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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.
Jian-Jun Fan   +4 more
semanticscholar   +1 more source

Short duration of Early Permian Qiangtang-Panjal large igneous province: Implications for origin of the Neo-Tethys Ocean

Earth and Planetary Science Letters, 2021
Northward drift of the Cimmerian microcontinents and opening of the Neo-Tethys Ocean in Early Permian are prominent events in northern Gondwana's protracted breakup history.
Wei Dan   +9 more
semanticscholar   +1 more source

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

, 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   +14 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 ...
Shao‐Cong Lai   +4 more
semanticscholar   +1 more source

The Bangong-Nujiang Suture Zone, Tibet Plateau: Its role in the tectonic evolution of the eastern Tethys Ocean

Earth-Science Reviews, 2021
The Tibet Plateau was generated from a long-term, multiple and complex convergence of many micro-blocks and the final Indian-Eurasian collision, which records the evolution of the eastern Neo-Tethys Ocean. In order to clarify the evolution of the eastern
Suhua Jiang   +7 more
semanticscholar   +1 more source

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.
Yun‐Chuan Zeng   +6 more
semanticscholar   +1 more source

Closure of the Proto-Tethys Ocean and Early Paleozoic amalgamation of microcontinental blocks in East Asia

Earth-Science Reviews, 2017
As a complex paleo-ocean located between the Tarim-North China and the Sibumasu/Baoshan blocks, the Proto-Tethys Ocean was opened from the rifting of the Supercontinent Rodinia and mainly closed at the end of the Early Paleozoic.
Sanzhong Li   +8 more
semanticscholar   +1 more source

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