Results 191 to 200 of about 40,548 (279)

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

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

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   +4 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.
Yunchuan Zeng   +6 more
semanticscholar   +1 more source

Paleomagnetic and Chronologic Data Bearing on the Permian/Triassic Boundary Position of Qamdo in the Eastern Qiantang Terrane: Implications for the Closure of the Paleo‐Tethys

Geophysical Research Letters, 2021
The tectonic evolution of the eastern Paleo‐Tethys in the Three‐Rivers headwater region remains uncertain, especially because of the lack of quality paleomagnetic data from the east Eastern Qiangtang Terrane (EQT).
Chong Guan   +10 more
semanticscholar   +1 more source

HP–UHP Metamorphic Belt in the East Kunlun Orogen: Final Closure of the Proto-Tethys Ocean and Formation of the Pan-North-China Continent

open access: yesJournal of Petrology, 2018
The East Kunlun Orogen, the northwestern part of the Central China Orogenic Belt, is a long-lived accretionary orogenic belt that records the evolution and eventual destruction of branches of the Tethys Ocean, from the Cambrian to the Triassic.
Shu-Guang Song   +2 more
exaly   +2 more sources

First mid-ocean ridge-type ophiolite from the Meso-Tethys suture zone in the north-central Tibetan plateau

GSA Bulletin, 2020
The Meso-Tethys was a late Paleozoic to Mesozoic ocean basin between the Cimmerian continent and Gondwana. Part of its relicts is exposed in the Bangong–Nujiang suture zone, in the north-central Tibetan Plateau, that played a key role in the evolution ...
Yue Tang   +8 more
semanticscholar   +1 more source

Home - About - Disclaimer - Privacy