Rea D K. The paleoclimatic record provided by eolian deposi-tion in the deep sea: the geologic history of wind[J]. Reviewof Geophysics, 1994, 32: 159-195.n5]吕厚远,韩家懋,吴乃琴,等中国现代土壤磁化率分析及其古气候意义[J]中国科学(D辑),1994,24:1291～1297.
[10]
Zhou L P, Oldfield F, Yu L, et al. Partly pedogenic origin ofmagnetic variations in Chinese loess[J]. Nature, 1990, 346:737 - 739.
[11]
Liu X M, Shaw J, Liu T S, et al. Magnetic mineralogy ofChinese loess and its significance[J]. Geophysical Journal In-ternational, 1992, 108:301 - 308.
[12]
Tsoar H, Pyr K. Dust transport and the question of desertloess formation[J]. Sedimentology, 1987, 34:139 - 154.
Gu Z, Lal D, Liu T, et al. Five million year 10Be record inChinese loess plateau and red - clay: climate and weatheringrelationships[J]. Earth Planet. Sci. Lett., 1996, 144:273 -287.
[22]
Kukla G, Heller F, Liu X M, et al. Pleistocene climates inChina dated by magnetic susceptibility[J]. Geology, 1988, 16:811-814.
[23]
Lu Y, Prescott J R, Robertson G B, et al. Thermolumines-cence dating of the Malan Loess at Zhaitang, China[J]. Geolo-gy, 1987, 15: 603-605.
[24]
于天仁,王振权(主编).土壤分析化学[M]北京:科学出版社,1988,1～531
[25]
Martinson D G, Pisias N G, Hays J D, et al. Age dating andthe orbital theory of the ice ages: development of a high resolu-tion 0 to 300 000 - year chrono- stratigraphy[J]. Quat.Res., 1987, 27:1-29.
