Fig. 6From: Delineation of sedimentary basin structure beneath the Banyumas Basin, Central Java, Indonesia, using ambient seismic noise tomographyShear-wave velocity (Vs) maps at various depths, A 0.5Â km, B 1Â km, C 2Â km, D 3Â km, E 5Â km, and F 8Â kmBack to article page