Using the band ratio approach, FULL-PIXEL (SAM and SFF) and SUB-PIXEL (MF and SID) methodologies to discover areas with alteration using the Aster sensor: a case study in north westen Iran - Sivardaghi Area

M. Bagheri, Afshin Ashja Ardalan, A. Ganji, S. H. Asiabar, Mohammad Ali Arin
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Abstract

ASTER sensor data is among the most potent satellite data accessible for doing geological investigations, with images for the whole earth's surface. In order to test the capability of this sensor to detect places with geochemical alterations, photographs of Mount Seiver Daghi in the western Iranian province of Samal were utilized in this study. This region, which comprises of magmatic and volcanic terrain, is part of the Arsbaran territory and is covered by intrusive masses with alluvial and sedimentary deposits. To conduct this study, an ASTER measuring frame was utilized, which, after performing atmospheric corrections using the internal average relative reflectance (IARR) method of false color composite images and principal component analysis (PCA), was able to differentiate between different lithological units using the Band assignment method, full-pixel methods of spectral angle mapper (SAM) and base spectrum algorithm of spectral  feature fitting (SFF) as well as sub-pixel methods of matched filtering. The study demonstrates that the approach of principal component analysis and false color composition is efficient for distinguishing sedimentary rock units from igneous rock units, and its application is suggested for the designated rock units. Due to the lack of spectral characteristics of feldspars and quartz in the short infrared wavelength range, the basic spectrum methods utilized in this work are incapable of identifying such minerals. It is not advised to use these algorithms to distinguish between various magmatic units.
利用波段比法、全像素(SAM和SFF)和亚像素(MF和SID)方法,利用Aster传感器发现变化区域:以伊朗西北部Sivardaghi地区为例
ASTER传感器数据是进行地质调查最有效的卫星数据之一,具有整个地球表面的图像。为了测试该传感器探测地球化学变化地点的能力,本研究使用了伊朗西部萨马勒省的Seiver Daghi山的照片。该地区由岩浆和火山地形组成,是Arsbaran领土的一部分,被带有冲积和沉积矿床的侵入体所覆盖。为了进行这项研究,利用ASTER测量框架,在使用假彩色合成图像的内部平均相对反射率(IARR)方法和主成分分析(PCA)进行大气校正后,能够使用波段分配方法区分不同的岩性单元。光谱角映射器(SAM)的全像元方法和光谱特征拟合(SFF)的基谱算法以及匹配滤波的亚像元方法。研究表明,主成分分析和伪色组成方法是区分沉积岩单元和火成岩单元的有效方法,并建议将其应用于指定的岩石单元。由于长石和石英在短红外波长范围内缺乏光谱特征,本工作中使用的基本光谱方法无法识别这类矿物。不建议使用这些算法来区分不同的岩浆单元。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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