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3D fault imaging using windowed Radon transforms: an example from the North Sea

机译:3D故障成像使用窗口氡变换:北海的一个例子

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摘要

The interpretation of fault surfaces is key to understanding the subsurface geology represented in 3D seismic volumes. The geologic structure represented by seismic reflections can be auto-tracked in the volume. Faults, however, are imaged as discontinuities or changes in curvature in the seismic data. For many years, fault interpretation involved manually picking fault cuts on orthogonal slices through the seismic volume. These fault cuts were grouped into conceptual faults, and 3D fault surfaces were created from the fault cuts.
机译:故障表面的解释是了解在3D地震卷中表示的地质地质的关键。 可以在体积中自动跟踪由地震反射表示的地质结构。 然而,故障被成像为地震数据中的不连续性或曲率的变化。 多年来,故障解释涉及通过地震体积手动挑选在正交切片上的故障切割。 这些故障切割被分组为概念性故障,并从故障切割中创建3D故障表面。

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