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Official Journal of the Asia Oceania Geosciences Society (AOGS)

Fig. 2 | Geoscience Letters

Fig. 2

From: Delineation of sedimentary basin structure beneath the Banyumas Basin, Central Java, Indonesia, using ambient seismic noise tomography

Fig. 2

A Cross-correlogram between station pairs C33 against all possible receiving stations with an average Rayleigh wave velocity of 2.12 km/s. The position between station C33 and the other stations is indicated on the inset map. The blue dashed line indicates the lag time trend of the Rayleigh EGF waves as the distance between stations increased. B The dispersion curve of the EGF picking process between stations C01–C02. The white dashed line indicates the result of group velocity picked at the top of the envelope, with the red area denoting the maximum energy possessed by the Rayleigh wave

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