摘要
刘屯金矿床由刘屯( Ⅰ) 和金屯( Ⅱ)两个地段组成。作者通过矿床地质特征、深部地球物理特征、金矿体地球化学异常模式判别及矿体剥蚀程度预测等研究,对刘屯金矿床深部成矿提出了新看法,认为Ⅰ地段矿体已剥蚀到中下部,40 m 以下矿化尖灭;Ⅱ地段矿体剥蚀至头部,向下有较大延深,可进一步开展深部找矿。
The Liutun gold deposit is composed of section Ⅰ,Liutun and section Ⅱ,Jintun.Based on the research on geologic characteristics,deep geophysical characteristics,model recongnition of geochemical anomalies of gold ore bodies,as well as the erosion level of gold ore bodies,the author proposes that the ore body at section Ⅰ has been eroded to the middle lower part,and the ore body pinches out at depth of 40m,but only the upper part of ore body at section Ⅱ was eroded,and ore body may have greater extension to the depth,and deep prospecting must be performed.
出处
《铀矿地质》
CAS
CSCD
2000年第1期37-41,共5页
Uranium Geology
关键词
金矿床
深部找矿
金
地球化学
异常模式
Gold deposit Liutun,Deep prospecting,Model of gold geochemical anomaly