Gómez, Demián D. http://orcid.org/0000-0002-5276-581X
Figueroa, Mara A. http://orcid.org/0000-0003-2586-1862
Sobrero, Franco S. http://orcid.org/0000-0002-9730-1875
Smalley, Robert Jr. http://orcid.org/0000-0002-7338-1401
Bevis, Michael G. http://orcid.org/0000-0003-0977-7708
Caccamise, Dana J. II http://orcid.org/0000-0002-4874-9761
Kendrick, Eric http://orcid.org/0000-0001-6053-7772
Funding for this research was provided by:
National Science Foundation (NSF - EAR 1602764, NSF - EAR-1118241)
Instituto Geográfico Nacional de Argentina
The University of Memphis, Center for Earthquake Research and Information
Division of Geodetic Science, School of Earth Sciences, The Ohio State University
Article History
Received: 27 September 2022
Accepted: 29 March 2023
First Online: 16 May 2023
Declarations
:
: The authors declare that they have no conflict of interest.
: Data are public and available through the websites of the Argentine IGN ExternalRef removed, the Chilean Centro Sismológico Nacional ExternalRef removed, the Instituto Brasileiro de Geografia e Estatística ExternalRef removed and through the UNAVCO Facility Archive. Surface displacement forward fields for Maule and Illapel (including co- and postseismic) are available through Github ExternalRef removed. LiCSAR contains modified Copernicus Sentinel data (2015) analyzed by the Center for the Observation and Modeling of Earthquakes, Volcanoes and Tectonics (COMET). LiCSAR uses JASMIN, the UK’s collaborative data analysis environment (ExternalRef removed). The aftershock sequence to delimit the Maule rupture zone and other metadata was obtained from ExternalRef removed. The aftershock sequence to delimit the Illapel rupture zone and other metadata was obtained from ExternalRef removed. The Slab 1.0 model for South America was obtained from ExternalRef removed. The Slab2 model for South America was obtained from ExternalRef removed.