This study is financially supported by the National Project of Scientific and Technological Support (Grant No: 2006BAB01A11).
YANG Pengtao
1 The Key Laboratory of Orogenic Belts and Crustal Evolution, Peking University, Beijing 100871 ;2 Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037;3 Northwest Geological Exploration and Mining Bureau for Nonferrous Metals, Xi’an, Shaanxi 710054 ;4 Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037LIU Shuwen
1 The Key Laboratory of Orogenic Belts and Crustal Evolution, Peking University, Beijing 100871 ;2 Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037;3 Northwest Geological Exploration and Mining Bureau for Nonferrous Metals, Xi’an, Shaanxi 710054 ;4 Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037LI Qiugen
1 The Key Laboratory of Orogenic Belts and Crustal Evolution, Peking University, Beijing 100871 ;2 Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037;3 Northwest Geological Exploration and Mining Bureau for Nonferrous Metals, Xi’an, Shaanxi 710054 ;4 Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037ZHANG Fan
1 The Key Laboratory of Orogenic Belts and Crustal Evolution, Peking University, Beijing 100871 ;2 Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037;3 Northwest Geological Exploration and Mining Bureau for Nonferrous Metals, Xi’an, Shaanxi 710054 ;4 Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037WANG Zongqi
1 The Key Laboratory of Orogenic Belts and Crustal Evolution, Peking University, Beijing 100871 ;2 Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037;3 Northwest Geological Exploration and Mining Bureau for Nonferrous Metals, Xi’an, Shaanxi 710054 ;4 Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037WANG Dongsheng
1 The Key Laboratory of Orogenic Belts and Crustal Evolution, Peking University, Beijing 100871 ;2 Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037;3 Northwest Geological Exploration and Mining Bureau for Nonferrous Metals, Xi’an, Shaanxi 710054 ;4 Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037WANG Ruiting
1 The Key Laboratory of Orogenic Belts and Crustal Evolution, Peking University, Beijing 100871 ;2 Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037;3 Northwest Geological Exploration and Mining Bureau for Nonferrous Metals, Xi’an, Shaanxi 710054 ;4 Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037YAN Quanren
1 The Key Laboratory of Orogenic Belts and Crustal Evolution, Peking University, Beijing 100871 ;2 Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037;3 Northwest Geological Exploration and Mining Bureau for Nonferrous Metals, Xi’an, Shaanxi 710054 ;4 Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037YAN Zhen
1 The Key Laboratory of Orogenic Belts and Crustal Evolution, Peking University, Beijing 100871 ;2 Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037;3 Northwest Geological Exploration and Mining Bureau for Nonferrous Metals, Xi’an, Shaanxi 710054 ;4 Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037This study is financially supported by the National Project of Scientific and Technological Support (Grant No: 2006BAB01A11).
YANG Pengtao, LIU Shuwen, LI Qiugen, ZHANG Fan, WANG Zongqi, WANG Dongsheng, WANG Ruiting, YAN Quanren, YAN Zhen.2011. Ages of the Laocheng Granitoids and Crustal Growth in the South Qinling Tectonic Domain, Central China: Zircon U-Pb and Lu-Hf Isotopic Constraints[J]. ACTA GEOLOGICA SINICA(English edition),85(4):854~869
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