Poisson laid the theoretical foundation of seismic wave.
奠定了地震波理论基础。
Question 18. What is the most destructive type of seismic wave?
问题18地震波中破坏力最强的波形是什么？
The reconstruction of seismic wave-speed distribution is nonlinear.
重建地下速度分布是一个非线性问题。
Question 19. Which seismic wave brings us shaking felt from an earthquake?
问题19地震中哪种波形会让我们感觉到震动？
The parameters of explosive seismic wave were measured by piezocrystal gages.
用压电晶体探头测量了爆炸时的地震波参数。
I condense my spirit in the core of spiritual seismic wave, and close my eyes.
我马上凝聚精神在精神震波的核心点，闭上眼睛。
The phenomenon of seismic wave poetry has its rationality , fold brilliant shine.
地震诗潮现象有其存在的理由，闪烁出褶褶光辉。
A given seismic wave field can be described using different kinds of seismic wavelets.
对于一个确定的地震波场，可用不同类型的子波来描述。
Seismic wave velocity is the most important parameter in geophysical prospecting and development.
地震波速度是地球物理勘探和开发中最重要的一个参数。
Numerical modeling result proves that plastic wave model shows more seismic wave properties than others do.
模拟结果表明，塑性波模型能更多地反映出地震波的传播特征。
The seismic wave oscillating up-down within the basin may result large damage for buildings above the basin.
能量消耗在盆地的沉积层内部，这可能对盆地上的建筑物造成严重的灾害。
Courses include acoustic and seismic wave propagation, seismic modeling, fluid hydraulics, and related subjects.
课程包括声波和地震波的联动、地震模型、水力学和相关其他。
Regional seismic wave carries lots of information about structural variations in the crust and the upper mantle.
区域地震波携带着大量的信息，可以很好地反映地壳和上地幔结构的变化。
Seismic wave spectrum can be decomposed into transmitting spectrum, medium effect spectrum and receiving spectrum.
将震波波谱分解为发射谱、介质作用谱以及接收谱。
In this paper, the theory and application of how to abstract and classify the seismic wave attributes are discussed.
本文对地震波属性的提取和分类进行了理论和应用的研究。
And the attenuation studies of seismic wave in the laboratory have provided studying base for the mechanism studies.
而实验室中对地震波衰减的研究为衰减机理提供了研究基础。
Propagation of seismic wave in complex medium is mostly simulated by numeric solution of oneway or two-way wave equation.
复杂介质中地震波的传播多是通过求取单程或双程波动方程的数值解进行模拟的。
Based on the theory of elastic wave in anisotropy medium, the characteristic of the seismic wave is analyzed in this paper.
从各向异性介质的弹性波理论出发，本文系统地分析了各向异性土介质中地震波的传播特性。
It computes the distribution of velocity in the rock and soil body using speed information of seismic wave by special methods.
这种技术利用大量的地震波速度信息进行专门的反演计算，得到测区内岩土体弹性波速度的分布规律。
In dynamic analysis of complicated structure, critical Angle of seismic wave is corresponding to critical response of structure.
对于复杂结构，在动力分析中地震波的最不利输入方向对应着结构的最不利反应。
This model can consider the effect of the viscosity of rock skeleton and saturation degree on the propagation of the seismic wave.
由于此模型不但考虑了岩层骨架的粘性，而且考虑了饱和度对地震波传播的影响，从而可以全面地了解地震波在准饱水岩层中的传播特性。
In the last, we make some suggestion about the study of seismic wave motion, detection and it's application in anisotropic medium.
最后对我国在各向异性介质中地震波动、检测和应用等研究提出了一些看法。
A new characterization method of explosion seismic wave is suggested on the basis of the analysis of experimental measured results.
在实验测试结果分析的基础上，提出一种新的爆炸地震波特征化描述方法。
It is important to study the physical property of anisotropic media using the information of seismic wave aimed at probing into the earth.
利用地震波的信息，研究各向异性介质的物理性质对深入探究地球内部结构有着重要的作用。
The attenuation of seismic wave in near offset can more correctly reflect the lithologic information of formation than that in far offset.
近炮检距处地震波的衰减较之远炮检距的相应衰减量更能准确反映地层的岩性信息。
Shaking table experiment not only has great load factor, but also can simulate crude seismic wave and artificial wave to load tested object.
地震模拟振动台试验不仅负载量大，而且能模拟天然地震波和人工地震波对试件加载。
The post -stack seismic wave impedance inversion methods are classified based on the fundamentals and realization ways of the inversion software.
根据反演软件的基本原理及实现方式，对叠后地震波阻抗反演方法进行了分类研究。
In this paper, seismic wave propagation in viscoelastic isotropic media is mainly addressed by the technology of wave field numerical simulation.
本文主要是通过波场数值正演模拟技术来研究粘弹性各向同性介质中地震波的传播问题。
Rock pore structure is one of the important parameters in controlling both seismic wave velocity and permeability in sandstones and carbonate rocks.
岩石孔隙结构是控制砂岩和碳酸盐岩的地震波速度和渗透率的重要参数之一。
Rock pore structure is one of the important parameters in controlling both seismic wave velocity and permeability in sandstones and carbonate rocks.
岩石孔隙结构是控制砂岩和碳酸盐岩的地震波速度和渗透率的重要参数之一。
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