Igneous Partition Coefficients
Igneous Partition Coefficient is a dimensionless geochemical parameter that quantifies the equilibrium distribution of a trace element between a crystalline silicate mineral and a coexisting silicate melt during igneous differentiation, defined as the ratio of the element's concentration in the solid phase to that in the liquid phase.
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Ilya V. Veksler, A. M. Dorfman, Maya Kamenetsky et al. · Geochimica et Cosmochimica Acta · 2005 · 228 citations · Full text
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University of New Mexico
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National Museum of Natural History
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Sorbonne Université
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Vrije Universiteit Amsterdam
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Freie Universität Berlin
Berlin, Germany
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British Museum
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Earth and Space Research
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