Subduction Termination
Subduction Termination is a geological process denoting the cessation of oceanic plate subduction at a convergent margin, distinguished by the collision of buoyant continental lithosphere that resists further descent into the mantle.
425
Publications
35.5K
Citations
1.4K
Authors
550
Institutions
Publications per year
2017–2026
129
Parents
425
1–5 of 425
1.4K
12
h-index
9
h-index
7
h-index
6
h-index
6
h-index
1–5 of 1.4K
550

Chinese Academy of Sciences
Beijing, China
29 h-index
142 publications
14.9K citations

Centre National de la Recherche Scientifique
Paris, France
22 h-index
77 publications
4.7K citations
Institute of Geology and Geophysics
Beijing, China
21 h-index
71 publications
8K citations
University of Chinese Academy of Sciences
Beijing, China
19 h-index
61 publications
2.9K citations

Chinese Academy of Geological Sciences
Beijing, China
16 h-index
40 publications
1.6K citations
ETH Zurich
Zurich, Switzerland
14 h-index
26 publications
3.4K citations

China University of Geosciences (Beijing)
Beijing, China
13 h-index
28 publications
1K citations

Sorbonne Université
Paris, France
12 h-index
23 publications
1.4K citations
1–8 of 550
32 publications · 3.6K citations
32
h-index
34 publications · 5.2K citations
29
h-index
36 publications · 2.8K citations
25
h-index
27 publications · 1.9K citations
21
h-index
26 publications · 2.2K citations
20
h-index
1–5