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Earth, Planets and Space
Fig. 11 | Earth, Planets and Space

Fig. 11

From: Ambient noise tomography for a high-resolution 3D S-wave velocity model of the Kinki Region, Southwestern Japan, using dense seismic array data

Fig. 11

a Enlarged view of the northern part of the Kinki region (shown in Fig. 9) showing the perturbation of S-wave velocity at a depth of 1 km below sea level. Also shown are the locations of the Yamada Fault (YDF), Yamasaki Fault (YSF), Yagi-Yabu Fault (YGF-YBF), Mitoke Fault (MTF), Hanaore Fault (HOF) and the Biwako-seigan Fault Zone members (Chinai Fault, CF; Aibano Fault, AF; Kamidera Fault, KF; Katsuno Fault, KtF; Hira Fault, HiF; Katata Fault, KaF; Hiei Fault, HF; Zeze Fault, ZF) (Kaneda et al. 2008). b perturbation of S-wave velocity at a depth of 3 km below sea level, overlaid with earthquake hypocenters (black dots; Yano et al. 2017) and active faults. Black triangles represent the Hira and Hiei mountains. Solid black lines show the location of documented active faults (Research Group for Active Faults of Japan 1991)

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