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U-Pb dating and Hf isotope study of detrital zircons from the Zhifu Group, Jiaobei Terrane, North China Craton: Provenance and implications for Precambrian crustal growth and recycling

文献类型：期刊论文

作者Liu, Jianhui1; Liu, Fulai1; Ding, Zhengjiang2,3; Yang, Hong1; Liu, Chaohui1; Liu, Pinghua1; Xiao, Lingling1; Zhao, Lei4; Geng, Jianzhen5
刊名PRECAMBRIAN RESEARCH
出版日期2013-09-01
卷号235页码:230-250
关键词North China Craton Jiaobei Terrane Zhifu Group Detrital Zircon Crustal Growth And Recycling
ISSN号0301-9268
DOI10.1016/j.precamres.2013.06.014
文献子类Article
英文摘要The Zhifu Group exposed in the northeastern Jiaobei Terrane is subdivided from base to top into the Laoyeshan, Bingying and Dongkou formations, and comprises mainly quartzites and muscovite- and tourmaline-bearing quartz schists. In order to define its provenance and depositional age, and to constrain the crustal growth and recycling of the source regions, we have conducted LA-ICP-MS U-Pb dating and in situ Hf isotopic study of detrital zircons from three quartz schists samples collected from the Zhifu Group. Most of the analyzed zircon grains have oscillatory zoning and Th/U ratios >0.4, suggesting igneous origins. 270 detrital zircons U-Pb analyses yield U-Pb ages of 1709-3679 Ma that cluster into three major age populations of 1.7-1.9 Ga with a peak at 1844 Ma, 1.9-2.0 Ga with a peak at 1936 Ma and 2.4-2.55 Ga with a peak at 2465 Ma, and two minor age populations of 2.2-2.35 and 2.6-2.7 Ga. The peaking age of 1844 Ma for the youngest age population indicates that the Zhifu Group must be deposited after 1844 Ma. Detrital zircons with ages of 1.7-2.35 Ga can be linked to pre- and post-tectonic polyphase magmatic events along the JLJB, and most of the zircons have negative epsilon(Hf(t)) values from +1.76 to -18.02 and two-stage Hf model ages (T-DM2) concentrating at similar to 2.7-3.0 Ga, indicating that source rocks of these zircons were derived from recycling of ancient crusts. Detrital zircons with ages of 2.4-2.9 Ga may have been sourced from the Archean granitoid (mainly TTG) gneisses in the Jiaobei Terrane, and these zircons have epsilon(Hf(t)) values from +6.4 to -7.53 and T-Dm2 of 2.6-3.4 Ga (peak at similar to 2.7-3.0 Ga), suggesting that source rocks of these zircons were mainly derived from juvenile crusts associated with a major crustal growth at similar to 2.7-3.0 Ga, and a limited amount of ancient crustal component. The two detrital zircons with ages of 3631 and 3679 Ma have negative epsilon(Hf(t)) values of -4.42 and -1.51 and T-Dm2 of 4137 and 4000 Ma, respectively, implying the recycling of ancient continental crust (>3.6 Ga) and crustal growth prior to 4.1 Ga in the NCC. (C) 2013 Elsevier B.V. All rights reserved.
WOS关键词LIAO-JI BELT ; PRESSURE MAFIC GRANULITES ; MAJOR TECTONIC UNITS ; METAMORPHIC EVOLUTION ; WESTERN BLOCK ; EASTERN BLOCK ; LU-HF ; JINING COMPLEX ; T PATH ; DEFORMATION HISTORY
WOS研究方向Geology
语种英语
WOS记录号WOS:000328522400013
出版者ELSEVIER SCIENCE BV
资助机构Major State Basic Research Development Program of China(2012CB416603) ; Major State Basic Research Development Program of China(2012CB416603) ; National Science Foundation of China(41102127 ; National Science Foundation of China(41102127 ; Basic Scientific Research Foundations of the Institute of Geology, CAGS(J1214 ; Basic Scientific Research Foundations of the Institute of Geology, CAGS(J1214 ; Geological Survey Funds of the China Geological Survey(1212011120150) ; Geological Survey Funds of the China Geological Survey(1212011120150) ; Shandong PRO(066) ; Shandong PRO(066) ; Fundamental Research Funds for the Central Universities(13CX02036A) ; Fundamental Research Funds for the Central Universities(13CX02036A) ; 40725007 ; 40725007 ; J1005) ; J1005) ; 41202075) ; 41202075) ; Major State Basic Research Development Program of China(2012CB416603) ; Major State Basic Research Development Program of China(2012CB416603) ; National Science Foundation of China(41102127 ; National Science Foundation of China(41102127 ; Basic Scientific Research Foundations of the Institute of Geology, CAGS(J1214 ; Basic Scientific Research Foundations of the Institute of Geology, CAGS(J1214 ; Geological Survey Funds of the China Geological Survey(1212011120150) ; Geological Survey Funds of the China Geological Survey(1212011120150) ; Shandong PRO(066) ; Shandong PRO(066) ; Fundamental Research Funds for the Central Universities(13CX02036A) ; Fundamental Research Funds for the Central Universities(13CX02036A) ; 40725007 ; 40725007 ; J1005) ; J1005) ; 41202075) ; 41202075) ; Major State Basic Research Development Program of China(2012CB416603) ; Major State Basic Research Development Program of China(2012CB416603) ; National Science Foundation of China(41102127 ; National Science Foundation of China(41102127 ; Basic Scientific Research Foundations of the Institute of Geology, CAGS(J1214 ; Basic Scientific Research Foundations of the Institute of Geology, CAGS(J1214 ; Geological Survey Funds of the China Geological Survey(1212011120150) ; Geological Survey Funds of the China Geological Survey(1212011120150) ; Shandong PRO(066) ; Shandong PRO(066) ; Fundamental Research Funds for the Central Universities(13CX02036A) ; Fundamental Research Funds for the Central Universities(13CX02036A) ; 40725007 ; 40725007 ; J1005) ; J1005) ; 41202075) ; 41202075) ; Major State Basic Research Development Program of China(2012CB416603) ; Major State Basic Research Development Program of China(2012CB416603) ; National Science Foundation of China(41102127 ; National Science Foundation of China(41102127 ; Basic Scientific Research Foundations of the Institute of Geology, CAGS(J1214 ; Basic Scientific Research Foundations of the Institute of Geology, CAGS(J1214 ; Geological Survey Funds of the China Geological Survey(1212011120150) ; Geological Survey Funds of the China Geological Survey(1212011120150) ; Shandong PRO(066) ; Shandong PRO(066) ; Fundamental Research Funds for the Central Universities(13CX02036A) ; Fundamental Research Funds for the Central Universities(13CX02036A) ; 40725007 ; 40725007 ; J1005) ; J1005) ; 41202075) ; 41202075)
源URL[http://ir.iggcas.ac.cn/handle/132A11/86342]  
专题中国科学院地质与地球物理研究所
通讯作者Liu, Jianhui
作者单位1.Chinese Acad Geol Sci, Inst Geol, Beijing 100037, Peoples R China
2.Jilin Univ, Coll Earth Sci, Changchun 130061, Peoples R China
3.Explorat Inst Geol & Mineral Resources, Yantai 264000, Peoples R China
4.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
5.Tianjin Inst Geol & Mineral Resources, Tianjin 300170, Peoples R China
推荐引用方式
GB/T 7714		 Liu, Jianhui,Liu, Fulai,Ding, Zhengjiang,et al. U-Pb dating and Hf isotope study of detrital zircons from the Zhifu Group, Jiaobei Terrane, North China Craton: Provenance and implications for Precambrian crustal growth and recycling[J]. PRECAMBRIAN RESEARCH,2013,235:230-250.
APA Liu, Jianhui.,Liu, Fulai.,Ding, Zhengjiang.,Yang, Hong.,Liu, Chaohui.,...&Geng, Jianzhen.(2013).U-Pb dating and Hf isotope study of detrital zircons from the Zhifu Group, Jiaobei Terrane, North China Craton: Provenance and implications for Precambrian crustal growth and recycling.PRECAMBRIAN RESEARCH,235,230-250.
MLA Liu, Jianhui,et al."U-Pb dating and Hf isotope study of detrital zircons from the Zhifu Group, Jiaobei Terrane, North China Craton: Provenance and implications for Precambrian crustal growth and recycling".PRECAMBRIAN RESEARCH 235(2013):230-250.

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来源：地质与地球物理研究所

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