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Comment on “Fractional crystallization of iron meteorites: Constant versus changing partition coefficients” by J. H. Jones |
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| Authors: | John W Morgan |
| Abstract: | Abstract— Jones (1994) demonstrated that fractional crystallization of IIIAB 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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