基于稳定因子的鲁棒频谱反演

IF 1.4 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Jie Zhou, Yaoguang Sun, Huailai Zhou
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引用次数: 0

摘要

反射率反演是联合储层参数和地震数据的关键步骤。基于 L1 规范约束的稀疏尖峰解卷积是一种广泛使用的反射率反演方法。但小波效应限制了该算法的分辨率。奇偶分解算法的出现削弱了小波调谐效应,使得基于 L1 准则的频谱反演得到进一步应用。由于频谱反演算法的不稳定性,反演反射率的横向连续性较差。因此,我们在传统频谱反演的基础上,引入稳定因子,提出了一种稳健的频谱反演方法。该算法继承了传统频谱反演的高分辨率特性和稀疏尖峰解卷积的鲁棒性。三种反射率反演方法在合成和野外数据实例中的表现证明了稳健光谱反演算法在分辨率和稳定性方面的改进。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Robust spectral inversion based on the stability factor

Robust spectral inversion based on the stability factor

Robust spectral inversion based on the stability factor

Reflectivity inversion is a critical step to joint reservoir parameters and seismic data. The sparse spike deconvolution is a widely used reflectivity inversion method based on the L1 norm constraint. But the wavelet effect limits the resolution of the algorithm. The emergence of the odd–even decomposition algorithm has weakened the wavelet tuning effect, which makes the spectral inversion based on the L1 norm further applied. Because of the instability of the spectral inversion algorithm, the lateral continuity of the inversion reflectivity is poor. Therefore, based on the conventional spectral inversion, we introduced a stability factor and proposed a robust spectral inversion method. The algorithm inherits the high-resolution characteristics of conventional spectral inversion and the robustness of sparse spiking deconvolution. The performances of three reflectivity inversion methods from synthetic and field data examples demonstrate the improvements in resolution and stability of the robust spectral inversion algorithm.

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来源期刊
Acta Geodaetica et Geophysica
Acta Geodaetica et Geophysica GEOCHEMISTRY & GEOPHYSICS-
CiteScore
3.10
自引率
7.10%
发文量
26
期刊介绍: The journal publishes original research papers in the field of geodesy and geophysics under headings: aeronomy and space physics, electromagnetic studies, geodesy and gravimetry, geodynamics, geomathematics, rock physics, seismology, solid earth physics, history. Papers dealing with problems of the Carpathian region and its surroundings are preferred. Similarly, papers on topics traditionally covered by Hungarian geodesists and geophysicists (e.g. robust estimations, geoid, EM properties of the Earth’s crust, geomagnetic pulsations and seismological risk) are especially welcome.
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