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 …

At subduction zones, fluid flow, pore pressure, and tectonic processes are tightly
interconnected. Excess pore pressure is driven by tectonic loading and fluids released by …

Slow slip events are part of a spectrum of aseismic processes that relieve tectonic stress on
faults. Their spatial distribution in subduction zones has been linked to perturbations in fluid …

Subduction zone megathrust faults host Earth's largest earthquakes, along with multitudes of
smaller events that contribute to plate convergence. An understanding of the faulting …

Because of a combination of new observational tools and a flurry of large megathrust
earthquakes, tremendous progress has been made in recent years towards understanding …

Modern geophysics highlights that the slip behaviour response of faults is variable in space
and time and can result in slow or fast ruptures. However, the origin of this variation of the …

We find that in young and warm subducting plates, earthquakes occur just below the Moho.
In older plates, earthquakes occur throughout the subducting oceanic crust, as well as the …

Episodic tremor and accompanying slow slip, together called ETS, is most often observed in
subduction zones of young and warm subducting slabs,,. ETS should help us to understand …

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 …

Deep tremor in subduction zones is thought to be caused by small repeating shear slip
events on the plate interface with significant slow components,,,. It occurs at a depth of about …