Single zircon LAM-ICPMS U-Pb dating of Guidong complex (SE China) and its petrogenetic significance

被引:75
作者
Xu, XS [1 ]
Deng, P
O'Reilly, SY
Griffin, WL
Zhou, XM
Tan, ZZ
机构
[1] Nanjing Univ, Dept Earth Sci, State Key Lab Mineral Deposits Res, Nanjing 210093, Peoples R China
[2] Macquarie Univ, ARC Natl Key Ctr Geochem Evolut & Metallogeny Con, N Ryde, NSW 2109, Australia
[3] CNNE, S China Bur Geol, Res Inst 290, Shaoguan 512026, Peoples R China
来源
CHINESE SCIENCE BULLETIN | 2003年 / 48卷 / 17期
基金
中国国家自然科学基金;
关键词
single zircon; U-Pb dating; granite; southeast China;
D O I
10.1360/03wd0028
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
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.
引用
收藏
页码:1892 / 1899
页数:8
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