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

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 …

Slow earthquakes represent an important conundrum in earthquake physics. While regular
earthquakes are catastrophic events with rupture velocities governed by elastic wave speed …

The scaling law for slow earthquakes, which is a linear relationship between seismic
moment and duration, was proposed 15 y ago and initiated a debate on the difference in …

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 …

Non-volcanic tremor is a weak, extended duration seismic signal observed episodically on
some major faults, often in conjunction with slow slip events,,,. Such tremor may hold the key …

Recently, a series of unusual earthquake phenomena have been discovered, including
deep episodic tremor, low-frequency earthquakes, very-low-frequency earthquakes, slow …

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 mechanics of slow slip events (SSE) in subduction zones remain unresolved. We
suggest that SSE nucleate in areas of unstable friction under drained conditions, but as slip …

Aseismic deformation transients can emerge as a natural outcome of the rate and state
friction processes revealed in laboratory fault‐sliding experiments. When that constitutive …