中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
The 3D lithospheric structure of China Seas and adjacent areas: Combining geoid, gravity, and topography data

文献类型:期刊论文

作者Ma, Jing1,4; Zeyen, Hermann1; Li, Zhongsheng4; Wang, Wanyin2,3,4; Zhang, Yimi4
刊名GONDWANA RESEARCH
出版日期2025-08-01
卷号144页码:151-166
关键词Lithospheric structure Free air gravity anomaly Geoid Topography China Seas and adjacent areas
ISSN号1342-937X
DOI10.1016/j.gr.2025.04.008
通讯作者Zeyen, Hermann(hermann.zeyen@universite-paris-saclay.fr)
英文摘要The convergence of the Pacific, Eurasian, Philippine Sea, and Caroline Plates makes the China Seas and adjacent areas a natural laboratory for studying lithospheric evolution at ocean-continent transitions. We present a novel three-dimensional (3D) lithospheric model through an advanced joint inversion framework integrating multi-geophysical datasets (geoid, free air gravity anomaly, topography, and seismic Moho constraints). This study features three key advances: (1) A zonal parameterization scheme achieving higher lateral resolution than conventional models, delineating 15 tectonic units (10 km grid) with distinct thermal and density properties; (2) Integration of seismic Moho constraints, depth-dependent crustal/sedimentary densities, and thermally modulated mantle densities to enable comprehensive lithospheric characterization; (3) Key lithospheric transects reveal: (i) Progressive lithospheric thinning from cratonic basins (Ordos: 160 f 5 km; Sichuan: 155 f 7 km) to active margins (Okinawa Trough: 80 f 10 km), with LAB uplift amplitudes (Bohai Bay: 50 f 8 km; South China Block: 35 f 6 km) correlating with Pacific slab rollback; (ii) Seafloor spreading in the South China Sea has resulted in LAB uplift of 40 f 5 km, associated with mantle upwelling consistent with previous geodynamic modeling. These findings redefine the 3D lithospheric framework of the study area, illustrating the interplay between plate boundary forces, mantle dynamics, and lithospheric deformation across ocean-continent transitions. Although our results don't change fundamentally the overall lithospheric image of the area, our results provide better constraints for advancing geodynamic models and offer key insights into non-isostatic subduction dynamics within complex plate interactions.
WOS关键词MOHO DEPTH ; JOINT INVERSION ; HEAT-FLOW ; CRUSTAL ; CRATON ; THICKNESS ; BASIN ; ZONE ; MOUNTAINS ; FEATURES
资助项目Scientific and Technological Project of China National Offshore Oil Corporation (CNOOC) Research Institute Co., Ltd.[CCL2021RCPS0167KQN] ; China Scholarship Council
WOS研究方向Geology
语种英语
WOS记录号WOS:001495258000002
出版者ELSEVIER
源URL[http://ir.qdio.ac.cn/handle/337002/202136]  
专题海洋研究所_海洋地质与环境重点实验室
通讯作者Zeyen, Hermann
作者单位1.Univ Paris Saclay, Dept Earth Sci, GEOPS, CNRS, Bat 504, F-91405 Orsay, France
2.Chinese Acad Sci, Key Lab Marine Geol & Environm, Qingdao 266071, Peoples R China
3.Natl Engn Res Ctr Offshore Oil & Gas Explorat, Beijing 100028, Peoples R China
4.Changan Univ, Sch Geol Engn & Geomatics, Key Lab Western Chinas Mineral Resources & Geol En, Minist Educ, Xian 710054, Peoples R China
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Ma, Jing,Zeyen, Hermann,Li, Zhongsheng,et al. The 3D lithospheric structure of China Seas and adjacent areas: Combining geoid, gravity, and topography data[J]. GONDWANA RESEARCH,2025,144:151-166.
APA Ma, Jing,Zeyen, Hermann,Li, Zhongsheng,Wang, Wanyin,&Zhang, Yimi.(2025).The 3D lithospheric structure of China Seas and adjacent areas: Combining geoid, gravity, and topography data.GONDWANA RESEARCH,144,151-166.
MLA Ma, Jing,et al."The 3D lithospheric structure of China Seas and adjacent areas: Combining geoid, gravity, and topography data".GONDWANA RESEARCH 144(2025):151-166.

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来源:海洋研究所

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