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.
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Publications
22.8K
Citations
1.4K
Authors
570
Institutions
Publications per year
2017–2026
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Chinese Academy of Sciences
Beijing, China
16 h-index
51 publications
2.3K citations

Centre National de la Recherche Scientifique
Paris, France
12 h-index
29 publications
1.6K citations

Scripps Institution of Oceanography
La Jolla, United States
8 h-index
18 publications
1.3K citations
University of Chinese Academy of Sciences
Beijing, China
7 h-index
13 publications
535 citations
United States Geological Survey
Reston, United States
6 h-index
13 publications
1.4K citations
The University of Tokyo
Tokyo, Japan
6 h-index
20 publications
1.2K citations
Qingdao National Laboratory for Marine Science and Technology
Qingdao, China
6 h-index
23 publications
705 citations
ETH Zurich
Zurich, Switzerland
5 h-index
10 publications
806 citations
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17 publications · 1.4K citations
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18 publications · 1.4K citations
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13 publications · 1K citations
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11 publications · 1.7K citations
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10 publications · 381 citations
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