摘要
顺昌仁寿铅锌银矿贮存于早元古代麻源群南山组变质岩中,受北东向断裂构造控制,呈脉状、透镜状产出,属中-低温热液充填交代型矿床。
The Renshou lead-zinc-silver deposit in Shunchang County exists in the metamorphic rocks of Early Proterozoic Nanshan Formation and is controlled by the NE-trending faulted structures.The orebody acts like a veiny and lenticular occurrence.It belongs to the mineral deposit of the intermediate and low temperature hydrothermal filling and metasomatic type.
出处
《福建地质》
2010年第3期183-188,共6页
Geology of Fujian
关键词
铅锌银矿
地质特征
找矿方向
顺昌仁寿
lead-zinc-silver ores
geological characteristics
ore-finding orientations
Shunchang County
