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目标函数叠前保幅偏移方法与应用
引用本文:刘伊克,常旭,卢孟夏,Hongchuan Sun.目标函数叠前保幅偏移方法与应用[J].地球物理学报,2006,49(4):1150-1154.
作者姓名:刘伊克  常旭  卢孟夏  Hongchuan Sun
作者单位:1.中国科学院地质与地球物理研究所,北京 100029 2 北京联合大学信息学院,北京 100101 3 Department of Geology and Geophysics, University of Utah, Utah 84112, U.S.A.
基金项目:国家自然科学基金(40374050,40235055)资助.
摘    要:将理论反射率与偏移反射率的差作为目标函数,给出一种迭代振幅补偿保幅偏移方法.把偏移看作一个反问题,寻找反问题中的最优解.偏移算子是正演算子的伴随共轭,其伴随矩阵非对角占优.通过预条件优化伴随矩阵,使Hessian矩阵准对角化.依据地震波传播稳定相位理论,计算反射点,以反射点为中心、菲涅耳带为半径偏移.考虑振幅几何扩散补偿、散射角度补偿,在迭代反演过程求出最优解,即保幅偏移解.本文给出了一个保幅数值模拟结果和一个实际地震数据实例.

关 键 词:保幅偏移  目标函数  权函数  
文章编号:0001-5733(2006)04-1150-05
收稿时间:2005-08-04
修稿时间:2005-08-042006-04-06

Objective function prestack amplitude preserving migration and its application
LIU Yi-Ke,CHANG Xu,LU Meng-Xia,Hongchuan Sun.Objective function prestack amplitude preserving migration and its application[J].Chinese Journal of Geophysics,2006,49(4):1150-1154.
Authors:LIU Yi-Ke  CHANG Xu  LU Meng-Xia  Hongchuan Sun
Institution:1.Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China 2 Information of College, Beijing Union University,Beijing 100101, China3 Department of Geology and Geophysics, University of Utah, Utah 84112, U.S.A.
Abstract:An iterative migrated method is developed by building a misfit function between the observed seismic data and forward modeling synthetic data. A weight function is used to compensate the amplitude attenuation for seismic wave transmitting in the earth. We consider migration as an inversion problem and find an optimal solution in the inversion. The migrated operator is the adjoint of forward modeling operator, and the transpose matrix is not dominant diagonal matrix. A preconditioning matrix is applied to make the Hessian matrix a diagonal approximation. Take-off and incidence angles are estimated for locating at the reflected points by applying stationary phase, which decreases greatly computing costs. An optimal solution, which is a true amplitude, is obtained in the process of iteration by considering the weighted factors to compensate the amplitude spreading and the angle effects with offset. Two numerical examples effectively illustrate the results of amplitude preserved and a case of field data is presented.
Keywords:Amplitude preserving  Objective function  Weighted function
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