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

Fluids play an integral role in the geodynamical system, from consumption through
serpentinization at mid-ocean ridges and outer rises, to release through dehydration and …

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 …

Anthropogenic fluid injections at depth induce seismicity which is generally organized as
swarms, clustered in time and space, with moderate magnitudes. Earthquake swarms also …

Abstract On 1 April 2014, a great (Mw 8.1) interplate thrust earthquake ruptured in the
northern portion of the 1877 earthquake seismic gap in northern Chile. The sequence …

Abstract Since November 30, 2020, an intense seismic swarm and transient deformation
have been continuously observed in the Noto Peninsula, central Japan, which is a non …

Earthquake swarms are manifestations of aseismic driving processes deep in the crust. We
examine the spatiotemporal distribution of aseismic processes in Southern California using …

We document a 1 week long slow slip event (SSE) with an equivalent moment magnitude of
6.0–6.3 which occurred in August 2010 below La Plata Island (Ecuador), south of the rupture …

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 …

Swarms are bursts of earthquakes without an obvious mainshock. Some have been
observed to be associated with transient aseismic fault slip, while others are thought to be …