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.

25

Publications

2.8K

Citations

65

Authors

57

Institutions

Publications per year

2017–2026

6

Authors

65

  1. RL
    Roger L. Nielsen

    Oregon State University, United States

    2 publications · 87 citations

    2

    h-index

  2. GA
    G. A. McKay

    Johnson Space Center, United States

    2 publications · 162 citations

    2

    h-index

  3. JA
    J. A. Philpotts

    Goddard Space Flight Center, United States

    1 publications · 731 citations

    1

    h-index

  4. DB
    Donald B. Dingwell

    Ludwig-Maximilians-Universität München, Germany

    1 publications · 228 citations

    1

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  5. MT
    Massimo Tiepolo

    Institute of Geosciences and Earth Resources, Italy

    1 publications · 87 citations

    1

    h-index

1–5 of 65

Venues

  1. Geochimica et Cosmochimica Acta

    4 publications · 1K citations

    4

    h-index

  2. American Mineralogist

    4 publications · 140 citations

    4

    h-index

  3. Chemical Geology

    3 publications · 807 citations

    3

    h-index

  4. Meteoritics

    1 publications · 18 citations

    1

    h-index

  5. Journal of Geophysical Research Atmospheres

    JGR · 1 publications · 27 citations

    1

    h-index

1–5