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Areas prone to slow slip events impede earthquake rupture propagation and promote afterslip
ArticleAbstract: At subduction zones, transient aseismic slip occurs either as afterslip following a large earthquakePalabras claves:Autores:Cubas N., Jean Mathieu Nocquet, Patricia A. Mothes, Paul Jarrin, Plain M., Rolandone F., Sandro Vaca, Stephen Hernández, Vallée M., Yvonne FontFuentes:googlescopusSeismic, volcanic, and geodetic networks in Ecuador: building capacity for monitoring and research
ArticleAbstract: The Instituto Geofísico of the Escuela Politécnica Nacional (IGEPN) is in charge of the monitoring aPalabras claves:Autores:Alexandra P. Alvarado, Andrea Córdova, Cristina Ramos, Daniel Alejandro Pacheco, Gabriela Ponce, Jorge Aguilar, Juan Carlos Singaucho, Mario C. Ruiz, Mayra Vaca, Mónica Segovia, Patricia A. Mothes, Paul Jarrin, Sandro Vaca, Wilson Acero, Wilson Enríquez, Yepes H.Fuentes:googlescopusRecurrent slow slip events as a barrier to the northward rupture propagation of the 2016 Pedernales earthquake (Central Ecuador)
ArticleAbstract: The northern Ecuador segment of the Nazca/South America subduction zone shows spatially heterogeneouPalabras claves:interseismic coupling, Pedernales earthquake, Propagation barrier, seismic swarm, Slow slip event, SubductionAutores:Battaglia J., Jean Mathieu Nocquet, Regnier M.M., Sandro Vaca, Vallée M.Fuentes:scopus