融合Transformer与多尺度注意力机制的地震数据重建方法OA
A seismic data reconstruction method integrating Transformers and multi-scale attention mechanisms
在山地地震勘探数据采集过程中,受地表条件及经济成本等因素限制,所采集的地震数据易存在因道缺失导致的空间不连续问题,严重影响后续的偏移成像与解释精度.针对传统插值方法在复杂构造处重建精度低,以及常规卷积神经网络(Convolutional Neural Network,CNN)难以捕捉地震波场全局长距离依赖关系的局限性,笔者提出一种融合 Transformer与多尺度注意力机制(Convolutional Block Attention Module,CBAM)的改进 U-Net3+地震数据插值方法.该方法以 U-Net3+为基础架构,利用全尺度跳跃连接实现多尺度特征的深度融合;在编码器末端引入 Transformer模块,通过自注意力机制有效建模地震信号的全局上下文信息,弥补卷积操作感受野受限的不足;同时在跳跃连接处嵌入 CBAM注意力模块,自适应地增强有效波场特征并抑制背景噪声.在二维理论合成地震记录及实际地震数据上的实验结果表明,该方法在 50%随机缺失率下仍能高质量地重建地震记录.相较于传统的 U-Net系列方法,本文方法在定量指标上优势明显:用于评估信号重建误差的峰值信噪比(Peak Signal-to-Noise Ratio,PSNR)最高提升达31.08%(5.89 dB),用于衡量波场同相轴等空间特征相似度的结构相似性指数(Structural Similarity Index Measure,SSIM)最高提升达 30.20%.该方法显著增强了地震数据的波场保真度,且能更清晰地恢复断层、不整合面等复杂地质纹理,具有较强的鲁棒性和实用价值.
During seismic data acquisition in mountainous regions,constraints such as surface conditions and economic costs often result in spatial discontinuities caused by missing traces in the collected seismic data,which severely compromise the accuracy of subsequent seismic reflection imaging and interpretation.To address the limitations of traditional interpolation methods—which suffer from low reconstruction accuracy in complex structural areas—and the difficulty of conventional Convolutional Neural Networks(CNNs)in capturing the global long-range dependencies of seismic wavefields,this paper proposes an improved U-Net3+seismic data interpolation method that integrates the Transformer architecture with a multi-scale attention mechanism(Convolutional Block Attention Module,CBAM).This method uses U-Net3+as its base architecture and employs full-scale skip connections to achieve deep integration of multi-scale features.A Transformer module is introduced at the end of the encoder to effectively model global contextual information in seismic signals via self-attention mechanisms,compensating for the limited receptive field of convolutional operations.Additionally,CBAM attention modules are embedded in the skip connections to enhance effective wavefield features while adaptively suppressing background noise.Experimental results on two-dimensional synthetic seismic records and real seismic data demonstrate that this method can still reconstruct seismic records with high quality even under a 50%random missing rate.Compared to traditional U-Net-based methods,the method proposed in this paper demonstrates significant advantages in quantitative metrics:the Peak Signal-to-Noise Ratio(PSNR),used to evaluate signal reconstruction error,improves by up to 31.08%(5.89 dB),and the Structural Similarity Index Measure(SSIM),used to assess the similarity of spatial features such as wavefield in-phase axes,improves by up to 30.20%.This method significantly enhances the wavefield fidelity of seismic data and can more clearly reconstruct complex geological features such as faults and unconformities,demonstrating strong robustness and practical value.
刘芳;李怀良;杨李欣
成都理工大学 地球物理学院,成都 610059成都理工大学 地球物理学院,成都 610059||成都理工大学 地质灾害防治与地质环境保护国家重点实验室,成都 610059成都理工大学 地球物理学院,成都 610059
天文与地球科学
地震数据插值深度学习U-Net3+波场重建
seismic data interpolationdeep learningU-Net3+wavefield reconstruction
《物探化探计算技术》 2026 (4)
499-513,15
四川省青年科学基金1001-1749B1001-1749类(No.2026NSFSC1134)中国国家自然科学基金面上项目(No.42474199)四川省青年科技创新团队项目(No.2026NSFSCZY0058)
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