Mantle Zn Isotopic Heterogeneity Caused by Melt‐Rock Reaction: Evidence From Fe‐Rich Peridotites and Pyroxenites From the Bohemian Massif, Central Europe

引用方式:

Huang, J., Ackerman, L., Zhang, X. C., & Huang, F. (2019). Mantle Zn isotopic heterogeneity caused by melt‐rock reaction: Evidence from Fe‐rich peridotites and pyroxenites from the Bohemian Massif, Central Europe. Journal of Geophysical Research: Solid Earth, 124(4), 3588-3604.