Fig. 2From: Temporal stability of coda Q in the northeastern part of an inland high strain rate zone, central Japan: implication of a persistent ductile deformation in the crustAn example of the estimation of coda Q. a Locations of an epicenter (star) and a station (square). b Seismic velocity waveforms recorded at the station N.YNTH. c Fitting of the single back scattering model (red line) to RMS amplitudes (black line)Back to article page