摘要
马头崖铜金矿位于沂沭断裂带西侧,受近南北向彭家岚子断裂控制。金矿体赋存于彭家岚子断裂及其次级断裂带内,已圈定铜金矿化带2个,并在其延伸部位发现了小型铜金矿化体。通过分析研究,认为马头崖地区金矿化主要受断裂构造控制,区内具有良好的找矿前景。
Matouya copper gold deposit is located in the west of Yishu Fault Zone and controlled by nearly NS trending pengjialanzi fault.The gold ore bodies occur in pengjialanzi fault and its secondary fault zone.Two copper gold mineralization zones have been delineated,and small copper gold mineralization bodies have been found in its extension.Through the analysis and study,it is considered that the gold mineralization in matouya area is mainly controlled by the fault structure,and the area has a good prospecting prospect.
作者
黄坤朋
陆林祥
李鹏飞
HUANG Kun-peng;LU Lin-xiang;LI Peng-fei(Shandong Lunan Geological Engineering Survey Institute(the second Geological Brigade of Shandong Geological Exploration Bureau),Jining 272100,China)
出处
《世界有色金属》
2020年第23期61-62,共2页
World Nonferrous Metals
关键词
找矿方向
地质特征
铜金矿
马头崖
prospecting direction
geological characteristics
copper gold deposit
matouya