Modelling the architecture of distal sand-rich lobe deposits : an example from Fan 2, Skoorsteenberg Formation, Tanqua Karoo, South Africa
dc.contributor.advisor | Wickens, H. de V. | en_ZA |
dc.contributor.advisor | Hodgson, D. | en_ZA |
dc.contributor.author | Steyn, Rochelle | en_ZA |
dc.contributor.other | University of Stellenbosch. Faculty of Science. Dept. of Earth Sciences. | |
dc.date.accessioned | 2009-02-17T07:07:43Z | en_ZA |
dc.date.accessioned | 2010-06-01T08:53:33Z | |
dc.date.available | 2009-02-17T07:07:43Z | en_ZA |
dc.date.available | 2010-06-01T08:53:33Z | |
dc.date.issued | 2009-03 | en_ZA |
dc.description | MSc | en_ZA |
dc.description | Thesis (MSc (Earth Sciences))—University of Stellenbosch, 2009. | |
dc.description.abstract | Fan 2, one of five submarine fan systems of the Tanqua fan complex in the south-western Karoo Basin, South Africa, is subdivided into Lower, Middle and Upper units. Here, detailed analysis of the internal architecture and distribution of lithofacies associations of Middle Fan 2 facilitated the 3-D visualisation of the sedimentological and stratigraphical changes towards the pinch-out. Middle Fan 2 is interpreted to be a lower-fan, sand-rich terminal lobe, comprising three sandstone-lobe elements, separated by two siltstone interlobe elements. It is fed by a distributary channel that is hypothetically positioned to the west-southwest of the study area. The sandstone-lobe elements pinch out downdip to the north-east and updip to the southsouthwest in the study area. The consecutive pinch out of lobe elements to the north-east indicates a progradational stacking pattern similar to the entire lobe complex. Palaeocurrent analysis and the interpretation of isopach maps indicate that the transport direction of Middle Fan 2 was in a north-easterly direction. The fringes of the lobe and the distribution of internal elements (channels, amalgamated sheets and sheets) show a finger-like geometry in plan-view, in contrast to simple radial-lobe bodies that are commonly envisaged. | en_ZA |
dc.identifier.uri | http://hdl.handle.net/10019.1/2608 | |
dc.language.iso | en | en_ZA |
dc.publisher | Stellenbosch : University of Stellenbosch | |
dc.rights.holder | University of Stellenbosch | |
dc.subject | Tanqua Karoo | en_ZA |
dc.subject | Co-genetic debrites | en_ZA |
dc.subject | Middle Fan 2 | en_ZA |
dc.subject | Dissertations -- Geology | en |
dc.subject | Theses -- Geology | en |
dc.subject.lcsh | Submarine fans -- South Africa | en_ZA |
dc.subject.lcsh | Turbidites -- South Africa | en_ZA |
dc.subject.other | Geology, Geography and Environmental Studies | en_ZA |
dc.title | Modelling the architecture of distal sand-rich lobe deposits : an example from Fan 2, Skoorsteenberg Formation, Tanqua Karoo, South Africa | en_ZA |
dc.type | Thesis | en_ZA |
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