International audienceSUMMARY Seismicity rate is sometimes observed to correlate with periodic stress oscillations, such as seasonal changes in hydrological loads, or solid-earth and oceanic tidal stresses. However, seismicity modulation is far from being systematic, often weak and the mechanical control is not yet fully understood. Here, a 3-D interacting fault population loaded by a periodic stress has been studied. For that a new earthquake simulator coupling rate-and-state friction and 3-D quasi-dynamic elasticity has been developed, and used to explore the mechanical conditions leading to seismicity modulation. It is first shown that seismicity modulation is maximized when the amplitude of periodic loading stress approaches aσ, a being...
International audienceWe describe a simple model that links static stress (Coulomb) modeling to the ...
International audienceCalculations of Coulomb stress changes have shown that moderate to large earth...
The stability state of fault systems is mainly controlled by the frictional properties of weak inter...
A number of outstanding questions in earthquake physics revolve around under-standing the relationsh...
[1] We perform a numerical experiment with quasi-dynamic continuous 3D fault model governed by a lab...
In this paper, we present a model for studying aftershock sequences that integrates Coulomb static s...
International audienceWe study the consequences of temporal stress perturbations on earthquake nucle...
International audienceThe paucity of detectable seismicity shadows in the days/months following a ma...
[1] The balance of forces implies stress transfers during the seismic cycle between the elastobrittl...
International audienceThe influence of normal and shear stress static perturbations on a strike-slip...
Abstract: We study fault interaction by modeling the spatial and temporal pattern of seismicity thro...
We model the spatial and temporal pattern of seismicity during a sequence of moderate-magnitude norm...
We compute the static displacement, stress, strain and the Coulomb failure stress produced in an ela...
Dynamic simulations of rupture propagation and multiple earthquake cycles for varying fault geometri...
International audienceWe describe a simple model that links static stress (Coulomb) modeling to the ...
International audienceCalculations of Coulomb stress changes have shown that moderate to large earth...
The stability state of fault systems is mainly controlled by the frictional properties of weak inter...
A number of outstanding questions in earthquake physics revolve around under-standing the relationsh...
[1] We perform a numerical experiment with quasi-dynamic continuous 3D fault model governed by a lab...
In this paper, we present a model for studying aftershock sequences that integrates Coulomb static s...
International audienceWe study the consequences of temporal stress perturbations on earthquake nucle...
International audienceThe paucity of detectable seismicity shadows in the days/months following a ma...
[1] The balance of forces implies stress transfers during the seismic cycle between the elastobrittl...
International audienceThe influence of normal and shear stress static perturbations on a strike-slip...
Abstract: We study fault interaction by modeling the spatial and temporal pattern of seismicity thro...
We model the spatial and temporal pattern of seismicity during a sequence of moderate-magnitude norm...
We compute the static displacement, stress, strain and the Coulomb failure stress produced in an ela...
Dynamic simulations of rupture propagation and multiple earthquake cycles for varying fault geometri...
International audienceWe describe a simple model that links static stress (Coulomb) modeling to the ...
International audienceCalculations of Coulomb stress changes have shown that moderate to large earth...
The stability state of fault systems is mainly controlled by the frictional properties of weak inter...