Planetary Isostasy
Planetary Isostasy is a geophysical theory in planetary geophysics that describes the large-scale gravitational and buoyant equilibrium of a planet’s or moon’s outer shell, in which surface loads and topography are compensated by variations in crustal/lithospheric thickness or density above a deeper, nearly hydrostatic interior.
149
Publications
10.1K
Citations
420
Authors
178
Institutions
Publications per year
2017–2026
12
149
Isostasy and Flexure of the Lithosphere
Marcia McNutt · Eos · 2002 · 1.2K citations · Full text
On the role of isostasy in the evolution of normal fault systems
Brian P. Wernicke, Gary J. Axen · Geology · 1988 · 586 citations
Earth Rheology, Isostasy and Eustasy
Andrew Goudie, Nils‐Axel Mörner, Nils‐Axel Mörner · Geographical Journal · 1982 · 470 citations
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178
University of Arizona
Tucson, United States
13 h-index
15 publications
755 citations
Jet Propulsion Laboratory
Pasadena, United States
12 h-index
19 publications
1.4K citations
Planetary Science Institute
Tucson, United States
9 h-index
17 publications
1.9K citations
California Institute of Technology
Pasadena, United States
8 h-index
22 publications
5.6K citations
Columbia University
New York, United States
7 h-index
10 publications
567 citations
Massachusetts Institute of Technology
Cambridge, United States
7 h-index
18 publications
973 citations

Lamont-Doherty Earth Observatory
Sparkill, United States
6 h-index
9 publications
493 citations
Goddard Space Flight Center
Greenbelt, United States
5 h-index
5 publications
372 citations
1–8 of 178
35 publications · 1.9K citations
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JGR · 10 publications · 700 citations
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9 publications · 320 citations
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7 publications · 217 citations
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7 publications · 191 citations
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