三维偏移距平面波有限差分叠前时间偏移  

3D offset plane-wave finite-difference pre-stack time migration

作　　者：冯波[1] 王华忠[1] 

机构地区：[1]同济大学海洋地质国家重点实验室,上海200092

出　　处：《地球物理学报》2011年第11期2916-2925,共10页Chinese Journal of Geophysics

基　　金：国家重点基础研究发展计划(973)项目(2012CB214800);重大专项(2008ZX05023-005-016)资助

摘　　要：本文提出了中点半偏移距域内的三维偏移距平面波(offset plane-wave)方程,并给出了其有限差分解法.偏移距平面波可通过对CMP道集进行平面波分解(倾斜叠加或线性Radon变换)生成,然而这样做会产生严重的噪音干扰.本文提出了局部倾斜叠加方法(1ocal slant stacking)来消除离散线性Radon变换引入的噪音.针对实际三维数据的不规则性(中点-偏移距域内方位角展布不均匀及偏移距采样不规则),本义还提出了与方位角无关的三维倾斜叠加方法(azimuth-independent 3D slant-stacking),解决了三维平面波分解中存在的问题.使用文中提出的平面波分解方法,可以得到高信噪比的偏移距平面波数据体.同时,三维偏移距平面波偏移可以输出偏移距射线参数域共成像点道集,基于此道集的剩余速度分析方法可以用来更新偏移速度场.偏移距平面波偏移具有很高的计算效率,相较Kirchhoff积分叠前时间偏移有较好的保幅特性,可作为水平地表三维叠前时间偏移的一个很好的解决方案.Based on the double-square-root equation, a 3D offset plane-wave equation for pre- stack time migration is derived and its finite-difference scheme is put forward. Offset plane waves can be generated by applying a plane-wave decomposition （slant-stacking or Linear Radon Transform） to CMP gathers. However, the resulting offset plane waves will be contaminated by coherent noise. We then present a local slant-stacking method to eliminate the noise. Meanwhile, an azimuth-independent 3D slant-stacking approach is developed to address the issue of uneven azimuth distribution and irregular offset distribution in CMP gathers. High-quality offset planewave datasets can be produced by the offset plane-wave decomposition approach proposed in this paper. Besides, residual curvature velocity analysis can be implemented in the offset ray- parameter common-image gathers. 3D offset plane wave migration will be a practical solution for prestack time migration.

关 键 词：三维叠前时间偏移 偏移距平面波分解 局部倾斜叠加 与方位角无关的三维倾斜叠加 

分 类 号：P631[天文地球—地质矿产勘探]