| 武山铜矿北矿带黄铁矿的成因矿物学研究 |
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| 引用本文： | 崔彬,杨明银,等.武山铜矿北矿带黄铁矿的成因矿物学研究[J].地质与勘探,2002,38(5):44-48. |
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| 作者姓名： | 崔彬 杨明银 |
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| 作者单位： | 中国地质大学地球与资源学院,北京,100083 |
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| 摘 要： | 武山铜矿是长江中下游铁、金成矿带一个重要组成部分，通过对武山铜矿北矿带的成因矿物学研究，可将其划分为沉积成因系列与热液成因系列两大类，从而进一步证明武山铜矿北矿带为在正常沉积基础上，由燕山期岩浆热液叠加改造的层控矿床。
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| 关 键 词： | 铜矿床 黄铁矿 成因矿物学 沉积成因 热液成因 层控矿床 |
| 文章编号： | 0495-5331(002)5-0044-05 |
| 修稿时间： | 2001年10月10 |
RESEARCH GENETIC MINERALOGY OF PYRITE FOR NORTH ORE ZONG OF WUSHAN COPPER DEPOSIT |
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| CUI Bin,YANG Ming-yin,ZHAN Zhao-Yang.RESEARCH GENETIC MINERALOGY OF PYRITE FOR NORTH ORE ZONG OF WUSHAN COPPER DEPOSIT[J].Geology and Prospecting,2002,38(5):44-48. |
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| Authors: | CUI Bin YANG Ming-yin ZHAN Zhao-Yang |
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| Abstract: | Wushan copper deposit is an important part of .Fe. Cu and Au metallogenetic belt in the middle and lower reaches of the Yangtze River. Through research genetic mineralogy of pyrite for North ore zone of Wushan copper deposit, its pyrites might be divided into the sedimentary series and the hydrothermal series. It is a stratabound deposit which formed on the basis of ordinary sedimentary formation and was superimposed and changed by Yanshan ore-bearing magma hydrothermal solution. |
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| Keywords: | Wushan copper deposit pyrite genetic mineralogg |
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