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    基于煤田三维地震数据的小断层智能识别技术研究进展

    Research progress in small-fault intelligent identification based on 3D seismic data of coal field

    • 摘要: 煤田小断层是煤与瓦斯突出、矿井突水等地质灾害的直接诱因,对其进行精准识别与精细刻画具有重要的理论意义与应用价值。长期以来,小断层识别主要依赖于传统的构造解释,之后发展了利用相干体、方差体、曲率等地震属性进行断层解释的方法,但在资料信噪比低、地震地质条件复杂等情况下存在漏判、误判等问题。近年来,随着机器学习和深度学习技术在地震资料解释中的应用,基于支持向量机(Support Vector Machine, SVM)、随机森林(Random Forest, RF)、卷积神经网络(Convolutional Neural Network, CNN)、循环神经网络(Recurrent Neural Network, RNN)、U-Net及其改进网络的人工智能方法,为小断层智能识别提供了新的思路。以小断层的传统地震属性解释—机器学习分类识别—深度学习端到端识别为主线,梳理基于煤田三维地震数据的小断层智能识别技术演进过程,剖析典型案例,重点讨论样本稀缺与煤层强反射背景下弱信号难以提取2类关键难题,并结合正演建模与数值模拟、数据增强与迁移学习、多属性联合输入及地质约束等思路,对煤田小断层智能识别技术的未来发展方向进行了展望。

       

      Abstract: Small faults in coal-fields are major triggers of geohazards, including coal-gas outbursts and mine water inrushes, and thus require accurate detection and fine-scale characterization. Conventional structural interpretation and seismic-attribute-based methods (e.g., coherence, variance, and curvature) often suffer from missed and false detections under low signal-to-noise ratios and complex geological settings. Recent advances in machine learning and deep learning — spanning SVM and random forests to CNN/RNN models and U-Net variants — have enabled increasingly automated small-fault identification from 3D seismic data. The evolution from attribute-driven interpretation to data-driven classification and end-to-end detection is summarized, representative studies are highlighted, and two key challenges are discussed: limited labeled samples and weak fault signatures masked by strong coal-seam reflections. Future directions are outlined, including physics-informed forward modeling, data augmentation and transfer learning, multi-attribute fusion, and geology-constrained interpretation.

       

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