Outcrop and microphotographs showing D1/D2 relationships. In Força Réal schists, (A) S2 in S0-1 quarzitic layers; (B) remnants of S1 in thin-section, S1 bears chlorites and muscovites, and S2 muscovites and biotites; F2 foldsin (C) Força Réal schists, (D) devonian marbles, (E) migmatitic paragneiss. (F) F2 folds in migmatitic paragneiss, cordierites are crystallized parallel to S2 inside leucosomes coeval with D2 deformation. (G) F2 folds in migmatitic paragneiss with injections of melts parallel to S2.