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Geothermal Energy

Science – Society – Technology

Fig. 12 | Geothermal Energy

Fig. 12

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. 12

Vertical component of the conductive heat flow density 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 three

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