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Fig. 6 | Earth, Planets and Space

Fig. 6

From: 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 crust

Fig. 6

Spatial 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 value

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