Results 201 to 210 of about 26,291 (281)
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Tectonic evolution and geodynamics of the Neo-Tethys Ocean
Science China Earth Sciences, 2021Rixiang Zhu
exaly +2 more sources
Dynamics of closure of the Proto-Tethys Ocean: A perspective from the Southeast Asian Tethys realm
Earth-Science Reviews, 2021Junlai Liu, Tianyu Zhao, Wenkui Fan
exaly +2 more sources
Gondwana dispersion and Asian accretion: Tectonic and palaeogeographic evolution of eastern Tethys
Journal of Asian Earth Sciences, 2013Ian Metcalfe
exaly +2 more sources
Tracing the sedimentary response to the rifting and opening of the Meso‐Tethys Ocean
Sedimentology, 2023Knowledge 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
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
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
, 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
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, 2022Western 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
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
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
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
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
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
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

