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作者 | Liang, Xiaofeng2,3; Chen, Ling1,2; Tian, Xiaobo2,3; Chu, Yang2,3; Li, Wentao1,2
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刊名 | SCIENCE CHINA-EARTH SCIENCES
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出版日期 | 2023-11-02
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页码 | 21 |
关键词 | Tibetan Plateau
Crustal structure
Moho doublet
Uplift of the plateau
Crustal channel flow
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ISSN号 | 1674-7313
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DOI | 10.1007/s11430-023-1158-5
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英文摘要 | The Tibetan Plateau has been known for its highest elevation and thickest crust on earth, and become a key region for comprehending the rheology and tectonic evolution of continental plates and associated dynamic processes. Over the past years, numerous geophysical studies have been conducted to explore the deep structure of the Tibetan Plateau, resulting in significant advancements in understanding the formation and growth of the Plateau. This paper aims to provide a comprehensive summary and discussion of the geophysical observations and underlying mechanisms of the plateau uplift. First, major relevant tectonic models are reviewed, and the corresponding features of crustal structures and related deformation are presented. Then, recent observations, including the identification of a high-velocity layer in the lower crust of the Lhasa block, the spatial distribution of crustal channel flow, and the decoupling of shallow and deep crustal deformation, are synthesized to gain insights into the crustal structures, and multidisciplinary data are integrated to discuss the potential mechanisms of the plateau uplift. Lastly, some pertinent suggestions are put forward for future research on the Tibetan Plateau. |
WOS关键词 | BENEATH WESTERN TIBET
; UPPER-MANTLE BENEATH
; RAYLEIGH-TAYLOR INSTABILITY
; TECTONIC STRESS-FIELD
; LOW-VELOCITY ZONE
; SOUTHERN TIBET
; CONTINENTAL COLLISION
; ANISOTROPY BENEATH
; SEISMIC ANISOTROPY
; EASTERN MARGIN
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资助项目 | Acknowledgements We would like to express our gratitude to Dr. Hao DONG from China University of Geosciences (Beijing) and Dr. Feng JIANG from the Institute of South China Sea, Chinese Academy of Sciences for sharing the crustal resistivity mo
; University of Missouri-St[42074067]
; National Natural Science Foundation of China[IGGCAS-202204]
; Key Research Program of the Institute of Geology and Geophysics, CAS
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WOS研究方向 | Geology
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语种 | 英语
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WOS记录号 | WOS:001095301000001
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出版者 | SCIENCE PRESS
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资助机构 | Acknowledgements We would like to express our gratitude to Dr. Hao DONG from China University of Geosciences (Beijing) and Dr. Feng JIANG from the Institute of South China Sea, Chinese Academy of Sciences for sharing the crustal resistivity mo
; Acknowledgements We would like to express our gratitude to Dr. Hao DONG from China University of Geosciences (Beijing) and Dr. Feng JIANG from the Institute of South China Sea, Chinese Academy of Sciences for sharing the crustal resistivity mo
; Acknowledgements We would like to express our gratitude to Dr. Hao DONG from China University of Geosciences (Beijing) and Dr. Feng JIANG from the Institute of South China Sea, Chinese Academy of Sciences for sharing the crustal resistivity mo
; Acknowledgements We would like to express our gratitude to Dr. Hao DONG from China University of Geosciences (Beijing) and Dr. Feng JIANG from the Institute of South China Sea, Chinese Academy of Sciences for sharing the crustal resistivity mo
; University of Missouri-St
; University of Missouri-St
; University of Missouri-St
; University of Missouri-St
; National Natural Science Foundation of China
; National Natural Science Foundation of China
; National Natural Science Foundation of China
; National Natural Science Foundation of China
; Key Research Program of the Institute of Geology and Geophysics, CAS
; Key Research Program of the Institute of Geology and Geophysics, CAS
; Key Research Program of the Institute of Geology and Geophysics, CAS
; Key Research Program of the Institute of Geology and Geophysics, CAS
; Acknowledgements We would like to express our gratitude to Dr. Hao DONG from China University of Geosciences (Beijing) and Dr. Feng JIANG from the Institute of South China Sea, Chinese Academy of Sciences for sharing the crustal resistivity mo
; Acknowledgements We would like to express our gratitude to Dr. Hao DONG from China University of Geosciences (Beijing) and Dr. Feng JIANG from the Institute of South China Sea, Chinese Academy of Sciences for sharing the crustal resistivity mo
; Acknowledgements We would like to express our gratitude to Dr. Hao DONG from China University of Geosciences (Beijing) and Dr. Feng JIANG from the Institute of South China Sea, Chinese Academy of Sciences for sharing the crustal resistivity mo
; Acknowledgements We would like to express our gratitude to Dr. Hao DONG from China University of Geosciences (Beijing) and Dr. Feng JIANG from the Institute of South China Sea, Chinese Academy of Sciences for sharing the crustal resistivity mo
; University of Missouri-St
; University of Missouri-St
; University of Missouri-St
; University of Missouri-St
; National Natural Science Foundation of China
; National Natural Science Foundation of China
; National Natural Science Foundation of China
; National Natural Science Foundation of China
; Key Research Program of the Institute of Geology and Geophysics, CAS
; Key Research Program of the Institute of Geology and Geophysics, CAS
; Key Research Program of the Institute of Geology and Geophysics, CAS
; Key Research Program of the Institute of Geology and Geophysics, CAS
; Acknowledgements We would like to express our gratitude to Dr. Hao DONG from China University of Geosciences (Beijing) and Dr. Feng JIANG from the Institute of South China Sea, Chinese Academy of Sciences for sharing the crustal resistivity mo
; Acknowledgements We would like to express our gratitude to Dr. Hao DONG from China University of Geosciences (Beijing) and Dr. Feng JIANG from the Institute of South China Sea, Chinese Academy of Sciences for sharing the crustal resistivity mo
; Acknowledgements We would like to express our gratitude to Dr. Hao DONG from China University of Geosciences (Beijing) and Dr. Feng JIANG from the Institute of South China Sea, Chinese Academy of Sciences for sharing the crustal resistivity mo
; Acknowledgements We would like to express our gratitude to Dr. Hao DONG from China University of Geosciences (Beijing) and Dr. Feng JIANG from the Institute of South China Sea, Chinese Academy of Sciences for sharing the crustal resistivity mo
; University of Missouri-St
; University of Missouri-St
; University of Missouri-St
; University of Missouri-St
; National Natural Science Foundation of China
; National Natural Science Foundation of China
; National Natural Science Foundation of China
; National Natural Science Foundation of China
; Key Research Program of the Institute of Geology and Geophysics, CAS
; Key Research Program of the Institute of Geology and Geophysics, CAS
; Key Research Program of the Institute of Geology and Geophysics, CAS
; Key Research Program of the Institute of Geology and Geophysics, CAS
; Acknowledgements We would like to express our gratitude to Dr. Hao DONG from China University of Geosciences (Beijing) and Dr. Feng JIANG from the Institute of South China Sea, Chinese Academy of Sciences for sharing the crustal resistivity mo
; Acknowledgements We would like to express our gratitude to Dr. Hao DONG from China University of Geosciences (Beijing) and Dr. Feng JIANG from the Institute of South China Sea, Chinese Academy of Sciences for sharing the crustal resistivity mo
; Acknowledgements We would like to express our gratitude to Dr. Hao DONG from China University of Geosciences (Beijing) and Dr. Feng JIANG from the Institute of South China Sea, Chinese Academy of Sciences for sharing the crustal resistivity mo
; Acknowledgements We would like to express our gratitude to Dr. Hao DONG from China University of Geosciences (Beijing) and Dr. Feng JIANG from the Institute of South China Sea, Chinese Academy of Sciences for sharing the crustal resistivity mo
; University of Missouri-St
; University of Missouri-St
; University of Missouri-St
; University of Missouri-St
; National Natural Science Foundation of China
; National Natural Science Foundation of China
; National Natural Science Foundation of China
; National Natural Science Foundation of China
; Key Research Program of the Institute of Geology and Geophysics, CAS
; Key Research Program of the Institute of Geology and Geophysics, CAS
; Key Research Program of the Institute of Geology and Geophysics, CAS
; Key Research Program of the Institute of Geology and Geophysics, CAS
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源URL | [http://ir.iggcas.ac.cn/handle/132A11/110679]  |
专题 | 地质与地球物理研究所_岩石圈演化国家重点实验室
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通讯作者 | Liang, Xiaofeng |
作者单位 | 1.Univ Chinese Acad Sci, Sch Earth & Planetary Sci, Beijing 100049, Peoples R China 2.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China 3.Chinese Acad Sci, Innovat Acad Earth Sci, Beijing 100029, Peoples R China
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推荐引用方式 GB/T 7714 |
Liang, Xiaofeng,Chen, Ling,Tian, Xiaobo,et al. Uplifting mechanism of the Tibetan Plateau inferred from the characteristics of crustal structures[J]. SCIENCE CHINA-EARTH SCIENCES,2023:21.
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APA |
Liang, Xiaofeng,Chen, Ling,Tian, Xiaobo,Chu, Yang,&Li, Wentao.(2023).Uplifting mechanism of the Tibetan Plateau inferred from the characteristics of crustal structures.SCIENCE CHINA-EARTH SCIENCES,21.
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MLA |
Liang, Xiaofeng,et al."Uplifting mechanism of the Tibetan Plateau inferred from the characteristics of crustal structures".SCIENCE CHINA-EARTH SCIENCES (2023):21.
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