基于柯西正则化和声阻抗转换的高分辨率反射率反演

H. Karslı
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引用次数: 0

摘要

声波阻抗(AI)是定量解释地震数据最有效的方法之一,可以通过转换次表层的反射率序列简单地获得。因此,地震资料的高分辨率反射率反演(HRRI)已成为地震资料处理的重要步骤。然而,当地震数据中含有噪声时,传统的阻尼和非阻尼最小二乘反演方法往往不可靠,反演结果质量较差。此外,从地震数据中估计反射率通常是带限制的,对阻抗产生有负面影响。出于这个原因,在本研究中,我使用柯西正则化(HRRI- cr)来执行HRRI。该方法可迭代产生高分辨率的反射率,并具有抗噪能力,从而获得准确的地震声阻抗结果。我测试了HRRI-CR方法在合成数据上获得AI的性能,并将亚表面层模型与计算的阻抗曲线进行比较,表明该方法提供了更准确的层信息。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
High Resolution Reflectivity Inversion with Cauchy Regularization and Acoustic Impedance Conversion
Summary Acoustic impedance (AI) is one of the most effective ways of quantitatively interpreting seismic data and can simply be obtained by converting the reflectivity series of the subsurface layers. Therefore, high resolution seismic reflectivity inversion (HRRI) of the seismic data has been an important step in the seismic data processing. However, when seismic data include noise, traditional damped and undumped least square inversion methods mostly lead to unreliable and low quality results. In addition, estimation of reflectivity from seismic data is generally band-limited and negatively affects impedance producing. For this reasons, in this study, I performed the HRRI with using Cauchy regularization (HRRI-CR). The method is iteratively applied to produce reflectivity with high resolution and has anti-noise ability, which leads to obtain accurate seismic acoustic impedance results. I tested the performance of the HRRI-CR method on synthetic data in obtaining the AI and showed that the method provides more accurate information about the layers when comparing the subsurface layer model with calculated impedance curves.
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