察尔汗盐湖线形沙丘沙物质来源及输移路径

[11] 青藏高原风沙地貌图集[M]. 西安地图出版社 , 董治宝, 2016

[12] 治沙研究[M]. 科学出版社 , 中国科学院治沙队编, 1962

[13] High-Altitude Aeolian Research on the Tibetan Plateau [J]. REVIEWS OF GEOPHYSICS, 2017, 55 (04) : 864 - 901

[14] A new terrestrial analogue site for Mars research: The Qaidam Basin, Tibetan Plateau (NW China)[J] . Long Xiao,Jiang Wang,Yanan Dang,Ziye Cheng,Ting Huang,Jiannan Zhao,Yi Xu,Jun Huang,Zhiyong Xiao,Goro Komatsu.Earth-Science Reviews . 2017

[15] 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: Comme[J] . Lupeng Yu,Zhibao Dong,Zhongping Lai,Guangqiang Qian,Tong Pan.Geological Society of America Bulletin . 2015 (1-2)

[16] 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: Discussion[J] . D.M. Rubin,A.M. Rubin.Geological Society of America Bulletin . 2013 (11-1)

[17] 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] . Jianxun Zhou,Ying Zhu,Chongqian Yuan.Geological Society of America Bulletin . 2012 (7-8)

[18] Multiple origins of linear dunes on Earth and Titan[J] . David M. Rubin,Patrick A. Hesp.Nature Geoscience . 2009 (9)

[19] Quantitative provenance analysis of sediments: review and outlook[J] . Gert Jan Weltje,Hilmar von Eynatten.Sedimentary Geology . 2004 (1)

[20] LONGITUDINAL DUNES CAN MOVE SIDEWAYS [J]. EARTH SURFACE PROCESSES AND LANDFORMS, 1989, 14 (05) : 447 - 451

[11] 青藏高原风沙地貌图集[M]. 西安地图出版社 , 董治宝, 2016

[12] 治沙研究[M]. 科学出版社 , 中国科学院治沙队编, 1962

[13] High-Altitude Aeolian Research on the Tibetan Plateau [J]. REVIEWS OF GEOPHYSICS, 2017, 55 (04) : 864 - 901

[14] A new terrestrial analogue site for Mars research: The Qaidam Basin, Tibetan Plateau (NW China)[J] . Long Xiao,Jiang Wang,Yanan Dang,Ziye Cheng,Ting Huang,Jiannan Zhao,Yi Xu,Jun Huang,Zhiyong Xiao,Goro Komatsu.Earth-Science Reviews . 2017

[15] 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: Comme[J] . Lupeng Yu,Zhibao Dong,Zhongping Lai,Guangqiang Qian,Tong Pan.Geological Society of America Bulletin . 2015 (1-2)

[16] 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: Discussion[J] . D.M. Rubin,A.M. Rubin.Geological Society of America Bulletin . 2013 (11-1)

[17] 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] . Jianxun Zhou,Ying Zhu,Chongqian Yuan.Geological Society of America Bulletin . 2012 (7-8)

[18] Multiple origins of linear dunes on Earth and Titan[J] . David M. Rubin,Patrick A. Hesp.Nature Geoscience . 2009 (9)

[19] Quantitative provenance analysis of sediments: review and outlook[J] . Gert Jan Weltje,Hilmar von Eynatten.Sedimentary Geology . 2004 (1)

[20] LONGITUDINAL DUNES CAN MOVE SIDEWAYS [J]. EARTH SURFACE PROCESSES AND LANDFORMS, 1989, 14 (05) : 447 - 451