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《Earth Science(Journal of China University of Geosciences)》 2008-01
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LA-ICP-MS U-Pb Zircon Geochronology of Basic Dikes within Maxianshan Rock Group in the Central Qilian Mountains and Its Tectonic Implications

HE Shi-ping1,2,WANG Hong-liang1,3,CHEN Juan-lu1,2,XU Xue-yi1,ZHANG Hong-fei2,REN Guang-ming1,YU Ji-yuan11.Xi’an Institute of Geology and Mineral Resources,CGS,Xi’an 710054,China2.Faculty of Earth Sciences,China University of Geosciences,Wuhan 430074,China3.Department of Geology,Northwest University,Xi’an 710069,China  
A large number of basic dikes which indicate an important tectonic-magmatic event in the eastern part of the middle Qilian orogenic belt were found in the Maxianshan rock group,Yongjing County,Gansu Province,China. According to research on their characteristics of geology and petrology,basic dike swarms,widely intruded in Maxianshan rock group,are divided into two phases. U-Pb isotopes of zircons from the basic dikes of the two phases were determined by LA-ICP-MS respectively in the State Key Laboratory of Continental Dynamics of Northwest University,and the causes of formation of the zircons were studied by using CL images. The formation age of the earlier phase of variational gabbro dikes is (441.1±1.4) Ma (corresponding to the early stage of Early Silurian),and the age of main metamorphic period is (414.3±1.2) Ma (corresponding to the early stage of Early Devonian). The formation age of the later phase of diabase dike swarms is (434±1.0) Ma (corresponding to the late stage of Early Silurian),and the age of main metamorphic period is (414.3±1.2) Ma (corresponding to the early stage of Early Devonian). The captured-zircons from diabase dike swarms retain some information of material interfusion by Maxiashan rock group (207Pb/206Pb apparent ages are (2 325±3) Ma-(2 573±6) Ma),and some zircons from diabase dike swarms also retain information impacted by tectonic thermal event during the late period of Caledonian Movement (206Pb/238U apparent ages are (400±2) Ma-(429±2) Ma). The study,together with others,suggests that,the basic dikes within Maxianshan rock group formed in the period when Qilian transferred from subductional orogeny towards collisional orogeny,which is the geological record of NW-SE extension during regional NE-SW toward intense compression in the Central Qilian block.
【Fund】: 中国地质调查局国土资源大调查项目“西北地区重要成矿带基础地质综合研究”(No.1212010510416)
【CateGory Index】: P588.124;P597
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6 LUO Mao-cheng 1),MAO Jing-wen 2),WANG Li-qiang 2),LENG Qiu-feng 3),CHEN Wei 3) 1) School of Earth Sciences and Resources,China University of Geosciences,Beijing 100083;2) MLR Key Laboratory of Metallogeny and Mineral Assessment,Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing 100037;3) College of Earth Sciences,Chengdu University of Technology,Chengdu,Sichuan 610059;Fluid Inclusion Evidence for Magmatic-Hydrothermal Evolution in the Bangpu Porphyry Molybdenum-Copper Deposit,Tibet[J];Acta Geoscientica Sinica;2012-04
7 LENG Qiu-feng 1),WANG Li-qiang 2),YING Li-juan 2),ZHENG Wen-bao 1),LUO Mao-cheng 3),CHEN Wei 1),LIN Bin 1),WANG Yi-yun 1) 1) College of Earth Sciences,Chengdu University of Technology,Chengdu,Sichuan 610059;2) MLR Key Laboratory of Metallogeny and Mineral Resource Assessment,Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing 100037;3) School of Earth Sciences and Resources,China University of Geosciences,Beijing 100083;LA-ICP-MS Zircon U-Pb Dating of Allgovite in the Bangpu Molybdenum(Copper) Deposit in Tibet and Its Geological Significance[J];Acta Geoscientica Sinica;2012-04
8 CHEN-Wei 1),WANG Li-qiang 2),HU Zheng-hua 1,3),LUO Mao-cheng 4),LENG Qiu-feng 1),TANG Xiao-qian 1),WANG Yi-yun 1),YANG Yi 1),ZHANG Zhi 1) 1) College of Earth Sciences,Chengdu University of Technology,Chengdu,Sichuan,610059;2) Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing 100037;3) Jiangxi Institute of Geological Survy,Nanchang,Jiangxi 330000;4) School of Earth Sciences and Resources,China University of Geosciences,Beijing 100083;Zircon U-Pb Ages,Hf Isotope and REE of Quartz Monzonite Porphyry in the Bangpu Pb-Zn Mining Area of Tibet and Their Geological Significance[J];Acta Geoscientica Sinica;2012-04
9 LIU Han1,2,WANG Guo-can1*,CAO Shu-zhao1,LUO Yan-jun1,GAO Rui1,HUANG Wen-xing1 1.Faculty of Earth Sciences,China University of Geosciences,Wuhan 430074,China 2.Chengdu Center of China Geological Survey,Chengdu 610081,China;Discovery of Nanhuaian Bimodal Volcanics in Northern Altyn Tagh and Its Tectonic Significance[J];Earth Science(Journal of China University of Geosciences);2012-05
10 WANG Liqiang~(1)),TANG Juxing~(1)),WANG Denghong~(1)),LUO Maocheng~(2)),CHEN Wei~(3)),HUANG Fan~(1)) 1)Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing,100037; 2)School of Earth Sciences and Resources,China University of Geosciences,Beijing,100083; 3)College of Earth Sciences,Chengdu University of Technology,Chengdu,610059;Rare Earth Element and Trace Element Features of Molybdenite in Bangpu Mo(Cu) Deposit,Maizhokunggar,Xizang(Tibet),and Their Constraints on the Nature of Ore-forming Fluid[J];Geological Review;2012-05
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1 Zhang Qi~1 Jiao Shoutao~2 Wu Haoruo~1 Jin Weijun~1 Li Chengdong~3 1 Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029 2 School of Earth Sciences and Natural Resources,China University of Geosciences(Beijing),Beijing 100083 3 Tianjin Institute of Geology and Mineral Resources,China Geological Survey,Tianjin 300170;Palaeotopographic map of the Triassic of China[A];[C];2014
2 Qingdong Zeng~*,Jianming Liu,Kezhang Qin,Hongrui Fan,Shaoxiong Chu,Yongbin Wang and Lingli Zhou Key Laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China;Types,characteristics,and time-space distribution of molybdenum deposits in China[A];[C];2014
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3 PEI Xian-zhi1, WANG Tao2, Ding Sa-ping1,3,LI Yong1,HU Bo1(1. Faculty of Earth Sciences and Land Resources, Chang'an University, Xi'an 710054, Shaanxi, China;2. Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China;3. Gansu Institute of Geological Survey, Lanzhou 730050, Gansu, China);Geochemical characteristics and geological significance of Neoproterozoic adakitic granitoids on the north side of the Shangdan zone in the East Qinling[J];Chinese Geology;2003-04
4 SU Jian-ping1,2, ZHANG Xin-hu2, HU Neng-gao3, FU Guo-min3, ZHANG Hai-feng2(1. Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, Gansu, China;2. Gansu Institute of Geological Survey, Lanzhou 730000, Gansu, China;3. School of Earth Sciences and Resource Management, Chang'an University, Xi′an 710054, Shaanxi, China);Geochemical characteristics and genesis of adakite-like granites at Yema Nanshan in the western segment of the Central Qilian Mountains[J];Chinese Geology;2004-04
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8 LIANG Xi-rong; LI Xian-hua; LIU Yong-kang; ZHU Bing-quan; ZHANG Hai-xiang(Cuangzhou Institute of Geochemistry Chinese Academy of Sciences, Cuangzhou 510640, China);U-Pb isotopic dating of young zircons by laser ablation microprobe-inductively coupled plasma mass spectrometry (LAM-ICPMS)[J];GEOCHIMICA;2000-01
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