Petrogenesis of the Northwest corner intrusive phases, Dutoitspan kimberlite, South Africa

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dc.contributor.advisorLe Roex, Antonen_ZA
dc.contributor.authorHanekom, Adrien_ZA
dc.date.accessioned2014-07-30T17:26:18Z
dc.date.available2014-07-30T17:26:18Z
dc.date.issued2008en_ZA
dc.descriptionIncludes bibliographical references.
dc.description.abstractThe Outoitspan Group 1 kimberlite pipe forms part of the well-known cluster of pipes located in and around the city of Kimberley, South Africa. Eight macroscopically distinct intrusive phases, i.e. D2 Type 2, D2 Type 3, D2/D5, D5, D18, Type 5, D16 and the D16 dyke are present in the Northwest Corner area of the mine. Microscopically they range from macrocrystic to aphanitic hypabyssal (magmatic) kimberlites with varying amounts of opaque minerals, monticellite and phlogopite. Olivine is the dominant macrocryst phase and alteration varies from unaltered to highly serpentinised. These intrusive phases also contain variable amounts of crustal xenoliths.en_ZA
dc.identifier.apacitationHanekom, A. (2008). <i>Petrogenesis of the Northwest corner intrusive phases, Dutoitspan kimberlite, South Africa</i>. (Thesis). University of Cape Town ,Faculty of Science ,Department of Geological Sciences. Retrieved from http://hdl.handle.net/11427/4200en_ZA
dc.identifier.chicagocitationHanekom, Adri. <i>"Petrogenesis of the Northwest corner intrusive phases, Dutoitspan kimberlite, South Africa."</i> Thesis., University of Cape Town ,Faculty of Science ,Department of Geological Sciences, 2008. http://hdl.handle.net/11427/4200en_ZA
dc.identifier.citationHanekom, A. 2008. Petrogenesis of the Northwest corner intrusive phases, Dutoitspan kimberlite, South Africa. University of Cape Town.en_ZA
dc.identifier.ris TY - Thesis / Dissertation AU - Hanekom, Adri AB - The Outoitspan Group 1 kimberlite pipe forms part of the well-known cluster of pipes located in and around the city of Kimberley, South Africa. Eight macroscopically distinct intrusive phases, i.e. D2 Type 2, D2 Type 3, D2/D5, D5, D18, Type 5, D16 and the D16 dyke are present in the Northwest Corner area of the mine. Microscopically they range from macrocrystic to aphanitic hypabyssal (magmatic) kimberlites with varying amounts of opaque minerals, monticellite and phlogopite. Olivine is the dominant macrocryst phase and alteration varies from unaltered to highly serpentinised. These intrusive phases also contain variable amounts of crustal xenoliths. DA - 2008 DB - OpenUCT DP - University of Cape Town LK - https://open.uct.ac.za PB - University of Cape Town PY - 2008 T1 - Petrogenesis of the Northwest corner intrusive phases, Dutoitspan kimberlite, South Africa TI - Petrogenesis of the Northwest corner intrusive phases, Dutoitspan kimberlite, South Africa UR - http://hdl.handle.net/11427/4200 ER - en_ZA
dc.identifier.urihttp://hdl.handle.net/11427/4200
dc.identifier.vancouvercitationHanekom A. Petrogenesis of the Northwest corner intrusive phases, Dutoitspan kimberlite, South Africa. [Thesis]. University of Cape Town ,Faculty of Science ,Department of Geological Sciences, 2008 [cited yyyy month dd]. Available from: http://hdl.handle.net/11427/4200en_ZA
dc.language.isoengen_ZA
dc.publisher.departmentDepartment of Geological Sciencesen_ZA
dc.publisher.facultyFaculty of Scienceen_ZA
dc.publisher.institutionUniversity of Cape Town
dc.subject.otherGeological Sciencesen_ZA
dc.titlePetrogenesis of the Northwest corner intrusive phases, Dutoitspan kimberlite, South Africaen_ZA
dc.typeMaster Thesis
dc.type.qualificationlevelMasters
dc.type.qualificationnameMScen_ZA
uct.type.filetypeText
uct.type.filetypeImage
uct.type.publicationResearchen_ZA
uct.type.resourceThesisen_ZA
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