Lynner C. auteur aut IRD Koch C. auteur aut IRD Beck S. L. auteur aut IRD Meltzer A. auteur aut IRD Soto-Cordero L. auteur aut IRD Hoskins M. C. auteur aut IRD Stachnik J. C. auteur aut IRD Ruiz M. auteur aut IRD Alvarado A. auteur aut IRD Charvis Philippe auteur aut IRD Font Yvonne auteur aut IRD Régnier Marc auteur aut IRD Agurto-Detzel H. auteur aut IRD Rietbrock A. auteur aut IRD Porritt R. W. auteur aut IRD text journalArticle eng text/pdf born digital access The Ecuadorian convergent margin has experienced many large mega-thrust earthquakes in the past century, beginning with a 1906 event that propagated along as much as 500 km of the plate interface. Many subsections of the 1906 rupture area have subsequently produced M-w >= 7.7 events, culminating in the 16 April 2016, M-w 7.8 Pedernales earthquake. Interestingly, no large historic events M-w >= 7.7 appear to have propagated southward of similar to 1 degrees S, which coincides with the subduction of the Carnegie Ridge. We combine data from temporary seismic stations deployed following the Pedernales earthquake with data recorded by the permanent stations of the Ecuadorian national seismic network to discern the velocity structure of the Ecuadorian forearc and Cordillera using ambient noise tomography. Ambient noise tomography extracts V-sv information from the ambient noise wavefield and provides detailed constraints on velocity structures in the crust and upper mantle. In the upper 10 km of the Ecuadorian forearc, we see evidence of the deepest portions of the sedimentary basins in the region, the Progreso and Manabi basins. At depths below 30 km, we observe a sharp delineation between accreted fast forearc terranes and the thick crust of the Ecuadorian Andes. At depths similar to 20 km, we see a strong fast velocity anomaly that coincides with the subducting Carnegie Ridge as well as the southern boundary of large mega-thrust earthquakes. Our observations raise the possibility that upper-plate structure, in addition to the subducting Carnegie Ridge, plays a role in the large event segmentation seen along the Ecuadorian margin. specialized Crustal imaging Seismic noise Crustal structure EQUATEUR PROGRESO BASSIN MANABI BASSIN 066 064 220 3 1965-1977 2020 0956-540X https://www.documentation.ird.fr/hor/fdi:010078994 10.1093/gji/ggz558 0956-540X [F B010078994] https://www.documentation.ird.fr/hor/fdi:010078994 https://www.documentation.ird.fr/intranet/publi/2020/05/010078994.pdf Accès réservé (Intranet de l'IRD) IRD - Base Horizon / Pleins textes 2020-06-09 2025-02-24 fdi:010078994 fre