Oxygen isotopic evidence for accretion of Earth’s water before a high-energy Moon-forming giant impact-Reference-Cited by-同舟云学术

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

Published:2018-03-02 Issue:3 Volume:4 Page:
ISSN:2375-2548
Container-title:Science Advances
language:en
Short-container-title:Sci. Adv.

Author:

Greenwood Richard C.¹^ORCID,Barrat Jean-Alix²,Miller Martin F.¹³^ORCID,Anand Mahesh¹⁴^ORCID,Dauphas Nicolas⁵^ORCID,Franchi Ian A.¹^ORCID,Sillard Patrick⁶,Starkey Natalie A.¹

Affiliation:

1. Planetary and Space Sciences, School of Physical Sciences, The Open University, Walton Hall, Milton Keynes MK7 6AA, UK.

2. Université de Bretagne Occidentale, Institut Universitaire Européen de la Mer, Laboratoire Géosciences Océan (CNRS UMR 6538), Plouzané, France.

3. British Antarctic Survey, High Cross, Madingley Road, Cambridge CB3 0ET, UK.

4. Department of Mineralogy, The Natural History Museum, Cromwell Road, London SW7 5BD, UK.

5. Origins Laboratory, Department of the Geophysical Sciences and Enrico Fermi Institute, The University of Chicago, 5734 South Ellis Avenue, Chicago, IL 60637, USA.

6. Centre de recherche en économie et statistique, 5 avenue Henry Le Chatelier, 91120 Palaiseau, France.

Abstract

We show that the bulk of Earth’s water was delivered before the high-energy collision that led to the formation of the Moon.

Funder

Science and Technology Facilities Council

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference59 articles.

1. Origin of the Moon in a giant impact near the end of the Earth's formation

2. Making the Moon from a Fast-Spinning Earth: A Giant Impact Followed by Resonant Despinning

3. Forming a Moon with an Earth-like Composition via a Giant Impact

4. Identification of the giant impactor Theia in lunar rocks

5. Oxygen isotopic evidence for vigorous mixing during the Moon-forming giant impact

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