The chlorine isotope fingerprint of the lunar magma ocean

Author:

Boyce Jeremy W.12,Treiman Allan H.3ORCID,Guan Yunbin1ORCID,Ma Chi1,Eiler John M.1,Gross Juliane4,Greenwood James P.5,Stolper Edward M.1

Affiliation:

1. Division of Geological and Planetary Sciences, Caltech, 1200 East California Boulevard, Pasadena, CA 91125, USA.

2. Department of Earth, Planetary, and Space Sciences, University of California, Los Angeles, Los Angeles, CA 90095–1567, USA.

3. Lunar and Planetary Institute, 3600 Bay Area Boulevard, Houston, TX 77058, USA.

4. Department of Earth and Planetary Sciences, American Museum of Natural History, Central Park West at 79th Street, New York, NY 10024, USA.

5. Department of Earth and Environmental Sciences, Wesleyan University, Middletown, CT 06459, USA.

Abstract

The unusually heavy Cl of the Moon is related not to degassing of dry magmas but rather to the loss of Cl from the lunar magma ocean.

Funder

National Aeronautics and Space Administration

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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