摘要
对东坪金矿１号脉深部系统采样并进行红外光谱光密度测定，得出了金矿化的＂尖灭＂与＂再现＂部位的规律性认识。这种认识被深部钻探结果证实。这种规律性对于勘探工程有实际指导意义。
A systematic sampling of ore veinⅠat deep in Dongping Au deposit has been made and its infrared spectroscopic den-sity in measured out the regular picture of Au mineralization about thinning-out and recurrence parts.This recognition was confirmed by drilling results at deep depth.The regular pattern obtained has practical instructive singficance to prospectingengineering.
出处
《地质与勘探》
CAS
CSCD
北大核心
1996年第1期13-16,共4页
Geology and Exploration
关键词
金矿床
红外光谱
含金石英脉
光密度
地质勘探
Au-bearing quartz vein
spectroscopic density
thinning-out and recurrence
