1980
DOI: 10.3133/ofr80367
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Alteration mapping using multispectral images: Cuprite mining district, Esmeralda County, Nevada

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Cited by 51 publications
(96 citation statements)
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“…The study area is located in Cuprite in western Nevada, U.S.A. Cuprite is one of the most popular sites for testing the performance of new sensors and spectral mapping methods in geologic remote sensing studies (e.g., Abrams et al, 1977;Ashley and Abrams, 1980;Swayze et al, 2014). In this area, the Tertiary volcanic rocks were hydrothermally altered in the Midto Late-Miocene epoch.…”
Section: Study Area and Datamentioning
confidence: 99%
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“…The study area is located in Cuprite in western Nevada, U.S.A. Cuprite is one of the most popular sites for testing the performance of new sensors and spectral mapping methods in geologic remote sensing studies (e.g., Abrams et al, 1977;Ashley and Abrams, 1980;Swayze et al, 2014). In this area, the Tertiary volcanic rocks were hydrothermally altered in the Midto Late-Miocene epoch.…”
Section: Study Area and Datamentioning
confidence: 99%
“…In this area, the Tertiary volcanic rocks were hydrothermally altered in the Midto Late-Miocene epoch. The hydrothermally altered rocks were divided into three groups: silicified rocks, opalized rocks and argillized rocks, as shown in Figure 1 (Ashley and Abrams, 1980).…”
Section: Study Area and Datamentioning
confidence: 99%
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“…Cuprite, NV, USA, located approximately 200 km northwest of Las Vegas, is well understood mineralogically [5,36,37] and has been used as a geological remote sensing test site since the early 1980s [36,[38][39][40][41]. Among the 18 minerals presented in this area, three of them (Alunite, Chalcedony, and Kaolinite) are selected because their outcrops can be spatially and spectrally clearly identified with both high SNR AVIRIS and low SNR Hyperion HSI data simultaneously.…”
Section: Experiments and Resultsmentioning
confidence: 99%
“…The site is ideal for remote sensing because it is relatively well known, there is little vegetation, there are a variety of minerals with sharp absorption features, and there are some areas of pure minerals. Materials at the surface consist primarily of volcanic rocks that have been hydrothermally altered (changed by hot water passing through the rocks) in a fossilized hot-springs environment [8,15]. Common hydrothermal alteration minerals present include silica (chalcedony), kaolinite, dickite, alunite, buddingtonite (an ammonium feldspar), muscovite, jarosite, and montmorillonite [8].…”
Section: Application Of Spectral Library Analysis Results To Airbornementioning
confidence: 99%