Finite element modeling of thrust faulting

dc.contributor.advisorDe Bremaecker, Jean-Claudeen_US
dc.creatorVague, Glen Edward, Jren_US
dc.date.accessioned2009-06-04T00:35:32Zen_US
dc.date.available2009-06-04T00:35:32Zen_US
dc.date.issued1992en_US
dc.description.abstractFinite Element modeling of thrust faulting shows that the faults will propagate upward at very low angles from the leading edge of a regional horizontal decollement surface located at various depths in a homogeneous block of crustal material. The angles are consistent with Mode II crack propagation in Linear Elastic Fracture Mechanics and the relationship of stress trajectory and failure in the classic theory of shear fracture. Shallow faults will propagate at a steeper angle than deeper ones. The coefficient of friction does not affect the fault angle, though it probably affects the likelihood of Mode II deformation.en_US
dc.format.extent138 p.en_US
dc.format.mimetypeapplication/pdfen_US
dc.identifier.callnoThesis Geol. 1992 Vagueen_US
dc.identifier.citationVague, Glen Edward, Jr. "Finite element modeling of thrust faulting." (1992) Master’s Thesis, Rice University. <a href="https://hdl.handle.net/1911/13640">https://hdl.handle.net/1911/13640</a>.en_US
dc.identifier.urihttps://hdl.handle.net/1911/13640en_US
dc.language.isoengen_US
dc.rightsCopyright is held by the author, unless otherwise indicated. Permission to reuse, publish, or reproduce the work beyond the bounds of fair use or other exemptions to copyright law must be obtained from the copyright holder.en_US
dc.subjectGeophysicsen_US
dc.subjectGeologyen_US
dc.titleFinite element modeling of thrust faultingen_US
dc.typeThesisen_US
dc.type.materialTexten_US
thesis.degree.departmentEarth Scienceen_US
thesis.degree.disciplineNatural Sciencesen_US
thesis.degree.grantorRice Universityen_US
thesis.degree.levelMastersen_US
thesis.degree.nameMaster of Artsen_US
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