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Recognition of Minor Faults in Carbonate Rock Reservoirs

机译:碳酸盐岩储层中小断层的识别

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摘要

Minor faults have great influence on the production of carbonate rock reservoirs. Recognizing these small scale faults is a big challenge with conventional seismic data. The spectrum decomposition method with the optimal fractional Gabor transform is produced by replacing the traditional Gabor transform kernel function with the fractional kernel function based on the fractional Fourier transform, and getting the optimal fractional order with the evaluation of the time bandwidth production parameter. High resolution anomaly detection algorithms such as the improved C3 coherence method are adopted to get the attribute cubes. A detailed comparison between the stratigraphic slices and time slices to the coherence cubes of high frequency decomposed subseismic data and the original seismic data shows that the stratigraphic slice to the coherence cube of high frequency decomposed subseismic data is the easiest and most visualized tool for minor faults recognition in map views. The decomposed high frequency subseismic data with the optimal fractional Gabor transform is much easier for minor faults interpretation than using the original seismic data.
机译:轻微的断层对碳酸盐岩储层的生产有很大影响。认识到这些小规模断层是传统地震数据的重要挑战。利用基于分数傅里叶变换的分数核函数替换传统的Gabor变换核功能,通过评估时间带宽生产参数的评估,通过替换传统的Gabor变换核函数来产生具有最佳分数Gabor变换的频谱分解方法。采用高分辨率异常检测算法,例如改进的C3相干方法来获取属性多维数据集。地层切片与时间切片之间的详细比较,对高频分解底物数据的相干立方体和原始地震数据表示,地层切片对高频分解底层数据的相干立方体是一个简单的故障最简单而最具可视化的工具在地图视图中识别。具有最佳分数Gabor变换的分解的高频次掩数据对于小故障解释比使用原始地震数据更容易。

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