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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:scopusJoint inversion of multichannel seismic reflection and wide-angle seismic data: Improved imaging and refined velocity model of the crustal structure of the north Ecuador south Colombia convergent margin
ArticleAbstract: Improving seismic imaging of the crust is essential for understanding the structural factors controlPalabras claves:Autores:Agudelo W., Jean Yves Collot, Operto S., Ribodetti A.Fuentes:scopusThe South Ecuador subduction channel: Evidence for a dynamic mega-shear zone from 2D fine-scale seismic reflection imaging and implications for material transfer
ArticleAbstract: Tectonic processes that control the transition from poorly consolidated sediment entering the subducPalabras claves:Autores:Agudelo W., Jean Yves Collot, Ribodetti A., Sage F.Fuentes:scopus