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    沉积相约束下的多方位属性融合砂体识别方法

    Sedimentary facies-constrained multi-azimuth attribute fusion for sand body identification

    • 摘要: 针对河潮联控背景下储层横向变化快、岩性圈闭边界识别困难的问题,提出了一种基于海底节点地震数据的储层预测方法。该方法在沉积相带约束下,以地下共反射点为基本计算单元,突破传统大套河道分析的尺度局限,自动提取优势方位角度以优化方位划分方案。在此基础上,开展分方位储层敏感参数反演,获取多方位属性数据体,精准求取各向异性优势方位。进一步,构建多方位属性融合的全局寻优目标函数,自适应确定权重分配参数,融合全方位高信噪比特征与分方位差异性信息。实际应用结果表明,该方法显著提高复杂砂体边界的刻画精度,融合结果与沉积相展布特征吻合良好,为复杂潮控储层的勘探开发提供可靠依据,对宽方位地震资料储层预测研究具有推广价值。

       

      Abstract: To address the challenges of rapid lateral reservoir variations and difficulty in identifying lithologic trap boundaries in fluvial-tidal coupled environments, this paper proposes a reservoir prediction method based on ocean bottom node (OBN) seismic data. Using common reflection points as the basic computational units within sedimentary facies zones, this method overcomes the scale limitations of traditional channel analysis by automatically extracting dominant azimuths to optimize azimuth division. On this basis, azimuth-specific inversion of reservoir-sensitive parameters is performed to obtain multi-azimuth attribute volumes, enabling accurate determination of dominant anisotropic orientations. To further integrate the high signal-to-noise ratio of full-azimuth data with the strong anisotropic information from divided azimuths, a global optimization objective function for multi-azimuth attribute fusion is constructed to adaptively determine weighting parameters. Application results demonstrate that the proposed method significantly improves the delineation accuracy of complex sand body boundaries, with fusion results showing strong agreement with sedimentary facies distribution. This provides a reliable basis for the exploration and development of complex tide-dominated reservoirs and offers valuable insights for reservoir prediction using wide-azimuth seismic data.

       

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