[1] Hayward R K,Fenton L K,Titus T N.Mars Global Digital Dune Database (MGD3):global dune distribution and wind pattern observations[J].Icarus,2014,230:38-46.
[2] Hesp P,Hyde R,Hesp V,et al.Longitudinal dunes can move sideways[J].Earth Surface Processes and Landforms,1989,14:447-451.
[3] Rubin D M,Hesp P A.Multiple origins of linear dunes on Earth and Titan[J].Nature Geoscience,2009,9(2):653-658.
[4] Zhou J X,Zhu Y,Yuan C Q.Origin and lateral migration of linear dunes in the Qaidam Basin of NW China revealed by dune sediments,internal structures,and optically stimulated luminescence ages,with implications for linear dunes on Titan[J].Geological Society America Bulletin,2012,124(7/8):1147-1154.
[5] Li J Y,Dong Z B,Zhang Z C,et al.Grain-size characteristics of linear dunes on the northern margin of Qarhan Salt Lake,northwestern China[J].Journal of Arid Land,2015,7(4):438-449.
[6] Li J Y,Dong Z B,Qian G Q,et al.Pattern analysis of a linear dune field on the northern margin of Qarhan Salt Lake,northwestern China[J].Journal of Arid Land,2016,8(5):670-680.
[7] Zhang Z C,Dong Z B,Qian G Q,et al.Formation and development of dunes in the northern Qarhan Desert,central Qaidam Basin,China[J].Geological Journal,2017,DOI:10.1002/gj.2947
[8] 鲍锋.柴达木盆地察尔汗盐湖地区风沙地貌发育环境与过程[D].西安:陕西师范大学,2016.
[9] 钟德才.柴达木盆地沙漠形成和演变的初步研究[M]//中国科学院兰州沙漠研究所集刊第3号.北京:科学出版社,1986:124-136.
[10] 辛彦林.柴达木盆地盐湖中的风成砂[J].中国沙漠,1995,15(3):252-255.
[11] 曾永年,冯兆东,曹广超.末次冰期以来柴达木盆地沙漠形成与演化[J].地理学报,2003,58(3):452-457.
[12] 鲍锋,董治宝,张正偲.柴达木盆地风沙地貌区风况特征[J].中国沙漠,2015,35(3):549-554.
[13] 徐贵江,董治宝,王中原.柴达木盆地新月形沙丘和线性沙丘共生现象[J].中国沙漠,2017,37(3):407-413.
[14] 鲍锋,董治宝.青藏铁路察尔汗盐湖段风沙活动特征[J].中国沙漠,2017,37(4):621-625.
[15] 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.
[16] 鲍锋,董治宝.察尔汗盐湖沙漠沙丘沉积物粒度特征分析[J].水土保持通报,2014,34(6):355-359.
[17] 鲍锋,董治宝.柴达木盆地沙漠地表沉积物矿物构成特征[J].西北大学学报:自然科学版,2015,45(1):90-96.
[18] 李超,董治宝,陈国祥,等.柴达木盆地察尔汗盐湖北侧沙丘黏性沉积物特征[J].中国沙漠,2018,38(1):68-75.
[19] 陈丽华,缪昕,魏宝和.扫描电镜在石油地质上的应用[M].北京:石油工业出版社,1990.
[20] 戴枫年.石英砂粒表面微结构特征的研究[J].中国沙漠,1986,6(3):20-23.
[21] Krinsley D H,Doornkamp J C.Atlas of quartz sand surface textures[M].New York,USA:Cambridge University Press,1973:5-102.
[22] 谢又予,崔之久,李洪云,等.中国石英砂表面结构特征图谱[M].北京:海洋出版社,1984.
[23] 孙有斌,安芷生.风尘堆积物中石英颗粒表面结构特征及其沉积学指示[J].沉积学报,2000,18(4):506-510.
[24] Krinsley D,Trusty P.Environmental Interpretation of quartz grain surface textures[M]//Zuffa G G.Provenance of Arenites.Dordrecht,Netherlands:Springer,1985.
[25] 谢又予,崔之久,李洪云.扫描电镜下石英砂的表面结构特征机器地址解译[J].石油与天然气地质,1981(1):66-74.
[26] 江新胜,徐金沙,潘忠习.鄂尔多斯盆地白垩纪沙漠石英沙颗粒表面特征[J].沉积学报,2003,21(3):416-422.
[27] 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.
[28] 吴正等.风沙地貌与治沙工程学[M].北京:科学出版社,2003.
[29] 王颖,迪纳瑞尔B.石英砂表面结构模式图集[M].北京:科学出版社,1985.
[30] 戴枫年.我国北方沙漠地区沙丘石英砂的表面特征与沉积环境的关系[J].干旱区资源与环境,1988,2(2):25-35.
[31] 李珍,张家武,马海洲.西宁黄土石英颗粒表面结构与黄土物质来源探讨[J].沉积学报,1999,17(2):221-225.
[32] 克林斯雷D H,杜尔坎普J C.石英颗粒表面结构图册[M].陈瑞君,译.北京:石油工业出版社,1980.
[33] 潘仁义,李川川,张梅,等.天山冰川与塔克拉玛干风沙沉积的颗粒特征和分异过程分析[J].北京大学学报:自然科学版,2012,48(5):744-756.
[34] Newsome D,Ladd P.The use of quartz grain microtextures in the study of the origin of sand terrains in Western Australia[J].Catena,1999,35(1):1-17.
[35] Mahaney W C,Dirszowsky R W,Milner M W,et al.Quartz microtextures and microstructures owing to deformation of glaciolacustrine sediments in the northern Venezuelan Andes[J].Journal of Quaternary Science,2004,19(1):23-33.
[36] Cardona J P M,Gutiecrrez Mas J M,Bellocn A S,et al.Surface textures of heavy-mineral grains:a new contribution to provenance studies[J].Sedimentary Geology,2005,174:223-235.
[37] Strand K,Psaachier S,Nasi J.Implications of quartz grain microtextures for onset Eocene/Oligocene glaciation in Prydz Bay,ODP Site 1166,Autarctica[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2003,198:101-111.
[38] 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.
[39] 李志忠,罗若愚,周勇,等.中国干旱区沙漠沉积与大陆架残留沉积特征比较研究[J].干旱区地理,1999,22(2):8-13.
[40] 陈国祥,董治宝,崔徐甲,等.毛乌素沙地中部风成沙的组成与微形态特征[J].中国沙漠,2018,38(3):1-11.