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- W2384361211 abstract "A Holocene soil profile was investigated on the Zhongtiaoshan Mountain pluvial-alluvial fan in Yuncheng basin,Shanxi province.From the analysis of soil magnetic susceptibility and grain size,the Holocene environmental change and erosional-depositional phases were revealed.In the early stage of Holocene,the climate became warm,the biological weathering pedogensis was beginning;in the middle stage of Holocene,the climate became warmer and wetter,the Holocene paleosoil(S_(0)) was formed,and in the late period of Holocene,the climate became dryer,the dust storms happened frequently,the aeolian loess(L_(0)) was accumulated and covered on the paleosoil(S_(0)).Because of the fluctuation and change of the Holocene climate the four sheet rainwash erosional-depositional phases happened approximately in 11500-11000a B.P.,3850~3300a B.P.,2200~2000a B.P.and 1300-800a B.P.in Yuncheng basin,which provided a new approach to study erosion history of Loess Plateau." @default.
- W2384361211 created "2016-06-24" @default.
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- W2384361211 date "2006-01-01" @default.
- W2384361211 modified "2023-09-23" @default.
- W2384361211 title "Holocene Environment Change of Pedogenesis and Erosion phases on Pluvial-alluvial Fan in Yuncheng Basin,Shanxi Province" @default.
- W2384361211 hasPublicationYear "2006" @default.
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