Reply to the comment by R. A. Astini and F. M. Dávila on -The West Andean Thrust, the San Ramón Fault, and the seismic hazard for Santiago, ChileReportar como inadecuado




Reply to the comment by R. A. Astini and F. M. Dávila on -The West Andean Thrust, the San Ramón Fault, and the seismic hazard for Santiago, Chile - Descarga este documento en PDF. Documentación en PDF para descargar gratis. Disponible también para leer online.

1 IPGP - Institut de Physique du Globe de Paris 2 Departamento de Geología, Universidad de Chile, Santiago 3 Departamento de Geofisica, Universidad de Chile, Santiago

Abstract : We have proposed earlier a new tectonic model for theevolution of the Andes mountain belt as a bivergent orogen.Here, to reply to a comment by Astini and Dávila 2010, wediscuss briefly the protracted diachronic evolution over tensof million years by propagating deformation at the largescaleover 102–103 km, its influence on basin formationin the back‐arc region retroarc foreland basin, and themechanical implications of the bivergence in the tectonics ofthe fore‐arc region, particularly the possible effects of theunderthrusting of the coastal crustal‐scale rigid block theMarginal Block beneath the West Andean Thrust





Autor: Rolando Armijo - Rodrigo Rauld - Ricardo Thiele - Gabriel Vargas - Jaime Campos - Robin Lacassin - Edgar Kausel -

Fuente: https://hal.archives-ouvertes.fr/



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