Fig. 9From: Spatial variation in shear wave splitting of the upper crust in the zone of inland high strain rate, central JapanPlots of the differential strain rate observed by GPS (Sagiya et al., 2000) versus the coda Q of (a) 1–2 Hz and (b) 3–4 Hz reported by Jin and Aki (2005). Dashed line is the least squares fit to the data. Gray lines and an arrow represent the definition of QC and Δ QC in Eq. (3).Back to article page