Fig. 2From: Seismicity induced during the development of the Rittershoffen geothermal field, Francea East–West simplified vertical section of the Rhine Graben crossing the Soultz-sous-Forêts GPK–2 and the Rittershoffen GRT-1 wells (from Edel et al. 2018); b temperature logs, at equilibrated thermal conditions, for the Soultz-sous-Forêts GPK-2 well (from Genter et al. 2010) and for the Rittershoffen GRT-1 well (from Baujard et al. 2017) (vertical scale is in MD)Back to article page