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Sedimentary facies from the Head of the Cape Canyon : insights into the Cenozoic evolution of the western margin of South Africa

Includes bibliographical references.

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Bibliographic Details
Main Author: Wigley, Rochelle Anne
Other Authors: Compton, John
Format: Thesis
Language:English
Published: Department of Geological Sciences 2014
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access_status_str Open Access
author Wigley, Rochelle Anne
author2 Compton, John
author_browse Compton, John
Wigley, Rochelle Anne
author_facet Compton, John
Wigley, Rochelle Anne
author_sort Wigley, Rochelle Anne
collection Thesis
description Includes bibliographical references.
format Thesis
id oai:open.uct.ac.za:11427/4232
institution University of Cape Town (South Africa)
language eng
last_indexed 2026-06-10T12:34:06.076Z
license_str Not specified — see source repository
provenance_str_mv Harvested via OAI-PMH from UCTD — University of Cape Town Open Access Repository
publishDate 2014
publishDateRange 2014
publishDateSort 2014
publisher Department of Geological Sciences
publisherStr Department of Geological Sciences
record_format dspace
source_str UCTD — University of Cape Town Open Access Repository
spelling oai:open.uct.ac.za:11427/4232 Sedimentary facies from the Head of the Cape Canyon : insights into the Cenozoic evolution of the western margin of South Africa Wigley, Rochelle Anne Compton, John Rogers, John Geological Sciences Includes bibliographical references. Cenozoic sedimentary successions have a restricted distribution and are largely incomplete due to erosion and non-deposition on the western margin of southern Africa. For this reason, much controversy and uncertainty remains on the geological evolution of the western margin. The wide western margin is largely devoid of bathymetric features, except for the deeply incised Cape Canyon that crosscuts the continental slope and shelf ~150 km to the northwest of Cape Town. The Head of the Cape Canyon forms a well-developeed trough landwards of the Western Ridge, which separates the middle and outer shelf. More than 50 cores, up to 6 m in length, at water depths between 190 and 450 m were recovered from the Head of the Cape Canyon region. Siliclastic, authigenic and biogenic sediments, varying in age from Cretaceous to Holocene provide the basis of a detailed sedimentary analysis. The diversity of lithostratigraphic units recovered from the condensed sedimentary record provides a unique opportunity to define in detail, for the first time, a late Cenozoic stratigraphic record for the western outer continental shelf. 2014-07-30T17:28:23Z 2014-07-30T17:28:23Z 2004 Doctoral Thesis Doctoral PhD http://hdl.handle.net/11427/4232 eng application/pdf Department of Geological Sciences Faculty of Science University of Cape Town
spellingShingle Geological Sciences
Wigley, Rochelle Anne
Sedimentary facies from the Head of the Cape Canyon : insights into the Cenozoic evolution of the western margin of South Africa
thesis_degree_str Doctoral
title Sedimentary facies from the Head of the Cape Canyon : insights into the Cenozoic evolution of the western margin of South Africa
title_full Sedimentary facies from the Head of the Cape Canyon : insights into the Cenozoic evolution of the western margin of South Africa
title_fullStr Sedimentary facies from the Head of the Cape Canyon : insights into the Cenozoic evolution of the western margin of South Africa
title_full_unstemmed Sedimentary facies from the Head of the Cape Canyon : insights into the Cenozoic evolution of the western margin of South Africa
title_short Sedimentary facies from the Head of the Cape Canyon : insights into the Cenozoic evolution of the western margin of South Africa
title_sort sedimentary facies from the head of the cape canyon insights into the cenozoic evolution of the western margin of south africa
topic Geological Sciences
url http://hdl.handle.net/11427/4232
work_keys_str_mv AT wigleyrochelleanne sedimentaryfaciesfromtheheadofthecapecanyoninsightsintothecenozoicevolutionofthewesternmarginofsouthafrica