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《Marine Geology & Quaternary Geology》 2007-04
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ROCK MAGNETIC RECORD OF CENOZOIC LAKE SEDIMENTS FROM THE LINXIA BASIN AND THE ARIDIFICATION OF ASIAN INLAND

XU Xian-hai1,FANG Xiao-min2,3(1 Anqing Teachers College,Anhui Anqing 246011,China;2 Institute of Tibetan Plateau Research,CAS,Beijing 100085,China;3 MOE Key Laboratory of West China's Environmental Systems,Lanzhou Universtiy,Lanzhou 730000,China)  
By means of high resolution research of rock magnetic records and quartz sands from Maogou section in the Linxia basin,we reveal that after a relative stable environment between 13.07 and 8.6 Ma,the basin was gradually influxed by eolian dusts at about 8.6 Ma,and the fluxes of eolian dusts got two rapid increases at about 6.4 Ma and 5.3 Ma respectively.The study suggests that the drying of northwest China began at 8.6 Ma and was strengthened rapidly at about 6.4 Ma and 5.3 Ma.
【Fund】: 国家自然科学基金重点基础项目(40334038);; 国家重点基础研究发展规划项目(2005CB42200)
【CateGory Index】: P532
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