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The isotopic nature of the Earth’s accreting material through time

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  • Nicolas Dauphas

    (Origins Laboratory, The University of Chicago, 5734 South Ellis Avenue)

Abstract

The mantle signatures of elements with distinct affinities for metal isotopically record different stages of Earth’s accretion, revealing that the Moon-forming impactor had a similar composition to the other impactors that made the Earth.

Suggested Citation

  • Nicolas Dauphas, 2017. "The isotopic nature of the Earth’s accreting material through time," Nature, Nature, vol. 541(7638), pages 521-524, January.
    • Handle: RePEc:nat:nature:v:541:y:2017:i:7638:d:10.1038_nature20830
    DOI: 10.1038/nature20830
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    Cited by:

    1. 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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