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共方位角波动方程偏移速度分析方法及其应用 被引量:6

Common angle wave equation migration velocity analysis method and application
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摘要 叠前深度偏移是复杂地质构造成象的有力工具,其成象的质量主要取决于所用速度—深度模型的精度。本文根据波场外推理论,给出了层剥离波动方程偏移速度分析方法。该方法利用沿层剩余速度分析直接修改层速度,适用于3D偏移速度分析,已在复杂潜山构造成象中取得较好的效果。 Prestack depth migration is a good tool imaging complex geologic structure. Imaging quality depends mainly onthe precision of used velocity-depth model. Migration velocity analysis method of formation baring wave equation isgiven according to wave field extrapolation theory. The method uses residual velocity of edge-formation to modify di-rectly horizon velocity, which is suitable for 3D migration velocity analysis. The method has been used for imagingcomplex burial hill structure with better effect.
出处 《油气地球物理》 2003年第3期22-25,共4页 Petroleum Geophysics
关键词 共方位角波动方程 偏移速度分析 叠前深度偏移 地质构造成象 地震勘探 地震资料 common angle, wave equation, migration velocity analysis, velocity -depth model
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参考文献6

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同被引文献38

  • 1杨淑卿,王华忠,程玖兵,马在田,孟祥宾,胡中标.基于地质层位约束的2D波动方程偏移速度分析方法[J].油气地球物理,2003,1(4):19-22. 被引量:2
  • 2潘宏勋,方伍宝.地震速度分析方法综述[J].勘探地球物理进展,2006,29(5):305-311. 被引量:59
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