Heterogeneous destruction of the North China Craton: Coupled constraints from seismology and geodynamic numerical modeling

doi:10.1007/s11430-017-9142-1

CORC > 地质与地球物理研究所 > 中国科学院地质与地球物理研究所 > 岩石圈演化国家重点实验室

	Heterogeneous destruction of the North China Craton: Coupled constraints from seismology and geodynamic numerical modeling
	Wang, Kun 1,2; Zhao, Liang 1,2; Xu, Xiaobing 1,2; Yang, Jianfeng 1,2
刊名	SCIENCE CHINA-EARTH SCIENCES
	2018-05-01
卷号	61 期号:5 页码:515-526
关键词	North China Craton Heterogeneity Seismic tomography Numerical modeling
ISSN号	1674-7313
DOI	10.1007/s11430-017-9142-1
文献子类	Review
英文摘要	The prevailing academic view regards mantle flow and the metasomatism triggered by the subduction of the Pacific plate as the cause and mechanism for the destruction of the North China Craton (NCC). However, the geodynamic destruction process remains ambiguous, necessitating detailed information at this stage. Combining the structural images obtained by the exploration of dense seismic arrays and the geodynamic simulations inspired by numerical modeling, this paper arrives at the following conclusions: the spatial variation of the P- and S-wave velocities, as well as their velocity ratio in the mantle transition zone, are key evidences of the nonuniform dehydration of the Pacific plate, the subducted plate induces hot upwellings in the mantle transition zone (MTZ), resulting in the heterogeneous distribution of the melt/fluid beneath the craton, characterized by small scale anomalies in the seismic velocity field, and as revealed by dense seismic array observation, the heterogeneities in the upper mantle structure and deformation are the synthetic results of lithospheric strain localization and the heterogeneous distribution of the melt/fluid. It is known that the nonuniform dehydration of the Pacific slab and the heterogeneous distribution of the melt/fluid have occured in the Cenozoic. If these scenarios could have already occurred in the Early Cretaceous, their interaction with the NCC lithosphere would be the dynamic mechanism for the heterogeneous lithospheric destruction of the NCC. The inference in this study is significant for further reconciling the multidisciplinary evidences in the NCC.
WOS关键词	METAMORPHIC CORE COMPLEXES ; MANTLE TRANSITION ZONE ; LITHOSPHERIC MANTLE ; WATER-CONTENT ; ELECTRICAL-CONDUCTIVITY ; CONTINENTAL BASALTS ; SEISMIC ANISOTROPY ; VELOCITY STRUCTURE ; EASTERN CHINA ; SUBDUCTION
WOS研究方向	Geology
语种	英语
出版者	SCIENCE PRESS
WOS记录号	WOS:000430858000002
资助机构	National Natural Science Foundation of China(91414301 ; National Natural Science Foundation of China(91414301 ; National Natural Science Foundation of China(91414301 ; National Natural Science Foundation of China(91414301 ; National Natural Science Foundation of China(91414301 ; National Natural Science Foundation of China(91414301 ; National Natural Science Foundation of China(91414301 ; National Natural Science Foundation of China(91414301 ; 41604081) ; 41604081) ; 41604081) ; 41604081) ; 41604081) ; 41604081) ; 41604081) ; 41604081) ; National Natural Science Foundation of China(91414301 ; National Natural Science Foundation of China(91414301 ; National Natural Science Foundation of China(91414301 ; National Natural Science Foundation of China(91414301 ; National Natural Science Foundation of China(91414301 ; National Natural Science Foundation of China(91414301 ; National Natural Science Foundation of China(91414301 ; National Natural Science Foundation of China(91414301 ; 41604081) ; 41604081) ; 41604081) ; 41604081) ; 41604081) ; 41604081) ; 41604081) ; 41604081) ; National Natural Science Foundation of China(91414301 ; National Natural Science Foundation of China(91414301 ; National Natural Science Foundation of China(91414301 ; National Natural Science Foundation of China(91414301 ; National Natural Science Foundation of China(91414301 ; National Natural Science Foundation of China(91414301 ; National Natural Science Foundation of China(91414301 ; National Natural Science Foundation of China(91414301 ; 41604081) ; 41604081) ; 41604081) ; 41604081) ; 41604081) ; 41604081) ; 41604081) ; 41604081) ; National Natural Science Foundation of China(91414301 ; National Natural Science Foundation of China(91414301 ; National Natural Science Foundation of China(91414301 ; National Natural Science Foundation of China(91414301 ; National Natural Science Foundation of China(91414301 ; National Natural Science Foundation of China(91414301 ; National Natural Science Foundation of China(91414301 ; National Natural Science Foundation of China(91414301 ; 41604081) ; 41604081) ; 41604081) ; 41604081) ; 41604081) ; 41604081) ; 41604081) ; 41604081)
内容类型	期刊论文
源URL	[http://ir.iggcas.ac.cn/handle/132A11/88294]
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	Zhao, Liang
作者单位	1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China 2.Chinese Acad Sci, Inst Earth Sci, Beijing 100029, Peoples R China
推荐引用方式 GB/T 7714	Wang, Kun,Zhao, Liang,Xu, Xiaobing,et al. Heterogeneous destruction of the North China Craton: Coupled constraints from seismology and geodynamic numerical modeling[J]. SCIENCE CHINA-EARTH SCIENCES,2018,61(5):515-526.
APA	Wang, Kun,Zhao, Liang,Xu, Xiaobing,&Yang, Jianfeng.(2018).Heterogeneous destruction of the North China Craton: Coupled constraints from seismology and geodynamic numerical modeling.SCIENCE CHINA-EARTH SCIENCES,61(5),515-526.
MLA	Wang, Kun,et al."Heterogeneous destruction of the North China Craton: Coupled constraints from seismology and geodynamic numerical modeling".SCIENCE CHINA-EARTH SCIENCES 61.5(2018):515-526.