Continental Underthrusting
Continental Underthrusting is a tectonic process in which one continental plate is forced beneath another at a convergent plate boundary, distinguished from subduction by the limited penetration of buoyant continental crust into the mantle.
141
Publications
15.3K
Citations
503
Authors
232
Institutions
Publications per year
2017–2026
21
Parents
141
Partially Molten Middle Crust Beneath Southern Tibet: Synthesis of Project INDEPTH Results
K. D. Nelson, Wenjin Zhao, L. D. Brown et al. · Science · 1996 · 1.2K citations
Deep seismic reflection evidence for continental underthrusting beneath southern Tibet
Wenjin Zhao, K. D. Nelson, J. Quo et al. · Nature · 1993 · 721 citations
1–5 of 141
503
4
h-index
4
h-index
4
h-index
3
h-index
3
h-index
1–5 of 503
232

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

Chinese Academy of Sciences
Beijing, China
8 h-index
24 publications
1.4K citations
GFZ Helmholtz Centre for Geosciences
Potsdam, Germany
7 h-index
16 publications
3.2K citations
Massachusetts Institute of Technology
Cambridge, United States
6 h-index
10 publications
1.2K citations
Institute of Tibetan Plateau Research
Beijing, China
5 h-index
16 publications
825 citations
United States Geological Survey
Reston, United States
5 h-index
12 publications
1.1K citations
Center for Excellence in Tibetan Plateau Earth Sciences
Beijing, China
4 h-index
12 publications
705 citations
University of Chinese Academy of Sciences
Beijing, China
4 h-index
9 publications
215 citations
1–8 of 232
18 publications · 1.7K citations
18
h-index
JGR · 14 publications · 3.8K citations
13
h-index
10 publications · 1K citations
10
h-index
8 publications · 431 citations
8
h-index
7 publications · 406 citations
7
h-index
1–5