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福鼎银硐铅锌矿区是一个赋存于石炭一二叠系地层中的层状矿床。它是福建省,也是南岭有色金属成矿带临近海域最东端的赋存于上部古生代地层中的层状矿床。研究它的成矿地质特征对于了解区域成矿规律、大地构造和古地理环境等都有一定意义。
Fuding silver lead-zinc deposit area is a layer of sedimentary deposits in the Permian stratigraphic bed deposits. It is a stratiform deposit hosted in the Upper Paleozoic strata in Fujian Province and also the easternmost part of the Nanling non-ferrous metallogenic belt adjacent to the sea. Studying its metallogenic geological features has some significance for understanding regional metallogenic regularity, tectonic setting and palaeogeographic environment.