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Fig. 7 | Earth, Planets and Space

Fig. 7

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

Fig. 7

The average orientation of faster shear waves and the average time delay normalize by path lengths in anisotropic upper crust. Black bars show that the angular difference between the average orientation and the orientation of the principal compressional axis of the strain rate is within 30° and the data number is greater than or equal to 3 that are used for the plot of Fig. 8. Dark gray bars indicate that the angular difference is within 30° and the data number is smaller than or equal to 2 and light gray bars indicate that the angular difference is greater than 30°. Lines are Quaternary active faults.

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