摘要
简要介绍地质雷达技术原理 ,利用大庆探区巴彦查干地区地质雷达实测资料进行解释 ,并结合微测井资料进行该地区地震波表层层速度的计算和静校正量的提取 .结果表明 ,地质雷达能获得连续的浅地下剖面 ,可弥补微测井资料的不足 ,因而在地震勘探表层地质调查和静校正量提取等方法方面上有实际应用价值 .
Ground penetrating radar field data was ured in Daqing prospect area Bayanchagan region to illustrate ground penetrating radar basic method about data and interpretation, which is based on ground penetrating radar theory. This the paper calculates seismic wave surface layer speed and extracts static correction. Data indicate that ground penetrating radar can get continuous shallow underground lateral section, and makes good the shortage of microlog data. Therefore ground penetrating radar takes on practical applied cost on seismic exploration surface layer geologic survey and static correction extraction etc.
出处
《地球物理学进展》
CSCD
2002年第4期745-752,共8页
Progress in Geophysics
基金
国家自然科学基金项目 (4 9974 0 31)资助
关键词
地质雷达
地震勘探
微测井
表层地质调查
静校正量
Ground penetrating radar
Seismic exploration
Microlog
Surface layer geologic survey
