摘要
庙岭金矿赋存于熊耳群焦园组火山熔岩—流纹岩及流纹质火山碎屑岩中 ,金矿化严格受断裂构造控制。本文通过对庙岭金矿床地质特征的研究 ,系统地讨论了该矿床的控矿因素 ,指出该区F2 2 、F16 1、F16 断裂带具有良好的找矿前景。
Miaoling Gold Deposit occurs in volcanic lava rhyolith and rhyolith structural volcaniclastic rock of Jiaoyuan Series,Xiong'er Group.The gold mineralization is controlled strictly by fracture structure.Through the study of its geologic characteristics,the ore controlling factors of the deposit are systematically discussed.That the fracturd belts F 22 ,F 161 ,F 16 have better prospects of ore finding is pointed out.
出处
《黄金》
CAS
2003年第4期19-21,共3页
Gold
关键词
金矿床
庙岭金矿
地质特征
找矿方向
Miaoling Gold Deposit
geological characteristic
ore finding orientation
