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southwestern Oklahoma

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Journal Article
Published: 01 May 2021
Journal of Paleontology (2021) 95 (3): 586–600.
... new species, Karstiulus fortsillensis new genus new species, and Dolesea subtila new genus new species) found in fossil-producing pockets of the Fort Sill fissures exposed in the Dolese Quarry near Richards Spur, southwest Oklahoma, USA. These are the first new genera of invertebrates to be described...
FIGURES | View All (7)
Journal Article
Journal: AAPG Bulletin
Published: 01 February 2017
AAPG Bulletin (2017) 101 (2): 205–232.
...Liu Li; R. Paul Philp; Thanh X. Nguyen ABSTRACT The Lawton oil field is located on the Wichita Mountain uplift in southwestern Oklahoma. This study focused on addressing three problems related to the Lawton oil field: (1) What is (are) the source(s) of the oils? (2) Have the oils been subjected...
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Journal Article
Journal: AAPG Bulletin
Published: 01 January 2002
AAPG Bulletin (2002) 86 (1): 145–160.
... that have not undergone active subsidence for tens or hundreds of millions of years. The Anadarko basin in southwestern Oklahoma has areas of extensive overpressuring ( Figure 1 ) ( Hunt, 1990 ; Al-Shaieb et al., 1992 , 1994a , 1994b ), yet the Anadarko basin has not experienced significant sedimentation...
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Journal Article
Journal: GSA Bulletin
Published: 01 January 1995
GSA Bulletin (1995) 107 (1): 98–112.
...Meridee Jones-Cecil Abstract Holocene reactivation of the aseismic Meers fault in southwestern Oklahoma illustrates the limitation of using the historical seismic record for identifying hazardous faults in the central United States. The 26- to 37-km-long fault scarp is one of the few known scamps...
Journal Article
Journal: AAPG Bulletin
Published: 11 November 1992
AAPG Bulletin (1992) 76 (11): 1649–1664.
...Guoqiu Gao; Lynton S. Land; Robert L. Folk ABSTRACT Thick, massive dolomite units from the upper Arbuckle (lower Ordovician) peritidal carbonate sequence, Slick Hills, southwestern Oklahoma, provide insight into two important problems: (1) modification of early dolomite, and (2) late dolomitization...
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Journal Article
Journal: Geophysics
Published: 01 January 1991
Geophysics (1991) 56 (1): 90–101.
...D. W. Vasco; C. Taylor Abstract The diagonal elements of the gravity gradient tensor, as recorded by the Bell airborne Gravity Gradient Survey System (GGSS), are used to determine the basement topography in southwestern Oklahoma. This determination is accomplished through a nonlinear inverse...
Journal Article
Published: 01 December 1990
Bulletin of the Seismological Society of America (1990) 80 (6A): 1677–1695.
... from a survey performed in 1985 by The University of Texas at El Paso and The University of Texas at Dallas across the Anadarko basin and the Wichita Mountains in southwestern Oklahoma. The results provide an independent look at details of near-surface structure and reflector configurations. Near...
Journal Article
Journal: GSA Bulletin
Published: 01 January 1990
GSA Bulletin (1990) 102 (1): 1–17.
... in southwestern Oklahoma. The eastern half of the scarp is formed on relatively ductile Permian Hennessey Shale and Quaternary alluvium, whereas the western half is formed on well-lithified, relatively brittle Permian Post Oak Conglomerate in the Slick Hills. At Canyon Creek on the eastern half of the scarp...
Journal Article
Published: 01 June 1989
Bulletin of the Seismological Society of America (1989) 79 (3): 873–887.
...Xianhuai Zhu; George A. McMechan Abstract In January of 1985, a densely-recorded, wide-aperture seismic experiment was performed by the University of Texas at El Paso and at Dallas, across the southwestern Oklahoma aulacogen. A two-dimensional P -wave velocity distribution is estimated...
Journal Article
Journal: GSA Bulletin
Published: 01 March 1988
GSA Bulletin (1988) 100 (3): 392–401.
Book Chapter

Author(s)
R.N. Donovan
Series: DNAG, Centennial Field Guides
Published: 01 January 1988
DOI: 10.1130/0-8137-5404-6.79
EISBN: 9780813754109
... Abstract The Meers fault scarp trends ESE-WNW along the northern edge of the Meers Valley in Commanche County, southwestern Oklahoma (Fig. 1 ). The impressively straight scarp can be traced for 16 mi (26 km). The southeastern two-thirds of the scarp intends across land that is under relatively...
Series: DNAG, Centennial Field Guides
Published: 01 January 1988
DOI: 10.1130/0-8137-5404-6.93
EISBN: 9780813754109
... Abstract The Bally Mountain Range is located in eastern Kiowa County in southwestern Oklahoma (T.6N., R.14W.). The closest important road is Oklahoma 58 (Fig. 1). This road can be accessed from the H. E. Bailey Turnpike by taking the Medicine Park exit a few miles north of Lawton. Alternatively...
Series: DNAG, Centennial Field Guides
Published: 01 January 1988
DOI: 10.1130/0-8137-5404-6.99
EISBN: 9780813754109
... Abstract Zodletone Mountain, a 250-ft-high (76 m) eminence in Kiowa County, southern Oklahoma, constitutes the northernmost member of the Slick Hills Range and rises 1,649 ft (500 m) above sea level (SW¼SW¼ Sec.9, T.6N., R.14W. Saddle Mountain 15-minute Quadrangle, Oklahoma). The best approach...
Series: DNAG, Centennial Field Guides
Published: 01 January 1988
DOI: 10.1130/0-8137-5404-6.109
EISBN: 9780813754109
... Abstract The Wichita Mountains extend for about 65 mi (105 km) northwest from Lawton, Oklahoma (Fig. 1). Four sites are described here: 27—Quartz Mountain State Park in the western part of the Wichita Mountains, near Oklahoma 44A; 28—The Tom Steed Reservoir area, along U.S. 183 in the central...
Series: DNAG, Centennial Field Guides
Published: 01 January 1988
DOI: 10.1130/0-8137-5404-6.127
EISBN: 9780813754109
... Abstract Blue Creek Canyon is located approximately 15 mi (24 km) north-northwest of Lawton in southwestern Oklahoma (T.4N., R.13W.). Oklahoma 58 (Fig. 1) runs through the canyon. The area can be most easily reached from Lawton by taking the Medicine Park exit from the H. E. Bailey Turnpike...
Journal Article
Journal: AAPG Bulletin
Published: 01 April 1983
AAPG Bulletin (1983) 67 (4): vii.
... County in southwestern Oklahoma, on the northeast flank of the Wichita Mountains ( Fig. 1 , Table 1 ). The study area lies between two major structural features of Oklahoma: the Wichita Mountains on the south and the Anadarko basin on the north. The structural pattern of the rocks on the northeast flank...
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Journal Article
Journal: AAPG Bulletin
Published: 01 May 1982
AAPG Bulletin (1982) 66 (5): 542–543.
...Zuhair Al-Shaieb; R. A. Lilburn The Permian red beds at Cement and Chickasha oil fields in southwestern Oklahoma have undergone extensive and intensive alteration. This diagenetic mineralization is a direct expression of hydrocarbon migration along unconformity surfaces and fault zones...
Journal Article
Journal: AAPG Bulletin
Published: 01 August 1981
AAPG Bulletin (1981) 65 (8): 1495–1496.
..., the “Kupferschiefer-type” copper deposits in southwestern Oklahoma (Creta and Mangum) contain only up to 12 ppm U. In southwestern Oklahoma (Clinton 2 × 1° Quadrangle) carnotite and tyuyamunite occur in siltstones of the basal part of the Doxey formation. Although the origin of the mineralization is not entirely...
Journal Article
Journal: AAPG Bulletin
Published: 01 May 1981
AAPG Bulletin (1981) 65 (5): 903–904.
...Salman Bloch; Joseph A. Curiale; Janina R. Bloch ABSTRACT Pyrobitumen nodules from the northern flank of the Wichita Mountains, Kiowa County, Oklahoma, contain unusually high concentrations of uranium (2, 235 to 10, 112 ppm), while the thorium content is low (0.1 to 2.0 ppm). The nodules...
Journal Article
Published: 01 March 1980
Journal of Sedimentary Research (1980) 50 (1): 43–50.