吴长航, 浮海梅, 李江山, 张振国, 马春萍, 韩新志. 河南吉家洼金矿床矿石特征及金的赋存状态[J]. 地质与资源, 2008, 17(4): 259-263. DOI: 10.13686/j.cnki.dzyzy.2008.04.010
    引用本文: 吴长航, 浮海梅, 李江山, 张振国, 马春萍, 韩新志. 河南吉家洼金矿床矿石特征及金的赋存状态[J]. 地质与资源, 2008, 17(4): 259-263. DOI: 10.13686/j.cnki.dzyzy.2008.04.010
    WU Chang-hang, FU Hai-mei, LI Jiang-shan, ZHANG Zhen-guo, MA Chun-ping, HAN Xin-zhi. CHARACTERISTICS OF ORE AND OCCURRENCE OF GOLD IN JIJIAWA GOLD DEPOSIT, HENAN PROVINCE[J]. Geology and Resources, 2008, 17(4): 259-263. DOI: 10.13686/j.cnki.dzyzy.2008.04.010
    Citation: WU Chang-hang, FU Hai-mei, LI Jiang-shan, ZHANG Zhen-guo, MA Chun-ping, HAN Xin-zhi. CHARACTERISTICS OF ORE AND OCCURRENCE OF GOLD IN JIJIAWA GOLD DEPOSIT, HENAN PROVINCE[J]. Geology and Resources, 2008, 17(4): 259-263. DOI: 10.13686/j.cnki.dzyzy.2008.04.010

    河南吉家洼金矿床矿石特征及金的赋存状态

    CHARACTERISTICS OF ORE AND OCCURRENCE OF GOLD IN JIJIAWA GOLD DEPOSIT, HENAN PROVINCE

    • 摘要: 通过对吉家洼金矿床矿石特征及金的赋存状态的研究,讨论了该矿床的矿石类型、结构构造、物质组成、矿物成分、金的赋存状态等.研究表明,该矿床矿石类型以氧化矿石为主,深部原生矿石逐渐增多.矿石中矿物种类多样,主要金属矿物为黄铁矿,脉石矿物以石英、斜长石、绢云母为主.金矿物主要为自然金,在矿石中分布极不均匀,以粒间金和裂隙金为主要赋存形式,粒度介于0.005~0.1 mm之间,金矿物的成色变化具有阶段性和分带性特征,受成矿温度控制明显.

       

      Abstract: Based on the study of gold ore characteristics and gold occurrence in Jijiawa gold deposit, Henan Provinee, it is concluded that the deposit is dominated by oxidized ore, with increasing primary ores in the deep. The minerals are diverse in the ore. The major metallic mineral is pyrite, with gangue minerals mainly quartz, plagioclase and sericite. The auriferous mineral, dominantly native gold, is unevenly distributed in the ore, occurring as intergranular gold and fracture gold. The size of the gold particles is about 0.005-0.1 mm. The fineness of gold, characterized by multistage and vertical zoning, is obviously controlled by temperature.

       

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