1·The propagation depth of Rayleigh waves was about 2.0 times of wavelengths.
瑞利波随深度衰减快，其传播深度约为波长的2.0倍。
2·The conventional interpretation theory has been based on propagation of free-surface Rayleigh waves.
传统的解释理论以自由表面瑞利面波的传播为基础。
3·There are two basic methods of Rayleigh wave exploration: transient Rayleigh waves and standing Rayleigh waves.
瑞雷波勘探的方法主要有两种，即瞬态法和稳态法。
4·Transmission and energy distribution characteristics of Rayleigh waves in layered ground were important for Rayleigh wave test.
掌握瑞利波在分层地基中的传播和能量分布特征是进行瑞利波勘测的关键。
5·The frequency domain response of single pile embedded in half-space saturated soil and subjected to Rayleigh waves was investigated.
研究了频域内半空间饱和土中单桩在瑞利波作用下的动力响应。
6·This paper introduces in detail the principle and working method of transient Rayleigh waves technique and its application in Jincheng coal co. Ltd.
论述了瞬态瑞利波探测技术的工作原理、工作方法和在山西晋城煤业集团矿区的应用情况。
7·Mechanism of disturbance of apparent phase velocity is analyzed from distribution of energies of Rayleigh waves and the reflected body waves in the responses.
根据表面质点响应中瑞利波和反射体波能量分配分析表观相速度扰动机制，讨论振源、测点、洞穴三者相对位置及频率对表面波表观相速度影响。
8·This paper consists of three sections, in the first section, the history of Rayleigh waves is introduced in detail and some problems unsolved are pointed out.
本论文包括三部分：第一部分详细介绍了瑞雷波的研究历史，并指出了存在的问题。
9·In petroleum seismic exploration records, Rayleigh waves belong in disturbing waves which should be removed from the records before deconvolution and stacking so as to raise signal-to-noise ratio.
石油地震勘探记录中的瑞雷面波是一种干扰波，在反褶积和叠加前必需首先将面波从炮记录中分离出来，以提高叠加剖面的信噪比。
10·In this paper, the method and theory relevant to inversion for source parameters by using long-period Rayleigh waves on IDA accelerograms (International Deployment of Accelerograph) are discussed.
本文讨论了利用国际部署加速度仪台网(IDA)的超长周期瑞雷波记录，反演震源参数的有关理论和方法。