Geological characterisation of the Bamboesberg Member within the Molteno-Indwe coalfield, Eastern Cape Province, South Africa

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dc.contributor.advisor Lenhardt, Nils
dc.contributor.coadvisor Hancox, John
dc.contributor.postgraduate Breakfast, Mzoli
dc.date.accessioned 2024-02-09T11:17:54Z
dc.date.available 2024-02-09T11:17:54Z
dc.date.created 2024-01-17
dc.date.issued 2024-01-02
dc.description Dissertation (MSc (Geology))--University of Pretoria, 2024. en_US
dc.description.abstract The Bamboesberg Member forms the basal member of the Late Triassic Molteno Formation. It hosts the two economically significant coal seams in the Molteno-Indwe coalfield, namely the Guba and Indwe seams. The Molteno-Indwe coalfield is located mainly in the northern region of the Eastern Cape Province in South Africa. The Council for Geoscience (CGS) drilled thirteen vertical boreholes within the Molteno-Indwe coalfield between 1984 and 1986. These cores were retrieved from the National Borehole Core Depository in order to characterise the sandstones of the Bamboesberg Member. To achieve this objective, the cores were logged in detail and scanned using a hyperspectral imaging scanner. Additionally, sandstone samples were collected for physio-chemical analysis. The Bamboesberg Member consists of fining-upwards cycles of sandstones, interbedded with argillaceous units and, in certain areas, coal. The coal seams typically occur on top of the argillaceous successions. These sandstones are classified as sub-litharenite and are sourced from the recycled orogenic provenance. Through SEM-EDX analysis it was observed that the sandstones contain large euhedral detrital garnets and sub-rounded zircons. The coal samples from the Bamboesberg Member were assessed for their rare earth element potential. Most samples displayed a rare earth element concentration ranging from 100 to 200 ppm, while five samples exhibited a higher concentration of over 350 ppm. The minerals hosting the rare earth element were observed to be monazite, parisite, and xenotime. Three-dimensional (3D) modelling revealed that the Bamboesberg Member has a concave shape at its centre and the maximum thickness observed is 120 meters. It tapers off to the north, pinching out to 20 m north of Aliwal North. The Bamboesberg Member is more exposed in the western and central parts of the Molteno-Indwe coalfield. Consequently, the western and central portions of the coalfield have potential for further coal prospecting within the Molteno-Indwe coalfield. en_US
dc.description.availability Unrestricted en_US
dc.description.degree MSc (Geology) en_US
dc.description.department Geology en_US
dc.description.faculty Faculty of Natural and Agricultural Sciences en_US
dc.description.sdg SDG-08: Decent work and economic growth en_US
dc.description.sdg SDG-09: Industry, innovation and infrastructure en_US
dc.description.sponsorship Council for Geoscience en_US
dc.identifier.citation * en_US
dc.identifier.doi 10.25403/UPresearchdata.25152059 en_US
dc.identifier.other A2024 en_US
dc.identifier.uri http://hdl.handle.net/2263/94429
dc.language.iso en en_US
dc.publisher University of Pretoria
dc.rights © 2023 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.
dc.subject UCTD en_US
dc.subject Bamboesberg Member en_US
dc.subject Sustainable Development Goals (SDGs)
dc.subject Molteno-Indwe coalfield
dc.subject Mineral dominant map
dc.subject Rare earth elements
dc.subject 3D modelling
dc.subject Provenance
dc.subject.other SDG-08: Decent work and economic growth
dc.subject.other Natural and agricultural science theses SDG-08
dc.subject.other SDG-09: Industry, innovation and infrastructure
dc.subject.other Natural and agricultural science theses SDG-09
dc.title Geological characterisation of the Bamboesberg Member within the Molteno-Indwe coalfield, Eastern Cape Province, South Africa en_US
dc.type Dissertation en_US


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