Publications tagged with West Texas
Title | Publication Year Sort ascending | Abstract | Author | Series | Publisher | |
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Chert reservoir development in the Devonian Thirtyone Formation: Three Bar field, West Texas | 1995 | Chert reservoirs of the Lower Devonian Thirtyone Formation represent a substantial part of the hydrocarbon resource in the Permian Basin. More than 700 million barrels of oil has been produced from these rocks, and an equivalent amount of mobile oil remains. |
Ruppel, S.C., Hovorka, S.D. | Report of Investigations | Bureau of Economic Geology |
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Sequence hierarchy and facies architecture of a carbonate-ramp system: San Andres Formation of Algerita Escarpment and western Guadalupe Mountains, West Texas and New Mexico | 1995 | This study offers a high-frequency sequence stratigraphic model of carbonate-ramp strata of the San Andres Formation. |
Kerans, Charles, Fitchen, W.M. | Report of Investigations | Bureau of Economic Geology |
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Guide to the Permian reef geology trail, McKittrick Canyon, Guadalupe Mountains National Park, West Texas | 1993 | Bebout, D.G., Kerans, Charles, Brown, Alton, Loucks, R.G., Mruk, Denise, Kirkland, B.L., Longacre, S.A., Stoudt, E.L. | Guidebook | Bureau of Economic Geology | |
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Surface fissures in the Hueco Bolson and adjacent basins, West Texas | 1992 | Surface fissures have been observed in many desert basins in the western United States. These surface-collapse features are usually discovered after a normally dry surface has been covered with water, either by runoff from intense rainfall, by flooding, or by irrigation. |
Baumgardner, R.W., Jr., Scanlon, B.R. | Geological Circular | Bureau of Economic Geology |
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Arid basin depositional systems and paleosols: Fort Hancock and Camp Rice Formations (Pliocene-Pleistocene), Hueco Bolson, West Texas and adjacent Mexico | 1991 | The Hueco Bolson is a segment of the Rio Grande Rift that formed as a result of late Tertiary Basin and Range deformation. The upper Tertiary Fort Hancock Formation and the upper Tertiary-Quaternary Camp Rice Formation compose the basin fill except in the deepest (western) parts of the bolson. |
Gustavson, T.C. | Report of Investigations | Bureau of Economic Geology |
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Stratigraphic analysis of the Upper Devonian Woodford Formation, Permian Basin, West Texas and southeastern New Mexico | 1991 | The Upper Devonian Woodford Formation is an organic-rich petroleum source rock that extends throughout West Texas and southeastern New Mexico and currently is generating oil or gas in the subsurface. |
Comer, J.B. | Report of Investigations | Bureau of Economic Geology |
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Integrated characterization of Permian Basin reservoirs, university lands, West Texas: targeting the remaining resource for advanced oil recovery | 1991 | Unrecovered mobile oil is oil that is movable at reservoir conditions but is prevented from migrating to existing we1 l bores because of geologic complexities or heterogeneities. |
Tyler, Noel, Bebout, D.G., Garrett, C.M., Jr., Guevara, E.H., Hocott, C.R., Holtz, M.H., Hovorka, S.D., Kerans, Charles | Report of Investigations | Bureau of Economic Geology |
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Identification of sources and mechanisms of salt-water pollution affecting ground-water quality: a case study, West Texas | 1990 | Occurrences of ground-water and soil salinization are numerous in the Concho River watershed and its confluence with the Colorado River in West Texas and in other semiarid regions of Texas and the United States. |
Richter, B.C., Dutton, A.R., Kreitler, C.W. | Report of Investigations | Bureau of Economic Geology |
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Depositional systems and karst geology of the Ellenburger Group (Lower Ordovician), subsurface West Texas | 1990 | The Ellenburger Group (Lower Ordovician) of Texas is a laterally extensive peritidal carbonate shelf sequence. It forms a major deep oil reservoir, having estimated reserves of 1.15 billion barrels of oil, and it also contains an estimated 2.2 billion barrels of oil equivalent. |
Kerans, Charles | Report of Investigations | Bureau of Economic Geology |
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Delineation of unrecovered mobile oil in a mature dolomite reservoir: East Penwell San Andres Unit, university lands, West Texas | 1990 | The East Penwell San Andres Unit produces from a depth of approximately 3,400 ft (1,040 m) on the east flank of a broad, low-relief anticline on the east side of the Central Basin Platform of the Permian Basin in Ector and Crane Counties, West Texas. |
Major, R.P., Vander Stoep, G.W., Holtz, M.H. | Report of Investigations | Bureau of Economic Geology |