摘要
阐述了茂祖铅-锌矿床的成矿地质背景、矿床地质特征,着重研究了赋矿地层、铅-锌矿体赋存及矿化特征,并通过该矿床的成矿时代、成矿物质来源、成矿温度方面的研究,综合分析后认为,茂祖铅-锌矿床的成因属同生断裂控矿的热水喷流-沉积改造型。
Geological background for metallogeny and characteristics of ore deposit of Maozu lead and zinc deposit was expatiated with a focus on ore bearing strata, occurrence of lead and zinc orebodies and characteristics of the mineralization. It is considered that the MaoZu Pb-Zn deposit belongs to syngenetic fault controlled hydrothermal exhalation-sediment transformation deposit according to the study on metallogenic era and matter source ,metaUogenic temperature of the deposit.
出处
《矿产与地质》
2006年第4期397-402,共6页
Mineral Resources and Geology
