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Forest Vale

Xenon in chondritic metal. Marti et al. (1989) have identified a xenon component (FVM-Xe) in a metal separate of the Forest Vale (H4) chondrite which appears to be distinct from xenon identified in other solar system reservoirs. It is characterized by relative abundances of the heaviest isotopes with unusually high " Xe. A possible e mlanation is recoil of fission fragments into the metal grains, possibly from Pu, " Tm or neutron induced fission of (Marti et al. 1989). This suggestion is consistent with the observed grain size dependence of FVM which favors a near-surface location. [Pg.91]

See other pages where Forest Vale is mentioned: [Pg.325]    [Pg.325]    [Pg.283]    [Pg.441]    [Pg.520]    [Pg.2499]    [Pg.325]    [Pg.325]    [Pg.283]    [Pg.441]    [Pg.520]    [Pg.2499]    [Pg.92]   
See also in sourсe #XX -- [ Pg.283 ]



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