Fig. 6From: Temporal stability of coda Q in the northeastern part of an inland high strain rate zone, central Japan: implication of a persistent ductile deformation in the crustSpatial distributions of the p value for the difference of the mean of log10 Q −1C for the successive two periods at each frequency band; left panels between the period II and the period I, and right panels between the period III (Dojo and Hiramatsu 2017) and the period II. Gray scale shows the p valueBack to article page