▪ Abstract Earthquake triggering is the process by which stress changes associated with an
earthquake can induce or retard seismic activity in the surrounding region or trigger other …

The discipline of seismology is based on observations of ground motion that are inherently
undersampled in space and time. Our basic understanding of earthquake processes and our …

Earthquakes follow a well-known power-law size relation, with smaller events occurring
much more often than larger events. Earthquake catalogs are thus dominated by small …

An immediate report of the source focal mechanism with full automation after a destructive
earthquake is crucial for timely characterizing the faulting geometry, evaluating the stress …

This essential reference for graduate students and researchers provides a unified treatment
of earthquakes and faulting as two aspects of brittle tectonics at different timescales. The …

Earthquakes occur as a result of global plate motion. However, this simple picture is far from
complete. Some plate boundaries glide past each other smoothly, while others are …

Large and destructive earthquakes on mature faults in Earth's crust occur as slip in a layer of
a fine granular material—fault gouge—produced by comminution during sliding,. A range of …

Abstract<? A3B2 twb 0.3 w?> The 2007 Working Group on California Earthquake
Probabilities (WGCEP, presents the Uniform California Earthquake Rupture Forecast …

Injecting fluids in the crust, or their extraction, changes pore pressure and poroelastic
stresses. Both pressure and stress changes can promote seismicity and, hence, the seismic …

Detection of low magnitude event is critical and challenging in seismology. We develop a
new method, named the match and locate (M&L) method, for small event detection. The M&L …