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Fig. 3 | Earth, Planets and Space

Fig. 3

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. 3

Spatial distributions of coda Q−1 at five frequency bands in the Period I (left panels), the Period II (middle panels), and the Period III (right panels; Dojo and Hiramatsu 2017). Blue squares are stations used to draw the coda Q maps. Gray lines show Quaternary active faults, and red triangles show Quaternary active volcanoes

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