1957
DOI: 10.2113/gsecongeo.52.5.499
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Occurrence of selenium in sulfides from some sedimentary rocks of the western United States

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Cited by 74 publications
(43 citation statements)
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“…Davidson (1963) surveyed uranium deposits in oxidized sandstones ranging from Paleozoic to Cenozoic age in several States across the United States and found selenium concentrations that ranged from 3 to 4,500 ppm. In a survey by Coleman and Delevaux (1957), selenium concentrations up to 3 weight percent were measured in uranium deposits of the Colorado Plateau.…”
Section: B Selenide Minerals In Unconformity-related Uranium Depositmentioning
confidence: 99%
“…Davidson (1963) surveyed uranium deposits in oxidized sandstones ranging from Paleozoic to Cenozoic age in several States across the United States and found selenium concentrations that ranged from 3 to 4,500 ppm. In a survey by Coleman and Delevaux (1957), selenium concentrations up to 3 weight percent were measured in uranium deposits of the Colorado Plateau.…”
Section: B Selenide Minerals In Unconformity-related Uranium Depositmentioning
confidence: 99%
“…Selenium is known to have volcanic, magmatic, and hydrothermal sources (Trelease and Beath, 1949;Coleman and Delevaux, 1957;Sindeeva, 1964;Howard, 1977) and is present in relation to hydrothermal and roll-type uranium deposits (Sindeeva, 1964;Fishman and others, 1985;Fishman and Reynolds, 1986). Selenium enrichment of geologic materials occurred during the Cretaceous age and was related to volcanic emanations of element-rich gases and ashes.…”
Section: Review Of Selenium Geochemistrymentioning
confidence: 99%
“…Selenium is present as a trace constituent in pyrite in the Mancos Shale within the study area; concentrations range from 0.003 to 1.6 percent (Coleman and Delevaux, 1957). When the Mancos Shale is exposed to weathering, selenium weathers (or is oxidized) from pyrite (where the selenium has a valence state of -2) to further transformations in valence state (-2 -> 0 -> +4 -> +6) that become increasingly more soluble with increasing valence: elemental selenium (Se°, selenium valence of 0), selenite (SeIVO32~, selenium valence of+4), biselenite (HSeIVO3~, selenium valence of +4), and selenate (SeVIO42~, selenium valence of +6).…”
Section: Ground-water Investigations 31mentioning
confidence: 99%
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