Deformation and hydrothermal alteration insights of a high strain sheared zone in a gneissic basement (Black Forest, Germany). An analogue for fractured geothermal crystalline reservoirs
Résumé
Enhanced geothermal systems in basement rocks consist in the exploitation of the hot brines circulating within the fracture network as the main fluid pathway within the reservoir. This is the case at Soultz-sous-Forêts and Rittershoffen (France).
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