Dataset for: Vanadium isotope fractionation in mantle rocks: constraints from peridotites and pyroxenites

The aim of this study is to constrain V isotope fractionation under different mantle processes such as mantle melting, melt-rock interaction, and metasomatism. We thus collect a series of well-studied mantle rocks from peridotite massifs and xenolith. These data include Table 1, the V isotopic composition of Whole-rock; Table 2, the V isotopic composition of mantle minerals; and Supplementary tables include detail chemical composition and modeling results.