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Supplemental Material: Origin of the Oligocene–Miocene Sailipu ultrapotassic volcanic rocks in southern Tibet: Melting of Asian mantle pyroxenites triggered by eastward tearing of the subducting Indian continental slab

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posted on 2024-10-08, 16:58 authored by Lin Liu, et al.

Table S1: The mineral assemblage, whole-rock major and trace element data for the Sailipu ultrapotassic rocks. Table S2: U-Pb age data of zircons from Sailipu ultrapotassic rocks. Table S3: Trace element data of zircons from Sailipu ultrapotassic rocks. Table S4: Hf isotopic data of zircons from the Sailipu ultrapotassic rocks. Table S5: Major element and trace element data of olivine from Sailipu ultrapotassic rocks. Table S6: Major element and trace element data of clinopyroxene from Sailipu ultrapotassic rocks. Table S7: Estimation of redox condition of the Sailipu ultrapotassic rocks based on olivine-liquid equilibrium. Table S8: Estimation of crystallization temperature of the Sailipu ultrapotassic rocks based on olivine-liquid equilibrium. Table S9: Estimation of crystallization temperature and pressure of the Sailipu ultrapotassic rocks based on clinopyroxene-liquid equilibrium. Table S10: Pressure-temperature estimates of the Sailipu ultrapotassic rocks. 

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