Fig. 10From: Estimation of seismic velocity changes at different depths associated with the 2014 Northern Nagano Prefecture earthquake, Japan (M W 6.2) by joint interferometric analysis of NIED Hi-net and KiK-net recordsRelationship between the observed velocity recovery rate m and the MDS in the shallow and deep zones at station N.MKGH. Gray curve represents the empirical relationship proposed by TenCate et al. (2000), where the solid and broken curves are the corresponding ranges examined in the rock experiment and their extrapolations, respectivelyBack to article page