Data of "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 Supplementary tables which comprise the chemical composition and the detail modeling results.