文章摘要
郑明泓,陈兴龙,金中国,董光贵,谢樨,刘玲.贵州维寨锑矿床辉锑矿矿物学研究及其地质意义[J].矿产勘查,2018,9(4):549-553
贵州维寨锑矿床辉锑矿矿物学研究及其地质意义
Study on stibnite and its geological significance in Weizhai antimony deposit in Guizhou Province
投稿时间：2017-08-07  
DOI：
中文关键词: 地质特征  电子探针  X衍射  维寨锑矿床  独山县  贵州
英文关键词: geological characteristics, electron probe, X-ray diffraction, Weizhai antimony deposit, Dushan county,Guizhou
基金项目:贵州省“246”找矿战略行动计划公益性、基础性项目(编号:2016-07)资助。
作者单位
郑明泓 贵州省有色金属和核工业地质勘查局,贵阳 550005 
陈兴龙 贵州省有色金属和核工业地质勘查局,贵阳 550005 
金中国 贵州省有色金属和核工业地质勘查局,贵阳 550005 
董光贵 贵州省有色金属和核工业地质勘查局,贵阳 550005 
谢樨 贵州省有色金属和核工业地质勘查局,贵阳 550005 
刘玲 贵州省有色金属和核工业地质勘查局,贵阳 550005 
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中文摘要:
      独山县维寨锑矿位于扬子陆块与华南褶皱带交接的过渡地带中。文章在野外地质调研的基础上,进行辉锑矿电子探针及X衍射分析研究,结果表明辉锑矿的化学成分较为单一(Sb,S含量分别为70.35%～71.54%和27.36%～28.36%),晶胞参数分别为:WZ01 a0=1.124,b0=1.132,c0=0.384；WZ02 a0=1.122,b0=1.131,c0=0.384；综合研究认为丹林群(D1d)及翁项群(S1-2wn)为维寨锑矿主要赋矿层位,NWW-NW向断裂为该区的主要控矿构造,维寨锑矿床属于低温热液充填型锑矿床。
英文摘要:
      Weizhai antimony deposit in Dushan county is located in the transition zone of Yangtze landmass and south China folds. Base on field geological investigation, stibnite electronic probe and X-ray diffraction analysis was conducted. The results showed that the chemical composition of the antimony was relatively single (Sb, S content was respectively 70.35%~71.54% and 27.36%~28.36%,), and the cellular parameters were WZ01:a0=1.124,b0=1.132,c0=0.384；WZ02:a0=1.122,b0=1.131,c0=0.384. Comprehensive research show that the Danlin group(D1d)and Wenxiang group(S1-2wn)are the main ore-bearing layers in the area, NWW-NW fault is the main ore-controlling structure and Weizhai antimony deposit is the type of low-temperature hydrothermal filling deposit.
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