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When using quartz OSL to date loess samples from the Chinese Loess Plateau, it has been reported that the agreement between OSL ages and the independent ages is limited to the samples younger than ~70 ka with a corresponding De of ~230 Gy, and a sample with an expected age of 780 ka was dated to 107 ka, corresponding to 403 Gy. The growth curves of these samples do not sat-urate at doses of 700 Gy, and a linear growth part was observed for doses higher than 200 Gy. How-ever, the maximum measured age of ~100 ka imply that the De determined using this linear part of a growth curve could be problematic, or that the quartz OSL signal is not as stable as previously thought and has a barrier age of ~100 ka. In the current study, we examine the reasons for the age un-derestimation. We examined the shape of growth curves, anomalous fading, thermal stability, etc. The results show that, for the loess samples examined, quartz OSL does not fade anomalously, and the barrier age of ~100 ka is due to the fact that the OSL signals are less thermally stable, the lifetime of 0.311 Ma at 20°C obtained is much smaller than those for quartz samples from other regions such as Australia (~100 Ma).
Słowa kluczowe
Wydawca
Czasopismo
Rocznik
Tom
Strony
57--64
Opis fizyczny
Bibliogr. 29 poz., tab., wykr.
Twórcy
autor
- Luminescence Dating Group, CAS Key Laboratory Of Salt Lake Resources and Chemistry, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining 810008, PR China
autor
- Dept of History of Science and Technology and Archaeometry University of Science and Technology of China (USTC), Hefei 230026, PR China
- USTC Archaeometry Laboratory, University of Science and Technology of China, Hefei 230026, PR China
Bibliografia
- 1.Aitken MJ, 1985. Thermoluminescence Dating. Academic Press, London.
- 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.Bailey RM, Smith BW and Rhodes RJ, 1997. Partial bleaching and the decay form characteristics of quartz OSL. Radiation Measurements 27(2): 123-136, DOI 10.1016/S1350-4487(96)00157-6.
- 4.Bonde A, Murray AS and Friedrich WL, 2001. Santorini: luminescence dating of a volcanic province using quartz. Quaternary Science Reviews 20(5-9): 789-793, DOI 10.1016/S0277-3791(00)00034-2.
- 5.Buylaert JP, Murray AS, Vandenberghe D, Vriend M, De Corte F and Van den haute P, 2008. Optical dating of Chinese loess using sand-sized quartz: establishing a time frame for Late Pleistocene climate changes in the western part of the Chinese Loess Plateau. Quaternary Geochronology 3(1-2): 99-113, DOI 10.1016/j.quageo.2007.05.003.
- 6.Chapot MS, Roberts HM, Duller GAT and Lai ZP, 2012. A comparison of natural- and laboratory-generated dose response curves for quartz optically stimulated luminescence signals from Chinese Loess. Radiation Measurements 47(11-12): 1045-1052, DOI 10.1016/j.radmeas.2012.09.001.
- 7.Choi JH, Murray AS, Cheong CS, Hong DG and Chang HW, 2003. The resolution of stratigraphic inconsistency in the luminescence ages of marine terrace sediments from Korea. Quaternary Science Reviews 22(10-13): 1201-1206, DOI 10.1016/S0277-3791(03)00022-2.
- 8.Debenham NC, 1985. Use of UV emission in TL dating of sediment. Nuclear Tracks and Radiation Measurements 10(4-6): 717-724, DOI 10.1016/0735-245X(85)90080-8.
- 9.Fan AC, Li SH and Li B, 2011. Observation of unstable fast component in OSL of quartz. Radiation Measurements 46(1): 21-28, DOI 10.1016/j.radmeas.2010.10.001.
- 10.Kukla G and An Z, 1989. Loess stratigraphy in central China. Palaeo-geography, Palaeoclimatology, Palaeoecology 72: 203-225, DOI 10.1016/0031-0182(89)90143-0.
- 11.Jain M, Murray AS and Bøtter-Jensen L, 2003. Characterisation of blue-light stimulated luminescence components in different quartz samples: implications for dose measurement. Radiation Measurements 37(4-5): 441-449, DOI 10.1016/S1350-4487(03)00052-0.
- 12.Lai ZP, 2010. Chronology and the upper dating limit for loess samples from Luochuan section in the Chinese Loess Plateau using quartz OSL SAR protocol. Journal of Asian Earth Sciences 37(2): 176-185, DOI 10.1016/j.jseaes.2009.08.003.
- 13.Lamothe M and Auclair M, 1999. A solution to anomalous fading and age shortfalls in optical dating of feldspar minerals. Earth and Planetary Science Letters 171(3): 319-323, DOI 10.1016/S0012-821X(99)00180-6.
- 14.Li B and Li SH, 2006. Comparison of De estimates using the fast com-ponent and the medium component of quartz OSL. Radiation Measurements 41(2): 125-136, DOI 10.1016/j.radmeas.2005.06.037.
- 15.Li SH and Chen G, 2001. Studies of thermal stability of trapped charges associated with OSL from quartz. Journal of Physics D: Applied Physics 34(4): 493-498, DOI 10.1088/0022-3727/34/4/309.
- 16.Lowick SE, Preusser and Wintle AG, 2010. Investigating quartz optically stimulated luminescence dose-response curves at high doses. Radiation Measurements 45(9): 975-984, DOI 10.1016/j.radmeas.2010.07.010.
- 17.Lowick SE and Preusser F, 2011. Investigating age underestimation in the high dose region of optically stimulated luminescence using fine grain quartz. Quaternary Geochronology 6(1): 33-41, DOI 10.1016/j.quageo.2010.08.001.
- 18.Lu HY, Liu XD, Zhang FQ, An ZS and Dodson J, 1999. Astronomical calibration of loess–paleosol deposits at Luochuan, central Chinese Loess Plateau. Palaeogeography, Palaeoclimatology, Palaeoecol-ogy 154(3): 237-246, DOI 10.1016/S0031-0182(99)00113-3.
- 19.Lu YC, Wang XL and Wintle AG, 2007. A new OSL chronology for dust accumulation in the last 130,000 yr for the Chinese Loess Plateau. Quaternary Research 67(1): 152-160, DOI 10.1016/j.yqres.2006.08.003.
- 20.Murray AS and Wintle AG, 1999. Isothermal decay of optically stimulated luminescence, Radiation Measurements 30(1): 119-125, DOI 10.1016/S1350-4487(98)00097-3.
- 21.Qin JT and Zhou LP, 2009. Stepped-irradiation SAR: A viable approach to circumvent OSL equivalent dose underestimation in last glacial loess of northwestern China. Radiation Measurements 44(5-6): 417-422, DOI 10.1016/j.radmeas.2009.06.008.
- 22.Singarayer JS, 2002. Linearly modulated optically stimulated luminescence of sedimentary quartz: physical mechanisms and implications for dating. PhD thesis, University of Oxford, Oxford.
- 23.Singarayer JS and Bailey RM, 2003. Further investigations of the quartz optically stimulated luminescence components using linear modulation. Radiation Measurements 37(4-5): 451-458, DOI 10.1016/S1350-4487(03)00062-3.
- 24.Tsukamoto S, Murray AS, Huot S, Watanuki T, Denby PM and Botter-Jensen L, 2007. Luminescence property of volcanic quartz and the use of red isothermal TL for dating tephras. Radiation Measure-ments 42(2): 190-197, DOI 10.1016/j.radmeas.2006.07.008.
- 25.Watanuki T, Murray AS and Tsukamoto S, 2003. A comparison of OSL ages derived from silt-sized quartz and polymineral grains from Chinese loess. Quaternary Science Reviews 22(10-13): 991-997, DOI 10.1016/S0277-3791(03)00053-2.
- 26.Watanuki T, Murray AS and Tsukamoto S, 2005. Quartz and poly-mineral luminescence dating of Japanese loess over the last 0.6 Ma: Comparison with an independent chronology. Earth and Planetary Science Letters 240(3-4): 774-789, DOI 10.1016/j.epsl.2005.09.027.
- 27.Wintle AG, 1973. Anomalous fading of thermoluminescence in mineral samples. Nature 245(5421): 143-144, DOI 10.1038/245143a0.
- 28.Wintle AG and Murray AS, 1998. Towards the development of a pre-heat procedure for OSL dating of quartz. Radiation Measurements 29(1): 81-94, DOI 10.1016/S1350-4487(97)00228-X.
- 29.Wintle AG and Murray AS, 2006. A review of quartz optically stimulated luminescence characteristics and their relevance in single-aliquot regeneration dating protocols. Radiation Measurements 41(4): 369-391, DOI 10.1016/j.radmeas.2005.11.001.
Typ dokumentu
Bibliografia
Identyfikator YADDA
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