converted wave信息详情
[地震]转换波
converted───v.转变;改变信仰(convert的过去式和过去分词形式);adj.修改的;改变信仰的
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
converted car───改装车
converted gpa───折算平均绩点
converted changed───已转换已更改
converted into───使转变;把…转化成;折合
streamer converted───已转换拖缆
make wave───制造浪潮;扰乱正常的做法或常规
black wave───黑波
Velocity analysis of converted wave is a very important step in multi-wave seismic data processing.───转换波速度分析在多波地震资料处理中占有重要地位。
Static correction is important for converted wave data processing.───静校正在转换波资料处理中有很重要的作用。
On that basis, the methods for three-parameter velocity analysis and NMO of converted wave have been formed.───在此基础上,形成了转换波三参数速度分析及动校正方法。
When hyperbolic time distance equation is used to do NMO correction. NMO stretch of converted wave is less than that of compressional wave.───当采用双曲时距方程进行动校正时,转换波的动校正拉伸要小于纵波的动校正拉伸;
The static correction method of converted P-SV waves is always a problem in converted wave processing.───P-SV转换波静校正一直是转换波处理中的一个难题。
The difficulties of multi-component seismic data processing are converted wave dissymmetrical ray path and anisotropy.───多分量资料处理的主要困难是转换波非对称性射线路径和地层各向异性等因素造成的。
This paper adopts the characteristics of kinematics to estimate the parameters for P-SV converted wave.───利用时差特征对P-SV转换波的参数进行了估计。
In this case, the converted wave static correction becomes converted wave in the emphasis and difficulty.───在这种情况下,转换波的静校正就成为了转换波技术中的重点和难点。
The positioning of common converted point is a key step in the processing of converted wave data.───共转换点(CCP)定位是转换波资料处理中的关键环节。
However, the use of convolution model is to deduce recursion formula of the reflection for the converted wave.
TDT ( Time - Depth - Time ) transformation is an important step in converted wave processing.
It is difficult to locate CCP exactly due to the asymmetry of converted wave ray path and the de pendency of CCP on depth, offset, P-wave velocity, and S-wave velocity.
Maximum offset of converted wave is greater than that of compressional wave for the same stretch.
For converted wave stacking and trace selection of common reflection point gathering, it is required to accurately calculate the location of conversion points.
The difficulties of multi-component seismic data processing are converted wave dissymmetrical ray path and anisotropy.
The essential of studying the forward and inverse problems of converted wave with the use of convolution model is to deduce recursion formula of the reflection coefficient.
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