Contrast in the process response of stacked clinothems to the shelf-slope rollover
Two stacked parasequences exposed continuously along a 35-km dip section in the Permian lower Waterford Formation, Karoo Basin, South Africa, form basin margin-scale clinothems, and their internal facies distributions have been mapped out from shelf to upper submarine-slope settings. Sedimentary fac...
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Veröffentlicht in: | Geosphere (Boulder, Colo.) Colo.), 2013-04, Vol.9 (2), p.299-316 |
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