蔡明明, 李光胜, 朱幸福, 等. 基于金矿岩芯的自动工艺矿物学[J]. 矿产综合利用, 2024, 45(3): 174-178. DOI: 10.3969/j.issn.1000-6532.2024.03.027
    引用本文: 蔡明明, 李光胜, 朱幸福, 等. 基于金矿岩芯的自动工艺矿物学[J]. 矿产综合利用, 2024, 45(3): 174-178. DOI: 10.3969/j.issn.1000-6532.2024.03.027
    CAI Mingming, LI Guangsheng, ZHU Xingfu, et al. Automatic process mineralogy based on gold ore core[J]. Multipurpose Utilization of Mineral Resources, 2024, 45(3): 174-178. DOI: 10.3969/j.issn.1000-6532.2024.03.027
    Citation: CAI Mingming, LI Guangsheng, ZHU Xingfu, et al. Automatic process mineralogy based on gold ore core[J]. Multipurpose Utilization of Mineral Resources, 2024, 45(3): 174-178. DOI: 10.3969/j.issn.1000-6532.2024.03.027

    基于金矿岩芯的自动工艺矿物学

    Automatic Process Mineralogy Based on Gold Ore Core

    • 摘要: 这是一篇工艺矿物学领域的论文。山东某石英脉型金矿,金品位2.51 g/t。为对该矿床的进一步开发及选矿工艺研究,对该矿物开展了工艺矿物学研究。本次研究涉及的技术方法包括多元素化学分析、化学物相分析、光学显微镜鉴定、X射线衍射(XRD)分析、矿物自动定量分析(BPMA)、扫描电镜-能谱仪(SEM-EDS)分析等。结果表明:(1)矿石中金矿物绝大多数为银金矿,偶见微量的金银矿和自然金;(2)矿石中金矿物与黄铁矿等硫化物的嵌布关系十分密切,黄铁矿是金矿物的最主要的载体矿物,矿石中单体及裸露金的占有率较高,为58.96%,黄铁矿等硫化物中包裹金的占有率为39.84%,脉石矿物中包裹金的占有率为1.20%;(3)矿石中金矿物粒度分布不均匀,整体粒度较细,矿石中可见粒度+0.020 mm的金矿物颗粒,其占有率为22.08%,-0.020 mm的金矿物占有率为77.92%,其中-0.005 mm的微粒金矿物占有率为24.83%,-0.001 mm的亚微米级微细粒金矿物占有率为0.35%。

       

      Abstract: This is an article in the field of process mineralogy. A quartz vein type gold deposit in Shandong has a gold grade of 2.51 g/t. In order to further develop the deposit and study the beneficiation process, the process mineralogy of the mineral was carried out. The technical methods involved in this study include multi-element chemical analysis, chemical phase analysis, optical microscope identification, X-ray diffraction (XRD) analysis, automatic quantitative mineral analysis (BPMA), scanning electron microscope energy spectrometer (SEM-EDS) analysis, etc. The results show that: (1) most of the gold minerals in the ore are silver-gold, and a small amounts of gold, silver and natural gold are occasionally found; (2) The embedding relationship between gold minerals and sulfides such as pyrite in the ore is very close. Pyrite is the main carrier mineral of gold minerals, and the proportion of single and exposed gold in the ore is high, which is 58.96%. The proportion of gold encapsulated in sulfides such as pyrite is 39.84%, and the proportion of gold encapsulated in gangue minerals is 1.20%; (3) The particle size distribution of gold minerals in the ore is uneven, and the overall particle size is relatively fine. Gold particles with a particle size larger than 0.020 mm can be seen in the ore, with an occupancy rate of 22.08%. Gold minerals with a particle size less than 0.020 mm have an occupancy rate of 77.92%, with an occupancy rate of 24.83% for micro gold minerals with a particle size less than 0.005 mm and 0.35% for sub micron sized gold minerals with a particle size less than 0.001 mm.

       

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