Vent Field Evolution
Vent Field Evolution is a geological process model that describes the temporal development and spatial reorganization of hydrothermal vent systems on the seafloor, distinguished by the dynamic interplay between magmatic activity, fluid circulation, and mineral deposition over successive stages of formation, maturation, and decline.
43
Publications
2.6K
Citations
202
Authors
96
Institutions
Publications per year
2017–2026
10
Parents
43
Rapid growth at deep-sea vents
Richard A. Lutz, Timothy M. Shank, Daniel J. Fornari et al. · Nature · 1994 · 228 citations
1–5 of 43
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Christian-Albrechts-Universität zu Kiel, Germany
3 publications · 174 citations
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1–5 of 202
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Woods Hole Oceanographic Institution
Falmouth, United States
6 h-index
10 publications
1K citations

GEOMAR Helmholtz Centre for Ocean Research Kiel
Kiel, Germany
5 h-index
14 publications
1.1K citations
University of Washington
Seattle, United States
4 h-index
6 publications
768 citations
University of California, Santa Barbara
Santa Barbara, United States
3 h-index
3 publications
509 citations
University of Bergen
Bergen, Norway
3 h-index
12 publications
1.4K citations
Stanford University
Stanford, United States
2 h-index
2 publications
77 citations
NOAA Pacific Marine Environmental Laboratory
Seattle, United States
2 h-index
5 publications
511 citations

Christian-Albrechts-Universität zu Kiel
Kiel, Germany
2 h-index
5 publications
491 citations
1–8 of 96
5 publications · 340 citations
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4 publications · 337 citations
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3 publications · 225 citations
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2 publications · 100 citations
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2 publications · 69 citations
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