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 …

The present status of research and understanding regarding the dynamics and the statistical
properties of earthquakes is reviewed, mainly from a statistical physical viewpoint. Emphasis …

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 …

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 …

We precisely locate 88 tremor families along the central San Andreas Fault using a 3D
velocity model and numerous P and S wave arrival times estimated from seismogram stacks …

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 …

D inversion techniques have become a widely used tool in magnetotelluric (MT) data
interpretation. However, with real data sets, many of the controlling factors for the outcome of …

Low‐frequency earthquakes (LFEs) are small, rapidly recurring slip events that occur on the
deep extensions of some major faults. Their collective activation is often observed as a …

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

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