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Fig. 2 | Earth, Planets and Space

Fig. 2

From: Stationarity of aftershock activities of the 2016 Central Tottori Prefecture earthquake revealed by dense seismic observation

Fig. 2

Orientation of P- and T-axes of optimal focal mechanisms. a P- and T-axes of aftershocks located at 4 ± 0.5 km projected onto the horizontal plane. b P-axes of aftershocks located within 0.5 km from the mainshock fault projected onto the vertical cross section along the fault. The plunge of each axis is indicated by axis color. Rectangles show the mainshock fault estimated from InSAR and GNSS data assuming uniform slip (GSI 2017)

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