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《Acta Sedimentologica Sinica》 1997-04
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Re determination on the Sedimentary Age of Salawusu Formation

Su Zhizhu 1 and Dong Guangrong 21 (Institute of Loess Plateau Geography,Shanxi University,Taiyuan 030006) 2 (Institute of Desert Research,Academia Sinica,Lanzhou 730000)  
The Salawusu River area is one of the standard sections of the Late Pleistocene strata in North China.However,there have been a lot of different views about the strata since the establishment of Salawusu Formation,especially in the aspects of sedimentary facies,stratigraphic data and its climate significance.According to the stratigraphic subdivision,age dating and the analysis of the sedimentary facies,the following recognitions can be gained: 1,The original Salawusu Formation could be further divided into Lishi Loess interbeded with sandy sediments(Q 2 2),Salawusuu Formation(Q 1 3),Cheng chuan Formation(Q 2 3),Dagouwan Formation (Q 1-2 4) and Dishaogouwan Formation(Q 3 4). 2,Salwusu Formation is mainly a fluvial lacustrine deposit corresponding to the Stage 5 of deep sea in δ18O and formed between about 140-70 Ka.BP.Chengchuan Formation is mainly fossil aeolian sands,with some lacustrine silty clay in the middle part,correspording to Stages 2-4 of deep sea in δ18O and formed between 70-10 Ka.BP.Dagouwan Formation is lacustrine sediments and black paleosoil,indicating the warm humid climate and formed in the middle early period of Holocene.Dishaogouwan Formation is mainly sub loess and aeolian sands,representing the cold dry climate and being believed to belong to the late Holocene. 3,As a fluvial lacustrine sedimentary stratum,Salawusu Formation is quite different from its upper Chengchuan Formation both in geochronology,lithology and sedimentary facies and in palaeontology.Chengchuan Formation and Malan Loess belong to heteropic deposits(sandy and loessic facies)formed contemporaneously under the same wind action. 4,As a flurial lacustrine aeolian sand sequence by observing the Dishaogou profile in the Salawusu River area,its climatic records can compete with the records of loess and deep sea deposits,they may be divided into 5 climatic periods just by oxygen isotope.It is suggested that the climatic change of this region during the last interglacial period is synchronous with that of the whole earth.
【CateGory Index】: P597.3
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