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《Earth Science(Journal of China University of Geosciences)》 2009-06
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Collision Processes of North China and Siberian Plates:Evidence from LA-ICP-MS Zircon U-Pb Age on Deformed Granite in Xar Moron Suture Zone

LI Yi-long1,2,ZHOU Han-wen1,2,ZHONG Zeng-qiu1,2,ZHANG Xiong-hua1,LIAO Qun-an1,GE Meng-chun11.Faculty of Earth Sciences,China University of Geosciences,Wuhan430074,China2.State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Wuhan430074,China  
The Fangkuangzigou granitic gneisses,extending with NEE trend along Fangkuangzi village in Linxi county,Inner-Mongolia province,are deformed and metamorphosed granites which intruded into the Shuangjing schists. The gneisses are nebulitic and homogeneous separately in its edge and center. The LA-ICP-MS zircon U-Pb dating method was applied to determine the ages of gneisses both from the edge and center. It is indicated that the magma emplacement initiated at about 271.9±1.6Ma ago and intruded into Shuangjing schists,then migmatization and nebulitic structure were induced into the contact zones. The pluton was formed dominantly at 264.8±1.8Ma ago. The pluton was deformed and metamorphosed into granitic gneiss by the collision betweenthe Siberian and North China plates. The collision was ended until 231±2Ma ago,then the Siberian and North China plates were finally converged.
【Fund】: 国家重点基础研究发展计划项目(No.2007CB411307);; 中国地质调查局项目(No.1212010510507)
【CateGory Index】: P597.3
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