Oxygen isotopic evidence for accretion of Earth’s water before a high-energy Moon-forming giant impact

  • Richard C. Greenwood
    Planetary and Space Sciences, School of Physical Sciences, The Open University, Walton Hall, Milton Keynes MK7 6AA, UK.
  • Jean-Alix Barrat
    Université de Bretagne Occidentale, Institut Universitaire Européen de la Mer, Laboratoire Géosciences Océan (CNRS UMR 6538), Plouzané, France.
  • Martin F. Miller
    Planetary and Space Sciences, School of Physical Sciences, The Open University, Walton Hall, Milton Keynes MK7 6AA, UK.
  • Mahesh Anand
    Planetary and Space Sciences, School of Physical Sciences, The Open University, Walton Hall, Milton Keynes MK7 6AA, UK.
  • Nicolas Dauphas
    Origins Laboratory, Department of the Geophysical Sciences and Enrico Fermi Institute, The University of Chicago, 5734 South Ellis Avenue, Chicago, IL 60637, USA.
  • Ian A. Franchi
    Planetary and Space Sciences, School of Physical Sciences, The Open University, Walton Hall, Milton Keynes MK7 6AA, UK.
  • Patrick Sillard
    Centre de recherche en économie et statistique, 5 avenue Henry Le Chatelier, 91120 Palaiseau, France.
  • Natalie A. Starkey
    Planetary and Space Sciences, School of Physical Sciences, The Open University, Walton Hall, Milton Keynes MK7 6AA, UK.

書誌事項

公開日
2018-03-02
DOI
  • 10.1126/sciadv.aao5928
公開者
American Association for the Advancement of Science (AAAS)

説明

<jats:p>We show that the bulk of Earth’s water was delivered before the high-energy collision that led to the formation of the Moon.</jats:p>

収録刊行物

  • Science Advances

    Science Advances 4 (3), eaao5928-, 2018-03-02

    American Association for the Advancement of Science (AAAS)

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