| [1]吴正.风沙地貌与治沙工程学[M].北京:科学出版社,2003:196-201.[2]Livingstone I,Warren A.Aeolian Geomorphology:An Introduction[M].London:Longman,1996.[3]钱征宇,刘守勤.线形沙丘的风沙沉积特征与内部构造[J].中国沙漠,1994,14(3):25-30.[4]钱亦兵,周兴佳,吴兆宁.准噶尔盆地沙物质粒度特征研究[J].干旱区研究,2000,17(2):34-41.[5]何清,杨兴华,霍文,等.库姆塔格沙漠粒度分布特征及环境意义[J].中国沙漠,2009,29(1):18-22.[6]钱广强,董治宝,罗万银,等.回涡沙丘的形态特征与表面物质组成[J].中国沙漠,2012,32(3):587-592.[7]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,2009,32(5):655-661.[8]Pye K.Negatively skewed aeolian sands from a humid tropical coastal dunefield,northern Australia[J].Sedimentary Geology,1982,31(3/4):249-266.[9]Lancaster K.Grain-size characteristics of linear dunes in the Southwestern Kalahali [J].Journal of Sedimentary Petrology,1986,56(3):395-405.[10]胡梦君,李森,高尚玉,等.风沉积物粒度特征及其反映的青海湖周边近32 ka以来土地沙漠化演变过程[J].中国沙漠,2012,32(5):1240-1247.[11]李继彦,董治宝,李恩菊,等.察尔汗盐湖雅丹地貌沉积物粒度特征研究[J].中国沙漠,2012,32(5):1187-1192.[12]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):1-4.[13]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):1-5.[14]杨东亮,王雪芹,胡永锋.风沙流输沙通量垂直分布研究——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.[15]唐进年,王继和,苏志珠,等.库姆塔格沙漠羽毛状沙丘表面沙粒度分布特征[J].干旱区地理,2008,31(6):918-925.[16]Lancaster N.Grain size characteristics of Namib desert linear dunes[J].Sedimentology,1981,28(1):115-122.[17]Vincent P J.Particle size variation over a transverse dune in the Nafud as Sirr,central Naudi Arabia[J].Journal of Arid Environments,1983,7:329-36.[18]Livingstone I.Grain-size variation on a “complex” linear dune in the Namib Desert[C]//Frostick L,Reid I.Desert Sediments,Ancient and Modern.Blackwell Oxford:Geological Society,1987,35 (1):281-291.[19]Folk R L,Ward W C.Brazos river bar:a study in the significance of grain size parameters[J].Journal of Sedimentary Petrology,1957,27(1):3-26.[20]陈渭南.塔克拉玛干沙漠84°E沿线沙物质的粒度特征[J].地理学报,1993,48(1):33-46.[21]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,1992,6(2):101-109.[22]张瑞军,何清,孔丹,等.塔克拉玛干沙漠北缘沙尘暴源区地表沉积物粒度特征[J].干旱区研究,2008,25(6):887-893.[23]钱亦兵,张希明,李小明,等.塔克拉玛干沙漠南缘绿洲沙物质粒度特征[J].中国沙漠,1995,15(2):131-136.[24]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,1996,13(2):37-43.[25]李振山,陈广庭,冯起,等.塔克拉玛干沙漠腹地纵向沙垅表面沙物质粒度特征[J].干旱区资源与环境,1998,12(1):21-28.[26]吉启慧.粒度分析在塔克拉玛干沙漠研究中的应用[J].中国沙漠,1996,16(2):173-179.[27]李恩菊,董治宝,赵景波.巴丹吉林沙漠典型高大沙山迎风坡粒度特征[J].干旱区地理,2011,34(3):471-478.[28]Lancaster N.Geomorphology of Desert Dunes[M].London:Routaledge,1995:526.[29]哈斯,王贵勇.沙坡头地区新月形沙丘粒度特征[J].中国沙漠,2001,21(3):271-275.[30]Barndorff-Nielsen O,Dalsgaard K,Halgreen C,et al.Variation in particle size distribution over a small dune[J].Sedimentology,1982,29(1):53-65.[31]Ahlbrandt T S.Comparison of textures and structures to distinguish eolian environment, Killpecker dunefield Wyoming[J].The Mountain Geologist,1975,12:58-61. |
2013, Vol. 33 
