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首页> 外文期刊>Journal of the Geological Society of India >Comparison of Mineralization Pattern of Geochemical Data in Spatial and Position-scale Domain Using New DWT-PCA Approach
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Comparison of Mineralization Pattern of Geochemical Data in Spatial and Position-scale Domain Using New DWT-PCA Approach

机译:新的DWT-PCA方法在空间和位置尺度范围内地球化学数据成矿模式的比较

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摘要

In the current research to determine the mineralization pattern and discuss the mineralization components, the information of position - scale domain of geochemical data has been analyzed. A new method is proposed based on coupling discrete wavelet transforms (DWT) and principal component analysis (PCA) for mineralization elements forecasting applications. The results of this study indicate the potential of DWT-PCA method for geochemical data processing. Wavelet transform (WT), as a multi-spectral analysis method, can decompose the spatial and temporal signals into different frequencies. The features of mineralization can be identified using the position - scale domain of geochemical data that may not be achievable in spatial domain. The geochemical data from the Dalli region have been processed in the spatial domain using PCA. The surface geochemical data of 30 elements have been transformed to position-scale domain using two-dimensional discrete wavelet transform (2DDWT). Wavelet functions (WFs) of Haar, Coiflet2, Biorthogonal3.3 and Symlet7 have been applied separately to decompose the geochemical data to high and low frequencies in one level. To obtain more accurate and complete information of mineralization, a new index has been presented based on wavelet coefficients. Based on this new index, significant results have been obtained by using PCA of the index. The coefficients distribution map (CDM) as a new exploratory criterion has been generated based on 2DDWT to show the geochemical distribution map (GDM). Finally, the results of WT have been compared with the results of spatial domain and the best method of wavelet for interpretation of geochemical data has been introduced. The results of geochemical data analysis by DWT-PCA approach have been confirmed by the exploratory drillings in the study area.
机译:在确定矿化模式和讨论矿化成分的当前研究中,分析了地球化学数据的位置-比例域信息。提出了一种基于离散小波变换(DWT)和主成分分析(PCA)耦合的矿化元素预测方法。这项研究的结果表明DWT-PCA方法在地球化学数据处理方面的潜力。小波变换(WT)作为一种多光谱分析方法,可以将空间和时间信号分解为不同的频率。可以使用在空间域中无法实现的地球化学数据的位置-比例域来识别矿化特征。来自达利地区的地球化学数据已使用PCA在空间域中进行了处理。使用二维离散小波变换(2DDWT)将30个元素的表面地球化学数据转换为位置尺度域。 Haar,Coiflet2,Biorthogonal3.3和Symlet7的小波函数(WFs)已分别应用,以将地球化学数据分解为一个高低频分量。为了获得更准确和完整的矿化信息,基于小波系数提出了一种新的指标。基于此新索引,通过使用该索引的PCA获得了显着结果。已基于2DDWT生成了作为新探索标准的系数分布图(CDM),以显示地球化学分布图(GDM)。最后,将WT的结果与空间域的结果进行了比较,并介绍了小波解释地球化学数据的最佳方法。 DWT-PCA方法进行的地球化学数据分析结果已被研究区的勘探钻探所证实。

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