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Frequency estimates of seismic traces

机译:地震道的频率估计

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Local estimates of amplitude, frequency, and phase have been used in the past to characterize seismic data. In particular, these attributes have sometimes been successfully related to well attributes at the reservoir scale (net pay thickness, sand fraction, etc.). This paper introduces a method called SINFIT for computing local amplitude, frequency, and phase estimates of seismic traces over short-time windows. The SINFIT method uses a sine-curve fitting approach. The method is shown to give more accurate and robust frequency estimates than four other common methods on a set of test traces where the true frequency components are known. The four methods compared with SINFIT are instantaneous frequency, zero-crossings, short-time Fourier analysis, and a more recent time-frequency method called AOK. In a field case with fluvial sands, an average frequency over a 30-ms time window of seismic data correlates with estimated shale volume from well logs. The SINFIT method gives an average frequency attribute that more strongly correlates with shale volume than corresponding attributes from any of the other four methods.
机译:过去已使用幅度,频率和相位的局部估计来表征地震数据。特别是,这些属性有时已成功地与储层规模的井属性(净产层厚度,砂分数等)相关。本文介绍了一种称为SINFIT的方法,用于计算短时窗内地震道的局部幅度,频率和相位估计。 SINFIT方法使用正弦曲线拟合方法。在已知真实频率分量的一组测试迹线上,该方法显示出比其他四种常见方法更准确,更可靠的频率估计。与SINFIT相比,这四种方法是瞬时频率,过零,短时傅立叶分析和一种最新的时频方法,称为AOK。在有河流砂的现场情况下,地震数据在30毫秒时间窗内的平均频率与测井中的页岩量估计值相关。与其他四种方法中任何一种的相应属性相比,SINFIT方法提供的平均频率属性与页岩体积的相关性更高。

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