculty of Science University of Cape Town
spellingShingle Geological Science
Gartz, Volker Heinrich
Post-depositional alteration of the Ventersdorp Contact Reef at Vaal Reef no. 10 shaft, Klerksdorp Goldfield
thesis_degree_str Master's
title Post-depositional alteration of the Ventersdorp Contact Reef at Vaal Reef no. 10 shaft, Klerksdorp Goldfield
title_full Post-depositional alteration of the Ventersdorp Contact Reef at Vaal Reef no. 10 shaft, Klerksdorp Goldfield
title_fullStr Post-depositional alteration of the Ventersdorp Contact Reef at Vaal Reef no. 10 shaft, Klerksdorp Goldfield
title_full_unstemmed Post-depositional alteration of the Ventersdorp Contact Reef at Vaal Reef no. 10 shaft, Klerksdorp Goldfield
title_short Post-depositional alteration of the Ventersdorp Contact Reef at Vaal Reef no. 10 shaft, Klerksdorp Goldfield
title_sort post depositional alteration of the ventersdorp contact reef at vaal reef no 10 shaft klerksdorp goldfield
topic Geological Science
url http://hdl.handle.net/11427/21406
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