Some main conclusions drawn from a basinal analysis of the Dwyka series in the Karroo basin

dc.contributor.author	Stratten, T.
dc.date.accessioned	2014-12-23T11:27:27Z
dc.date.available	2014-12-23T11:27:27Z
dc.date.issued	1968
dc.description	Main article	en_ZA
dc.description.abstract	The investigation of the Dwyka glaciation and its relationship to the pre-Karroo surface was undertaken as a research project at the University of the Witwatersrand under the sponsorship of Union Corporation, Limited. A thesis on this study has been submitted for the degree of Doctor of Philosophy under the supervision of Professor T. W. Gevers. The research fell mainly into two separate but related fields of study. The first field was to investigate the pre-Karroo surface with special reference to the geology beneath the Karroo System. The second field was to investigate the paleo-ice flow directions of the Dwyka Tillite and relate this to the position and lithology of the source areas.	en_ZA
dc.description.sponsorship	None	en_ZA
dc.identifier.citation	None	en_ZA
dc.identifier.issn	0078-8554
dc.identifier.uri	http://hdl.handle.net/10539/16117
dc.language.iso	en	en_ZA
dc.publisher	Bernard Price Institute for Palaeontological Research	en_ZA
dc.relation.ispartofseries	None;
dc.subject	Dwyka; Karroo basin; geology; paleo-ice flow	en_ZA
dc.title	Some main conclusions drawn from a basinal analysis of the Dwyka series in the Karroo basin	en_ZA
dc.type	Article	en_ZA

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