Thermal Subsidence
Thermal Subsidence is a geological process in basin evolution whereby lithospheric cooling and associated densification following tectonic extension or magmatic underplating lead to progressive, long-term subsidence of the crust and formation of sedimentary basins.
340
Publications
22.7K
Citations
949
Authors
371
Institutions
Publications per year
2017–2026
33
Parents
340
A Neoproterozoic Snowball Earth
Paul F. Hoffman, Alan J. Kaufman, Galen P. Halverson et al. · Science · 1998 · 2.7K citations
Episodic Rifting and Subsidence in the South China Sea
John D. Pigott Ke Ru · AAPG Bulletin · 1986 · 523 citations
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371

Centre National de la Recherche Scientifique
Paris, France
12 h-index
29 publications
1.3K citations

Chinese Academy of Sciences
Beijing, China
12 h-index
49 publications
1.6K citations
Institute of Geology and Geophysics
Beijing, China
11 h-index
31 publications
1.1K citations
University of Chinese Academy of Sciences
Beijing, China
9 h-index
17 publications
375 citations
Dalhousie University
Halifax, Canada
8 h-index
15 publications
781 citations

Lamont-Doherty Earth Observatory
Sparkill, United States
8 h-index
13 publications
1.2K citations

University of Liverpool
Liverpool, United Kingdom
7 h-index
10 publications
485 citations
BP (United Kingdom)
London, United Kingdom
7 h-index
12 publications
469 citations
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32 publications · 1.8K citations
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JGS · 21 publications · 1.6K citations
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16 publications · 1.4K citations
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19 publications · 1.3K citations
16
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16 publications · 777 citations
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