摘要
<正>The late Miocene-Pliocene deposited red-clay sequence on the Chinese Loess Plateau is encoded with important information of past climate changes.However,in comparison to the overlying Pleistocene loesspaleosol sequence,it has received much less study.In this paper,we review recent progress in environmental
引文
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Nie,J.,King,J.and Fang,X.,2007.Enhancement mechanisms of magnetic susceptibility in the Chinese Red-Clay sequence.Geophys.Res.Lett.,34:L19705,doi:10.1029/2007GL031430
Nie,J.,Song,Y.,King,J.W.,Fang,X.and Heil,C.,2010.HIRM variations in the Chinese red-clay sequence:Insights into pedogenesis in the dust source area.J.Asian Earth Sci.,38(3-4):96-104