Deep-seated slow slip and tremor (SST), including slow slip events, episodic tremor and
slip, and low-frequency earthquakes, occur downdip of the seismogenic zone of numerous …

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

Slow slip events have become recognized in the last decade as an important mode of fault
slip, and are most widely observed at subduction zones. Many episodes of tectonic tremor …

В монографии приведены результаты многолетних исследований закономерностей
деформирования нарушений сплошности массивов горных пород. На основе …

We document a sequence of simultaneous short‐term and long‐term slow slip events
(SSEs) at the Hikurangi subduction zone during the 2010/2011 period. The sequence of …

Subduction of hydrated oceanic lithosphere can carry water deep into the Earth, with
consequences for a range of tectonic and magmatic processes. Most of the fluid is released …

Slow slip along the plate interface at subduction zones can generate weak seismic tremor in
a quasi-periodic process called episodic tremor and slip. This process differs in character …

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 …

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 fault slip includes a range of transient phenomena that occur over timescales longer
than those of standard earthquakes. Slow slip events are often closely associated with …