4.5 Article

Stratigraphic evolution of the upper slope and shelf edge in the Karoo Basin, South Africa

Journal

BASIN RESEARCH
Volume 21, Issue 5, Pages 502-527

Publisher

WILEY
DOI: 10.1111/j.1365-2117.2009.00409.x

Keywords

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Funding

  1. Natural Environment Research Council
  2. BP
  3. Chevron
  4. ConocoPhillips
  5. ExxonMobil
  6. Norsk Hydro
  7. Statoil

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The Permian Ecca Group of the Karoo Basin, South Africa preserves an extensive well-exposed siliciclastic basin floor, slope and shelf-edge delta succession. The Kookfontein Formation includes multiple sedimentary cycles that display clinoform geometries and are interpreted to represent the deposits of a slope to shelf succession. The succession exhibits progradational followed by aggradational stacking of deltaic cycles that is related to a change in shelf-edge trajectory, and lies within two depositional sequences. Sediment was transferred to the slope via overextension of deltas onto and over the shelf edge, resulting in failure and re-adjustment of local slope gradients. The depositional facies and architecture of the Kookfontein Formation record the change from a bypass-to accretion-dominated margin, which is interpreted to reflect a decrease in sediment transport efficiency as the slope gradient decreased, slope length increased and shelf-edge trajectory rose. During this time the delivery system changed from point-sourced basin-floor fans fed by slope channels to starved basin-floor with sand-rich slope clinoforms. This is an example of a progradational margin in which the younger slope system is interpreted to be of a different style to the older slope system that fed the underlying sand-rich basin floor fans.

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