A Comparative Study of Landsat‐7 and Landsat‐8 Data Using Image Processing Methods for Hydrothermal Alteration Mapping. Issue 1 (January 2017)

• Record Type: Journal Article
• Authors: Masoumi, Feizollah; Eslamkish, Taymour; Honarmand, Mehdi; Abkar, Ali Akbar
• Is Part Of: Resource geology. Volume 67:Issue 1(2017:Jan.)
• Page Start: 72
• Page End: 88
• Publication Date: 2017-01
• Subjects: Landsat‐7 -- Landsat‐8 -- hydrothermal alteration -- Spectral angle mapper -- Principal component analysis -- Band ratio; Mining geology -- Periodicals; Mining geology -- Pacific Area -- Periodicals; Mining geology -- Asia -- Periodicals; Geochemistry -- Periodicals; Environmental geology -- Periodicals; 553
• DOI: 10.1111/rge.12117
• Languages: English
• ISSNs: 1344-1698

Abstract

Abstract: Comparing spaceborne satellite images of Landsat‐8 Operational Land Imager (OLI) and Landsat‐7 Enhanced Thematic Mapper plus (ETM+) was undertaken to investigate the relative accuracy of mapping hydrothermal alteration minerals. The study investigated the northern part of Rabor, which contains copper mineralization occurrences, and is located in the Kerman Cenozoic magmatic assemblage (KCMA), Iran. Image processing methods of band ratio, principal component analysis (PCA), and spectral angle mapper (SAM) were used to map the distribution of hydrothermally altered rocks associated with the porphyry copper mineralization. The band ratio combination of both sensors for mapping altered areas showed similar outcomes. PCA exposed variations in the spatial distribution of hydroxyl‐bearing minerals. The representation of hydrothermal areas using OLI data was more satisfactory than when using ETM+ data. SAM analysis found similar results for mapping hydroxyl‐bearing zones. Verification of the results came through ground investigation and laboratory studies. Rock samples ( n = 56) were collected to validate results using thin sections, X‐ray diffraction (XRD) and spectral analyses. Field observations and laboratory analysis revealed that phyllic and propylitic alterations dominate the alteration zones in the study area. Argillic and iron oxides/hydroxides alterations were observed to a lesser degree. The results indicate that alteration maps prepared by OLI data using PCA for visual interpretation are more suitable than those of ETM+ due to a higher radiometric resolution and lower interference between vegetation and altered areas. As the spectral bandwidth of ETM+ band 7 covers absorption feature of propylitic alteration, better mapping of propylitic alterations is achieved using ETM+ data. Abstract : SAM analysis of both datasets found similar results for mapping hydroxyl‐bearing zones. Propylitic alteration was mapped by ETM+ data better than OLI data. Color composite of band ratios show similar results for mapping alterations whereas PCA found that OLI data were suitable than ETM+ data.