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[地震]地震波；海啸，海啸波
1、evanescent wave───衰逝波; 渐逝波; 瞬逝波; 损耗波；[地物]消散波；损耗波；[光]隐失波
2、wave───v.挥手；挥手示意；挥舞；飘扬；使（头发）略呈波形；n.海浪；心潮；涌现的人（或物）；挥手；波；（头发）卷曲；（感情）爆发
3、body wave───[力][地物]体波
4、seismic surveys───地震测量
5、crime wave───（某一地区短时期内的）犯罪率激增；恶浪
6、black wave───黑波
7、make wave───制造浪潮；扰乱正常的做法或常规
8、bungles wave───蹦极波
9、Wave hooves───波蹄
1、The tests include seismic wave excitation parameter test, observation system parameters test and seismic reflection data processing test.───试验内容包括地震波激发参数试验、观测XiTong参数试验和地震反射资料处理方法试验。
2、Poisson laid the theoretical foundation of seismic wave.───奠定了地震波理论基础。
3、Roof is composed of heterogeneous rock. When roof failure happens, a large amount of energy would release in the form of seismic wave.───顶板是一种典型非均质岩石材料，在其PoHuai演化过程中将释放能量产生地震波。
4、Question 18. What is the most destructive type of seismic wave?───问题18地震波中PoHuai力最强的波形是什么？
5、The essential feature of the seismic wave propagation in viscous-elastic media is the attenuation of its energy.───地震波在粘弹性介质中传播的一个基本特征是能量的衰减及地震波的瞬时波形变化。
6、These appealing characters of this Improved method would make It effective to model seismic wave propagation in complex media.───这种改进的方式，这些吸引人的特点将使有效的模型在复杂介质地震波传播。
7、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？
8、The separation of the cross-well seismic wave field can be regarded as an extension of the VSP wave field separation.───井间地震反射波场分离可以看成是VSP波场分离的一种延伸。
9、The seismic wave did not being affected generally in easy near surface or plains region.───这在简单的近地表结构地区或在平原地区可近似认为对地震波场不产生影响。
1、Seismic wave attenuation in rock means wave energy loss in rock.
2、But to layered strata, the seismic wave path is complicated when reservoir changes, and it is difficult to directly define vertical time difference by pre stack far offset seismic data.
3、At present, the vertical incidence of seismic wave is considered in the seismic response analysis of arch dam.
4、The seismic wave is input by way of coherent-vibration input program and program compiled by APDL.
5、Based on the propagation theory of seismic wave in one dimensional layered medium this paper gives the recurrence formula of such a propagation.
6、The present seismic wave data is given in the form of acceleration time history; and the velocity and displacement time histories obtained by direct integration exist obvious baseline drift.
7、The directions of seismic wave have no effect on pseudo-static displacement.
8、I analyse seismic wave propagation in directionally fractured medium and the anisotropy.
9、With the use of reciprocal principle in seismic wave propagation, the algorithm may be used to compute the travel times of reflected compressional wave or converted shear wave.