[1] Wang N,Li Z,Li Y,et al.Millennial-scale environmental changes in the Asian monsoon margin during the Holocene,implicated by the lake evolution of Huahai Lake in the Hexi Corridor of northwest China[J].Quaternary International,2013,313/314:100-109.
[2] Wang N,Zhang J,Cheng H,et al.The age of formation of the mirabilite and sand wedges in the Hexi Corridor and their paleoclimatic interpretation[J].Chinese Science Bulletin,2003,48(14):1439-1445.
[3] Wang N,Zhao Q,Li J,et al.The sand wedges of the last ice age in the Hexi Corridor,China:paleoclimatic interpretation[J].Geomorphology,2003,51(4):313-320.
[4] Wang N,Li Z,Li Y,et al.Younger Dryas event recorded by the mirabilite deposition in Huahai lake,Hexi Corridor,NW China[J].Quaternary International,2012,250:93-99.
[5] 王乃昂,王涛,高顺尉,等.河西走廊末次冰期芒硝和砂楔与古气候重建[J].地学前缘,2000,7(增刊):59-66.
[6] 王乃昂,王涛,史正涛,等.河西走廊末次冰期砂楔的发现及其古气候意义[J].冰川冻土,2001,23(1):46-50.
[7] 胡刚,王乃昂,高顺尉,等.花海湖泊全新世古风成砂的发现及其古环境解释[J].中国沙漠,2002,22(2):159-165.
[8] 胡刚,王乃昂,罗建育,等.花海湖泊古风成砂的粒度特征及其环境意义[J].沉积学报,2001,19(4):642-647.
[9] 李卓伦,王乃昂,李育,等.河西走廊花海古湖泊早、中全新世湖水盐度变化及其环境意义[J].冰川冻土,2013,35(6):1481-1489.
[10] 李卓伦,陈晴,王乃昂,等.河西走廊花海古湖泊全新世白云石的发现及其环境意义[J].湖泊科学,2013,25(4):558-564.
[11] 李卓伦,张乃梦,王乃昂,等.晚冰期以来河西走廊花海古湖泊演化过程及其对气候变化的响应[J].中国沙漠,2014,34(2):342-348.
[12] 李并成.河西走廊西部汉长城遗迹及其相关问题考[J].敦煌研究,1995(2):135-145.
[13] 李并成.河西走廊历史时期沙漠化研究[M].北京:科学出版社,2003.
[14] 李并成.河西走廊汉唐古绿洲沙漠化的调查研究[J].地理学报,1998,53(2):106-115.
[15] 王乃昂,赵强,胡刚,等.近2 ka河西走廊及毗邻地区沙漠化过程的气候与人文背景[J].中国沙漠,2003,23(1):95-100.
[16] Wang N,Zhang C,Li G,et al.Historical desertification process in Hexi Corridor,China[J].Chinese Geographical Science,2005,15(3):245-253.
[17] 程弘毅.河西地区历史时期沙漠化研究[D].兰州:兰州大学,2007:200-225.
[18] 王涛.中国北方沙漠与沙漠化图集[M].北京:科学出版社,2014.
[19] Yang B,Qin C,Shi F,et al.Tree ring-based annual streamflow reconstruction for the Heihe River in arid northwestern China from AD 575 and its implications for water resource management[J].The Holocene,2011,22(7):773-784.
[20] Chen F,Yuan Y,Wei W,et al.Tree-ring-based annual precipitation reconstruction for the Hexi Corrodor,NW China:consequences for climate history on and beyond the mid-latitude Asian continent[J].Boreas,2013,42(4):1008-1021.
[21] Dong Z,Qin D,Kang S,et al.Physicochemical characteristics and sources of atmospheric dust deposition in snow packs on the glaciers of western Qilian Mountains,China[J].Tellus B,2014,66:20956.
[22] Gou X,Gao L,Deng Y,et al.An 850-year tree-ring-based reconstruction of drought history in the western Qilian Mountains of northwestern China[J].International Journal of Climatology,2015,35(11):3308-3319.
[23] Wu G,Zhang C,Zhang X,et al.The environmental implications for dust in high-alpine snow and ice cores in Asian mountains[J].Global and Planetary Change,2015,124:22-29.
[24] 夏训诚,赵元杰,王富葆,等.罗布泊地区红柳沙包年层的环境意义探讨[J].科学通报,2005,50(19):2176-2177.
[25] 夏训诚,曹琼英,王富葆,等.罗布泊地区红柳沙包年层的研究意义[J].干旱区地理,2005,28(5):565-568.
[26] 程水英.疏勒河流域景观动态变化研究[D].西安:西北大学,2004:12.
[27] 刘惠峰.基于时序NDVI的疏勒河流域植被覆盖分类研究[D].兰州:兰州大学,2014:11.
[28] 陈翔舜,魏金平.花海农场沙产业综合开发及沙漠化防治对策[J].甘肃林业科技,2000,25(4):63-66.
[29] Stuiver M.Extended14C data base and revised CALIB 3.014C age calibration program[J].Radiocarbon,1993,35(1):215-230.
[30] Reimer P J,Baillie M G L,Bard E,et al.IntCal09 and Marine09 radiocarbon age calibration curves,0-50,000 years cal BP[J].Radiocarbon,2009,51(4):1111-1150.
[31] Wang X,Lang L,Hua T,et al.Variations in the wind-energy regime of the Taklimakan Desert,central Asia,over the last 700 years as inferred from nebkha sedimentology and chronology[J].Boreas,2014,43(4):882-894.
[32] 郎丽丽.风沙堆积体发育过程及风沙运动中物质组成的风洞实验研究[R].北京:中国科学院地理科学与资源研究所,2015:24.
[33] Wang X,Lang L,Hua T,et al.Geochemical and magnetic characteristics of aeolian transported materials under different near-surface wind fields:an experimental study[J].Geomorphology,2015,239:106-113.
[34] 李亚林.疏勒河花海灌区地下水开发利用状况分析[J].甘肃水利水电技术,2014,50(6):11-12.
[35] 邓新功.甘肃省"农业学大寨"运动研究(1964-1980)[D].兰州:西北师范大学,2012:69.
[36] Wang X,Xia D,Zhang C,et al.Geochemical and magnetic characteristics of fine-grained surface sediments in potential dust source areas:Implications for tracing the provenance of aeolian deposits and associated palaeoclimatic change in East Asia[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2012,323-325(2):123-132.
[37] Wang X,Wang T,Dong Z,et al.Nebkha development and its significance to wind erosion and land degradation in semi-arid northern China[J].Journal of Arid Environments,2006,65(1):129-141.
[38] Wang X,Xiao H,Li J,et al.Nebkha development and its relationship to environmental change in the Alaxa Plateau,China[J].Environmental Geology,2008,56(2):359-365.
[39] Wang X,Zhang C,Zhang J,et al.Nebkha formation:implications for reconstructing environmental changes over the past several centuries in the Ala Shan Plateau,China[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2010,297(3/4):697-706.
[40] 赵元杰,宋艳,夏训诚,等.近150年来罗布泊红柳沙包沉积纹层沙物质粒度特征[J].干旱区资源与环境,2009,23(12):103-107.
[41] 赵元杰,夏训诚,王富葆,等.罗布泊地区红柳沙包纹层沙粒度特征与环境指示意义[J].干旱区地理,2007,30(6):791-796.
[42] Khalaf F I,Misak R,Al-Dousari A.Sedimentological and morphological characteristics of some nabkha deposits in the northern coastal plain of Kuwait,Arabia[J].Journal of Arid Environments,1995,29(3):267-292.
[43] Langford R P.Nabkha(coppice dune) fields of south-central New Mexico,U.S.A.[J].Journal of Arid Environments,2000,46(1):25-41.
[44] Zou X,Li J,Liu B,et al.The protective effects of nebkhas on oasis[J].Aeolian Research,2016,20:71-79.
[45] 刘铁庚,叶霖,王兴理,等.化学作用是干旱地区岩石风化的主要因素——蒸发和淋漓模拟实验[J].中国地质,2007,322(5):815-821.
[46] Chen J,Li G.Geochemical studies on the source region of Asian dust[J].Science China Earth Sciences,2011,54(9):1279-1301.
[47] Wang Y,Zhang X,Arimoto R,et al.Characteristics of carbonate content and carbon and oxygen isotopic composition of northern China soil and dust aerosol and its application to tracing dust sources[J].Atmospheric Environment,2005,39(14):2631-2642.
[48] Yokoo Y,Nakano T,Nishikawa M,et al.Mineralogical variation of Sr-Nd isotopic and elemental compositions in loess and desert sand from the central Loess Plateau in China as a provenance tracer of wet and dry deposition in the northwestern Pacific[J].Chemical Geology,2004,204(1):45-62.
[49] Rao W,Tan H,Jiang S,et al.Trace element and REE geochemistry of fine-and coarse-grained sands in the Ordos deserts and links with sediments in surrounding areas[J].Chemie der Erde-Geochemistry,2011,71(2):155-170.
[50] 马健,何元庆,冯起,等.黑河下游地区柽柳沙丘的气候与环境记录[J].中国沙漠,2016,36(2):319-326.
[51] 郎丽丽,王训明,花婷,等.蒙古高原东南缘现代灌丛沙丘的发育过程及其对沙漠化的指示意义[J].第四纪研究,2013,33(2):325-333.
[52] Chen J,Chen Y,Liu L,et al.Zr/Rb ratio in the Chinese loess sequences and its implication for changes in the East Asian winter monsoon strength[J].Geochimica et cosmochimica acta,2006,70(6):1471-1482.