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Fig. 4 | Geothermal Energy

Fig. 4

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. 4

Generic model geometry representing the simplified Molasse Basin geology along cross section AA’ shown in Fig. 1. It spans from the Franconian Alb in the north (left) over Ingolstadt to the Inn valley (near Rosenheim close to the Alpine Front) in the south (right). Vertical exaggeration equals five

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