dc.contributor.advisor | Denne, Richard | |
dc.contributor.author | Patterson, Samantha A.,author. | en_US |
dc.date.accessioned | 2018-12-19T19:51:06Z | |
dc.date.available | 2018-12-19T19:51:06Z | |
dc.date.created | 2018 | en_US |
dc.date.issued | 2018 | en_US |
dc.identifier | aleph-005058762 | en_US |
dc.identifier | UMI thesis | en_US |
dc.identifier.uri | https://repository.tcu.edu/handle/116099117/22839 | |
dc.description.abstract | The 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.extent | 1 online resource (vi, 161 pages) : | en_US |
dc.format.medium | Format: Online | en_US |
dc.relation.ispartof | TCU Master Thesis | en_US |
dc.title | The Maness Shale: a comparison of the geomechanical and mineralogical properties within the Lower Eagle Ford Formation, South 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 | Department of Geology | |
dc.type.genre | Thesis | |
local.subjectarea | Geological Sciences | |
etd.degree.name | Master of Science | |