基于卷积神经网络的速度约束海洋大地电磁反演OA
Velocity constrained marine magnetotelluric inversion based on convolutional neural networks
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.
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.
卢艳艳;裴建新;封常青;吴俊良
中国海洋大学海洋地球科学学院,青岛 266100中国海洋大学海洋地球科学学院,青岛 266100||中国海洋大学海底科学与探测技术教育部重点实验室,青岛 266100中国海洋大学海洋地球科学学院,青岛 266100中国海洋大学海洋地球科学学院,青岛 266100
海洋科学
卷积神经网络速度约束海洋大地电磁反演分辨能力
convolutional neural networkvelocity constraintmarine magnetotelluric inversionspatial resolution
《海洋地质与第四纪地质》 2026 (1)
114-122,9
山东省重点研发计划-重大科技创新工程项目"海洋矿产资源电磁探测和高光谱成像关键技术及设备研发"(2020CXGC010706)国家自然科学基金项目"海洋极低频电磁噪声产生机理及数据模型研究"(U2241201)国家自然科学基金面上项目"东沙海域海流感应电磁场特征及海流速度反演方法研究"(41974085)
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