摘要
矿床赋存于断裂构造中,受构造控制,具有明显的后期改造和次生富集现象,属中低温热液脉状充填型矿床,经后期改造和次生氧化富集作用形成。
The ore deposit is in the fault, which is controlled by the fault and with the evident posterior reformation and secondary concentration characteristics. It belongs to the hematite deposit of middle - low T hydrothermal veined filling type and it is formed by the later reformation, secondary oxidation and concentration.
出处
《云南地质》
2013年第2期174-176,共3页
Yunnan Geology
关键词
充填型赤铁矿
中低温热液脉状
后期改造
次生氧化富集
云南玉溪市洛河
Hematite Deposit of Filling Type
Middle-Low T Hydrothermal Filling
Posterior Reformation
Secondary Oxidation-Concentration
Luohe
Yuxi
Yunnan
