Cenozoic kinematics of the Wenchuan-Maoxian fault implies crustal stacking rather than channel flow extrusion at the Tibetan plateau eastern margin (Longmen Shan)

G.E. Chenglong (1) , Philippe Hervé Leloup (2) , Yong Zheng (1) , Stéphane Scaillet (3, 4) , Laura Airaghi (3, 4) , Florian Duval (3) , Jinjiang Zhang , Haibing Li (1)

1 Key Laboratory of Deep‐Earth Dynamics of Ministry of Natural Resources, Institute of Geology, Chinese Academy of Geological Sciences, Beijing, China
2 LGL-TPE - Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement
3 ISTO - Institut des Sciences de la Terre d'Orléans - UMR7327
4 Géodynamique - UMR7327

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Domains: Sciences of the Universe [physics]

G.E. Chenglong, Philippe Hervé Leloup, Yong Zheng, Stéphane Scaillet, Laura Airaghi, et al.. Cenozoic kinematics of the Wenchuan-Maoxian fault implies crustal stacking rather than channel flow extrusion at the Tibetan plateau eastern margin (Longmen Shan). Tectonophysics, 2023, pp.229816. ⟨10.1016/j.tecto.2023.229816⟩. ⟨insu-04057375⟩