摘要
郭城地区金矿床受郭城断裂派生的次级构造和元古界荆山群层间滑动破碎带控制明显,控矿层位在区域上较为稳定,显示出巨大的找矿潜力。
The secondary structure derived from the Guocheng fault of the gold deposit in Guocheng area and the sliding crushing zone between Proterozoic Jingshan Group are obviously controlled, and the ore-controlling layer is stable in the region, which shows great potential for prospecting.
作者
秦连元
QIN Lian-yuan(Shandong Yantai Xintai Gold Mining Co., Ltd.,Yantai 265147,China)
出处
《世界有色金属》
2019年第3期294-295,共2页
World Nonferrous Metals
关键词
郭城地区
金矿床
找矿潜力
Guocheng area
gold deposit
prospecting potential