ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
热泉热液系统金的成矿地球化学研究
  
关键词:boiling spring  stream spring  gold metallogenetic geochemistry  microbral mineralization  mineralization effect
基金项目:国家自然科学基金,地质科技发展基金
作者单位
刘宝耽 中国地质科学院成都地质矿产研究所 
陆元法 中国地质科学院成都地质矿产研究所 
薛堂荣 中科院成都生物所 
贝丰 成都理工学院 
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摘要:
Study on the Gold Metallogenetic Geochemistry in Hot Spring-Hydrothermal Systems
      The Gold mineralizing actions and effect are expounded here based on the investigation of the geology , geochemistry , hydrothermal chemistry , microbe and organic matter of the gold mineralization bodies in the geothermal fields such as in Rehai , in Xiaotang, in Yangbajing and in Yangyingxiang field et al , and based on the test of microbial function . Gold mineralization happens in the hydrothermal fluids of nonequilibrium condition and of the unsaturation and unsteady state of the solute gold , the deposition gold is enriched in the amorphous and crystalline sulfide phases . There are different Au mineralization effect and characterizing mineralization bodies in the upflow zones and spring ponds of the boiling spring , stream spring and hot spring fluids ; reflecting the varied mineralizing actions . It is demonstrated that thermophilic microbe especially sulfate_reducing bacteria are the internal dynamic role which make the oxidation_reduction of - or [Au(S 2O 3) 2] 3- and Au_sulfide precipitation from the hydrothermal fluids.
LIU Bao-dan,LU Yuan-fa,XUE Tang-rong,BEI Feng.1998.Study on the Gold Metallogenetic Geochemistry in Hot Spring-Hydrothermal Systems[J].Acta Geoscientica Sinica,19(3):251-260.
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