ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
西南天山布隆金矿床成矿作用同位素地质年代学
  
关键词:quartz-barite vein-type gold deposit  isotopic geochronology for mineralization  Bulong  southwestern Tianshan Mountains  Xinjiang
基金项目:中国地质调查局基金项目“西南天山矿产资源潜力综合评价”(编号:199910200249)
作者单位E-mail
杨建国 中国地质调查局西安地质矿产研究所710054 xayjianguo@cgs.gov 
杨林海 中国地质调查局西安地质矿产研究所710054  
吕昌国 宁夏地质调查院银川750021  
李智佩 中国地质调查局西安地质矿产研究所710054  
于浦生 中国地质调查局西安地质矿产研究所710054  
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摘要:
Isotopic Geochronology of Minerogenesis of the Bulong Gold Deposit in Southwestern Tianshan Mountains
      The Bulong gold deposit, located in the southwestern Tianshan Mountains, Xinjiang Uygur Autonomous Region, is a rare epithermal quartz-barite vein-type gold deposit in China. It occurs in Devonian fine clastic rocks and is controlled by fractures zones. According to the mineral assemblages and intercalated relationship, minerogenesis of protogene mineralization phase can be divided into: ① pyrite-quartz stage; ② quartz-pyrite-siderite-barite stage; ③ calcite-quartz-barite stage; ④ barite stage. Chronology study showed that the Rb-Sr isochron age of auriferous quartz of the main mineral stage(②) is 258±15 Ma and the minerogenesis happened between Late Permian epoch and Early Triassic epoch. So it is in accordance with the tremendous minerogenesis of South Tianshan Mountains in Central Asia.
YANG Jian-guo,YANG Lin-hai,LÜ Chang-guo,LI Zhi-pei,YU Pu-sheng.2006.Isotopic Geochronology of Minerogenesis of the Bulong Gold Deposit in Southwestern Tianshan Mountains[J].Acta Geoscientica Sinica,27(1):51-55.
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