Planetary Subsidence
Planetary Subsidence is the large-scale downward vertical displacement of a planet’s lithospheric surface due to internal or external forces, distinguished from other tectonic deformations by its sustained, often gradual, sinking motion resulting from processes such as mantle convection, cooling, or loading.
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170
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108
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2017–2026
9
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Tectonic discrimination of granitoids
P.D. Maniar, Philip M. Piccoli · Geological Society of America Bulletin · 1989 · 4.6K citations
Robert P. Sharp · Journal of Geophysical Research Atmospheres · 1973 · 144 citations · Full text
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Japan Agency for Marine-Earth Science and Technology, Japan
2 publications · 142 citations
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Planetary Science Institute
Tucson, United States
7 h-index
11 publications
10.3K citations
United States Geological Survey
Reston, United States
4 h-index
6 publications
454 citations
California Institute of Technology
Pasadena, United States
4 h-index
4 publications
281 citations

Centre National de la Recherche Scientifique
Paris, France
3 h-index
4 publications
329 citations
Deutsches Zentrum für Luft- und Raumfahrt e. V. (DLR)
Cologne, Germany
3 h-index
3 publications
95 citations

Lunar and Planetary Institute
Houston, United States
3 h-index
6 publications
128 citations
Brown University
Providence, United States
3 h-index
8 publications
522 citations

Southwest Research Institute
San Antonio, United States
3 h-index
8 publications
255 citations
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10 publications · 662 citations
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JGR · 7 publications · 713 citations
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4 publications · 4.9K citations
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2 publications · 86 citations
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2 publications · 54 citations
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