It has been known for a long time that slip accompanying earthquakes accounts for only a
fraction of plate tectonic displacements. However, only recently has a fuller spectrum of …

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 …

More than a decade after the discovery of deep episodic slow slip and tremor, or slow
earthquakes, at subduction zones, much research has been carried out to investigate the …

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 …

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 …

There are several ways of generating episodic slow slip events in models of rate‐and‐state
friction. Here I explore the possibility that they arise on velocity‐weakening faults whose …

Shallow slow slip events have been well documented offshore Gisborne at the northern
Hikurangi subduction margin, New Zealand, and are associated with tectonic tremor …

Swarm-like earthquake sequences are commonly observed in a diverse range of geological
settings including volcanic and geothermal regions as well as along transform plate …

Transient slip events, which occur more slowly than traditional earthquakes, are increasingly
being recognized as important components of strain release on faults and may substantially …

Migration‐based location methods (eg, time‐reverse imaging based on wave equation,
Kirchhoff summation, and diffraction stacking) can effectively locate events of low signal‐to …