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《Acta Geologica Sinica》 2009-03
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Geochronology and Geochemistry of Haergentoukoubu Granites in the Beishan Area,Gansu,China and Their Geological Significance

WANG Lishe1,2),YANG Jianguo2),XIE Chunlin2),LEI Yongxiao2),WANG Yuxi2),CAO Hongxia1),YANG Pengfei2),QI Yalin3),JIN Suanlian3)1) State Key Laboratory of Continental Dynamics,Department of Geology,Northwest University,Xi'an,Shaanxi,710069;2) Xi'an Institute of Geology and Mineral Resources,Xi'an,Shannxi,710054;3) Research Institute of Changqing Oil Field,Xi'an,Shannxi,710021  
LA-ICP-MS U-Pb isotopic dating for zircon separated from the Haergentoukoubu granites yields two ages: 387.6±8.2Ma and 1172±7Ma.These granites were emplaced in the Changcheng System,Jixian System and Silurain System in Huoshishan,Beishan,Gausu.The former probably represents intrusive age(early-middle Devonian)of the granites and the latter probably represents the age of late Jixian System inherited zircon inside the granites.Composed mainly of moyites,monozogranite,granodiorite,the granites are characterized by high SiO2(70.28%~79.4%),and high Na2O + K2O(6.52%~9.11%),low Al2O3(8.82%~14.05%),and low Sr(40~150×10-6,averaging 101.5×10-6).Trace elements analysis shows that the average ΣREE is 168.52×10-6,the ratios of LREE/HREE and LaN/YbNare 2.89~16.4,1.82~25.18 respectively.The REE distribution patterns show that the granites are enriched in Rb,Th Ce and Sm,and depleted in Eu,TZ,Nb,Zr and Hf,with LREE/HREE=2.89~16.4,LaN/YbN= 1.82~25.18.The comprehensive analysis also suggests that the granites are metaluminous to slightly peraluminous calcicolous alkaline series rocks,which formed in the tectonic setting of transformation from collision to extension in earlier-middle Devonian.
【Fund】: 中国地质地调查局战略性矿产远景调查项目(编号矿调[2004]8-2号);; 中央地质勘查基金2007年度地质矿产勘查项目(编号2007651139)资助的成果
【CateGory Index】: P597
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9 Lü Xin-biaoa,b,ZHU Jianga,CAO Xiao-fenga,CHEN Chaoa,WU Chun-minga,HU Qin-chenga(a.Faculty of Earth Resources;b.State Key Laboratory of Geological Processes and Minerical Resources,China University of Geosciences,Wuhan 430074,China);Magmatism and Its Metallogenetic Effects during the Paleozoic-Triassic Continental Crustal Construction in the Liuyuan Area,South Beishan,NW China[J];Geological Science and Technology Information;2012-05
10 QIN Ya1a,LIANG Yi-hong1a,HU Zhao-chu2,LIU Xue-song1b 1a.College of Earth Sciences;1b.Museum of Geology,Jilin University,Changchun 130061,China; 2.Faculty of Earth Science,China University of Geosciences,Wuhan 430074,China;Geochemical characteristics and tectonic significance of Jurassic granites in Huanggoushan area,south of Jilin,China[J];Journal of Chengdu University of Technology(Science & Technology Edition);2013-01
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1 ZHANG Qi Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China;The central belt of the North China Craton during Paleoproterozoic is an orogenic belt?[A];[C];2012
2 ZHANG Qi~1,JIN Weijun~1,LI Chengdong~2,WANG Yan~3 and WANG Yuanlong~1 (1.Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China;2.Tianjin Institute of Geology and Mineral Resources,China Geological Survey,Tianjin 300170,China;3.Guangzhou Institute of Geochemistry, Chinese Academy of Sciences,Guangzhou 510640,Guangdong,Cnina);Granitic Rocks and Their Formation Depth in the Crust[A];[C];2012
3 ZHANG Qi (Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China);GUESS ON THE SILURIAN-DEVONIAN NORTH CHINA HIGHLAND:EVIDENCE FROM THE INFORMATION OF GANSU[A];[C];2012
4 ZHANG Qi (Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China);Are-discussion on the classification of granites and their relationship with Cu-Au and W-Sn mineralization:A reply to the comments by Messrs Hua Renmin and Wang Denghong about"Zhang Qi et al(2010):Relationship between granitic rocks and Au-Cu-W-Sn minerali[A];[C];2012
5 Zhang Qi (Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China);Reappraisal of the origin of C-type adakitic rocks from East China[A];[C];2012
6 ZHANG Qi,JIN WeiJun,LI ChengDong and WANG YuanLong 1.Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2.Tianjin Institute of Geology and Mineral Resources,Tianjin 300170,China;On the classification of granitic rocks based on whole-rock Sr and Yb concentrationsⅢ:Practice[A];[C];2011
7 Qianqian Guo~(a,b),Wenjiao Xiao~(a,*),Brian F.Windley~c,Qigui Mao~d,Chunming Han~a,Junfeng Qu~a, Songjian Ao~a,Jiliang Li~(a,b),Dongfang Song~(a,b),Yong Yong~a a State Key laboratory of Lithospheric Evolution,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China b Graduate University of Chinese Academy of Sciences,Beijing 100049,China c Department of Geology,University of Leicester,Leicester LEI 7RH,UK d Beijing Institute of Geology for Mineral Resources,Beijing 100012,China;Provenance and tectonic settings of Permian turbidites from the Beishan Mountains,NW China:Implications for the Late Paleozoic accretionary tectonics of the southern Altaids[A];[C];2013
8 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
9 ZHANG Qi (Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China);The criteria and discrimination for A-type granites:A reply to the question put forward by Wang Yang and some other persons forⅥA-type granite:what is the essence?"[A];[C];2014
10 YAN Hai-qing;HE Bao-lin;LIU Qiao-feng;JIA Hui-min;LI Fei;School of Earth Science and Resources,Chang'an University;No.1 Institute of Geological and Mineral Resources Survey,Henan Provincial Bureau of Geo-exploration and Mineral Development;No.5 Gold Geological Party of Chinese People's Armed Police Force;;Characteristics of Magmatic Geochronology and Geochemistry of Dashui Gold Deposit in West Qinling[A];[C];2014
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