In this paper, we show the impact of Thermo-Hydro Mechanical couplings (THM) on the stability of a saturated fault gouge under shear. By resorting to Cosserat continuum mechanics, that allows to take into account rotational degrees of freedom, we regularize the problem of localisation and we predict the thickness of a shear band. A linear stability analysis of the homogeneous state is performed and then the system of equations is integrated using a Finite Element (FE) analysis. These analyses can be used for studying the evolution of the thickness of the principal slip zone in a fault under undrained adiabatic shear. Good agreement is found between theoretical predictions and field observations
Abstract. Field and laboratory observations indicate that at seismic slip rates most shearing is con...
Accepted for publication in "Handbook of Nonlocal Continuum Mechanics for Materials and Structures",...
A lattice solid model was developed to study the physics of rocks and the nonlinear dynamics of eart...
A Thermo-Hydro-Mechanical (THM) model for Cosserat continua is developed to explore the influence of...
International audienceIn this paper, we study the phenomenon of localization of deformation in fault...
International audienceA Thermo-Hydro-Mechanical (THM) model for Cosserat continua is developed to ex...
When materials are subjected to large deformations, most of them experience inelastic deformations. ...
In this paper we study the impact of thermal pressurization and mineral decomposition reactions unde...
Les matériaux soumis à de grandes déformations présentes pour la plupart l’apparition de déformation...
International audienceA numerical model for thermo-hydro-mechanical strong couplings in an elasto-pl...
Strain localisation is a widespread phenomenon often observed in shear and compressive loading of ge...
Abstract. Field observations of major earthquake fault zones show that shear defor-mation is often c...
ABSTRACT Shear deformation of fault gouge or other particulate materials often results in observed s...
It is well known that strain localization during seismic slip occurs as the result of a plastic inst...
Shear deformation of fault gouge or other particulate materials often results in observed strain loc...
Abstract. Field and laboratory observations indicate that at seismic slip rates most shearing is con...
Accepted for publication in "Handbook of Nonlocal Continuum Mechanics for Materials and Structures",...
A lattice solid model was developed to study the physics of rocks and the nonlinear dynamics of eart...
A Thermo-Hydro-Mechanical (THM) model for Cosserat continua is developed to explore the influence of...
International audienceIn this paper, we study the phenomenon of localization of deformation in fault...
International audienceA Thermo-Hydro-Mechanical (THM) model for Cosserat continua is developed to ex...
When materials are subjected to large deformations, most of them experience inelastic deformations. ...
In this paper we study the impact of thermal pressurization and mineral decomposition reactions unde...
Les matériaux soumis à de grandes déformations présentes pour la plupart l’apparition de déformation...
International audienceA numerical model for thermo-hydro-mechanical strong couplings in an elasto-pl...
Strain localisation is a widespread phenomenon often observed in shear and compressive loading of ge...
Abstract. Field observations of major earthquake fault zones show that shear defor-mation is often c...
ABSTRACT Shear deformation of fault gouge or other particulate materials often results in observed s...
It is well known that strain localization during seismic slip occurs as the result of a plastic inst...
Shear deformation of fault gouge or other particulate materials often results in observed strain loc...
Abstract. Field and laboratory observations indicate that at seismic slip rates most shearing is con...
Accepted for publication in "Handbook of Nonlocal Continuum Mechanics for Materials and Structures",...
A lattice solid model was developed to study the physics of rocks and the nonlinear dynamics of eart...