U and Th concentrations and isotope ratios of samples from ODP Leg 166
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 attemp...
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Format: | Other/Unknown Material |
Language: | English |
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PANGAEA
2002
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.710924 https://doi.org/10.1594/PANGAEA.710924 |