Uranium in submarine metalliferous deposits |
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Authors: | Harold S Rydell Enrico Bonatti |
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Affiliation: | Rosenstiel School of Marine and Atmospheric Science, University of Miami, Miami, Florida 33149, U.S.A. |
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Abstract: | Hydrothermal submarine metalliferous deposits, common in areas of the ocean floor with high heat flow, contain generally about 10 ppm U as an order of magnitude. The ratio is in the majority of cases close to that of seawater; only in a few cases is it anomalously high. Anomalous ratios are coupled with low U concentrations. These data are explained by a model where thermal water (essentially heated seawater) in its sub-bottom circulation often is unable to leach U from the basaltic oceanic crust; in fact, these thermal waters may in some cases lose U. When leaching of U from the basalt does take place, probably during shallow stages of the sub-bottom circulation, the resulting anomalous ratio can be preserved in the hydrothermal deposit only if mixing with ‘seawater’ U is prevented. |
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