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叠加法静校正 被引量:5
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作者 赵峰 郑鸿明 《新疆石油地质》 CAS CSCD 2001年第2期124-125,共2页
叠加法静校正方法,是采用叠加原理,充分利用地震数据中的折射波信息、反射波信息以及目前使用的较强的地震数据交互处理系统,分别求取炮点和检波点的相对静校正值,以消除不同波长静校正对地震数据的影响,提高地震数据处理分辨率。... 叠加法静校正方法,是采用叠加原理,充分利用地震数据中的折射波信息、反射波信息以及目前使用的较强的地震数据交互处理系统,分别求取炮点和检波点的相对静校正值,以消除不同波长静校正对地震数据的影响,提高地震数据处理分辨率。就该方法的原理、实现过程以及运用效果加以介绍。 展开更多
关键词 叠加法静校正方法 叠加原理 地震数据 折射信息 反射波信息 地震勘探
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Reflection full-waveform inversion using a modified phase misfit function
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作者 崔超 黄建平 +2 位作者 李振春 廖文远 关哲 《Applied Geophysics》 SCIE CSCD 2017年第3期407-418,461,共13页
Reflection full-waveform inversion (RFWI) updates the low- and high- wavenumber components, and yields more accurate initial models compared with conventional full-waveform inversion (FWI). However, there is stron... Reflection full-waveform inversion (RFWI) updates the low- and high- wavenumber components, and yields more accurate initial models compared with conventional full-waveform inversion (FWI). However, there is strong nonlinearity in conventional RFWI because of the lack of low-frequency data and the complexity of the amplitude. The separation of phase and amplitude information makes RFWI more linear. Traditional phase-calculation methods face severe phase wrapping. To solve this problem, we propose a modified phase-calculation method that uses the phase-envelope data to obtain the pseudo phase information. Then, we establish a pseudophase-information-based objective function for RFWI, with the corresponding source and gradient terms. Numerical tests verify that the proposed calculation method using the phase-envelope data guarantees the stability and accuracy of the phase information and the convergence of the objective function. The application on a portion of the Sigsbee2A model and comparison with inversion results of the improved RFWI and conventional FWI methods verify that the pseudophase-based RFWI produces a highly accurate and efficient velocity model. Moreover, the proposed method is robust to noise and high frequency. 展开更多
关键词 Reflection full-waveform inversion full-waveform inversion misfit function
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