Trace Element Enrichment

Trace Element Enrichment is a hydrothermal geochemical phenomenon characterized by the selective concentration of minor and trace elements in submarine vent fluids relative to seawater, driven by water-rock interactions, phase separation, and redox processes distinct from major element cycling.

405

Publications

22.8K

Citations

1.4K

Authors

570

Institutions

Publications per year

2017–2026

92

Authors

1.4K

  1. GD
    G.R. Davies

    Vrije Universiteit Amsterdam, Netherlands

    6 publications · 765 citations

    6

    h-index

  2. JD
    Jonathan D. Cooper

    King's College London, United Kingdom

    5 publications · 179 citations

    5

    h-index

  3. UB
    U.A.Th. Brinkman

    Vrije Universiteit Amsterdam, Netherlands

    5 publications · 152 citations

    5

    h-index

  4. CW
    Cameron W. McLeod

    University of Sheffield, United Kingdom

    4 publications · 134 citations

    4

    h-index

  5. ED
    Edward D. Burton

    Southern Cross University, Australia

    4 publications · 141 citations

    4

    h-index

1–5 of 1.4K

Venues

  1. Journal of Petrology

    17 publications · 1.4K citations

    16

    h-index

  2. Chemical Geology

    18 publications · 1.4K citations

    15

    h-index

  3. Geochimica et Cosmochimica Acta

    13 publications · 1K citations

    12

    h-index

  4. Earth and Planetary Science Letters

    11 publications · 1.7K citations

    11

    h-index

  5. Journal of Chromatography A

    10 publications · 381 citations

    10

    h-index

1–5