Lithospheric Cooling
Lithospheric Cooling is a geophysical process in which the oceanic lithosphere gradually loses heat to the overlying hydrosphere and atmosphere as it moves away from a mid-ocean ridge, resulting in progressive thermal contraction, thickening, and increased density with age.
161
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11.6K
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359
Authors
195
Institutions
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2017–2026
12
161
Melt-rich channel observed at the lithosphere–asthenosphere boundary
Samer Naif, Kerry Key, Steven Constable et al. · Nature · 2013 · 285 citations
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Laboratoire d’Études en Géophysique et Océanographie Spatiales, France
6 publications · 209 citations
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Massachusetts Institute of Technology
Cambridge, United States
10 h-index
16 publications
1.2K citations

Lamont-Doherty Earth Observatory
Sparkill, United States
7 h-index
10 publications
1.4K citations
Columbia University
New York, United States
7 h-index
10 publications
1.4K citations

Centre National de la Recherche Scientifique
Paris, France
6 h-index
16 publications
888 citations
Woods Hole Oceanographic Institution
Falmouth, United States
5 h-index
7 publications
1.1K citations

National Oceanography Centre
Southampton, United Kingdom
5 h-index
6 publications
185 citations
GFZ Helmholtz Centre for Geosciences
Potsdam, Germany
5 h-index
17 publications
1.8K citations

Chinese Academy of Sciences
Beijing, China
5 h-index
13 publications
683 citations
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JGR · 27 publications · 2.6K citations
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21 publications · 1.7K citations
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15 publications · 1.6K citations
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12 publications · 404 citations
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11 publications · 1.5K citations
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