The study was support by China Geological Survey (1212010911028), NSFC (40802020), Ministry of Land and Resources (1212010633902, 1212010633903 and 121201 0711814), and CUGB (GPMR 0735). We thank Shao Jidong, Shang Hengseng and Tao Jixiong of the Geological Survey Institute of Inner Mongolia for their assistance during the field work and thoughtful discussion. And we appreciate the guidance and help of Lu Songnian.?Meanwhile, thanks are due to Shi Yuruo for the fruitful discussion with him on the zircon.?We also thank You Zhendong, Liu Jiajun and Tian Shihong for their riview of the paper. Single zircon selection was made by Wang Xiaoyan in TCNBCMGB;?LA-ICP?MS, Lu-Hf?isotope analysis and CL were carried out in Northwestern University; reflection photographs and data processing were completed by Liu Yong; molybdenite Re-Os dating by Li Chao and Qu Wenjun from the Chinese Academy of Geological Sciences. To them we are deeply indebted.
LIU Cui
1 State Key Laboratory of Geological Process and Mineral Resources, China University of Geosciences (Beijing), Beijing 100083, China; 2 Graduate University of Chinese Academy of Sciences, Beijing 100049, China; 3 The Fourth Institute of Geological and Mineral Exploration of Gansu Province, Jiuquan, Gansu 735000, China; 4 Geological Survey Institute of Inner Mongolia, Hohhot, Inner Mongolia 010020, ChinaDENG Jinfu
1 State Key Laboratory of Geological Process and Mineral Resources, China University of Geosciences (Beijing), Beijing 100083, China; 2 Graduate University of Chinese Academy of Sciences, Beijing 100049, China; 3 The Fourth Institute of Geological and Mineral Exploration of Gansu Province, Jiuquan, Gansu 735000, China; 4 Geological Survey Institute of Inner Mongolia, Hohhot, Inner Mongolia 010020, ChinaKONG Weiqiong
1 State Key Laboratory of Geological Process and Mineral Resources, China University of Geosciences (Beijing), Beijing 100083, China; 2 Graduate University of Chinese Academy of Sciences, Beijing 100049, China; 3 The Fourth Institute of Geological and Mineral Exploration of Gansu Province, Jiuquan, Gansu 735000, China; 4 Geological Survey Institute of Inner Mongolia, Hohhot, Inner Mongolia 010020, ChinaXU Liquan
1 State Key Laboratory of Geological Process and Mineral Resources, China University of Geosciences (Beijing), Beijing 100083, China; 2 Graduate University of Chinese Academy of Sciences, Beijing 100049, China; 3 The Fourth Institute of Geological and Mineral Exploration of Gansu Province, Jiuquan, Gansu 735000, China; 4 Geological Survey Institute of Inner Mongolia, Hohhot, Inner Mongolia 010020, ChinaZHAO Guochun
1 State Key Laboratory of Geological Process and Mineral Resources, China University of Geosciences (Beijing), Beijing 100083, China; 2 Graduate University of Chinese Academy of Sciences, Beijing 100049, China; 3 The Fourth Institute of Geological and Mineral Exploration of Gansu Province, Jiuquan, Gansu 735000, China; 4 Geological Survey Institute of Inner Mongolia, Hohhot, Inner Mongolia 010020, ChinaLUO Zhaohua
1 State Key Laboratory of Geological Process and Mineral Resources, China University of Geosciences (Beijing), Beijing 100083, China; 2 Graduate University of Chinese Academy of Sciences, Beijing 100049, China; 3 The Fourth Institute of Geological and Mineral Exploration of Gansu Province, Jiuquan, Gansu 735000, China; 4 Geological Survey Institute of Inner Mongolia, Hohhot, Inner Mongolia 010020, ChinaLI Ning
1 State Key Laboratory of Geological Process and Mineral Resources, China University of Geosciences (Beijing), Beijing 100083, China; 2 Graduate University of Chinese Academy of Sciences, Beijing 100049, China; 3 The Fourth Institute of Geological and Mineral Exploration of Gansu Province, Jiuquan, Gansu 735000, China; 4 Geological Survey Institute of Inner Mongolia, Hohhot, Inner Mongolia 010020, ChinaThe study was support by China Geological Survey (1212010911028), NSFC (40802020), Ministry of Land and Resources (1212010633902, 1212010633903 and 121201 0711814), and CUGB (GPMR 0735). We thank Shao Jidong, Shang Hengseng and Tao Jixiong of the Geological Survey Institute of Inner Mongolia for their assistance during the field work and thoughtful discussion. And we appreciate the guidance and help of Lu Songnian.?Meanwhile, thanks are due to Shi Yuruo for the fruitful discussion with him on the zircon.?We also thank You Zhendong, Liu Jiajun and Tian Shihong for their riview of the paper. Single zircon selection was made by Wang Xiaoyan in TCNBCMGB;?LA-ICP?MS, Lu-Hf?isotope analysis and CL were carried out in Northwestern University; reflection photographs and data processing were completed by Liu Yong; molybdenite Re-Os dating by Li Chao and Qu Wenjun from the Chinese Academy of Geological Sciences. To them we are deeply indebted.
LIU Cui, DENG Jinfu, KONG Weiqiong, XU Liquan, ZHAO Guochun, LUO Zhaohua, LI Ning.2011. LA-ICP-MS Zircon U-Pb Geochronology of the Fine-grained Granite and Molybdenite?Re-Os?Dating in the Wurinitu Molybdenum Deposit, Inner Mongolia, China[J]. ACTA GEOLOGICA SINICA(English edition),85(5):1057~1066
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