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.

本研究的宗旨在于限制在不同地幔过程，诸如地幔熔融、熔体-岩石相互作用以及交代作用下的钒同位素分馏。为此，我们收集了一系列经深入研究的地幔岩石，包括来自橄榄岩岩体和异质岩。这些数据包括表1中的全岩钒同位素组成；表2中的地幔矿物钒同位素组成；以及补充表格中详尽的化学组成和建模结果。