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      Interplay of gouge, fluid pressure and porosity in fault zones

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      Author(s)
      Tuncay, K.
      Ozkan, G.
      Ortoleva, P.
      Date
      2003-05
      Source Title
      Journal of Geochemical Exploration
      Print ISSN
      0375-6742
      Publisher
      Elsevier
      Volume
      78-79
      Pages
      191 - 195
      Language
      English
      Type
      Article
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      Abstract
      The 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.
      Keywords
      Faults
      Fluid Pressure
      Gouge
      Rheology
      Permalink
      http://hdl.handle.net/11693/11316
      Published Version (Please cite this version)
      http://dx.doi.org/10.1016/S0375-6742(03)00104-3
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      • Department of Mathematics 688
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