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反射转换波
相关语句
  reflected converted wave
    Five reflected waves which are reflected compressional wave, reflected converted wave, W 1, W 2 and W 3 were observed at the depth of 1 210 m in the fracture dominating direction in Shun 5 Well.
    在顺 5井裂隙优势方向 ,12 10m深度上观测到 5种反射波 :反射纵波、反射转换波、W1 、W2 、W3波 ;
短句来源
    The focal depth of the earthquake with M 7 0 occurred in Eastern Jilin on April 8,1999 is determined by use of deep phases of simulation and digital records at Nanping Seismic Station. The result shows that the focal depth determined by centrosphere interface wave is close to that determined by China seismic network. But when we use reflected converted wave around epicentre to determine the focal depth,there is a little error between the results from Seismic Station of Nanping and from China seismic network.
    用南平台模拟地震记录和数字观测记录 1 999年 4月 8日吉林东部 7级地震的不同深震震相来测定其地震深度 ,结果为南平台用地核界面波测定的震源深度与中国地震台网所测定的深度接近 ,用震中附近反射转换波定震源深度与中国地震台网所测定的深度有一定的误差。
短句来源
    Four reflected waves which are reflected compressional wave, reflected converted wave and two slow speed waves named as W 4 and W 5 for the distinction from the slow speed waves in Shun 5 Well, were observed.
    在顺 4井 15 3 2m深度上观测到 4种反射波 :反射纵波、反射转换波 ,还有 2种慢速波至 ,为了区别于顺 5井中观测到的慢速波至 ,将其命名为W4 、W5波 .
短句来源
  “反射转换波”译为未确定词的双语例句
    DMO FOR P-SV CONVERTED REFLECTION
    P-SV反射转换波的倾角时差校正(DMO)方法研究
短句来源
    he focal depths of earthquakes are determined using the reflected PcP,and the converted ScP and PcS by the nuclear interface,which are recorded by DD1 seismograph in Nanping station.
    利用南平台DD-1地震仪所记录到的地核界面反射波PcP、地核界面反射转换波ScP、PcS测定震源深度。
短句来源
    The SP' phases denote those direct S waves which are reflected from the earth surface, these are transformed from S into P, and then the P waves are once again reflected up to the earth surface from the M-discontinuity.
    本文讨论利用S波与它的反射转换波SP′的走时差来测定我国各基本台(武汉除外)附近地壳厚度的某些结果。 所谓SP′波是直达的S波经地表面反射转换为P波,再被M界面反射到地面来的波。
短句来源
    By adopting suitable crustal parameters, it can be calculated that the energy of SP' is much greater than that of other transformed waves.
    本文讨论了SP′震相的分析问题,采用适当的地壳参数,可以算得在S波的数种反射转换波中,SP′波的能量最大。
短句来源
    In this paper, the techniques for the SV-wave observation in the ultrasonic model experiment were introduced and described. Through the experiment mentioned above, the reflected-transformed waves P1S1 and the transverse waves S11 from the single boundary were obtained. It thus provides an experimental technique for the study of SV-wave exploration by model experiments.
    本义讨论了超声模型试验中SV型横波的观测技术,通过改变发射、接收探头的安置角度,取得了单界面上的反射转换波P_1S_1和反射横波S_(11),为横波地震勘探的理论研究和实际应用提供了一种实验观测方法.
短句来源
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The SP' phases denote those direct S waves which are reflected from the earth surface, these are transformed from S into P, and then the P waves are once again reflected up to the earth surface from the M-discontinuity. By adopting suitable crustal parameters, it can be calculated that the energy of SP' is much greater than that of other transformed waves. By analysing the records and travel time curves, SP' can be distinguished. From the difference of travel times between S and its corresponding SP', the crustal...

The SP' phases denote those direct S waves which are reflected from the earth surface, these are transformed from S into P, and then the P waves are once again reflected up to the earth surface from the M-discontinuity. By adopting suitable crustal parameters, it can be calculated that the energy of SP' is much greater than that of other transformed waves. By analysing the records and travel time curves, SP' can be distinguished. From the difference of travel times between S and its corresponding SP', the crustal thicknesses near the seismic stations are obtained.

本文讨论利用S波与它的反射转换波SP′的走时差来测定我国各基本台(武汉除外)附近地壳厚度的某些结果。所谓SP′波是直达的S波经地表面反射转换为P波,再被M界面反射到地面来的波。本文讨论了SP′震相的分析问题,采用适当的地壳参数,可以算得在S波的数种反射转换波中,SP′波的能量最大。对其它易与SP′相混的波也进行了一些讨论。所得各地区的地壳厚度如下:

The present situation of using manifold seismic waves in China's energy resource exploration is briefed.Then,the experience of the com- bined observation of reflected longitudinal wave and converted wave is summed up,and the preliminary data processing results presented.Final- ly some topics worthy of study are put forward in this paper.

本文简述了我国利用多种地震波进行能源勘探的状况,并介绍了反射纵波及反射转换波的联合观测经验与初步处理效果,最后提出一些值得研究的课题。

In this paper, the techniques for the SV-wave observation in the ultrasonic model experiment were introduced and described. Through the experiment mentioned above, the reflected-transformed waves P1S1 and the transverse waves S11 from the single boundary were obtained. It thus provides an experimental technique for the study of SV-wave exploration by model experiments.

本义讨论了超声模型试验中SV型横波的观测技术,通过改变发射、接收探头的安置角度,取得了单界面上的反射转换波P_1S_1和反射横波S_(11),为横波地震勘探的理论研究和实际应用提供了一种实验观测方法.

 
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