| 福建清流赖坊铁多金属矿地质特征及找矿前景分析 |
| |
| 引用本文： | 林喜.福建清流赖坊铁多金属矿地质特征及找矿前景分析[J].福建地质,2014,33(4):278-285. |
| |
| 作者姓名： | 林喜 |
| |
| 作者单位： | 福建省地质调查研究院,福州,350013 |
| |
| 摘 要： | 清流赖坊铁多金属矿主矿体呈似层状贮存于早石炭世林地组上段至晚石炭世经畲组中,以中低温矿化蚀变为主,与近东西向断裂有一定内在的联系.根据矿床成矿地质背景和地质特征,认为该矿床属沉积-热液改造的层控型铁多金属矿.目前工程控制为氧化带褐铁矿石,深部有望探寻铁多金属原生矿.
|
| 关 键 词： | 铁多金属矿 地质特征 找矿前景 清流赖坊 |
Geological Characteristics and the Ore-finding Perspective of Laifang Iron Polymetallic Deposit in Qingliu County,Fujian Province |
| |
| Lin Xi.Geological Characteristics and the Ore-finding Perspective of Laifang Iron Polymetallic Deposit in Qingliu County,Fujian Province[J].Geology of Fujian,2014,33(4):278-285. |
| |
| Authors: | Lin Xi |
| |
| Institution: | Lin Xi (Fujian Institute of Geology Survey and Research, Fuzhou, 350013) |
| |
| Abstract: | The main ore body of iron polymetallic mine is like a layer ed ore bodies occurred in upper of early carboniferous Lindi to late carboniferous Jinse in Laifang town, Qingliu county, mainly forming from the mineralized alteration in medium and low temperature and having a certain inner link to nearly east-west fracture. According to the metallogenic geological back- ground and geological characteristics, it is believed that the deposit belongs to the stratabound sedimentary-hydrothermal transformation type. At present, oxidation zone limonite stone by engineering controlling, which is expected to explore polymetallic native iron ore in deep. |
| |
| Keywords: | iron polymetallic deposit geological characterisitcs ore-finding perspec- tive Laifang in Qingliu county |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
|
