Earthquake swarms commonly occur along the Chilean subduction zone, witnessing fast
seismic and slow aseismic slip behavior at the plate interface. However, the largest seismic …

We search for earthquake swarms along the Chilean subduction, from− 18° to− 39° of
latitude, 2003–2020 by developing an objective, model-based method that detects potential …

The Mexican subduction zone is an ideal location for studying subduction processes due to
the short trench-to-coast distances that bring broad portions of the seismogenic and …

We relocated the six large-magnitude (5.2< M w< 6.2) earthquakes of the destructive,
tsunamigenic Aysen seismic swarm, which occurred from 2007 January–October in …

The Aysen seismic swarm began January 23, 2007, with a magnitude 5.2 (USGS)
earthquake and, after an apparent decrease in activity, continued with a magnitude 5.6 …

The last best documented historical large earthquakes in the Copiapo region (27 S)
occurred on 1819, Mw= 8.3 and 1922, Mw= 8.5. The 1983, Mw= 7.4 earthquake ruptured the …

Seismicity along subduction interfaces is usually dominated by large main-shock–aftershock
sequences indicative of a continuum distribution of highly coupled large asperities. In the …

The recent expansion of dense GPS networks over plate boundaries allows for remarkably
precise mapping of interseismic coupling along active faults. The interseismic coupling …

Preexisting networks of seismometers and continuous GPS in Northern Chile successfully
captured surface motions and seismicity leading up to the 1 April Mw 8.1. Here we compare …

Megathrust ruptures and the ensuing postseismic deformation cause stress changes that
may induce seismicity on upper plate crustal faults far from the coseismic rupture area. In …