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Fig. 3 | Geothermal Energy

Fig. 3

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. 3

Overview sketch on the different Malm permeability scenarios (see also Table 1; scenarios in first row refer to model runs in the corresponding second and fourth columns) and surface temperature scenarios (scenarios in first column refer to model runs in the corresponding rows) including modifications thereof (i.e. thermal and/or hydraulic conditions considered individually). Individual model runs as well as selected results shown in the specified figures are indicated

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