ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
滇黔桂地区微细浸染型金矿硫铅同位素地球化学研究
  
关键词:sulfur isotope lead isotope micro-disseminated type gold deposit Yunnan-Guizhou-Guangxi
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作者单位E-mail
李毅 中南大学湖南 长沙410083桂林矿产地质研究院广西桂林541004 Liyitom@163.com 
徐文忻 桂林矿产地质研究院广西桂林541004  
刘悟辉 中南大学湖南 长沙410083  
李蘅 桂林矿产地质研究院广西桂林541004  
戴塔根 中南大学湖南 长沙410083  
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摘要:
Sulfur-Lead Isotope Geochemistry of Micro-disseminated Gold Deposits in Yunnan-Guizhou-Guangxi Area
      The sulfide and lead minerals in the micro-disseminated gold deposits of Yunnan-Guizhou-Guangxi area were analyzed bysulfur lead methods.It is shown that 206Pb/204Pb values vary from 17.636 to 19.530;207Pb/204Pb from 15.451 to 16.092;208Pb/204Pb from 37.871 to 40.854 in such deposits as Maxiong,Langchuan,Jingya,Gaolong and Changshang.The gold deposits were formed later than their host sedimentary rocks.The origins of lead are complicated.Thδ34S values of sulfides in the Jingya deposit vary from -23‰ to -1‰,those in the Gaolong deposit vary from - 15.3‰ to 15.6‰,those in the Banqi deposit vary from -1.5‰ to 14.7‰,those in the Chaimohan deposit vary from 0.2‰ to 18.0‰.those in the Guochang deposit vary from -29.2‰ to 5.0‰,and those in the Yata deposit vary from 5.5‰ to 8.0‰,These data indicate that exist three sulfur sources,i.e., magma,seawater and mixed magma and sulfate in seawater.
LI Yi,XU Wenxin,LIU Wuhui,LI Heng,DAI Tagen.2005.Sulfur-Lead Isotope Geochemistry of Micro-disseminated Gold Deposits in Yunnan-Guizhou-Guangxi Area[J].Acta Geoscientica Sinica,26(z1):168-170.
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