ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
新疆萨瓦亚尔顿金锑矿床成矿作用同位素地质年代学
  
关键词:gold-antimony deposit  isotopic geochronology for mineralization  Sawayaerdun  China-Kirghiz border area
基金项目:国家重点基础研究发展规划项目(编号:2001CB409810和G1999043201),国家科技攻关计划“新疆优势矿产资源勘查综合研究”(编号2001BA609A0718)
作者单位
陈富文 中国地质调查局宜昌地质矿产研究所湖北宜昌443003 
李华芹 中国地质调查局宜昌地质矿产研究所湖北宜昌443003 
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摘要:
Metallogenic Chronology of the Sawayaerdun Gold-Antimony Deposit in Xinjiang
      The ore-forming ages and phases of the Sawayaerdun gold-antimony deposit constitute a problem of long controversy. Isotopic geochronological study of the ore-forming process shows that fluid inclusion Rb-Sr isochron ages for gold- and polymetallic sulfides-bearing quartz veins and gold-bearing quartz veins with small quantities of sulfides are 342±27 Ma and 246±16 Ma,respectively,which indicate that mineralization of gold in this orefield experienced at least two epochs,namely Carboniferous and Late Permian-Early Triassic. The single zircon U-Pb age of 133.7~131.0 Ma for monzonite-porphyry in the orefield implies that the magma was intruded after the ore-forming process in Late Jurassic to Early Cretaceous.
CHEN Fu-wen,LI Hua-qin.2003.Metallogenic Chronology of the Sawayaerdun Gold-Antimony Deposit in Xinjiang[J].Acta Geoscientica Sinica,24(6):563-567.
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