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《Geotectonica Et Metallogenia》 2007-04
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GEOCHEMICAL CHARACTERISTICS AND ZIRCON SHRIMP U-PB DATING OF THE TONGSHANLING GRANITE IN HUNAN PROVINCE,SOUTH CHINA

WEI Daofang1,3, BAO Zhengyu2,1 and FU Jianming3(1.Faculty of Earth Sciences, China University of Geosciences, Wuhan, Hubei 430074, China; 2.State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan, Hubei 430074, China; 3.Yichang Institute of Geology and Mineral Resources,CGS, Yichang, Hubei 443003, China)  
The Tongshanling granite is poor in silicon and rich in iron, magnesium and calcium, belonging to high-potassium calc-alkaline series with weak to intermediate negative Eu anomalies and K2O/Na2O1. New SHRIMP zircon U-Pb dating results yield a 238U/206Pb age of 149±4Ma, representing the crystallization age of the intrusion. The Tongshanling granitoids were formed during the stage of Middle Yanshanian tectonomagmatic events. Compared with regional other counterparts, these granitiods have relatively low ISr (0.71060~0.71124), εSr(t) (77.6~81.0) and δ18O (8.62‰~9.67‰) values, spanning εNd(t) and TDM ranges from -7.1 to -5.2 and from 1226 to 1536Ma, respectively. Besides, small mafic inclusions can be found in the granite body. Combined geological observations and geochemical data suggest that the Tongshanling granitoids were derived from a mixture between juvenile mantle-derived materials and the ancient crust.
【Fund】: 中国地质调查局南岭锡矿成矿规律研究项目(200310200072)资助
【CateGory Index】: P588.121
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