Seawater (U-234/U-238) during the last 800 thousand years
Constraining the history of seawater (234U/238U) is important because this ratio is used to assess the validity of U/ Th ages, and because it provides information about the past rate of physical weathering on the continents. This study makes use of U-rich slope sediments from the Bahamas in an attem...
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Format: | Journal article |
Language: | English |
Published: |
2002
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