Transformation of silica-rich to carbonated silicate melts in a big mantle wedge revealed by geochemistry of mantle xenoliths
Published: 26 June 2025| Version 3 | DOI: 10.17632/c4bf2jwrky.3
Contributor:
Pengtao XuDescription
Table S1 Whole-rock major (wt.%) and trace elements (ppm) of Shulan and Yitong peridotite and pyroxenite xenoliths Table S2 Magnesium isotopic compositions (‰) of olivines and clinopyroxenes from Shulan and Yitong peridotite and pyroxenite xenoliths Table S3 Whole-rock magnesium, zinc, and iron isotopic compositions (‰) of Shulan and Yitong peridotite and pyroxenite xenoliths Table S4 The endmember values are used in isotope simulation
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Geology