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- W119150134 abstract "Seven late Paleozoic inliers are shown on various published maps to occur in three areas of the Edwards Plateau of central Texas. Two of these inliers are early Wolfcampian (Permian) and contain a rich, well preserved, undescribed fusulinacean fauna including Pseudoschwagerina, Paraschwagerina, and Leptotriticities. These inliers are near the eastern boundary of Sutton County in the beds of Epps and West Copperas creeks. The carbonate rock of these inliers consist of thin to medium bedded wackestone and grainstone. A sponge-bryozoan-crinoid mound and a phylloid algal mound or bank are present in the Epps Creek section. Other fossils include gastropods, corals, brachiopods, smaller foraminifers, and conodonts. Depositional setting is interpreted to have been in the shallow, normal marine, middle shelf of the southern Eastern Shelf of the Midland Basin. These inliers are dominated by carbonate deposition with much less terrigenous clastic input than is characteristic of most exposures of Eastern Shelf rocks. Fusulinid correlations can be made with similar faunas from the middle part of the Wichita Group of north-central Texas and the middle part of the Council Grove Group of Oklahoma and Kansas. Other correlations can be made with rocks in the Hueco and Glasss mountains, the Eastern Shelf, andmore » the Big Hatchet Mountains of New Mexico. Several species resemble forms described from Asiatic fusulinacean faunas of Asselian age.« less" @default.
- W119150134 created "2016-06-24" @default.
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- W119150134 date "1988-01-01" @default.
- W119150134 modified "2023-09-23" @default.
- W119150134 title "Wolfcampian fusulinid biostratigraphy of the Edwards Plateau, central Texas" @default.
- W119150134 hasPublicationYear "1988" @default.
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