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Geoscience Letters

Official Journal of the Asia Oceania Geosciences Society (AOGS)

Fig. 8 | Geoscience Letters

Fig. 8

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

Fig. 8

Comparison of results of the ANT in this study with gravity and geological studies. A Tomogram model of Vs at a depth of 2 km and interpretation of the structure and delineation. The area within the black dashed line represents the resolution limit of the ANT method. The two red dashed line of low Vs indicate the Majenang Low and the Citanduy Low, separated by the Cipari Anticline. The Citanduy Fault located SW and the Karangbolong Fault located NE, according to C; B the residual Bouguer anomaly map (modified from Hidayat et al. 2020); the red dashed line depicted in A shows low Vs delineation; C configuration of Miocene structure in the southern Central Java (modified from Muchsin et al. 2002). The black square is the study area, utilizing ANT

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