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Mantle Zn Isotopic Heterogeneity Caused by Melt‐Rock Reaction: Evidence From Fe‐Rich Peridotites and Pyroxenites From the Bohemian Massif, Central Europe
- 1.Huang, J., Ackerman, L., Zhang, X.-C. 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. 2019, 124(4), 3588-3604. ISSN 2169-9313. E-ISSN 2169-9356. Available: doi: 10.1029/2018JB017125.
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