Evidence for the solar wind in lunar magmas: A study of slowly cooled samples of the Apollo 12 olivine basalt suite

Author:

Singer Jack A.1,Greenwood James P.1,Itoh Shoichi23,Sakamoto Naoya2,Yurimoto Hisayoshi2

Affiliation:

1. Department of Earth & Environmental Sciences, Wesleyan University

2. Department of Natural History Sciences, Hokkaido University

3. Department of Earth and Planetary Sciences, Kyoto University

Publisher

Geochemical Society of Japan

Subject

Geochemistry and Petrology,Geophysics

Reference45 articles.

1. Albarède, F., Albalat, E. and Lee, C.-T. A. (2015) An intrinsic volatility scale relevant to the Earth and Moon and the status of water in the Moon. Meteor. Planet. Sci. 50, 568–577.

2. Baldridge, W. S., Beatty, D. W., Hill, S. M. R. and Albee, A. L. (1979) The petrology of the Apollo 12 pigeonite basalt suite. Proc. 10th Lunar Planet. Sci. Conf. 1, 141–179.

3. Boyce, J. W., Liu, Y., Rossman, G. R., Guan, Y., Eiler, J. M., Stolper, E. M. and Taylor, L. A. (2010) Lunar apatite with terrestrial volatile abundances. Nature 466, 466–470.

4. Boyce, J. W., Tomlinson, S. M., McCubbin, F. M., Greenwood, J. P. and Treiman, A. H. (2014) The lunar apatite paradox. Science 344, 400–402.

5. Champness, P. E., Dunham, A. C., Gibb, F. G. F., Giles, H. N., MacKenzie, W. S., Stumpfl, E. F. and Zussman, J. (1971) Mineralogy and petrology of some Apollo 12 lunar samples. Proc. 2nd Lunar and Planet. Sci. Conf. 1, 359–376.

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