Waterford Formation in the south-eastern Karoo: Implications for basin development

South African Journal of Science

 
 
Field Value
 
Title Waterford Formation in the south-eastern Karoo: Implications for basin development
 
Creator Rubidge, Bruce S. Hancox, P. John Mason, Richard
 
Subject Geosciences Karoo Supergroup; Beaufort; Ecca; stratigraphy; deposits
Description Extensive research on the rocks of the Karoo Supergroup has shown that this sequence, which contains an unsurpassed record of Permian–Jurassic tetrapods, records a largely unbroken stratigraphic succession from 300 Ma to 180 Ma. This Gondwanan succession was deposited in a changing environmental setting reflecting glacial marine through deltaic to fluvial and aeolian desert conditions. The contact between the Ecca and Beaufort Groups (at the top of the Waterford Formation of the Ecca Group) in the southern and western Karoo represents a change in depositional environment from a subaqueous to a subaerial delta plain. By contrast, the Waterford Formation has not yet been recognised in the south-eastern Karoo Basin, which might imply that a major unconformity is present between the Fort Brown Formation of the Ecca Group, deposited in a prodelta environment, and the overlying fluvially deposited Koonap Formation of the Beaufort Group. From careful documentation of lithofacies and sedimentological data, it can be demonstrated that the Waterford Formation is indeed present in the south-eastern part of the basin and that no major unconformity is present – a fact that has implications for the mapping of Karoo rocks in the Eastern Cape Province of South Africa, for understanding the depositional environment of ’reptilian‘ fossils from the lowermost Beaufort in this part of the Karoo basin, and for basin development models.
 
Publisher AOSIS
 
Contributor NRF DST PAST
Date 2012-03-07
 
Type info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion — Geological analysis
Format application/pdf text/html application/epub+zip text/xml
Identifier 10.4102/sajs.v108i3/4.829
 
Source South African Journal of Science; Vol 108, No 3/4 (2012); 5 pages 1996-7489 0038-2353
 
Language eng
 
Relation
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https://journals.sajs.aosis.co.za/index.php/sajs/article/view/829/1065 https://journals.sajs.aosis.co.za/index.php/sajs/article/view/829/1106 https://journals.sajs.aosis.co.za/index.php/sajs/article/view/829/1114 https://journals.sajs.aosis.co.za/index.php/sajs/article/view/829/1108 https://journals.sajs.aosis.co.za/index.php/sajs/article/downloadSuppFile/829/3375 https://journals.sajs.aosis.co.za/index.php/sajs/article/downloadSuppFile/829/3376 https://journals.sajs.aosis.co.za/index.php/sajs/article/downloadSuppFile/829/3377 https://journals.sajs.aosis.co.za/index.php/sajs/article/downloadSuppFile/829/3378
 
Coverage South Africa; Karoo Permian Period —
Rights Copyright (c) 2012 Bruce S. Rubidge, P. John Hancox, Richard Mason https://creativecommons.org/licenses/by/4.0
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