| 云南马龙马鞍山铁矿成矿地质条件 |
| |
| 引用本文： | 陈伟. 云南马龙马鞍山铁矿成矿地质条件[J]. 云南地质, 2011, 30(3): 326-328 |
| |
| 作者姓名： | 陈伟 |
| |
| 作者单位： | 云南省有色地质局317队,云南曲靖,655000 |
| |
| 摘 要： | 铁矿床由基底岩石中黄铁矿、菱铁矿在近地表经风化淋滤后,搬运沉积形成。属风化残积型褐铁矿。
|
| 关 键 词： | 褐铁矿 风化残积型 黄铁矿和菱铁矿 第四纪地层 云南马龙马鞍山 |
THE METALLOGENETIC GEOLOGICAL CONDITIONS OF MAANSHAN FE DEPOSIT IN MALONG, YUNNAN |
| |
| CHEN Wei. THE METALLOGENETIC GEOLOGICAL CONDITIONS OF MAANSHAN FE DEPOSIT IN MALONG, YUNNAN[J]. Yunnan Geology, 2011, 30(3): 326-328 |
| |
| Authors: | CHEN Wei |
| |
| Affiliation: | CHEN Wei(Geological Team 317,Yunnan Bureau of Nonferrous Geology,Qujing 655000) |
| |
| Abstract: | The Fe deposit is formed by the pyrite and siderite in the basement rock because of the transporta- tion and sedimentation after the surface weathering and leaching processes. It is a limonite deposit of weathering sedentary type. |
| |
| Keywords: | Limonite Weathering Sedentary Type Pyrite ＆ Siderite Quarternary Maanshan,Malong,Yunnan |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
