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

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

本研究的补充材料包含分析方法（文本S1）、LA-ICP-MS（激光剥蚀-电感耦合等离子体质谱法）锆石U-Pb谐和图与阴极发光图像图S1、中生代幔源岩浆的(⁸⁷Sr/⁸⁶Sr)初始比值与εNd(t)值关系图S2、晚白垩世及晚白垩世前俯冲相关埃达克质岩地球化学图解S3、泽当及邻区新生地壳生成速率与构造侵蚀速率定量计算图S4，以及分析结果表S1至S8。