广东信宜长坑铜多金属矿矿床地质特征及找矿方向  

Geological characteristics and prospecting orientation of Changkeng Cu polymetallic deposit,Xinyi,Guangdong Province

作　　者：杨胜虎 

机构地区：[1]广东省有色地质勘查院,广东广州510080

出　　处：《世界有色金属》2017年第5期16-17,共2页World Nonferrous Metals

摘　　要：长坑铜多金属矿区位于吴川-四会深大断裂带中段之北侧,本文通过综合分析矿区区域地质背景和矿床地质、化探异常特征,结合目前已有地质成果,提出下一步工作的找矿方向。Changkeng Cu polymetaUic deposit located in the north of the intermediate Wuchuan-Sihui fault zone. This study has proposed a further prospecting orientation based on the combination of geological background, geochemical anomaly and previous geological findings.

关 键 词：长坑铜多金属矿 矿床地质特征 中低温热液充填交代型 吴川-四会断裂带 

分 类 号：P618.2[天文地球—矿床学]