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《Chinese Geology》 2002-03
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Grain-size distribution and material source analysis of loess on the nort heastern margin of the Qinghai-Tibet Plateau

XIE Yuan-yun 1,2 ,ZHANG Xu-qiang 2 ,HE Kui 2 ,LI Chang-'an 1 ;(1.Institute of Eorth Science,China University of Geoscicnces Wuhan4 30074,Hubei,China2.Geography department ,Harbin Normal University,Har bin150080,Heilongjiang,China)  
Grain-size analysis of the Minhe loess on the northern margin of the Qinghai-Tibet Plateau in-dicates that the grain-size distribution of t he Minhe loess is obviously different from that in other areas such as Lanzhou and Luochuan and Xi'an.Its grain size is notably much higher.It seems too sim ple to as-sign the Minhe loess to the southern part of the loess belt traditio nally because of ignorance of the effect of the plateau source area induced b y the uplift of the Qinghai-Tibet Plateau.It is advisable to assign the Minhe loess to a transition zone between loess and sandy loess.The sandy dust produc ed as a result of re-peated glacial ablation and abrasion of the plateau has supplied a substantial amount of coarse material for the Minhe loess.The vol uminous dust produced by the Quaternary glaciation and melting of glaciers on the Qinghai-Tibet Plateau is not only the principal material source for the l oess area in the interior of the plateau but alsoone of the principal materi al sources for the loess on the margins of the plateau.
【Fund】: 国家自然科学基金(49972057);; 国土资源部甘肃兰州红古城、新寺乡1∶5万区调成果
【CateGory Index】: P531
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