Fig. 3From: Delineation of sedimentary basin structure beneath the Banyumas Basin, Central Java, Indonesia, using ambient seismic noise tomographyA–C Synthetic Rayleigh wave group velocity models for each cell grid size, ranging between ~ 8.5 km × 8.5 km, ~ 6.5 km × 6.5 km, and ~ 5.5 km × 5.5 km; and the final model obtained after applying the checkerboard resolution test for period 1 s of the synthetic model, showing the distribution of stations in the study areaBack to article page