广西象州县大蚕铅锌矿地质特征及矿床成因探讨
Discussion on geological characteristics and origin of big silkworm lead-zinc deposit in Xiangzhou County,Guangxi
周伟清 1韦仁源1
作者信息
- 1. 广西壮族自治区地球物理勘察院,广西 柳州 545005
- 折叠
摘要
广西象州县大蚕铅锌矿位于华南板块南华活动带的来宾凹陷带与大瑶山隆起的交接部位,属大瑶山西侧铜铅锌多金属矿成矿带的北段,该区构造运动复杂、区域地质成矿条件良好.本文通过对广西象州县大蚕铅锌矿床的成矿特点、地质条件进行总结研究,为区域上找同类型矿床提供参考.
Abstract
Dami lead-zinc mine in Xiangzhou County,Guangxi is located at the junction between the Laibin depression belt and the uplift of Dayao Mountain in the Nanhua activity belt of south China plate.It belongs to the northern section of the copper,copper-lead-zinc polymetallic metallogenic belt on the west side of Dayao Mountain.The tectonic movement in this area is complex and the regional geological metallogenic conditions are good.This paper summarizes the minerenic characteristics and geological conditions of silkworm lead-zinc deposit in Xiangzhou County,Guangxi,to provide reference for finding the same deposit in the region.
关键词
广西象州县大蚕铅锌矿/地质特征/矿床成因Key words
big silkworm lead-zinc mine in Xiangzhou County,Guangxi/geological features/deposit origin引用本文复制引用
出版年
2024
国家科技期刊平台
NSTL
万方数据