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《Journal of Jilin University(Earth Science Edition)》 2008-03
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SHRIMP U-Pb Ages of Zircon and Its Geological Implications from Metamorphic Dacite of the Wudaogou Group in Yanbian Area

YU Jie-jiang,MEN Lan-jing,CHEN Lei,ZHAO Jun-kang,LIANG Shu-neng,CHEN Dong,PANG Wei College of Earth Sciences,Jilin University,Changchun 130061,China  
Zircons from the metamorphic dacite of the Wudaogou Group in Yanbian area have euhedral-subhedral shapes and high Th/U ratios(0.28-0.81),implying their magmatic origin.The dating of these zircons indicates that they can be divided into two groups according to their ages.One group,206Pb/238U ages of 10 spots ranging from(265±5)Ma to(291±5)Ma,the weighted mean age of(274±7)Ma(MSWD= 3.4),represents the formation time of the metamorphic dacite(the Early Permian),the other include three zircon grains,and its weighted mean 206Pb/238U age of is(323±37)Ma(MSWD = 3.6),should be interpreted as the captured zircon ages.Combining with the recently dating data,it is suggested that the Wudaogou Group formed in the Early Permian.Together with the Qinglongcun Group,it constitutes a volcanic-sedimentary formation in the Late Paleozoic continental margin.
【Fund】: 国家自然科学基金项目(40472050 40772052);; 南京大学内生金属成矿机制国家重点实验室基金(2005-2006 2006-2008)
【CateGory Index】: P588.3;P597
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