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首页> 外文期刊>IEEE Transactions on Geoscience and Remote Sensing >Joint Inversion of Audio-Magnetotelluric and Seismic Travel Time Data With Deep Learning Constraint
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Joint Inversion of Audio-Magnetotelluric and Seismic Travel Time Data With Deep Learning Constraint

机译:具有深度学习约束的音频 - 磁音和地震行程时间数据的联合反演

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摘要

Deep learning is applied to assist the joint inversion for audio-magnetotelluric and seismic travel time data. More specifically, deep residual convolutional neural networks (DRCNNs) are designed to learn both structural similarity and resistivity-velocity relationships according to prior knowledge. During the inversion, the unknown resistivity and velocity are updated alternatingly with the Gauss-Newton method, based on the reference model generated by the trained DRCNNs. The workflow of this joint inversion scheme and the design of the DRCNNs are explained in detail. Compared with describing the resistivity-velocity relationship using empirical equations, this method can avoid the necessity in modeling the correlations in rigorous mathematical forms and extract more hidden prior information embedded in the training set, meanwhile preserving the structural similarity between different inverted models. Numerical tests show that the inverted resistivity and velocity have similar profiles, and their relationship can be kept consistent with the prior joint distribution. Furthermore, the convergence is faster, and final data misfits can be lower than separate inversion.
机译:深入学习应用于协助音频 - 磁能和地震行程数据的联合反演。更具体地,深剩余卷积神经网络(DRCNNS)旨在根据先前知识来学习结构相似性和电阻率 - 速度关系。在反转期间,基于由训练的DRCNNS产生的参考模型,通过Gauss-Newton方法交替更新未知电阻率和速度。详细解释了这种联合反演方案的工作流程和DRCNN的设计。与使用经验方程描述电阻率 - 速度关系相比,该方法可以避免在嵌入训练集中的严格数学形式和提取更多隐藏的先前信息的情况下建模相关性的必要性,同时保留不同反相模型之间的结构相似性。数值测试表明,倒置电阻率和速度具有相似的轮廓,并且它们的关系可以与现有的接头分布保持一致。此外,收敛速度更快,最终数据不足可能低于单独的反转。

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