Fig. 3From: Porosity estimation of a geothermal carbonate reservoir in the German Molasse Basin based on seismic amplitude inversionStructural geological model of the Munich area with color-coded marker horizons based on the GRAME 3D seismic data set (a), and overview of the fault inventory and the well paths of the six Schäftlarnstraße boreholes Th1–Th6 (b). The cross section marked by the red line is shown in Fig. 4Back to article page