Tectonic Controls on Block Rotation and Sheeted Sill Emplacement in the Xigaze Ophiolite (Tibet): The Construction Mode of Slow-Spreading and Ultraslow-Spreading Oceanic Crusts
文献类型：期刊论文
| 作者 | Liu, Tong2; Dick, Henry J. B.3; Liu, Chuan-Zhou1,2,4,5; Wu, Fu-Yuan2,4; Ji, Wen-Bin6; Zhang, Chang2 ; Zhang, Wei-Qi2,4; Zhang, Zhen-Yu2,4; Lin, Yin-Zheng2,4; Zhang, Zhen2,4
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| 刊名 | GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS
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| 出版日期 | 2021-03-01 |
| 卷号 | 22期号:3页码:23 |
| 关键词 | block rotation detachment fault sheeted sill complex slow‐ spreading and ultraslow‐ spreading ridges Tibetan Plateau Xigaze ophiolite |
| DOI | 10.1029/2020GC009297 |
| 英文摘要 | The internal structure of oceanic crusts is not well understood due to the limitation of deep drilling. However, that of ophiolites, i.e., on-land ancient analogs of oceanic lithosphere, could be precisely mapped and measured. The Xigaze ophiolite in Tibet has been regarded as "peculiar", due to the sheeted sill complex in its upper crust, and non-sheeted diabase sills/dikes crosscutting its mantle and lower crust, which are geometrically different from the primarily vertical sheeted dike complex. Based on extensive field observations, here we present petrological and geochemical data for the Xigaze ophiolite to decipher the origin of sheeted sill complex and its implications for the construction of oceanic crusts. Diabases in the Xigaze ophiolite could be subdivided into sheeted sills, Group 1 non-sheeted dikes, and Group 2 non-sheeted sills, based on their orientations. These diabases cut other lithologies, and hence belong to the latest-stage products. Based on petrological, geochemical, and structural data, we highlight the important role of detachment fault in the generation of sheeted and non-sheeted sills. During the formation of oceanic crust, large block exhumation, multi-stage rotations, and foundering are argued here as key mechanisms for the generation of Xigaze sheeted and non-sheeted dikes/sills, all of which are in the evolution of detachment fault systems. These processes are also not uncommon for asymmetrical segments at modern slow-spreading and ultraslow-spreading ridges, but are rare at symmetrical segments. Due to the evolution of detachment fault, the internal structures of (ultra)slow-spreading ridges are more complex than those at fast-spreading ridges. |
| 资助项目 | National Natural Science Foundation of China[42025201] ; National Natural Science Foundation of China[41802062] ; Key Research Program of Frontier Sciences from CAS[QYZDB-SSW-DQC032] ; NSFC[91755000] ; Open Fund Project of State Key Laboratory of Lithospheric Evolution[201707] |
| WOS研究方向 | Geochemistry & Geophysics |
| 语种 | 英语 |
| WOS记录号 | WOS:000636360200015 |
| 出版者 | AMER GEOPHYSICAL UNION |
| 资助机构 | 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 Frontier Sciences from CAS ; Key Research Program of Frontier Sciences from CAS ; Key Research Program of Frontier Sciences from CAS ; Key Research Program of Frontier Sciences from CAS ; NSFC ; NSFC ; NSFC ; NSFC ; Open Fund Project of State Key Laboratory of Lithospheric Evolution ; Open Fund Project of State Key Laboratory of Lithospheric Evolution ; Open Fund Project of State Key Laboratory of Lithospheric Evolution ; Open Fund Project of State Key Laboratory of Lithospheric Evolution ; 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 Frontier Sciences from CAS ; Key Research Program of Frontier Sciences from CAS ; Key Research Program of Frontier Sciences from CAS ; Key Research Program of Frontier Sciences from CAS ; NSFC ; NSFC ; NSFC ; NSFC ; Open Fund Project of State Key Laboratory of Lithospheric Evolution ; Open Fund Project of State Key Laboratory of Lithospheric Evolution ; Open Fund Project of State Key Laboratory of Lithospheric Evolution ; Open Fund Project of State Key Laboratory of Lithospheric Evolution ; 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 Frontier Sciences from CAS ; Key Research Program of Frontier Sciences from CAS ; Key Research Program of Frontier Sciences from CAS ; Key Research Program of Frontier Sciences from CAS ; NSFC ; NSFC ; NSFC ; NSFC ; Open Fund Project of State Key Laboratory of Lithospheric Evolution ; Open Fund Project of State Key Laboratory of Lithospheric Evolution ; Open Fund Project of State Key Laboratory of Lithospheric Evolution ; Open Fund Project of State Key Laboratory of Lithospheric Evolution ; 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 Frontier Sciences from CAS ; Key Research Program of Frontier Sciences from CAS ; Key Research Program of Frontier Sciences from CAS ; Key Research Program of Frontier Sciences from CAS ; NSFC ; NSFC ; NSFC ; NSFC ; Open Fund Project of State Key Laboratory of Lithospheric Evolution ; Open Fund Project of State Key Laboratory of Lithospheric Evolution ; Open Fund Project of State Key Laboratory of Lithospheric Evolution ; Open Fund Project of State Key Laboratory of Lithospheric Evolution |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/101106]  |
| 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 | Liu, Tong |
| 作者单位 | 1.CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing, Peoples R China 2.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing, Peoples R China 3.Woods Hole Oceanog Inst, Dept Geol & Geophys, Woods Hole, MA 02543 USA 4.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing, Peoples R China 5.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Geol, Qingdao, Peoples R China 6.Northwest Univ, Dept Geol, Xian, Peoples R China |
| 推荐引用方式 GB/T 7714 | Liu, Tong,Dick, Henry J. B.,Liu, Chuan-Zhou,et al. Tectonic Controls on Block Rotation and Sheeted Sill Emplacement in the Xigaze Ophiolite (Tibet): The Construction Mode of Slow-Spreading and Ultraslow-Spreading Oceanic Crusts[J]. GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS,2021,22(3):23. |
| APA | Liu, Tong.,Dick, Henry J. B..,Liu, Chuan-Zhou.,Wu, Fu-Yuan.,Ji, Wen-Bin.,...&Zhang, Zhen.(2021).Tectonic Controls on Block Rotation and Sheeted Sill Emplacement in the Xigaze Ophiolite (Tibet): The Construction Mode of Slow-Spreading and Ultraslow-Spreading Oceanic Crusts.GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS,22(3),23. |
| MLA | Liu, Tong,et al."Tectonic Controls on Block Rotation and Sheeted Sill Emplacement in the Xigaze Ophiolite (Tibet): The Construction Mode of Slow-Spreading and Ultraslow-Spreading Oceanic Crusts".GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS 22.3(2021):23. |
入库方式： OAI收割
来源：地质与地球物理研究所
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