Fig. 9From: Coda wave interferometry during the heating of deep geothermal reservoir rocksa Zoom in a 100 µs long window (from 50 to 150 µs, after first arrivals) of the waveforms recorded in the laboratory during second heating and cooling cycles. b Zoom in the last 100 µs of the waveforms recorded in the simulation. Grayscale indicates the normalized amplitude of the particle motionBack to article page