[1] 刘东生,等黄土与环境[M]北京:科学出版社,1985.1~481. [2] 丁仲礼,刘东生.中国黄土研究新进展(一),黄土地层[J].第四纪研究,1989,(D:24~35. [3] 安芷生,Kukla G,刘东生.洛川黄土地层学[J].第四纪研究,1989,(2):155~168. [4] Ding Z L, Yu Z W, Rutter N W, et al. Towards an orbitaltime scale for Chinese loess deposits[J]. Quaternary Science Re-views, 1994. 13:39-70. [5] 孙湘君,宋长青,王奉瑜,等.黄土高原南缘l0万年以来的植被-陕西渭南黄土剖面的花粉记录[J].科学通报,1995,40:1222~1224. [6] 吕厚远,吴乃琴,刘东生,等.最近15万年以来宝鸡黄土剖面植物硅酸体组合所反映的季节性气候变化[J].中国科学(D辑),1996,26:131~137. [7] 吴乃琴,Rousseau D D,刘东生.110万年来洛川黄土地层中蜗牛化石记录与环境因子分析[J].中国科学(D辑),1996,26:405~410 [8] 郭正堂,刘东生,安芷生.渭南黄土沉积中十五万年来的古土壤及其形成时的古环境[J].第四纪研究,1994,(3):256~269. [9] Heller F, Liu T S. Magnetostratigraphical dating of loess depos-ites in China[J]. Nature, 1982, 300:431-433. [10] 安芷生,Porter S,Kukla G,等最近13万年黄土高原季风变迁的磁化率证据[J].科学通报,1990,35:529~532. [11] 顾兆炎.黄土-古土壤序列碳酸盐同位素组成与古气候变化[J].科学通报,1991,36:767~770 [12] ShenCD, Beer J, LiuTS, etal. 10Bein Chinese loess[J].Earth Planet. Sci. Lett., 1992, 109: 169- 177. [13] 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. [14] 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. [15] Zhou L P, Oldfield F, Yu L, et al. Partly pedogenic origin ofmagnetic variations in Chinese loess[J]. Nature, 1990, 346:737 - 739. [16] 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. [17] Kukla G, Heller F, Liu X M, et al. Pleistocene climates inChina dated by magnetic susceptibility[J]. Geology, 1988, 16:811-814. [18] 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. [19] 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 [20] 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. [21] 熊尚发,刘东生,丁仲礼东亚冬夏古季风变化的相位差及热带太平洋在季风变化中的驱动作用[¨.第四纪研究,1996,(3):202~210 [22] Tsoar H, Pyr K. Dust transport and the question of desertloess formation[J]. Sedimentology, 1987, 34:139 - 154. [23] 刘东生,等中国的黄土堆积[M]北京:科学出版社,1965 1~130. [24] 丁仲礼,孙继敏,刘东生.联系沙漠-黄土演变过程中耦合关系的沉积学指标[J]中国科学(D辑),1999,29(1):82~87. [25] Hays J D, Imbrie J, Shackleton N J, et al. Variations in theEarth's orbit: pacemaker of the ice ages[J]. Science, 1976,194:1121 - 1132. [26] Broecker W S, van Donk J. Insolation changes, ice volumes,and the δ18O record in deep- sea cores[J]. Rev. Geophy.And Space Phys., 1970, 8:169 - 198. |