充填矿床

充填矿床充填矿床
  1. 半坡锑矿床是典型的断裂控矿,热液充填型矿床。

    Banpo antimony deposit is a typical fracture-controlling and hydrothermal fluid filling deposit .

  2. 通过系统分析,本文认为龙山金锑矿是中温岩浆期后热液充填型矿床;

    According to the comprehensive analysis , the author suggests that the genesis of LongShan Au-Sb ore deposit should be middle-temperature and injection type deposit .

  3. 各矿区矿化蚀变带较发育,硅化、黄铁矿化、钾化、叶腊石化、绿泥石化、绢云母化等具有一定的水平分带,反映出中低温热液充填交代矿床的某些特征。

    In all of mines , the alteration zones developed , silicification , pyritization , potassic alteration , pyrophyllitization , chloritization , and sericitization show that the deposits have the features of middle-low temperature hydrothermal filling-metasomatic deposit . 5 .

  4. 广东陆丰硫铁矿床为一个中低温热液交代充填型脉状矿床。伴生有综合利用价值的Cu、Au、Ag、Te、Bi等元素。

    The Lufeng pyrite deposit in Guangdong , a vein filling , micro mesothermal , metasomatic deposit , accompanies such comprehensively usable elements as Cu , Au , Ag , Te and Bi .

  5. 鄂西东岳中低温热液充填型大理石矿床的地质特征

    Geological characteristics of the mesothermal epithermal marble deposit in

  6. 充填法开采矿床的不安全因素及对策

    Unsafe factors of back-fill mined orebodies and Its Countermeasures

  7. 南风坳银矿是产于震旦系浅变质碎屑岩中受北北东&北东向断裂控制的热液充填交代型矿床。

    The Nanfeng'ao Ag deposit is a hydrothermal fissure filling-metasomatism type deposit controlled by NNE-NE trend faults .

  8. 渣滓溪钨锑矿床位于湘西雪峰山弧形构造带的中段,是我国典型的脉状充填型锑矿床。

    The Zhazixi W-Sb deposit , located in the middle part of Xuefengshan arc tectonic zone , is one of typical vein-filled hydrothermal deposits in China .

  9. 简要论述了典型热液裂隙充填钨铋钼石英脉矿床地质及其以黑钨矿辉铋矿辉钼矿为主的矿物组合纵向逆分带现象。矿体与围岩界线清晰,属中-低温热液充填型矿床。

    The paper discusses the hydrothermal filling deposit of W-Bi-Mo quartz vein type and the vertical reverse zoning distribution of wolframite-bismuthinite - molybdenite mineral group . The boundary line between ore body and country rock is distinct , being a meso-epithermal filling deposit .