Fig. 10From: Porosity estimation of a geothermal carbonate reservoir in the German Molasse Basin based on seismic amplitude inversionCross sections along three crosslines (a–c) showing the reflection seismic data, the acoustic impedance and the porosity. The crosslines are roughly west–east oriented and have a vertical exaggeration of 5:1. Reef R2 is the same a shown in Figs. 11 and 12. See text for interpretationBack to article page