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Uncertainties on the luminescence ages and anomalous fading

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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
It is well known that some minerals give underestimated luminescence ages due to anomalous fading. The anomalous fading follows a logarithmic decay law characterized by its slope, the socalled fading rate or g-value. Using the fading rate, Huntley and Lamothe (2001) suggested some correction for the fading underestimation of young samples (<40-50 ka). For polymineral fine grains, we observe a fading rate of 0-4%/decade for TL and BL-OSL and 4-6%/decade for IR-OSL. Extending the laboratory observation to archaeological age, the underestimation on the age for 10 ka is estimated to a mean of 5% for TL, 10% for BL-OSL and 45% for IR-OSL. Due to the non-linearity of the Huntley and Lamothe's fading correction, the contribution of the fading to the total uncertainty is estimated by a Monte-Carlo simulation. The inference on dating shows that the uncertainty on the anomalous fading can be a significant term of the combined uncertainty on the age, even for low fading rates.
Wydawca
Czasopismo
Rocznik
Tom
Strony
47--50
Opis fizyczny
Bibliogr. 13 poz., rys., tab.
Twórcy
autor
  • Centre de Recherche et de Restauration des Musées de France, Palais du Louvre, Porte des lions, 14 quai F. Mitterrand, 75001 Paris, antoine.zink@culture.gouv.fr
Bibliografia
  • 1. Adamiec G and Aitken MJ, 1998. Dose-rate conversion factors: update. Ancient TL 16: 37-49.
  • 2. Aitken MJ, 1985, Thermoluminescence dating. London, Academic Press: 360 pp.
  • 3. Auclair M, Lamothe M and Huot S, 2003. Measurement of anomalous fading for feldspar IRSL using SAR. Radiation measurements 37(4-5): 487-492, DOI 10.1016/S1350-4487(03)00018-0.
  • 4. Buck CE, Cavanagh WG and Litton CD, 1996. Bayesian approach to interpreting archaeological data. Chichester, John Wiley and sons: 382 pp.
  • 5. Huntley DJ and Lamothe M, 2001. Ubiquity of anomalous fading in Kfeldspars and the measurement and correct. Canadian Journal of Earth Science 38(7): 1093-1106, DOI 10.1139/cjes-38-7-1093.
  • 6. Kacker R, Toman B and Huang D, 2006. Comparison of ISO-GUM, draft GUM Supplement 1 and Bayesian statistics using simple linear calibration. Metrologia 43: S167–S177, DOI 10.1088/0026-1394/43/4/S02.
  • 7. Kerman J and Gelman A, 2006. Bayesian Data Analysis using R. Rnews 6: 21-24.
  • 8. Lai Z-P, Brückner H, 2008. Effects of feldspar contamination on equivalent doses and the shape of growth curves for OSL of siltsized quartz extracted from Chinese loess. Geochronometria 30: 49-53, DOI 10.2478/v10003-008-0010-0.
  • 9. Preusser F, 2003. IRSL dating of K-rich feldspars using the SAR protocol: Comparison with independent age control. Ancient TL 21: 17-23.
  • 10. R Development Core Team, 2007. R: A language and environment for statistical computing. R Foundation for Statistical Computing, Vienna, Austria. ISBN 3-900051-07-0, URL http://www.Rproject. org.
  • 11. Visocekas R, 1988. Comparison between tunnelling afterglows following alpha and beta irradiation. Nuclear Tracks and Radiation Measurements 14: 163-166, DOI 10.1016/1359-0189(88)90058-1.
  • 12. Winlte AG, 1973. Anomalous fading of thermoluminescence in mineral samples. Nature 245(5421): 143-144, DOI 10.1038/245143a0.
  • 13. Zimmerman DW, 1971. Thermoluminescence dating using the fine grains from pottery. Archaeometry 13(1): 29-52, DOI 10.1111/j.1475-4754.1971.tb00028.x.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BAT8-0012-0051
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