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Fig. 1 | Geothermal Energy

Fig. 1

From: 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 play

Fig. 1

Regional geological map of the Southern German Molasse Basin, modified after Bousquet et al. (2012) and Doben et al. (1996). Maximum extent of the Würm Glaciation according to digital maps by Gibbard et al. (2011). Dark red line AA’ indicates the studied cross section. Inset map shows the location of the map in Germany (MB = Molasse Basin)

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