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Precambrian crustal evolution of the eastern North China Craton as revealed by U-Pb ages and Hf isotopes of detrital zircons from the Proterozoic Jing'eryu Formation

文献类型：期刊论文

作者Sun, Jin-Feng1,2; Yang, Jin-Hui2; Wu, Fu-Yuan2; Wilde, Simon A.3
刊名PRECAMBRIAN RESEARCH
出版日期2012-04-01
卷号200页码:184-208
关键词North China Craton Eastern Block Crustal evolution Detrital zircon U-Pb age and Hf isotope
ISSN号0301-9268
DOI10.1016/j.precamres.2012.01.018
文献子类Article
英文摘要Simultaneous in situ U-Pb dating, trace element and Hf isotopic analyses have been carried out on detrital zircons obtained from sandstones in the Neoproterozoic Jing'eryu Formation from the Eastern Block, North China Craton (NCC), with the aim of constraining the ages of magmatic and metamorphic events and hence the Precambrian crustal evolution of the NCC. Two groups of zircons, i.e., magmatic and metamorphic in origin, have been identified based on cathodoluminescence images, zircon Ti-temperatures and Th/U ratios. Zircon U-Pb dating shows two main magmatic events with ages of 2.55-2.47 Ga and 1.80-1.70 Ga, and four metamorphic events, with ages of 2.51-2.48 Ga, 1.96-1.90 Ga, 1.87-1.85 Ga and similar to 1.80 Ga in the NCC. No zircons with ages of similar to 3.8 Ga have been identified in this study, indicating either these were covered at the time of deposition or the limited presence of 3.8 Ga rocks in the NCC.
WOS关键词SINO-KOREAN CRATON ; ND ISOCHRON AGE ; TI-IN-ZIRCON ; LU-HF ; GEOLOGICAL SIGNIFICANCE ; HEBEI PROVINCE ; ICP-MS ; SM-ND ; TECTONIC EVOLUTION ; CONTINENTAL-CRUST
WOS研究方向Geology
语种英语
WOS记录号WOS:000302593700011
出版者ELSEVIER SCIENCE BV
资助机构NSFC(40925007 ; NSFC(40925007 ; NSFC(40925007 ; NSFC(40925007 ; State Key Laboratory of Lithospheric Evolution(Zhuan0809) ; State Key Laboratory of Lithospheric Evolution(Zhuan0809) ; State Key Laboratory of Lithospheric Evolution(Zhuan0809) ; State Key Laboratory of Lithospheric Evolution(Zhuan0809) ; 40873010) ; 40873010) ; 40873010) ; 40873010) ; NSFC(40925007 ; NSFC(40925007 ; NSFC(40925007 ; NSFC(40925007 ; State Key Laboratory of Lithospheric Evolution(Zhuan0809) ; State Key Laboratory of Lithospheric Evolution(Zhuan0809) ; State Key Laboratory of Lithospheric Evolution(Zhuan0809) ; State Key Laboratory of Lithospheric Evolution(Zhuan0809) ; 40873010) ; 40873010) ; 40873010) ; 40873010) ; NSFC(40925007 ; NSFC(40925007 ; NSFC(40925007 ; NSFC(40925007 ; State Key Laboratory of Lithospheric Evolution(Zhuan0809) ; State Key Laboratory of Lithospheric Evolution(Zhuan0809) ; State Key Laboratory of Lithospheric Evolution(Zhuan0809) ; State Key Laboratory of Lithospheric Evolution(Zhuan0809) ; 40873010) ; 40873010) ; 40873010) ; 40873010) ; NSFC(40925007 ; NSFC(40925007 ; NSFC(40925007 ; NSFC(40925007 ; State Key Laboratory of Lithospheric Evolution(Zhuan0809) ; State Key Laboratory of Lithospheric Evolution(Zhuan0809) ; State Key Laboratory of Lithospheric Evolution(Zhuan0809) ; State Key Laboratory of Lithospheric Evolution(Zhuan0809) ; 40873010) ; 40873010) ; 40873010) ; 40873010)
源URL[http://ir.iggcas.ac.cn/handle/132A11/84588]  
专题中国科学院地质与地球物理研究所
通讯作者Sun, Jin-Feng
作者单位1.Chinese Acad Sci, Grad Univ, Beijing 100049, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
3.Curtin Univ Technol, Dept Appl Geol, Perth, WA 6845, Australia
推荐引用方式
GB/T 7714		 Sun, Jin-Feng,Yang, Jin-Hui,Wu, Fu-Yuan,et al. Precambrian crustal evolution of the eastern North China Craton as revealed by U-Pb ages and Hf isotopes of detrital zircons from the Proterozoic Jing'eryu Formation[J]. PRECAMBRIAN RESEARCH,2012,200:184-208.
APA Sun, Jin-Feng,Yang, Jin-Hui,Wu, Fu-Yuan,&Wilde, Simon A..(2012).Precambrian crustal evolution of the eastern North China Craton as revealed by U-Pb ages and Hf isotopes of detrital zircons from the Proterozoic Jing'eryu Formation.PRECAMBRIAN RESEARCH,200,184-208.
MLA Sun, Jin-Feng,et al."Precambrian crustal evolution of the eastern North China Craton as revealed by U-Pb ages and Hf isotopes of detrital zircons from the Proterozoic Jing'eryu Formation".PRECAMBRIAN RESEARCH 200(2012):184-208.

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来源：地质与地球物理研究所

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