利用遥感技术进行岩性填图:以蒙古多诺戈壁省阿拉格巴扬地区为例

Badrakh Munkhsuren, B. Enkhdalai, T. Narantsetseg, Khurelchuluun Udaanjargal, D. Orolmaa, Dolgorjav Munkhjin
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引用次数: 0

摘要

本研究调查了包括ASTER、Landsat 8 OLI和Sentinel 2A数据在内的多光谱遥感技术,以区分蒙古多尔诺戈比省Alagbayan地区的不同岩性单元。因此,主成分分析(PCA)、带比(BR)和支持向量机(SVM)这些广泛使用的图像增强方法已被应用于岩性测绘的卫星图像。监督分类的结果表明,当选择以前的地质图和薄片分析作为训练样本的参考时,Landsat数据给出了更好的分类,总体准确率为93.43%,kappa系数为0.92。此外,从ASTER获得的(带7+带9)/带8)的带比率与碳酸盐岩非常一致。根据陆地卫星RGB中的PCs、PC4、PC3和PC2,ASTER数据的PC3、PC2、PC6被选为不同岩性单元的良好指标,志留系、石炭系、侏罗系和白垩纪地层很容易区分。就陆地卫星图像而言,最有效的BR是冲积层的BR为5/4,片岩的BR为4/7,花岗岩的BR为7/6。此外,由于BR和PCA,可以确定前寒武纪Khutag-Uul变质杂岩和Norovzeeg地层,但花岗片麻岩和片岩没有给出令人满意的结果。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Lithological mapping using remote sensing techniques: A case study of Alagbayan area, Dornogobi province, Mongolia
This study investigated the multispectral remote sensing techniques including ASTER, Landsat 8 OLI, and Sentinel 2A data in order to distinguish different lithological units in the Alagbayan area of Dornogobi province, Mongolia. Therefore, Principal component analysis (PCA), Band ratio (BR), and Support Vector Machine (SVM), which are widely used image enhancement methods, have been applied to the satellite images for lithological mapping. The result of supervised classification shows that Landsat data gives a better classification with an overall accuracy of 93.43% and a kappa coefficient of 0.92 when the former geologic map and thin section analysis were chosen as a reference for training samples. Moreover, band ratios of ((band 7 + band 9)/band 8) obtained from ASTER corresponds well with carbonate rocks. According to PCs, PC4, PC3 and PC2 in the RGB of Landsat, PC3, PC2, PC6 for ASTER data are chosen as a good indicator for different lithological units where Silurian, Carboniferous, Jurassic, and Cretaceous formations are easily distinguished. In terms of Landsat images, the most efficient BR was a ratio where BRs of 5/4 for alluvium, 4/7 for schist and 7/6 to discriminate granite. In addition, as a result of BR as well as PCA, Precambrian Khutag-Uul metamorphic complex and Norovzeeg formation can be identified but granite-gneiss and schist have not given satisfactory results.
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