| 铜陵地区矽卡岩型铜矿的构造控制 |
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| 引用本文： | 吴明光.铜陵地区矽卡岩型铜矿的构造控制[J].华南地质与矿产,2003(1):46-48. |
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| 作者姓名： | 吴明光 |
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| 作者单位： | 安徽省淮北市窦庄矿,安徽,淮北,235000 |
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| 摘 要： | 铜陵地区矽卡岩型铜矿沿近EW向基底断裂构造－岩浆带分布，构成一条构造－岩浆－铜矿带，含矿岩体及矿田（床）常分布在盖层构造与基底断裂交汇部位。容矿构造可分为圈闭构造、热动（塑性）构造、岩体接触带、断裂与裂隙带及层间构造，几种构造并存的复合部位控制着矿体的定位及产状。
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| 关 键 词： | 矽卡岩型铜矿 构造控制 构造控制 铜陵地区 |
| 文章编号： | 1007-3701(2003)01-0046-03 |
| 修稿时间： | 2002年9月4日 |
Structural control to skarn-type copper deposits in Tongling area, Anhui Province |
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| WU Ming-guang.Structural control to skarn-type copper deposits in Tongling area, Anhui Province[J].Geology and Mineral Resources of South China,2003(1):46-48. |
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| Authors: | WU Ming-guang |
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| Abstract: | Skarn-type copper deposits in Tongling area distribute along a set of nearly EW-striking basement faults,constituting a tectonomagmatic copper-mineralized belt. The copper-mineralized plutons and copper deposits usually located in the convergence points of the basement faults with superficial faults. The host structures can be divided into trap-type,thermodynamic(ductile) type, contact zone-type and interlayer gliding faults or fissure zone, They jointly control the location and occurrence of the copper orebodies. |
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| Keywords: | skarn-type copper deposit structural controlling Tongling |
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