摘要
浅层地震是工程地质勘察中的一种重要手段,其特有的高分辨率特性有利于确定地层界面、基岩起伏变化的形态。针对不同的地质情况,采用相应的野外观测方法,经过资料的解释、处理得到较好的效果。本文主要介绍浅层地震反射波法在某过江通道勘察中的地质效果。
The seismic reflection wave method is one important method in the engineering geology reconnaissance, its unique high resolution characteristic is good to definite bed boundary and the change of basement relief. In view of the different geological situation,after the material explanation and processing ,we use the corresponding method to obtain the good effect. This paper mainly introduces the application of seismic reflection wave method in Exploration of The Channel of River
出处
《科技广场》
2008年第5期24-26,共3页
Science Mosaic
关键词
地震反射波
数据采集
过江通道
时间剖面
Seismic Reflected Wave
Data Acquisition
the Channel of River
Time Section