Fig. 10From: Integration of distributed acoustic sensing for real-time seismic monitoring of a geothermal fieldWadati diagrams computed using the P- and S-wave arrival times associated with the February [panel (a)] and the April [panel (b)] events. The color map shows the depth (TVD) of the sensing points along the TH3 fiber. The dashed lines in red show the linear regressions adapted to measurements below and above 500 mBack to article page