摘要
辽宁凤城白云金矿床赋存于下元古界辽河群盖县组与大石桥组接触部的东西向白云推覆构造带中,矿床类型为含金硅钾蚀变岩型。文章通过对白云金矿床的地质特征、矿石特征等的系统研究,总结了找矿标志,进而指出了找矿方向。
Baiyun gold deposit occurred in the EW Baiyun tectonic belt of the contact zone of lower Proterozoic Liaohe cluster Gaixian formation and Dashiqiao formation. The deposit is of auriferous silicon kalium altered rock type deposit. A systematic research on geologic characteristics and ore features was carried out. As a result, the ore prospecting indicators were summarized and the prospecting orientation was pointed out.
出处
《黄金》
CAS
北大核心
2007年第11期16-20,共5页
Gold
关键词
地质特征
找矿方向
白云金矿床
geologic characteristics
ore prospecting orientation
Baiyun gold deposit
