A Review of Mineral Exploration at the Karingarab Carbonatite, Southern Namibia
| dc.contributor.author | Nehoya, Jennifer Ndapanda | |
| dc.contributor.supervisor | Nex, Paul | |
| dc.date.accessioned | 2024-11-26T11:53:32Z | |
| dc.date.available | 2024-11-26T11:53:32Z | |
| dc.date.issued | 2023 | |
| dc.description | A research report submitted in partial fulfillment of the requirements for the degree of Master of Science in Economic Geology by coursework and research to the Faculty of Science, School of Geosciences, University of the Witwatersrand, Johannesburg 2023 | |
| dc.description.abstract | This research report reviews the Karingarab Carbonatite, which is one of several alkaline and carbonatite occurrences in Namibia targeted for rare earth element (REE) potential which are used in medical, renewable energy, technology and military applications. Several exploration campaigns have occurred at the Karingarab Carbonatite since 1977 and all indicate positive concentrations of REEs at the deposit. The Karingarab Carbonatite (68 Ma) is one of 41 alkaline and carbonatite occurrences in Namibia which is documented in this report and is very similar in terms of composition, age and emplacement to the Dicker Willem (49 Ma) and the Gross Brukkaros carbonatites (77 Ma) all located along south-west to north-east trending structures on the west coast of southern Namibia. The Karingarab Carbonatite lies in the center of a 2.5 km diameter circular vent raise 300 m above sea level, the edges of the vent are brecciated extrusive phonolites and other alkali silicate rocks with country rock fragments of phyllites and schists of the Oranjemund group, crosscut with late stage dykes of varying compositions in the alkaline and carbonatite series. Four main lithology types are identified through their distinct geochemical signatures with varying degrees of weathering and alteration. The target and main lithology is a layered extrusive carbonatite with lapilli of various shapes and sizes diluted in parts with mostly phonolites, schists and phyllites. The second more common lithology is extrusive phonolites which are mostly brecciated with cross cutting carbonatite dykes. The third lithology type is formed by clay rich autoclastic volcanic breccias which are a mixture of all the proximal and local rock types of the Oranjemund group, lastly the fourth lithology is formed by overburden which includes wind-blown dune sands and calcrete. The extrusive carbonatite lapilli is the dominant ore type, with deeper, fresh and unaltered carbonatites still mineralized and carrying lower grades while the shallower, weathered and altered carbonatite shows supergene enrichment and extremely high grades. This enrichment was upgraded by events in the early Paleogene which included deep erosion and surface weathering events along with a regional surface silcretization event capping and trapping mineralization. Preliminary findings following the first two drilling campaigns indicate a potential to produce from the carbonatite, 181 million tonnes of ore with 3.5 million tonnes of total rare earth oxides (REOs) at an average grade of 1.9% total REEs. The deposit remains partly open at depth, with satellite concealed volcanic occurrences still to be explored. Should the target become an operational mine, responsible sourcing will need to be considered particularly how to extract, refine, transport and process REEs in a manner which satisfies environmental, social and governance requirements (ESG) while ensuring the mineral value chain and potential industry spill-over is managed sustainably. Major risks to the target involve the criticality of supply which may be managed through monitoring geopolitics in supply, and technology improvements in substitution and recycling for the REEs and their products. Apart from these economic interests, the observations and studies on the subsurface lithologies at Karingarab will be invaluable to academia through improved literature on carbonatites, REE deposit genesis and the regional geology where much is covered by sand | |
| dc.description.submitter | MM2024 | |
| dc.faculty | Faculty of Science | |
| dc.identifier | https://orcid.org/ 0000-0001-5305-2937 | |
| dc.identifier.citation | Nehoya, Jennifer Ndapanda. (2023). A Review of Mineral Exploration at the Karingarab Carbonatite, Southern Namibia [Master’s dissertation, University of the Witwatersrand, Johannesburg]. WireDSpace. | |
| dc.identifier.uri | https://hdl.handle.net/10539/42906 | |
| dc.language.iso | en | |
| dc.publisher | University of the Witwatersrand, Johannesburg | |
| dc.rights | © 2023 University of the Witwatersrand, Johannesburg. All rights reserved. The copyright in this work vests in the University of the Witwatersrand, Johannesburg. No part of this work may be reproduced or transmitted in any form or by any means, without the prior written permission of University of the Witwatersrand, Johannesburg. | |
| dc.rights.holder | University of the Witwatersrand, Johannesburg | |
| dc.school | School of Geosciences | |
| dc.subject | Karingarab Carbonatite | |
| dc.subject | Renewable energy | |
| dc.subject | Mineral Exploration | |
| dc.subject | UCTD | |
| dc.subject.other | SDG-8: Decent work and economic growth | |
| dc.title | A Review of Mineral Exploration at the Karingarab Carbonatite, Southern Namibia | |
| dc.type | Dissertation |