Fig. 5From: The source model and recurrence interval of Genroku-type Kanto earthquakes estimated from paleo-shoreline dataOptimum fault-slip distribution of the Genroku event estimated from paleo-shoreline data. a Optimum fault-slip distribution of the 1703 Genroku event estimated in case 350_4 (T = 350 year, n = 4; T G = 1400 year). The red contours and black arrows indicate the slip amounts and slip vectors, respectively. The contour interval is 4 m. b Contour map of estimation errors at the interval of 2 m. The red arrow indicates a hollow placeBack to article page