金寨县迎峰崖铅锌多金属矿有用矿物分布特征
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作者单位:

1.-东华理工大学核资源与环境国家重点实验;2.-安徽省地矿局;3.安徽省地质实验研究所

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P575.(2,4,5)

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2016.06 安徽省地矿局基金 《安徽省金寨县迎峰崖铅锌矿多金属矿详查》(2014-DZ-04〕)


Distribution of useful minerals in yingfengya lead zinc polymetallic deposit, Jinzhai County
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National key experiment on nuclear resources and environment, Donghua University of technology

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    摘要:

    为了查清矿区内矿石的物质组分及其嵌布特征,本次采用多组分元素分析、光薄片镜下鉴定、X射线衍射分析,单矿物组分析析等方法对矿石的物质组分及其在矿石中的分布情况,嵌布特征进行分析研究。结果表明:矿石中主要为方铅矿、闪锌矿、黄铜矿、黄铁矿、石英、白云母等。方铅矿、闪锌矿以包裹嵌镶或粘连镶布为主,细小的方铅矿矿物与其他矿物之间以直接毗邻,交代成因的闪锌矿呈融滴状分布于被交代矿物之上,难以分离;石英以包裹或镶嵌方式呈他形或半自形柱状存在于上述矿物间隙之中。通过研究,为矿物的分离及后期的开发利用提供有益的线索和应用价值。

    Abstract:

    In order to find out the material composition and embedding characteristics of the ore in the mining area, they are been analyzed and studied that is material composition and embedding characteristics by means of multi-component element analysis, identification under light slice microscope, X-ray diffraction analysis and single mineral composition analysis. The results show that the ores are mainly composed of galena, sphalerite, chalcopyrite, pyrite, quartz and muscovite. Galena and sphalerite are mainly wrapped and inlaid or adhesive inlaid, and the fine galena minerals are directly adjacent to other minerals. The metasomatic sphalerite is distributed on the metasomatic minerals in the form of melt droplets, which is difficult to separate; Quartz exists in the above mineral gaps in the form of heteromorphic or subhedral column in the form of wrapping or inlaying. The research provides useful clues and application value for mineral separation and later development and utilization.

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王西荣,张青,李磊. 金寨县迎峰崖铅锌多金属矿有用矿物分布特征[J]. 科学技术与工程, , ():

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  • 收稿日期:2021-11-29
  • 最后修改日期:2022-05-25
  • 录用日期:2022-05-29
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