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《Chinese Geology》 2002-03
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Zircon U-Pb ages of leucoleptite on the southern margin of the Dabie Mountains and their geological implications

GAO Tian-shan 1,2 ,LI Hui-min 3 ,TANG Jia-fu 1 ,HOU Ming-jin 1(1.Anhui Institute of Geological Survey,Hefei230001,Anhui ,Ch ina2.China University of Science and Technology,Hefei230026,Anhui ,Ch ina3.Tianjin Institute of Geology and Mineral Resources,Tianj  
Abundant leucoleptite is exposed in the Dabie orogen.Zircon U -P b dating of two leucoleptite samples from the Susong Group-complex on the sou thern margin of the orogen and its adjacent Dabie Group-complex to its north suggests that the protolith of the leucoleptite in the Susong Group-complex fo rmed in the early Neoproterozoic(866±48Ma ),while that in the Dabie Gro up-complex at the end of the Mesoproterozoic(1159±80Ma )and was rewor ked by a tectono -thermal event in the Caledonian(479±16Ma ).It furni shes important evidence for the determination of the age of the Susong Group -com-plex and correlation with the leucoleptite in the Dabie Group-complex
【Fund】: 地质行业基金(959632);; 安徽省地矿局联合资助
【CateGory Index】: P588.3;P597
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