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Sub pixel mapping of alteration minerals using SOM neural network model and hyperion data

机译:使用SOM神经网络模型和高离子数据对蚀变矿物的亚像素映射

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This study applies the self-organizing map (SOM) neural network model for sub pixel mapping of alteration minerals in the Masahim volcano, SE Iran, using Hyperion data. Four end-members including sericite, kaolinite, epidote, and montmorillonite/illite were identified from the imagery, and based on these end-members training areas were generated and used to train the model. Numerous tests were conducted for selecting the optimal neural network architecture. The confusion matrix was calculated to identify the accuracy of map produced by SOM. The confusion matrix indicated that among the different SOM architectures, the result of 55 x 55 array of nodes with overall accuracy of 83 % was the best architecture for describing the spatial distribution of alteration unit. The coefficient of determination (R-2) was also calculated to assess the accuracy of sub pixel fraction maps. The R-2 coefficient was 0.60 for kaolinite, 0.72 for sericite, 0.58 for epidote and 0.62 for montmorillonite/illite .The mapping results revealed that kaolinite, sericite and montmorillonite/illite are emplaced in the caldera of the volcano and epidote is mainly found at the northwestern part of caldera. It can be concluded that the SOM is useful in mineral mapping and exploration activities.
机译:这项研究使用Hyperion数据,将自组织映射(SOM)神经网络模型用于伊朗东南部Masahim火山蚀变矿物的亚像素成像。从图像中识别出了4个最终成员,包括绢云母,高岭石,榴辉岩和蒙脱石/伊利石,并根据这些最终成员生成了训练区域并用于训练模型。为了选择最佳的神经网络架构,进行了大量测试。计算混淆矩阵以识别SOM生成的地图的准确性。混淆矩阵表明,在不同的SOM体系结构中,以55 x 55的节点阵列(总精度为83%)的结果是描述变更单元空间分布的最佳体系结构。还计算确定系数(R-2)以评估子像素分数图的准确性。高岭石的R-2系数为0.60,绢云母的R-2系数为0.72,蒙脱石/伊利石的R-2系数为0.52,蒙脱石/伊利石的0.62。破火山口的西北部。可以得出结论,SOM在矿物测绘和勘探活动中很有用。

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