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Single zircon LAM-ICPMS U-Pb dating of Guidong complex (SE China) and its petrogenetic significance
作者姓名:XU Xisheng    DENG Ping    S. Y. OReilly  W. L. Griffin  ZHOU Xinmin & TAN Zhengzhong . State Key Laboratory for Mineral Deposits Research  
作者单位:XU Xisheng1,2,DENG Ping1,3,S. Y. OReilly2,W. L. Griffin2,ZHOU Xinmin1 & TAN Zhengzhong3 1. State Key Laboratory for Mineral Deposits Research,Department ofEarth Sciences,Nanjing University,Nanjing 210093,China; 2. ARC National Key Centre for the Geochemical Evolution and Metal-logeny of Continents,Macquarie University,NSW 2109,Australia; 3. Research Institute No. 290,South China Bureau of Geology,CNNE,Shaoguan 512026,China
摘    要:Because of the strong effects of the Caledonian and Indosinian orogenies and Yanshanian magmatism since early Paleozoic time, different types of granites and ore deposits occur widely in the Nanling region of SE China1]. The Guidong complex is situated at the border between the South Jiangxi—North Guangdong post-Caledonian orogenic belt and the Hercynian-Indosinian belt, which is constrained by an E-W regional deep fault (Guidong-Da- dongshan deep fault) and therefore is elongated nea…

关 键 词:中国东南部  成岩作用  锆石  U-Pb测年  电感耦合等离子体质谱法  花岗岩
收稿时间:10 June 2008

Single zircon LAM-ICPMS U-Pb dating of Guidong complex (SE China) and its petrogenetic significance
XU Xisheng,,DENG Ping,,S. Y. OReilly,W. L. Griffin,ZHOU Xinmin & TAN Zhengzhong . State Key Laboratory for Mineral Deposits Research,.Single zircon LAM-ICPMS U-Pb dating of Guidong complex (SE China) and its petrogenetic significance[J].Chinese Science Bulletin,2003,48(17):1892-1899.
Authors:Email author" target="_blank">Xisheng?XuEmail author  Ping?Deng  S?Y?O’Reilly  W?L?Griffin  Xinmin?Zhou  Zhengzhong?Tan
Institution:XU Xisheng1,2, DENG Ping1,3, S. Y. OReilly2, W. L. Griffin2, ZHOU Xinmin1 & TAN Zhengzhong3 1. State Key Laboratory for Mineral Deposits Research, Department ofEarth Sciences, Nanjing University, Nanjing 210093, China; 2. ARC National Key Centre for the Geochemical Evolution and Metal-logeny of Continents, Macquarie University, NSW 2109, Australia; 3. Research Institute No. 290, South China Bureau of Geology, CNNE, Shaoguan 512026, China
Abstract:Single zircon LAM-ICPMS U-Pb dating indicates that the Guidong granitic complex is a multistage batholith formed during Indosinian-Yanshanian time. The Luxi body (239 ± 5 Ma) and the Xiazhuang body (235.8 ± 7.6 Ma) intruded during Indosinian time, whereas the Aizi body (160.1 ± 6.1 Ma) and the Siqian body (151 ± 11 Ma) formed during Yanshanian time. Inherited zircons (1275-2137 Ma) in the Xiazhuang body imply that at least part of the source rocks of the Guidong complex are from the Proterozoic basement of southeast China. Detailed single zircon LAM-ICPMS U-Pb dating results provide important evidence for understanding the evolution, tectonic setting and mineralisation of the complex.
Keywords:single zircon  U-Pb dating  granite  southeast China    
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