--> Seismic Sedimentology of Incised Valley, Lowstand Delta, and Slope Fan Systems in the Eocene Wilcox Group, Central South Texas Coast
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Seismic Sedimentology of Incised Valley, Lowstand Delta, and Slope Fan Previous HitSystemsNext Hit in the Eocene Wilcox Group, Central South Texas Coast

Abstract

Tectonic and stratigraphic architecture of the Wilcox Group along the central coastal plain of Texas defines a series of growth-fault-controlled subbasins similar to those in the Frio Formation in South Texas. A seismic sedimentologic study was performed to map fourth- and fifth-order Previous HitsystemsNext Hit Previous HittractsNext Hit in a 2,500-km2 3D seismic survey in Bee and Goliad Counties. Guided by third-order sequence-stratigraphic correlations from seismic and sparse wireline-log data, we prepared stratal-slice maps to reveal high-resolution (10-m scale) sediment-dispersal patterns and associated Previous HitsystemsNext Hit Previous HittractsNext Hit in a relative geologic-time domain, particularly in lowstand subbasins. The integration of core, wireline log, and seismic-geomorphologic patterns in stratal slices makes it possible to identify three Previous HittypesNext Hit of depositional Previous HitsystemsNext Hit in a typical third-order lowstand Previous HitsystemsNext Hit tract: (1) incised valleys and associated fluvial Previous HitsystemsNext Hit on an exposed shelf; (2) lowstand prograding deltaic Previous HitsystemsNext Hit composed of strike-oriented and lobate deltaic sandstone bodies at the shelf edge; and (3) fault-controlled, off-shelf slope fans best characterized by point-sources, fan-like channel/levee Previous HitsystemsNext Hit or line-sourced, complex mudslide/gully Previous HitsystemsNext Hit. Sand-dispersal patterns are controlled primarily by accommodation resulting from rollover topography associated with growth faulting. Sandstone thickness and dispersal patterns can be predicted by integrating wireline-log measurements and seismic amplitude patterns. The high-quality, large 3D seismic data set provides a rare opportunity to visually inspect spatial relationships between incised valleys, self-edge deltas, and slope fans in a high-resolution stratigraphic framework. A sequential display of stratal slices reveals how the depositional Previous HitsystemsTop respond to accommodation controlled by gravity tectonics.