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 …

Exhumed fault zones offer insights into deformation processes associated with earthquakes
in unparalleled spatial resolution; however it can be difficult to differentiate seismic slip from …

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 …

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

We report on laboratory experiments designed to investigate the influence of pore pressure
oscillations on the effective permeability of fractured rock. Berea sandstone samples were …

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 …

Recent geodetic observations indicate that a single fault may slip slowly and silently or fast
and seismically in different circumstances. We report laboratory experiments that …

Episodes of nonvolcanic tremor and accompanying slow slip recently have been observed
in the subduction zones of Japan and Cascadia. In Cascadia, such episodes typically last a …

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 …

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 …