首页 | 官方网站   微博 | 高级检索  
     

一种用于背景速度估计的新全局优化算法
引用本文:于建华,方正茂.一种用于背景速度估计的新全局优化算法[J].石油地球物理勘探,1998,33(5):573-582.
作者姓名:于建华  方正茂
作者单位:[1]石油地球物理勘探局研究院 [2]同济大学海洋地质系
摘    要:利用叠前地震数据正确地估计地下介质的背景速度对于复杂构造成像具有重要意义。这一问题的复杂性需要一种良好的优化方法来求解。本文给出了一种新的用于求解连续全局优化问题的计算方法,并将其应用于非线性速度反演计算。与随机法如模拟退火、遗传算法,均场退火等)不同的是,新的优化方法利用一动态方程来控制寻优计算过程。该动态方程的优点是利用梯度信息使解快速逼近极小点;当解逼近当前极小点后,动态方程的第二项可以使解

关 键 词:地震数据处理  全局优化算法  速度场  地震勘探

A new overall optimization algorithm used in background velocity estimation
Yu Jianhua, Fang Zhengmao, Li Youming, Yang Changchun and Liu Hong Yu Jianhua.A new overall optimization algorithm used in background velocity estimation[J].Oil Geophysical Prospecting,1998,33(5):573-582.
Authors:Yu Jianhua  Fang Zhengmao  Li Youming  Yang Changchun and Liu Hong Yu Jianhua
Abstract:To derive correct medium velocity from prestack seismic data is very significantto complicated structure imaging. The complexity solution of the above problemneeds a good optimization method. A new successive overall optimization calculation method will be used in the solution and non--linear velocity inversion calculation. The method is different from random methods (such as analog annealing, genetic algorithm and average field annealing), and it applies a dynamic equation tocontrol optimizing computation process. The dynamic equation uses gradient information to make the solution fast approximate the minimum point. The 2nd term ofthe dynamic equation may make the solution escape local extreme value and causethe overall optimization capacity when the solution approximates the minimumpoint; the application of gradient information has made the solution efficiency improved obviously. There will be no need to pick large amount of reflection traveltimes in calculation of objective function by the velocity estimation method based onoptimization algorithm. What is needed is only to derive zero--offset travel-timesfrom stack section to establish optimization objective function with the use of similitude criterion. Background velocity estimation will be automatically completed bythe method. The example in this paper proves that its computing efficiency is muchbetter than that of random method. Correct result has been obtained in velocity estimation.
Keywords:Seismic data processing  gradient information  objective function  dynamic equation  overall optimization algorithm  velocity field  
本文献已被 CNKI 维普 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司    京ICP备09084417号-23

京公网安备 11010802026262号