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Cost effective prestack depth imaging of marine data

机译:具有成本效益的海洋数据叠前深度成像

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Common-azimuth imaging can significantly reduce the cost of full-volume 3-D prestack depth imaging of marine data sets. The common-azimuth imaging procedure comprises of two steps: first, transformation of the prestack data to common azimuth data by azimuth moveout (AMO); second, imaging the transformed data by common-azimuth migration. Both these steps are computationally efficient. AMO is a partial migration operator and thus it has narrow spatial aperture. Common-azimuth migration is based on downward continuation of the wavefield; therefore, its computational cost increases only as the square of the image depth. In contrast, the cost of conventional Kirchhoff migration is proportional to the cube of the image depth.Because it is a wavefield-continuation method, common-azimuth migration does not require the computation of asymptotic Green functions. Therefore, common-azimuth imaging is likely to overcome some of the accuracy problems encountered by Kirchhoff migration in the presence of complex wave-propagation phenomena.The proposed common-azimuth imaging procedure successfully depth imaged a marine data set recorded in the North Sea. These positive results suggest the application of common-azimuth imaging to velocity estimation based on wavefield focusing.
机译:共方位角成像可以显着降低海洋数据集的全尺寸3D叠前深度成像的成本。共方位成像过程包括两个步骤:首先,通过方位角偏移(AMO)将叠前数据转换为共方位数据。其次,通过共方位角偏移对变换后的数据进行成像。这两个步骤在计算上都是有效的。 AMO是部分迁移算子,因此它的空间孔径很窄。共方位角偏移是基于波场的向下连续性。因此,其计算成本仅随着图像深度的平方而增加。相比之下,常规Kirchhoff迁移的成本与图像深度的立方成正比。 因为它是一种波场连续方法,所以共方位偏移不需要渐近格林函数的计算。因此,在存在复杂的波传播现象的情况下,共方位角成像可能会克服Kirchhoff偏移所遇到的一些精度问题。 所提出的共方位角成像程序成功地对在北海记录的海洋数据集进行了深度成像。这些积极的结果表明共方位成像技术在基于波场聚焦的速度估计中的应用。

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