The structural geology of the Naukluft Nappe Complex and its relationship to the Damara Orogenic Belt, South West Africa/Namibia

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dc.contributor.authorHartnady, Christopher John Huberten_ZA
dc.date.accessioned2016-03-21T19:13:23Z
dc.date.available2016-03-21T19:13:23Z
dc.date.issued1978en_ZA
dc.description.abstractThe Naukluft nappe complex has been quoted as a classic example of gravity gliding tectonics (Korn & Martin, 1959). Situated close to the southern margin of the Damara orogenic belt, it provides a key to the persistent controversy over the correlation of the "geosynclinal" Damara Supergroup with the Nama Group on the Kalahari craton. It also contains critical evidence bearing on the timing and large-scale geodynamics of the Late Precambrian-Early Palaeozoic Damara orogeny, particularly the hypothesis that it involved plate tectonic processes of subduction and continental collision in the southern zones.en_ZA
dc.identifier.apacitationHartnady, C. J. H. (1978). <i>The structural geology of the Naukluft Nappe Complex and its relationship to the Damara Orogenic Belt, South West Africa/Namibia</i>. (Thesis). University of Cape Town ,Faculty of Science ,Department of Geological Sciences. Retrieved from http://hdl.handle.net/11427/18057en_ZA
dc.identifier.chicagocitationHartnady, Christopher John Hubert. <i>"The structural geology of the Naukluft Nappe Complex and its relationship to the Damara Orogenic Belt, South West Africa/Namibia."</i> Thesis., University of Cape Town ,Faculty of Science ,Department of Geological Sciences, 1978. http://hdl.handle.net/11427/18057en_ZA
dc.identifier.citationHartnady, C. 1978. The structural geology of the Naukluft Nappe Complex and its relationship to the Damara Orogenic Belt, South West Africa/Namibia. University of Cape Town.en_ZA
dc.identifier.ris TY - Thesis / Dissertation AU - Hartnady, Christopher John Hubert AB - The Naukluft nappe complex has been quoted as a classic example of gravity gliding tectonics (Korn & Martin, 1959). Situated close to the southern margin of the Damara orogenic belt, it provides a key to the persistent controversy over the correlation of the "geosynclinal" Damara Supergroup with the Nama Group on the Kalahari craton. It also contains critical evidence bearing on the timing and large-scale geodynamics of the Late Precambrian-Early Palaeozoic Damara orogeny, particularly the hypothesis that it involved plate tectonic processes of subduction and continental collision in the southern zones. DA - 1978 DB - OpenUCT DP - University of Cape Town LK - https://open.uct.ac.za PB - University of Cape Town PY - 1978 T1 - The structural geology of the Naukluft Nappe Complex and its relationship to the Damara Orogenic Belt, South West Africa/Namibia TI - The structural geology of the Naukluft Nappe Complex and its relationship to the Damara Orogenic Belt, South West Africa/Namibia UR - http://hdl.handle.net/11427/18057 ER - en_ZA
dc.identifier.urihttp://hdl.handle.net/11427/18057
dc.identifier.vancouvercitationHartnady CJH. The structural geology of the Naukluft Nappe Complex and its relationship to the Damara Orogenic Belt, South West Africa/Namibia. [Thesis]. University of Cape Town ,Faculty of Science ,Department of Geological Sciences, 1978 [cited yyyy month dd]. Available from: http://hdl.handle.net/11427/18057en_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.otherGeologyen_ZA
dc.titleThe structural geology of the Naukluft Nappe Complex and its relationship to the Damara Orogenic Belt, South West Africa/Namibiaen_ZA
dc.typeDoctoral Thesis
dc.type.qualificationlevelDoctoral
dc.type.qualificationnamePhDen_ZA
uct.type.filetypeText
uct.type.filetypeImage
uct.type.publicationResearchen_ZA
uct.type.resourceThesisen_ZA
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