Mineralogy of Dhofar 309, 489, and Yamato-86032 and Varieties of Lithologies of the Lunar Farside Crust

Details Mineralogy of Dhofar 309, 489, and Yamato-86032 and Varieties of Lithologies of the Lunar Farside Crust Mineralogy of Dhofar 309, 489, and Yamato-86032 and Varieties of Lithologies of the Lunar Farside Crust

Mar 2007

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007lpi....38.1607t&link_type=abstract

38th Lunar and Planetary Science Conference, (Lunar and Planetary Science XXXVIII), held March 12-16, 2007 in League City, Texas

Physics

2

Scientific paper

Dhofar 489 and Yamato(Y)-86032 are keys to understanding the lunar
farside crust. Mg-rich anorthosites were found in Dhofar 309, as well as
Dhofar 489. Fe-rich anorthosite with negative epsilon Nd in Y-86032
requires the crustal formation process of farsi

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