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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:googlescopusStructural Control on Megathrust Rupture and Slip Behavior: Insights From the 2016 Mw 7.8 Pedernales Ecuador Earthquake
ArticleAbstract: The heterogeneous seafloor topography of the Nazca Plate as it enters the Ecuador subduction zone prPalabras claves:aftershock sequence, megathrust rupture, subduction zone earthquakesAutores:Agurto-Detzel H., Alexandra P. Alvarado, Beck S.L., Bergman E., Charvis P., Hayes G.P., Hoskins M.C., Jean Mathieu Nocquet, León-Ríos S., Lynner C., Mario C. Ruiz, Meltzer A., Regnier M.M., Rietbrock A., Rolandone F., Soto-Cordero L., Stachnik J.C., Stephen Hernández, Yvonne FontFuentes:scopus