Deltaic sedimentation in a rift valley lake: New seismic reflection data from Lake Malawi (Nyasa), East Africa
1993
Digital seismic reflection data acquired over the subaqueous parts of five rift-lake deltas in Lake Malawi (Nyasa), Africa, reveal a striking variability in delta morphology. Gross variations appear to be controlled by tectonic setting. Border-fault margin and accommodationzone margin deltas have steeply sloping depositional surfaces, acoustic signatures dominated by chaotic seismic facies, and an overall aggradational character. Shoaling margin deltas that are opposite the main border faults and axial-margin deltas that parallel the rift axis have slopes generally
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