We report on the experimental observation of spontaneously nucleated supershear rupture and on the visualization of sub-Rayleigh–to–supershear rupture transitions in frictionally held interfaces. The laboratory experiments mimic natural earthquakes. The results suggest that under certain conditions supershear rupture propagation can be facilitated during large earthquake events
International audienceSupershear earthquake ruptures propagate faster than the shear wave velocity. ...
International audienceSupershear earthquake ruptures propagate faster than the shear wave velocity. ...
Destructive large earthquakes occur as dynamic frictional ruptures along pre-existing interfaces (or...
We report on the experimental observation of spontaneously nucleated supershear rupture and on the v...
We report on the experimental observation of spontaneously nucleated supershear rupture and on the v...
We report on the experimental observation of the phenomenon of, spontaneously nucleated, supershear ...
We report on the experimental observation of the phenomenon of, spontaneously nucleated, supershear ...
We report on the experimental observation of the phenomenon of, spontaneously nucleated, supershear ...
Abstract. We report on the experimental observation of the phenomenon of, spontaneously nucleated, s...
We report on the experimental observation of spontaneously nucleated ruptures occurring on frictiona...
The goal in designing dynamic frictional experiments simulating earthquake rupture has been to creat...
We report on the experimental observation of spontaneously nucleated ruptures occurring on frictiona...
Seismic inversions show that earthquake risetimes may be much shorter than the overall rupture durat...
Seismic inversions show that earthquake risetimes may be much shorter than the overall rupture durat...
The goal in designing dynamic frictional experiments simulating earthquake rupture has been to creat...
International audienceSupershear earthquake ruptures propagate faster than the shear wave velocity. ...
International audienceSupershear earthquake ruptures propagate faster than the shear wave velocity. ...
Destructive large earthquakes occur as dynamic frictional ruptures along pre-existing interfaces (or...
We report on the experimental observation of spontaneously nucleated supershear rupture and on the v...
We report on the experimental observation of spontaneously nucleated supershear rupture and on the v...
We report on the experimental observation of the phenomenon of, spontaneously nucleated, supershear ...
We report on the experimental observation of the phenomenon of, spontaneously nucleated, supershear ...
We report on the experimental observation of the phenomenon of, spontaneously nucleated, supershear ...
Abstract. We report on the experimental observation of the phenomenon of, spontaneously nucleated, s...
We report on the experimental observation of spontaneously nucleated ruptures occurring on frictiona...
The goal in designing dynamic frictional experiments simulating earthquake rupture has been to creat...
We report on the experimental observation of spontaneously nucleated ruptures occurring on frictiona...
Seismic inversions show that earthquake risetimes may be much shorter than the overall rupture durat...
Seismic inversions show that earthquake risetimes may be much shorter than the overall rupture durat...
The goal in designing dynamic frictional experiments simulating earthquake rupture has been to creat...
International audienceSupershear earthquake ruptures propagate faster than the shear wave velocity. ...
International audienceSupershear earthquake ruptures propagate faster than the shear wave velocity. ...
Destructive large earthquakes occur as dynamic frictional ruptures along pre-existing interfaces (or...