Fig. 4From: The architecture of long-lived fault zones: insights from microstructure and quartz lattice-preferred orientations in mylonites of the Median Tectonic Line, SW JapanMacrofracture densities measured within the Ryoke mylonites in the hanging wall of the MTL. Profile locations are indicated in Fig. 2a, b. The width of the damage zone associated with the MTL is estimated using the change in slope of cumulative fracture countsBack to article page