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PRESTACK PLANE-WAVE KIRCHHOFF MIGRATION IN LATERALLY VARYING MEDIA

机译:横向变化介质中的前波平面波基尔霍夫偏移

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Conventional Kirchhoff migration methods are applied to seismograms in the offset-time (x - t) domain. We describe the theory, numerical details, and examples of a prestack depth migration method in the plane-wave domain that is valid in laterally inhomogeneous media. The theory is based on a Kirchhoff-Helmholtz formulation of the wavefield and uses plane-wave-transformed shot gathers for migration. We use geometric ray theory for the source wavefield continuation operator and a plane-wave expansion of the receiver wavefield in the integrand of the Kirchhoff-Helmholtz integral. The source and receiver plane-wave traveltimes are computed at each grid point in the subsurface using a finite-difference approximation of the eikonal equation with appropriate initial and boundary conditions. We developed an efficient technique to compute imaging time by a combination of these two times. The technique allows us to design algorithms for migrating shot gather or constant ray-parameter sections efficiently. We evaluate the efficiency and accuracy of the algorithm with three sets of synthetic data examples with varying degrees of complexity. We also compare the performance of the parallel algorithms using Parallel Virtual Machine (PVM). Migration of a marine data set results in excellent images of a mud volcano and the top of an accretionary prism of an active continental margin on the Nicoya Peninsula of Costa Rica. [References: 20]
机译:常规的Kirchhoff偏移方法应用于偏移时间(x-t)区域的地震图。我们在平面波域中描述了在横向非均匀介质中有效的叠前深度偏移方法的理论,数值细节和示例。该理论基于波场的Kirchhoff-Helmholtz公式,并使用经过平面波变换的散点集进行偏移。我们将几何射线理论用于源波场连续算符,并在Kirchhoff-Helmholtz积分的积分中将接收器波场的平面波扩展。在适当的初始条件和边界条件下,使用标准方程的有限差分近似,可以计算出地下每个网格点的源和接收器平面波传播时间。我们开发了一种有效的技术来结合这两次来计算成像时间。该技术使我们能够设计算法,以有效地迁移镜头集或恒定的射线参数部分。我们使用复杂程度不同的三组合成数据示例评估算法的效率和准确性。我们还比较了使用并行虚拟机(PVM)的并行算法的性能。海洋数据集的迁移产生了出色的火山泥图像以及哥斯达黎加尼科亚半岛活跃大陆边缘增生棱镜的顶部。 [参考:20]

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