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《Acta Petrologica Sinica》 2006-02
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Petrogenesis of the Neoproterozoic strongly peraluminons granitoids from Northern Guangxi:constraints from zircon geochronology and Hf isotopes.

WANG XiaoLei~1 ZHOU JinCheng~1 QIU JianSheng~1 ZHANG WenLan~1 LIU XiaoMing~2 ZHANG GuiLin 1.State Key Laboratory for Mineral Deposits Research,Department of Earth Sciences,Nanjing University,Nanjing 210093,China 2.Department of Geology,Northwest University,Xi'an 710069,China 3.Department of Resource and Environmental Engineering,Guilin Institute of Technology,Guilin 541004,China  
The western end of the Proterozoic Jiangnan orogen is located at Northern Guangxi,South China.Neoproterozoic strongly peraluminous granitoids are dominant(>90%)in the area,with ca.8%being the mafic-ultramafic rocks.The granitoids in Northern Guangxi can be geochemically divided into two groups:granodiorites and granites.Their generations were previously considered to be related to a mantle plume(or superplume)event that led to the breakup of the Rodinia supercontinent.In this work,we present new laser ablation (LA)-ICP-MS U-Pb zircon dating and LA-MC-ICP-MS zircon Hf isotopic results for the granitoids from Northern Guangxi.The ages for the Zhaigun,Bendong,Dongma,Sanfang and Tianpeng granitic plutons are 835.8±2.5Ma,822.7±3.8Ma, 824±13Ma,804.3±5.2Ma and 794.2±8.1Ma,respectively.These dating results suggest that the two types of the granitoids in the area were formed in two episodes.The granodiorites formed at ca.835±820Ma,whereas the granites emplaced at ca.810~800Ma. The analyses for 8 spots of zircon cores and 2 spots from single zircon xenoliths show early Neoproterozoic ages ranging from ca.870 Ma to 950 Ma.These ages might record the subduction or collision-related magmatic events during 950~870 Ma in Northern Guangxi.Hf isotopes of zircons were also analyzed by La-MC-ICP-MS.The(~(176)Hf/~(177)Hf)_i ratios for the zircons from the Bendong,Sanfang and Tianpeng plutons are 0.282176±0.000021,0.282149±0.000021 and 0.282175±0.000030,respectively.Coupling zircon Hf isotopes and published whole rock Nd isotopes data suggest a basement sedimentary series source for the granitoids and the involvement of relatively more mantle-derived marie materials in the source of the granodiorites.The dating results also reveals a ca.35Ma magmatic duration,which is inconsistent with the plume models that predict widespread magmatic eruption and emplacement within period of 1- 5Ma.The Neoproterozoie granitoids from Northern Guangxi are generally plotted in the collision-related and post-collisional granites areas in the tectonic discrimination diagrams.They have been formed after the collision peak(ca.870 Ma) between the Yangtze and Cathysia blocks,belonging to the post-collisional granites.The upwelling of deep mantle due to the detachment of subdueted slab and the delamination of the lithosphere might cause the partial melting of the basement rocks to generate the strongly peraluminous granitoids.
【Fund】: 国家自然科学基金(批准号:40572039);; 国家创新研究群体科学基金(批准号:40221301);; 江苏省研究生创新工程和南京大学研究生创新中心资助.
【CateGory Index】: P588.121
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4 ZHANG Yong~(1,2),LIANG GuangLin~3,QU Xun~3,DU Shijun~1,WU Qi~(1,2),ZHANG ZhengFeng~3,DONG LianHui~(1,3) and XU XingWang~(1**) 1.Key Laboratory of Mineral Resources,Institute of Geology and Geophysics,CAS,Beijing 100029,China 2.Graduate School of Chinese Academy of Sciences,Beijing 100049,China 3.Xinjiang Bureau of Geology and Mineral Resources,Uramqi 830000,China;Evidence of U-Pb age and Hf isotope of zircons for Early Paleozoic magmatism in the Qiongheba arc,East Junggar[A];[C];2011
【Secondary Citations】
Chinese Journal Full-text Database 10 Hits
1 Liu Jiayuan(Institute of Hidden Ore Deposits Prognostication,Gullin College of Geology);TECTONIC EVOLUTION AND GENETIC TYPES OF THE PRECAMBRIAN GRANITOIDS IN SOUTH CHINA AND THEIR RELATIONSHIPS WITH MINERALIZATION[J];GEOLOGY OF ANHUI;1994-Z1
2 XIAO Yong-jun 1,2,CHEN Guang-hao1,FU Gong-gu1 (1.Changsha Institute of Geotectonics,Chinese Academy of Sciences,Changsha410013,China;2.Post-graduate School of the Chinese Academy of Sciences,Beijing100039);DISCUSSION ON THE TECTONOMETALLOGENIC BACKGROUND OF THE DAWAN GOLD ORE DISTRICT,NORTHEASTERN HUNAN PROVINCE[J];Geotectonica Et Metallogenia;2002-02
3 Wu Shi(Lab. of Isotopic Geology, Yichang Institute of Geology and Mineral Resources, National Geological General Administration);A STUDY ON ISOTOPIC GEOCHRONOLOGY OF LATE PROTOROZOIC BENDONG INTRUSIVE MASSIF, GUANGXI, CHINA[J];Geochimica;1979-03
4 Li Xianhua Zhao Zhenhua Gui Xuntang Yu Jinsheng(Institute of Geochemistry, Guangzhou Branch, Academia Sinica, 510640);Sm-Nd ISOTOPIC AND ZIRCON U-Pb CONSTRAINTS ON THE AGE OF FORMATION OF THE PRECAMBRIAN CRUST IN SOUTHEAST CHINA[J];Geochimica;1991-03
5 Cheng Hai Instituse of Ceology, Academa Sinica Beijing. 100029;GEOCHEMISTRY OF PROTEROZOIC ISLAND-ARC VOLCANIC ROCKS IN NORTHWEST ZHEJIANG[J];Geochimica;1993-01
6 GE Wen-chun, LI Xian-hua, LI Zheng-xiang, WANG Jian, ZHOU Han-wen, Lee Chi-yu (Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Cuangzhou 510640 China; Department of Geology and Geophysics, University of Western Australia, Nedlands,A6;Geological and geochemical evidence for the genesis of tremolitized mafic rocks from Baotan in northern Guangxi[J];GEOCHIMICA;2000-03
7 GE Wen- chun1, LI Xian- hua1, LI Zheng- xiang2, ZHOU Han- wen3, LEE Chi- yu4 (1. Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China; 2. Tectonic Special Research Center, Department of Geology and Geophysics, Univer;Geochemical studies on two types of Neoproterozoic peraluminous granitoids in northern Guangxi[J];Geochimica;2001-01
8 GE Wen- chun1, LI Xian- hua1, LIANG Xi- rong1, WANG Ru- cheng2, LI Zheng- xiang3, ZHOU Han- wen1 (1. Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China; 2. Department of Earth Sciences, Nanjing University, Nanjing;Geochemistry and geological implications of mafic- ultramafic rocks with the age of~ 825 Ma in Yuanbaoshan- Baotan area of northern Guangxi[J];Geochimica;2001-02
9 LI Xian hua, LIU Ying, TU Xiang lin, HU Guang qian, ZENG Wen(Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China);Precise determination of chemical compositions in silicate rocks using ICP AESand ICP MS: A comparative study of sample digestion techniquesof alkali fusion and acid dissolution[J];Geochimica;2002-03
10 GanXiaochun; LiXianhua; Zhao Fengqing; HuangHaibo (Programs in Geosciences, The University of Texas at Dallas. Richardson, TX 75083-0688)(Guangzhou Institute of Geochemistry, Chinese Academy of Sciences)(Tianjin Institute of Geology and Mineral Resources);ZIRCON U-Pb AND Sm-Nd ISOCHRON AGES OF SPILITE FROM DANZHOU GROUP, GUANGXI ZHUANG AUTONOMOUS REGION[J];GEOCHIMICA;1996-03
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