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Processes of the deposition and vicissitude of Mu Us Desert, China since 150 ka B.P.
Authors:Li Baosheng  Jin Heling  Lü Haiyan  Zhu Yizhi  Dong Guangrong  Sun Donghuai  Zhang Jiashen  Gao Quanzhou  Yan Mancun
Affiliation:(1) Geography Department of South China Normal University, 510631 Guangzhou, China;(2) Lanzhou Institute of Desert Research, Chinese Academy of Sciences, 730000 Lanzhou, China;(3) Graduate School, China University of Geosciences, 430074 Wuhan, China;(4) Xi'an Laboratory of Loess & Quaternary Geology, Chinese Academy of Sciences, 710061 Xi'an, China;(5) Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, 510650 Guangzhou, China
Abstract:“Milanggouwan stratigraphical section” named lately takes down 27 cycles of alternately evolutionary histories of desert depositions in the Mu Us area with the fluviolacustrine facies and palaeosols since 150 ka B. P. Studies show that the sedimentary form was induced by the growth and decline and confrontation each other between the winter monsoon and the summer monsoon of East Asia in the past 150 ka. Project supported by the National Natural Science Foundation of China (Grant No. 49473192).
Keywords:Mu Us Desert  Milanggouwan stratigraphical section  150 ka  27 periods of desert depositions
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