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 …

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 …

Subducting oceanic plates carry large amounts of carbon into the Earth's interior. The
subducted carbon is mobilized by fluid and encounters ultramafic rocks in the mantle wedge …

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 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 …

Formation and preservation of extremely high-pressure fluid in sedimentary basins is critical
to understanding petroleum accumulation and basin evolution; however, this issue remains …

Abstract Deep Slow Slip and Tremors (SSTs) are a combination of transient clusters of
tectonic tremors and slow slip associated with extremely elevated fluid pressures. SSTs are …

Cataclasites are a characteristic rock type found in drill cores from active faults as well as in
exposed fossil subduction faults. Here, cataclasites are commonly associated with evidence …

More than one teramole of carbon per year is subducted as carbonate or carbonaceous
material. However, the influence of carbonation/decarbonation reactions on seismic activity …

Fluids in subduction zones play a key role in controlling seismic activity, drastically affecting
the rheology of rocks, triggering mineral reactions, and lowering the effective stress …