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• W1970193315 abstract "Low-temperature alteration of the oceanic crust is a major sink for the U supplied to the oceans and may account for about 50% of the estimated present-day input of this element. Uranium uptake by organic-rich sediments and coexisting phosphorites on continental margins is also important and may remove in excess of 10% of the total supply. High-temperature alteration of oceanic basalts, metalliferous sediments, carbonate sediments, and sediments in anoxic basins deeper than 200 m play a relatively minor role in the removal of U. Each of these sinks is responsible for the uptake of less than 5% of the overall input." @default.
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• W1970193315 date "1980-02-01" @default.
• W1970193315 modified "2023-09-26" @default.
• W1970193315 title "Some factors controlling the concentration of uranium in the world ocean" @default.
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• W1970193315 doi "https://doi.org/10.1016/0016-7037(80)90145-3" @default.
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