Fig. 2From: Characterisation of the fracture- and karst-controlled geothermal reservoir below Munich from geophysical wireline and well informationConceptual faciies characteristics and composition of the Upper Jurassic Malm strata below the Molasse Basin, separated into two hyper-facies: massive- and bedded-facies (drawn after Freudenberger and Schwerd 1996a)Back to article page