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The geochemistry and petrology of the upper critical zone in the boshoek section, of the Western Bushveld complex

Dissertation (MSc (Geology))--University of Pretoria, 1991.

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Other Authors: Von Gruenewaldt, G. (Gerhard), 1942-
Format: Thesis
Language:English
Published: University of Pretoria 2024
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access_status_str Open Access
author2 Von Gruenewaldt, G. (Gerhard), 1942-
author_browse Von Gruenewaldt, G. (Gerhard), 1942-
author_facet Von Gruenewaldt, G. (Gerhard), 1942-
collection Thesis
dc_rights_str_mv © 2024 University of Pretoria. All rights reserved. The copyright in this work vests in the University of Pretoria. No part of this work may be reproduced or transmitted in any form or by any means, without the prior written permission of the University of Pretoria.
description Dissertation (MSc (Geology))--University of Pretoria, 1991.
format Thesis
id oai:repository.up.ac.za:2263/99476
institution University of Pretoria (South Africa)
language English
last_indexed 2026-06-10T12:40:26.265Z
license_str Other — see source repository
provenance_str_mv Harvested via OAI-PMH from UPSpace — University of Pretoria Institutional Repository
publishDate 2024
publishDateRange 2024
publishDateSort 2024
publisher University of Pretoria
publisherStr University of Pretoria
record_format dspace
source_str UPSpace — University of Pretoria Institutional Repository
spelling oai:repository.up.ac.za:2263/99476 The geochemistry and petrology of the upper critical zone in the boshoek section, of the Western Bushveld complex Von Gruenewaldt, G. (Gerhard), 1942- Schurmann, L.W. Geochemistry Petrology Upper critical zone Boshoek Western bushveld complex UCTD Dissertation (MSc (Geology))--University of Pretoria, 1991. The Boshoek section is located in the mafic part of the southwestern Bushveld Complex. The tectonic setting of the section is characterized by two deformational stages prior and during emplacement of the lower and critical zones. The warped floor of the southwestern Bushveld Complex resulted in lithological differences of the lower zone sequences in the Rustenburg and Marikana sections, and the subsequent transgression northwards towards the Boshoek section in response to the addition of fresh magma into the magma chamber. The upper critical zone in the Boshoek section is stratigraphically subdivided into several units on the basis of lithological features and geochemical trends. The Intermediate and Merensky Footwall units are further subdivided into sub-units on the basis of modal-mineral proportions and whole rock geochemical trends. The mechanism introduced for the formation of the upper critical zone is based on mineralogical and geochemical trends, together with the characteristics of the potential parental magmas to the lower and critical zones. The feldspathic pyroxenite layers are produced by the slumping of Bl magma from an elevated position down to the floor, while the sub-units of the Intermediate and Merensky Footwall units are initiated by periodic, gentle influxes of B2/B3 magma. Such an influx of magma can cause an increase in temperature and thus the return to plagioclase as the only mineral phase on the liquidus, in order to produce a mottled anorthosite. On cooling, orthopyroxene will join plagioclase on the liquidus to produce the noritic rocks. The formation of the Merensky and Bastard units is initiated by the emplacement of the main zone magma, B4, together with the slumping of Bl magma from an elevated position. The Bl magma is responsible for the feldspathic pyroxenite layers, while the hybrid magma consisting of Bl and B4, together with the B4 magma produced the more felsic layers by crystal settling. Geology MSc (Geology) 2024-11-27T09:15:57Z 2024-11-27T09:15:57Z 22/05/04 1991 Dissertation http://hdl.handle.net/2263/99476 en © 2024 University of Pretoria. All rights reserved. The copyright in this work vests in the University of Pretoria. No part of this work may be reproduced or transmitted in any form or by any means, without the prior written permission of the University of Pretoria. application/pdf University of Pretoria
spellingShingle Geochemistry
Petrology
Upper critical zone
Boshoek
Western bushveld complex
UCTD
The geochemistry and petrology of the upper critical zone in the boshoek section, of the Western Bushveld complex
title The geochemistry and petrology of the upper critical zone in the boshoek section, of the Western Bushveld complex
title_full The geochemistry and petrology of the upper critical zone in the boshoek section, of the Western Bushveld complex
title_fullStr The geochemistry and petrology of the upper critical zone in the boshoek section, of the Western Bushveld complex
title_full_unstemmed The geochemistry and petrology of the upper critical zone in the boshoek section, of the Western Bushveld complex
title_short The geochemistry and petrology of the upper critical zone in the boshoek section, of the Western Bushveld complex
title_sort geochemistry and petrology of the upper critical zone in the boshoek section of the western bushveld complex
topic Geochemistry
Petrology
Upper critical zone
Boshoek
Western bushveld complex
UCTD
url http://hdl.handle.net/2263/99476