基于并行gpu的单向波动方程迁移实现

A. Pleshkevich, V. Lisitsa, D. Vishnevsky, V. Levchenko, B. Moroz
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引用次数: 1

摘要

基于单向波动方程的深度波场外推,提出了一种新颖的地震成像算法。该算法的并行实现是基于几个层次的并行性。输入数据的并行性允许处理某些区域(最多一平方公里)的全覆盖;因此,数据被分成几个子集,每个子集由单个MPI进程处理。数学方法允许独立处理每个频率,并逐层处理解决方案;因此,同时处理一组2D横截面而不是初始的3D共偏移矢量集。这部分算法是在GPU上实现的。接下来,每个共偏移矢量图像可以单独堆叠、处理和存储。因此,我们设计并实现了基于CPU-GPU架构的并行算法,该算法允许使用基于单向波方程的保幅偏移来计算共偏移矢量图像。将该算法应用于实际地震地表数据的地震图像计算。
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Parallel GPU-based Implementation of One-Way Wave Equation Migration
We present an original algorithm for seismic imaging, based on the depth wavefield extrapolation by the one-way wave equation. Parallel implementation of the algorithm is based on the several levels of parallelism. The input data parallelism allows processing full coverage for some area (up to one square km); thus, data are divided into several subsets and each subset is processed by a single MPI process. The mathematical approach allows dealing with each frequency independently and treating solution layer-by-layer; thus, a set of 2D cross-sections instead of the initial 3D common-offset vector gathers are processed simultaneously. This part of the algorithm is implemented suing GPU. Next, each common-offset vector image can be stacked, processed and stored independently. As a result, we designed and implemented the parallel algorithm based on the use of CPU-GPU architecture which allows computing common-offset vector images using one-way wave equation-based amplitude preserving migration. The algorithm was used to compute seismic images from real seismic land data.
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