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dc.contributor.authorTuncay, K.en_US
dc.contributor.authorOzkan, G.en_US
dc.contributor.authorOrtoleva, P.en_US
dc.date.accessioned2015-07-28T11:57:22Z
dc.date.available2015-07-28T11:57:22Z
dc.date.issued2003-05en_US
dc.identifier.issn0375-6742
dc.identifier.urihttp://hdl.handle.net/11693/11316
dc.description.abstractThe objective of this study is to demonstrate how fault dynamics may naturally be placed in the context of incremental stress theory, rock textural evolution modeling and standard conservation laws. Casting the fault dynamics problem in this framework naturally introduces rock memory for failure, fluid pressure effects and the autonomous nature of fault evolution. Poroelasticity, nonlinear viscosity and gouge are combined in an incremental stress rheology approach to examine the effect of changes in particle size distribution on fluid pressure in fault zones. © 2003 Elsevier Science B.V. All rights reserved.en_US
dc.language.isoEnglishen_US
dc.source.titleJournal of Geochemical Explorationen_US
dc.relation.isversionofhttp://dx.doi.org/10.1016/S0375-6742(03)00104-3en_US
dc.subjectFaultsen_US
dc.subjectFluid Pressureen_US
dc.subjectGougeen_US
dc.subjectRheologyen_US
dc.titleInterplay of gouge, fluid pressure and porosity in fault zonesen_US
dc.typeArticleen_US
dc.departmentDepartment of Mathematicsen_US
dc.citation.spage191en_US
dc.citation.epage195en_US
dc.citation.volumeNumber78-79en_US
dc.identifier.doi10.1016/S0375-6742(03)00104-3en_US
dc.publisherElsevieren_US


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