Trace Element Fractionation

Trace Element Fractionation is a geochemical process characterized by the preferential partitioning of trace elements between coexisting phases during magmatic crystallization, metamorphic reactions, or weathering transformations, driven by differences in ionic radius, valence state, and site occupancy that distinguish it from major element behavior.

243

Publications

34.2K

Citations

764

Authors

338

Institutions

Publications per year

2017–2026

30

Authors

764

  1. LG
    Lawrence Grossman

    University of Chicago, United States

    5 publications · 517 citations

    5

    h-index

  2. MJ
    M. J. Drake

    University of Arizona, United States

    4 publications · 262 citations

    4

    h-index

  3. JH
    J. H. Jones

    Johnson Space Center, United States

    4 publications · 319 citations

    4

    h-index

  4. BJ
    Bernard J. Wood

    University of Bristol, United Kingdom

    4 publications · 869 citations

    4

    h-index

  5. RG
    R. Ganapathy

    University of Chicago, United States

    3 publications · 340 citations

    3

    h-index

1–5 of 764

Venues

  1. Geochimica et Cosmochimica Acta

    44 publications · 7.7K citations

    33

    h-index

  2. Chemical Geology

    17 publications · 1.7K citations

    17

    h-index

  3. Earth and Planetary Science Letters

    16 publications · 10K citations

    16

    h-index

  4. Contributions to Mineralogy and Petrology

    15 publications · 2.9K citations

    15

    h-index

  5. Journal of Petrology

    15 publications · 2.2K citations

    15

    h-index

1–5