Fig. 13From: The interplay of Malm carbonate permeability, gravity-driven groundwater flow, and paleoclimate – implications for the geothermal field and potential in the Molasse Basin (southern Germany), a foreland-basin playGeothermal gradient at present (time = 1.3E5 a) under paleoclimatic conditions in a the low Malm permeability scenario (i.e. model run D introduced in Fig. 3), and b the high Malm permeability scenario (i.e. model run E). Vertical exaggeration equals threeBack to article page