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Prestack depth imaging and velocity analysis for P-P and P-S data with nonstationary integral extrapolators.

机译:使用非平稳积分外推器对P-P和P-S数据进行叠前深度成像和速度分析。

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摘要

Practical parallel implementation of the nonstationary integral wavefield extrapolators is presented. Two approaches, the windowed split-step algorithm and full integral algorithm, were implemented. The integral extrapolators are suitable for large-step wavefield extrapolation, even when lateral velocity variations are strong, provided that the static phase-shift and the focusing phase-shift velocities are replaced by time-average and depth-average velocities, respectively. Linear vertical wavefield interpolation between reference wavefields produced by large-step extrapolation algorithms can be used to compute the intermediate depth image. This dual algorithm significantly reduces the run time of the integral wavefield extrapolators.; Nonstationary extrapolators are found to be very capable of imaging shallow events at large dipping angles as well as at deep events, even when severe topography variations and high near-surface velocity is present. The Marmousi synthetic data set and the Alberta Foothills synthetic data set were migrated and superior depth images were achieved.; P-P prestack depth imaging techniques can be conveniently applied to converted-wave data based on the primary-only P-S wave propagation model. Prestack P-S shot gather migration with the dual algorithm produced a very good depth image for the 1997 Blackfoot 3C-2D survey.; The concept of downward-continuation migration velocity analysis (DMVA) is proposed. It can be used to partially eliminate the assumption of laterally invariant velocity in the established migration velocity analysis techniques and hence provide a better velocity estimation.
机译:提出了非平稳积分波场外推器的实际并行实现。实现了窗口分割步算法和完全积分算法两种方法。积分外推器适用于大步长波场外推,即使横向速度变化较大,但前提是静态相移速度和聚焦相移速度分别用时间平均和深度平均速度代替。由大步外推算法产生的参考波场之间的线性垂直波场插值可用于计算中间深度图像。这种双重算法大大减少了积分波场外推器的运行时间。即使存在严重的地形变化和较高的近地表速度,非平稳外推器也能够对大倾角和较深的事件进行浅层成像。迁移了Marmousi综合数据集和Alberta Foothills综合数据集,并获得了较高的深度图像。可以将P-P叠前深度成像技术基于仅主要的P-S波传播模型方便地应用于转换波数据。使用双重算法进行的叠前P-S镜头集集偏移,为1997年Blackfoot 3C-2D勘测产生了非常好的深度图像。提出了向下连续迁移速度分析(DMVA)的概念。它可以用来部分消除已建立的迁移速度分析技术中横向不变速度的假设,从而提供更好的速度估计。

著录项

  • 作者

    Mi, Yanpeng.;

  • 作者单位

    University of Calgary (Canada).;

  • 授予单位 University of Calgary (Canada).;
  • 学科 Geophysics.
  • 学位 Ph.D.
  • 年度 2002
  • 页码 187 p.
  • 总页数 187
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 地球物理学;
  • 关键词

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