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Residual doses in recent alluvial sediments from the Ardenne (S Belgium)

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Języki publikacji
EN
Abstrakty
EN
We report on our first investigations into the potential of optical dating for determining the rate of river flood sedimentation in the Ardenne region (S Belgium). Two samples collected from a recent alluvial deposit were used to investigate the extent of resetting in different particle size fractions of quartz (4-11 µm, 63-90 µm, 90-125 µm, 125-180 µm, 180-212 µm and 212-250 µm) as well as in polymineral fine (4-11 µm) grains. Both samples show satisfactory OSL and IRSL characteristics. The IRSL signals from the polymineral fine grains yield an equivalent dose (De) of 3-4 Gy, while a De of 0.3-0.6 Gy was measured using large aliquots of quartz. Small aliquot analyses of 63-90 µm and 212-250 µm quartz grains confirm that the coarser fraction contains more grains with lower De's. Furthermore, for a modern sample (‹ 3 years old), ˜60% of the aliquots yields a De consistent with zero, indicating that these contain only well-bleached grains. These findings suggest that it might be possible to extract the true burial dose from dose distributions measured using small aliquots of coarse-grained (e.g. 212-250 µm) quartz.
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Tom
Strony
1--8
Opis fizyczny
Bibliogr. 22 poz., rys.
Twórcy
autor
  • Laboratory of Mineralogy and Petrology (Luminescence Research Group), Geological Institute, Ghent University, Krijgslaan 281 (S8), B-9000 Gent, Belgium, dimitri.vandenberghe@UGent.be
Bibliografia
  • 1. Alexanderson H, 2007. Residual OSL signals from modern Greenlandic river sediments. Geochronometria 26: 1-9, DOI 10.2478/v10003-007-0001-6.
  • 2. 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.
  • 3. Bøtter Jensen L, Andersen CE, Duller GAT and Murray AS, 2003. Developments in radiation, stimulation and observation facilities in luminescence measurements. Radiation Measurements 37(4-5): 535-541, DOI 10.1016/S1350-4487(03)00020-9.
  • 4. Frechen M, Schweitzer U and Zander A, 1996. Improvements in sample preparation for the fine grain technique. Ancient TL 14(2): 15-17.
  • 5. Fuchs M, Straub J and Zöller L, 2005. Residual luminescence signals of recent river flood sediments: a comparison between quartz and feldspar of fine- and coarse-grain sediments. Ancient TL 23: 25-30
  • 6. Houbrechts G, 2005. Utilisation des macroscories et des microscories en dynamique fluviale: application aux rivières du massif ardennais (Belgique) (Using macroscopic and microscopic slags in fluvial dynamics: application to Ardenne’s rivers (Belgium)). PhD thesis, University of Liège: 328 pp (in French).
  • 7. Houbrechts G and Petit F, 2006, Utilisation des microscories métallurgiques comme traceur de la sédimentation dans les plaines alluviales ardennaises (Use of metallurgic microscopic slags as tracer for sedimentation in the alluvial plains of the Ardenne). L’érosion entre société, climat et paléoenvironnement, Collection Nature et Société, Presses universitaires Blaise Pascal 3: 93-98 (in French).
  • 8. Jain M, Murray AS and Bøtter-Jensen L, 2004. Optically stimulated luminescence dating: how significant is incomplete light exposure in fluvial environments? Quaternaire 15: 143-157.
  • 9. Juvigné E, 1979. L’encaissement des rivières ardennaises depuis le début de la dernière glaciation (Downcutting of Ardenne’s rivers since the beginning of the last glaciation). Zeitschrift für Geomorphologie 23: 291-300 (in French).
  • 10. Lang A, Lindauer S, Kuhn R and Wagner GA, 1996. Procedures used for optically and infrared stimulated luminescence dating of sediments in Heidelberg. Ancient TL 14(3): 7-11.
  • 11. Lepper K, Agersnap Larsen N, McKeever SWS, 2000. Equivalent dose distribution analysis of Holocene eolian and fluvial quartz sands from Central Oklahoma. Radiation Measurements 32(5-6): 603-608, DOI 10.1016/S1350-4487(00)00093-7.
  • 12. Mauz B, Bode T, Mainz E, Blanchard H, Hilger W, Dikau R and Zöller L, 2002. The luminescence dating laboratory at the University of Bonn: equipment and procedures. Ancient TL 20(2): 53-61.
  • 13. Murray AS and Olley JM, 2002. Precision and accuracy in the optically stimulated luminescence dating of sedimentary quartz: a status review. Geochronometria 21: 1-16.
  • 14. Murray AS and Wintle AG, 2000. Luminescence dating of quartz using an improved single-aliquot regenerative-dose protocol. Radiation Measurements 32(1): 57-73, DOI 10.1016/S1350-4487(99)00253-X.
  • 15. Murray AS and Wintle AG, 2003. The single aliquot regenerative dose protocol: potential for improvements in reliability. Radiation Measurements 37(4-5): 377-381, DOI 10.1016/S1350-4487(03)00053-2.
  • 16. Olley JM, Caitcheon G and Murray AS, 1998. The distribution of apparent dose as determined by optically stimulated luminescence signals in small aliquots of fluvial quartz: implications for dating young sediments. Quaternary Science Reviews 17(11): 1033-1040, DOI 10.1016/S0277-3791(97)00090-5.
  • 17. Petit F, Gob F, Houbrechts G and Assani AA, 2005. Critical specific stream powers in gravel-bed rivers. Geomorphology 69(1-4): 92-101, DOI 10.1016/j.geomorph.2004.12.004.
  • 18. Truelsen JL and Wallinga J, 2003. Zeroing of the OSL signal as a function of grain size: investigating bleaching and thermal transfer for a young fluvial sample. Geochronometria 22: 1-8.
  • 19. Vandenberghe D, 2004. Investigation of the optically stimulated luminescence dating method for application to young geological sediments. PhD thesis, Ghent University: 358pp.
  • 20. Vandenberghe D, Hossain SM, De Corte F and Van den haute P, 2003. Investigations on the origin of the equivalent dose distribution in a Dutch coversand. Radiation Measurements 37(4-5): 433-439, DOI 10.1016/S1350-4487(03)00051-9.
  • 21. Vandenberghe D, Vanneste K, Verbeeck K, Paulissen E, Buylaert JP, De Corte F. and Van den haute P, accepted. Late Weichselian and Holocene earthquake events along the Geleen fault in NE Belgium: OSL age constraints. Quaternary International.
  • 22. Wallinga J, 2002. Optically stimulated luminescence dating of fluvial deposits: a review. Boreas 31(4): 303-322, DOI 10.1080/030094802320942536.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BATA-0001-0054
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