Genesis of the Early Indosinian Darongshan Granitoid in South China: Response to the Subduction of the Eastern Paleo-Tethys Ocean

Figure 12

(a) Cr vs. Ni diagram (after [121]). (b) Zircon U–Pb age versus diagram. Hf isotopic data for the Daling granite are from Wen and Pang [72]. DM: depleted mantle. Data sources are referenced in Table S6 of the Supplementary Materials. (c) Initial vs. diagram. The Sr–Nd isotopic data describing the Darongshan granitoid and mafic igneous rocks (250 Ma) are from Qi et al. [30], Fang [122], Wang et al. [43], Li et al. [24], and Qin et al. [78, 100]. Data sources are referenced in Table S7 of the Supplementary Materials. (d) vs. diagram (after [79]). Legend is shown in Figure 6.

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