Abstract: Palaeopermeability anisotropies of a strike-slip fault damage zone: 3D Insights of quantitative fluid flow from µCT analysis. (2017 AGU Fall Meeting)

Palaeopermeability anisotropies of a strike-slip fault damage zone: 3D Insights of quantitative fluid flow from µCT analysis.

Rodrigo Gomila^1,2, Gloria Arancibia^3,4, Mathias Nehler^5,6, Rolf Bracke^6,7 and Diego Morata^8,9, (1)Università di Genova, Genova, Italy, (2)Andean Geothermal Center of Excellence (CEGA), Santiago, Chile, (3)Pontifical Catholic University of Chile, Department of Structural and Geothecnical Engineering, Santiago, Chile, (4)Andean Geothermal Center of Excellence (CEGA), Universidad de Chile, Santiago, Chile, (5)Ruhr University Bochum, Bochum, Germany, (6)International Geothermal Center (GZB), Bochum, Germany, (7)Hochschule Bochum, Bochum, Germany, (8)University of Chile, Department of Geology and Andean Geothermal Center of Excellence (CEGA), Santiago, Chile, (9)University of Chile, Geology Departmet, Santiago, Chile

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