[1]Chen Jiansheng,Li Ling,Jiyang Wang, et al.Groundwater maintains dune landscape[J].Nature,2004,432:459. [2]吴正 等著.风沙地貌与治沙工程学[M].北京:科学出版社,2003.142,240-241. [3]Cooke R,Warren A,Goudie A.Desert Geomorphology[M].UCL Press,1993.368. [4]Lancaster N,Greeley R.Sediment volume in the north polar sand seas of Mars[J].Journal of Geophysical Research,1990,95:921-927. [5]朱震达.中国沙漠、沙漠化、荒漠化及其治理的对策[M].北京:中国环境科学出版社,1999.132. [6]Lancaster N.Dune morphology and dynamics[A].In: Athol A D,Parsons A J (eds). Geomorphology of Desert Environments[C].Hapman & HallL,1994.480. [7]Breed C S,Fryberger S C,Andrews S,et al.Regional studies of sand seas using LANDSAT(ERTS) imagery[A].Mckee E D (ed).A Study of Global Sand Seas[C].USGS Professional Ppaper 1052,1979.305-397. [8]Mainguet M,Chemin M C.Wind system and sand dunes in the Taklamakan Desert[J].Chinese Journal of Arid Land research,1988,1:135-42. [9]刘贤万.实验风沙物理与风沙工程学[M].北京:科学出版社,1995.210. [10]凌裕泉,吴正,刘绍中,等. 新月形沙丘形态的模拟实验研究[J]. 地理科学,1998,18(1):88-93. [11]朱震达,吴正,刘恕,邸醒民,等.中国沙漠概论(修订版)[M].北京:科学出版社,1980.73-76. [12]Ross G M.Bigbear erg:a Proterozoic inter-montane sand sea in the Hornby Bay Group,Northwest Territories,Canada[A].Brookfield M E, Ahlbrandt T A (eds).Eolian Sediments and Processes[C].Amsterdam:Elsevier,1983.483-519. [13]费道洛维奇(方城译).奥布鲁切夫开始考察以来沙漠学的成就[A]. 见:亚洲地貌学与古地理学问题[C].北京:科学出版社,1959.97-130. [14]Schwmmle V,Herrmann H J.Solitary wave behaviour of sand dunes[J].Nature,2003,426:619. [15]张伟民,李孝泽,屈建军,等.金字塔沙丘地表气流场及其动力学过程研究[J].中国沙漠,1998,18(3):215-220. [16]哈斯,董光荣,王贵勇.腾格里沙漠东南缘格状沙丘的形态动力学研究[J]. 中国科学(D),1999,29(5):466-471. [17]McKee E D.A Study of Global Sand Seas[M]. Washington:United States Government Printing Office,1979. [18]Brookfield M.The origin of bounding surfaces in ancient aeolian sandstones[J].Sedimentology,1977,24:303-332. [19]Stockes S L.Multiple parallel-truncation bedding planes-a feature of wind deposited sandstone formations[J].J.Sed.Petrol.,1968,38:510-515. [20]Glennie K W. Desert Sedimentary Environments:Developments in Sedimentology 14[M].Amsterdam:Elsevier,1970. [21]Warren A,Allison D.The palaeoenvironmental significance of dune size hierarchies[J].Palaeog.,Palaeoc.,Ppalaeoe.,1998,137:289-303. [22]李孝泽. 普若岗日冰原西侧冰前风沙地貌地形成于我国冰川型沙漠的发现[J].中国沙漠,2003,23(6):703-708. [23]钟德才.中国现代沙漠动态演变图(1∶400万)[Z].中国地图出版社, 2003. [24]陆锦华,郭迎胜.《巴丹吉林高大沙山典型区景观图》的编制研究[J].中国沙漠,1995,15(4):385-391. [25]屈建军,常学礼,董光荣,等.巴丹吉林沙漠高大沙山典型区风沙地貌的分形特性[J].中国沙漠,2003,23(4):361-365. [26]杨萍,巴丹吉林沙漠北部风沙地貌形态类型的分区研究[J].中国沙漠, 1999,19(3): 210-213. [27]Hrner N G.Geomorphic processes in continental basins of central Asia[A].Internat.Geol.Cong.,16th[C]. Washington D C,1933.Rept.,V.2:721-735. [28]于守忠,等.内蒙古西部戈壁及巴丹吉林沙漠考察[A].见:治沙研究(第三号)[C].北京:科学出版社,1962.96-108. [29]Petrov M P.Geographica exploration in the deserts of central Asia[R].U.S.Joint Publications Research Service JPRS 9221,1961.31.(Technical translation from Russian). [30]谭见安.内蒙古阿拉善荒漠的类型[A]. 见: 地理集刊(第八号)[C].北京:科学出版社,1964.1-31. [31]孙培善,孙德钦.内蒙古高原西部水文地质初步研究[A].见:治沙研究(第六号)[C].北京:科学出版社,1964.245-317. [32]王涛.巴丹吉林沙漠形成演变的若干问题[J]. 中国沙漠,1990,10(1):29-40. [33]高全洲,董光荣,李保生,等.晚更新世以来巴丹吉林南缘地区沙漠演化[J].中国沙漠,1995,15(4):345-352 . [34]闫满存, 王光谦, 李保生, 等.巴丹吉林沙漠高大沙山的形成发育研究[J]. 地理学报,2001, 56(1): 83-91. [35]Yang X.Late Quaternary evolution and paleoclimates, Western Alashan Plateau,Inner Mongolia,China[J].Z.Geomorph.N.F.,2001,45:1-16. [36]德日进.中国之大陆沉积[J].中国地质学会志(丁文江先生纪念册),1937,16:195-220. [37]周廷儒.新生代古地理[A].见:《中国自然地理》编辑委员会.中国自然地理古地理(上册)[C].北京:科学出版社,1984.1-233. [38]李吉均,方小敏.新生代晚期青藏高原强烈隆起及其对周边环境的影响[J].第四纪研究,2001,21(5):381-391. [39]董光荣,高全洲,邹学勇,等.晚更新世以来巴丹吉林沙漠南缘气候变化[J].科学通报,1995,40:1214-1218. [40]张川波,何元良.辽宁北票附近中侏罗世晚期的沙漠沉积[J].沉积学报,1983,1(4):48-58. [41]郭正堂,彭淑贞,郝青振,等.晚第三纪中国西北干旱化的发展及其对北极冰盖形成演化和青藏高原隆升的关系[J].中国第四纪研究,1999,(6):556-567. [42]Dong Zhibao, Wang Tao, Wang Xunming. Geomorphology of the megadunes in the Badain Jaran Desert[J].Geomorphology,2004,60:191-203. [43]Lancaster N. Dune morphology, chronology, and Quaternary climatic change[A]. In: Alsharhan A S, Glennie K W, Whittle G L, et al. Quaternary Deserts and Climatic Change[C]. A.A.Balkema/Rotterdam/Brookfield/1998. 339-350. [44]Ma Jinzhu, Li Ding, Zhang Jiawu, et al. Ground water recharge and climatic change during the last 1000 years from unsaturated zone of SE Badain Jaran Desert[J].Chinese Science Bulletin, 2003, 48(14): 1469-1474. [45]张虎才,马玉贞,彭金兰,等.距今42~18 ka腾格里沙漠古湖泊及古环境[J].科学通报,2002,47(24):1847-1857. [46]董光荣,王贵勇,李孝泽,等.末次间冰期以来我国东部沙区的古季风变迁[J].中国科学(D辑),1996,26(5):437-444. [47]杨小平.巴丹吉林沙漠及其毗邻地区的景观类型及其形成机制初探[J].中国沙漠,2000,20(2):166-170. [48]楼桐茂.甘肃民勤至巴丹吉林庙间沙漠成因及其改造利用[A].见:治沙研究(第三号)[C].北京:科学出版社,1962.90-95. [49]张伟民, 王涛. 巴丹吉林沙漠高大沙山形成演化初步探讨[J].中国沙漠,2005,25(2):281-286. [50]闫满存,王光谦,李保生,等.巴丹吉林沙漠更新世古风向变化与环意义[J]. 清华大学学报,2001,(11):118-122. [51]李云卓,李保生,高全洲,等.巴丹吉林查格勒布剖面记录的150 ka BP以来的常量化学元素波动[J].中国沙漠,2005,25(1):8-14. [52]吕玉晓,李保生,靳鹤龄,等.萨拉乌苏河流域末次间冰期全球变化区域响应的主元素记录[J].中国沙漠,2004,24(2):136-143. [53]张林源,蒋兆理.论我国西北干旱气候的成因[J].干旱区地理,1992,15(2):1-11. [54]Wüunnemann B, Pachur H J, Zang H. Climatic and environmental changes in the deserts of Inner Mongolia, China, since the Late Pleistocene[A]. In: Alsharhan A S, Glennie K W, Whittle G L, et al. (eds). Quternary Deserts and Climatic Change[C]. Rotterdam: A A Balkema, 1998. 381-394. [55]马金珠,李丁,李相虎,等.巴丹吉林沙漠包气带Cl-示踪与气候记录研究[J].中国沙漠,2004,24(6):674-679. |