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The stratigraphy and structural evolution of the late Proterozoic Gariep belt in the Sendelingsdrif-Annisfontein area, northwestern Cape Province

Bibliography: pages 128-143.

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Main Author: Von Veh, Mark Wolter
Format: Thesis
Language:English
Published: Department of Environmental and Geographical Science 2016
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access_status_str Open Access
author Von Veh, Mark Wolter
author_browse Von Veh, Mark Wolter
author_facet Von Veh, Mark Wolter
author_sort Von Veh, Mark Wolter
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description Bibliography: pages 128-143.
format Thesis
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institution University of Cape Town (South Africa)
language eng
last_indexed 2026-06-10T12:32:17.361Z
license_str Not specified — see source repository
provenance_str_mv Harvested via OAI-PMH from UCTD — University of Cape Town Open Access Repository
publishDate 2016
publishDateRange 2016
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publisher Department of Environmental and Geographical Science
publisherStr Department of Environmental and Geographical Science
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spelling oai:open.uct.ac.za:11427/17695 The stratigraphy and structural evolution of the late Proterozoic Gariep belt in the Sendelingsdrif-Annisfontein area, northwestern Cape Province Von Veh, Mark Wolter Geology Bibliography: pages 128-143. A geological investigation of the Port Nolloth metasediments in the central external parts of the Gariep Beit has led to a re-interpretation of tbeir lithostratigraphy and Pan-African geotectonic evolution. During the rifting stage of passive continental margin evolution, the basal elastic Stinkfontein Sequence was deposited in an alluvial fan environment. Fluviatile conglomerates and quartz arenites (Lekkersing Formation) interfinger with feldspathic arenites and minor volcanics (Vredefontein Formation), and prograde into marginal marine elastics and carbonates (Gumchavib Formation). Rift faulting produced local grabens into which massflow sediments (Kaigas Formation) and volcaniclastics (Rosh Pinah Formation) were shed. During the sea-floor spreading stage, a shallow-water carbonateclastic unit, the Hilda Sequence, was deposited. Conglomerates, quartzites, and schists with resedimented gravity-flow characteristics (Wallekraal Formation) are sandwiched between lower and upper platform carbonates (Pickelhaube and Dabie River Formations). The Hilda is unconformably overlain by the Numees Sequence, consisting of a widespread glaciogenic diamictite (Sendelingsdrif Formation) and a near-basal banded iron formation (Jakkalsberg Formation). A deep-water elastic unit, the Holgat Sequence, was laid down during the early stage of the lower Nama transgression. 2016-03-14T07:13:44Z 2016-03-14T07:13:44Z 1988 Doctoral Thesis Doctoral PhD http://hdl.handle.net/11427/17695 eng application/pdf Department of Environmental and Geographical Science Faculty of Science University of Cape Town
spellingShingle Geology
Von Veh, Mark Wolter
The stratigraphy and structural evolution of the late Proterozoic Gariep belt in the Sendelingsdrif-Annisfontein area, northwestern Cape Province
thesis_degree_str Doctoral
title The stratigraphy and structural evolution of the late Proterozoic Gariep belt in the Sendelingsdrif-Annisfontein area, northwestern Cape Province
title_full The stratigraphy and structural evolution of the late Proterozoic Gariep belt in the Sendelingsdrif-Annisfontein area, northwestern Cape Province
title_fullStr The stratigraphy and structural evolution of the late Proterozoic Gariep belt in the Sendelingsdrif-Annisfontein area, northwestern Cape Province
title_full_unstemmed The stratigraphy and structural evolution of the late Proterozoic Gariep belt in the Sendelingsdrif-Annisfontein area, northwestern Cape Province
title_short The stratigraphy and structural evolution of the late Proterozoic Gariep belt in the Sendelingsdrif-Annisfontein area, northwestern Cape Province
title_sort stratigraphy and structural evolution of the late proterozoic gariep belt in the sendelingsdrif annisfontein area northwestern cape province
topic Geology
url http://hdl.handle.net/11427/17695
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