文章摘要
张沛,唐攀科,陈爱清.湖南沃溪金锑钨矿床中成矿物质来源的硫同位素地球化学证据[J].矿产勘查,2019,(3):529-535
湖南沃溪金锑钨矿床中成矿物质来源的硫同位素地球化学证据
The evidences of sulfur isotope geochemistry for the source of metallogenic substance in the Woxi Au-Sb-W deposit
投稿时间:2018-07-12  
DOI:
中文关键词: 硫同位素  Au-Sb-W矿床  地球化学  黄铁矿  辉锑矿
英文关键词: sulfur isotope,Au-Sb-W deposit,geochemistry,pyrite,stibnite
基金项目:全国危机矿山接替资源找矿资助项目(编号:20109901)资助。
作者单位
张沛 有色金属矿产地质调查中心,北京 100012 
唐攀科 有色金属矿产地质调查中心,北京 100012 
陈爱清 广州海洋地质调查局,广州 510075 
摘要点击次数: 33
全文下载次数: 23
中文摘要:
      沃溪AuSbW矿床是湖南湘西前寒武纪地层中最具有代表性的金矿床之一,位于扬子准地台江南地轴南缘的雪峰弧形构造隆起带的中段。矿石以石英-金-硫化物型为主,与金共存的矿石矿物为辉锑矿、黑钨矿、白钨矿、黄铁矿等。文章对沃溪矿床深部矿段中辉锑矿和黄铁矿的硫同位素地球化学进行了研究,结果表明:黄铁矿的δ34S变化范围-4.05‰~ 0.42‰,极差4.47‰,平均值-1.54‰;辉锑矿的δ34S变化范围-4.99‰~-1.52‰,极差3.47‰,平均值-2.87‰。δ34S变化范围小,说明其来源的均一性,同时与赋矿的马底驿组富硫围岩的δ34S很相近,表明硫来源于赋矿地层。同时,δ34S具有从浅部向深部增大的趋势。
英文摘要:
      The Woxi Au-Sb-W deposit ,situated in the central sector of Xuefeng arc-structural mole track located on the southern margin of Jiangnan Earth axis in Yangtze Para platform,is one of the most representative gold deposits in Precambrian stratum of western Hunan province。Ores are mainly quartz-gold-sulfide。Minerals coexisting with gold are stibnite,wolframite,scheelite and pyrite ect.。Studies on the sulfur isotope geochemistry of pyrite and stibnite in the Woxi deep mines,show that the δ34S of pyrite varies from -4.05‰ to 0.42‰,range4.47‰,with an average of -1.54‰ and that the δ34S of stibnite varies from-4.99‰ to -1.52‰,range3.47‰,with an average of -2.87‰。The centralized distribution of δ34S, showing the uniformity of its source,very close to the δ34S of sulfur-rich wall rock of the Ma di yi formation ,indicates that the sulfur deriveds from the stratigraphic ,with δ34S increaseing from shallow to deep。
查看全文   查看/发表评论  下载PDF阅读器
关闭