Structural diagenetic attributes of the late Cretaceous Williams fork sandstones with implications for petrophysical interpretation and fracture prediction, Piceance Basin, Colorado

dc.contributor.advisorLaubach, Stephen E. (Stephen Ernest), 1955-en
dc.contributor.advisorMilliken, K. L.en
dc.contributor.committeeMemberHorton, Brianen
dc.contributor.committeeMemberSteel, Ronen
dc.contributor.committeeMemberTinker, Scotten
dc.contributor.committeeMemberBonnell, Lindaen
dc.creatorOzkan, Aysen, 1974-en
dc.date.accessioned2010-09-17T18:18:58Zen
dc.date.accessioned2010-09-17T18:19:14Zen
dc.date.accessioned2017-05-11T22:20:13Z
dc.date.available2010-09-17T18:18:58Zen
dc.date.available2010-09-17T18:19:14Zen
dc.date.available2017-05-11T22:20:13Z
dc.date.issued2010-05en
dc.date.submittedMay 2010en
dc.date.updated2010-09-17T18:19:14Zen
dc.descriptiontexten
dc.description.abstractDiagenetic and structural aspects of tight gas sandstones must be addressed concurrently in order to fully understand low-permeability sandstones and to better predict their reservoir quality attributes that arise from a combination of pore-scale and fracture distribution characteristics. This dissertation focuses on aspects of rock evolution that are germane to concurrent structural and diagenetic evolution, such as loading and thermal history, rock mechanical property evolution, and fracture timing. I tested the hypothesis that the cement precipitation step, governed by thermal exposure and grain surface attributes, governs how sandstone attributes evolve using observations from the Late Cretaceous Williams Fork sandstones from the Piceance Basin, Colorado. My research shows that essential information for predicting and understanding fracture patterns in sandstone can be obtained by unraveling cement precipitation (diagenetic) history. Fractures depend on the mechanical properties existing during fracture growth. I show that key rock mechanical properties (subcritical crack index, Young's modulus and Poisson's ratio), petrophysical behavior, and reservoir quality depend in a systematic way on time-temperature history and the intrinsic grain surface attributes of these sandstones. I classified the Williams Fork lithofacies petrographically and correlated those with log responses to create a model that can be used to predict reservoir quality and diagenesis directly from well logs. I determined rock mechanical characteristics by measuring the subcritical crack index (SCI), a mechanical property that influences fracture distribution characteristics, and by examining log-derived bulk mechanical properties. To quantify the influence of quartz cementation on the SCI and to determine the range of SCI values for sandstone of given framework composition at different diagenetic stages, I measured SCI on Williams Fork core samples and their outcrop equivalents. Diagenetic modeling is applied to determine the sandstone characteristics during fracturing.en
dc.description.departmentGeological Sciencesen
dc.format.mimetypeapplication/pdfen
dc.identifier.urihttp://hdl.handle.net/2152/ETD-UT-2010-05-767en
dc.language.isoengen
dc.subjectSandstonesen
dc.subjectLate Cretaceous sandstonesen
dc.subjectWilliams Fork sandstonesen
dc.subjectDiagenetic attributesen
dc.subjectStructural evolutionen
dc.subjectDiagenetic evolutionen
dc.subjectRock evolutionen
dc.subjectPiceance Basin, Coloradoen
dc.subjectThermal historyen
dc.subjectRock mechanical propertiesen
dc.subjectFracturesen
dc.titleStructural diagenetic attributes of the late Cretaceous Williams fork sandstones with implications for petrophysical interpretation and fracture prediction, Piceance Basin, Coloradoen
dc.type.genrethesisen

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