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Home > Wen Yuan (Primary School Edition) > 2021 No.11 > 葫芦岛甸子银多金属矿矿床地质特征及成因分析

  • 葫芦岛甸子银多金属矿矿床地质特征及成因分析

    Author(s)：

    卢继兵

    Publication Title：

    Wen Yuan (Primary School Edition) 2021 No.11

    Affiliations：

    马道矿业有限责任公司 辽宁 葫芦岛 125315

    Abstract：

    甸子银多金属矿是辽宁葫芦岛市发现的一重要矿床，主要在燕山台褶带辽西台陷和山海关台拱交接部位分布，中元古界蓟县系雾迷山组地层在矿区比较发育，并发育有新元古界青白口系景儿峪组，区内构造主要为北东向断裂构造，中生代花岗岩和成矿有着最为紧密的关联性，优越的成矿条件，对于葫芦岛甸子银多金属矿的形成起到了很大的促进作用。下文中主要对该矿地质特征予以分析探讨，并探究其矿床成因，总结找矿标志，希望能对该矿地质找矿工作提供一些借鉴和参考。

    Keywords：

    葫芦岛甸子银多金属矿；地质特征；成因；找矿标志

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    [1] 卢继兵.葫芦岛甸子银多金属矿矿床地质特征及成因分析[J].Wen Yuan (Primary School Edition),2021(11),.

文渊(小学版)
Wen Yuan (Primary School Edition)

Language: 中文

CN：11-9274/G

ISSN：2096-6261

Publication Frequency: 月刊

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