Analysis reveals strong zinc isotope fractionation during felsic crust melting, suggesting origins of high-silica granites.
Table S1: Major- and trace-element compositions of samples investigated from the Bengbu and Dabie area. Table S2: Detailed melting simulation of Dabie granitoid. Table S3: Zn isotopic composition in lower crustal xenoliths from the North China Craton.
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Yang et al. (2025) studied this question.
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