摘要
为了查明东源县矿山地质形态、矿产资源赋存规模、分布范围和变化规律,研究矿山发育层位、地段和程度,应用瞬变反磁通法对矿区进行相关的勘查工作。通过后期的钻孔异常验证,表明瞬变法在寻找矿床发育区,是行之有效的物探方法。
In order to find out the geological form of the mine,the occurrence scale,distribution range and change law of mineral resources in Dongyuan County,study the development horizon,section and degree of the mine,and apply the transient inverse magnetic flux method to carry out relevant exploration work in the mining area.Through the later verification of borehole anomalies,it shows that the transient method is an effective geophysical method in finding the deposit development area.
作者
陈宇
CHEN Yu(Guangdong Nonferrous Metals Geological Exploration Institution,Guangzhou 510080,China)
出处
《世界有色金属》
2022年第17期187-189,共3页
World Nonferrous Metals
关键词
瞬变反磁通
地球物理特征
断裂构造
transient inverse flux
Geophysical characteristics
Fault structure
