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Additional info for Deep-water sandstones, Brushy Canyon Formation, West Texas (AAPG Course Notes 40)
In contrast to the deeply incised slope channels of the upper member, these channels exhibit simple erosional bases, are much less incised and have higher width to thickness (aspect) ratios. Some erosional surfaces associated with the channel bases are overlain by coarse lags. Channels tend to be filled from axes to margins by fine grained amalgamated, thick-bedded cross-stratified sandstones exhibiting aggradational bed forms. These features suggest deposition from long-lived currents and relatively high sedimentation rates.
Complexes such as these are viewed as intermediate between the main channel complex at Colleen Canyon and the layered sheet complexes seen on the previous page. They represent deposition within a transitional environment between confined and unconfined settings. 3. Summary of Outer Basin Floor Fan Sheet Complex Characteristics Sandbody Geometry: Sharp based, extremely continuous, 5-7 m layered sandstone "packets" that are either compensationally stacked, laterally offset from one another, or stacked aggradationally.
Silver, B. A. and Todd, R. G. 1969, Permian Cyclic Strata, Northern Midland and Delaware Basins, West Texas and Southeastern New Mexico, American Association of Petroleum Geologists Bulletin, 53, p. 2223-2225. M. , 1998, Stratigraphic Hierarchy of Organic Carbon-rich Siltstones in Deep-water Facies, Brushy Canyon Formation (Guadalupian), Delaware Basin, West Texas, Geology, 26, p. 451-454. R. , 1998, Siltstone Facies of the Upper Brushy Canyon and Lower Cherry Canyon Formations (Guadalupian), Delaware Basin, West Texas: Depositional Processes and Stratigraphic Distribution; in The Search Continues into the 21st Century: West Texas Geological Society, Publication, DeMis, W.