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

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 recognition of slow earthquakes in geodetic and seismological data has transformed the
understanding of how plate motions are accommodated at major plate boundaries. Slow …

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 …

Repeating earthquakes, or repeaters, are identical in location and geometry but occur at
different times. They appear to represent recurring seismic energy release from distinct …

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 …

The relationship (scaling) between scalar moment, M0, and duration, T, potentially provides
key constraints on the physics governing fault slip. The prevailing interpretation of M0‐T …

Low‐frequency earthquakes (LFEs) are small, rapidly recurring slip events that occur on the
deep extensions of some major faults. Their collective activation is often observed as a …