Show simple item record

dc.contributor.advisorCarey, Paul
dc.contributor.advisorDomoney, Reginald
dc.contributor.authorVan Bloemenstein, Chantell Berenice
dc.contributor.otherDept. of Earth Science
dc.contributor.otherFaculty of Science
dc.date.accessioned2013-08-27T12:24:40Z
dc.date.available2007/09/07 08:41
dc.date.available2007/09/07
dc.date.available2013-08-27T12:24:40Z
dc.date.issued2006
dc.identifier.urihttp://hdl.handle.net/11394/1982
dc.descriptionMagister Scientiae - MScen_US
dc.description.abstractThe reservoir quality (RQ) of well E-BA1 was characterized using thin sections and core samples in a petrographic study. Well E-BA1 is situated in the Bredasdorp Basin, which forms part of the Outeniqua Basin situated in the Southern Afircan offshore region. Rifting as a result of the break up of Gondwanaland formed the Outeniqua Basin. The Bredasorp Basin is characterized by half-graben structures comprised of Upper Jurassic, Lower Cretaceous and Cenozoic rift to drift strata. The current research within the thesis has indicated that well E-BA1 is one of moderate to good quality having a gas-condensate component.en_US
dc.language.isoenen_US
dc.publisherUniversity of the Western Capeen_US
dc.subjectSandstone - South Africaen_US
dc.subjectPetrology - South Africaen_US
dc.subjectSedimentary basins - South Africaen_US
dc.titlePetrographic characterization of sandstones in borehole E-BA1, Block 9, Bredasdorp Basin, Off-Shore South Africaen_US
dc.typeThesisen_US
dc.rights.holderUniversity of the Western Capeen_US
dc.description.countrySouth Africa


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record