Fig. 11From: Evaluating variability in coseismic slips of paleoearthquakes from an incomplete slip history: an example from displaced terrace flights across the Kamishiro fault, central JapanFlowchart illustrating the procedure to calculate the COVs. S2014 is the dip slip of the 2014 event. ST1, T2, T5 is the dip slip of terraces T1, T2, and T5; they do not include that of the 2014 event. Si is the dip slip of the ith most recent event at the Oide siteBack to article page