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Fig. 1 | Earth, Planets and Space

Fig. 1

From: Spatial variation in shear wave splitting of the upper crust in the zone of inland high strain rate, central Japan

Fig. 1

Distribution of the principal strain rate axes (black bars: compression, white bars: extension), the high strain rate zone called the Niigata-Kobe Tectonic Zone (gray zone) (Sagiya et al., 2000), the trajectories of the maximum horizontal compressional stress (Ando, 1979) (gray dashed lines), Quaternary active faults (lines), and recent large earthquakes in and around the high strain rate zone (circles).

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