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Late Jurassic to early Early Cretaceous tectonic nature on the NE Asian continental margin: Constraints from Mesozoic accretionary complexes
Li, Yu1,2; Xu, Wen-Liang2; Zhu, Ri-Xiang1; Wang, Feng2; Ge, Wen-Chun2; Sorokin, A. A.3
2020
Source PublicationEARTH-SCIENCE REVIEWS
ISSN0012-8252
Volume200Pages:18
AbstractIt is widely accepted that subduction of the Paleo-Pacific Plate beneath. Eurasia began in the early Mesozoic. However, the tectonic nature and processes of the NE Asian continental margin in the Late Jurassic to early Early Cretaceous remain unclear. In this contribution, lithological, provenance, and metamorphic-deformation data are used to constrain the formation of Mesozoic accretionary complexes (AC) along the NE Asian continental margin and determine the tectonic relationship between the NE Asian continental margin and the Paleo-Pacific Plate in the Late Jurassic to early Early Cretaceous. The Mesozoic AC formed during the Late Jurassic (including the Raohe AC in NE China; the Khabarovsk, Samarka, and Taukha ACs in the Russian Far East; and the Mino-Tamba AC in Japan) and Early Cretaceous (including the Shimanto AC in Japan and the Kiselevka-Manoma AC in the Russian Far East). The Jurassic AC underwent a complex evolution, including the formation of seamounts, Middle-Late Jurassic terrigenous clastic sedimentation adjacent to the trench; collision of seamounts with Eurasia, northward migration of the AC, early Early Cretaceous terrigenous clastic sedimentation, a second period of accretion, and final emplacement. The earliest Mesozoic AC arrived at the trench at ca. 195 Ma. Combined with the occurrence of early Mesozoic calc-alkaline igneous rocks along the NE Asian continental margin, we suggest that subduction of the Paleo-Pacific Plate beneath Eurasia began in the Early Jurassic. Jurassic AC in Japan was affected by a regional high-P/T metamorphic event at 160 Ma, which might have been related to subduction-collision of seamounts with Eurasia at the trench. Ages and Hf isotopic compositions of detrital zircon grains from the Middle-Upper Jurassic and Cretaceous AC sandstones, together with paleontological and paleomagnetic data, indicate that Jurassic clastic sediments were sourced mainly from the South China Block (SCB), whereas the Lower Cretaceous sandstones were sourced from the eastern Central Asian Orogenic Belt (CAOB). The inferred northward migration of Jurassic AC in the Late Jurassic to early Early Cretaceous indicates that the boundary between the NE Asian continental margin and the Paleo-Pacific Plate was characterized by strike-slip tectonics at this time, likely due to a small angle of obliquity in the subduction of the Paleo-Pacific Plate beneath Eurasia. In the late Early Cretaceous, westward subduction of the Paleo-Pacific Plate beneath Eurasia resulted in the emplacement of the Raohe and Khabarovsk ACs at 137-130 Ma and the formation of ACs in the Russian Far East and Japan.
KeywordNortheast Asian continental margin Mesozoic Accretionary complex Paleo-Pacific Plate Strike-slip tectonics
DOI10.1016/j.earscirev.2019.103042
Funding OrganizationNational Natural Science Foundation of China ; National Natural Science Foundation of China ; Open Project of the State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences ; Open Project of the State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Open Project of the State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences ; Open Project of the State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Open Project of the State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences ; Open Project of the State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Open Project of the State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences ; Open Project of the State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation
WOS KeywordZIRCON U-PB ; NORTH CHINA CRATON ; GREAT XINGAN RANGE ; RUSSIAN FAR-EAST ; MONGOL-OKHOTSK OCEAN ; EARLY PALEOZOIC GRANITOIDS ; PERMO-TRIASSIC COLLISION ; RIVER METALLOGENIC BELT ; ALIN OROGENIC BELT ; A-TYPE GRANITES
Language英语
Funding ProjectNational Natural Science Foundation of China[91858211] ; National Natural Science Foundation of China[41688103] ; National Natural Science Foundation of China[41902054] ; Open Project of the State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences[SKL-K201903] ; China Postdoctoral Science Foundation[2018M641466]
Funding OrganizationNational Natural Science Foundation of China ; National Natural Science Foundation of China ; Open Project of the State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences ; Open Project of the State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Open Project of the State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences ; Open Project of the State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Open Project of the State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences ; Open Project of the State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Open Project of the State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences ; Open Project of the State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation
WOS Research AreaGeology
WOS SubjectGeosciences, Multidisciplinary
WOS IDWOS:000514749100025
PublisherELSEVIER
Citation statistics
Document Type期刊论文
Identifierhttp://ir.iggcas.ac.cn/handle/132A11/95524
Collection岩石圈演化国家重点实验室
Corresponding AuthorXu, Wen-Liang
Affiliation1.Chinese Acad Sci, State Key Lab Lithospher Evolut, Inst Geol & Geophys, Beijing 100029, Peoples R China
2.Jilin Univ, Coll Earth Sci, Changchun 100029, Peoples R China
3.Russian Acad Sci, Inst Geol & Nat Management, Far Eastern Branch, Ul B Khmelnitskogo 2, Blagoveshchensk 675000, Russia
Recommended Citation
GB/T 7714
Li, Yu,Xu, Wen-Liang,Zhu, Ri-Xiang,et al. Late Jurassic to early Early Cretaceous tectonic nature on the NE Asian continental margin: Constraints from Mesozoic accretionary complexes[J]. EARTH-SCIENCE REVIEWS,2020,200:18.
APA Li, Yu,Xu, Wen-Liang,Zhu, Ri-Xiang,Wang, Feng,Ge, Wen-Chun,&Sorokin, A. A..(2020).Late Jurassic to early Early Cretaceous tectonic nature on the NE Asian continental margin: Constraints from Mesozoic accretionary complexes.EARTH-SCIENCE REVIEWS,200,18.
MLA Li, Yu,et al."Late Jurassic to early Early Cretaceous tectonic nature on the NE Asian continental margin: Constraints from Mesozoic accretionary complexes".EARTH-SCIENCE REVIEWS 200(2020):18.
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