摘要
吉林金银别地区位于华北地台北缘东段,夹皮沟金矿带的南东延长部分,清茶馆—白水滩断裂构造带与北东向溜河构造带交汇处。区内金矿床、金矿点多分布于太古宙、古生宙表壳岩中,矿体分布主要受NE、NW向断裂构造控制。文章通过对金矿地质特征和控矿因素的总结分析,指出找矿方向。
Jilin Jinyinbie area is located in the eastern part of north margin of North China Platform, southeast extension of Jiapigou gold ore belt, the junction of Qingchaguan-Baishuitan fault structure belt and northeast Liuhe structure belt. The gold deposits, gold occurrences are distributed in supracrustal rocks of the Archean, Paleozoic, ore body distribution is mainly controlled by NE, NW faults. Based on the analysis of geological features and ore controlling factors, the authors point out the prospecting direction.
出处
《吉林地质》
2014年第2期31-35,共5页
Jilin Geology
关键词
地质特征
找矿方向
金银别地区
geological features
prospecting direction
Jinyinbie area