Fig. 8From: Subduction-related mafic to felsic magmatism in the Malayer–Boroujerd plutonic complex, western IranPrimitive mantle-normalized trace element pattern (a) and chondrite-normalized rare earth element (REE) pattern (b) of mafic rocks: gabbroic intrusions and dykes, of intermediate rocks: MMEs, dioritic intrusions and dykes (c, d), of granitic rocks (e, f). Trace element abundances for primitive mantle are from Taylor and McLennan (1985). REE abundances for Chondrite are from Sun and McDonough (1989)Back to article page