摘要
对高密度电阻率法和浅层地震法两种地球物理分支方法应用于采空区勘探的地质效果进行了较为系统地介绍,对同一测线上两种方法的解释成果作了分析。通过试验并经过钻探验证,得出以高密度电祖率法双边三极观测系统为主,浅层地震映像法相辅的勘探思路;说明由于地下情况的复杂性,运用不同的物探方法可以达到相互验证、相互补充的作用。
This paper gives a systematic description of the geological effects of applying the high-density resistivity method and shallow seismic method to the exploration of exhausted areas,and makes an analysis of the interpretation results of these two methods along the same survey line.Test and drilling verification show that the bilateral triode observation system of the high-density resistivity method should be mainly employed with the aid of the shallow seismic image method.As the underground situation is very complex,the application of different geophysical methods can attain the aim of mutual verification and mutual supplement.
出处
《物探与化探》
CAS
CSCD
北大核心
2010年第6期732-736,共5页
Geophysical and Geochemical Exploration
关键词
高密度电祖率法
浅层地震映像法
采空区
双边三极观测系统
high-density resistivity method； shallow seismic image method； exhausted area； bilateral triode observation system
