高级检索

甘肃舟曲羊里尾沟金矿床矿石特征及金的赋存状态研究

Study on ore characteristics and gold occurrence state in Yangliweigou Gold Deposit,Zhouqu,Gansu

  • 摘要: 利用光学显微镜鉴定和电子探针分析等方法,研究了羊里尾沟金矿床矿石特征及金的赋存状态。矿石中金属矿物主要为黄铁矿,其次为毒砂、辉锑矿,金矿物主要为自然金,其次为银金矿;金以细粒金为主,其次为微粒金和中粒金,少量次显微金;嵌布形态主要为尖角粒状、板片状、细脉状;嵌布状态以裂隙金和粒间金为主,其次为包裹金;载金矿物为黄铁矿、石英、褐铁矿、毒砂、碳质。黄铁矿电子探针分析结果表明,羊里尾沟金矿床形成于中低温环境,且与岩浆作用有关;结合该矿区及其外围泥盆系和石炭系地层中的金丰度,认为羊里尾沟金矿床成矿物质可能为地层和岩浆的混合来源。

     

    Abstract: By means of optical microscope identification and electron probe analysis,the ore characteristics and gold occurrence state of Yanliweigou Gold Deposit were studied.The metallic minerals in the ore were mainly pyrite,followed by arsenopyrite and stibnite.The gold mineral is mainly native gold followed by electrum.The gold is dominated by fine-grain gold followed by micro-grain gold and mediumgrain gold and there is a small amount of submicroscopic grain gold;the shape in which gold is embedded is mainly pointed grain,lamellar,veinlet;the occurrence state is dominated by fissure gold and intergranular gold followed by encased gold;the gold-bearing minerals are pyrite,quartz,limonite,arsenopyrite and carbonatite.Pyrite electron probe analysis shows that the Yangliweigou Gold Deposit was formed in a medium-low temperature environment,and is related with magmatism;Based on the gold enrichment in the strata of the area and its peripheral Devonian and Carboniferous systems,it is believed that the metallogenic materials in Yangliweigou Gold Deposit may be a mixed source of strata and magma.

     

/

返回文章
返回