[1]林承坤.第四纪古长江与砂山地形[J].南京大学学报(自然科学版),1959,(2):93-106.[2]杨达源.江南晚更新世风成砂丘[J].中国沙漠,1985,5(4):32-36.[3]邹学勇.赣江下游地区的风成沉积物[J].中国沙漠,2001,21(4):340-345.[4]吴艳宏,羊向东,王苏民,等.九江—澎泽一带砂山研究存在问题探讨[J].海洋地质与第四纪地质,2000,20(2):103-106.[5]刘健.江西彭泽末次冰期风砂沉积序列磁学特征及其古气候意义[J].中国科学(D辑),2001,31(8):626-633.[6]庄检平,贾玉连,马春梅,等.末次冰期间冰阶晚期长江中游风尘堆积及其环境意义[J].沉积学报,2007,25(3):424-428[7]Jia Y L,Lai Z P,Zhang J R,et al.Chronology and provenance of aeolian sediments from Poyang Lake area in the middle reaches of the Yangtze River in China[J].Quaternary Geochronolohy,2012,10:44-49.[8]Hu X F,Gong Z T. A “Yellow Cap” on quaternary red clay in Jiujiang Jiangxi province[J].Pedosphere,1999,9(4):311-318.[9]杨达源.中国东部的第四纪风尘堆积与季风变迁[J].第四纪研究,1991,(4):354-360. [10]刘东生,安芷生,郑洪波.黄土与环境[M].北京:科学出版社,1985:106-112.[11]熊尚发,丁仲礼,刘东生.赣北红土与北京邻区黄土及砂漠砂粒度特征对比[J].科学通报,1999,44(11):1216-1219.[12]Hao Q Z,Guo Z T,Qiao Y S,et al.Geochemical evidence for the provenance of middle Pleistocene loess deposits in southern China[J].Quaternary Science Review,2010,29:3317-3326.[13]Folk R L,Ward W C. Brazos river bar:a study of the significance of grain size parameters[J].Journal of Sedimentary Petrology,1957,27:3-27.[14]戴东林,陈庸勋.沉积岩(物)粒度分析及其应用[M].北京:地质出版社,1976:55-117.[15]柯于义,尹华刚,郭峰,等.三峡库区“巫山黄土”成因研究[J].人民长江,2007,38(9):72-76.[16]李长安,张玉芬,袁胜元,等.“巫山黄土”粒度特征及其对成因的指示[J].地球科学——中国地质大学学报,2010,35(5):879-884.[17]张平,宋春晖,杨用彪,等.稳定湖湘沉积物和风成黄土粒度判别函数的建立及其意义[J].沉积学报,2008,26(3):501-507.[18]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.[19]鹿化煜,安芷生.洛川黄土粒度组成的古气候意义[J].科学通报,1997,42(1):66-69.[20]王均平,潘保田,高红山,等.豫西黄土中砂砾含量及其环境意义[J].中国沙漠,2005,25(5):629-634.[21]肖舜,周爱峰,黄小忠,等.柴达木盆地表土与大气降尘粒度Weibull组成及其环境意义[J].中国沙漠,2012,32(5):1193-1200.[22]雷祥义.秦岭黄土的粒度分析及其成因探讨[J].地质学报,1998,72(2):178-188.[23]李徐生,韩志勇,杨达源,等.镇江下蜀黄土的REE地球化学特征研究[J].土壤学报,2006,43(1):1-7.[24]李徐生,韩志勇,杨守业,等.镇江下蜀土剖面的化学风化强度与元素迁移特征[J].地理学报,2007,62(11):1174-1184.[25]李徐生,杨达源,鹿化煜.镇江下蜀黄土粒度特征及其成因初探[J].海洋地质与第四纪地质,2001,21(1):25-32.[26]Liu J,Wu X H,Li S O,et al.The last glacial stratigraphic sequence,depositional environment and climatic fluctuations from the aeolian sand dune in Hongguang,Pengze,Jiangxi(China)[J].Quaternary Science Reviews,16(6):535-546.[27]Lai Z P,Zhang W G,Chen X,et al.OSL chronology of loess deposits in East China and its implications for East Asian monsoon history[J].Quaternary Geochronology,5(2/3):154-158.[28]Chappell J,Omura A,Esat T,et al.Reconciliation of Late Quaternary sea levels derived from coral terraces at Huon Peninsula with deep sea oxygen isotope records[J].Earth and Planetary Science Letters,1986,141(14):227-236.[29]Dansgaard,W,Johnsen S J,Clausen H B,et al.Evidence for general instability of past climate from a 250-kyr ice-core record[J].Nature,364:218-220. |