Gomis-Cartesio, LE, Poyatos-Moré, M, Hodgson, DM orcid.org/0000-0003-3711-635X et al. (1 more author) (2018) Shelf-margin clinothem progradation, degradation and readjustment: Tanqua Depocentre, Karoo Basin (South Africa). Sedimentology, 65 (3). pp. 809-841. ISSN 0037-0746
Abstract
Degradation of basin-margin clinothems around the shelf-edge rollover zone may lead to the generation of conduits through which gravity flows transport sediment downslope. Many studies from seismic-reflection datasets show these features, but they lack small-scale (centimetre to metre) sedimentary and stratigraphic observations on process interactions. Exhumed basin-margin clinothems in the Tanqua depocentre (Karoo Basin) provide seismic-reflection-scale geometries and internal details of architecture with depositional dip and strike control. At the Geelhoek locality, clinothem parasequences comprise siltstone-rich offshore deposits overlain by heterolithic prodelta facies and sandstone-dominated deformed mouth bars. Three of these parasequences are truncated by a steep (6 to 22°), 100 m deep and 1.5 km wide asymmetrical composite erosion surface that delineates a shelf-edge canyon. The fill, from base to top comprises: (i) thick-bedded sandstone with intrabasinal clasts and multiple erosion surfaces; (ii) scour-based interbedded sandstone and siltstone with tractional structures; and (iii) inverse-graded to normal-graded siltstone beds. An overlying 55 m thick coarsening-upward parasequence fills the upper section of the canyon and extends across its interfluves. Younger parasequences display progressively shallower gradients during progradation and healing of the local accommodation. The incision surface resulted from initial oversteepening and high sediment supply triggering deformation and collapse at the shelf edge, enhanced by a relative sea-level fall that did not result in subaerial exposure of the shelf edge. Previous work identified an underlying highly incised, sandstone-rich shelf-edge rollover zone across-margin strike, suggesting that there was migration in the zone of shelf-edge to upper slope incision over time. This study provides an unusual example of clinothem degradation and re-adjustment with three-dimensional control in an exhumed basin margin succession. The work demonstrates that large-scale erosion surfaces can develop and migrate due to a combination of factors at the shelf-edge rollover zone, and proposes additional criteria to predict clinothem incision and differential sediment bypass in consistently progradational systems.
Metadata
Item Type: | Article |
---|---|
Authors/Creators: |
|
Copyright, Publisher and Additional Information: | (c) 2017 The Authors. Sedimentology (c) 2017 International Association of Sedimentologists. This is the peer reviewed version of the following article: Gomis-Cartesio, Luz. E., Poyatos-Moré, M., Hodgson, D. M. et al. Shelf-margin clinothem progradation, degradation and readjustment: Tanqua Depocentre, Karoo Basin (South Africa). Sedimentology, which has been published in final form at https://doi.org/10.1111/sed.12406. This article may be used for non-commercial purposes in accordance with Wiley Terms and Conditions for Self-Archiving. |
Keywords: | Clinothem degradation; Karoo basin; sediment bypass; shelf-edge deltas; shelf-margin evolution; submarine canyon |
Dates: |
|
Institution: | The University of Leeds |
Academic Units: | The University of Leeds > Faculty of Environment (Leeds) > School of Earth and Environment (Leeds) > Institute for Applied Geosciences (IAG) (Leeds) |
Depositing User: | Symplectic Publications |
Date Deposited: | 24 Aug 2017 08:24 |
Last Modified: | 08 Aug 2018 00:38 |
Status: | Published |
Publisher: | Wiley |
Identification Number: | 10.1111/sed.12406 |
Open Archives Initiative ID (OAI ID): | oai:eprints.whiterose.ac.uk:120527 |