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:
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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.
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A New Method of Determination of Loess Sequence Age with the Correlation between Sedimentation Rate and Grain Size
- 1.
Lanzhou Institute of plateau Atmospheric Physics,Chinese Academy of Sciences,Lanzhou 730000;
- 2.
State Key Laboratory of Loess and Quaternary Geology,Chinese Academy of Sciences,Xi'an 710054
- Received Date: 1997-11-19
- Rev Recd Date:
1998-06-03
- Publish Date:
1999-03-10
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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
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References
[1]
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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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Proportional views
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