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Coupled thermo-hydro-mechanical processes in fault zones during rapid slip
Sulem J.
Dans Rock Mechanics in Civil and Environmental Engineering, EUROCK 2010 - Rock Mechanics in Civil and Environmental Engineering, EUROCK 2010, Lausanne : Suisse (2010) - http://hal.archives-ouvertes.fr/hal-00562457
Invited conference talk
Physics/Mechanics/Mechanics of the solides
Engineering Sciences/Mechanics/Mechanics of the solides
Coupled thermo-hydro-mechanical processes in fault zones during rapid slip
Jean Sulem () 1
1:  Laboratoire Navier
Ecole des Ponts ParisTech – CNRS : UMR8205 – IFSTTAR
Ecole des Ponts ParisTech 6 / 8 avenue Blaise Pascal 77455 CHAMPS SUR MARNE
France
Géotechnique
The physical processes which occur during an earthquake exhibit several coupled phenomena as large variations of stress, pore pressure and temperature take place in the slip zone. Thermo-poro-mechanical couplings due to shear heating can be associated to phase transition such as vaporization of the pore fluid, melting of fault gouge and to chemical effects such as dehydration of minerals or decarbonation of calcite. Different competing effects may influence dynamic slip and affect the weakening of the shear stress. In this paper, we show how thermal pressurization of the pore fluid and thermal decomposition of minerals induced by shear heating limit the co-seismic temperature rise which may explain the lack of pronounced heat outflow, and the lack of shallow frictional melting, along major tectonic faults.
English

Rock Mechanics in Civil and Environmental Engineering, EUROCK 2010
international
2010
15-25
CRC Press
J. SZhao, V. Labiouse, J.-P. Dudt, J.-F. Mathier

Rock Mechanics in Civil and Environmental Engineering, EUROCK 2010
2010-06-15
2010-06-18
Lausanne
Switzerland

seismic slip – fault weakening – multi-physics couplings

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