中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Evolution and final closure of the Mongol-Okhotsk Ocean

文献类型:期刊论文

作者Zhao, Pan2; Xu, Bei3; Chen, Yan1
刊名SCIENCE CHINA-EARTH SCIENCES
出版日期2023-11-01
卷号66期号:11页码:2497-2513
ISSN号1674-7313
关键词Northeastern Asia Mongol-Okhotsk Ocean Paleozoic-Mesozoic Subduction initiation Scissor-like closure
DOI10.1007/s11430-023-1165-9
英文摘要Mongol-Okhotsk Orogenic Belt is the last main orogen that constructs modern tectonic framework of northeastern Asia. It has recorded the long-term evolution of the Mongol-Okhotsk Ocean (MOO) from its Early Paleozoic initial opening, through the Late Paleozoic-Early Mesozoic subduction, to its Mesozoic final closure, leading to the amalgamation of the Siberian Craton (SIB) and North China-Amuria Block (NCC-AMB). Opening of the MOO can be traced to the early stage of the Early Paleozoic. Northward subduction of the Mongol-Okhotsk oceanic slab beneath the southern margin of the SIB initiated in the Silurian, whereas the southward subduction beneath the northern margin of the NCC-AMB started in the Late Devonian. The bidirectional subduction of the Mongol-Okhotsk oceanic slab resulted in pulse arc magmatism, with three main peaks in the earliest Carboniferous, Late Permian, and Late Triassic-Early Jurassic. In the Late Triassic, the collision between the AMB and Western Mongolian Blocks led to the bending of the Western Mongolian Blocks, which caused the initial closure of the MOO in its western segment. Due to the clockwise rotation of the SIB and counterclockwise rotation of the NCC-AMB, the MOO showed a scissor-like closure from west to east. The final closure of the MOO occurred in the Middle-Late Jurassic, which also resulted in the formation of the Mongol Orocline. Since then, the amalgamation of blocks in northeastern Asia has finished, and the northeastern Asian continent went into the intraplate evolutional stage.
WOS关键词NE CHINA IMPLICATIONS ; GREAT XINGAN RANGE ; TRUE POLAR WANDER ; ACTIVE CONTINENTAL-MARGIN ; ASIAN OROGENIC BELT ; TECTONIC EVOLUTION ; ERGUNA MASSIF ; U-PB ; PALEOMAGNETIC CONSTRAINTS ; WESTERN TRANSBAIKALIA
资助项目Acknowledgements We thank Yanyang WANG, Yanjie ZHANG, Yan XU and Liyang ZHANG for their assistant in the field, and Zhenhua JIA and Yifei HOU for their help in the paleomagnetic measuring process. We appreciate the two anonymous reviewers for[92155203] ; National Natural Science Foundation of China
WOS研究方向Geology
语种英语
出版者SCIENCE PRESS
WOS记录号WOS:001088802300002
资助机构Acknowledgements We thank Yanyang WANG, Yanjie ZHANG, Yan XU and Liyang ZHANG for their assistant in the field, and Zhenhua JIA and Yifei HOU for their help in the paleomagnetic measuring process. We appreciate the two anonymous reviewers for ; Acknowledgements We thank Yanyang WANG, Yanjie ZHANG, Yan XU and Liyang ZHANG for their assistant in the field, and Zhenhua JIA and Yifei HOU for their help in the paleomagnetic measuring process. We appreciate the two anonymous reviewers for ; Acknowledgements We thank Yanyang WANG, Yanjie ZHANG, Yan XU and Liyang ZHANG for their assistant in the field, and Zhenhua JIA and Yifei HOU for their help in the paleomagnetic measuring process. We appreciate the two anonymous reviewers for ; Acknowledgements We thank Yanyang WANG, Yanjie ZHANG, Yan XU and Liyang ZHANG for their assistant in the field, and Zhenhua JIA and Yifei HOU for their help in the paleomagnetic measuring process. We appreciate the two anonymous reviewers for ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Acknowledgements We thank Yanyang WANG, Yanjie ZHANG, Yan XU and Liyang ZHANG for their assistant in the field, and Zhenhua JIA and Yifei HOU for their help in the paleomagnetic measuring process. We appreciate the two anonymous reviewers for ; Acknowledgements We thank Yanyang WANG, Yanjie ZHANG, Yan XU and Liyang ZHANG for their assistant in the field, and Zhenhua JIA and Yifei HOU for their help in the paleomagnetic measuring process. We appreciate the two anonymous reviewers for ; Acknowledgements We thank Yanyang WANG, Yanjie ZHANG, Yan XU and Liyang ZHANG for their assistant in the field, and Zhenhua JIA and Yifei HOU for their help in the paleomagnetic measuring process. We appreciate the two anonymous reviewers for ; Acknowledgements We thank Yanyang WANG, Yanjie ZHANG, Yan XU and Liyang ZHANG for their assistant in the field, and Zhenhua JIA and Yifei HOU for their help in the paleomagnetic measuring process. We appreciate the two anonymous reviewers for ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Acknowledgements We thank Yanyang WANG, Yanjie ZHANG, Yan XU and Liyang ZHANG for their assistant in the field, and Zhenhua JIA and Yifei HOU for their help in the paleomagnetic measuring process. We appreciate the two anonymous reviewers for ; Acknowledgements We thank Yanyang WANG, Yanjie ZHANG, Yan XU and Liyang ZHANG for their assistant in the field, and Zhenhua JIA and Yifei HOU for their help in the paleomagnetic measuring process. We appreciate the two anonymous reviewers for ; Acknowledgements We thank Yanyang WANG, Yanjie ZHANG, Yan XU and Liyang ZHANG for their assistant in the field, and Zhenhua JIA and Yifei HOU for their help in the paleomagnetic measuring process. We appreciate the two anonymous reviewers for ; Acknowledgements We thank Yanyang WANG, Yanjie ZHANG, Yan XU and Liyang ZHANG for their assistant in the field, and Zhenhua JIA and Yifei HOU for their help in the paleomagnetic measuring process. We appreciate the two anonymous reviewers for ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Acknowledgements We thank Yanyang WANG, Yanjie ZHANG, Yan XU and Liyang ZHANG for their assistant in the field, and Zhenhua JIA and Yifei HOU for their help in the paleomagnetic measuring process. We appreciate the two anonymous reviewers for ; Acknowledgements We thank Yanyang WANG, Yanjie ZHANG, Yan XU and Liyang ZHANG for their assistant in the field, and Zhenhua JIA and Yifei HOU for their help in the paleomagnetic measuring process. We appreciate the two anonymous reviewers for ; Acknowledgements We thank Yanyang WANG, Yanjie ZHANG, Yan XU and Liyang ZHANG for their assistant in the field, and Zhenhua JIA and Yifei HOU for their help in the paleomagnetic measuring process. We appreciate the two anonymous reviewers for ; Acknowledgements We thank Yanyang WANG, Yanjie ZHANG, Yan XU and Liyang ZHANG for their assistant in the field, and Zhenhua JIA and Yifei HOU for their help in the paleomagnetic measuring process. We appreciate the two anonymous reviewers for ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China
源URL[http://ir.iggcas.ac.cn/handle/132A11/110737]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
通讯作者Zhao, Pan
作者单位1.Univ Orleans, ISTO, UMR 7327, CNRS,BRGM, F-45071 Orleans, France
2.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
3.Hebei GEO Univ, Hebei Key Lab Strateg Crit Mineral Resources, Shijiazhuang 050031, Peoples R China
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Zhao, Pan,Xu, Bei,Chen, Yan. Evolution and final closure of the Mongol-Okhotsk Ocean[J]. SCIENCE CHINA-EARTH SCIENCES,2023,66(11):2497-2513.
APA Zhao, Pan,Xu, Bei,&Chen, Yan.(2023).Evolution and final closure of the Mongol-Okhotsk Ocean.SCIENCE CHINA-EARTH SCIENCES,66(11),2497-2513.
MLA Zhao, Pan,et al."Evolution and final closure of the Mongol-Okhotsk Ocean".SCIENCE CHINA-EARTH SCIENCES 66.11(2023):2497-2513.

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来源:地质与地球物理研究所

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