Sentence examples for a rupture event from inspiring English sources

For most of the unstable slip experiments carried out in this study, a rupture event nucleated at one end of the fault in the shear direction and propagated to the other, as shown in Figure 3.

Binding is detected as a rupture event which is sensed by a vertically oscillated cantilever(7) preferably under simultaneous monitoring of sample topography.

This is similar to the analysis of the 2011 Tohoku earthquake, which is also a bilateral rupture event (Hwang 2014).

This would imply that at temperatures below roughly 250°C, and the pressure conditions explored here, nucleation of slip at low velocities is possible, but arrests before a dynamic rupture event can develop.

The essence of this effect is that the local elastic recoil following a bond rupture event can lead to large surface separation, thereby preventing future rebinding of the bond.

However, the source-fault lengths of those events are short and a validation of a multi-segment rupture event in a long active-fault zone has not yet been carried out.

We give multiple characterized source models for the 1891 Nobi earthquake as an example of a multi-segment rupture event.

The simulations show that, beyond a critical extension rate, elongating filaments of a micellar fluid described by the VCM model exhibit a dramatic and sudden rupture event as a result of the scission of the entangled wormlike chains.

This means that the 1891 Nobi earthquake was a multi-segment rupture event.

We also discuss the preferred construction methodology for the characterized source model for strong ground-motion prediction in a multi-segment rupture event.

We use the two methodologies to construct characterized source models for strong ground-motion simulations of the 1891 Nobi earthquake, which was a multi-segment rupture event occurring in the Nobi active-fault system.