Fully Reversible Neural Networks for Large-Scale 3D Seismic Horizon Tracking

B. Peters, E. Haber
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引用次数: 4

Abstract

Tracking a horizon in seismic images or 3D volumes is an integral part of seismic interpretation. The last few decades saw progress in using neural networks for this task, starting from shallow networks for 1D traces, to deeper convolutional neural networks for large 2D images. Because geological structures are intrinsically 3D, we hope to see improved horizon tracking by training networks on 3D seismic data cubes. While there are some 3D convolutional neural networks for various seismic interpretation tasks, they are restricted to shallow networks or relatively small 3D inputs because of memory limitations. The required memory for the network states and weights increases with network depth. We present a fully reversible network for horizon tracking that has a memory requirement that is independent of network depth. To tackle memory issues regarding the network weights, we use layers that train in a factorized form directly. Therefore, we can maintain a large number of network channels while keeping the number of convolutional kernels low. We use the saved memory to increase the input size of the data by order of magnitude such that the network can better learn from large structures in the data. A field data example verifies the proposed network structure is suitable for seismic horizon tracking.
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大尺度三维地震层位跟踪的全可逆神经网络
在地震图像或三维体中跟踪水平是地震解释的一个组成部分。在过去的几十年里,在这项任务中使用神经网络取得了进展,从用于1D轨迹的浅层网络到用于大型2D图像的深层卷积神经网络。由于地质结构本质上是三维的,我们希望通过在三维地震数据立方体上训练网络来改进层位跟踪。虽然有一些3D卷积神经网络用于各种地震解释任务,但由于内存限制,它们仅限于浅层网络或相对较小的3D输入。网络状态和权值所需的内存随着网络深度的增加而增加。我们提出了一种完全可逆的水平跟踪网络,它具有独立于网络深度的记忆需求。为了解决与网络权重有关的内存问题,我们使用直接以分解形式训练的层。因此,我们可以在保持低卷积核数量的同时保持大量的网络通道。我们使用节省的内存以数量级增加数据的输入大小,以便网络可以更好地从数据中的大型结构中学习。现场数据算例验证了所提出的网络结构适用于地震层位跟踪。
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