Liu Q S, Banerjee S K, Jackson M J, et al. 2004. New insights into partial oxidation model of magnetites and thermal alteration of magnetic mineralogy of the Chinese loess in air. Geophysical Journal International, 158(2): 506-514, doi: 10.1111/j.1365-246X.2004.02348.x.
[2]
Liu Q S, Roberts A P, Larrasoana J C, et al. 2012. Environmental magnetism: principles and applications. Reviews of Geophysics, 50(4), doi: 10.1029/2012RG000393.
[3]
Liu X M, Lü B, Li P Y, et al. 2013. Effects of heating environments on thermomagnetic behaviors of synthetic maghemite. Chinese Journal of Geophysics (in Chinese), 56(5): 1560-1567, doi: 10. 6038/cjg20130514.
[4]
Liu X M, Shaw J, Jiang J Z, et al. 2010. Analysis on variety and characteristics of maghemite. Sci. China Earth Sci. (in Chinese), 40(5): 592-602, doi: 10.1007/s11430-010-0030-2.
[5]
Mullins C E. 1977. Magnetic susceptibility of the soil and its significance in soil science—a review. Journal of Soil Science, 28(2): 223-246, doi: 10.1111/j.1365-2389.1977.tb02232.x.
[6]
?zdemir ?, Dunlop D J. 1996. Thermoremanence and Néel temperature of goethite. Geophysical Research Letters, 23(9): 921-924, doi: 10.1029/96GL00904.
[7]
Retallack G J. 1997a. Palaeosols in the Upper Narrabeen Group of New South Wales as evidence of Early Triassic palaeoenvironments without exact modern analogues. Australian Journal of Earth Sciences: An International Geoscience Journal of the Geological Society of Australia, 44(2): 185-201, doi: 10.1080/08120099708728303.
[8]
Retallack G J. 1997b. A Colour Guide to Paleosols. Michigan: John Wiley & Sons Ltd.
[9]
Retallack G J. 2010. Lateritization and bauxitization events. Economic Geology, 105(3): 655-667, doi: 10.2113/gsecongeo.105.3.655.
[10]
Roberts A P, Cui Y L, Verosub K L. 1995. Wasp-waisted hysteresis loops: Mineral magnetic characteristics and discrimination of components in mixed magnetic systems. Journal of Geophysical Research: Solid Earth (1978—2012), 100(B9): 17909-17924, doi: 10.1029/95JB00672.
[11]
Sidhu P S. 1988. Transformation of trace element-substituted maghemite to hematite. Clays Clay Miner, 36(1): 31-38.
[12]
Soreghan G S L, Elmore R D, Lewchuk M T. 2002. Sedimentologic-magnetic record of western Pangean climate in upper Paleozoic loessite (lower Cutler beds, Utah). Geological Society of America Bulletin, 114(8): 1019-1035, doi: 10.1130/0016-7606(2002)114〈1019:SMROWP〉2.0.CO;2.
[13]
Thompson R, Oldfield F. 1986. Environmental Magnetism. London: Allen and Uniwin.
[14]
Van Velzen A J, Dekkers M J. 1999a. The incorporation of thermal methods in mineral magnetism of loess-paleosol sequences: a brief overview. Chinese Science Bulletin, 44(S): 53-63.
[15]
Van Velzen A J, Dekkers M J. 1999b. Low-temperature oxidation of magnetite in loess-paleosol sequences: a correction of rock magnetic parameters. Studia Geophysica et Geodaetica, 43(4): 357-375, doi: 10.1023/A:1023278901491.
[16]
Wang X S, Yang Z Y, Lvlie R, et al. 2006. Environmental magnetism and paleoclimatic interpretation of the Sanmenxia loess-paleosol sequence in the southeastern extremity of the Chinese Loess Plateau. Chinese Science Bulletin, 51(22): 2755-2762, doi: 10.1007/s11434-006-2192-z.
[17]
Ao H, Deng C L. 2007. Review in the identification of magnetic minerals. Progress in Geophysics (in Chinese), 22(2): 432-442, doi: 10.3969/j.issn.1004-2903.2007.02.015.
[18]
Cogoini M, Elmore R D, Soreghan G S, et al. 2001. Contrasting rock-magnetic characteristics of two upper Paleozoic loessite-paleosol profiles. Physics and Chemistry of the Earth, Part A: Solid Earth and Geodesy, 26(11-12): 905-910, doi: 10.1016/S1464-1895(01)00140-5.
[19]
Collinson D W. 1983. Methods in Rock Magnetism and Palaeomagnetism: Techniques and Instrumentation.Chapman & Hall.
[20]
Day R, Fuller M, Schimidt V A. 1977. Hysteresis properties of titanomagnetites: Grain-size and compositional dependence. Physics of the Earth and Planetary Interiors, 13(4): 260-267, doi: 10.1016/0031-9201(77)90108-X.
[21]
De Boer C B, Dekkers M J. 1996. Grain-size dependence of the rock magnetic properties for a natural maghemite. Geophysical Research Letters, 23(20): 2815-2818, doi: 10.1029/96GL00781.
[22]
Dearing J. 1999. Magnetic susceptibility. // Oldfield F, Walden J, Smith J eds. Environmental Magnetism: A Practical Guide, Technical Guide, Vol.6. London: Quaternary Research Association, 35-62.
[23]
Deng C L, Liu Q S, Pan Y X, et al. 2007. Environmental magnetism of Chinese loess-paleosol sequences. Quaternary Sciences (in Chinese), 27(2):193-209.
[24]
Deng C L, Shaw J, Liu Q S, et al. 2006. Mineral magnetic variation of the Jingbian loess/paleosol sequence in the northern Loess Plateau of China: Implications for Quaternary development of Asian aridification and cooling. Earth and Planetary Science Letters, 241(1-2): 248-259, doi: 10.1016/j.epsl.2005.10.020.
[25]
Dunlop D J, ?zdemir ?. 1997. Rock Magnetism: Fundamentals and Frontiers. Cambridge: Cambridge University Press.
[26]
Faniran A. 1968. A deeply-weathered surface and its destruction: a geomorphological study of duricrusts in the northern Sydney district [Ph. D. thesis]. Sydney: University of Sydney.
[27]
Faniran A. 1971. The parent material of Sydney laterites. Journal of the Geological Society of Australia, 18(2): 159-164.
[28]
Fu C F, Song Y G, Qiang X K, et al. 2009. Environmental magnetism and its application progress in paleoclimatic and paleoenvironmental changes. Journal of Earth Sciences and Environment (in Chinese), 31(3): 312-322
[29]
Goguitchaichvili A, Morales J, Urrutia-Fucugauchi J, et al. 2001. On the use of continuous thermomagnetic curves in paleomagnetism: a cautionary note. Comptes Rendus de l''Académie des Sciences-Series IIA-Earth and Planetary Science, 333(11): 699-704, doi: 10.1016/S1251-8050(01)01686-x.
[30]
Hanesch M H, Petersen S N. 2006. Thermomagnetic measurements of soil iron minerals: the role of organic carbon. Geophysical Journal International, 165(1): 53-61, doi: 10.1111/j.1365-246X.2006.02933.x.
[31]
Hao Q Z, Oldfield F, Bloemendal J, et al. 2008. The magnetic properties of loess and paleosol samples from the Chinese Loess Plateau spanning the last 22 million years. Palaeogeography, Palaeoclimatology, Palaeoecology, 260(3-4): 389-404, doi: 10.1016/j.palaeo.2007.11.010.
[32]
Hao Q Z, Oldfield F, Bloemendal J, et al. 2009. The record of changing hematite and goethite accumulation over the past 22 Myr on the Chinese Loess Plateau from magnetic measurements and diffuse reflectance spectroscopy. Journal of Geophysical Research: Solid Earth (1978-2012), 114(B12), doi: 10.1029/2009JB006604.
[33]
Hao Q Z, Oldfield F, Bloemendal J, et al. 2012. Hysteresis and thermomagnetic properties of particle-sized fractions from loess and palaeosol samples spanning 22 Myr of accumulation on the Chinese Loess Plateau. Geophysical Journal International, 191(1): 64-77, doi: 10.1111/j.1365-246X.2012 05622.x.
[34]
Heller F, Liu T S. 1982. Magnetostratigraphical dating of loess deposits in China. Nature, 300(5891): 431-433, doi: 10.1038/300431a0.
[35]
Heller F, Liu T S. 1984. Magnetism of Chinese loess deposits. Geophysical Journal International, 77(1): 125-141, doi: 10.1111/j.1365-246X.1984.tb01928.x.
[36]
Hopkinson J. 1889. Magnetic and other physical properties of iron at a high temperature. Philosophical Transactions of the Royal Society of London. A, 46: 443-465.
[37]
Hrouda F. 1994. A technique for the measurement of thermal changes of magnetic susceptibility of weakly magnetic rocks by the CS-2 apparatus and KLY-2 Kappabridge. Geophysical Journal International, 118(3): 604-612, doi: 10.1111/j.1365-246X.1994.tb03987.x.
[38]
Hunt P A, Mitchell P B, Paton T R. 1977. "Laterite profiles" and "lateritic ironstones" on the Hawkesbury sandstone, Australia. Geoderma, 19(2): 105-121, doi: 10.1016/0016-7061(77)90019-2.
[39]
Jia J, Xia D S, Wei H T, et al. 2009. Asynchronous evolution of East Asia summer and winter monsoons of the Holocene recorded by Yao County Loess. Quaternary Sciences (in Chinese), 29(5): 966-975.
[40]
Johnson B D, Powell C M, Veevers J J. 1976. Spreading history of the eastern Indian Ocean and Greater India''s northward flight from Antarctica and Australia. Geological Society of America Bulletin, 87(11): 1560-1566, doi: 10.1130/0016-7606(1976)87〈1560:SHOTEI〉2.0.CO;2.
[41]
Qiang X K, An Z S, Song Y G, et al. 2010. New eolian red clay sequence on the western Chinese Loess Plateau linked to onset of Asian desertification about 25 Ma ago. Sci. China Earth Sci., 54(1): 136-144, doi: 10.1007/s11430-010-4126-5.
[42]
Retallack G J. 1976. Triassic palaeosols in the Upper Narrabeen Group of New South Wales. PartⅠ: features of the palaeosols. Journal of the Geological Society of Australia, 23(4): 383-399.
[43]
Retallack G J. 1977. Triassic palaeosols in the Upper Narrabeen Group of New South Wales. Part Ⅱ: Classification and reconstruction. Journal of the Geological Society of Australia, 24(1-2): 19-35.
[44]
Tramp K L, Soreghan G S L, Elmore R D. 2004. Paleoclimatic inferences from paleopedology and magnetism of the Permian Maroon Formation loessite, Colorado, USA. Geological Society of America Bulletin, 116(5-6): 671-686, doi: 10.1130/B25354.1.
[45]
Kukla G, Heller F, Liu X M, et al. 1988. Pleistocene climates in China dated by magnetic susceptibility. Geology, 16(9): 811-814, doi: 10.1130/0091-7613(1988)016〈0811:PCICDB〉2.3.CO;2.