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The geology of the coal-bearing rocks of the Karoo Sequence in the Tshikondeni Mine area, northern Transvaal

Dissertation (MSc)--University of Pretoria, 1995.

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Other Authors: Eriksson, Patrick George
Format: Thesis
Published: University of Pretoria 2021
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access_status_str Open Access
author2 Eriksson, Patrick George
author_browse Eriksson, Patrick George
author_facet Eriksson, Patrick George
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, 1995.
format Thesis
id oai:repository.up.ac.za:2263/82500
institution University of Pretoria (South Africa)
last_indexed 2026-06-10T12:36:40.309Z
license_str Other — see source repository
provenance_str_mv Harvested via OAI-PMH from UPSpace — University of Pretoria Institutional Repository
publishDate 2021
publishDateRange 2021
publishDateSort 2021
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:2263/82500 The geology of the coal-bearing rocks of the Karoo Sequence in the Tshikondeni Mine area, northern Transvaal Eriksson, Patrick George Snyman, C.P. Sullivan, John Hendrey UCTD Geology coal bearing rocks Dissertation (MSc)--University of Pretoria, 1995. This study describes the general geology of the Tshikondeni Mine area, and suggests a reconstruction of the depositional palaeoenvironment of the different sedimentary units. The palaeoenvironmental model is further related to the quality of the main coal seams. The sedimentary palaeoenvironment was established by identifying and describing seven vertically stacked genetic units of sedimentation, comprising twelve different lithofacies. These are related to sedimentary processes, from which a palaeoenvironmental model is derived. The sedimentation at Tshikondeni commenced with glacial, glaciofluvial and glaciolacustrine deposition. This was followed by deltaic, fluvial and lacustrine settings with associated coal seams. Coal distribution, petrography and quality parameters (ash, volatile matter) appear to be closely related to inferred palaeoenvironmental characteristics. Structurally, the area is complex and numerous faults occur. The faulting is due to extensional tectonism. Intrusive basaltic dykes and sills are numerous and further complicate exploitation of the economic coal seams. Geology MSc Unrestricted 2021-11-02T10:19:46Z 2021-11-02T10:19:46Z 2021 1995 Dissertation * http://hdl.handle.net/2263/82500 © 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 coal bearing rocks
The geology of the coal-bearing rocks of the Karoo Sequence in the Tshikondeni Mine area, northern Transvaal
title The geology of the coal-bearing rocks of the Karoo Sequence in the Tshikondeni Mine area, northern Transvaal
title_full The geology of the coal-bearing rocks of the Karoo Sequence in the Tshikondeni Mine area, northern Transvaal
title_fullStr The geology of the coal-bearing rocks of the Karoo Sequence in the Tshikondeni Mine area, northern Transvaal
title_full_unstemmed The geology of the coal-bearing rocks of the Karoo Sequence in the Tshikondeni Mine area, northern Transvaal
title_short The geology of the coal-bearing rocks of the Karoo Sequence in the Tshikondeni Mine area, northern Transvaal
title_sort geology of the coal bearing rocks of the karoo sequence in the tshikondeni mine area northern transvaal
topic UCTD
Geology coal bearing rocks
url http://hdl.handle.net/2263/82500