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1·Simulate a complete seismic refraction survey.

模拟一次完整的地震的折射。

2·The layered characteristic is the foundation to use the seismic refraction method investigating.

它的层状特性是开展地震折射层析方法的地球物理基础。

3·This paper describes the application of shallow seismic refraction wave method to the exploration of foundation for railway Bridges.

介绍了浅层地震折射波法在铁路桥基础勘查中的应用。

4·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。

5·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。

6·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。

7·The surface wave is treated as interference wave in oil seismic prospecting, however, the Rayleigh wave, like the refraction and reflection waves, contains the information of underground medium.

在石油地震勘探中，面波一般是作为干扰波处理的，然而，瑞利面波也和折射波、反射波一样包含有地下介质的信息。

8·In this paper, the method and principle of the shallow refraction seismic tomography for the ray theory is briefly expounded and applied samples are provided.

本文由射线理论出发，简要地阐述了浅层折射地震层析成像方法的原理，并给出了应用实例。

9·The shallow refraction seismic survey is a good method in shallow engineering geology sur - vey.

浅层工程地震折射波法是进行浅层工程地质勘察十分有效的方法。

10·The refraction static corrections using refraction first-break time in seismic data becomes a main method in current seismic data processing.

利用地震资料得到的表层折射初至进行静校正是目前生产中的主要静校正方法。