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- W2474824614 abstract "Exposures in the lower Witteberg Group in the vicinity of Grahamstown record the change-over from a lobate deltaic shoreline to a linear barrier-island shoreline. The basal part of the sequence, the Weltevrede Formation, was formed by a process of delta progradation, abandonment, and transgressive reworking in a continuation of the coastal style established during Bokkeveld sedimentation. The persistence of quartz arenites throughout the overlying Witpoort Formation suggests a change in shoreline configuration brought about by a reduction in sediment supply to the coastal region and a reduction in the subsidence rate. These led to a greater reworking of the sediment resulting in increased maturity and longshore redistribution by waves" @default.
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- W2474824614 date "1992-12-01" @default.
- W2474824614 modified "2023-09-26" @default.
- W2474824614 title "Late Devonian shoreline changes; an analysis of Witteberg Group stratigraphy in the Grahamstown area" @default.
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