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A PRE-STACK DEPTH DIFFRACTION IMAGING WORKFLOW BASED ON ANGLE GATHERS

机译:基于角度聚积器的叠前深度衍射成像工作流程

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摘要

A new workflow is presented that can image diffracted waves for pre-stack seismic data based on angle gathers. This workflow combines the advantages of pre-stack time migration and pre-stack depth migration. For simplicity in calculations and parameter estimations, we mute the Fresnel zones related to reflections to enhance diffractions in the common angle gathers by shot-domain pre-stack time migration. A structural dip estimation scheme is provided to obtain the best Fresnel zones for accurate attenuation of reflections. Then, the demigration processing is used to remove the effect of previous pre-stack time migration on the imaged diffracted events to obtain diffracted wavefield. At last, the diffracted wavefield is imaged again by pre-stack depth migration, which adapt to imaging for complex structure. The result of my method is an effective complement to conventional interpretation workflow in detecting of small-scale geological discontinuities. Synthetic example and field data example demonstrate that my method is accurate, robust and easy to implement.
机译:提出了一种新的工作流,该工作流可以基于角度聚集为叠前地震数据成像衍射波。此工作流程结合了叠前时间迁移和叠前深度迁移的优点。为了简化计算和参数估算,我们将与反射相关的菲涅耳区域静音,以通过散粒域叠前时间偏移来增强公共角度集中的衍射。提供了一种结构倾角估计方案,以获得最佳的菲涅耳区,以精确地衰减反射。然后,使用偏移处理来消除先前的叠前时间偏移对成像的衍射事件的影响,以获得衍射波场。最后,通过叠前深度偏移再次对衍射波场进行成像,从而适应复杂结构的成像。我方法的结果是对常规解释工作流程的有效补充,可用于检测小规模地质不连续性。综合实例和现场数据实例表明,该方法准确,鲁棒,易于实现。

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