Crustal deformation patterns are affected by multiscale granulation and healing processes
associated with phase transitions between continuum and discrete states of rocks. The …

We provide an overview of the basic models of the aftershock processes and advanced
methods used to predict postseismic hazard. We consider both the physical mechanisms for …

Aftershocks induced by a large mainshock can cause additional damage to structures and
infrastructure, hampering building reoccupation and restoration activities in a post‐disaster …

Two of the long-standing relationships of statistical seismology are power laws: the
Gutenberg–Richter relation describing the earthquake frequency–magnitude distribution …

A large mainshock triggers numerous aftershocks, exposing evacuees and residents to
significant risk and hampering building reoccupation and restoration activities in a post …

Abstract<? A3B2 twb 0.3 w?> A reliable estimate of completeness magnitude, M c, above
which all earthquakes are considered to be detected by a seismic network, is vital for …

We investigate the early aftershock activity associated with four moderate earthquakes (M w
6.6–6.7) that occurred recently in Japan. For each aftershock sequence, we examine …

We investigate the validity of a proposed generalized Omori–Utsu law for the aftershock
sequences for the Landers, Hector Mine, Northridge and Superstition Hills earthquakes, the …

In many important systems exhibiting crackling noise—an intermittent avalanchelike
relaxation response with power-law and, thus, self-similar distributed event sizes—the “laws” …

A reliable estimate of completeness magnitudes is vital for many seismicity-and hazard-
related studies. Here we adopted and further developed the Probability-based Magnitude of …