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《Geotectonica Et Metallogenia》 2010-03
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SHRIMP U-Pb Zircon Dating of the Liyuan Granites

CHEN Xiqing,FU Jianming,CHENG Shunbo,XU Deming and MA Liyan(Wuhan Center,Chinese Geological Survey,Wuhan 430223,Hubei,China)  
The Liyuan granites situate in southeastern part of Lechang-Lianping W-Sn-Pb-Zn metallogenetic belt in northern Guangxi,on the border between Guangxi and Guangxi.The granites consist mainly of medium grained porphyritic biotite monzonitic granite,with minor fine grained biotite(monzonitic) granite.SHRIMP U-Pb zircon dating of the medium grained granite,yielded an age of(227.2±4.4)Ma(MSWD=3.4),indicating that the early stage granite was formed in late Indosinian.Considering the geochemical characteristics and regional granite intrusions and W-bearing veins,it can be deduced that the late stage fine grained granite was probably formed in early Yanshanian.
【Fund】: 中国地质调查局南岭地区锡矿选区评价与成果集成项目(1212010981028)资助
【CateGory Index】: P597.3
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