Supplemental Material: High transient stress in the lower crust: Evidence from dry pseudotachylytes in granulites, Lofoten Archipelago, northern Norway

List of the localities, description of the methods, supplemental figures detailing the composition of the host rocks (Fig. S1), the distribution and orientation of pseudotachylytes (Fig. S2), the relationship between amphibole and pseudotachylytes (Fig. S3) and the residual pressures of quartz inclusions in garnet (Fig. S4), and supplemental tables on host rock geochemistry (Table S1) and Raman data (Table S2).