| 内蒙古丰镇市开花山银多金属矿矿床地质特征及成因分析 |
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| 引用本文： | 何其芬,刘锋,魏印涛.内蒙古丰镇市开花山银多金属矿矿床地质特征及成因分析[J].山东国土资源,2014,30(7):29-32. |
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| 作者姓名： | 何其芬 刘锋 魏印涛 |
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| 作者单位： | 山东省物化探勘查院;山东省物化探勘查院;山东省物化探勘查院 |
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| 摘 要： | 内蒙古丰镇市开花山银多金属矿床赋存于太古宙集宁(岩)群片麻岩分布区的构造破碎带中,为小型银多金属矿矿床,共揭露3个矿体,矿体规模较小,矿石结构简单,矿石品位相对较稳定。岩浆热液和断裂构造破碎带对成矿、控矿具有重要作用。矿床成因属浅成中低温热液型矿床。
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| 关 键 词： | 银多金属矿 地质特征 矿床成因 内蒙古丰镇市 |
Analysis on Geological Characteristics and the Origin of Silver Polymetallic Deposit in Kaihuashan in Fengzhen Town of Inner Mongolia |
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| HE Qifen,LIU Feng and WEI Yintao.Analysis on Geological Characteristics and the Origin of Silver Polymetallic Deposit in Kaihuashan in Fengzhen Town of Inner Mongolia[J].Land and Resources in SHANDONG Province,2014,30(7):29-32. |
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| Authors: | HE Qifen LIU Feng and WEI Yintao |
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| Institution: | ( Shandong Geophysical and Geochemical Exploration Institute, Shandong Jinan 250013, China) |
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| Abstract: | Kaihuashan silver polymetallic deposit in Fengzhen town in Inner Mongolia occurred in fractural zones of Archean Jining group. It is a small type silver polymetallic deposit .Three ore deposits have been exposed totally with small scale, simple ore structure and stable ore grades. The magmatic hydrothermal and fault fracture zones play important roles in ore formation and control. Iris medium and low temperature magmatic hydrothermal type deposit. |
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| Keywords: | Silver polymetallic ore geological characteristics origin of the deposit Inner Mongolia |
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