Fig. 3From: Characterisation of the fracture- and karst-controlled geothermal reservoir below Munich from geophysical wireline and well informationElectrical image log (CMI) showing examples of the differentiated a facies (massive, bedded, areas that remain uncharacterised because of bad quality); b fractures (conductive, resistive, partial conductive); c karst features (massive, vuggy porosity, karst along fractures); and d stress indicators (borehole breakouts, drilling-induced fractures)Back to article page