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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:scopusOrigin of a crustal splay fault and its relation to the seismogenic zone and underplating at the erosional north Ecuador-south Colombia oceanic margin
ArticleAbstract: Splay faults within accretionary complexes are commonly associated with the updip limit of the seismPalabras claves:Autores:Agudelo W., Jean Yves Collot, Marcaillou B., Ribodetti A.Fuentes:scopusThermal regime from bottom simulating reflectors along the north Ecuador-south Colombia margin: Relation to margin segmentation and great subduction earthquakes
ArticleAbstract: The north Ecuador-south Colombia (NESC) margin has three transverse morphotectonic segments (the ManPalabras claves:Autores:Jean Yves Collot, Marcaillou B., Spence G., Wang K.Fuentes:scopus