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- W2159504460 endingPage "1093" @default.
- W2159504460 startingPage "1076" @default.
- W2159504460 abstract "The geomorphology and seismic stratigraphy of deep-water clastic systems from slope valleys through channel-levee systems to basin-floor fans have been observed and described in modern and ancient subsurface examples around the world. However, the distribution of sedimentary facies, grain size, and small-scale architectural elements remains poorly constrained. Extensive exposures (>2500 km2) of four stacked deep-water composite sequences have been mapped from heterolithic channel-levee systems on the slope to sand-rich basin-floor deposits. The data set from Units C–F of the Fort Brown Formation in the Permian Laingsburg depocenter of South Africa permits a unique opportunity to document and compare their depositional architecture at a high resolution for tens of kilometers downdip." @default.
- W2159504460 created "2016-06-24" @default.
- W2159504460 creator A5027713105 @default.
- W2159504460 creator A5043420934 @default.
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- W2159504460 date "2014-12-01" @default.
- W2159504460 modified "2023-10-16" @default.
- W2159504460 title "Depositional architecture of sand-attached and sand-detached channel-lobe transition zones on an exhumed stepped slope mapped over a 2500 km2 area" @default.
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- W2159504460 doi "https://doi.org/10.1130/ges01035.1" @default.
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