Fig. 14From: The architecture of long-lived fault zones: insights from microstructure and quartz lattice-preferred orientations in mylonites of the Median Tectonic Line, SW JapanA summary of the inferred architecture (upper panel) and evolution of fault rocks (lower panel) in the hanging wall of the MTL in the study area. Progressive overprinting was associated with deformation mechanism transitions during uplift and cooling of the fault zoneBack to article page