Following laboratory experiments and friction theory, slow slip events and seismicity rate
accelerations observed before mainshocks are sometimes interpreted as evidence of a …

Geodetically constrained interseismic interplate coupling has been widely used to assess
seismic potential in subduction zones. Modeling interseismic deformation is challenging, as …

We compiled a novel microseismicity catalog for the Central Chile megathrust (29°–35° S),
comprising 8,750 earthquakes between April 2014 and December 2018. These events …

We deployed a dense geodetic and seismological network in the Atacama seismic gap in
Chile. We derive a microseismicity catalog of> 30,000 events, time series from 70 GNSS …

We use continuous and survey GNSS data to image the spatial and temporal evolution of
afterslip during the 2 months following the Mw 8.3 2015 Illapel earthquake. Our approach …

Over the last 3 decades, GPS measurements have been instrumental in quantifying tectonic
plates current motion and deformation. Complex patterns of deformation along the plate …

We studied the along‐dip influence of the Copiapó ridge subduction in the Atacama region,
North‐Central Chile by building a new seismicity catalog, including similar events and non …

Various earthquake models predict that aseismic slip modulates the seismic rupture process
but actual observations of such seismic‐aseismic interaction are scarce. We analyze seismic …

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 …

Four years ago, using survey GPS measurements, the first deep slow slip event (SSE) was
detected in Chile (near Copiapó, Atacama region), unrelated to any major earthquake. It was …