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- W339075983 abstract "The San Andres Formation on the Northern and Northwestern shelves of the Midland Basin is a progradational stratigraphic unit consisting predominantly of carbonate facies. Lithofacies include dolomite, laminated anhydrite and dolomite, massive bedded anhydrite, limestone, salt, and red beds. These lithofacies represent depositional environments that include deep-water outer shelf, shallow-water inner shelf, shallow-water to emergent shoals, and a sabkha complex that comprises intertidal to supratidal algal mud flats, hypersaline lagoons or brine pans, and terrigenous mud flats. Deposition was cyclic; a cycle began with a transgression followed by a gradual shoaling-upward sequence. Cycles commonly terminated with subaerial exposure before renewed transgression initiated a new cycle. Much of the dolomitization probably occurred during periods of subaerial exposure in schizohaline environments. Porosity probably was developed also during subaerial exposure. San Andres reservoirs of the Northern and Northwestern shelves yielded 12.7% of the total oil production for Texas in 1980. Trapping mechanisms are both structural and stratigraphic. 44 references." @default.
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- W339075983 date "1982-01-01" @default.
- W339075983 modified "2023-09-27" @default.
- W339075983 title "Facies and Stratigraphy of the San Andres Formation, Northern and Northwestern Shelves of the Midland Basin, Texas and New Mexico" @default.
- W339075983 doi "https://doi.org/10.23867/ri0128d" @default.
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