Fig. 7From: 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 differential strain rate in left panel the period I, middle panel the period II, and right panel the period III (taken from Dojo and Hiramatsu 2017). Gray lines show Quaternary active faults, and red triangles show Quaternary active volcanoesBack to article page