Fig. 13From: The architecture of long-lived fault zones: insights from microstructure and quartz lattice-preferred orientations in mylonites of the Median Tectonic Line, SW JapanIntensity of quartz c-axis fabrics vs. mean aspect ratio for recrystallised quartz grains for the Tsukide (a) and Ako-Miyamae (b) areas. Samples displaying low fabric intensity and elongate grains in (a) may have deformed via pressure-solution creepBack to article page