Early Cretaceous (similar to 138-134 Ma) Forearc Ophiolite and Tectonomagmatic Patterns in Central Tibet: Subduction Termination and Re-initiation of Meso-Tethys Ocean Caused by Collision of an Oceanic Plateau at the Continental Margin?-MedSci.cn

Early Cretaceous (similar to 138-134 Ma) Forearc Ophiolite and Tectonomagmatic Patterns in Central Tibet: Subduction Termination and Re-initiation of Meso-Tethys Ocean Caused by Collision of an Oceanic Plateau at the Continental Margin?

Zeng, YC; Xu, JF; Chen, JL; Wang, BD; Huang, F; Xia, XP; Li, MJ

Xu, JF (corresponding author), China Univ Geosci, Sch Earth Sci & Resources, Beijing, Peoples R China.; Xu, JF (corresponding author), China Univ Geosci, State Key Lab Geol Proc & Mineral Resources, Beijing, Peoples R China.

TECTONICS, 2021; 40 (3):

Abstract

The Bangong-Nujiang Suture Zone (BNSZ) in central Tibet represents relics of the Meso-Tethys Ocean that once separated the Lhasa and Qiangtang terrane......

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Early Cretaceous (similar to 138-134 Ma) Forearc Ophiolite and Tectonomagmatic Patterns in Central Tibet: Subduction Termination and Re-initiation of Meso-Tethys Ocean Caused by Collision of an Oceanic Plateau at the Continental Margin?

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