The subduction of the west Pacific plate and the destruction of the North China Craton
文献类型：期刊论文
| 作者 | Zhu, Rixiang1,3; Xu, Yigang2,3 |
| 刊名 | SCIENCE CHINA-EARTH SCIENCES
 |
| 出版日期 | 2019-09-01 |
| 卷号 | 62期号:9页码:1340-1350 |
| 关键词 | Early Creatceous Cratonic destruction Subduction of west Pacific plate |
| ISSN号 | 1674-7313 |
| DOI | 10.1007/s11430-018-9356-y |
| 英文摘要 | While a general concensus has recently been reached as to the causal relationship between the subduction of the west Pacific plate and the destruction of the North China Craton, a number of important questions remain to answer, including the initial subduction of west Pacific plate beneath the eastern Asian continent, the position of west Pacific subduction zone during the peak period of decratonization (i.e., Early Cretaceous), the formation age of the big mantle wedge under eastern Asia, and the fate of the subducted Pacific slab. Integration of available data suggests that the subduction of the western Pacific plate was initiated as early as Early Jurrasic and the subduction zone was situated to 2,200 km west of the present-day trench in the Early Creataceous, as a result of eastward migration of the Asian continent over a distance of ca. 900 km since the Early Cretaceous. The retreat of the subducting west Pacific plate started similar to 145 Ma ago, corresponding to the initial formation of the big mantle wedge system in the Early Cretaceous. The subduction of the Pacific slab excerted severe influence on the North China Craton most likely through material and energy echange between the big mantle wedge and overlying cratonic lithosphere. The evolution history of the west Pacific plate was reconstructed based on tectonic events. This allows to propose that the causes of phases A and B for the Yanshanian orogeny were respectively related to rapid low-angle subduction and to lowering subduction angle of the west Pacific plate. At ca. 130-120 Ma, the subduction of the west Pacific plate was characterized by increasing subducting angle, slab rollback and rapid trench retreat, leading to the final stagnation of the subducting slab within the mantle transition zone. This process may have significantly affected the physical property and viscosity of the mantle wedge above the stagnant slab, resulting in non-steady mantle flows. The ingression of slab-released melts/fluids would significantly lower the viscosity of the mantle wedge and overlying lithosphere, inducing decratonization. This study yields important bearings on the relationship between the subduction of the west Pacific plate and the evolution of the lithospheric mantle beneath the North China Craton. |
| WOS关键词 | MESOZOIC VOLCANIC-ROCKS ; BIG MANTLE WEDGE ; NE CHINA ; SOUTH CHINA ; HEILONGJIANG PROVINCE ; CONTINENTAL-MARGIN ; EAST-ASIA ; BENEATH ; CONSTRAINTS ; GEOCHEMISTRY |
| 资助项目 | National Natural Science Foundation of China[1688103] ; Chinese Academy of Sciences Strategic Priority Program B[XDB18000000] ; State Oceanography Bureau[GASIGEOGE-02] |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000484999000002 |
| 出版者 | SCIENCE PRESS |
| 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 ; Chinese Academy of Sciences Strategic Priority Program B ; Chinese Academy of Sciences Strategic Priority Program B ; Chinese Academy of Sciences Strategic Priority Program B ; Chinese Academy of Sciences Strategic Priority Program B ; State Oceanography Bureau ; State Oceanography Bureau ; State Oceanography Bureau ; State Oceanography Bureau ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Chinese Academy of Sciences Strategic Priority Program B ; Chinese Academy of Sciences Strategic Priority Program B ; Chinese Academy of Sciences Strategic Priority Program B ; Chinese Academy of Sciences Strategic Priority Program B ; State Oceanography Bureau ; State Oceanography Bureau ; State Oceanography Bureau ; State Oceanography Bureau ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Chinese Academy of Sciences Strategic Priority Program B ; Chinese Academy of Sciences Strategic Priority Program B ; Chinese Academy of Sciences Strategic Priority Program B ; Chinese Academy of Sciences Strategic Priority Program B ; State Oceanography Bureau ; State Oceanography Bureau ; State Oceanography Bureau ; State Oceanography Bureau ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Chinese Academy of Sciences Strategic Priority Program B ; Chinese Academy of Sciences Strategic Priority Program B ; Chinese Academy of Sciences Strategic Priority Program B ; Chinese Academy of Sciences Strategic Priority Program B ; State Oceanography Bureau ; State Oceanography Bureau ; State Oceanography Bureau ; State Oceanography Bureau |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/93563]  |
| 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 | Zhu, Rixiang |
| 作者单位 | 1.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China 2.Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Isotope Geochem, Guangzhou 510640, Guangdong, Peoples R China 3.Univ Chinese Acad Sci, Sch Earth & Planetary Sci, Beijing 100049, Peoples R China |
| 推荐引用方式 GB/T 7714 | Zhu, Rixiang,Xu, Yigang. The subduction of the west Pacific plate and the destruction of the North China Craton[J]. SCIENCE CHINA-EARTH SCIENCES,2019,62(9):1340-1350. |
| APA | Zhu, Rixiang,&Xu, Yigang.(2019).The subduction of the west Pacific plate and the destruction of the North China Craton.SCIENCE CHINA-EARTH SCIENCES,62(9),1340-1350. |
| MLA | Zhu, Rixiang,et al."The subduction of the west Pacific plate and the destruction of the North China Craton".SCIENCE CHINA-EARTH SCIENCES 62.9(2019):1340-1350. |
入库方式： OAI收割
来源：地质与地球物理研究所
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