Integrating complementarity into the 2D displacement discontinuity boundary element method to model faults and fractures with frictional contact properties-Reference-Cited by-同舟云学术

Integrating complementarity into the 2D displacement discontinuity boundary element method to model faults and fractures with frictional contact properties

Published:2012-08 Issue: Volume:45 Page:304-312
ISSN:0098-3004
Container-title:Computers & Geosciences
language:en
Short-container-title:Computers & Geosciences

Author:

Ritz Elizabeth,Mutlu Ovunc,Pollard David D.

Funder

DOE Basic Energy Sciences

Publisher

Elsevier BV

Subject

Computers in Earth Sciences,Information Systems

Reference59 articles.

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3. Slip distributions on faults: effects of stress gradients, inelastic deformation, heterogeneous host-rock stiffness, and fault interaction;Bürgmann;Journal of Structural Geology,1994

4. Friction of rocks;Byerlee;Pure and Applied Geophysics,1978

5. Frictional characteristics of granite under high confining pressure;Byerlee;Journal of Geophysical Research,1967

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