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《Acta Scientiarum Naturalium Universitatis Pekinensis》 2009-01
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Zircon U-Pb Age of Tonghualing Intermediate-Acid Intrusive Rocks,Eastern Junggar,Xinjiang

GUO Lishuang~ 1,3 , ZHANG Rui~2, LIU Yulin~ 1, XU Fajun~2, SU Li~41. The Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, School of Earth and Space Sciences, Peking University, Beijing 100871; 2. Xinjiang Geological Institute of Nonferrous Geoexploration Bureau, Urumqi 830000; 3. Key Laboratory of Western China's Environmental Systems of the Ministry of Education,Lanzhou 730000; 4. The Geological Lab Center, China University of Geosciences, Beijing 100083  
Tonghualing intermediate-acid intrusive rocks is located in Yemaquan arc between Armantai fault and Kelameili fault, Eastern Junggar, North Xinjiang. The intermediate-acid intrusive rocks are principally composed of diorite-porphyry, tonalite and monzogranite. Zircons from these rocks are dated using LA-ICP-MS U-Pb method and yield weighted mean ~ 206 Pb/ ~ 238 U age of 427.4±3.2, 422.8±3.2 and 418.5±2.6 Ma respectively, indicating that there are Early Paleozoic magmatic activities in Eastern Junggar. This work supplies evidence for orogenic evolution in Early Paleozoic in this area.
【Fund】: 国家重点基础研究发展计划项目(2007CB411305);; 兰州大学2008年接受国内博士生访学项目资助
【CateGory Index】: P597.3
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