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《Geological Review》 1997-05
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Lei Xiangyi and Yue Leping(Department of Geology,Northwest University,Xian,Shaanxi)  
In Nanyuan of Jingyang (34°28'N and 108°53'E)and Xiwang of Xi'an (34°17'N and 109° 04'E), Guanzhong, Shaanxi Province, the Late Pleistocene loess-paleosol sequence is best preserved and typical in the Loess Plateau of China at present. In the loess sections, S0 is the top layer 1.1-1. 5 m thick. L1 , 6. 5-7. 9 m thick, consists of 3 loess beds and 2 paleosol beds intercalated in between. L1 and S1 have gradational relationship. S1, 3. 1-4. 5 m thick is composed of 4 paleosol beds and 3 loess beds arranged alternately. Studies of stratigraphical structure, magnetic susceptibility and geochemical characteristics of the above-mentioned sections show that there were twelve stages of warm-humid and cold-arid climatic changes which belong to six climatic cycles during the Late Pleistocene in the Loess Plateau of China. It is a shorter time-scale pattern of climatic changes during the Late Pleistocene (130-10 ka B P) in the Loess plateau of China at present. It does not correspond with the deep-sea oxygen isotopic stages.
【Fund】: 国家自然科学基金资助项目部分研究成果(编号49472132)
【CateGory Index】: P531
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