The discovery of slow-slip phenomena has revolutionized our understanding of how faults
accommodate relative plate motions. Faults were previously thought to relieve stress either …

Nonvolcanic tremor is observed in close association with geodetically observed slow-slip
events in subduction zones. Accumulating evidence points to these events as members of a …

Slow earthquakes are episodic slow fault slips. They form a fundamental component of
interplate deformation processes, along with fast, regular earthquakes. Recent …

Since its initial discovery nearly a decade ago, non-volcanic tremor has provided information
about a region of the Earth that was previously thought incapable of generating seismic …

As oceanic lithosphere subducts beneath continental lithosphere it experiences variable
degrees of interaction with the overriding plate and movement is accommodated by a …

Dynamic triggering of earthquakes by seismic waves is a robustly observed phenomenon
with well-documented examples from over 30 major earthquakes. We are now in a position …

Deep tremor in subduction zones is thought to be caused by small repeating shear slip
events on the plate interface with significant slow components,,,. It occurs at a depth of about …

We perform a systematic survey of triggered tremor along the San Andreas Fault in central
California for the 31 teleseismic earthquakes with Mw≥ 7.5 since 2001. We identify 10 …

Clear evidence for earthquake triggering by the earth tides has remained elusive for more
than a century. Using the largest global earthquake catalog available (the NEIC catalog with …

Deep tectonic tremor occurs at various sites worldwide, and the source characteristics are
heterogeneous, even at small scales. In this study, tremor sources were determined using …