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Velocity Analysis by Residual Moveout after Migration from VSP Data

机译:VSP数据迁移后残余震动的速度分析

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Assessing residual moveout after migration is a useful way to undertake velocity analysis in surface seismic data. In this paper, we apply this concept to walk-away vertical seismic profile (VSP) data. Because of the non-symmetric source and receiver geometry, it is hard to detect the depth residual moveout in conventional common image gathers (CIGs) for VSP data. In this case, we changed the horizontal axis from horizontal offsets from the common image point (CIP) to be receiver depths. We derive a residual moveout function for migrated common receiver gathers assuming a constant velocity model having a single horizontal reflector. We then extend this tool to a layered medium using a layer stripping, V_(rms) approach, which allows us to obtain interval velocities of the model layers. It has better results than the classic depth residual moveout. This is further applied to more complex, laterally varying velocity models with good results. This is valid since with VSP data we are generally imaging within a small (compared to surface seismic) distance away from the borehole and our analysis method allows us to estimate velocity perturbations away from the trial migration velocity model.
机译:迁移后评估残余震动是在表面地震数据中进行速度分析的有用方法。在本文中,我们将此概念应用于行走的垂直地震型材(VSP)数据。由于非对称源和接收器几何形状,很难检测到VSP数据的传统常见图像收集(CIGS)中的深度残余偏移。在这种情况下,我们将水平轴从公共图像点(CIP)从水平偏移更改为接收器深度。假设具有单个水平反射器的恒定速度模型,我们得出了迁移的公共接收器聚集的剩余移位功能。然后,我们使用层剥离,V_(rms)方法将该工具扩展到分层介质,这允许我们获得模型层的间隔速度。它具有比经典深度残余震动更好的结果。这进一步应用于更复杂,横向变化的速度模型,效果良好。这是有效的,因为随着VSP数据,我们通常在距钻孔的小(与表面地震比较)内成像,并且我们的分析方法允许我们估计远离试验速度模型的速度扰动。

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