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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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 |
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en |
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Others
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Geology -- South Africa -- Bushveld. |
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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 |
work_keys_str_mv |
AT courtnagepaulmichael posttransvaaldeformationbetweenthejohannesburgdomeandthebushveldcomplex |
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1719083966678433792 |