Supplemental Material: Magmatic–hydrothermal evolutionary processes in highly evolved granitic systems: Insights from zircons of the Baishitouquan pluton, NW China

Figure S1: Backscattered electron images of the three types of zircon grains in the Baishitouquan pluton. (A) Type-I zircon in leucogranite, (B) Type-Ⅱa zircon in amazonite pegmatite, (C) Type-Ⅱa and -IIb zircon grains, and (D, E, F) zircon grains with core–rim structures. Figure S2: Frequency histograms illustrating the variability in (A–C) FWHM and (D–F) degree of peak offset of the Eg, A1g, and B1g bands of the different types of zircon grains in the Baishitouquan pluton. Table S1: Zircon particle size distribution in lithological zones of the Baishitouquan pluton. Table S2: The FWHM and peak offset of zircon crystals in the Baishitouquan pluton. Table S3: Trace-element concentrations of zircon grains in the Baishitouquan pluton. Table S4: The α-radiation dose received by zircon grains in the Baishitouquan pluton.