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Key new pieces of the HIMU puzzle from olivines and diamond inclusions

Author

Listed:
  • Yaakov Weiss

    (Lamont-Doherty Earth Observatory of Columbia University)

  • Cornelia Class

    (Lamont-Doherty Earth Observatory of Columbia University)

  • Steven L. Goldstein

    (Lamont-Doherty Earth Observatory of Columbia University
    Columbia University)

  • Takeshi Hanyu

    (Japan Agency for Marine-Earth Science and Technology)

Abstract

Trace-element analyses of olivine phenocrysts and diamond inclusions indicate that carbonatite-metasomatized subcontinental mantle may be the source of the HIMU mantle end-member, as opposed to recycled basaltic oceanic crust.

Suggested Citation

  • Yaakov Weiss & Cornelia Class & Steven L. Goldstein & Takeshi Hanyu, 2016. "Key new pieces of the HIMU puzzle from olivines and diamond inclusions," Nature, Nature, vol. 537(7622), pages 666-670, September.
    • Handle: RePEc:nat:nature:v:537:y:2016:i:7622:d:10.1038_nature19113
    DOI: 10.1038/nature19113
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    Cited by:

    1. Xiaohui Li & Osamu Ishizuka & Robert J. Stern & Sanzhong Li & Zhiqing Lai & Ian Somerville & Yanhui Suo & Long Chen & Hongxia Yu, 2024. "A HIMU-like component in Mariana Convergent Margin magma sources during initial arc rifting revealed by melt inclusions," Nature Communications, Nature, vol. 15(1), pages 1-11, December.
    2. Xiao-Yu Zhang & Li-Hui Chen & Xiao-Jun Wang & Takeshi Hanyu & Albrecht W. Hofmann & Tsuyoshi Komiya & Kentaro Nakamura & Yasuhiro Kato & Gang Zeng & Wen-Xian Gou & Wei-Qiang Li, 2022. "Zinc isotopic evidence for recycled carbonate in the deep mantle," Nature Communications, Nature, vol. 13(1), pages 1-7, December.

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