| 某多金属矿床地质特征及成因分析 |
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| 引用本文： | 赵刚,黄明然,韩建,路兴. 某多金属矿床地质特征及成因分析[J]. 中国矿山工程, 2012, 41(2): 16-19,30 |
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| 作者姓名： | 赵刚 黄明然 韩建 路兴 |
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| 作者单位： | 中国有色集团抚顺红透山矿业有限公司,辽宁抚顺,113321 |
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| 摘 要： | 矿床赋存在高于庄组合锰白云岩与大红峪组陆源碎屑岩的接触破碎带中,断裂构造不仅是重要的容矿构造,而且是重要的导矿构造。通常情况下,矿体规模的大小决定于构造破碎带规模。矿体的形态主要呈透镜状、脉状、似层状以及不规则状等。通过对含矿岩系、构造及矿体的地质特征进行分析,确定了矿床成因,并指出了找矿标志。
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| 关 键 词： | 地质特征 找矿标志 成因分析 |
Geological characteristics and genesis analysis of a polymetallic deposit |
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| Abstract: | This deposit occurs in the contact fracture zone between Gaoyuzhuang manganese dolomite and Dahongyu terrigenous clastic rock.The fracture structure is not only host structure but also ore-transmitting structure.The orebody scale usually depends on the structural fracture zone scale.The shape of orebodys are mainly lenticular,vein,stratoid and irregular.The genesis of this deposit is determined by analyzing the ore bearing rock,structure and geological feature of orebody.The ore prospecting criteria is indicated. |
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| Keywords: | geological characteristics prospecting criteria genesis analysis |
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