Fig. 3From: Spatial variation in coda Q in the northeastern part of Niigata–Kobe Tectonic Zone, central Japan: implication of the cause of a high strain rate zoneSpatial distributions of a the differential strain rate during 2012–2014, and b–e the coda Q at five frequency bands in this study area. Blue squares are stations used to draw the coda Q maps, in five frequency bands in this study area, black lines show Quaternary active faults, and red triangles show Quaternary active volcanoesBack to article page