Incorporating wave physical priors into diffusion models: A novel approach to seismic resolution enhancement
将波动物理先验融入扩散模型:一种提高地震分辨率的新方法
Huanhuan Tang, Shijun Cheng, Weijian Mao, Haoran Zhang, Yingying Zhang
AI总结 提出物理引导的自监督扩散模型(PG-SSDM),通过自监督训练、地震卷积模型硬约束和不确定性量化,无需配对高分辨率标签即可提升地震数据分辨率。
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地震分辨率增强仍然是勘探地球物理学中的一个关键挑战,特别是在处理带宽有限、噪声强且标记训练样本不足的野外数据时。现有的深度学习方法通常依赖合成训练数据的监督学习,导致分布不匹配,在真实地震采集数据上泛化能力差。为了解决这些局限性,我们开发了一种物理引导的自监督扩散模型(PG-SSDM),该模型直接从野外观测中学习,无需配对的高分辨率标签。所提出的框架结合了三个关键创新。首先,自监督训练策略通过逐步滤波观测数据本身来构建学习目标,通过多阶段迭代细化消除了对高分辨率真实值的需求。其次,地震卷积模型作为硬物理约束嵌入到训练损失函数和反向采样过程中,确保生成的高分辨率输出符合基本的地震波传播物理规律。第三,扩散模型的概率性质实现了不确定性量化,提供了空间置信度图,用于识别分辨率增强可能不太可靠的区域。我们在各种噪声条件下的合成数据以及一个三维叠后野外数据集上验证了PG-SSDM。实验结果表明,所提出的方法能够有效恢复薄层和细微结构,抑制噪声,保持结构连续性,从而显著提高地震数据的分辨率和可解释性。
Seismic resolution enhancement remains a critical challenge in exploration geophysics, particularly when processing field data characterized by limited bandwidth, strong noise, and insufficient labeled training samples. Existing deep learning methods typically rely on supervised learning with synthetic training data, leading to distribution mismatch and poor generalization on real seismic acquisitions. To address these limitations, we develop a physics-guided self-supervised diffusion model (PG-SSDM) that learns directly from field observations without requiring paired high-resolution labels. The proposed framework combines three key innovations. First, a self-supervised training strategy constructs learning targets by progressively filtering the observed data itself, eliminating the need for high-resolution ground truth through iterative refinement across multiple stages. Second, seismic convolution model is embedded as a hard physical constraint in both the training loss function and the reverse sampling process, ensuring that generated high-resolution outputs respect fundamental seismic wave propagation physics. Third, the probabilistic nature of diffusion models enables uncertainty quantification, providing spatial confidence maps that identify regions where resolution enhancement may be less reliable. We validate PG-SSDM on synthetic data under various noise conditions and on a 3D post-stack field dataset. Experimental results demonstrate that the proposed method effectively recovers thin layers and subtle structures, suppresses noise, preserves structural continuity, thereby significantly improving the resolution and interpretability of seismic data.