摘要
昆都铅锌矿集区位于林西—突泉铅锌银多金属成矿亚带的中部,近年来找矿成果十分突出,区内先后发现了一批典型的铅锌多金属矿床及重要矿化线索。系统总结了区域上和矿集区内的地质、地球物理、地球化学特征,并对矿集区内典型的铅锌矿床进行了对比,从赋矿层位、断裂构造等方面进行深入研究,提出了矿集区及外围的找矿思路,为进一步的找矿工作提供指导。
Kundu lead-zinc ore-concentrated area is located in the middle of Linxi-Tuquan Pb-Zn-Ag polymetallic metallogenic sub-belt.In recent years,prospecting breakthroughs have been made and a number of typical Pb-Zn polymetallic deposits and important mineralization clues are found in the area.The paper systematically summarized the geological,geophysical and geochemical characteristics in the region and the ore-concentrated area,compared typical Pb-Zn deposits in the ore-concentrated area,deeply studied the ore-hosting strata and fault structures,proposed prospecting ideas for the ore-concentrated area and its peripherals,and provided guidance for further prospecting work.
作者
李伟
吴桐
张渝金
张超
郭建刚
刘世峰
Li Wei;Wu Tong;Zhang Yujin;Zhang Chao;Guo Jiangang;Liu Shifeng(Shenyang Center of China Geology Survey;School of Mining Industry,Liaoning Technical University)
出处
《黄金》
CAS
2018年第12期23-26,共4页
Gold
基金
中国地质调查局地质调查项目(DD20160048-04)
关键词
昆都铅锌矿集区
铅锌银多金属成矿亚带
铅锌矿床
地质特征
地球物理特征
地球化学特征
Kundu lead-zinc ore-concentrated area
Pb-Zn-Ag polymetallic metallogenic sub-belt
Pb-Zn deposit
geological characteristics
geophysical characteristics
geochemical characteristics
