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

作　　者：周伟清 韦仁源 ZHOU Wei-qing;WEI Ren-yuan(Guangxi Zhuang Autonomous Region Geophysical Survey Institute,Liuzhou 545005,China)

机构地区：[1]广西壮族自治区地球物理勘察院,广西柳州545005

出　　处：《世界有色金属》2024年第19期61-63,共3页World Nonferrous Metals

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。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 

分 类 号：P618.4[天文地球—矿床学]