Discovery of moganite in a lunar meteorite as a trace of H 2 O ice in the Moon’s regolith-Reference-Cited by-同舟云学术

Discovery of moganite in a lunar meteorite as a trace of H 2 O ice in the Moon’s regolith

Published:2018-05-04 Issue:5 Volume:4 Page:
ISSN:2375-2548
Container-title:Science Advances
language:en
Short-container-title:Sci. Adv.

Author:

Kayama Masahiro¹²^ORCID,Tomioka Naotaka³^ORCID,Ohtani Eiji¹^ORCID,Seto Yusuke⁴,Nagaoka Hiroshi⁵^ORCID,Götze Jens⁶^ORCID,Miyake Akira⁷,Ozawa Shin¹^ORCID,Sekine Toshimori⁸⁹,Miyahara Masaaki⁸^ORCID,Tomeoka Kazushige⁴,Matsumoto Megumi⁴,Shoda Naoki⁴^ORCID,Hirao Naohisa¹⁰^ORCID,Kobayashi Takamichi¹¹

Affiliation:

1. Department of Earth and Planetary Materials Science, Graduate School of Science, Tohoku University, Sendai 980-8578, Japan.

2. Creative Interdisciplinary Research Division, Frontier Research Institute for Interdisciplinary Sciences, Tohoku University, Sendai 980-8578, Japan.

3. Kochi Institute for Core Sample Research, Japan Agency for Marine-Earth Science and Technology, 200 Monobe Otsu, Nankoku, Kochi 783-8502, Japan.

4. Department of Planetology, Graduate School of Science, Kobe University, 1-1 Rokkodai-cho, Nada-ku, Kobe 657-8501, Japan.

5. Research Institute for Science and Engineering, Waseda University, Shinjuku, Tokyo 169-8555, Japan.

6. TU Bergakademie Freiberg, Institute of Mineralogy, Brennhausgasse 14, 09596 Freiberg, Germany.

7. Department of Geology and Mineralogy, Graduate School of Science, Kyoto University, Kitashirakawa-Oiwake, Sakyo-ku, Kyoto 606-8502, Japan.

8. Department of Earth and Planetary Systems Science, Graduate School of Science, Hiroshima University, Higashi-Hiroshima 739-8526, Japan.

9. Center for High Pressure Science and Technology Advanced Research, Pudong, Shanghai 201203, P.R. China.

10. Japan Synchrotron Radiation Research Institute, 1-1-1 Kouto Sayo, Hyogo 679-5198, Japan.

11. National Institute for Materials Science, 1-1 Namiki, Tsukuba, Ibaraki 305-0044, Japan.

Abstract

Discovery of moganite in a lunar meteorite indicates the possibility of H 2 O ice accumulated in the Moon’s regolith.

Funder

JSPS KAKENHI

Grant-in-Aid award for Scientific Research

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference40 articles.

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