| 云南镇沅下岔河金矿成矿地质特征及成因 |
| |
| 引用本文： | 罗书斌.云南镇沅下岔河金矿成矿地质特征及成因[J].云南地质,2011,30(4):428-430. |
| |
| 作者姓名： | 罗书斌 |
| |
| 作者单位： | 中国有色金属工业昆明勘察设计研究院,云南昆明,650051 |
| |
| 摘 要： | 镇沅下岔河金矿床位于哀牢山金矿带,矿体赋存于石英脉中,金矿化与硅化、黄铁矿化、褐铁矿化、毒砂化等围岩蚀关系密切,为喜马拉雅期的中低温热液矿床。
|
| 关 键 词： | 石英脉型金矿 包裹金为主 黄铁矿-毒砂矿 裂隙空矿 云南镇沅下岔河 |
THE GEOLOGICAL CHARACTERISTICS AND GENESIS OF XIACHAHE AU DEPOSIT IN ZHENYUAN,YUNNAN |
| |
| LUO Shu-bin.THE GEOLOGICAL CHARACTERISTICS AND GENESIS OF XIACHAHE AU DEPOSIT IN ZHENYUAN,YUNNAN[J].Yunnan Geology,2011,30(4):428-430. |
| |
| Authors: | LUO Shu-bin |
| |
| Institution: | LUO Shu-bin (Kunming Institute of Exploration and Design,China Nonferrous Industry,Kunming 650051) |
| |
| Abstract: | The Xiachahe Au deposit of Zhenyuan is in the Ailaoshan Au metallogenesis zone.And the Au ore body is in the quartz vein,which is close related with the alteration of wall rock,such as silisification,pyritization,limonitization,arsenopyritization,etc.It is a Himalayan middle-low T hydrothermal ore deposit. |
| |
| Keywords: | Au Deposit of Quartz Vein Type Major Included Au Pyrite-Arsenopyritization Ore-Bearing Fissure Xiachahe Zhenyuan Yunnan |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
