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首页> 外文期刊>Journal of geophysics and engineering >Azimuth-opening angle domain imaging in 3D Gaussian beam depth migration
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Azimuth-opening angle domain imaging in 3D Gaussian beam depth migration

机译:3D高斯光束深度偏移中的方位角开口角域成像

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Common-image gathers indexed by opening angle and azimuth at imaging points in 3D situations are the key inputs for amplitude-variation-with-angle and velocity analysis by tomography. The Gaussian beam depth migration, propagating each ray by a Gaussian beam form and summing the contributions from all the individual beams to produce the wavefield, can overcome the multipath problem, image steep reflectors and, even more important, provide a convenient and efficient strategy to extract azimuth-opening angle domain common-image gathers (ADCIGs) in 3D seismic imaging. We present a method for computing azimuth and opening angle at imaging points to output 3D ADCIGs by computing the source and receiver wavefield direction vectors which are restricted in the effective region of the corresponding Gaussian beams. In this paper, the basic principle of Gaussian beam migration (GBM) is briefly introduced; the technology and strategy to yield ADCIGs by GBM are analyzed. Numerical tests and field data application demonstrate that the azimuth-opening angle domain imaging method in 3D Gaussian beam depth migration is effective.
机译:在3D情况下,通过成像点处的张开角度和方位角索引的共同图像集合是幅度振幅随角度变化和层析成像速度分析的关键输入。高斯光束深度迁移,以高斯光束形式传播每条射线,并汇总所有单个光束的贡献以产生波场,可以克服多径问题,使反射器成像陡峭,甚至更重要的是,提供了一种方便有效的策略提取3D地震成像中的方位角角度域共同图像集合(ADCIG)。我们提出了一种通过计算源和接收器波场方向矢量来计算成像点的方位角和张开角,以输出3D ADCIG的方法,这些矢量限制在相应高斯光束的有效区域内。本文简要介绍了高斯光束迁移(GBM)的基本原理。分析了GBM产生ADCIG的技术和策略。数值试验和现场数据应用表明,方位角开角域成像方法在3D高斯光束深度偏移中是有效的。

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