shallow seismic refraction methods 浅层地震折射波法
The shallow seismic refraction method is one of the main methods of exploration for engineering, hydrogeological and environmental geology.
浅层地震折射波法是在工程地质、水文地质及环境地质勘查中广泛应用的地震探测方法之一。
The shallow seismic refraction method is one of the main exploration methods of engineering, hydrogeological and environmental geology.
浅层地震折射波法是在工程地质、水文地质及环境地质勘查中广泛应用的地震探测方法之一。
This paper discusses the application range of interpretation methods of traditional seismic refraction data according to need of actual work and points out problems of the methods.
根据实际工作需要对传统的地震折射资料解释方法的适用范围进行了讨论，指出了传统折射资料解释方法所存在的问题。
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