Continental growth and secular evolution: Constraints from U-Pb ages and Hf isotope of detrital zircons in Proterozoic Jixian sedimentary section (1.8-0.8 Ga), North China Craton

doi:10.1016/j.precamres.2011.07.007

	Continental growth and secular evolution: Constraints from U-Pb ages and Hf isotope of detrital zircons in Proterozoic Jixian sedimentary section (1.8-0.8 Ga), North China Craton
	Ying, Ji-Feng; Zhou, Xin-Hua; Su, Ben-Xun; Tang, Yan-Jie
刊名	PRECAMBRIAN RESEARCH
	2011-09-01
卷号	189 期号:3-4 页码:229-238
关键词	Crustal growth Detrital zircon Sedimentary rocks North China Craton
ISSN号	0301-9268
DOI	10.1016/j.precamres.2011.07.007
文献子类	Article
英文摘要	In order to understand the Precambrian crustal growth and reworking history of the North China Craton, in situ U-Pb and Lu-Hf isotope analyses were carried out on the detrital zircons from a well-preserved, nearly undeformed Proterozoic sedimentary section with time interval of 1.8-0.8 Ga. Totally, 806 zircons separated from 7 samples collected from each representative stratigraphic unit were measured for U-Pb and Lu-Hf isotopic compositions, of which 430 grains yielded concordant U-Pb ages. The concordant zircons show three prominent age groups of 1.6-1.8 Ga, 1.9-2.2 Ga and 2.3-2.6 Ga. Both positive and negative epsilon Hf(t) values were exhibited by zircons from all groups, suggesting both juvenile crust addition and crustal reworking for all age groups. The Hf crustal model ages of zircons reveal that the juvenile materials were continuously added to the crust between 4.0 and 2.0 Ga with a prominent peak at 2.7-3.0 Ga and a less significant peak at 3.1-3.4 Ga. The juvenile contributions to the newly formed crust decrease step-wise through time, and crustal reworking has dominated over juvenile inputs to the continental crust since 2.6 Ga. Compared with the detrital zircons from modern rivers running within the North China Craton, the sedimentary rocks contain more older zircons, implying the relatively poor preservation of Archean crustal rocks in modern river sand, and accordingly the weights of Archean crystallizations ages and crustal growth inferred from detrital zircons in modern river are significantly underestimated. The integrated studies of detrital zircons from both modern river sands and ancient sedimentary rocks are essential to decipher the early crustal growth history more faithfully. (C) 2011 Elsevier B.V. All rights reserved.
WOS关键词	EPISODIC CRUSTAL GROWTH ; LASER-ABLATION ; TRACE-ELEMENT ; LU-HF ; XIAMALING FORMATION ; TECTONIC EVOLUTION ; OXYGEN ISOTOPES ; MANTLE ; SUPERCONTINENT ; GEOCHRONOLOGY
WOS研究方向	Geology
语种	英语
出版者	ELSEVIER SCIENCE BV
WOS记录号	WOS:000295767500001
资助机构	National Natural Science Foundation of China(40673034 ; National Natural Science Foundation of China(40673034 ; National Natural Science Foundation of China(40673034 ; National Natural Science Foundation of China(40673034 ; Chinese Academy of Sciences(KZCX2-YW-Q08-3-1) ; Chinese Academy of Sciences(KZCX2-YW-Q08-3-1) ; Chinese Academy of Sciences(KZCX2-YW-Q08-3-1) ; Chinese Academy of Sciences(KZCX2-YW-Q08-3-1) ; 40973027 ; 40973027 ; 40973027 ; 40973027 ; 90714008) ; 90714008) ; 90714008) ; 90714008) ; National Natural Science Foundation of China(40673034 ; National Natural Science Foundation of China(40673034 ; National Natural Science Foundation of China(40673034 ; National Natural Science Foundation of China(40673034 ; Chinese Academy of Sciences(KZCX2-YW-Q08-3-1) ; Chinese Academy of Sciences(KZCX2-YW-Q08-3-1) ; Chinese Academy of Sciences(KZCX2-YW-Q08-3-1) ; Chinese Academy of Sciences(KZCX2-YW-Q08-3-1) ; 40973027 ; 40973027 ; 40973027 ; 40973027 ; 90714008) ; 90714008) ; 90714008) ; 90714008) ; National Natural Science Foundation of China(40673034 ; National Natural Science Foundation of China(40673034 ; National Natural Science Foundation of China(40673034 ; National Natural Science Foundation of China(40673034 ; Chinese Academy of Sciences(KZCX2-YW-Q08-3-1) ; Chinese Academy of Sciences(KZCX2-YW-Q08-3-1) ; Chinese Academy of Sciences(KZCX2-YW-Q08-3-1) ; Chinese Academy of Sciences(KZCX2-YW-Q08-3-1) ; 40973027 ; 40973027 ; 40973027 ; 40973027 ; 90714008) ; 90714008) ; 90714008) ; 90714008) ; National Natural Science Foundation of China(40673034 ; National Natural Science Foundation of China(40673034 ; National Natural Science Foundation of China(40673034 ; National Natural Science Foundation of China(40673034 ; Chinese Academy of Sciences(KZCX2-YW-Q08-3-1) ; Chinese Academy of Sciences(KZCX2-YW-Q08-3-1) ; Chinese Academy of Sciences(KZCX2-YW-Q08-3-1) ; Chinese Academy of Sciences(KZCX2-YW-Q08-3-1) ; 40973027 ; 40973027 ; 40973027 ; 40973027 ; 90714008) ; 90714008) ; 90714008) ; 90714008)
内容类型	期刊论文
源URL	[http://ir.iggcas.ac.cn/handle/132A11/74642]
专题	中国科学院地质与地球物理研究所
通讯作者	Zhou, Xin-Hua
作者单位	Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
推荐引用方式 GB/T 7714	Ying, Ji-Feng,Zhou, Xin-Hua,Su, Ben-Xun,et al. Continental growth and secular evolution: Constraints from U-Pb ages and Hf isotope of detrital zircons in Proterozoic Jixian sedimentary section (1.8-0.8 Ga), North China Craton[J]. PRECAMBRIAN RESEARCH,2011,189(3-4):229-238.
APA	Ying, Ji-Feng,Zhou, Xin-Hua,Su, Ben-Xun,&Tang, Yan-Jie.(2011).Continental growth and secular evolution: Constraints from U-Pb ages and Hf isotope of detrital zircons in Proterozoic Jixian sedimentary section (1.8-0.8 Ga), North China Craton.PRECAMBRIAN RESEARCH,189(3-4),229-238.
MLA	Ying, Ji-Feng,et al."Continental growth and secular evolution: Constraints from U-Pb ages and Hf isotope of detrital zircons in Proterozoic Jixian sedimentary section (1.8-0.8 Ga), North China Craton".PRECAMBRIAN RESEARCH 189.3-4(2011):229-238.