Fig. 9From: Estimation of paleo-permeability around a seismogenic fault based on permeability tensor from observable geometric information of quartz veinsSummary of measurement data, and result of estimation. The variation of the a length \(l\), b aperture \(t\), c \({S}_{0}\), and d paleo-permeability \({k}_{i}\) with the distance from the fault coreBack to article page