“…Although the Basel geothermal project failed, the collected data of the induced seismicity improved our understanding of EGS in several scientific studies that investigated the reservoir structure and the orientation of fault planes (e. g., Asanuma et al, ; Dyer et al, ; Dyer et al, ; Deichmann et al, ; Kraft & Deichmann, ), performed statistical analyses for earthquake forecasting purposes (e.g., Bachmann et al, ; Mena et al, ; Gischig & Wiemer, ; Király‐Proag et al, ), modeled geomechanical properties (e.g., Goertz‐Allmann et al, ; Goertz‐Allmann & Wiemer, ; Bachmann et al, ), studied the larger events in terms of their trigger mechanism (e.g., Mukuhira et al, ) and rupture propagation (e.g., Folesky et al, ), analyzed ground motion and macroseismic intensities (e.g., Edwards et al, ; Ripperger et al, ), and performed seismic risk analysis (e.g., Baisch et al, ; Mignan et al, ). These studies benefited from the six‐station borehole seismometer network (three stations used in this study are shown in Figure ) and a surface network with 30 stations in the area (Deichmann & Ernst, ).…”