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Do the Billecocha normal faults (Ecuador) reveal extension due to lithospheric body forces in the northern Andes?
ArticleAbstract: Active compressional and transcurrent structures are widely reported for the entire northern Andes,Palabras claves:Autores:Bernardo O. Beate, Carey-Gailhardis E., Ego F., Sébrier M.Fuentes:scopusGeological constraints on the kinematics and fault-plane solution of the Quiches Fault Zone reactivated during the 10 November 1946 Ancash earthquake, northern Peru
ArticleAbstract: The earthquake (Mw=6.8) produced surface faulting along the Quiches normal-slip fault. Field studiesPalabras claves:Autores:Bellier O., Jean François Dumont, Mercier J.L., Sébrier M.Fuentes:scopusQuaternary state of stress in the Northern Andes and the restraining bend model for the Ecuadorian Andes
ArticleAbstract: Inversion of shallow focal mechanisms in the Northern Andes, together with a neotectonic analysis ofPalabras claves:Autores:Ego F., Egues A., Hugo Yepes, Lavenu A., Sébrier M.Fuentes:scopus