江西省德兴市水石坞金矿床地质特征及找矿方向  

Geological characteristics and prospecting directions of the Shuishiwu gold deposit in Dexing City,Jiangxi Province

作　　者：吴宏富 赵辉[2] 李冰[2] WU Hong-fu;ZHAO Hui;LI Bing(China National Gold Group Jiangxi Mining Co,Ltd,Shangrao 334000,China;China Gold Group Geological Co.,Ltd,Beijing 100000,China)

机构地区：[1]中国黄金集团江西金山矿业有限公司,江西上饶334000 [2]中国黄金集团地质有限公司,北京100000

出　　处：《世界有色金属》2024年第7期73-75,共3页World Nonferrous Metals

摘　　要：水石坞金矿定位于金山推覆剪切变形带中,为一中型隐伏盲矿床,是金山金矿向北倾向延深部分。成矿物质来源于赋矿地层,主要受金山—朱林韧性剪切带控制,矿石类型有超糜棱岩—糜棱岩型、千糜岩型和石英脉型三种。本文在前人勘查和研究工作的基础上论述了水石坞金矿床的地质特征、矿化富集规律及资源潜力,并指出了下一步找矿的方向。初步认为:水石坞金矿深边部还有较大找矿空间,通过进一步开展地质工作,不仅可能发现新矿体,也有可能发现新的矿化类型。The Shuishiwu gold deposit is located in the Jinshan nappe shear deformation zone.It is a medium-sized concealed blind deposit and is a northward trending extension of the Jinshan gold deposit.The ore-forming materials come from the ore bearing strata and are mainly controlled by the Jinshan Zhulin ductile shear zone.The ore types include ultramylonite-mylonite type,phyllonite type and quartz vein type.On the basis of previous exploration and research work,this article discusses the geological characteristics,mineralization enrichment patterns,and resource potential of the Shuishiwu gold deposit,and points out the next direction for ore exploration.It is preliminarily believed that there is still a large exploration space in the deep edge of the Shuishiwu gold deposit.Through further geological work,it is possible to discover not only new ore bodies but also new types of mineralization.

关 键 词：水石坞 金矿 地质特征 资源潜力 找矿方向 

分 类 号：P618.51[天文地球—矿床学]