山东栖霞台前—陡崖断裂带构造特征及找矿方向浅谈  

Structural characteristics and prospecting direction of Taiqian steep cliff fault zone in Qixia,Shandong Province

作　　者：钮涛 NIU Tao(The Sixth Geological and Mineral Exploration Institute of Shandong Province,Weihai 264209,China)

机构地区：[1]山东省第六地质矿产勘查院,山东威海264209

出　　处：《世界有色金属》2022年第5期55-57,共3页World Nonferrous Metals

摘　　要：台前-陡崖断裂带为胶西北地区4条S形断裂之一,是西林-陡崖S形断裂的一部分,控制着西陡崖-笏山金矿床、台前金矿床等多处金矿床的产出,已探明金金属量超过20t。通过分析该断裂带地质特征及所赋存的金矿床矿体特征,认为西陡崖-笏山金矿床东南侧一带深部具有较大的找矿空间。Taiqian-Douya fault zone is one of the four"S"-shaped faults in the northwestern Jiaodong area.It is a part of Xilin-Douya"S"-shaped fault zone and controls the occurrence of Xidouya-Hushan gold deposit,Taiqian gold deposit and many other gold deposits,more than 20 tons of metals have been found.Based on the analysis of the geological characteristics of the fault zone and the characteristics of the gold ore bodies,it is considered that there is a large prospecting space in the deep part of the area on the southeast side of the Xidouya-Hushan gold deposit.

关 键 词：台前-陡崖断裂带 西陡崖-笏山金矿床 台前金矿床 

分 类 号：P618.51[天文地球—矿床学]