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Voyager 1: Saturn encounter. Summary of events [PDF]

core   +1 more source

An oblique subduction model for closure of the Proto-Tethys and Palaeo-Tethys oceans and creation of the Central China Orogenic Belt

Earth-Science Reviews, 2023
Tao Wen
exaly   +2 more sources

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Tectonic evolution and geodynamics of the Neo-Tethys Ocean

Science China Earth Sciences, 2021
Ri-Xiang Zhu, Pan Zhao, Liang Zhao
exaly   +2 more sources

Tectono-thermal evolution of the Qilian orogenic system: Tracing the subduction, accretion and closure of the Proto-Tethys Ocean

Earth-Science Reviews, 2021
The Qilian orogenic system in the northern Tibetan Plateau records the complete tectonic cycle from opening of Proto-Tethys Ocean, initial subduction, to continental subduction and collision, and extensional collapse during Neoproterozoic to Devonian ...
Sheng-Yao Yu, Yin-Biao Peng, Jianxin Zhang   +2 more
exaly   +2 more sources

Gondwana dispersion and Asian accretion: Tectonic and palaeogeographic evolution of eastern Tethys

Journal of Asian Earth Sciences, 2013
I Metcalfe
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Tracing the sedimentary response to the rifting and opening of the Meso‐Tethys Ocean

Sedimentology, 2023
Knowledge of the rifting and opening process of the Meso‐Tethys Ocean is important for understanding the evolution of the Tethys tectonic domain and for an in‐depth understanding of Tethys dynamics.
Jianjun Fan, Bo‐Chuan Zhang, Y. Niu, An‐Bo Luo, Yu-jie Hao   +4 more
semanticscholar   +1 more source

Granitic Magmatism in Eastern Tethys Domain (Western China) and their Geodynamic Implications

Acta Geologica Sinica - English Edition, 2022
Western China locates in the eastern section of the Tethys domain, granitic rocks in this region with variable formation ages and geochemistry record key information about the crust‐mantle structure and thermal evolution during the convergent process of ...
Shaocong Lai, R. Zhu, Jiangfeng Qin, Shao-Wei Zhao, Yu Zhu   +4 more
semanticscholar   +1 more source

Paleo-Tethys subduction induced slab-drag opening the Neo-Tethys: Evidence from an Iranian segment of Gondwana

Earth-Science Reviews, 2021
The Iranian plateau has a more straightforward relationship between the Paleo-Tethys and Neo-Tethys, than other regions in the Tethyan realm and is an ideal place to test the genetic connection of how the Paleo-Tethys affected the Neo-Tethys.
B. Wan, Y. Chu, Ling Chen, Xiaofeng Liang, Zhiyong Zhang, S. Ao, M. Talebian   +6 more
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Early Cretaceous (∼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?

Tectonics, 2021
The Bangong‐Nujiang Suture Zone (BNSZ) in central Tibet represents relics of the Meso‐Tethys Ocean that once separated the Lhasa and Qiangtang terranes.
Yunchuan Zeng, Ji‐Feng Xu, Jian‐Lin Chen, Bao-di Wang, F. Huang, X. Xia, Mingjian Li   +6 more
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Dynamics of closure of the Proto-Tethys Ocean: A perspective from the Southeast Asian Tethys realm

Earth-Science Reviews, 2021
Wenkui Fan, Tianyu Zhao
exaly   +2 more sources