Fig. 5From: Delineation of sedimentary basin structure beneath the Banyumas Basin, Central Java, Indonesia, using ambient seismic noise tomographyA–C Three examples of dispersion curve inversions at three different locations; D coordinates of three examples (denoted by blue dots) of the application of dispersion curve inversion in the study area. Small, gray dots denote the 121 grid points of the dispersion curve inversionBack to article page