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Resolution enhancement of seismic data using spectral modeling based on dominant Ricker components and separable nonlinear least squares

机译:基于主要Ricker分量和可分离的非线性最小二乘法的频谱建模提高地震数据的分辨率

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Seismic resolution enhancement has a key role in seismic interpretation, especially in reservoir characterization and geologic interpretation. Exploration seismology has a limitation in temporal resolution and thin-layer detection, so any effort to improve the resolution of available data is valuable. Seismic deconvolution is one of the main steps in seismic processing and is intensively used for enhancing the vertical resolution. In this procedure, the seismic wavelet is compressed in order to decrease wavelet interferences and improve temporal resolution. In the common method of seismic deconvolution-i.e., Wiener deconvolution-the seismic wavelet is estimated by using the early part of autocorrelation of traces. Assuming the reflection series is a random function, the smoothed version of the amplitude spectrum of traces can be considered as the amplitude spectrum of the seismic wavelet. The wavelet spectrum can be properly reconstructed by the linear combination of a number of Ricker wavelets with different peak frequencies. The authors aim to introduce a novel method for resolution improvement based on fitting and finding main Ricker components of the source-wavelet spectrum. This attempt is classified under the group of the separable nonlinear least squares (SNLS), the objective function of which is a combination of linear and nonlinear functions. A variable projection method is applied to recognize the optimum peak frequency of Ricker wavelets involved in the wavelet spectrum. Our synthetic tests indicate that the SNLS algorithm is able to achieve a very close approximation of dominant Ricker components of the source spectrum. Considering the minimum phase assumption of the wavelet, the phase spectrum is also computed by Hilbert transform of the estimated amplitude spectrum. Once the amplitude and phase information are available, the deconvolution operator can be designed. Our synthetic and real tests indicate that, in comparison with Wiener deconvolution, spectral modeling based on dominant Ricker components (SMDRC) has improved the deconvolution outputs.
机译:地震分辨率的提高在地震解释中,尤其是在储层表征和地质解释中具有关键作用。勘探地震学在时间分辨率和薄层探测方面有局限性,因此,为改善可用数据的分辨率所做的任何努力都是有价值的。地震反褶积是地震处理中的主要步骤之一,被广泛用于提高垂直分辨率。在此过程中,地震子波被压缩以减少子波干扰并提高时间分辨率。在普通的地震反卷积方法中,即维纳反卷积,地震子波是通过使用迹线的自相关的早期部分来估计的。假设反射序列是一个随机函数,则迹线振幅谱的平滑版本可以视为地震子波的振幅谱。通过将多个具有不同峰值频率的Ricker小波进行线性组合,可以正确地重建小波频谱。作者旨在介绍一种基于拟合和找到源小波谱的主要Ricker分量的分辨率提高的新方法。这种尝试被归类为可分离的非线性最小二乘(SNLS)组,其目标函数是线性函数和非线性函数的组合。应用可变投影法来识别参与小波频谱的里克小波的最佳峰值频率。我们的综合测试表明,SNLS算法能够非常接近源频谱的主要瑞克分量。考虑小波的最小相位假设,也通过估计幅度谱的希尔伯特变换来计算相位谱。一旦幅度和相位信息可用,就可以设计反卷积算子。我们的综合测试和实际测试表明,与维纳反卷积相比,基于主要Ricker分量(SMDRC)的频谱建模提高了反卷积输出。

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