Fig. 12From: The architecture of long-lived fault zones: insights from microstructure and quartz lattice-preferred orientations in mylonites of the Median Tectonic Line, SW JapanGrain size distribution histograms for recrystallised grains in protomylonite samples from Tsukide (a and d) and Ako-Miyamae (b and c). Area fractions are included to account for the bias toward small grains created during grain reconstructionBack to article page