Off-axis Hydrothermal Activity
Off-Axis Hydrothermal Activity is a geological phenomenon characterized by the circulation of heated fluids and associated mineral deposition occurring distal to the primary axis of mid-ocean ridge spreading centers, distinguished from on-axis systems by its spatial separation from the neovolcanic zone and often associated with tectonically driven permeability in the oceanic crust.
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An off-axis hydrothermal vent field near the Mid-Atlantic Ridge at 30° N
Deborah S. Kelley, Jeffrey A. Karson, Donna K. Blackman et al. · Nature · 2001 · 1.1K citations
30,000 Years of Hydrothermal Activity at the Lost City Vent Field
Gretchen L. Früh‐Green, Deborah S. Kelley, Stefano M. Bernasconi et al. · Science · 2003 · 415 citations
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Woods Hole Oceanographic Institution
Falmouth, United States
10 h-index
16 publications
634 citations

GEOMAR Helmholtz Centre for Ocean Research Kiel
Kiel, Germany
7 h-index
21 publications
1.5K citations
University of Washington
Seattle, United States
6 h-index
21 publications
13.7K citations
United States Geological Survey
Reston, United States
6 h-index
12 publications
550 citations
University of Bremen
Bremen, Germany
5 h-index
7 publications
272 citations

Scripps Institution of Oceanography
La Jolla, United States
5 h-index
10 publications
2.5K citations

Centre National de la Recherche Scientifique
Paris, France
5 h-index
23 publications
445 citations
NOAA Pacific Marine Environmental Laboratory
Seattle, United States
5 h-index
13 publications
4.8K citations
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JGR · 10 publications · 808 citations
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9 publications · 1.3K citations
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7 publications · 158 citations
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7 publications · 162 citations
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5 publications · 1.6K citations
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