基于Hartley变换的三维真振幅偏移算子研究
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
在实际应用中,以快速Fourier变换为基础的偏移方法,将本来是实数的地震道转化为复数参加运算,导致了计算机内存的增加。本文把只有纯实数运算的Hartley变换引入到基于Fourier变换的偏移算法,再利用三维真振幅偏移单程波方程,结合Fourier变换与Hartley变换的内在关系,经过数学推理,具体导出了裂步Hartley变换真振幅偏移算子。与一般裂步Fourier法相比,裂步Hartley变换真振幅偏移算法既提高了计算效率又对球面扩散问题进行了振幅补偿。
In real application,the migration methods based on Fast Fourier transform change real seismic trace into complex to operate results the increase of computer memory.In this paper,we introduce the Hartley transform with the pure real calculation into migration algorthm.The Split Step Hartley transform migration operator with true amplitude is derived by mathematical inference based on the inherent relations between Fourier transform and Hartley transform and a one-way wave equation with true amplitude created,and steps are given.Compared with the common Split Fourier,The Split Step Hartley transform migration operator with true amplitude both enhances with computing efficiency and proceeds the amplitude compensation about spherical proliferation.
引文
[1]罗纳德.N.布雷斯韦尔.傅立叶变换及其应用[M].殷勤业,张建国.西安:西安交通大学出版社,2005,231-255.
    [2]Hartley R VL.Amore symmetrical Fourier analysis appliedtotransmission problems[J].Proceeding of the IEEE,1942,30,144-150.
    [3]Saatcilar R.,S.Ergintav,and Canitez N.The use of the Hartleytransformin geophysical applications.Geophysics,1990,55(11),1488-1495.
    [4]Zhang Y,Xu S,Zhang G,et al.Howto obtaintrue amplitude common=angle gathers fromone-way wave equation mi-gration?[J].Expanded Abstracts of74thAnnual International SEG M-Eeting,2004,1021-1024.
    [5]崔兴福,张关泉,吴雅丽.三维非均匀介质中真振幅地震偏移算子研究[J].地球物理学报,2004,47(3):509-513.

版权所有:© 2023 中国地质图书馆 中国地质调查局地学文献中心