Fig. 5From: A look at the blind Kumamoto experiment: combining active and passive seismic observations to avoid Rayleigh-wave mode misidentificationDispersion curve; Broadband fundamental mode Rayleigh wave phase velocity dispersion curve created by combining different arrays and MASW analysis (blue dots). Small portion of higher mode energy is picked from one shot gather downline, though not used in the inversion for Step 1 and Step 4Back to article page