Comment on "Fractional crystallization of iron meteorites: Constant versus changing partition coefficients" by J. H. Jones 352 (1995).

Details Comment on "Fractional crystallization of iron meteorites: Constant versus changing partition coefficients" by J. H. Jones 352 (1995). Comment on "Fractional crystallization of iron meteorites: Constant versus changing partition coefficients" by J. H. Jones 352 (1995).

May 1995

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1995metic..30..352m&link_type=abstract

Meteoritics, vol. 30, p. 352 (1995).

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Scientific paper

Jones (1994) demonstrated that fractional crystallization of llIAB
iron meteorites may result in a log Au vs. log Ni plot of constant
slope even though kAu and kNi change. Jones'
example is a special case, however, and does not necessarily describe
behavior by other elements or in other metallic magmas.

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