Slow earthquakes are characterized by a wide spectrum of fault slip behaviors and seismic
radiation patterns that differ from those of traditional earthquakes. However, slow …

The recognition of slow earthquakes in geodetic and seismological data has transformed the
understanding of how plate motions are accommodated at major plate boundaries. Slow …

We develop a novel method for seismic event detection that can be applied to large-N
arrays. The method is based on a new detection function named local similarity, which …

Abstract The 2011 Mw 9.0 Tohoku‐oki earthquake is one of the world's best‐recorded
ruptures. In the aftermath of this devastating event, it is important to learn from the complete …

Shallow slow slip events have been well documented offshore Gisborne at the northern
Hikurangi subduction margin, New Zealand, and are associated with tectonic tremor …

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 …

We present the first comprehensive tectonic tremor catalog for the northern Hikurangi Margin
obtained from the systematic analysis of data from the New Zealand Seismic Network …

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 …

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 …