[1] Pye K, Aeolian dust and dust deposits[M] . Academic Press, 1987, 1～256
[2] 陈隆勋.东亚季风[M] .北京：气象出版社,199l 1～262
[3] 乔全明,张雅高,青藏高原天气学[M] .北京：气象出版社,1994.1～250
[4] 刘东生.黄土与环境[M] .北京：科学出版社,1985.1～481
[5] Bronger A, Heinkele T. Mineralogical and clay mineralogical aspects ofloess research[J] . Quaternary International, 1990, 7:37～53
[6] Konert M, Vandenberghe J. Comparison of laser grain size analysis withpipette and sieve analysis: a solution for the underestimation of the clayfraction. 1997, 44:523～535
[7] Ashley G M. Interpretation of polymodal sediments[J] . Journal of Ge-ology, 1978,86:411～421
[8] Paton T R. The formation of soil material[M] . London. George Allen＆Uniwin Press,1978.1～143
[9] 鹿化煜,安芷生.前处理方法对黄土沉积物粒度测量影响的实验研究[J] .科学通报,1997,42：2535～2538
[10] XiaoJ, PorterS, AnZ, Kumai H,YoshikawaS. Grain size of quartzas an indicator of winter monsoon strength on the loess plateau of Cen-tral China during the last 130,000 Yr[J] . Quaternary Research.1995, 43:22～29
[11] 么枕生,丁裕国,气候统计[M] .北京：气象出版社,1990.266～300
[12] 张秀芝.Weibull分布参数估计方法及其应用[J] .气象学报,1996,54(1)：108～116
[13] Rea D K, Hovan S. Grain size distribution and depositional processes ofthe mineral component of abyssal sediments: Lessons from the NorthPacific[J] .Paleoceanography, 1995, 10:251～258
[14] Gillette D A,Blifford I B. The influence of wind velocity on the sizedistribution of aerosols generated by the wind erosion of soils[J ] . Jour-nal of Geophysical Research, 1974, 79:4068～4075
[15] Janecek T R, Rea D K. Quaternary fluctuations in the morthem hemi-sphere trade winds and westeries [J] . Quaternary Research, 1985,24:150～163
[16] Rea D K, Leinen M,Janecek T R. Geologic approach to the long -term history of atmospheric circulation[J] . Science, 1985, 227: 721～725
[17] 安芷生,吴锡浩,汪品先等.最近130Ka中国的古季风－－Ⅱ古季风记录[J] .中国科学(B辑),1991,10：1076～1081
[18] 鹿化煜,安芷生.黄土高原黄土粒度组成的古气候意义[J] .中国科学(D)辑,28(3)：1991,278～283
[19] Zhang Xiaoye, Shen Zhibao, Zhang Guangyu, Chen Tuo, LiuHaiyan. Remote mineral aerosols in Westeries and their contributionsto the Chinese loess[J] . Science in China (D), 1996 39: 134～143
[20] 郭正堂,魏兰英,吕厚远,吴乃琴,姜文英,刘东生,晚第四纪风成物质组成的变化及其环境意义[J] .第四纪研究,1999,(1)：41～48
[21] Pye K, Zhou L P, Late Pleistocene and Holence aeolian dust depositionin North China and the Northwest Pacific Ocean [ J ] . Palaeo-geography, Palaeoclimatology, Palaeoecology, 1989,73: 11～23
[22] 丁仲礼,杨石岭,孙继敏,刘东生.2.6 Ma前后大气环流重构的黄土－古土壤沉积证据[J] .第四纪研究,1999,(3)：277～281
[23] 钱林清.黄土高原气候[M] .北京：气象出版社,1991.54～70
[24] 鹿化煜,安芷生.洛川黄土粒度组成的古气候意义[J] .中国科学(D辑),28(3)：278～283
[25] 鹿化煜,安芷生.黄土高原红粘土与黄土古土壤粒度特征对比－红粘土风成成因的新证据[J] .沉积学报,1999,17(2)：226～232
[26] 丁仲礼,孙继敏,杨石岭等.灵台黄土－红粘土序列的磁性地层及粒度记录[J] .第四纪研究,1998,(1)：86～94