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《Journal of Glaciology and Geocryology》 2008-02
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A Preliminary Study of the Rare Earth Elements in Surface Soil on the Tibetan Plateau

ZHANG Cheng-long1,2,WU Guang-jian1,GAO Shao-peng1(1.Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing 100085,China;2.Graduate University of Chinese Academy of Sciences,Beijing 100049,China)  
Mountain processes(including glacial grinding,hill-slope erosion,and fluvial deposition) on the Tibetan Plateau produced amounts of sand-and silt-like materials that was thought to be the main source for Asian dust.In this paper,the preliminary study results are presented on the rare earth elements(REE) from surface sand soils sampled on the Tibetan Plateau and adjacent regions and their patterns are compared with the loess and upper continental crustal(UCC).REE content,which is mainly caused by its parent rock and partly by weathering,varies largely in different sites,with the highest value in southern Tibetan Plateau where it is warm and humid.Chondrite-normalized REE distribution pattern,enrichment in LREE,and negative Eu anomaly closely resemble to those in loess regions and UCC showing that the Tibetan Plateau is a potential source area for Chinese loess deposition.
【Fund】: 国家自然科学基金项目(4057103840121101);; 国家重点基础研究发展计划(973计划)项目2005CB422004)资助
【CateGory Index】: P595
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