| 连州小带碳酸铁锰矿床地质特征及成因探讨 |
| |
| 引用本文： | 谢小占.连州小带碳酸铁锰矿床地质特征及成因探讨[J].矿业工程,2016(2):3-5. |
| |
| 作者姓名： | 谢小占 |
| |
| 作者单位： | 广东省核工业地质局二九一大队,广东 广州,510800 |
| |
| 摘 要： | 总结了连州小带碳酸铁锰矿床的矿体特征、矿石矿物特征、矿石结构、构造和矿石类型、围岩蚀变等地质特征。地层和构造是矿床的主要控矿因素,矿床的成因存在两个矿化期,主要形成于锰铁碳酸盐矿化期。确定小带碳酸锰铁矿床成因类型应为层控型铅锌铁锰矿床。
|
| 关 键 词： | 铁锰矿床 地质特征 成因 |
Discussion on Geologic Characteristics and Genesis of Iron Carbonate Manganese Deposit in Xiaodai,Lianzhou |
| |
| Abstract: | Ore body and mineral characteristics,ore structure,tectonic and type as well as wallrock alteration of iron carbonate manganese deposit in Xiaodai area is summarized. Formation and tectonic are the main ore-controlling factors. The ore deposit goes through two mineralization stages,primarily formed in ferromanganese carbonate mineralization period. It’s confirmed that the deposit falls into the category of strata-bound type lead-zinc iron manganese deposit. |
| |
| Keywords: | iron manganese deposit geologic characteristics genesis |
| 本文献已被 CNKI 万方数据 等数据库收录！ |
|
