Thin section microphotographs in plane polarized light. a. Undeformed metagabbros. The epidote and albite aggregate is a pseudomorph after magmatic plagioclase. b. Mylonitic metagabbros. c. Schist dominated by amphibole with a chlorite-rich pod. d. Schist with relic of magmatic clinopyroxene, locally transformed into amphibole along fractures and cleavages. e. Serpentinite clast dominated by antigorite. f. Local occurrence of amphibole with serpentinite clast. Abbreviations after Whitney and Evans (2010).