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Fig. 8 | Geothermal Energy

Fig. 8

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. 8

a Darcy’s velocity magnitude at present (time = 1.3E5 a) for the high Malm permeability scenario with a constant surface temperature (i.e. model run B), and b difference of Darcy’s velocity magnitude between the high and low Malm permeability scenarios (i.e. difference between model runs B and A). Darcy’s velocity magnitude is expressed as logarithm base 10 and unit m a−1. Vertical exaggeration equals three

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