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《Journal of Changchun University of Science and Technology》 2004-01
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The geochemistry and tectonic settings of two-mica granite in Zhewu area,Tibet

ZHAI Qing-guo, LI Cai, WANG Tian-wu, ZHU Zhi-yong (College of Earth Sciences,Jilin University,Changchun130061,China)  
The KAr age of two-mica granite in Zhewu town of Nanmulin county,Tibet is 93.4 Ma, and the granite intruded into Carboniferous sandstone. The content of SiO(2),Al(2)O(3) and K(2)O in the two-mica granite is very high, A/CNK is higher than 1.11, and the content of corundum exceeds 2.6% through CIPW standard mineral calculating. On one hand Rb and Th are much richer than others in the two-mica granite, and K(2)O,Ba,Ta,Nb and Ce are also rich, on the other hand, Hf,Zr,Sm,Y and Yb are relatively lower. LREE is relatively rich, HREE is relatively lower and Eu have clearly negative abnormity. Judged from the figure of the cause of granite coming into being, the two-mica granite belongs to syn-collision granites. It is clear that the granites are the peraluminous granites, which were produced under the condition of the continentcontinent collision.
【Fund】: 中国地质调查局区域地质调查项目(H45C002004)
【CateGory Index】: P588.1
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