摘要
根据成矿地质背景和矿床组合特征 ,认为湘南西部内生金属矿床的形成受一定沉积建造、地质构造和岩浆岩的控制 ,可划分三个成矿系列 ,即与I型花岗岩类有关的铅锌铜银成矿系列、与S型花岗岩类有关的钨锡铅锌铜银成矿系列和沉积改造型铁锰铅锌成矿系列 ,根据上述特征分析了找矿远景。
Based on analyses of metallogenic background and characteristics of endogenic deposit assemblage, it is concluded that formation of endogenic ore deposits is controlled by sedimentary formation, structural and magmatic activities. Endogenic ore deposits in this area can be divided into three metallogenic series,namely Pb Zn Cu Ag metallogenic series related to I type granitoid, W Sn Pb Zn Au Ag metallogenic series related to S type granitoid and Fe Mn Pb Zn metallogenic series related to sedimentary remobilization. A prospecting prognosis is also made on the basis of geological features.
出处
《华南地质与矿产》
CAS
2002年第1期62-66,共5页
Geology and Mineral Resources of South China