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    瞬时谱相位分解方法及隐蔽河道砂体识别应用

    Instantaneous Spectral Phase Decomposition Method and Application in Concealed Channel Sand Body Identification

    • 摘要: 传统地震储层预测,特别是针对薄互层河道砂体,频率域属性分析已取得了显著进展并得到了广泛应用。然而,在四川盆地蓬莱镇组等浅层沉积环境中,面对厚度接近地震分辨率极限、多期叠置且横向变迁频繁的薄层砂体,频率域方法因其对背景噪声敏感、对横向不连续边界刻画能力有限而逐渐显现瓶颈。本文在此基础上探索新的研究方法,聚焦于地震信号中蕴含丰富地质信息的相位属性,提出一种基于改进广义S变换的瞬时谱相位分解方法。该方法通过高精度时频分析提取瞬时振幅与相位谱,利用相位域分解技术将地震信号按特定相位区间进行重构,有效分离出被强背景噪声掩盖的、与薄层砂体相关的弱响应信号。在川西地区蓬莱镇组的应用表明,相较于传统均方根振幅属性图中河道的“断续消失”现象,分相位振幅属性能显著压制泥岩背景干扰,清晰刻画常规方法难以识别的窄河道与多期叠置河道边界,该方法能快速便捷实现相位分解,为薄层砂体的精细预测提供了相位域的有效补充,取得了显著的实际应用效果。

       

      Abstract: Traditional seismic reservoir prediction, especially for thin interbedded channel sand bodies, has made significant progress in frequency domain attribute analysis and has been widely used. However, in shallow sedimentary environments such as the Penglaizhen Formation in the Sichuan Basin, facing thin sand bodies with thickness close to the limit of seismic resolution, multi-stage superimposition and frequent lateral changes, the frequency domain method has gradually shown its bottleneck due to its sensitivity to background noise and limited ability to depict the lateral discontinuous boundary. On this basis, this paper explores a new research method, focusing on the phase attribute of seismic signals containing rich geological information, and proposes an instantaneous spectral phase decomposition method based on improved generalized S transform. This method extracts the instantaneous amplitude and phase spectrum through high-precision time-frequency analysis, and reconstructs the seismic signal according to the specific phase interval by using the phase domain decomposition technology, so as to effectively separate the weak response signal related to thin sand body covered by strong background noise. The application in Penglaizhen Formation in Western Sichuan shows that, compared with the "intermittent disappearance" phenomenon of the river channel in the traditional root mean square amplitude attribute map, the phase division amplitude attribute can significantly suppress the mudstone background interference, and clearly depict the narrow channel and multi-phase superimposed channel boundary that are difficult to identify by the conventional method. This method can quickly and conveniently realize the phase decomposition, which provides an effective supplement to the phase domain for the fine prediction of thin sand bodies, and has achieved significant practical application effect.

       

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