| 大兴安岭东坡甘珠尔庙银多金属矿地质特征及找矿方向 |
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| 引用本文： | 李玉芹,王学贞,王振生,李红超.大兴安岭东坡甘珠尔庙银多金属矿地质特征及找矿方向[J].矿物学报,2011,31(3):610-614. |
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| 作者姓名： | 李玉芹 王学贞 王振生 李红超 |
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| 作者单位： | 1. 河南省有色金属地质矿产局第七地质大队,河南郑州,450016
2. 河南省有色金属地质矿产局,河南郑州450052／南京大学地质与工程学院,江苏南京210093 |
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| 摘 要： | 甘珠尔庙银多金属矿区地处内蒙大兴安岭东坡南段，位于黄岗梁一甘珠尔庙铜多金属成矿带北东部、白音诺一甘珠尔庙银铜多金属成矿亚带的北东段。矿体具有品位高而不均，厚度相对较薄而密集分布的特点，构造及其节理裂隙控矿作用明显，矿体视电阻率和视充电率异常表现为低阻高极化组合特征，推测密集蚀变脉群的深部可能存在与本区成矿有关的隐伏岩体，在进一步找矿工作中应加以重视。同时，在各矿化脉体的深部交汇部位是找矿的最有利部位，在今后找矿中应加强该部位的钻探验证工作。
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| 关 键 词： | 银多金属矿 地质特征 找矿方向 甘珠尔庙 |
A Tentative Study of the Geology and Ore Potentiality of Ganzhuermiao Ag Polymetallic Deposit,East-Side Hill of Daxinganling,China |
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| LI Yu-qin,WANG Xue-zhen,WANG Zhen-sheng,LI Hong-chao.A Tentative Study of the Geology and Ore Potentiality of Ganzhuermiao Ag Polymetallic Deposit,East-Side Hill of Daxinganling,China[J].Acta Mineralogica Sinica,2011,31(3):610-614. |
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| Authors: | LI Yu-qin WANG Xue-zhen WANG Zhen-sheng LI Hong-chao |
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| Institution: | LI Yu-qin1,WANG Xue-zhen1,WANG Zhen-sheng1,LI Hong-chao2,3(1.The 7th Geological Team of Henan Bureau of Nonferrous Geology and Mineral Resources,Zhengzhou 450016,China,2.Henan Bureau of Nonferrous Geology and Mineral Resources,Zhengzhou 450052,3.School of earth science and engineering of the Nanjing University,Nanjing 210093,China) |
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| Abstract: | Ag poly-metallic deposit of Ganzhuermiao is situated on the South segment of east-side hill of Daxinganling.It lies in the northeastern Huanggangliang-Ganzhuermiao's metallogenic belt and Baiyinnuo-Ganzhuermiao's Ag-Cu metallogenic belt.Ore body has the following characteristics: The tenor is high but uneven;the thickness is opposite thinner but distributes intensively.The structure and subsidiary joints and fissures showing parallel clusters in occurrence control the metallogenesis to a great extent.The co... |
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| Keywords: | Ag poly-metallic deposit geological characteristics ore potentiality Ganzhuermiao |
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