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金属矿山 ›› 2023, Vol. 52 ›› Issue (03): 140-146.

• 矿物工程 • 上一篇    下一篇

某极难选蚀变岩型金矿石工艺矿物学研究

胡梦忠1,2 熊召华1,2 铁 颖1,2 丁 超1,2 马生萍1,2 马全明1,2 洪秋阳3
  

  1. 1. 青海省第六地质矿产勘查院,青海 格尔木 816000;2. 青海省金矿资源开发工程技术研究中心,青海 都兰 816100;3. 广东省科学院资源利用与稀土开发研究所,广东 广州 510630
  • 出版日期:2023-03-15 发布日期:2023-04-12
  • 基金资助:
    柴达木盆地大型金矿资源高效提质降杂新技术研究与示范项目(编号:22QYCX0061)。

Study on Process Mineralogy of a Gold Ore With Extremely Refractory Altered Rock Type

HU Mengzhong1,2 XIONG Zhaohua1,2 TIE Ying1,2 DING Chao1,2 MA Shengping1,2MA Quanming1,2 HONG Qiuyang3   

  1. 1. Qinghai 6th Institute of Geology and Mineral Exploration,Golmud 816000,China;2. Qinghai Engineering Research Center of Gold Mineral Resource Development,Dulan 816100,China;3. Institute of Resource Utilization and Rare Earth Development,Guangdong Academy of Sciences,Guangzhou 510630,China
  • Online:2023-03-15 Published:2023-04-12

摘要: 为有效利用某极难选蚀变岩型金矿石,对原矿石开展了系统的工艺矿物学试验,重点研究了矿石的物 质组成、粒度组成、结构构造、主要矿物嵌布特征及金粒特征等。 结果表明:① 原矿中主要可利用元素为金,有害杂质 As 含量较高,并含有一定的碳;金主要以硫化物包裹金的形式存在,其次为裸露金。 ② 原矿中自然金痕量,主要载金 矿物黄铁矿、磁黄铁矿的含量分别为 3. 829%、0. 111%;脉石矿物以石英为主,占 45. 176%,此外还含有 0. 779%的毒 砂。 ③ 原矿中-0. 01 mm 粒级含量及 Au 分布率均小于 10%,各粒级 Au 的品位变化不大,仅有 0. 043 ~ 0. 02 mm 粒级 水析沉砂中富集已解离金粒。 ④ 矿石主要结构包括自形—半自形晶粒状、他形晶粒状、他形碎裂化及乳滴状,主要构 造包括稀疏浸染状、条带状、角砾状、细脉状。 ⑤ 金主要包含于毒砂、黄铁矿等硫化矿物中,其次包含于石英、绢云母 等脉石矿物中,90%的金粒度小于 8 μm,以微细和超微细粒金为主。 ⑥ 主要载金矿物嵌布粒度由粗到细依次为黄铁 矿、磁黄铁矿、毒砂,毒砂嵌布粒度微细,浮选要注意细粒毒砂的回收。 ⑦ 在磨矿细度为-0. 075 mm 占 62. 57%时,黄 铁矿、毒砂和硫砷矿物的解离度分别为 90. 04%、81. 95%和 90. 04%。 根据工艺矿物学研究成果,采用浮选回收游离金 和硫化矿物,理论回收率 89%左右。 研究结果对制定合理的选矿工艺具有重要的指导意义。

关键词: 极难选蚀变, 工艺矿物学, 嵌布粒度, 黏土矿物

Abstract: In order to make effective use of an extremely refractory gold ore,systematic process mineralogy tests have been carried out aiming at the raw ore. The material composition,particle size composition,texture and structure,main mineral distribution characteristics and gold particle characteristics of the ore have been studied. The results showed that:① The main available element in raw ore is gold,and the content of harmful impurity As is high with some carbon. Gold mainly exists in the form of sulphide coated gold,followed by exposed gold. ② The natural gold in raw ore is of trace amount,and the content of main gold-bearing minerals pyrite and pyrrhotite are 3. 829% and 0. 111%,respectively. Gangue mineral is mainly quartz,accounting for 45. 176%,in addition to containing arsenopyrite of 0. 779%. ③ The content of -0. 01 mm and the distribution rate of Au in the raw ore are less than 10%,and the grade of Au in each grain size has little change. The gold is only enriched in 0. 043 ~ 0. 02 mm of water precipitation sand. ④ The main texture of the ore include euhedral and semi-euhedral grains,heteromorphic grains,heteromorphic fragmentation and emulsion drops,and the main structure include sparsely disseminated,banded,brecciform and veined. ⑤ Gold is mainly contained in sulfide minerals such as arsenopyrite and pyrite,followed by gangue minerals such as quartz and sericite. 90% of the gold particle size is less than 8 μm,mainly fine and ultra-fine gold. ⑥ The distribution size of main gold-bearing minerals from coarse to fine is pyrite,pyrrhotite and arsenopyrite. The distribution size of arsenopyrite is very fine. Attention should be paid to the recovery of fine arsenopyrite in flotation. ⑦ When the grinding fineness is -0. 075 mm accounting for 62. 57%,the dissociation degrees of pyrite,arsenopyrite and sulfur and arsenic minerals are 90. 04%,81. 95% and 90. 04%,respectively. According to the research results of process mineralogy,free gold and sulfide minerals were recovered by flotation with a theoretical recovery of about 89%. The research results have important guiding significance for formulating reasonable beneficiation process.