Correction factors for systematic errors related to the track counts in fission-track dating with the external detector method
Tracks from uranium fission are the basis of fission-track dating of minerals. The fission-track method has not attained the status of an independent dating method because of problems related to neutron fluence measurements and the decay constant. Fission-track ages are instead determined relative t...
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Published in | Radiation measurements Vol. 36; no. 1; pp. 351 - 356 |
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Main Authors | , |
Format | Journal Article Conference Proceeding |
Language | English |
Published |
Oxford
Elsevier Ltd
01.09.2003
Elsevier |
Subjects | |
Online Access | Get full text |
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Summary: | Tracks from uranium fission are the basis of fission-track dating of minerals. The fission-track method has not attained the status of an independent dating method because of problems related to neutron fluence measurements and the decay constant. Fission-track ages are instead determined relative to the reference ages of standards using an empirical calibration factor (
ζ-method). Methodical advances during the last decade imply that these problems need not remain obstacles to establishing fission-track dating as an independent method. However, sources of systematic error related to the track density measurements need to be corrected before this can be the case.
A correction factor (GQR), determined by experiment, is in good agreement with its calculated value. The ages of apatites of known age determined with the
φ-method are also in good agreement with their reference ages. When applied to a set of samples of unknown age, the
φ-method produces results that are consistent with those obtained with the
Z- and
ζ-methods. These results lend support to the method of neutron fluence measurement, to the recommended value of the decay constant and to the calculated and measured GQR-value. On the other hand, these results call into question the validity of age corrections based on confined track length measurements. |
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ISSN: | 1350-4487 1879-0925 |
DOI: | 10.1016/S1350-4487(03)00150-1 |