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• W2273759158 abstract "We have evaluated the temporal distribution of Mississippi Valley-type (MVT) Zn-Pb deposits with special attention to the nature and number of deposits of Precambrian age. Our evaluation is based on the widely used model for MVT mineralization involving metal-bearing brines that lack reduced S and that deposit sulfides only where they encounter a reservoir of sulfide or where sulfate in the metal-bearing brine is reduced to sulfide. For MVT systems of this type, basins with abundant sulfate would be most favorable for development of MVT mineralization because these would allow transport of metals in sulfate-rich brines and deposition of metals in areas where the sulfate was reduced. Because abundant sulfate requires abundant atmospheric oxygen, the distribution of MVT deposits through time might reflect compositional changes in Earth's atmosphere, especially the suggested Great Oxidation Event (GOE)." @default.
• W2273759158 created "2016-06-24" @default.
• W2273759158 creator A5030224049 @default.
• W2273759158 creator A5067288937 @default.
• W2273759158 date "2006-01-01" @default.
• W2273759158 modified "2023-09-25" @default.
• W2273759158 title "Precambrian Mississippi Valley–type deposits: Relation to changes in composition of the hydrosphere and atmosphere" @default.
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• W2273759158 doi "https://doi.org/10.1130/2006.1198(11)" @default.
• W2273759158 hasPublicationYear "2006" @default.
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