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《Geology in China》 2006-03
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Petrographic and geochemical characteristics of the Tulargen Cu-Ni-Co sulfide Deposit,East Tianshan,Xinjiang,and its tectonic setting

SUN He1,2,QIN Ke-zhang1,LI Jin-xiang1,2,XU Xing-wang1,SAN Jin-zhu3,DING Kui-shou1,HUI Wei-dong3(1.Key Lab of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China;2.Graduate School of Chinese Academy of Sciences,Beijing 100039,China;3.704 Geological Party,Xinjiang Geoexploration for Nonferrous Metals,Hami 839000,Xinjiang,China)  
The Tulargen Cu-Ni-Co deposit,lying in the northeastern segment of the Kangurtag-Huangshan ductile sheer zone,is a semi-hidden deposit formed mainly by deep-level liquation of sulfide,combined with in-situ liquation and hydrothermal superimposition.Intrusion No.1 is characterized by whole-rock mineralization and can be divided into four rock facies:hornblende peridotite,pyroxene peridotite,hornblende pyroxenite and gabbro.The rocks show the features of repeated pulsatory magmatic upwelling and ore formation in a single phase.The m/f ratio of the intrusion varies from 3.1 to 4.8,falling into the range of ferrous-ultramafic rocks.The intrusion is featured by low Ti,low total alkalis and low Al2O3,similar to the petrochemical characteristics of the Huangshan-Jing'erquan mafic-ultramafic complex.The REE distribution patterns and trace element and transition element spidergrams indicate that the No.1 and No.2 mafic-ultramafic intrusions in the Tulargen ore district are comagmatic and supplementary,implying that the deep part of the No.2 intrusion has a great ore potential though gabbro of the No.2 intrusion shows weak mineralization at the surface.According to the MT section across both the No.1 and No.2 intrusions,it is clear that they share only one magma conduit at depth and originated from the same magma source.Lower La/Sm(2)and Th/Ta(4.6)ratios suggest a mantle origin of the ore magma and little contamination with crustal material during the emplacement of the intrusion.
【Fund】: 中国科学院知识创新工程重要方向项目(KZCX3-SW-137);; 国家“十五”科技攻关新疆305项目(2003BA612A-06-07)
【CateGory Index】: P618.4
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4 XI Ai-hua~(1,2),REN Hong-mao~(2),ZHANG Bao-fu~(2),WANG Yong-xiang~(3),ZHI Xue-jun~(3) (1.Department of Geoscience, Nanjing University, Nanjing210093,China;2.College of Earth Sciences,Jilin University, Changchun130061,China;3.Jilin Nickel Industry Company,Hongqiling132311,China);Characteristics on ore minerals in Hongqiling CuNi sulfide deposit, Jilin Province[J];Journal of Jiling University (Earth Science Edition);2004-03
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1 Yin Jiang-ning1,Xiao Ke-yan1,Zou Wei1,Wang Zhong2,Lu Lu1 1.Institute of Mineral Resources,Chinese Academy of Geological Science,Beijing 100037,China 2.Resources and Environment School,Hefei University of Technology,Hefei 230009,China;Applying Geostatistics to Extract Geochemical Information in East Tianshan[J];Journal of Jilin University(Earth Science Edition);2012-03
2 WANG Lishe1,2,YANG Jianguo2,XIE Chunlin2,WANG Yuxi2,LEI Yongxiao2,CAO Hongxia1,YANG Pengfei2 and QI Yalin3(1.MOE Key Laboratory of Continental Dynamics,Northwest University,Xi'an 710069,Shaanxi,China;2.Xi'an Geological Survey Center,Xi'an 710054,Shaanxi,China;3.Research Institute of Changqing Oil Field,Xi'an 710021,Shaanxi,China);METALLOGENIC POTENTIALITY OF GUAISHISHAN CU-NI MINERALIZED BASIC-ULTRABASIC ROCKS IN BEISHAN AREA,GANSU PROVINCE[J];Geotectonica Et Metallogenia;2008-03
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4 XIAO Yuan-fu, SUN Yan, ZHAO Zhi-qiang, NIU Gang, ZHANG Lin, KANG Cong-xuan (College of Earth Sciences, Chengdu University of Technology, Chengdu 610059, Sichuan, China);Modes of occurrence of useful associated components in the Lala copper deposit, Sichuan Province[J];Geology in China;2010-02
5 LI Yu-hang 1,2,YANG Xing-ke 3,WANG Qing-liang 1,CUI Du-xin 1,JI Ling-yun 1,HAO Ming 1(1.Second Crust Monitoring and Application Center,CEA,Xi’an 710054,Shaanxi,China;2.Institute of Geology,CEA,Beijing 100029,China;3.Chang’an University,Xi’an 710054,Shaanxi,China);Redetermination of the volcanic eruption time and analysis of geochemical characteristics of volcanic rocks in eastern Maotoushan of Beishan area,Xinjiang[J];Geology in China;2012-03
6 FU Piao-er1, HU Pei-qing1*, ZHANG Ming-jie1, JIA Yuan-qin1, TANG Zhong-li1 and LI Wen-yuan21.Institute of Geological Science, College of Earth and Environmental Sciences , Lanzhou University, Lanzhou 730000, China;2.Xi’an Institute of Geology and Mineral Resources, Xi’an 710054, China;Metallogenic magmatism of Huangshan Cu-Ni sulfide deposit in Xinjiang[J];Geochimica;2009-05
7 LIU Yan-rong1,Lü Xin-biao1,2,MEI Wei1 and HUI Wei-dong3 1.Faculty of Resource Department,China University of Geosciences,Wuhan 430074,China;2.State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Wuhan 430074,China;3.Xinjiang Hexin Mining Co.,Ltd,Hami 839000,China;Compositions of olivine from the mafic-ultramafic complexs in eastern Tianshan, Xinjiang and implications to petrogenesus:Examples from Huangshandong and Tulargen complexes[J];Geochimica;2012-01
8 LIU Cheng-zhi1, YU Hai-shan1, L Yan-fang1, SUN Yu-kai2,3, YANG Wen-min1, LEI Hai-yan1 1.College of Earth Sciences, Northeast Petroleum University, Daqing 163318, China 2.Exploration and Development Institute of Tuha Oilfield Company, Hami 839009, China 3.Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China;Volcanic Oil and Gas Reservoir Characteristics and Formation Mechanism in Kalagang Formation of Malang Sag in Santanghu Basin[J];Earth Science(Journal of China University of Geosciences);2012-S1
9 SUN Tao 1,2),QIAN Zhuang-zhi 1,2),TANG Zhong-li 1,2),LIU Min-wu 1,2),GAO Ping 3),ZHANG Jiang-jiang 1),ZHANG Rui 1),JIANG Chao 1) 1) Key Laboratory of Western China's Mineral Resources and Geological Engineering;Ministry of Education,Xi'an,Shaanxi 710054;2) College of Earth Science and Land Recourses,Chang'an University,Xi'an,Shaanxi 710054;3) Geophysical and Geochemical Exploration Corporation of Northwest Geological Exploration and Mining Bureau for Nonferrous Metals,Xi'an,Shaanxi 710068;Geological Characteristics and Ore-forming Potential of Sidingheishan Stratified Mafic-ultramafic Intrusion in East Tianshan Mountains[J];Acta Geoscientica Sinica;2012-01
10 Fu Yong1, Wang Lijin1, Chai Fengmei1, Deng Gang2, Chen Yong3, Chen Junhua3 1.Institute of Geological and Exploration Engineering,Xinjiang University, rümqi 830046, China2.No. 6 Geological Party of Xinjiang Bureau of Geology and Mineral Resources, Hami 839000, China3.No. 2 Geological Party of Xinjiang Bureau of Geology and Mineral Resources, Kashi 844000, China;The application of multi-variate linear regression combined with stepwise regression analysis for Cu-Ni sulfide deposit of Baishiquan[J];Earth Science Frontiers;2009-01
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1 Ben-Xun Su~(a,b,*),Ke-Zhang Qin~(b,*),Patrick Asamoah Sakyi~c,Xian-Hua Li~a,Yue-Heng Yang~a,He Sun~b, Dong-Mei Tang~b,Ping-Ping Liu~d,Qing-Hua Xiao~b,Sanjeewa P.K.Malaviarachchi~e a State Key Laboratory of Lithospheric Evolution,Institute of Geology and Geophysics,Chinese Academy of Sciences.P.O.Box 9825.Beijing 100029,China b Key Laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,P.O.Box 9825,Beijing 100029,China c Department of Earth Science,University of Ghana,P.O.Box LG 58,Legon-Accra,Ghana d Department of Earth Sciences,the University of Hong Kong,Pakfulam Road,Hong Kong,China e Research School of Earth Sciences,The Australian National University,Building 61,Mills Road Acton,Canberra,Act 0200,Australia;U-Pb ages and Hf-O isotopes of zircons from Late Paleozoic mafic-ultramafic units in the southern Central Asian Orogenic Belt:Tectonic implications and evidence for an Early-Permian mantle plume[A];[C];2012
2 Ben-Xun Su~(a,b,*),Ke-Zhang Qin~(a,*),Patrick Asamoah Sakyi~c,Ping-Ping Liu~d,Dong-Mei Tang~a, Sanjeewa P.K.Malaviarachchi~e,Qing-Hua Xiao~a,He Sun~(a,b),Yu-Cai Dai~f,Yan Hu~b a Key Laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,P.O.Box 9825,Beijing 100029,China b State Key Laboratory of Lithospheric Evolution,Institute of Geology and Geophysics,Chinese Academy of Sciences,P.O.Box 9825,Beijing 100029,China c Department of Earth Science,University of Ghana,P.O.Box LG 58,Legon-Accra,Ghana d Department of Earth Sciences,The University of Hong Kong,Pakfulam Road,Hong Kong,China e Research School of Earth Sciences,The Australian National University,Building 61,Mills Road Acton,Canberra,Act 0200,Australia f No.6 Geological Party,Xinjiang Bureau of Geology and Mineral Resources,Hami 839000,China;Geochemistry and geochronology of acidic rocks in the Beishan region,NW China:Petrogenesis and tectonic implications[A];[C];2012
3 SU BenXun,QIN KeZhang,TANG DongMei,DENG Gang,XIAO QingHua,SUN He,WANG Heng and DAI YuCai 1.Key Laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2.No.6 Geological Party,Xinjiang Bureau of Geology and Mineral Resources,Hami 839000,China;Petrological features and implications for mineralization of the Poshi mafic-ultramafic intrusion in Beishan area,Xinjiang[A];[C];2012
4 KE-ZHANG QIN~(*,+),BEN-XUN SU(*,+),PATRICK ASAMOAH SAKYI~(**), DONG-MEI TANG~*,XIAN-HUALI~(***),HE SUN~*,QING-HUA XIAO~*, and PING-PING LIU~§~*Key Laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,P.O.Box 9825,Beijing 100029,China ~(**)Department of Earth Science,University of Ghana,P.O.Box LG 58,Legon-Accra,Ghana ~(***)State Key Laboratory of Lithospheric Evolution,Institute of Geology and Geophysics,Chinese Academy of Sciences.P.O.Box 9825,Beijing 100029,China ~§Department of Earth Sciences,the University of Hong Kong,Pokfulam Road,Hong Kong,China;SIMS ZIRCON U-Pb GEOCHRONOLOGY AND Sr-Nd ISOTOPES OF Ni-Cu-BEARING MAFIC-ULTRAMAFIC INTRUSIONS IN EASTERN TIAN SHAN AND BEISHAN IN CORRELATION WITH FLOOD BASALTS IN TARIM BASIN(NW CHINA):CONSTRAINTS ON A CA.280 MA MANTLE PLUME[A];[C];2012
5 Dongmei Tang~(a,*),Kezhang Qin~a,Chusi Li~(b,*),Liang Qi~c,Benxun Su~a,Wenjun Qu~d ~aKey Laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China ~bDepartment of Geological Sciences,Indiana University,Bloomington,IN 47405,USA ~cInstitute of Geochemistry of Chinese Academy of Sciences,Guiyang,550002,China ~dNational Research Center of Geoanalysis,Chinese Academy of Geological Sciences,Beijing,100037,China;Zircon dating,Hf-Sr-Nd-Os isotopes and PGE geochemistry of the Tianyu sulfide-bearing mafic-ultramafic intrusion in the Central Asian Orogenic Belt,NW China[A];[C];2012
6 DING KuiShou,QIN KeZhang,XU YingXia,SUN He,XU XingWang,TANGDongMei,MAO Qian and MA YuGuang (Key Lab.of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China);Typomorphic characteristics and ore-forming significance of pyrrhotite in the major Cu-Ni deposits,East Tianshan,Xinjiang[A];[C];2008
7 QIN KeZhang,DING KuiShou,XU YingXia,SUN He,XU XingWang,TANG DongMei and MAO Qian (Key Lab.of Mineral Resources,Institute of Geology and Geophysics,CAS,Beijing 100029,China);Ore potential of protoliths and modes of Co-Ni occurrence in Tulargen and Baishiquan Cu-Ni-Co deposits,East Tianshan,Xinjiang[A];[C];2008
8 SHEN Ping,SHEN YuanChao,LIU TieBing,LI GuangMing,QIN KeZhang and ZENG QingDong (Key Lab.of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China);Application of stratagem EH4 system to prediction of hidden ore bodies[A];[C];2008
9 SUN He~(1,2),QIN KeZhang~1,XU XingWang~1,LI JinXiang~(1,2),DING KuiShou~1,XU YingXia~(1,2)and SAN JinZhu~(1,3) (1 Key Lab of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029, China;2 Graduate School of Chinese Academy of Sciences,Beijing 100039,China;3 No.704 Geological Party,Xinjiang Bureau of Geoexploration for Nonferrous Metals,Hami 839000,Xinjiang,China);Petrological characteristics and copper-nickel ore-forming processes of Early Permian mafic-ultramafic intrusion belts in East Tianshan[A];[C];2008
10 QIN KeZhang,DING KuiShou,XU YingXia,MIAO Yu,FANG TongHui and XU XingWang 1.Key Laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2.Department of Geology,Hebei Polytechnic University,Tangshan 063009,China 3.Beijing Institute of Geology for Mineral Resources,Beijing 100012,China;Tremendous crystal-Paracoquimbite and its polytype coquimbite found for the first time in Hongshan Hs-epithermal Cu-Au deposit,eastern Tianshan,NW-China,and its significance.[A];[C];2009
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