黑龙江二道坎银多金属矿工艺矿物学研究

Process Mineralogy Study about Erdaokan Silver Polymetallic Deposit

  • 摘要: 二道坎银多金属矿床是以Ag为主共伴生Db、Zn、Mn等多种元素的多金属矿床,采用化学分析、光薄片鉴定、MLA分析、电子探针分析等方法对其进行了详细的工艺矿物学研究。分析结果表明,矿石中Ag含量为444 g/t,主要赋存在辉银矿等矿物中,少量赋存在深红银矿、银黝铜矿等矿物中;铅含量0.77%、锌含量0.36%,主要赋存在方铅矿和闪锌矿中;锰含量7.76%、铁含量23.22%,主要赋存在铁锰碳酸盐中。矿石中主要脉石矿物为铁锰碳酸盐和石英,金属矿物主要为黄铁矿、磁铁矿、方铅矿和闪锌矿等矿物。矿石中辉银矿等银矿物粒度细,主要分布在在75~150 μm 和20 μm以下,与各种矿物均紧密共生,不利于其单体解离;闪锌矿含量0.58%,主要分布在38~150 μm;方铅矿含量1.62%,主要分布在75 μm以下;黄铁矿含量4.50%,主要分布在在38~150 μm;铁锰碳酸盐含量58.59%,主要分布在38~150 μm,锰平均含量22.34%;磁铁矿含量2.87%,主要分布在20~150 μm。矿石有用元素多,有用矿物粒度细、相互包裹严重。由于矿石中辉银矿等银矿物粒度细、与其他矿物紧密共生,且黄铁矿含量高,建议在铅银一起回收外,单独回收黄铁矿中的银。同时由于铁锰都赋存在铁锰碳酸盐中,对锰精矿品位影响很大,建议铁锰一起回收。

     

    Abstract: Erdaokan silver polymetallic deposit is associated with lead, zinc, manganese and other elements. The Chemical analysis, microscopic research, MLA, EPMA and other analysis was used to study the process mineralogy of the Erdaokan silver polymetallic deposit in this article. The result showed that the contents of silver, lead, zinc, manganese and iron in the ore were respectively 444×10−6, 0.77%, 0.36%, 7.76% and 23.22%. The silver mainly existed in pyroxenite. And a small amount existed in pyrargyrite and freibergite. The lead mainly existed in galena, the zinc was in sphalerite, while the manganese and iron were in Fe−Mn carbonates. The main mineral composition in the ore were Fe−Mn carbonates and quartz, while the metal minerals were pyrite, magnetite, galena, and sphalerite. The granularity of pyroxenite in the ore was mainly distributed in the range of 75−150 μm and below 20 μm. pyroxenite was closely coexisting with various minerals, which was not conducive to their liberation. The sphalerite’s content was 0.58%. Its granularity mainly distributed in 38−150 μm; The galena’s content was 1.62%. Its granularity mainly distributed below 75 μm; The pyrite’s content was 4.50%. Its granularity mainly distributed in the range of 38−150 μm. The Fe−Mn carbonates’ content was 58.59%. Its granularity was mainly distributed in 38−150 μm. Its manganese average content was 22.34%. The content of magnetite was2.87%, its granularity mainly distributed in 20−150 μm. There were many useful elements in the ore, and the useful minerals were fine in particle size and were seriously wrapped with each other. Due to the fine particle size of silver minerals in the ore, and their close coexistence with other minerals, and the high content of pyrite, it is recommended to separate the recovery of silver from pyrite in addition to the unified recovery of lead and silver. Meanwhile, due to the presence of iron and manganese in siderite−rhodochrosite, it has a significant impact on the grade of manganese concentrate. It is recommended to recycle iron and manganese together.

     

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