Results 151 to 160 of about 1,111,472 (195)
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Gondwana Research, 2017
Abstract The formation and evolution of the Central Asian Orogenic Belt (CAOB) are intimately related to the opening and closure of the Paleo-Asian Ocean. The final closure led to amalgamation or collision between the CAOB and North China Craton. However, the issue about the subduction polarity and final closure of the Paleo-Asian Ocean has long been
Bor-Ming Jahn, Guochun Zhao
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Abstract The formation and evolution of the Central Asian Orogenic Belt (CAOB) are intimately related to the opening and closure of the Paleo-Asian Ocean. The final closure led to amalgamation or collision between the CAOB and North China Craton. However, the issue about the subduction polarity and final closure of the Paleo-Asian Ocean has long been
Bor-Ming Jahn, Guochun Zhao
exaly +4 more sources
Gondwana Research, 2022 Zhangguangcailing Orogen constitutes a significant part of the Eastern Asian Continental margin. Its evolution was constrained by the oceanic consumption processes between the Jiamusi and Songliao blocks during late Paleozoic and Mesozoic time, resulted ...
Guochun Zhao
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Influence of subducted carbonate on the composition of basalts in the Paleo-Asian Ocean domain
Gondwana Research, 2023 The fate of subducted carbonate of the Paleo-Asian Ocean and its control on the compositional variability of Cenozoic basalts to the west of the Daxing'anling-Taihang Gravity Lineament remain uncertain.
Sheng-Peng Wang +7 more
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Tectonophysics, 2015 The Central Asian Orogenic Belt (CAOB) evolved through complex closure of the Paleo-Asian Ocean from the Neoproterozoic to the late Phanerozoic. This caused the Chinese cratons to collide with Eurasia and led to the formation of the world's largest ...
Simon Wilde
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Geological Society of America BulletinUnderstanding subduction initiation and mantle plume dynamics is central to plate-tectonic evolution but remains poorly constrained in ancient orogens. The tectonic evolution of the North Tianshan paleo-ocean basin, a key segment of the Paleo-Asian Ocean of the Altaids, has long been debated owing to the scarcity of diagnostic ophiolitic records.
Pengde Liu +8 more
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Journal of Geophysical Research: Solid Earth, 2019 When the Paleo-Asian Ocean closed and the Paleo-Pacific subduction started in NE China remains controversial. To constrain these key issues, we carried out zircon U-Pb-Hf isotopic and whole-rock geochemical studies of Early Mesozoic igneous rocks in ...
Wenchun Ge, Feng Wang, Yi-Ni Wang
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Crustal-scale Seismic-reflection Profiling Constrains How the Paleo-Asian Ocean Was Closed
Tectonics, 2023AbstractThe Central Asian Orogenic Belt (CAOB) is the most significant accretionary orogenic belt since the Phanerozoic and the most ideal site for studying continental growth evolution processes. A 460‐km‐long high‐resolution crustal‐scale seismic reflection study was conducted across the eastern CAOB in North‐Central China to constrain the closure ...
Wang, Hai-Yan +4 more
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Opening and Tectonic Evolution of the Paleo-Asian Ocean
International Geology Review, 1995The Paleo-Asian ocean is defined by units located between the Russian (East European), Siberian, Tarim, and Sino-Korean (North China) continents. The study of the composition, age, and structural position of island-arc magmatic rocks, ophiolites, and high-pressure meta-morphic assemblages and their mutual correlations made it possible to identify ...
N. L. Dobretsov +2 more
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