Petrology and Geochemistry of Lunar Regolith Particle 65903,16-7: Evidence for Extreme

Details Petrology and Geochemistry of Lunar Regolith Particle 65903,16-7: Evidence for Extreme Petrology and Geochemistry of Lunar Regolith Particle 65903,16-7: Evidence for Extreme

Mar 2001

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2001lpi....32.1242r&link_type=abstract

32nd Annual Lunar and Planetary Science Conference, March 12-16, 2001, Houston, Texas, abstract no.1242

Physics

Scientific paper

Apollo 16 particle 65903,16-7 is a magnesian, alkali-rich impact melt
breccia. Low Fe/Mn and high phosphide/phosphate ratios are evidence of
severe reduction during impact-melt cooling. Presence of carbonate and
FeOOH is evidence for later oxidation.

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