The stationary phase analysis of the Kirchhoff-type d emigrated field  

Kirchhoff型反偏移场稳相分析(英文)

作　　者：孙建国[1,2] 

机构地区：[1]吉林大学地球探测科学与技术学院,长春130026 [2]国土资源部应用地球物理综合解释理论开放实验室-波动理论与成像技术实验室,长春130026

出　　处：《Applied Geophysics》2010年第1期18-30,98,共14页应用地球物理（英文版）

基　　金：supported by the National Natural Science Foundation of China (Grant No.40574052)

摘　　要：In the literature,stationary phase analysis of Kirchhoff-type demigrated fields is carried out mainly under the following two conditions：（1） The considered isochrone and the target reflector are tangential to each other;（2） The spatial duration of the wavelet of the depthmigrated image is short.For the isochrones that are not tangential to the target reflector and for the depth-migrated images that have a large spatial duration,the published stationary phase equation for the demigrated field will become invalid.For performing the stationary phase analysis of the Kirchhoff-type demigrated field under the conditions that the considered isochrone and the target reflector are not tangential to each other and that the spatial duration of the wavelet of the depth-migrated image is not short（the general conditions）,I derive the formulas for the factors appearing in the stationary phase formula in two dimensions,from which I find that for different isochrones the horizontal coordinates of the stationary point of the depth difference function are different.Also,the equation for the Kirchhoff-type demigrated field consists of two parts.One is the true-amplitude demigrated signal and the other is the amplitude distortion factor.From these facts the following two conclusions can be drawn：（1） A demigrated signal is composed of many depth-migrated images and one depth-migrated image trace provides only one sample to the demigrated signal;and（2） The amplitude distortion effect is an effect inherent in the Kirchhoff-type demigration and cannot be eliminated during demigration.If this effect should be eliminated,one should do an amplitude correction after demigration.在文献中,Kirchhoff型反偏移场的稳相分析主要是在下列两个条件下进行的:(1)等时面和目标反射面相切;(2)深度偏移像场信号的长度接近于零。对于与目标反射面不相切的等时面和长度远大于零的深度偏移像场子波,已有的结果将不再成立。为了在等时面和目标反射面不相切和深度偏移像场的子波长度远大于零的条件(一般条件)下对Kirchhoff型反偏移场进行稳相分析,我推导了出现在二维稳相分析公式中的诸因子的计算公式,并从中发现:(1)对于不同的等时面,距离差函数的稳相点具有不同的水平坐标;(2)Kirchhoff型真振幅反偏移的输出场由两部分(真振幅反偏移信号与振幅畸变因子)的乘积组成。由此得到下列两个结论:(1)一个给定的反偏移信号由多个深度偏移信号上的采样点组装而成,反偏移信号上的采样点个数等于对于这种组装有贡献的偏移信号的个数。(2)振幅畸变效应是Kirchhoff型反偏移中的固有效应,靠反偏移本身无法消除。如果一定要消除这种振幅畸变效应,必须对反偏移结果进行振幅校正。

关 键 词：Kirchhoff-type demigration stationary phase analysis amplitude distortion 

分 类 号：P631.4[天文地球—地质矿产勘探]