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3D TRUE-AMPLITUDE PRESTACK DEPTH MIGRATION

机译:3D真振幅前景深度迁移

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The angle-dependent reflectivity of a reservoir target is crucial input for reservoir characterization. 3D prestack depth migration should be able to produce not only an accurate structural image, but also reliable angle-dependent amplitude information. However, none of the currently available 3D migration algorithms satisfy this requirement. Geometrical spreading is the only consideration in most existing true-amplitude migrations; intrinsic attenuation, and transmission losses also distort the wavefield amplitudes during propagation through the earth. We develop an integrated algorithm that compensates all three of these factors, in a two-pass recursive reverse-time 3D prestack depth migration. Applications to 3D synthetic models demonstrate production of both high quality subsurface images and angle-dependent (prestack) reflection coefficients at the target. The velocity ratio at the target is also obtained by least square fitting over the estimated angle-dependent reflection coefficients. Because of the nature of reverse-time migration and the recursive procedure, the 3D algorithm is computationally and memory intensive. However, for application to real seismic data, 3D true amplitude processing is necessary.
机译:储层目标的角度相关反射率是表征储层的关键输入。 3D叠前深度偏移不仅应能够生成准确的结构图像,而且还应生成可靠的角度相关振幅信息。但是,当前没有可用的3D迁移算法满足此要求。在大多数现有的真振幅偏移中,几何扩展是唯一考虑的因素。固有衰减和传输损耗也会使通过地球传播的波场幅度失真。我们开发了一种集成算法,可在两次遍历递归逆时3D叠前深度偏移中补偿所有这三个因素。在3D合成模型中的应用演示了在目标处产生高质量的地下图像和角度相关(叠前)反射系数的情况。还可以通过对估计的角度相关反射系数进行最小二乘拟合来获得目标处的速度比。由于逆时迁移和递归过程的性质,3D算法需要大量的计算和内存。但是,为了应用于真实地震数据,必须进行3D真实振幅处理。

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