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The Chlorine Isotope Composition of the Moon and Implications for an Anhydrous Mantle

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Science  27 Aug 2010:
Vol. 329, Issue 5995, pp. 1050-1053
DOI: 10.1126/science.1192606

Article Information

vol. 329 no. 5995 1050-1053

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History: 
  • Received for publication May 20, 2010
  • Accepted for publication July 26, 2010

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Author Information

  1. Z. D. Sharp1,*,
  2. C. K. Shearer1,2,
  3. K. D. McKeegan3,
  4. J. D. Barnes4 and
  5. Y. Q. Wang5
  1. 1Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, NM 87122, USA.
  2. 2Institute of Meteoritics, University of New Mexico, Albuquerque, NM 87122, USA.
  3. 3Department of Earth and Space Sciences, University of California, Los Angeles, CA 90095, USA.
  4. 4Department of Geological Sciences, University of Texas, Austin, TX 78712, USA.
  5. 5Materials Science and Technology Division, Los Alamos National Laboratory, Los Alamos, NM 87545, USA.
  1. *To whom correspondence should be addressed. E-mail: zsharp{at}unm.edu

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