摘要
双过山地区地处处于上杭-云霄成矿亚带与福鼎-云霄成矿亚带结合部位,具备多金属矿产成矿地质条件,是闽南重要找矿地段。铅锌矿床矿体主要赋存于晚侏罗世南园组火山岩地层中,明显受断裂构造控制,属中低温热液型矿床。
Shuangguo Mountain area is located in the combination of Shanghang-Yunxiao metallogenic subbelt and Fuding-Yunxiao metallogenic subbelt.It has the metallogenic geological conditions of polymetallic minerals and is an important ore prospecting area in southern Fujian.The ore bodies of Pb-Zn deposit mainly occur in volcanic rock strata of Nanyuan Formation in Late Jurassic,and are obviously controlled by fault structure.
作者
严健
YAN Jian(The Eighth Geological Brigade of Fujian Province,Longyan,364000,China)
出处
《世界有色金属》
2023年第5期223-225,共3页
World Nonferrous Metals
关键词
双过山
铅锌矿床
地质特征
物化探特征
成因
Shuangguo Mountain
Lead-zinc deposit
Geological characteristics
Geophysical and geochemical characteristics
cause
作者简介
严健,男,生于1988年,汉族,福建龙岩人,本科,地质矿产工程师,研究方向:地质找矿。
