| 锦丰（烂泥沟）金矿地质特征及找矿方向浅析 |
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| 引用本文： | 王旭阳,王方里,王宏阳.锦丰（烂泥沟）金矿地质特征及找矿方向浅析[J].云南地质,2014(1):130-132,137. |
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| 作者姓名： | 王旭阳 王方里 王宏阳 |
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| 作者单位： | 桂林理工大学地球科学学院,广西桂林541004 |
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| 摘 要： | 锦丰（烂泥沟）金矿由磺厂沟复式向斜控制了矿体的空间分布,发育于磺厂沟复式向斜中的一系列断裂控制了矿床的产出位置,不同的岩性组合控制了矿体的具体产出层位.在矿床的形成过程中F3断裂不仅是矿区的主要导矿构造也是矿区的主要容矿构造,在矿床的形成过程中由于不同断块的差异运动导致了磺厂沟向斜不同的变形部位出露在同一水平的现象,为今后的矿床预测指明了方向.
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| 关 键 词： | 锦丰（烂泥沟） 断块 差异运动 成矿构造 贵州贞丰锦丰（烂泥沟） |
A PRELIMINARY ANALYSIS OF GEOLOGICAL FEATURE AND PROSPECTING DIRECTION OF JINFENG （LANNIGOU） AU DEPOSIT |
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| WANG Xu-yang,WANG Fang-li,WANG Hong-yang.A PRELIMINARY ANALYSIS OF GEOLOGICAL FEATURE AND PROSPECTING DIRECTION OF JINFENG （LANNIGOU） AU DEPOSIT[J].Yunnan Geology,2014(1):130-132,137. |
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| Authors: | WANG Xu-yang WANG Fang-li WANG Hong-yang |
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| Institution: | ( College of Geosciences, Guilin University of Science and Technology, Guilin 541004) |
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| Abstract: | The orebody distribution of Jinfeng （Eannigou） Au deposit is controlled by Huangehanggou syn- elinore, the position of ore deposit is controlled by a series of faults in Huangehanggou synclinore, the specific ho- rizon of orebody is controlled by different rock assemblage. In the forming process of ore deposit, the fault F3 is not only the main ore channel structure but also the main ore-bearing structure in the orefield, the differential move- ment of different fault block causes the different deformation part of Huangchanggou syncline to outcrop on the same level, which shows the prognosis direction of ore deposit in the future. |
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| Keywords: | Fault Block Differential Movement Metallogenetic Structure Jingfeng （Lannigou） Guizhou |
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