Résumé of the Geology of the Wichita Mountains, Oklahoma1
Gerald W. Chase, E. A. Frederickson, William E. Ham, 1956. "Résumé of the Geology of the Wichita Mountains, Oklahoma", Petroleum Geology of Southern Oklahoma, I. Curtis Hicks, Jerome Westheimer, C. W. Tomlinson, D. M. Putman, E. L. Selk
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A general survey of the geology of the Wichita Mountains is presented here as a means of broadening the geologic background for structural and stratigraphic interpretations in subsurface studies of southern Oklahoma. Detailed descriptions of the common Precambrian igneous rocks, along with measured sections and important faunal markers of Upper Cambrian and Lower Ordovician strata, are taken partly from published sources and partly from unpublished studies by the writers. New mapping of the conglomerates in the eastern part of the region by Chase shows clearly that they are part of the Wichita formation of early Permian age, thus indicating the date of the latest significant orogenic movement in the Wichita Mountains.
Figures & Tables
Because of the excellent pioneer work done by Eldridge in mapping occurrences of oil seeps, asphaltic sandstones, and showings in water wells, in southern Oklahoma, and by Taff and Gould on the structure and stratigraphy of the Arbuckle and Wichita mountain areas, there was ample evidence of the presence of petroleum to lure the prospector when Oklahoma and Indian Territories were opened for leasing just after the turn of the century.
About one-fourth the area covered by the oil fields of southern Oklahoma has Pennsylvanian rocks on the surface. This portion has been very well described in the literature. The remaining three-fourths is covered with Permian rocks, the oldest being the upper Pontotoc massive cherty brown sandstones. These are overlain by the Wichita formation consisting of 700 feet of alternating gray sandstones and interbedded purplish-maroon shales and barite beds, and bone beds with the remains of Permian reptiles, sharks, and amphibians. Next above is the basal asphaltic gray sandstone of the Garber formation resting unconformably on whatever may be below it, and carrying the huge “flying saucer” concretions; above which is the remaining 300-foot section of maroon conglomeratic sandstones and shales. The Garber crops out around and over more oil fields than any other formation in southern Oklahoma—like the Mesaverde of the Rockies. Next above is the 400-foot greenish-gray sandy shale section of the Hennessey, followed in turn by the 200-foot maroon sandstone section of the Duncan, the 4oo-foot “purple” shale of the Chickasha, and the 400-foot Whitehorse group. At the top are the Cloud Chief gypsum and the Quartermaster formation.
The conspicuous surface folds along the old lines of weakness prove that the folding at the close of Permian time and again after Cretaceous time was pronounced, supporting ideas of Bullard (1928) and Freie (1930).
From the discovery of the Granite field in 1901, Wheeler in 1905, Cruce in 1906, through Loco and Healdton in 1913, Fox in 1915, Wildcat Jim in 1916, and Velma in 1917, to Robberson in 1920, Sholom Alechem in 1923, and Apache in 1941, most of the fields of southern Oklahoma have been discovered by adhering strictly to common sense rules of oil finding by testing areas of favorable structure close to oil seeps, showings of oil and gas, and asphaltic sandstone occurrences.