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Comment on “The Chongón/Colonche orocline transrotational bending and the coeval opening of the Progreso basin in southwestern Ecuador” by Alemán et al
ArticleAbstract:Palabras claves:Autores:Carlos Aizprua, D. Barba, Poujol M., Reynaud J.Y., Witt C.Fuentes:scopusCenozoic Stages of Forearc Evolution Following the Accretion of a Sliver From the Late Cretaceous-Caribbean Large Igneous Province: SW Ecuador-NW Peru
ArticleAbstract: The SW Ecuador-NW Peru forearc region is the southernmost location, where the Caribbean large igneouPalabras claves:Accretionary wedge, Backstop, Forearc, North Andean SliverAutores:Carlos Aizprua, D. Barba, Johansen S.E., Witt C.Fuentes:scopusFrom accretion to forearc basin initiation: The case of SW Ecuador, Northern Andes
ArticleAbstract: The SW of Ecuador offers a great opportunity to study the long-term behavior of an almost entire forPalabras claves:Andes, ECUADOR, Forearc Basin, Outer forearc high, SubductionAutores:Amberg C., Carlos Aizprua, D. Barba, M. Rivadeneira, Poujol M., Reynaud J.Y., Witt C.Fuentes:scopusForearc Crustal Structure of Ecuador Revealed by Gravity and Aeromagnetic Anomalies and Their Geodynamic Implications
ArticleAbstract: Along the Western Cordillera of Ecuador, fault-bounded ophiolites derived from the Late Cretaceous CPalabras claves:Autores:Brönner M., Carlos Aizprua, D. Barba, Johansen S.E., María José Hernández, Witt C.Fuentes:scopusThe Esmeraldas Canyon: A Helpful Marker of the Pliocene-Pleistocene Tectonic Deformation of the North Ecuador-Southwest Colombia Convergent Margin
ArticleAbstract: Deciphering the migration pattern of the Esmeraldas submarine Canyon (EC) and its history of cut-andPalabras claves:convergent margin tectonics, fore-arc basin, Natural hazards, Paleoseismology, submarine canyonAutores:Alexandra P. Alvarado, D. Barba, Jean Noël Proust, Jean Yves Collot, Khumara S., María José Hernández, Michaud F.A., Migeon S., P. Silva, Pazmino A., Ratzov G.Fuentes:scopus