River-dominated, shelf-edge deltas: Delivery of sand across the shelf break in the absence of slope incision

Sedimentology

Volumn 59, Issue 4, 2012, Pages 1133-1157

  Dixon, Joshua F ^a   Steel, Ronald J ^a   Olariu, Cornel ^a  

^a UNIVERSITY OF TEXAS AT AUSTIN   (United States)

Author keywords

Clinoforms; Hyperpycnal flow; Karoo Basin; Shelf edge delta; Soft sediment deformation

Indexed keywords

CLINOFORMS; HYPERPYCNAL FLOWS; KAROO BASIN; SHELF-EDGE DELTA; SOFT-SEDIMENT DEFORMATION;

DEBRIS; DEFORMATION; RIVERS; SANDSTONE; SEDIMENTOLOGY; SEDIMENTS; STRATIGRAPHY; THREE DIMENSIONAL;

SLOPE STABILITY;

CORRELATION; DEBRIS FLOW; DEEP WATER; DEFORMATION; DENSITY CURRENT; DEPOSITION; PERMIAN-TRIASSIC BOUNDARY; SAND; SANDSTONE; SEDIMENT TRANSPORT; SHALLOW WATER; SHELF BREAK; SILTSTONE;

KAROO; SOUTH AFRICA;

TANQUA;

EID: 84861188805     PISSN: 00370746     EISSN: 13653091     Source Type: Journal    
DOI: 10.1111/j.1365-3091.2011.01298.x     Document Type: Article

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