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Fig. 1 | Geothermal Energy

Fig. 1

From: How do the geological and geophysical signatures of permeable fractures in granitic basement evolve after long periods of natural circulation? Insights from the Rittershoffen geothermal wells (France)

Fig. 1

Location of the Rittershoffen geothermal site. a Simplified geological and structural map of the Rittershoffen and Soultz-sous-Forêts (SsF) area. The isotherms at the top of the basement are from Baillieux et al. (2014). b Geological cross section through the Rittershoffen and Soultz-sous-Forêts geothermal sites with the Rittershoffen well trajectories, after the GeOrg Team (2017). The dashed lines are schematic trajectories of the GRT-1 (blue) and GRT-2 (red) geothermal wells (Vidal et al. 2018)

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