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浙江省遂昌县治岭头矿区在中矿段金银矿勘探过程中发现Ⅰ号铅锌矿体,1997—2007年完成矿床详查工作。矿体产于燕山晚期火山通道隐爆形成的岩石中,赋存岩石为隐爆岩、爆裂角砾岩和爆破角砾岩,矿体呈筒状,平面上矿体呈不规则状,长度29·5～130m,厚度11～58m,矿体垂向延伸大于481m,平均品位Pb+Zn6·07%,伴生Ag、S、In、Cd等有用组分,属火山期后中低温隐爆岩型矿床,类型独特,对今后找矿有一定示范指导意义。
The Zhilingtou Mining Area, Suichang County, Zhejiang Province, discovered the lead-zinc ore body of No. 1 during the exploration of the gold-silver deposits in the mid-ore section and completed the detailed investigation of the deposits during 1997-2007. The ore body is produced in the rocks formed by the implosion of late Yanshan volcanic channel. The rocks are cryptoexplosive rocks, brecciated breccias and brecciated breccias. The ore bodies are in a cylindrical shape with an irregular ore body in the plane and a length of 29 · 5 ~ 130m in thickness and 11 ~ 58m in thickness. The vertical extension of the orebody is more than 481m with the average grade of Pb + Zn6 · 07%, associated with useful components such as Ag, S, In and Cd. Mineral deposits, the type of unique prospecting for the future demonstration of some guidance.