摘要
脉状矿体赋存于高黎贡山群下亚群第三层(Ptgl31),品位取决于大理岩、片麻岩破碎程度,典型的中低温热液裂隙充填型铅矿。
The veined ore body is in Gaoligongshan Group Lower Subgroup the 3rd bed （ Ptgf13 ）. The grade is determined by the fracture degree of the marble and the gneiss. It is a typical middle - low T hydrothermal Pb de- posit of fissure filling type.
出处
《云南地质》
2013年第4期417-420,共4页
Yunnan Geology
