[1] 任明达.现代沉积环境概论[M].北京:科学出版社,1981:17-18. [2] Lancaster N.Geomorphology of Desert Dunes[M].New York,USA:Routledge,1995:525-530 [3] 陈渭南,雷加强.塔克拉玛干沙漠新月形沙丘不同部位的粒度特征[J].干旱区资源与环境,1992(2):101-108. [4] 杨东亮,王雪芹,胡永锋,等.风沙流输沙通量垂向分布研究——以塔克拉玛干沙漠南缘流沙地表风沙流观测为例[J].中国沙漠,2012,32(3):631-639. [5] 哈斯,董光荣,王贵勇.腾格里沙漠东南缘沙丘表面气流与坡面形态的关系[J].中国沙漠,1999,19(1):1-5. [6] 哈斯,王贵勇,董光荣.腾格里沙漠东南缘格状沙丘表面气流及其地貌学意义[J].中国沙漠,2000,20(1):30-34. [7] 俞胜清,阿布都米基提,周向玲,等.新疆喀拉库姆沙漠新月形沙丘不同部位粒度特征[J].中国沙漠,2013,33(6):1629-1635. [8] Livingstone I.Temporal trends in grain-size measures on a linear sand dune[J].Sedimentology,1989,36:1017-1022. [9] Mainguet M,Chemin M C.Wind degradation on the sandy soils of the Sahel of Mali and Niger and its part in desertification[M]//Aeolian Grain Transport.1991:113-130. [10] Livingstone I.A twenty-one-year record of surface change on a Namib linear dune[J].Earth Surface Process and Landforms,2003,28:1025-1031. [11] Thomas D S G,O'Connor P W,Bateman M D,et al.Dune activity as a record of late Quaternary aridity in the Northern Kalahari:new evidence from northern Namibia interpreted in the context of regional arid and humid chronologies[J].Palaeogeography Palaeoclimatology Palaeoecology,2000,156(3/4):243-259. [12] Thomas D S G.Arid Zone Geomorphology[M].Chichester,USA:John Wiley & Sons,2011:425-568. [13] Middleton N J,Goudie A S.Saharan dust:sources and trajectories[J].Transactions of the Institute of British Geographers,2002,26(2):165-181. [14] CIA.The CIA World Factbook 2012-Mauritania[EB/OL]. (2014-06-20)[2016-07-10]. [15] Mainguet M,Dumay F,Guang H,et al.Accelerated desertification in the deserts of Mauritania and China in the 20th century[M]//Security and Environment in the Mediterranean.Berlin,Germany:Springer,2003:677-686. [16] Bennoune M.Mauritania:a neocolonial desert[J].Dialectical Anthropology,1978,3(1):43-66. [17] 周娜,雷加强,王永东,等.1973-2010年毛里塔尼亚气候变化与风况特征[J].中国沙漠,2015,35(6):1683-1692. [18] 赵澄林,沉积岩石学[M].北京:石油工业出版社,2001:48-72,253-260. [19] 哈斯,王贵勇.腾格里沙漠东南缘横向沙丘粒度变化及其与坡面形态的关系[J].中国沙漠,1996,16(3):215-220. [20] 庞红丽,程捷,丛殿阁,等.腾格里沙漠北缘沙丘粒度特征及区域差异分析[J].宁夏大学学报:自然科学版,2015,36(3):267-273. [21] Folk R L,Ward W C.Brazos River bar:a study in the significance of grain size parameters[J].Journal Sedimentary Petrology,1957,27(1):3-26. [22] Udden J A.Mechanical composition of clastic sediments[J].Geological Society of America Bulletin,1914,25(1):655-744. [23] Wentworth C K.A scale of grade and class terms for clastic sediments[J].Journal of Geology,1922,30(5):377-392. [24] Sahu B K.Depositional mechanisms from the size analysis of clastic sediments[J].Journal of Sedimentary Research,1964,34(1):2-24. [25] Kocurek G,Havholm K G,Deynoux M,et al.Amalgamated accumulations resulting from climatic and eustatic changes,Akchar Erg,Mauritania[J].Sedimentology,1991,38(4):751-772. [26] 李志忠,关有志,孙忠,等.塔克拉玛干沙漠腹地纵向沙垄的粒度分布特征[J].干旱区研究,1996(2):37-43. [27] Tsoar H.The Dynamics of Longitudinal Dunes[R].U.S.Army European Research Office,1978. [28] 魏怀东,王继和,徐先英,等.库姆塔格沙漠各沙丘类型沙粒粒度分析[J].甘肃科技,2007,23(5):85-88. [29] Steffen Mischke.内蒙古巴丹吉林沙漠成因的粒度分析和热发光测年新证据[J].古地理学报,2005,7(1):79-97. [30] 王雪芹,李丙文,张元明.古尔班通古特沙漠沙垄表面的稳定性与顶部流动带的形成[J].中国沙漠,2003,23(2):126-131. [31] 钱广强,董治宝,罗万银,等.巴丹吉林沙漠地表沉积物粒度特征及区域差异[J].中国沙漠,2011,31(6):1357-1364. [32] 钱亦兵,吴兆宁,杨海峰,等.古尔班通古特沙漠南部风沙土粒度分布的空间异质性[J].干旱区地理,2009(5):655-661. [33] 哈斯.腾格里沙漠东南缘格状沙丘粒度特征与成因探讨[J].地理研究,1998,17(2):178-184. [34] 王训明,董治宝,屈建军,等.塔克拉玛干沙漠简单线形沙丘形态动力学过程研究[J].中国沙漠,2003,23(3):257-262. [35] 庞红丽.腾格里沙漠北缘沙丘分布及粒度特征研究[D].北京:中国地质大学(北京),2012. [36] 魏怀东,徐先英,王继和,等.库姆塔格沙漠沙丘的粒度特征[J].水土保持学报,2007,21(3):6-9. |