Fig. 10From: S-wave experiments for the exploration of a deep geothermal carbonate reservoir in the German Molasse Basinvp/vs within the Upper Jurassic unit. vp/vs ratio for the reservoir from Top Priabonian to Base Tithonian (grey areas, see Fig. 1 for stratigraphic position). Each pixel corresponds to a single bin (50 × 50 m2). The relative distribution of the traveltime-derived ratios are collaborated by the sparsely applied velocity analysis points (left- and rightmost figures). The black dashed line in the panels represents the averaged traveltime-derived vp/vs value of the corresponding supergathers (black squares in the map)Back to article page