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VELOCITY AND INTERFACE DEPTH DETERMINATION BY TOMOGRAPHY OF DEPTH MIGRATED GATHERS

机译:用X射线测深仪进行速度和界面深度的测定

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A method for velocity and interface depth determination based on tomography of migrated common reflecting point (CRP) gathers is presented. The method is derived from the tomographic principle that relates traveltime change along a given ray to perturbations in slowness and layer depths. The tomographic principle is used to convert depth errors in migrated CRP gathers to time errors along a CRP ray pair and thus enable use of conventional traveltime tomography, It is also used to affect a very fast prestack migration and set up the tomography matrix. The velocity-depth determination method uses the available offsets of all CRPs and inverts for the parameters of all layers simultaneously, Hand picking of depth errors on CRP gathers is avoided by a method where the tomography matrix operates directly on the migrated gathers. The velocity-depth determination method is demonstrated on a synthetic example and on a field example from the North Sea. [References: 11]
机译:提出了一种基于层析成像的移动共反射点(CRP)道集确定速度和界面深度的方法。该方法源自断层摄影原理,该原理将沿给定射线的传播时间变化与慢度和层深度的扰动联系起来。层析成像原理用于将迁移的CRP道集中的深度误差转换为沿CRP射线对的时间误差,从而可以使用常规的行进时间层析成像。它还可以用于影响叠前非常快速的偏移并建立层析成像矩阵。速度深度确定方法使用所有CRP的可用偏移量,并同时对所有图层的参数求反。通过层析成像矩阵直接对迁移的道集进行操作的方法,避免了在CRP道集上进行人工拾取深度误差。在北海的一个合成实例和一个现场实例上演示了速度深度确定方法。 [参考:11]

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