文章摘要
陆晓,徐福忠.内蒙古碱场铅锌多金属矿床地质特征及找矿标志[J].矿产勘查,2018,9(4):554-558
内蒙古碱场铅锌多金属矿床地质特征及找矿标志
Geological characteristics and prospecting indicator of Jianchang Pb-Zn deposit, Inner Mongolia
投稿时间:2017-10-18  
DOI:
中文关键词: 碱场  铅锌矿床  地质特征  找矿标志  内蒙古
英文关键词: Jianchang,Pb-Zn deposit,geological characteristics, prospecting criteria,inner Mongolia
基金项目:
作者单位
陆晓 中国冶金地质总局矿产资源研究院,北京 101300 
徐福忠 中国冶金地质总局矿产资源研究院,北京 101300 
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中文摘要:
      碱场铅锌多金属矿床位于得耳布干成矿带北段。赋存于新元古界额尔古纳河组大理岩、板岩地层中。矿化受 NNE 向断裂和构造裂隙控制明显,矿体呈脉状产出;矿区内发现4条铅锌矿体,I号、II号、III号、IV号,矿石中金属矿物以闪锌矿、方铅矿、黄铁矿为主;矿体及围岩发育中低温热液蚀变。该铅锌矿床属于中低温热液脉型铅锌矿床。
英文摘要:
      Jianchang Pb-Zn deposit is located in the north of Deerbugan metallogenic belt. Orebodies occured in the marble and slate rocks of Ergunhe formation, the upper Proterozoic, controlled obviously by the NNE-trending fault and structural fracture. There are four Pb-Zn orebodies:I,II,III,IV. Metal minerals in ores mainly include sphalerite galenite and pyrite, developed medium-and-low temperature hydro-therm alterations. So we can draw an conclusion that Jianchang deposit is a typical medium-and-low temperature hydro-therm vein deposit.
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