Abstract Recent earthquakes in Chile, 2014, Mw 8.2 Iquique, 2015, Mw 8.3 Illapel and 2016,
Mw 7.6 Chiloé have put in evidence some problems with the straightforward application of …

Earthquake precursory processes have been central to scientific inquiry for nearly a century.
Recent advancements in earthquake monitoring, geodesy, and data analysis including …

We have produced a large set of broadband (0–10 Hz) synthetic seismograms for M w 9.0
earthquakes on the Cascadia megathrust by combining synthetic seismograms derived from …

The Chilean subduction zone is one of the most active in the world. Six events of magnitude
greater than M_w= 7.5 M w= 7.5 have occurred in the last 10 years, including the 2010 …

Abstract The US Geological Survey (USGS) National Earthquake Information Center (NEIC)
routinely produces finite‐fault models following significant earthquakes. These models are …

Aftershocks region have been extensively reported to expand logarithmically with time. The
associated migration velocity is typically of the order of several km/decade but can be much …

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

Along a subduction zone, great megathrust earthquakes recur either after long seismic gaps
lasting several decades to centuries or over much shorter periods lasting hours to a few …

Abstract The September 16, 2015 Mw8. 3 Illapel Earthquake occurred on a locked segment
of the South American subduction in Chile. This segment ruptured during comparable size …

The postseismic deformation following a large (Mw> 7) earthquake is expressed both
seismically and aseismically. Recent studies have appealed to a model that suggests that …