黄振强. 冷水坑银矿田成矿条件及矿床特征[J]. 地质与资源, 1993, 2(4): 284-291. DOI: 10.13686/j.cnki.dzyzy.1993.04.005
    引用本文: 黄振强. 冷水坑银矿田成矿条件及矿床特征[J]. 地质与资源, 1993, 2(4): 284-291. DOI: 10.13686/j.cnki.dzyzy.1993.04.005
    Huang Zhenqiang. THE MINERAELZATION CONDITIONS AND DEPOSIT CHARACTERISTICS OF LENGSHUIKENG SILVER OREFIELD IN JIANGXI, CHINA[J]. Geology and Resources, 1993, 2(4): 284-291. DOI: 10.13686/j.cnki.dzyzy.1993.04.005
    Citation: Huang Zhenqiang. THE MINERAELZATION CONDITIONS AND DEPOSIT CHARACTERISTICS OF LENGSHUIKENG SILVER OREFIELD IN JIANGXI, CHINA[J]. Geology and Resources, 1993, 2(4): 284-291. DOI: 10.13686/j.cnki.dzyzy.1993.04.005

    冷水坑银矿田成矿条件及矿床特征

    THE MINERAELZATION CONDITIONS AND DEPOSIT CHARACTERISTICS OF LENGSHUIKENG SILVER OREFIELD IN JIANGXI, CHINA

    • 摘要: 冷水坑中生代陆相火山-次火山岩型银矿田的成矿地质条件,着重论述矿田层控叠加型、斑岩型矿床的分布规律、物质组分、矿化分带等基本地质特征。

       

      Abstract: In this paper the author introduces the geological conditions of mineralization in Mesozoic subaerial volcanicsubvolcanic type of Lengshuikeng silver orerield and specially discusses the pricipal geological characteristics of the deposits of stratabound superimposed and porphry types in the orefield, such as distribution and composition of ores and zones of mineralization.

       

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