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Liu Xiaodong, Lu Huayu, An Zhisheng. A New Method of Determination of Loess Sequence Age with the Correlation between Sedimentation Rate and Grain Size[J]. Acta Sedimentologica Sinica, 1999, 17(1): 145-148.
Citation: Liu Xiaodong, Lu Huayu, An Zhisheng. A New Method of Determination of Loess Sequence Age with the Correlation between Sedimentation Rate and Grain Size[J]. Acta Sedimentologica Sinica, 1999, 17(1): 145-148.

A New Method of Determination of Loess Sequence Age with the Correlation between Sedimentation Rate and Grain Size

  • Received Date: 1997-11-19
  • Rev Recd Date: 1998-06-03
  • Publish Date: 1999-03-10
  • On the basis of linear correlation between loess sedimentation rate and grain size,a new method of establishment of loess sequence age was developed. In this method, we assume that there is a linear relationship between the loess sedimentation rate R and the grain size S at the same horizon in a loess sequence,that is, S=aR+b,where a and b are coefficients awaiting determination. Supposing that the loess between two time control points is divided into n layers.the depths of which are indicated by Δh1,Δh2......Δhn and the time Δt1,Δt2......Δtn,respectively,a system of equations can be established by proceeding. fi(Δt1,Δt2,......Δtn-1,Δtn,a,b)=0 i=1,2......n,n+1,n+2 in which Δt1,Δt2......Δtn,a and b are unknown numbers. As this is a system of special nonlinear algebraic equations,which consists of n+2 equations,its numerical solution will be obtained with a iteration method.In this way,we can carry out a transformation from depth to age for a loess sequence. As an example,the depth-age transformation in the Luochuan loess section
  • [1] 1.刘东生黄土与环境 1985

    2.An Zhisheng;Liu Tungsheng;Lu Yanchou The long-term paleomonsoon variation recorded by the loess-paleosol sequence in central China 1990

    3.Heller F;Liu T S Magnetism of Chinese loess deposits 1984

    4.Kukla G;An Z S Loess stratigraphy in central China 1989

    5.Ding Z L;Yu Z W;Rutter N W;Liu T S Towards an otbital time scale for Chinese loess deposit 1994

    6.安芷生;Porter S C;Chappell J 最近130 ka洛川黄土堆积序列与格陵兰冰芯记录 1994(24)

    7.Porter S C;An Zhisheng Correlation between cilmate events in the North Atlantic and China during the last glaciation[外文期刊] 1995

    8.Vandenberghe J;An Z;Nugteren G;Lu H, Huissteden K V New absolute time scale for the quaternary climate in the Chinese loess region by grain-size analysis 1997

    9.Xiao Jule;Zheng Hongbo;Zhao Hua Variation of winter monsoon intensity on the loess plateau,central China during the last130 000 years:evidence form grain size distribution 1992

    10.鹿化煜;安芷生洛川黄土粒度组成的古气候意义 1997(01)

    11.Rea D K;Leinen M;Janecek T R Geologic approach to the long-term history of atmospheric circulation[外文期刊] 1985

    12.An Zhisheng;Kukla G;Proter S C Late Quaternary dust flow on the Chinese loess plateau 1991

    13.Martinson D G;Pisias N G;Hays J D Age dation and the orbital theory of the ice ages:development of a high-resolution 0 to 300 000 yr chronostatigraphy 1987
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  • Received:  1997-11-19
  • Revised:  1998-06-03
  • Published:  1999-03-10

A New Method of Determination of Loess Sequence Age with the Correlation between Sedimentation Rate and Grain Size

Abstract: On the basis of linear correlation between loess sedimentation rate and grain size,a new method of establishment of loess sequence age was developed. In this method, we assume that there is a linear relationship between the loess sedimentation rate R and the grain size S at the same horizon in a loess sequence,that is, S=aR+b,where a and b are coefficients awaiting determination. Supposing that the loess between two time control points is divided into n layers.the depths of which are indicated by Δh1,Δh2......Δhn and the time Δt1,Δt2......Δtn,respectively,a system of equations can be established by proceeding. fi(Δt1,Δt2,......Δtn-1,Δtn,a,b)=0 i=1,2......n,n+1,n+2 in which Δt1,Δt2......Δtn,a and b are unknown numbers. As this is a system of special nonlinear algebraic equations,which consists of n+2 equations,its numerical solution will be obtained with a iteration method.In this way,we can carry out a transformation from depth to age for a loess sequence. As an example,the depth-age transformation in the Luochuan loess section

Liu Xiaodong, Lu Huayu, An Zhisheng. A New Method of Determination of Loess Sequence Age with the Correlation between Sedimentation Rate and Grain Size[J]. Acta Sedimentologica Sinica, 1999, 17(1): 145-148.
Citation: Liu Xiaodong, Lu Huayu, An Zhisheng. A New Method of Determination of Loess Sequence Age with the Correlation between Sedimentation Rate and Grain Size[J]. Acta Sedimentologica Sinica, 1999, 17(1): 145-148.
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