Post-Transvaal deformation between the Johannesburg dome and the Bushveld complex

A dissertation submitted to the Faculty of Science, University or the Witwatersrand, for the degree of Master of Science. === The study of an area north of the Johannesburg Dome has revealed that the rocks of the Transvaal Supergroup have been affected by widespread deformation, as well as metamo...

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Main Author: Courtnage, Paul, Michael
Format: Others
Language:en
Published: 2018
Subjects:
Online Access:https://hdl.handle.net/10539/24288
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spelling ndltd-netd.ac.za-oai-union.ndltd.org-wits-oai-wiredspace.wits.ac.za-10539-242882019-05-11T03:41:31Z Post-Transvaal deformation between the Johannesburg dome and the Bushveld complex Courtnage, Paul, Michael Geology -- South Africa -- Bushveld. A dissertation submitted to the Faculty of Science, University or the Witwatersrand, for the degree of Master of Science. The study of an area north of the Johannesburg Dome has revealed that the rocks of the Transvaal Supergroup have been affected by widespread deformation, as well as metamorphism to the greenschist facies. Thermal modelling suggests that the metamorphism, and hence porphyroblast growth, can probably be attrIbuted to the thermal effect of the Bushveld Complex. Thus, textural relationships between porphyroblasts and cleavage microstructure in slates could be utilized to establish the relative timing of ductile deformation events in the area. (Abbreviation abstract) AC 2018 2018-04-06T10:02:03Z 2018-04-06T10:02:03Z 1995 Thesis https://hdl.handle.net/10539/24288 en application/pdf
collection NDLTD
language en
format Others
sources NDLTD
topic Geology -- South Africa -- Bushveld.
spellingShingle Geology -- South Africa -- Bushveld.
Courtnage, Paul, Michael
Post-Transvaal deformation between the Johannesburg dome and the Bushveld complex
description A dissertation submitted to the Faculty of Science, University or the Witwatersrand, for the degree of Master of Science. === The study of an area north of the Johannesburg Dome has revealed that the rocks of the Transvaal Supergroup have been affected by widespread deformation, as well as metamorphism to the greenschist facies. Thermal modelling suggests that the metamorphism, and hence porphyroblast growth, can probably be attrIbuted to the thermal effect of the Bushveld Complex. Thus, textural relationships between porphyroblasts and cleavage microstructure in slates could be utilized to establish the relative timing of ductile deformation events in the area. (Abbreviation abstract) === AC 2018
author Courtnage, Paul, Michael
author_facet Courtnage, Paul, Michael
author_sort Courtnage, Paul, Michael
title Post-Transvaal deformation between the Johannesburg dome and the Bushveld complex
title_short Post-Transvaal deformation between the Johannesburg dome and the Bushveld complex
title_full Post-Transvaal deformation between the Johannesburg dome and the Bushveld complex
title_fullStr Post-Transvaal deformation between the Johannesburg dome and the Bushveld complex
title_full_unstemmed Post-Transvaal deformation between the Johannesburg dome and the Bushveld complex
title_sort post-transvaal deformation between the johannesburg dome and the bushveld complex
publishDate 2018
url https://hdl.handle.net/10539/24288
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