A ferroan region of the lunar highlands as recorded in meteorites MAC88104 and MAC88105

Details A ferroan region of the lunar highlands as recorded in meteorites MAC88104 and MAC88105 A ferroan region of the lunar highlands as recorded in meteorites MAC88104 and MAC88105

Nov 1991

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1991gecoa..55.3051j&link_type=abstract

(The MacAlpine Hills Lunar Meteorite Consortium - Lunar and Planetary Science Conference, 21st, Special Session, Houston, TX, Ma

Computer Science

17

Anorthosite, Breccia, Impact Melts, Lunar Crust, Meteoritic Composition, Aluminum Oxides, Glass, Igneous Rocks, Metamorphism (Geology), Space Debris, Trace Elements

Scientific paper

MAC88104 and 88105, paired meteorites of noritic anorthosite composition, are examined. Results indicate that these meteorites contain a variety of materials including impact-melt breccias, igneous and metamorphosed bressia clasts, glass clasts and veins, mineral clasts, and extralunar meteoritic debris. Compositions of the bulk meteorite and its components suggest that it came from a region of the moon's crust that was highly aluminous, low in incompatible trace elements, and ferroan in character.

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