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《Geology in China》 2006-03
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Characteristics and geological significance of adakitic rocks in copper-bearing porphyry in Baogutu,western Junggar

ZHANG Lian-chang1,WAN Bo1,JIAO Xue-jun2,ZHANG Rui2(1.Key Lab.of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China;2.Xinjiang Nonferrous Geoexploration Bureau,ürümqi 830000,Xinjiang,China)  
In the Darbute-Baogutu area,western Junggar,there outcrop two types of intermediate-acid intrusive rocks:late Hercynian(270 Ma)granite batholiths and late-mid Hercynian(330-320 Ma)intermediate-acid small porphyry bodies.The Baogutu porphyry copper deposit is hosted in the latter.The Major element and trace element analysis of the rocks indicate that the Baogutu copper-bearing small porphyry in the mine meets the conditions of adakitic rocks,i.e.:SiO256%,Al2O315%,MgO3%,Y18×10-6,Yb1.9×10-6 and Sr400×10-6 and pronounced HREE depletion.Its Nd and Sr isotopic compositions are close to that of MORB.However,the composition of some samples,which is characterized by relatively high MgO contents(3%)and a relatively low LREE abundance),is deviated from the compositional range of adakitic rocks.According to the geochemical composition of porphyries,combined with the regional geological characteristics,the authors think that the Baogutu copper-bearing porphyry originated in an island-arc environment related to intraoceanic subduction but that the initial melt of the oceanic crustal slab was subjected to inhomogeneous contamination with mantle peridotite during its rise.
【Fund】: 国家重点基础研究发展规划项目(2001CB409805);; 国家自然科学基金项目(40473028)
【CateGory Index】: P618.41
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8 GUO Junhua1,MAO Shidong1,2,3,CHEN Yanjing2,4,QIN Yan2,YANG Fuli1,LI Jianzhong1 and NAN Zhenglu1(1.The 12th Detachment of Gold Headquarters of China Armed Police Force,Chengdu 610036,Sichuan,China;2.Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou 510640,Guangdong,China;3.Graduate School of the Chinese Academy of Sciences,Beijing 100049,China;4.Key Laboratory of Orogen and Crust Evolution,Peking University,Beijing 100871,China);Geological Features and Ore-Controlling Factors of the Yangshan Gold Field in Wen County,Gansu Province[J];Geotectonica Et Metallogenia;2009-02
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2 Ji'en Zhang~(a,b),Wenjiao Xiao~(a,b,*),Chunming Han~a,Qjgui Mao~c,Songjian Ao~(a,b), Qianqian Guo~(a,b,d),Chong Ma~(b,d) a State Key Laboratory of Lithospheric Evolution,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China b Xinjiang Research Center for Mineral Resources,Urumqi 830011,China c Beijing Institute of Geology for Mineral Resources,Beijing 100012,China d Graduate University,Chinese Academy of Sciences,Beijing 100049,China;A Devonian to Carboniferous intra-oceanic subduction system in Western Junggar,NW China[A];[C];2012
3 Jun Gao~(a*).Reiner Klemd~b,Qing Qian~a,Xi Zhang~a,Jilei Li~(a,b),Tuo Jiang~a,Yongqiang Yang~c ~aKey Laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,P.O.Box 9825,Beijing 100029,China ~bGeoZentrum Nordbayern,Universitt Erlangen,Schlossgarten 5a,91054 Erlangen,Germany ~cState Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Beijing 100083,China;The collision between the Yili and Tarim blocks of the Southwestern Altaids:Geochemical and age constraints of a leucogranite dike crosscutting the HP-LT metamorphic belt in the Chinese Tianshan Orogen[A];[C];2012
4 ZHANG Xi~(1,2),GAO Jun~1,DONG LianHui~3,LI JiLei~(1,2),JIANG Tuo~(1,2),QIAN Qing~1 and SU Wen~1 1.Key Laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2.Graduate University of Chinese Academy of Sciences,Beijing 100049,China 3.The Bureau of Geology and Mineral Resources Development of Xinjiang,Urumqi 830000,China;Zircon LA-ICP-MS U-Pb age of I type granitoids from Qiaohuote copper deposit in Central Tianshan of Xinjiang and its geological implications[A];[C];2012
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6 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
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8 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
9 Chunming Han~(a,*),Wenjiao Xiao~a,Guochun Zhao~b,Wenjun Qu~c,Andao Du~c * State Key laboratory of Lithospheric Evolution,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing,100029,China b Department of Earth Sciences,The Uttiversity of Hong Kong,Pokfulam Road,Hong Kong,China c National Research Center of Geoanalysis,Beijing,100037,China;Re-Os dating of the Kalatongke Cu-Ni deposit,Altay Shan,NW China,and resulting geodynamic implications[A];[C];2008
10 LONG LingLi,GAO Jun,XIONG XianMing and QIAN Qing 1.Key Laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2.Earth Science College,Graduate University of Chinese Academy of Science,Beijing 100039,China;Geochemistry and geochronology of granitoids in Bikai region,southern Central-Tianshan mountains,Xinjiang.[A];[C];2008
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