Financial support was provided by the National Science Foundation of China grant (40472088).
LIU Dongyan
1 College of Marine Geoscience, Ocean University of China, Qingdao 266100, China； 2 Key Laboratory of Submarine Science and Prospecting Techniques, Ministry of Education, Qingdao 266100, China； 3 Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China； 4 College of Physical and Environmental Oceanography, Ocean University of China, Qingdao 266100, China；5 Department of?Meteorology, University of Hawaii at Manoa, Honolulu 96822, USAQIAO Yansong
1 College of Marine Geoscience, Ocean University of China, Qingdao 266100, China； 2 Key Laboratory of Submarine Science and Prospecting Techniques, Ministry of Education, Qingdao 266100, China； 3 Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China； 4 College of Physical and Environmental Oceanography, Ocean University of China, Qingdao 266100, China；5 Department of?Meteorology, University of Hawaii at Manoa, Honolulu 96822, USALI Weiran
1 College of Marine Geoscience, Ocean University of China, Qingdao 266100, China； 2 Key Laboratory of Submarine Science and Prospecting Techniques, Ministry of Education, Qingdao 266100, China； 3 Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China； 4 College of Physical and Environmental Oceanography, Ocean University of China, Qingdao 266100, China；5 Department of?Meteorology, University of Hawaii at Manoa, Honolulu 96822, USAXIE Ruihuang
1 College of Marine Geoscience, Ocean University of China, Qingdao 266100, China； 2 Key Laboratory of Submarine Science and Prospecting Techniques, Ministry of Education, Qingdao 266100, China； 3 Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China； 4 College of Physical and Environmental Oceanography, Ocean University of China, Qingdao 266100, China；5 Department of?Meteorology, University of Hawaii at Manoa, Honolulu 96822, USAPENG Shasha
1 College of Marine Geoscience, Ocean University of China, Qingdao 266100, China； 2 Key Laboratory of Submarine Science and Prospecting Techniques, Ministry of Education, Qingdao 266100, China； 3 Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China； 4 College of Physical and Environmental Oceanography, Ocean University of China, Qingdao 266100, China；5 Department of?Meteorology, University of Hawaii at Manoa, Honolulu 96822, USAFinancial support was provided by the National Science Foundation of China grant (40472088).
LIU Dongyan, QIAO Yansong, LI Weiran, XIE Ruihuang, PENG Shasha.2011. Chronological Link Between the Abrupt Change of the Loess Grain Size Sequence and the Formation of River Terraces on the Eastern Margin of the Qinghai-Tibetan Plateau Since the Late Early-Pleistocene[J]. ACTA GEOLOGICA SINICA(English edition),85(3):723~732
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