Effect of rate dependence in shear heating of a fluid-saturated fault zone

Poromechanics III: Biot Centennial (1905-2005) - Proceedings of the 3rd Biot Conference on Poromechanics

Volumn , Issue , 2005, Pages 789-794

  Garagash, Dmitry I ^a   Schaeffer, David G ^b   Rudnicki, John W ^c  

^a CLARKSON UNIVERSITY   (United States)

^b DUKE UNIVERSITY   (United States)

^c NORTHWESTERN UNIVERSITY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

FRICTION; HEATING;

FRICTION LAWS; FRICTIONAL SLIP; NONUNIQUENESS; RATE DEPENDENCE; SIMPLE MODELING; SLIP-DEPENDENT FRICTION; STATE DEPENDENCE; STATE VARIABLES;

SHEAR FLOW;

EID: 33845577295     PISSN: None     EISSN: None     Source Type: Conference Proceeding    
DOI: 10.1201/noe0415380416.ch117     Document Type: Conference Paper

References (10)

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3. Garagash, D.I. & Rudnicki, J.W. 2003b. Shear Heating of a Fluid-Saturated Slip-Weakening Dilatant Fault Zone 2. Quasi-drained regime. Art. No 2472. J. Geoph. Res., 108(B10):1-20.
4. Jacques, L.M. & Rice, J.R. 2002. Partial melting and liquefaction of granular fault gouge during earthquake slip. EOS Trans. Amer. Geophys. Union, 83(47), Fall Meeting Supplement, Abstract T11F-07.
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8. Ruina, A. 1983. Slip Instability and State Variable Friction Laws. J. Geoph. Res., 88:10359-10370.
9. Segall, P. & Rice, J.R. 1995. Dilatancy, compaction, and slip instability of a fluid-infiltrated fault. J. Geoph. Res., 100:22155-22171.
10. Wibberley, C.A.J., Shimamoto, T. 2003. Internal structure and permeability of major strike-slip fault zones: the MedianTectonic Line in Mie Prefecture, Southwest Japan. J. Struct. Geology, 25(1):59-78.