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Fig. 16 | Geothermal Energy

Fig. 16

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. 16

Temperature difference between the paleo-temperature condition and the constant surface-temperature condition in the low Malm permeability scenario (i.e. difference between model runs D and F introduced in Fig. 3): a 80 ka ago (time = 50,000 a), b 20 ka ago (time = 1.1E5 a), and c at present (time = 1.3E5 a). Vertical exaggeration equals three

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