Subduction erosion revealed by Late Mesozoic magmatism in the Gangdese arc, South Tibet

The supporting information includes the Analytical methods (Text S1), Figures S1 of LA-ICP-MS zircon U-Pb concordia diagrams with cathodoluminescence images in this study, Figures S2 of ⁸⁷Sr/⁸⁶Sr_(i) versus ε _Nd(t) diagram for Mesozoic mantle-derived magma, Figures S3 of Geochemical diagrams for Late Cretaceous and pre-Late Cretaceous subduction-related adakitic rocks, Figures S4 of quantitative calculation of juvenile crust generation rate and tectonic erosion rate from Zedong and nearby area, and Table S1-S8 of the analytical results.