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《Acta Geoscientica Sinica》 2012-04
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Sulfur and Lead Isotope Characteristics of No.Ⅰ Ore Body in the Xiongcun Porphyry Copper-Gold Ore Concentration Area of Tibet:Implications for the Source of Metals in the Ore Deposit

LANG Xing-hai 1),TANG Ju-xing 2),LI Zhi-jun 1),HUANG Yong 1),DING Feng 1),WANG Cheng-hui 2),ZHANG Li 3),ZHOU yun 1) 1) College of Earth Science,Chengdu University of Technology,Chengdu,Sichuan 610059;2) Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing 10037;3) Chengdu Center of China Geological Survey,Chengdu,Sichuan 610081  
The Xiongcun porphyry copper-gold ore concentration area,one of the large-size metallogenic areas discovered along the Gangdise porphyry copper belt,occurs in an island arc environment associated with northward intra-oceanic subduction of Neo-Tethys oceanic crust.The ore-forming age of the Xiongcun porphyry copper-gold ore concentration area is middle Jurassic.It is located in the middle of the southern margin of the Gangdise orogenic belt,and its south margin is Shigatse forearc basin.The latest exploration data indicate that there are several potential mineralization-alteration areas and three large-size copper-gold ore bodies(No.Ⅰ,Ⅱ and Ⅲ) in the Xiongcun porphyry copper-gold ore concentration area.In this paper,Xiongcun No.Ⅰ ore body was chosen as the research object.According to sulfur and lead isotope composition of ore-baring porphyry,tuff and main sulfides of the ore,the authors have reached the following two conclusions:1) Sulfur isotopic compositions vary in a narrow range of δ 34 S values from 3.5‰ to +2.7‰(1.07‰ on average) and are close to zero,indicating a mantle sulfur signature.2) They have uniform Pb isotope compositions with low content of radiogenic Pb.The 206 Pb/204 Pb,207 Pb/204 Pb,and 208 Pb/204 Pb ratios vary in the ranges of 18.104-18.432,15.473-15.533 and 37.918-38.3072,respectively.They are located in the transition zone of mantle Pb and orogen Pb but are closer to the former,reflecting a mixing between the mantle material and minor crust material.Through a comparative study of sulfur and lead isotopes of porphyry copper deposits of the island arc environment(e.g.,Xiongcun No.I ore body) and those of the collisional orogenic environment in the Gangdise porphyry copper belt,the authors found that they have similar metal sources,but porphyry copper deposits of the island arc environment have experienced weak contamination of crust materials,whereas porphyry copper deposits of the collisional orogenic environment have experienced strong contamination of crust materials.
【Fund】: 国家自然科学基金(编号:41172077);; 国家973项目(编号:2011CB403103);; 西藏天圆矿业资源开发有限公司项目(编号:2006G-07);; 中国地质调查局地调项目“西藏大型矿床成矿专属性研究”(编号:资[2012]03-002-055)联合资助
【CateGory Index】: P618.41;P618.51;P597
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6 WANG Huan1,TANG Jux-ing1,YING Li-juan1,WANG Li-qiang1,QIN Zhi-peng2 1.Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing 100037,China;2.College of Earth Sciences,Chengdu University of Technology,Chengdu 610059,China;Characteristics of the main ore minerals in the Jiama Cu-polymetallic ore deposit,Tibet[J];Journal of Chengdu University of Technology(Science & Technology Edition);2011-01
7 HUANG Yong1,4,DING Jun2,TANG Ju-xing3,LANG Xing-hai1,4,CHEN Yuan4,ZHANG Li21.Chengdu University of Technology,Chengdu 610059,China;2.Chengdu Center of China Geological Survey,Chengdu 610082;3.Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing 10037,China;4.Tibet Tianyuan Minerals Exploration Ltd.Tibet 857000,China;Tectonic setting and source of ore-forming materials of No.Ⅰ orebody in the Xiongcun copper-gold deposit,Tibet[J];Journal of Chengdu University of Technology(Science & Technology Edition);2011-03
8 Zhu Zhan-xiang;Liao Yuan-an(Regional Geological Surveying Team,Sichuan Bureau of Geology and Mineral Resources, Sichuan, 610213)Teng Yun(Regional Geological Surveying Team, Xizang Bureau of Geology and Mineral Resources, Xizang, 851400).Pan Yun-tang(Gradu;The Ophiolitic Stratigraphy in the Open-close Belt in Yarlung Zangbo River, Tibet, China[J];JOURNAL OF STRATIGRAPHY;1996-04
9 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
10 MO Jihai 1,2 , LIANG Huaying1, YU Hengxiang3, XIE Yingwen1 and ZHANG Yuquan1 (1. Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, GD 510640, China; 2. Graduate School, Chinese Academy of Sciences, Beijing 100039, China; 3. Guilin Institute of Technology, Guilin, GX 541004, China);COMPARISON OF ELA-ICP-MS AND SHRIMP U-PB ZIRCON AGES OF THE CHONGJIANG AND QULONG ORE-BEARING PORPHYRIES IN THE GANGDESE PORPHYRY COPPER BELT[J];Geotectonica Et Metallogenia;2006-04
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