Simulate a complete seismic refraction survey.
模拟一次完整的地震的折射。
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。
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。
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。
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。
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。
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。
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。
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。
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。
A refraction seismic tomographic method is proposed for the first time to determine the distribution of seismic velocity in shallow levels in Talimu Basin.
首次提出了用于解决塔里木盆地地震资料数据处理中浅部地震速度分析的折射层析成象方法。
An appearance of seismic data as a diffraction, reflection, refraction or other similar feature produced by an arrival of seismic energy.
在地震剖面上，由地震能量产生的绕射、反射、折射或其他相似特征的地震数据轨迹。
The shallow refraction seismic is widely used in engineering geology exploration, because this method may ascertain the velocity of the refraction surface.
地震折射波法以其能够确定折射界面的速度而广泛用于工程地质勘察。
The used seismic data are prestack data:therefore, this method considers the energies of direct wave, refraction wave and multiple wave.
因所用资料是叠前资料，所以该方法考虑了直达波、折射波和多次波能量。
The seismic reflection method can provide more detailed and more information about underground geological structure than refraction method.
对于地下复杂的地质构造，地震反射波法比折射波法能够提供更多更详细的地下信息。
Application of the method in seismic data acquisition in refraction-developed zone has been seen a good results.
应用此方法在折射发育区的地震数据采集中见到了良好效果。
According to the data of surface seismic exploration and database theory, the authors put forward a method of database for refraction static correction and develop the DBRSC static correction system.
基于模型法静校正原理和数据库方法，提出了数据库静校正，并开发了DBRSC数据库静校正系统。
According to the data of surface seismic exploration and database theory, the authors put forward a method of database for refraction static correction and develop the DBRSC static correction system.
基于模型法静校正原理和数据库方法，提出了数据库静校正，并开发了DBRSC数据库静校正系统。
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