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《Geotectonica Et Metallogenia》 2008-02
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SHRIMP ZIRCON U-PB DATING OF GRANODIORITES FROM XIETONGMEN PLUTON,TIBET AND ITS GEOLOGICAL IMPLICATION

XIA Bin1, XU Lifeng1,2, ZHANG Yuquan1, DENG Xiongye3, LI Jiangfeng1,2, WEI Zhenquan1,2 and WANG Yanbin4 (1.Key Laboratory of Marginal Sea Geology, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, Guangdong, China; 2.Graduate University of the Chinese Academy of Sciences, Beijing 100049, China; 3.Guangdong Nonferrous Metal Geological Exploration Ageney, Guangzhou 510080, Guangdong, China; 4.Beijing SHRIMP Center, Beijing 100037, China )  
The Xietongmen pluton is located between Xietongmen County and Rikaze City, which belongs to middle part of the Gangdise belt in southern Tibet. The pluton invades in the Carboniferous and Cretaceous in the north; and is covered by the Quaternary sandstones in the south. The pluton is composed mostly of granodiorites and porphyritic biotite granites. Chemically,the granodiorite is peraluminous series.SHRIMP zircon U-Pb dating technique is applied to the granodiorites of the Xietongmen pluton. The result shows that the formation time of the Xietongmen pluton is 45.1±1.7Ma. Most geologists think the Indian-Asian collision began 50Ma ago, so the Xietongmen pluton is syn-collision granodiorite. This result provides a significant evidence for accurately ascertaining the time of the Indian-Asian continental collision.
【Fund】: 国家自然科学基金重点项目(40534019)资助.
【CateGory Index】: P588.121
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