- 更多网络例句与地震横波相关的网络例句 [注：此内容来源于网络，仅供参考]
-
In this paper, we research the imaging problems beneath volcanic area. We sort common asymptotic conversion point gathers and perform velocity analysis to establish the initial velocity which will be used in PSTM. By scanning migration velocity and V p/ V s, we get the optimum migration velocity and
本文针对火山岩地震屏蔽层的转换波成像问题，通过对转换波共近似转换点道集进行速度分析，建立了转换波叠前时间偏移的初始速度场，通过速度扫描和纵、横波速度比值扫描确定最佳的偏移速度场和纵、横波速度比值，实现了在火山岩高速层覆盖区域的转换波偏移成像。
-
Finally, seismic Rayleigh wave velocity inversion for P-SV wave S-statics isstudied, which is mainly including the flowing contents: the separation of Rayleighwave signals from seismic data, the pickup of Rayleigh dispersion curves, seismicRayleigh wave velocity inversion, and the principle and the processing flow ofresolving P-SV wave S-statics.
最后研究了地震瑞雷面波速度反演求取P-SV波横波静校正量，包括地震瑞雷波信号分离方法、地震瑞雷波频散曲线拾取方法、地震瑞雷波速度反演以及P-SV波横波静校正量求取方法和处理流程。
-
The transverse and longitudinal wave velocities of rock are important parameters in evaluation of stratum and seismic exploration and petroleum geology.
岩石纵、横波速度是地层评价和地震勘探的重要参数，衰减在地震勘探和石油地质研究中早已受到关注，但对于气源断裂的性能，一直没有很好的判断方法。
-
According to the three-components teleseismic records from portable digital seismic station deployed in Himalaya mountain chain region, the S-wave velocity structure beneath 46 teleseismic stations are investigated by using transform function method and SA technique. As reliable geophysics evidence, these results help us to understand the geodynamic process of Himalaya mountain region of Tibet.
利用流动数字地震台网提供的三分量地震波形记录，应用转换函数及快速模拟退火算法对喜马拉雅山脉地区46个地震站下的地壳横波速度结构进行了反演，为进一步揭示青藏高原喜马拉雅山脉地区的动力学演化过程提供了可靠的地球物理证据。
-
When using full wave train logging data to make C wave synthetic seismogram,it needs to consider the influence of many kinds of factors such as dip and anisotropy of bed as well as environment correction of S wave logging data etc.
采用全波列测井资料制作转换波人工合成地震记录，需要考虑地层倾角、岩层各向异性、横波测井资料的环境校正等多种因素的影响；在纵、横波资料对比中，又需要考虑极性、井资料的深时转换、子波带宽等的影响。
-
Seismic anisotropy can be studied by four basic seismic wave behaviors, e.g, direction-dependent travel time anomalies, shear-wave birefringence, surface-wave scattering, and direction-dependent conversion of compressional waves to shear waves.
目前人们利用4种基本的地震波现象研究地震各向异性，如横波双折射、面波散射、与传播方向有关的走时异常和PS转换波震相。
-
It＇s difficult to deal with seismic acoustic forward modeling and seismic inversion for the absence of shear wave data usually.
在测井资料中，通常缺乏的就是横波资料，这给地震波正演模拟和地震反演都带来很大的困难。
-
Based on the case of urban geologic survey in Guangzhou, the paper introduces data collection method used in shallow exploration in process of seismic transverse wave detection, and analyses the geologic explanation for results as well as divides the strata in this way coupled with method of well logging.
并以广州市城市地质调查项目为例，介绍了地震横波勘探在浅层地层勘测中的数据采集方法，分析了地质解释依据，并结合波速测井方法对地层层面进行了划分。
- 更多网络解释与地震横波相关的网络解释 [注：此内容来源于网络，仅供参考]
-
Moho：莫霍
摆为STS2),并于2006年5月取得首批数据.利用宽频带地震仪提供的三分量地震波形记录,应用转换函数及快速模拟退火算法对珠峰站下的地壳横波速度结构进行了反演.反演结果表明,珠峰站的莫霍(Moho)面深度在70 km,
-
segmented display：断码式显示
segment 扇形体 | segmented display 断码式显示 | seism 地震横波传感器
-
seism：地震横波传感器
segmented display 断码式显示 | seism 地震横波传感器 | seismic 地震的
-
shear wave：横波
通过分析这种地震波数据,地震学家能够区分纵波(compressiona wave)和横波(shear wave):前者又叫P波,由岩石交替挤压、拉张而产生,振动方向和传播方向一致;后者又叫S波,因岩层剪切而产生,振动方向与传播方向垂直.
-
shear wave：剪力波
S波的S也可以代表剪力波(shear wave),因为S波是一种横波,地球内部粒子的震动方向与震波能量传递方向是垂直的. S波与P波不同的是,S波无法穿越外地核. 所以S波的阴影区正对著地震的震源.