Pb-204, Bi, Tl, and Zn have been measured in Apollo 16 samples and Apollo 17 orange soil. These data in addition to already reported Apollo 14 and 15 Pb-204 results and literature data are used to support the Pb-204-metallic phase coherence. The partition of Pb-204 into very fine metallic grains appears to be the result of an impact process rather than metal segregation in a magma.


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    Titel :

    A study of Pb-204 partition in lunar samples using terrestrial and meteoritic analogues


    Beteiligte:
    Allen, R. O., Jr. (Autor:in) / Jovanovic, S. (Autor:in) / Reed, G. W., Jr. (Autor:in)

    Kongress:

    Lunar Science Conference ; 1974 ; Houston, TX


    Erscheinungsdatum :

    01.01.1974


    Medientyp :

    Sonstige


    Format :

    Keine Angabe


    Sprache :

    Englisch