Seafloor Venting
Seafloor Venting is a geological process in which heated, mineral-rich fluids are expelled from the ocean floor through fissures or hydrothermal vents, typically at tectonic plate boundaries, as a result of subsurface magmatic and hydrothermal activity.
58
Publications
3.1K
Citations
296
Authors
149
Institutions
Publications per year
2017–2026
10
Parents
58
1–5 of 58
296
Woods Hole Oceanographic Institution, United States
4 publications · 411 citations
4
h-index
Observatoire Océanologique de Banyuls-sur-Mer, France
3 publications · 173 citations
3
h-index
2
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2
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2
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1–5 of 296
149
Woods Hole Oceanographic Institution
Falmouth, United States
6 h-index
22 publications
2.3K citations

Centre National de la Recherche Scientifique
Paris, France
5 h-index
5 publications
380 citations
The University of Texas at Austin
Austin, United States
5 h-index
10 publications
411 citations
University of Washington
Seattle, United States
4 h-index
5 publications
462 citations
Geological Survey of Canada
Ottawa, Canada
4 h-index
10 publications
235 citations
Ifremer
Brest, France
4 h-index
10 publications
614 citations

Monterey Bay Aquarium Research Institute
Castroville, United States
4 h-index
13 publications
456 citations

National Oceanography Centre
Southampton, United Kingdom
3 h-index
6 publications
420 citations
1–8 of 149
5 publications · 439 citations
5
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5 publications · 196 citations
5
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5 publications · 195 citations
5
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2 publications · 187 citations
2
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JGR · 2 publications · 151 citations
2
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1–5