Thermo-hydro-mechanical loading

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Fault friction for different values of coseismic slip and coseismic slip velocity.
Fault friction, Pressure and Temperature after the completion of coseismic slip.
On the left: Frictional response of the fault gouge under shear for large displacements.
In th middle: Traveling of strain localization inside the fault gouge.
On the right: Profiles of the pore fluid pressure and temperature.
Fault friction during initial stages of coseismic slip for different values of the shear velocity $\dot{\delta}$.

Temperature ∆T and pore fluid pressure ∆P fields along the height of the layer for a bounded fault gouge – traveling strain localization.

Temperature ∆T and pore fluid pressure ∆P fields along the height of the layer for a bounded fault gouge – stationary strain localization.

Temperature ∆T and pore fluid pressure ∆P fields along the height of the layer for an unbounded fault gouge – traveling strain localization.

Temperature ∆T and pore fluid pressure ∆P fields along the height of the layer for an unbounded fault gouge – stationary strain localization.

Other topics of « Complex multi-physics stresses »

Hydro-mechanical loading
Instabilities in granular materials

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