Show simple item record

dc.contributor.advisorAlsleben, Helge
dc.contributor.authorReed, Amber Bibb,author.en_US
dc.date.accessioned2017-08-29T21:59:52Z
dc.date.available2017-08-29T21:59:52Z
dc.date.created2017en_US
dc.date.issued2017en_US
dc.identifieraleph-004597807en_US
dc.identifierUMI thesisen_US
dc.identifier.urihttps://repository.tcu.edu/handle/116099117/20535
dc.description.abstractThe 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.extent1 online resource (vii, 66 pages) :en_US
dc.format.mediumFormat: Onlineen_US
dc.relation.ispartofTCU Master Thesisen_US
dc.titleStructural geology of the Priddy fault block adjacent to the Muenster Arch in Cooke County, Texasen_US
dc.typeTexten_US
etd.degree.levelMaster
local.collegeCollege of Science and Engineering
local.departmentGeological Sciences
local.academicunitSchool of Geology, Energy and the Environment
dc.type.genreThesis
local.subjectareaGeological Sciences
etd.degree.nameMaster of Science


Files in this item

Thumbnail
This item appears in the following Collection(s)

Show simple item record