摘要
王家庄铜钼矿床位于鲁西隆起北部边缘区域的邹平火山盆地中,区域成矿地质条件良好,具有较大的找矿潜力。研究表明,王家庄铜钼矿床与王家庄复式岩体具有成因联系,成岩成矿年龄基本一致;矿床发育钾化蚀变带、钾硅化蚀变带和强钾硅化蚀变带,并在垂向上延深较稳定,有利于深部找矿;128Ma左右的石英二长闪长岩和钾化蚀变带、钾硅化蚀变带和强钾硅化蚀变带是矿床的主要间接找矿标志,地表黄铜矿、辉钼矿露头是直接找矿标志。
The wang-jiazhuangcopper molybdenum deposit is located in the zouping volcano basin in the northern edge of Luxi,and the geological conditions of regional mineralization are good and have great prospecting potential.The research shows that wang-jiazhuangcopper molybdenum deposit has an causal relationship with Wang-jiazhuang duplex rock body,the age of rock formation is basically the same,the mineral deposit develops potassium erosion belt,potassium siliconization corrosion belt and strong potassium siliconization corrosion belt,and is stable in the upward extension,which is beneficial to Deep prospecting;128Ma or so of quartz two long flash long rock and potassium erosion zone,potassium silicone erosion belt and strong potassium silicone erosion belt are the main indirect prospecting signs of the deposit,the surface yellow copper ore,huiyu ore outcrops are direct finding signs.
作者
孟兆磊
MENG Zhao-lei(Xintai Natural Resources and Planning Bureau,Xintai 271200,China)
出处
《世界有色金属》
2020年第13期80-81,共2页
World Nonferrous Metals
关键词
铜钼矿床
地质特征
找矿标志
copper molybdenum deposit
geological features
prospecting signs
