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《Geological Review》 2010-04
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Discovery and Significance of Indium Mineralization Belt in Bangong Lake——Nujiang River Metallogenic Belt and Adjacent Regions in Xizang(Tibet)

ZHAO Yuanyi1),LIU Yan1),CUI Yubin2),LU¨ Lina1),SONG Liang2),QU Xiaoming1)1) Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing,100037;2) China University of Geosciences,Beijing,100083  
Indium is one kind of dissipated metallic elements,and its content is 0.1×10-6 in the earth’s crust.The reserves of Indium in China ranks 1st in the world.The Dachang orefield in Guangxi is the biggest production base of indium in our country.Based on many geological surveys in the field,indoor analytical tests,observing with scanning electron microscope and so on,writers finds out the content and occurrence of indium element in the Bangong Lake—Nujiang River Metallogenic belt and adjacent area.Among of the 13 deposits in which the content of indium is higher,there are 5 deposits in which the average content of the samples reaches the requirement of industrial grade.The area where the content of indium is high usually shows belt-like,and is a new metallogenic belt of indium mineralization in China.The kinds of indium minerals are dzhalindite and native indium.The high content part situates in skarn deposit.The mineralized age of indium in the Bangong Lake—Nujiang River Metallogenic belt should be the encounter stage after the Bangong Lake—Nujiang River Metallogenic dived southward (the Gangdese plate) and made itself close.The Lawu polymetallic deposit,Dangxiong County,is exploiting now.Its average content of indium in ores is 45.44×10-6,and the highest content is 166×10-6.So the evaluation of indium resource need to be strengthened in order to improve comprehensive utilization of this resource.
【Fund】: 国家科技支撑课题“西藏班公湖岛弧带铜、金、富铁矿评价与综合找矿技术方法示范研究”(编号2006BAB01A05)之专题“区域成矿模型与典型矿床成因模型研究”;; 中国地质调查局青藏专项“西藏班公湖—怒江成矿带找矿远景区评价”(编号1212010818097)的成果
【CateGory Index】: P618.6
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4 LI Guangming~1 and RUI Zongyao~2 (1. Chengdu Institute of Geology and Mineral Resources, Chengdu, SC 610082, China; 2. Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China.);DIAGENETIC AND MINERALIZATION AGES FOR THE PORPHYRY COPPER DEPOSITS IN THE GANGDISE METALLOGENIC BELT, SOUTHERN XIZANG[J];Geotectonica Et Metallogenia;2004-02
5 QIU Rui-zhao1, ZHOU Su2,3, DENG Jin-fu3, LI Jin-fa4, XIAO Qing-hui1,3, CAI Zhi-yong5(1. Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China;2. Key Laboratory of Lithospheric Tectonics, Deep Process and Exploration, Ministry of Education, Beijing, 100083, China;3. China University of Geosciences, Beijing 100083, China;4. China University of Geosciences, Wuhan 430074, Hubei, China;5. Guangzhou Institute of Geochemistry,Chinese Acadeng of Science Guangzhou 510640, Guangdong, China);Dating of gabbro in the Shemalagou ophiolite in the westernsegment of the Bangong Co-Nujiang ophiolite belt, Tibet-with a discussion of the age of the Bangong Co-Nujiang ophiolite belt[J];Chinese Geology;2004-03
6 WU Xu-ling1,2, CHEN Zhen-hua2(1. China University of Geosciences, Wuhan 430074, Hubei, China;2. Jiangxi Institute of Geological Survey, Nanchang 330201, Jiangxi, China);Geochemistry and genesis of the Nyixung rock body in northern Tibet[J];Chinese Geology;2005-01
7 ZHANG QIAN ; ZHAN XINZHI; PAN JIAYONG ;AND SHAO SHUXUN (Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry,Chinese Acade Academy of Sciences, Guiyang, 550002 );Geochemical Enrichment and Mineralization of Indium[J];中国地球化学学报(英文版);1998-03
8 Li Tung (The University of Science and Technology of China);CHEMICAL ELEMENT ABUNDANCES IN THE EARTH AND IT'S MAJOR SHELLS[J];Geochimica;1976-03
9 Zhang Qian(Institute of Geochemistry, Academia Sinica, Guiyang 550002);GEOCHEMICAL CHARACTERISTICS OF HUANREN SKARNTYPE Cu-Pb-Zn POLYMETAL DEPOSIT IN LIAONING PROVINCE, CHINA[J];Geochimica;1992-03
10 Ye Xusun Yan Yunxiu He Haizhou(Guangxi Geological Institute for Nonferrous Metals, Nanning 530031);The mineralization factors and tectonic evolutionof Dachang superlarge tin deposit, Guangxi, China[J];GEOCHIMICA;1999-03
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