摘要
矿体赋存于通安组第四段(Pt_1t^4)顶部灰色板岩层间裂隙中,矿床受地层、岩性、构造、蚀变多因素控制,其中地层、岩性的控制较为明显,属沉积型矿床。
The ore body is in Tongan fourth group（Pt1t4） at the top of the grey slate interlayer fissure, the deposit is controlled by multi factor variable control strata, lithology, structure, corrosion, which control the formation and lithology obviously belongs to sedimentary type deposit.
出处
《世界有色金属》
2017年第7期293-293,295,共2页
World Nonferrous Metals
