摘要
通过对长城岭铅锌银多金属矿田成矿地质背景及特征的分析研究,总结出赋矿地层为D2q,是一套低能、富含藻类化石和泥质、有机质以及陆源碎屑的碳酸盐岩。具层控型Pb、Zn、Ag多金属矿床特征。
Through the analyzing and studying on geological ver, lead and zinc polymetallic ore field in Changchengling background of mineralization and characteristic of silarea, we come to a conclusion that the host strata is D2q, which is a set of low -energy carbonate rocks containing algac fossil richly, shales, the organic material and terrestrial clastic rock, as well as possesses the polymetallic deposit characterestic of Pb, Zn, Ag stratabound.
出处
《有色矿冶》
2009年第4期8-10,14,共4页
Non-Ferrous Mining and Metallurgy
关键词
铅锌银多金属矿田
成矿地质背景
特征
silver, lead and zinc polymetallic ore field
geological background of mineralization
characteristic
