Abstract: Tectonic meaning of anomalous fault-slip strain solutions in the Southern Volcanic Zone of the Andes: insights to assess the structural permeability of the Liquiñe-Ofqui Fault System and the Andean Transverse Faults (39°-40°S) (2017 AGU Fall Meeting)

Tectonic meaning of anomalous fault-slip strain solutions in the Southern Volcanic Zone of the Andes: insights to assess the structural permeability of the Liquiñe-Ofqui Fault System and the Andean Transverse Faults (39°-40°S)

Josefa Sepúlveda^1,2, Tomas Roquer^3,4, Gloria Arancibia^2,3, Eugenio A. Veloso^2,3, Diego Morata^5,6 and Eduardo Molina Piernas^1,7, (1)Andean Geothermal Center of Excellence (CEGA), Santiago, Chile, (2)Pontificia Universidad Católica de Chile, Departamento de Ingeniería Estructural y Geotécnica, Santiago, Chile, (3)Andean Geothermal Center of Excellence (CEGA), Universidad de Chile, Santiago, Chile, (4)Pontificia Universidad Católica de Chile, Department of Structural and Geothecnical Engineering, Santiago, Chile, (5)University of Chile, Department of Geology and Andean Geothermal Center of Excellence (CEGA), Santiago, Chile, (6)Universidad de Chile, Departamento de Geología, Santiago, Chile, (7)Pontifical Catholic University of Chile, Department of Structural and Geothecnical Engineering, Santiago, Chile

Back to: Multidisciplinary Approaches to Outstanding Questions in Andean Tectonics Posters