Oxygen isotopic evidence for accretion of Earth’s water before a high-energy Moon-forming giant impact
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- Richard C. Greenwood
- Planetary and Space Sciences, School of Physical Sciences, The Open University, Walton Hall, Milton Keynes MK7 6AA, UK.
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- Jean-Alix Barrat
- Université de Bretagne Occidentale, Institut Universitaire Européen de la Mer, Laboratoire Géosciences Océan (CNRS UMR 6538), Plouzané, France.
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- Martin F. Miller
- Planetary and Space Sciences, School of Physical Sciences, The Open University, Walton Hall, Milton Keynes MK7 6AA, UK.
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- Mahesh Anand
- Planetary and Space Sciences, School of Physical Sciences, The Open University, Walton Hall, Milton Keynes MK7 6AA, UK.
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- 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.
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- Ian A. Franchi
- Planetary and Space Sciences, School of Physical Sciences, The Open University, Walton Hall, Milton Keynes MK7 6AA, UK.
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- Patrick Sillard
- Centre de recherche en économie et statistique, 5 avenue Henry Le Chatelier, 91120 Palaiseau, France.
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- 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
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- 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
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- Science Advances
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Science Advances 4 (3), eaao5928-, 2018-03-02
American Association for the Advancement of Science (AAAS)