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Joint imaging of angle-dependent reflectivity and estimation of the migration velocity model using multiple scattering

机译:使用多个散射的角度依赖反射率的联合成像和迁移速度模型的估计

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摘要

Migration velocity analysis is an important method for providing an accurate velocity model for seismic imaging, which is crucial for correct focusing and localization of subsurface information. Conventionally, only primaries are considered as a source of information for both methods. The use of surface multiples in imaging is becoming more common due to the use of inversion-based approaches, which allow us to handle the crosstalk associated with multiples. However, including internal multiples in imaging and velocity estimation is not straightforward using the standard combination of reverse time migration in combination with image-domain velocity tomography. Incorporating internal multiples in imaging and velocity estimation is possible with the joint migration inversion (JMI) methodology, in which internal multiples are explicitly modeled using the estimated reflectivity via a data-domain objective function. However, to correctly match the observed data, the angle-dependent reflectivity and the migration velocity model need to be determined, which provide an over-parameterization of the inversion problem. Therefore, we have extended the JMI methodology to carry out velocity analysis via the extended image domain, in which the angle-dependent reflectivity is updated via data-domain matching. Examples of synthetic and field data with strong internal multiples demonstrate the validity of our method.
机译:迁移速度分析是提供用于地震成像的精确速度模型的重要方法,这对于正确的聚焦和地下信息的定位至关重要。传统上,只有初选被认为是两种方法的信息源。由于使用基于反转的方法,因此使用表面倍数变得越来越常见,这使我们能够处理与倍数相关联的串扰。然而,包括在成像和速度估计中的内部倍数使用与图像域速度断层扫描结合的反向时间迁移的标准组合并不简单。通过联合迁移反演(JMI)方法可以在成像和速度估计中结合内部倍数,其中通过通过数据域目标函数使用估计的反射率明确建模内部倍数。然而,为了正确匹配观察到的数据,需要确定角度依赖的反射率和迁移速度模型,其提供反演问题的过参数化。因此,我们已经扩展了JMI方法,以通过扩展图像域进行速度分析,其中通过数据域匹配更新角度依赖性反射率。具有强大内部倍数的合成和现场数据的示例展示了我们方法的有效性。

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