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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. 1.
    Huang, J. - Ackerman, Lukáš - Zhang, X-CH.
    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. Roč. 124, č. 4 (2019), s. 3588-3604. ISSN 2169-9313. E-ISSN 2169-9356
    OECD category: Geology
    Impact factor: 3.639, year: 2019
    Method of publishing: Limited access
    https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/2018JB017125
    http://hdl.handle.net/11104/0296572
Number of the records: 1  

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