面波

由于合理地选取了采集、处理参数，面波勘探深度超过250m，取得了满意的勘探效果。

With just collecting and processing parameters , the depth of surface wave exploration is larger than 250 meters .

大庆电场地震实验资料的面波特征

The surface wave characteristic of seismic experiment in electric field in Daqing

均匀覆层梯度半空间中的Love面波

Love Wave in Graded Half - Space with Homogeneous Layer

Love面波法机理的进一步讨论

Further discussing on the principle of Love surface wave method

竖向非均匀介质中的Love面波

Love waves in vertical inhomogeneous media

青藏高原东部地区的面波Q值

Q-value for surface waves in the eastern region of Xizang Plateau

实际观测地震面波品质因数Q值空间分布的反演方法

The inversion of Q & value Spatial Distribution of Practical Observed Surface-Waves

地震面波品质因数Q值的模拟反演及误差估算

The Inversion of Q-value Simulations of Surface-waves and it 's errors estimation

研究了面波震级（MS）与近震震级（ML）间的转换关系，并推荐了新的转换公式。

We also studied the relationship between MS and ML and a new converting formula was recommended .

梯度介质半空间Rayleigh面波传播性能研究

Propagation Behavior of Rayleigh Waves in Graded Half-Space Medium

Rayleigh面波衰减系数γ计算。

Calculating of the Rayleigh Surface wave attenuation factor y. In the first step .

在计算区域内结构将采用有限单元划分，而在边界上则根据Love面波特性使用传递边界有限单元。

The finite elements are used in calculated domain of struc-ture . The transmitting boundary finite elements are used in calculated domain boundary of structrue accord-ing to Love surface wave charateristic .

在其沿界面的传播过程中，显示出和弹性介质中经典的Rayleigh面波一样的强振幅能量。

The surface-wave mode propagates with strong energy , as the classical Rayleigh wave in elastic media .

用面波反演风化层Q值&补偿风化层吸收提高分辨率

Inversion of quality factor Q for weathered layer using surface waves ── Compensating seismic wave absorption in weathered layer to increase resolution

二维TIM中的传播矩阵与面波相速度

Propagating matrix and analytical solutions to the phase velocity of surface waves in 2-D transversely isotropic media

瑞利面波数值模拟中的PML吸收边界条件

PML absorbing boundary condition for numerical modeling of Rayleigh wave

在此基础上，本文给出了利用实测的Love面波的弥散曲线反分析土层参数的方法，并编制了相应的计算机程序。

[ 1 ] - Based on it , the authors present the method of back calculation of soil parameters from the measured Love wave dispersion curve , and its computer program is worked out .

通过将已经过压水试验、钻孔取芯和面波等方法检验注浆已合格断面的电磁波CT测量数据进行统计分析，得出适用于南广铁路岩溶路基注浆质量电磁波CT检测评判标准。

The measured data by electromagnetic tomography method in the sections are statistically analyzed , whose grouting tests have passed the examinations of over water pressure tests , coring and surface wave .

由于与经典Rayleigh面波的相似性，我们可以用这种面波模式来描述真实的面波资料。

For similarity to the classical Rayleigh wave , we can use this surface-wave mode to describe the real world surface wave data .

将时域有限差分法（FDTD）和平面波法作为光子晶体理论研究的工具。

The finite-difference time-domain ( FDTD ) method and plane wave method are developed for analyzing the 2-D square lattice photonic crystals .

由SK地震仪的尾波持续时间快速测定面波震级

Fast determination of surface wave magnitude m_s from duration of coda waves recorded by SK seismograph

在文中，根据干扰特征设计出了合适的算法对噪声进行压制，例如：对线性干扰和面波的干扰，本文提出了交互式F-K滤波的方法，验证得到比较好的效果。

According to the characteristics of interference designed appropriate algorithm to noise suppression .

利用天然地震波测量Q值的主要方法有：利用地球自由振荡资料、利用体波、利用面波和利用尾波来研究Q值。

The major methods of measuring Q-value by the natural earthquakes are the ones of using the data of free vibration of earth , body wave , surface wave and coda .

提出了将多道瞬态面波勘察和SH波反射法勘探结合进行联合勘探的可行性。

At last the paper raised the feasibility of a exploration method , which combine the Multi-trace transient surface wave and SH transverse wave .

DK-1面波震级偏差在二维空间的变化研究

Study on difference of the M_S magnitude for DK-1 instrument in two-dimensional space

为了分析不同路面波与车辆振动的关系，推导建立了四个自由度的1/2车辆-路面模型及其在Matlab中的时域仿真系统。

In order to analyse the relationship between road wave and vehicle vibration , this paper establishes a half vehicle-road model with four freedom degrees and the time domain simulation system of the model is built in Matlab .

在另一实验中，使用HHT方法进行面波的压制，与其它方法相比，显示其具有较好的去噪效果。

In another experiment , using the HHT method , surface wave is eliminated , compared with other methods , its better denoising is shown .

本文首次采用Rayleigh面波双台法研究中国西部及其邻域的三维横波速度结构。

It 's the first time that interstation method for Rayleigh wave is used to study the 3-D V-S structure in the crust and upper mantle beneath western China and adjacent area .

以国家地震台网测定的面波震级为标准，利用福建区域数字地震台网测定的近距离面波震级MS结果与国家地震台网测定的面波震级结果进行比较和统计分析。

We take the surface wave magnitude M S measured by the state seismic network as the standard . The comparison and statistical analysis between Fujian regional digital seismic network and state seismic network for M S had been made .

由于横波只在固体骨架上传播，斑块饱和模型中纵波和横波的耦合可以在自由表面上产生等效Rayleigh面波。

As the S wave propagates in the solid frame skeleton , the combination of P wave and S wave in patchy saturation model generates the effective Rayleigh surface wave at the free surface .