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《Journal of Stratigraphy》 2001-02
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A STUDY OF THE AGE OF THE DINGCUN FORMATION USING LOESS-PALEOSOL SEQUENCE ANALYSIS

LI You li 1) , HU Xiao meng 1) , YANG Jing chu 1) , and MA Zhi zheng 2) ( 1) MOE Laboratory for Earth Surface Processes and Department of Geography, Peking University, Beijing, 100871; 2) Shanxi Normal College, Linfen, 041004)  
This paper deals with studied three sections on the third terrace of the Fen River, on which the Dingcun Formation is widely distributed. Based on field investigation, chemical and magnetic susceptibility analysis, it is concluded that the Dingcun Formation is covered by loess younger than 70 kaB.P., and was deposited during the formation of S 1 paleosol (14—7 kaB.P.).
【Fund】: 国家自然科学基金!(No.0 0 710 16 )资助
【CateGory Index】: P534.63
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