摘要
东川萝卜地铁矿区内主要铁矿体呈似层状、透镜状产出于中元古界大营盘组铁质板岩中。矿体产状与围岩产状一致,两者呈渐变过渡关系。矿床成因属于沉积变质型赤铁矿床。
The main Fe ore body of Luobudi Fe orefield in Dongchuan is is stratoid, lenticular in Middle Proterozoic Dayingpan Formation Fe slate. The occurrence of ore body is consistent with that of the wall rock. The relationship between them is transitional each other. It is a hematite deposit of sedimentary metamorphic type in genesis.
出处
《云南地质》
2016年第1期15-17,共3页
Yunnan Geology
关键词
矿床成因
沉积变质型矿床
东川萝卜地铁矿
Genesis of Ore Deposit
Deposit of Sedimentary Metamorphic Type
Luobudi Fe Deposit in Dongchuan
