The Development of Porosity in the Upper Cretaceous Austin Chalk Group of Texas

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dc.contributor.advisorGodet, Alexis
dc.contributor.authorBernardo, Miguel
dc.contributor.committeeMemberGodet, Alexis
dc.contributor.committeeMemberLambert, Lance
dc.contributor.committeeMemberGray, Walter
dc.date.accessioned2024-02-09T19:29:32Z
dc.date.available2024-02-09T19:29:32Z
dc.date.issued2020
dc.descriptionThis item is available only to currently enrolled UTSA students, faculty or staff. To download, navigate to Log In in the top right-hand corner of this screen, then select Log in with my UTSA ID.
dc.description.abstractThe Austin Chalk Group is an upper Cretaceous carbonate succession in Texas that results from the deposition of sediment along a carbonate ramp. Shallower marine deposits are enriched in benthic organisms, and deeper water facies are characterized by the presence of calcareous plankton and the high amount of micrite. Previous works show that the original mineralogy of the Austin Chalk Group controls its early compactional history and is responsible, at least in part, for its diagenetic history and the evolution of its porosity. This study aims to assess the relationship between depositional facies and differential diagenetic pathways within the upper Cretaceous Austin Chalk Group to constrain the parameters that favored the formation of porosity. Outcrops at Del Rio, San Antonio, and Dallas are analyzed for their depositional setting, diagenesis, microtexture, and porosity. This research tests the hypothesis that different facies environments and different burial depth across the study area controlled the development of porosity. The petrographic analysis of rock slabs and thin sections allows the description of fossil content, depositional texture, and matrix to inform on ecological changes and are interpreted as changes in sea level within the Austin Chalk Group. Cathodoluminescence microscopy helps constrain the chronology of diagenetic events that promoted or hampered the formation of porosity. Scanning electron microscopy is used to assess the microtexture and to measure pore throat diameters. Finally, porosity values are obtained for each sample by calculating the volume displacement and difference between dry and water-saturated weight. Porosity and pore throat values are compared to facies and microtextures to further understand the evolution of porosity. This research concludes that the highest porosity values are found in the Dallas area due to a shallower depositional setting and less influence of burial diagenesis compared to San Antonio and Del Rio, where the lowest porosity values are measured. As a result, this study helps exploration efforts that focus on chalk series deposited above basement or salt-related topographic highs to identify intervals with better reservoir properties.
dc.description.departmentGeosciences
dc.format.extent84 pages
dc.format.mimetypeapplication/pdf
dc.identifier.isbn9798557049924
dc.identifier.urihttps://hdl.handle.net/20.500.12588/2966
dc.languageen
dc.subjectCathodoluminescence
dc.subjectFacies
dc.subjectMicro-pores
dc.subjectMicrotexture
dc.subjectPaleobathymetry
dc.subjectPorosity
dc.subject.classificationGeology
dc.subject.classificationGeophysics
dc.subject.classificationSedimentary geology
dc.titleThe Development of Porosity in the Upper Cretaceous Austin Chalk Group of Texas
dc.typeThesis
dc.type.dcmiText
dcterms.accessRightspq_closed
thesis.degree.departmentGeosciences
thesis.degree.grantorUniversity of Texas at San Antonio
thesis.degree.levelMasters
thesis.degree.nameMaster of Science

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