Supplemental Material: Origin of Late Cretaceous, enclave-bearing granitoids in southern Tibet: Implications for magma recharge and crustal thickening
Table S1: Results of synthesized age data. Table S2: Zircon U–Pb dating. Table S3: Zircon Hf isotopic compositions. Table S4: Whole-rock chemical compositions. Table S5: Whole-rock Sr–Nd isotopic compositions. Table S6: Mineral EMPA analysis. Table S7: Non-modal batch melting modeling.