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    刘斌, 余昌涛. 辽南猫岭细脉浸染型金矿床的成矿模式[J]. 地质与资源, 1994, 3(2): 103-106. DOI: 10.13686/j.cnki.dzyzy.1994.02.004
    引用本文: 刘斌, 余昌涛. 辽南猫岭细脉浸染型金矿床的成矿模式[J]. 地质与资源, 1994, 3(2): 103-106. DOI: 10.13686/j.cnki.dzyzy.1994.02.004
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    Liu Bin, Yu Changtao. THE METALLOGENIC MODEL FOR MAOLINGVEINLET-DISSEMINATED GOLD DEPOSITIN THE SOUTH LIAONING[J]. Geology and Resources, 1994, 3(2): 103-106. DOI: 10.13686/j.cnki.dzyzy.1994.02.004
    Citation: Liu Bin, Yu Changtao. THE METALLOGENIC MODEL FOR MAOLINGVEINLET-DISSEMINATED GOLD DEPOSITIN THE SOUTH LIAONING[J]. Geology and Resources, 1994, 3(2): 103-106. DOI: 10.13686/j.cnki.dzyzy.1994.02.004
    shu

    辽南猫岭细脉浸染型金矿床的成矿模式

    THE METALLOGENIC MODEL FOR MAOLINGVEINLET-DISSEMINATED GOLD DEPOSITIN THE SOUTH LIAONING

      摘要
    • 摘要: 辽南猫岭金矿床是低品位细脉浸染型金矿床，矿体为含金石英细脉和含金毒砂-黄铁矿化绢云千枚岩。本文研究了该矿区地质特征、矿床地质特征及矿化的物质来源，认为其成因与岩浆活动有关。本文在此基础上建立了猫岭细脉浸染型金矿床的成矿模式。

       

      Abstract: Maoling gold deposit,located in the southwest of Liaodong Peninsula, discovered in 1985, is a giant veinlet-disseminated ore with low grade. The ore bodies are auriferous quartz veinlets and-arsenopyritized-pyritized sericite phyllite or schist. Au grade ranges from 3 to 5g/t. The country rock is the second member of Gaixian formation. Magmatic activities were common in the area.

       

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