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dc.contributor.advisorOkujeni, C.
dc.contributor.advisorSiad, A-M.
dc.contributor.authorMudanalwo, Ratshalingwa Patience
dc.date.accessioned2021-02-24T09:20:45Z
dc.date.available2021-02-24T09:20:45Z
dc.date.issued2020
dc.identifier.urihttp://hdl.handle.net/11394/7871
dc.description>Magister Scientiae - MScen_US
dc.description.abstractThe Platreef, is a contact-type pyroxenitic reef in the Northern Limb of the Bushveld Complex, enriched in platinum group elements (PGE) and base metal sulfides (BMS). Relatively subdued mining in the Platreef, compared to RLS, has been attributed to limited knowledge regarding irregular distribution, complex style and genesis of PGE mineralisation in the Platreef. This study was, therefore, aimed at investigating the petrogenesis of the Platreef, particularly to evaluate whether the formation of the ore reefs resulted from a single or multiple sill-like magma intrusions. The study also sought to unveil the interplay of fractional crystallisation, hydrothermal fluid activities, floor rock and crustal contamination on the formation of Platreef types, PGE mineralisation and the magma source.en_US
dc.language.isoenen_US
dc.publisherUniversity of the Western Capeen_US
dc.subjectPlatreefen_US
dc.subjectPGE-BMS mineralisationen_US
dc.subjectPetrogenesisen_US
dc.subjectSr-Nd isotope geochemistryen_US
dc.subjectMultiple-staged magmaen_US
dc.titleGeochemical controls of platinum-group elements distribution patterns in the Patreef, bushveld complex, South Africa: a case study at Zwartfontein farm, Akanani prospect areaen_US
dc.rights.holderUniversity of the Western Capeen_US


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