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《地球科学学刊(英文版)》 2012-02
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Environmental Changes Recorded by Major Elements in Loulan Stupa Section during Early-Middle Holocene

Hongjuan Jia* Experiment & Practice Teaching Center, Shijiazhuang University of Economics, Shijiazhuang 050031, China; Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China Xiaoguang Qin , Jiaqi Liu Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China  
Holocene palaeoweathering conditions and environmental changes of Loulan (楼兰) Stupa Sec-tion were reconstructed by major elements analysis results and optical stimulated luminescence dating results. Major element results show source rock change little, with the composition equivalent to granodiorite. The low R value and high CIA (chemical index of alteration) value indicating the section at primary weathering phases. The muddy silt and silty clay have low R value and high CIA value and total iron content. In contrast, the sandy clay silt and sandy silt have high R value and low CIA and total iron value. Deglaciation time climate was relatively humid. In comparison to previous and posterior hiatus, the Middle-Holocene climate was relatively wet but still displayed high-frequency and high-amplitude fluctuations.
【Fund】: supported by the Key Consultation Project (No. 2008-ZD-05)of Chinese Academy of Engineering;; the National Natural Science Foundation of China (Nos. 40472094 40772212);; National Project (No. NP2010-033)
【CateGory Index】: P595
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