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. Additional information is contained in the original extended abstract.


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    Titel :

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


    Beteiligte:
    Zeigler, R. A. (Autor:in) / Jolliff, B. L. (Autor:in) / Korotev, R. L. (Autor:in) / Kremser, D. T. (Autor:in) / Haskin, L. A. (Autor:in)


    Erscheinungsdatum :

    01.01.2001


    Medientyp :

    Aufsatz (Konferenz)


    Format :

    Keine Angabe


    Sprache :

    Englisch




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