摘要
对产于新第三系底部的黄松甸子砾岩型金矿的矿区地质、含金砾岩、矿床特征、金的赋存状态和富集规律进行了叙述。指出砾岩型金矿的形成受构造运动、矿质来源和古地理环境控制，并提出今后找矿方向。
The paper sets forth mineral geology,goldbearing conglomerarte,features of deposit,existing characteristics of gold and law of enrichment of conglomeratetype gold deposit in Huangshong dianzi,which occurs in the bottom of Neogene.The author points out the forming of the deposit is controlled by structural moveirent,source of mineral and paleogeographic environment,and gives the direction of the future exploring.
出处
《黄金地质》
1995年第1期34-41,共8页
Gold Geology
关键词
砾岩型
金矿床
地质特征
找矿方向
Jiling,conglomeratetype gold deposit,geological feature,direction of exploring
