Prescott J R,Hutton J T.Cosmic ray contribution to dose rates for luminescence and ESR dating:Large depthsand long-term time variations.Radiation Measurements,1994,23(2-3):497～500.
[3]
Mejdhal V.Thermoluminescence dating:beta-dose attenuation in quartz grains.Archaeometry,1979,21(1):61～72.
[4]
Lai Z P.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,2010,37(2):176～185.
[5]
Lai Z P,Z？ller L,Fuchs M,et al.Alpha efficiency determination for OSL of quartz extracted from Chinese loess.Radiation Measurements,2008,43(2-6):767～770.
Grafenstein U,Erlenkeuser H,Brauer A,et al.A mid-European decadal isotope-climate record from 15500to5000years B.P.Science,1999,284:1654～1657.
[8]
Huang C C,Pang J L,Su H X,et al.The Ustic Isohumisol(Chernozem)distributed over the Chinese Loess Plateau:Modern soil or palaeosol?Geoderma,2009,150(3-4):344～358.
Zha X C,Huang C C,Pang J L.Palaeofloods recorded by salckwater deposits on the Qishuihe River in the middlereaches of the Yellow River.Journal of Chinese Geography,2009,19(6):681～690.
Baker V R.Paleoflood hydrology:Origin,progress,prospects.Geomorphology,2008,101(1-2):1～13.
[15]
Carrivick J L.Hydrodynamics and geomorphic work of Jokulhlaups(glacial outburst floods)from Kverkfjoll volcano,Iceland.Hydrological Processes,2007,21(6):725～740.
[16]
Harvey J E,Pederson J L.Reconciling arroyo cycle and paleoflood approaches to late Holocene alluvial records indryland streams.Quaternary Science Review,2011,30(7-8):855～866.
[17]
Benito G,Sopenab A,Sánchez-Moyac Y,et al.Palaeoflood record of the Tagus River(Central Spain)during theLate Pleistocene and Holocene.Quaternary Science Review,2003,22(15-17):1737～1756.
[18]
Yang D Y,Yu G,Xie Y B,et al.Sedimentary records of large Holocene floods from the middle reaches of theYellow River,China.Geomorphology,2000,33(1-2):73～88.
Huang C C,Pang J L,Zha X C,et al.Impact of monsoonal climatic change on Holocene overbank flooding alongSushui River,middle reach of the Yellow River,China.Quaternary Science Reviews,2007,26:2247～2264.
[21]
Huang C C,Pang J L,Su H X,et al.Climatic and anthropogenic impacts on soil formation in the semiarid loesstablelands in the middle reaches of the Yellow River,China.Journal of Arid Environments,2007,71(3):280～298.
[22]
Huang C C,Pang J L,Zha X C,et al.Extraodinary floods of 4100～4000aB.P.recorded at the late Neolithic ruins in the Jinghe river gorges,middle reach of the Yellow River,China.Palaeogeography,Palaeoclimatology,Palaeoecology,2010,289(1-4):1～9.
[23]
Huang C C,Pang J L,Zha X C,et al.Extraordinary floods related to the climatic event at 4200aBP on theQishuihe River,middle reaches of the Yellow River,China.Quaternary Science Reviews,2011,30(1-4):460～468.
[24]
Wallinga J.Optically stimulated luminescence dating of fluvial deposits:A review.Boreas,2002,31(4):303～322.
[25]
Rittenour T M,Goble R J,Blum M D.An optical age chronology of Late Pleistocene fluvial deposits in the northern lower Mississippi valley.Quaternary Science Reviews,2003,22(11-13):1105～1110.
[26]
Thomas P J,Jain M,Juyal N,et al.Comparison of single-grain and small-aliquot OSL dose estimates in<3000years old river sediments from South India.Radiation Measurements,2005,39:457～469.
Aitken M J.An Introduction to Optical Dating.New York:Oxford University Press,1998.60～68.
[31]
Armitage S J,Bailey R M.The measured dependence of laboratory beta dose rates on sample grain size.RadiationMeasurements,2005,39(2):123～127.
[32]
Buylaert J P,Murray A S,Vandenberghe D,et al.Optical dating of Chinese loess using sand-sized quart:Establishing a time frame for Late Pleistocene climate changes in the western part of the Chinese Loess Plateau.Quaternary Geochronology,2008,3:99～113.
[33]
Wallinga J,Murray A S,Duller G A T,et al.Testing optically stimulated luminescence dating of sand-sizedquartz and feldspar from fuvial deposits.Earth and Planetary Science Letters,2001,193(3-4):617～630.
[34]
Roberts H M.Assessing the effectiveness of the double-SAR protocol in isolating a luminescence signal dominatedby quartz.Radiation Measurements,2007,42:1627～1636.
[35]
Bùtter-Jensen L,Duller G A T,Murray A S,et al.Blue light emitting diodes for optical stimulation of quartz inretrospective dosimetry and dating.Radiation Protection Dosimetry,1999,84(1-4):335～340.
[36]
Duller G A T.Distinguishing quartz and feldspar in single grain luminescence measurements.Radiation Measurements,2003,37(2):161～165.
[37]
Murray A S,Wintle A G.Luminescence dating of quartz using an improved single-aliquot regenerative-dose protocol.Radiation Measurements,2000,32(1):57～73.
[38]
Aitken M J,Smith B W.Optical dating:Recuperation after bleaching.Quaternary Science Reviews,1988,7(3-4):387～393.
[39]
Rhodes E J,Baily R M.The effect of thermal transfer on the zeroing of the luminescence of quartz from recent glacio fluvial sediments.Quaternary Science Reviews,1997,16:291～298.
Zhang J F,Zhou L P,Yue S Y.Dating fluvial sediments by optical stimulated luminescence:Selection of equivalent doses for age calculation.Quaternary Science Reviews,2003,22(10-13):1123～1129.
[42]
Steffen D,Preusser F,Schlunegger F.OSL quartz age underestimation due to unstable signal components.Quaternary Geochronology,2009,4(5):353～362.
[43]
Ou X J,Xu L B,Lai Z P,et al.Potential of quartz OSL dating on moraine deposits from eastern Tibetan Plateauusing SAR protocol.Quaternary Geochronology,2010,5:257～262.
[44]
Wallinga J.On the detection of OSL age overestimation using single-aliquot techniques.Geochronometria,2002,21(1):17～26.
