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Construction of a quartz OSL standardised growth curve (SGC) for aeolian samples from the Horqin dunefield in northeastern China


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[1] Berger GW, Mulhern PJ and Huntley DJ, 1980. Isolation of silt-sized quartz from sediments. Ancient TL 11: 8–9. Search in Google Scholar

[2] Burbidge CI, Duller GAT and Roberts HM, 2006. De determination for young samples using the standardised OSL response of coarse-grain quartz. Radiation Measurements 41(3): 278–288, DOI 10.1016/j.radmeas.2005.06.038. http://dx.doi.org/10.1016/j.radmeas.2005.06.03810.1016/j.radmeas.2005.06.038Search in Google Scholar

[3] Duller GAT, 2008. Single-grain optical dating of Quaternary sediments: why aliquot size matters in luminescence dating. Boreas 37(4): 589–612, DOI 10.1111/j.1502-3885.2008.00051.x. http://dx.doi.org/10.1111/j.1502-3885.2008.00051.x10.1111/j.1502-3885.2008.00051.xSearch in Google Scholar

[4] Hong DG and Choi JH, 2008. Investigations on standardized growth curve (SGC) procedure for optical dating of heated quartz. Journal of Radioanalytical and Nuclear Chemistry 275(3): 613–617, DOI 10.1007/s10967-007-7076-4. http://dx.doi.org/10.1007/s10967-007-7076-410.1007/s10967-007-7076-4Search in Google Scholar

[5] Lai ZP, 2006. Testing the use of an OSL standardized growth curve (SGC) for De determination on quartz from the Chinese Loess Plateau. Radiation Measurements 41(1): 9–16, DOI 10.1016/j.radmeas.2005.06.031. http://dx.doi.org/10.1016/j.radmeas.2005.06.03110.1016/j.radmeas.2005.06.031Search in Google Scholar

[6] Lai ZP, 2010. Chronology and the upper dating limit for loess samples from Luochuan section in 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. http://dx.doi.org/10.1016/j.jseaes.2009.08.00310.1016/j.jseaes.2009.08.003Search in Google Scholar

[7] Lai ZP and Brückner H, 2008. Effects of feldspar contamination on equivalent dose and the shape of growth curve for OSL of silt-sized quartz extracted from Chinese loess. Geochronometria 30: 49–53, DOI 10.2478/v10003-008-0010-0. http://dx.doi.org/10.2478/v10003-008-0010-010.2478/v10003-008-0010-0Search in Google Scholar

[8] Lai ZP, Brückner H, Zöller L and Fülling A, 2007. Existence of a common growth curve for silt-sized quartz OSL of loess from dif-ferent continents. Radiation Measurements 42(9): 1432–1440, DOI 10.1016/j.radmeas.2007.08.006. http://dx.doi.org/10.1016/j.radmeas.2007.08.00610.1016/j.radmeas.2007.08.006Search in Google Scholar

[9] Long H, Lai ZP, Fan QS, Sun YJ and Liu XJ, 2010. Applicability of a quartz OSL standardised growth curve for De determination up to 400 Gy for lacustrine sediments from the Qaidam Basin of the Qinghai-Tibetan Plateau. Quaternary Geochronology 5(2–3): 212–217, DOI 10.1016/j.quageo.2009.05.005. http://dx.doi.org/10.1016/j.quageo.2009.05.00510.1016/j.quageo.2009.05.005Search in Google Scholar

[10] 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. http://dx.doi.org/10.1016/S1350-4487(99)00253-X10.1016/S1350-4487(99)00253-XSearch in Google Scholar

[11] 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. http://dx.doi.org/10.1016/S1350-4487(03)00053-210.1016/S1350-4487(03)00053-2Search in Google Scholar

[12] Nagelkerke NJD, 1991. A Note on a general definition of the coefficient of determination. Biometrika 78(3): 691–692, DOI 10.1093/biomet/78.3.691. http://dx.doi.org/10.1093/biomet/78.3.69110.1093/biomet/78.3.691Search in Google Scholar

[13] Qiu SW, 2008. Sandy land and sandy desertification in western northeast China. Beijing, Science Press (in Chinese). Search in Google Scholar

[14] Ren HC, Lü YL, Yang P, Chen HZ and Shi YJ, 2004. History and present status of desertification in Horqin sandy land region. Journal of Desert Research 24(5): 544–547 (in Chinese with English abstract). Search in Google Scholar

[15] Roberts HM and Duller GAT, 2004. Standardised growth curves for optical dating of sediment using multiple-grain aliquots. Radiation Measurements 38(2): 241–252, DOI 10.1016/j.radmeas.2003.10.001. http://dx.doi.org/10.1016/j.radmeas.2003.10.00110.1016/j.radmeas.2003.10.001Search in Google Scholar

[16] Stevens T, Armitage SJ, Lu H and Thomas DSG, 2007. Examining the potential of high-resolution OSL dating of Chinese loess. Quaternary Geochronology 2(1–4): 15–22, DOI 10.1016/j.quageo.2006.03.004. http://dx.doi.org/10.1016/j.quageo.2006.03.00410.1016/j.quageo.2006.03.004Search in Google Scholar

[17] Telfer MW, Bateman MD, Carr AS and Chase BM, 2008. Testing the applicability of a standardized growth curve (SGC) for quartz OSL dating: Kalahari dunes, South African coastal dunes and Florida dune cordons. Quaternary Geochronology 3(1–2): 137–142, DOI 10.1016/j.quageo.2007.08.001. http://dx.doi.org/10.1016/j.quageo.2007.08.00110.1016/j.quageo.2007.08.001Search in Google Scholar

[18] Wang XM, Chen FH, Hasi E and Li JC, 2008. Desertification in China: An assessment. Earth-Science Reviews 88(3–4): 188–206, DOI 10.1016/j.earscirev.2008.02.001. http://dx.doi.org/10.1016/j.earscirev.2008.02.00110.1016/j.earscirev.2008.02.001Search in Google Scholar

[19] Yang LB, 1995. The formation and evolution of Songliao Plain. Journal of Northeast Normal University 2: 191–124 (in Chinese with English abstract). Search in Google Scholar

[20] Yang LH, Zhou J, Lai ZP, Long H, Zhang JR, 2010. Lateglacial and Holocene dune activities in the Horqin desert of northeastern China based on OSL dating. Palaeogeography, Palaeoclimatology, Palaeoecology 296(1–2): 44–51, DOI 10.1016/j.palaeo.2010.06.014. http://dx.doi.org/10.1016/j.palaeo.2010.06.01410.1016/j.palaeo.2010.06.014Search in Google Scholar

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