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Fig. 8 | Earth, Planets and Space

Fig. 8

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. 8

Upper panels: plots of differential strain rate in the period I versus coda Q at five frequency bands in the periods I and II. Lower panels: plots of differential strain rate in the period II versus coda Q at five frequency bands in the periods I and II. Black line is the least square fit to the plot. Gray lines represent the definition of ΔQC and QC

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