dc.contributor.advisor | Alsleben, Helge | |
dc.contributor.author | Reed, Amber Bibb,author. | en_US |
dc.date.accessioned | 2017-08-29T21:59:52Z | |
dc.date.available | 2017-08-29T21:59:52Z | |
dc.date.created | 2017 | en_US |
dc.date.issued | 2017 | en_US |
dc.identifier | aleph-004597807 | en_US |
dc.identifier | UMI thesis | en_US |
dc.identifier.uri | https://repository.tcu.edu/handle/116099117/20535 | |
dc.description.abstract | The Barnett Shale and overlying units adjacent to the Muenster Arch in Cooke County, Texas, are significantly deformed. Well log and dipmeter data indicate that a west-directed reverse fault system folded and faulted the Barnett Shale and possibly Marble Falls units, and brought in rock of unknown origin. Observations indicate an additional, south-directed faulting event led to offset between wells. These features are likely related to the Late Mississippian through Late Pennsylvanian reactivation of the basement-cored faults of the Muenster Arch. | en_US |
dc.format.extent | 1 online resource (vii, 66 pages) : | en_US |
dc.format.medium | Format: Online | en_US |
dc.relation.ispartof | TCU Master Thesis | en_US |
dc.title | Structural geology of the Priddy fault block adjacent to the Muenster Arch in Cooke County, Texas | en_US |
dc.type | Text | en_US |
etd.degree.level | Master | |
local.college | College of Science and Engineering | |
local.department | Geological Sciences | |
local.academicunit | School of Geology, Energy and the Environment | |
dc.type.genre | Thesis | |
local.subjectarea | Geological Sciences | |
etd.degree.name | Master of Science | |