Fig. 4From: Estimation of paleo-permeability around a seismogenic fault based on permeability tensor from observable geometric information of quartz veinsPhotographs of outcrops and photomicrographs of thin sections of quartz veins under crossed Nicol. a Shows the quartz veins in the grid F and an arrow in b shows the veins near the a. Both a and b formed during a single seismic event. c, d Show the quartz vein formed during multiple seismic events whose location is indicated as a solid circle in Fig. 2Back to article page