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Extra info for Deep-water sandstones, Brushy Canyon Formation, West Texas (AAPG Course Notes 40)
Tc = current ripple dominated sst. Td = planar-stratifiedshaly sst. Te = planar-stratifiedto massive mdst. A. = Channel Axis deposit C. M. B. = Confined Channel Com~lex a = bioturbation M = massive bedding = ash bed 41 = current ripples a = contorted beds a:. 2-= trough cross-beds --= water escape structures EPR Co. 6. Core Summary Plot 'd, Te rc, TC - Te The EPR Co. Buena Vkta #2 well penetrates the upper member of the Bmshy Canyon Formation. The Buena Vista outcrop is oriented slightly oblique to the paleo-flow direction (see Fig.
A50. S. Thesis, University of Texas, 242 p. 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.
Although the sandstone "packages" are highly continuous, lenticular and compensatory sandstone bedding styles and small scale scour surfaces are locally present. Loaded bedding contacts, flame structures and evidence for dewatering are abundant and indicate high rates of deposition. The bases of these sheet complexes are relatively sharp but tend to be nonerosional. They are either overlain by thinner siltstone dominated intervals or, where amalgamated, the base of a younger sandstone "packet".