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Fig. 7 | Earth, Planets and Space

Fig. 7

From: The source model and recurrence interval of Genroku-type Kanto earthquakes estimated from paleo-shoreline data

Fig. 7

Coseismic vertical displacements of the Genroku event computed from the optimum fault slip distribution. The vertical displacements were computed from the optimum fault slip distribution in Fig. 5a. The red, green, and blue contours indicate uplifts, neutral, and subsidence, respectively. The contour interval is 1 m. The red arrow indicates a hollow place. The solid triangles indicate the change points from uplift to subsidence estimated from historical records (Shishikura 2000b). The solid diamond indicates the location of Oiso

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