Anadarko Basin
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Chapter 11 Tectonic and Structural Evolution of the Anadarko Basin and Structural
Chapter 11 Tectonic and Structural Evolution of the Anadarko Basin and Structural Click here to return to Interpretation and Modeling of a Composite Volume Title Page Regional 2D Seismic Line By Ofori N. Pearson and John J. Miller Chapter 11 of 13 Petroleum Systems and Assessment of Undiscovered Oil and Gas in the Anadarko Basin Province, Colorado, Kansas, Oklahoma, and Texas—USGS Province 58 Compiled by Debra K. Higley U.S. Geological Survey Digital Data Series DDS–69–EE U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior SALLY JEWELL, Secretary U.S. Geological Survey Suzette M. Kimball, Acting Director U.S. Geological Survey, Reston, Virginia: 2014 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment, visit http://www.usgs.gov or call 1–888–ASK–USGS. For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this information product, for the most part, is in the public domain, it also may contain copyrighted materials as noted in the text. Permission to reproduce copyrighted items must be secured from the copyright owner. Suggested citation: Pearson, O.N., and Miller, J.J., 2014, Tectonic and structural evolution of the Anadardo Basin and structural inter- pretation and modeling of a composite regional two-dimensional seismic line, chap. -
Structure and Tectonics of the Palo Duro Basin: Meeting with Doe and Their Contractors
#WWwiyfr(tio6 MRIUnapp WMGT r/f PSJustus 15 1986NMSS nEMliegel JAN 15 198R EBrowning JTrapp & rE STRUCTURE TRIP REPORT Mell RIII.ee HMiller Albrahim -- 1 T~Werma FRoss MEMORANDUM FOR: Malcolm Knapp, Chief iLinehan, WMRP JGreeves WMGT RJohnson MWokar JKennedy Jpearring FROM: John Trapp, Richard Lee, AboduM PV brahim, PDR and Fred Ross, WMGT SUBJECT: TRIP REPORT - STRUCTURE AND TECTONICS OF THE PALO DURO BASIN: MEETING WITH DOE AND THEIR CONTRACTORS On November 19-21, 1985, members of WMGT staff and their technical assistance contractors met with DOE and their contractors at the Parke University Motel in Columbus, Ohio to discuss the geologic structure of the Palo Duro Basin, Texas. The purpose of the meeting was to examine the existing data that serves as the basis for interpretations of structural features In the Palo Duro Basin as presented in DOE contractor reports. The emphasis of the meeting was to evaluate the structural configuration and tectonic history of the basin. Principle meeting objectives were to determine the availability of data for structural interpretations, the differences in published interpretations, the significance of these differing interpretations, and methods for resolving these differences. Enclosed are copies of the list of meeting attendees (Enclosure 1), the meeting agenda (Enclosure 2), the signed meeting summary (Enclosure 3), and copies of all presentation materials (Enclosure 4). Since these enclosures are quite extensive, they have only been provided to Mr. Browninq and the DCC. Additional copies are available in the offices of Robert Johnson and John Trapp. John rapp, WMGT Richard Lee, WMGT 8606160002 860115 Abou-e4krIbrahim, WMGT PDR WASTE PD rdR ,Wmt T-"' Fred bnID ocketkkNo.__ PDR a _ Enclosures: LPDR Ad _ As Stated Distribution _ _ _ (Returnto WM 623SS) 'C :WMGT :WMGT :WMGT ,ME :tlTrapp;mt :RLee :Albrahim :FRoss TE :861011 17 :861011/ :86/01/ /4- :86/01/ ::: * * . -
University of Nevada Reno Late Quaternary Tectonic Activity of The
University of Nevada Reno Late Quaternary Tectonic Activity of the Meers Fault, Southwest Oklahoma A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science m Geology. by Alan Ray Ramelli April 1988 The thesis of Alan Ray Ramelli is approved. April 1988 ii ABSTRACT The Meers fault in southwestern Oklahoma is an active fault capable of producing large, damaging earthquakes. The most recent large event is late Holocene, occurring some 1,200 - 1,300 years ago, and it was preceded by one or more earlier Quaternary events. Few faults in stable continental interior (SCI) areas are known to be active, so this fault holds many implications for seismic hazards in these poorly understood regions. Paleoseismic events probably had magnitudes of at least 6 3/4 to 7 1/4. Seismic events may be relatively larger in SCI regions and magnitudes of 7 1/2 or greater may be possible. The minimum scarp length is 37 km. Displacements have both left-lateral and high-angle reverse components. Vertical separation of the surface reaches about 5 m, while lateral separation exceeds vertical by a ratio of about 3:1 to 5:1, reaching approximately 20 m. Individual events appear to have had maximum surface displacements of several meters. This fault may be part of a larger active zone. The Washita Valley and Potter County faults also have surface expressions believed to indicate recent surface faulting. No additional active surface faults have been recognized in the Meers fault area, but activity may be concealed by poor preservation or non-brittle surface deformation. -
General Disclaimer One Or More of the Following Statements May Affect
General Disclaimer One or more of the Following Statements may affect this Document This document has been reproduced from the best copy furnished by the organizational source. It is being released in the interest of making available as much information as possible. This document may contain data, which exceeds the sheet parameters. It was furnished in this condition by the organizational source and is the best copy available. This document may contain tone-on-tone or color graphs, charts and/or pictures, which have been reproduced in black and white. This document is paginated as submitted by the original source. Portions of this document are not fully legible due to the historical nature of some of the material. However, it is the best reproduction available from the original submission. Produced by the NASA Center for Aerospace Information (CASI) Post-Carboniferous Tectonics in the Anadarko Basin, Oklahoma: Evidence from Side-Looking Radar Imagery K. C. Nielsen and R. J. Stern (NASA-CH-1754 5 8) FOST•-CARECIIIFERCUS NE5-1fi498 TECTONICS IN 4Nn ANADARKO EASIN, CKLABCNA: EVIDENCE FROM SIDE — LOCKING SAIAR IMAGERY (Texas Univ.) 18 p NC A02/MF A01 CSCL 17I Unclas G3/43 14305 UTD Contribution No. 471 Programs in Geosciences The University of Texas at Dallas P. 0. Box 830688 Richardson, Texas 75083-0688 This report was prepared for the Jet Pro ,)ulsion, Laboratory, California Institute of Technology, sponsored by the National Aeronautics and Space Administration. SM 1 ABSTRACT The Anadarko Basin is a WNW-ESE elongated trough filled with 10+ km of Paleozoic sediments. Most models call for tectonic activity to end in Pennsylvanian times. -
Anadarko Basin
December 2014 Bibliography of Oklahoma Anadarko Basin Brian J. Cardott Oklahoma Geological Survey Adler, F.J., 1971, Anadarko Basin and central Oklahoma area, in Future petroleum provinces of the United States—their geology and potential: AAPG Memoir 15, v. 2, p. 1061-1070. Agena, W.F., M.W. Lee, and J.A. Grow, 1989, Reprocessing of the COCORP data recorded across the Wichita Uplift and the Anadarko Basin in southern Oklahoma: U.S. Geological Survey Open File Report OF-89-0357, 20 p. Ali, F.M., 2008, A subsurface study of the Lower Red Fork sandstone in the deeper part of the Anadarko Basin in Caddo and Washita counties, Oklahoma: Norman, Oklahoma, University of Oklahoma, unpublished M.S. thesis. Al-Shaieb, Z., and P. Walker, 1986, Evolution of secondary porosity in Pennsylvanian Morrow Sandstones, Anadarko Basin, Oklahoma, in C.W. Spencer and R.F. Mast, eds., Geology of tight gas reservoirs: AAPG Studies in Geology 24, p. 45- 67. Al-Shaieb, Z., 1988, Hydrocarbon-induced diagenetic aureole at Cement-Chickasha Anticline, Oklahoma, in O.T. Hayward, ed., South-Central Section of the Geological Society of America: GSA, Centennial Field Guide v. 4,, p. 103-108. Al-Shaieb, Z., J.W. Shelton, and J.O. Puckette, 1989, Sandstone reservoirs of the Mid- Continent: Oklahoma City Geological Society, syllabus for short course, 125 p. Al-Shaieb, Z., 1991, Compartmentation, fluid pressure important in Anadarko exploration: Oil & Gas Journal, v. 89, no. 27, p. 52-56. Al-Shaieb, Z., J. Puckette, P. Ely, and V. Tigert, 1992, Pressure compartments and seals in the Anadarko Basin, in K.S. -
What Lies Beneath
Newspapers for this educational program provided by: WHAT LIES BENEATH OKLAHOMA ROCKS! Welcome 2014 I hope you will enjoy reading this publication that will focus on Oklahoma’s geologic past and what lies beneath what we see on the surface! This state’s rich geologic history spans some 1.6 billion years, and has provided us with the great variety of geography and scenery we see today: The high mesas, caves, and red rocks of the northwest; the Wichita and Arbuckle Mountains and Turner Falls of the south and southwest; the beautiful Ouachita mountains and forests of the southeast; and the rolling plains and Ozark hills of the north and northeast. Few other states, and certainly none our size, can boast of going from cypress swamps to high mesas! Beneath what is now Oklahoma, continents once came together then broke apart; land masses moved and collided; shallow seas came and went; rocks were folded, faulted, uplifted and eroded and great changes (sometimes rapidly in geologic time, and seemingly forever in human years) came about. These movements formed the Anadarko basin (now filled in), that at one time was deeper than the Marianas Trench, which is today’s deepest ocean feature and is more than 7 miles deep. Some of the ancient rock masses that were tilted, faulted, and folded can now be seen at the surface in the Arbuckle Mountains. The I-35 road cuts through these mountains make it possible to see dramatic evidence of these geologic movements as we travel that stretch of road. These now visible features are so unique that geologists from around the world have stopped to get a look.