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Assessment of Various Fuzzy c-Mean Clustering Validation Indices for Mapping Mineral Prospectivity: Combination of Multifractal Geochemical Model and Mineralization Processes

机译:用于绘制矿物前景的各种模糊C型聚类验证指标的评估:多分术地球化学模型和矿化过程的组合

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This paper describes the application of an unsupervised clustering method, fuzzy c-means (FCM), to generate mineral prospectivity models for Cu ± Au ± Fe mineralization in the Feizabad District of NE Iran. Various evidence layers relevant to indicators or potential controls on mineralization, including geochemical data, geological-structural maps and remote sensing data, were used. The FCM clustering approach was employed to reduce the dimensions of nine key attribute vectors derived from different exploration criteria. Multifractal inverse distance weighting interpolation coupled with factor analysis was used to generate enhanced multi-element geochemical signatures of areas with Cu ± Au ± Fe mineralization. The GIS-based fuzzy membership function MSLarge was used to transform values of the different evidence layers, including geological-structural controls as well as alteration, into a [0-1] range. Four FCM-based validation indices, including Bezdek's partition coefficient (V_(Pe)) and partition entropy (V_(Pe)) indices, the Fukuyama and Sugeno (V_(FS)) index and the Xie and Beni (V_(Xb)) index, were employed to derive the optimum number of clusters and subsequently generate prospectivity maps. Normalized density indices were applied for quantitative evaluation of the classes of the FCM prospectivity maps. The quantitative evaluation of the results demonstrates that the higher favorability classes derived from V_(FS) and V_(xb) (N_d = 9-19) appear more reliable than those derived from V_(Pc) and V_(Pe) (N_d = 6.12) in detecting existing mineral deposits and defining new zones of potential Cu ± Au ± Fe mineralization in the study area.
机译:本文介绍了无监督的聚类方法,模糊C-MEARION(FCM)的应用,为NE IRAN的FEIZABAD区生成CU±AU±FE矿化的矿物前景模型。使用与矿化的指标或潜在控制相关的各种证据层,包括地球化学数据,地质结构地图和遥感数据。使用FCM聚类方法来减少九个关键属性载体的尺寸,来自不同的探索标准。与因子分析相结合的多重型逆距离加权插值用于产生具有Cu±Au±Fe矿化的区域的增强的多元素地球化学签名。基于GIS的模糊会员函数MSLARGE用于转换不同证据层的值,包括地质结构控制以及改变,进入[0-1]范围内。基于FCM的验证指数,包括Bezdek的分区系数(V_(PE))和分区熵(V_(PE))指数,福山和Sugeno(V_(FS))索引和XIE和Beni(v_(xb))索引,用于得出最佳数量的群集,随后产生潜在级映射。归一化密度指数用于对FCM勘探地图的类别进行定量评估。结果的定量评估表明,从V_(FS)和V_(XB)(N_D = 9-19)导出的较高的合理性等级看起来比来自V_(PC)和V_(PE)的那些更可靠(N_D = 6.12 )在检测现有的矿物沉积物并在研究区域定义新的潜在Cu±Au±Fe矿化区。

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