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

dc.contributor.authorCourtnage, Paul, Michael
dc.date.accessioned2018-04-06T10:02:03Z
dc.date.available2018-04-06T10:02:03Z
dc.date.issued1995
dc.descriptionA dissertation submitted to the Faculty of Science, University or the Witwatersrand, for the degree of Master of Science.en_ZA
dc.description.abstractThe 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)en_ZA
dc.description.librarianAC 2018en_ZA
dc.identifier.urihttps://hdl.handle.net/10539/24288
dc.language.isoenen_ZA
dc.subjectGeology -- South Africa -- Bushveld.en_ZA
dc.titlePost-Transvaal deformation between the Johannesburg dome and the Bushveld complexen_ZA
dc.typeThesisen_ZA

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