A review of recent advances in red-clay environmental magnetism and paleoclimate history on the Chinese Loess Plateau
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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
Song,Y.et al.,2007.Late Neogene rock magnetic record of climatic variation from Chinese eolian sediments related to uplift of the Tibetan Plateau.J.Asian Earth Sci.,30:324-332
    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

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