Fig. 10From: Evaluating variability in coseismic slips of paleoearthquakes from an incomplete slip history: an example from displaced terrace flights across the Kamishiro fault, central JapanThe slip at the recent three surface-rupturing events at Oide. a Terrace ages and their cumulative dip slip; both are shown in the 2 σ range. Note that the amount of slip in this figure includes that of the 2014 event. b Earthquake timings estimated from paleoseismic trenches. The trench sites are shown in Fig. 1b: Oide and Iida (Toda et al., 2016), Iimori (Katsube et al., 2017a), and Kamishiro (Okumura, 2001)Back to article page