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Edge-preserving smoothing for seismic image using coherence-enhancing anisotropic diffusion

机译:使用相干性增强各向异性扩散的地震图像的边缘保持平滑

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Currently, there are a variety of post-stack time-domain and frequency-domain de-noising method, but they will reduce the vertical and horizontal resolution of seismic data. Actually it is negative for analysis of geometric attribute and other follow-up work, so we need a filtering that can maintain the reflection angle as well as the contact relationship of strata. Coherence-enhancing diffusion filtering is just to meet the requirements, because it combines the smoothing and edge detection. The technique improves signal-to-noise ratio of seismic data as well as enhance the continuity of reflection events and protect important geological structure. In this paper, coherence-enhancing anisotropic diffusion filtering is used to process seismic image, and as a result it is really useful for interpretation of low S/N ratio seismic data. Examples show the remarkable effects of this operation.
机译:目前,存在各种堆栈的时域和频域取消通知方法,但它们将减少地震数据的垂直和水平分辨率。实际上它是对几何属性和其他后续工作的分析,因此我们需要一个可以保持反射角度以及地层的接触关系的过滤。连贯增强的扩散滤波只是为了满足要求,因为它结合了平滑和边缘检测。该技术提高了地震数据的信噪比以及增强反射事件的连续性,保护重要地质结构。在本文中,使用相干的各向异性扩散滤波来处理地震图像,因此它对于解释低S / N比地震数据来说真实有用。例子显示了该操作的显着效果。

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