International audienceWe numerically investigate the supershear transition of inplane rupture under slip weakening friction and tectonic loading, using a non-smooth spectral element method. Nucleation of the rupture in the vicinity of an initial stress concentration is consistently solved together with the dynamic propagation. Nucleation is shown to influence the transition to the supershear propagation and, depending upon the initiation process and the level of the stress out of the nucleating asperity, crack-like or pulse-like solutions can be selected in the intersonic regime. Pulses are triggered by dynamic unloading of the traction ahead of the Rayleigh wave and tend to become metastable. The asymptotic numerical solution is always a c...
Abstract. We report on the experimental observation of the phenomenon of, spontaneously nucleated, s...
We report on the experimental observation of spontaneously nucleated supershear rupture and on the v...
Destructive large earthquakes occur as dynamic frictional ruptures along pre-existing interfaces (or...
International audienceWe numerically investigate the supershear transition of inplane rupture under ...
International audienceWe numerically investigate the supershear transition of inplane rupture under ...
We numerically investigate the supershear transition of inplane rupture under slip weakening fricti...
We numerically investigate the supershear transition of inplane rupture under slip weakening fricti...
We numerically investigate the supershear transition of inplane rupture under slip weakening fricti...
International audience[1] We numerically investigate the supershear transition of inplane rupture un...
International audience[1] We numerically investigate the supershear transition of inplane rupture un...
Understanding sub-Rayleigh-to-intersonic transition of mode II cracks is a fundamental problem in fr...
The introduction of the linear slip–weakening friction law permits the solution of the elasto–dynami...
Understanding sub-Rayleigh-to-intersonic transition of mode II cracks is a fundamental problem in fr...
During an earthquake, frictional rupture fronts mainly propagate at subshear speedalong tectonic fau...
Shear ruptures propagating along natural faults or simulated faults in analog laboratory experiments...
Abstract. We report on the experimental observation of the phenomenon of, spontaneously nucleated, s...
We report on the experimental observation of spontaneously nucleated supershear rupture and on the v...
Destructive large earthquakes occur as dynamic frictional ruptures along pre-existing interfaces (or...
International audienceWe numerically investigate the supershear transition of inplane rupture under ...
International audienceWe numerically investigate the supershear transition of inplane rupture under ...
We numerically investigate the supershear transition of inplane rupture under slip weakening fricti...
We numerically investigate the supershear transition of inplane rupture under slip weakening fricti...
We numerically investigate the supershear transition of inplane rupture under slip weakening fricti...
International audience[1] We numerically investigate the supershear transition of inplane rupture un...
International audience[1] We numerically investigate the supershear transition of inplane rupture un...
Understanding sub-Rayleigh-to-intersonic transition of mode II cracks is a fundamental problem in fr...
The introduction of the linear slip–weakening friction law permits the solution of the elasto–dynami...
Understanding sub-Rayleigh-to-intersonic transition of mode II cracks is a fundamental problem in fr...
During an earthquake, frictional rupture fronts mainly propagate at subshear speedalong tectonic fau...
Shear ruptures propagating along natural faults or simulated faults in analog laboratory experiments...
Abstract. We report on the experimental observation of the phenomenon of, spontaneously nucleated, s...
We report on the experimental observation of spontaneously nucleated supershear rupture and on the v...
Destructive large earthquakes occur as dynamic frictional ruptures along pre-existing interfaces (or...