U-234/U-238 RATIOS IN QUATERNARY PLANKTONIC-FORAMINIFERA
234U 238U measurements on foraminifera could potentially provide an indicator of foraminifera diagenesis, a proxy for past seawater 234U 238U and, significantly, a direct dating tool for foraminifera. Such measurements are complicated, however, by the very low concentration of U in foraminifera and...
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Format: | Journal article |
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1995
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