Research on Seismic Velocity Inversion Method Based on Deep Learning

XU Wang, Wang Feiyi, Zhiqiang Zhang, Gongli Liu, Duan Xinyi
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Abstract

Methods for obtaining seismic velocity include offset velocity analysis, tomography velocity inversion and full waveform. inversion, but these methods all share common problems: As the amount of seismic data increases, the time required to process the data to obtain the seismic velocity increases exponentially, and the latter two methods are more dependent on the initial seismic velocity. To address the problems of the above methods, this paper improves a seismic velocity inversion method based on deep learning. At the same time, a method that can generate a large number of velocity models randomly with geological features (undulation layer, faults, anomalies, etc. ) similar to those of real subsurface structures is also proposed. The generated velocity model and fluctuation equation for forward modeling are used to perform. the forward modeling, which allows for the efficient establishment of data set. The basic principle of the improved deep learning inversion method in this paper is as follows: the characteristic information of the training data is extracted by convolution neural network, which is trained with large data to obtain a nonlinear mapping relationship between seismic record and seismic velocity. In the inversion stage, the seismic velocity can be inversed quickly by inputting the seismic records into the trained network. In order to make the network give full play to the advantages of processing seismic data, the authors obtained the dominant network structure by means of numerical simulation, and achieved satisfactory inversion results. Finally, through comparative experiments, this paper verifies the advantages and applicability of the method.
基于深度学习的地震速度反演方法研究
地震速度的获取方法包括偏移速度分析、层析速度反演和全波形。但这些方法都有一个共同的问题:随着地震数据量的增加,处理数据获得地震速度所需的时间呈指数增长,后两种方法更依赖于地震初始速度。针对上述方法存在的问题,本文改进了一种基于深度学习的地震速度反演方法。同时,提出了一种能够随机生成大量具有与真实地下构造相似地质特征(起伏层、断层、异常等)的速度模型的方法。利用生成的速度模型和波动方程进行正演模拟。采用正演建模,可以有效地建立数据集。本文改进的深度学习反演方法的基本原理是:通过卷积神经网络提取训练数据的特征信息,利用大数据对其进行训练,得到地震记录与地震速度的非线性映射关系。在反演阶段,通过将地震记录输入训练好的网络,可以快速反演地震速度。为了使网络充分发挥地震资料处理的优势,通过数值模拟的方法获得了优势网络结构,并取得了满意的反演结果。最后,通过对比实验,验证了该方法的优越性和适用性。
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