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The geology of the country surrounding Loskop Dam, Transvaal

Dissertation (MSc)--University of Pretoria, 1954.

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Other Authors: Willemse, J.
Format: Thesis
Language:English
Published: University of Pretoria 2022
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access_status_str Open Access
author2 Willemse, J.
author_browse Willemse, J.
author_facet Willemse, J.
collection Thesis
dc_rights_str_mv © 2021 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)--University of Pretoria, 1954.
format Thesis
id oai:repository.up.ac.za:2263/83195
institution University of Pretoria (South Africa)
language English
last_indexed 2026-06-10T12:39:40.578Z
license_str Other — see source repository
provenance_str_mv Harvested via OAI-PMH from UPSpace — University of Pretoria Institutional Repository
publishDate 2022
publishDateRange 2022
publishDateSort 2022
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:2263/83195 The geology of the country surrounding Loskop Dam, Transvaal Willemse, J. Koen, G.M. Wolhuter, L.E. UCTD Geology Loskop Dam Transvaal Dissertation (MSc)--University of Pretoria, 1954. The Loskop System in its type locality has been investigated. It consists predominantly of arenaceous sediments and minor shales, siltstones a.no. conglomerates·. Lithologically the components ·of this system are remarkably similar to those of the overlying Waterberg System. Heavy mineral concentrates from rocks of both systems were investigated to determine whether there were sufficient points of difference to demarcate the Loskop System from the Waterberg System on petrographical data. The similarity of these heavy mineral suites agrees with the close correspondence in nature of the sediments in which the minerals occur and is not corroborative of the grouping of the rocks on the Loskop System into a separate stratigraphical entity. Evidence of volcanicity contemporaneous with the deposition of a portion of the Waterberg System is present in the area mapped in the form of pyroclastic material intimately associated with intensely folded Waterberg beds. The latter are overlain by practically undisturbed strata of the same system. The intraformational and local folding in the Waterberg beds is thought to be due to subaqueous slumping at the time of eruption of the pyroclastic material. A description is given of the Rooiberg Felsite in particular its chemical composition is compared with that of Karroo Rhyolite and with felsite of the “Premier Mine Type” The latter type is distinctive in several respects but especially in its high mg content. When plotted on Smithson diagrams, the length breadth ratios of zircons obtained from the felsitic lava of the Bushveld Complex are found to be very much the same as those obtained for sediment of the Loskop System. Two new chemical analyses are reported. Geology MSc Unrestricted 2022-01-12T06:00:09Z 2022-01-12T06:00:09Z 19/8/2021 1954 Dissertation * http://hdl.handle.net/2263/83195 en © 2021 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 UCTD
Geology
Loskop Dam
Transvaal
The geology of the country surrounding Loskop Dam, Transvaal
title The geology of the country surrounding Loskop Dam, Transvaal
title_full The geology of the country surrounding Loskop Dam, Transvaal
title_fullStr The geology of the country surrounding Loskop Dam, Transvaal
title_full_unstemmed The geology of the country surrounding Loskop Dam, Transvaal
title_short The geology of the country surrounding Loskop Dam, Transvaal
title_sort geology of the country surrounding loskop dam transvaal
topic UCTD
Geology
Loskop Dam
Transvaal
url http://hdl.handle.net/2263/83195