Late Cretaceous to Early Cenozoic extension in the Lower Yangtze region (East China) driven by Izanagi-Pacific plate subduction
文献类型：期刊论文
| 作者 | Xu, Xi1,6,7,8,9; Zuza, Andrew, V3; Chen, Lin4; Zhu, Weilin5,6; Yin, An1; Fu, Xiaowei6; Gao, Shunli2; Xu, Xuhui10; Kuang, Xingtao8,9; Zhang, Fengqi7 |
| 刊名 | EARTH-SCIENCE REVIEWS
 |
| 出版日期 | 2021-10-01 |
| 卷号 | 221页码:25 |
| ISSN号 | 0012-8252 |
| 关键词 | East Asia Lower Yangtze region Extensional tectonics Izanagi-Pacific plate Oceanic slab subduction Big mantle wedge |
| DOI | 10.1016/j.earscirev.2021.103790 |
| 英文摘要 | The intracontinental response to plate-boundary and mantle processes, such as subduction or continental collisions, is an important topic in the Earth Sciences. Cretaceous to Cenozoic extension across East China is related to the interaction between the Asian continental lithosphere and western Pacific oceanic subduction system, and the associated intra-plate structures and basins provide robust temporal and spatial records of regional continental deformation. Although extension may primarily be driven by slab rollback and/or back-arc opening, midocean-ridge subduction may have played a significant role in this process. To explore how the western Pacific subduction system impacts intracontinental deformation across East China, we use onshore-offshore geological records, geophysical survey observations, and time-dependent Pacific plate models to document the temporal and spatial variation of continental deformation in the Lower Yangtze region adjacent to the Yellow Sea. Based on our compilation, we argue that mantle-wedge convection, with coupled subduction of the trench-parallel Izanagi (Paleo-Pacific)-Pacific mid-ocean ridge, exerts a first-order control on extensional deformation in East China. Beneath eastern China, the mantle wedge history consists of two phases: (1) initial development of the mantle wedge as the Cretaceous Izanagi slab transitioned from flat-slab to steep subduction; and (2) mature mantle wedge convection during Cenozoic subduction of the Pacific plate. Relatively steep subduction of the progressively younging Izanagi plate during the Late Cretaceous-Paleocene resulted in strong mantle convection and coupled upper plate extension in eastern China. The collision of the Izanagi-Pacific plate ridge system with the trench resulted in a magmatic gap and short-lived uplift of eastern China. Following this, subduction of the rapidly aging Pacific plate resulted in a larger, but relatively weaker, mantle convection cell that drove weaker upper plate extension. The vigor of wedge mantle convection was modulated by the age of the Pacific subducting slab, which directly influenced the formation and evolution of intracontinental extension and sedimentary basins across eastern China. The pre-existing Triassic Tan-Lu fault zone has reactivated since the Late Eocene (ca. 40 Ma) due to westward subduction of the Pacific slab to partition strain between extensional dextral faulting in the Bohai Bay and Lower Yangtze basins, thereby diversifying Cenozoic lithospheric extensional deformation in eastern China. Several major Cenozoic extensional basins spatially correlate with the Triassic Sulu orogenic belt, which we interpret to suggest that these basins are underlain by the older and fragmented orogenic basement that acted as mechanically weak zones for localized high-magnitude extension. We present a comprehensive |
| WOS关键词 | TAN-LU FAULT ; BOHAI BAY BASIN ; MESOZOIC SEDIMENTARY BASINS ; TRANSITION-ZONE INTERACTION ; STRIKE-SLIP DEFORMATION ; ASIA COLLISION ONSET ; NORTH CHINA ; SOUTH CHINA ; TECTONIC EVOLUTION ; OROGENIC BELT |
| 资助项目 | National Natural Science Foundation of China[41902202] ; National Science Foundation[EAR 1914501] ; Chinese Postdoctoral Science Foundation[2019M652062] ; Key Laboratory of Airborne Geophysics and Remote Sensing Geology Ministry of Natural Resources[2020YFL13] ; State Key Scientific Research Program of China[2011ZX0523-003] ; Geological Survey Project of China[DD20211396] |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| 出版者 | ELSEVIER |
| WOS记录号 | WOS:000703698300001 |
| 资助机构 | National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Science Foundation ; National Science Foundation ; Chinese Postdoctoral Science Foundation ; Chinese Postdoctoral Science Foundation ; Key Laboratory of Airborne Geophysics and Remote Sensing Geology Ministry of Natural Resources ; Key Laboratory of Airborne Geophysics and Remote Sensing Geology Ministry of Natural Resources ; State Key Scientific Research Program of China ; State Key Scientific Research Program of China ; Geological Survey Project of China ; Geological Survey Project of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Science Foundation ; National Science Foundation ; Chinese Postdoctoral Science Foundation ; Chinese Postdoctoral Science Foundation ; Key Laboratory of Airborne Geophysics and Remote Sensing Geology Ministry of Natural Resources ; Key Laboratory of Airborne Geophysics and Remote Sensing Geology Ministry of Natural Resources ; State Key Scientific Research Program of China ; State Key Scientific Research Program of China ; Geological Survey Project of China ; Geological Survey Project of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Science Foundation ; National Science Foundation ; Chinese Postdoctoral Science Foundation ; Chinese Postdoctoral Science Foundation ; Key Laboratory of Airborne Geophysics and Remote Sensing Geology Ministry of Natural Resources ; Key Laboratory of Airborne Geophysics and Remote Sensing Geology Ministry of Natural Resources ; State Key Scientific Research Program of China ; State Key Scientific Research Program of China ; Geological Survey Project of China ; Geological Survey Project of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Science Foundation ; National Science Foundation ; Chinese Postdoctoral Science Foundation ; Chinese Postdoctoral Science Foundation ; Key Laboratory of Airborne Geophysics and Remote Sensing Geology Ministry of Natural Resources ; Key Laboratory of Airborne Geophysics and Remote Sensing Geology Ministry of Natural Resources ; State Key Scientific Research Program of China ; State Key Scientific Research Program of China ; Geological Survey Project of China ; Geological Survey Project of China |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/102695]  |
| 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 | Xu, Xi |
| 作者单位 | 1.Univ Calif Los Angeles, Dept Earth Planetary & Space Sci, Los Angeles, CA 90925 USA 2.China Natl Offshore Oil Corp CNOOC China Ltd Shan, Shanghai 200092, Peoples R China 3.Univ Nevada, Nevada Bur Mines & Geol, Reno, NV 89557 USA 4.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China 5.China Natl Offshore Oil Corp CNOOC, Beijing 100010, Peoples R China 6.Tongji Univ, Sch Ocean & Earth Sci, Shanghai 200092, Peoples R China 7.Zhejiang Univ, Sch Earth Sci, Hangzhou 310027, Peoples R China 8.China Geol Survey, Remote Sensing Ctr Nat Resources, Beijing 100083, Peoples R China 9.China Geol Survey, China Aero Geophys Survey, Beijing 100083, Peoples R China 10.SINOPEC Petr Explorat & Prod Res Inst, Beijing 100083, Peoples R China |
| 推荐引用方式 GB/T 7714 | Xu, Xi,Zuza, Andrew, V,Chen, Lin,et al. Late Cretaceous to Early Cenozoic extension in the Lower Yangtze region (East China) driven by Izanagi-Pacific plate subduction[J]. EARTH-SCIENCE REVIEWS,2021,221:25. |
| APA | Xu, Xi.,Zuza, Andrew, V.,Chen, Lin.,Zhu, Weilin.,Yin, An.,...&Yang, Shufeng.(2021).Late Cretaceous to Early Cenozoic extension in the Lower Yangtze region (East China) driven by Izanagi-Pacific plate subduction.EARTH-SCIENCE REVIEWS,221,25. |
| MLA | Xu, Xi,et al."Late Cretaceous to Early Cenozoic extension in the Lower Yangtze region (East China) driven by Izanagi-Pacific plate subduction".EARTH-SCIENCE REVIEWS 221(2021):25. |
入库方式： OAI收割
来源：地质与地球物理研究所
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