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

Short-and long-term processes at or close to the subduction plate interface (eg, mineral
transformations, fluid release, seismicity and more generally deformation) might be more …

Modern geodetic and seismologic observations describe the behavior of fault slip over a
vast range of spatial and temporal scales. Slip at sub-seismogenic speeds is evident from …

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 …

Metamorphic devolatilization of subducted slabs generates aqueous fluids that ascend into
the mantle wedge, driving the partial melting that produces arc magmas. These magmas …

Episodic tremor and slow slip (ETS) occurs in the transition zone between the locked
seismogenic zone and the deeper, stably sliding zone. Actual mechanisms of ETS are …

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 …

Non-volcanic tremor (NVT) and episodic slow slip events (SSEs) have been observed below
the seismogenic zone of relatively warm subduction zones for the past 20 years …

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 …

Slow slip and tremor is observed along many subduction margins and is commonly linked to
fluid pressure variations and migration. Accurate estimates of porosity and permeability …