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The geology and the structure of the area in the vicinity of Magnet Heights, Eastern Transvaal, with special reference to the Magnet Iron Ore
Dissertation (MSc)--University of Pretoria, 1964.
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| Format: | Thesis |
| Language: | English |
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University of Pretoria
2022
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| _version_ | 1867613508894457856 |
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| access_status_str | Open Access |
| author2 | Molyneux, Thomas Gordon |
| author_browse | Molyneux, Thomas Gordon |
| author_facet | Molyneux, Thomas Gordon |
| 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, 1964. |
| format | Thesis |
| id | oai:repository.up.ac.za:2263/83268 |
| institution | University of Pretoria (South Africa) |
| language | English |
| last_indexed | 2026-06-10T12:37:16.203Z |
| 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:2263/83268 The geology and the structure of the area in the vicinity of Magnet Heights, Eastern Transvaal, with special reference to the Magnet Iron Ore Molyneux, Thomas Gordon UCTD Geology Magnet Heights Eastern Transvaal Dissertation (MSc)--University of Pretoria, 1964. The area investigated at Magnet Heights covers ten miles of strike of the uppermost six thousand feet of the layered mafic rocks of the Bushveld Complex. A fall of a thousand feet southwards from the Magnet Heights trading store has caused the almost complete "stripping off" of the soil cover to produce excellent rock exposures; a situation unique in this zone of the Bushveld Complex Monomineralic layered rocks identified are magentitite, anothorsite and pyroxenite. The remaining layered rocks are predominantly gabbroic. In mapping the Mair Magenetitite Seam was taken as a datum line relative to which fur lower seams and 21 upper seams were numbered and mapped. Each of these seams can be recognized by notng its V2OE content, its thickness and its field relationships. Geology MSc Unrestricted 2022-01-12T06:01:04Z 2022-01-12T06:01:04Z 19/8/2021 1964 Dissertation * http://hdl.handle.net/2263/83268 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 Magnet Heights Eastern Transvaal The geology and the structure of the area in the vicinity of Magnet Heights, Eastern Transvaal, with special reference to the Magnet Iron Ore |
| title | The geology and the structure of the area in the vicinity of Magnet Heights, Eastern Transvaal, with special reference to the Magnet Iron Ore |
| title_full | The geology and the structure of the area in the vicinity of Magnet Heights, Eastern Transvaal, with special reference to the Magnet Iron Ore |
| title_fullStr | The geology and the structure of the area in the vicinity of Magnet Heights, Eastern Transvaal, with special reference to the Magnet Iron Ore |
| title_full_unstemmed | The geology and the structure of the area in the vicinity of Magnet Heights, Eastern Transvaal, with special reference to the Magnet Iron Ore |
| title_short | The geology and the structure of the area in the vicinity of Magnet Heights, Eastern Transvaal, with special reference to the Magnet Iron Ore |
| title_sort | geology and the structure of the area in the vicinity of magnet heights eastern transvaal with special reference to the magnet iron ore |
| topic | UCTD Geology Magnet Heights Eastern Transvaal |
| url | http://hdl.handle.net/2263/83268 |