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Are 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:scopusFields of multi-kilometer scale sub-circular depressions in the Carnegie Ridge sedimentary blanket: Effect of underwater carbonate dissolution?
ArticleAbstract: Offshore Ecuador, the Carnegie Ridge is a volcanic ridge with a carbonate sediment drape. During thePalabras claves:Carbonate dissolution, ECUADOR, karst, Pockmark, Volcanic ridgeAutores:Bialas J., Chabert A., Charvis P., Flueh E.R., Graindorge D., Gustcher M.A., Jean Yves Collot, Michaud F.A., Sallarès V.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