Sentence examples for world seismicity patterns from inspiring English sources

World seismicity patterns show that earthquakes tend to occur along active plate boundaries where there is subduction (Japan) or strike-slip motion (California) and along strike-slip faults (as in China, where they are the result of the northward migration of India into Asia).

Therefore, it is necessary to compile an earthquake catalog with consistent magnitudes to facilitate meaningful delineation of seismicity patterns and reliable assessment of seismic hazards in Taiwan.

Global seismicity patterns had no strong theoretical explanation until the dynamic model called plate tectonics was developed during the late 1960s.

More recently, researchers have sought to associate electromagnetic fields, the radon or hydrogen content of the soil and seismicity patterns with impending earthquakes.

Seismicity patterns after large earthquakes suggest that the earthquake hazard can rise sharply in areas well beyond the mainshock rupture zone.

This study aims to quantify the seismicity patterns of this sequence by using the ETAS model.

This network has recorded a change in seismicity patterns after the Tohoku earthquake, with seismicity increasing in a number of areas, including the southeast of the Tohoku region.

We follow the fundamental process for seeking time- and space-dependent seismicity incorporating stress perturbations developed by Toda et al. (2005), which retrospectively applied their method to the evolution of seismicity in southern California and then roughly reproduced the time-space-dependent seismicity patterns.

It is necessary to identify these types of slip statistically based on space time seismicity patterns to allow empirical evaluation of the probability gain of large earthquakes.

The NCER value is also important to understand how the energy release process varies depending on seismicity patterns such as mainshock aftershock, foreshock mainshock aftershock, and swarm types.

Seismicity patterns vary substantially from place to place, showing various clustering features, though some of the fundamental physical processes leading to earthquakes may be common to all events.