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

dc.contributor.advisorLenhardt, Nils
dc.contributor.coadvisorHancox, John
dc.contributor.emailmbreakfast@geoscience.org.zaen_US
dc.contributor.postgraduateBreakfast, Mzoli
dc.date.accessioned2024-02-09T11:17:54Z
dc.date.available2024-02-09T11:17:54Z
dc.date.created2024-01-17
dc.date.issued2024-01-02
dc.descriptionDissertation (MSc (Geology))--University of Pretoria, 2024.en_US
dc.description.abstractThe 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.availabilityUnrestricteden_US
dc.description.degreeMSc (Geology)en_US
dc.description.departmentGeologyen_US
dc.description.facultyFaculty of Natural and Agricultural Sciencesen_US
dc.description.sdgSDG-08: Decent work and economic growthen_US
dc.description.sdgSDG-09: Industry, innovation and infrastructureen_US
dc.description.sponsorshipCouncil for Geoscienceen_US
dc.identifier.citation*en_US
dc.identifier.doi10.25403/UPresearchdata.25152059en_US
dc.identifier.otherA2024en_US
dc.identifier.urihttp://hdl.handle.net/2263/94429
dc.language.isoenen_US
dc.publisherUniversity 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.subjectUCTDen_US
dc.subjectBamboesberg Memberen_US
dc.subjectSustainable Development Goals (SDGs)
dc.subjectMolteno-Indwe coalfield
dc.subjectMineral dominant map
dc.subjectRare earth elements
dc.subject3D modelling
dc.subjectProvenance
dc.subject.otherSDG-08: Decent work and economic growth
dc.subject.otherNatural and agricultural science theses SDG-08
dc.subject.otherSDG-09: Industry, innovation and infrastructure
dc.subject.otherNatural and agricultural science theses SDG-09
dc.titleGeological characterisation of the Bamboesberg Member within the Molteno-Indwe coalfield, Eastern Cape Province, South Africaen_US
dc.typeDissertationen_US

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