22. In the last, we make some suggestion about the study of seismicwave 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。
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23. 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。
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24. 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。
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25. 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。
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26. Shaking table experiment not only has great load factor, but also can simulate crude seismicwave 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。
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27. 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。
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28. 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。
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29. 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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30. 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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Seismic sections show the response of the earth to seismic waves. 地震剖面是地壳对地震波的响应。
Seismic waves move out from the focus of an earthquake in all directions. 地震波从震中向周围的各个方向传播。
When the blast wave expands, it breaks the bubbles and thereby loses energy. 爆震波扩张时,会由气泡吸收,因而丧失能量。
When this happens, seismic waves travel faster than usual through the rock. 当这种情况发生,震波穿过岩石的移动速度要比往常快。
By sheer coincidence, a trio of earth-monitoring satellites gave modelers the pristine, undistorted wave heights they needed for the Indian Ocean tsunami. 十分巧合的是,有一组地球观测卫星提供了最原始且如实的海啸波高值,这是模型设计师模拟印度洋海啸时不可或缺的。