广东省佐坑幅矿产地质特征及成矿规律的分析  

Analysis of geological characteristics and metallogenic regularity of Zuokeng area in Guangdong Province

作　　者：赵新胤 汤琳 廖静 易其森 李表鹏 ZHAO Xin-yin;TANG Lin;LIAO Jing;YI Qi-sen;LI Biao-peng(No.931 Geological Team,Geology Bureau for Nonferrous Metals of Guangdong Province,Shantou 515000,China)

机构地区：[1]广东省有色金属地质局九三一队,广东汕头515000

出　　处：《世界有色金属》2024年第18期79-81,共3页World Nonferrous Metals

摘　　要：广东省佐坑幅区域上位于紫金-博罗大断裂与莲花山断裂带(西带)的夹持区域,属于华南成矿省永安-梅州-惠州成矿带(Ⅲ-82)之Ⅴ-13松坑Fe-W-Sn-Cu-Pb-Zn矿集区核心区域。通过佐坑幅1:5万矿产地质调查工作,大致查明成矿地质条件,了解矿产资源分布概况,概略检查矿床矿体特征,合理分析化探异常特点,梳理区域地质条件与成矿的关系,总结区域成矿规律,为后续矿产勘查工作提供依据。Guangdong province Zuokeng area belongs to the core area of V-13 Songkeng Fe-W-Sn-Cu-Pb-Zn ore cluster of Yongan-Meizhou-Huizhou metallogenic belt(III-82).Through the 1:50000 mineral geological survey of Zuokeng area,the metallogenic geological conditions were roughly found out,the distribution of mineral resources was understood,the orebody characteristics of the deposit were roughly examined,the characteristics of geochemical exploration abnormalities were reasonably analyzed,the relationship between regional geological conditions and metallogenic were sorted out,and the regional metallogenic laws were summarized,which provided a basis for the subsequent mineral exploration.

关 键 词：佐坑幅 矿产特征 成矿地质条件 成矿规律 

分 类 号：P612[天文地球—矿床学]