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A new extension of seismic instantaneous frequency using a fractional time derivative

机译:使用分数时间导数的地震瞬时频率的新扩展

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The seismic instantaneous frequency attribute has been applied to interpret a depositional layer. Instead of the standard instantaneous frequency, the Caputo fractional differential operator has been demonstrated as a more suitable mathematical tool of nonlinear analysis for the depositional layer. Based on the Caputo operator, we propose a fractional extension of instantaneous frequency attribute to detect thin layers of sandstone formations. From numerical analysis of a 25-Hz Ricker wavelet, we found that the fractional instantaneous frequency of 0.99 order keeps an approximation of standard instantaneous frequency and enhances the negative frequency (anomalous frequency spike), which help in more precise geological interpretation. A three-layer wedge model and a case history from the Bohai Bay Basin showed that the 0.99 order instantaneous frequency provides more depositional sandstone information than the standard instantaneous frequency. The anomalous frequency spike, at the merging point of the top and the base reflections or at the tip of the stratum, of 0.99 order instantaneous frequency is more prominent than that of the standard one. The results help to interpret the thickness changes of thin sandstone formations. In practical application, the 0.99 order instantaneous frequency has revealed several deposition phases and lateral heterogeneity of a fluvial reservoir system. Therefore, the 0.99 order instantaneous frequency is a valuable seismic attribute for reservoir characterization.
机译:地震瞬时频率属性已应用于解释沉积层。已经证明,Caputo分数微分算子可以替代沉积层的标准瞬时频率,它是一种更合适的非线性分析数学工具。基于Caputo算子,我们提出了瞬时频率属性的分数扩展来检测砂岩地层的薄层。通过对25 Hz Ricker小波的数值分析,我们发现0.99阶分数的瞬时频率保持了标准瞬时频率的近似值,并增强了负频率(异常频率尖峰),这有助于更精确的地质解释。一个三层楔形模型和一个来自渤海湾盆地的案例历史表明,0.99阶瞬时频率比标准瞬时频率提供了更多的沉积砂岩信息。 0.99阶瞬时频率的异常频率尖峰在顶部和基部反射的合并点处或在地层的尖端处比标准频率处更为突出。结果有助于解释薄砂岩地层的厚度变化。在实际应用中,0.99阶瞬时频率揭示了河流储层系统的几个沉积阶段和横向非均质性。因此,0.99阶瞬时频率对于储层表征是有价值的地震属性。

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