Research Article

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

Figure 6

Geochemical classification diagrams of granitoid samples from the Darongshan pluton: (a) total alkalis versus silica diagram (after [114]); (b)An–Ab–Or diagram (after [115]); (c) K2O vs. SiO2 diagram (after [116]); (d) A/NK vs. A/CNK diagram (after [117]). A/CNK–molar (Al2O3/(CaO+Na2O+K2O)); A/NK-molar (Al2O3/(Na2O+K2O)); (e) SiO2 vs. FeOT/(FeOT+MgO) diagram; (f) SiO2 vs. Na2O+K2O–CaO (MALI) diagram. Boundaries between magnesian and ferroan and alkali, alkali-calcic, calc-alkalic, and calcic are from Frost et al. [118]. Data sources are referenced in Table S1 of the Supplementary Materials.
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