
doi: 10.1002/2017gl074767
AbstractIn April 2017, a sequence of earthquakes offshore Valparaíso, Chile, raised concerns of a potential megathrust earthquake in the near future. The largest event in the 2017 sequence was a M6.9 on 24 April, seemingly colocated with the last great‐sized earthquake in the region—a M8.0 in March 1985. The history of large earthquakes in this region shows significant variation in rupture size and extent, typically highlighted by a juxtaposition of large ruptures interspersed with smaller magnitude sequences. We show that the 2017 sequence ruptured an area between the two main slip patches during the 1985 earthquake, rerupturing a patch that had previously slipped during the October 1973 M6.5 earthquake sequence. A significant gap in historic ruptures exists directly to the south of the 2017 sequence, with large enough moment deficit to host a great‐sized earthquake in the near future, if it is locked.
finite fault models, Geophysics, coulomb stress, Valparaíso earthquake, General Earth and Planetary Sciences, moment accumulation, subduction zones, relocation
finite fault models, Geophysics, coulomb stress, Valparaíso earthquake, General Earth and Planetary Sciences, moment accumulation, subduction zones, relocation
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