| 崔彬,杨明银.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,(5):44-48 |
| 武山铜矿北矿带黄铁矿的成因矿物学研究 |
| RESEARCH GENETIC MINERALOGY OF PYRITE FOR NORTH ORE ZONG OF WUSHAN COPPER DEPOSIT |
| 修订日期：2001-10-10 |
| DOI： |
| 中文关键词: 铜矿床 黄铁矿 成因矿物学 沉积成因 热液成因 层控矿床 |
| 英文关键词: Wushan copper deposit, pyrite, genetic mineralogg, |
| 基金项目: |
| 崔彬 杨明银 |
| 中国地质大学地球与资源学院，北京100083 |
| 摘要点击次数: 2182 |
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| 中文摘要: |
| 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。 |
| 英文摘要: |
| 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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