【摘要】 锁龙金矿从1998年发现之后,经过十余年规模不等的露采,实践证明矿体延伸稳定,矿床规模较大,矿化向深部有一定规模的延伸。东矿段深部矿化在不同方向的构造交汇部位较为富集,矿床成因为浅成中～低温热液作用下形成的微细粒浸染型金矿床。更多还原

【Abstract】 After the discovery of the Suolong Gold Mine in 1998, after more than ten years of open-pit mining, the practice has proved that the ore body extends steadily, the ore deposit is large, and the mineralization extends to a certain extent to the deep. The deep mineralization of the eastern ore section is enriched at the intersection of structures in different directions. The genesis of the deposit is a fine disseminated gold deposit formed under the action of epithermal medium-low temperature hydrothermal fluid.更多还原