Fig. 3From: Subduction-related mafic to felsic magmatism in the Malayer–Boroujerd plutonic complex, western Irana Weak foliation in mylonitic granite cross cut by sedimentary xenolith elongated along the magmatic flow. b Small rounded FME in granodioritic host. c, d Globular and ellipsoid-like MMEs in granodioritic host. e, f Linear arrangement of flaky biotite across the boundary between enclaves and host rock, indicating ductile deformation in semi-molten stateBack to article page