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- W2007923596 abstract "Trace element analyses using proton induced x-ray emission (PIXE) and synchrotron x-ray fluorescence (SXRF) have been made on metal and troilite from 9 iron meteorites representing 5 geochemical groups. Nickel and copper distribution coefficients D (troilitemetal) vary by factors of 600 and 20, respectively, correlate positively with kamacite band width and correlate negatively with bulk nickel content. Meteorites with bulk Ni < 10% have Cu-enriched troilite (DCu > 1) while those with Ni > 10% have Cu-depleted troilite (DCu < 1). Since magmatic evolution and partial melting will produce Cu-enriched troilite only, the observation of Cu-depleted troilite in Ni-rich meteorites is evidence for subsolidus re-equilibration, a process which reduces DCu by transfer of Cu to exsolving metal. Elemental redistribution may have played an important role in establishing the present chemical trends in iron meteorites." @default.
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- W2007923596 date "1987-10-01" @default.
- W2007923596 modified "2023-09-26" @default.
- W2007923596 title "Copper and nickel partitioning in iron meteorites" @default.
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- W2007923596 doi "https://doi.org/10.1016/0016-7037(87)90146-3" @default.
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