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本文主要介绍浅层地震与静力触探联合探测黄土洞穴的基本原理及工作方法。说明其应用效果与黄土洞穴在地震波时间剖面中的反映特征。
This paper introduces the basic principles and working methods of shallow earthquakes and static exploration to detect loess caves. The effect of the application of the loess cave on the reflection characteristics of seismic wave time profile is illustrated.