Fig. 4From: Porosity estimation of a geothermal carbonate reservoir in the German Molasse Basin based on seismic amplitude inversionCross section through the GRAME 3D seismic intersecting the Munich Fault (a), and the corresponding geological interpretation (b). In the Schäftlarnstraße area the Munich Fault splits into two branches resulting in a three-part fault geometry which consists of a hanging wall, an intermediate block and a footwallBack to article page