2019
DOI: 10.18520/cs/v116/i10/1639-1647
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Landsat 8 OLI Data for Identification of Hydrothermal Alteration Zone in Singhbhum Shear Zone using Successive Band Depth Difference Technique–A New Image Processing Approach

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Cited by 19 publications
(4 citation statements)
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“…Therefore, additional reference detectors collect the signal from the 20.7, 21.5, and 31.5 µm lines (483, 465, and 317 cm −1 ), where sulfides and ilmenite do not show spectral features. Such an approach will allow determining the influence of the Sun's geometry and topography on the obtained results -a similar approach is applied in the Landsat 8 (Safari et al, 2018;Banerjee et al, 2019;Sekandari et al, 2020), ASTER (Safari et al, 2018;Zoheir et al, 2019;Sekandari et al, 2020), Sentinel-2 (Zoheir et al, 2019;Sekandari et al, 2020;Soydan et al, 2021), or PRISMA (Loizzo et al, 2018;Bedini and Chen, 2022;Chirico et al, 2023) spectral bands on Earth. Apart from minor interferences with H 2 O and CO 2 molecules in the FIR band, which in any case is nearly irrelevant on the Moon, the main FIR advantage is the robust absorption features of oxides and sulfides (Figure 6A) compared to rock-forming silicates (Figure 6B) and other common minerals (Figure 6C; Figure 7).…”
Section: Spectral Ranges and Interferencesmentioning
confidence: 99%
“…Therefore, additional reference detectors collect the signal from the 20.7, 21.5, and 31.5 µm lines (483, 465, and 317 cm −1 ), where sulfides and ilmenite do not show spectral features. Such an approach will allow determining the influence of the Sun's geometry and topography on the obtained results -a similar approach is applied in the Landsat 8 (Safari et al, 2018;Banerjee et al, 2019;Sekandari et al, 2020), ASTER (Safari et al, 2018;Zoheir et al, 2019;Sekandari et al, 2020), Sentinel-2 (Zoheir et al, 2019;Sekandari et al, 2020;Soydan et al, 2021), or PRISMA (Loizzo et al, 2018;Bedini and Chen, 2022;Chirico et al, 2023) spectral bands on Earth. Apart from minor interferences with H 2 O and CO 2 molecules in the FIR band, which in any case is nearly irrelevant on the Moon, the main FIR advantage is the robust absorption features of oxides and sulfides (Figure 6A) compared to rock-forming silicates (Figure 6B) and other common minerals (Figure 6C; Figure 7).…”
Section: Spectral Ranges and Interferencesmentioning
confidence: 99%
“…Multispectral images are generated from monochromatic bands by the application of a layer-stacking process [38][39][40][41]. CC allows the production of color images using the spectral signature of the targets [42]. They are commonly deployed to highlight different surface types in multispectral images or to make evident some crucial environmental phenomena, such as sandstorms, forest fires, and sea ice The CC simplifies it to describe and understand a multiband image by using different colors as indicators of the values of single-channel [43].…”
Section: Color Composition(cc)mentioning
confidence: 99%
“…The following supporting information can be downloaded at: https: //www.mdpi.com/article/10.3390/su142215349/s1, Figure S1 S1: Summary of selected satellite sensors; Table S2: Details of the most color composite used in geology; Table S3: Details band ratios usefulness in geological studies; Table S4: Accuracy assessment for SAM for SAM classification of ASTER image. Refs [23][24][25][26][39][40][41][42][43] are citied in supplementary materials.…”
Section: Supplementary Materialsmentioning
confidence: 99%
“…There are many case studies [1][2][3] illustrating the application of multispectral data (such as ASTER and Landsat TM data) in geological mapping that allow discrimination of lithological units, structural interpretation and detection of minerals bearing host rocks. Many researchers have made use of ASTER, Landsat TM and Landsat 8 data for geological mapping, visualising lineaments, and mineral prospecting [4][5][6][7][8][9][10].…”
Section: Introductionmentioning
confidence: 99%