Stratigraphic evolution and characteristics of lobes : a high-resolution study of Fan 3, Tanqua Karoo, South Africa
dc.contributor.advisor | Wickens, H. de V. | en_ZA |
dc.contributor.advisor | Hodgson, D. M. | en_ZA |
dc.contributor.author | Neethling, J. M. | en_ZA |
dc.contributor.other | University of Stellenbosch. Faculty of Science. Dept. of Earth Sciences. | |
dc.date.accessioned | 2009-02-17T10:23:25Z | en_ZA |
dc.date.accessioned | 2010-06-01T08:44:25Z | |
dc.date.available | 2009-02-17T10:23:25Z | en_ZA |
dc.date.available | 2010-06-01T08:44:25Z | |
dc.date.issued | 2009-03 | en_ZA |
dc.description | Thesis (MSc (Earth Sciences))--University of Stellenbosch, 2009. | en_ZA |
dc.description.abstract | Fan 3 is one of four basin-floor fans that form part of the Tanqua Karoo Fan Complex in South Africa. It can be subdivided into several sandstone lobes, based on the presence of thin-bedded siltstone intervals above and below major sandstone packages. Six lobes are identified in the mid fan section, as well as two older groups of thin, low-volume turbidite deposits at the base. Some of the lobes are further divided into an upper and lower lobe-element based on depositional behaviour. The volumetrically and spatially larger lobes have a finger-like appearance in plan view, which is attributed to multiple lobe-scale axial zones. This is especially visible towards the eastern margins of Lobes 2, 4 and 5. The stratigraphy and facies distribution are presented on several 2D panels. Computer generated isopach maps are presented for each lobe, lobe-element and interlobe unit. Autogenic control on the depositional pattern of the Fan 3 lobe complex was inferred from the palaeoflow patterns of the composing lobes and lobe-elements. The majority of the lobes show a north-eastern palaeoflow direction in the south, with a gradual westward shift in the north. Inferred controls are basin-floor topography, the presence of pre-existing lobes, and characteristics of the depositional flow, such strength, density, sediment load, palaeoflow direction. | en_ZA |
dc.identifier.uri | http://hdl.handle.net/10019.1/2249 | |
dc.language.iso | en | en_ZA |
dc.publisher | Stellenbosch : University of Stellenbosch | |
dc.rights.holder | University of Stellenbosch | |
dc.subject | Lobes | en_ZA |
dc.subject | Axial zones | en_ZA |
dc.subject | Finger-shaped deposits | en_ZA |
dc.subject | Dissertations -- Geology | en |
dc.subject | Theses -- Geology | en |
dc.subject.lcsh | Formations (Geology) -- South Africa. | en_ZA |
dc.subject.lcsh | Geology, Stratigraphic | en_ZA |
dc.subject.lcsh | Submarine fans -- South Africa | en_ZA |
dc.title | Stratigraphic evolution and characteristics of lobes : a high-resolution study of Fan 3, Tanqua Karoo, South Africa | en_ZA |
dc.type | Thesis | en_ZA |
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