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 …

Recent technological advances combined with more detailed analyses of seismologic and
geodetic observations have fundamentally changed our understanding of the ways in which …

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

A new autonomous seismic location and detection methodology enables real‐time
opportunities for high‐resolution spatio‐temporal monitoring of non‐volcanic tremor …

Deep tremor under Shikoku, Japan, consists primarily, and perhaps entirely, of swarms of
low‐frequency earthquakes (LFEs) that occur as shear slip on the plate interface. Although …

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 …

Slow slip and tectonic tremor in subduction zones take place at depths where there is
abundant evidence for distributed shear over broad zones (∼ 10–103 m) composed of rocks …

Abstract The San Andreas fault is one of the most extensively studied faults in the world, yet
its physical character and deformation mode beneath the relatively shallow earthquake …

An ensemble‐averaging technique is used to remove the long‐wavelength topography and
gravity field associated with subduction zones. Short‐wavelength residual anomalies are …

An approach to invert GPS time series to estimate crustal block rotations, fault locking and
strain rates while simultaneously solving for transient slow slip events is described and …