通过重建格林脉冲响应实现浅水多重衰减

IF 1.8 3区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Yike Liu, Xiaopeng Zhou, Peng Li
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引用次数: 0

摘要

由于缺乏近偏移数据,在浅水中去除与水层相关的倍频仍然是一项挑战。我们开发了一种浅水多重衰减方法,通过构建水底的脉冲响应来去除与水层相关的多重。海底的脉冲响应由其行进时间响应和振幅响应的卷积形成。它利用原始浅水解多重算子的叠加来获取旅行时间信息,并利用解卷积方法从原始浅水解多重算子中估算其动态分量,从而建立新的算子。不仅能正确构建近偏移的脉冲响应,而且能正确构建中等偏移和远偏移的脉冲响应。我们的方法采用了三项减法策略,即预测源端、接收端以及源端和接收端的倍频,从而在不过度预测的情况下减弱浅层倍频。两个合成数据集以及二维和三维实地数据集的数值示例表明,我们的方法具有理想的性能。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Shallow water multiple attenuation through the reconstruction of Green's impulse response
Removal of water‐layer‐related multiples in shallow water remains a challenge due to a lack of near‐offset data. We have developed a shallow water multiple attenuation approach by constructing the impulse response of the water bottom for the removal of water‐layer‐related multiples. The impulse response of the seafloor is formed by the convolution of its traveltime response and amplitude response. It uses the superposition of the original shallow water demultiple operator to obtain traveltime information and uses the deconvolution method to estimate its dynamic components from the original shallow water demultiple operator to build new operators. The impulse response can be correctly constructed not only for near offsets but for moderate and far offsets as well. A three‐term subtraction strategy by predicting source‐side, receiver‐side and both source‐side and receiver‐side multiples is adopted in our approach for attenuating shallow multiples without over‐prediction. Numerical examples with two synthetic datasets and 2D and 3D field datasets demonstrate that our approach gives a desirable performance.
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来源期刊
Geophysical Prospecting
Geophysical Prospecting 地学-地球化学与地球物理
CiteScore
4.90
自引率
11.50%
发文量
118
审稿时长
4.5 months
期刊介绍: Geophysical Prospecting publishes the best in primary research on the science of geophysics as it applies to the exploration, evaluation and extraction of earth resources. Drawing heavily on contributions from researchers in the oil and mineral exploration industries, the journal has a very practical slant. Although the journal provides a valuable forum for communication among workers in these fields, it is also ideally suited to researchers in academic geophysics.
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