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Ratios of S, Se and Te in the silicate Earth require a volatile-rich late veneer

Author

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  • Zaicong Wang

    (Freie Universität Berlin, Institut für Geologische Wissenschaften, Malteserstrasse 74-100, 12249 Berlin, Germany)

  • Harry Becker

    (Freie Universität Berlin, Institut für Geologische Wissenschaften, Malteserstrasse 74-100, 12249 Berlin, Germany)

Abstract

Newly determined ratios and abundances of sulphur, selenium and tellurium in mantle peridotites are consistent with the view that a ‘late veneer’ of slightly volatile-depleted, carbonaceous-chondrite-like material supplied between 20 and 100 per cent of the silicate Earth’s highly volatile elements, such as hydrogen and carbon.

Suggested Citation

  • Zaicong Wang & Harry Becker, 2013. "Ratios of S, Se and Te in the silicate Earth require a volatile-rich late veneer," Nature, Nature, vol. 499(7458), pages 328-331, July.
    • Handle: RePEc:nat:nature:v:499:y:2013:i:7458:d:10.1038_nature12285
    DOI: 10.1038/nature12285
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    Cited by:

    1. Yifan Tian & Peiyu Zhang & Wei Zhang & Xiaolei Feng & Simon A. T. Redfern & Hanyu Liu, 2024. "Iron alloys of volatile elements in the deep Earth’s interior," Nature Communications, Nature, vol. 15(1), pages 1-7, December.
    2. Wenzhong Wang & Michael J. Walter & John P. Brodholt & Shichun Huang, 2024. "Early planetesimal differentiation and late accretion shaped Earth’s nitrogen budget," Nature Communications, Nature, vol. 15(1), pages 1-11, December.
    3. Lanlan Shi & Wenhua Lu & Takanori Kagoshima & Yuji Sano & Zenghao Gao & Zhixue Du & Yun Liu & Yingwei Fei & Yuan Li, 2022. "Nitrogen isotope evidence for Earth’s heterogeneous accretion of volatiles," Nature Communications, Nature, vol. 13(1), pages 1-15, December.

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