The phenomenon of dynamic earthquake triggering, when seismic waves from an
earthquake trigger seismicity at distant sites, has been recognized for over 25 years, yet …

The aftershock zone of each large (M≥ 7) earthquake extends throughout the shallows of
planet Earth. Most aftershocks cluster near the mainshock rupture, but earthquakes send out …

Geothermal/volcanic regions are most susceptible to local earthquake triggering by regional
and remote earthquakes. Transient stresses caused by surface waves of these earthquakes …

This article describes a database that provides various catalogs of slow earthquakes. The
catalogs list the times and the locations of the events, with additional information depending …

Seismic waves from large earthquakes have been shown to trigger seismicity large
distances from a mainshock, and this is termed remotely or dynamically triggered seismicity …

We investigate the triggering of seismic tremor and slow slip event in Guerrero (Mexico) by
the February 27, 2010 Maule earthquake (Mw 8.8). Triggered tremors start with the arrival of …

Abstract The 2011 M w 9.0 Tohoku, Japan, earthquake triggered deep tectonic tremor and
shallow microearthquakes in numerous places worldwide. Here, we conduct a systematic …

SUMMARY The Salton Sea Geothermal Field (SSGF) is one of the most seismically active
and geothermally productive fields in California. Here we present a detailed analysis of short …

Abstract The Arunachal Himalaya has been hosting some notable events in the recent past.
The tectonic history of Arunachal Himalaya is complex and has been influenced by several …

Tectonic tremor, an extremely stress‐sensitive seismic phenomenon occurring in the brittle‐
ductile transition section of a fault, is associated with the shearing mechanism of slow slip …