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Improving curvature analyses of deformed horizons using scaledependent filtering techniques

机译:使用比例依赖滤波技术改善变形层的曲率分析

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Fractures, which are common structural heterogeneities in geological folds and doms, impact the charge, seal, and trapping potential of hydrocarbon reservoirs. Because of their effects on reservoir quality, the numerical prediction of fractures has recently been the focus of petroleum geoscientists. A horizon's curvature is commonly used to infer the state of deformation in those strata. It is assumed that areas of elevated calculated curvatures underwent elevated deformation, resulting in a concentration of fractures and faults there. usually, curvatures are calculated from spatial data after sampling the continuous horizon at discrete points. This sampled geometry of the horizon includes surface undulations of all scales, which are then also included in the calculated curvatures. Including surface undulations of all scales in the curvature analysis leads to noisy and questionable results. We argue that the source data must be filtered prior to curvature analysis to separate different spatial scales of surface undulations, such as broad structures, faults, and sedimentary features. Only those surface undulations that scale with the problem under consideration should then be used in a curvature analysis. For the scale-dependent decomposition of spatial data, we test the suitability of four numerical techniques (Fourier [spectral] analysis, wavelent transform filtering, singular value decomposition, factorial kriging) on a seismically mapped horizon in the North Sea. For surfaces sampled over a regular grid (e.g., seismic data), Fourier (spectral) analysis extracts meaningful curvatures on the scale of broad horizon features, such as structural domes and basins.
机译:裂缝是地质褶皱和地壳中常见的结构异质性,会影响油气藏的充注,封闭和圈闭潜力。由于其对储层质量的影响,裂缝的数值预测近来已成为石油地球学家关注的焦点。地平线的曲率通常用于推断这些地层的变形状态。假定计算出的曲率升高的区域经历了较大的变形,从而导致裂缝和断层的集中。通常,曲率是在离散点对连续水平线进行采样后根据空间数据计算得出的。地平线的这种采样几何包括所有比例的表面起伏,然后这些起伏也包括在计算的曲率中。在曲率分析中包括所有尺度的表面起伏都会导致嘈杂和可疑的结果。我们认为,在曲率分析之前必须对源数据进行过滤,以分离出表面起伏的不同空间尺度,例如广阔的结构,断层和沉积特征。然后,仅应将与所考虑的问题成比例的那些表面起伏用于曲率分析。对于空间数据的比例依赖分解,我们在北海地震映射的地平线上测试了四种数值技术(傅立叶[频谱]分析,波峰变换滤波,奇异值分解,阶乘克里金法)的适用性。对于在规则网格上采样的表面(例如地震数据),傅里叶(频谱)分析可在诸如建筑物穹顶和盆地之类的宽视野特征的尺度上提取有意义的曲率。

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