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    基于改进V-Net与自适应难样本挖掘的三维地震断层智能识别

    Intelligent 3D seismic fault identification based on improved V-Net and adaptive hard example mining

    • 摘要: 三维地震断层的准确识别是地震解释中的关键技术难题。传统的人工解释方法效率低且主观性强,而现有的深度学习方法在断层不连续性识别和样本不平衡处理方面仍存在不足。为此,提出了一种基于改进V-Net与自适应难样本挖掘的三维地震断层智能识别方法。首先,鉴于传统V-Net中反卷积上采样会产生棋盘伪影,采用卷积通道变换结合最近邻插值的改进上采样策略,有效消除了伪影对断层边界特征的干扰,提升了小尺度断层和断层边界的识别精度,同时减少了参数冗余,降低了计算成本。其次,针对地震数据中断层样本稀疏、边界模糊等问题,设计了融合地质先验知识的自适应难样本挖掘损失函数;该函数通过动态阈值机制识别困难样本,并对断层区域实施差异化权重策略,使模型能够充分学习断层的细节特征,有效缓解了因断层样本稀少导致的训练不平衡问题。同时,引入连续性约束项,通过梯度惩罚机制确保断层预测结果的地质合理性。合成数据和实际地震数据测试结果表明,改进V-Net与自适应难样本挖掘的三维地震断层智能识别方法在断层检测精度、连续性和泛化能力方面均优于传统V-Net,其F1(F1-score)分数达到0.7962,平均交并比(mIoU)达到0.7891。该方法不仅为三维地震断层自动识别提供了新的技术途径,也为深度学习在地球物理勘探中的应用拓展了思路。

       

      Abstract: Accurate 3D fault identification remains a key technical challenge in seismic interpretation. Traditional manual interpretation methods are inefficient and highly subjective, while existing deep learning-based approaches suffer from incomplete fault continuity characterization and sample imbalance. To address these issues, we propose a 3D seismic fault intelligent recognition method based on an improved V-Net architecture and adaptive hard example mining. The architecture adopts an improved upsampling strategy that combines convolutional channel transformation with nearest-neighbor interpolation to address the checkerboard artifacts introduced by deconvolution-based upsampling in conventional V-Net. This strategy effectively mitigates the interference of artifacts on fault boundary features, improves the recognition accuracy of small-scale faults and fault boundaries, and simultaneously reduces parameter redundancy and computational cost. To tackle the challenges of sparse fault samples and ambiguous boundaries in seismic data, we design an adaptive hard example mining loss function that incorporates geological prior knowledge. This loss function employs a dynamic threshold mechanism to identify hard examples and applies a differentiated weighting strategy to fault regions, enabling the model to more effectively learn fine-scale fault features and alleviate the imbalance caused by the scarcity of fault samples. Additionally, a continuity constraint term implemented via gradient penalty is introduced to ensure the geological plausibility of the predicted fault structures. Experimental results on both synthetic and field seismic data demonstrate that the proposed method achieves superior accuracy, continuity, and generalization compared with the conventional V-Net, with an F1 score of 0.7962 and a mIoU of 0.7891. This work provides a new technical pathway for automatic 3D seismic fault identification and broadens the application potential of deep learning in geophysical exploration.

       

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