Thrusting, folding and stratigraphy of the Ghaap Group along the southwestern margin of the Kaapvaal Craton

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dc.contributor.authorAltermann W.
dc.contributor.authorHalbich I.W.
dc.date.accessioned2011-05-15T16:00:36Z
dc.date.available2011-05-15T16:00:36Z
dc.date.issued1990
dc.description.abstractThe lower sedimentary sequence of the Transvaal Supergroup underwent multiple folding and thrusting along the southwestern margin of the Kaapvaal Craton, between Prieska and Boegoeberg Dam. This tectogenesis is expressed in three folding phases with successively diminishing intensities. Thrusting occurred during the first and second phase. The stratigraphy of these rocks needs to be reviewed, taking into account the complex structure. -from Authors
dc.identifier.citationSouth African Journal of Geology
dc.identifier.citation93
dc.identifier.citation4
dc.identifier.issn10120750
dc.identifier.urihttp://hdl.handle.net/10019.1/11784
dc.subjectfolding
dc.subjectPrecambrian
dc.subjectstratigraphy
dc.subjectstructural analysis
dc.subjectthrusting
dc.subjectTransvaal Supergroup
dc.subjectSouth Africa, Kaapvaal Craton
dc.titleThrusting, folding and stratigraphy of the Ghaap Group along the southwestern margin of the Kaapvaal Craton
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