| 莫测辉,刘丹英,冯志文,夏卫华.一种特殊的矿化分带──银山Cu－Au多金属矿床多级多中心矿化分带模式[J].地质与勘探,1996,(5): |
| 一种特殊的矿化分带──银山Cu－Au多金属矿床多级多中心矿化分带模式 |
| A SPECIAL KIND OF MINERALIZATION ZONING:MULTI-GRADE AND MULTICENTRE MINERALIZATION ZONING MODEL OF Cu-Au POLYMETALLIC ORE DEPOSIT IN YINSHAN |
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| DOI： |
| 中文关键词: 多金属矿床，矿化分带，成矿作用，班岩，江西银山 |
| 英文关键词: polymetallic ore deposit,mineralization zoning,mineralization, porphyry,Yinshan in Jangxi |
| 基金项目: |
| 莫测辉 刘丹英 冯志文 夏卫华 |
| 中国科学院广州地球化学研究所，中国地质大学 |
| 摘要点击次数: 2429 |
| 全文下载次数: 1439 |
| 中文摘要: |
| 根据银山Ｃｕ－Ａｕ多金属矿床是由构造动力热液和火山－岩浆热液双重耦合成矿作用而形成的新认识，建立了银山矿床新的矿化分带体系──二级多中心矿化分带模式，并探讨了其形成机制及找矿意义。 |
| 英文摘要: |
| According to the new recognition that Yinshan Cu-Au polymetallic deposit was formed by double-coupling mineralization between tectonic dynamic hydrothermal solution and volcanic-magmatic hydrothermal solution, the system of mineralization zoning of the deposit, sedond-order and multi-centre mineralization zoning model,was set up, and the mechanism and ore prospecting significance were approached. |
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