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  • ISSN 1000-694X
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Surface Texture of Quartz Grains from Dune Sediments of Northern Qarhan Salt Lake of China

  • Chen Guoxiang ,
  • Dong Zhibao ,
  • Li Chao ,
  • Xiao Weiqiang ,
  • Yang Junhuai ,
  • Shi Weikang ,
  • Zhang Yuemin
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  • School of Geography and Tourism/National Experimental Teaching Demonstration Center of Geography Science, Shaanxi Normal University, Xi'an 710062, China

Received date: 2018-01-27

  Revised date: 2018-03-12

  Online published: 2018-11-03

Abstract

Surface texture characteristic of quartz grains from linear dunes and barchan dunes in northern Qarhan Salt Lake of Qaidam Basin was compared and analyzed by scanning electron microscopy (SEM). The results show that the quartz grains from linear dunes and barchan dunes in northern Qarhan Salt Lake of Qaidam Basin are mainly sub-angular shape, and massively developed dish-shaped impact scars, crescent-shaped impact scars, which suggests typical features of aeolian environment. The sediments in northern Qarhan Salt Lake are dominated by physical decomposition and mechanical action while the chemical weathering plays a small role, which reflects the arid and hot sedimentary environment at that time. The existence of conchoidal breakages, parallel striations and V-shaped pits indicate that the sediments in the Qaidam Basin have been subjected to glaciation or flowing water. It can be inferred that the erosion products from the mountains around the Qaidam Basin or sediments from Qarhan Salt Lake may be one of the sources of dune sediments in northern Qarhan Salt Lake.

Cite this article

Chen Guoxiang , Dong Zhibao , Li Chao , Xiao Weiqiang , Yang Junhuai , Shi Weikang , Zhang Yuemin . Surface Texture of Quartz Grains from Dune Sediments of Northern Qarhan Salt Lake of China[J]. Journal of Desert Research, 2018 , 38(5) : 954 -962 . DOI: 10.7522/j.issn.1000-694X.2018.00018

References

[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.
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