Kinetic Mg–Fe isotope fractionation in natural basalts during melt-peridotite interaction

Table 1 shows the Mg-Fe isotopic compositions of low-Ca alkaline basalts and peridotite xenoliths in Nanjing basaltic field, eastern China. The Appendix A. Supplementary Material comprises four supplementary tables, showing the Mg (Table S1) and Fe (Table S2) isotopic compositions of standards/rock reference materials in this study, the major element compositions for peridotite xenoliths hosted by low-Ca alkaline basalts in Nanjing basaltic field (Table S3), and the mineral assemblages, partition coefficients and fractionation factors used in partial melting models (Table S4).<br>