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Phase Decomposition for Interpretation of Thin Layers–Possibilities and Limitations

机译:相位分解以解释薄层可能性和限制

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The relatively new method of phase decomposition (Castagna et al. 2016) is complex to understand and use, but has good potential for the analysis of lateral changes in thin layers. To develop a better understanding of this technology, a set of synthetic models of wedges and the subsequent phase gathers for these models was calculated and analyzed. The results obtained from this analysis demonstrate that changes in the phase depend on the layer thickness and the proportion between the reflection coefficient of the top and the bottom of the layer. We can see that the phase split and shifted from the original in tuning zones. For wedges with Reflection Coefficient (RC) in different polarity for top and bottom, phase gathers were more differentiated than for wedges with RC in the same polarity for top and bottom. For analyzing phase difference, we use prestack offset visualization technology (Fink 2010), which helps visualize changes in phase in the tuning zone by horizon. For analyzing lateral changes in the tuning zone, we must select zones with equal thickness of thin layers, because thickness also influences phase changes and will mask lateral property changes. The proposed method of using phase decomposition will help to analyze the property changes of the thin layer below traditional seismic resolution.
机译:相对阶段分解的方法(Castagna等,2016)是理解和使用的复杂性,但具有良好的潜在潜力,用于分析薄层的横向变化。为了更好地了解这项技术,计算并分析了一组合成楔形的楔形和随后的相阶段的聚集。从该分析获得的结果表明,相位的变化取决于层厚度和层的顶部和底部的反射系数之间的比例。我们可以看到该阶段分裂并从原始区域中移位。对于具有反射系数(RC)的楔形楔,在顶部和底部的不同极性,相数比具有RC在顶部和底部相同极性的楔更分化。为了分析相位差,我们使用Prestack偏移可视化技术(FICK 2010),这有助于通过Horizo​​ n可视化调谐区域中的相位变化。为了分析调谐区域的横向变化,必须选择具有相等厚度薄层的区域,因为厚度也影响相位变化并将屏蔽横向性能发生变化。所提出的使用相位分解方法将有助于分析低于传统地震分辨率的薄层的性能变化。

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