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Independent component analysis for reservoir geomorphology and unsupervised seismic facies classification in the Taranaki Basin, New Zealand

机译:新西兰塔拉纳基盆地水库地貌和无监督地震相分类的独立分量分析

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During the past two decades, the number of volumetric seismic attributes has increased to the point at which interpreters are overwhelmed and cannot analyze all of the information that is available. Principal component analysis (PCA) is one of the best-known multivariate analysis techniques that decompose the input data into second-order statistics by maximizing the variance, thus obtaining mathematically uncorrelated components. Unfortunately, projecting the information in the multiple input data volumes onto an orthogonal basis often mixes rather than separates geologic features of interest. To address this issue, we have implemented and evaluated a relatively new unsupervised multiattribute analysis technique called independent component analysis (ICA), which is based on higher order statistics. We evaluate our algorithm to study the internal architecture of turbiditic channel complexes present in the Mold A sands Formation, Taranald Basin, New Zealand. We input 12 spectral magnitude components ranging from 25 to 80 Hz into the ICA algorithm and we plot 3 of the resulting independent components against a red-green-blue color scheme to generate a single volume in which the colored independent components correspond to different seismic facies. The results obtained using ICA proved to be superior to those obtained using PCA. Specifically, ICA provides improved resolution and separates geologic features from noise. Moreover, with ICA, we can geologically analyze the different seismic facies and relate them to sand- and mud-prone seismic facies associated with axial and off-axis deposition and cut-and-fill architectures.
机译:在过去的二十年中,体积地震属性的数量增加到了解释器不堪重负的点,无法分析可用的所有信息。主成分分析(PCA)是通过最大化方差来将输入数据分解为二阶统计的最佳已知的多变量分析技术之一,从而获得数学上不相关的组件。不幸的是,将多个输入数据卷中的信息投影到正交基础上通常混合而不是分离感兴趣的地质特征。为了解决这个问题,我们已经实施并评估了一个相对较新的无监督的多级多特征分析技术,称为独立分量分析(ICA),该技术基于更高阶统计数据。我们评估我们的算法研究模具中存在的砂岩频道复合物的内部架构,新西兰塔拉纳尔盆地塔拉纳尔盆地。我们将12个光谱幅度分量从25到80 Hz输入到ICA算法,我们将所得独立组件的3个绘制与红绿蓝色方案的3,以产生单个体积,其中彩色独立组分对应于不同的地震相。使用ICA获得的结果证明优于使用PCA获得的结果。具体而言,ICA提供改进的分辨率并将地质特征与噪声分开。此外,对于ICA,我们可以在地质上分析不同的地震相,并将它们与与轴向和轴外沉积和切割和填充架构相关的沙子和静态抗震相。

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