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Lithological Analysis of Nain Ophiolitic Zone Using ASTER Data

机译:艾斯特数据Nain Opholitic区的岩性分析

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The Mesozoic ophiolitic Mélange, north of Nain in the Central-East Iran Microplate (CEIM) comprises serpentinized ultramafic rocks, harzburgites, dunite, gabbro, peridotite, pelagic limestone and other carbonate rocks. The excellent and vast exposure of this desert region is well suited for geologic mapping of this rock suite using remote sensing, especially using data from the satellite-borne advanced Space borne Thermal Emission and Reflection Radiometer (ASTER) imaging system which was designed for mapping mineral information. In this study, data processing methods like Method Minimum noise fraction (MNF), Feature Oriented Principal Components Selection (FPCS), Band Ratios (BR) and Optimum Index Factor (OIF) were used to process ASTER data to optimize the mapping of ophiolite rock types. For example, a simple color composites of OIF (Red: B3, Green: B4, and Blue: B8) and Band ratios (e.g. Red: (B2 + B4)/B3, Green: (B5 + B7)/B6, Blue: (B7 + B9)/B8) were useful for discriminating serpentinite, meta-basalt and granite rock types. It is concluded here that proposed ASTER data has the potential for mapping similar ophiolites elsewhere using the global archive of ASTER imagery.
机译:中生代OphioliticMélange,位于伊朗中央东伊朗墨水(CEIM)的北部,包括蛇形化超岩石,哈尔茨伯里菌素,鹿洞,古氏菌,橄榄石,木质石灰石和其他碳酸盐岩石。这种沙漠地区的优秀和广泛曝光非常适合使用遥感的岩石套件的地质映射,特别是使用卫星传播的先进空间传播的热发射和反射辐射计(紫色)成像系统的数据,该系统被设计用于绘制矿物信息。在该研究中,使用方法最小噪声分数(MNF),特征导向的主成分选择(FPC),带比(BR)和最佳指标因子(OIF)来处理ASTER数据以优化Ophiolite Rock的映射类型。例如,OIF的简单颜色复合材料(红色:B3,绿色:B4和蓝色:B8)和带比(例如,红色:(B2 + B4)/ B3,绿色:(B5 + B7)/ B6,蓝色: (B7 + B9)/ B8)可用于区分蛇形素,Meta玄武岩和花岗岩岩石类型。这里得出结论,提出的紫砂数据具有使用Aster Imagery的全球档案的其他地方在其他地方映射类似的眼镜岩。

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