ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
西藏哈姆曲锑(金)矿床曲珍矿段S、Pb同位素组成及意义
  
关键词:sulfur isotope  lead isotope  source of ore-forming materials  Quzhen  Hamuqu  Tibet
基金项目:国家重点研发计划“深地资源勘查开采”重点专项(编号: 2018YFC0604106);中国地质科学院矿产资源研究所基本科研业务专项(编号: KK1903);国家自然科学基金项目(编号: 41873046);中国地质调查局地质调查项目(编号: DD2019167)
作者单位E-mail
李保亮 中国地质科学院矿产资源研究所, 自然资源部成矿作用与资源评价重点实验室 503585986@qq.com 
王立强 中国地质科学院矿产资源研究所, 自然资源部成矿作用与资源评价重点实验室 wlq060301@163.com 
张相国 西藏自治区地质矿产勘查开发局区域地质调查大队  
平措多吉 西藏自治区地质矿产勘查开发局区域地质调查大队  
高腾 中国地质科学院矿产资源研究所, 自然资源部成矿作用与资源评价重点实验室  
王勇 成都理工大学, 地球科学学院  
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摘要:
Sulfur and Lead Isotope Compositions and Their Geological Significances in the Quzhen Sb Mineralization Section of the Hamuqu Sb-Au Deposit, Tibet
      The Hamuqu antimony deposit in Tibet is located in the western margin of the Yarlung Zangbo suture zone, and ore bodies are mainly found in the Late Cretaceous mylonitized diorite porphyrite. The ore bodies in the Quzhen mineralization section, which are mainly veined, layered and lenticular-like are controlled by NNE–SSW trending faults. On the basis of field geological investigation and analysis of ore-forming geological conditions, the S and Pb isotopes of stibnite in the deposit were studied, and the sources of metallogenic materials of the deposit were discussed. The δ34S values of stibnite range from –4.7‰ to –3.2‰, with an average of –3.97‰. The distribution of sulfur isotope composition is relatively concentrated and similar to the range of magmatic sulfur (–4‰ to 9‰), indicating that sulfur isotope has the characteristics of magmatic sulfur. 206Pb/204Pb isotope compositions of stibnite ranges from 18.557 to 18.690, with an average value of 18.622; 207Pb/204Pb ranges from 15.607 to 15.681, with an average of 15.647; 208Pb/204Pb isotope value ranges from 38.793 to 39.147, with an average of 38.967. The lead isotope composition of the deposit is little variable and shows normal lead features. Combined with the μ values (9.46~9.59) of lead isotope and the lead isotopic tectonic evolution features, we propose that the lead isotope of the deposit has the characteristics of crust-mantle mixed sources.
LI Bao-liang,WANG Li-qiang,ZHANG Xiang-guo,PINGCUO Duo-ji,GAO Teng,WANG Yong.2022.Sulfur and Lead Isotope Compositions and Their Geological Significances in the Quzhen Sb Mineralization Section of the Hamuqu Sb-Au Deposit, Tibet[J].Acta Geoscientica Sinica,43(2):202-210.
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