Fig. 2From: Influence of low-velocity superficial layer on long-period basin-induced surface waves in eastern Osaka basinLeft: Osaka basin geological model—bedrock depth (SN x WE = 85 km × 90 km). Right: Computational Vsmin250 model Vs velocity of the 0—50 m depth. See Fig. 10 in Appendix for further depths’ detailsBack to article page