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现代矿业 ›› 2014, Vol. 30 ›› Issue (04): 34-37.

• 地质·测量 • 上一篇    下一篇

复兴村金矿地质构造与工程地质岩组划分

王常金,晋海滨,刘忠田,葛永森,王振宇,胡军海   

  1. 武警黄金第三支队
  • 出版日期:2014-04-15 发布日期:2014-06-06
  • 基金资助:

    黄金指挥部黄金地质工作专项业务费项目(编号:2011—20120306)。

Divison of Geologic Structures and Rock Groups of Fuxingchun Gold Deposit

Wang Changjin,Jin Haibin,Liu Zhongtian,Ge Yongsen,Wang Zhenyu,Hu Junhai   

  1. Third Gold Geological Party,Chinese Armed Police Forces
  • Online:2014-04-15 Published:2014-06-06

摘要: 复兴村金矿区断裂构造发育,主要控矿构造是发育于珍珠门组大理岩与大栗子岩组片岩接触界面层间断裂及北东向、北西向脆性剪切断裂带;岩体的结构面对岩体的力学性质具有较大影响,可分为Ⅱ级、Ⅲ级、Ⅳ级结构面;依据岩性、岩石力学性质,工程地质岩组可划分为第四系松散岩类岩组、较坚硬薄层变质岩组、坚硬块状碳酸盐岩组、坚硬块状火山岩组。其中较坚硬薄层变质岩组分布区,岩体中层理、页理、节理发育,完整性较差,并夹有软弱夹层,工程地质性质较差,应是今后矿区工程地质问题的主要研究层位。

关键词: 地质构造, 工程地质岩组, 岩体结构面

Abstract: The fault structures of Fuxingchun gold deposit is well developed.The main ore-controlling structures is developed in the layered structures of the contact zone of marble of Zhenzhumen formation and schist of Dalizi formation,and northwestern,northeastern brittle shear fault zones.Rock structural plans have great impact on the rock mechanical property,so it can be divided into II,IIIand IV structural plane.The engineering geological petrofabric is divided into the Quaternary lax rock,harder-strong thin thick metamorphic rock,hard lump carbonate rock and hard lump volcanic rock in line with the lithology and rock mechanical property.The well developed bedding,foliation and joints,and poor integrity and engineering geological conditions of the rocks in the distribution area of hard lump carbonate rock group.Therefore,layers of the rocks should be studied in the future so as to deal with the engineering geological problems in the mining area.

Key words: Geologic Structures, Groups in engineering geology, Rock structural plane