贺州南乡镇龙水脉石英矿成矿地质背景及成矿规律探讨  

Discussion on Metallogenic Geological Background and Metallogenic Regularity of Longshui in Nanxiang Town, Hezhou

作　　者：何光 谭志勤 黄惠及 He Guang;Tan Zhiqin;Huang Huiji(No.204 Geological Team of Guangxi Zhuang Autonomous Region,Hezhou Guangxi 542899,China)

机构地区：[1]广西壮族自治区二〇四地质队,广西贺州542899

出　　处：《山西冶金》2025年第2期118-120,123,共4页Shanxi Metallurgy

摘　　要：龙水脉石英矿床位于广西贺州市八步区,该区地质成矿条件优越。经过调查研究发现,该矿体规模较大,呈(脉)透镜体状,矿石质量优良。该矿床赋存于龙水断裂带,其成因受构造控制,属于中-低温热液充填型脉石英矿床。通过总结矿床特征、矿体特征和矿石质量,分析矿床的成因以及控制因素,旨在为该地区寻找同类型或类似的脉石英矿提供有价值的参考。The Longshui vein quartz deposit is located in the Babu District of Hezhou City,Guangxi,where the geological and metallogenic conditions are superior.Through investigation and research,it is found that the ore body is large in scale,in the shape of(vein)lens,and the ore quality is excellent.The deposit occurs in the Longshui fault,and its genesis is controlled by the structure.It belongs to the medium-low temperature hydrothermal filling vein quartz deposit.By summarizing the characteristics of the deposit,the characteristics of the ore body and the quality of the ore,the genesis and control factors of the deposit are analyzed in order to provide a valuable reference for finding the same type or similar vein quartz ore in this area.

关 键 词：脉石英矿 地质背景 成矿规律 龙水 贺州 

分 类 号：P57[天文地球—矿物学]