Fig. 4From: A look at the blind Kumamoto experiment: combining active and passive seismic observations to avoid Rayleigh-wave mode misidentificationActive source MAS; high-resolution MASW images computed with the deblurring method (Mikesell et al. 2017). The Step 4 active-source dispersion curve was picked using the area, where forward and reverse shot record MASW images appeared to agreeBack to article page