1 Zhou L P, Oldfield F, Wintle A G, et al. Partly pedogenic origin of magnetic variations in Chinese loess. Nature, 1990, 346: 737-739？？
[2]
2 Maher B A, Thompson R. Mineral magnetic record of the Chinese loess and paleosols. Geology, 1991, 19: 3-6？？
[3]
3 Liu Q S, Banerjee S K, Jackson M, et al. Grain sizes of susceptibility and anhysteretic remanent magnetization carriers in Chineseloess-paleosol sequences. J Geophys Res, 2004, 109: B03101
[4]
7 Nie J S, King J W, Fang X M. Enhancement mechanisms of magnetic susceptibility in the Chinese red-clay sequence. Geophys Res Lett,2007, 34: 19705？？
[5]
8 Nie J, Song Y, King J, et al. Consistent grain size distribution of pedogenic maghemite of surface soils and Miocene loessic soils on theChinese Loess Plateau. J Quat Sci, 2010, 25: 261-266？？
[6]
10 Maher B A, Thompson R. Paleorainfall reconstructions from pedogenic magnetic susceptibility variations in the Chinese loess and paleosols.Quat Res, 1995, 44: 383-391？？
[7]
11 Maher B A. Magnetic properties of modern soils and Quaternary loessic paleosols: Paleoclimatic implications. Palaeogeogr PalaeoclimatolPalaeoecol, 1998, 137: 25-54？？
[8]
12 Florindo F, Zhu R X, Guo B. Low-field susceptibility and palaeorainfall estimates: New data along a N-S transect of the Chinese LoessPlateau. Phys Chem Earth (A), 1999, 24: 817-821？？
[9]
13 Evans M E, Rokosh C D, Rutter N W. Magnetoclimatology and paleoprecipitation: Evidence from a north-south transect through theChinese Loess Plateau. Geophys Res Lett, 2002, 29: 1285？？
[10]
14 Bloemendal J, Liu X M. Rock magnetism and geochemistry of two Plio-Pleistocene Chinese loess-palaeosol sequences.Implications forquantitative palaeoprecipitation reconstruction. Palaeogeogr Palaeoclimatol Palaeoecol, 2005, 226: 149-166？？
[11]
15 Begét J E, Stone D B, Hawkins D B. Paleoclimatic forcing of magnetic susceptibility variations in Alaska loess during the late Quaternary.Geology, 1990, 18: 40-43？？
[12]
16 Chlachula J, Evans M E, Rutter N. A magnetic investigation of a late Quaternary loess/palaeosol record in Siberia. Geophys J Int, 1998,132: 128-132？？
18 Zhu R X, Matasova G, Kazansky A, et al. Rock magnetic record of the last glacial-interglacial cycle from the Kurtak loess section, southernSiberia. Geophys J Int, 2003, 152: 335-343？？
[15]
19 Liu X M, Hesse P, Rolph T, et al. Properties of magnetic mineralogy of Alaskan loess: Evidence for pedogenesis. Quat Int, 1999, 62:92-102
22 Sun J M, Liu T S. Multiple origins and interpretations of the magnetic susceptibility signal in Chinese wind-blown sediments. Earth PlanetSci Lett, 2000, 180: 287-296？？
26 Evans M E, Heller F. Environmental Magnetism: Principles and Applications of Enviromagnetics. New York: Academic Press, 2003
[28]
27 Dankers P. Relationship between median destructive field and remanent coercive force for dispersed natural magnetite, titanomagnetiteand hematite. Geophys J Res, 1981, 64: 447-461
[29]
28 Hattori Y, Suzuki K, Honda M, et al. Re-Os systematics of the Taklimakan Desert sands, moraines and river sediments around the TaklimakanDesert, and of Tibetan soils. Geochim Cosmochim Acta, 2003, 67: 1195-1205
