Lithospheric Delamination
Lithospheric Delamination is a geodynamic process in which the dense lower portion of the continental lithosphere detaches and sinks into the underlying asthenosphere, driven by gravitational instability, thereby enabling replacement with hotter, more buoyant mantle material and influencing mountain building and surface uplift.
189
Publications
18.8K
Citations
607
Authors
256
Institutions
Publications per year
2017–2026
65
189
T. Mark Harrison, Peter Copeland, W. S. F. Kidd et al. · Science · 1992 · 1.3K citations
Svend Duggen, Kaj Hoernle, Paul van den Bogaard et al. · Journal of Petrology · 2005 · 531 citations · Full text
Delamination and recycling of Archaean crust caused by gravitational instabilities
Tim Johnson, Michael Brown, Boris Kaus et al. · Nature Geoscience · 2013 · 463 citations · Full text
1–5 of 189
607
7
h-index
5
h-index
5
h-index
4
h-index
4
h-index
1–5 of 607
256

Chinese Academy of Sciences
Beijing, China
22 h-index
75 publications
4.1K citations
Institute of Geology and Geophysics
Beijing, China
14 h-index
36 publications
2.7K citations

China University of Geosciences (Beijing)
Beijing, China
11 h-index
29 publications
3.5K citations
China University of Geosciences
Wuhan, China
11 h-index
40 publications
2.7K citations
Guangzhou Institute of Geochemistry
Guangzhou, China
10 h-index
32 publications
1.2K citations
GFZ Helmholtz Centre for Geosciences
Potsdam, Germany
9 h-index
23 publications
1.3K citations
University of Chinese Academy of Sciences
Beijing, China
9 h-index
19 publications
1.1K citations

Centre National de la Recherche Scientifique
Paris, France
9 h-index
9 publications
1.3K citations
1–8 of 256
JGR · 14 publications · 3K citations
14
h-index
13 publications · 1.1K citations
13
h-index
13 publications · 1.4K citations
13
h-index
13 publications · 851 citations
13
h-index
GJI · 10 publications · 510 citations
10
h-index
1–5