In-situ Sr isotope disequilibrium in plagioclases from Late Cenozoic basalts in Leiqiong Area: Evidence for the role of the Hainan Plume and mantle metasomatism due to a paleo-subduction event

Analytical Method, Geochemical Data, and Supplementary Figures generated in this study are included in the Supplementary I, Tables S1-S6, and Figures S1-S9

本研究生成的分析方法、地球化学数据及补充附图均收录于补充材料I、表S1~S6及图S1~S9中。