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《Acta Sedimentologica Sinica》 2009-01
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Response of Magnetic Fabric of Xichagou Section in Late Tertiary to Climate Change,Western Qaidam Basin

GAO Jun-ping1 LI Ai-yin1 SONG Chun-hui1 PENG Yang-hong1 ZHANG Wei-lin2 LI Sheng-xi1(1.Key Laboratory of Western China’s Environmental Systems (Ministry of Education) & School of Resources and Environmental Sciences, Lanzhou University, Lanzhou 730000;2.Institute of Tibetan Plateau Research, Chinese Academy of Science, Beijing 100085)  
Through equidistantly sampling on 2~3 meters and accurate systematic measurement of samples of Xichagou stratotype section, located in southwesern limb of Ganchaigou anticline in western Qaidam Basin(Chaixi area) ,integrated high resolution and high precision magnetostratigraphy and sedimentological study in this section, authors think the changing trends of magnetic fabric parameters of sedimentary rocks may act as proxies of climate change.It was indicated that environmental change between 22.4 to 6.2 Ma may divide into three stages: first stage: humid context between ~22.4 to 13.4 Ma; secondary stage: warm-arid environment transformed arid-cold one from 13.4 to 8.2 Ma, and third stage from 8.2 to 6.2 Ma, climate lasted dry-cold, and more complexly. It can be considered that rhythm of climate change or tectonism correlated to formation of modern monsoon since 7.8 Ma. This result provides available evidence for the uplift process of Tibetan Plateau and its environmental effectes.
【Fund】: 国家重点基础研究发展规划(973项目)(批准号:2005CB42001);; 国家自然科学基金委青年科学家群体研究项目(批准号:40421101);; 教育部重大项目(批准号:306016)资助
【CateGory Index】: P618.13
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