| 内蒙古获各琦铜多金属矿床地质特征及其找矿方向 |
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| 引用本文： | 梁彦波.内蒙古获各琦铜多金属矿床地质特征及其找矿方向[J].有色金属(矿山部分),2021,73(2):106-109. |
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| 作者姓名： | 梁彦波 |
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| 作者单位： | 巴彦淖尔西部铜业有限公司 |
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| 摘 要： | 获各琦铜多金属矿基础地质工作研究程度较高,属于以沉积岩为容矿岩石的喷流沉积(Sedex)矿床,后期经热液改造。矿床铜矿石品位变化较均匀,但受到断层构造的影响使得矿体发生错断和品位富集的现象。通过分析矿石品位空间分布特征、断层构造特征、褶皱构造特征,推测了矿床找矿方向,对获各琦铜多金属矿深部及边部找矿具有指导意义。
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| 关 键 词： | 品位分布 找矿方向 构造特征 获各琦铜多金属矿 |
| 收稿时间： | 2020/6/19 0:00:00 |
| 修稿时间： | 2020/7/2 0:00:00 |
Geological characteristics and prospecting direction of the Huogeqi copper polymetal deposit in Inner Mongolia |
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| Authors: | LIANG Yanbo |
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| Affiliation: | Bayan Nur Western Copper Co., Ltd., Bayan Nur Inner Mongolia 015000, China) |
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| Abstract: | The research degree of basic geological work of the Huogeqi copper polymetal deposit is relatively high,which belongs to a sedimentary deposits(Sedex)using sedimentary rock as the ore-holding rock,after-reforming by hydrothermal.The grade of copper ore in the deposit is relatively uniform;however,due to the influence of fault structure,the orebody is faulted and grade is enriched.This paper speculated the prospecting direction of the deposit through the spatial distribution characteristics of ore grades,fault structural characteristics and fold structural characteristics,providing a guiding significance for the prospecting of the deep and edge of the Huogeqi copper polymetal deposit. |
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| Keywords: | Grade distribution Prospecting direction Structural characteristics Huogeqi copper polymetallic deposit |
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