Reassessing the uranium decay constants for geochronology using ID-TIMS U Pb data

Details Reassessing the uranium decay constants for geochronology using ID-TIMS U Pb data Reassessing the uranium decay constants for geochronology using ID-TIMS U Pb data

Jan 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006gecoa..70..426s&link_type=abstract

Geochimica et Cosmochimica Acta, Volume 70, Issue 2, p. 426-445.

Mathematics

Logic

47

Scientific paper

As the internal precision of radiometric dates approaches the 0.1% level, systematic biases between different methods have become apparent. Many workers have suggested that calibrating other decay constants against the U Pb system is a viable solution to this problem. We test this assertion empirically and quantitatively by analyzing U Pb systematics of zircon and xenotime on the single- to sub-grain scale by high-precision ID-TIMS geochronology on 11 rock samples ranging from 0.1 to 3.3 Ga. Large statistically equivalent datasets give 207Pb/206Pb dates that are systematically older than 206Pb/238U dates by ˜0.15% in Precambrian samples to as much as ˜3.3% in Mesozoic samples, suggesting inaccuracies in the mean values of one or both of the U decay constants. These data are used to calculate a ratio of the U decay constants that is lower than the accepted ratio by 0.09% and is a factor of 5 more precise. Four of the samples are used to augment existing data from which the U Pb and 40Ar/39Ar systems can be compared. The new data support most previous observations that U Pb and 207Pb/206Pb dates are older than 40Ar/39Ar by ⩽1%, though scatter in the amount of offset in samples as a function of age suggests that the bias is not entirely systematic, and may incorporate interlaboratory biases and/or geologic complexities. Studies that calibrate other decay schemes against U Pb should include an assessment of inaccuracies in the U decay constants in addition to other systematic biases and non-systematic geologic uncertainty.

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