slip associated with coseismic faulting. 40Ar–39Ar dating of pseudotachylytes represents a
powerful tool to directly determine the age of brittle faulting which is otherwise dated only
indirectly. However, the pronounced spatial heterogeneity of most endogenically generated
pseudotachylytes, due to the intimate coexistence of unmelted mineral clasts from the
source rock, frictional glass and neogenic igneous minerals, often precludes a …