Fig. 3 | Nature Communications

Fig. 3

From: Continuous plate subduction marked by the rise of alkali magmatism 2.1 billion years ago

Fig. 3

Combined Nb, TiO2, and P2O5-SiO2 compositional trends of mafic rocks. ac Diagrams of the combined Nb-SiO2, TiO2-SiO2, and P2O5-SiO2 compositional trends of mafic rocks formed in the Archean and in the Phanerozoic, respectively. The round circles are mean values corresponding to SiO2 concentrations ranging from 45 to 52 wt% (1 wt% SiO2 interval) as estimated by the Bootstrap methods. Error bars denote two standard errors of the mean (s.e.m.). The gray vertical-dashed lines divide the rocks into low-silica (45–49 wt% SiO2) and high-silica (49–52 wt% SiO2) mafic rock groups

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