| 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: |
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| 摘要点击次数: 1726 |
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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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