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这次地震波及周围几个城市。This earthquake affected several cities in the vicinity.
数据和人工地震波都与抵达的P波或SH波同步。Both data and synthetic seismograms are aligned on the P or SH arrivals.
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孔隙率和温度有时也能影响地震波速。Seismic velocity can occasionally be affected by porosity and temperature.
地震波衰减性质的研究是地震学研究的重要课题。The study of seismic attenuation property is a major subject in seismology.
地震波的传播方向对拟静力位移分布规律没有影响。The directions of seismic wave have no effect on pseudo-static displacement.
用压电晶体探头测量了爆炸时的地震波参数。The parameters of explosive seismic wave were measured by piezocrystal gages.
视速度和偏振是地震波的两个重要特性。Apparent velocity and polarization are important characters of seis- mic wave.
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数据和人工地震波都与地震起始时间同步。Both data and synthetic seismograms are aligned with the earthquake origin time.
对湖试数据做了传统谱及小波谱的分析对比，得到舰船地震波信号的时频特征。And the characteristic of the ship seismic-wave field have been obtained the paper.
宽角数据用于建立地表到MHT的地震波速度模型。The wideangle data were used to construct a crustal seismic-velocity model down to the MHT.
这为反射地震波的旅行时及速度分析提供了基础。This lays a foundation for the traveltime and velocity analysis of reflective seismic waves.
本文针对二维层状介质提出了一种识别地震波速度的新方法。A method for determining the velocity of seismic wave in two-dimensional medium is presented.
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地震波记录曲线的分析表明，初至波是P波，随后是S波。The analysis of seismograms indicates that the first arrival is a P-wave, followed by a S-wave.
对比了不同地震波下结构双维时程分析结果。The two-dimensional Time-History analysis results are contrasted in the different seismic waves.
对比了不同地震波下结构单维时程分析结果。The single dimensional Time-History analysis results are contrasted in the different seismic waves.
借助于越来越先进的地震波成像技术，科学家正在研究地球这个庞大机器的运作过程。By using Seismic Wave Imaging, scientists are now studying on the process of the big machine's work.
这种现象，为观测地震波特性的前兆异常给予了启示。Such a phenomenon has enlightened us on the precursory anomaly of the observed wave characteristics.
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地震波的聚焦使对应每个地面位置的同相轴上具有三个反射点。The focusing of the seismic wave produces three reflection points on the event per surface location.
可控震源激发的地震波是一个扫描信号，将此扫描信号与参考扫描作互相关得到相关记录。A scanning signal from vibroseis is correlated with reference one to give rise to a correlation record.
地震波在地下介质中传播时，高频成分易被吸收。The high frequency part of seismic wave propagation in subsurface is easy to be absorbed or attenuated.