Transition zone escape induced by India-Eurasia collision explains Cenozoic intracontinental basalts in Central Asia
Description
Table S1. Major-element data of minerals, including olivine, clinopyroxene and Fe-Ti oxides from the Piqiang basalts (analyzed by EPMA). Table S2. Trace-element data of olivine phenocrysts from the Piqiang basalts (analyzed by LA-ICP-MS). Table S3. U-Pb age data of zircons from the Piqiang basalts. Table S4. Trace-element data of zircons from the Piqiang basalts and estimated oxygen states. Table S5. Hf-isotope data of zircons from the Piqiang basalts. Table S6. Whole-rock major- and trace-element data for the Piqiang basalts. Table S7. Whole-rock Sr-Nd-Pb-Hf isotope data for the Piqiang basalts. Table S8. Estimation of water content, redox condition, and crystallization temperature of the Piqiang magmas based on olivine-liquid equilibrium. Table S9. Trace-element and isotope data for end-members used in geochemical modelling.