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Petrology and Geochemistry of Lunar Regolith Particle 65903,16-7: Evidence for Extreme Reduction and OxidationApollo 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. Additional information is contained in the original extended abstract.
Document ID
20010044671
Acquisition Source
Goddard Space Flight Center
Document Type
Conference Paper
Authors
Zeigler, R. A. (Washington Univ. Saint Louis, MO United States)
Jolliff, B. L. (Washington Univ. Saint Louis, MO United States)
Korotev, R. L. (Washington Univ. Saint Louis, MO United States)
Kremser, D. T. (Washington Univ. Saint Louis, MO United States)
Haskin, L. A. (Washington Univ. Saint Louis, MO United States)
Date Acquired
August 20, 2013
Publication Date
January 1, 2001
Publication Information
Publication: Lunar and Planetary Science XXXII
Subject Category
Lunar And Planetary Science And Exploration
Funding Number(s)
CONTRACT_GRANT: NAG5-4172
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.

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