Fig. 10
From: Tectonic significance of Triassic mafic rocks in the June Complex, Sanandaj–Sirjan zone, Iran
a (La/Sm)PM versus (Tb/Yb)PM diagram for the cumulate and isotropic mafic rocks of the June Complex; ratios are normalized to primitive Mantle values of McDonough and Sun (1995). The discrimination dashed line separates two fields for melting of garnet-bearing peridotite and of spinel-bearing peridotite (Wang et al. 2002). b Diagram showing variations in (Th/Yb)PM and (Nb/Yb)PM ratios. N-MORB composition is from Hofmann (1988), Upper Continental Crust (UCC) composition is from Taylor and McLennan (1985), and enriched mantle (EMI, EMII) and HIMU values are from Condie 2001. c Nb/La vs. Nb/Th diagram showing the trend of crustal contamination (after Zhang et al. 2014)