Abstract: Fault-controlled permeability and fluid flow in low-porosity crystalline rocks: an example from naturally fractured geothermal systems in the Southern Andes (2017 AGU Fall Meeting)

Fault-controlled permeability and fluid flow in low-porosity crystalline rocks: an example from naturally fractured geothermal systems in the Southern Andes

Gloria Arancibia^1,2, Tomas Roquer^1,3, Josefa Sepúlveda^2,4, Eugenio A. Veloso^2,5, Diego Morata^6,7 and Julie V Rowland⁸, (1)Andean Geothermal Center of Excellence (CEGA), Universidad de Chile, Santiago, Chile, (2)Pontificia Universidad Católica de Chile, Departamento de Ingeniería Estructural y Geotécnica, Santiago, Chile, (3)Pontificia Universidad Católica de Chile, Department of Structural and Geothecnical Engineering, Santiago, Chile, (4)Andean Geothermal Center of Excellence (CEGA), Santiago, Chile, (5)Pontifical Catholic University of Chile, Deparment of Structural and Geotechnical Engineering, Santiago, Chile, (6)University of Chile, Department of Geology and Andean Geothermal Center of Excellence (CEGA), Santiago, Chile, (7)Universidad de Chile, Departamento de Geología, Santiago, Chile, (8)University of Auckland, School of Environment, Auckland, New Zealand

Back to: Advances in Hydrological Characterization of Flow and Transport in Fractured Media: Numerical and Experimental Observations III Posters