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黔西南泥堡金矿床矿石地球化学特征及其地质意义

Geochemical characteristics of ores from Nibao Gold Deposit in Southwestern Guizhou and their geological significance

  • 摘要: 泥堡金矿床是黔西南地区重要的复合型卡林型金矿床,其产出断裂型矿体、层控型矿体和氧化矿体,矿石类型分别对应角砾岩型矿石、凝灰岩型矿石和氧化矿石。对3类矿石进行了系统的地球化学测试,测试结果显示各类矿石化学组分含量差异较大,但均表现出富As、Cu和贫Na的特点,暗示了原生矿石在后期表生作用下载金矿物表现出相似的地球化学行为。矿石中K2O并未因后期热液作用的影响而流失,而是形成伊利石,反映后期成矿环境相对稳定。不同类型矿石中Au元素与Hg、Ag、Tl等元素显示出了显著的相关性,因此认为,Au-Hg-Ag-Pb-Tl-As组合异常应为泥堡金矿区的地球化学找矿标志。

     

    Abstract: Nibao Gold Deposit,located in Southwestern Guizhou,is regarded as an important composite Carlin-type gold deposit.Fault-controlling type,stratum-controlling type and oxidized type ore bodies have been recognized in the deposit and are correspondingly composed of breccia-type,tuff-type and oxide ores.This paper systematically tested the geochemical characteristics of the 3 ores.The results show that the chemical compositions in the ores vary greatly,but share the same geochemical characteristic of As-,Cu-rich and Na-poor,suggesting that the gold-bearing minerals in original ores show similar geochemical behavior under supergene conditions.The K2O formed illite instead of running away with fluids during hydrothermal process that came after,which suggested a sustainable ore-forming environment in the late phase.There are significant correlations between Au and Hg,Ag,Tl,etc.,suggesting that Au-Hg-Ag-Pb-Tl-As composite anomaly should be used as geochemical marker for mineral exploration in Nibao Gold District.

     

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