Fig. 7
From: Continuity in geochemistry and time of the Tertiary Bergell intrusion (Central Alps)
Trace element patterns for the rocks of the transition zone normalized to N-MORB (Sun and McDonough 1989) compared to: a typical granodiorite, typical tonalite and other acidic rocks of the Bergell intrusion; b mafic dykes, enclaves and cumulates from the Bergell; c the adjacent S-type Novate granite and the compositional array of the Adamello batholith, and d the Peninsular Range batholith