用信号先验融合纹理模型,提升地震层位追踪精度。
Contrastive Learning for Seismic Horizon Tracking with Domain-Specific Priors

- 用反射坡度生成可靠对应关系作为先验,指导深度模型训练
- 在真实与合成数据上均低于无监督基线的平均绝对误差
- 适合需要高精度层位追踪但标注成本高的地质场景
无监督三维地震层位追踪面临核心挑战:基于信号的传播器虽能实现精确的道级对齐,但在断层附近常失效;而基于纹理的深度模型虽对不连续性更鲁棒,通常需大量标注数据且道级精度下降。本文提出一种自监督融合方法,将信号导出的局部层位对应关系作为领域特定先验,训练纹理驱动的深度学习模型。具体地,通过反射坡度估计可靠的道间流场,用于构建对比学习中的正样本对,并仅在高置信度区域训练,可选地结合断层掩码。目标并非推断断层附近的模糊对应,而是保持断层处层位身份的一致性。结果表明,网络学习到的体素嵌入既保留局部信号连续性,又可通过相似性搜索实现断层外的层位传播。在公开的F3数据集和带断层的合成数据集上的实验显示,该方法的平均绝对误差(MAE)低于无监督基线,且与使用单个标注切片的半监督方法性能相当。
原文摘要 · Abstract (English)
Unsupervised 3D seismic horizon tracking faces a key limitation: signal-based propagators provide accurate trace-level alignment but often fail near faults, whereas texture-driven deep models are more robust to discontinuities, typically at the cost of labeled data requirements and reduced trace-level precision. We propose a self-supervised fusion of both paradigms in which signal-derived local horizon correspondences act as domain-specific priors to train a texture-based deep learning model. Specifically, we estimate reliable trace-to-trace flows from reflector slopes and use them to form positive pairs in a contrastive objective, while restricting training to high-confidence neighborhoods, optionally augmented with a fault mask. The objective is not to infer ambiguous correspondences close to discontinuities, but to preserve horizon identity across them. As a result, the network learns voxel-wise embeddings that preserve local signal continuity while enabling horizon propagation beyond discontinuities through similarity search. Experiments on the public F3 dataset and a faulted synthetic dataset achieve lower mean absolute error (MAE) than unsupervised baselines and competitive performance against a semi-supervised method using a single labeled slice.
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