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Remote Sensing Study of Sittampundi Anorthosite Complex, India

机译:印度实兑蓬迪钙硅钙石复合体的遥感研究

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In the present study, The Landsat 7 ETM satellite data was collected for the Sittampundi anorthosites complex and digital image analysis was carried out. The anorthositic rocks available at Sittampundi complex is considered as an equivalent of lunar highland rocks. Hence, a remote sensing study comprises of image analysis and spectral profile analysis was carried out. The satellite data was digitally processed and generated various outputs like band combinations, color composites, stretched outputs, and PCA. The suitable processed outputs were identified for delineating the anorthosite complex. The diagnostic absorption features of reflectance spectra are the sensitive indicators of mineralogy and chemical composition of rocks, which are interest to the planetary scientists. The spectral profile of Landsat ETM plotted for pure and mixed anorthosite pixels and compared with the field and lab reflectance spectra. The percentages of image spectra vary from 30% to 60% for Sittampundi anorthosite. The spectral bands 2, 4 and 6 have low reflectance and bands 3 and 5 have high reflectance. The spectral range of bands 2,3,4,5 and 6 are 525 nm–605 nm, 630 nm–690 nm, 750 nm–900 nm, 1550 nm–1750 nm and 10400 nm–12500 nm respectively. The field spectral curve has weak absorptions at 650 nm and 1000 nm due to the iron transition absorption and low ca- pyroxene respectively available in the anorthosite, matching with the image spectra. However, hyperspectal image with narrow bandwidth could be more useful in selecting the suitable spectrum for remotely mapping the anorthosite region, as equivalent test site for lunar highland region.
机译:在本研究中,Landsat 7 ETM卫星数据被收集用于实兑蓬松石原位复合体,并进行了数字图像分析。 Sittampundi复合体中可用的抗寄生虫岩石被认为等同于月球高地岩石。因此,进行了包括图像分析和光谱轮廓分析的遥感研究。对卫星数据进行数字处理,并生成各种输出,例如波段组合,彩色合成,拉伸输出和PCA。确定了合适的处理后的输出,以描绘出原位复合体。反射光谱的诊断吸收特征是岩石的矿物学和化学组成的敏感指标,这是行星科学家感兴趣的。 Landsat ETM的光谱轮廓针对纯正和混合的原铁矿像素绘制,并与野外和实验室反射光谱进行了比较。实兑蓬原石的图像光谱百分比从30%到60%不等。光谱带2、4和6具有低反射率,光谱带3和5具有高反射率。 2,3,4,5和6波段的光谱范围分别为525 nm–605 nm,630 nm–690 nm,750 nm–900 nm,1550 nm–1750 nm和10400 nm–12500 nm。场谱曲线在铁原石中分别具有铁跃迁吸收和低二茂铁,因此在650 nm和1000 nm处吸收较弱,与图像光谱匹配。但是,窄带宽的高光谱图像在选择合适的光谱用于遥测正畸位区域时,可能更有用,作为月球高地区域的等效测试点。

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