Three methods of visco-acoustic migration based on the De Wolf approximation and comparison of their migration images

IF 1.8 3区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Huachao Sun, Jianguo Sun, Zhenghui Gao
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引用次数: 0

Abstract

The viscosity of a medium affects the amplitude attenuation and velocity dispersion of seismic waves. Therefore, it is necessary to consider these factors during migration. First, to eliminate the viscous effect of a medium, we combine the Futterman model with the integral equation of the De Wolf approximation to construct a compensation operator of the De Wolf approximation for a visco-acoustic medium. Next, we use the visco-acoustic screen approximation method to realize the continuation operator then establish a prestack depth migration algorithm. Finally, an error analysis, impulse response test and model test are performed. The results show that three different generalized visco-acoustic screen methods (phase screen method, generalized screen method and extended local Born Fourier method) can satisfactorily compensate for the attenuation of deep interface amplitude. Among these methods, the visco-acoustic extended local Born Fourier method has the highest accuracy and the best compensation effect.

基于De Wolf近似的三种粘声偏移方法及其偏移图像的比较
介质的黏度影响地震波的振幅衰减和速度弥散。因此,在迁移过程中有必要考虑这些因素。首先,为了消除介质的粘性效应,我们将Futterman模型与De Wolf近似的积分方程结合起来,构造了粘声介质的De Wolf近似的补偿算子。其次,采用粘声屏近似方法实现延拓算子,建立叠前深度偏移算法。最后进行了误差分析、脉冲响应试验和模型试验。结果表明,三种不同的广义粘声屏蔽方法(相位屏蔽法、广义屏蔽法和扩展局部玻恩傅立叶方法)都能较好地补偿深部界面振幅的衰减。其中,粘声扩展局部玻恩傅立叶法精度最高,补偿效果最好。
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来源期刊
Geophysical Prospecting
Geophysical Prospecting 地学-地球化学与地球物理
CiteScore
4.90
自引率
11.50%
发文量
118
审稿时长
4.5 months
期刊介绍: Geophysical Prospecting publishes the best in primary research on the science of geophysics as it applies to the exploration, evaluation and extraction of earth resources. Drawing heavily on contributions from researchers in the oil and mineral exploration industries, the journal has a very practical slant. Although the journal provides a valuable forum for communication among workers in these fields, it is also ideally suited to researchers in academic geophysics.
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