We proposed a source model for the 16 September 2015 Illapel (Chile) tsunamigenic earthquake using teleseismic and tsunami data. The 2015 epicenter was at the northernmost of the aftershocks zone of the 2010 M-w 8.8 Maule earthquake. Teleseismic body wave inversions and tsunami simulations showed optimum rupture velocities of 1.5- 2.0 km/s. The agreement between observed and synthetic waveforms was quantified using normalized root-mean-square (NRMS) misfit. The variations of NRMS misfits were larger for tsunami data compared to the teleseismic data, because tsunami waveforms are more sensitive to the spatial distribution of slip. The large-slip area was 80 km (along strike) x 100 km (along dip) with an average slip of 5.0m and depth of 12-33 km, located similar to 70 km to the northwest of the epicenter. We obtained a seismic moment of 4.42 x 10(21) Nm equivalent to M-w 8.4. Results may indicate a northward stress transfer from the 2010 Maule earthquake.
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IPMA, Rua C Aeroporto Lisboa, P-1749077 Lisbon, Portugal
Univ Lisbon, FCUL, Inst Dom Luiz, Lisbon, PortugalIPMA, Rua C Aeroporto Lisboa, P-1749077 Lisbon, Portugal
Omira, R.
Baptista, M. A.
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Univ Lisbon, FCUL, Inst Dom Luiz, Lisbon, Portugal
Inst Polten Lisboa, Inst Super Engn Lisboa, Lisbon, PortugalIPMA, Rua C Aeroporto Lisboa, P-1749077 Lisbon, Portugal
Baptista, M. A.
Lisboa, F.
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IPMA, Rua C Aeroporto Lisboa, P-1749077 Lisbon, PortugalIPMA, Rua C Aeroporto Lisboa, P-1749077 Lisbon, Portugal
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ASR Ltd, Marine Consulting & Res, Raglan, New Zealand
Univ So Calif, Los Angeles, CA USANanyang Technol Univ, Earth Observ Singapore, Singapore 639798, Singapore