Fully joint inversion of the 2016 Mw 7.6 Chiloé earthquake

Summary A large (Mw 7.6) megathrust earthquake occurred on 25 December 2016 in Southern Chile, south of the Chiloé Island (74.2○ W, 43.3○ S) in the South America - Nazca subduction zone. This earthquake was the first large event in this seismotectonic segment since the Mw 9.5 1960 Valdivia megathrust earthquake, and broke a ~50 km long segment of the southern part of its rupture zone. Source parameters are inferred from teleseismic broadbands, strong motions, GPS, cGPS, InSAR, and tide gauge data. We show that the joint inversion significantly improves the resolution of the slip distribution, taking advantage of each dataset. Our slip models predict a single slip patch of 70 km x 60 km with a maximum slip of 3.2 ± 0.8 m and a moment magnitude of 7.64. The hypothesis from previous studies that the Chiloé earthquake released energy accumulated before the Valdivia earthquake is not supported by the ensemble of geodetic, seismological and tsunami data. Hence the Chiloé earthquake most likely released all the strain accumulated in the rupture area since the 1960 earthquake.