Fractal-geometry techniques are widely applied to the quantification of complex rock
structures. Important properties of such structures are (i) different scaling behaviour on …

Earthquake fault systems interact over a broad spectrum of spatial and temporal scales and,
in recent years, studies of the regional seismicity in a variety of regions have produced a …

We analyze seismicity rate immediately before and after 82 main shocks with the
magnitudes ranging from 3 to 5 using waveforms recorded by the Hi‐net borehole array in …

The statistical properties of aftershock sequences are associated with three empirical
scaling relations:(1) Gutenberg-Richter frequency-magnitude scaling,(2) Båth's law for the …

'Tensile Fracturing in Rocks' presents field observations on fracturing of sedimentary rocks
and granite outcrops from various provinces in three continents. It also combines results of …

We compare the aftershock decay rate in natural data with predictions from a stochastic
analytical model based on a Markov process with stationary transition rates. These transition …

In order to examine variations in aftershock decay rate, we propose a Bayesian framework to
estimate the {K, c, p}‐values of the modified Omori law (MOL), λ (t)= K (c+ t)− p. The …

Large, extended fault systems such as those in California demonstrate complex space-time
seismicity patterns, which include repetitive events, precursory activity and quiescence, and …

Hydroacoustic data from autonomous arrays and the US Navy's Sound Surveillance System
(SOSUS) provide an opportunity to examine the temporal and spatial properties of seismicity …

An automatic, adaptive, correlation-based algorithm for adjusting phase picks in large digital
seismic data sets provides significant improvement in resolution of microseismic structures …