摘要
梁子寨铁矿矿石矿物主要为磁铁矿,呈似层状、条带状、致密块状产出,矿体与岩浆岩和构造关系紧密,主要赋存于平掌寨断裂旁的燕山期基性辉长岩中,属岩浆结晶分异型磁铁矿床。
The main ore mineral of Liangzishai Fe deposit is magnetite, which is stratoid, striped, densely massive. The ore body is related close to magmatic rock and structure, which is mainly in Yanshanian basic gabbro beside Pingzhangzhai fault, belonging to magnetite deposit of magmatic crystalline differentiation type.
出处
《云南地质》
2014年第2期234-236,共3页
Yunnan Geology
关键词
岩浆结晶分异型磁铁矿
基性辉长岩
平掌寨断裂
云南澜沧梁子寨
Magnetite Deposit of Magmatic Crystalline Differentiation Type
Basic Gabbro
Pingzhangzhai Fault
Liangzizhai, Lancang, Yunnan
