Diapirism
Diapirism is a geological process in which a mobile, ductile subterranean material, typically salt or shale, intrudes into overlying rock layers through buoyancy-driven upward flow, forming dome-like structures known as diapirs.
161
Publications
9.7K
Citations
394
Authors
192
Institutions
Publications per year
2017–2026
17
Parents
161
1–5 of 161
394
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Islamic Azad University, Science and Research Branch, Iran
4 publications · 116 citations
4
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4
h-index
1–5 of 394
192

Uppsala University
Uppsala, Sweden
13 h-index
24 publications
1.8K citations
The University of Texas at Austin
Austin, United States
8 h-index
14 publications
3.5K citations

Bureau of Economic Analysis
Washington D.C., United States
6 h-index
12 publications
3.5K citations

Vrije Universiteit Amsterdam
Amsterdam, The Netherlands
5 h-index
9 publications
612 citations
Equinor (Norway)
Stavanger, Norway
5 h-index
10 publications
570 citations

Durham University
Durham, United Kingdom
4 h-index
4 publications
156 citations
Istituto di Scienze Marine del Consiglio Nazionale delle Ricerche
Venice, Italy
4 h-index
5 publications
156 citations

University of Milan
Milan, Italy
4 h-index
6 publications
741 citations
1–8 of 192
14 publications · 1.5K citations
13
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13 publications · 639 citations
11
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10 publications · 774 citations
10
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8 publications · 1.3K citations
8
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8 publications · 349 citations
8
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1–5