摘要
对贵岭矿区铅锌矿矿床地质特征进行总结,通过分析成矿温度、成矿流体、成矿物质来源和成矿时代,总结矿床成因,认为矿床成因为中低温火山热液交代充填型。
This paper summarizes the geological characteristics of the Pb-Zn deposit in Guiling mining area,summarizes the genesis of the deposit by analyzing the metallogenic temperature,ore-forming fluid,source of ore-forming material and metallogenic age,and considers that the deposit is formed by medium low temperature volcanic hydrothermal metasomatic filling type.
作者
杨仲可
于春
杨锦洁
YANG Zhong-ke;YU Chun;YANG Jin-jie(The 11th Geologic Teamof Zhejiang Province,Wenzhou 325006,China)
出处
《世界有色金属》
2021年第4期85-86,共2页
World Nonferrous Metals
关键词
铅锌矿
地质特征
成因探讨
Pb-Zn deposit
geological characteristics
deposit genesis