dc.contributor.advisor | Cemen, Ibrahim | |
dc.contributor.author | Collins, Marline Renee | |
dc.date.accessioned | 2014-03-14T21:51:25Z | |
dc.date.available | 2014-03-14T21:51:25Z | |
dc.date.issued | 2006-05-01 | |
dc.identifier.uri | https://hdl.handle.net/11244/8022 | |
dc.description.abstract | This study was aimed at determining the structural geometry of the transitions zone between the Ouachita Mountains and the Arkoma Basin, and better understand the subsurface geometry of the triangle zone in the Wilburton and Damon Quadrangles, Arkoma Basin, Southeastern Oklahoma. Five structural cross-sections, two structural contour maps, two cumulative gas production maps, and a topographic map were constructed. From the study, it was determined that a duplex structure composed of three horses marked the structural geometry of the transition zone in the Wilburton and Damon Quadrangles. To the west of the study area, the south dipping Choctaw fault and the north dipping Carbon fault form a triangle zone. A lateral ramp causes an offset in the duplex structure, and a possible displacement of the triangle zone. | |
dc.format | application/pdf | |
dc.language | en_US | |
dc.publisher | Oklahoma State University | |
dc.rights | Copyright is held by the author who has granted the Oklahoma State University Library the non-exclusive right to share this material in its institutional repository. Contact Digital Library Services at lib-dls@okstate.edu or 405-744-9161 for the permission policy on the use, reproduction or distribution of this material. | |
dc.title | Geometry of Late Paleozoic Thrusting, Wilburton and Damon Quadrangles, Arkoma Basin, Southeast Oklahom | |
dc.type | text | |
dc.contributor.committeeMember | Paxton, Stan | |
dc.contributor.committeeMember | Puckette, Jim | |
osu.filename | Hepner_okstate_0664M_1852.pdf | |
osu.college | Arts and Sciences | |
osu.accesstype | Open Access | |
dc.description.department | Boone Pickens School of Geology | |
dc.type.genre | Thesis | |