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- Seismic wave field and seismic exploration II. 地震波场与地震勘探2。
- A surface at which seismic wave velocities change. 不连续面间断面，地震波速度突变面
- Seismic wave AVO and formation lithology analysis. 地震波AVO与地层岩性分析
- 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。
- Body waves, the fastest seismic waves, move through the earth. 体波是最快的地震波，可贯穿地球。
- Body waves,the fastest seismic waves,move through the earth. 体波是最快的地震波，可贯穿地球。
- 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。
- There are two chief kinds of seismic waves: body waves and surface waves. 有两种主要的地震波：体波和面波。
- Attenuation of seismic waves between such surfaces can be similarly diagnostic. 在这些界面之间地震波的衰减，同样可以作为一种标志。
- Seismic waves from elephant vocalizations: A possible communication mode? 根据起伏干扰发声法得到的地震波:一个可能的通信模式?
- 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。
- This prediction was recently supported by studies of seismic waves passing through the core. 这个预测最近被穿过地核的地震波研究所证实。
- A seismograph produces wavy lines that reflect the size of seismic waves passing beneath it. 地震仪能产生反映在其下面通过的地震波大小的波状线。
- Let us now face the problem of the actual mechanical generation of the seismic waves. 现在让我们来看看地震波的实际发生机制问题。
- A seismograph is equipped with sensors called seismometers that can detect ground motions caused by seismic waves from both near and distant earthquakes. 地震仪配备了能探测到来自近震和远震的地震波所引起的地面运动的传感器，这个传感器被称为地震检波器。
- For instance the geomagnetic field, the heat flow, the propagation of seismic waves, the force of gravity, etc. 例如，应用地球物理勘探，可以了解诸如地磁场、热流、地震波的传播和重力等地球物理性质。
- When an elephant rumbles, the sound generates seismic waves that travel through the ground. 在大象低沉地发声时，会生成可以穿过地面行进的震动波。
- There are many seismographic stations in the world, that receive seismic waves generated by earthquakes. 目前地球上有成千上万个地震台，但它们都是接收地震波的地震台。
- C VSP logging data contains plenty of information about seismic waves such as P waves and converted S waves. VSP三分量测井记录含有丰富的地震波场信息 ,除纵波外还有转换横波资料。
- Caitlin believes the seismic waves are felt in the toenails and move up to the ear via bone conduction. 凯特琳认为震动波是通过脚趾感知并通过骨骼向上传导到耳朵的。
