地震相智能识别方法研究进展

Advances in research on methods for intelligent identification of seismic facies

  • 摘要:
    背景 地震相智能识别可显著提升沉积体系刻画与油气储层解释效率,但受地质体非平稳性、样本标注成本高与训练样本不足等因素影响,传统方法往往难以兼顾识别精度与推广应用需求。
    进展 系统梳理地震相智能识别的无监督、有监督与半监督/深度学习三类技术路线,并以亚马逊地区东部实际工区三维地震资料开展对比验证。无监督聚类(K均值、自组织映射、生成拓扑映射等)可快速揭示地震相相对分布格局,但对参数与初始化敏感,且需要地质约束与人工赋相,难以形成稳定、可量化的井控精度对标体系。有监督学习中,人工神经网络、支持向量机与随机森林在9口井验证下的宏平均准确率分别为79.11%、81.56%与85.78%。深度学习方面,改进型深度扩张卷积网络总体精度为91.56%,Cohen’s Kappa为90.35%,空间连续性与边界刻画能力明显增强。半监督学习在低标注条件下优势更为突出:半监督深度自编码器总体精度92.67%、Kappa 91.56;半监督对比学习总体精度91.33%、Kappa 88.97;在相近精度水平下,所需标注比例可由10%~15%降低至3%~4%。
    展望 未来应进一步融合地质先验与可解释机制,发展自监督/对比预训练、跨数据分布自适应与不确定性量化的质量控制流程,提升复杂地质条件下的稳健性与工程可用性。实验进一步表明:在“标注成本高、样本少”的典型工业约束下,半监督学习能够以显著更少的标注样本维持高精度识别效果,从而为工业界提供明确且高效的技术选型方向,支撑地震相智能识别的规模化应用与推广。

     

    Abstract:
    Background The intelligent identification of seismic facies can significantly improve the efficiency of sedimentary system characterization and hydrocarbon reservoir interpretation. However, influenced by factors such as non-stationary geological bodies, high costs of sample labeling, and limited training samples, conventional methods for intelligent identification are generally insufficient to achieve high identification accuracy and widespread application concurrently.
    Advances  This study presents a systematic review of three types of technologies for the intelligent identification of seismic facies, namely unsupervised, supervised, and semi-supervised learning, with each type including deep learning methods. The three technological types are comparatively verified using 3D seismic data from a practical survey area in the eastern Amazon region. The results indicate that unsupervised clustering methods, including K-means, self-organizing map (SOM), and generative topographic mapping (GTM), can rapidly reveal the relative distribution patterns of seismic facies. However, these methods are sensitive to parameter setting and initialization while also relying on geological constraints and manual facies assignment typically. These limitations pose challenges in establishing a stable and quantifiable well-tied accuracy benchmarking system. In terms of the supervised learning technology, the validation results based on nine wells indicate that the artificial neural network (ANN), support vector machine (SVM), and random forest (RF) methods yielded macro-averaged accuracies of 79.11%, 81.56%, and 85.78%, respectively. Among the deep learning algorithms in the supervised learning technology, the improved deep dilated convolutional neural network (DDCNN) exhibited an overall accuracy of 91.56%, Cohen's Kappa of 90.35%, and significantly enhanced capacities to characterize the spatial continuity and facies boundaries of seismic profiles. In contrast, semi-supervised learning delivers more pronounced advantages under conditions of limited labels. Specifically, the semi-supervised deep auto-encoder (SSDAE) yielded an overall accuracy of 92.67% and Cohen's Kappa of 91.56%, while the semi-supervised contrastive learning (SSCL) model exhibited an overall accuracy of 91.33% and Cohen's Kappa of 88.97%. Compared to that of the SSDAE, the required labeling ratio of the SSCL model can be reduced from approximately 10%–15% to 3%–4% under comparable accuracy.
    Prospects  In the future, it is necessary to further integrate geological prior knowledge and interpretable mechanisms, as well as developing self-supervised/contrastive pretraining, the adaptation to cross-data distribution, and the quality control process of uncertainty quantification. These efforts are expected to enhance the robustness and engineering application of the intelligent identification of seismic facies under complex geological conditions. The experimental results further indicate that under typical industrial constraints of high labeling costs and limited samples, semi-supervised learning can maintain high accuracy in the identification of seismic facies using substantially fewer labeled samples. This finding offers a definite and efficient direction for technology selection, thereby supporting the large-scale application of the intelligent identification of seismic facies.

     

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