Fig. 7From: Visualization of attenuation structure and faults in incoming oceanic crust of the Nankai Trough using seismic attenuation profilingVelocity model and synthetic seismogram for testing Q estimation errors caused by frequency distortion associated with NMO stretching. The orange solid curve is the stacking velocity function used for NMO correction. The synthetic seismogram contains four Ricker wavelets of center frequency of 25, 22, 19 and 16 HzBack to article page