Subduction-collision Transition
Subduction-Collision Transition is a geodynamic process denoting the shift from oceanic subduction to continental collision within convergent plate margins, characterized by the cessation of slab pull and the onset of crustal thickening due to buoyant continental lithosphere entering the subduction zone.
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Zagros orogeny: a subduction-dominated process
Philippe Agard, Jafar Omrani, Laurent Jolivet et al. · Geological Magazine · 2011 · 960 citations · Full text
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Centre National de la Recherche Scientifique
Paris, France
24 h-index
62 publications
6.4K citations

Chinese Academy of Sciences
Beijing, China
14 h-index
48 publications
7K citations

Peking University
Beijing, China
13 h-index
19 publications
3.1K citations

China University of Geosciences (Beijing)
Beijing, China
13 h-index
32 publications
2.4K citations

Sorbonne Université
Paris, France
12 h-index
26 publications
5.3K citations

Chinese Academy of Geological Sciences
Beijing, China
12 h-index
35 publications
2.8K citations

National Taiwan University
Taipei, Taiwan
11 h-index
15 publications
2.1K citations
Institute of Geology and Geophysics
Beijing, China
10 h-index
25 publications
5.1K citations
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