中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Destruction of the North China Craton in the Mesozoic

文献类型:期刊论文

作者Wu, Fu-Yuan1,2; Yang, Jin-Hui1,2; Xu, Yi-Gang3,4; Wilde, Simon A.5; Walker, Richard J.6
刊名ANNUAL REVIEW OF EARTH AND PLANETARY SCIENCES, VOL 47
出版日期2019
卷号47页码:173-+
关键词craton destruction North China Mesozoic oceanic subduction mantle plume
ISSN号0084-6597
DOI10.1146/annurev-earth-053018-060342
英文摘要The North China Craton (NCC) was originally formed by the amalgamation of the eastern and western blocks along an orogenic belt at similar to 1.9 Ga. After cratonization, the NCC was essentially stable until the Mesozoic, when intense felsic magmatism and related mineralization, deformation, pull-apart basins, and exhumation of the deep crust widely occurred, indicative of destruction or decratonization. Accompanying this destruction was significant removal of the cratonic keel and lithospheric transformation, whereby the thick (similar to 200 km) and refractory Archean lithosphere mantle was replaced by a thin (<80 km) juvenile one. The decratonization of the NCC was driven by flat slab subduction, followed by a rollback of the paleo-Pacific plate during the late Mesozoic. A global synthesis indicates that cratons are mainly destroyed by oceanic subduction, although mantle plumes might also trigger lithospheric thinning through thermal erosion. Widespread crust-derived felsic magmatism and large-scale ductile deformation can be regarded as petrological and structural indicators of craton destruction. A craton, a kind of ancient continental block on Earth, was formed mostly in the early Precambrian (>1.8 Ga). A craton is characterized by a rigid lithospheric root, which provides longevity and stability during its evolutionary history. Some cratons, such as the North China Craton, can be destroyed by losing their stability, manifested by magmatism, deformation, earthquake, etc.
WOS关键词LITHOSPHERIC MANTLE BENEATH ; SINO-KOREAN CRATON ; CENOZOIC INTRAPLATE BASALTS ; SUBCONTINENTAL LITHOSPHERE ; PERIDOTITE XENOLITHS ; TECTONIC EVOLUTION ; LIAODONG PENINSULA ; WATER-CONTENT ; REFERTILIZATION ; GEOCHEMISTRY
WOS研究方向Astronomy & Astrophysics ; Geology
语种英语
WOS记录号WOS:000470274200008
出版者ANNUAL REVIEWS
源URL[http://ir.iggcas.ac.cn/handle/132A11/92271]  
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Wu, Fu-Yuan
作者单位1.Chinese Acad Sci, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, Inst Earth Sci, Beijing 100029, Peoples R China
3.Chinese Acad Sci, State Key Lab Isotope Geochem, Guangzhou 510640, Guangdong, Peoples R China
4.Chinese Acad Sci, Inst Earth Sci, Guangzhou Inst Geochem, Guangzhou 510640, Guangdong, Peoples R China
5.Curtin Univ Technol, Inst Geosci Res, Dept Appl Geol, Perth, WA 6845, Australia
6.Univ Maryland, Dept Geol, Isotope Geochem Lab, College Pk, MD 20742 USA
推荐引用方式
GB/T 7714
Wu, Fu-Yuan,Yang, Jin-Hui,Xu, Yi-Gang,et al. Destruction of the North China Craton in the Mesozoic[J]. ANNUAL REVIEW OF EARTH AND PLANETARY SCIENCES, VOL 47,2019,47:173-+.
APA Wu, Fu-Yuan,Yang, Jin-Hui,Xu, Yi-Gang,Wilde, Simon A.,&Walker, Richard J..(2019).Destruction of the North China Craton in the Mesozoic.ANNUAL REVIEW OF EARTH AND PLANETARY SCIENCES, VOL 47,47,173-+.
MLA Wu, Fu-Yuan,et al."Destruction of the North China Craton in the Mesozoic".ANNUAL REVIEW OF EARTH AND PLANETARY SCIENCES, VOL 47 47(2019):173-+.

入库方式: OAI收割

来源:地质与地球物理研究所

浏览0
下载0
收藏0
其他版本

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。