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ESR dating of sedimentary quartz from two pleistocene deposits using Al and Ti-centers

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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
One sample from a fluvial terrace of Loir river (France) deposited during isotopic stages 7-8 and two samples from isotopic stage 5 marine sediments of Echizen Coast (Japan) were dated by ESR of quartz grains. Both additive and regenerative techniques were used on Ti-Li and Ti-H centers of quartz. No change of sensitivity of the centers was observed during regeneration which significantly reduced the errors on the equivalent doses. Bleaching experiments indicated that the Ti-Li center is less sensitive to UV(ultra-violet)-A (365-412 nm) than to the full sun spectrum whereas UVA alone is sufficient to reset the bleachable component of the Al-center. This effect could be the origin of the strong overestimation of the ages determined using the Ti-Li center in this study. The comparison of the equivalent doses determined by the two Ti-centers indicated that bleaching before deposition of the fluvial sediment was apparently better than for the marine sample.
Słowa kluczowe
Wydawca
Czasopismo
Rocznik
Tom
Strony
23--31
Opis fizyczny
Bibliogr. 19 poz., rys., tab.
Twórcy
autor
autor
autor
autor
autor
autor
autor
  • Department of Applied Physics, Okayama University of Science, 1-1 Ridai, Okayama, 700-0005, Japan, tissoux@mnhn.fr
Bibliografia
  • 1. Bahain JJ, Laurent M, Falguères C, Voinchet P, Farkh S and Tissoux H, 2002. Datation par résonance paramagnétique électronique (RPE) des formations fluviatiles pléistocènes et des gisements archéologiques ou paléontologiques associés (Electron spin resonance (ESR) dating of Pleistocene fluvial formations and of associated archaeological or palaeontological sites). Quaternaire 13: 91-103 (in French).
  • 2. Beerten K and Stesmans A, 2006. The Use of Ti centers for estimating burial doses of single quartz grains: A case study from an aeolian deposit ~ 2 Ma old. Radiation Measurements 41(4): 418-424, DOI 10.1016/j.radmeas.2005.10.004.
  • 3. Beerten K and Stesmans A, 2006. Some properties of Ti-related paramagnetic centres relevant for electron spin resonance dating of single sedimentary quartz grains. Applied Radiation and Isotopes 64(5): 594-602, DOI 10.1016/j.apradiso.2005.12.001.
  • 4. Beerten K, Lomax J, Clémer K, Stesmans A and Radtke U, 2006. On the use of Ti centres for estimating burial ages of Pleistocene sedimentary quartz: Multiple-grain data from Australia. Quaternary Geochronology 1(2): 151-158, DOI 10.1016/j.quageo.2006.05.037.
  • 5. Despriée J, Voinchet P, Bahain JJ, Falguères C, Lorain JM and Duvialard J, 2003. Les nappes alluviales pléistocènes du Loir dans la région de Vendôme (Loir-et-Cher, France) : contexte morphosédimentaire et chronologie RPE. Quaternaire 14 : 207-218 (in French).
  • 6. Falguères C, Yokoyama Y and Quaegebeur JP, 1988. Datations de sédiments quaternaires par la méthode de résonance de spin électronique (ESR) (Electron spin resonance (ESR) Dating of Quaternary Sediment). L’Anthropologie 92: 723-726 (in French).
  • 7. Grün R, Tani A, Gurbanov A, Koschung D, Williams I and Braun J, 1999. A new method for the estimation of cooling and denudation rates using paramagnetic centers in quartz : a case study on the Eldzhurtinskiy Granite, Caucasus. Journal of Geophysical Research 104(B8): 17531-17549.
  • 8. Imai N, Shimokawa K, Sakaguchi K and Takada M, 1992. ESR dates and thermal behaviour of Al and Ti centers in quartz for the tephra and welded tuff in Japan. Quaternary Science Reviews 11(1-2): 257-265, DOI 10.1016/0277-3791(92)90071-F.
  • 9. Laurent M, Falguères C, Bahain JJ, Rousseau L and Van Vliet Lanoe B, 1998. ESR dating of quartz extracted from quaternary and neogene sediments: method, potential and actual limits. Quaternary Science Reviews 17(11): 1057-1062, DOI 10.1016/S0277-3791(97)00101-7.
  • 10. Machida H and Arai F 2003. Atlas of Tephras in and around Japan. University of Tokyo Presse : 120 pp (in Japanese).
  • 11. Tanaka K, Hataya R, Spooner NA, Questiaux DG, Saito Y and Hashimoto T, 1997. Dating of marine terrace sediments by ESR, TL and OSL methods and their applicabilities. Quaternary Science Reviews 16(3-5): 257-264, DOI 10.1016/S0277-3791(96)00092-3.
  • 12. Tissoux H, Falguères C, Voinchet P, Toyoda S, Bahain JJ and Despriée J, 2007. Potential use of Ti-center in ESR dating of Fluvial Sediment. Quaternary Geochronology 2(1-4): 367-372., DOI 10.1016/j.quageo.2006.04.006.
  • 13. Toyoda S and Ikeya M, 1991. Thermal stabilities of paramagnetic defect and impurity centers in quartz : basis for ESR dating of thermal history. Geochemical Journal 25: 437-445.
  • 14. Toyoda S and Falguères C, 2003. The method to represent the ESR intensity of the aluminium hole center in quartz for the purpose of dating. Advances in ESR applications 20: 7-10.
  • 15. Toyoda S, Voinchet P, Falguères C, Dolo JM and Laurent M, 2000. Bleaching of ESR signals by the sunlight: a laboratory experiment for establishing the ESR dating of sediments. Applied Radiation and Isotopes 52(5): 1357-1362, DOI 10.1016/S0969-8043(00)00095-6.
  • 16. Voinchet P, Falguères C, Laurent M, Toyoda S, Bahain JJ and Dolo JM, 2003. Artificial optical bleaching of the aluminium center in quartz implications to ESR dating of sediments. Quaternary Science Reviews 22(10-13): 1335-1338, DOI 10.1016/S0277-3791(03)00062-3.
  • 17. Voinchet P, Bahain JJ, Falguères C, Laurent M, Dolo JM, Despriée J, Gageonnet R and Chaussé C, 2004. ESR dating of quartz extracted from Quaternary sediments: Application to fluvial terraces systems of Northern France. Quaternaire 15: 135-141.
  • 18. Yamamoto H, Nakagawa T and Arai F, 1996: Marine and Tectonic Uplift along the Echizen Coast, Fukui prefecture, Central Japan. The Quaternary research 35: 75-85 (in Japanese, abstract in English).
  • 19. Yokoyama Y, Falguères C and Quaegebeur JP, 1985: ESR dating of quartz from quaternary sediments: first attempt. Nuclear Tracks and Radiation Measurements 10(4-6): 921-928, DOI 10.1016/0735-245X(85)90109-7.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BATA-0001-0069
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