Data for: Derivation of Jurassic HIMU-like intraplate basalts from mantle transition zone in South China: New geochemical constraints from olivine-hosted melt inclusion

Published: 31-03-2020| Version 1 | DOI: 10.17632/z2c2c7984y.1
Contributor:
Feng Guo

Description

Table S1. The analytical results of standards. Table S2. Whole-rock major oxide (wt%), trace element (ppm) and Sr-Nd-Pb-Hf-Os isotopic compositions of the Antang basalts. Table S3. Major oxide (wt%) compositions and δ18O values of the olivine phenocrysts. Table S4. The measured and "Fe-loss" corrected compositions of melt inclusions and the calculated primary melt and mantle potential temperature of the Antang basalts. Table S5. Trace element compositions of the homogenized melt inclusions. Table S6. H2O contents and δD values of melt inclusions in the Antang basalts. Table S7. The analysed chemical compositions of glass and mineral in unhomogenized melt inclusion. Table S8. Sr-Nd-Pb-Hf isotopic evolution of recycled oceanic crust.

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