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《Geological Review》 2007-03
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SHRIMP Zircon Dating of Two-Mica Granite from Dala Pluton in Southern Xizang (Tibet) and Its Geological Implications

XIA Bin1),WEI Zhenquan1,2),ZHANG Yuquan1),XU Lifeng1,2),LI Jianfeng1,2),WANG Yanbin3)1)Key Laboratory of Marginal Sea Geology,Guangzhou Institute of Geochemistry,Chinese Academy of Science,Guangzhou,510640;2)Graduate School of the Chinese Academy of Sciences,Beijing,100039;3)Beijing SHRIMP Center,Beijing,100037  
SHRIMP Ⅱ technique is applied to U-Pb dating of the two-mica granite of Dala pluton which belongs to Lhagoi Kangri belt in southern Xizang(Tibet).The result shows that the formation time of the Dala pluton is 24.7 Ma.Magma composite zircons with old core and new margin are abundant in Dala pluton.The age of the old core of magma composite zircons change from 2796.8 Ma to 3196 Ma.It indicates that there is Archaean basement under the area Dala pluton locates in.
【Fund】: 国家自然科学基金重点资助项目(编号40534019)的成果
【CateGory Index】: P597.3
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