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 …

Abstract The Geodesy Advancing Geosciences and EarthScope (GAGE) Facility Global
Positioning System (GPS) Data Analysis Centers produce position time series, velocities …

This essential reference for graduate students and researchers provides a unified treatment
of earthquakes and faulting as two aspects of brittle tectonics at different timescales. The …

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 …

Slow earthquakes are episodic slow fault slips. They form a fundamental component of
interplate deformation processes, along with fast, regular earthquakes. Recent …

Tectonic faults slip in various manners, which range from ordinary earthquakes to slow slip
events to aseismic fault creep. Slow slip and associated tremor are common to many …

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

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

Slow slip transients on faults can last from seconds to months and stitch together the
earthquake cycle. However, no single geophysical instrument is able to observe the full …

Slow slip events (SSEs) represent a slow faulting process leading to aseismic strain release
often accompanied by seismic tremor or earthquake swarms. The larger SSEs last longer …