Sparse-Spike Deconvolution Promoting Frequency Dependent Seismic Stratigraphic Analysis and an Application

Liu Chang
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引用次数: 0

Abstract

Low-frequency components of seismic data tend to characterize thicker litho-stratigraphic units, while high-frequency components tend to characterize thinner isochronous-stratigraphic units. Thus, frequency dependent interpretation can help to achieve fine sedimentary sequence analysis. However, in current seismic sedimentology method, a certain frequency profile generated by frequency filtering, loses some stratum reflection information, which is out of the limited frequency band. To achieve real frequency dependent stratum reflection profiles with whole stratum information, a time-varying sparse-spiking deconvolution based method is proposed in this paper. A synthetic example and a real delta progradation example show the accuracy and effectiveness of proposed method.
稀疏尖峰反褶积促进频率相关地震地层分析及其应用
地震数据的低频分量倾向于表征较厚的岩性地层单元,而高频分量倾向于刻画较薄的等时地层单元。因此,依赖频率的解释可以帮助实现精细的沉积序列分析。然而,在目前的地震沉积学方法中,通过频率滤波生成的某个频率剖面,会丢失一些地层反射信息,这些信息超出了有限的频带。为了获得具有完整地层信息的真实频率相关地层反射剖面,本文提出了一种基于时变稀疏尖峰反褶积的方法。综合算例和实际三角洲进积算例验证了该方法的准确性和有效性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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