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dc.contributor.advisorDenne, Richard
dc.contributor.authorPatterson, Samantha A.,author.en_US
dc.date.accessioned2018-12-19T19:51:06Z
dc.date.available2018-12-19T19:51:06Z
dc.date.created2018en_US
dc.date.issued2018en_US
dc.identifieraleph-005058762en_US
dc.identifierUMI thesisen_US
dc.identifier.urihttps://repository.tcu.edu/handle/116099117/22839
dc.description.abstractThe Maness Shale is a clay-rich mudrock that has been correlated to the basal Lower Eagle Ford in South Texas. Where present, the Maness may prove beneficial, acting as a fracture barrier between hydraulically fractured Eagle Ford wellbores and underlying aquifers. Geomechanical studies demonstrate that the Maness is 34% weaker than the Eagle Ford and 76% weaker than the Buda. XRD analyses found that the samples from the Maness contain an average of 10% more clay than the Eagle Ford. A regression analysis established a 91.7% correlation between Maness thickness and oil/water ratios, which are based on cumulative first year oil and water production, indicating that the Maness may be acting as a fracture barrier in the region. This analysis also found a 50% decrease in oil/water ratios between Maness thicknesses of 5 to 10 ft (1.5 to 3.1 m), suggesting that a minimum of 10 ft is needed for the Maness to effectively act as a fracture barrier.en_US
dc.format.extent1 online resource (vi, 161 pages) :en_US
dc.format.mediumFormat: Onlineen_US
dc.relation.ispartofTCU Master Thesisen_US
dc.titleThe Maness Shale: a comparison of the geomechanical and mineralogical properties within the Lower Eagle Ford Formation, South Texasen_US
dc.typeTexten_US
etd.degree.levelMaster
local.collegeCollege of Science and Engineering
local.departmentGeological Sciences
local.academicunitDepartment of Geology
dc.type.genreThesis
local.subjectareaGeological Sciences
etd.degree.nameMaster of Science


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