| 大兴安岭多布库尔钼多金属矿床地质特征及找矿远景 |
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| 引用本文： | 李宪臣,胡文岭.大兴安岭多布库尔钼多金属矿床地质特征及找矿远景[J].矿产与地质,2010,24(5):391-394. |
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| 作者姓名： | 李宪臣 胡文岭 |
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| 作者单位： | [1]黑龙江省有色金属地质勘查七0六队,黑龙江齐齐哈尔161006 [2]河南金渠黄金股份有限公司,河南三门峡472000 |
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| 摘 要： | 大兴安岭多布库尔钼多金属矿床主要产于燕山晚期次流纹斑岩和隐暴角砾岩中,成矿与火山—次火山活动密切相关。矿化以细网脉状辉钼矿为主,围岩蚀变具有一定的分带性。矿床成因为斑岩型,具有形成超大型钼矿床的潜力。
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| 关 键 词： | 钼多金属矿床 地质特征 找矿远景 多布库尔 大兴安岭 |
Geological characteristics and prospecting potential of Duobukuer molybdenum polymetallic deposit in Daxinganling |
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| LI Xian-chen,HU Wen-ling.Geological characteristics and prospecting potential of Duobukuer molybdenum polymetallic deposit in Daxinganling[J].Mineral Resources and Geology,2010,24(5):391-394. |
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| Authors: | LI Xian-chen HU Wen-ling |
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| Institution: | 1.Geological Team 706#,Heilongjiang Provincial Non-Ferrous Metal Geological Exploration Bureau,Qiqihaer 161006,Heilongjiang;2.Henan Jinqu Gold Company Limited,Sanmenxia 472000,Henan) |
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| Abstract: | Duobukuer molybdenum polymetallic deposit in Daxinganling is mainly bedded in rhyolite porphyry and exploded breccia in late Yanshan epoch,and its mineralization was closely relative to volcano or sub-volcano activity.Its mineralization was mainly thin net-vein type molybdenite and the wallrock alteration shows the feature of zonal distribution.The genesis of the deposit is porphyry type and it has the potential to form super large molybdenum deposit. |
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| Keywords: | molybdenum polymetallic deposit geological characteristic prospecting potential Duobukuer |
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