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《Acta Mineralogica Sinica》 1996-02
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MULTIPLE-STAGE EVOLUTION OF ZIRCON U-Pb ISOTOPIC SYSTEMATICS IN S-TYPE GRANITES AND ITS CHRONOLOGICAL SIGN1FICANCE:A CASE STUDY ON SANFANG GRANITE,NORTHERN GUANGXI

Li Xianhua; Liu Ying; Tu Xianglin; Liu Haichen; Ling Xiangshou(Guangzhou Institute of Geochemistry, Chinese Academy of Sciences,Guangzhou, 510640)  
It is a common phenomenon that some S-type granites contain inherited zircons and have undergone subsequent disturbance, resulting in radiogenic Pb loss. Zircons in such granites are characterized by the multiple-stage evolution of the U-Pb isotopic system. Ion microprobe is con-sidered to be the most powerful tool to date complicated zircon populations, but its application is limited due to its huge price and high operating cost. In fact, the conventional chemical-TIMS technique is still widely used in zircon age determination. lt is worth to note that the selection of single-or multiple-grain zircon fraction for U-Pb analysis is highly dependent on the analytical Pb blank level.Inherited radiogenic Pb and suhsequent Pb loss in zircons from the Sanfang granite, northern Guangxi, were identified in this study. Hence, the zircon U-Pb system in the granite is character-ized by a three-stage evolution. A concordant 207Pb/206Pb age of 820+9 Ma, which is interpreted as the crystallization age of the granite, is obtained by means of both SHRIMP and conventional multiple-grain zircon U-Pb dating techniques- The previously reported zircon U-Pb age of 899 Ma is only a geologically meaningless" upper intercept age ".
【Fund】: 中国科学院院长基金
【CateGory Index】: P597
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