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Deep structures of the Ecuador convergent margin and the Carnegie Ridge, possible consequence on great earthquake recurrence interval
ArticleAbstract: The deep structure of the Ecuador subduction zone and adjacent Carnegie Ridge (CR) was investigatedPalabras claves:Autores:Bethoux N., Calahorrano A., Charvis P., Graindorge D., Jean Yves CollotFuentes:scopusAre rupture zone limits of great subduction earthquakes controlled by upper plate structures? Evidence from multichannel seismic reflection data acquired across the northern Ecuador-southwest Colombia margin
ArticleAbstract: Subduction of the Nazca plate beneath the Ecuador-Colombia margin has produced four megathrust earthPalabras claves:Active margin structures, Ecuador-Colombia, MORPHOLOGY, Multichannel seismic reflection, Subduction earthquakesAutores:Agudelo W., Charvis P., Graindorge D., Gutscher M.A., Jean Yves Collot, Marcaillou B., Michaud F.A., Sage F., Spence G.Fuentes:scopusSubducted oceanic relief locks the shallow megathrust in central Ecuador
ArticleAbstract: Whether subducted oceanic reliefs such as seamounts promote seismic rupture or aseismic slip remainsPalabras claves:interseismic coupling, megathrust earthquake, Seamount subduction, seismic imaging, Slow slip eventAutores:Charvis P., Chlieh M., Eddy Sanclemente, Graindorge D., Jean Mathieu Nocquet, Jean Yves Collot, Leprêtre A., Paul Jarrin, Ribodetti A.Fuentes:googlescopus