基于卷积神经网络的速度约束海洋大地电磁反演

Velocity constrained marine magnetotelluric inversion based on convolutional neural networks

  • 摘要: 海洋大地电磁的高分辨率反演一直都是海洋大地电磁测深领域的重要课题。为提高海洋大地电磁反演精度,本文利用海洋地震探测方法成像精度高的特点,将深部地震探测获得的速度结构作为先验信息加入到卷积神经网络大地电磁反演中,构建双通道数据作为反演网络的输入,实现基于速度约束的卷积神经网络大地电磁反演。基于本方法对南黄海千里岩区域地质概况建立数据集进行训练,模型研究表明,本方法能够提高卷积神经网络大地电磁反演精度,同时可提高垂向分辨能力,并且抗噪试验结果也表明该方法对于加噪数据集仍能实现较高分辨率的反演,这为海洋大地电磁高分辨率反演提供了一种新思路。

     

    Abstract: High-resolution marine magnetotelluric inversion has always been an important topic in the field of marine magnetotelluric sounding. To improve the accuracy of marine magnetotelluric inversion, by taking advantage of the high imaging accuracy of marine seismic detection methods, the velocity structure obtained by deep seismic detection as prior information was added into the convolutional neural network magnetotelluric inversion. By constructing two-channel data as input of inversion network, the velocity-constrained convolutional neural network magnetotelluric inversion was realized. Based on the proposed method, data sets established for geological profiles of the Qianliyan region in the South Yellow Sea were trained. Results show that the proposed method could improve the accuracy and the vertical resolution of the inversion. Moreover, the results of anti-noise tests also show that the proposed method could achieve higher resolution inversion for noisy data sets. This study provided a new idea for high-resolution marine magnetotelluric inversion.

     

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