A multi-proxy study of the Kalkkop impact Crater Lake deposits in south-central South Africa: implications for late neogene climate evolution

dc.contributor.advisorHarris, Chrisen_ZA
dc.contributor.advisorRoberts, Daveen_ZA
dc.contributor.authorMthembi, Ponanien_ZA
dc.date.accessioned2014-11-05T03:45:31Z
dc.date.available2014-11-05T03:45:31Z
dc.date.issued2014en_ZA
dc.descriptionIncludes bibliographical references.en_ZA
dc.description.abstractThe Kalkkop Crater Lake deposit formed as a result of a meteorite impact, and is situated ~51 km southwest of Graaff-Reinet in the Southern part of South Africa. The structure is about 650 m wide, and contains 90 m of lake deposits that are mainly carbonate precipitates. A 90 m sediment core from the Kalkkop Crater Lake was investigated using sedimentology, palynology and geochemical analysis. The KK1 core, along with the other two boreholes (KK2 and KK3), comprise of finely laminated and massive, structureless carbonates interrupted by debris flows from the crater rim.en_ZA
dc.identifier.apacitationMthembi, P. (2014). <i>A multi-proxy study of the Kalkkop impact Crater Lake deposits in south-central South Africa: implications for late neogene climate evolution</i>. (Thesis). University of Cape Town ,Faculty of Science ,Department of Geological Sciences. Retrieved from http://hdl.handle.net/11427/9107en_ZA
dc.identifier.chicagocitationMthembi, Ponani. <i>"A multi-proxy study of the Kalkkop impact Crater Lake deposits in south-central South Africa: implications for late neogene climate evolution."</i> Thesis., University of Cape Town ,Faculty of Science ,Department of Geological Sciences, 2014. http://hdl.handle.net/11427/9107en_ZA
dc.identifier.citationMthembi, P. 2014. A multi-proxy study of the Kalkkop impact Crater Lake deposits in south-central South Africa: implications for late neogene climate evolution. University of Cape Town.en_ZA
dc.identifier.ris TY - Thesis / Dissertation AU - Mthembi, Ponani AB - The Kalkkop Crater Lake deposit formed as a result of a meteorite impact, and is situated ~51 km southwest of Graaff-Reinet in the Southern part of South Africa. The structure is about 650 m wide, and contains 90 m of lake deposits that are mainly carbonate precipitates. A 90 m sediment core from the Kalkkop Crater Lake was investigated using sedimentology, palynology and geochemical analysis. The KK1 core, along with the other two boreholes (KK2 and KK3), comprise of finely laminated and massive, structureless carbonates interrupted by debris flows from the crater rim. DA - 2014 DB - OpenUCT DP - University of Cape Town LK - https://open.uct.ac.za PB - University of Cape Town PY - 2014 T1 - A multi-proxy study of the Kalkkop impact Crater Lake deposits in south-central South Africa: implications for late neogene climate evolution TI - A multi-proxy study of the Kalkkop impact Crater Lake deposits in south-central South Africa: implications for late neogene climate evolution UR - http://hdl.handle.net/11427/9107 ER - en_ZA
dc.identifier.urihttp://hdl.handle.net/11427/9107
dc.identifier.vancouvercitationMthembi P. A multi-proxy study of the Kalkkop impact Crater Lake deposits in south-central South Africa: implications for late neogene climate evolution. [Thesis]. University of Cape Town ,Faculty of Science ,Department of Geological Sciences, 2014 [cited yyyy month dd]. Available from: http://hdl.handle.net/11427/9107en_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.titleA multi-proxy study of the Kalkkop impact Crater Lake deposits in south-central South Africa: implications for late neogene climate evolutionen_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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