中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Lithospheric velocity structure of South China Sea basin from ocean bottom seismometer ambient noise tomography

文献类型:期刊论文

作者Cheng, Liqun2,3; Fang, Yinxia2,3; Niu, Xiongwei2,3,10; Li, Tingzi4; Dong, Chongzhi3; Zhao, Yanghui3; Hu, Hao5; Kong, Fansheng3; Tan, Pingchuan3; Ruan, Aiguo3
刊名TECTONOPHYSICS
出版日期2023-10-05
卷号864页码:14
ISSN号0040-1951
关键词Ocean Bottom Seismometer (OBS) Ambient noise Phase velocity South China Sea basin Post-spreading magmatism
DOI10.1016/j.tecto.2023.230008
英文摘要The South China Sea (SCS) is a typical marginal sea basin formed by the seafloor spreading under the tectonic background of plate convergence. Many crustal-scale studies indicate that the SCS basin has undergone asymmetric spreading, multi-phase ridge jumps, and intense post-spreading volcanic activity. Due to the lack of seismic data in the oceanic basin of the SCS, it remains unclear about the scale and basin control of the Zhongnan fault, the magma source depth of the SCS basin, and the transport channel after the cessation of seafloor spreading. Phase velocity derived from ambient noise surface wave tomography may provide useful information to shed light on the mechanisms of the aforementioned problems. From October 2019 to July 2020, a passive source seismic experiment was carried out with many Ocean Bottom Seismometers (OBS) deployed in a broad area of the SCS. Based on the seismic ambient noise data recorded by 16 OBSs in the SCS basin, we inverted the phase velocity images over a period range of 10-20 s using ambient noise surface wave tomography. Our results indicate that the Zhongnan fault zone is a lithospheric-scale fault, which played a regulating role in the expansion of the SCS basin from the East Subbasin to the Southwest Subbasin. In addition, the low-velocity body in the north flank of the Southwest Subbasin extends from the post-spreading seamounts on the ocean crust to the uppermost mantle (i.e., about 10-30 km), which indicates an oblique magma migration during the postspreading volcanism.
WOS关键词SOUTHWESTERN SUBBASIN ; SEISMIC NOISE ; BENEATH ; MANTLE ; EVOLUTION ; INSIGHTS ; CRUST ; CONSTRAINTS ; INVERSION ; VOLCANO
资助项目National Natural Science Foundation of China[41890811] ; National Natural Science Foundation of China[42276064] ; National Natural Science Foundation of China[42076047] ; National Natural Science Foundation of China[42106068] ; Scientific Research Fund of the Second Institute of Oceanography[JG2204] ; Scientific Research Fund of the Second Institute of Oceanography[2021M691412] ; China Postdoctoral Science Foundation[DH-2022KF0213] ; Science Foundation of Donghai Laboratory ; [JG1901]
WOS研究方向Geochemistry & Geophysics
语种英语
出版者ELSEVIER
WOS记录号WOS:001078504900001
资助机构National Natural Science Foundation of China ; National Natural Science Foundation of China ; Scientific Research Fund of the Second Institute of Oceanography ; Scientific Research Fund of the Second Institute of Oceanography ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; Science Foundation of Donghai Laboratory ; Science Foundation of Donghai Laboratory ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Scientific Research Fund of the Second Institute of Oceanography ; Scientific Research Fund of the Second Institute of Oceanography ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; Science Foundation of Donghai Laboratory ; Science Foundation of Donghai Laboratory ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Scientific Research Fund of the Second Institute of Oceanography ; Scientific Research Fund of the Second Institute of Oceanography ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; Science Foundation of Donghai Laboratory ; Science Foundation of Donghai Laboratory ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Scientific Research Fund of the Second Institute of Oceanography ; Scientific Research Fund of the Second Institute of Oceanography ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; Science Foundation of Donghai Laboratory ; Science Foundation of Donghai Laboratory
源URL[http://ir.iggcas.ac.cn/handle/132A11/110767]  
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Fang, Yinxia; Niu, Xiongwei
作者单位1.Taihu Lab Deepsea Technol Sci, Wuxi 214028, Peoples R China
2.Shanghai Jiao Tong Univ, Sch Oceanog, Shanghai 200030, Peoples R China
3.Minist Nat Resources, Inst Oceanog 2, Key Lab submarine Geosci, Hangzhou 310012, Peoples R China
4.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
5.Southern Univ Sci & Technol, Acad Adv Interdisciplinary Studies, Shenzhen 518055, Peoples R China
6.Southern Marine Sci & Engn Guangdong Lab Zhuhai, Zhuhai 519082, Peoples R China
7.Sun Yat sen Univ, Sch Earth Sci & Engn, Zhuhai 519082, Peoples R China
8.Chinese Acad Sci, Inst Oceanol, Qingdao 266071, Peoples R China
9.Univ Malaysia Terengganu, Fac Sci & Marine Environm, Paleoceanog Res Interest Grp, Kuala Nerus 21300, Terengganu, Malaysia
10.Donghai Lab, Zhoushan 316021, Zhejiang, Peoples R China
推荐引用方式
GB/T 7714
Cheng, Liqun,Fang, Yinxia,Niu, Xiongwei,et al. Lithospheric velocity structure of South China Sea basin from ocean bottom seismometer ambient noise tomography[J]. TECTONOPHYSICS,2023,864:14.
APA Cheng, Liqun.,Fang, Yinxia.,Niu, Xiongwei.,Li, Tingzi.,Dong, Chongzhi.,...&Du, Xinguang.(2023).Lithospheric velocity structure of South China Sea basin from ocean bottom seismometer ambient noise tomography.TECTONOPHYSICS,864,14.
MLA Cheng, Liqun,et al."Lithospheric velocity structure of South China Sea basin from ocean bottom seismometer ambient noise tomography".TECTONOPHYSICS 864(2023):14.

入库方式: OAI收割

来源:地质与地球物理研究所

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