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- W2067968632 abstract "Introduction The Oklahoma Panhandle was once called no man's land because it was a narrow strip of land of doubtful value lying between Kansas and Texas. Geologically, the Oklahoma Panhandle is situated along the northwest flank of the Anadarko Basin and separates the Dalhart Basin from the Hugoton Embayment of the Anadarko Basin. This is a geographic separation rather than a tectonic separation. As a result, the Panhandle has been subject to a basin-flank Panhandle has been subject to a basin-flank geological history as compared with the basin troughs on either side. Initial production of natural gas in the Oklahoma Panhandle was from rocks of Permian age: the Herington, Krider and Winfield porous limestones and dolomites in the Hugoton field. Production came from above 3,000 ft [drilled Production came from above 3,000 ft [drilled depth] and many wells were rated as being major producers. producers. Prior to the early 1950's, there had been only limited, sporadic production from reservoirs older than the Permian. With the discovery of gas in Beaver County [eastern county in the panhandle] in upper Pennsylvanian limestones, major development and exploitation of other Pennsylvanian and Mississippian horizons quickly Pennsylvanian and Mississippian horizons quickly followed. In addition to the Permian production in the Oklahoma Panhandle, variable production has been found in the Pennsylvanian rocks: Wabaunsee, Hoover, Tonkawa, Topeka, Kansas City lime, Toronto, Douglas, Council Grove, Hodges, Lovell, Des Moines, Oswego, Marmaton, Cherokee, Morrow, Purdy, Keyes, Collier, Atoka, basal Pennsylvanian; Mississippian: Chester, Meramec Pennsylvanian; Mississippian: Chester, Meramec and Devonian Hunton. Some of these beds are correlative, being local names of a given horizon. The Morrow is by far the most important of this list,, followed by the Chester, the Hoover, Tonkawa and Topeka in approximately equal proportions. REGIONAL GEOLOGY Fig. 1 illustrates the subsurface structure across the Oklahoma Panhandle as shown on the datum at the base of the Pennsylvanian system of rocks. Starting in the western part, in Cimarron County, depths to the pre-Pennsylvanian sequence of rocks average some 1,000 ft below sea level. Because of the lack of drilling, this part of the county is poorly known. One fault probably related to the faults in Texas County, is shown. Keyes Dome is situated within the closing contour in the northeast corner of Cimarron County. Differences in subsurface elevations across Texas County range from 1,000 ft to 4,400 ft below sea level." @default.
- W2067968632 created "2016-06-24" @default.
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- W2067968632 date "1969-09-28" @default.
- W2067968632 modified "2023-10-18" @default.
- W2067968632 title "Geologic Factors Which May Affect the Occurrence of Natural Gas in the Oklahoma Panhandle" @default.
- W2067968632 doi "https://doi.org/10.2118/2566-ms" @default.
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