We investigate significant heterogeneous stresses along bimaterial interfaces in laboratory and numerical experiments. These stresses, partially induced by model or experimental configuration, affect the supershear transition length and rupture speed, mode and directivity in uniaxial compression tests and dynamic rupture experiments with bimaterial interfaces. Using numerical simulations we show that normal and tangential stresses at the fault are distorted by the different stress-strain relationships of the materials. This distortion leads to altered supershear transition lengths, higher rupture potencies and amplifies the preference for rupture in the direction of slip of the slower and more compliant material. We demonstrate how this str...
Geological and geophysical observations reveal along‐strike fault zone heterogeneity on major strike...
The transition from sub-Rayleigh to supershear propagation of mode II cracks is a fundamental proble...
Shear ruptures propagating along natural faults or simulated faults in analog laboratory experiments...
Numerical modelling of dynamic rupture is conducted along faults separating similar and dissimilar m...
We study in-plane ruptures on a bimaterial fault governed by a velocity-weakening friction with a re...
[1] Seismic inversions show that earthquake risetimes may be much shorter than the overall rupture d...
Seismic inversions show that earthquake risetimes may be much shorter than the overall rupture durat...
To better understand the asymmetric distribution of microearthquake aftershocks along the central Sa...
Theoretical studies have shown that the issue of rupture modes has important implications for fault ...
During an earthquake, frictional rupture fronts mainly propagate at subshear speedalong tectonic fau...
Although kinematic earthquake source inversions show dominantly pulse-like subshear rupture behavior...
The goal in designing dynamic frictional experiments simulating earthquake rupture has been to creat...
Earthquake ruptures are modeled as dynamically propagating shear cracks with the aim of gaining insi...
[1] Earthquake ruptures are modeled as dynamically propagating shear cracks with the aim of gaining ...
UnrestrictedThis thesis examines dynamic ruptures along frictional interfaces and seismic radiation ...
Geological and geophysical observations reveal along‐strike fault zone heterogeneity on major strike...
The transition from sub-Rayleigh to supershear propagation of mode II cracks is a fundamental proble...
Shear ruptures propagating along natural faults or simulated faults in analog laboratory experiments...
Numerical modelling of dynamic rupture is conducted along faults separating similar and dissimilar m...
We study in-plane ruptures on a bimaterial fault governed by a velocity-weakening friction with a re...
[1] Seismic inversions show that earthquake risetimes may be much shorter than the overall rupture d...
Seismic inversions show that earthquake risetimes may be much shorter than the overall rupture durat...
To better understand the asymmetric distribution of microearthquake aftershocks along the central Sa...
Theoretical studies have shown that the issue of rupture modes has important implications for fault ...
During an earthquake, frictional rupture fronts mainly propagate at subshear speedalong tectonic fau...
Although kinematic earthquake source inversions show dominantly pulse-like subshear rupture behavior...
The goal in designing dynamic frictional experiments simulating earthquake rupture has been to creat...
Earthquake ruptures are modeled as dynamically propagating shear cracks with the aim of gaining insi...
[1] Earthquake ruptures are modeled as dynamically propagating shear cracks with the aim of gaining ...
UnrestrictedThis thesis examines dynamic ruptures along frictional interfaces and seismic radiation ...
Geological and geophysical observations reveal along‐strike fault zone heterogeneity on major strike...
The transition from sub-Rayleigh to supershear propagation of mode II cracks is a fundamental proble...
Shear ruptures propagating along natural faults or simulated faults in analog laboratory experiments...