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《Geotectonica Et Metallogenia》 2009-03
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Geology and Metallogenesis of Daolundaba Copper Polymetallic Deposits,Inner Mongolia

PAN Xiaofei1,WANG Shuo2,HOU Zengqian1,TONG Ying1,XUE Huaimin1,ZHOU Xiwen1 and XIE Yuling3(1.Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037,China;2.Geological Prospecting Limited Company,Hohot 010020,Inner Mongolia,China;3.University of Science and Technology Beijing,Beijing 100029,China)  
The Daolundaba copper polymetallic deposit is located in Xiwuqi,Xilinguole Union of Inner Mongonia. It lies on the west side of southern Daxing′anling ore belt,which is tectonically enclosed by the Siberian Block to the north,North China Block to the south and Songliao block to the east.The deposit is hosted by lower Proterozoic biotite amphibolite (Pt1by),upper Permian Linxi formation sandy slate (P2l) and the Hercynian Qianjinchang biotite granite. There are about 136 ore veins,striking NE and dipping south with angle varying between 20° and 50°. They are controlled by the NE to NEE-striking Mishengmiao anticlinorium as well as a series of secondary NE-,NEE-and nearly EW-striking faults along the contact zone between the Linxi formation and Qianjinchang granite.The alteration includes silicification,beresitization,carbonatization,chloritization,kaolinization,potassic alteration,greisenization,fluoritization and tourmalination. The silicification,greisenation and fluoritization are strongly related with the mineralization of the deposit. The major metallic minerals are pyrrhotite,pyrite,wolframite and cassiterite containing copper,zinc,tungsten and stannum. Detailed studies on wall rock lithology,structural control,magma evolution,alteration and mineralization style,ore mineral paragenesis have been conducted. Based on the detailed investigation,it is proposed that the Daolundaba copper polymetallic deposit is a typical mesothermal to high temperature hypothermal vein deposit. It is suggested that the Qianjinchang granite provides thermal driving force for the transport of the ore-forming material and the Linxi formation is the source of the metal.
【Fund】: 国家自然科学基金项目(编号:40802022);; 基本科研业务费(所长基金 编号:J0811)资助
【CateGory Index】: P618.41
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3 LIN Ge1,ZHANG Y H2, WANG Yuejun1,GUO Feng1, FAN Weiming1 and YAN Yi1 (1. Key Laboratory of Marginal Sea Geology, Guangzhou Institute of Geochemistr y &South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangz hou 510640, China; 2. CSIRO Exploration &Mining, Kensington, WA 6251, Australia );LITHOSPHERIC THINNING IN THE NORTH CHINA BLOCK:A NUMERICAL APPROACH ON THERMA L PERTURBATION AND TECTONIC EXTENSION[J];Geotectonica Et Metallogenia;2004-01
4 CHEN Guoda~(1,2), PENG Shenglin~1 and DAI Tagen~1(1. Central South University, Changsha, HN 410083, China; 2. Guangzhou Institute of Geochemistry, Chinese (Academy) of Sciences, Guangzhou, GD 510640, China);HISTORISTIC-DYNAMIC TECTONIC DIFFERENTIATION OF E-W OF CENTRAL ASIA CONTINENTAL CRUSTOBODY AND ITS SIGNIFICANCE[J];Geotectonica Et Metallogenia;2005-01
5 FAN Weiming and GUO Feng (Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Wushan, Guangzhou, GD 510640, China);LATE MESOZOIC MAFIC MAGMATISM FROM THE EASTERN PART OF NORTH CHINA BLOCK AND ITS ADJACENT REGIONS: MAGMA GENESIS AND GEODYNAMIC IMPLICATIONS FOR LITHOSPHERIC THINNING[J];Geotectonica Et Metallogenia;2005-01
6 CHEN Shengzao(Geomatrix Consultants, Inc., 2101 Webster St., 12~(th) Floor, Oakland, CA 94612, USA);CRUST-MANTLE DYNAMICS AND ACTIVATED TECTONICS (DIWA) THEORY[J];Geotectonica Et Metallogenia;2005-01
7 DENG Jinfu~1, ZHAO Guochun~(1,2), SU Shangguo~1, LIU Cui~1, CHEN Yihan~1, LI Fangning~1 and ZHAO Xingguo~1 (1. Key Laboratory of Lithospheric Tectonics and Lithoprobe Techniques under Ministry of Education, China University of Geosciences, Beijing 100083, China; 2. Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China);STRUCTURE OVERLAP AND TECTONIC SETTING OF YANSHAN OROGENIC BELT IN YANSHAN ERA[J];Geotectonica Et Metallogenia;2005-02
8 LIU Jiangfeng and Xu Yigang(CAS Key Laboratory of Geochronology and Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Science, Guangzhou, GD 510640, China);MINERAL CHEMISTRY AND GEOCHEMISTRY OF THE TWO SUITES OF PYROXENITE XENOLITHS IN CENOZOIC BASALTS FROM YANGYUAN, HEBEI[J];Geotectonica Et Metallogenia;2006-01
9 LI Xiaoyong 1,2 , FAN Weiming 2, 3 , WANG Yuejun2, XIA Bin2 and FAN Liyong2 (1. Zhuzhou Institute of Technology, Zhuzhou, Hunan 412082, China; 2. CAS Key Laboratory of Marginal Sea Geology, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, GD 510640, China; 3. Resource and Environmental Bureau of Chinese Academy of Science, Beijing 100864, China);PETROGENESIS OF THE EARLY CRETACEOUS INTERMEDIATE-MAFIC VOLCANICS FROM SOUTHERN MARGIN OF NORTH CHINA CRATON AND ITS GEOLOGICAL IMPLICATION[J];Geotectonica Et Metallogenia;2006-02
10 ZHAI Mingguo (Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China);GEOLOGICAL SIGNIFICANCE OF THE NEOARCHEAN GLOBAL CRATONIZATION EVENT AND THE BOUNDARY BETWEEN ARCHEAN AND PROTEROZOIC[J];Geotectonica Et Metallogenia;2006-04
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