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 …

Because of a combination of new observational tools and a flurry of large megathrust
earthquakes, tremendous progress has been made in recent years towards understanding …

Abstract The 2014 Working Group on California Earthquake Probabilities (WGCEP14)
present the time‐independent component of the Uniform California Earthquake Rupture …

Many types of hydrothermal ore deposits form at overpressured conditions during high fluid
flux through fault zones in the continental seismogenic regime. These include many …

The seismicity pattern along the San Andreas fault near Parkfield and Cholame, California,
varies distinctly over a length of only fifty kilometres. Within the brittle crust, the presence of …

Episodic tremor and accompanying slow slip, together called ETS, is most often observed in
subduction zones of young and warm subducting slabs,,. ETS should help us to understand …

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 …

The San Andreas Fault Observatory at Depth (SAFOD) was drilled to study the physical and
chemical processes controlling faulting and earthquake generation along an active, plate …

Deep fluids are important for the evolution and properties of the lower continental and arc
crust in tectonically active settings. They comprise four components: H2O, nonpolar gases …

The passage of radiating seismic waves generates transient stresses in the Earth's crust that
can trigger slip on faults far away from the original earthquake source. The triggered fault …